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An Obsession with Meaning: A Critical Examination of the Pictograph Sites of the Lake of the Woods Alicia]. M. Colson Department of Anthropology Mc Gill University June 2006 A Thesis submÏtted to McGill University in partial fulfi1ment of the requirements of the degree of Doctor of Philosophy © Alicia J. M. Colson, 2006
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Page 1: An obsession with meaning: a critical examination of the pictograph sites of the Lake of Woods

.~.

An Obsession with Meaning: A Critical Examination of the Pictograph Sites of the Lake of the Woods

Alicia]. M. Colson Department of Anthropology

Mc Gill University

June 2006

A Thesis submÏtted to McGill University in partial fulfi1ment of the requirements of the degree of Doctor of Philosophy

© Alicia J. M. Colson, 2006

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Errata:

Appendix 6 commences on page 551 instead of page 550 as stated in the Table of Contents. Page 550 do es not exist.

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Table of Contents Abstracts .............................................................................................................................................. vi Acknowledgements ........................................................................................................................ vüi Note on spelling .............................................................................................................................. xüi Note on Kl.EIO lAS ...................................................................................................................... xiv List of Figures ................................................................................................................................... xv List of Tables ................................................................................................................................. xxiv Chapter 1 - Introduction ....... ....................................... , ................................................................... 1 Where are these sites? .......................................................................................................................... 1 Overview of rock image studies ......................................................................................................... 2 The use of informants ......................................................................................................................... 4 \Vhat is an interpretive appraach? ..................................................................................................... 5

The culture-historical approach (Level 1): .......................................................................... 6 The contextual approach (LeveI2): ...................................................................................... 6 The intuitive approach (Level 3): .......................................................................................... 7 The analogical approach (Level 3): ....................................................................................... 9 The homogical approach (Level3): .................................................................................... 10

The debate between the "lumpers" and the "splitters" ................................................................ 11 The structure of this thesis: ............................................................................................................... 16 Chapter II - Lake of the Woods: Regional Setting of the Sites ......................................... 17 Section 1: Geohistory and geography of the region ...................................................................... 17

(a) Geology ............................................................................................................................. 17 (b) Changing lake levels ........................................................................................................ 23

Section 2: History and ethnography ................................................................................................ 27 (a) Who lived in this regian during the early historical times? ........................................ 28 (b) The unresolved debate between historians and archaeologists over ethnic identification at the time of contact with Europeans ....................................................... 35 (c) Understanding the archaeological record of the Boreal Forest ............................... .48 (d) Can biological evidence resolve the problem of ethnic identity? ............................. 62

Section 3: The images created and used by the Algonquian-speaking peoples ......................... 74 (a) Is establishing the ethnic origins and its objects possible? ........................................ 76

.~. (b) Images as a means of communication .......................................................................... 97 Conclusion: ........................................................................................................................................ 123 Chapter III: A Review of the Literature concerning the Study of Rock Images Sites in the Lake of the Woods in the Canadian Shie1d prior to 2001. ................................... '" ..... 127 Section 1: The earliest investigation of these images .................................................................. 127 Section 2: More recent literature ................................................................................................... 128 Section 3: Techniques used to record the pictographs ............................................................... 136

(a) Subdividing the sites into sections ............................................................................... 136 (b).Terminology ................................................................................................................... 161 Cc) The development of the techniques used ta record the images ............................ 163

Section 4: Technical Analysis .......................................................................................................... 168 (a) Technical issues involved in recording and interpreting rock image sites ............. 168 (b) Conservation and Analytical Techniques ................................................................... 167

Section 5: Culture-Historical Approach .............................................. ......................................... 173 Section 6: Contextual Approach .................................................................................................... 191 Section 7: Literature concerned with meaning ............................................................................. 194

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(a) Intuitive Approach: ........................................................................................................ 194 (b) Analogical Approach: ................................................................................................... 197 (c) Homological Approach ................................................................................................. 197

Conclusion ......................................................................................................................................... 209 Chapter IV - My Work on the Rock Image Sites ................................................................. 213 Section 1: Numbers of images ...................................................................................................... 217 Section 2: Defining sites .................................................................................................................. 218 Section 3: What methods were used? ............................................................................................ 218

(a) Examination of maps from different periods ............................................................ 218 (b) Methods for coilecting data ......................................................................................... 223 (c) Image analysis of potential sites in the field ................................ ; .............................. 232

Section 4: The method used for describing shapes and how does one consider time: .......... 235 (a) Exfoliation ...................................................................................................................... 235 (b) White mineraI deposits ................................................................................................. 236 (c) Lichen and rock tripe growth and encroachment .................................................... 237

Section 5: Assessing age .................................................................................................................. 238 Section 6: Description of a shape .................................................................................................. 239 Section 7: The tools used to aid the analysis of the data ........................................................... .242

Ca) IZLEIO lAS ................................................................................................................... 242 (b) Image analysis using Adobe Photoshop 6.0 and VIPS ............................................ 244 Conclusion ............................................................................................................................ 245

Section 8: Vocabulary used to de scribe each type of shape found ........................................... 245 Section 9: Possible relationships between rock image sites and other archaeological sites .. 252 Conclusion: ........................................................................................................................................ 253 Chapter V: Culture-History Approach .................................................................................... 255 Section 1: Blurring/overlay discussion and clarity of images ................................................... .254 Section 2: Distribution of images ................................................................................................... 267 Section 3: Analysis of the rock image style in relation to Northern Ontario and to adjacent

areas ............... : ...................................................................................................................... 268 Section 4: The techniques used to make paintings ..................................................................... .277 Section 5: Discussion of the offerings left at sites ....................................................................... 279 Section 6: Discussion of dates ........................................................................................................ 297 Conclusion ........................................................................................................................................ 387 Chapter VI - Contextual Approach .......................................................................................... 391 Section 1: ............................................................................................................................................ 391

Caves: ............................................................................................................................. 412 Summary for Section 1: ...................................................................................................... 414

Section 2: ........................................................................................................................................... 415 Summary for Section 2: ...................................................................................................... 417

Section 3: ........................................................................................................................................... 417 Summary for Section 3 ....................................................................................................... 435

Conclusion ......................................................................................................................................... 439 Chapter VII - Application of Approaches Concerned with Meaning ........................... .441 Section 1: The two useful approaches concerned with meaning ............................................. .441

(a) Analogical approach: .................................................................................................... 442 Cb) Homological approach: .............................................................................................. .444

Section 2: An exarnination of four birch bark scroils ................................................................ .452

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(a) How were the seroIls examined? ............................................................................... .455 (b) Culture-historical Approaeh: ....................................................................................... 456

Comparison of the images found on bireh bark seroIls and on the roek image sites ................................................................................................................................. 458

(e) Contextual Approaeh: .................................................................................................. 460 The eontext of the information on the seroIls: ..................................................... .460

SeroIl1: .................................................................................................................... 460 SeroIls 2 and 3: ....................................................................................................... 460 SeroIl4: .................................................................................................................... 461

(d) Meaning: ......................................................................................................................... 461 Seroil 1: ......................................................................................................................... 462 SeroIls 2 and 3: ............................................................................................................ 463 SeroIl 4: ......................................................................................................................... 466

(e) Coneluding eomments: ................................................................................................ 467

.~ .. Seetion 3: Efforts to treat roek image eombinations as stories: ............................................... .467 (a) DiKm-4: .................................................................................................................. 468 (b) DhKm-3: ................................................................................................................ 469 (e) DgIZtn-1: ................................................................................................................. 470 (d) DhI<.:n-1: ................................................................................................................. 470 (e) DhKo-1: .................................................................................................................. 471

Coneluding Remarks: ........................................................................................................ 472 Seetion 4: The eontinuing importance of the images and the sites .......................................... .4 72 Conclusion: ........................................................................................................................................ 473 Chapter VIII: There is no Holy Grail: An Obsession with Meaning . .......................... ..477 Introduction: ..................................................................................................................................... 477

What has been going on here? ................................................................................................ 481 Seetion 1: Four Goals ...................................................................................................................... 484 Seetion 2: The theoretieal and methodologieal implieations of this thesis: ............................ .497 Seetion 3: Further researeh - What should be done next and whieh way should the field

go? ............................................................................................................................................... 500 Appendices ...................................................................................................................................... 502 Appendix 1: Summary of the information available on the pietograph sites prior to 2001 .. 502 Appendix 2: What some of the Tools of Adobe PhotoShop 6.0 ean reveal. ......................... .525 Appendix 3: A Blank Copy of Form A and Form B for Sites on Cliffs and Caves ............... 531 Appendix 4: The Mod file used by KLEIO lAS ......................................................................... 534 Appendix 5: Uehen, Roek Tripe, Exfoliation, and White Mineral Deposits in eonjunetion

with Site Orientation .......................................................................................................... 542 Appendix 6: The Different Types of the Shape Loosely Categorised as a 'Creature' ............ 550 Appendix 7: Examples of the Different Types of Shapes in Each Group .............................. 557 Appendix 8: The Geology, Geomorphology, and Type of Land Mass of Eaeh Site ............. 565 Appendix 9: Possible Correlations between the Type of Track, Reserves, Offerings in 2001

and before, and Type of Site ................................................................................... 570 Appendix 10: Indian Reserves, Offerings in 2001 and before, Type of Site, Type of Land

Mass, and Orientation of Sites ................................................................................ 577 Appendix 11: Data regarding the Type of Aecess to the Pictograph Site, Vegetation at base

of site, water levels, and the number of eliffs used .............................................. 582 Appendix 12: Do ail the sites have the necessary physieal features for pietographs? ............ 585

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Appendix 13: Sites grouped according to the number of physical attributes present ............ 588 Appendix 14: Sites grouped according to number of physical attributes present plus offerings .

..................................................................................................................................... 589 Appendix 15: Sites grouped according to number of physical attributes present and with

rocks at base of cliff face ......................................................................................... 590 Appendix 16: The "presence and absence" tables and the dendrograms from the Pearson

correlation and the Euclidean distance method ta consider the relationship· between the physical attribûtes of the sites, the different sites and the images, and the relationship between the sites and sorne of the largest shapè types .. .591

Appendix 17: The "presence and absence" tables for the images of the birch bark scrolls .. 635 Cited Bibliographic References ...................................................................................................... 637 Ethics Certificate .............................................................................................................................. 681

(Ail the figures in this the sis including the appendices are available for viewing on the CD in the envelope on the inside of the back cover.)

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Abstract

Most researchers who study rock image sites tend to be interested in the meaning of

images, even though they could obtain more empirical information about these images and

their physical location. Furthermore, very little of the work done in the past on rock image

sites has been systematic. In this thesis I address the dearth of detailed information on the

images and their context. This thesis presents a thorough examination of the images of the

twenty-seven pictograph sites in the Lake of the Woods, in the Canadian Shield. These

pictograph sites were selected because they exhibit traits evident in rock image studies in

other parts of the world.

This study is based on data col1ected during three months of fieldwork conducted in

2001. Images were found on cliff faces and inside caves. New images and new sites were

found and identified.

Here, as elsewhere, the choice of theoretical approach influences the fieldwork,

analysis, and search for meaning. Each prescribes the types of questions asked and

determines the levels of understanding obtained about whichever form of archaeological

evidence is being considered. The different but complementary theoretical approaches

should be employed in a definite order. The same data must be examined in sequential order

using these different approaches to increase the potential quantity and quality of information

gained. Archaeologists should use the foilowing sequence of approaches: culture-historical,

contextual, foilowed by either the homological, or analogie al approaches, or a combination

of the latter two.

Classifying and describing any image is very difficult, since the level of description

given to an image affects the way in which it can be analysed, and heavily influences the

possible outcome of any discussion of perceived meaning. A rigorous examination of the

images of these sites was conducted to (a) identify the possible vocabulary of images, (b)

de termine whether combinatory rules exist, (c) reconstitute the life history of each site, and

(d) as certain whether the images can be related to other indigenous images to determine if

this can provide information about the meaning(s) of the rock images. In assessing the

meaning of the rock images, the images of a few birch bark scroils were considered, since it

was posited that a detailed investigation of the scroils, the ethnographic record, and their

pictographs might provide some answers regarding the meanings of the images found on the

rock faces.

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Résumé

La plus grande partie des chercheurs qui étudient les sites rupestres tendent à

s'interesser à la signification propre des images bien qu'ils puissent en tirer plus

d'informations empiriques sur les images et leurs cadres physiques. En outre, très peu de ces

études ont été systématiques. Cette thèse se met à considerer le grand manque de détails sur

les images dans leur contexte par le moyen d'un examen détaillé, rigoureux et objectif de

vingt-huit sites rupestres dans la région du Lac des Bois sur le Bouclier canadien. Ces sites

ont été choisis.car ils démontrent des traits communs qui se trouvent parmi bien d'autres

sites rupestres à travers le monde. Les données ont été recueillies au cours de trois mois de

travaux sur le terrain entrepris en 2001 et comprennent de nouveaux sites, falaises et abris, et

de nouvelles images identifiés pour la première fois pendant cette période.

Ici, de même qu'ailleur, la méthodologie théorétique choisie pour l'étude détermine la

direction des travaux sur le terrain, leur analyse et les questions qui mènent à la signification

des résultats. Chaque méthodologie ordonne les questions posées et le niveau de

compréhension des réponses selon la catégorie de l'evidence examinée. Des approches

différentes mais complémentaires devraient être employées dans une succession bien

définie.en examinant les mêmes données à fin d'assurer et augmenter la quantité et la qualité

des résultats. Les archéologues devraient déployer ces approches dans l'ordre suivant: sur le

plan culturel-historique; dans le contexte des données; puis par des enquêtes homologiques

ou analogiques, seule ou en combinaison.

La classification et description d'une image est difficile car le niveau de description

influe sur la façon de l'analyser de même que sur l'issue de sa signification. Un examen

détaillé et minutieux des images a été entrepris dans le but de: a) identifier un vocabulaire

possible des images; b) determiner s'il existe des règles combinatoires; c) reconstituer

l'histoire de chaque site; et d) apprendre si ces images pourraient avoir un rapport à d'autres

images hors des sites rupestres, ce qui pourraient aider à éclairer la signification des images

rupestres. Puisqu'on a proposé qu'une enquête détaillée sur les images posées sur écorce de

bouleau pourrait peut-être mener à des réponses aux questions sur la signification de l'art

rupestre, quelques rouleaux d'écorce ont été examinés.

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. r--'-.

Acknowledgements

My PhD committee is headed by Professor Bruce Trigger and consists of Professors

Toby Morantz, Michael Bisson, and Andre Costopolous from the Department of

Anthropology, McGill and Professor José Igartua from Département d'histoire, Université

du Québec à Montréal. l must thank Bruce Trigger, my supervisor, for the numerous

opportunities to play with ideas and explore their possibilities especially when he may have

thought that they were not sensible but he let me discover for myself that they were really

not very useful. l must thank him for his guidance, his patience, and for always being there

whenever l needed his help and advice and for giving me the opportunity to think carefully,

clearly, critically, and to evaluate everything with an open mind and the widest possible

perspective. l have tried at aIl times throughout this degree to follow his advice regarding

data to make sure that l squeezed the orange until nothing more could be extracted.

Imust thank Bruce Trigger, Toby Morantz, and José Igartua for aIl their thoughtful

editing and writing advice. l would like to thank José Igartua for his advice and assistance

with regard to the computing tools utilised and for his advice when writing about something

technical in computing so that l used as few technical words as possible but still got the ideas

and concepts across to the reader. l must thank Andre Costopolous for his advice and

technical assistance and Michael Bisson for his thoughtful comments. l must thank Toby

Morantz for her support and help during the final year of this PhD.

l must thank Professors Bruce Trigger and Toby Morantz for financial support

whilst writing up my thesis. l am immensely grateful for their help .

l would like to thank various members of the Anthropology department at McGill

with whom l took courses including Professors Colin Scott, Toby Morantz and Jerome

Rousseau for the opportunity to explore and obtain a solid grounding in the field of

anthropology as it is perceived in North America

l must thank Dr. Scott Hamilton (Department. of Anthropology, Lakehead

University, Ontario) for his advice on various drafts of the conclusion of my thesis.

l must thank Robert von Bitter (Ontario Ministry of Culture and Communication,

Toronto, Ontario); Dr. Stewart Baldwin, Dr. Scott Hamilton, and Dr. Joe Stewart (professor

Emeritus) of the Department of Anthropology, Lakehead University, Ontario), C. S. Reid

(formally Regional Archaeologist, Ontario Ministry of Culture and Communications, Kenora,

Ontario), Dr. Jean-Luc Pilon, Curator of Ontario Archaeology, Canadian Museum of

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.,.--.. ..

Civilization, Hull, Québec), Dr. J. Peter Denny (professor Emeritus, Department of

Psychology, The University of Western Ontario), Dr. Richard Preston (professor Emeritus,

Dept. of Anthropology, McMaster University, Ontario), Dr. Rhonda Telford (Historical

Research and Consulting, Hamilton, Ontario), W. A. Ross (formally Regional Archaeologist,

Ontario Ministry of Culture and Communications and currently Ross Archaeological

Research Associates, Thunder Bay, Ontario), Dr. Martin Magne (Manager, Cultural Resource

Services, Western and Northern Service Centre, Parks Canada), Dr. Cath Oberholtzer

(Conjunct Professor, Department of Anthropology, Trent University, Ontario), Dena

Doroszenko (Ontario Heritage Trust, Toronto, Ontario), Dr. 1. N. M. Wainwright

(Analytical Research Laboratory, Canadian Conservation lnstitute, Ottawa, Ontario),

Margaret McMahon (Water Statistics Analyst, Water Resources Division, Ontario Power

Generation), Mike Larson (Minnesota Department of Natural Resources, Minnesota), Rick

Cousins (Senior Water Resources Engineer, Lake of the Woods Secretariat, Lake of the

Woods Water Control Board, Canada), Dr. Daniel Arsenault (Départment d'histoire de l'art,

Université du Québec à Montréal, Québec), Dr. Beth A. S. Shook (Department of

Anthropology, CSU Chico, California, USA), Dr. Tim Jones (Executive Director,

Saskatchewan Archaeological Society, Saskatoon, Saskatchewan), Dr. lan A. Cowx

(International Fisheries lnstitute, University of Hull, UK), Dr. Charles A. Bishop (Research

Professor of Anthropology, Union College, Schenectady, New York, USA), Dr. John Long,

(Associate Professor, Faculty of Education, Nipissing University, Ontario), Dr. Jane Down

(Senior Conservation Scientist, Conservation Processes and Materials Research, Canadian

Conservation Institute, Ottawa, Ontario), Nancy Binnie (Conservation Scientist, Canadian

Conservation Institute, Ottawa, Ontario), Mark J. Dudzik (State Archaeologist, Fort Snelling

History Center, St. Paul, Minnesota, USA), Marie-Louise Perron (Library and Archives

Canada, Canadian Genealogy Centre, Library and Archives Canada, Ottawa, Ontario),

Jonathan Moore (Underwater Archaeology Service, Parks Canada Agency, Ottawa, Ontario),

Kari Layman (Hydraulics, USACE - St. Paul District, Minnesota, USA), Dr. Lisa Dillon

(Départment de demongraphiè, Université de Montréal, Québec), Dr. Sara Louri, and Hayley

Fitzsimmons for giving me references, information, archaeological reports, data of different

types, slides, files, and opportunities to discuss ideas.

l must also thank those archaeologists who had worked on sites in the Lake of the

Woods prior to myself and who kindly provided the references of their work: C. S. Reid

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(formally Regional Archaeologist, Ontario Ministry of Culture and Communications, Kenora,

Ontario), Dr. Brian L. Molyneaux (Department of Anthropology, University of South

Dakota, Vermillion, South Dakota, USA), Dr. Jack Steinbring (Department of Anthropology,

Ripon College, Ripon, Wisconsin, USA), and William A. Fox (Field Unit Superintendent,

Western Arctic District, Parks Canada).

l must thank my field assistant Melinda Bell and my volunteer Elizabeth Campbell

for their help and assistance in the field. l must also thank W. A. Ross (Regional

Archaeologist, Thunder Bay, Ontario) for technical help and advice while in the field. l must

also thank David Fraser and the diving team from Sunset Diving, Kenora, Ontario for their

assistance while surveying and recording the pictograph sites. 1 must thank the Kast family

and everyone at Tomahawk Lodge and Marina, Wendal Dafcik and his guides of Crow Rock

Lodge, the owners and the guides of Monument Bay Lodge, Paul and Beverly Eliuk, Bill and

Billie-Jean Murphy from Sioux Narrows provided advice and expertise which made the

practical aspects of conducting field work possible.

l must also thank Professor Wendy Hall, Head of School, Professor Paul Lewis, and

Dr Kirk Martinez (Intelligence, Agents, Multimedia Group, School of Electronics and

Computing Science, University of Southampton, UK) for their help, guidance, and advice

when 1 used VIPS and for the experimental work 1 did in their laboratory. l must thank Dr

Mike Westmacott, Dr M. Faizal A. Fauzi, Dr David P Dupplaw, and Dr. Fazly Salleh Abas

who were doing research for their PhDs while 1 was there as well as Dr. David Millard and

Dr. Christopher Bailey for their technical assistance and for their questions because 1 realised

that the manner in which images are described fundamentally and directly affects its

subsequent interpretation.

1 must thank Dr. Andrew Sawyer (Hon. Research Fellow, Department of Museum

Studies, University of Leicester & mwr ltd) for teaching me how to use KLEIO IAS. l must

thank both Professor Manfred Thaller (professor in Computer Science for the Humanities,

Universitat zu KaIn, Germany) and Dr. Gerhardt Jaritz (Department of Medieval Studies,

Central European University, Central European University, Prague, Hungary) for help and

advice regarding the technical and theoretical aspects of KLEIO and KLEIO lAS.

l must thank Dr. Mima Kapches for permission to consult the Selwyn Dewdney

Papers in the New \Vorld Department Collection, in the Royal Ontario Museum, Toronto,

Ontario and Lori Nelson, the Director of the Lake of the Woods Museum in Kenora,

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Ontario for letting me examine the papers of several early settlers in the Lake of the Woods

and using the photograph of the Massacre Scroll.

Numerous people gave me advice on how to track down a photograph of a birch

bark scroll and their combined efforts made the chapter on birch bark scrolls possible. l

must thank Moira McCaffrey (Director, Research and Exhibitions, McCord Museum of

Canadian History, Montréal, Québec); Dr. Jban Vastokas (professor Emerita, Department of

Anthropology, Trent University, Ontario), Dr. Jennifer S.H. Brown, (Director of The Centre

for Rupert's Land Studies/Department of History, The University of Winnipeg, Manitoba),

Dr. George Fulford (Department of Anthropology, The University of Winnipeg, Manitoba),

Dr. Sally Cole (Department of Anthropology and Sociology, Concordia University, Montréal,

Québec), Dr. J. c. H. King (Keeper, Department of Africa, Oceania and the Americas,

British Museum, London, England), Dr. Teresa Schenk (Center for the Study of Upper

Midwestern Cultures, University of Wisconsin, Madison, Wisconsin, USA), Lori Nelson

(Director, Lake of the Woods Museum, Kenora, Ontario), and finally Dr Heidi Bohdaker

(SSHRC Postdoctoral Fellow, Institute for Comparative Studies in Literature, Art and

Culture, Carleton University, Ontario).

l must thank several friends and colleagues who took cime from their own work to

read, comment, and discuss various versions of my thesis: Harry Lerner, Dr. Csilla Dallos

(Department of Anthropology, St. Thomas University, New Brunswick), Apryl

Wassaykeesic, Cecil Chabot, Loretta Flegel, Sheila Oakley, Yasir Khan, Dr. André LeBlanc

(Visiting Assistant Professor, History of Science and Technology Programme, University of

King's College, Nova Scotia) and Dr. Carolyn Podruchny (Department of History, York

University, Ontario). l must thank Elizabeth Campbell for editing this thesis, Francis Carson

who translated my abstract into French, and Neha Gupta and Rebekah Jobling who helped

convert sorne electronic fIles from one format to another.

l must thank the interlibrary loans department and the Blackadder-Lauterman,

Redpath, McClennan, Schulich libraries and particularly Rosa Orlandini and Joanna Hobbins

from the Walter Hitschfeld Geographie Information Centre for their assistance. l am grateful

for the continual assistance and guidance of Rose Marie Stano, Cynthia Romanyk, and Diane

Mann from the Department of Anthropology at McGill.

l must thank several people for technical support and advice regarding any computer

hardware problems that l had including Sean Colson (pC Consultants, Ryde, Isle of Wight,

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UK), University Bytes (Montréal, Quebec), Computech (Kenora, Ontario), Ian Shaw

(Managing Director of mwr InfoSecurity, Basingstoke, Hampshire, UK) and Joanna

Hobbins.

l must thank the following organizations for providing funding for m)' research: Max

Bell Fellowship for Canadian and Northern Studies, Sigma Xi Grant-in-Aid, Sigma Xi,

MacKenzie Ward Trust, Sioux Narrows, Ontario, Ontario Rock Art Conservation

Association, Canadian Historical Association, two Alma Mater Student Travel Grants, as weIl

as in-kind funding from the Ontario Ministry of Culture, Tourism and Recreation.

l must thank those friends who have not been involved in any aspect of my research

for having provided moral support: Alice Anderson, Denise Arthur, Andrea Cardarello, Sara

and Jim Busby, Nancy Chapman, Dr. Cristina Redko Meir, Dr. Caroline Gooch, Dr.

Doralice Barros Pereira, Angela Boville, Melissa Anderson, Ruth Greenaway, Gavin Taylour,

Judy Petch, Masami Waki, Rieko Sasa, Teresa deI Blanco, Nuzhat Dunn, Debra Irons, Sarah

Phillips, Lucy Braga, Rita Weidendorfer, Jennifer Famery, Heather Podruchny, Simone

Abuhab, Belinda Beaton, Alessandra Crippa, Eleanor Roff, and Dan Friesting. l come from a

large family and all of them have been incredibly supportive while undertaking this degree

but l must specifically thank a few of them: Professor Richard and Betty Preston, Finbar and

Susie Coison, my godparents Professor Henry and Mercedes Ettinghausen, my brother-in­

law Ian Shaw, my sister Beth Coison, and finally my parents Dr. R. Frank and Jean Coison

l would like to dedicate this the sis to two people: my paternal grandmother Kathleen

Cotter Colson and my maternaI grandfather MacKenzie Belfield Ward. My grandmother

taught me that it was important to stand up for the freedom of speech and thought no

matter how hard it rnight be to do this. My grandfather, MacKenzie Ward had a reputation

of being both strong rninded and highly opinionated. Both of us disagreed with each other

numerous times about many things but ultimately we both knew that it was better to agree to

disagree because our disagreements stemmed from each of us having different perspectives

and attitudes about the world and the way it functioned. He repeatedly told me that it was

better to stand up for what l believed, if l believed my perspective was weIl grounded and

researched, regardless of how hard it might be at the time than to buckle and back down

because of someone else's opinion.

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r--' ..

N ote on Spelling

The author of this thesis has used standard British English grammar, punctuation,

and spelling from the O:x.ford English Dictionary throughout her research and her thesis since

she started at McGill in September 1998.

Page xiü

Page 16: An obsession with meaning: a critical examination of the pictograph sites of the Lake of Woods

Note on KLEIO lAS

The combination of the two letters 'xq' plus a number appear throughout several of the chapters in this thesis. This is not a special code. The letters 'xq' indicate that the result was provided as a consequence of a query numbered 'xq and a number'. It is a convention of KLEIO to use these letters and numbers as references to a particular database query.

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List of Figures

Figure 1.1: Physical Location of the Lake of the Woods ............................................................... 2 Figure 1.2: Examples of shapes loosely categorised as 'crescents' and the sites that they come

from in the Lake of the Woods .................................................................................... 13-15 Figure 2.1: Cliffs in the southern end of Whitefish Bay with clearly defined high water levels ............................................................................................................................................................... 24 Figure 3.1: Map of the sites that Lawson recorded in 1885 ....................................................... 127 Figure 3.2: Lawson's published drawing of the images at DiKo-2, the petroglyph site. In:

Lawson, A. C 1885. Ancient Rock Inscriptions on the Lake of the Woods. Amm'can NaturalistXIX (7): 654-657.Pp.: 656 ................................................................................ 128

Figure 3.3: Lawson's published drawing of the images at DiKp-l, the pictograph site from 1885. Lawson, A. C 1885. Ancient Rock Inscriptions on the Lake of the Woods. American Naturalist XIX (7): 654-657. Pp: 657 ............................................................... 128

Figure 3.4: Annotated photograph of DiKp-l taken in June 2001 ........................................... 129 Figure 3.5: The four sites that Cameron recorded in 1978 ........................................................ 131 Figure 3.6: Fox's photograph of DhKm-l in 1974. Courtesy of Ontario Ministry of Culture

and Communications .......................................................................................................... 133 Figure 3.7: Dewdney's 15 July 1960 field record of Site # 92A, now called DhKm-l and

DhKm-4. © Royal Ontario Museum, Toronto Canada .............................................. .135 Figure 3.8: A field recording by Dewdney of two pictograph sites in Lake of the Woods, Site

#70 Sunset Channel (DiKp-l) and Site # 69 Picture Rock Island (DhKm-3). © Royal Ontario Museum, Toronto Canada ...................................................................... 136

Figure 3.9: Dewdney's field drawing of Site # 28, undertaken on 15 August 1953. © Royal Ontario Museum, Toronto Canada .................................................................................. 138

Figure 3.10: Face 2 and 3 of Site # 28 by Dewdney in 1953. © Royal Ontario Museum, Toronto Canada .................................................................................................................. 139

Figure 3.11: Dewdney's field drawing of Site #106 undertaken on August 19 1960. © Royal Ontario Museum, Toronto Canada .................................................................................. 139

Figure 3.12: The Close Proximity of DhKm-4 to DhKm-l ...................................................... 140 Figure 3.13: Annotated photograph of DhKm-l in 2001 by Cols on according to Dewdney's

divisions ................................................................................................................................ 141 Figure 3.14: Annotated photograph by toIson of DhKm-1 taken in 2001 according to

Lambert's divisions ............................................................................................................. 142 Figure 3.15: Dewdney's field drawing of Site # 69 undertaken on 8 August 1959. © Royal

Ontario Museum, Toronto Canada .................................................................................. 142 Figure 3.16: Part 1 of Dewdney's field drawing of Site # 91A and B, undertaken on 15 July

1960. © Royal Ontario Museum, Toronto Canada ....................................................... 143 Figure 3.17: Part 2 of Dewdney's field drawing of Site # 91A and B, undertaken on 15 July

1960. © Royal Ontario Museum, Toronto Canada ....................................................... 143 Figure 3.18: Setting with offerings and CD., Site # 29 by Dewdney. © Royal Ontario

Mùseum, Toronto Canada ................................................................................................. 144 Figure 3.19: Photôgraph of part of DjKn-1 called Site # 29 taken by Dewdney in 1959. ©

Royal Ontario Museum, Toronto Canada ...................................................................... 144 Figure 3.20: Part of DjKn-l,July 2001 ......................................................................................... 145 Figure 3.21: Dewdney's 1964 field drawing of Site # 197 (DgKl-l) and # 198 (DgKl-2). ©

Royal Ontario Museum, Toronto Canada ...................................................................... 146 Figure 3.22: Photograph of DgKl-l in July 2001 with Pastershank's 1989 subdivisions ...... 146

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Figure 3.23: DgKl-2 in 1989 bl' Pastershank. Courtes)' of Ontario Ministry of Culture and Communications ................................................................................................................. 147

Figure 3.24: Dewdney's published images from this site. In: Dewdney S. and K. Kidd. 1967. Indian Paintings if the Great Lakes. 2nd Edition Toronto: University of Toronto Press. p.l10 ..................................................................................................................................... 148

Figure 3.25: Three of the new images at DgKl-2 in July 2001 .................................................. 148 Figure 3.26: The new image at DgKl-2 not painted upon the older ochre images in July 2001

............................................................................................................................................... 149 Figure 3.27: Annotation by Coison in 2004 of DgKl-2 taken by Pastershank in 1989 ......... 150 Figure 3.28: Field recording of detail of Face l, DgKI-2, Pastershank in 1989. In:

Pastershank, G. 1989. An Archaeological Sun1ry if Sabaskong B'!)', Lake if the Woods. Ontario Conservation Archaeology Report #13, North-western Region. Kenora: Ontario Ministry of Culture and Communications. p. 56 ............................................ 150

Figure 3.29: Photograph of Face 1 by Pastershank in 1989. Courtesy of Ontario Ministry of Culture and Communications ............ ; ........................................................................... 151

Figure 3.30: Annotation by Coison in 2004 of photograph, of Face II by Pastershank in 1989. Courtesy of Ontario 1linistry of Culture and Communications .............................. 152

Figure 3.31: Field drawing with detail of Morph 4 at DgKl-2. In: Pastershank, G. 1989. An Archaeological S urvry if S abaskong B'!)', Lake if the Woods. Ontario Conservation Archaeology Report #13, North-western Region. Kenora: Ontario Ministry of Culture and Communications. p. 58 ................................................................................ 152

Figure 3.32: Field recording of detail of Face III. In: Pastershank, G. 1989. An Archaeological Survry if Sabaskong B'!)'J Lake if the Woods. Ontario Conservation Archaeology Report #13, North-western Region. Kenora: Ontario Ministry of Culture and Communications. p. 60 ...................................................................................................... 153

Figure 3.33: Field recording of Face IV of DgKl-2. In: Pastershank, G. 1989. An Archaeological Survry if Sabaskong B'!)'J Lake if the Woods. Ontario Conservation Archaeology Report #13, North-western Region. Kenora: Ontario Ministry of Culture and Communications. p. 61 ................................................................................ 154

Figure 3.34: DgKI-2, Detail of Face IV by Pastershank in 1989. Courtesy of Ontario Ministry of Culture and Communications ...................................................................................... 155

Figure 3.35: Pastershank's Field recordings of Faces V, VI and VII. In: Pastershank, G. 1989. An Archaeological Survry if Sabaskong B'!)'J Lake if the Woods. Ontario Conservation Archaeology Report #13, North-western Region. Kenora: Ontario Ministry of Culture and Communications. p. 62 ................................................................................ 155

Figure 3.36: U sing Pastershank's (1989) subdivisions of rock surface to divide the paintings in 2001 into Faces V, VI and VIl ..................................................................................... 156

Figure 3.37: Face l of DgKl-17 by Pastershank in 1989. Courtesy of Ontario Ministry of Culture and Communications ........................................................................................... 158

Figure 3.38: DgKl-17 _ Pastershank's FaceII and II in 1989. In: Pastershank, G. 1989. An Archaeological Survry of Sabaskong B'!)'J Lake of the Woods. Ontario Conservation Archaeology Report #13, North-western Region. Kenora: Ontario Ministry of Culture and Communications. p. 66 ................................................................................ 159

Figure 3.39: Pastershank divided this Face into NO parts called Panel i and ü in 1989. In: Pastershank, G. 1989. An Archaeological Survry if Sabaskong B'!)'J Lake if the Woods. Ontario Conservation Archaeology Report #13, North-western Region. Kenora: Ontario Ministry of Culture and Communications. p.68 .............................................. 159

Figure 3.40: DhKm-5 in June 2001 ............................................................................................... 160

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.~ ..

Figure 3.41: The new part ofDhKm-5 ......................................................................................... 161 Figure 3.42: Dewdney working with a colleague on an improvised platform at Site #108. ©

Royal Ontario Museum, Toronto Canada ...................................................................... 164 Figure 3.43: The plastic being taped to the surface of the cliff face and the mineraI

precipitation and patination being recorded by a black pen by Rusak in 1991. Courtesy of Ontario Ministry of Culture and Communications .................................. 167

Figure 3.44: DiKp-l, Sunset Channel, 25th July 1975 © Canadian Conservation Institute . .170 Figure 3.45: The table drawn by Dewdney to illustrate how he classified the images at these

sites. In: Dewdney S. and K. Kidd. 1962. lndian Paintings of the Great Lakes. Toronto: University of Toronto Press, p. 18 ................................................................................... 174

Figure 3.46: The Massacre Scroll photographed in 1993 by J. Rusak. Collections of the Lake of the Woods Museum, Kenora, Ontario ....................................................... : .............. .190

Figure 3.47: Part of DhKn-l beside Obabikon Channel ........................................................... l92 Figure 3.48: The serpents and the turtles described by Dewdney in 1960 .............................. 199 Figure 4.1: Examples of cliff faces examined for pictographs during 2001 ............................ 220 Figure 4.2: DhKm-18 (an "oId" site) and DhKm-20 Ca "new" site) ....................................... .221 Figure 4.3: A map of where the diving took place ...................................................................... 222 Figure 4.4: Overview of DgKI-2 taken in 2001 ........................................................................... 224 Figure 4.5: Physical location of DgKI-2 in Sabaskong Bay, Lake of the Woods. C4nadian

Hydrographic Services. "Sabaskong Bay, Lake of the Woods, Southeastern Channel" [hydrographic chart]. 1 :40,000. Sheet 6214. Ottawa: Department of Oceans and Fisheries, 1989 .................................................................................................................... 225

Figure 4.6: Field drawing of DgKI-2 by M. Bell in 2001 ............................................................ 229 Figure 4.7: Red/orange lichen on the western end of Crowrock Island ................................. .233 Figure 4.8: Part of DjKn-l used as the control file ..................................................................... 234 Figure 4.9: DiKp-l in June 2001 annotated by Colson in 2002 to indicate locations of previously unknown images ......................... ; .............................................. 241 Figure 4.10: Map indicating location of other known archaeologïcal sites to pictograph sites ............................................................................................................................................................. 253 Figure 5.1: DkIZn-6 in 2001 ............................................................................................................ 256 Figure 5.2: The different shapes of 'creatures' at DhKn-l in 2001 .......................................... 257 Figure 5.3: Overview of DhKm-4 in Whitefish Bay in 2001 ..................................................... 257 Figure 5.4: DhKm-l has images affected by exfoliation, white mineraI deposits and rock tripe

and lichen encroachment in 2001 .................................................................................... .258 Figure 5.5: The exfoliated images at DhKm-l in 2001. © Elizabeth Campbell 2001 ........... .259 Figure 5.6: The smear at DhKm-l in 2001. © Elizabeth Campbell 2001 .............................. .259 Figure 5.7: The upper part of DiKn-1 in 2001. © Elizabeth Campbell 2001 ......................... 260 Figure 5.8: Severe deposition of white mineraI deposits at DiKq-l 0 in 2001 ......................... 261 Figure 5.9: AIl of the images at DhKm-3 in 2001. © Elizabeth Campbell 2001 ............ 262-263 Figure 5.10: Screenshot of some of the red images below the white mineraI deposits ......... 264 Figure 5.11: If this screen shot is compared with the screen shot above it is clear that the

accumulation of white mineraI deposits at DhKm-S is not uniform .......................... 264 Figure 5.12: Screenshot showing what occurs to the same im4ges using different tools when 1

mathematically tried to rem ove the white pixels deemed 'noise" ................................ 266 Figure 5.13: A map of the Lake of the Woods area showing the numbers of images at each

site ......................................................................................................................................... 267 Figure 5.14: D1Jn-l from Harmon Lake Courtesy of Ontario Ministry of Culture and

Communications ................................................................................................................. 270

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Figure 5.15: DjKp-l0 on Moberly Lake. Courtesy of Ontario J\1inistry of Culture and Communications ................................................................................................................. 270

Figure 5.16: DjJp-l on Moberly Lake. Courtesy of Ontario J\1inistry of Culture and Communications ................................................................................................................. 271

Figure 5.17: Close up of a rectangle with the circle and the diagonallines fromDhKm-3 in 2001 ....................................................................................................................................... 276

Figure 5.18: The rectangle with the stick figure at DhKo-l in 2001 ........................................ 277 Figure 5.19: Sites where offerings were found in 2001 .............................................................. .281 Figure 5.20: Sites where tobacco was found as an offering in 2001 ......................................... 282 Figure 5.21: Sites where money was found as an offering in 2001 ........................................... 283 Figure 5.22: Offerings discovered by Fox in 1974 at DhKm-1. Courtesy of Ontario J\1inistry

of Culture and Communications ...................................................................................... 284 Figure 5.23: Sites where clothing was found as offerings in 2001 ............................................ 285 Figure 5.24: Sites where liquor botdes were found as offerings in 2001 ................................. 286 Figure 5.25: Offerings that Dewdney found at DjKq-l0 called Site # 95, Picture Rock Point

in 1960. © Royal Ontario Museum, Toronto Canada ................................................... 287 Figure 5.26: Offerings that Dewdney found at DjKq-l0 called Site # 95, Picture Rock Point

in 1960 .................................................................................................................................. 287 Figure 5.27: The lower part of the DiKn-l, Hayter's Point in 2001.. ....................................... 288 Figure 5.28: The largest pile of the offerings found at DgKl-2 in June 2001.. ....................... .289 Figure 5.29: Offerings stuffed in the crevice at DhKm-1 in 2001 © Elizabeth Campbell 2001

............................................................................................................................................... 290 Figure 5.30: The Bowl near DiKm-50 © Elizabeth Campbell 2001 ........................................ 291 Figure 5.31: The Marker's Mark © Elizabeth Campbell 2001 ................................................... 291 Figure 5.32: The Vial © Elizabeth Campbell 2001 ..................................................................... .292 Figure 5.33: The Hand Tooled Top © Elizabeth Campbell 2001 ............................................ 292 Figure 5.34: Close-up of Top © Elizabeth Campbell 2001 ....................................................... 292 Figure 5.35: The Lead Shot © Elizabeth Campbell 2001 ........................................................... 292 Figure 5.36: The Vial Opening © Elizabeth Campbell 2001 .................................................... .292 Figure 5.37: Outside of Pot © Elizabeth Campbell 2001 .......................................................... 293 Figure 5.38: Inside of Pot © Elizabeth Campbell 2001 .............................................................. 293 Figure 5.39: Side view of Pot © Elizabeth Campbell 2001 ........................................................ 293 Figure 5.40: Outside of Pot © Elizabeth Campbell 2001 .......................................................... 294 Figure 5.41: Inside of Pot © Elizabeth Campbell 2001 .............................................................. 294 Figure 5.42: Surface of Pot © Elizabeth Campbell 2001 .......................................................... .294 Figure 5.43: Base of Pot © Elizabeth Campbell 2001 ................................................................ 294 Figure 5.44: Rim of Pot © Elizabeth Campbell 2001 ................................................................. 295 Figure 5.45: Setting of Site # 197. © Royal Ontario Museum, Toronto Canada ................... 299 Figure 5.46: Face 1 Site # 197 by Dewdney in 1964. © Royal Ontario Museum, Toronto

Canada .................................................................................................................................. 300 Figure 5.47: Face 2, Site # 197 by Dewdney in 1964. © Royal Ontario Museum, Toronto

Canada .................................................................................................................................. 300 Figure 5.48: Face 1 of DgKl-1 and Face 2 of DgKl-2 taken by Pastershank in 1989. Courtesy

of Ontario J\1inistry of Culture and Communications .................................................. 301 Figure 5.49: Face 3 of DgKl-1 by Pastershank in 1989. Courtesy of Ontario J\1inistry of

Culture and Communications ........................................................................................... 301 Figure 5.50: Photograph of DgKl-2 in 2001 ................................................................... : ............ 302

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Figure 5.51: Face 1 of Site # 198 by Dewdney in 1964. © Royal Ontario Museum, Toronto Canada .................................................................................................................................. 303

Figure 5.52: "Cave" at Site # 198 in 1964 by Dewdney. © Royal Ontario Museum, Toronto Canada .................................................................................................................................. 303

Figure 5.53: Pastershank's Face 1 by Pastershank in 1989. Courtesy of Ontario Ministry of Culture and Communications .................................... : ...................................................... 304

Figure 5.54: Faces II, III and IV by Pastershank in 1989. Courtesy of Ontario Ministry of Culture and Communications ........................................................................................... 305

Figure 5.55: Setting from distance of Site # 28, Sioux Narrows by Dewdney in 1953. Courtesy of Ontario Ministry of Culture and Communications .................................. 306

Figure 5.56: Face 2 and 3 of Site # 28 by Dewdney in 1953. Courtesy of Ontario Ministry of Culture and Communications ........................................................................................... 307

Figure 5.57: Close-up of DiKm-3 taken in 1991 ......................................................................... 307 Figure 5.58: Close-up of DiKm-3 taken in 2001 ......................................................................... 308 Figure 5.59: Face 2, Site # 106 by Dewdney in 1960. © Royal Ontario Museum, Toronto

Canada .................................................................................................................................. 309 Figure 5.60: Site # 106, Sabaskong-Obabikon Channel, Watercolour reproduction of Face II

by Dewdney. © Royal Ontario Museum, Toronto Canada .......................................... 309 Figure 5.61: Close-up ofleft hand part of DhKn-1 in 2001 ...................................................... 310 Figure 5.62: Close-up of right hand part of DhKn-1 in 2001 ................................................... 311 Figure 5.63: Setting "the hole" at Devil's Hole Site #92 by Dewdney in 1960. © Royal

Ontario Museum, Toronto Canada .................................................................................. 312 Figure 5.64: Setting with W. F. and offerings beside Site # 92 by Dewdney in 1960. © Royal

Ontario Museum, Toronto Canada .................................................................................. 312 Figure 5.65: DhKm-1 taken in September 1974 by W. Fox. Courtesy of Ontario Ministry of

Culture and Communications ........................................................................................... 313 Figure 5.66: DhKm-1 in June 2001 ............................................................................................... 314 Figure 5.67: Thompson's Drawings of the images at the pictograph site. © Royal Ontario

Museum, Toronto Canada ................................................................................................. 316 Figure 5.68: DhKo-1 by K. Campbell in 1951. © K.athleen Campbe1l2001 .......................... 317 Figure 5.69: Dewdney's field recording of Site # 108 undertaken on August 20 August 1960.

© Royal Ontario Museum, Toronto Canada .................................................................. 318 Figure 5.70: Dewdney's photograph of Site # 108. © Royal Ontario Museum, Toronto

Canada .................................................................................................................................. 319 Figure 5.71: Section of DhKo-1 taken by Molyneaux. In: Molyneaux, B. L. 1987. The Lake of

the Painted Cave Archaeology 40 (4) p.20 ..................................................................... ;319 Figure 5.72: Overview of DhKo-1 in 2001 .................................................................................. 320 Figure 5.73: Dewdney's Site # 93 wruch he called an "offering site" in July 1960. © Royal

Ontario Museum, Toronto Canada .................................................................................. 321 Figure 5.74: Setting of Site # 93 by Dewdney in 1960. © Royal Ontario Museum, Toronto

Canada .................................................................................................................................. 321 Figure 5.75: Jerry Corpine at Site #93 by Dewdney in 1960. © Royal Ontario Museum,

Toronto Canada .................................................................................................................. 322 Figure 5.76: DiKm-4 by Moll'neaux. In: Molyneaux, B. L. 1980a. Landscape Images Rotunda

13 (3): 10 .................................................................. ; ........................................................... 323 Figure 5.77: DiKm-4 bl' Pelshea in 1978. Courtesy of Ontario Ministry of Culture and

Communications ................................................................................................................. 323 Figure 5.78: DiKm-4 taken in 1991 ............................................................................................... 324

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Figure 5.79: DiKm-4 taken in 2001 ............................................................................................... 324 Figure 5.80: Dewdney's field drawing of Site # 69 called Picture Rock Island undertaken on

8 August 1959. © Royal Ontario Museum, Toronto Canada ...................................... 325 Figure 5.81: Face lof Site # 69 in Whitefish Bay, Lake of the Woods taken by Dewdney in

1959. © Royal Ontario Museum, Toronto Canada ....................................................... 325 Figure 5.82: Face II of Site # 69 taken by Dewdney in 1959. © Royal Ontario Museum,

Toronto Canada .................................................................................................................. 326 Figure 5.83: Water colour reproduction of Face III of Site # 69 by Dewdney in 1959. ©

Royal Ontario Museum, Toronto Canada ...................................................................... 327 Figure 5.84: Black and White photograph of DhKm-3 taken by Molyneaux. In: Molyneaux,

B. L. 1980a. Landscape Images Rotunda 13 (3): 7 ........................................................... 327 Figure 5.85: The images at DhKm-3 taken by Pelshea in 1978. Courtesy of Ontario Ministry

of Culture and Communications ...................................................................................... 328 Figure 5.86: Left hand side of DhKm-3 taken in 2001 .............................................................. 329 Figure 5.87: Annotated section of DhKm-3 by Colson taken in 2001 .................................... 329 Figure 5.88: Right hand end of DhKm-3 ..................................................................................... 330 Figure 5.89: Face 1- Figure a & b, Site # 92A taken by Dewdney in 1960. © Royal Ontario

Museum, Toronto Canada ................................................................................................. 331 Figure 5.90: Left hand side of DhKm-4 in 2001 ......................................................................... 332 Figure 5.91: Right hand side of DhKm-4 in 2001 ....................................................................... 332 Figure 5.92: Dewdney's field drawing of Site # 105 undertaken on 19 August 1960. © Royal

Ontario Museum, Toronto Canada .................................................................................. 333 Figure 5.93: Close view of Site # 105 taken by Dewdney in 1960. © Royal Ontario Museum,

Toronto Canada .................................................................................................................. 334 Figure 5.94: Closer view of DhKm-5 by Pelshea in 1978 .. © Royal Ontario Museum, Toronto

Canada .......................................................... ; ....................................................................... 334 Figure 5.95: Molyneaux's photograph of DhKm-5. © Royal Ontario Museum, Toronto

Canada .................................................................................................................................. 335 Figure 5.96: Photograph of DhKm-5 taken in 2001. © Royal Ontario Museum, Toronto

Canada .................................................................................................................................. 337 Figure 5.97: Dewdney's field drawing of Site # 70 in Sunset Channel undertaken on August

12, 1959. © Royal Ontario Museum, Toronto Canada .................................... ; ........... .337 Figure 5.98: Photograph of DiKp-l taken by C. S. Reid in May 1975. © Royal Ontario

Museum, Toronto Canada ................................................................................................. 339 Figure 5.99: DiKp-l, Sunset Channel, 25thJuly 1975 annotated by A. Colson in 2001 ....... 340 Figure 5.100: Photograph of DiKp-l taken in June 2001 .......................................................... 340 Figure 5.101: Lichen growth and encroachment as marked by A Colson in 2001 .......... ~ ...... 341 Figure 5.1 02: The areas containing missing images at DiKp-l indicated by Colson ............. 342 Figure 5.103: DgKm-l in Splitrock Bay taken in 2001 ............................................................... 343 Figure 5.104: Left hand part ofDgKI-17 ...................................................................................... 344 Figure 5.105: Right hand part of DgKl-17 ................................................................................... 344 Figure 5.106: Cyclone Point (unknown photographer and unknown date). © Royal Ontario

Museum, Toronto Canada ................................................................................................. 345 Figure 5.107: DgKl-19 by Pastershank taken in 1989. Courtesy of Ontario Ministry of

Culture and Communications ........................................................................................... 346 Figure 5.108: DgKl-19 photographed in 2001 ............................................................................. 346 Figure 5.109: Annotation by Colson of Site # 95 taken by Dewdney in 1960. © Royal

Ontario Museum, Toronto Canada .................................................................................. 347

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Figure 5.110: Left hand side and right hand side of DiKq-l0 in 2001 ..................................... 348 Figure 5.111: "Setting of Site # 94 with P.D." Photograph taken by Dewdney in 1960. ©

Royal Ontario Museum, Toronto Canada ...................................................................... 349 Figure 5.112: Annotated setting of DjKr-23 in 2001 by Colson ............................................... 349 Figure 5.113: DjKr-23 in July 2001 ................................................................................................ 350 Figure 5.114: Dewdney field drawing of Site # 104 undertaken on 19 August in 1960. ©

Royal Ontario Museum, Toronto Canada ...................................................................... 351 Figure 5.115: Setting of Site#- 104 taken by Dewdney (© Royal Ontario Museum, Toronto

Canada) annotated by A. Coison on the right ................................................................ 351 Figure 5.116: Devil's Bay Site # 104 taken by Dewdney © Royal Ontario Museum, Toronto

Canada .................................................................................................................................. 352 Figure 5.117: Bird identified by Dewdney and Lambert beside the two vertical stick identified

in 2001 .................................................................................................................................. 353 Figure 5.118: Smear at DhKm-18 in 2001 ........................ ; .......................................................... 353

~ .. Figure 5.119: Oblong blob at DhKm-18 in 2001 ........................................................................ 354 Figure 5.120: Close up of Site # 270 Horseshoe Island in Whitefish Bay by Dewdney. ©

Royal Ontario Museum, Toronto Canada ...................................................................... 355 Figure 5.121: DiKm-51 taken in 2001. © Elizabeth Campbell 2001.. ...................................... 355 Figure 5.122: Annotated by Colson in 2001 ofDiKm-51 taken in 2001.. ............................... 356 Figure 5.123: Annotated by Colson in 2001 ofDiKm-51 taken by Dewdney ....................... .356 Figure 5.124: DkKn-7 in 2001 ........................................................................................................ 357 Figure 5.125: DkI<n-6 in 2001 ........................................................................................................ 358 Figure 5.126: Dewdney's field drawing of Site # 107 in Obabika Narrows undertaken on

August 191960. © Royal Ontario Museum, Toronto Canada .................................... 359 Figure 5.127: Part of DjI<n-l taken by Molyneaux. In: Molyneaux, B. L. 1980a. Landscape

Images Rotunda 13 (3): 9 ..................................................................................................... 360 Figure 5.128: Pelshea's photograph of the le ft hand side of DjI<n-l taken in 1978. Courtesy

of Ontario Ministry of Culture and Communications .................................................. 361 Figure 5.129: Pelshea's photograph of the right hand side of DjI<n-l taken in 1978. Courtesy

of Ontario Ministry of Culture and Communications .................................................. 362 Figure 5.130: Part of DjI<n-l in June 2001 .................................................................................. 363 Figure 5.131: Part of DjI<n-l in June 2001 .................................................................................. 363 Figure 5.132: Part of DjI<n-l in June 2001 .................................................................................. 364 Figure 5.133: Setting from a Distance of Site # 91A and B taken by Dewdney. © Royal

Ontario Museum, Toronto Canada .................................................................................. 365 Figure 5.134: "Face lB figure c + d" by Dewdney in 1960. © Royal Ontario Museum,

Toronto Canada .................................................................................................................. 365 Figure 5.135: "Face lA fig a + b" by Dewdney in 1960. © Royal Ontario Museum, Toronto

Canada .................................................................................................................................. 366 Figure 5.136: DiKn-l in J une 2001 ................................................................................................ 366 Figure 5.137: Blob beside exfoliated area at DiI<n-l in 2001 .................................................... 367 Figure 5.138: Dewdney's "Face lA fig a + b" at DiI<n-l in 2001.. .......................................... 367 Figure 5.139: Red images are visible although partially hidden by the lichen and rock tripe in

the upper half of DiKn-l in 2001 .................................................................................... 368 Figure 5.140: Shapes above the main collection of shapes at DiI<n-l ..................................... 368 Figure 5.141: DhKm-20 in June 2001 ........................................................................................... 369 Figure 5.142: DhKm-19 in 2001 .................................................................................................... 370 Figure 5.143: DgKm-2 in July 2001 ............................................................................................... 371

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Figure 5.144: DiKm-49 in June 2001 .................................................... : ...................................... ;372 Figure 5.145: DiKin-50 in June 2001 ............................................................................................ 373 Figure 5.146: DhKrn-20 created by R, Bird and signed in 1982 ............................................... 374 Figure 5.147: Two of the modern solid spray painted images at DgKl-2 ................................ 374 Figure 5.148: The third modern image which is solid at DgKl-2 .............................................. 375 Figure 5.149: The modern hollow spray painted image at DgKl-2 ........................................... 375 Figure 5.150: Modern spray paint image at DhKrn-20 ............................................................... 376 Figure 6.1: DhKm-l photographed August 27'h 2003 ................................................................ 398 Figure 6.2: Annotated photograph by Colson of the holes which are called caves at DgKI-2

in the rock above the water level.. ................................................................................... .403 Figure 6.3: Inside the cave at DgKl-2 ........................................................................................... .403 Figure 6.4: Map of the pictograph sites that have deep holes in 2001 .................................... .404 Figure 6.5: Map of pictograph sites with large cracks in 2001 .................................................. .405 Figure 6.6: Map of pictograph sites with crevices in 2001 ........................................................ .406 Figure 6.7: Map of pictograph sites with overhangs in 2001 ................................................... ..407 Figure 6.8: Map of pictograph sites with rock shelves, or benches or ledges in 2001 .......... .409 Figure 6.9: Map of pictograph sites with rocks at their base in 2001 ...................................... .411 Figure 6.10: DiKm- 50 on Horseshoe Island, Whitefish Bay ................................................... .412 Figure 6.11: The black marks on the surface of the rock's surface ........................... ..413 Figure 6.12: Sites with smears ......................................................................................................... 419 Figure 6.13: Sites with blobs ........................................................................................................... 421 Figure 6:14: Sites with unidentifiable shapes .............................................................................. .423 Figure 6.15: Sites with vertical stick figures ................................................................................. .424 Figure 6.16: Sites that the shape of the 'upper torso of a vertical stick figure' ...................... .425 Figure 6.17: Sites that had the shape of hand prints .................................................................. .425 Figure 6.18: Location of sites that had both a left and a right hand print shape ................... .426 Figure 6.19: Sites with shapes of loosely categorised creatures ............................................... ..427 Figure 6.20: An example of a shape called 'one vertical and one horizontal short line that

cross each other at ninety degrees' ................................................................................... 430 Figure 6.21: Sites with one vertical and one horizontal short line that cross each other at

ninety degrees ...................................................................................................................... 431 Figure 6.22: An example of a shape called 'one vertical and one horizontal short line that

cross each other at ninety degrees with short lines at the end of each of the vertical and horizontallines' ........................................................................................................... 431

Figure 6.23: Sites with the shape called one vertical and one horizontal short line cross each other at ninety degree angle with short lines at the end of each of the vertical and horizontallines .................................................................................................................... 432

Figure 6.24: Sites with groups of four diagonallines ................................................................. .433 Figure 6.25: Sites with shapes called 'three lines joined at one end' ........................................ .434 Figure 7.1: The left hand part of scroll number 1. Courtesy of Lake of the Woods Museum,

Kenora, Ontario, Canada ................................................................................................... 452 Figure 7.2: The right hand part of scroll number 1. Courtes)' of Lake of the Woods

Museum, Kenora, Ontario, Canada ................................................................................ .453 Figure 7.3: One of the scrolls that Densmore photographed. In: Densmore, F. 1910.

Chippewa Music I. Washington Government Printing Office. Srnithsonian Institution, Bureau of American Ethnology. Bulletin 45. p. 110 ................................ .453

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Figure 7.4: One of the serolls that Densmore photographed. In: Densmore, F. 1910. Chippewa Music I. Washington Govemment Printing Office. Smithsonian Institution, Bureau of Ameriean Ethnology. Bulletin 45. p. 110 ................................ .453

Figure 7.5: The scroll published by Dewdney in 1970. In: Dewdney, S. 1970c. Ecologicai Notes on the Objiway shaman-artist. Artscanada. August: 17-28. P.: 27-28 .............. .454

Figure 7.6: Dewdney's tracing of the scroll in figure 7.5. In: Dewdney, S. 1975b. The Sacred Scroils of the Southem Ojibwqy. Toronto and Buffalo: University of Toronto Press: Figure 146 Song record with herbaI references (ROM -3), on p. 141 ....................... .455

Figure 7.7: The nine differences between the Dewdney's drawing and the original seroll .. .455 Figure 7.8: Scroll number 2 annotated by Colson from left to right in 2005 ......................... .464 Figure 7.9: Mnemonic for the Song of Good Medicine. In: Densmore, F. 1910. Chippewa

Music 1. Washington Government Printing Office. Smithsonian Institution, Bureau of American Ethnology. Bulletin 45. p. 1 00 ....................................................................... .464

Figure 7.10: Mnemonic for the Song of the Crab Medicine Bag. In: Densmore, F. 1910. Chippewa Music 1. Washington Government Printing Office. Smithsoruan Institution, Bureau of American Ethnology. Bulletin 45. p. 102 ..................................................... .464

Figure 7.11: Mnemonie for the Song of the Fire-Charm. In: Densmore, F. 1910. ChippelJJa Music 1. Washington Government Printing Office. Smithsoruan Institution, Bureau of American Ethnology. Bulletin 45. p. 103 ....................................................................... .465

Figure 7.12: Scroll number 3 annotated by Colson in 2005. In: Densmore, F. 1910. Chippewa Music 1. Washington Government Printing Office. Smithsonian Institution, Bureau of Ameriean Ethnology. Bulletin 45. p. 106 ....................................................................... .465·

Figure 7.13: Mnemonic for the Song of the Owl Medicine. In: Densmore, F. 1910. Chippe1va Music 1. Washington Government Printing Office. Smithsoruan Institution, Bureau of American Ethnology. Bulletin 45. p. 1 04 ....................................................................... .465

Figure 7.14: Mnemonic for the Song of Starvation. In: Densmore, F. 1910. Chippewa Music 1. Washington Govemment Printing Office. Smithsoruan Institution, Bureau of American Ethnology. Bulletin 45. p.l 04 ........................................................................ .466

Figure 7.15: Mnemonic for the Song of the Man who Succeeded. In: Densmore, F. 1910. Chippewa Music 1. Washington Govemment Printing Office. Smithsonian Institution, Bureau of American Ethnology. Bulletin 45. p. 98 ....................................................... .466

Figure 7.16: Seroll number 4 annotated by Coison in 2005 ...................................................... .467 Figure 7.17: The shapes at DiKm-4 according to Ann Seymour ............................................. .468 Figure 7.18: The turde, snake, and the first lattice discussed by Seymour at DhKm-3 ........ .469 Figure 7.19: The thunderbird, line, handprint, lattice, and the human figure with hands raised

upwards at DhKm-3 identified by Seymour. ................................................................. .470 Figure 7.20: The annotated photographs of images at DhKn-l .............................................. .471 Figure 7.21: An annotated photograph ofDhKo-l ................................................................... .471

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List of Tables:

Table 1.1: Sequence in which approaches must be utilised ............................................................ 6 Table 6.1: Hierarchical Cluster Analysis - dendrogram using Average Linkage (Between

Groups) using Euclidean distance method to establish whether a relationship exists between the sites and the different features .................................................................. .401

Table 6.2 Hierarchical Cluster Analysis - dendrogram using Average Linkage (Between Groups) using Pearson correlation method to establish whether a relationship exists between the sites and the different features .................................................................. .401

Table 6.3 Hierarchical Cluster Analysis - dendrogram using Average Linkage (Between Groups) using Euclidean distance method to determine the nature of the relationship between smears and sites ................................................................................................. 420

Table 6.4: Hierarchical Cluster Analysis - dendrogram using Average Linkage (Between Groups) using Euclidean distance method to determine the nature of the relationship between smears and sites .................................................................................................. 420

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,~.

Chapter 1 - Introduction

While most people who study rock image sites tend to be interested in the meaning

of images, much more empirical information can be obtained about these images and their

physical location. Very little of the work done in the past on rock image sites has been

systematic. Hence, in this thesis l will address the dearth of detailed information on the

images and their context. l will subsequently suggest a new approach to studying rock images

that is as systematic, rigorous and objective as possible using a group of sites in the Canadian

Shield. The goal of this thesis is to rigorously conduct a detailed and thorough examination

of the images of the pictograph sites in the Lake of the Woods region to (a) identify the

possible vocabulary of images, (b) determine whether combinator)' mIes exist, (c)

reconstitute thelife history of each site, and (d) ascertain whether the images can be related

to other images outside the rock image sites to de termine if this can provide information

about the meaning(s) of the rock images.

Where are these sites?

The rock image sites of the Lake of the Woods region exhibit traits evident in rock

Image studies in other parts of the world. Here, as elsewhere, the choice of theoretical

approach influences the fieldwork, analysis, and search for meaning. This study is based on

data collected during three months of fieldwork conducted on the pictographs in the Lake of

the Woods in 2001. Petroglyph sites were not included in this study because the high water

levels in the field season of 2001 inundated these sites. l did not examine petroforms since

this study only concerns images on rocks and not images created using rocks. Only the

pictograph sites were examined.

l chose the sites of the Lake of the Woods area, in Northwestern Ontario, because

they appear representative of the data resulting from the archaeological surveys conducted

on the rock images of the Canadian Shield. The map below, in figure 1.1, indicates the

physicallocation of the Lake of the Woods with respect to the Great Lakes and Hudson Bay.

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,-MANtTOBA ~~~4

(

:

/ ......... . .'

.,,,,,CO

lKE OF THE WOODS

.' /

Figure 1.1: Physical Location of the Lake of the Woods

QUE BEC

The majority of the scholars interestèd in rock images of the Canadian Shield (for

example: Dewdney and Kidd 1962, 1967, and 1975; Fox 1974; Lanoue 1989; Lambert 1983,

1985, n.d.; Molyneaux 1975; Rajnovich 1989, 1994; Reid 1977) examined the sites in the Lake

of the Woods from 1885 (Lawson 1885) onwards. The individu al pictograph sites associated

with this lake vary in the number and range of their images. Most of the known pictographs

occur at the base of vertical granitic rock walls, either immediately beside the water or several

metres from the water's surface. None of these sites can be dated using absolute·

chronometrie techniques. l based ml' research on archaeological experience gained from

conducting fieldwork in the Canadian Shield region since 1990.

My views on rock image studies in general

In preparation for my thesis, l carried out a comparative survey of rock image studies

around the world. l examined the effects both of different theoretical approaches, and the

interpretative themes used by each scholar. The term 'rock art' is applied world-wide to

images that are placed on the surfaces of rocks. 1t occurs in many different places and

settings: Australian rock shelters, the surfaces of boulders in the Jordanian desert, vertical

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r---..

rock faces or rock outcrops on the Canadian Shield, the sides of the stone passages of New

Grange in Ireland, and the walls of deep caves in France and Spain. 'Rock art' also covers

features created using rocks of different sizes to produce 'rock,' or 'boulder alignments.'

The term 'art' is problematic because it suggests that these images have primarily a

decorative value and no intrinsic value or meaning of their own. lt also implies classification

of these images according to Western notions of high or low art, or, perhaps, a craft. These

terms have loaded meanings, since they impose the analyst's conventional values. Rock

images should not be considered within such a perspective, since, evidently, the cultural

context of the 'reader' or 'viewer' influences perception and classification. This prejudgement

affects how images are understood (Blocker 1994; Conkey 1987; Price 1989).

Not:withstanding these continuaI dangers, scholars interested in the se images

continue to use the term 'art'. Images similar to those found on rock surfaces of the

Canadian Shield are encountered in other cultural contexts (Densmore 1974 [1928]; Phillips

1999; Ritzenthaler and Ritzenthaler 1970). The designation of all these sorts of images as

'art', 'folk art' or 'hanrucrafts' has created problems for their analysts.\ There are no clearly

delineated guidelines indicating the way in which the meaning of such images should be

unpacked. Yet, whether or not these images were intended as 'art', they are a form of

communication, and, therefore, they challenge us to understand them. l rusagree with

Whitley's (2001: 22-23) argument that the term 'rock art' should not be changed since a

western intellectual tradition has used it for over one hundred years. The use of a term for a

long period of time should not justify its continued usage, particularly if the users

acknowledge that problems exist with it. Continuing such a practice or 'tradition' merely

Ieaves the arena open for continuaI disputes and discussions over whether these images are

art or not. l therefore propose that these representations should be termed rock images, or

petroglyphs and pictographs.

Rock image sites cannot be studied using the same techniques as are applied to other

archaeologicai sites. The theoretical approaches used and the questions asked may be the

same but the data sources are rarucally different and generally far more limited. These images

cannot be excavated using the techniques for recovering, cataloguing, and analysing data that

1 Frank (2000: 1-18) in her introduction clearly surrimarises the intellectual arguments, and debates concerning the development of the different theories that have led to different objects and images being termed "decorative" or "flne" arts or handicrafts. Dondis (1973), Gombrich (1984), Lay ton (1991), Morphy (1989), and Rapaport (1997) considered the question of what can be defmed as art, crafts, and visualliteracy. Haselberger (1961) proposed a method for dealing with ethnological art.

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archaeologists apply to 'conventional' archaeological sit~s. The area surrounding such images

may be excavated but the physical context of the site often provides little or no information

about the meaning(s) of the images themselves.

The subjective beliefs and ideas held by the people who created these images did

more to shape them than technological processes or the economic or political systems in

which these people lived. Therefore, the archaeologist must rely to an unusual degree on a

range of non-archaeological sources in order to establish the meaning of the images. It is

very difficult to access this information for a group whose past is available only through the

archaeological record. The difficulties in accessing the symbolic knowledge of a group of

people through the inherent attributes and physicallocation of such images may explain why

these sites have often been ignored, or merely described, in contrast to similar images found

on birch bark scrolls. Fieldwork and archivaI work must be considered as equally important

in this study, since information must be drawn from a wide range of disciplines, induding

archaeology, anthropology, history, art history, geology, and geography.

It is time to re-examine the fundamental daims regarding rock images and their

study. Rock images have fallen into 'the domain of archaeology because they are found

outside on the surface of rocks, and not on clothes, canvases, portable objects or documents

in archives. My own fieldwork has demonstrated that, contrary to common beliefs, sites in

the Lake of the Woods region did not always exist in conjunction with a body of water. It

also shows that rock images occasionally are found in caves rather than on cliff faces.

Suppositions about the known physicallocations of the pictographs have had a fundamental

influence upon their discovery, and how and by whom they are interpreted (see Brown and

Brightman 1988: 55-56; Dewdney and Kidd 1962: 13-14; Kohl 1985 (1860]: 415; Wheeler

1977a, 1977b, 1979; Rajnovich 1989: 185-186).

The influence of divergent disciplinary perspectives and paradigms of thought upon

the analysis of images in general must be understood. The contrasting ways in which images

are regarded has affected their interpretation.

The use of informants

The question exists whether or not to rely upon informants for information

regarding both the name and meaning of a shape. l decided not to rely on informants for

ethnographic information for several reasons. Firstly, several archaeologists in Northwestern

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Ontario informed me that archaeologists do not have a good relationship with the local

indigenous peoples. lt would be very diffic~lt, if not impossible, to consider undertaking

ethnographie fieldwork in conjunction with archaeological fieldwork. In addition, 1

discovered that information regarding the meaning of these images is a politically sensitive

topie. Indeed, 1 established a connection between sorne of the new images at DgKl-2 and a

court case regarding charges of incest at one of the reserves in the Lake of the Woods.

However, W. A. Ross, who was the regional archaeologist in 2001, asked me not to provide

any more details regarding the images and why they were created (Ross, Pers. Comm. July

and August 2001). My third reason is that indigenous peoples currently living on the local

reserves are currently using the rock image sites, in severalland daims, as evidence that they

have always lived in the Lake of the \Voods region. Indeed, DgKm-1, in Splitrock Bay near

Blueberry Island in Sabaskong Bay, was to be used in 2001 as a means of claiming that the

Ojibwa had always lived in this region. Finally, anthropological evidence suggests that the

local inhabitants may not always have" spoken Ojibwa. The first section of Chapter II

addresses the problem of identifying who spoke Cree and Ojibwa in the large region which

includes the Lake of the Woods.

What is an interpretive approach?

Archaeologists, unlike scholars from other disciplines, often cannot utilise tex tuaI

data. Instead, they must interpret how different groups of people thought, behaved, and

interacted by drawing upon the remaining material evidence of these groups. Five different

interpretive approaches exist in archaeology: culture-historical, contextual, intuitive,

analogical, and homological. Archaeologists use these approaches to infer human behaviour

and meaning from archaeological data. Each approach dictates the types of questions used,

and determines the levels of understanding obtained about whatever archaeological evidence

is being considered. Analysts must examine the same data using these different approaches

sequentially, since this increases the potential quantity of information gained concerning

these images. The different theoretical approaches are complementary rather than exclusive,

and should be employed in a definite order (fable 1).

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CULTURE-HISTORY

Levell: Establishes the shape, location, and date of the images.

j CONTEXTUAL

Level 2: Relates various types of empirical information to the site where they were

found, and considers a broad set of associations and relations among the images themselves,

and between the images and their physical settings. A contextual approach involves a search

for patterns relating different images and combinations of images within sites.

l INTUITIVE and/or ANALOGICAL and/or HOMOLOGICAL

Level 3: Assigns meanings to images on the basis of three methodologies which are

employed together or separately.

Table 1.1 Sequence in which approaches must be utilised

The culture-history approach (Levell):

Archaeologists ought to apply the culture-history approach prior to interpreting these

images because it permits them to establish the form, date, and location of the images. This

approach provides archaeologists with the basic data that they need to perform higher-Ievel

operations. Archaeologists should concentrate on assembling detailed information about

each individual site and consider each image as a separate entity at this level.

The contextual approach (Level 2):

Those wishing to connect the culture-historical information with the totality of the

images and the natural features of the site itself subsequently take the contextual approach. l

use the word contextual in a broader and less technical sense than Hodder (1991) intended.

At this level, the scholar can propose low-Ievel generalisations about relating their data,

without searching for explanations of what these data mean. The contextual approach

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permits archaeologists ta consider a broader set of associations and relationships among the

images themselves, the images and rock surfaces, and the generallocation of the site. Prior to

proceeding to Level 3, it is imperative that scholars search for patterns in their data.

Archaeologists must use this approach before attempting to assign meaning to images. Sin ce

relatively little work has been devoted to studying problems of this sort, it is evident that

archaeologists are more interested in assigning meanings or explanations to the images

themselves, or to groups of images, than in systematically analysing the images and their

formaI relationships. Archaeologists seeking to assign meanings to different images must

employ the analogical, the homological, or the intuitive (narrative or constructivist) approach,

or a combination of these.

The intuitive approach (Leve! 3):

The intuitive (narrative, constructivist, or so called 'humanist') approach associated

with post-processual archaeology developed as a reaction against the positivism of the

processual archaeologists during the 1970s and 1980s. Hodder (1985) had problems with

many of the key te nets of positivism and processualism. He, as weIl as Shanks, Tilley, Ucko,

and Thomas, were concerned by the lack of interest with cognitive factors. Yet, it was

Hodder's students, Shanks and Tilley, who really developed this approach into a force with

which to be reckoned. For the extreme relativist, there is no possibility that one person's

interpretation is better than another's. These scholars maintain that it is impossible to

demonstrate empirically that one interpretation is right while another interpretation is wrong.

The scholar frequently reaches conclusions based upon thought processes or information

known only to him. They argue that, because gender, class, cultural background, and racial

prejudices so strongly influence the interpretation of archaeological data, it is difficult to

accept such interpretations. Strong relativists and archaeologists, such as Thomas, Shanks,

and Tilley, also reason that it is only possible to understand segments of a culture in relation

to its entirety. Each culture must be understood hermeneutically because it constitutes a

unique system of independently defined entities. Meaning, they reason, must be contextual,

especially in historical hermeneutics, if the archaeologist is determined to understand another

world. Hence the development of the fourfold hermeneutic circle: archaeologists must work

through the hermeneutic of their own discipline first, then the hermeneutic where they must

operate and live as human beings, thirdly the hermeneutic of understanding a dramatically

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different culture from their own, and finally the hermeneutic of moving between the past

and the present (Shanks and Tilley 1994: 107-108).

Shanks and Tilley (1987: 76) asserted that universals did not exist because culture and

rustory both represent contingency. Cross-cultural studies could be undertaken only by

"translating" precisely how members of the culture being studied understood that culture.

Bence the difficulty in undertaking any type of cross-cultural analysis. Cross-cultural

comparisons are rughly problematic because things only have meanings within their own

cultures. Strong relativists believe that cultures are incomprehensible to anyone outside of

that culture.

So, what can we conclude?

Weak relativists, such as Wylie, stress that archaeological interpretation cannot be

free from bias. Weak relativists contend that beliefs held by individu al archaeologists

influence how they choose and excavate a site, and how they identify, classify and interpret

artefacts. They argue that what passes as an archaeologist's interpretation is influenced by her

beliefs and, therefore, it is difficult to be certain about that interpretation's validity. This is

because the archaeologist, with her bias, unconsciously has the power to dis tort

interpretations.

The intuitive or narrative approach is popular among petroglyph and pictograph

scholars because it enables them to draw conclusions, even when there is a paucity of

detailed textual records pertaining to the images' meaning. The question remains whether

trus position is usefuL The strong relativists load their theoretical discussions with tortuous

vocabulary. Their texts invariably claim a great deal but, in reality, fail to advance beyond the

subjective. The tone of these interpretations is always authoritative and assertive but they

remain exercises in "navel gazing" or introspection. Readers, who cannot verify how

interpreters reached their conclusions, find themselves at the whim of each scholar's

intuition. The applications of trus approach cannot be duplicated, since researchers rarely

explain how their conclusions were achieved. If an archaeologist uses the intuitive approach,

it is not feasible for another archaeologist to apply any of his interpretations in another

context. Therefore, a scholar interested in establishing the meaning of rock images in a more

rigorous and persuasive fasruon should adopt the analogical or homological approach (see

Table 1).

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The analogical approach (Leve1 3):

The analogical approach, associated with processual archaeology, was a reaction by

positivists against the culture-history approach during the 1960s. Proponents argued that

behaviour was predictable from material culture because many uniform connections existed

between the various components of socio-cultural systems, material culture, and hum an

behaviour. As Lyman and O'Brien (2001: 303) observed, the use of general comparative

analogies reflected the theory of orthogenesis. Yet general comparative analogies were not

new in the 1960s, sin ce archaeologists had used them, as weil as homologies (specific

historical analogies), to examine the archaeological record of North America during the late

nineteenth and the first part of the twentieth century (ibid.: 304).

Biologists define analogies as similar features of different specles without close

evolutionary relations. The similarities have resulted from natural selection operating to adapt

different species to a similar environment (Abercrombie, Hickman and Johnson 1985: 20).

An archaeological analogy is a likeness or partiallikeness assumed to exist as a consequence

of convergent development under comparable conditions. Interpretation using analogies

allows scholars to use strong cross-cultural regularities between behaviour and material

culture in systemic contexts to attribute behavioural correlates to material remains recovered

from archaeological contexts.

Binford (1977: 288) maintained that ethnographic analogies are useful sources of

middle-range generalisations. An analogical interpretation is based upon the existence of

strong functional correlations between specific aspects of behaviour and specifie aspects of

material culture. Given such a correlation, the presence of similar material culture in the

archaeological record allows an archaeologist to presume that similar or associated

behaviours existed in the pasto Watson, LeBlanc and Redman (1971: 51) argued that

analogies provided archaeologists with the "richest sources of hypothesis" available.

What are the types of bridging arguments used for justifying an analogical

interpretation?

Scholars who privilege an analogie al approach conclude that it is only worth

employing regularities in human behaviour that are universal. They presume that correlations

exist between past and present day cognitive and behavioural capabilities of human beings.

Proponents assume that, if similar behavioural characteristics can be established between

specifie aspects of material culture and behaviour in the modern (present day) world,

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scholars can extend them to cover the same, or similar aspects of material culture in the

archaeological record (Binford 1981). Scholars adopting analogical approaches use universal

generalisations, rather than concepts specifie to individu al or historically related cultures. It is

impossible to include the idiosyncratic facets of an historical tradition if analysts consider

only universal correlations relevant.

The homological approach (Leve13):

An archaeological homology is a similarity in two or more cultures occurring as the

result of shared historical origin unobscured by adaptation to different cultural

environments. Archaeological homologies result from diffusion as well as common descent,

they differ from biologie al ones. In biology, reproductive isolation ensures that homologies

occur only among species descended from a common ancestor. Consequently, homological

similarities imply evolutionary relationships among organisms (Abercrombie, Hickman, and

Johnson 1985: 145).

Scholars establish homologies by tracing cultural continuities through time in a single,

or a series of historically related cultural traditions. Interpretations employing homologies

frequently utilise the direct historical approach. This approach identifies parallels between

culturally specifie beliefs and their material expressions during the eariy historical period, and

employs material culture to trace these beliefs back into prehistoric times. The bridging

arguments for establishing homologies between the present and the past are culturally

specifie. According to Watson, LeBlanc, and Redman (1971: 50), homologies are

advantageous in regions of strong cultural continuity and where the same techniques and

implements have been utilised for a long period of time. Written records, oral heritage, and

ethnographie observations are probably the strongest types of evidence used when devising

bridging arguments (Trigger 1995: 452). Scholars exploit these materials to establish which

beliefs existed in specifie cultures.

The direct historical approach connects archaeology with other disciplines, providing

information concerning the practices and beliefs of specifie, or groups of, historically related

societies. By relying on a wide variety of evidence, archaeologists can attempt to establish

whether continuity exists in the practices and beliefs in question. The homological approach

allows in-depth analysis of a specifie group and its material culture. It permits archaeologists

to consider what human beings might have thought about in the past, and the meaning of

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specific symbols and objects. It may be possible to determine that similar images used in a

variety of different mediums held similar meanings. Scholars intending to use homological

interpretations must have a detailed understanding of the skills required to use

archaeological, historical, and ethnographic materials from the region in question. These

materials are multidisciplinary in nature. Those taking this approach must verify how cultures

establish entrenched beliefs, and how susceptible these are to evaluation in terms of that

culture. Any scholar intending to use the homological approach must be aware of different

cultural perspectives. He must acknowledge that using the direct historical approach is

neither straightforward nor simple. Continuity of form does not necessarily imply continuity

of meaning. Meaning can also change, especially since kons tend to be polysemie. Material

symbols can ob tain new meanings and become examples of what Davis (1992: 25) called an

"iconographic disjunction." Continuity or discontinuity in beliefs over time is not correlated

simply with material culture.

In sum, culture history and the contextual approach seek to answer questions such as

what mate rial there is to study, when images were created, and who created them. The

analogical, homological, and intuitive approaches seek to ascertain for what purposes they

were created, and what their meanings were to their creator(s). Inadequacies in each of the

first two stages limit the effectiveness of the stage of analysis. Therefore, an archaeologist

studying a rock image site must first implement the culture-historical approach, then the

contextual approach, and finally the intuitive, analogical or homological approach.

The debate between the "lumpers" and the "splitters"

As discussed earlier in this chapter the philosophical approach dicta tes the questions

asked of and applied to the data. But the taxonomy applied by the archaeologist determines

the degree of resolution or the level of aggregation used to collect, describe, and classify the

data, which in turn affects the conclusions. In archaeology, two methods of classifying

information and creating taxonomies are prevalent: those of "lump ers" and "splitters". It is

important to understand the differences between splitters and lumpers because it affects how

archaeological evidence and information is drawn upon and used. It affects how the origins

of early man are considered. Indeed, Clark (1999: 2029-2032) argued that archaeological

research concerned with the examination of modern human origins in Europe was

epistemologically naïve. It could he maintained, be summarised, in terms of two paradigms:

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/~"

the replacement and the continuity paradigm. What is important about this debate for my

argument is that both paradigms define and consider variables that are used by both models

in distinctly different manners. Scholars utilise different taxonomies and phylogenies

according to the paradigm that they invoke. Therefore advocates of the replacement

paradigm use 'splitter' taxonomies and dendritic phylogenies and argue that a distinction

exists between archaic Homo sapiens and neandertals (ibid.). Advocates of the continuity

paradigm employ "lumper" taxonomies and reticulate phylogenies. These researchers also do

not distinguish between archaic Homo sapiens and neandertals because they maintain that

the neandertals were one of several geographical clades that existed amongst archaic Homo

sapiens (ibid.). This split between lumpers and splitters is not unique to this discussion sin ce

it occurs exists in other discussions in archaeology as weIl as in other disciplines (see Hall and

Chase-Dunn 1993; Lieberman, Wood, and Philbeam 1996; Nurse 1997).

Essentially people termed "lumpers" look for similarities and group whatever is being

classified according to whether they share a few major characteristics, and thus work with a

limited number of categories. People called "splitters" classify things into different groups

based on minor characteristics and thus use a finer categorization. l had during the initial

phases of my research, as discussed in chapter IV, used the VIPs software to determine the

physical nature and the boundaries of each image. It became clear that the images at aIl of the

pictograph sites were not solid and physically different from each other once closely

examined. This argument that the images are different is easier to understand if the example

of the 'crescent' is used. This shape occurred twelve times at seven sites: DgKl-l, DgI<J-2,

DhKm-S, DiKn-l, DjKn-l, DiKm-3, and DiKm-S1. One could argue that they should aIl be

loosely categorised as crescents because if they are described according to each of their

physical attributes, a different technique of grouping them emerges. Each crescent below, in

figure 1.2, is slightly different.

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A vertical crescent at DgKl-2

~ ..

Two horizontal crescents at DgKl-l

A horizontal crescent at DiKm-51

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A horizontal crescent and a diagonal crescent at DhKm-5

Two horizontal cres cents at DjKn-l.

Two horizontal crescents at DiKm-3

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Figure 1.2 Examples of shapes loosely categorised as 'crescents' and the sites that they come from in the Lake of the Woods.

It should be evident from these photographs above (figure 1.2) that the red images have

suffered from the passage of time and numerous climatic changes. Sorne of them are quite

pale and difficult to see. Furthermore, none of the images is probably exactly the same image

that it was when originaIly created. Sin ce aIl of the se images were clearly different from each

other in sorne respect, the "splitter" approach was utilised when the data was described

rather than the "lumper" approach. A nested classification system was attempted and it is for

this reason that each type of shape was examined in loose groups. Therefore each shape was

examined as a shape and loosely categorised as type within a specific group so as to try to

find general patterns. Shapes could be loosely categorised as a type within that larger group.

Therefore loosely categorised shapes could be compared with distributions of other loosely

categorised shapes. As discussed in Chapter IV in considerable detail it is important that the

archaeologist should describe, not interpret, the evidence when recording a rock image site.

This operation involves thinking very carefuIly about how one describes images, since any

description will affect subsequent analysis. This should explain why groups are referred to in

Chapters V, VI, and VII as shapes loosely categorised as types of 'crescents' for example. But

it was discovered when the data was analysed and discussed in Chapter VI that using a nested

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classification system was not possible because of the variability of the data. This discovery is

supported by the results presented in the dendrograms in Appendix 15.

The structure of this thesis:

This thesis has seven chapters, beginning with this introduction.

Chapter II discusses the regional setting of the pictograph sites examined. This

chapter will consider the ethnicity of the people who lived in this region, establish which

ethnic group was responsible for the creation of these images, and determine which bodies

of ethnographic evidence can be drawn upon when the question of these images' meaning

arises. This chapter ends with a discussion of the range of images used by the Aigonquian­

speaking peoples and the Assiniboine to establish whether it is possible to examine these

images as a means of communication.

Chapter III presents and discusses earlier research on the pictograph and petroglyph

sites in the Lake of the Woods area.

Chapter IV explains the basis for my decision-making while conducting fieldwork,

and how l identified and classified the images found. My goal was to systematically collect

detailed information about rock image sites over a portion of the Canadian Shield in order to

better understand the nature of the available evidence.

Subsequent chapters deal with the archaeological data according to each of the

approaches that must be applied to this data as outlined in Chapter 1. Therefore Chapter V

applies the culture-historical approach to this data, and seeks to establish the total range of

the images. Chapter VI presents the conclusions that are drawn after applying the contextual

approach, and considers whether combinatory rules exist regarding the relation of the

different sorts of images to one another. Chapter VII uses mainly the homological approach

to consider how to establish the meaning of these images, and whether they are related to

other images outside the Lake of the Woods rock image sites. Chapter VIII summarises the

findings, discusses whether and if the goals established at the beginning of the thesis were

achieved, considers the theoretical and methodological implications of this research, and

posits some thoughts for future research.

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Chapter II: Lake of the Woods: Regional Setting of the Sites

This chapter discusses the regional setting of the pictograph sites that this thesis

examines. It considers the ethnicity of the people who lived in this region, hence, which

ethnic group created these images. It aims to determine which body of ethnographic

evidence can be drawn on when the question of the meaning of these images arises.

This chapter has three sections grouped according to different factors. The first

section examines how the physical geography, geology, and climate influenced the

production and survival of rock image sites as well as the history, ethnographic record, and

the physical anthropology of the peoples who lived in the Lake of the Woods area located

between Lakes Winnipeg and Superior. The second part considers the debates about the

history and the ethnography of the indigenous people who lived there. Problems include: (a)

the inability to create a clear chronological framework for the cultural and ethnic identities of

former inhabitants; (b) understanding the archaeological record of the Boreal Forest; (c) the

unresolved debate between historians and archaeologists concerning the ethnic identification

of those peoples who were in early contact with the Europeans; and finally (d) whether

biological evidence can help resolve the problem of the precise ethnic identity of these

peoples. The third section of this chapter has two goals. The first is to establish the ethnicity

of all the different images and the objects upon which they exist, so that it can be determined

which images the Algonquian-speaking peoples created, and which the Assiniboine made.

The second goal is to examine these images as a means of communication, since similar

images were used throughout this geographical region.

Section 1 - Geohistory and geography of the region.

(a) Geology

Climate, soils, physical geography, and hydrology have influenced the settlement

patterns, movements, and the size of populations inhabiting the Boreal Forest and the Great

Lakes-St. Lawrence Forest. The Lake of the Woods is part of a watershed that flows from

the Boundary Waters into the Winnipeg River and northwards to the Arctic Ocean. It is a

remnant of glacial Lake Agassiz, and has two distinct parts. The bedrock geology and glacial

action have caused the differences that distinguish the northern and southern portions of

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Lake of the Woods. Therefore, the history of the geology, the soils, climate, and hydrology

must be discussed.

This region is also part of the Canadian, or Precambrian Shield, one of the major

physiographic units of the North American continent (Gardner 1981: 6). The effects of

glaciation on the Canadian Shield are evident. Both thin soils and bedrock outcrops are

abundant as a consequence of much of the area being scoured by the massive ice sheets. The

sediment that does exist is glacial-Iacustrine connected to the glacial retreat (Meyer and

Hamilton 1994: 96-97). The Wisconsin maximum occurred between 19,000 and 16,000 years

BP and deglaciation occurred between 14,000 years and 12,000 BP (Bird 1973: 165 and Hare

1976: 509). The beginning of the Holocene period, about 11,000 years ago, resulted in a

sudden withdrawal of the ice margin. The ice margin coincided with the southern edge of the

Canadian Shield about 10,500 BP and vast glacial lakes such as Lake Agassiz developed

between 11,600 and 8,400 BP (Hamilton 1996: 12). Lake Agassiz covered parts of

Saskatchewan, Manitoba, Ontario, Northern Dakota, and Minnesota (Winterhalder 1983:

10). Bryson and his colleagues (1969: 8) argue that, immediately following the Cockburn

glacial phase around 8500 BP, the ice sheet rapidly disintegrated in the Hudson Bay region. A

saltwater incursion formed the Tyrrell Sea, later called Hudson Bay, which covered the area.

By 7,000 BP Lake Agassiz drained northward through the Nelson channel, into the Tyrrell

Sea (Elson 1965) . Post-glacial warming reached its maximum about 7,000 to 5,000 years ago

in the Hypsithermal Interval. Tt was warmer in this period than at present but initially it was

drier but later on it became wetter (Terasmae 1970). Wright (1976: 592) argues that this

climate period was subsequently followed by the Neoglacial, which was a period of cooling.

A climatic optimum, partially corresponding to the Neo-Atlantic episode, was

reached around AD 1090-1230, when the northern hemisphere experienced a period of

warmer weather (Bryson and Wendland 1967: 294). The climate subsequently became colder

but during the late 1400s the temperatures improved. The "Little Ice Age" occurred between

1550 and 1850 du ring which the region experienced considerably colder temperatures. Hare

and Thomas (1979) stated that between 1885 and the 1940s, the Northern Hemisphere

experienced a warming trend, so that by 1970 this region had achieved half of the post-1885

temperature gain. However, larger ranges of variability occurred in the northern regions of

Canada.

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Much of the crystalline bedrock in this region is exposed or close to the surface

(Gardner 1981). MineraIs such as silver, gold, platinum; associated sulphides of iron, copper,

zinc, and lead have been found in conjunction with the sedimentary and igneous rocks

(Minning, Cowan, Sharpe and Warman 1994: 12). Hematite, the principal constituent of iron

ore, is readily available as a primary constituent as well as a secondary product in the

sedimentary and igneous rocks of this region (Bates and Jackson 1984: 233).

Glaciers covered the Subarctic region for most of the past 20,000 years; consequently

the soil is thin and not very extensive. Chemical and biochemical breakdown and mechanical

weathering is slow in the Subarctic. Thin podzol soils coyer the Shield area leaving rock

outcrops and peat deposits. Consequently these processes affect neither the bedrock nor any

unconsolidated material to create a soil profile (Gardner 1981: 13). The soil profile typically

consists of a thick leaf mulch, a leached (ash colour) horizon, a second horizon with deposits

of organic colloids leached from the first horizon and the clays of prehistoric Lake Agassiz.

On the southern margins of the Shield, where the Boreal Forest vegetation meets that of

Great Lakes-St. Lawrence Forest, the soils become "brown-wooded and grey-wooded"

(ibid.). Both of these soils, in comparison to the podzols farther north, can be put to

agricultural use with careful management and proper drainage.

Two vastly different major forests co-exist in this region: the Boreal Forest, and the

Great Lakes-St. Lawrence forest. The Great Lakes-St. Lawrence forest occupies a large part

of northeastern North America, reaching its western extremity in southeastern Manitoba. It

covers the northern half of Minnesota and in northwestern Ontario it is found in a narrow

east-west strip extending about eighty-five kilometres north of the international border

(Meyer and Hamilton 1994: 97; Gardner 1981: 12). The softwoods found in this region

include eastern white and red pines, eastern hemlock, and yellow birch, while hardwoods

include red oak, sugar and red maples, basswood, and white elm (Rowe 1972: 11). This pine­

hardwood forest provides a variety of potential food sources including nuts, berries, and sap.

Wild rice was a major foodstuff for the peoples of the Late Prehistoric period in the Great

Lakes-St. Lawrence fore st zone. The wild rice stands, the great variety of fish (especially

sturgeon), and other aquatic animaIs were vital for survival. The sturgeon contains isinglass, a

natural binder that could have been used in the manufacture of the paint used for

pictographs. Isinglass, a transparent gelatine prepared from the air bladder of the sturgeon,

can be used as an adhesive and clarifying agent. The fauna of this forest included white-tailed

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deer, moose, woodland caribou, and waterfowl, the latter frequently found amongst the wild

rice stands.

Rowe (1972: 6) identifies the Boreal Forest as a conifer rich zone distinct from the

hardwood-rich Great Lakes-St Lawrence forest to the south and the tundra to the north. He

noted that deciduous forests decreased northwards, becoming more open in the forest­

tundra transition. The Boreal Forest is in a state of "quasi-equilibrium", since it is connected

to the summer and the winter positions of the Arctic front (Bryson 1966: 257). Long-term

variations in climatic patterning, essentially shifts in the win ter or summer positioning of the

Arctic front, cause the expansion or contraction of the Boreal Forest region (Bryson 1966).

Furthermore, the floral and faunal resources of the Boreal Forest on the Pre-Cambrian

Shield are not nearly as rich as those of the Great Lakes-St. Lawrence Forest. Winterhalder

argued that this fore st was in reality a "mosaic of vegetation habitats or patch-types" (1983:

28). This region is covered by dense spruce forest, open bogs, lichen woodlands, tundra­

covered ridge tops, alpine tundra, and wet forested depressions or river valleys (Gardner

1981: 12). According to Gardner (ibid.) and Winterhalder (1983: 32), the vegetation, under

the influence of moisture conditions, climate, soil conditions, and topography, defined a

habitat. Winterhalder (ibid.) argued that the vegetation also had an "internaI rhythm of

disturbance and succession" abetted by snow, wind, and more importantly cyclical fires that

provided the forest with a short-term historical time frame.

Fires have beneficial effects on the soils of coniferous forests since the natural rate of

decomposition is slow and the build up of litter hinders rapid plant growth (Kelsall, Telfer

and Wright 1977: 15). Forest fires enable mineraIs and other nutrients to be released for use

by other plants (ibid.). Fire increases the variety and range of plants and animaIs in an are a

making it an important factor in the creation of this mosaic community. Areas that do not

experience forest fires inevitably undergo a sharp decrease regarding both the number and

variety of their flora and fauna (ibid.: 24). Forest fires also affected the human populations of

this area. Wright (1981: 86) postulates that forest fires invariably forced inhabitants to shift

their hunting regions. This diversity of different ecological communities enables varying

levels of usable biomasses to coexist. Closed coniferous forests are examples of ecological

communities that provide limited or unusable food resources. Rich ecological communities

include aquatic areas such as rivers and lakes with wild rice, wild fowl and fish; and recently

burnt out areas undergoing colonisation by new plants and animaIs.

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Today the region between Lakes Winnipeg and Superior has up to 120 frost-free days

and its climate is considerably less harsh than the area to its north (Anfinson 1990: 150;

Meyer and Hamilton 1994: 99). Gardner (1981: 10) argues that the maximum period of frost­

free days in this northern region number between forty and sixty. Snow is an important

ecological factor in the Boreal and Great Lakes-St. Lawrence Forests, but it is far more

significant for the inhabitants of the Boreal Forest, since accumulations are heavier and snow

cover can last for at least six months. Additional significant ecological factors for this region

include the density, hardness, structure, and cover-temperatures of the snow (ibid.). The

topography, distribution and structure of vegetation, air temperature, wind speed, and wind

direction affects both the depth and the duration of the snow cover. Tt is possible that the

different ecological communities of the Boreal Forest invariably influence the movement and

activity of the snow. Gardner (1981: 10) argues that snow was an "effective mediator" for the

water and energy balances in the Subarctic.

Lakes of different sizes, bogs, and large numbers of streams and rivers covering the

Shield region drain either into the Arctic or Adantic Oceans. The Lake of the Woods, and

Red Lake, Thief Lake, and Mud Lake in Minnesota are remnants of glacial Lake Agassiz

(Anfinson 1990: 150). Rivers and lakes played a vital role in the seasonal transportation and

communication of regional inhabitants. AIthough they provided the only feasible avenues of

transport through most of the year, the freezing and breaking-up of the ice on these rivers

and lakes impeded transportation. Birch bark canoes were used in the summer months; in

winter people used snowshoes on the snow-topped ice. Food resources were closely tied to

these bodies of water, sin ce fish was a major food resource, as was caribou. Wright claimed

that humans could not have survived solely on the migra tory fowl or other seasonal

resources; therefore fish and caribou were fundamental parts of their diet (1981: 90).

Drainage patterns and large bodies of water served as focal points for setdements,

subsistence, and commercial activities.

The size of prehistoric populations is difficult to assess but was probably connected

to climate, vegetation, and the ability to travel through the region. Formulas exist based upon

ethnographic data (see Brose 1970; Leacock 1973; Rogers 1972) but they must be used with

caution, since archaeologists must extrapolate from ethnographic data without a detailed

knowledge of the conditions of the pasto

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The utilisation of aquatic foodstuffs and the fauna is difficult to gauge in this region,

since very little organic evidence survives in the highly acidic soils. Wright notes that bone is

rarely found (Wright 1981: 90), although the neutralising effects of the ash from the hearths

found at the Heron Bay site, a Laurel site on the north shore of Lake Superior, enabled bone

tools and refuse to be preserved (ibid.). It is likely that both wild rice and the resources

provided by aquatic environments were vital to the subsistence economies of Late

Prehistoric populations (Meyer and Hamilton 1994: 98).

Although Clelland's (1982) discussion focused on the fisheries of the Upper Great

Lakes region, he made some interesting observations that could be applied to the area west

of Lake Superior. He maintained that archaeologists and anthropologists have not properly

appreciated the value of the inshore fishery (ibid.: 761) and that the archaeological record

suggests an increased understanding of aquatic resource availability from the Late Archaic

period to the Late Woodland (ibid.: 777). He also postulated that, while the Late Woodlands

people resided in areas that hindered the domestication of food products because of the

short growing season, these regions had a high degree of residential stability and

concentration of population (ibid.: 756). Increased reliance on the fish may have aided this

population growth. Clelland posits that the Late Woodland peoples observed the

concentration of fish-spawning in streams, stream mouths, and coastal shallows before they

noticed that in the late autumn fish concentrated in shoals offshore (ibid.). Arthurs (1984,

1986) contended that the Laurel and Blackduck inhabitants of the Long Sault site, or

Manitou Mounds, along the Rainy River, probably relied heavily on the seasonal fish spawns.

Anfinson contended that, during the early historie period, one third of the northern

region of northern Minnesota was wet prairie, with patches of aspen and oak woodlands

(ibid.). Wild rice grew in this region and in the border lakes of northern Minnesota but not in

the Lake Superior shore region (ibid.: 150-151). Archaeologists Johnson (1969a, 1969b) and

Gibbon and Caine (1980), reasoned that the abundance of wild rice provided a stable, rich,

and perennial - if annually variable - resource base, enabling permanent large village sites.

Johnson (1969a) postulated that perhaps the populations increased between AD 1000 and

AD 1400. Johnson (1985) argued that the Cooper, Vineland and Wilford sites are examples

of such Late W oodland settlements. The type of resource utilisation practised there

permitted a large population size compared to the subsistence and settlement patterns of the

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Siouan groups, who lived in this reglOn at the time of contact and du ring most of the

"colonial period" (Whelan 1990: 82).

Gibbon and Caine (1980: 57-72) claimed that intensive harvesting of wild rice caused

a dramatic increase in population between the Middle and the Late Woodland cultures in

eastern :Minnesota. La Vérendrye wrote about the abundant wild rice in the Lake of the

Woods in a letter of 1732 sent to the Marquis de Beauharnois, Governor General of France

(Burpee 1927: 97). Rajnovich (1984: 198) asserted that this document is the first written

record of abundant wild rice in the Lake of the Woods; unfortunately, the rice crop of the

following year failed.

Using palynological evidence from Northern Ontario and Northern Minnesota,

Rajnovich determined that in the Lake of the Woods region wild rice was harvested as early

as the start of the Laurel cultural tradition (ibid.: 204). She based this conclusion on

McAndrews' (1969) analysis of the sudden increase in Gramineae pollen approximately 2450

±100 years ago. The majority of this grass pollen was identified as wild rice pollen and she

concluded that wild rice was present at the beginning of the cooler, wetter climatic stage

about 2450 years ago, or 1935 years if the chronology obtained by the sediments from Rice

Lake is used (ibid.: 1678). Rajnovich (1980a) observed that this period corresponded to the

beginning of the Laurel cultural tradition in Minnesota and the Lake of the Woods region.

She (1984: 204) asserted that the lack of archaeological evidence from local sites was

probably a consequence of recovery and identification techniques rather than evidence of "a

real lack of utilisation" (ibid.). She also concluded from examinations of the setclement

patterns of the Middle and Late Woodland periods that a tendency existed for wild rice areas

to cluster around the archaeological sites. However, she warned that this relationship must

only be viewed as tentative until confirmed by the retrieval, through the use of soil flotation

techniques, of wild rice grains in a major archaeological excavation (ibid.).

(b) Changing lake levels

The question of changing lake levels must be considered because archaeologists in

northern Ontario have traditionally found rock image sites by examining large expanses of

cliff faces along the shores of lakes and rivers. The consequences of changes in water levels

could be important for the existence and discovery of pictograph sites, since some could be

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completely or partially submerged, or exist along former waterways that have dried up after

waterways have changed.

Despite the association of pictographs with water, archaeologists have tended to

neglect the possibility that water levels fluctuate for any river or lake. They must pay

attention to the past use of the area in question and consider whether the water levels and

the shapes of the bodies of water have changed.

Lake of the Woods water levels have fluctuated over time and these changes can

affect the discovery, visibility, condition, and recording of rock image sites. Dramatic

changes in the Lake of the Woods water levels are indicated on the rock surfaces. Horizontal

bands of different shades of grey visible in the figure 2.1 below indicate the different water

levels that the lake has experienced.

Figure 2.1: etiffs in the southem end ofWhitefish Bay with c1early defined high water levels.

The photograph above (figure 2.1) was taken in late summer 2003, when the reglOn

experienced a major drought and previous high water levels were clearly visible. The topmost

and the strongest of the thin white bands visible on the granite cliffs at Whitefish Bay and

throughout the Lake of the Woods indicates the most recent highest water level. The bottom

edge of the lichen above that is the highest marker. White and Meyer (1916: 166), the chief

engineers of the survey that took place between 1913 and 1916, maintained that no exact

record existed of the length of time required for "standing water to remove lichen growth

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sufficiently to create a water mark." They argued that, based upon observations made while

surveying, a high water mark could be created within a single season. Once a mark was

created, it required a number of years to fade, since the slow lichen growth rate required

several years of lower water for it ta grow downwards "to rem ove the sharpness of the edge

of the mark" (ibid.).

The "natural outlets" of the Lake of the Woods were unchanged, according to the

local informants, until 1879 (International Joint Commission 1917: 16), when a headrace was

constructed as an overflow channel for power purposes in a depression in the extreme

western end of Portage Bay, Keewatin. In 1885, the power intake was deepened and used by

a sawing and planing mill until 1906, when the plant closed down (ibid.). In 1887-88 the

water level was changed again by the construction of the Rollerway Dam, on Tunnel Island,

at the western outlet of the Lake of the Woods (International Joint Commission 1917: 16).

Portage Bay and the western outlet were about one mile apart. This dam raised the water

level by an average of o. 45m (1.5 feet) and above the previous high water levels by O. 30 m

(1 foot) between 1893 and 1898, for which continuous water level records are available (ibid.:

17).

Before 1896 the area had suffered from low rainfall levels but it was difficult to

establish the level of the Lake of the Woods until 1899 when a gauge was set up at Warroad

(ibid.: 22 & Meyer and White 1916: 104). Between 1894 and 1895, the Norman Dam was

built in the Winnipeg River about a mile below the Rollerway (White and Meyer 1916: 21).

The effect of the Norman Dam on lake level was more marked than the Rollerway since it

raised the mean by 1.07 m (or 3.5 feet) (International Joint Commission 1917: 18). The

authors of the International Joint Commission Report noted that the increase of the levels of

the Lake before the construction of the dams was between 22.86 cm (0.9 feet) in 1899 to

1.83 m (6.0 feet) in 1913 (ibid.). White and Meyer (1916: 106) also observed, while surveying

the Lake of the Woods region, that changes occurred in the lake level by a foot or more as a

consequence of shifts in direction of the wind. Both argued that it was important to keep this

type of change in mind given the proposed regulation of the lake.

However, this region had been the subject of several previous treaties concerning

question of the changing water levels, who controlled them and who could use these bodies

of water. The most notable was the Ashburton-Webster Treaty signed in 1842 between the

governments of Great Britain and the United States which created a "workable and lasting

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boundary" between Canada and the United States (Carroll 2001: 286). Article II of this

Treaty enabled the citizens and subjects of the British Empire (Canada) and the United States

to use the region from Grand Portage, on the shore of Lake Superior, to Pigeon River

(Gibbons 1929: 8).

The International Joint Commission of the United States and Canada controls and

monitors the water level of the Lake of the Woods today. This commission was established

by Article VII signed on 11 th January 1909, of the Treaty of Ashburton-Webster, at the

request of the Dominion of Canada and the United States of America (Gibbons 1929: 8;

Keeper 1912: 3). Concern regarding the use of water resources caused the US. to pass an

Act in 1902 to report upon the condition of the water of the Lakes as weIl as the water

between the St. Lawrence River and the Atlantic Ocean. Prior to the signing of the 1909

treaty, no agreement existed regarding the use or the diversion of boundary waters or streams

crossing this international boundary (ibid.). Today, the water flows into the Lake of the

Woods from both sides of the border and its waters are used for a wide range of purposes

including power, sanitation, irrigation, navigation, and transportation. The International Joint

Commission of the United States of America and Canada uses dams to maintain the level of

the water year-round so that these activities can continue undisturbed.

The consequences of this agreement are readily evident to archaeologists. The

building of the dams, from 1888 onwards, meant that the water level rose and was

maintained. However, the increase in the water level also caused the shape of the Lake of the

Woods to change and, possibly, completely or partially submerged pictograph sites. It seems

likely that known pictographs that are visible today while sitting in a boat would have been

located physically higher up the cliff faces. Yet if the water level had fluctuated as much as

seven feet prior to keeping careful records, the positioning of images could have reflected the

differing high water levels at the time they were painted.

The geology of the rock on which the images exist must be considered because

archaeologists have argued that pictograph sites in the Precambrian Shield region always

occur on granite cliffs immediately beside water. The sites exist on granite arguably because it

is a major component of the bedrock outcrops which are visible because massive ice sheets

scoured much of the Shield. Clearly the sites occur in a locale where the geology and the

geomorphology are considerably more complex. However, none of the archaeologists have

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considered whether the geology and the geomorphology in the immediate vicinity of the site

is the same. This is a question that must be considered.

The changing water levels must be considered sin ce these affect the images both with

respect to their physical deterioration, and the ability to view and create them from a boat. It

is important to consider whether images are accessible by boat because archaeologists argue

that pictographs always are visible while sitting in a canoe and that they exist near to the edge

of the water. Clearly, a possible relationship exists between water level, the images, the

physicallocation of the sites and their immediate geology and geomorphology.

Section 2: History and ethnography.

The second part of this chapter considers the debates in the history and ethnography

of the indigenous peoples of this area in prehistoric and historical times. Four sets of

problems have been identified: (a) the inability to establish a clear framework for the cultural

and ethnic identities of those who lived here during the historic period; (b) understanding the

archaeological record of the Boreal Forest; Cc) the unresolved debate between historians and

archaeologists concerning the ethnic identification of those peoples at the time of contact

with the Europeans, and finally (d) whether bioanthropological evidence can resolve the

problems of the ethnic identity of these peoples.

To establish the ethnicity of the people who lived in this part of North America is

fundamental because anyone concerned with a homological approach to interpreting these

pictograph sites must establish which ethnic groups produced them. Knowledge of the

ethnicity of different indigenous groups at specific times assists in identifying the precise

body of data required to interpret these rock images. Unfortunately, it is difficult to identify

past ethnic groups from archaeological records. It is easier to gather information about

different ethnographie cultures from the ethnohistorical record. To determine the ethnic

identity of a group of people from a specific geographical region during the historical period

a scholar carefully consults historical records, if they exist. These records begin with the

arrivaI of the Europeans in this region, sometime in the mid-eighteenth century. The

archaeological record must be connected with the historical record in order to determine

which indigenous groups resided in a specific region at specific times. Both historians and

archaeologists have collected a vast amount of information about the peoples who resided in

this area. Many ethnohistorians also have discussed how land tenure, settlement patterns, and

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.r'.

mobility changed during the historical period (Bishop 1976; Cooper 1939; Hickerson 1966;

Rogers 1963; Rogers and Black 1976). Ali of these issues influence how archaeologists

interpret the archaeological record.

(a) Who lived in this region during the early historical times?

The first of the four problems is connected to the inability to create a clear

chronological framework regarding the "Northern Ojibwa". This ethnological question has

occupied numerous scholars (for example: Bishop 1976; Dawson 1987; Greenburg and

Morrison 1982; Schenk 1994; Valentine 1995), who have drawn on a wide range of

disciplines including history, anthropology, linguistics, and ethnohistory. Different arguments

apply, according to which documents scholars use to substantiate their conclusions.

Unfortunately, there is no agreement about a clear demarcation between the Cree

and the Ojibwa groups or who their ancestors might have been. The designation of the Oji­

Cree causes additional problems for scholars trying to establish the identity of the peoples at

the time of contact in northwestern Ontario, northern Minnesota, and southeastern

Manitoba. It is evident that individuals cali themselves Oji-Cree. This term causes confusion

both for other indigenous groups and for anthropologists, archaeologists, and historians.

Valentine (1995), in her discussion of the historical background of the Severn Ojibwa

groups, suggested why confusion might arise over the identity of the Oji-Cree. She noted

that very little historical documentation existed for the northern Ontario Ojibwa groups

(ibid.: 24). The early documents concerned with the region calied the people of this region

"Cree" and this term was understood as referring to the specific linguistic and cultural group

Cree, whether they were Moose or Swampy Cree (ibid.: 25). Valentine argued that an error

occurred here: many contemporary Severn Ojibwa cali themselves Cree, although they

recognise that their language is different from that of the Cree, who live north and east of

them in James and Hudson Bay (ibid.). The two languages, she stated, are closely related and

share many linguistic features including aspects of morphology, some discourse particles, and

some lexical items (ibid.) . Valentine noted that early historical records from the French J esuit

missionaries and the Hudson's Bay Company indicate that the Ojibwa were in the area

around Lake Superior north of Lake Huron and east to Georgian Bay (ibid.: 24). The

geographic location of these Ojibwa, she asserted, appeared to correspond with that of the

southern Ojibwa dialect. Documentation exists, Valentine observed, that the Ojibwa had

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moved westwards into Manitoba and Saskatchewan, which in turn indicated that it was the

dialectical differences between the Severn Ojibwa and the southern Ojibwa that caused the

southern Ojibwa to believe that the Severn Ojibwa dialect was a type of Cree (ibid.).

Despite the brevity of his fieldwork, Father John Cooper (1936), an anthropologist,

obtained valuable information concerning the Ojibwa and the Cree in the Lake of the

Woods. He was informed that the Ojibwa were not the original inhabitants of the area but

had driven out the Sioux (ibid.: 2). He also discovered that sorne of the older people spoke

Cree as a result of the Ojibwa-Cree mixture "of long ago" (ibid.). However, no one spoke

Sioux. One of his informants mentioned that the Ojibwa spoken in the Lake of the Woods

differed from that spoken around Lake Nipigon (ibid.).

Greenburg and Morrison (1982: 83) postulated that the individual called "La

Marteblance" by La Vérendrye in 1729 was the Cree Captain "Martin" of the Hudson's Bay

Company. They (ibid.) observed that "La Marteblance" was captain of the Lake of the

Woods Cree, who according to La Vérendrye spoke a "corrupted Cristinaux" and was allied

with the Monsoni of Rainy Lake. Greenburg and Morrison maintained this information

suggested that these Cristinaux were the same individuals who, along with the Monsoni in

1678, had taken furs to the English at Port Nelson to avoid the Ottawa middlemen who had

pillaged them on Lake Superior (Greenburg and Morrison 1982: 83-84 quoting Margry 1888

6: 30-31). Greenburg and Morrison postulated that the Lake of the Woods Cree had not

moved anywhere by the 1730s, since they came from trus part of northwestern Ontario

(Greenburg and Morrison 1982: 84 based upon Burpee 1927: 164). They argued that their

"disappearance" was made explicable by the arrivaI of the French in their lands which meant

the Cree no longer needed to travel to Fort Albany to trade (ibid.).

Both suggested that the descendants of the Lake of the Woods Cree were called

Ojibwa, based upon Warren's designation of the area as being inhabited by people of the

goose totem. Warren, writing during the nineteenth century, stated that those peoples

belonging to the goose totem lived on the remote northern boundaries of the Ojibwa

territory amongst the "Muskeegoes" and the "Bois Forts" (Warren 1984: 45). Greenburg

and Morrison did not dispute both Hickerson's (1956 and 1962) and Hallowell's (1936 and

1955) opinion that during the eighteenth century the "Ojibwa" or "Saulteaux" moved into

the prairies. Greenburg and Morrison agreed with Wheeler's hypothesis (1977b: 123) that

both groups assimilated with other Saulteaux speakers or "Cristinaux" that they met en

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.~ ..

route. Greenburg and Morrison argued this would account for the statements Cooper (1936:

2) obtained from informants during the 1930s that the older residents of the Lake of the

Woods spoke "Cree", which reflected a mixture of Ojibwa-Cree that had existed long ago.

Greenburg and Morrison's article examined the dominant hypothesis concerning the

migration and emergence of the peoples called the Northern Ojibwa. Researchers postulated,

based on documentary evidence and fieldwork amongst northern peoples, that the groups

known today as the Northern Ojibwa had inhabited the area since contact with the

Europeans (ibid.: 76-78). No migration, or population movement, had occurred sin ce, but

only a diffusion of the term "Ojibwa" to ethnic groups that at the time of contact with the

Europeans were known by a range of different names. These names included: Kilistinon or

Cree, Monsoni, Muskego, and Gens de Terres (ibid.: 76). Greenburg and Morrison offered

an alternative view of Ojibwa culture history to explain this phenomenon. These authors

asserted that the anthropologists Bishop and Hickerson and the geographer Ray had made

two "unwarranted assumptions" about the words "Kilistinon" and "Ojibwa" (ibid.: 78).

Firstly, "IZilistinon" should not be equated with contemporary Algonquians speaking the

language termed "Cree" (ibid.). Secondly, those scholars should have not equated the term

"Ojibwa" with Ojibwa-speakers (ibid.). Greenburg and Morrison argued that Bishop, Ray

and Hickerson applied "misleading and invariant linguistic and cultural categories to

historical documents" (ibid.). Greenburg and Morrison posited that the terms "IZilistinon"

and "Ojibwa" must not be taken at face value because the ethnic groups named in

seventeenth century records were ancestral to those inhabiting the same regions. They

asserted that detailed investigations of the Boreal Forest, stretching from north-central

Quebec to eastern Manitoba, would reveal that many of the hunters spoke a "mixed" dialect

of Ojibwa at the time of contact (ibid. 87).

Greenburg and Morrison suggested that the emergence of the Northern Ojibwa

could be eXplained (ibid.: 90), as it was known from historical records. They noted that La

Vérendrye stated that the groups of hunters who resided north and west of Lake Superior

spoke "corrupted Cristinaux" or "bad Saulteux" (La Vérendrye: Appendix A in Burpee

1927). Greenburg and Morrison argued that since these same people travelled to James and

Hudson Bays they were called "l(ilistinon". Greenburg and Morrison subsequently

postulated that these people started to spend their summers at Sault Ste. Marie either just

before or just after contact with the Europeans in order to fish and take part in intertribal

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trade and ceremonies (ibid.: 90-91). They agreed with Hickerson (1966) that these groups had

the opportunities to meet other peoples who lived in clan villages along the shores of Lakes

Superior and Huron, yet during the winter they returned to their own lands to hunt and trap.

Greenburg and Morrison hypothesized that during the latter half of the seventeenth century

the hunters who resided north and west of Lake Superior stopped coming to Sault Ste. Marie

because the French and English fur traders built large numbers of trading posts on Lake

Superior and Hudson Bay (1982: 91). This explained, the authors argued, Warren's (1984: 85)

observation, recorded during the nineteenth century, that the Northern "division" of the

Ojibwa, also called Muskegoes (or Muskego or Muskeegoes) and Bois Forts, had been

separated from the southern Ojibwa for at least eight generations, since neither of these

groups had been together at Sault Ste. Marie for at least two centuries. Greenburg and

Morrison (1982: 91) speculated that terms "Ojibwa" and "Saulteaux" accompanied the

Midewiwin ceremony, which Hallowell (1936) and Dewdney (1975b) posited had expanded

along the southern shores of Lake Superior, throughout the prairies and back towards Lake

Winnipeg and the headwaters of the Albany River. Furthermore, Greenburg and Morrison

argued that the only "Northern Ojibwa", who did not practice the Midewiwin ceremony,

used the Severn Ojibwa dialect and considered themselves Cree (1982: 91).

Greenburg and Morrison (ibid.: 91-92) concluded that the application of the blanket

tribal designations of "Ojibwa" or "Cree" produced either erroneous impressions of cultural

homogeneity or discreteness mas king local ecological and social variability of ethnic groups.

What occurred, in reality, was that the blanket designation "Cree" and "Ojibwa" had diffused

among a wide range of Algonquian speakers who already inhabited the Boreal Forest region

but were gradually recognised by the Europeans and therefore appeared to increase in

number over time. Greenburg and Morrison concluded that this explanation was more

consistent with "the dynarnics of population in hunting and gathering groups" (ibid.: 91).

This explanation dealt with Ray's (1974: 102) question of why "Ojibwa" hunters would settle

in regions supposedly abandoned by the "Cree" hunters who left the area because it was

depleted of fur-bearing animaIs. Greenburg and Morrison maintained that these "Cree" and

any other peoples who lived in this region had not left but had merely become "Ojibwa".

They (ibid.: 92) concluded that the use of the term "northern Ojibwa" for the peoples who

lived north and west of Lake Superior created more problems than it solved, and preferred

the term "Boreal Forest Ojibwa-Cree" or Rogers' (1963) term "Cree-Ojibwa".

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Rogers and Taylor (1981: 213), like Greenburg and Morrison, argued that insufficient

data hindered any attempts to create rigid boundaries for the area of land inhabited by the

Northern Ojibwa at any time in their history. Rogers and Taylor postulated that these

boundaries were blurred by population movements, intermarriage with surrounding groups

and cultural traits originating with other lndian groups and Europeans (ibid.). Both scholars

suggested that the peoples called Northern Ojibwa have never considered themselves as a

distinct group. Rogers and Taylor documented that many names existed that attested the

Northern Ojibwa were either a part or a small subdivision of a larger entity (ibid.) The term

ocipwe was used as a self-designation for a band that lived north of Sault Ste. Marie which

Andrew Graham, a fur trader reported in 1775 was the Nakawakuck Nation (Williams 1969:

204). Graham discovered this term from the Keischatchewan, or Plains Cree, who also told

him that these people were few in numbers, caught their own furs, were excellent beaver

hunters and caught a variety of fish. Graham (ibid.) also established that the Keischatchewan,

although their language was not very different from that spoken by the Nakawakuck Nation,

could not understand it. Rogers (1963: 65) objected to this use of information provided by

Graham's informants, postulating that, since they inhabited the coastal area between York

Factory and Fort Severn and were not Plains Cree, this term would merely imply people who

lived to the south of them. He (ibid.: 66) maintained that the term "Nakawakuck" had no

linguistic, cultural or tribal significance.

Like Greenburg and Morrison, Schenk (1994), an historian, debated the

methodological problems involved in the identification of the Ojibwa during the historie

period. She observed that most archaeological studies proceeded from two premises: (a) that

the groups called Ojibwa were originally Ojibwa and (b) that all native cultures are static.

Schenk observed that the term Ojibwa was used beyond its original boundaries in the

seventeenth century. She proposed it was possible to identify the Ojibwa based on historical

records of Ojibwa tradition, to trace the use of the names from the seventeenth century

through the early period after contact and to explain why people who were not originally

Ojibwa came to be called Ojibwa (ibid.: 395). The people, who came to be known as the

Ojibwa, were first mentioned in Du Peron's letter of 1639 as the nation of the Sault, found at

the rapids or the falls between Lake Superior and Lake Huron (Thwaites 1959 (15): 155).

During the seventeenth century Sault Ste. Marie was at the centre of a vast circumference

filled with Algonquian nations that for a long period of time behaved as separate entities

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(Schenk 1994: 403). By 1640, Le Jeune referred to the Ojibwa as the Saulteurs, meaning

those peoples who resided at the rapids (Thwaites 1959 (18): 231). The term, Saulteurs,

subsequently became the term used to refer to the Ojibwa throughout much of the French

period (Schenk 1994: 395).

Schenk maintained that, while historians, anthropologists, and archaeologists have

confused these different groups, the Ojibwa peoples themselves knew who they were. She

concluded that the extended use of this name was by outsiders and not the people

themselves, the Ojibwa and their allies calling themselves "the Anishinabeg". Hence, it is

likely that the use of this term Ojibwa is a recent phenomenon. Since these people were once

few in number, scattered over a wide area, and without an overarching political system, it is

probable that the people referred to themselves using localised names rather than one

general name. U sing a single name for small scale societies implies social cohesion of the

people involved as well as self-identity.

Several principles, Schenk argued, existed for naming Amerindian groups. Firstly, the

name varied according to time, place, and who was doing the naming. Secondly, the names

that people had for each other were often different from those given to them by outsiders.

People were either distinguished as enernies (Nadouesioux) or as allies (Algoumequin), or by

where they lived (Winnebago, Saulteur). Thirdly, Schenk argued, most Amerindians do not

even use their name, since they see no need to identify themselves as a group. They refer to

themselves as "the people". She hypothesized that names could be linguistically transformed

to the point where their original meaning was lost.

Peers, also an historian, in 1994 debated the identity of the Ojibwa and the Cree

during the early historie period. She postulated that the names utilised by Europeans were

related to the different relations between themselves and the rival European trading

companies (ibid.: xv). The French, who encountered the ancestors of the western Ojibwa at

Sault Ste. Marie, called them Saulteurs, later Saulteaux and Outchibouec, and still later

Ojibwa or Chippewa (ibid.). Peers asserted that the development of fur trade posts and

missions throughout the interior may have eroded ethnie differences between local groups

connected by kinship and trade, as well as by language and cultural practices, which in turn

may have influenced the widespread use of the terms Saulteur and Ojibwa (ibid.). Peers

contended that the term Saulteur indicated a common heritage rather than a place of origin.

Frequently the same people had different names, or different written versions of the same

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name, if they traded with both the French and the Hudson's Bay Company (ibid.: xvi). Peers

noted that the Saulteur were calied "Eecheepos" and Oachiapoia lndians" in the Fort Albany

journals of the 1720s and the 1730s. She maintained that these words "were renderings of

ocipwe or Ojibwa" whom the French had identified as the Outchibouec a hundred years

earlier (ibid.). Peers (ibid.) suggested that the Hudson's Bay Company servants used terms for

the Ojibwa which reflected the rivalry between the Hudson's Bay Company and the North

West Company. Hence, different labels, or names, were applied by the Europeans either

because other lndians calied them that, or because the Europeans grouped them according

to their own criteria of dialect, dress, and socio-economic lifestyle.

The inability to create a framework for the peoples who lived in this reglOn ln

historical times stems from two larger problems, namely a limited understanding of the

archaeological record and the continuous changes in the European naming of the people

who lived here. The names applied to the groups who lived between Lakes Superior and

Winnipeg in historical times are unreliable and reflect the various organizing principles of

missionaries, and fur traders rather than linguistic ties. Rhodes and Todd (1981: 60), two

linguists, noted that government documents listed groups by the names that each group had

officialiy been assigned. Anthropologists and linguists, they argued, in contrast, labeled

groups by the name of a group's setdement and language or cultural affiliation. lndeed, the

people that are referred to as Sioux cali themselves as either the Lakota, the Nakota, or the

Dakota. Rhodes and Todd asserted that the reconstruction of prehistoric populations and

movements solely from linguistic evidence was incredibly difficult: the nomadic hunter­

gatherer activities of the ancestors of the modern Ojibwa and the Cree created huge

problems for scholars seeking to associate a particular group with a particular point on the

map (ibid.). Goddard argued that it was impossible to determine accurately how long ago

Proto-Algonquian was spoken, although he guessed that it was between 2,500 and 3,000

years ago (1978: 586). He (ibid.) accepted Siebert's (1967) proposition that the most probable

homeland of the Proto-Algonquian language was the area between Georgian Bay and Lake

Ontario. Siebert had located this homeland by pinpointing the multiple intersections of the

names of significant species reconstructed in proto-Algonquian and the actual distributions

of those species (1967: 40).

Rhodes and Todd noted that the Proto-Algonquian language had numerous

descendants, two of which were Cree and Ojibwa (1981: 60). Both linguists maintained that

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dialect srufting in both languages was a setlous problem for anyone interested in

reconstructing prehistoric population movements using linguistic evidence. Rhodes and

Todd stated that it was possible for a group to speak a different dialect from that of their

ancestors, rendering any conclusions based on modern dialects worthless (ibid.: 64).

The final problem was the confusion caused by how anthropologists and linguists

used these terms (ibid.: 66). Linguists have problems establisrung the history of each

language, especialiy given how dialects have changed. The problems evident from the

changing of groups' names might only be resolved by the careful use of historical documents

to gain a better understanding of the synonyms that existed. Perhaps scholars should

consider an examination of the names of the different groups based upon changes in place

names over time, in a similar manner to Hartley's (1980) study of the Lake Superior region.

Continuous changes in the naming of the people who lived in this region rend ers it difficult

or impossible to de termine who lived in this region in historical times.

The examination of only one body of data exacerbates the problem. Different

arguments exist according to the type of documents used to substantiate conclusions. The

designation of the Oji-Cree causes additional problems for scholars trying to establish the

past ethnic identity of the peoples who cali themselves Oji-Cree. This term causes confusion

both for other indigenous groups and for anthropologists, archaeologists, linguists, and

historians. Although establishing the ethnicity of the different indigenous groups in this

region is problematic, it is important because it helps to indicate the ethnicity of the possible

creators of the images. This information in turn assists the researcher in identifying the body

of data required to interpret them.

(b) The unresolved debate between historians and archaeologists over ethnie

identification at the time of contact with Europeans

Historians and archaeologists have hotly debated the ethnic identification of the

peoples who lived in the Lake of the Woods region at the time of contact with Europeans

(Bishop and Smith 1975; Bishop and Ray 1976; Bishop 1976; Dawson 1977, 1987; Evans

1961; Hickerson 1966; Mayer-Oakes 1970; Rogers and Smith 1973; Wheeler 1977b; Wilford

1941, 1955; Wright 1968b, 1968c). The positions taken by scholars will be examined to

determine how and why their opinions have differed.

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Archaeologists have spent a considerable amount of time defining reccurnng

combinations of design traits on ceramics from different periods in search of typological

characteristics that have general cultural significance (see Wright 1967; Stoltman 1973; Reid

and Rajnovich 1991; Lugenbeal 1976). Archaeological research has examined the spatial and

temporal distribution of the different prerustoric cultures, foilowing the standard

archaeological practice of placing past societies in a culture-rustorical context. Historians,

unlike archaeologists, rely upon information provided about the identities and movements of

specifie peoples from written documents created by fur traders, missionaries, or explorers.

Archaeologists rely upon visible changes in the ceramic and litruc assemblages as weil

as other changes that are possibly symbolic expressions of social identity in the

archaeological record. Ceramic and litruc assemblages are especiaily important in this region

as the rest of the cultural material is destroyed by the high acidity, poor preservation, and

lack of stratigrapruc clarity of the archaeological record. The ceramic assemblage is

considered more important than the litruc one for establisrung the identity of peoples prior

to European contact because changes in the construction, materials used, and decorative

elements serve as crucial markers of possible change. Different styles are readily visible and

change more quickly than is the case with litrucs (Meyer and Hamilton 1994: 96 and

Hamilton 1981: 41).

Archaeologists classify ceramics found in the region into three major types: Laurel,

Blackduck, and Selkirk. Each of these types is associated with a cultural tradition composed

of a number of temporaily and regionaily defined phases, such as the Rainy River Composite,

wruch consists of the Sandy Lake, Duck Bay, Bird Lake, and Winnipeg River complexes.

Considerable contributions have been made with respect to understanding the archaeological

record in the larger geograprucal area witrun wruch the Lake of the Woods exists (e.g.

MacNeish 1958). Furthermore, the several taxonomie systems have been employed to

organise the material (Wilford 1955; Syms 1977; Reid and Rajnovich 1990; Lenius and Olinyk

1990) unfortunately complicate any understanding of this larger region. At the same time,

archaeologists often apply different terms to the same thing. Lugenbeal (1978: 45) observed

that Wilford defined the Laurel Focus based upon rus 1933 excavations of Mound 4 in the

Rainy River region, wruch became the Laurel Tradition according to Wright (1967) or,

according to Stoltman (1973), the Laurel Culture.

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However, if each cultural tradition is ordered chronologically for the area in question

- Laurel, Blackduck, and Selkirk - the problem exists that each successive one could not have

sim ply expelled or erased the previous cultural group responsible for the different types of

ceramics and lithics evident within the archaeological record. Radiocarbon dates from

individual site components date the Laurel period between 900 B.P and 2,000 B. P.,

Blackduck sites have been dated between 400 B. P. and 1400 B. P. while Selkirk materials

date from 300 B. P. to 1,000 B. P. Each period overlaps with the others. Each has its own

early period of dominance based on these radiocarbon dates, which are themselves

considered problematic. The radio carbon dates indicate that there is some sort of overlap

but, to date, archaeologists have recovered very little transitional or mixed ceramic material

that cross-cuts typological boundaries and demonstrates exactly how these ceramic traditions

co-existed.

1t is difficult to equate archaeological cultures identified in assemblages with ethnic

boundaries of specific groups especially if have problems exist in trying to recognise or

identify these symbolic signatures if they are still present. Stark (1998: xvüi) realised that

conventional methods of stylistic analysis used by North Americanists were ineffective in her

attempts to analyse the iconological or symbolic aspects of undecorated goods that

"circulated in very restricted systems". More productive results could be obtained she

asserted by taking alternative methods to the analysis of stylistic variation. She (ibid.) asserted

observed that different scales of social boundaries existed, the ceramics of the Tonto Basin,

in central Arizona, that otherwise remained hidden in the archaeological record. Her edited

volume of papers considered the relationship of style, as it had been defined, to social

boundaries and whether it was possible to "detect" the conditions under which social

boundaries and mate rial culture might concur. Stark maintained (ibid.: 2-3) that scholars

should question why they desire a "unified theory of style" and consider how material

cultural patterning is examined. She observed that the archaeologists who responded to her

request could be divided into two groups based on two basic premises: that "Anglo­

American archaeologists had refined" a range of techniques for conducting studies of spatial

analysis and interpreting distributional patterning and while the French archaeologists had

devised a "useful set of methods studying formaI variation". 1ndeed, Chilton's (1998), Dietler

and Herbich's (1998), Hegmon's (1998), and Goodby's (1998) studies are particularly useful

because each discussed, utilising different archaeological assemblages in a North American

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context, how to determine social boundaries and material culture. Chilton's (1998) article is

probably the most useful for the region between Lakes Superior and Winnipeg. She

examined the ceramic assemblage so as to consider the relationships between the technical

choices, historical context and society for three late Woodland (AD 1000-1600) sites in the

northeastern United States. She (ibid.: 159) concluded based on the variations in the ceramic

assemblages of these sites that both the Algonquian and the lroquoian peoples, in this

region, were active agents of their own social change who made choices regarding their

subsistence, settlement and social structures.

Shennan, an archaeologist, (1989) has argued that the "question" of the origin of

ethnie groups should be "analytically" separate from the "nature of archaeological cultures"

(1989: 6). He postulated that archaeological culture should not be equated with specifie

ethnie groups in the past because this assertion was "positively misleading". Archaeological

entities should be perceived instead as "summary descriptions of patterns of spatial analysis,"

while ethnicity should refer to "self-consciousness" (ibid.). He outlined four arguments,

suggested by other scholars, why the notion of archaeological cultures as entities should be

rejected. Shennan (ibid.: 13) rejected the idea that archaeological 'cultures' are equivalent to

ethnie groups, demonstrating that distributions in the archaeological record are the outcome

of a number of disparate processes. He postulated that, if archaeologists used quantitative

analytical techniques rather than "presence-absence information," a wide variety of cross­

cutting patterns would be revealed, rather than readily identifiable "bounded entities" (ibid.).

He also maintained that entities such as "cultures" did not exist but were unpredictable

interrelations of various distributions produced by different processes. Concerns with

ethnicity in archaeology were for Shennan (ibid.: 18) becoming "refocused around the

concept of style".

Hodder has argued that, despite interaction across tribal boundaries, distinctions in

material culture persisted for some artefacts (Hodder 1982). He considered (ibid.: 185) how

matetÏal culture influenced, and was a "product" of various groupings of people who created,

used and manipulated it. Hodder asserted (ibid.) that a simple link could not exist between

degrees of interaction, scales of production, and material culture patterning sin ce other

factors intervene such as ideologies, attitudes, intentions, and strategies.

It appears that in the archaeological literature from the region between Lake

Winnipeg and Lake SupetÏor the term ethnicity implies ethnie group. However, Isajiw (1974)

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discovered, from a survey of sixty-five sociological and anthropological studies on ethnicity,

that only thirteen studies included a definition of some sort. The remainder of these studies

did not clarify what was meant by "ethnicity".

The definition of this term is not easy. Jones (1997: 55) proposed that henceforth

scholars should employ "a processual analysis of ethnicity" rather than the previous rigid

categories of 'race', 'culture', 'society', and 'tribe' (ibid.). Jones maintained (ibid.) that these

rigid categories had various ideological meanings for different groups of people in different

parts of the world. The notion of ethnicity is complex and possibly elusive and not a clear­

cut theoretical tool to be used by archaeologists. Nevertheless, a detailed examination of the

archaeologicalliterature of this region demonstrates that archaeologists are concerned to find

symbolic expressions of social identity in the archaeological record.

Wilford (1941, 1955), an archaeologist, studied the prehistoric cultures of Minnesota

and identified the Late Woodland Blackduck focus and defined the characteristics of

Blackduck ceramics. Other cultural traits included triangular projectile points, long-bone

fleshers, unilateral barbed bone points, bird-bone whistles, antler flakers, and several types of

side scrapers. These people built mounds containing flexed burials with ochre and grave

goods in cylindrical pits (1941: 313-315, 1955: 136). He postulated that the people of the

Blackduck cultural tradition in the Rainy River region might be the ancestors of historie

Assiniboine, who spoke a Siouian language (1955: 136).

MacNeish (1958) identified the Manitoba Focus at a number of sites in southeastern

Manitoba dating AD 1000 to AD 1750 and argued that this focus was similar to the

Blackduck Focus of northern Minnesota (1958: 76-77). MacNeish noted that the Selkirk

Focus occurred between AD 1350 and AD 1750 but did not develop from the Manitoba

Focus. He postulated that similarities between the two were due to "natural interchange"

resulting from contact rather than a common origin (ibid.: 77). These two traditions differed

in terms of burial traditions, the decoration of the ceramics, and other parts of the

archaeological assemblage (ibid. 73). MacNeish postulated that, during the fourteenth

century, the Cree had moved southwards and replaced the Assiniboine between the Lake of

the Woods and the southern part of Lake Winnipeg (ibid.).

Evans (1961), another archaeologist, argued that the burial practices were critical to

the ethnic identities of these peoples. He agreed with Bushnell (1927) that the Assiniboine,

during the seventeenth century, separated from the Yanktonai Dakota. They left the

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headwaters of the Mississippi to move northwards to the Lake of the Woods and

subsequendy to Lake Winnipeg. Evans disagreed that sites classified as Blackduck were

Assiniboine because they were located outside the present limits of Siouan groups (1961:

271-275). Wright (1963, 1965, 1968b, 1968c), agreed with Evans (1961) that the Blackduck

sites were not occupied by prehistoric or early historie Assiniboine. He asserted that the

presence of Selkirk and the Blackduck ceramics on the north shore of the Great Lakes was

explicable since it reflected the mobility of women, who made the pottery and who moved

residencies as a consequence of "patrilocal residence requirements" (Wright 1968b and

1968c: 107). Both maintained that Algonquian speakers occupied the area alongside the

modern day international border when contact occurred with the Europeans.

However, Wright disagreed with Evans over their precise ethnie identification.

Wright posited that the Ojibwa occupied the heardand of the Blackduck area while Evans

asserted that the Cree were living in this area. Wright (1968b) maintained that

anthropologists would have a difficult task to distinguish between southern Cree and

northern Ojibwa based upon the associations and differences between the Selkirk and

Blackduck foci ceramics (ibid.: 23). He contended that this task would be easy if the Selkirk

focus had belonged to the Cree and the Ojibwa were responsible for the Blackduck ceramics

(ibid.). He also acknowledged, however, that the use of the terms 'Cree' and 'Ojibwa' created

pitfails and argued it was probably more appropriate if these archaeological assemblages were

cailed "Boreal Forest Algonkians" and "Great Lakes-St. Lawrence Forest Algonkians" after

the forest classification. Yet, assigning new names to these archaeological assemblages does

not aid an understanding of ethnicity. It merely confuses the situation further by making the

terminology more complex.

Skinner (1911: 117), Hailoweil (1955: 114-115), Dunning (1959: 3-4), and Hickerson

(1966:4 and 1967: 45), ail of whom were anthropologists, disagreed with Rogers, another

anthropologist (1963), and Wright (1968b), postulating that the Ojibwa arrived in this region

during the historie period. Hickerson (1967), an ethnohistorian, argued that the history of

this region was "indissolubly linked with the history of European exploration and history"

(ibid.: 47). He asserted that the Cree, who were influenced by the fur trade, first occupied this

area. By the late eighteenth century, groups of Chippewa, otherwise cailed Ojibwa, that

originaily inhabited clan-named villages along the north shore of Lake Huron displaced these

ab original Cree, and their close relatives the Monsoni-Cree (ibid.: 45, 47), from the are a to

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the west of Lake Superior. Hickerson (ibid.: 44) argued from historical documents that, by

1660, the Cree inhabited the are a north of Lake Superior and that between 1660 and 1680

intertribal conflict broke out among the Dakota, the Chippewaj Ojibwa, the Cree, and other

groups in the region west of Lake Superior. The Chippewa and the eastern Dakota made

peace in 1679 that lasted until 1736. Hickerson maintained that at this time the Cree and

their allies, the Assiniboine, were the chief occupants of the area to the northwest and west

of Lake Superior. Consequently, the French traders and officiaIs, who arrived in this region

between 1717 and 1721 with their goal of finding the Western Sea, had to deal with the Cree

and their allies, who controlled Rainy Lake and the Lake of the Woods.

Hickerson's (1967) view, based on La Vérendreye's reports, is different from that

held by his colleagues. La Vérendreye wrote in his letter of June 1736 to the Marquis de

Beauharnois, Governor General of New France, that the Cree and the Monsoni-Cree came

to see him at Fort Charles in the Lake of the Woods to ask about the massacre of the twenty­

one men from Fort St. Charles (Burpee 1927: 213-219). La Vérendreye wrote earlier in the

same letter that he was aware of a group of Sioux in the Lake of the Woods "who were

100 king for Cree and who might perhaps do them sorne harm" (ibid.: 216). Rogers' (1963)

view supported Wright's (1968b) claims; based on information from informants from Round

Lake Ojibwa, northwest of Lake Superior, Rogers (1963: 65-66) asserted that the Ojibwa had

always lived in the interior region north and west of Lake Superior and that farther north

they blended into the Cree.

Bishop and Smith, both anthropologists, (1975: 59) disagreed with Evans'

conclusions (1961: 271-275), describing his arguments as "unsubstantial and weak". Evans

doubted that the Blackduck sites in northern Minnesota were Assiniboine, since the burial

practices evident in the excavated mounds would have had to change twice and the

Blackduck sites extended eastwards beyond the historically known range of the Siouan

groups. Evans based his arguments on Bushnell's daim (1927) that during the seventeenth

century the Assiniboine separated from the Yanktonai Dakota, left the headwaters of the

Mississippi and moved northwards to the Lake of the Woods and then to Lake Winnipeg.

For Evans, burial practices are crucial for identifying each cultural group. He argued

that the Mille Lacs Aspect, assumed to be Siouan, which lies 75 miles southwest of the west

end of Lake Superior, contained secondary burials. The Headwaters Lake Aspect, that lies to

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the north of the Mille Lacs Aspect, assumed to be a site of Algonquian-speaking Cree, has

primary burials containing Blackduck ceramics.

Essentially, Bishop and Smith (1975: 54- 61) believed Evans did not use the historical

data very weIl. Aware of the divergent views held by archaeologists and historians, they (ibid.

59) postulated that the central question was the affinity of the Yanktonai and the

Assiniboine. Lowie (1910), an anthropologist, had demonstrated that the separation of the

Yanktonai and the Assiniboine languages predated the historie period. Bishop and Smith

(1975: 59), therefore posited that, if the Assiniboine occupied Blackduck sites, the

archaeological evidence should support this claim. Furthermore, they argued that, following

the arrivaI of the fur trade, the cultural differences between the Yanktonai and the

Assiniboine led to animosity between these two peoples. They suggested that the Cree might

have resided in the area and, occasionally, during the early historie period, they and the

Assiniboine could have occupied the same camps; therefore it was highly likely that inter­

tribal trade occurred, possibly involving foodstuffs in ceramic vessels. They proposed that

this might explain the co-existence of Selkirk and Blackduck assemblages at some

archaeological sites.

Bishop and Smith (ibid.) argued that little evidence substantiated the claims that the

Blackduck and Manitoba Focus sites were Cree in origin. They disagreed with Wright's

(1965, 1968b) conclusions that the Blackduck focus was Ojibwa. Wright had based his

conclusions upon direct archaeological and historical evidence with supporting data from

linguistics, ethnology, and physical anthropology. Bishop and Smith (1975) agreed with

MacNeish's (1958), Wilford's (an archaeologist) (1955), and Hlady's (an archaeologist) (1970:

108) conclusions that Blackduck was Assiniboine, as explained below.

Bishop and Smith (1975) argued that archaeological data and the early historical

references supported the view that the Assiniboine, at the time of contact, about AD 1620,

lived in the region from Lake of the Woods, to Lac Seul, to the mouth of the Kaministikwia

River, near present day Thunder Bay. This region was also the heartland of the Blackduck

focus ceramics. Historical documentation led Bishop and Smith (ibid.) to reason that Cree

subsequently moved west beyond the Pigeon River, since the Cree were reported to be

"visiting on the north Shore of Lake Superior" in the seventeenth century. The Ojibwa were,

at the time of earliest European contact, living as far west as Michipicoten Bayon the

northeastern shore of Lake Superior. The Cree lived to the north and the west of the Ojibwa.

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The Assiniboine lived westward from the Kaministikwia River on Lake Superior in Northern

Ontario, Northern Minnesota, and Manitoba. Bishop and Smith concluded that the early

historicalliterature both supported their findings and explained the discontinuity between the

archaeological and historical materials. Nevertheless, they warned that it was problematic to

"draw a one-to-one relationship between ceramic fod and their ethnic manufacturers" (ibid.:

61).

Articles by Dawson (1975; 1977), an archaeologist, suggest that he violently disagreed

with the perspective of the historians regarding the ethnic identities of the peoples of this

region. He argued that the Algonquian speakers were not recent arrivaIs to northwestern

Ontario (1975: 158 and 1977: 67) and agreed with MacNeish (1958) and Wilford (1941, 1955)

that the Terminal Woodland, or the Late Woodland, period of the Blackduck Tradition could

be equated with Assiniboine (Dawson 1975: 158; 1977: 72). The main strength of his

arguments rejects the reliance by historians on "second hand information" recorded in early

French written records and cartographic evidence of this region (Dawson 1975: 159-169;

1977: 67-73). Dawson (1987: 145) later argued that the "identity of the peoples resident in

the area at the beginning of the contact period cannot be stated unequivocally, for records do

not begin until about the middle of the period". In this paper he appears to imply that the

archaeological record shouid be the sole provider of information because of the lack of good

historical records for the contact period (ibid. 1987: 151).

Bishop and Ray posited that the inability to resolve the ethnic identity of who lived in

this region of North America arose from "methodologicai and conceptual biases" (1976:

117). This "generai failure" occurred because scholars found it difficult "to appreciate" the

transformations consequentiai to European-Canadian influences over the past three to four

centuries (ibid.). Problems would be avoided if scholars considering the protohistoric and

prehistoric period used the archivaI materials relevant to the region in conjunction with

anthropologicai studies.

Bishop and Ray subsequently discussed the problems invoived in attempts to

combine archaeological, ethnographic, and archivaI data to "produce an accurate and

meaningful culture history" using the direct historical approach (ibid.: 123). They argued that

the Iack of knowledge of the early contact period hindered attempts to establish a secure

baseline, and to make assumptions about the rate of acculturation of the lndian groups living

in this region (ibid.). However, they concluded that the available evidence, both historicai and

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ethnographie, supported their view that the Assiniboine and the Cree occupied the southern

margins of the northwestern Ontario prior to European intervention (ibid.: 137). Wheeler, an

archaeologist (1977b), disputed the notion that the historical facts could "speak for

themselves" and argued that interpretation of these historical sources must be undertaken

with great care (ibid.: 123). He contested the interpretations of the documents used by

scholars to assert that the Assiniboine were the occupants of the region between Lake

Nipigon and the Lake of the Woods when the Europeans arrived (ibid.: 122). Unfortunately,

he failed ta state whether northern Minnesota or southwestern Manitoba were included in

this statement. Wheeler believed that confusion would continue if scholars continued to

identify specifie historical groups with specifie terri tories based on these "vague and

ambiguous records" (ibid.: 123). He asserted that insufficient evidence existed to argue that

the Assiniboine resided in the Lake Forest and the Southern Boreal Forest from Lake

Nipigon to the Lake of the Woods. Wheeler (ibid.: 122) supported the notion that a major

westward expansion of the Ojibwa had occurred through the Boundary region as proposed

by Rogers (1963) and Hailowell (1955). However, he (1977b: 122) stated that, unlike his

colleagues, he was "most dubious of accepting a Cree-Ojibway expansion and Assiniboine

withdrawal" from the Boundary Waters region prior to 1720.

Meyer and Hamilton (1994), unlike their predecessors in this debate, refrained from

violendy disagreeing with previous views. As archaeologists, they realised that the entire

culture-history of this region was based on changing ceramic styles. They asserted that the

peoples from the Great Lakes-St Lawrence Forest and the Boreal Forest interacted with

those who lived in the Plains region to the west and to the south of them throughout

prehistory (ibid. 127). These interactions included the movement of ideas as weil as of

people. They posited that Selkirk ware was produced by northern Algonquians who later

were called Cree (ibid.). Sandy Lake ware, in contrast, was connected to the Siouans, while

sorne of the northerly material was probably created by predecessors of the people

historically called Assiniboine (ibid.). Evidendy, they agreed with Arthurs' conclusion (1986:

263-64) as to the crea tors of the Sandy Lake material on the northern fringes of its

geographical distribution. Meyer and Hamilton maintained that this argument was possible if

proponents correlated the protohistoric distribution of Selkirk and Sandy Lake ware with the

distribution of lndian groups at the time of contact. These archaeologists argued that the

occupants of northwestern Ontario, southeastern Manitoba, and northern Minnesota made

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Duck Bay, Selkirk, and Sandy Lake ware. Unfortunately, Meyer and Hamilton did not discuss

the identity of those peoples who created the Duck Bay ware. Both acknowledged the

problematic nature of the assumption that a specifie sort of archaeological artefact equated

to a specifie ethnie entity (1994: 125).

Yet, Duck Bay was one of three archaeological complexes that belonged to the Rainy

River composite, along with the Winnipeg River and Bird Lake complexes. Lenius and

Olinyk (1990: 82) argued that these small complexes shared common ceramic traits, and that

the peoples associated with them may have shared similar social, political, and religious

activities. They existed at the same time as the burial mounds, dated to the Late Woodland

period, were being built along the banks of the Rainy River (ibid.). Lenius and Olinyk (ibid.:

83) argued that the Rainy River composite was created by a coalescence of the Blackduck

and Laurel cultures. It was very difficult to find a precise definition of what is implied by the

terms "composite" or "complex" within trus body of literature; however, it is likely that a

composite is probably a larger entity which encompasses two or more complexes. These

composites appear to have a shorter time scale and possibly a smaller geograprucal scale than

the cultural traditions called Laurel, Blackduck, or Selkirk.

Lugenbeal (1976) proposed that the variation ln Laurel pottery of northern

Minnesota was directly linked to temporal change and that Laurel assemblages could be

dated loosely by the changing proportions of the stylistic types of pottery. Reid and

Rajnovich (1991) argued that regional expressions existed witrun the Laurel cultural tradition,

wruch lasted 1,000 years, implying geopolitical divisions. Lenius and Olinyk posited that from

AD 700 to 1000 the Blackduck and the Laurel cultural tradition co-existed but maintained

their own distinctive pottery forms. They speculated that about AD 1000 the ceramics that

belonged to the Rainy River composite emerged as a consequence of a coalescence of the

Blackduck and Laurel cultures. Neither author clarifies why this would have occurred. Trus

change, Lenius and Olinyk asserted, was accompanied by a diminution in the size of the

mounds built in trus region in the Late Woodland period (Kenyon 1970: 66; Arthurs 1986:

19). Lenius and Olinyk noted that mounds belonging to the Rainy River composite and the

Laurel cultural tradition existed together on the same site (ibid.).

Kenyon acknowledged that, although it was difficult to establish whether the

occupation of trus region was continuous, it was used intermittently for 8,000 years (Kenyon

1970: 68). He was confident that this region had probably been used continuously for the

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previous 2,000 years. Kenyon's conclusions were based on his excavation of the Armstrong

Mounds, which he dated to the Late Laurel cultural tradition and argued were built about

1,000 years ago (ibid.). Unfortunately, Kenyon did not provide any detailed discussion in his

1970 report of the ethnic affiliation of the peoples. It is likely that his conclusions were based

on the excavation of five mounds in the same locality (Kenyon 1986). He argued that the

principal goal of these mounds was to denote sacred places and to verify territorial

occupation. He postulated that (ibid.: 80), after spending the winter in small groups, large

numbers of people gathered there for ceremonial purposes in either the spring or the

autumn, when sufficient food resources were available.

Kenyon's (1970, 1986) opinion regarding the use of these mounds is consistent with

the osteological research conducted by Tobenson and his colleagues (fobenson et. al. 1992;

1994) and the archaeological analysis conducted by Johnson and Ready (1992). Kenyon

(1986) supported his arguments with his descriptions of the burial practices evident from the

skeletal remains and detailed information about grave goods. Kenyon (ibid.: 112-116) found

a large number of small ceremonial ceramic vessels, which Lenius and Olinyk (1990: 83) later

argued belonged to the Rainy River composite and were rare outside the region. These

vessels are of interest to the author of this the sis since a similar vessel was found in the

summer of 2001 at the base of a pictograph site in the Lake of the Woods, at a depth of fifty­

two feet below the present day water level. The discovery of this vessel supplements Lenius'

and Olinyk's (ibid.) observation that only two such vessels were known from outside the

Rainy River composite. Lenius and Olinyk (ibid.: 101) subsequendy argued that the Rainy

River composite had evolved out of the Blackduck and Laurel cultures. Meyer and Russell

(1987: 22) postulated that the Blackduck and Laurel were also the base of the Selkirk

composite tradition. Hence it was believed that both the Rainy River and the Selkirk

composites had developed from the same distant ancestors and shared a common ceramic

technology. Wright (1971: 22-23), Dawson (1976b: 3) and Meyer and Russell (1987: 25-26)

posited that, probably, ancestors of Algonquian-speaking groups made the ceramics of both

composites.

Yet, what was the ethnie identity of these people associated with the Laurel and

Blackduck cultures? Lenius and Olinyk tried to identify each group using a study based upon

glottochronology developed by Voorhis (1978). Both Lenius and Olinyk (1990: 101) and

Syms (1980: 5) disagreed with linguists who rejected glottochronology, since these linguists

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ignored absolute chronology in favour of identifying sub-group relationships within language

families on the basis of similar patterns of innovation. Syms maintained that

glottochronology was invaluable and therefore linguists ought to reassess its value.

Voorhis (1978) determined that a Cree-Ojibwa split occurred between AD 987 and

AD 1079. Lenius and Olinyk asserted that this date range was similar to the date suggested

for the emergence of the Selkirk composite, which represented the northern "Cree" people,

and the Rainy River composite, which represented the more southerly "Ojibwa" people

(1990:101).

Syms argued that the Blackduck should be reconsidered as belonging to a number of

Algonquian alternatives such as Ojibwa, Cheyenne, or Arapaho (Syms 1982: 7). He figured

that if scholars preferred an Assiniboine identification for the Selkirk culture then the Sandy

Lake and the closely related northerly Wanikan complex, were related to another group. He

asserted that archaeologists should come to a consensus concerning the terminology used.

Glottochronology, although it is considered problematic, provides support for both Lenius'

and Olinyk's (1990) and Syms' (1982) conclusion as to the ethnic identify of these peoples

and how they were related.

The debate about who lived west of Lake Superior remalnS unresolved and as

problematic as ever. Two groups of scholars are embroiled in an academic argument over

which ethnic group resided in the region first. Unfortunately, most of the archaeological

literature for this region is dominated by inventories. Yet, the archaeologists are concerned

with identifying traits so they can be connected to each other and possibly to an ethnic

group. At the same time there is growing evidence of the problematic nature of the

assumption that an archaeological feature is equivalent to a specific cultural entity. The vast

quantity of descriptive literature results from most archaeologists having employed a culture­

historical approach which, although important, remains highly empirical. The culture­

historical approach only requires an archaeologist to provide detailed descriptions of the sites

in question. The entire situation is further complicated because the archaeologists working in

this region rely solely on one primary diagnostic, ceramics.

Archaeologists have agreed that three major cultural types exist: Laurel, Blackduck,

and Selkirk and each is called a tradition, culture, or focus. All these terms refer to different

things. All archaeologists agree that, temporally and regionally, each tradition consists of a

number of phases. The Laurel tradition, for example, has the Rainy River Composite, which

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consists of the Sandy Lake, Duck Bay, Bird Lake, and Winnipeg River complexes. Each

tradition, or culture, is presumed to be chronologically ordered. However, each successive

cultural group could not have simply expelled or erased the previous one responsible for the

different types of ceramics and lithics. This argument is supported by the radiocarbon dates

which indicate an overlap, but very little transitional or mixed ceramic mate rial has been

recovered to support the co-existence of these traditions. Unfortunately, archaeologists used

different terms for the same thing, and none of them agree who the ancestors of the Cree

and the Ojibwa were during each cultural tradition. It is impossible to consider whether the

Cree or the Ojibwa were related to one specifie culture. Indeed, each culture was composed

of composites and complexes that themselves had links to other groups within the

geographical region in question. It is easier to state whether the Algonquin or the

Assiniboine were in the region. It appears that both groups were, in the region at different

times, but it is unclear precisely which group was where at any specifie times. Clearly it is

very difficult to consider the precise ethnicity of the people who may have created the rock

images of the Lake of the Woods.

(c) Understanding the archaeological record of the Boreal Forest

Archaeologists have argued over how hard it is to find and excavate sites in the

Boreal Forest. Successful archeological research there requires understanding the problems

inherent in the archaeological record of that part of the Subarctic. Hamilton has asserted that

the current interpretation of the archaeological record of this region is a "rather nasty, messy,

and simplistic culture-history" (Hamilton pers. comm. October 2000). Much of the synthesis

of this region is heavily dependent upon the work of MacNeish (1954, 1958), G. E. Evans

(1961), L. A. Wilford (1941), ]. V. Wright (1967, 1972a), E. N. Lugenbeal (1976), W. ].

Mayer-Oakes (1970),]. B. Stoltman (1973) and K. C. A. Dawson (1974, 1976a, 1976b). The

relatively small quantity of information is probably a consequence of the vegetation and the

climate.

Reid (1988) has identified and discussed eleven problems associated with site

excavation in this region, which he subdivided into "syndromes" and "conditions". He

defined "syndromes" as the problems connected to the approachesj explanations created by

archaeologists (ibid.: 188). Eight syndromes exist which he identifies as follows: Telephone

Booth, Telephone Book, Small Site, Sparse Site, Cigarette Package, Flat Earth, Immaculate

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Conception, and Superficial Analysis. A final syndrome was also a condition: the 49th ParaUel

Syndrome/Condition. "Conditions" were defined as the problems germane to the nature of

habitation sites within the Boreal Forest and to the modem environment of the Boreal

Forest. Two were identified: Collapsed Stratigraphy and Remote Access. To appreciate the

precise nature of each syndrome, it is crucial ta examine them one by one.

Reid argued that Telephone Booth syndrome was evident in terms of how

archaeological excavation was undertaken in the Boreal Forest. Essentially, archaeological

sites were excavated using metre square grids where each individu al was responsible for their

one-metre square and excavated and recorded it at his or her own speed (ibid.: 189). This

syndrome became more prevalent, Reid (ibid.: 190) asserted, as a consequence of cultural

management resource studies conducted by archaeological contractors for profit under

environmental protection legislation. An example of such legislation was the Province of

Ontario's Environmental Assessment Act (ibid.).

Reid asserted it was possible to compare these contractors' reports to a telephone

book because, like a Telephone Book, conservation archaeological reports consisted of

"endless lists of sites discovered on surveys complete with artefact catalogues but little

interpretation and even less Gustified) hypothesis formulation" (ibid.).

The problems with this approach were compounded by archaeological terminology.

Artefacts, whether lithics or ceramics, were measured, counted, classified according to types,

and assigned to a specifie cultural tradition, but sites were described as having a number of

cultural affiliations.

The frequency of sites having multiple cultural attributions causes problems for

archaeologists trying to establish the distribution of specifie cultural traditions and ethnic

groups through time. Halverson (1988), for example, undertook a survey of Cameron, Flint,

Kakagi (Crow), and Stephen Lakes, about 120 kilometres south of Kenora in Northwestern

Ontario. A typical conclusion for a site in this report is as follows: DhKk-22 was culturally

affiliated with "the Selkirk or Blackduck and modern use" (Halverson 1988: 29). Halverson

reached this conclusion based upon the evidence excavated from test pits at this site, which

consisted of four utilised local chert flakes, five fabric impressed body sherds, one primary

unused local chert flake, three unused local chert secondary flakes, fourteen local chert

tertiary flakes, one used quartz secondary flake, and one unused local rhyolite secondary flake

(ibid.: 29).

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Sorne surveys do not provide an in-depth analysis of the material collected, while

others present the information in a format that makes it impossible to use (for ex ample:

Haywood 1983; Riddle 1982). The description provided for the cultural affiliation of the

Ouimet Site, FbIx-2, on Attawapiskat Lake is an example of a pie ce of archaeological

information that cannot be used anywhere else than within the published report. It was

classified as having "cultural affiliations to the Archaic, Initial Woodland, Terminal

Woodland and heavy modern use" (Riddle 1982: 24-25). Riddle, like many archaeologists,

classified sorne sites as being prehistoric of an unknown affinity, historie and modern. But

the division of the terms Initial and Terminal Woodland, according to Wright (1981: 91), was

for archaeological convenience rather than any indication of a major culture change or event.

Sometimes archaeologists cause additional problems by creating statistics that are

useless and incomprehensible other than within the context of the report itself. Haywood

observed (1983: 32) that only three, or 11.1 %, of the twenty-seven sites he surveyed had

Paleo-Indian artefacts. Rock image sites are treated as separate units of analysis and not

interpreted in conjunction with nearby archaeological sites (see Pastershank 1989 and

Halverson 1988).

Reid argued that the difficulties that exist in accessing the Boreal Forest because of

the Remote Access Condition compounded the Telephone Book syndrome, resulting in little

research being conducted in this region. The Small Site Syndrome was, according to Reid, a

people problem caused by absence of universities in a region the size of Europe, and by

institutions elsewhere not training archaeologists at the graduate level for working in the

Boreal Forest. Only two universities exist in Northern Ontario, and neither institution had a

graduate programme in archaeology and anthropology. Reid argued that the lack of

universities in northern Ontario with graduate and comprehensive research programmes

compounded the logistical problems of working in the Boreal Forest region, since the nearest

universities involved in research were in Manitoba and southern Ontario (1988: 191).

Consequently, the training provided to students in Canadian institutions elsewhere caused

"an almost unavoidable bias towards Iroquoian [big site] 'mind sets' at least for the

Woodland period" or for the Siouian area of the east central Plains (ibid.). Hence the number

of hunter-gatherer sites of the Boreal Forest of Ontario was assumed to be "small" . Very few

large sites have been excavated in northern Ontario, Manitoba and Minnesota. Reid (1988:

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191) was concerned that current researchers refused to acknowledge that recent literature

discussed examples of large hunter-gatherer habitation sites in the Boreal Forest.

The Sparse Site Syndrome occurred, Reid asserted, because researchers believed that

even small sites occurred only sporadically. Reid relates this syndrome to the Telephone

Booth Syndrome, the Small Sites Syndrome, and the "resultant self-fulfilling prophetic nature

of the associated research designs, methodologies, and interpretations" (ibid.: 192).

The Cigarette Package Syndrome, like the Sparse Site Syndrome, was also a people

problem. Reid maintained that it afflicted the "macho northern archaeologists [the MNA, an

identifiable species which shall be the subject of a suitable paper] who having braved the

Remote Access Condition through sheer possession of the "Right Stuff', beset by black flies,

mosquitoes, keep their field notes on the back of their Players cigarette packs" (ibid.: 193).

He asserted that the existence of this syndrome meant it was impossible to resolve the

Compressed Stratigraphy Condition.

The Flat Earth Syndrome, like the Cigarette Package Syndrome, was for Reid another

problem created by people rather than by the archaeological record. He argued that this

syndrome occurred if archaeologists misunderstood the meaning of the word 'level' since it

did not mean that the archaeologicallayer was flat. If archaeologists did not understand that

this word 'level' meant a cultural episode, the consequences were severe because the

archaeologist could unwittingly cut through several strata (ibid.: 193).

The Immaculate Conception Syndrome was also a people problem since it occurred

when theories and hypotheses "spring full blown from the fertile minds of researchers"

without any serious background research or justification (ibid.). Reid posited that

archaeologists will use whatever hypothesis is currently in vogue and consequently this

problem was an "incurable" one as weil as being very difficult to detect by the "average

reader." He observed that in almost every case where this syndrome existed, very little field

investigation had occurred. If it had occurred, then the resulting fieldwork was superficiaL

He posited that the Immaculate Conception Syndrome was difficult to identify because "the

hypotheses always conform in style."

Reid (ibid.: 195) contended that another people problem, the Superficial Analysis

Syndrome, was closely connected to the Telephone Booth, Small Site, Sparse Site, Cigarette

Package, and Immaculate Conception Syndromes. This syndrome Reid (ibid.) directly

connected to the fact that the examination of the archaeological record of this region did not

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belong to Willey and Sabloff's Explanatory Period. Archaeological methodologies and

research designs for the Boreal Forest belonged, Reid argued (ibid.: 187), to what Willey and

Sabloff (1980: 130) had termed the "Classificatory-Historical Period: Concern with Context

and Function." Reid maintained that researchers should not be "lazy" and should concern

themselves with moving beyond the preliminary conclusions of the pioneers in the discipline.

The 49th Parallel Syndrome/Condition, he argued, was a people and a geo-political

problem and arising when archaeologists only read the literature pertinent to the region in

which they worked, regardless of the provincial, international, or state boundaries that

defined these regions. Resolution occurred only if archaeologists ignored the current

geopolitical boundaries, read the pertinent literature, and commurucated with their colleagues

in neighbouring regions.

Two "conditions" existed according to Reid: the compressed stratigraphy and the

remote access condition. Conditions, unlike syndromes, were physical problems rather than

problems caused by archaeologists. Reid (1988: 191) maintained that the problem of

compressed stratigraphy, or "collapsed stratigraphy" according to Syms (1977), was

characterised by "multiple long term occupations without sterile soil horizons between them,

compressed into a very shallow site". The problem of a compressed soil horizon was caused

by two principal factors: the slow rate of soil development in the Boreal Forest and the fact

that sites were not occupied on a year round basis but behaved as "way stations" (ibid.).

The second condition was Remote Access. Archaeologists who work in the Boreal

Forest experience severe logistical problems because there is very litde road access to mu ch

of this area. Indeed, most of the region can be only explored by bush plane or canoe.

Valuable and limited resources are frequendy "eaten up" by the sheer expense and time taken

to travel. Travelling by foot is problematic, given the vegetation mosaic of the Boreal Forest,

which includes impenetrable muskeg and bush. Reid argued that the high financial costs

involved in conjunction with no graduate programmes in universities in Northern Ontario

compounded the problem. It is likely that many sites in this region remain unmapped and

unknown as a consequence of difficult logistical problems. He postulated that this remote

access condition intensified the Superficial Analysis, Telephone Booth, Small Sites, Sparse

Sites, Cigarette Package, and Immaculate Conception Syndromes.

He reasoned that if archaeological examinations of this reglOn were to develop

beyond the Classificatory-Historical stage, two factors must be considered. Pirst, realistic

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research design parameters were required. Second, field methodologies that were pertinent to

the Boreal Forest should be considered because each field methodology had its own unique

problems. He maintained that archaeologists needed ta think carefully about their field

methodologies since no one achieved anything if they sim ply borrowed field methodologies

from areas with radically different cultural and physical environments. Reid (ibid.: 197 - 202)

subsequently considered nine minimum principles that could be "translated directly" into

specific field applications for use while excavating "conventional" archaeological sites.

Reid (ibid. 202) concluded that the archaeological investigation of the Boreal Forest

was on the verge of a new paradigm. He implemented the guidelines he had suggested at the

site DkKp-8 (Reid and Rajnovich 1987). This study has had sorne impact on the excavation

of sites elsewhere in Northwestern Ontario. Halverson (1992) used Reid's (1988) guidelines

for the excavation of DgKl-3, situated on the eastern shore of the Lake of the Woods.

However, although Pastershank (1989) was trained by Reid in archeological field techniques,

as was Halverson (1992), she did not use these guidelines.

The information collected by archaeologists often appears as "in-house" research

reports, frequently referred to as "grey" literature, since they are not published in refereed

journals but by provincial governments or individuals or remain as unpublished licence

reports or even reports to funding bodies. These unpublished reports are difficult to ob tain,

although they are often valuable sources of information, enabling researchers to establish the

level of data collection and analysis in a specific region.

It is evident that the methods by which archaeological information is disseminated

have changed over time. Sorne unpublished reports of the Ontario Ministry of Culture,

Tourism and Recreation, were reproduced in limited numbers and distributed on an

individual basis to select archaeological researchers who were "actively engaged in field

work". The Conservation Archaeology Reports were intended to provide a quick and

economical means of informing those archaeologists involved in regional archaeological

conservation and resource management. These archaeologists were involved in salvage and

emergency excavation, and in creating archaeological inventories under the Ontario Heritage

Act and the Environmental Assessment Act (1983). Archaeologists conducted surveys for

research, conservation, and cultural resources according to regional guidelines, and wrote

reports for each salvage, mitigation, and assessment or inventory project. Vast quantities of

data were generated according to regional guidelines, making them difficult to utilise in any

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.~.

other format. These reports may appear superficially dull and uninteresting but, despite their

limitations, they are valuable. They provide opportunities to establish whether a particular

region has been surveyed and to search for comparable collections of data.

Since these guidelines ensure that archaeologists apply the same fieldwork methods

and analytical techniques to rock image sites as to other archaeological sites, examinations of

these images are "trapped within a formula". This is a serious limitation, because the practical

methods of obtaining the data are radically different and far more limited; these images

cannot be excavated using the techniques for recovering, cataloguing and analysing data that

archaeologists apply to "traditional" archaeological sites. Sometimes, archaeologists can

excavate the area surrounding these images, but the physical context of the site rarely

provides information about the cultural context of the images themselves. Therefore the

archaeologist must rely to an unusual degree on a range of non-archaeological sources to

study and establish the "meaning(s)" of these images. The difficulties in accessing the

symbolic knowledge of a group of people through the attributes and physicallocation of the

images they produced alone may explain why many archaeologists have often ignored, or

merely described, these images in a perfunctory manner. But the interest in images also

accounts for why others have studied them.

Archaeologists in this region have spent a considerable amount of time examining

the spatial and temporal distributions of different prehistoric cultures. Unfortunately, much

of the work in this region has taken the form of inventory and salvage projects. This makes it

difficult to establish the geographical or temporal extent of these cultures so that scholars

can examine them in relation to other contemporaneous groups.

Hamilton argued that previous attempts to understand the temporal and spatial

distribution of prehistoric cultures have made implicit use of the concept of "edge" or

"boundary" to clarify the relationships between archaeological entities (Hamilton 1988: 39).

The meaning of this term, Hamilton postulated (ibid.), was analogous to the situation that

occurred in an ecological zone when "two disparate biotic communities come into contact"

(ibid.). Like Bird (1961), he argued that these boundaries were not clearly defined but rather

discontinuous cultural boundaries between human populations (Hamilton 1988: 39-40). He

contended that the concept of rnixed elements, which enabled boundaries to exist between

different communities, empowered archaeologists in this region to discuss several artefacts

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with design traits associated with several different cultural entities. It also provided an

interpretative framework to discuss cultural interchanges and contact (ibid.).

The evidence presented in the gray literature implies that transition periods were

quick. Yet archaeologists have sought to identify possible "transitional pots" in the artefacts

obtained during excavations, based on detailed knowledge of the ceramics that belong to

each cultural tradition of this large geographic area. These pots provide stylistic traits

belonging to more than one cultural tradition and therefore demonstrate clear evidence of

traditions overlapping one another.

It is agreed by archaeologists that a pot or a sherd is to be classified as Laurel if the

body is either tapered or conically shaped and has a slightly outflaring lip profile. Although

their decorative characteristics may vary, they were usually decorated with linear stamps and

serrated working edges. A wide range of decorative effects are found on these smoothed

vessels involving the use of a combination of stamps and variable motifs (Hamilton 1988:

41). Blackduck ceramics are characterised by globular bodies with constricted necks and

wide, outflaring rims. These pots exhibit a wide range of decorative elements done with a

linear cord-wrapped stick as well as punctate impressions on the rim and neck and textile

impressed body surfaces. Selkirk ceramics are distinguishable by their large globular body,

constricted neck, and an upright, straight-sided rim and lip. Surface decoration is limited to a

narrow range of cord wrapped and punctate impressions on the rim, above a textile

impressed body. These textile impressions are distinct from those of the Blackduck ceramics.

As previously stated, these three ceramic traditions spatially and temporally overlap

one another; yet each had its own period of dominance, if one considers the radiocarbon

dates. Yet very little ceramic material has been recovered to date that cross-cuts typological

boundaries and clearly demonstrates how these ceramic traditions interrelated. Hamilton

(pers. comm. October 2000) and Ross (pers. comm. October 2000) assert that very few

sherds exist to explain what happened as the result of the overlap between the Laurel and the

Blackduck periods. Yet it seems possible that both types were used at the same time. A sherd

that is deemed "transitional" might have a shape and/or decorative characteristics that are

identified with two different periods. Reid and Rajnovich discovered from the excavations of

House 1 at DkKp-8 that Blackduck and Laurel ceramics lay side-by-side (Reid and Rajnovich

1983: 6).

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Several archaeologists, induding Dawson (1976a), Gibbon and Caine (1980), Goetlz

(Goetlz personal communication in Halverson 1992: 57), Halverson (1992) and Koezur and

Wright (1976), daim to have identified examples of "transitional ceramics". Clearly very little

evidence exists for the existence of these types of pots. Goetlz found a "transitional" vessel

on Big Rice Lake in Cass County, Minnesota. Koezur and Wright provided detailed

descriptions of the nine "transitional ceramic type" vessels found at the Potato Island Site,

EIKc-l, near the headwaters of the Albany, English, and Berens river systems in northern

Ontario (1976). The authors (ibid.: 38-39) postulated that these vessels represented the

transition from the Laurel to the Blackduck period. However, the situation was further

complicated by the presence of a Selkirk trait, twined fabric impressions, on the nine

transitional vessels as weil as the Blackduck ones. To Koezur and Wright this suggested that

the Selkirk and the Blackduck periods and the preceding Laurel cultural tradition had a

"clinal aspect in their spatial relationships and that the traditions were not completely dis crete

and unrelated developments" (ibid.: 39). However, only two of the occupations of this site,

affiliated to the Terminal Woodland and Archaic, were excavated, presumably because

disturbance of the site was so extensive (ibid.: 16-18).

Dawson (1977) identified vessels belonging to the assumed transitional period

foilowing the Laurel culture in the Lake Nipigon area at several sites: DiJc-l, DiJc-2, DkJc-l,

and EaJf-1. He (ibid.: 17) observed that transitional Laurel ceramics were found at sites only

in conjunction with late Traditional Laurel ceramics as weil as Blackduck ceramics that were

designated as belonging to the "later Western Area Algonkian culture". Ceramics were

apparently also found in the same region, that were deemed as a "late manifestation for

south of the height of land mixed attributes on Laurel rim forms," since the Laurel Period

occurred prior to the Transitional period (ibid.: 78). He asserted that the Blackduck period

ceramics, whose attributes were evident in the Transitional period, marked the beginning of

the Terminal Woodland Period, which Dawson (ibid.) termed the "Algonkian culture". He

also contended that the existence of mixed Blackduck-Laurel ceramics, and Blackduck

ceramics with fabric-impressed exteriors rather than the Laurel plain exteriors, or Blackduck

cord-maileated exteriors, hinted at an "early close affinity with Selkirk fabric-impressed

wares" (ibid.). Dawson maintained that Blackduck traits developed from mixed ceramics and

marked the beginning of the Terminal Woodland Period Algonkian Culture (Dawson 1976a:

77).

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Halverson (1992) identified one vessel, from DgKl-3 on the eastern shore of the

Lake of the Woods, as possibly representing the hypothesized cultural shift between the

Middle and Late Woodland periods. The coil technique used to manufacture the pot was

interpreted as a Middle Woodland trait, while the overall cord impression on its exterior

surface was considered a Late Woodland trait (ibid.: 56-57).

Gibbon and Caine (1980: 57-72) examined the transition from Middle Woodland to

Late Woodland cultures in eastern Minnesota. They contrasted the data from four Middle

Woodland complexes with data from transitional St. Croix phase sites, and from early

Woodland phases. Gibbon and Caine (ibid.: 61) considered the St. Croix phase, not the St.

Croix site, to be transitional between the Middle to Late Woodland cultures stretching from

the north-western corner of Wisconsin across eastern and central Minnesota, through the

Boundary Waters Region into the Red River Valley. The dating for this phase was based on

stratigraphie relationships at four habitation sites where St. Croix phase pottery was

associated with Brainerd ware, two radio carbon dates of AD 340 ± 135 and AD 600 as weIl

as the relationship between the St. Croix phase and the Arvilla burial complex. Gibbon and

Caine (ibid.: 62) used this evidence to argue, that the period AD 300 to 800 was the most

probable time range of the St. Croix phase. The ceramic type belonging to the St. Croix

phase retained many Middle Woodland ceramic characteristics, including dentate stamping

and general vessel shape, but St. Croix sites demonstrated an increased variability in size and

quantity in comparison to Middle Woodland sites. They postulated that the transition from

Middle to late Woodland in the eastern Minnesota region involved several major shifts in

subsistence emphasis and in directly related cultural practices. These scholars asserted that

several interrelated variables eXplained this transition: firstly, the increased availability of wild

rice in the major lakes of Minnesota after AD 600-800 (ibid.: 64-65); secondly, climate

change since the appearance of a distinctive Late Woodland subsistence-settlement pattern

corresponded with the beginning of late warmer and mois ter neo-Atlantic climatic episode

(ibid. 65); and finally an increase in population sizes and a resulting increased pressure on

traditional food resources (ibid.). Gibbon and Caine also concluded that, after AD 900, an

increase occurred in population in the Carolinian-Canadian transition zone that correlated

with a way of life based on the intensive harvesting of wild rice.

Vessels that provide evidence of cultural transitions are important despite their rarity.

It seems it is the transition between Laurel and Blackduck with which archaeologists are

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concerned rather than the transition between the Blackduck and Selkirk cultural tradition.

Why archaeologists are interested in the earlier transitional phase rather than the later one is

unclear. It is agreed that a mixture of decorative traits identified with two cultural traditions

indicates that a pot could be classified as transitional. This leads one to postulate that the

presence of different sorts of traits may indicate that different groups of people were making

ceramic vessels. More evidence should exist to explain what occurred.

Hamilton (1988: 41) observed that the small quantity of sherds that crosscut

"typological boundaries" has caused speculation concerning the relations between the

cultures represented. Does the adoption of technologies reflect the diffusion of new

technologies from one group to another over a wide area, with each group incorporating

innovations into the designs? It is important that archaeologists are relying upon stylistic and

decorative traits, visual elements to identify these ceramics. Hamilton has repeatedly asserted

that these speculations illustrate sorne of the shortcomings of archaeological research in this

region (ibid.). He argues that archaeological sites must be excavated using good stratigraphie

controls, that good survey and sampling strategies are required for locating the sites

themselves, that detailed inter-site comparisons are needed, and finally that solid sociological

explanations are required to explain what brought about the overlaps between the different

cultures.

Arthurs (1978: 58) observed that Sandy Lake ware, which Birk (1977) argues is

diagnostic of the recently defined Wanikan Culture, was corn mon in Northwestern Ontario.

Initially, Sandy Lake Ware was found from northwestern Wisconsin westwards across east­

central ~1innesota into the extreme ~ssissippi River headwaters region. Cooper and

Johnson (1964) found it associated with Clam River focus pottery and Blackduck ceramics at

several sites in northern Wisconsin and northern ~nnesota. The Sandy Lake pottery is

clearly different from Blackduck type ceramics both in its construction and treatment

(Cooper and Johnson 1964: 475; Arthurs 1978: 59). Cooper and Johnson (1964: 479)

postulated that, although more data were required, Sandy Lake ware probably followed

Blackduck in northern ~nnesota.

Arthurs noted that almost all the sites in Northwestern Ontario with Sandy Lake

ware were within a one hundred mile radius of the "hub" of the Wanikan Culture of

northern-central ~nnesota (1978: 59). All of the sites were located either beside or within

close proximity to major waterways that provided access to the ~ssissippi headwaters (ibid.).

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Unfortunately, although Sandy Lake ware was found associated with Blackduck ware and

historie trade goods, it remains difficult to establish the relations between those cultural

groups. Slight differences existed in the Ontario Sandy Lake ware when compared to that

found in Minnesota (ibid. 59-60). However, the late-prehistoric/ early historie context of the

Wanikan Culture caused speculation concerning its ethnohistoric identity. Wright (Koezur

and Wright 1976: 39) argued that it was Assiniboine, while Johnson (Rackerby 1975: 479)

asserted that it represented the proto-historie Eastern Dakota. Dawson, on the other hand,

stated that it represented the incursion or influence of Mississippian peoples from the south

into Northwestern Ontario. Arthurs refrained from drawing any conclusions as to which

ethnie groups created the Sandy Lake ceramics. Instead, he concluded that future research

should consider its distribution and its stratigraphie and temporal relations with the

Blackduck, Selkirk, and European cultures; and with similar pottery types in Minnesota and

Manitoba.

As ever, the questions concerning the ethnic affiliation of each cultural tradition

remain unanswered. Archaeologists have deemed specifie ceramic elements to be indicators

of cultural traditions. Yet, it is difficult to establish the cultural affiliation of sorne ceramics if

elements of two different and possibly not contemporaneous cultural traditions are present.

Wright (1968b) examined the Ojibwa bands who occupied the northern shores of the Upper

Great Lakes. He argued that it would be "anticipated" that the Ojibwa hunters and gatherers

of that region differed in a number of important aspects from their kinsmen to the west and

the south (ibid. 98). Their kinsmen to the west occupied a richer gathering environment,

while their kinsmen to the south relied substantially on agriculture. Unfortunately, he fai!ed

to identify the specifie bands of the Ojibwa in question. Wright (ibid.: 105) noted that the

evidence of the Ojibwa along the northern shores of the Great Lakes was sparse and recently

obtained. However, these weaknesses in the information provided by the archaeological

record could be "compensated" by the stratified sites containing debris from seasonal

occupations accumulated over a considerable period of time. The evidence provided by these

sites enabled Wright to examine the culture history of the Ojibwa from the historical period

back to approximately the tenth century (ibid.).

Wright's argument is riddled with unsubstantiated claims. He suggested that the

isolated location of the northern Aigonquian speakers meant that their culture had remained

intact until it was "effectively studied by trained ethnographers" (ibid.: 106). Wright assumed

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that these peoples were not affected either directly or indirectly by the changes that occurred

among the other groups around them. This statement presumes that these peoples did not

move around and that they had always resided in this region. Furthermore, Wright fai!ed to

provide any ethnographie evidence that cultures remained intact over a long period and that

the physical environment remained statie. Instead, he assumed that the evidence indicated

that ceramics were either a borrowed trait, or an erratic foreign element that was weakly

integrated into the indigenous culture. Evidently, two or more different ceramic traditions

were mixed in single components, while the frequency and the presence of the various

ceramic traditions varied through time at single stratified sites. Apparently, according to

Wright, each individual ceramic tradition had a "heart" outside the region in question where

it represented a unified and developing cultural element.

Wright argued that homogeneous lithic assemblages found at Ojibwa sites were,

unlike the ceramics, not subject to spatial and temporal inconsistencies. He maintained that

this "paradoxical" situation could be eXplained in terms of the social behaviour of the

Ojibwa. Wright based his subsequent proposition on McPherron's (1967) and Owen's (1965)

claims that the archaeological situation around the Upper Great Lakes could be eXplained if

one accepted the notion that, in areas of low population densities, exogamous patrilocal

groups acquired women from considerable distances, resulting in a stable male culture and a

mobile female culture (ibid.: 107). Wright argued that, as pottery manufacture was a

manifestation of female culture, the mixture of traits reflected the high mobility of women

amongst different groups. Wright asserted that the relative stability visible in the lithic

assemblages was a natural expression of male cultures. Although Wright assumed that men

created the lithics and women created the ceramic objects, he provided no evidence to

substantiate why he drew these conclusions. The lithic assemblage, Wright maintained,

possessed a "local character" that was associated with the drainage systems in the region and

hence they could be used to make broad spatial comparisons. This conclusion was supported

by the paucity of exotic siliceous stone and other stone trade items in the archaeological sites

in question. The women who used different ceramic traditions in adjacent areas

accommodated to the patrilocal residence pattern which existed in each region. Wright

claimed that the men were closely bound to their specifie localities since they required an

intimate knowledge of the local faunal resources to ensure the survival of the group (ibid.

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107). This statement is arguably supported by the ethnographie studies conducted by Rogers

(1963) and Bishop (1976).

Culture change, for Wright, was evidently graduaI and he believed this reflected the

semi-isolated development of conservative hunting and fishing bands who, because they

maintained "sufficient contacts" with each other, remained "broadly similar". This article

substantiates the argument that it is possible to discuss the archaeological record of this part

of North America without clearly delineating cultural boundaries and correlating cultural

periods with specifie ethnic entities.

Even examinations of mortuary practices can be useful. Johnson and Ready's (1992)

study, although it is unconcerned with the physical remains themselves, is concerned with

mortuary practices of a specifie group of people. If the mortuary practices are established in

datable archaeologicallayers, it is possible to as certain the mortuary practices associated with

specific cultural traditions. They examined four burial masks from the MdGnstry Mound 2

belonging to the Blackduck period. They concluded that the masks were probably associated

with rites and ceremonies related ta the Earth Diver, Water Panther, or other spirits

discussed by Hall (1979), who considered Menominee or Potawatomi mythical divers.

Johnson and Ready (1992), like Tobenson and his colleagues (Tobenson et. al. 1992; 1994),

did not consider the ethnic or biological identity of the individuals who lived during the

Laurel and the Blackduck periods. These results are use fuI for cultural identification but do

not provide information regarding ethnie or biological identity or any convergence between

the two.

A disconnection exists in the relationship of the identity of the peoples who used the

habitation sites, camp sites, and were buried in this geographical region. It is impossible to

correlate the ethnie, cultural and biological identities of the peoples whose lives are indicated

by evidence in the archaeological record. This is caused by the numerous difficulties that

exist in connecting these different identities. The complex nature of the archaeological

record of the Boreal Forest region probably needs more detailed investigation.

Unfortunately, even if it was possible to obtain more information about the culture-history

of the region, it remains unlikely that we would know more about the ethnie, social, cultural

and biological identity of the people who created rock image sites in this region.

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(cl) Can biologieal eviclence resolve the problem of ethnie iclentity?

Osteological, biological, and genetic evidence gained from analysing bones, blood

groups, DNA, and mitochrondrial DNA informs the archaeologist about the genetic

relationships, not about the cultural affiliations, of the groups involved. Despite these

limitations, genetic and biological evidence offers sorne hope of aid for those seeking to

determine whether a common ancestry existed, to what ex te nt neighboring groups have

interbred, or even from where sorne cultural elements were derived. Biological anthropology

itself can be subdivided according to whether the scholars were concerned with the

osteology, human blood group analysis, or mitochrondrial DNA.

Three groups of researchers conducted osteological examinations of the burials from

the Rainy River Region of Minnesota and Ontario (Ossenberg 1974; Tobenson, Aufderheide

and Johnson 1992; Tobenson, Langsjoen and Aufderheide 1994). Osteological examinations

of bones recovered through excavation of the burials can aid the identification of specific

groups since skeletal traits are often associated with particular archaeological cultures.

Ossenberg, in 1974, attempted to trace the lineage of certain historic Plains people

back to the Woodland period, and to test the hypothesis that they were descended from

prehistoric Hopewell groups (1974: 15). The frequencies of twenty-six discrete

morphological traits of the skull were analysed for a sample of 942 individuals from 19

locations. It employed a multivariate estimate of biological distance to explore the relative

"affinities" within an archaeological and ethnographic framework. Ossenberg drew her

samples from archaeological complexes classified by archaeologists as burial mounds. The

assumption was that a complex represented the material culture of a single group of people

over time and that successive generations of this population are represented genetically as

belonging to different phases, cultures, or foci. The results demonstrated that the data taken

from the Laurel, Blackduck, Arvilla, Manitoba, Melia, and Devil's Lake complexes

represented a cluster of closely related populations ancestral to the Dakota, Assiniboine,

Cheyenne, and possibly the Blackfoot. Although they were closely related to several

Woodland and historic groups, their affinity to Illinois Hopewell was weak. She concluded

that comparisons needed to be extended to include Archaic period burials and those

associated with other Woodland areas within the Great Lakes Region to try to trace both the

antiquity and the geographic ramifications of this putative relationship (ibid.: 37).

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Two groups could be distinguished: the southern and the northern Blackduck

population. Ossenberg concluded that "southern" skeletons were similar to the historie

Assiniboine materials and the "northern" Blackduck skeletons were closer to the Chippewa

or Cheyenne (ibid. 37 and 38). She argued that more skeletal data were required for the

Laurel culture.

Analysis of the morphological traits was a useful beginning. lndeed, Lugenbeal (1978:

49), an archaeologist, argued the possibility that the skeletal differences observed by

Ossenberg between the "northern" and "southern" Blackduck populations could be

correlated with the Blackduck ceramic phases from the Smith site, in northern Minnesota.

Lugenbeal (1978: 49) observed that Ossenberg had noted the differences in the skeletons

from the Osufsen, and Shocker sites of the Mississippi headwaters region and from Hungry

Hall 2 and McKinstry Mound 2 of the Rainy River region in northern Minnesota. Ossenberg

(1974: 37, 38) had concluded that despite the similarities between the "southern" skeletons

and the historie Assiniboine materials, the "northern" Blackduck skeletons were closer to the

Chippewa or Cheyenne. He recognised ~bid.: 50) that the ceramics of the McKinstry Mound

2 burials were related to the later Smith site Blackduck phases, as were numerous rims found

in the fill of Hungary Hall Mound 2. Furthermore, the Osufsen site, which was the source of

the majority of the "southern Blackduck skeletons" had more ceramics that resembled those

belonging to the earlier Blackduck phase of the Smith site (ibid.).

Other scholars in archaeology or pathology and medicine (Tobenson et. al. 1992;

Tobenson et. al. 1994) postulated that specifie mortuary practices were related to specifie

culture groups in the Boundary Waters region of Northern Minnesota and western Ontario.

Perhaps differentiating between different mortuary practices could aid those scholars trying

to distinguish biologie al groups. Evidence of the mortuary practices included skulls lacking

occipitals, punctured long bones, eut marks, and the presence of red ochre. Pathological

changes in the bones suggested that infection had resulted in significant morbidity for these

peoples. Other pathologies found could have been caused by a variety of traumas,

degenerative joint diseases, and congenital abnormalities.

Tobenson, Aufderheide, and Johnson (1992) examined 929 long bones from 727

adults and 202 sub-adults buried in Mound 4 built by the Laurel people of the Middle

Woodland period. Four intrusive burials, or thirty-four additionallong bones, also in Mound

4, dated to the Blackduck period. Since none of these long bones was punctured, with

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intentionally placed holes, they were excluded from the study (ibid.: 507). Blackduck sites,

dating from AD 800 to 1400, co-exist along sites dating to the Laurel tradition in this region.

Holes were found only on the humeri, femora and the tibiae belonging to the Laurel

culture rather than the Blackduck culture (ibid.: 507). Tobenson, Aufderheide, and Johnson

postulated that social differentiation probably existed in the Laurel culture because not all of

the individuals were selected for bone puncturing (ibid.: 511). They concluded that a simple

non-achieved characteristic that included both sexes and adults and sub-adults would be

inherited group affiliation (ibid.: 512).

Tobenson, Langsjoen, and Aufderheide (1994) analysed the hum an remains from

Smith Mounds dating to the Laurel culture. These researchers examined the remains to

determine burial practices, describe more fully the skeletal collection, and generate sorne

important demographic values. The skeletal collection from McKinstry Mound Two served

as the control for their study. The results revealed that the people of the Laurel Culture built

the mounds around 95 Be. They postulated that each episode of burial contained the dead

from a one-year interval of time. Women and sub-adults under the age of three were

underrepresented and were, presumably, interred elsewhere. Life expectancy at birth was 20

years. The average male reached 177 centimetres in height while the average female reached

160 centimetres. Examination of the Harris lines suggested increased stress in the first years

of life. Red ochre was not significantly associated with gender but was much less likely to be

applied to adult skeletons.

This information is useful because it is possible that different biological groups have

distinct mortuary practices. Genetic data may indicate biological similarities or differences

among living groups of lndians. Biologists and geneticists se arch for genetic differences in

the hope that it is possible to solve the bigger question of how exactly different modern

North American lndian tribes are related to each other.

Many researchers wondered whether it was possible that genetic drift rather than

natural selection could explain the genetic differences between different groups of Ojibwa

(Matson, Koch, and Levine 1954; Szathmary and Reed 1972; Szathmary, Cox, Gershowitz,

Rucknagel, and Schanfield 1974; Szathmary, Mohn, Gershowitz, Lambert, and Reed 1975).

Szathmary and Auger (1983) considered the idea that these populations were descended

from one source. Although they considered three tribes in the Pacific Northwest, Ward and

his colleagues (1993), highlighted a valid point that linguistic differentiation could occur

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much faster than the rates of biological differentiation. However, they (ibid.: 10667)

concluded that it was equally possible to assume that population differentiation had preceded

linguistic differentiation.

Several studies were undertaken to examine the genetic markers among the Ojibwa

or Chippewa (Matson, Koch, and Levine 1954; Szathmary and Reed 1972; Szathmary, Cox,

Gershowitz, Rucknagel, and Schanfield 1974; Szathmary, Mohn, Gershowitz, Lambert, and

Reed 1975). These studies appear to build upon each other. This line of research provides a

complementary, but different, source of information for archaeologists and historians trying

to establish ethnic differences.

Matson, Koch, and Levine (1954) wished to identify the inherited blood factors of

the Chippewa Indians of Minnesota by examining the genetic markers. They discovered that

blood group 0 was the large st blood group and no individu al in the group tested had the

blood group B or AB if they were "full-blooded" Chippewa (ibid.: 416). They also examined

the genetic frequencies of this group to discover and compare the Chippewa genetic makeup

with that of the resident white population, Swedish in origin, to establish whether genetic

drift had occurred. Matson and his colleagues discovered that some genetic drift had

occurred amongst the Chippewa (ibid.: 425). These scholars also noted that, if the

characteristic differences in genes 0 and A were excluded, the genetic information gained

concerning the Chippewa was comparable to that of the Blood and Blackfeet in Western

Canada (ibid.). However, Eull-blooded Chippewa could be differentiated from members of

the Blood tribe by a higher R2, the absence of fj and a higher Ff (ibid.). They argued that the

discrepancy evident in the MN-Ss system among the Chippewa and the Blood tribes was an

expression of the higher M gene in the Blood tribe type. Matson and his colleagues identified

that the Chippewa had the highest frequency of R2 in comparison to other human

populations in the world. The genetic makeup of this group is significant for those

concerned with genetic markers.

Eighteen years later, Szathmary and Reed (1972) discussed their analysis of blood

taken from two widely separated Ojibwa communities living on reserves in Ontario, and

critically examined the results. They were also interested in genetic markers. Genetic data

were taken from the Pikangikum band in northwestern Ontario which they knew had been

exposed to continuous European contact since 1933 (ibid.: 657) and from the Wikwemikong

band on Manitoulin Island, northwestern Lake Huron (ibid. 656) which had been in contact

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with Caucasians for over three hundred years. These researchers built upon work conducted

to estimate the proportion of Caucasian genes in Indian populations. One of the factors

causing gene variability in the northern American Indian population was the entry of

Caucasian alleles into these gene pools. Szathmary and Reed (ibid.: 667) discovered that

European admixtures in the Pikangikum band in north-western Ontario were insignificant.

However, the authors argued that the sam pIe size taken from the Wikwemikong band on

Manitoulin Island was also too small to be able to "detect any selection" of alleles (ibid.).

The authors discovered that Rh was the most valuable blood group system for

measuring Cauca sian gene flow among North American Indians (ibid.). Szathmary and Reed

(1972: 668) asserted that the GM system was "the most informative of all the genetic

systems" if scholars intended to calculate the rate of gene flow into North American lndian

populations. Genetic markers were crucial for scholars wishing to calculate gene flow.

Two years later Szathmary collaborated with Cox, Gershowitz, Rucknagel, and

Schanfield to compare the serum protein and red cell enzyme systems of the Wikwemikong

and the Pikangikum bands as examples of different branches of the Ojibwa "tribe"

(Szathmary, Cox, Gershowitz, Rucknagel and Schanfield 1974: 49). Their experiments

demonstrated the presence of the genetic markers Al Naspaki and Cc Chippewa among groups

and Tf Dchi only in the Pikangikum band. Szathmary and her colleagues (ibid.: 53-62) were

shocked to discover that neither group had the Mongoloid marker Cm 1, 3, 5, Il.

Ceruplasmin was equal in both groups and all the individu aIs tested were B homozygotes

(ibid.).

Szathmary and her colleagues asserted that genetic flow was not entirely responsible

for the heterogeneity observed between the groups. Instead, genetic drift and the founder

effect had probably played substantial roles in shaping the genetic makeup of the groups

tested. They postulated that this had occurred because, at European contact, the Ojibwa

were not a single homogeneous group; rather they were small groups scattered over a large

region. Yet, these researchers realised that the small size of their samples, the short time

period of only 200 years which had elapsed for the bands to have a separate evolution, and

the 900 miles separating the Wikwemikong and the Pikangikum bands prevented the

researchers from statistically demonstrating the effects of other genetic pressures (ibid.: 63).

Several years later, Szathmary, Mohn, Gershowitz, Lambert, and Reed (1975) again

analysed the blood from 105 Ojibwa from the Wikwemikong band and 96 Ojibwa from the

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Pikangikum band. Szathmary and her colleagues (1975: 352) considered whether genetic

differentiation had occurred between the two populations in the period during which their

ancestors had lived in geographical proximity. Furthermore, the authors speculated that

genetic divergence and selection might have occurred in both groups after this population

split. They observed that both populations lacked the r" and the R 0 gene identified among

the cognate Chippewa in Minnesota. Szathmary and her colleagues (ibid.: 358) were surprised

at the extent to which the Wikwemikong and Pikangikum bands differed quantitatively and

qualitatively concerning the genetic characteristics of their blood groups. The Wikwemikong

band had the genes called Dia, r, Lua and B which the Pikangikum band did not have (ibid.:

359). DifferentiaI frequencies occurred for the R NS) and MS gene complexes for both

bands. The authors argued that these differences contributed to the "extremely high genetic

and phenotypic chi-square between both populations which was a measure of their genetic

divergence" and explained these differences (ibid.).

Szathmary and her colleagues concluded that it was a matter of genetic drift rather

than rapid genetic divergence amongst the Ojibwa when they stopped being nomadic

hunting bands, settled on reserves and had little contact with the "extremes of the Ojibwa

continuum" (ibid.: 363). The authors (ibid.: 365) postulated that genetic drift, rather than

natural selection, accounted for the genetic differences between the two bands.

Szathmary (1983) examined the possibility of people originating from one place and

collaborated with Auger to consider the idea that those populations descended from a single

source continue share sorne biological, linguistic, and cultural traits acquired through a

common heritage. They (ibid.: 289) argued that in theory a relationship in one sphere could

predict a relationship in other spheres. Szathmary and Auger (1983: 291) argued that

Goddard's (1979) model of historical development from Proto-Algonquian provided a

framework for analyses to be undertaken utilizing biologie al data (ibid.). They also realised

that the Cree and the Ojibwa were closely related and were so closely related that Wright

(1968b: 23) and Dawson (1983: 76) considered their distinction to be an anthropological

convenience rather than "ethnie reality". Szathmary and Auger observed that Dawson (1983)

disagreed with Rogers (1983) and Bishop (1983) but both groups suggested that Cree and

Ojibwa had, over a long period of time, lived adjacently in northwestern Ontario. Szathmary

and Auger (1983: 307-308) viewed this was an excellent case for them to examine by

measuring inter-lndian gene flow.

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No gene was identified to belong to the Aigonquian speakers in general, but

Szathmary and Auger (ibid.: 295) argued that a variant allele of the Gc system could be called

an Ojibwa marker gene. The presence of this allele was not detected in any other American

lndian population, induding the four Algonquian speaking groups: the Blackfoot, Cree,

Naskapi, and Montagnais. Szathmary and Auger posited that the restriction of trus variant

suggested that a mutation had occurred prior to the Ojibwa territorial expansion. lndeed, its

restriction to the Ojibwa suggests that this mutation is relatively recent, since the gene has

not had time to diffuse beyond the Ojibwa (ibid.).

Szathmary and Auger conduded that genetic data demonstrated that the central

Algonquian Cree and Ojibwa were similar to each other, although they displayed sorne

genetic differences. They explained this genetic similarity as "recent common descent from a

single joint ancestral population". Detailed examination of these differences indicated that

extensive genetic flow between the groups explained these data. They refrained from stating

whether the pattern exhibited by Ojibwa and Cree similarities and differences dearly resolved

the argument among Bishop (1976), Bishop and Smith (1975), Rogers (1983), and Dawson

(1983). However, Szathmary and Auger asserted that the geograpruc presence of the variant

allele of the Gc system, the Ojibwa marker gene, pointed to a recent population movement

by the descendants of the group in wruch the mutation first occurred. These results support

the daim that the Ojibwa resided in the northern Lake Huron-eastern Lake Superior region

prior to their westward expansion three hundred years ago (Szathmary and Auger 1983: 311-

312).

Ward, Redd, Velanica, Frazier, and Piiiibo (1993) raised a crucial point concerning

linguistic and genetic variation in the Americas, wruch is applicable to the debate about the

ethnic identity of the peoples in the central Subarctic. Ward and rus colleagues noted that

world studies of human population had conduded that because "major linguistic phyla

exrubit a pattern of dustering that is congruent with genetic dusters defined by genetic

markers" (ibid.: 1 0663), linguistic evolution probably parallels genetic differentiation in

humans.

They appraised trus observation by evaluating the linguistic and biological

evolutionary affiliations of three tribes of the Pacific Northwest. The results of their analysis

indicated that the ruerarchy of genetic relationships failed to match the linguistic ruerarchy,

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implying that the time span needed for languages to change into phyla and families was

significantly shorter than that required for molecular differentiation (ibid.: 10667).

The authors concluded that the "tempo and mode" of linguistic and genetic

divergence was discordant if they were compared over a short period of time (ibid.). This

discrepancy occurred because linguistic diversity was generated in a fundamentally different

way from genetic diversity. Furthermore, if language change was a cultural phenomenon

driven by historical and cultural events, then languages should experience periods of change

and stasis. Molecular evolution, in sharp contrast to language evolution, develops at a

steadier rate. Research on the mitochrondrial DNA of North American lndian populations

has meant that the biological relationship between modern and ancient peoples can be

examined. This mitochrondrial DNA research could easily supplant earlier genetic research

as well as research on blood types and osteology since it is probably more reliable. However,

it is still in its infancy and its limitations in aiding archaeological concerns need to be

established before this type of research is accepted as the solution to archaeological

problems.

Five mtDNAs (A, B, C, D, X) have been identified as directly descending from five

founding Asian mtDNAs (Wallace and Torroni 1992: 406-412; Schurr et. al. 1990; Torroni

et. al. 1992). What is fascinating for scholars, regardless of discipline, is that haplogroup X

was found amongst the Chippewa (Smith, Malhi, Eshleman, Lorenz, and Kaestle 1999). Very

few North American lndian groups have this marker in their genetic makeup. AlI five of

these haplogroups are found in Asia, which is presumed to be the homeland of all Native

Americans.

These haplogroups occupy central nodes in a phylogeny of New World mtDNA

haplotypes and are widespread throughout North, Central, and South America (Smith et. al.

1999: 272). Researchers have used mitochrondrial DNA to study the phylogenetic history of

the human genetic population and archaeological and anthropological questions about the

colonization of the New World (Lorenz and Smith 1994, 1996, 1997; Torroni and Wallace

1995; Stone and Stoneking 1993; Wallace and Torroni 1992). Lorenz and Smith (1996)

argued that sorne correspondence exists between language group affiliations and the

frequencies of mtDNA haplogroups in sorne tribes, while geographical proximity perhaps

influences the genetic similarity among other tribes. Yet, Smith and his colleagues (1999) and

Lorenz and Smith (1996) postulated that genetic drift was not so widely distributed as to

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explain the uniformity in the mtDNA haplogroup distribution evident amongst many tribal

groups of modern North America. Researchers should be aware of this if they wish to use

modern data ta assess ancestorj descendant relationships between living populations and

prehistoric skeletal material (Smith et. al. 1999: 272).

These advances in genetic technology have enabled archaeologists and linguists to

test hypotheses about the temporal and cultural origins of Algonquian history. Although this

research has revealed interesting information, these scholars do not question the ethnic

identity of the inhabitants at the time of European contact. Some researchers were

concerned with establishing whether the Proto-Algonquian speakers had a western homeland

prior to arriving in northeastern North America (Scozzari et. al. 1997; Smith et. al. 1999;

Schultz, Malhi and Smith n.d.).

Recent regional studies have investigated genetic diversity on smaller regional scales

(Malhi et. al. 2001,2003,2004; Bolnick and Smith 2003, Eshleman et. al. 2004). Their results

have indicated that populations within a geographical region exhibit genetic similarity that

indicates that genetic flow limited genetic drift. This contradicts the early studies of genetic

differences and their distribution in North America which had argued that genetic

differences resulted primarily from genetic drift (e.g. Schurr et. al. 1990). Shook (2004: 3)

argued that these early studies were undertaken with "a limited understanding of the genetic

diversity and its distribution geographically and temporally across the New World". The

mtDNA patterns provided by these small regional studies strongly supports the hypothesis

that North America probably was colonised by small bands of people who were sufficiently

large to sus tain gene flow but small enough for significant genetic drift to be evident (Malhi

et. al. 2002). Genetic drift gradually declined as populations grew and bands became more

sedentary. Consequently specific regional genetic patterns emerged (Shook 2004: 4). She

asserted that variation in geographically similar populations in northwestern North America

possibly resonates with shared cultural traditions, language patterns, and even recent

demographic history. Ancient populations from two specific locations within northwestern

North America were compared with ones from southwestern Ontario and the Central

Illinois River Valley (ibid.: 9).

Shook (ibid.: 8) examined how mtDNA patterns changed in a large region over time

and geographical space by comparing genetic patterns of ancient populations. She compared

the genetic patterns of ancient populations from different time periods in the same

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. ~.

geographic locality with the same time period in two different geographic localities. The

hypotheses generated from the archaeological record and historical linguistics were also

contrasted to establish the nature of the role of cultural factors in genetic variation in the

Northeast. This region of North America was chosen because the mtDNA variations in

these populations represented multiple language families (Malhi et. al. 2001) and the Norris

Farms Oneota which is the largest ancient population studied to date (Shook 2004: 4).

Modern Algonquian speakers have high frequencies of haplogroups A, C, and X but

low frequencies of Band D (Lorenz and Smith 1996; Malhi et. al. 2001; Scozzari et. al. 1997,

Smith, et. al. 1999). Only 3 % of ail native North Americans belong to haplogroup X and

individuals belonging to this group are absent in native South America (Smith et. al. 1999) .

Shook and Smith (2004) knew that linguistic studies of Algonquian demonstrated

that at least one extensive expansion had occurred in northeastern North America over the

past 3000 years. The samples used for MtDNA analysis for Shook and Smith's study were

taken from prehistoric samples that represented this time period (2004: 5). However, the

Winnebago and another language family also existed in this are a, namely the Northern

Iroquoian.

The original speakers of the Proto-Algonquian language, whose descendants

currently inhabit almost a quarter of North America, arrived in this Central Canadian region

from the northwest approximately 3000 BP according to Denny (1989, 1991), who based his

estimate upon linguistic relationships between the Algonquin and several West Coast

language groups (Sapir 1916; Haas 1960, 1965; Goddard 1975, 1994). Fiedel (1987, 1990) had

speculated that language and possible cultural expansion and diversification of the

Algonquians occurred between 2600 BP and 1500 BP.

All of the samples that were used for mtDNA sampling came from populations that

had burial complexes. Shook (2004: 21) observed that genetic continuity was evident in both

localities tested and that both populations tested were biologicaily unrelated. However, the

mtDNA haplotypes demonstrated that lineages were shared between ancient and extant

individuals in each locality. She concluded that these lineages have been present in the

Northeast for the last 3000 years, that the Northeast exhibited genetic homogeneity and that

"variation was distributed clinicaily", which could be explained as "gene flow restricted by

geography" (ibid.: 22).

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Shook conduded that her study highlighted how important it was to consider the

genetic analysis of prehistoric populations to "determine when the patterns of population

genetic structure of extant populations were established" (ibid.). She maintained that

examining genetic data even from populations dating from 3000 BP was useful for those

concerned with the interpretation of the relationships between different archaeological

traditions. She also speculated that patterns of genetic variation could be eXplained by

linguistic and archaeological data.

Parr, from another research group based in Canada, rather than in the D.S., as were

Shook and her coileagues, directed a project where morphological analysis was conducted in

conjunction with paleogenetic data obtained through DNA from the Armstrong Mound first

excavated by Kenyon in 1966 (1970, 1986). The Armstrong Mound is part of a large complex

of ceremonial mounds in the Rainy River region. Parr and his coileagues intended to identify

the founding Amerindian haplogroup of these skeletal remains. These results will be

interesting but the report will only be published once a complete bioarchaeological

assessment on this burial mound has been completed.

However, Bianchi and Rothhammer (1995: 1238) warned that mtDNA research

might not be the "panacea that will resolve ail our anthropological doubts". lndeed, it is

important to keep in mind that such genetic data can inform only the archaeologists about

genetic relations, not about the cultural affiliations of the group involved.

Osteological, biologïcal, and genetic information informs the archaeologist about the

genetic relationships, not about the cultural affiliations, of the groups involved. This body of

information is incredibly useful if genetic analysis is used to question linguistic and

archaeological theories and data.

Osteological analysis by Ossenberg (1974) tested the assumption that a burial

complex represented the material culture of a single group of people over time. She

conduded that comparisons needed to be extended to indude Archaic period burials and

those associated with other Woodland areas within the Great Lakes Region to try to trace

both the antiquity and the geographic ramifications of this putative relationship (ibid.: 37).

She identified two groups: the southern and the northern Blackduck population. Ossenberg

conduded that "southern" skeletons were similar to the historie Assiniboine materials and

the "northern" Blackduck skeletons were doser to the Chippewa or Cheyenne (ibid. 37 and

38).

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Tobenson and bis colleagues (1992, 1994) tested the ide a that specific mortuary

practices were related to specific culture groups in the Boundary Waters region of Northern

Minnesota and western Ontario during the Laurel and the Blackduck period. They posited

that differentiating between different mortuary practices could aid those scholars trying to

distinguish biological groups in the archaeological record.

Matson, Koch, and Levine (1954); Szathmary and Reed (1972); Szathmary, Cox,

Gershowitz, Rucknagel, and Schanfield (1974); Szathmary, Mohn, Gershowitz, Lambert, and

Reed (1975) searched for the genetic differences to try to solve the bigger question of

precisely how different modern North American lndian tribes are related to each other. They

searched for genetic markers to identify whether genetic drift rather than natural selection

explained the genetic differences between different groups of Ojibwa. Matson and bis

colleagues identified that the Cbippewa had the bighest frequency of R2 in comparison to

other human populations in the world.

Szathmary and Auger (1983) examined the possibility that different populations

descended from a single source continue share sorne biological, linguistic, and cultural traits

acquired through a common heritage. Hence a relationsbip in one sphere could predict a

relationsbip in other spheres. They concluded that genetic data demonstrated that the central

Algonquian Cree and Ojibwa were similar to each other, although sorne genetic differences

as a consequence of extensive genetic flow between the groups.

The work of Ward and his colleagues (1993) highlighted a key point that linguistic

diversity was generated in a fundamentally different way from genetic diversity. They stated

that if language change was a cultural phenomenon driven by bistorical and cultural events,

then languages should experience periods of change and stasis. Molecular evolution, in sharp

contrast to language evolution, develops at a steadier rate.

Examination of the mitochrondrial DNA of North American lndian populations

enabled the biological relationship between modern and ancient peoples to be considered. It

could supplant earlier genetic research, research on blood types and osteology because it is

probably more reliable. However, it is still in its infancy and its limitations in aiding

archaeological concerns should be acknowledged before tbis type of research is accepted as

the solution to archaeological problems.

Five mtDNA haplogroups (A, B, C, D, X) were identified as directly descending

from five founding Asian mtDNAs (Wallace and Torroni 1992: 406-412; Schurr et. al. 1990;

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Torroni et. al. 1992). Haplogroup X was found to exist predominately amongst the

Chippewa since very few North American Indian groups have this marker in their genetic

makeup (Smith, Malhi, Eshleman, Lorenz, and Kaestle 1999).

Lorenz and Smith (1994, 1996, 1997), Torroni and Wallace (1995), Stone and

Stoneking (1993), and Wallace and Torroni (1992) used mitochrondrial DNA to study the

phylogenetic history of the hum an genetic population and archaeological and anthropological

questions about the colonization of the New World. Sorne researches argued that sorne

correspondence exists between language group affiliations and the frequencies of mtDNA

haplogroups in sorne tribes, but geographical proximity may influence the genetic similarity

among other tribes. Others argue that genetic drift was not so widely distributed as to explain

the uniformity in the mtDNA haplogroup distribution evident amongst many tribal groups

of modern North America.

These advances are interesting and enable archaeologists and linguists to test

hypotheses about the temporal and cultural origins of Algonquian history, but this

technology does not allow us to determine the ethnic identity of the inhabitants at the time

of European contact. Shook's (2004) study concluded that researchers concerned with the

interpretation of the relationships between different archaeological traditions should examine

genetic data, even from populations dating from 3000 BP. She also speculated that patterns

of genetic variation could be eXplained by linguistic and archaeological data. Unfortunately, it

remains very hard to relate the results of these studies to the study of rock images in the

Lake of the Woods because archaeologists and historians remain unclear as to who precisely

lived in the region and the ethnic identity of the individuals who may have created these

1mages.

Section 3: The images created and used hy the AIgonquian speaking peoples

This section discusses the imagery created by the Aigonquian speaking peoples and

the Assiniboine. It has two goals. The first is to establish the ethnicity of different images

and the objects upon which they exist so that it can be determined which images were

associated with either the Algonquian-speaking peoples or the Assiniboine. The second goal

is an examination of the images as a means of communication to better understand the rock

image sites.

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It is widely acknowledged that visual representations play an important role in

communicating information to the viewer (Boone 1994; ]aritz 1993; Vastokas 1996). It is

likely that these images were polysemie in their meaning and pointers to further sources of

information. The individuals involved in the creation of the objects and their decoration

manipulated their meaning.

Images and the objects upon which they exist have been examined by scholars from

a range of disciplines, including art history, new art history, archaeology, and anthropology.

The attitudes, perceptions, and the discipline of each scholar also have influenced inevitably

the examination of AIgonquian images, whether etched, quille d, embroidered, drawn, or

beaded.

Sorne regions have been examined more than others. Faulkner, Prince and Neptune

(1998: 32) asserted that the bead working traditions of northeastern North America have

received "scant attention in comparison" to the quantity of work undertaken on the Plains

groups.

Moreover, sorne of these images exist on objects traditionally viewed as marginal

sources of information since the objects belonged to such categories as art, decorative crafts,

handmade objects, handicrafts, souvenirs, or garments (Densmore 1974 [1929]; Ritzenthaler

and Ritzenthaler 1970; Ritzenthaler 1972). Phillips (1999: 17) argued that this western

method of dichotomizing high art and crafts and souvenirs provided no framework for

understanding objects on which AIgonquian images appear, which she called "souvenirs".

She overcame this problem by combining anthropological and historical data in conjunction

with field, archivaI, and museum research to contextualize her analysis and discussion of the

meanings of the objects known as 'native souvenirs' and of the images upon them.

Overcoming these imposed terms is important. Brasser (1976), unlike Ritzenthaler

(1972), realised that garments made and decorated by Aigonquian speaking peoples could

only be understood as clothing if they were contextualised within an historical setting. Reid

and Vastokas (1984) hailed the exhibition entitled "From the Four Corners: Native and

European Art in Ontario 5000 BC to AD 1867" as a landmark in Canadian history because

both European and Native artistic traditions were given equal attention in terms of a single

chronological framework, and were examined as a mutually interacting aesthetic system in

response to a common set of historical, geographical, and cultural circumstances. Reid and

Vasto kas (ibid.: 9) reacted against the old categorisations of native art as "primitive and

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lac king a documented history." They asserted that these divisions only supported an

'apartheid status' for native art. They argued that, henceforth, these objects should no longer

be perceived as handicrafts but as important, although difficult, to understand.

The objects that concern us come from a very wide graphical region which

encompasses the Lake of the Woods area between Lakes Winnipeg and Superior, specifically

Northwestern Ontario, northern Minnesota, and southeastern Manitoba. The geographic

region in question must be expanded westward and eastward to include the Great Lakes

region to the east of Lake Superior and the Plains region west of the Lake of the Woods. The

Algonquian speaking peoples, who were probably residing in the region described ab ove at

the time of contact, were being pu shed westward and were influenced to some degree, both

direcdy and indirecdy, by different indigenous groups and recendy arrived non-native

peoples. It is likely that some Algonquian groups were pu shed into the Plains region in

conjunction with the Assiniboine.

(a) Is establishing the ethnie origins and its objects possible?

It is evident from earlier sections in this chapter that, at least by the early seventeenth

century, the Assiniboine resided seasonally on the western half of the Lake of the Woods and

would do so continually until the middle of the eighteenth century (Heidenreich 1987: Plate

37). The Algonquian speaking peoples, throughout this time period, had lived in the eastern

portion of the Lake of the Woods. They gradually took control of the region as the

Assiniboine moved westward into the Plains (Heidenreich and Noël 1987: Plate 40).

Essentially the Algonquian speaking peoples lived in this region for a long period of time.

Distinguishing between the images produced by the two groups is harder since

stylistic, cultural, and social influences can remain long after a group is no longer in direct

contact with the groups from whom it learned a particular technique and manner of doing

something. This task of distinguishing between the traits that are Assiniboine and those that

are Algonquian is limited to the nineteenth century, because much of the material was made

of perishable materials that frequendy fail to survive in the archaeological record.

Greene (2001: 1038) observed that for a long period of time quillwork was the major

decorative art form in the Plains. During the latter part of the nineteenth century, quill use

declined with the introduction of pony and, subsequendy, seed beads. Large simple

beadwork designs were created on a white background that stylistically resembles that made

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by the Plains Cree (DeMallie and Miller 2001: 1041). Whereas the Assiniboine, in contrast to

many other Plains groups, used the overlay stitch, which results in a flat, rather than a ridged,

surface (ibid.).

Rock image sites also exist in the Plains region (Keyser and I<lassen 2001) but the

"biographic" and the robe and ledger styles are quite different from those of the Canadian

Shield. Images that belong to the "biographical" style were created "to advertise a person's

standing in society and the world" (Keyser and I<lassen 2001: 244). This pers on was usually a

warrior. Keyser and I<lassen (ibid.: 224) argued that images deemed as biographie were

"largely "narrative"" since they portrayed everyday events and recorded historical occasions.

Images invariably consisted of different scenes containing large numbers of figures. The rock

images sites that are biographic in style date between the early 1700s and the late 1800s. The

robe and ledger styles associated with this region are connected to bison robes and the ledger

book paintings used during the late eighteenth and early nineteenth century (Keyser 1977,

Greene 2001: 1042).

Skinner's (1915) article is useful, sin ce it indicates how a group maintained decorative

traits and designs which were part of the original Algonquian group mindset, while changing

and gradually becoming part of another cultural mindset. He based his claims on the Bungi

Ojibwa, a Plains group originally from the Woodland region, who had not abandoned all the

Woodlands traits but had adopted and amalgamated sorne Plains traits. Skinner (ibid.: 315)

observed that their "decorative art" was only found on painting on raw hide, quillwork, or

bead work and that they used rectangular and triangular designs to create complex figures.

However, the Bungi often (ibid.: 317) thoroughly mixed the floral designs from the "forest"

with the Plains geometric images, while their "decorative art was more inclined to

conventional flower forms" (ibid.: 316). He concluded that (ibid.: 318) the Bungi used sorne

Woodland features because they were recent arrivaIs in the Plains region and that their

culture was under pressure from "outside influences". The Bungi also were slowly adopting

Plains cultural traits, su ch as the Sun Dance and other "folklore elements" (ibid.), including

various facets of the Plains religious, social, and politicallife.

Sager (1994) considered eight pairs of beaded moccasins, collected in southern

Saskatchewan, as an example of cultural borrowing by the Cree and the Ojibwa (Saulteaux).

Several bands of Cree and Ojibwa (Saulteaux) had become permanent residents of the

grassland borders as a consequence of the establishment of reserves in western Canada

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during the late nineteenth century. The Plains Cree were permanent residents of this region

before the establishment of the reserves. Sager (1994) concluded that the decorative elements

of these moccasins demonstrated that their makers had adopted Plains aspects of material

culture. His (1995) paper examined the origins and significance of the "crooked nose"

moccasin design of the Northern Plains. He argued (ibid: 38) that this design was identified

with the Blackfoot tribe but should be considered as generally Northern Plains, although it

had existed longer amongst the Blackfoot than any other group. Irrefutable evidence, he

asserted (ibid.: 42), existed for the presence of quilled and beaded crooked nose type designs

on Ojibwa and Iroquois moccasins dating back ta the 1700s. Sager concluded that evidence

of the crooked nose design was found on early moccasin types from many groups, who

added the longitudinal seam to the terminus of their centre longitudinal seam.

He argued that attention ought to be given to the design of moccasins made by the

Cree. He maintained that evidence existed that one or more Eastern Algonquian groups,

including the Cree and the Ojibwa, as well as the Métis had introduced the notion of vamp­

like decorations on moccasins amongst the Plains and the Intermontane groups (Sager 2000).

He (ibid.: 68) asserted, however, that both types, the false vamp and the form fitting vamp

type of moccasin, had slighrly different origins in the Subarctic region. The form fitting vamp

moccasins emerged during the late eighteenth century somewhere east of Lake Superior and

were the more widely distributed of the two types in the regions south of the Subarctic. The

false vamp moccasin, which was a simpler design, also had its origins in the Subarctic region

and the Red River region. It began gaining wider distribution during the early nineteenth

century, when it was worn by Cree, Ojibwa, and Métis and traded by everyone regardless of

whether they were native or not. Its use eventually spread as far south as Minnesota, to the

Dakotas, and northwest to the Saskatchewan River.

Objects made by the Algonquian speakers had an influence far beyond their linguistic

boundaries. Sager (2002: 76) maintained that no clear line of demarcation existed between

the Woodland and Plains groups in what he termed "artistic expression". Indeed, he asserted

that there were a "significant number of designs which eventually appeared in Assiniboine

quill- and beadwork which were omnipresent in the East". He suspected that part of the

problem in identifying Assiniboine quill- and beadwork stemmed from the fact that very litrle

may have existed in the first place. A second reason for the lack of distinction was that the

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Assiniboine, although they had moved westward, were associated with their allies to the East,

and with those in Red River and the Lake Winnipeg region (ibid.: 77).

He (ibid.: 80) contended that design elements were "too fundamental to be readily

assigned to any kind of regional exclusivity" since they were found throughout the entire

continent. However, by the reserve period, specific features enabled Assiniboine objects to

be identified (ibid.). They used lane stitch beadwork; the backgrounds of their quiilwork were

often undyed white, or dyed red or bright yeilow, and there were more dark green

backgrounds in their beadwork in comparison to other groups. They also widely employed

the bicoloured lozenge feather symbol. Assiniboine moccasins were decorated with three

bands of lane stitch beadwork, the centre of which was a darker contrasting colour, which

frequently formed part of the designs (ibid.: 80-81). Design elements usuaily included stacked

low triangles, or complex designs such as "radiating opposed isosceles triangles" and

rhomboids (ibid.: 81). The Assiniboine also continued to make quilled objects, although the

Blackfoot had abandoned this technique du ring the 1880s (ibid.).

Sager (ibid: 81) claimed that it was difficult to establish the precise date when the

Assiniboine started to utilise floral designs in their beadwork and quillwork for a fuiler

discussion), since the documentation on specimens from the early nineteenth century was

vague. This made it difficult to determine whether the Assiniboine or another group made a

specific item, although it had been obtained from the Assiniboine. However, Sager (ibid.: 82)

stated that a "limited amount of work could be reliably attributed to" them, but that the

farther away from the region where floral work was done, the more abstract designs became.

Specific design traits that are pertinent to different groups in different parts of North

America result from indirect or direct contact possibly involving either native or non-native

groups. However, a large body of historical and ethnographical literature exists, enabling

some of these traits and trends to be established. Some scholars have examined the

development of images on specific items to determine whether certain traits are Algonquian

or Plains (for example Duncan 1991; Sager 1994, 1995, 1996, 2000, and 2002). Others have

considered the evolution of imagery, now recognised as belonging to the Great Lakes region,

regardless of the object in question (penny 1991; Phillips 1984 and 1991; Whiteford 1991).

Still others have summarised ail of the studies conducted on Ojibwa bead- and quillwork

(Garte 1985).

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Sorne have considered the influences of other indigenous lndians groups, European

traders, and settlers regarding the range and type of designs utilised, as weIl as how their

meanings were manipulated (for example Lenz 1986, Phillips 1999, Lanford 1984; Peers

1999). Peers' (1999) interest lay principally in how the meaning of one octopus bag, made in

the early 1840s in the Red River region had shifted and changed from the time it was made

to its becoming a museum artefact. Sorne of the designs used by the Algonquians have

developed and changed in the shapes of images used in bead- and quillwork. The least

amount of change has occurred in the images on birch bark scroIls. A connection also exists

between the designs created using birch bark biting, bead- and quillwork, and the images on

birch bark scroIls.

It is important to determine whether the use of different designs has changed over

time and whether shifts in meaning accompanied any change in design and shape. It is

equaIly crucial to include information as whether changes have occurred in the execution of

these designs because the techniques used might be meaningful. Yet it is frequently very

difficult to establish which designs belong to which groups, especially if first, the criterion of

time is taken into account, and second, a group of lndians has changed from using geometric

shapes to floral designs. Fortunately, this shift has been tracked by Hoffman (1888, 1889,

1891), Schoolcraft (1983 [1860]), Densmore (1910, 1913, 1941, 1974 [1928], 1979 [1929]),

and Coleman (1947).

lt should also be remembered, as Braaten and Ellingson (1992: 27) stated, that

choices were made by the individual involved in creating these images probably reflect their

cultural group. At the same time, King's (1991) arguments regarding western coIlecting biases

must be remembered. What has survived from previous centuries may only represent what

was used for special occasions and not what was worn everyday (see Braaten and Ellingson's

1992 examination of moccasins belonging to the Ojibwa and the Sioux from the late

nineteenth century).

Densmore's (1974[1928]: 183) publication, based on informants from the Vermillion

Lake, White Earth, Cass Lake, Mille Lac, Leech Lake, and Red Lake reservations in

Minnesota, the Lac Court Oreilles Reservation in Wisconsin, and the Manitou Rapids

Reserve in Canada, concludes that a developmental shift occurred in design use. Geometrie

and "line" designs were older than floral designs. She discussed in great detail the simplest

designs and how they became more complex. She (ibid.: 184) established that the geometric

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patterns found on birch bark transparencies were copied and used in woven bead bands.

However, her informants told her that "in the early times" beads were often used as edging

on leggings and moccasins, consisting of small white opaque beads usually in combination

with simple line patterns. The main geometric designs, or units, as she termed them (ibid.),

were the star and a cruciform "combined from various lines and angles". Geometric images

were often combined with images such as "a rose, a star, a heart and a butterfly" (ibid.: 185).

Densmore differentiated between patterns with angular outlines and those that had

geometric designs. She observed that patterns with angular outlines were believed to be

similar to those made by "the white race" (ibid.). Geometric designs were deemed very

suitable for woven beadwork while those patterns which had angular outlines were best

adapted for use in applied designs. She, like Speck (1937), observed that the double curve

pattern was used and that angular patterns represented leaves. Several informants told her

that the bird was often used as a dream symbol, while the star was a "favourite" pattern as a

dream symbol (1974[1928]: 185). She subsequently discussed how the double curve motif

had developed and reviewed the literature regarding its physical distribution amongst the

AIgonquian groups north and south of the St. Lawrence Seaway. She noted that three of her

informams used this motif for the fronts of moccasins and as paper-cut designs from birch

bark.

Densmore discussed floral designs and patterns in considerable depth. The "rose"

image occurred when the lines and angles of the geometric patterns were combined. The

wild rose could be considered as the representative flower of the Chippewa since it existed

"in profusion throughout the country" (ibid.: 186). She argued that one of the oldest floral

designs was the "round-bead pattern" and that the "grouping of the four dots with or

without a smaller dot in the center is a natural development of designs" (ibid.). Individuals

who wanted designs that imitated nature used these floral designs. However, her informants

assertion that the later objects that used these images had no artistic value indicated shifts ln

the development of these designs ..

Informants distinguished between the older patterns of flowers and leaves and those

that have been prevalent since 1860-1870. Densmore (ibid) postulated that this was possibly

the time period when the Chippewa came into extensive contact with the white populations.

Densmore ascertained that the earlier floral designs were deemed "truthful", while the

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r·,

subsequently "modem" Chippewa designs "lacked truth" as well as "freedom of expression"

(ibid.: 187).

Densmore also described at great length the images cut from birch bark using

scissors, which aided the women to create designs. She established that the early cut-outs

were made using a sharp fish bone; the pricks being placed close together and then the bark

eut along the lines with a knife (ibid.: 188-189). These eut-outs were principally used for

floral beadwork but could be used for any other decorative work (ibid.: 188). They included

leaves, flowers, angular patterns, and double-curve motifs. The women seldom exchanged

patterns, "but a good designer" often traced patterns for less gifted workers (ibid.:189).

Densmore discussed the applied beadwork at length, arguing that it was considered easier

and older than woven beadwork. She argued that "in early times" the bead embroidery was

placed on the broadcloth of the garment to be made. Later, the embroidery was applied on

black velvet which was subsequently applied to the garment (ibid.: 191).

She identified the three simplest patterns that she posited were probably used first:

"the jumping pattern, the zig-zag, and the ottertail pattern" (ibid.). Women used the designs

they created using the birch bark cut -outs. Densmore described at considerable length how

these designs were transferred to the fabric so that they couId be utilised. She maintained

(ibid.: 192) that the admiration of colour, as a consequence of using coloured rather than

white beads, had led the women to lose "their appreciation for graceful lines, and the art

value of their work is further impaire d, if not entirely destroyed". White beads, regardless of

whether they were opaque or opalescent, were used for backgrounds.

Woven beadwork was for Densmore the continuation of an early form of porcupine

quill work (ibid.) and she described in considerable depth how this was undertaken. She

ascertained that the person who wove the beadwork never followed a pattern while weaving

and rarely repeated a pattern (ibid. 194). She (ibid.) observed that sorne bead workers used

birch bark transparencies as suggestions, while others had "the patterns in their heads".

Densmore, (1974[1928]: 329-397) repeated Schoolcraft's (1857) observations and

comments about birch bark biting. Schoolcraft (1857: 631) had described this technique as

dental pictographs and noted that it made use of the fine inner layers of the bark of the birch

tree. Both he (ibid.) and Kohl (1860:213) described the designs used as flowers, human

beings, and fancy baskets. Yet Kohl's (1860: 413) remark about the creation of a design of a

tomahawk contradicts Schoolcraft's (1857:631) conclusion that it was a "pretty art" and an

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example of one of the first "imitative and aesthetic arts" amongst the Ojibwa. Kohl (1860:

412-414) visited a women who was a birch bark biter and observed that she used her only

remaining tooth on her upper jaw to create a wide variety of designs. He (ibid.: 413)

described her selecting a suitable piece of bark and putting it into her mouth. Kohl (ibid.)

discerned that she did not cut through the bark but only pressed it with her tooth so that

when the designs were held up to the light they resembled porcelain transparencies.

Densmore, noted (1974[1928]: 393) that Speck (1914) recorded modern examples of

this art form amongst the Montagnais and the techniques used by the women to create these

images. She determined from her informants (1974[1928]: 393) that the designs to be used

were in the mind of the pers on prior to biting the birch bark. One of her informants told her

that the piece of bark was placed between the upper and lower teeth, generally between the

eye teeth, while the bark was slightly twisted between the teeth (ibid. 393). Densmore (1974

[1928]: 394) discovered that if two or more pieces were indented simple patterns were used,

but if the designs were complex then only one piece of bark was bitten at a time. She (ibid.:

393-396) identifie d, described, and provided numerous examples of birch bark biting on

several plates in this publication. Densmore (ibid.: 396-397) established that sorne of the

designs were subsequently used as patterns for beadwork and that etching and "self­

patterns" were created on the surface of birch bark containers. Descriptions were provided

of the containers, how they were made, and how they were subsequently used.

Densmore (1941) provided additional information from her fieldwork in northern

Minnesota and southern Canada. She observed that only human teeth were used and that the

marks were made using the eye teeth and the side teeth (ibid.: 678). She asserted that it "was

not unusual for 12 thicknesses of bark to be inserted at a time" (ibid.: 678-679) but knew of

one example that had 241ayers of bark. She stated that (ibid. (1941: 679), according ta her

oldest informants, such work was undertaken only by women, in the maple sugar camp, in

the evenings once work was completed. These transparencies were done at this time of year

because the bark of the birch tree was soft and fresh. Since many of Densmore's informants

were more than 80 years old, this information dated this practice "back about a century"

(ibid.). Densmore observed that Schoolcraft and another unstated "early writer" had

mentioned birch bark bitings but that this art form had not been discussed by "traders and

explorers" (ibid.). She established that the designs included geometric, abstract, or

conventionalized natural shapes such as "roses and stars, and there were sorne animais and

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/--~

/'

Indians" arranged in what Densmore termed "running patterns" (ibid.: 679). Ber informants

told her that only older women eould do these transpareneies, since middle aged women

laeked "the mental concept and their work was not arf' (ibid.) (italies are Densmore's).

Densmore's (1941) article eonsidered another unnamed form of imagery using birch

bark. Bireh bark was eut with a sharp edge, possibly a fish bone or a knife, since points were

prieked in the bireh bark and then the bark was eut between the points to ereate a pattern.

Densmore (ibid.) deseribed the patterns as "angular" but she observed that the zig-zag

outlines ereated in this manner were used to make bead patterns on moccasin cuffs. The use

of scissors, Densmore (ibid.: 679-80) observed, made possible a new form of art using birch

bark to create "little pictures or silhouettes" but these, like the birch bark biting, were only

made for pleasure. Anything could be cut including "conventional flowers, and leaves,

changing the curves to straight lines" (ibid.: 680). She asserted (ibid.) that the Chippewa, in

northwestern Minnesota and southern Canada, argued that these designs were "interpretations

as natural forms and maybe regarded as art [.]" (italics are Densmore's). Ber informants told

her that these designs in their beadwork came after the geometric patterns.

This article supplied additional information regarding the development of the floral

beadwork. Densmore discovered from her informants that use of conventional flowers and

leaves as designs elements eould be viewed as "art" and was viewed as an interpretation of

nature. This is interesting since it appears that her informants are talking about "art" which

means that a western idea had become part of their culture. These patterns according to her

informants arose after the development of the geometric designs and before the modern

floral patterns which imitated nature. It could be eoncluded that she thought that her

informants possibly adopted, or imported the western idea of art.

Friedl (1944: 150) observed that information from her Chippewa informant, from

Lac Courtes Oreilles in Wisconsin, contradicted both Schoolcraft's (1860: 631) and

Densmore's (1929: 184-185) information that only women created these images. Friedl's

female informant was taught with her brothers and her sister, by their father, a birch bark

game which taught them to invent stories from interpreting the patterns and figures that

were used to create these birch bark transparencies (FriedI1944: 149). Friedl (ibid.: 150) also

established, from her informant, that it was easier to separate the "tissue-thin layers" of the

birch bark if it was opened in a heated room while still frozen.

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Fieber (1978: 56) argued that the origins of the images found on birch bark bitings

were obscure but the technique developed in a casual manner. He maintained that this skill

was practiced for the pleasure of creating the object. Fieber (ibid.) asserted that birch bark

biting was used to create designs for woven beadwork since the designs were adapted for use

on headbands, knee bands, or shirts. He posited that the designs and skills involved became

more developed and gained artistic value as they were handed down over generations. This is

an interesting but unfortunately unsubstantiated statement. Dewdney (1975: 15) observed

that the thinnest cork layers of the birch bark were folded several times and then bitten using

the eye teeth and stated that the resulting pattern was revealed once the folded birch bark

was opened.

Oberholtzer and Smith (1995) argued that birch bark biting was becoming a lost art

which they observed had been recorded in the writings of the early ethnographers. They

(ibid.: 311) asserted that birch bark biting as a "truly indigenous art form" was distributed

throughout the boreal forest from the Atlantic to the Plains. From the seventeenth century

onwards, the increasingly large numbers of non-native peoples settling alongside them did

not influence its development. This is an interesting daim, since Phillips (1984, 1991 and

1999), Whiteford (1991; 1997), Penny (1991), and Lanford (1984) were in the process of

establishing that the meanings and the images used in beadwork, quillwork and embroidery

were influenced by Europeans.

Oberholtzer and Smith (1995: 312), like Friedl (1944: 150), argued that men also

participated in this activity, thus contradicting Fieber's (1978: 56) assertions that only women

practiced this art as a form of social entertainment. Oberholtzer and Smith (1995: 312-314)

debated whether women were the sole users of these images because evidence existed that

women frequently used images resulting from dreams and divination practiced on bumt

animal scapulae. Both (ibid.: 314) observed that Speck (1937), Davidson (1941), Spier (1915)

and Rousseau (1956) had recorded the characteristic symmetrical formation evident in the

images in the birch bark bitings. Oberholtzer and Smith (1995: 314) maintained that these

simple patterns were the "basic features of the double-curve motif' that was very prevalent

amongst the imagery of various Algonquian groups. Both Oberholtzer and Smith (ibid.: 315-

316) conduded that the socialization that occurred when something was presented as

entertainment, essentially creating images, was an important means of encoding and recalling

information required by the Aigonquians. So, despite birch bark biting being an example of

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indigenous 'art for art's sake', it was a means of learning new skills and assessing designs, new

ideas and cultural values. Both substantiated their statements by drawing upon their own

fieldwork, as well upon information Friedl (1944) obtained from a Chippewa woman.

Coleman's (1947: xi) descriptive study was based on fieldwork which she conducted

at the White Earth, Leech Lake, Fond du Lac, Mille Lacs, Nett Lake, Grand Portage, and

Cass Lake reservations in northern Minnesota. She drew extensively upon work by a variety

of people, including Hoffman (1891), Mallory (1893), Copway (1851), Kohl (1986 [1860]),

Lyford (1943), Densmore (1929) and Warren (1984 [1885]). She identified all of the

geometric designs, which included angular and curvilinear motifs, and what she termed

realistic motifs. She considered how the different types of images were utilised in a variety of

contexts, including social, material, and religious culture, amongst the communities she

examined. Nevertheless, it is possible to posit the idea that the material and social culture are

essentially the same.

Coleman examined the role of images in the material culture of the Ojibwa and (ibid.:

45) concluded that designs on clothing and bags were floral and geometric. However, if floral

work occurred on clothing, it was possible occasionally to find the double curve. She (ibid.)

observed that, if floral and geometric designs were used for birch bark objects, they

invariably were "arranged in bands" and the designs were "simple isolated floral figures".

Geometrie and realistic designs were usually found on textiles and the designs in bands on

yarn and nettle fibre bags. She concluded that none of the images, except for those on the

nettle fibre bags, held any symbolic significance.

Coleman (ibid.: 64) made five generalisations concerning the usage of images in the

category she called "social culture". Social classification did not influence decorative designs

except for "gens-totem associations", where she argued realistic representations of certain

animaIs were employed. Floral and geometric designs were frequently used for decorating

clothes worn for public occasions, but the articles worn by the chief were usually more

elaborate. Coleman (ibid.) established that social convention determined the type of designs

used by men and women. W omen used both geometric and floral designs for their own

clothes but "more ritually defined realistic designs" on ceremonial objects (ibid.). She

observed that in "more recent times" women decorated their husband's clothing and

weapons with geometric and realistic floral designs, while men previously utilised geometric

and animal figures. She (ibid.) observed that marks on "implements for games" only enabled

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them to be identified and these marks included simple geometric figures and realistic motifs

of men and animaIs. Colour, Coleman (ibid.) established, was used only symbolically for the

body paintings of warriors, hunters, the ill, and the dead. She noted these images were simple

geometric designs that did not hold any symbolic meaning. Her fifth generalisation was that

animal figures occurred more often in decorations that she believed were part of the category

that she called "social culture" rather than material culture. She observed that few designs

belonged to the social category, which included human beings, natural phenomena, and floral

designs.

However, Coleman (ibid.: 89) concluded that designs had an important place in the

religious context of the Ojibwa and that most ceremonial objects had specifie images wruch

either symbolised sorne phrase or practice of their religion. "Representations" of the bear,

panther, lynx, thunderbird, birds, turtle, otter, fish, and serpent existed on Midewiwin

ceremonial objects and scrolls. Designs of hum an beings, especially those having received

"mystic power", were indicated by "wavy lines around the head or proceeding from the

mouth". She observed that creatures and human figures were common but that all the

designs lacked details when they were used in a religious context. Floral designs were not

present.

Coleman also considered the history of Ojibwa designs from 1830 to 1947, since

none of the objects that she studied was more than one hundred years old and little

archaeological evidence existed. She (ibid.: 91) asserted that almost all of the cultural

exchange experienced by the Ojibwa of trus region was with the whites, and so she posited

that sorne of the greatest influences on the creation of the designs used by the Ojibwa

occurred with the introduction of cloth, such as broadcloth and velveteen, wruch replaced

rudes (ibid.: 92). Clotrung styles also changed, particularly clothes such as the vest, gauntlet,

and shoulder pouch (ibid.: 93). The final reason for the changes was the introduction of

beads of different colours and sizes (ibid.: 92). From information obtained from her

informants and examining museum collections, she learned that many designs came from

patterns of embroidery or cross stitcrung provided by government schools, such as the

booklet written by Lyford (1943).

Lyford's descriptive publication drew upon published sources and museum

collections and contained a substantial quantity of information concerning the "handicrafts"

made by the Ojibwa. Her study was written to be used in schools where these handicrafts

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had begun to be revived. Coleman (ibid.: 94) ascertained that booklets such as Lyford's were

used for over two generations and that the women she spoke to, between the ages of fifty

and sixty years old, only used the designs learnt from their white teachers at school. Later,

pattern books on lace introduced by Episcopalian missions in northern Minnesota became

an additional source of designs (ibid.: 95), which the native women used to crotchet.

Coleman (ibid.) argued that the imagery from the 1870-1930 period (i) was floral, (ii) lacked

cohesion and unit y, and was (iii) elaborate, (iv) large and (v) showy. Each of these

characteristics was examined in detail and Coleman observed that they existed on various

items of clothing, wood, and birch bark. Several geometric motifs (ibid.: 101-104) exhibited

design traits from other native groups, such as the Western Sioux, Turtle Mountain Cree, and

Plains Ojibwa, including the Western Sioux coyote track and forked designs. One seventy­

three year old informant in 1943 told her that the Ojibwa were aware that they tended to

assimilate designs they deemed "worthwhile" from other groups (ibid.: 101-104). Coleman

indicated that she was not entirely convinced that ail Ojibwa designs had strong European

influences but she admitted that this could be a false presumption.

She claimed that, although floral designs were present on objects dating to the 1870-

1930 period, they were not as common as from 1830 to 1870. She established from her

oldest informants that images belonging to the 1830-1870 period were not created using

patterns, but they were always weil planned (ibid.: 107). The images from this period were,

according to Coleman, classified as (i) geometric, floral and zoic, (ii) cohesive, (iii) simplistic,

(iv) smail, and (v) having "soft" colouring. Once again she examined each feature with regard

to objects in museums. She asserted that these were aboriginal Ojibwa designs or, "at least

had no evidence of outside influences" (ibid.: 111). Coleman's final and third period was

1940 to 1943, which she argued witnessed a considerable change in the attitude of the

Ojibwa regarding their designs (ibid.: 113-117). There was, she believed a lack of interest

amongst the youngest members of the Ojibwa populations in learning the craftsmanship of

their parents and grandparents. This was a consequence of commercialisation, the lack of

interest in preserving old designs, as weil as the education of the younger people in

government schools.

King (1991), an art historian, highlighted the existence of two biases that prejudiced

western knowledge concerning sub-arctic clothing. Although Densmore (1979 [1929], 1974

[1938]) and Hilger (1992 [1951]) provided detailed descriptions of men's and women's

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clothing amongst the ChippewajOjibwa, they only described their summer clothes. Firstly,

very little was known about winter clothing and secondly most published collections

included a large percentage of highly embelli shed and unused summer garments. King

postulated that information amassed by different researchers while working in this

geographic region exacerbated this problem. He used the example of twined bags and

referred to Phillips (1989)'s and Whiteford (1977)'s argument that it was very difficult to

determine which tribe had produced each object. However, he (1991: 91) argued that it was

possible to distinguish the 'arts' of the Anishinaabe peoples of the Great Lakes from those of

the Athapaskan peoples to the northwest and the Algonquian peoples to the East. He (ibid.)

postulated that art of any type was an important ingredient in maintaining the equilibrium

between early peoples and the sacred world, and he asserted that the motifs used in the

decoration of these art objects carried sacred and mystical powers. Yet, an additional reason

for the lack of win ter clothing and unembellished summer clothing could that these items of

clothes were used to the point that they wore out or they were not perceived as important to

collect.

Brasser's (1999) article provided sorne useful pieces of information. He (ibid.: 49)

argued that highly elongated triangles were characteristic elements in early paintings of the

Great Lakes region. He found that on indigenous shirts in a collection from New France

long narrow triangles were often combined with shapes that were reminiscent of feathers,

forked bird tails, and arrows. He also observed images of birds worked in quills attached to

the bottoms of the bags in this collection.

Lanford, an art historian, (1984) examined several Winnebago bandolier bags also

called pony bags, shoulder bags or friendship bags. She used the term band olier bags since it

suggested that the most common use of these bags was ornamental. She contended that,

although this bag had several styles in North America, within the Great Lakes region it had a

decorative rather than a functional role. The bag's shape had evolved either from European

shot pouches or from pouches used by native foot travellers to transport provisions (ibid.:

30). Prior to the nineteenth century, the bases of these bags were dyed black-brown or dark

smoked tan and decorated with quillwork in the Great Lakes area and eastwards. Bags made

du ring the nineteenth century were covered in the floral beadwork typical of the Great Lakes

region. Lanford (ibid.) asserted that, by the mid-nineteenth century, these bags had become

part of the assemblage worn with one's best clothes. She arrived at this conclusion noting

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that bags belonging to this period had fragile cloth foundations, and that some bags did not

have a pocket, or had un-backed beadwork. Lanford (ibid.: 36-37) suggested that several

features of construction and decorative elements made bandolier bags easy to identify, and

that a predominance of certain colours existed in their woven beadwork. She (ibid.: 37)

stated that there was a distinct lack of symmetry in Winnebago bags in contrast to bags made

by Algonquian groups. Lanford concluded that sin ce relatively few differences were evident

in bandolier bags, it was possible to argue that each person who made these bags had a

distinct conception of the decoration before its creation. Whiteford (1986), like Lanford

(1984), examined four bandolier bags which could be dated since documentation exists as to

their provenience. He (1986: 35-36) discussed their size, proportions, materials, and the

techniques used to create them, as well as their structure, decoration, and the beaded designs.

Whiteford (ibid.: 38) compared these four bags with bandolier bags from other museum

collections to try to learn who might have made them. He (ibid.: 43) concluded that the four

bags represented a stage in the evolution from the small buckskin pouches of the early

eighteenth century to the large ornate bandolier bags that emerged between 1850 and 1860.

He argued that, by the 1870s, these bags had achieved the basic styles to be used for decades

in the Great Lakes region.

Lanford (1986) discussed the development of woven beadwork in the Great Lakes

area. She posited that the Chippewa, Potawatomi, Menominee, and Winnebago of the Upper

and Western Great Lakes areas, provided greater quantities of woven beadwork from the

nineteenth century onwards. During the late eighteenth and early nineteenth centuries,

geometric and straight-line motifs predominated. Lanford (ibid.: 62) observed that these

motifs could be found sewn and woven in the porcupine quillwork of this region dating back

at least to the early historic period. She also (ibid.: 63) observed that relations could be

posited between the geometric motifs of woven beadwork and those found on stone, pottery

and shell objects dating to the prehistoric period. Geometrie and zoomorphic forms and

human design elements, were incorporated, carved or incised on antler, wood, bulrush mats,

scraped birch bark containers, and porcupine quillwork from the historic period (ibid.). Both

Lanford (ibid.) and Lessard (1986) postulated that woven porcupine quillwork and fibre

weaving techniques contributed to the evolution of woven beadwork. Appliqué floral

beadwork replaced this woven beadwork in the Great Lakes area during the late nineteenth

century. Lanford (1984: 64) argued that the speed of this transformation demonstrated that

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styles could shift according to fashion in a very short period of time. He (ibid.: 64-65)

suggested that additional research was required to determine precisely when woven quillwork

declined and to pinpoint possible European influence upon the development of woven quill­

and woven beadwork motifs in the Great Lakes region. She hesitated to ascribe direct

assimilation of non-Indian motifs in the Great Lakes area, but stated that it was unlikely that

highly complex examples would suddenly appear.

Phillips (1984: 418) disagreed with Lanford (1984) regarding all the motifs and their

special co-ordinates. In her short paper, Phillips, attempted to understand the manner in

which these images carried and conveyed information. She developed the idea that an image

is polysemie and its meaning can be manipulated. Phillips (ibid.: 418) observed that the

geometric motifs, deemed to be the oldest types of images used by the peoples in the Great

Lakes region, existed on the fringes at the bottom of many transitional loom-woven bag

types, while large curvilinear floral designs in appliquéd beadwork were found elsewhere on

the bag. She posited that this mixture of images may have occurred because of the threat

posed to indigenous traditional religious institutions as a result of increased missionary

activities. In addition, the intensified White presence during the nineteenth century might

have produced this intentional marketing of visual imagery. She argued that the geometric

imagery probably was associated with the Midewiwin and other indigenous religious practices

that appear to have been in decline during the nineteenth century. Phillips (ibid.: 411) posited

the idea that it was doubtful that similar complex designs on clothing could be equally

meaningful.

Phillips (ibid.) stated that the 'geometric designs' on the birch bark scrolls belonging

to the Midewiwin had symbolic meaning. One strategy to determine the meaning of these

designs, Phillips posited, involved examining a group of quilled and woven designs from an

early period that might have been sources for the later woven beadwork. Hence she (ibid.:

416) analysed several designs on items from the Jasper Grant collection to demonstrate that

visual designs varied in time and space. She utilised this collection, despite difficulties in

specifically attributing various items because it consisted of images that were "iconographie

representations of cosmic spirits" (ibid.: 412) that were used "concurrently" during the first

decade of the nineteenth century, just before intensive White settlement which had

"accelerated disruptions of traditional religious systems" (ibid.). She claimed that people who

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"were and had been in close contact with each other" made these objects, which, therefore,

probably were shaped by a "shared and widespread" "world-view" (ibid.).

One of the several examples she considered was a group of early nineteenth century

finger woven bags with images that she stated alternated between "figurative design and

abstraction" (ibid.: 414). Phillips (ibid.: 415) claimed that the woven bags in this collection

"display a fascinating range of imagery". She (ibid.: 416) argued that shapes, or design

elements, as she termed them, such as "interlaced wavy lines," zig-zags, and wavy lines, were

"the common vocabulary" utilised to infuse "spirit power in the Great Lakes art". She

believed that these images dated from the early contact period to the first part of the

twentieth century. Unfortunately, she did not provide any pictures of the images. She

referred to them as "Thunderbird", "Underwater Panther", various Images of

"Misshipeshu", and a variety of zigzags, which she appeared to interpret as being "the chief

manifestations of the powers of the sky spirits, lightening and thunder" (ibid.). Although this

is interesting, she did not indicate her source of information for naming the shapes that she

identifies, or the ethnographie sources she drew on to provide the meaning of these images.

Later in her discussion, she (ibid.: 417) utilised Hoffman's descriptions of the imagery

used on the Midé costumes at the end of the nineteenth century. She concluded that, since

zigzag and wavy lines existed on their ritual clothes, their meaning had not changed despite

the changes in techniques and materials over time. These design elements "still expressed

symbolically the cosmic powers whose protection was reaffirmed" during the Midé

ceremonies. Other images, such as "crosses", wavy lines, human figures, and ho ur glass

images, were examined and meanings attributed. Crosses were interpreted as the four

cardinal winds that "blow across the surface of the earth from the four cardinal directions".

They signified the "transition between the upper and the underworlds" (ibid.). She argued

that images of Thunderbirds or human figures often appeared as geometric figures on the

woven bags from the Grant Collection (ibid.). Phillips suggested that bandolier bags dating

from the late nineteenth century could be "mapping the cosmos and the spirit forces", but

she realised that not all of the bandolier bags had beadwork and imagery similar to those of

the Grant collection. Many loomed bags dated around 1900 had large geometric floral

motifs.

Phillips argued that these abstract designs ought to be interpreted as having symbolic

rather than decorative meanings. She (ibid.: 418) postulated that the obscure symbolism and

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hidden meanings were perhaps what was left of a religious system forced to go underground.

The abstract images in the art of the Great Lakes region created during the nineteenth

century were a means of expressing the concept of severallevels of reality and the visionary

perception of this reality. This could explain, she believed, why the older geometric images

were used on the bottom of bags that had floral imagery. She concluded that religious and

spiritual concepts were expressed by means of "abstract motifs". She claimed that early

writers, who remain unnamed, asserted that geometric images were connected to personal

dream experiences. The images, she maintained, were created in a "concrete visual form" to

keep the "blessing of the guardian spirit" but the vision itself must remain private to retain

its power (ibid.). Phillips asserted that these images should be called "ambiguous" since they

were capable of altering their physical appearance, which she maintained was a "basic belief

of Great Lakes lndian belief' (ibid. 419). She concluded that during the nineteenth century

the different styles of abstract imagery used reflected not just numerous levels of reality, but

what she called "particular visionary perceptions of these realities" (ibid.).

Seven years after Phillips (1984), Whiteford (1991) postulated that it was possible to

distingwsh Anishinaabe material culture from that of other Algonquian groups and also from

that of Athapaskan tribes to the northwest of the Great Lakes. 'Anishinaabe', he argued

(ibid.: 74), was an Algonquian name used to describe the Ojibwa/Chippewa who arrived with

other Algonquian groups around the Great Lakes from the East during the early 1800s. He

wished to identify the key traits of the Anishinaabe arts and considered weaving, beadwork

and work on birch bark. Much of this information was already discussed at great length by

Lanford (1986), Lessard (1986), and Hoffman (1891). Whiteford maintained that

Anishinaabe designs were bolder in conception and highly distinctive in the use of strongly

beaded backgrounds with strong floral patterns compared to those of the Cree and the

Athapaskans (Dene). He (ibid.: 76-77) claimed that the sophisticated weaving techniques

used by the Anishinaabe combined with the range of designs for marked twined bags unique

to this cultural group. Furthermore, colour splitting designs and the 'protruding hairs' feature

found on the edges of the stems of Cree and Athapaskan floral patterns were relatively rare

in Anishinaabe beadwork (ibid.: 80). Whiteford drew heavily on Blessing (1963) and

Hoffman (1891). His aim of comparing the arts of one group with those of their

geographical neighbours was a valid attempt to deterrnine which motifs and styles were

executed on which items, and the specialties of each group.

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Duncan (1991), an art historian, considered two different types of bags: panel bags

and octopus bags. She argued that, despite the paucity of documentation for both types,

regional and tribal preferences were expressed in their form and decoration. Duncan

maintained that pre-nineteenth century roots existed for both types of bags, but she did not

provide any evidence to substantiate her claim. She examined each bag in its classic central

sub-arctic version, and described its geographic and diachronie distributions along with its

variants in the Great Lakes, Plains, Plateau, and Northwest Coast areas (ibid.: 57-65).

Duncan utilised a taxonomie approach to place the bags in a tree-like structure to indicate

the probable patterns of historical diffusion and stylistic development. The oldest

ornamented bags, Duncan (ibid. 57) argued, probably were sacred in contrast to the most

recent ornamental bags. She reached this conclusion because the more recent bags appear in

photographs taken at the turn of the nineteenth century and were "proudly displayed on

dress occasions" (ibid) as symbols of family pride, tribal affiliation, and personal prestige.

Penny (1991) would have disagreed with Whiteford's (1997) perspective concerning

these floral motifs. Penny (1991: 53) asserted that American lndian art history was concerned

with historical change and that this history should record and identify the events and

processes contributing to that change or innovation. He (ibid.) examined the historical

factors leading to innovations in dress style that accommodated the advent of the floral style.

Penny (1991) observed that Speck (1937), Barbeau (1930), and Brasser (an unpublished paper

given in 1987 that Penny used) had also considered the origins of this floral ornamentation.

Speck (1937), an ethnographer, argued that floral motifs grew out of indigenous double

curve designs prominent in the Penobscot decorative arts of the eastern seaboard, ex tant

prior to European contact, as prophylactic depictions of medical plants. Barbeau (1930), a

folklorist, maintained that floral designs were taught in mission schools as early as the

seventeenth century, and argued that their appearance on native clothing originated in this

formaI training. Brasser (1987) concluded, from a thorough lite rature survey, that litde

evidence existed for plant or flower motifs in the prehistoric art of the Great Lakes until

1800.

Penny (1991: 59) claimed that clothing and its decorative elements could be read as a

semantic system functioning on different levels. He argued that for the indigenous groups of

the Great Lakes, these images denoted gender, sexual attractiveness, social status, identity

and occasionally certain facets of information from their biography, particularly "in the

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realms of warfare and spiritual power". Floral ornamentation functioned as a sign on two

levels: mimetic and semiosic (ibid.). Penny defined the term "mimetic plane", or level, as the

representational function of sign; hence "its relationship to the thing that it represents"

(ibid.). This meant that, if sorne one asked their informants about floral ornamentation, they

would be told that the images represented flowers. He (ibid.: 60) defined the "semiosic" level

as referring to the social method by which meanings are created and bartered. Since neither

was the same, this process enabled (ibid.: 60) the meanings of signs to be debated, modified,

and intensified. He argued that the manner in which these signs were subject to historical

analysis enabled new meanings to occur that could be understood as historical incidents.

Penny (ibid.: 61) posited that this categorization of the world led to the existence of polarity

with respect to Indian attitudes regarding clothing, since a category developed that polarized

into White European style clothing versus Indian style clothing. Clothing used by white

Europeans signified civilization, while Indian clothing, such as moccasins, leggings, and

garments with 'exotic patterning', implied a state of savagery to Whites. Indian dress, from

the indigenous perspective (ibid.) signified cultural integrity and resistance to the White

domination. The term 'dress', Penny (ibid.: 54) argued, meant a special category of clothing

reserved for formaI social occasions. White people, as defined by Penny (ibid.: 62), were the

missionaries who yearned to convert the Indians, the government authorities who desired to

control them, and European neighbours who were frightened of them.

Three groups were pre-eminently associated with the making of floral style

embroidery from 1800 onwards: the Huron of Lorette, the Ottawa and the Chippewa of

Michigan, and the Métis (ibid.61-68). Missionary endeavours of the Catholic Church

influenced heavily ail three communities (ibid.). This suggests that the techniques and the

imagery of floral embroidery were taught in the schools they attended. Penny (ibid.: 68)

argued that in each case potential existed for disjunction between White and indigenous

interpretations of floral style decoration as a sign of social identity. The Huron, Ottawa,

Chippewa, and Métis artists used this instruction to manufacture handicrafts for sale as an

expression of ethnic identity to 'Christian and civilized' Indians, while the White observers

interpreted the embroidery as signs of Indianness, which translated into successful marketing

of these products.

After the mid-nineteenth century, Penny asserted (ibid.: 69), the native North

Americans of the Great Lakes used two fashion systems: White and Indian. Each system

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operated concurrendy and congruendy. Penny did not indicate what would have been worn

by someone who utilised the lndian fashion system. However, he argued that, during the

mid-nineteenth century in Wisconsin and Michigan everyday clothing used by the lndian

community was "largely indistinguishable from that of neighbouring (low income)" white

communities (ibid.: 68). The White dominant culture, he argued, used the White fashion

system as an expression of accommodation. Penny (ibid. 71) maintained that the use of

'formaI dress' by the lndian population grew to be one of the most important "symbols of

ethnic solidarity and persistence of tradition" during the reservation era. Essentially a native

North American artist used specific styles for Penny refers to as historically and socially

incidental motives. Hence such innovations in culture often become traditions (ibid.: 72).

Penny's (1991) article established that floral ornamentation existed on clothes for reasons

that went deeper than aesthetics, and that two sets of meanings were held for different

audiences, since these native artists were masters in manipulating not just the motifs, but also

their meanings.

Phillips (1991) observed that in art history and anthropology, the two disciplines that

usually examine native art, style and meaning were usually considered as separa te. Phillips

(1991) like Penny (1991) considered factors that led to the development of the floral motifs.

She argued that, since European cultures defined the floral motifs on which lndian ones

were modelled as secular, it was presumed that their significance remained the same once

they were adopted by native Americans (ibid.: 97). Phillips argued that, if the new floral

decoration was non-referential, the changes that occurred constituted a de-sacrilisation of

important categories holding great cognitive significance for hunting peoples. Both Penny

(1991) and Phillips (1991) concluded that the indigenous people of the Great Lakes

understood and operated within two conceptual frameworks during the nineteenth century.

Phillips (ibid.: 98) believed that the relationship of style to meaning in American art objects

must take account of this relationship. Phillips (1999) expanded and developed the ide a that

meanings and images could be manipulated in her analysis of the objects called 'souvenirs' of

northwestern North America.

Whiteford (1997) also considered the origins of floral beadwork in the Great Lakes

region. He (ibid.: 75) identified the different plants used in designs as part of the increasing

use of floral motifs on objects dating from the 1860s onwards. Like Phillips (1999), he was

aware of Penny's (1991) article which considered the various factors responsible for the

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development of the floral motifs. Whiteford (1997: 75) argued that evidence existed for the

origins of the plant motifs prior to European contact and for the subsequent development of

these motifs after European contact. This evidence (ibid.: 75-76) included: (a) simple patterns

of semi-florallinear motifs in native porcupine quiilwork that dated as early as 1800, (b) the

light coloured angular and curvilinear designs that existed prior to the eighteenth century on

the surface of birch bark containers and (c) the images created as a consequence of birch

bark biting. European influence, Whiteford (ibid.: 77) maintained, commenced with the

French fur traders and missionaries farther east during the seventeenth century. Direct

influences occurred when the Catholic and the Anglican mission schools were established in

the Lake Winnipeg-Red River region in 1824 (ibid.). InformaI and formaI influences were

derived from the European women on the frontier, the wives of officers of the government

and the Hudson's Bay Company, and Métis women. Whiteford (ibid.: 79) asserted that the

floral designs resonated with the awe of the natural environment, represented the

supernatural power of nature, expressed Indian solidarity and at the same time appealed to

the tas tes of those non-Indians who purchased the objects on which they existed.

(b) Images as a means of communication.

The images and the designs produced by the Algonquian-speaking peoples have

changed and been influenced by numerous groups of people. lt is possible to conclude that,

although ail images are a form of communication, not ail images changed radicaily in

appearance or experienced changes in meaning. Copway (1851: 132) observed that over two

hundred figures, or images, were generaily used for ail types of "correspondence" or

communication. He asserted that the Ojibwa used these images, what he termed "picture

representations," until they adopted the use of "European manners" (ibid.: 134). What,

precisely, he meant by this remains unclear. He stated that the Ojibwa only communicated

with other indigenous groups using messengers. Otherwise, the Ojibwa became guarded as

far as their own religion was concerned because "the white s, ridiculed it" (ibid.).

Coleman (1947: 63) observed that the totem of the individual buried was placed

upon grave markers. Landes (1968: 172) noticed that birch bark was used to record "mystic

songs" by means of pictographs. She stated that the patterns used in pictographs were

familiar to ail Ojibwa hunters, trappers and traveilers who used them to indicate boundaries,

trails, notices of different sorts, and grave markers.

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Dewdney (1975b: 12), based on information from informants, asserted that unnamed

Ojibwa communities from northem Minnesota created census records on wood using the

"totemic signs" to identify the clan of the person buried as weil as taily marks to indicate the

number in "his family". He (ibid.: 13) observed that "pictographic images" were used on

grave markers and headboards of bark canoes. Ali these examples fail into his category of

secular writing. Indeed, he earlier (1970c: 22) had identified three types of writing: secular,

tutorial, and visionary. Secular writing was defined as trail messages left on birch bark at a

portage to give useful information to those who were foilowing. Dewdney assented that

using an individual's totem was similar to a "signature". It was recognised over a large

geographical area and existed on each person's personal objects (ibid.: 22-23). Tutorial

writing enabled an initiate to le am by rote the traditions and practices of the Midewiwin from

his or her teacher, the Midé. These images occurred on the Midé scroils and the images, as

mnemonics and were "read" by those who had been initiated into the Midewiwin Society.

The third type of writing, defined as a dream symbol, was obtained from a person's dream

guardian during their puberty dream. This dream and its meaning could not be disclosed to

anyone without risk of losing the guardian spirit, but occasionaily the dream symbol was used

as an "identity mark" provided that it was disguised in some way so that its meaning could

not be detected (ibid.).

Those images that changed most radicaily in their physical appearance may have been

used in a social rather than a religious context. It appears that those images that did not

experience radical changes belonged to the religious life of the Algonquian speaking peoples.

Here, images behaved as mnemonics in a variety of scenarios, since they were designed to

convey information over several generations to specific individuals cailed Midé. A

considerable quantity of information exists concerning the images recorded on birch bark

scroils. A large number of people have been interested in these images for over a hundred

and fifty years (Schoolcraft (1851); Kohl (1986 [1860]); Warren (1984 [1885]); Hoffman

(1883; 1888, 1889, and 1891); Mailory (1894); Densmore (1910, 1913, 1974 [1928], and 1979

[1929]); Skinner (1915); Reagan (1927, 1928, and 1935); Cadzow (1926); Kinietz (1940);

Voegelin (1942); Coleman (1947); Blessing (1963); Dewdney (1970c and 1975b); Vennum

(1978); Nelson (1983); Fulford (1988, 1989, and 1990), and Vastokas (1984, 1986-1987, and

1996).

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Schoolcraft was an American explorer and topographer from Watervliet, New York

State. He served as a topographer for an expedition led by the American General Cass to

explore the Lake Superior region in 1820. This experience coupled with ethnographie

fieldwork on the Upper Mississippi and in the Lake Superior region led to his appointment

as the Indian Agent for the peoples of the Lake Superior region from 1822 to 1836. From

1836 to 1841 he was Superintendent of Indian affairs in Michigan, where he settled in Sault

Ste. Marie after his marriage to an Ojibwa. He devoted much of his life to the study of

American Indians.

Schoolcraft (1851: 351) observed that the Ojibwa distinguished between

"kekeeowin" and "kekeewin". The term "kekeewin" was defined as a system of marks that

represented Ojibwa clan symbols and other images that were readily recognised and

understood by everyone in the tribe, and were used to leave messages, and on grave markers

to provide information about the person who had died. However, if these images were used

on rocks, Schoolcraft stated that they were cailed "mussinabiks". He (ibid.) defined the term

"kekeeowin" as a system of symbolic notation "for the songs and incantations of the Indian

meda [Midé] and priests, making it appear to the memory for the presentation of language

and musical notes". Schoolcraft described (ibid.) the images on the birch bark scroils as

"picture writing". He (ibid.: 361) observed that the members of the Midewiwin used these

pictographs as mnemonics to remember the words of their chants. These chants were

performed inside the sacred midewegan, 'spirit lodge', during curing rites and initiations.

Schoolcraft recorded these chants and discerned they functioned in a similar manner to

prayers or hymns. He was impressed by the Midé's ability to recoilect both the words and the

music, based upon the images on the birch bark scroils and concluded that each chant had a

key symbol wruch acted as a trigger to a body of information residing in the memory of the

shaman. Unfortunately, he did not identify the key symbols on the birch bark scroils and was

unable to elicit support for future research from the Smithsonian Institution.

Kohl (1985[1860]: xiii) provided sorne information regarding the images on the birch

bark scroils belonging to the Ojibwa Indians who lived on the south shore of Lake Superior

in northern Wisconsin. A German geographer, ethnologist, and travel writer, Kohl spent

four months with them as they adjusted to life on four of the new reservations in northern

Wisconsin. He (ibid.: 145) noticed that the "northern savages" used birch bark sheets of

varying sizes on wruch to write. He described the Ojibwa practice of creating pictographie

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dream records and suggested that many song scroils had iconographic onglns ln the

Algonquian dream or vision quest experience. He (ibid.: 143-144) observed that, at

Chequamegon, the Ojibwa also le ft records of their dreams on trees, rocks, birch bark,

blankets, and clothes. He (ibid.: 145) coilected, purchased, and copied many of these objects,

sorne which were possibly birch bark scroils. Kohl (ibid. 143-166) established through his

interpreters that the scroils were related to the Midewiwin Society and depicted different

totems as weil as the migration movement of the Ojibwa from the Atlantic to Lake

Superior.5 Unfortunately, his efforts at transcribing the images were not very comprehensive;

perhaps a consequence ofhis attitudes towards the Indians. He wrote that he (ibid.: 165-166)

became annoyed with "these savages" after his attempts to buy scroils from two of them

failed; foilowing an attempt to bribe them with pouches of sugar or tobacco.

Warren (1984[1885]) worked among the Ojibwa of Minnesota and Wisconsin and

was of mixed Ojibwa and Euro-American heritage. He wrote very little about these images

but he stated (ibid.: 67) that the songs and rites of the Midewiwin were transcribed using

"hieroglyphics". The only ex ample of these "hieroglyphics" that he (ibid.: 89-90) discussed

was of sorne images inscribed on a copper disc which recorded the number of generations of

a family of the Loon totem who had lived in the La Pointe area. The indentations indicated

that eight generations had lived ln this region. Warren (ibid.: 26-27) argued in the

introduction of his volume that he intended to conduct a detailed examination and

interpretation of the images used to record the religious idioms and the songs sung, but

unfortunately he died from a haemorrhage before beginning the projected book on the

Midewiwin (Fletcher Williams 1984: 18). Although a practising Episcopalian, he believed that

the Midewiwin was central to the Ojibwa world view.

Three decades after Schoolcraft (1856), the Smithsonian Institution provided funding

for further research into Ojibwa pictures. Hoffman, a Colonel in the US Army, carried out

fieldwork for three months amongst the Ojibwa of northern Minnesota under the

supervision of Garrick Mailory, who remained in Washington D. C. (Hoffman 1891: 156).

Mailory (1893: 202) and Hoffman (1891: 156) were concerned with complex sequences of

symbols and rejected Schoolcraft's (1851: 351) idea that any of these symbols could be

5 The debate regarding the origins of the Midewiwin, the Grand Medicine Society, will not be considered because it is not pertinent to the discussion. However, it has been discussed in sorne depth by others including Angel (2002), Bhar (1991), Balikci (1956), Dailey (1958), Grirn (1983), Hallowell (1936), Hickerson (1962, 1963, and 1970), Hoffrnan (1891), Landes (1968), Meyer (1990), Vecsey (1983, 1984); Rogers (1973).

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deciphered using a key. They rejected his distinction between "kekeeowin" and "kekeewin",

believing that he exaggerated many of his observations. Hoffman's (1883) paper focused

principaily on comparing "Eskimo" pictographs with those created by other indigenous

groups. He argued that the Ojibwa used birch bark for mnemonic records and personal

exploits (ibid.: 128) and that the style of drawing used by the Alaskans was "very similar to

that of the Ojibwa" (ibid.: 135). He (ibid.: 135) examined the images found on the stem of a

pipe presumably made by the Ojibwa, but did not distinguish between the images that could

be used and read by ail the members of the Ojibwa community and those images that only

the Midé could use. He (ibid.: 139) claimed that the method of recording transactions and

events on birch bark scroils was "almost, if not entirely discontinued". He therefore posited

that it was crucial to coilect as many examples as were stiil being used, in order to increase

the quantity of information concerning these images. Nevertheless, he concluded that the

Eskimo images were "greatly superior" to those made by any other group, especiaily with

respect to the "delineation of natural objects, especiaily animate forms" (ibid.: 146). He

placed the Ojibwa bark records second among ail the indigenous peoples' imagery. He also

stated that only through a thorough familiarity with Ojibwa "ceremonies and mythology"

could any understanding of these mnemonic images be obtained (ibid.).

Much of the information in Hoffman's (1888) article was republished almost

verbatim in his (1891) report for the Bureau of Ethnology at the Smithsonian Institution.

Yet, this 1888 article discusses two other birch bark scroils that were not described in the

1891 report. Both scroils came from Red Lake, Minnesota, and, although he did not ob tain

assistance in transcribing them, he made a copy without the knowledge of the Midé to whom

the scroils belonged. He (1888: 216) observed that the characters on both scroils were

identical and that one appeared to be copied from the other. He also (ibid.: 217) claimed to

have seen an ancient cosmological chart that apparently had never been shown to any white

man or to any non-Midé Indians. Hoffman described this map, its physical condition, and its

images but unfortunately did not provide any analysis of the images themselves.

Hoffman (1889: 215) discussed the meanings of the images, the mnemonics, on a

Midé birch bark seroil that had not been shown to a "white man" before in Red Lake in

northern Minnesota. Whether this is the same bireh bark seroil diseussed in his previous

article is diffieult to determine. Apparently, this seroil was not shown to an Indian unless he

had paid the required fees, and then only once he had undergone the necessary training and

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instruction to be initiated into the Midewiwin Society (ibid.). This seroll belonged to

Skwekom' -ik who had received it from his father-in-Iaw who in turn had received it from

Ba-da'-san the Grand Shaman and chief of the Winnibigo'shish Ojibwa. Ba-da'-san himself

had obtained this scroll, which was a copy of the original, from the Grande Midé at La Point

where the Midewiwin was held annually and ceremonies were conducted strictly in

accordance with ancient and traditional rites. Hoffman (ibid.: 216-217) subsequently

examined this scroll and a few others. He realised that, if a shaman was only a second degree

Midé, he could not actively participate in ceremonies that went beyond Midé of the second

degree. It also meant that he was not privy to information known about these same images

by a Midé who was also higher than second degree. Hoffman (ibid.: 218) discussed at length

the differences in the colours used in the sacred poles used by the Midewiwin based upon

information from Sicos 'ige, a second degree Midé. The remainder of this article considered

the facial decoration used by initiates into different degrees, the ceremonial procedures, the

types of medicine bags used by the Midé of different degrees, what occurred at a Ghost

Lodge, and finally an event where a Midé treated and brought back from the Spirit Land a

dead young man.

Hoffman's (1891) monograph discussed the collection of twenty-four song scrolls

used in religious ceremonies of the Midewiwin at the White Earth Reservation in Minnesota

during the late 1880s. He published reproductions of twenty of these scrolls along with

several other examples of images. Hoffman considered the various types of shamans existing

among the Ojibwa (ibid: 165) and stated that the Midé and Jiissakid were the most highly

regarded individuals in the community for their curing and medicinal skills. Both skills were

achieved either by visions alone or by visions and purchase. Midé priests (ibid.: 165)

customarily preserved birch bark records with incised lines that pictorially represented the

ground plan of the ceremony and the number of degrees to which the owner of the scroll

was entitled when he conducted a ceremony. Severallevels of knowledge and understanding

existed because of the hierarchy within the Midewiwin Society, and therefore some Midé

were more knowledgeable and powerful than others. This, in turn, affected the meaning of

the images depicted on birch bark scrolls. Hoffman (ibid.) established than these records

were sacred and could not be exposed to public view; they could be examined only after a

candidate had paid his initiation fee, fasted, and provided offerings of tobacco. These

pictographs were used by the Midé as mnemonic devices to remember the words of their

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chants, for the instruction of new members, to record oral traditions, and to correct

ceremonial procedures (ibid.: 191-193). Hoffman (ibid.: 267) established that the seroils

eould be read from left to right, right to left, and sometimes some seroils used both styles.

He observed that the Ojibwa used images to express ideas by shamans, hunters, and the

traveilers. However, a reeognised system of using these images that enabled one person to

completely comprehend the work of another did not exist. Essentiaily, an image acted as a

key symbol and behaved as a trigger of information, a mnemonic that resided in each

person's memory. He observed (ibid.: 289) that the songs sung by the shamans were based

upon the characters recorded on the seroils and in many cases words or phrases were not

recited. Unfortunately, he did not provide any analysis concerning the images themselves.

Densmore's (1910) publication discussed the song scroils coilected during 1907, 1908

and 1909 from the Chippewa lndians of White Earth, Leech Lake, and Red Lake

reservations in Minnesota, and from a Chippewa who lived in the Bois Fort reservation in

Minnesota, and from a Chippewa who lived in the Bois Fort reservation in Minnesota. She

discovered that the melody was more important than the words and that "in a succession of

renditions of a song" the words were often only used once (ibid.: 2). She determined that the

ide a of the song was firmly assoeiated with the melody and not with the words (ibid.).

Densmore observed that it was "permissible and customary" to compose new words for old

tunes, but she noticed that the words were "always similar in general charaeter" to the words

previously used. She concluded that although changes could occur and be introduced, the

identity of the songs remained unaffeeted. Densmore asserted that these tendencies did not

apply to songs used by the Midé.

Densmore (ibid: 8-11) considered the structure of the songs sung and established

that certain songs were harmonie and others were melodic in structure. The results she

presented in tables. She observed that the songs used by the Midé required a "special skill" to

translate (ibid.: 8) and that different songs were used when singing the Midewiwin (ibid.: 11-

12). She (ibid.: 13-14) also considered the beliefs of the Midewiwin, their goals, and aims, and

argued that their songs "represented the musical expressions of religious ideas" (ibid.: 14).

This meant that she often found translating the words very difficult. She established that a

Midé song was not considered fini shed unless it ended with the syilables "ho ho ho ho"

(ibid.: 15).

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Densmore (ibid.) established that the beliefs and the teachings of the Midewiwin

were the words of the songs, which often functioned as texts for discourses (ibid.). The

songs were only taught to those who paid for the privilege of learning them and the words

were recorded in mnemonics on birch bark. Densmore (ibid.: 16-17) ascertained that

members of the Midewiwin universally understood the images, or mnemonics, of the Midé.

However, she noted that these mnemonics could be used in other circumstances. She (ibid.:

20) also considered the role of the Jiissalcid (known as doctors or jugglers - a different type of

shaman amongst the Algonquians) who were different from the Midé. Densmore recorded a

wide range of songs, the medicinal songs which the Midé, rather than the Jiissalcid used. She

established that, for a charm to work properly, the correct song and the correct medicine

must be used. Therefore the person who bought the medicine from the Midé also bought the

song.

Densmore's (1913) publication continued from her earlier (1910) study of Ojibwa

music but only dealt with mate rial from the White Earth reservation in Minnesota. She relied

upon numerous informants for translations, including Mrs. Mary Warren, Rev. C. Beaulieu,

and Rev J. A. Gilfillian. Both ministers helped with the analysis and translation of the

Chippewa words. Rev. C. Beaulieu was a member of the White Earth Chippewa, while Rev J.

A. Gilfillian had lived on the reservation for twenty-five years.

She discovered that the rhythm was repeated more exactly than the melody. She also

discovered that a number of the songs did not have words and that, if songs had words, they

"suggested rather than expressed" the ide a of the song (ibid.: 2). If the words changed, they

conformed to the music, but the same word could be accented differently in different parts

of the song. She (ibid: 15) asserted that the principal reason for singing a song was directly or

indirectly to seek supernatural aid. However, a large variety of songs existed for different

reasons. She (ibid: 17) clarified that most of the old songs that had a major tonality included

the old "dream songs" used by the Midé, the practise of medicine, the pursuit of war, and the

essential nature of a dream associated with the idea of reliance upon supernatural help.

However, songs that expressed sadness, distress, or uncertainty used a minor tonality (ibid.).

Densmore's (1979[1929]) publication discussed "picture writing", which she (ibid.:

174) defined as "that form of thought writing which seeks to convey ideas by means of

picture signs or marks more or less imitative of the object of the idea". Significance was,

according to Densmore, an essential element of the pictographs and she maintained that they

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were "alike in that they all express thought, register a fact, or convey a message." She (ibid.)

observed that figures included "crude delineations" of men, animaIs, birds and other

"material objects" and that the Midé used symbols that represented the sky, earth, lakes, and

hills, and sounds including concepts such as "spirit power". Simpler symbolism was used for

messages, including signs that indicated days, direction and duplication of numbers.

Occasionally these were combined with possible ideographs to indicate "progressive action".

Densmore maintained that two types of writing existed: esoteric and non-esoteric.

The esoteric writing could only be understood by initiates, while the non-esoteric writing was

used by everyone to convey information. She argued that examples of esoteric writing

included the Midé records, writings and songs, stories of Winabojo, and drawings used to

work charms. Non-esoteric writing included "totem marks," messages left along a route and

maps used by travellers, illustrations for a narrative, records of time, as well names of

individuals (ibid.: 175). She developed and expanded upon each type of writing using

drawings.

Skinner's (1914) article briefly considered how the Plains Ojibway, known as the

Bungi, employed birch bark. He (ibid.: 317) observed that they used "picture writing", as he

termed it, on birch bark and wood, which in turn reflected this group's origins in the

Woodlands region. Skinner argued that this type of writing was connected with religion and

that the Midewiwin was important. However, he did not describe the images, who used

them, what they may have meant, or how their meanings were transferred from one pers on

to another.

Several very descriptive articles provide little analysis of the images on the scrolls (for

example Cadzow 1926; Kinietz 1940, Reagan 1921 and 1922). Reagan conducted fieldwork

while he acted as lndian Agent at Nett Lake in Minnesota. His (1921) article published some

medicinal recipes made from plants. George Farmer, Ne-bay-day-ke-shi-go-kay, "a medicine

man" of the Bois Fort in Minnesota allowed Reagan to copy them from his notebook.

Reagan (ibid.: 246) stated that the recipes were written in the Chippewa language using

Roman characters. Reagan also (1922: 332) published the words of the songs used by the

Midé, which he found were recorded by the same "medicine man". He (ibid.: 332) observed

that Farmer had used Roman characters, but that the "phonetic values were similar to

French". Reagan published a few translations of the songs, recorded in Farmer's notebook,

stating their meaning, and when in the Midewiwin ceremony the songs were used. At the end

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of his (1922: 366-369) article, he provided a brief description of the Midewiwin Society in

this region. Both articles are interesting, since it is possible to establish what these songs

meant. However, it would have been useful to know which song was connected to which

mnemonic and whether songs could exist without mnemonics.

Kinietz (1940) unsuccessfully sought birch bark records while conducting fieldwork

among the Chippewa of northwestern Michigan over several seasons. He (ibid.: 38) asserted

that the type of symbols used, the size of the record, and "the excellence of the delineation"

affected the type of record. He argued that "the excellence of the delineation" varied not just

with the purpose of the designs, but with the artists of the different bark images.

Unfortunately, he did not provide any indication as to his methodology or evidence that

could substantiate his claims. However, he distinguished two types of birch bark scrolls

based upon subject matter. The first, understood only by instructed persons called Midé,

were, according to I<inietz (ibid.), "ideographic, esoteric and mnemonic". The second type of

scroll he described as being descriptive in character, and was related to the sign language of

the Indians. Unfortunately, he provided little evidence to substantiate his daims. Otherwise,

he reiterated many of the findings of early ethnographers and preceding researchers

regarding both scrolls and the Midé.

Voegelin (1942: 44), unlike I<inietz (1940), stated that she was successful in her

research. Voegelin (1942: 44) conducted her fieldwork amongst the northern Minnesota,

Wisconsin, and eastern Ontario Ojibway. She maintained that pictographs were used to

convey messages, provide topographic information, and "illustrate narratives". She observed

that the Midé used pictographs to record esoteric history or songs. She (ibid.: 45) established,

based on information from informants, that, in post-contact times, a pointed piece of metal

was used to cut images into the birch bark while in "pre-white times" a wooden or bone

stylus was employed. She was also told that red paint made from blood root often filled in

the outlines of the incised figures (ibid.: 44-45). Voegelin (ibid. 45-46) described and

identified a number of images found on the birch barks scrolls using information gained

from her informants. She observed that when she asked her informants for the terms

"picture, photograph, pictographic representation and so on" (ibid.: 46) that the words given

for each of these terms were numerous and varied considerably between different dialectic

groups, especially on the edges of the Ojibwa and the Ottawa groups.

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Coleman's (1947) publication examined, discussed at length, and compared the

images from two birch bark scroils as part of her discussion of how the Ojibwa in northern

Minnesota used images in religious contexts. She established that these scroils were read

from left to right (ibid.: 79). One, a Midewiwin scroil, belonged to her informant Charlie

Fox, a Midé who also was the leader of the Midewiwin at Naytahwaush (ibid.: 77). The

second scroil belonged to a Mr Gustavson, an Ojibway from the White Earth reservation.

She observed that the images on the second scroil were larger and more finely delineated, but

that the details of the "faces were lacking and the manitos were not nearly so artisticaily

executed" (ibid.: 80).

Both Blessing's (1963) and Kidd's (1965) papers indicate that archaeologists were

also interested in birch bark scroils. Blessing's (1963) study of a coilection of birch bark

scroils differed from Kidd's (1965) and indicates that he was determined to establish the

meaning of these images on the birch bark scroils. Blessing (ibid.: 91) used a number of

informants who were Midé, sorne of whom were from Madeline Island, Wisconsin and had

since died. His principal informant was Thomas Shingobe, a Midé and member of the Miile

Lacs band whose ancestors originaily came from Madeline Island, down the St. Croix River

and into Minnesota. Blessing (ibid.: 93) argued that the Midé were members of a "cult" that

was "more or less an elaboration of earlier hunting societies which had been formed in the

pressing need for the organized gathering of food". He continued his line of argument by

stating that, as religious activities grew increasingly multifaceted, it became necessary to

devise a method of keeping records. Hence the individuals involved "utilized natural and

conventionalised forms" as mnemonic devices. He posited that the scroils from Minnesota

no longer served as memory aids but as a means of communicating information. These

mnemonic images remained "almost exclusively the property of the originator," but, later,

became part of the larger group. Among the Ojibwa (ibid.: 94), these images became more

complex and "approached the stage of hieroglyphics." He considered the scroils to be old.

Blessing further asserted that the largest number of scroils had been produced in Minnesota.

How he arrived at this conclusion is unclear. Blessing examined scroils from Minnesota,

Wisconsin, Michigan, and Canada, but it remains unclear where the Canadian scroils

originated (1963: 95). He established that the eIder Midé took time and effort in interpreting

the images on the scroils during the instruction of the younger Midé. It was in this manner

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that the meanings and significance of the images were transmitted from one generation to

another.

Blessing considered the Midé, the Midewiwin, and their activities in Minnesota in

considerable depth: from where and how the Ojibwa had come to settle where they did in

Minnesota, what were guardian spirits to the Ojibwa and the Midé, and how a scroil was

made and inscribed (ibid.: 100-109). Blessing argued that he had accumulated substantiai

quantities of information on the practices of the Midewiwin from two reservations: White

Earth sometime after 1946 and Miile Lacs in 1968. U sing informants, he (ibid 109)

established that the "minor" animal species were associated with lower degrees of the

Midewiwin and that the "rugher species" of animaIs were connected with the higher degrees.

For example, weasels, otters, and mink were associated with the first degrees wrule mytrucal

creatures were associated with the fifth to eighth degrees (ibid.: 109-110). Scroils from

different geographic areas exrubited slight differences.

Blessing (ibid.: 110) established that the scroils in his study consisted of three types:

30% were "instruction" scroils, 50% "ri tuaI" scroils, and 20% were "master" scroils.

Candidates used an "instruction" scroil to prepare for the initiation ceremony (ibid.: 110-

111), while the Midé who conducted the Midewiwin ceremonies employed a "ritual" scroil as

a "weil illustrated edition wruch served as a guide or a reference" (ibid.: 111). The "master

scroil" was cailed an rustoricai document but also indicated the four to eight degrees which

could be obtained by the Midé. Blessing subsequently examined seven scrolls wruch included

ail three of these types. He provided detailed drawings or tracings of seven scroils.

Unfortunately, by using the terms "natural" (ibid. 96) and "invented" to classify sorne

images, he demonstrated a potential problem in rus study since rus own judgement seems to

interferes in rus description.

Kidd's (1965) very descriptive article discussed two scroils discovered witrun an

archaeological context. Kidd wished to make archaeologists aware that the discovery of this

type of object could occur in regions where birch bark was used. P. Ryan accidentaily made

the first find in 1924, reporting it to Kidd in 1959 (ibid.: 480). The first group of birch bark

scroils were found when the water from the fire fighter's hose washed away the soil of a

mound on the north shore of Rainy Lake that covered them. Ryan recailed that it contained

probably around 200 to 300 hundred pieces of birch bark (ibid.: 481). W. T. Daigetty and

Bruce Littlejohn made the second find in 1962 in a cave on Burntside Lake in Quetico

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Provincial Park. Kldd examined both sites and both groups of bireh bark. He (ibid.: 483)

eoncluded that "seroils" and their assoeiated artefacts eould be found buried in the ground in

places seemingly "out of the way" in the woods, or hidden in caves. He eould not date when

this happened for either group of bireh bark objeets but maintained that arehaeologists

should be aware of the possibility of similar diseoveries in the future.

Chapter III eovers Dewdney's and Kldd's (1962, 1967) examination of the rock

image sites of the Canadian Shield in depth. However, Dewdney (1962: 110 -116) posited

that a eonneetion existed between the images of rock image sites and those made by the

Midewiwin, based upon their similarity. Dewdney eompared a few of the pietograph and

petroglyph images with those of the bireh bark seroils that were known to belong to the

Algonquians of the Great Lakes region. He eoncluded that a study of the depietions of

supernatural beings in the mythology of the Algonquians might aid the identification of these

images. Over ten years later, Vasto kas and Vastokas (1973) suggested that a eonneetion

existed between the engravings of the Peterborough petroglyphs, the images on the bireh

bark seroils, and Algonquian shamans (please see Chapter III for a detailed examination of

their study).

Landes (1968) eonsidered images on bireh bark seroils in her examination of the

Ojibwa religion and the Midewiwin. She (ibid.: 172) stated that only the shaman who ereated

the seroil understood the specifie meaning of the images used. It was the shaman's role, she

(ibid.: 172 - 173) asserted, to teaeh "this explieitly" to someone else "before the notation was

useable"; the shaman's intentions dietated the level of knowledge or seereey. She (ibid.: 224)

deseribed bireh bark seroils and their images, and stated that its intention and, frequently the

availability of bireh bark, determined the size of a seroil. She (ibid.) argued that the

"partieular message" of a seroil, essentiaily, what the pietographs meant, was probably

impossible to establish unless eaeh figure was labeiled or translated by the owner.

Dewdney's (1975) publication is valuable, although it was eriticised by Rogers (1975)

and Veesey (1976). Dewdney (1975: 21-22) posited that six categories of seroils existed based

on the variations in the themes he had identified in ail of the seroils that he examined. This

list included: (a) origin seroils, (b) migration eharts, (e) mas ter ritual seroils, (d) ghost lodge

and sky degree, (e) deviant seroils, and (f) enigmatie seroils. He asserted the importance of

remembering that the principal funetion of the bireh bark seroil was mnemonie. From 1966

to 1972 he undertook to identify and traek down over 150 bireh bark seroils in public and

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private collections in Britain, Canada, and the United States of America. He noted their

current physical location, type of scroll, its catalogue number, where it came from, who

collected it, its length in inches, number of sections, and a source code. He recorded the

images of sorne of the scrolls using a technique that he described in depth, whereby he traced

the scrolls, or, if a collection was deemed too large, only the "most important specimens"

(ibid.: 7) and sketched the remainder. He did not indicate the process by which he

determined which scrolls were more important. Dewdney (ibid.: 5) distinguished between an

instruction scroll or chart and what he called a song scroll. He (ibid.) argued that an

instruction scroll was a linear series of images to be utilised as memory aids "in rendering

either a sacred Midé song, or a profane personal one." The profane song was dreamed by a

"visionary shaman" for a various purposes, while a Midé composed a sacred song, which

could be sold or traded. However, he believed that the contents of the latter could only be

interpreted by the composer of the scroll or the owner. He (ibid.: 15-18) described in

considerable depth how scrolls were constructed from birch bark, and the possible

techniques used to draw the images on their surface. It remains unclear who made the

scrolls, but Dewdney maintained that the task of stitching of birch bark together to create a

larger scroll was 'traditionally - but not always - women's work." He did not provide any

evidence to support this statement. The stitching cou Id be "highly decorative" (ibid.). He

conducted an in-depth analysis of the styles used to depict the images, using terms such as

"rectilinear, abstraction, condensation, symbol conversion, atrophy, amputation" (ibid.: 18)

to describe the processes by which shapes changed as the scrolls were repeatedly copied.

Unfortunately, his terminology makes it very difficult, even impossible, to comprehend

precisely what information he wished to convey to the reader. His terminology is,

consequently, difficult to use. He also transcribed a number of the scrolls with the aid of

James Redsky from Shoal Lake Reserve, on the western portion of the Lake of the Woods,

relying on an interpreter when Redsky used Ojibwa rather than English.

Rogers (1975: 83) reviewed this book and asserted that Dewdney frequently allowed

his own perspective to colour the way in which he classified the spirit world of the Ojibwa.

Rogers argued that present day Ojibwa "do not" and never did adhere to the Euro-Canadian

worldview. According to Rogers (ibid.), the Ojibwa believe that the same spirits were helpful

in one context while they were injurious in another. He cautioned the reader of this book to

be wary of Dewdney's (1975) interpretations of the significance of the symbols on the

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/~.,

scrails. Rogers (1975) is considerably harsher than Vecsey (1976) in his review of Dewdney's

(1975) book but both reviewers severely criticised Dewdney's study for numeraus

weaknesses, which they ascribed to his laek of scholarly expertise.

Nelson (1983) diseussed a eoileetion of bireh bark scrails and objeets of unclear

origin. His article pravided a detailed review of previous work undertaken on these scroils by

Hoffman (1891) Sehoolcraft (1854), and Densmore (1979 [1929]). He also examined a

number of serails illustrated in various gailery catalogues. He (1993: 220-221) listed the

serails that Dewdney had not reeorded that were in other publications. Nelson subsequently

used Dewdney's (1975) publication in conjunction with Blessing's (1976, 1977) to identify

and de scribe at length the different types of serails that he had identified using Dewdney's

classification (1975: 21-22).

Vastokas (1984: 425), an art historian, acknowledged the work of her predecessors

but asserted that the interpretation of the images on the birch bark scrails stiil presented "the

most pressing chailenge to scholars" interested in Algonquian art history. She eould have

included archaeologists, anthrapologists, and historians. Vastokas (1984: 435) maintained

that the scrails were the most significant body of visual documents available for the study of

native North Ameriean art history. This paper outlined sorne preliminary and exploratory

observations in interpretation theory and methods whieh she maintained were applicable to

bireh bark serails. She (ibid.: 426) postulated that the style, iconography, and development of

the serails should be eonsidered from an art historical perceptive. Vastokas believed that,

since further fieldwork was impossible (ibid 427), two methods of researeh existed to

interpret these serails: (i) examination of the images depicted on the scrails themselves, and

(ii) external praof supplied by comparison with analogous or related visual systems.

She subsequently outlined each avenue of research and argued that data could be

obtained thraugh detailed examinations of the manner in which the motifs and elements

were organized on the scroils. Art historians, she maintained (ibid.: 428), eould use the

notion of style as a tool. Preliminary observations of the style in which these images were

executed, Vasto kas eontended, highlighted clear differences between the official Midewiwin

scroils and the personal song seroils that belonged to individual members, and these in turn

suggested significant differences in their funetions and meanings. She maintained that these

differences were observable without ailuding to the cultural eontext of each scrail. The most

intrinsic and explicit virtue (ibid.) was their narrative structure in which separate pictorial

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units were arranged to convey information to the beholder regarding mythological, historical,

or ritualistic events across time and space. This narrative role was crucial in any analytical

procedure aimed at interpreting the "form" or content of each scroil's images; the form

being the physical outline of an image. She maintained that narrative art differed from iconic

representations since, unlike iconic representations, narrative art could communicate events

in time and space. Narrative compositions she (ibid.: 430) defined as multiple motifs

organised in a "more perceptuaily scattered disposition ailuding sequence and movements to

the eye across the surface of pictorial ground." Furthermore, profile images denoted motion,

while frontal views indicated action. Vastokas (ibid.: 431) postulated that narrative art forced

the observer to detect the greater visual complexities of the composition. She concluded that

the birch bark scroils were "narrative visual wholes" to be interpreted in terms of their form

and context. She disagreed with early endeavours to decipher the images, such as Mailory's

(1893) attempts to examine them as writing systems, because these scroils were visual rather

than verbal documents.

Vastokas' (ibid.: 427) second avenue of research, outlined at the beginning of her

paper, was that external proof should be supplied by comparison with analogous or related

visual systems. The Midewiwin scroils play crucial roles as visual religious texts, as mnemonic

aids in the instruction of new members, and as a means to record oral tradition and correct

ceremonial procedure. Essentiaily, they recorded the history, origins, and ritual of the

Midewiwin Society. It was vital, therefore, to understand these scroils within the larger

context of Ojibwa shamanism and the numerous scroils that record the songs of individual

Midé. The song scroils contained, Vasto kas maintained, links with traditional motifs, since

personal scroils habituaily used traditional motifs that derived from personal vision quests.

Advances in the interpretation of the images, Vastokas (ibid.: 437) concluded, could occur if

theories and methods were utilised from a range of fields including art history, symbolic

anthropology, history of religions, and philosophical hermeneutics. Future examinations of

these images, she asserted, would be advantageous if they were undertaken in the context of

a circumpolar shamanic art tradition, since it had a cross-cultural system that was fairly

consistent.

Vennum's (1978) study could be placed in Vastokas' (1984: 427) second line of

research. He drew extensively upon the data and the songs of the Mide collected by Blessing

from the Mille Lacs and White Earth reservations. Vennum argued that larger numbers of

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Mide songs existed in this coilection than Densmore had coilected. He was interested in the

origin migration scroils of the Midewiwin, and so, he reiterated the legend of the Ojibwa

westward migration. He argued this had to be undertaken because the migration charts

"pravided the necessary dues for the identification and the interpretation of the origin­

migration" serails. Hence he pravided a considerable quantity of information about this type

of chart and about understanding its raIe within the Midewiwin. Vennum asserted that this

type of serail was distinguishable fram other serails beeause images behave as mnemonics

for the place names of "real or legendary resting places" used by the Ouer or Bear as they

traveiled westwards (ibid.: 761), while in other serails these places were presented by dots.

Serails were read from left to right, sin ce the Ouer, in the origin-migration story told by the

Midé, traveiled from the east to the west. Vennum argued (ibid.: 753) that the development

of the origin-migration story was linked with the migration of the Ojibwa as they moved

from the east to the west side of Lake Superior before the end of the seventeenth century.

Vennum diseovered that twelve migration charts existed in the Miile Lacs-White

Earth papers coilected and transeribed by Blessing (1963) and his informants. Vennum

(1978: 762-763) identified the place names, and was able to establish precisely where on Lake

Superior they had stopped. He argued that this information "chailenged" Dewdney's (1975:

9) statement about the indigenous knowledge of Lake Superior, while corroborating and

expanding the versions of the migration coilected by Warren (1984 [1885]) and Hoffman

(1891) during the nineteenth century. However, Vennum (1978: 764) could not identify ail

the images as place-names, and conduded that these were probably the "texts of songs". He

established that specifie motifs from sorne song scroils bore a striking resemblance to those

surviving in the song texts, suggesting that regularities also existed in their meaning. He drew

extensively upon Densmore, Schoolcraft, Kohl, Hoffman, and Landes (1968) to identify the

songs and discuss how they might be interpreted. Vennum (1978: 787) argued that these

migration serails may have been performed near the end of the Midewiwin ceremony, based

upon information in the Miile Lac-White Earth papers. He subsequently argued, based on

Blessing (1963: 93-94), Hoffman (1891: 290), and Densmore (1910: 26), that the images, as

mnemonics, "were less generalized and their meanings secretly guarded" (1978: 788).

Vennum (1978: 789) suspected that this could explain why Densmore (1910: 26) had

observed that two Midé may have had the same song, but posited that this occurrence was

possibly a coincidence. Based upon the Mille Lac-White Earth papers, Vennum believed

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(ibid.) that, in the post-1900 period, shared ownership of the songs began occurring in the

pictographs and the texts, but he was unsure as to whether the songs also shared melodic

similarities. He observed that Densmore had not considered whether her informants

recognised the songs by their texts, their images, or, as he termed them, pictographs, or by

their music. He (1978: 790) concluded firstly, that the Mille Lac-White Earth papers made

possible an understanding of the wide variety of ways in which the same Midé song could be

utilised, and, secondly, that a detailed examination of these songs was an excellent start for

anyone attempting to establish the meaning behind other "abstruse Ojibwa song scrolls."

Finally, he concluded that details found in the migration scrolls were useful for interpreting

Ojibwa pictography and song poetry in general.

Closs' (1986) article is the only one that built upon Dewdney's (1975) work with

birch bark scrolls. It examined the ritual importance and use of numbers, especially the

number 4, for the Ojibway, and in particular for the Midewiwin. He utilised the ethnography

collected by Densmore (1929), Dewdney (1975), Hoffman (1891), ]ohnston (1976), Landes

(1968), and Warren (1885). Closs (1986: 181) followed Dewdney's (1975: 12) definition of

pictography, which was used as "a generic term for any form of preliterate art-executed on

any available surface - that is known, or is assumed to have had communicative rather than

decorative or aesthetic intent". He (ibid.: 182) agreed with Dewdney and argued that this

pictography was mnemonic and "did not represent the written word." Closs applied the

information concerning the use of numbers to the drawings of six birch bark scrolls. He

(1986: 189) examined six Midé scrolls that he believed exhibited "graphic properties of the

ritual importance of the number 4" and "illustrate the usage of the number series in the Midé

cult." He argued that five of these scrolls were, according to Dewdney's (1975: 21-22)

classification system "master scrolls," while the sixth was a "possible migration scroll."

Closs' argument is interesting, but it remains unclear whether he examined the

original scrolls, or used drawings published by Densmore in her 1929 publication and

Dewdney in his 1975 publication. It is important to examine the actual scrolls rather than a

drawing or sketch of the scroll, because it is possible that the person who made the drawings

inadvertently made mistakes in copying the images.

Vastokas (1986-87) stated that any investigation of prehistoric and post-contact

native North American art presented new challenges for art historians, because it lacked

written documents, which, she acknowledged, were crucial for historians. New art historians

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(ibid.: 13) could examine these art works as primary data because they did not recognise the

lack of written documents as an obstacle. New art history allowed academics from different

scholarly areas to draw upon a wide variety of disciplines, themes, and methodologies.

Vastokas, like Rlfkin (1986), argued that new art history assumed the universality of human

visual expressiveness and adopted a cross-cultural perspective in which to explore art from a

point of view held by a particular social group, time period, or culture and instead of a

twentieth century perspective.

Vastokas (1996: 48) developed ideas introduced in her previous article. She argued

that images had been insufficiendy exploited in the writing of Aboriginal history and

suggested that these visual documents should be carefully drawn upon as "aids" when

writing Aboriginal history. She promoted the idea that much of Aboriginal art was produced

intentionally as "history", so that pictorial depictions should be recognised as writing.

Aboriginal artworks, she maintained (ibid.: 49-51) had different purposes in traditional

culture, and, since the arrivaI of the Europeans to North America, new functions were

attached to these objects (also see Phillips 1999).

Vastokas identified the problem as stemming from the viewpoint of European

historians and art historians who held that Aboriginal societies lacked a history despite the

fact that Aboriginal societies often recorded it. She posited that previous academics had

ignored the most important function of pictorial representation in traditional native culture

which was the recording of history. According to these scholars, Aboriginal peoples lived in

an "anonymous and static present". Vastokas argued that this attitude had affected both the

interpretation and presentation of the Aboriginal artworks and Aboriginal history.

According to her, there were four different ways by which Aboriginal art works

"served" the writing of Aboriginal history: firsdy, as "historical documents", in the same

manner as a textual document used by an historian with its own date and characteristics,

enabling the development of historical chronologies (ibid.) (an ide a she had introduced in her

1986-87 article); secondly, as "cultural expressions" that were visual embodiments of

Aboriginal beliefs, values, and society as recognised by practitioners in new art history;

thirdly, as "representations" of events taking place in time and space; and finally as "writing"

(1996: 52-53). She reiterated her idea that Aboriginal art in North America could be

subdivided into two dis crete functional types called iconic and narrative that she had

discussed at length in her 1984 article.

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Vastokas (1996: 53) supported Boone and Mignolo's (1994) daim that it was

important to get away from the modernist \Yj estern conception of art as something to be

appreciated strictly aestheticaily and to consider seriously the idea of visual representations as

communication. Vastokas (ibid.: 53-54) subsequently developed her argument regarding

Aboriginal art as "writing," stating that there was a good reason why aboriginal people

referred to pictographs and pictorial representations as "writing." She (ibid.: 54) daimed that

for Aboriginal North America the birch bark images, or "birch bark manuscripts," were the

most noteworthy expressions of the relations between image and word.

She described in considerable depth the structure and role of the Midé and of the

Midewiwin Society for the Ojibwa, the role of the birch records for the Midé, the range of

their physical dimensions, the range of images being used "from depictive to symbolic, to

entirely abstract in character" (ibid.: 54). Vastokas cited Boone and Mignolo's (1994) daim

that the terms writing and art, if applied to most of Aboriginal America, were problematic

since, unlike western and other phonological writing systems, the goal in the Americas was

not "visible speech." In further support of her supposition, Vastokas (1996: 57 ) cited Boone

and Mignolo's proposition that Pre-Columbian American art and writing were largely the

same thing.

For Vastokas (1996: 57), the Ojibwa birch bark scroils belong to "semasiographic

writing systems" which communicate ideas independently of language.6 She asserted that, if

scroils could be accepted as examples of "semasiographic writing systems," historians could

obtain an insider's view of native American history. Boone and Mignolo had argued that,

within these systems, a subset of iconic writing systems exist composed of representational

pictographic units that transmit meaning without employing speech. Anyone wanting to read

these pictographic units already knew the general meaning of individu al units and so, could

ascertain the meaning of the different combinations.

However, this notion does not distinguish between the fact that different groups of

people might have the knowledge to use certain images and not others. It is impossible under

Boone and Mignolo's definition that a general vocabulary of pictographic units exists that

can be subdivided into groups which are in turn recognised by the general population as

6 Warkentin (1999:3) argued that historians of writing divide sign systems into two groups: semasiographic language systems (pictography) and phonographic (language based) systems. She asserted that phonographic systems were further subdivided into logographic (where the sign is the equivalent to the word), syllabic (the sign is a syllable) and alphabetic systems.

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having sorne meanings. Each group of pictographie units is used by either ail or specifie

groups, within that society, for different purposes and reasons. Therefore, sorne of these

pictographie units are not understood by ail.

Boone and Mignolo argued that, not pictorial and conventionalized images, but the

placement and context of the images carried meaning. They (1994: 18) asserted that images

behaved as texts in semasiographic writing systems; however, these writing systems did not

have fuil running texts but a highly conventional set of symbols with meanings similar to

those associated with paintings.

Vastokas (1996: 57) maintained that Boone and Mignolo's (1994) conclusions

regarding Mixtec and Aztec writing systems were pertinent to the pictorial narratives of the

Algonquians, since the scroils were among a variety of visual narratives that historians could

use to examine native American history. Therefore, if the images on the birch bark scroils

were accepted as "semasiographic writing systems," these scroils could be accepted by

historians as one of a number of visual narratives that provide an insider's perspective on

native American history.

The consequences of this claim are interesting, since they mean that an image can be

treated as valid a primary document as is a piece of text. Vasto kas stated that considering the

scroils as documents "merely presented a different set of historical chailenges" (ibid.: 57).

She believed that the "most obvious" problem was "the absence of absolute dating" (ibid.).

She believed that additional research was required into the oral traditions that accompanied

visual documents, and into the contexts in which they were utilised. She acknowledged that,

although information had been lost, a considerable body of information still existed.

Vasto kas also lamented that "very few elders" among the Aboriginal community were "stiil

in touch with the traditions" that created these images (ibid.: 58). Vastokas remained

optimistic that fundamental research into these birch bark scroils could be conducted,

despite these considerable obstacles, especiaily if Native and non-Native historians workcdin

conjunction with each other.

Fulford's (1989, 1990) articles fail into Vastokas' first avenue of research. His

findings demonstrate that use fuI and interesting information can be obtained if a detailed

examination of these images is undertaken. He considered the shapes of the twenty-four

song scroils utilised by members of the Midewiwin from White Earth Reservation in

Minnesota (Fulford 1989). Hoffman coilected them during the late 1880s for the Bureau of

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American Ethnology. Fulford examined them for patterns of structural variations, and

outlined how three complex symbols or shapes, which he identified as the otter, bear, and

bird, had evolved from clan markers into pictographic markers. It was impossible (ibid.: 134)

to examine precisely how the interactive process influenced the form of the pictographs

because this required comparative observations to be made by potential members of the

Midewiwin as they re-transcribed the record.

Systematic variations were observable ln redundant forms once the White Earth

pictographs were arranged into concordances (indexes). Twenty-four scroils were reproduced

in three concordances, which were published in conjunction with this paper. Fulford (ibid.)

maintained that this method was similar to that used by historicallinguists to reconstruct the

protoforms of a spoken language, because it highlighted the changes introduced by iteration.

The subtle variations existing in redundant pictographs reflected the changes introduced in

the process of recopying the images. Over time, these changes become highlighted and

modulated directly with the rate of iteration, as weil as with the formaI complexity of the

pictographs. A delicate balance existed, Fulford suggested, between those pictographs, cailed

forms, that were too simple to be recognised, and those that were too complex to be stable.

He argued that a certain degree of formaI simplification or standardization assisted

communication. Complexity, he suggested, introduced changes into the system that increased

its adaptability, and enhanced the potential flow of new information.

He used two interrelated indices to evaluate the complexity of each form and image,

and to reduce the potential of projecting ethnocentric conjectures that the complexity of the

symbols encouraged. Two terms were used, "simple" and "complex", to refer to the

symbol's frequency of distribution throughout the sample, and its capacity for

transformation (ibid.: 135). Symbols were termed "complex" by Fulford if they were clearly

distinguishable throughout the sam pIe and had an obvious capacity for transformation, while

"simple" symbols had a homogeneous distribution and were incapable of being transformed.

However, a symbol could be complex because of the frequency of its distribution and its

capacity for transformation, but simple in the wider context of its meaning to Hoffman's

informants.

Fulford (ibid.: 149) discovered that the otter, bear and bird shapes were weil

distributed throughout each of these scroils, and indicated a "high capacity for

transformation". He concluded that the transformation that he found arose as a consequence

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of the re-transcription of the song scroils. He maintained that the grain of the birch bark

could not entirely explain the syntagmatic and associative relations between the shapes,

which he cailed pictographs, of the White Earth scroils.

Fulford (ibid. 150), based upon Vygotsky, posited that the movement of the stylus

and eye aeross the birch bark scroils was connected to higher psychologie al functions, and

that the formation variations introduced through iteration had potential symbolic

significance. He maintained that Midé symbolism achieved its most powerful exposition if

the relationship between the sequential linguistic elements and the complex symbols was

examined, since the particular transformation features of these symbols could be identified as

the projection of the human form into natural objects.

The patterns revealed in the three concordances, Fulford asserted, provided an

insight into the symbolic world of the Midewiwin. He argued that the propensity of the otter,

bear, and bird symbols to fluctuate as a consequence of iteration into distinct human forms

echoed the unconscious maintenance of earlier symbolic associations. He contended that the

elemental symbols used during the protohistoric period were linked to those used by the

Ojibwa clans of the late nineteenth century through Midé rites. Images (ibid.) that were once

associated with real human faces from the Ojibwa clans during the eighteenth century

subsequently developed into the ghostly figures of the Midé birch bark scroils during the

nineteenth century. He concluded that the Midé were able to distinguish the images of their

ancestors in the symbols of the otter, bear and bird, although the Ojibwa clan system had

disintegrated.

Fulford's study demonstrated that connections existed between different shapes,

which he cailed motifs or symbols, and ethnographie details, although the context of these

meanings had changed.

Fulford (1990) later considered the verbal structure of these Midé chants to establish

how they were pictographicaily encoded. He limited his discussion to seven song scroils, six

of which shared the otter symbol. The seventh scroil was included since it shared several

other formaI characteristics with the six otter scroils. He (ibid.: 127-128) retranscribed and

re-translated the chants that Hoffman had compiled before reworking the entire corpus to

develop glosses to improve the flow, or simply supply better connections between the words

and the pictographs. It was impossible, he maintained, to provide definitive transcriptions

and translations of the Hoffman material due in part to Hoffman's informants' poetic use of

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languages. Fulford concluded that the reproductions of the scroils were generaily accurate by

comparing Hoffman's published reproductions with the originals in the US National

Anthropological Archives. He subsequendy placed the changes of the seven scroils in a

concordance by typing the revised version of Hoffman's original transcriptions of the chants

and attaching photocopies of the related pictographs to the top of the transcription. This

information he put on file cards in horizontal rows where each row corresponded with the

sequence of pictographs and changes of one song scroil.

Fulford (ibid.: 128-135) believed that the recognition of the taboo that existed on

uttering the otter's name eXplained the relationship between the pictographs of otters and

hum an arms in the song scroils. He argued that the recognition of this taboo was clarified by

chants that accompanied otter pictographs, since they ailuded to incidents in the Midewiwin

creation story but did not directly describe the pictographs themselves. These differences

caused a mismatch to occur between the visual and the verbal forms and transformed the

meanings of the pictographs and the chants. Fulford (ibid.: 135) maintained that the verbal

transformation that occurred was the result of an iterative process that occurred in traditional

Midewiwin chants and mirrored the taboos connected with enunciating the names of "animal

brothers" linked with totemic ancestors.

Both of Fulford's papers complement each other and demonstrate that, with careful

deliberation, these images can be analysed. Both papers arguably support Vastokas' (1996)

argument that native artwork could be used as "historical documents".

Similar shapes to those on birch bark scroils were examined by Fulford (1992: 190)

who considered the ninety-two page account of Vincent Roy, a fur trader of Scottish and

Ojibwa ancestry. Roy administered the American Trader's Post at Vermillion Lake between

1835 and 1839. Roy's account book, which could be securely dated to the 1830s, contained

drawings that strongly resembled those on birch bark scroils, Fulford argued. He identified

forty of the forty-eight different types of the trade goods recorded in the account book and

twelve species of fur-bearing animaIs. He determined which pictographs signified debits and

credits of each account and the identities of sorne of Vincent Roy's customers.

In being able to identify Roy's customers, and that they were not local to the post,

Fulford could indicate that people were willing to travel vast distances to ob tain goods.

Fulford (ibid.: 192-193) established that sorne of Roy's customers used remote posts such as

Roy's, which was outside Schoolcraft's jurisdiction. Schoolcraft was the nearest

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Superintendent of lndian Affairs in Michigan, and he discouraged Americans from doing

business with Ojibway who sustained ailegiance with the British crown.

Fulford (ibid.: 192-194) believed that Roy was semi-literate but his two years of

schooling while living at La Pointe had taught him numeracy, literacy, and a Calvinistic

attitude to business. These basic reading, writing, and mathematical tools enabled him to deal

with suppliers in St. Louis or New York. However, the pictographs Roy utilised to record his

inventory were familiar to his Ojibwa contemporaries including those used Midewiwin song

scroils (ibid.: 194). Fulford argued that Roy provided evidence of an assimilation process that

occurred amongst the Ojibwa over two generations during the nineteenth century, as the

proliferation of schools encouraged reading, writing, arithmetic, and the Christian religion

among the indigenous populations. He ascertained from Roy's account book that, despite

this process, Ojibwa stiil used traditional names, and considered themselves as living in

harmony with the natural world, although by the 1830s the fur trade had destroyed their

traditional economic, social, and political structures. Fulford's article indicates that the

indigenous people of the Great Lakes area understood and operated within two conceptual

frameworks and confirms that these images, although they appeared on the birch bark

scroils, were also used elsewhere as carriers of meaning and information.

A question exists regarding the relevance of this body of information, especiaily since

this materiallacks written documentation. The Aigonquian-speaking peoples, rather than the

Assiniboine, used a specifie group of images. Unfortunately, knowledge of Assiniboine art,

and of other Plains groups from before the nineteenth century is limited, given that much of

it was made of perishable materials that frequendy failed to survive in the archaeological

record. Greene (2001: 1038) observed that quillwork was the major decorative art form in

the Plains over a long period of time. Yet rock image sites also exist in the Plains region

(Keyser and I(lassen 2001), but the "biographic" style associated with this region is

connected to bison robes and the ledger book paintings used during the late eighteenth and

early nineteenth century (K.eyser 1977 and Greene 2001: 1042).

It is evident that the images, made by the Aigonquian groups and used as a means of

communication, and the techniques used to create them, have shifted over time. However, it

is clear that not ail of these images changed radicaily in appearance and experienced changes . . ln mearung.

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It appears that three groups of images exist, based upon who used them and their

audience.

The first group of images have not undergone considerable changes in their shape.

The Midé used these images to record their religious and medicinal information, and this

group has been examined by Fulford (1989, 1990), and Vastokas (1984, 1986, 1996).

The second group consists of the early geometric shapes that changed to floral

designs examined by Densmore, Coleman (1947), Penny (1991), Phillips (1984, 1991), and

Whiteford (1986, 1991, 1997). Many of the people who analyse these images invariably use

terms such as 'Thunderbirds', and 'Underwater Panthers,' rather than describe the shape of

the images.

The final group consists of those images that everyone in the Algonquian-speaking

community used. Unfortunately, little evidence exists of the images associated with this

group, but perhaps some of these were used by Roy (Fulford 1992). Nevertheless, Landes

(1968: 172) stated that images were familiar to ail Ojibwa hunters, trappers, and traveilers,

who used them to indicate boundaries, trails, notices of different sorts, and on grave

markers. Coleman (1947: 63) observed that the totem of the deceased individual was placed

on grave markers. Warren (1984 [1885]: 89-90) discussed some images inscribed on a copper

disc that he maintained recorded the number of generations of a family of the Loon totem

who had lived in the La Pointe area. The indentations indicated that eight generations had

lived in this region. Although relatively little is known it is clear that this group of images was

important to the Algonquian speaking peoples as a means of communication

Although relatively little information exists about this last group of images, they must

be considered, because this group of images indicates that everyone within the Algonquian

speaking community used images. It is therefore likely that everyone knew the entire range of

images, and understood how they were utilised and combined. An individu al could perhaps

use one or several images to express an idea, something about an individual, or leave a

message. It appears from Landes (1968) and Coleman (1947) that anyone could use, make,

and understand them. The creator of these images could be an ordinary individual, and did

not need to be a Midé, or any other specialist within the community.

Since ordinary people used images as a means of communication, it is possible that

they were known by everyone, and that an image meant more than just one thing.

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Unfortunately, little information exists as to what these images looked like, how

many existed, their range, or how they were combined, but it appears from Coleman (1947)

and Landes (1968) that they occurred individually rather than as the image groups of the

birch bark scrolls. The fact that they were used by a wide variety of individuals implies

everyone knew how to use how to use them and that specialists did not exist. Hence, these

images retained their shape much like those used by the Midé regardless of the considerable

changes in the imagery used in beadwork and weaving. However, whether any shifts in

meaning occurred remains impossible to establish.

Conclusion:

It evident that the information needed to contextualise the pictograph sites in the

Lake of the Woods derives from a range of disciplines. There is considerable agreement

about the climatic changes, and the geological history of the region. But the historians and

archaeologists find it difficult to agree who lived there, in part because each discipline uses

different types of evidence to solve their problem. Ethnohistorians (Bishop, Ray, and Smith)

argue that historical documents are useful for tracing ethnicity in the early historie period.

Many archaeologists, who pre fer to equate ethnicity with archaeological cultures, do not

share this opinion. There is sorne agreement that the Sandy Lake materials around the

Winnipeg River are possibly Assiniboine.

With the exception of Meyer and Hamilton (1994), archaeologists tend to assume

that the area was occupied by only one ethnie group at a time. While sorne archaeologists

adamantly as sert that the Ojibwa had already arrived in this region by the early historie

period, historians argue that several groups of people from different ethnie backgrounds,

Cree, Ojibwa, and Assiniboine resided here.

The inadequate archaeological data, in conjunction with the insufficient historical

references to the individual groups who lived in this region prior to contact, at contact, and

du ring the early historie period, inhibits scholars from identifying the terri tories of various

groups. The problems resulting from different names for the same groups could perhaps be

resolved by the careful use of the historical documents and the identification of synonymous

designations.

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1t also, so far, has proved impossible to ascertain which specific groups of

Algonquians, Cree or Ojibwa, lived in the region between Lake Superior and Lake Winnipeg.

However, both groups shared a similar symbolic system.

From the letter written by La V érendreye, in 1736 scholars know that Siouan­

speaking peoples were in the region at the same time as the Algonquian speakers. Since the

early part of the eighteenth century, the Assiniboine were allies of the Cree against the Sioux,

although the Assiniboine are linguistically closely related to the Sioux (DeMallie and Miller

2001: 572).

The first reference to the Assiniboine in the J esuit Relations for 1657-1658 describes

them as living about 100 miles from Lake Nipigon, east of the Lake of the Woods (DeMallie

and Miller 2001: 573). Jean-Baptiste Louis's map, dated 1697, indicates that the Assiniboine

resided north and west of the Lake of the Woods while the Sioux were in the south in the

area now called Minnesota (DeMallie and Miller 2001: 572). 1ndeed, the Lake of the Woods

is referred to as Lake of the Assiniboine. This calls into question Wright's suggestions (1987:

Plate 9) that the Ojibwa, Cree, Algonquian, or Montagnais peoples inhabited the Lake of the

Woods between AD 500 and European contact.

By the early seventeenth century, the Assiniboine resided seasonally on the western

half of the Lake of the Woods, and would do so continually until the middle of the

eighteenth century (Heidenreich 1987: Plate 37). Algonquian-speaking peoples, throughout

this period lived in eastern portion of the Lake of the Woods and gradually took control of

the region as the Assiniboine moved westwards (Heidenreich and Noël 1987: Plate 40).

The question of changing lake levels was considered, since archaeologists in northern

Ontario have traditionally found sites by examining the large expanses of cliff faces along the

shores of lakes and rivers. The graduaI but dramatic increase in the water level starting at the

end of the nineteenth century caused the shape of the Lake of the Woods to change, and

possibly completely or partially submerged pictograph sites. 1t seems likely that pictographs

that are known today were once physically located higher up the cliff faces. Yet, if the water

level had fluctuated as much as seven feet prior to keeping careful records, the positioning of

images could have reflected the differing high water levels at the time they were painted.

1t is very difficult to create a chronological framework regarding the precise ethnie

identify of those who lived in this region in prehistoric times. Historians and archaeologists

have had severe problems in attempting to connect the archaeological and the historical

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record to determine which indigenous groups resided in a specifie region at specifie rimes. It

is relatively easy to use historical records to determine the ethnic identity of a group of

people from a specific geographical region during the historical period. However, prior to the

arrivaI of the Europeans in this region, such records do not exist. This is caused parrially by

continuous changes in the naming of the people who lived in this region, and the difficulties

of identifying which archaeological complex was associated with which ethnic group.

Osteological information is interesting but, like other archaeological information,

bones do not indicate the ethnic identity of the individuals. However, it cannot be excluded

from a discussion of the identities of individuals. Examination and information regarding

burial practices possibly provides information about the social, religious and cultural

identities of the individuals concerned but not about their ethnic identity. Examination of the

bioanthropological evidence (osteology, human blood group analysis or mitochrondrial

DNA) indicates that considerable advances have been made, but these sciences inform the

archaeologist about the genetic relationships, not about the cultural affiliations, of the groups

involved. Specific traits were shared by the Cree and the Ojibwa.

Many of these images have the same physical appearance despite the passing of time.

Several scholars have demonstrated that similar stylistic and design traits could be shared

with others, and may have belonged to specific groups (Duncan 1991; Lanford 1984; Phillips

1984 and 1999; Sager 1994, 1995 and 1996).

Solid evidence regarding whether the images of the pictograph sites in the Lake of

the Woods region were created by the Cree or the Ojibwa does not exist. It is easier to

conclude that these images were made by the Aigonquians rather than trying to ascertain

whether they were created by the Cree or the Ojibwa. It is possible to posit that they were

probably created by Algonquian-speaking peoples rather than Assiniboine-speaking peoples,

since the rock images in the Lake of the Woods visually strongly resemble those of sites

elsewhere in northwestern Ontario where groups of Algonquian-speaking peoples resided.

lndeed, the images of the rock images created by the Assiniboine are visually very different

from those created by the various groups of Algonquian-speaking peoples in northwestern

Ontario. A specifie group of images were used by the Algonquian-speaking peoples rather

than the Assiniboine.

The physicallocation of the sites in the Lake of the Woods also fits in to the general

Algonquian pattern of the rock image sites in northwestern Ontario. This warrants using the

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/ '

Algonquian ethnographie data ta interpret the meaning(s) of these images and, hence,

justifies using homologies for eonsidering the meaning of the Lake of the Woods images.

Bence without either the arehaeologieal or the ethnographie proof for warranting the ethnie

origins of this imagery, but based upon eulture-historieal data, 1 argue that a basis exists for

using general Algonquian cultural data to interpret the rock images 1 am studying in this

thesis.

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Chapter III: A Review of the Literature concerning the Study of Rock Image Sites in the Lake of the Woods in the Canadian Shield prior to 2001.

The collection and interpretation of data are intergenerational processes in which

each new generation amplifies, modifies, and builds upon the work of previous generations

of researchers. A critical evaluation of previous work is an essential part of planning and

executing any new research project. It is important to acknowledge, at the same time, that

most investigators work within their own paradigm. However, this acknowledgement should

not prevent their work from being critically and carefully examined.

The goal of this chapter is ta present and discuss the work undertaken prior to my

own by previous researchers concerned with the pictograph and petroglyph sites in the Lake

of the Woods area. 1 intend to establish which approaches have been the most popular, what

previous researchers have thought of pictograph sites, and how they examined that in which

they were interested. This information is important to examine sin ce it provides a standard of

comparison, a yard stick against which to compare, examine, and contrast the new data that 1

collected. Although this chapter is specifically concerned with the analysis of the pictograph

sites of the Lake of the Woods area, sometimes 1 will make reference to analogous studies of

sites elsewhere in the Canadian Shield.

The literature in this chapter is divided into seven sections. The first discusses the

earliest investigation of these images with specific reference to the Lake of the Woods.

Section two examines the technical literature that has discussed how pictograph sites have

been studied with special emphasis on Ca) subdividing the sites into sections, (b) the

vocabulary used to describe the images and Cc) the development of the techniques used to

record the images. Section three is concerned with the considerable body of literature that

presents the issues involved in the technical analysis of these sites. It is divided into two

parts: Ca) recording and interpreting the pictographs and petroglyphs and (b) the

conservation of the pictographs and the different methods used to analyse them. The last

three sections critique the literature that belongs to one of the five different approaches that

exist in archaeology: culture-historical, contextual, and intuitive, analogical, or homological.

Since these approaches are different, and a clear order exists Csee discussion in Chapter 1), it

is important for the literature belonging to each approach to be examined in sequence.

Therefore, section five considers the literature belonging to the culture-historical approach,

where archaeologists have considered the shape, location, and date of the images. Section six

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deals with the literature classified as belonging to the contextual approach, which involves

the search for patterns relating different images and combinations of images both between

and within sites. The seventh and final section reviews the literature in which archaeologists

assign meanings to images on the basis of three methodologies which are employed either

together or separately. Since three alternative approaches exist, this section contains three

parts: (i) the intuitive approach, (ii) the analogical approach, and finally (iii) the homological

approach.

Section 1. The earliest investigation of these images

Mackenzie (1793), Schoolcraft (1851-1857), Bell (1879-80), and Lawson (1885)

recorded the presence of images either painted or engraved on rocks in the Canadian Shield

prior to the twentieth century. While examining the geology of Molson's Lake to the west of

Hudson Bay in 1879, Bell (1881: 7c) found a pictograph site on the north side ofPai-Musk­

taban Sipi near its mouth. The painted figures existed on a gneiss cliff that "measured up to

100 feet" (ibid.) in the form of "small figures in red ochre, said to have been painted by the

father of the present chief of the colony of lndians which removed a few a years ago from

Little Playgreen Lake to Fisher River, on the west side of Lake Winnipeg". The largest

images were "not more than one foot high" (ibid.), and most of them were not more than

eight inches. According to Bell, among them were "represented[ed] a boat, canoe, tortoise,

bird, deer, oUer, lndian, pipes, etc." He stated that the local lndians described them "as being

much more wonderful than they really are".

The geologist Lawson's (1885) publication was the first to consider the meaning of a

pictograph (DiKp-1) and a petroglyph (DiKo-2) site in the Lake of the Woods. It is difficult

to establish which rock image site was the first to be recorded in the Lake of the Woods area,

but Lawson's detailed descriptions and drawings of DiKp-1, and a nearby petroglyph site,

DiKo-2 probably hold that distinction.

• Site \inde!' diseuss! on

Figure 3.1: Map of the sites that Lawson recorded in 1885.

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,~

Lawson commented on the groupings of the images at the petroglyph site, DiKo-2 (figure

3.2) and posited that there was "little hope" of establishing any meaning or narrative because

the groups of images, or archaeological sites, were so isolated from each other (ibid.: 656).

· ~ , . ~K .. 1: HU

~ "

'>i 8 I~ 1.

Y r.- Ct, """ 4;fr~"'~

U " 'J< <1-'" · F';, 0 ... C<$ ~~

" 0 :D"t ,.":7l#'M;,S. ... " ~ • ~7

· • b .. t •

Figure 3.2: Lawson's published drawing of the images at DiKo-2, the petroglyph site.

Lawson compared the images that he described in DiKp-l and DiKo-2 to engravings

on large rocks found in the Alagoas, Brazil, described by John Brenner in a previous issue of

the American Naturalist (ibid.). Lawson also noted the similarity of the images at DiKo-2

with the painted images at the pictograph site (DiKp-l) painted on hard greenstone nearby

(figure 3.3).

Figure 3.3: Lawson's published drawing of the images at DiKp-1, the pictograph site from 1885.

Lawson concluded that the similarity between the engraved images and the painted

images suggested that they were "closely related in authorship." He was obviously interested

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in who might have created them, sin ce he concluded his paper with: "[1]he Indians of

present day have no traditions about these inscriptions beyond the supposition that they

must have been made by the "old people" of long ago" (ibid.: 657). However, if the

pictograph site in 2001 is compared with how Lawson drew it in 1885, it is clear that he did

not see or record the red images to the right and above the ones he published. The

photograph of DiKp-1 below demonstrates that what Lawson saw differed from what

existed in 2001. It is possible that the other images were painted later.

Figure 3.4: Annotated photograph of DiKp-1 taken in June 2001.

Section 2. More recent literature.

More recent examinations of rock image sites are published in a variety of places.

Sorne of these publications have summarised the discoveries of pictograph and petroglyph

sites in the Canadian Shield (Brenner 1994; Conway, T. 1979; Dewdney 1963, 1965, 1977,

1979a; Molyneaux 1977, 1980a; Nute 1948; Wellmann 1979a). A few have considered issues

such as tourism (Arsenault 1996) and political and ideological conflicts (Arsenault 1997;

Nelson and Hinshelwood 1998). Others have discussed trips that involved searching for,

finding or visiting, sometimes recording sites in the Canadian Shield, and also speculating on

the meanings of images found (Cameron and Cameron 1979; Dewdney 1958, I<nowlton

1992; Macfie 1992; Mallory 1961; OIson 1961; Pettipas 1991a). Sorne briefly discussed and

referenced rock image sites as being widespread throughout the Canadian Shield within a larger

discussion of sorne other related topie. One of this group, Dickason (1972: 13), used part of

DhKm-3 as her example of the pictographs of the Canadian Shield. Several archaeologists were

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determined to find the oidest pictographs or petroglyphs in the Canadian Shieid (pohorecky

& Jones 1968a; Steinbring 1993, 1999).

During the 1970s and the 1980s, archaeologists concerned with pictograph sites were

interested in two related issues: the selection of a place in the lands cape and the orientation

of the site. Reid (1980) observed from the information on the pictograph sites in the West

Patricia region north of the Lake of the Woods that pictograph sites tended to occur on

straight shorelines, or coastlines that were not broken into parts by bays, islands or points

and that the creators of these sites preferred rock faces that faced in a south-to-east

direction. Rajnovich (1980b: 34) developed this ide a further in her discussion of pictograph

sites in Cuttle Lake, arguing that straight shorelines were predominately selected "to increase

the spectacular effect" of the images because these shorelines enabled the images to be

visible both from nearby and from afar. She argued that, based on her examination of sites

from the Rainy River region (south of the Lake of the Woods), south-to-east facing rock

walls were selected as light conditions here were best for creating and seeing paintings. The

"rising and noontime sunsrune reflected from the water" beside the cliff face caused

"dancing light sparkles over the work heightening its dramatic value" (ibid.). She asserted

that cliff faces which faced west-to-north only experienced "shadows or the weakest sunset

light." She assumed that pictograph sites always occurred on a cliff face immediately beside a

body of water close enough to reflect light on any images painted upon the rock's surface.

Licence reports are useful for finding sites and establisrung the range of work

conducted at different sites in the Lake of the Woods (for example: Cameron 1982,

Molyneaux 1978, 1979, and 1981). Cameron (1989) described fieldwork activities in the Lake

of the Woods where she recorded and described the images at four petroglyph sites:

Kennedy Island, called DjKp-4, Sunset Channel, called DiKo-2, Tranquil Channel, called

DjKp-3, and Mud Portage, called DkKr-4. She referenced these sites only by their local

names and did not use their Borden numbers. Such practise makes trac king what sort of

archaeological fieldwork was conducted at each site and by whom difficult for subsequent

archaeologists.

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• Sites _der m!IeU!llsi61l

• Picmgra,ph shes • Petmglypb !J'tes

Figure 3.5: The four sites that Cameron recorded in 1978.

Molyneaux (1978) wrote in his report to the Ontario Heritage Foundation that his

intention was to create a photographie record of two petroglyph sites when the water level

was abnormally low. He noticed that Lawson (1885) had described the lake levels as varying

over a range of 10 feet (ibid.: 1) but that the lake's flow and therefore its level was now

artificially controlled. Molyneaux, like Cameron (1989), did not use Borden numbers, only

local names: Kennedy Island, or DjKp-4, and Sunset Channel, or DiKo-2. Molyneaux (1979)

for his subsequent study produced a detai!ed photographie record of six of the seven

pictograph sites in Whitefish Bay, in the south eastern portion of the Lake of the Woods:

DiKm-3, DiKm-4, DiKm-l, DhKm-3, DhKm-4, and DhKm-5. Molyneaux hoped to use

photography to record the images systematically, accurately, and efficiently given the

"difficult field conditions" (ibid.: 4) and also to minimise human error and interpretation.

Other reports by Molyneaux discuss sites in areas neighbouring the Lake of the

Woods (Molyneaux 1981, 1982, 1985a; 1985b). Both his 1974 and 1975 publications resulted

from projects conducted under the auspices of Trent University and the Canadian

Conservation Institute. The Trent University team headed by Molyneaux examined eleven

pictograph sites and twelve rock image sites in Northwestern Ontario. Eight of these sites

existed in the Lake of the Woods, including DiKm-3, DhKm-5, DhKm-l, DhKm-4, DhKn-

1, DiKo-l, DjKn-l, and the now extinct lichenoglyph site called DhKn-2. However, the

team considered only one Lake of the Woods site, DiKp-l on Cliff Island, in the 1975 study.

Still other studies only mentioned or briefly described pictograph and petroglyph

sites in the Lake of the Woods (Fox 1974; Reid 1976 and 1977). Reid surveyed numerous

archaeological sites, among which were fifteen pictograph sites. These sites were examined as

part of an inventory that was conducted at the request of the Regional Lands Co-ordinator,

Northwestern Region, Ministry of Natural Resources (1976: ü). The goal of this

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archaeological project was to coliect data for the Lake of the Woods General Land Use Plan

and its principal concern was the "dense st current and potential development within the

northern half of the Planning Area" (ibid.). A number of specific archaeological sites were

tested at the request of the Senior Lands Planner. A total of seventy-one archaeological sites

were recorded in May 1975. Ali the pictograph sites were aliotted Borden numbers and

assessed as to their level of "interpretability" to the public as weli as their level of

"representability" (ibid.: 13-15). What these terms meant is unclear. Reid provided the

precise geographical location of, and specified how to reach each site. He also postulated

their "cultural affiliation," essentialiy their age, and sought to determine whether the site had

any religious significance to the local indigenous population. The physical condition of each

site was evaluated, and Reid established whether the general public knew of its existence and

whether it had been discussed in print. He did not describe the images but photographed and

determined the size each site.

Fox (1974: 3) described only DhKm-1, a pictograph site calied Devil's Hole, in the

southern part of Whitefish Bay, Lake of the Woods. He observed that bundles of clothing

were stuffed into a cleft in the rock surface of this site. An informant told him of rumours

that these bundles had been "placed there by local native people attempting to affect a cure

for a sick child." He considered that perhaps the offerings of these bundles were closely

connected to the "offering tree" which Ritzenthaler (1970) had described as existing among

the southern Chippewa. Fox found similar items of clothing such as buttons, buckles, and

suspender components at this site which he presumed to be evidence of earlier offerings. He

also found lead sinkers, a corroded metal bowl, and numerous coins (1974: 3.). The presence

of these objects was recorded and they were left where they had been found. He speculated

that the clothing bundles had not been disturbed since they were left as offerings. Birch bark

scrolis were not found at this site, although fragments of birch bark with stitching punctures

were found one to two metres back in the large cleft at this site. Fox posited that these

fragments might have been part of a birch bark container used to hold food offerings and

sent these fragments to the Canadian Conservation Institute for preservation. Before Fox

finished recording this site, ali the adjacent clefts in the rock were checked and photographs

were taken (ibid.: 4).

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Figure 3.6: Fox's photograph of DhKm-1 in 1974.

Lambert (n.d.) used the same procedures as Reid had in 1975 (1976) to record eight

pictograph sites (DkKn-7, DkKn-6, DjKn-l, DhKm-5, DjKn-2, DhKm-18, DhKm-4, and

DhKm-l) in the Lake of the Woods. This report was never published. Ali the pictograph

sites he recorded in the Lake of the Woods were photographed, recorded using direct 'dot­

for-dot' tracing (ibid.: 20) and described in considerable depth. These sites were discussed in

the findings of the third Northwestern Ontario Rock Art Project, conducted in 1985-1986.

This project considered some of the pictograph sites in the Lake of the Woods. The other

reports dealt with pictograph sites elsewhere in Northwestern Ontario (Lambert 1983, 1985).

Lambert (n.d. 201) argued that classification of the images from the pictographs examined in

the 1985-1986 project permitted him to distinguish between sub-areas of the Winnipeg River

drainage basin and the Bloodvein River drainage basin (ibid.: ii). The abstract of his third

survey indicates that he viewed these images not as 'art' but as a method of communication.

Lambert (n.d.: 201) argued that the largest number of animal creatures occurred in

the Bloodvein River Region, north of the Winnipeg River drainage basin. He asserted that

his results indicated that sympathetic hunting magic was an important function of the rock

images in the Bloodvein drainage basin, since more images of creatures were present in this

region. In the Winnipeg River region, images of canoes and anthropomorphs occurred more

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often. He (ibid.: 199-200) observed that there were more hand prints, and pairs of handprints

in the Winnipeg River region than in the Bloodvein River drainage basin.

For two sites in the Bloodvein River region, Lambert (ibid.: 202) posited that a

connection existed between the orientation of the site and its function. Almost ail of the

images at both sites were hand prints and both had similar orientations. He suggested that

both sites "signposted a possible avenue, by way of a portage" to another lake (ibid.: 202).

The pictograph sites he cailed the Rushing River sites, DjKn-1 and DjKn-2, in the Lake of

the Woods region acted in a similar manner, since they both used to exist on rapids or fails

prior to the raising of the Lake of the Woods water level (ibid.). He argued that pictograph

sites had "a function ta guide the traveiler" especiaily when they occurred in narrow

"situations" since those site areas were difficult to avoid. This meant for Lambert (ibid.) that

these sites could be interpreted as "message boards, maps or navigation aids." Unfortunately

he was unclear whether the message was to "guide or identify, or warn of fast water or

malevolent spirits".

He (ibid.: 204) argued that the images he examined were related to various secular

activities such as hunting, fishing, and horticulture. Specifie images he argued (ibid.: 204-

205), although unstated, were connected to hunting ungulates and sturgeon, others indicated

a life-threatening disaster connected to horticulture, and that sorne images were connected to

the Midewiwin. It is evident, upon close examination of Lambert's discussion of DhKm-1

and DhKm-4, that he has included and treated the images which comprise the site DhKm-1

as part and parcel of DhKm-4.

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Faœl-f)2A ~~ $'

t \ el ~If

VI 1'.4/sm, -/"

5ITE#!J2A "()eyih /fal" P

os' Whitd'lsh l>~ Lake "f th<r bods

Q ",.

'l.f·~J""f"'. 1 i , \) i ) ."."

1 ~~ :S"

.,.t.rf • ...r N=Jf fi2tJ(Z" Dl auf JtlI1 IS; IJ.tJ

Figure 3.7: Dewdney's 15 July 1960 field record of Site # 92A, now called DhKm-1 and DhKm-4.

This may have occurred because Dewdney, in 1960, called DhKm-4 Site # 92 and

DhKm-1 Site # 92A. It is clear from his field drawings that the images on Faces II and III of

Site # 92A are part of the pictograph site subsequently classified as DhKm-1. Face I of Site

# 92A is now called DhKm-4.

Pictograph and petroglyph sites were frequently recorded as part of larger

archaeological surveys concerned with other types of archaeological sites in the Lake of the

Woods. One notable example in the Lake of the Woods is Pastershank's (1989) report, in

which she considered pictograph sites as separate units of analysis, therefore not to be

analysed in conjunction with the archaeological sites examined at the same time. These

studies, aimed to establish that sites existed and to describe them, did not analyse them in

detail. This treatment occurred elsewhere in the Canadian Shield (Conway 1975, 1984;

Dawson 1973; C. Halverson 1988; Hill 1982, 1983; Lemaître 1995; Smith 1981). Occasionally

archaeological surveys were conducted for the sole purpose of surveying for pictographs and

petroglyphs but not for "conventional" archaeological sites that could be excavated (Lambert

1983, 1985, and n.d.; Rusak 1992a; Scott 1980; Pelshea 1980; Pelleck 1981; Rajnovich 1980b,

1981 b). The quantity of literature published in other government reports indicates that

archaeologists were concerned with these images (Conway n. d. c; Friend 1983; Jones 1966,

1981a; Petch 1991; Pohorecky and Jones 1968b; Rajnovich 1980c, 1980d, 1981c; Rusak 1991,

1992b; Steinbring and Iwacha 1982; Steinbring 1998; Tassé 1977a). These sites would have

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been recorded and discussed at sorne length in the reports required by the relevant

government bodies to inventory and analyse the archaeological sites in a given region.

Section 3. Techniques used to record the pictographs.

Subsequent methods used to record and analyse rock images are derived from

Dewdney's work. Indeed, Dewdney is rightly considered to be the "father of Canadian rock

art studies" since he was the first person to undertake a comprehensive study of these

images. The initial method for determining the size of sites appears to have emerged as

Dewdney (Dewdney and I<idd 1962) developed rus techniques for sketching and measuring

pictograph sites.

The technical lite rature is divided into three parts: Ca) subdividing the sites into

sections; (b) describing the images; and Cc) recording the images.

a) Subdividing sites into sections

It is crucial to understand the problems involved in Dewdney's use of the terms 'face'

and sometimes 'panel'. If the area covered with ochre is large, sites are invariably subdivided

into smaller components to aid recording, photography, and description. The initial method

for determining the size of a site emerged as Dewdney developed rus techniques for

sketcrung and measuring pictograph sites.

5itfE #10' 5uns"r ChclrJlleI­Lake of thRWoodr Ailg./Z'S9

(perroglyplzs of 5" .. 1171 sbawn ds~wh.-n:)

rwa>'/!f

Figure 3.8: A field recording by Dewdney of two pictograph sites in the Lake of the Woods, Site # 70 Sunset Channel (DiKp-l) and Site # 69 Picture Rock Island (DhKm-3).

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Dewdney's sketches of the rock features of the different parts of a new site probably

enabled him to identify the physical location of various groups of images (ibid.). Yet

Dewdney did not identify different parts of a 'face' as 'panels' if they had different

orientations to each other. It is possible that this practise developed as a result of other

fieldworkers beginning to take compass bearings of rock faces. It was observed that the

surface of the rock used for paintings faces the rising or the setting sun or in a southerly

direction (ibid.: 6). Hence the pictograph sites that Dewdney examined faced towards the

east, the west, and the south. Indeed, Dewdney (ibid.) stated that he had "seen only three

sites on wruch the sun never shines" where lichen grew, but he did not state in wruch

direction the surface of the rock was faced.

Difficulties exist with the meaning of the terms 'face' and 'panel' since researchers

often do not clarify their meanings. Unlike Pastershank (1989), who used these terms but did

not define them, Rusak (1992: 1) defined a 'Face' as a single figure or group of figures on a

common rock plane. She argued that the "F" must have its first letter capitalised to

distinguish it from its common meaning. It appears that she used the concept of panels to

subdivide large sites, especially if two areas containing pictographs were physically separated

on the same face. These panels were numbered sequentially if the panels had different

orientations.

It seems likely that the concepts of faces and panels were used to divide the rock face

into surfaces that could be discussed and analysed easily. In rus unpublished report (n.d.: 21),

Lambert developed the ide a of splitting sites even further into manageable parts, if cliff faces

with paintings were "sufficiently large to warrant supplementing the standard Face and panel

designations with seriaI, horizontal data points." Lambert maintained that seriaI horizontal

points were useful if separations appeared on the rock face. He (ibid.) applied it at Bloodvein

1 Pictograph, EiKs-l, in the Bloodvein drainage basin, but maintained that trus technique

would have been useful in the 1982 and 1984 Northwestern Ontario Rock Art Project

(Lambert 1983, 1985) studies. However, he acknowledged that he had not discovered many

sites where there were "continuous paintings for long, relatively flat, clifflengths" (ibid.: 23).

While archaeologists use this technique to subdivide pictograph sites for the purpose

of making them easier to describe and quantify, it can cause problems for subsequent

researchers, since precise rules do not exist concerning how trus technique should be

employed. Twelve pictograph sites were divided into parts when they were first recorded.

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This group includes DiKm-3, DhKm-3, DhKm-1, DhKm-4, DiKn-1, DhKn-1, and DjKll-1.

Each site will be examined in sequence. It is clear that both Dewdney and Pastershank

invariably subdivided sites into parts if they were the first individuals to examine a site. It is

therefore easy to subdivide this group into two smaller groups according to whether

Dewdney or Pastershank recorded the site. Dewdney examined DiKm-3, DhKm-3, DhKm-

1, DhKm-4, DiKll-1, DhKll-1, and DjKll-1, while Pastershank examined DgKl-19 and

DgKl-17 first. However, Pastershank contradicted Dewdney's divisions of DgKl-1 and

DgKl-2 when she examined them in 1989. DhKm-5 will also be examined because, rather

than being subdivided, it grew in size.

DiKm-3:

Dewdney used the crack visible in the middle of the field drawing (figure 3.9) and

photograph (figure 3.10) below to differentiate between the two parts, or Faces, of the site

called Site # 28. tt.: ---

about thrre md6 S)E. of 510ux St=lôALSO:

Narrowr- t'fu: I"t<;fc/'*hing i-km~d"po{,ft,.dafth'sr;,~,I;'field Book2

thfT rv.sl.dlJt2 of Q 'Pf'4!:P" t'rlH-"Fou"d hli!t""i~ now il! f1I", ROMdfrnogroph{c:coIJochon

faC', l

"

ettiUSTOPHIR DIWON..,

Figure 3.9: Dewdney's field drawing of Site # 28, undertaken on 15 August 1953.

Dewdney's first Face is the left side of the rock tripe growing vertically across the

pictographs, which is evident on the extreme left hand side of the photograph below.

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Figure 3.10: Face 2 and 3 of Site # 28 by Dewdney in 1953.

Unfortunately, it is unclear whether Reid, who examined the site in 1975, and Molyneaux,

who photographed and examined it in 1979, used Dewdney's subdivisions in their analysis.

DhKn-l:

Dewdney subdivided this site into Face l and II probably using the large vertical

crevice that exits in the cliff face that separates the two clusters of paintings in figure 3.11.

r", fU1'~" '---

IJ'q~

18"'''

a6<W12'waftzr Auy,Ij.l5'i/{J .

!

Sire #/OG 06abikonNofTi:JW5, /VOFtt7@a'of ObobikonlJO'/{. S'outil of AU!I71?atl Pel7il7su(<1, Lake oft~ W'oodr

Figure 3.11: Dewdney's field drawing of Site # 106 undertaken on August 19 1960.

l t is not clear whether Reid in 1975 and Molyneaux who examined it in 1974 and

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1981 followed Dewdney's method of dividing this site into two parts.

DhKm-l and DhKm-4:

Dewdney's field drawing of Site #92 A and Site # 92 indicates that the two sites

DhKm-1 and DhKm-4 were considered one site (see figure 3.7). Dewdney found and

recorded both in 1960, classifying them as one site. He recorded only half of the encire site,

possibly because he did not think that smears of ochre were paincings. However, why

Dewdney only recorded the images from part of DhKm-1, which he called Site # 92,

remains unclear. Dewdney's Face l is DhKm-4, while Faces II and III are part of DhKm-1.

DhKm-4 is clearly not immediately beside DhKm-1 as Dewdney's field drawings (figure 3.7)

of both sites imply. However, why Dewdney only recorded the images from part of DhKm-

1, which he called Site # 92, is unclear. The sites are more than a few metres apart from each

other as the annotated photograph in figure 3.12 below indicates.

Figure 3.12: The Close Proximity of DhKm-4 to DhKm-l.

Dewdney missed an image now classified as a smear as indicated by the annotated

photograph and Dewdney's photograph of the site below.

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Figure 3.13: Annotated photograph of DhKm-1 in 2001 by Colson according to Dewdney's divisions.

Lambert, in his (1985) unpublished study of sorne of the pictograph sites, made the

mistake of considering sorne of the paintings of DhKm-1 as part of DhKm-4, despite Reid

(1976) in 1975 reporting that the two sites were separate entities with their own Borden

numbers. Why this confusion existed for Lambert is difficult to determine, since he would

have known that Reid had already designated DhKm-1 as a separate entity from DhKm-4.

His own records show that Lambert (n.d.) knew of Dewdney's 1973 publication and had

probably seen Dewdney's 1960 field drawings of DhKm-4 and DhKm-1. The images of

Lambert's Face II of DhKm-4 are images of DhKm-1 that he recorded, if one examines the

annotated photograph below in figure 3.15. Lambert recorded the images that he deemed

were the site. He applied a technique of classification developed during his field survey of

sorne pictograph sites in the Upper Severn region of Northwestern Ontario in 1982 (1983).

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Figure 3.14: Annotated photograph by Colson of DhKm-1 taken in 2001 according to Lambert's divisions.

DhKm-3:

Dewdney was the first person to record this site. He subdivided it into three sections

as seen below in rus field drawing (figure 3.16).

#69 P,cTure Rgd; /,/<7nd WI)!fefish Boy,Lake of the Woods Aug855'

16,50 Fow$

CHili STOPHtR otWONEY

Figure 3.15: Dewdney's field drawing of Site # 69 undertaken on 8 August 1959.

It is unclear whether Molyneaux in 1974 and 1979, Reid in 1975, or Pelshea in 1978

paid any attention to Dewdney's subdivisions of the paintings.

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DiKn-1:

According to the two field drawings below (figures 3.16 and 3.17), Dewdney divided

this site, initially called Site # 91, into five parts. Several of these parts were subdivided again .

• rth<:ilsttip of Ha'{A:r Penil/sale; '/letfn e/ltranœ toWlJtlefishfJar,ta/œoftil<?/Iiâ"ds :j

lB·

\ 'tl ;i' [~:~~I-::~ lB'

,7:1..170

Face 1

[ '\,

Facclb Fac,z Il/:'

CH~U STOPHER DEWONtV

Figure 3.16: Part 1 of Dewdney's field drawing of Site # 91A and B, undertaken on 15 July 1960.

wntinued)

/t(!'1'1IttÇ ,;'own"

OruVII wc/ur kw/

or; cr /u/,/ 15; INO

{ace V

'"

,,' ./,,,"'" "",du·

50' _ ~ __

Ct11\1 STOPHi'R DEWDNEY

Figure 3.17: Part 2 of Dewdney's field drawing of Site # 91A and B, undertaken on 15 July 1960.

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DjKn-1:

Dewdney recorded this site as Site # 29 in 1958. From examining two photographs

of trus site, rus field notes in New World Arcruves at the Royal Ontario Museum, and

Dewdneyand Kidd's publication (Dewdney and Kidd 1962: 27 and 1967: 29) it seems that it

contained two components.

Figure 3.18: Setting with offerings and C.D., Site # 29 by Dewdney.

The second part of the site was published in Dewdney and Kidd's publication

(Dewdney and Kidd 1962: 27 and 1967: 29).

Figure 3.19: Photograph of part of DjKn-1 called Site # 29 taken by Dewdney in 1959.

Unfortunately, it remains unclear whether Molyneaux in 1974, Reid in 1975, or

Pelshea in 1978 used Dewdney's method of dividing the site into two parts. However,

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Lambert (n.d.) considered the site as two separate parts, recording two parts of this site as

Face l and Face II. Rusak in 1993 expanded the site to include a new section which she

called Face III. This was the location of a hand print that existed higher up the same cliff as

part of the same site but not near the water's edge. Unfortunately, l was unable to ob tain

coptes of Rusak's photographs, so l have provided my photograph of this image (figure

3.20).

Figure 3.20: Part of DjKn-1, July 2001.

Dewdney recorded and examined the following two sites ln August 1964.

Pastershank challenged his subdivisions in 1989. Both sites are close to each other, but differ

in terms of size, and in what has occurred since Dewdney first, then Pastershank, examined

them.

DgKl-1:

The water below this site is shallow, and the site is partially protected from the main

channel by two of the three small, neighbouring islands. It lies on a south facing spit of land

on the main travel channel, between red marker S56 and S60 at the northern end of

Sabaskong Bay. Dewdney identified two groups of images which he called Face l and II of

Site # 197 (figure 3.21).

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/lit orm d' 5a&/$konq i3aq, Cqk~ orthe Wood~

Sd!(~ #('/7 uod#198

"<" ... :, '!.i.... r'"

-. ~1 q~~~~~~~~~.'~~'~_~'~_~~" __ ' __ ~_~A_

'\ CMfUSTOPHIft lIlWf)NW

Figure 3.21: Dewdney's 1964 field drawing of Site # 197 (DgK1-1) and # 198 (DgK1-2).

Pastershank in 1989 (1989: 51) contradicted his method of subdividing the images. She

found images on a surface to the left of his Face 1 and, hence, renamed his Face 1 as her Face

II and his Face II as her Face III. The 'new' images to the left of her Face II were cal1ed Face

1. The site was clearly subdivided as indicated in the photograph in figure 3.22, into three

parts, cal1ed Faces, based upon the physical structure of the cliff face.

Figure 3.22: Photograph of DgK1-1 in July 2001 with Pastershank's 1989 subdivisions.

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DgKl-2:

Pastershank disagreed with Dewdney's subdivision of DgKl-2 when she recorded it.

Her divisions, unlike Dewdney's of 1964, did not depend on the identification of specifie

images, which she termed motifs, of DgKl-2.

Figure 3.23: DgKl-2 in 1989 hy Pastershank.

DgKl-2 is the larger of the two sites that Dewdney examined. The decisions

Pastershank made in subdividing it in 1989, when she recorded the site again with her crew,

are harder to understand and replicate than with DgKl-1. Dewdney recorded the part of

DgKl-2 called Face 1 by Pastershank in 1964, but since then the number of paintings present

at this site had increased in number. The image in figure 3.24 is the image that Dewdney

recorded at DgI<J-1 although it was published 90 degrees counter clockwise in Dewdney's

1962 publication with Kidd.

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Sabaskong Bay, Site #198

Figure 3.24: Dewdney's published images from this site.

l also discovered four additional and obviously new images at DgKl-2 in 2001 (figure

3.25). The presence of these images reflects the issue that Pastershank's subdivisions of the

site may have affected her description of the site. Therefore, it was important to replicate

Pastershank's subdivisions of DgKl-2.

Figure 3.25: Three of the four new images at DgK1-2 in July 2001.

Unfortunately, almost ail the images Pastershank identified, except for two

recognisable handprints and sorne parallel lines, were very pale and next to impossible to

distinguish. The disappearance or fading of the images recorded by Pastershank in 1989

could be a consequence of the exfoliation of the images, possibly in conjunction with the

deposition of mineraIs. Mineral deposition often causes a white deposit to form on images

painted using ochre.

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The new paintings found in 2001, in figure 3.25 above, were produced using modern

paint instead of ochre. The new paintings including an type of creature, a six pointed star and

a vertical crescent with its points facing right, were both superimposed on older paintings

and painted directly on the rock surface beside paintings Pastershank (1989:54-63) had

described, recorded, and photographed. The fourth new image was created not on any of the

designated "Faces" but was placed beside the area called a "site" by Pastershank. This image

is radically different from any of the new images since it is hollow rather than solid. Large

quantities of offerings also were discovered in the 2001 field season. .

Figure 3.26: The new image at DgKl-2 not painted upon the older ochre images in July 2001.

Pastershank (1989) designated Face I as being at right angles to the rest of the site on

the right hand side of figure 3.27. The large overhang was divided into Faces V, VI, and VII.

The rock underneath the overhang was divided into Faces II, III, and IV.

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Figure 3.27: Annotation by Coison in 2004 of DgKl-2 taken by Pastershank in 1989.

Face 1, first recorded by Dewdney in 1964, is relatively easy to relocate from its clear

images and Pastershank's published field recording in figure 3.28 below.

Figure 3.28: Field recording of detail of Face l, DgKl-2, by Pastershank in 1989.

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Figure 3.29: Photograph of Face 1 by Pastershank in 1989.

However, the remaining Faces are not allocated to the surface of the rock in a way

that can be identified easily, since Pastershank described their location on the rock surface in

relation to specifie morphs that she identified. Unfortunately, by 2001, these morphs were no

longer recognisable. Consequendy, it was difficult to determine the precise location of each

Face. Her published report designated Face II as the area of rock underneath the overhang

where she observed "an overpowering red ochre smear" (ibid.: 55). The image below is her

field recording of Face II (ibid.: 57). Pastershank argued that, when she recorded this "Face",

the clearest morph was a "zoomorphic bird (Morph 4)" found at the bottom corner on the

north side of the panel (ibid.).

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~ ...

Figure 3.30: Annotation by Colson in 2004 ofphotograph of Face II by Pastershank in 1989.

Figure 3.31: Field drawing with detail of Morph 4 at DgK1-2 by Pastershank in 1989.

Unfortunately, by 2001 this morph, which she called a "thunderbird," was not as

bright or distinct as Pastershank had described it. Consequendy, it was difficult to establish

its precise location. Pastershank argued that the base of this bird image, was "in sorne danger,

as it is sitting on the top of the middle of the roof-laminating caverns" shown in figure 3.31.

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The bird image she is concerned with is the arca of concentrated dots in figure 3.31. She

asserted that distinct handprints, called Morphs 5, 6, 8, and 10, were also on Face II. Three

"finger strokes" were recorded as existing in the central area of the red ochre smear cailed

Morph 7 (ibid.: 59). Pastershank found fresh tobacco left as an offering, in a smail crack

fifty-three centimetres below Morph 10. She stated that trus part of the site suffered from the

largest quantity of rock spalling. There was crumbling over the whole site and smail colonies

of lichen were growing there. She argued that mineraI seepage was evident both above and at

the sides of the red smear and throughout the he ad of the bird morph (Morph 4).

10cm

+ 1m22ahw 2m30aw.

Figure 3.32: Field recording of detail of Face III by Pastershank in 1989.

Pastershank maintained that Face III was located twenty-eight centimetres left of

Morph 10, and forty-seven centimetres below it (see figure 3.32). The only recognisable

morph on trus Face was a "possible hand print" called Morph 11 (ibid.: 59). However, by

2001 it was difficult to identify the morphs that Pastershank had used in 1989 to subdivide

the site. Pastershank (ibid.) located Face IV farther south, i.e. below ail of the Faces that she

had already designated as protected by the roof of the shelter from any "weathering agents."

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10cm

Figure 3.33: Field recording of Face IV of DgK1-2 by Pastershank in 1989.

Several morphs were identified, including the outline of an image she described as an

"upside-down man with his elbow bent on the right as if to place one's hand on this rup"

(ibid.) (figures 3.33 and 3.34). She maintained that the depiction of trus image was indicative

of "its importance and possibly predicts the death of some-one prestigious" but,

unfortunately, did not provide any evidence to substantiate her conclusion. Pastershank

identified another morph, a smear that apparendy measured "the size of a handprint" to the

left of the upside down stick figure. She identified nine handprints as existing at trus site and

maintained (ibid.: 63), as Lambert (1985:123-125) had done, that the hand was "an indicator

of death of a warrior." She argued that farther left of trus smear was a similar sized but

"indistinguishable" smear of red ochre. Pastershank photographed the same part of the site

where Morph 12 was found. However, by 2001 this morph was no longer distinguishable.

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Figure 3.34: DgKl-2, Detail of Face IV by Pastershank in 1989.

Faces V, VI, VII were stated to exist on the overhang created by the rock shelter.

These faces were contiguous and the morphs were adjacent to each other on the curved

overhang. According to Pastershank, Faces V and VI had one hand print each, called

Morphs 14 and 15 respectively, while Face VII had a horizontal undulating red line

measuring twenty-seven centimetres, called Morph 16 (ibid.) (figure 3.35).

Figure 3.35: Pastershank's Field recordings of Faces V, VI, and VII in 1989.

Pastershank observed that ail three faces suffered from mineraI deposition which she

argued was indicative of heavy water leaching that was caused by precipitation and lichen

growing above the red images.

It was difficult to utilise the arbitrary framework that Pastershank used to divide

DgI<1-2 into manageable units. Pastershank's subdivisions superimposed on the photographs

in figure 3.36 do not foilow the physical structure of the rock but depend on the

identification of specific morphs. Furthermore, problems exist for subsequent archaeologists

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Slnce the images fade and decay. The deterioration of the morphs underneath the rock

shelter made it impossible to identify the precise boundaries between Faces II, III, and IV.

Figure 3.36: Using Pastershank's (1989) subdivisions of rock surface to divide the paintings in 2001 into Faces V, VI, and VII.

Some of the difficulties in establishing the precise location of Pastershank's morphs

may be the results of the techniques by which they were reproduced for the final

archaeological report. The published field recordings are the final product of the whole

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~ .. 1

process to which the field recordings were subjected, once they had been taken to the

archaeological laboratory. The field copies of the sites were subsequendy traced onto acid

free albene paper in the laboratory. The field copies were reduced considerably in size using a

process called photo-mechanical transfer, so that they could be readily published using 8.5 x

11 inch paper. Therefore, it is possible that tiny details, which enabled Pastershank to readily

identify morphs, became difficult to determine.

Pastershank interpreted DgKl-2 as follows:

The environmental setting and the extensive ochre red paintings have made this site overpowering. Death may be the subject of Face IV as seen in the form of an upside down man, positioned over the third cavern, perhaps the death of an important person. A total of nine handprints were recorded at this pictograph site. The interpretation of the hand being an indicator of death may be valid (Lambert 1985: 123-125). To make this site even more spectacular is the placement of the powerful spiritual figure, the Thunderbird, over the middle cavern.

Pastershank (1989: 63)

Pastershank clearly considered the location of the images in this cavern-like setting as highly

significant. Her naming this site "Three Caverns Pictograph Site" (ibid.: 54) seems to reflect

this fa ct. Yet, only two caverns existed at this site since the second "entrance" is in reality a

hole in the wall of the larger of the two caverns. Pastershank (ibid.: 70) identified this site,

and the three other sites in Sabaskong Bay, as "tentatively called 'Boreal Forest' Aigonkian."

She argued that they were dated circa 1600, which she maintained was "characteristic" of the

majority of the rock image sites in the Lake of the Woods. This is an interesting conclusion

but she does not provide any evidence to support it.

DgKl-17:

Pastershank recorded the site in 1989 and subdivided it into three parts designated

Faces l, II, and III. Face l did not exist nearby Face II and III, which are beside each other.

Pastershank (1989: 63) described Faces II and III as "approximately seven metres away from

the eastern start of the bedrock cliff and Face l is an additional 5.4 metres away just from a

southward bend." She stated that the images at this site occurred in two "components"

(ibid.: 67). The first group, or component, if her word is used, are in the photograph below

in figure 3.37.

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Figure 3.37: Face 1 of DgK1-17 by Pastershank in 1989.

The images in this part of the site are quite faint, although she described them in

sorne detail. She asserted that this part of the site had "paired horned anthropomorphs, and

one hand print" (ibid.). Pastershank divided the images of her second component at this site

into two parts which she called Face II and Face III, although they are immediately beside

each other. Unfortunately, a photograph does not exist of this part of the site, nevertheless

her field recording in figure 3.38 provides sorne indication of the images present in

Pastershank's Face II and Face III.

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Figure 3.38: DgK1-17 - Pastershank's Face II and II in 1989.

No-one recorded this site between 1989 and 2001.

DgK1-19:

Pastershank (ibid.: 67) described this site as "only 18 metres west of DgKI-17" but,

because the images had "different styles, elevations, and hues of pigmentation," this site was

"not contemporaneous" with DgKl-17. She (ibid.) asserted that this site could be divided

into two smal1er parts since sorne of the images existed on a "perpendicular, south-facing

hiatus ofbedrock," as shown in the field recording in figure 3.39.

!il!' (,

Figure 3.39: Pastershank divided this Face into two parts called Panel i and ii in 1989.

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. ,r-

DhKm-5:

It appears that this site was considered as a single entity and not subdivided into

several parts by any of the archaeologists who recorded it including Dewdney in 1960, Reid

in 1975, Molyneaux in 1975 and 1979, Pelshea in 1978, and Lambert in 1985.

Figure 3.40: DhKm-5 in June 2001.

However, when l visited this site in the 1991 with Rusak, an archaeologist who at the

time was conducting fieldwork in the White Otter Lake/Turtle River system (1992a), she

pointed out that DhKm-5, in figure 3.40, consisted of not only the rock face recorded by

Dewdney and his subsequent colleagues, but an additional part in figure 3.41 that existed to

the left of the rock surface that was already termed DhKm-5 .

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Figure 3.41: The new part of DhKm-5.

Clearly, if a site could be subdivided into smailer units, faces and panels it could also

be increased.

b) Terminology

Pastershank's (1989) identification of specific morphs at DgI(J-2 inadvertendy

caused her descriptions to become blurred with low-Ievel interpretations. Identifying the

images was a crucial part of Pastershank's description of the sites and her subdivisions

enabled her description of each site to have a structure and become manageable. The

boundaries for each Face were dependant on her ability to recognise specific images that she

labeiled as morphs. Yet, by 2001 many of the images that she had described in 1989 were

impossible to identify.

The vocabulary used to describe the images of pictograph sites is important, since it

enables the archaeologist to classify the images, and to create an inventory of ail the images

at each site. The vocabulary used to describe each image influences how it is examined, both

as a separate entity and within a group. The words used to describe an image can and do

influence how the shape and ultimately the style is considered. Archaeologists are interested

in style because different modes of depiction are often equated with different ethnic groups,

while similarities are interpreted as evidence of those interactions.

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Pastershank's (1989) classification of all of the readily identifiable morphs on each

Face enabled her ta group them by type, and by whether they were hollow or not. In doing

this, she followed the technique of analysing these ochre images advocated by Dewdney

(Dewdney and Kidd 1962, 1967), Vastokas and Vastokas (1973), Lambert (1983, 1985 and

n.d.) and Rajnovich (1980b, 1980c, 1980d, 1981a, 1989, and 1994). Pastershank (1989: 70),

who was trained by Rajnovich, determined in her archaeological survey of four pictograph

sites in Sabaskong Bay that 76 identifiable morphs were found on 15 Faces. DgKI-1 had 26

of ail of the identifiable morphs found at these four sites, while DgKI-2 had 17, DgKI-17 had

30, and DgKI-19 had 3 morphs. Unfortunately, she did not describe the shapes of these

images. The names she gave to different morphs were also problematic.

Pastershank's verbal descriptions of each type of morph cause problems because they

imply meaning to the reader according to their physical shape. As Dewdney (1979b) had

noted earlier, this problem was widespread amongst archaeologists and others interested in

these images. He observed that numerous difficulties ensued when archaeologists described

visual images verbaily and admitted that his own work suffered from these flaws and

problems (1979b: 326). In one case, he had argued that at over half the sites he had recorded

images that bore:

no recognizable likeness to any known form and l designate them as abstractions. Many of them are single strokes occurring in groups or series that suggest tally marks. The remainder range from simple to relatively complex forms.

The other half of the symbols subdivided roughly into five groups: miscellaneous man-made objects, hand-prints, other human subject matter, animaIs, and composite-presumably mythological-creatures.

Dewdney and Kidd (1967: 18)

Dewdney (1979b) realised that verbal descriptions of images were prone to subjective

variation (ibid.: 326-328). He (ibid.) subsequently suggested that a series of graphic and visual

models could provide the level of rigour needed to classify images because words were

insufficient. Dewdney argued, drawing upon a number of examples from the literature on

rock image sites from both the Canadian Shield and elsewhere in North America, that he and

his colleagues had been careless "in assigning captions to our illustrations" (ibid.: 330) in the

publications of their research on rock image sites.

He (ibid.: 333-336) also questioned the manner ln which his coileagues had

reproduced rock image sites. He harshly criticised the practice of examining these images one

at a time, often extracting a single image and connecting it with similar images from another

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~ ..

group. He insisted that images which formed a group should be examined in conjunction

with each other as weil as in relation to their original location, and that a site must be studied

in relation to its local environment. Not doing so was the equivalent of treating sites and

images at "the level of an artifact picked up in a ploughed field."

Unfortunately, Dewdney's (1979b) hopes were not realised quickly. Sorne

archaeologists conducting field surveys in the Boreal Forest have continued to define the

images at rock image sites over-narrowly. For example, Haywood (1983) wrote that thirty

pictograph sites depicting "moose, caribou, deer, heron, human figures, canoes, handprints

and abstract symbols" (ibid. 17) existed in Quetico Provincial Park. He was concerned with

describing to someone who was not visiting each site what the images resembled. ]. Conway

(1979: 19-32) labeiled a range of images at several sites she recorded in northern Ontario as

including: "thunderbird," "abstract paintings," "beetle," "turtle man," "taily marks," "human

figure," and "fish." Both the perception and value judgements of the archaeologist have

affected the description of these images. Dewdney (1979b: 336-337) concluded that those

concerned with rock image sites should develop new recording standards independent from

the conventional methods of attributing meaning to images.

(c) The development of the techniques used to record the images

The development of how the images were recorded commenced with Dewdney in

the 1950s (Dewdney and Kidd 1962). After he had sketched the images, Dewdney measured

the distances between the physical places on the rock surface where the images existed and

designated them as individual parts using Roman numerals (1962: 8-9). He took colour

photographs, and recorded the compass bearing of the site, the depth of the water nearby,

and the height of the cliff (ibid.: 8-9). At first, a three-inch grid was lightly chalked on to the

rock to ensure an accurate scale copy of the images at each site (ibid.). He washed the chalk

off afterward. This grid enabled Dewdney to determine the location of a key point on a rock

face. The distances to key points in a painting were measured from string co-ordinates across

the rock face. The use of thin ]apanese rice paper employed for block printing, which

became transparent when it was wet, soon superseded this technique, as visible in the

photograph below.

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Figure 3.42: Dewdney working with a colleague on an improvised platform at Site #108.

Sometimes Dewdney built physical structures beside the site to enable him to record

them. The photograph in figure 3.42 demonstrates that Dewdney used a log probably

attached by rope to a tree growing above the cliff face at DhKo-1. Two rectangular shaped

grey areas exist beside and in the middle of the images. The one in the middle of the

paintings immediately in front of the standing individual is probably rice paper. The nature

of the second rectangular shape is unknown and appears perhaps to have been applied to

coyer something up.

Dewdney used a sponge roller to wet the paper, which also caused it to adhere to the

rock surface. The images below and visible through the paper were subsequently recorded on

the rice paper using Conté chalk allowing him to record all but the faintest of images.

Dewdney also made notes directly on the paper regarding cracks and the height of the

images above the water level. This development permitted Dewdney to reduce the time

taken in recording these images. However, as Dewdney noticed, the rice paper both

obscured the recorder's view of the fainter images and lighter details of the stronger coloured

motifs, especially if the stronger images were superimposed on larger, fainter images.

Dewdney's site numbering sequence reflected the order in which he recorded the site rather

than anything else. He argued that, as he recorded, his accuracy increased "due to practice"

(ibid.: 9).

Pelshea (1979: 24) expanded the range of colours used so that red recorded ochre

and green was used for lichen, frost spalls, and rock level changes. He also started to replace

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or substitute the Conté chalk with Dixon Lumber crayons since they did not cause the wet

rice paper to tear.

Jones (1968: 110) believed that the images should be outlined using felt pens, rather

than duplicated using a method called "the solid-line technique." The latter resulted in the

"character and the distinctiveness" of rock images in different geographical regions being

omitted. According to Jones (ibid.: 110), solid-line recording was the most common and

widespread technique for recording pictographs. It was no t, however, a good method for

"conveying actual appearance of painted symbols, and, as importantly, the char acter (his italics]

and distinctiveness of the rock art of a particular area." Jones was concerned that key aspects

of the images of different regions were being ignored and simplified, since that made "the

symbols more subject to gratuitous classification" and "interpretation." He subsequently

advocated that the best alternative was to record every aspect of these "symbols and their

settings that set them off from other styles" (ibid.: 111). Evidently, according to Jones a

recording technique had to render any distinctions in the style of the images evident in the

field recordings.

According to Jones (ibid.), Dewdney initiated the method of recording whereby the

edges of images were outlined. Jones either crosshatched or shaded the interiors of the

images to indicate gaps in the pigments of faded areas. Pictographs were recorded on

transparent plastic using different coloured pens to differentiate between the pictographs and

lichen encroachment and damage to the rock surface. Jones advocated that notes should be

made on the plastic where spalling, differential fading of the images, and unusual features

existed. Later in the laboratory, a stencil copy was made of this field recording using a light

celluloid paper and inking equipment. The resulting image was checked against photographs

so that the colours could be verified, ensuring a good reproduction of the original image. The

technique of Jones' recording as many precise details of these images as possible likely led to

the development of the dot-for-dot technique.

Questions regarding image reproduction had already been raised in the minds of

several archaeologists. Since Dewdney was aware that rice paper prevented faint paintings

from being discerned, he quickly adopted Jones' (1968) and Pohorecky's (1968) refinement

of the technique, using Saran Wrap (thin clear clinging plastic usually used for wrapping le ft­

over food) that was electrified with a brush, and grease or felt pens for tracing the images. It

is possible that Pohorecky (1968) advocated Saran Wrap because of its tendencies to stick or

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"ding" to surfaces. This new recording technique did not obscure the images, enabling

recorders to salvage faint images invisible under the wet rice paper. The water required to

adhere the rice paper to the rock surface possibly also reduced future visibility of the

pictographs, since it left mineraI deposits on the surface of the site. However, Steinbring and

Elias (1968a) questioned Dewdney's rapid adoption of this technique. They argued that,

sometimes, it was difficult to record a site using Saran Wrap, and that, in these instances,

field researchers should record the images using metre grids. The representational advantage

of the dot-for-dot recording technique is evident, given that a number of researchers on

pictograph sites in Northwestern Ontario (see C. Halverson 1988; Lambert 1983, 1985, n. d;

Rusak 1992a), including Pastershank (1989) used it for several decades. EssentiaIly each dot

of ochre visible on the rock surface was recorded by a dot, using a red felt tip pen, upon

clear plastic that was held by sticky tape to the rock face. Lambert (n.d.: 20) asserted that this

technique enabled the "duplication of the cultural, as weIl as the equaIly important non­

cultural information." He argued that recording both the ochre and the colour-coded "linear

and areal symbolics" conveyed "contextual associations for both types of information." This

type of record, he asserted, enabled archaeologists to provide more detailed tmage

descriptions and analyses of specific paintings. Lambert (ibid.) argued that the plastic

recording was a good idea and, since it used a 1:1 ratio, rendered "an almost exact, complete

reproduction." He maintained that this record was important for preservation purposes

because the pictographs that he examined suffered from erosion.

However, changes in pigment could not be replicated easily using the dot-for-dot

technique. Superimposed images were recorded with dots positioned close to each other if

they were dark, or, if the ochre was faint, relatively far apart. The relative distancing and

spacing of the dots appears to have been at the discretion of the recorder. Rusak advocated

that the 2 millimetre thick plastic be cut to size, and fastened to the rock face with tape.

Whatever was visible below Rusak reproduced immediately above it on the plastic using

waterproof felt-tip pens (Rusak 1992a). Rusak, as weIl as Lambert, did not use Saran Wrap

but did not inform the reader why it was not used. Red denoted ochre and blue, minerai

precipitation and patination. Any organic matter, such as lichen, rock tripe and moss

encroachment, was recorded using a green felt tip pen, while a black felt tip pen recorded

cracks and fissures on the rock surface (ibid) (figure 3.43). Pohorecky and Jones (1966: 104)

coded their felt tip pens according to colours on the MunseIl soil colour chart.

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Figure 3.43: The plastic being taped to the surface of the cliff face and the mineraI precipitation and patination being recorded by a black pen by Rusak in 1991.

Pastershank did not darify which colours were used to denote which features for recording

the pictograph sites in Sabaskong Bay, Lake of the Woods, but it appears from her 1989

report that she used the dot-for-dot recording technique. It is probable that Pastershank

(1989) used the same colours as Rusak (1992a), because Pastershank trained Rusak as a crew

member for the archaeological survey during which the four pictographs sites in Sabaskong

Bay were recorded. Field recordings, created using this technique, were once again traced

onto acid free albene paper in the laboratory and reduced in size considerably so that they

could readily be printed on 8.5 x 11 inch paper by a process called photo-mechanical transfer

(Rusak 1992a: 23).

This process of physically recording these images is problematic despite Pohorecky

and Jones's (1966) daim that this technique required "no artistic skill" and allowed relatively

few opportunities for the recorder to make mistakes. Both the field recording process and

the creation of a duplicate in a laboratory are laborious. Mistakes can accur if the recorder or

a copier is a novice, since the image produced could reflect the impression of the images in

their minds rather than being an accurate reproduction of the images. The recording of faint

and superimposed images is an especially difficult and possibly subjective activity.

Superimposition of images occurs when images are painted one top of another at different

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times and consequendy the colour of the image varies in intensity. During the intervals

between repainting, these images could have faded, weathered, or become partially covered

in lichen, rock tripe, or mineraI deposits. Photography provides a detailed record of the

images themselves. Dewdney (Dewdney and Kidd 1962:8-9) took colour photographs of the

sites he described. Only Molyneaux (1979) considered the use of the photographie record as

the sole means of documenting the pictograph sites of the Lake of the Woods. Others

continued to use black and white and colour photographs and slides as additional means of

recording the images (see Pastershank 1989 and Reid 1975). Still other researchers working

on sites elsewhere in the Canadian Shield maintained that photography was too problematic

because photographs were often "distorted" as a consequence of "many factors". They did

not list these factors, other than to state that one of them was the distance of the camera

from the site. It was for these unstated reasons that Pohorecky and Jones considered detailed

field recordings and tracing of the images more important than photographs, whieh,

nevertheless, were important for checking details of the images in question. Pohorecky and

Jones (1967: 305) argued that photography "allowed too much artistic licence" and "too litde

accurate draughtsmanship."

Section 4: T echnical analysis

(a) Technical issues involved in recording and interpreting rock image sites

Sorne archaeologists have discussed the technical issues involved in recording and

interpreting pictographs and petroglyphs (Brand 1979; Chisholm 1982; Pelshea 1979;

Pohorecky and Jones 1966, 1967; Pohorecky 1981; Pufahl 1990; Steinbring and Elias 1968a).

Pufahl (1990) considered that computer enhancement of the images from the Eagle Lake

area was a good idea because he had been forbidden, by the EIders and the Chief of the

Eagle Lake Reserve nearby to touch or trace the images at each local rock image site. Yet

Pufahl was aware that both the EIders and the Chief were concerned about the severe

physical deterioration of these sites because they were sacred to the local indigenous

community and "routinely receive[d] offerings of tobacco" (ibid. 19). Consequendy

photographs were the oilly means allowed by which these sites could be recorded.

Pufahl's initial efforts at using photography were thwarted because of slow shutter

speed, insufficient naturallight, and the need to take all the photographs from a boat. Pufahl

resolved to use polarizing filters with both his camera lens and the flash unit in conjunction

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with graphically enhancing the images on the computer. He proposed replacing those pixels

where the lichen had encroached upon red images with matching red ochres from the same

area (ibid.: 20). This meant that the image became completely visible instead of partially

obscured. He was aware that potential problems could occur if this process substantially

distorted these images. Pufahl was not only enhancing these images but also manipulating

them. In "replacing" the grey or non-red bits of images, he perhaps unconsciously changed

their shapes. Therefore his daim that his was a radical breakthrough technique for recording

images is slightly misleading.

(b) Conservation and analytical techniques

The concern of sorne researchers lay solely in the conservation of pictograph sites

(Tassé 1979); others desired to conserve petroglyph sites, particularly the petroglyphs in

Petroglyph Provincial Park in southern Ontario (Bahn, Bednarik and Steinbring 1996;

Wainwright, Sears and Michalski 1997). Molyneaux (1974) and a te am from the Department

of Anthropology at Trent University visited twelve pictograph sites in Northwestern Ontario

du ring the 1974 field season to document them and determine the general condition of each

site using "previously defined weathering variables" (ibid.: 1). The reader of this report is not

provided with any means of determining what these variables were, but they dearly were

important enough to warrant a detailed description of the sites for conservation and

protection purposes. Occasionally he described the images that he found at each of the sites.

Seven of the twelve pictograph sites covered in the 1974 study were in the Lake of the

Woods region. The team examined the following Lake of the Woods sites: DiKm-4, DhKm-

5, DhKm-4, DhKm-1, DhKn-1, DhKn-2, DhKo-1, DjKn-1, and DiKn-1. All of the sites

discussed were referenced using Selwyn Dewdney's numbers and their Borden numbers.

A year later, Molyneaux and his colleagues (1975) from the Canadian Conservation

Institute and the Department of Anthropology, Trent University, sought to document in

detail fifteen pictograph sites in the Canadian Shield in terms of physical conditions such as

moi sture access, seepage deposit formation, seepage deposit flaking, exfoliation, and

biological growth. They assessed each site to establish its physical condition with regard to

these criteria. Topographical maps illustrating site locations and scale drawings of the

pictographs were also recorded for each site. One site, DiKp-1, called Sunset Channel in

figure 3.44, in the Lake of the Woods was induded in this study.

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Figure 3.44: DiKp-1, Sunset Channel, 25th July 1975

The site DiKp-1 was assessed as follows:

The most significant factor affecting the condition of the site appears to be the heaving undercutting of the face by a fracture. The resulting instability will ultimately lead to the destruction of the site when the slab fractures away from the cliff face. Other weathering factors have a moderate effect, although a progressive decrease in pigment density appears to have occurred. The deterioration of the lower sections of the morphs 1 c and 1 e may be related to their proportional1y greater accessibility to wave splash and high water submersion.

(Molyneaux 1975: 4)

Other studies were concerned with the conservation of the paints used ln

pictographs, the conservation of pictograph sites in the Canadian Shield, and the different

ways of examining them (Myers and Taylor 1974; Taylor, Myers and Wainwright 1974, 1975;

Wainwright 1990, 1997; Wainwright and Taylor 1977).

Steinbring and Elias (1968a) advocated establishing the pH level of the mineraI

washes on the surface of pictographs to as certain whether the acidity of the soil above the

site affected the images below. They maintained that the acidity of the soil could affect the

visibility of the images.

Goods (1992) analysed the paint of one morph from the Rice River Pictograph Site in

Manitoba to determine the micrographical, elemental and mineralogical composition, the

constituents, and the paint binder. He discovered the presence of hematite, quartz, potassium

oxide, and aluminium oxide. He argued that organic matter was not detectable either in the

vehicle or the binder.

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Two additional studies were conducted to discover the composition of the paint, so

as to aid the conservation of the rock image sites in the Canadian Shield. Establishing the

nature of the paint aided conservation since the archaeologists would know what to expect in

the way of deterioration. The discovery of the paint recipes and the organic binders could

also have important consequences for archaeologists investigating pictographs world-wide

regarding their conservation, meaning, and the motives behind their creation. Archaeologists

involved in these experiments argued that the results demonstrated that the artists who

created these paints probably thought about what they were doing (Buisson et. al. 1989;

Clottes et. al. 1990a, 1990b; Clottes 1993; Couraud 1983, 1988; Leroi-Gourhan 1982:84-85;

Lorblanchet et. al. 1990; Menu and Walter 1991; Pepe et. al. 1991). An important implication

of these studies is how the results affect the procedures taken by conservators.

Taylor, Meyer, and Wainwright (1974: 32) wished to establish the causes of the

natural deterioration of pictograph sites in the Canadian Shield, prior to devising any

conservation treatments. Previous researchers had attributed the deterioration of these

paintings to physical and chemical weathering of the rock surfaces. Seven samples were

examined to determine the formation and the composition of the paint from the Agawa

pictograph site, on Lake Superior in Ontario, and a site on Lac Wapizonke, Quebec (ibid.).

Litcle information is provided as to the sampling strategy used and the size of the samples

removed. X-ray diffraction was used with a Debye-Scherrer camera equipped with a

Gandolfi attachment for single particle analysis. Cross-sectioned samples were examined

using a scanning-electron microscope equipped with an x-ray energy analyser under

magnifications of up to Xl0, 000 (ibid.: 33). The results of these experiments revealed that

the paint was anhydrous iron oxide. They observed that the pigment was "firmly attached to

and intimately mixed with the [white] mineraI deposit in a sandwich structure" instead of

adhering to the surface of the rock (ibid.: 40). The white deposit found on these cliffs coats

the images and provides a "protective coating from the leaching action of the rain and

erosion by wind" (ibid.) as well as preventing the pigment from dissolving away. Taylor and

his colleagues also argued that the graduaI accumulation of this white mineraI deposit on

pictographs led to "the faded appearance" of many of the images.

The authors noticed that two scatter patterns were evident within the samples. One

scatter pattern was identified as hematite and the other as calcium carbonate, a white mineraI

(ibid. 34). They argued that the scatter patterns indicated that the pigment was not direccly

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attached to the surface of the rock but was intimately mixed with calcium carbonate deposit,

on the rock's surface, in a sandwich-like structure (ibid. 40). The calcium carbonate deposit

consequently acted as a protective coating for the pigment against the leaching actions of the

rain and wind erosion. They asserted that these results eXplained why wet surface chemical

field tests conducted on the paintings failed to identify the hematite. The results also found

that the calcium carbonate prevented the pigment from dissolving away (ibid.). Taylor, Myers

and Wainwright asserted that the rate at which these mineraI deposits accumulated had to be

constant, but that it was impossible to establish this fact with certainty. They established

from microscopic analysis that although brighter red images often appear not to suffer from

white mineraI accumulations they still accumulated white mineraI deposits on their surface

because they were affected, although to a lesser extent, by groundwater seepage. Essentially

paintings on surfaces that are dryer suffer less from the accumulation of white mineraI

deposits than images that are continuously affected by groundwater seepage (ibid.: 40).

The information gained from examining these samples aided conservators ln

designing the methods by which pictographs might be conserved. The white mineraI deposit

on the surface of the images is a crucial component of the sites. Any efforts to conserve

these sites must take these results into consideration. The white deposit will accumulate

through time until it completely obscures the painting. The results also demonstrated that

exfoliation was not the principal cause of the deterioration at other sites.

This study subsequently prompted another examination of paint samples to

determine the structure of the pigments used in the pictographs of the Canadian Shield.

Wainwright and Taylor (1977:31) used scanning-electron microscopy to determine the

structure of the pigment of two samples. One was from a painting on Lac Wapizagonke,

Quebec, and the other from a painting on Mazinaw Lake in Ontario. Here again, information

is not provided concerning the sampling strategy and the size of the samples involved.

Analysis of cross-sections of the samples revealed distinct, almost parallel layers of pigment

(ibid.). Wainwright and Taylor posited that a chemical or a physical process separated the

original pigment into distinct layers and concluded that the pigment must have migrated

within the deposit because the samples were taken from images that appeared not to have

been repainted.

Both experiments demonstrate that conservators must undertake detailed studies of

the pigment prior to attempting to conserve rock paintings, especially in the Canadian Shield.

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Wainwright and Taylor's (1977) study demonstrated that pigment analysis revealed that a site

had been repainted or that the pigment may have migrated. However, these results must be

considered as preliminary, since only two samples were tested. Nevertheless, they

demonstrate that several layers of pigment may exist at pictograph sites which appeared to

have been painted only once.

Archaeologists were concerned to establish detailed information on the physical state

of the rock surface upon which these images existed, and technical information concerning

their physical composition and structure, that might be useful for the conservation,

preservation, and possible interpretation of the pictograph sites.

Section 5: Culture-Historical Approach

Archaeologists employ the culture-historical approach if they want to investigate the

shape, location, and date of the images with which that they are concerned. lndeed,

establishing the age of Shield rock images is central to the culture-historical approach and for

some rock image specialists establishing the styles of these images is a means by which the

age of an image can be determined (Grant 1967; Dewdney 1970c, Pettipas 1982; Pohorecky

1981; Rajnovich 1980b; Reid 1979; Rogers 1962; Steinbring 1977, 1979a, 1990, 1993;

Steinbring and Simpson 1986; Steinbring, Danziger and Callaghan 1987; Steinbring and

Callaghan 1985). Approximately half of these authors, with the exception of Grant (1967),

Rogers (1962), Rajnovich (1980b), and Dewdney (1970c) considered the petroglyph sites in

the Lake of the Woods.

Grant (1967: 145) considered the style of these images within this geographic region of

North America as "Northern Woodland" which "continued westward" into the prairies of

western Canada as far as the Columbia-Fraser Plateau (ibid.). He maintained that some

"simple abstract elements" existed but that they were subordinate to the naturalistic style

(ibid: 20) and that this style of painting was:

confined to the regions dominated by a nomadic hunting economy. The paintings are mainly simple, rather erude representations of men and animais. In sorne areas the drawings are done in red alone, though black and white were sometimes added.

(Grant 1967: 20)

Other images included: "men in canoes, moose, elk and buffalo," Ojibwa mythological

creatures such as the "water panther," and the "thunderbird," animaIs such as deer and

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mountain sheep, fish and buffalo, an abstract element which was a semicircle with rays, and

"human forms" of different types (ibid.). The pictographs were "painted (naturalistic)" (ibid:

20), while the petroglyphs existed on horizontal surfaces in Ontario and northern Minnesota

(ibid: 149) and had "crudely pecked animaIs, thunderbirds, and humans" which Grant

asserted were similar to those found at unnamed examples of petroglyph sites in southern

Minnesota. Much of his discussion in his chapter on the Northern Woodland rock image

sites reflects his consultation with Dewdney who was recording sites at the time that this

work was written and published. lndeed, he clearly stated in his acknowledgements (ibid.:

viii) that he could only have discussed the Canadian work after consulting with Dewdney,

who had been actively involved in surveying and recording sites in the Canadian Shield.

Grant clearly recognised a wide range of images. Unfortunately the vocabulary he used to

describe these images implies sorne meaning to the reader. He did not indicate the precise

technique he used to establish the identity of an image. Furthermore, he did not consider

local stylistic traits specifie to different regions in the Canadian Shield.

A site was deemed to exist if Dewdney recognised a clearly defined image existing

there. Dewdney obviously had thought careful1y about how to de scribe these images so that

they could be classified into groups. He classified images according to the categories in the

pie chart in figure 3.45 published in both editions of the book that he co-authored with Kidd

(Dewdney and Kidd 1962: 18, 1967: 18).

Figure 3.45: The table drawn by Dewdney to illustrate how he c1assified the images at these sites.

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~ ..

Unfortunately, Dewdney's description of these types of images inadvertedly implied their

meaning to either himself or to others. Dewdney probably classified the images using art

historical terms laden with Western cultural baggage such as "naturalism" in his 1962 and

1967 book with Kidd. This was probably because he had been trained as an artist and

illustrator. He stated (ibid.) that his own work suffered from these flaws and problems.

Dewdney (1979: 326) later realised that verbal descriptions of images were prone to

subjective variation and he argued that others were equally guilty of this problem. He

subsequendy suggested that a series of graphic and visual models could provide the level of

rigour needed to classify images because words were not sufficient.

When he commenced searching for pictographs, Dewdney felt that the presence of

red iron ochre on the rock surface was insufficient to designate a physical location in the

landscape as a site. Smears of ochre were "not shapes," from Dewdney's viewpoint in the

1962 publication with Kidd, since they were not recognisable symbols. Older images that had

decayed to the point of becorning amorphous shapes were also excluded as shapes. For

Dewdney, a shape must have a defined edge and be "recognisable."

Images such as blobs and smears, which could have been recognisable images blurred

by time, exfoliation, the accumulation of white mineraI deposits, and by the growth of rock

tripe and lichens, he ignored or left undescribed. Indeed, Dewdney (1975a:4) acknowledged

that he omitted the images that he considered "ambiguous" "when in doubt, leave it out."

Smears differ from blobs since they are usually not only larger than blobs but they could

have been placed on the rock's surface intentionally. Images could fade becoming blobs, but

if Dewdney's approach was used, places with only smears and blobs were not important and

not recorded.

Perhaps the lack of smears, washes, or shapes without clearly defined edges in his

field drawings reflects the fact that Dewdney did not consider these shapes as images. Faint

pale images probably would not be present on his field recordings using paint and rice paper

since the rice paper would probably obscure them when placed on top of them. Perhaps

Dewdney's perspective regarding smears stems from his training as an artist accustomed to

paintings and art objects created in the ]udeo-Christian perspective. However, the index of

his 1967 edition of his publication with Kidd indicates that "smearing of paint on rock" was

considered important since this term was included and it had not appeared in the index or in

the text of the previous publication (1967: 190). Indeed, Dewdney (ibid.: 107) wrote in the

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text of this edition that "the vague hints of frequent over painting suggest that this was a

long over-used site". The second edition of his publication with Kidd indicates that he had

changed his opinion as to the value of the smear as an image. Dewdney (1979: 326) later

realised that verbal descriptions of images were prone to subjective variation and he argued

that others were equally guilty of this problem.

Rajnovich (1981 b: 286) acknowledged areas of ochre as washes or smears. lndeed,

she argued that a style of image existed in the Canadian Shield region whereby the edge of

the image was painted first and the shape was subsequently filled in with an ochre wash.

Rusak (1992a: 124) observed that only two sites, DhJx-9 and DgJx-2, of the seventeen

pictograph sites that were examined during her 1991 field season in White Otter Lake

(twenty-seven sites are located in this lake) in 1991, did not possess an "ochre wash or

smear". She stated that

the location of washes and smears along prominent naturalledges, in small cubby holes, along noticeable cracks and crevices on the rock surface, indicates the ochre's intentional placement. It is therefore hypothesized that these washes and smears designate the suitable location to leave offerings for the powerful Manitous within [the rock].

(Rusak 1992a: 124) Smears and ochre washes were obviously important images for Rusak smce she

argued that their presence confirmed that these places were important in the world view of

the Aigonquian-speaking peoples. Rusak, like Pastershank (1989), viewed them as individual

images in themselves while Rajnovich (1981 b) perceived washes as a part of an image. Two

years after Reid, Pelshea in 1978, photographed and recorded the images of DiKm-4, DjKn-

1, and DhKm-3 in the Lake of the Woods. Unfortunately, it is impossible to determine what

he and Reid (1976, 1977) thought of the stylistic qualities of the images. Molyneaux (1979)

did not consider the stylistic aspects of the six pictograph sites that he considered. This is

because he (ibid.: 2) argued that "regional interpretations based upon the style typologies and

style areas and supported by ethnographie ethnologies are expedient but largely

indefensible." Rajnovich (1981 b) had discovered several styles of images from either her

involvement in or reading the results of a large number of field surveys in Northwestern

Ontario. lndeed, Dewdney (Dewdney and Kidd 1967: 176) had speculated that more than

one style of paintings existed in the Shield region and that only detailed studies would reveal

the regional styles.

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Rajnovich (1891 b: 286) maintained that four styles of images existed in Deer Lake:

"open or outlined morphs", "open or outlined morphs subsequently filled in with ochre

wash", "finger lined, or stock morphs" and "closed morphs". She argued that the lines of the

first style of image could signify "internaI organs," a stylistic feature frequently used by Cree

and Ojibwa artists during the twentieth century. She (ibid.: 286) claimed that the images at

the Deer Lake pictograph sites were "distinctive" since a large number of sites occurred in a

relatively small area with "the complete range of morph styles known to Shield rock art". She

(ibid.: 282) claimed that these sites were the sorne of most northerly sites to have been

discovered in Ontario.

Her system of classification of these images indicates that the images and the centres

of the images were not the same. Fortunately she provided a few examples of each style of

image so it is possible to compare the images she recorded with other examples elsewhere.

She reviewed work by her colleagues (Smith 1981 and Pelshea 1980) who also had conducted

research in the West Patricia district, and Dewdney, and concluded that geographical patterns

did not exist regarding the distribution of the morphs in northwestern Ontario. However,

she argued (1981 b: 286) that "open style morphs" were usually found north and south of an

imaginary line between the Lake of the Woods and Lake St. Joseph. She argued that the most

common style of image was the "open and closed style".

Rajnovich (ibid. 287) maintained that the images at Deer Lake were "abstract" rather

than "realistic" based on Dewdney's (Dewdney and Kidd 1967: 19) use of these terms. The

term 'abstract' was more appropriate because she argued that the creators of these images

were more concerned with their meaning rather than their physical shape.

It is interesting to observe that, although Pastershank (1989), Rusak (1992b), Smith

(1981), and Pelleck (1981) each recorded at least one pictograph site, none of them discussed

the possible style of the images.

Rajnovich (1980b and 1981 b) also considered the idea that images occurred in

groups. She observed that occasionally single images occurred at sites such as those in Deer

Lake (1981 b: 287), at the Pukamo Island, the Cuttle Lake, and the Jackfish Lake sites (1980b:

34). She inferred that the presence of repeatedly occurring images indicated that the

"pictograph artists did not perceive the Images as single, isolated figures but drew the

morphs within the framework of a "story"" (ibid.). The presence of a single shape image

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implied "an object, thought or character" whereas if two images of the same type were

present, then a relationship existed between the two shapes.

Conway (n.d. a. and n. d. b) considered three morphs, from various pictograph sites

in Northeastern Ontario, which occurred in conjunction with each other: an open armed

man, his canine companion, and an animal pelt. Another morph, which Conway identified as

a beaver, existed above the man and his animal companion. He identified these images as

specific star constellations. Rajnovich (1980b: 35) argued that Conway's (1978) identification

of Orion and Canis Major (see discussion page 199ff) at different sites across the Canadian

Shield was problematic. Bear images, she asserted, either occurred alone or in pairs as she

had observed in the pictograph sites of both Rainy Lake and Lake of the Woods. Pairs of

images also existed at Cuttle Lake (Rajnovich 1980d). She did not discuss canine images

although Conway had identified a canine image existing with a human figure.

She also observed that images described as a "canoe-with-passenger" motif existed

throughout the Canadian Shield but that two styles of this shape existed at Pukamo Island

and Jackfish Lake, two sites in the Rainy Lake region. She (ibid.) argued that the image from

the site on Pukamo Island had "stick" passengers while a similar image on the pictograph site

at Jackfish Lake, had "open armed passengers." Unfortunately Rajnovich did not provide any

photographs of either of the images under discussion. She (ibid.) posited that the differences

occurred since the passengers in the canoe were men in one canoe and Maymaygwayshi in

the other. Rajnovich (1980b: 35) maintained that the different style of canoe reflected either

different cultural affiliations of those drawing the se images or time periods in which the

images were drawn.

Rajnovich was clearly concerned with the style of the images in the Canadian Shield,

but she did not pay any attention to Dewdney's advice (Dewdney and Kidd 1967: 176) about

resolving the problem of dating pictograph sites. She asserted that a correlation existed

between Blackduck ceramics and images of hand prints in the Rainy River region. She

established that Blackduck ceramics were found in association with one pictograph site. This

information, in conjunction with information from her informant that sorne of the images

were created by the Midé, led Rajnovich to posit that these images dated to the Blackduck

period and provided a date for the origins of Midewiwin Society. Pastershank (1989: 71), like

Rajnovich (1980b: 35), observed that paired images could be important since pairs of images

were present at each of the pictograph sites she examined in Sabaskong Bay.

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At two pictograph sites where the images, he believed, conformed ta Grant's (1967)

designation of the Northern Woodland style, Pohorecky (1981) categorised and assigned to

different groups ail the images deemed to be human figures. However, he argued that the

standard categories of classification available for examining images could not be applied to

the "hum an figures" at both sites. Pohorecky did not indicate how he concluded that any of

the figures were human rather than supernatural. He (1981: 12) was principaily interested in

the "human" figures at the two sites on Smith Narrows between Hickson and Maribel1 Lakes

in northern Saskatchewan. He believed that these represented the northwestern tip of this

style, the epicentre of which occurred in Northwestern Ontario. Grant (1967: 147) had stated

that the large concentrations of pictographs had been described in Ontario, specificaily, in

the Lake of the Woods area. The criteria Pohorecky used were whether the figures had

upraised arms, arms hanging down, or one arm up and one arm down or whether the images

were hum an faces with no hands (1981: 13). He stated that the figures in the third category

had box-like shapes.

Lambert (n.d) examined DhKm-l, DhKm-4, DhKm-18, DhKm-5, DhKn-7, DhKn-

6, DjKn-l, and DjKn-2 during the field season of 1985. He applied a technique that he had

developed du ring his field survey of some pictograph sites in the Upper Severn region in

northwestern Ontario during the field season of 1982 (1983) for dealing with images. He first

subdivided images into twenty and, later, into thirty-five classes (n.d.) that he devised based

upon his own recognition and identification of each image. Therefore ail the images that he

classified as anthropomorphs he put in Class A; hand-prints in Class B, finger-prints in Class

C, canoes in Class D, pipes in Class E, crescents in Class F, taily-marks in Class G, arrows in

Class H, animaIs in Class l, struck animaIs in Class J, fish in Class F, birds in Class M,

lightening in Class N, turtles in Class 0, crosses in Class P, chevrons in Class Q, simple lines

in Class R, double lines in Class S, and unclassified images in Class T (1983: 113). Lambert

asserted that each image placed into each class ought to be examined "for its ability to

convey alternative meanings through differences in morphological attributes and associations

in the context of narratives" (ibid.: 111). Therefore images were placed into different but

larger groups. This grouping ailowed assignation of some level of meaning, according to

whether an image was identified as abstract, naturalistic, symbolic, or realistic. He believed

these terms "were normaily used to classify art and its elements" (ibid.: 110) and applied

them as defined by the Webster Third International Dictionary, published in 1976. Lambert

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(ibid.: 111) guessed at the meaning given to the image both by the creators of the images

themselves and the intended audiences.

The question of the authorship of these images remained for Lambert (1983: 1 09) an

unresolved issue. He assumed, however, that they were created by human beings rather than

foilowing "the contemporary belief' that they were created by the Maymaygwashi. He (ibid.:

110) acknowledged that the interpretation of these images was "a difficult process for those

who did not author them," due to the inherent problem whereby the observer, the researcher

needed to be as objective as possible to classify and describe the images for comparative

purposes.

The foilowing papers concern themselves with dating the images rather than with

style. Dewdney's (1970a) publication reveals his concern to resolve the dating problem for

paintings in the Canadian Shield. This paper had four parts, through which Dewdney

approached the resolucion of the problem. The first part discussed information concerning

the measurement of physical features, lichen, rock tripe and mineraI deposits to see whether

paintings from two different periods could be distinguished at the Hickson-Maribelli site in

northern Saskatchewan. Dewdney (ibid.: 8) argued that the site was in "traditional

Chipewayan territory" and had a "very impressive setting" (ibid.: 10) as weil as a deep crack

large enough to "hide a smail canoe." He examined the orientation of the rock surface; the

"protection of the site" (ibid.: 13), in which he considered the overhangs and cracks that

diverted the water seeping and drips from above; the height of the paintings above the

water, and whether rock benches existed at the base to prevent water splash from below. He

(ibid.) measured the level of lichen, mineraI deposits, and determined the "nature of the rock

surface," or type of rock, which he maintained affected the vulnerability of the paintings to

the weather. He argued that granite was more resistant to weathering than chIo rite schist. He

examined the colour and pigment impairment, the manner in which the paint was affected by

cime, but subsequently decided that the categories were too subjective. He concluded that he

could not measure variables objectively due to the difficulty in finding a variable that had

some significance as a dating device.

The second part of this paper presents conclusions that Dewdney obtained from

reviewing the world literature to see how other researchers throughout the world tackled the

question of dating rock image sites. He realised that the specialists from France, Spain, and

USSR had attempt to deal with the question of dating these images by excavating the area

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immediately adjacent ta the images themselves, a technique impossible in the Shield region

since images existed immediately beside water. Dewdney (ibid.: 14) maintained that offerings

could not provide any "stratigraphic issue" and they reflected a "cult" that could be of a

recent development. He argued that the water level mark could indicate something and that

analysis of the white mineraI deposit, which was calcareous, might be use fuI (ibid.: 15).

Through reading the world literature, he determined that examining the paintings for

superpository evidence was interesting, since this was common in Shield region. He asserted

that, where it was possible to establish which image had been superimposed, a sequence

could be established. He realised that, even if this technique was possible, too few examples

of this existed, such as on Face X of Site #181, and too few paintings showed what he called

"sufficient evidence of stylistic affinity with any other painting" (ibid.: 17).

Another method that could aid the dating of these images would be determining

stylistic sequences. Yet Dewdney argued that it was very difficult to define the style of a

painting, as evident from the literature from elsewhere in the world. His review of this body

of literature led Dewdney (ibid.: 18) to condude that relatively few numbers of images were

similar. He also (ibid.: 19) asserted that it was too early to discuss in any depth the

"complexities of sorting out style features" for the rock image sites of the Shield region.

Dewdney conduded that the "greatest common style denominator" of the images of the

Shield region was "their individuality". He argued that the use of "[L]aboratory techniques"

enabled the examination of pigment samples for their organic binder that caused the paint to

adhere to the rock surface. He (ibid.: 21) stated that considerable developments had occurred

using chromatography (e.g. Denniger 1971), spectroscopy of different types, and analysis

using scanning-electron microscopy. However, he identified the biggest problem as the

difficulty in obtaining a large enough sample to guarantee that most of the binding agent had

not disappeared. This he believed would cause researchers to scrape pigment samples from

an undetermined number of paintings.

Dewdney posited that patination, although it rarely occurred in the Shield region,

offered sorne hope of dating. Patination occurred, he argued, when the colour and texture of

the rock's surface changed when the surface broke away either as a consequence of

exfoliation or weathering (1970a: 23 -24). He asserted that oxidation of the pigment could

occur whereby the pigment became redder, oxidised as it was exposed to the sun. This is an

interesting idea, but Dewdney did not provide any evidence to substantiate this daim. He

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posited that lichenometry was a useful dating technique but he stated that more information

was required as to their growth rate and why lichen grew where it grew.

Dewdney reviewed the ethno-historic literature written by researchers elsewhere in

the world. He argued that by combining the information from informants, ethnohistoric

data, ethnographic data, and archaeological data that it might be possible to establish a secure

continuous cultural sequence. Therefore, according to Dewdney, it might be possible to

establish which images occurred when, especiaily given the depictions and/or impressions of

specific European innovations at seven sites in the Canadian Shield, such as flags on poles,

European forts, and guns. He maintained this, although he had discussed this topic earlier in

Dewdney and I<jdd (1967: 50), where he observed that several images represented as

European, by their painters, were very similar to those of buildings drawn by the Midé on

birch bark scroils.

The other key reference that Dewdney used as a means of dating was Schoolcraft's

information regarding the pktographs at Agawa rock image site on the north shore of Lake

Superior. Schoolcraft (1857: 405-411), Dewdney (1970a: 28) argued, "reliably" dated the site

as having been painted by Mygeangun, a shaman practitioner from the south shore, as

approximately 1800 given or taken twenty years. Dewdney asserted that prehistoric dues to

dating these images induded the recognition of objects such figures with objects such as

bows and arrows, and medicine bags.

Dewdney conduded from the world literature that rock image sites were not reliably

dated. He (ibid.: 30) posited that examining each site, its setting and its painting" in as mu ch

detail and as much precision as routinely employed in an archaeological excavation" afforded

the only method by which to date sites.

This paper's third section deals with his new approach, involving fieldwork to

develop a more intensive examination of the variables that caused or increased the "physical

impairment of the paint and rock substrate" at sites in Manitoba and Northwestern Ontario

(ibid.: 3). He (ibid.: 30) chose three pictograph sites that he argued "promised maximum

return for such detailed examination" namely: Agawa since its paintings were recent and

could be dated, as discussed above, a site on Frances Lake, and a site with an "early origin"

on Fishing Lake (ibid.:31). He (ibid.) argued that early sites should combine "evidence of

considerable paint impairment," "maximum of protection from weather," and "a

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combination of factors that were weather resistant," but did not state or clarify what he

meant by these statements.

Dewdney (ibid.) believed that the pictograph sites at Fishing and Frances Lakes

shared similar painting styles and context different to other sites in the Shield region, and

that both were "impressively protected from weathering." Why and how remains unclear. He

also (ibid.) argued that both sites showed "obvious impairment to suggest a substantial age."

He did not state what these impairments might have been. Dewdney's (ibid.: 36) subsequent

fieldwork had four objectives: (a) to review and extend the understanding of all the variables

involved in the "vulnerability and impairment of all paintings," (b) to record all the data that

could be useful for dating purposes, (c) "to test a variety of equipment and instruments and

the practicability of accurate recording," and (d) "to collect samples of both painting and

rock substrate for laboratory examination and analysis".

At each site, Dewdney (ibid.: 39) measured the quantity of moisture experienced

from three main sources: rainwater, groundwater and shore water. He argued that wind

driven rain still affected sites with an overhang or a bench at the base, because neither

physical feature protected the site. His experiments revealed that sites with a northerly

exposure, especially those that faced northeast, suffered most from wind driven rain. Those

cliff faces facing south, southeast, and east-southeast received the least amount of wind

driven rain. He calculated the maximum effect of direct sunlight available annually

experienced by a site to establish the temperature differences that occurred on a cliff face so

as to determine the possible rate of exfoliation.

Dewdney (ibid.: 40) estimated the quantity of ground water seepage because he

asserted that those physical features that may have protected the images from rain "ensured"

groundwater seepage. Dewdney observed that blank streaks on the surface of the rock face

indicated groundwater seepage while groundwater seepage was not constant if "tracks of

mineraI precipitates" were present on the rock surface. Unfortunately, the precise meaning of

the words "blank streak" remains unclear. He (ibid.: 40) devised the "time-of-wetness test"

using an instrument called a "splash test device," which he himself invented (1972: 1) so that

he (1970a: 40) could measure the elapsed time for a droplet to run down the surface and

evaporate.

He concluded that the largest physical affect of water on a painted surface and rock

substrate was frost action. Dewdney posited that perhaps thermographs could be set up near

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selected sites allowing information regarding the tempe ratures to be collected at each Face.

Results could be compared with maximum and minimum temperatures at the nearest

weather stations. This, he argued, might make it possible to assess the vulnerability of the

rock to frost action. He also argued that ice erosion was a possible problem for sites.

Dewdney (ibid.: 46) studied the lichen at Agawa, Frances, and Fishing Lakes to

establish the level of encroachment. He and his assistant recorded the dimensions of the

lichen thaluses. Dewdney also tried to establish the level of patination by comparing the

colour of the "mother rock" in a deep fracture. He stated that he was no longer a sceptic

concerning the colours of the pictographs, and argued that the colour of the pigment may

have changed according to the degree of impurity present or the extent of weathering. He

argued that it was possible that colour could increase because of the interaction between

solar radiation, moisture, and radiation. Unfortunately, it is unclear how much Dewdney

knew about the relationship between the solar radiation, moisture, and radiation.

Dewdney concluded that the problem of dating the pictographs in the Canadian

Shield could be resolved only by using what he termed a "three forked approach." Field-,

laboratory, and desk work were conducted simultaneously and considered equally important.

He argued that fieldwork included determining the importance of the pictograph sites to the

local indigenous peoples. Research ought to be conducted on petroglyph sites, sin ce he

believed that examination of these images could offer insights into pictograph sites. He

argued that future studies of these images must always include examination of the paint and

the rock itself, so samples must be removed for scientific analysis.

"Desk" research had three goals: (i) a stylistic analysis of the images supplemented by

an analysis of the images found on hide and birch bark scrolls; (ü) an examination of the

ethnohistoric literature for recent archaeological surveys and developments, analytical

techniques for field samples and comparative purposes; and, finally, (üi) to continue to

communicate with those colleagues also interested in the rock image sites of the Canadian

Shield.

There has been much controversy about the dating of rock image sites from the Lake

of the Woods area. Steinbring, an archaeologist from the University of Winnipeg, has

undertaken the largest number of studies of the petroglyph sites in the Lake of the Woods.

He argued that the pecked images of the petroglyph site called the Mud Portage Site (DkK.r-

4) on Clearwater Bay belonged to the Lake-of-the-Woods Style (Steinbring 1977). He

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described the site as containing ninety-four petroglyphs, twenty of which were found

through the excavation of up to one metre of archaeological deposits (ibid.: 139). The

images, or glyphs as Steinbring described them, were found upon "a grey-ish green [the

colour of the rock] basaltic formation which is essentially horizontal" (ibid.). Steinbring and

Callaghan (1985: 8-9) had observed that changes in the water levels had caused erosion of

these soils and started to expose the petroglyphs. They argued that, although this site had

been disturbed by rodent tunnelling and roots, the archaeological deposits were stratified,

and demonstrated a long continuum of intermittent occupations starting at 9,000 B.P., and

ending around the time of European contact in this region, which was postulated to have

occurred around 1732. Excavation at this site revealed more petroglyphs but these

archaeologists acknowledged that both radiometric and typological dating did not permit

clear projections of any artistic activity to before 7,000 B.P.

Steinbring and Callaghan knew that the highly acidic soils of the Shield region meant

that bone artefacts did not survive and hence one of the principal sources for radio carbon

dating was non-existent. Wood charcoal from levels 6 and 8 of the excavation provided dates

in the range of 2000-2500 B.P., which Steinbring asserted indicated the "substantial antiquity

for the deeper positions" (ibid.). Levels 8 to 12 of the excavation provided a large quantity of

archaeological objects which were deemed to be Archaic and to belong to the "Oxbow­

McKean" complex prevalent in this part of the sub-Arctic and dated to about 5000 B.P.

Steinbring argued that these layers covered the petroglyphs at several places throughout the

area. Beneath level 12, cultural materials existed that were not of "the usual type", that is, not

objects, lithics, that were readily identifiable as belonging to a known cultural type (ibid.).

Although Steinbring had discussed the style of the images in his (1977) publication, his later

publications do not clarify how an image can be classified by someone other than himself as

belonging to the "Lake-of-the-Woods-Style" (1979a: 13). Steinbring argued that images

belonged to the "Lake-of-the-Woods-Style" if they demonstrated something he termed a

"gross form" and if they were similar to an image depicted "in the nature of a classical art

style." Unfortunately, he is not clear as to what constitutes either "gross form" or "a classical

art style" (ibid.). Steinbring, likewise, did not elaborate on the difference between solidly

pecked and lightly pecked forms. He observed that "vague linear" forms, which remain

undefined, belonged to a different stylistic group and were evident at the peripheries of the

main panels of the Mud Portage Site (DkKr-4) and the Kennedy Island Site (DjKp-4). This

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style, as yet unnamed, was evident at two other nearby petroglyph sites in the northwestern

part of the Lake of the Woods, called the Dowse site, DrKr-2, and Macrun Point, DjKr-1

(ibid.: 16).

Steinbring concluded that those images classified as "Lake-of-the-Woods-Style" were

similar to those from the ]effers Petroglyph site in northern Minnesota, dated as Archaic in

age, since some of the images depicted copper projectile points and atl-atls. It is likely that in

doing so he drew upon his Ph.D. research on early Copper artefacts (Steinbring 1975). He

concluded that those images of "Lake-of-the-Woods-Style" belonged to the same time

period as those at the ]effers Petroglyph site, because the glyphs resembling bird tracks were

solidly pecked in both central and peripheral locations and consequently were not

"assignable" to either the pre-ceramic or ceramic horizons (ibid.). However, Steinbring did

not state precisely how sites could be subdivided into "central" and "peripheral" parts. It is

likely that he used rus own cultural perspective to deterrnine the identity of the images visible

on the rock surface. Description of these images is clearly intermixed with low-Ievel

interpretation and his approach to the classification of these images cannot be replicated.

It was his later work that established precisely how he found the images were

dateable, where specific styles were found, and how they were identified. Studies by

Steinbring and Nielson (1986) had established that some of the litruc materials came from a

quarry nearby, wruch was part of an early litruc complex associated with the rugh water levels

of glacial Lake Agassiz, at least 1,000 years before the initial occupation of Mud Portage,

DkKr-4. Steinbring posited that these early peoples had migrated to the present lakeshore

when glacial Lake Agassiz drained away and that their cultural materials were characterised

by unifaces and used platform flakes. This combination, Steinbring noted, was classified as

the earliest cultural remains in North America and was either termed the "Pre-Projectile

Point Stage" or "Early Litruc" (ibid.: 141). Steinbring argued that it was impossible to exclude

the idea that people who had lived in trus region during trus early time period had created the

petroglyphs. He argued that rus estimate of the date 7,000 BP "was conservative" and was

based on the presence of the materials from the Oxbow-McKean complex evident in Levels

8 to 12, which were at least three levels above the petroglyphs.

Once again Steinbring observed that the petroglyphs at trus site, DkKr-4, could be

conveniently divided into two styles based on their location (ibid.). The most prominent style

for Steinbring was the "Lake-of-the-Woods-Style" found on the crown of rock formations

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that he asserted "took advantage of the smoothest and most commanding locus". He argued,

based on these observations, that this was possibly the oldest style and that this conclusion

was confirmed by his excavation of the Mud Portage site. The images that belonged to this

style were "naturalistic and representational". Also belonging to this style were images that

were "highly eroded unclassified masses," which Steinbring argued could sometimes form

"solid iconic masses". Furthermore, Steinbring maintained that it was these masses that

linked the Lake-of-the-Woods-Style" to the "Clearwater-Bay-Style".

The second style of petroglyphs, the Clearwater Bay Style, in contrast, was found in

images created on the peripheral edges of the exposed rock surfaces and "virtuaily absent

from excavated surfaces" (ibid.). Only one example of a morph in this style existed beneath

the excavated layers of the site at Mud Portage, DkKr-4. Images belonging to this style were

linear and reflected iconic incongruence, since, invariably they were created using the glacial

striations that exist upon the surface of the rocks in this region. Steinbring maintained that

the striations were "exaggerated by pecking, and lines or curves were added". Linear bird-like

forms and insectiforms, such as a "dragonfly", were present in this style.

Steinbring (ibid.: 142- 143) conduded that both styles of images exist at the Mud

Portage Site, DkKr-4. He provided drawn examples, but did not provide photographs of

each style, so that others could observe precisely what he meant by each style, even though

he had argued that photographs are always more use fuI than drawings to a novice in this

aspect of archaeological research.

Steinbring and Cailaghan (1985: 3) contrasted the "Clearwater Bay Style", where

images were linear and outlined, with the "Lake-of-the-Woods Style" (ibid.: 2), where images

were "solid", because their centres were entirely pecked, and not outlined. Both authors were

clearly satisfied as to the pre-ceramic context for the "Lake-of-the-Woods Style" in

Northwestern Ontario, as weil as with the idea that the images at DkKr-4 were created over

a period of at least 5,000 years (ibid.).

Two years, later Steinbring, Danziger, and Cailaghan (1987: 3) dated the style of the

petroglyphs at the Clearwater Bay site, Lake of the Woods by the overlying archaeological

deposits in the soil mande immediately above the petroglyphs. The three archaeologists

reiterated a previous daim published by Steinbring and Cailaghan (1985) that the "Lake-of­

the-Woods-Style" dated to 9,000 B.P., using a radio carbon date based on one charcoal

sample taken from the archaeological deposit immediately above the petroglyphs at Mud

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Portage, DkKr-4. They speculated that these images, belonging to the "Lake-of-the-Woods­

Style" at Mud Portage, indicated "possible movements by mobile pre-Archaic populations

into the Canadian Shield" (ibid.: 9). However, this published date of 9,000 BP is not the

same as the result provided by the laboratory that dated this sample (BGS 1101, Brock

University Geological Society, Radiocarbon Laboratory, 1986). The laboratory report from

Brock University [Radio Geological Sciences Radiocarbon Laboratory] dated the sample

submitted by Steinbring and Callaghan and analysed by Melville on April 26th 1986 to 1,320

± 80 years.

Steinbring and his colleagues claimed, in print, that this sample was taken from soil

immediately above the petroglyphs but the diagram drawn on the form submitted to Brock

indicates it did not originate at, but above, the base of the soil horizon. If the sample was

taken from the base of the horizon, there should not have been any organic materials.

However Melville, the laboratory assistant who ran the test, wrote on the sheet that

accompanied the result of the test that were there numerous penetrating rootlets in the

sample to be tested and that he had removed as many as possible. Such an observation by

the scientist running the experiment suggests that perhaps the sample may have originated

from somewhere in the rootlet zone. Steinbring wrote in the section of the form that

required information concerning the "state of preservation, factors that may result in

anomalous age (present or past geological environment, sampling, storage, etc") that both

archaeologists speculated that the sample came from a feature such as a hearth, rather than

modern root burn. When asked for the "regional stratigraphie setting, geological or other

significance or probable age," Steinbring wrote that the sample in question was taken from a

deposit slightly below a deposit that had yielded a date of 2,550 ± 140 years.

Steinbring's (1993 and 1999) publications highlight the fact that he was determined to

use this "new" date of 9,000 BP, rather than the date obtained from the radiocarbon

laboratory at Brock, of 1,320 ± 80 years, since it confirmed his published hypothesis about

the se images in earlier works. Steinbring's (1993) publication argued that the images at DrKr-4

that were deemed to be of the "Lake-of-the-Woods-Style" were definitely Archaic in age.

Steinbring (1999) contended that the date for the petroglyphs at Mud Portage provided "a

base line for attempting a review of early rock art in the North American Mid-Continent."

Clearly, Steinbring wished to be the archaeologist who had discovered the oldest rock image

site in North America.

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Reid (1979), on the other hand, attempted to establish the age of several petroglyph

sites in the Lake of the Woods by relating the images there to those found on other

pictograph sites, and on the birch bark Massacre Scroll that related the murder of Father

Aulneau, the son of La V érendreye, and their companions. He disagreed with Steinbring's

attempts to date the images of DkKr-4 and discussed the newly discovered images from

DjKp-3, called Tranquil Channel, in conjunction with images from the other petroglyph sites

in the Lake of the Woods. He examined the relations among the different petroglyph sites,

and realised that three images were found at DiKo-2 (Sunset Channel), DkKr-4 (Mud

Portage), DjKp-4 (Kennedy Island), and DkKq-24 (Clearwater Bay): fertility symbols, stick

figures, and turtles. Reid (ibid.: 246) observed that none of these sites had images which were

deemed as "typically Archaic projectile points, or atl-atls", which Lothson (1976: 31) had

used to date the] effers Petroglyphs in Minnesota, but a number of similar animal and human

forms were present. He reasoned that the excavation of the Meek Site, DjKp-3, which had a

habitation site as well as petroglyphs, provided sufficient evidence for testing two

hypotheses: (a) that the majority of the rock image sites on the Lake of the Woods were

"temporally placed" in the Middle and Late Woodland period and were "a product" of the

Algonquian speaking peoples, and (b) that the petroglyphs at DjKp-3 (Tranquil Channel)

were created by the Cree during the tenth to the fifteen centuries AD.

Reid maintained that these petroglyphs indicated an Algonquian cultural affiliation of

these sites. Based on two radiocarbon samples, this archaeological site belonging to the

Selkirk culture was dated to 935 AD. and 1420 A D (ibid.: 252). Reid (ibid.: 253) reasoned

that majority of the Lake of the Woods sites were interrelated, based on their shared imagery.

He argued that the date from the habitation site supported his hypothesis that the Lake of

the Woods sites were relatively recent Algonquian ones, because the fertility images at

Tranquil Channel were connected to the nearby archaeological site.

If the ]effers Petroglyph site and DrKr-4 were connected, they belonged to "an

extremely long cultural" period and that the relationship between the petroglyph and

pictograph sites in the Lake of the Woods must be considered (Reid 1979: 247). He noted

that the Canadian sites shared similar animal and human forms with the American site. Reid

reasoned that several images at petroglyph sites DjKp-3, DiKp-2, DrKr-4, DiKp-4 and

DkKq-24, in the Lake of the Woods, could be identified as fertility symbols, stick figures,

and turtle shaped images. He concluded that, since the petroglyph sites in the Lake of the

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Woods shared the same images, they were probably connected to each other as weIl as to the

pictograph sites. Reid (ibid.: 247-250) asserted that the offerings left at DiKm-1, DhKm-1,

DiKp-1, DjKl-2, DkKn-7, DkKr-4, DhKm-3, and DhKo-1 were additional evidence of a

connection between the pictograph sites and DiKo-2, a petroglyph site. These offerings

were, for Reid, an indicator of religious importance and provided a sense of "the sacred" for

local indigenous communities.

One particular morph, the key factor for Reid (ibid.: 250), demonstrated a link

between these sites and the belief system of the Midé of the modern Ojibwa. This morph

was identified by Redsky, a Midé practitioner from Shoal Lake (part of the Lake of the

Woods) as a "paisq", which he roughly translated as a "bird of omen". This image was

identified at two of the petroglyph sites: DiKo-2 and DjKp-3, three times on the Massacre

birch bark scroIl in figure 3.46 and on an Ojibwa birch bark scroIl caIled a "migration chart"

held in the National Museum of Canada.

Figure 3.46: The Massacre Scroll photographed in 1993 by J. Rusak.

Reid (1979) has taken a different approach to dating the images of the petroglyph

sites since he did not rely on absolute dating techniques. He argued that none of the

petroglyph sites from the Lake of the Woods had shapes that resembled the images at the

]effers Petroglyph Site in Minnesota dated to the Archaic period. Steinbring and his

coIleagues (Steinbring and CaIlaghan 1985; Steinbring, Danziger and CaIlaghan 1987)

subsequently advanced an Archaic date for the Algonquian occupation and creation of

DkI<r-4 (Mud Portage), one of the sites that Reid had considered. They argued that DrI<r-4

was connected to the ]effers Petroglyph site since Archaic projectile points and atl-atls were

depicted at this site.

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Two articles debated about how a method might be developed so that images from

different sites could be related to each other. Whelan's (1983) study built upon the work of

Maurer and Whelan (1977). They sought to develop a method applicable to other forms of

"pictography within this region" (ibid.: 196), by which sites and paintings could be classified

and catalogued according to the subject matter of each image. Each image, termed data, was

placed into different levels: class, subclass, and attribute (ibid.).

Maurer and Whelan observed that problems existed in trying to conduct this type of

analysis since the descriptions of the images were invariably affected by the personal

interpretation of the observer. They discovered that difficulties existed in developing a

format that was relatively adaptable to a computer programme: how could an archaeologist

de termine and identify what constituted a class, a subclass, and their respective attributes,

and how could they identify specific symbol types and names (Maurer and Whelan 1977:

199).

Maurer and Whelan were determined to deal with the increasing quantity of data and

to clearly describe and classify these images without imposing meaning upon them during the

culture-historical approach. They understood the issues of unintentionally imposing meaning

to an image in the course of describing its attributes.

Section 6: Contextual approach:

This approach will be used, only after the application of the culture-historical

approach, to relate various types of empirical information to the site where the images were

found. It considers a broad set of associations and relations among the images themselves,

and between the images and their physical settings. This approach involves a search for

patterns relating different images, and combinations of images both between and within sites

Archaeologists inevitably describe the immediate physical landscape. Petroglyphs

exist on the surface of a rock while pictographs exist on rock surfaces either on rock walls or

in caves. It was traditionally believed that pictographs exist at the base of vertical granitic

rock walls, either immediately beside the water, or near the water's surface. Pohorecky (1968:

103) stated that:

the micro-environment of the rock paintings is easily categorised. The paintings occur either singly, or, more commonly, in small groupings on fiat, vertical and sloping rock faces or cliffs just above the surface of sorne body of water, and can be reached usually from sitting or standing position in a canoe, and sometimes by stepping onto ledges just back from the water. AlI paintings are visible from the vantage point of a canoe. This

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kind of setting, where paintings lie near the edge of the water in summer or ice in winter, is itself one of the most distinctive features of rock paintings throughout the entire area.

Yet, pictograph sites are not always found immediately near water. This statement is

supported by the pictograph site DhKn-1, first recorded by Dewdney as Site # 106 on 19th

August 1960 in figure 3.11. It is on the southwest facing shore of Aulneau Penin sula

immediately opposite Wisakode Island and north of Rabbit Island. It lies beside one of the

channels that can be used to enter Obaibikon Bay to the north. The paintings here can be

reached by standing on a narrow, long rock ledge immediately behind the large boulders and

the birch trees visible in figure 3.47. These boulders are a few metres from the water's edge,

where various grasses, trees, and short plants grow.

Figure 3.47: Part of DhKn-l beside Obabikon Channel.

Two studies from neighbouring regions exemplify the contextual approach because

the authors sought to ascertain how rock image sites were related to other features in their

vicinity (Noble 1968; Sweetman 1955). Noble described and discussed the pits, cairns, and

petroglyph sites found in close proximity to each other at Rock Lake, in Algonquin Park in

southern Ontario. He (ibid.: 63) contended that the rock cairns behind the rock lined pits

were not definitely connected with each other, although they were related in some manner.

The pits were interpreted as '''vision pits'" (ibid.: 62), while the cairns were interpreted, based

upon comparison with cairns at Red Sucker Point, on Lake Superior, as possibly being

""tobacco-drops", dedication cairns erected to a guardian spirit after a successful vision"

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(ibid.: 63). The petroglyphs were interpreted as being both archaeological and artistic in

nature and "of probable socio-religious import" (ibid.). He asserted that they were not as

complex, numerous, or detailed as those elsewhere in the Canadian Shield, discussed by

Sweetman (1955) and Dewdney and Kidd (1962). Noble also concluded that it was

impossible to infer the cultural affiliations of the people who used the pits.

Sweetman (1955) described how the images at the Peterborough Petroglyph site were

mapped and recorded. The images, called "glyphs" (ibid.: 101), were recorded using plaster

moulds, drawn, and photographed. Test pits were dug near the petroglyphs to establish

whether the people who had created the glyphs had left their tools nearby, or camped in its

vicinity while they created the images (ibid.: 101-104). Nothing but tree stumps or windfalls

were found in the test pits and these could not provide any information about the creation of

these images. An archaeological site of an Iroquoian village, which he called the Quakenbush

site was found nearby (ibid.: 104). Sweetman argued that it was unlikely that the inhabitants

of this village had created the petroglyphs, but he did not indicate why he arrived at this

conclusion. He (ibid.: 108) concluded that it was impossible to arrive at any clear conclusions

regarding the age and meaning of the images.

Arsenault and his colleagues have examined in considerable detail eight pictograph

sites in Quebec (Arsenault 1997; Arsenault, Gagnon, Martijn and Watchman 1995; Arsenault

and Gagnon 1998). Arsenault (1998) examined in considerable detai! the sacred space, and

physicallocality of eight pictograph sites in northern Quebec. They are in different regions of

the province: one is in the James Bay area, two are in Abitibi area, one is in the

Témiscamingue, two in the Outaouais region, one in Mauricie, and one in Haute-Côte-Nord.

Nevertheless, he drew considerably upon ethnographic data from western Ontario. He

argued from the substantial ethnographic record of the Ojibwa, that rock image sites in

Quebec were sacred places used by shamans.

He drew on ethnographic data collected from throughout Canadian Shield rather

than just specific regions in Quebec. This is surprising, especially since the Algonquian

groups of the western Canadian Shield probably had different cultural experiences from

those in Quebec; although these images were created by Algonquian-speaking peoples, they

were created by different groups. It is therefore possible that there were specific differences

in the religious practices and perhaps the use of images between the Ojibwa, living farther

west, and the local groups of Algonquian speaking peoples living in these regions of Quebec.

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Arsenault considered that pictograph sites may have acoustic properties that explain

why some rock faces rather than others were utilised. Archaeologists, elsewhere in the world,

have investigated whether site selection occurred as a consequence of the special sound

effects that could have been produced in specific spaces (Rainbird 2003, Waller 1993).

Both Dewdney and Kidd (1967) were obviously concerned with identifying what

constituted a site. Yet, in the same breath as they (ibid.: 6-8) delineated the properties of a

"typical site," they stated that it was difficult to generalise about the properties of a typical

site. Evidently, the visual landscape was not considered important for understanding these

images. Nor is much information recorded as ta how, precisely, sites were located. It appears

that Dewdney relied upon information provided by inhabitants of the areas where he sought

to find rock art sites (ibid.: 7-8).

Section 7: Literature concerned with meaning

The three remaining approaches are aU concerned with establishing the meaning of

these images. For a detailed discussion of each approach see Chapter I.

(a) Intuitive approach:

Archaeologists who have adopted the intuitive approach to explain rock image sites

in the Canadian Shield include Granzberg and Steinbring (1995), Lanoue (1989), Pettipas

(1982), Steinbring (1976, 1979b, 1982), Steinbring and Elias (1967, 1968b), Steinbring,

Granzberg and Lanteigne (1995), Steinbring and Steinbring (1978) and Vickery (1991). Only a

few of them have referred to sites in the Lake of the Woods.

Steinbring and Steinbring (1978) postulate that the images found at Machin Point,

DjKr-1, in the northwest part of the Lake of the Woods, were created as a consequence of

shamanism, based on a study of shamanism in connection with a petroglyph site in British

Columbia by Walker in 1977, and ethnographic data from the Winnipeg River watershed

(Steinbring and Steinbring 1978: 13). Both archaeologists speculated that a "template effect"

existed in the distribution of the glyphs of DjIv-1, which "seemed to be closely related to"

the naturallines evident in the rock upon which the images existed (ibid.: 13). The authors

concluded that the natural lines guided the creation of the images in a manner related to

Algonquian scapulimancy.

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Some of the images were identified and discussed according to the identification of

both archaeologists rather than merely described. According to the authors, careful scrutiny

of the images indicated that "vandalism" had occurred at this site. The green paint in some

of the "authentic-appearing" images, which had been created using a variety of pecking

techniques, was considered as evidence of vandalism. The authors maintained that they were

able to deduce that "fraudulent glyphs," made by short pecked lines, also existed at this site.

Low-level interpretation is embedded in the descriptions of these images, such as the

"dragonfly" petroglyph discussed by Steinbring and Steinbring (ibid.).

Steinbring (1982) later drew upon a variety of ethnographic sources to substantiate

his arguments that the images found in pictographs and petroglyphs in the Canadian Shield

existed as a consequence of Ojibwa and Algonquian shamanistic activities and dreams. The

petroglyphs of the Lake of the Woods sites were only briefly mentioned. The goal of his

paper was to argue that the art of contemporary native artists, with Algonquian backgrounds,

had the same origins as the crea tors of the petroglyphs, created during the Archaic Period.

He overlooked demonstrating precisely how this was possible, since he neither provided

evidence that he had consulted or interviewed contemporary native artists, nor suggested

who these peoples might be.

Steinbring (1976) speculated about the origins of the copper technology and lunar

cultism in the ancient Great Lakes region. He (ibid.: 164) argued that creseent shaped forms,

which he eailed lunar motifs, were present at rock image sites and on bireh bark seroils

created by the Ojibwa. He asserted that substantial ethnographie details existed concerning

lunar symbolism in the ethnology of the Great Lakes Algonquians, but provided no

references for his readers. He subsequently identified erescent shaped motifs at the

Peterborough Petroglyph site and disagreed with the Vastokases' (1973) identification of

these images as boats. He argued that some of them were probably not boats with people in

them but eould "actuaily represent copper erescentie symbols" (Steinbring 1976:. 164). He

subsequently argued that similar images are found at a number of sites in the Lake of the

Woods and elsewhere in Northwestern Ontario and eastern Manitoba (ibid.: 164-165). For

eaeh example given of a erescent shape at a site, he disagreed with its interpretation by

previous archaeologists, arguing that "many crescents have probably been misinterpreted as

boats or eanoes, the most obvious of these being the "upside down" ones (ibid.: 156).

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Granzberg and Steinbring (1995) classified glyphs by type usmg the intuitive

approach. They argued that line, tree, and circle motifs were "core symbols with a

transcultural base line of archetypal usage" based on examples taken from sites in the

American Southwest and from northern Manitoba and Northwestern Ontario (1995: 52).

They postulated that their data suggested, despite the lack of ethnographic references, that a

certain level of trans-culturally valid meaning existed, allowing the authors to identify distinct

types. However, both authors maintained that considerable research was necessary before

any categories could be securely identified (ibid.).

Lanoue's (1989) study considered the petroglyphs of the Lake of the Woods. He and

Richard Doble, from the University of Winnipeg, exarnined and recorded an unknown

number of petroglyph sites in 1981. Lanoue asserted that these rock image sites were

"stylistically Algonkian". He argued that these images, which could not be placed "in the

tradition of 'great art'" (ibid.: 7), were "the product of similar intellectual processes and

formally the same everywhere at all times" (ibid.: 9). Lanoue drew (ibid.: 42) upon

Steinbring's work (Steinbring et. al. 1987) to postulate that the petroglyphs were at least

5,000, and possibly even 9,000, years old. He maintained that his own examination was

flawed because he did not have the full body of data available to him since the full repertoire

of images in the Lake of the Woods was not yet established. He posited this was because (a)

not all the petroglyph sites had been found and (b) sorne were covered up with water and

therefore not visible.

Using CUITent knowledge concerning hunter-gatherer and tribal societies, Lanoue

proposed that, if the style used to create the images was related both to their meaning and

content, useful information regarding the "central paradox of territoriality" might be

obtained. He maintained that the Ojibwa material from Rama Reserve, northwest of

Toronto, should be used to illustrate his answer rather than analyse his data. He was

particularly interested in the animal images, referring to them as "symbolic mediators of a

paradox which characterises territorial hunting and gathering societies" (ibid.: 64). Images

were stylised since their meaning occurred as a consequence of its association with different

"symbols and symbol sets" instead of being a point of reference (ibid.: 67). Two sub-styles

were identified in the depiction of the animal images that were not easily recognisable. He

claimed that those naturalistic petroglyphs that were "stylized through simplification"

represented the paradox of location and mobility (ibid.: 68), while those animal images that

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were simple in design but distinguishable from the first group because traits had been added

that were "clearly not natural" (ibid.: 69), represented the intellectual paradox. The second

group had arisen as a consequence of the creation of boundaries which separated human

beings from animaIs, on the one hand, and the required dependency on the world of animaIs

to create a social world. Therefore, if specifie design traits indicated that an image was not

normal, or "natural," it meant that the authors of the images referred to ideas about the

supernatural rather than natural beings. Lanoue maintained that the people who occupied the

Lake of the Woods during the historie period were "preoccupied" with questions of

territoriality and desired to situate themselves not just using "a social and spatial grid" but

also by involving "abstract expression."

(b) Analogical Approach:

Cailahan (1998) has applied the neuropsychological "model", developed by Lewis­

Williams and Dowson (1988) to this geographical region of North America but only to sites

in Minnesota (Cailahan 1998). The rarity of this approach is interesting, given its popularity

elsewhere in the world.

(c) Homological Approach:

This is the most popular approach for archaeologists interested in determining the

meaning of rock image sites since meaning was drawn by comparing archaeological data with

related historie and ethnographie cultures (Conway n.d. a, n. d. b; Conway and Conway 1989,

1990a, 1990b; Dewdney 1970b, 1970c; Lévesque 1968; Lipsett 1970; Molyneaux 1980b,

1980c, 1987; Tassé 1977b; Turner 1979; Vastokas and Vastokas 1973).

Lipsett (1970) compared the images of specifie pictographs with images created and

used by the Ojibwa, as discussed in Hoffman's (1891) report on the Midewiwin Society and

the different types of religious practitioners among the Ojibwa. Molyneaux (1987) took a

similar approach to the images he found at several pictograph sites in Northern Ontario,

including DhKo-l and DhKm-5 in Whitefish Bay, in the Lake of the Woods. Dewdney

(1970a) developed the idea that by comparing the style of rock images and those made by the

Midewiwin on birch bark scroils, it might be possible to distinguish between historie and

precontact images. He and Kidd (1967: 171) had argued that the images on the birch bark

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scroils would probably provide clues to the meaning of the images on the rocks ln the

Canadian Shield.

Dewdney and I<idd's (1962, republished 1967) study was arguably the first

comprehensive investigation of rock image sites of the Canadian Shield. Dewdney examined

twenty pictograph and petroglyph sites in the Lake of the Woods. He also posited a

connection between the images on rocks and the Midewiwin, based on the similarities in

morphs executed at rock image sites and on the birch bark scroils (1967: 106-110).

Numerous sites were described in varying degrees of detail (ibid.: 22). Unfortunately, detailed

interpretations of each site were not provided, although much of this information was

retained in Dewdney's private archive, which is now kept by the Royal Ontario Museum.

The age of the images was estimated from their style. Dewdney and I<idd speculated

as to why the sites were painted and who the artists were (ibid.: 16-20, 102-116). They

hypothesised that sorne of these sites depicted articles of European origin such as "an early

European fort" and "the f1ag" (ibid.: 48). The distinction between explicit "description" and

low-level "interpretation" is blurred in Dewdney and I<idd's descriptions of the different

images at each site. An example of this exists for site # 106 on the shores of Obaibikon

Channel, on Sabaskong Bay, now cailed DhKn-1, in the Lake of the Woods (figure 3.11).

Dewdney wrote about this site:

Speeding up the channel from Sabaskong Bay we caught a glimpse of red through the trees high up on the east shore. On shore, expecting to find another example of iron stains, we were happily astorushed to discover the paintings shown here: two serpentine figures one with antlers the other with horns, symmetrically facing a large turtle. To the left, rather crudely painted on very rough granite, was a serpent fifteen feet long, with open mouth, ears and three large flippers - a veritable Ogopogo.

A deep cleft between the ledge we stood on and the rock was almost filled with dirt and rubble. Lying on the ground was an ancient, weathered overcoat, and various rags that had rotted beyond recognition.

(Dewdney and Kidd 1962:43)

The "veritable Ogopogo" is visible in figure 3.47 while his "serpentine figures" are visible in

figure 3.48 below.

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Figure 3.48: The serpents and the turtles described by Dewdney in 1960.

Dewdney often classified the images using Western art historical terms such as

"naturalism", perhaps because he had been trained as an artist and illustrator. His cultural

background clearly influenced rus verbal descriptions of the different sites. Another example

relates to a pictograph site called Painted Rock in Lac La Croix:

For sheer naturalism there are no other paintings of moose that l have seen in the Shield country ta compare with the three on this site. Ail are surely by the same hand, as is the little antelope-or deer. Unique, too, are the pipe-smoking figures: one beside an hour-glass figure and tracks, the other not far from the initiaIs "L.R. 1781".

(Dewdneyand Kidd 1967: 26-27)

Dewdney and Kidd each dealt with separate components of this study. Dewdney

located, recorded, and described the pictograph sites and occasionally obtained sorne

ethnographie details (ibid.: 11-14), while Kidd considered and examined the related

anthropological data (ibid.: 159-177). However, trus split between the work undertaken by

Dewdney and Kidd is misleading: it may simply reflect academic traditions at the time their

book was written. Yet, throughout, Dewdney speculated as to the authors of these images,

why the images existed, their meaning, and the paint ingredients, prior ta discussing the

different sites and their respective paintings. Kidd (ibid.: 159-177) summarised the rustory of

the interest in these images, the archaeology and the early rustory, and considered the

Algonquian-speaking peoples in the Canadian Srueld. He, like Dewdney, speculated as to

why the images were created, the possible authors of these images, the paint's constituents,

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and the techniques of applying these images, as well as different possibilities for establishing

their meanings. Neither I<idd nor Dewdney considered that the meanings of these images

might be polysemic, despite I<idd's discussion of the Midewiwin Society and its members

(ibid.: 167-168).

The second (1967) edition contains considerably more information, but suffers from

the same problems. Dewdney and I<idd's study represents the first major step in the

homological analysis of these images. Although Dewdney was not an archaeologist, his work

on these images was immensely influential.

Dewdney (1970b) used ethnographic evidence concerning shamanic practises among

the Ojibwa to postulate the reasons for the creation of pictograph sites. He illustrated his

arguments using individual images from four sites in Whitefish Bay, Lake of the Woods:

DiKm-3, DhKm-3, DhKm-S, and DiKm-4. He drew upon information regarding the

worldview and religious practices of the Algonquian-speaking peoples collected by

anthropologists, and from his numerous conversations with indigenous informants, including

Norval Morrisseau, the Ojibwa artist, to try to determine how and why these paintings were

created, and what they meant (ibid.).

Dewdney argued that the pictographs, like the other images created by the

Algonquians on wood, birch bark, and hide were all forms of expression (ibid.: 22) that he

subdivided into three categories: secular, tutorial, and visionary. The images on the birch

bark were deemed secular and possibly included those le ft at portages for others, to give

practical information such as an individual's 'signature', a representation of his totem or his

name" (ibid.). He maintained this mark or image would have also existed on personal objects

that belonged to individuals. Yet, since Algonquian society was collective, an individual

would only have left a "mark" for territorial reasons. Tutorial images were defined as those

that were used between a shaman and his clients or those used as mnemonics on the birch

bark scrolls (ibid. 23). Dewdney deemed sorne images as visionary, based upon his interviews

with older generations of Ojibwa.

Dewdney (1970b) asserted that the description and classification of images grouped

together by their physical shape was problematic, since images should not be examined

separately if they were originally part of a larger group from a site. This daim occurs in an

article that seems to have been part of a larger research project that he was undertaking prior

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r-..

~ ..

to ms death. It seems evident from reading ms research and field notes3 that Dewdney may

have been synthesising the information he had collected. He had noted that twenty-six

percent of the sites that he had recorded were dry sites and seventy-four sites were wet sites.

What he meant by the terms "wet" and "dry" is undear. It is also dear that he sought to

identify ail the different variations of each type of image he had recorded. He provided the

number and gave the name of the pictograph site, if it had one, where each image existed.

What precisely Dewdney intended to do with this analysis remains unknown.

He was also interested in whether the type of image he had identified at each site

existed only at certain orientations, or in certain parts of a pictograph site and whether tms

changed according to where in the Canadian Smeld the site was physically situated. This

work is possibly related to some ideas that Dewdney (197 Sa: 1) expressed in an

Archaeological Newsletter that perhaps understanding how the stylistic variations were

distributed throughout a region provided chronological dues to dating the images of the

Shield region. He argued that he initially posited that using a computer provided the most

objective means of sorting and correlating the images which he had collected over the course

of ms research. He posited that he had approximately 3,000 figures which he termed morphs

(ibid.: 2). He realised that although he had used a computer that "an inadequate typology,

loosely defined coding values and inconsistencies (Plus too many errors)" led mm to

condude that higher standards were required in the initial phase of a study (ibid.). He

concluded ms short piece by reminding his colleagues that it was important to be as

meticulous and objective as possible and that he was guilty of being too subjective when

recording and describing ambiguous images (ibid.: 4).

It is dear from ms notes, held by the ROM, that he was conducting sorne systematic

analysis using a computer with colleagues at the University of Western Ontario. Another line

of research that concerned mm in ms notes is mentioned in an ROM Archaeological

Newsletter dated 1971. He discussed his observed correlations between specific pictograph

sites and "vision pits" which were special places that he believed were chosen by shamans

for their vision quests (ibid: 3). He posited that DhI<m-3 was possibly one such example of a

place that a shaman had chosen as a "shaman's retreat," especially given its physical

characteristics: the images were beside a bench "large enough to pitch a tent on, and far

3 Dewdney's field notebooks, field drawings, slides and photographs are held by the Department of Anthropology, Royal Ontario Museum, in Toronto Ontario, Canada.

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above the water" (ibid.: 4). However, he concluded that further research was required to

substantiate his opinion that pictographs sites were probably connected with "vision pits"

(ibid.). Clearly severallines of research were being explored and developed for some purpose

that is now unclear and difficult to establish.

Vastokas and Vastokas (1973) attempted to understand the mearung of the

Peterborough Petroglyph Site. These images were pecked from crystalline lime stone, one of

the softest rocks in the Canadian Shield, and ground out using gneiss hammerstones (ibid.:

14-18). The petroglyphs were speculatively dated, based on available data, to the end of the

Woodland period, between A. D. 900 and 1400 and attributed to prehistoric Aigonquians

(ibid.: 20-27). The Vastokases postulated that a connection existed between the engraved

images on the rock faces and the images on birch bark scroils created by the members of the

Midewiwin Society (ibid.: 40-47). They surmised, from ethnohistorical and anthropological

sources, that the images were located where individual shamans believed they could consult

the resident spirits (ibid.: 47-54) and that unusuaily shaped large rock outcrops, rocky hiils

and boulders with crevices and holes were the "dwelling-places of the manitous and mythical

creatures such as the Maymaygwayshi" (ibid.: 48).

Vasto kas and Vastokas discussed at considerable length how the Algonquian universe

was organised and how the physical locations of the rock images in the landscape were key

loci, since these places were where the different worlds co-existed and hence these places

were "the seat[s] of visionary experience and super natural counsel" (ibid.: 54). They (ibid.:

29-40) discussed the nature of Algonquian hunting and gathering practices and the different

objects upon which similar images appeared, and maintained that the manner in which

shamanism, Algonquian cosmology, manitous, vision quests, and guardian spirits were

interrelated provided the information required to understand the petroglyphs. They

postulated that a detailed understanding of Aigonquian use of pictographs to convey

information would aid modern acadernics to understand these images.

Images were analysed once they had been classified by type and placed in different

broad groups according to subject matter (ibid.: 55-129). The Vastokases noted that,

although over nine hundred glyphs existed at the site, only three hundred were readily visible.

The others were deemed "vague and their identity is difficult to de termine owing to the

degree of overlap and superimposition, wear and erosion of the limestone surface" (ibid.:

55). They subsequently asserted that the variety and extent of the images' meaning was only

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accessible once detailed analysis of this site was completed (ibid.). Interpretation and

discussion of the possible meanings of each group could occur once the identifiable images

had been classified by shape and subject matter, and with reference to ethnographic and

ethnohistoric data. Three years earlier, Dewdney (1970b) had asserted that the description

and classification of images that were grouped by type (their physical shape) was problematic,

since images should not be examined separately according to their physical shape; especially

if they were originally part of larger group of images which were different.

It was possible that the meanings of the different images were interrelated. Based on

the changes in the styles of the images, the Vastokases (ibid.: 131-134) concluded that the site

had probably been used repeatedly over a long period of time. They speculated that these

stylistic changes were possibly connected to technological, cultural, or temporal factors. They

(ibid.: 137) asserted that the images of the Peterborough Petroglyph site should only be

compared with other petroglyph rather than pictograph sites to establish stylistic affinities.

However, this statement is problematic, because it is possible that the crea tors of these

images did not differentiate between images ground into stone and those painted on stone.

The Vastokases concluded that the rock itself, the landscape, was crucial to the meaning for

these images and to understanding why it was used for these images. Although this study is

over thirty years old, many of its conclusions remain important to the analysis of these

images today.

Both of Conway's (n.d. a. and n. d. b) papers examined sites in northeastern Ontario.

He (n.d.a) was concerned specifically with three morphs, from various pictograph sites in

northern Canada, which occurred in conjunction with each other: an open armed man, his

canine companion, and an animal pelt. Another morph, which Conway identified as a beaver,

the pelt, existed above the man and his animal companion. He identified these images as

specific star constellations. The open armed man was identified as Orion since the paintings

had anatomical attributes that were similar to those of the constellation. The position of

canine companion, identified in the pictograph sites as either a dog or wolf, concurred with

that of Canis Major. The bilateral symmetry and location of the beaver matched that of

Gemini to Orion (ibid: 1). Conway (ibid. 1-2) drew upon ethnographic information collected

by Schoolcraft, Speck and some other unnamed individuals, and from his own informants, to

identify specific constellations as animaIs and supernatural heroes. Schoolcraft was important

for Conway, because he was particularly interested in native astronomy and cosmographic

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information. Conway Qbid.: 3) maintained, based on unknown sources, that native

astronomy depicted at pictograph sites had "considerable antiquity" since according to him

such paintings had ceased to be created after 1650 A. D. by Ojibwa shamans and medieine

people. He asserted that few sites showed historie scenes involving Europeans, but provided

little evidence to substantiate this daim. He argued that the style changes and presence of

constellation groups in the pictograph sites indicated that native cosmographie information

had existed since the prehistoric era. Fourteen constellations were identified, but Conway

was specifically interested in the Orion trio whieh he identified as existing on a birch bark

scroll made for Schoolcraft by a Lake Superior shaman as weIl as in some unnamed

"examples of Ojibwa rock art sites" (ibid.: 4).

Conway (ibid.: 4-5) asserted that the "Orion trio of paintings" was explicable using

information from popular native folklore. However, he argued that it was possible to put

forth another interpretation of these images, since the constellation paintings behaved as a

mechanism by which seasonal changes were indicated to the local indigenous population.

Orion was interpreted as a celestial marker for "a shift from late fall to winter camps" (ibid.:

5). The depiction of constellations at pictograph sites indicated that these sites were "sky

maps" which enabled information about seasonal migrations through the landscape to be

transferred from one generation to another. Conway conduded that rock image sites should

be considered as "one of the few permanent markers" in the lands cape that provided

knowledge to the transitory Ojibwa hunter-gathers of this region.

Another paper by Conway (n. d. b) is perhaps a later draft of the paper previously

discussed (n. d. a) as its content is similar. In this second paper, he hypothesised that specific

images were based upon the constellations recognised by prehistoric Algonquians. These

images originated from sites in an area occupied by the historie Ojibwa, Cree and other

Algonquian bands (ibid.: 5). Conway argued that this combination of morphs was first

identified at a site by himself in Matagamasi Lake, in northem Ontario (ibid.: 7). He

subsequently briefly discussed Dewdney's published works, the Vastokas and Vastokas

(1973) publication, as weIl as various site reports from throughout Ontario in an attempt to

establish whether this triad of images existed. Conway maintained it was easier to identify

whether these three images existed together if the painted figures were "not as dustered"

(ibid.: 8). This triad of images existed in only two clusters in the Temagami stylistic and

Shield Edge stylistic areas (ibid.: 9). It was absent elsewhere in the Upper Great Lakes area

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and north central Ontario. Unfortunately, Conway did not define what constituted the

Temagami or the Shield Edge styles. Two types of canines were identified to exist on their

own or with a human figure: a dog and a wolf. Two examples of the dog morph were

identified at two sites in the Lake of the Woods: DiKo-2 and DhKm-3. Wolf morphs were

identified at one undisclosed site in the Lake of the Woods. But Conway did not establish

how wolf and dog morphs were different from each other.

Conway's conclusion had four points. Firstly, two distinct canine morphs existed in

the rock images sites in Ontario, which Conway identified as a wolf and a dog. Nevertheless

both images could denote "the same Algonkian concept" (ibid.: 12). Secondly, both morphs

had comparable limited geographical distributions, namely the northeastern edge of the

Canadian Shield in Ontario and north and west part of the Lake of the Woods in north

western Ontario. Thirdly, dog canine morphs often occurred with hum an figures while wolf

canine morphs existed with human figures that had their arms open. Conway's fourth

conclusion was that "an Algonkian triad" existed at the majority of sites that had the wolf

morphs, and consisted of "a human figure or shaman figure with outstretched arms, a pelt or

a cross" (ibid.: 12). Conway's conclusion is interesting since it demonstrates that his own

Eurocentric cultural perspective was influential in his choice of images to examine, despite

his utilising the pertinent ethnographie evidence from the region where the sites existed.

Fol1owing Hodder (1987), Rajnovich (1994: 160) argued that it was possible to arrive

at sorne conclusions that could not "be absolutely proven" (Rajnovich after Hodder 1987: 6)

but were plausible. Rajnovich (1989, 1994) repeatedly drew on the Lake of the Woods as a

source of examples for her discussion of rock image sites in the Canadian Shield. She

postulated that archaeological, ethnographie, and anthropological evidence should be

combined with linguistic and oral evidence to establish the link between the different types

of Ojibwa shamans, Midé and Jiissakid, to obtain an understanding of these images. She

(1994: 19-22) asserted these images were signs, probably mostly polysemie metaphors, since

Algonquian languages are metaphorical. She (ibid.: 22-39) discussed the Algonquian world

view, the practice and use of indigenous plant medicines, and the different types of religious

practitioners. Rajnovich (ibid.: 29) maintained that only the Midé and Jiissakid, two of three

types of religious practitioners, rather than the Wabeno, created rock images.

She appears to base her arguments on two rock image sites, providing a field drawing

of each site: Dewdney's field drawing of Painted Rock Island, DhKo-1, in the Lake of the

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Woods and a petroglyph site in Uskik Lake in Saskatchewan. She (ibid.: 41-55) debated the

age of these images and concluded that it was only possible to use relative dating techniques

and to draw upon ethnographie, and related archaeological data from nearby peoples to posit

the age of individual sites.

She (ibid.: 57-63) related the images present on the Qjibwa birch bark song scroils to

those on the surface of rocks by drawing on the work of Garrick Mailory (1880, 1881 and

1884), Tanner Games 1956), Hoffman (1888, 1891, 1896), Kohl 1985 [1860], and Densmore

(1910, 1913, 1926, 1979), as weil as sorne unpublished studies in the Smithsonian

Institution). Rajnovich (1994: 57-63) postulated that the metaphorical nature of the

Algonquian languages provide clues to the interpretation of the paintings and engravings.

She (ibid.: 65-66) argued that the pictographs were standardised in the sense that other

people could recognise the images and interpret them but that different and legitimate

meanings could be attached to specifie symbols.

To demonstrate why and how these images were polysemie, Rajnovich first discussed

the importance of the cliff faces and then a range of images with reference to ethnographie

sources and informants (ibid.: 66- 143). Each type of image was analysed and interpreted

after it had been grouped into a broad shape type. Meaning was ascribed to an individual

shape through references to data from ethnographie and ethnohistoric materials, as weil as

from informants.

She ignored Dewdney's (1970b) stricture that images should not be interpreted

individuaily from the other images with which they exist. Her practice of first dividing images

into broad groups also may cause problems. This activity is probably related to the manner in

which rock image sites are treated by archaeologists accustomed to coilecting data according

to archaeological conventions and guidelines. It is surprising that her discussion of these

images did not draw on the conclusions about these images that she had published earlier in

government reports (for example Rajnovich 1980b, 1981b).

Rajnovich (ibid.: 145) observed that a common explanation for the presence of these

images was "hunting-magic", (ibid.: 145- 157) and discussed at great length what this could

mean with reference to the Algonquians of the Canadian Shield. She subsequendy argued,

based upon ethnographie data, that rock images appeared on rocks where manitous lived

(ibid.: 160), and that these sites occurred beside water because that was where the sky, earth,

water, underground, and underwater meet. Places su ch as deep lakes, whirlpools, bases of

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lakeside cliffs, caves, and crevices were the locations used to cross from one world into

another (ibid.: 35). For Coleman (1937:34) these places were where the manitous lived and

where the manitous and the medicine people could meet.

Rajnovich asserted that paintings were done principaily using red ochre because this

mineraI was "a powerful medicine itself and used in sorne cures" (ibid.). Specific images were

painted because they referred to particular experiences of the medical practitioners of the

Algonquians, the Midé, since they created the images on the birch bark scroils. The images

were painted on rock surfaces, where these medical practitioner people wanted "to leave

lessons" (ibid.: 161). Rajnovich (ibid.: 163) postulated that the paintings in this region were

"intimately" connected to Algonquian beliefs, legends, and songs. She concluded that the

best approach for those wishing to establish the meanings of these images was for

information from the Algonquian people's history and philosophy to be combined with

ethnographic data. Although Rajnovich's (1994) study has sorne flaws, it remains the most

recent and sustained contribution to research to date on the meaning of rock image sites of

the Canadian Shield.

Sorne archaeologists have used Rajnovich's approach to analyse specific rock image

sites from other parts of the Canadian Shield, but not from the Lake of the Woods

(Hamilton 2000; Pettipas 1991 b). They have explored the concept that different bodies of

ethnographic information could aid archaeologists in answering specific questions regarding

these images. It is important that the archaeologist also acknowledges the problems of using

ethnographic evidence from present day informants to interpret images from the

archaeological record. Jones (1981b: 46-47) maintained that ethnographic information from

Northern Saulteaux and the Cree groups aided the "empirical concerns of archaeologists"

seeking to establish the binder used to create the paint to make pictographs. Wheeler (1977a,

n. d.) argued that attention should be paid to studies of the structure of the Cree and Ojibwa

languages where the May May Quah Sao (often cailed Maymaygwayshi), who were spirit

helpers, were associated with stones in the sacred stories told by Algonquian-speaking

peoples (n.d.: 1). The word "stone" belonged, Wheeler asserted, "in an animate grammatical

category in Algonkian languages" that was "linguisticaily distinguished as that which interacts

with man and that which does not" (ibid.). Wheeler (n.d.: 5) recorded a rock image site on

the Semple River near Oxford House in northeastern Manitoba including the legend

connected to this site by informants. Information existed, Wheeler noted, regarding the

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relationship of these spirit helpers and rock image sites ln the ethnographie and

anthropologicalliterature such as such as that produced by Dewdney and Kidd (1962; 1967)

and Landes (1968), while others (Stevens 1971) had recorded stories that connected these

spirit helpers to rock image sites.

Two more in-depth studies of two large rock image sites must be mentioned since

they are found in the Canadian Shield, although neither site is in close proximity ta the Lake

of the Woods (Conway and Conway 1990b; Vasto kas and Vastokas 1973). Conway and

Conway were archaeologists based in the Sault Ste Marie region of Ontario and, so, this

study reflects the ethnographic and historical details of this area. Bath archaeologists asserted

that the paintings at the Agawa rock images site on the north shore of Lake Superior were

created by "Ojibwa Indian shaman artists" (ibid.: 7) who in the indigenous communities were

the link between the human world and the spirit worlds. They (ibid.) argued that Agawa was

"an exceptional site" with several components.

Conway and Conway (1990b) drew upon information from a variety of sources

including Schoolcraft's published date for the images, and from several Ojibwa elders,

including (a) Fred Pine, who Conway identified as a "noted Ojibwa tribal elder" born in 1897

and Shingwauk's great-grandson (ibid.: 19), (b) Chief Norma Fox from the Cockburn Island

band of Lake Huron (ibid.: 21), and (c) Bill Sheskekwin who lived in the Dog Lake area of

the Upper reaches of the Michipicoten River. Conway and Conway argued that their

informants enabled them to establish that several individuals had painted the images at

Agawa, including: a 17,h century Amikwa band leader called Myeengun (the Wolf) and a 19th

century shaman called Shingwauk, or 'The White Pine', from Lake Superior.

Conway and Conway argued that, because the water level of Lake Superior was

higher than the painted are as of the cliff over three thousand years ago, the paintings had to

be younger. They estimated that the most visible paintings were created during the last five

hundred years. Conway and Conway (ibid.: 7-8) posited that the images were created for

religious reasons and were the "end products of religious experiences such as vision quests,

group ceremonies, and acknowledgement of spiritual assistance," and did not directly

chronicle episodes from the pasto

The images are examined in seventeen "panels" (ibid.: 15), and as one hundred and

seventeen individual images (ibid.: 8, 15). Conway and Conway asserted (ibid.: 15) that the

panels were "numbered from north to south (left to right)" if an individuallooking at the site

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was in a canoe in front of the cliff face. They established the meanings of the pictographs of

Agawa Bay with reference to ethnographic and ethnohistoric data as weil as information

from Fred Pine, Chief Norma Fox, and Bill Sheskekwin. The images on each panel were

described and identified in considerable depth and each panel was interpreted. It is, however,

unclear whether the division of the Agawa rock image site was based on information gained

from their indigenous informants or not.

The examination of pictograph and petroglyph sites has developed and advanced

over the last hundred years. Considerable time, effort, and money have been spent on the

development of the techniques to physicaily record and date them, and many have tried to

interpret the se images. People want to find out how to discover more of them, satisfactorily

record the images, and preserve them for posterity. Yet, the most important goal is to

establish what these images may mean.

Different people have clearly taken different approaches, although it is clear that the

homological approach is more popular amongst those determined to establish the meaning

of these images. The current understanding of these sites in the Lake of the Woods is that

they were created by shamans, ritual specialists, in key places in the landscapes where the sky,

the underground, the underwater, and the earth meet and where the traveling soul of the

shaman could cross from one world to another.

Conclusion

The goal of this chapter was to present and discuss the work undertaken prior to my

own by previous researchers concerned with the pictograph and petroglyph sites in the Lake

of the Woods area. l determined to establish the most popular philosophical approach, what

previous researchers have thought of pictograph sites, how they examined what they were

interested in, and to understand the origins and the reasons behind the terminology used to

identify the images found. This critical review of the literature demonstrated that a large body

of data ranging from conservation of the paints used in pictographs and the different ways of

examining them (e.g. Myers and Taylor 1974; Wainwright 1990, 1997), how to establish the

age and style of specific pictograph and petroglyph sites in the Lake of the Woods (e.g. Reid

1979 and Steinbring 1977), the context of the physical surroundings of the images (e.g.

Noble 1968), to whether particular images only exist together and how to establish their

meaning (e.g. Cailahan 1989; Conway and Conway 1990b). Much of the literature was

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obviously concerned with the sites of the Lake of the Woods but it is important to consider

analogous studies of sites elsewhere in the Canadian Shield. Sorne of the literature is

descriptive (e.g. Lawson 1885), and sorne is concerned with technical issues, but much of it

was taken using several of the five approaches that exist in archaeology: culture-rustorical,

contextual, intuitive, analogical, and homological. As I argued in Chapter I, it is important to

initialiy use the culture-rustorical approach, then the contextual approach, and, if one is

concerned to establish the meanings of the images then either the intuitive, the analogical or

the homological approach should be used. Several archaeologists have used only the culture­

historical approach (e.g. Grant 1967; Reid 1979; Steinbring, Danziger and Caliaghan 1987;

Steinbring and Caliaghan 1985). Others utilised the contextual approach (e.g. Arsenault 1997;

Pohorecky 1968; Noble 1968). Many were determined to establish the meaning of the images

they found. The homological approach is the most popular approach for archaeologists (e.g.

Dewdney and Kidd 1962; Rajnovich 1994, Vastokas and Vastokas 1973), wrule the intuitive

approach is the second most popular approach (e.g. Granzberg and Steinbring 1995; Lanoue

1989). Only one archaeologist utilised the analogical approach (Caliahan 1989).

A considerable quantity of fieldwork and research has been conducted on the

pictographs of the Lake of the Woods, and my field work in 2001 should contribute to trus

larger body of information. It was for trus reason that prior to conducting my own fieldwork

I summarised ali of the information available for each of the pictograph sites pertaining to it:

alternative names; whether photographs were taken; how was it recorded; measurements if

taken; location of field recordings and published works making reference to the site; the

name of each researcher who examined it, with the dates and rus profession; rock type;

location of the sites; whether offerings had been le ft, and whether any statements had been

made as to its possible cultural affiliations (Trus information is in Appendix 1.). Ali of this

information was required so that I knew who had conducted research, what type of analysis

they had undertaken, and at wruch pictograph sites in the Lake of the Woods.

Previous researchers have established several key pieces of information about

pictograph sites. Pictographs occur on cliff faces while petroglyphs occur on horizontal

surfaces throughout the Canadian Shield, both in close association with bodies of water.

Images in caves are relatively rare and therefore little information has been accumulated

about these sites. Previous researchers agree that the paint used was made from hematite

mixed with an organic binder wruch cannot be identified. It is also agreed that these images

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occur in places that usuaily have ail of the foilowing five physical features: rock benches

(sometimes cailed shelves), overhangs, large cracks, large crevices, and holes. Absolute dating

techniques cannot be utilised, therefore, relative dating techniques are usuaily used to

ascertain the age of these images. Sorne researchers have recorded the quantities of lichen

and rock tripe growth and encroachment, exfoliation, and the accumulation of white mineraI

deposits present at each site. This information is often compared with the orientations of

these sites. Pictograph sites on cliff faces tend to face south, east, and occasionaily west. Very

few sites face north. Previous researchers have described the images they found, and

attempted to organise systems of stylistic classification to aid in establishing local and

regional patterns in the Canadian Shield. But there is no consensus about which classification

scheme is best used to describe the images. It is acknowledged that the description of these

images is highly subjective, since the vocabulary used influences their interpretation, and each

researcher tends to use their own system. Site description has also influenced the manner in

which a site can be subdivided into parts, facilitating its description but causing problems for

subsequent archaeologists. Researchers have observed that pairs of the same image often

occur at the same site.

Ali researchers agree that it is unclear which ethnic group created these images, but

they agree that the images were created by the Algonquian-speaking peoples. Consensus

exists regarding the importance of the sites to the current local indigenous peoples, who

consider these places as important and integral to their own world view. Objects left at sites

as "offerings" have always been recorded by previous researchers. Consensus exists

regarding the polysemic nature of these images, and that they were used to convey

information to other people. Ali researchers concur that the images of the pictograph sites

are similar to those on birch bark scroils made by the Midé ritual specialists. Hence, everyone

has posited that a detailed investigation of the images on birch bark scroils, the ethnographic

record, and the pictographs might provide sorne answers as to the meanings of the images

on the rock faces.

Unfortunately, l was only able to examine the pictograph sites in 2001 because the

water level was far too high for me to survey and examine the petroglyph sites. It was equaily

important for my research to foilow the three levels outlined in Chapter 1. Therefore, l used

the culture-historical approach, then the contextual approach, and finaily the most pertinent

of ail the approaches that should be used to establish the meaning of these images. Each

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subsequent chapter de aIs with and discusses the data that l collected according to this

sequence. However, the next chapter, Chapter 4, presents the basis for making the decisions

that l made while conducting field work and how l identified and classified images that were

found. The goal of my fieldwork was to systematically collect detailed information about

rock image sites over a portion of the Canadian Shield in order to better understand the

nature of the evidence that was available. Each of the subsequent chapters will deal with the

archaeological data according to each of the different philosophical approaches that must be

applied to this data in sequence as outlined in Chapter I.

However, l do not use the intuitive approach, sin ce l think that it is important ta

articulate to other researchers how my conclusions were reached. l do not think that readers

should be reliant on the whims of the author, and they should be able to understand

precisely how an interpretation was reached. l think it is important for discussions and

arriving at conclusions to use vocabulary that is easy to understand. If an archaeologist is

determined to establish the meaning of these images in a more rigorous and persuasive

fashion, the analogical or homogical approaches should be adopted (see Table 1 in Chapter

I). Chapter V presents how the culture-historical approach is applied to this data, and seeks

to establish the total range of the images. Chapter VI presents the conclusions that are drawn

once the contextual approach is described, and considers whether combinatory rules exist

regarding the relation of the different sorts of images to one another. Chapter VII uses the

most applicable approach concerned with meanings to consider how to establish the

meaning of these images, and whether these images are related to others outside the rock

images sites.

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Chapter IV: My Work on the Rock Image Sites.

This chapter presents the ground work required to collect the data I needed on each

of these sites. It presents the basis for my decision making while conducting field work, and

how l identified and classified the images found. Through fieldwork, I systematically

collected detailed information about rock image sites over a portion of the Canadian Shield

in order to better understand the nature of the available evidence. This required not only re­

recording the known sites, standardizing and verifying current knowledge, but also locating

as many unknown sites as possible. This data will enable me to achieve the four goals of my

thesis to (a) identify the possible vocabulary of images, (b) determine whether combinatory

rules exist, (c) reconstitute the life history of each site, and (d) ascertain whether the images

can be related to other images outside the rock image sites to determine if this can provide

information about the meaning(s) of the rock images.

Therefore, in 2001, l conducted three and a half months of fieldwork on the

pictograph sites in the Lake of the Woods area located between North latitudes 49° 00" - 49°

50" and West longitudes 93° 53" - 95° 09". I implemented a newly developed method of

collecting survey and field data on the pictograph sites in the hope that perhaps new

pictograph sites could be found. l based my research on my experience, gained conducting

fieldwork in the Canadian Shield region since 1990; and working on conventional

archaeological sites in the Canadian Shield and the United Kingdom since 1989. I undertook

this fieldwork with an assistant, Melinda Bell; a volunteer, Elizabeth Campbell, who also

provided valuable photographie advice and assistance; and a team of approximately four to

five professional divers, from Sunset Diving, in Kenora. The divers examined specifie

underwater cliff faces that we suspected of being completely or partially submerged sites.

They also examined the base of sites that either had large quantities of offerings or were near

sites with large quantities of offerings. l did not conduct ethnographie research or use

informants for information regarding both the name of a shape and its meaning for the

reasons discussed in the introduction of this thesis.

This type of archaeological fieldwork is unconventional for two reasons. It must be

conducted from a boat. In addition, pictograph sites cannot be excavated in the same

manner as conventional archaeological sites. Fieldwork commenced in the middle of the

eastern portion of Lake of the Woods, since l rented a boat from the private marina owned

by Tomahawk Lodge, in the township of Sioux Narrows. l chose this marina because its

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owners have excellent business relationships with other private marinas throughout the Lake.

Long distances between the sites and Tomahawk Lodge necessitated the purchase of

additional gas from these other marinas.

l rented a boat so that l could start fieldwork each day with the maximum of gas (50

litres), and a 30 horse power motor free of mechanical problems. l am accustomed to

conducting fieldwork using sorne form of boat. l knew the importance of keeping the boat

where someone had the required mechanical skills to repair a boat engine. Most of my

previous fieldwork in the Canadian Shield involved canoes as transport to run rapids and line

rivers (move upstream against the current), since we moved through river systems and lakes

in remote parts of the bush usually reached by float plane. Many fieldwork contracts required

portaging from one lake to another to get from one site to another. Carrying an engine and

sufficient gas, portaging field equipment, field gear, and foodstuff was not feasible for a small

field crew who had to travel and work over a region extending a considerable distance in the

bush. Usually, l did not cross very large expanses of open water typical of the Lake of the

Woods. It is impossible to survey the Lake of the Woods in a single field season using a

canoe. However, occasionally the water was so shallow that a motor boat could not get close

enough for a detailed examination of a few the sites so a canoe had to be used to examine

them.

l used knowledge that l had obtained regarding the edible plants readily available in

the bush; the possible number and nature of rapids, especially waterfalls; information on

local water currents; types of portages; and as many detailed maps of the region as possible.

My previous experience had occasionally involved using a radio to maintain daily contact

with the nearest remote Ontario Ministry of Natural Resources outposts. However, this time

l could use a telephone rather than a radio. This was important, since there was always the

danger of being caught in a fore st fire, something to which Northwestern Ontario is prone.

Forest fires occur without warning and are very dangerous, especially if the winds cause the

flames to spread rapidly. Fortunately, during 2001, there was little danger from fore st fires in

the Lake of the Woods. However, this region did experience a large tornado which hit

unexpectedly and caused large numbers of older white pines to be ripped from the ground.

During my 2001 field season, l had a cell phone which occasionally functioned, while

working, so that l could find out the latest marine and weather report whilst travelling by

boat. l did not use a global positioning unit because l was told by the regional archaeologist

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based in Thunder Bay that l must learn how to travel through the bush without one before l

. could learn how to use one. l did not use a guide from one of the local reserves.

Conducting fieldwork in the Lake of the Woods differed from working in smaillakes

and rivers elsewhere in the Canadian Shield. l could use highly detailed marine charts. l

needed to acquire a detailed understanding of the many different local weather patterns, and

highly variable winds. l developed the ability to relate information from marine maps to a

landscape, the configuration of which changed as the level of the Lake rose or fell. In many

cases, islets morphed into reefs, muskeg became floating islands, and shallows became bays

or inlets. l had to rely upon my ability to navigate through a landscape that looked the same

regardless of where l was, be aware of rapidly changing weather and water conditions, and

know the location of marinas, while managing one or two small boats and a crew that varied

from two to eight. l employed equipment ranging from digital cameras, anchors, ropes of

various types, paddles, boat lights, an electronic depth finder, life jackets, permits to travel by

water into the USA, measuring tapes, food supplies, fresh water, a cell phone, ail weather

gear, to pens and pencils.

We worked from nine a.m. to nine p.m. for six to seven days a week, depending on

the weather, through June, July, August and half of September. l decided not to camp using

tents since l had to undertake digital analysis of my data while in the field. l had one

assistant, and one volunteer on a tight budget and a large geographical area that had to be

covered in a short period of time. Therefore l decided to stay in a small log building with

basic facilities including full internet, hydro, and running water. This enabled me to set up a

small computer laboratory on site.

l chose the Lake of the Woods area, in Northwestern Ontario, because the rock

Image sites in this area appeared representative of the data resulting from archaeological

surveys conducted elsewhere on rock images of the Canadian Shield. l could not find one

previously known pictograph site called DjKn-2, despite numerous attempts to do so.

Nevertheless, l re-recorded twenty-two known sites, and five additional sites were discovered

for a total of twenty-seven sites.

Two of these new sites constitute a new type of rock image site, since the paintings

were found inside caves, not on cliff faces. Pictographs in caves should not be considered

unusual, or an oddity, but rare. Another pictograph site, DcJh-45, found in Confederation

Park in downtown Thunder Bay in 2001 (Bell pers. comm. 2001), exists in a cave within a

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serÏcs of granite cliffs that border a dry riverbed (Ross pers. comm. October 2001). Given

the occurrence of these three sites beside water, it is possible to argue that this type of site

follows the rule of thumb that pictograph sites occur in conjunction with water.

Only nineteen of the twenty-two known sites had Borden numbers, possibly because

previous archaeologists had neglected to ob tain Borden numbers for three sites. Dewdney

recorded all three, but in 1960 and 1967. For many years, one of the sites was called the

pictograph site on Picture Rock Point, or Dewdney's Site # 95, while the neighbouring

pictograph site in Portage Bay, also first recorded by Dewdney in 1960, was called Site # 94.

However, the third of these 'known' sites without a Borden number had been forgotten,

since Dewdney did not publish any information about it, although he found and recorded it

in 1967. l discovered trus when l read his field notes and examined rus slides at the Royal

Ontario Museum.

l initially had intended to include petroglyph sites in my survey of the Lake of the

Woods. However, with the exception of one site at Machin Point in Shoal Lake in the

northwestern portion of the Lake of the Woods, the extremely high water levels covered all

sites to a depth of approximately 75 centimetres, rende ring this goal impossible. The water

level did not drop fast enough over the period of my field season to consider recording these

Images.

Based on my reVlew of the work by previous archaeologists on pictograph sites

discussed in Chapter 3, l designed two forms, A and B, which l used in the field.

l deeided not to use the established technique of subdividing pictograph sites into

segments although it has been used by Pastershank (1989), Dewdney (Dewdney and Kidd

1962 and 1967), and Lambert (n.d). This practice subdivides sites into parts and inadvertendy

causes the images to be placed into groups in the culture-historical approach. Analysts must

complete the culture-historical approach, then the contextual approach prior to establishing

the meanings of these images.

l also discovered insurmountable difficulties in obtaining sorne desirable information.

l removed these categories from Form A: (a) prehistoric and historie setdements in vieinity

of the site, (b) present-day population with date, Cc) prehistoric and historie populations with

dates. l also omitted several categories from Form B. l removed the category "small island

visible" because of the possibility that islands occur near sites created, as a consequence of

the construction of the dams at the turn of the twentieth century construction and the

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artificiaily raised water level present in 2001. l eliminated the category "water reflection on

rock surface" because l realised that it was too subjective or dependant on factors beyond

the control of the individu al archaeologist. l cut the category cailed "rock fail visible"

because rock fails could have occurred in the previous few years and not in any time period

related to the creation of the images. l excluded a section cailed "mineral offerings" since it

was difficult to de termine whether smail rocks existed on the site naturaily or had been

purposely left there. l merged the category entitled "exfoliation" with "general notes", which

describes the physical state of the rock surface upon which the images exist. l removed the

categories "rocks present at the top of cliff', "rocks present on top of cave", rocks present

on cliff shelves/ shelf', and "rocks present in crevices" because the presence of rocks only

indicates that the surfaces of larger rocks are experiencing exfoliation and wearing away over

time.

The individual pictograph sites associated with this lake vary in geographical

concentration, located in the eastern and northern parts rather than the western and the

southern portions of the Lake of the Woods. Sorne of the southern portion are not in the

Canadian Shield. Most of the known pictographs occur at the base of vertical granitic rock

wails either immediately beside the water or several metres from the water's surface. It is

impossible to date these sites using absolute chronometric techniques. Local indigenous

groups, who daim these sites belong to them, do not ailow removal of pigment samples.

This is unfortunate because analysis of the images for their age and for the paint composition

would be valuable.

Section 1: Numbers of images

Three hundred and eighteen 1mages were recorded. The smailest number at a

pictograph site is one and the largest number is thirty-seven (DhKm-5). Three sites have only

one image: DhKm-19, DiKm-50, and DkKn-6. The average number of images at a site is

eleven. The most common shape is a 'blob,' and seventy-three different types were identified

at these twenty-seven sites. Seven other types of blobs were also connected together or

occurred attached to lines or with curves. The second most popular shape is a 'creature,'

which is an animal-like shape, and there are twenty-three of them, ail slightly different from

each other (see for example Appendix 6).

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Section 2: Defining sites

The presence of the water in and nearby the caves raises the question of how and

whether previous archaeologists recorded the water level and considered whether it may have

changed. The problem of changing water levels relates to the quandary of how to define a

'site'. Clearly, from the discussion in Chapter III, the definition of the size of a site affects

how researchers have recorded the images, taken photographs, and created written

descriptions. Nevertheless, sorne previous archaeologists also presumed that the water level

beside these sites did not experience radical, dramatic changes. They invariably recorded the

water level and noted that the water levels have fluctuated over time occasionally affecting

the recording of sites. Archaeologists concerned with these sites invariably indicated the

drainage system on which the pictograph sites is situated and the type of rock upon which

these images exist. Dramatic shifts in the water levels recorded on the sites have resulted

from large-scale alterations to the drainage system of Northwestern Ontario. The Lake of the

Woods is part of the Winnipeg River Primary Watershed Division. This watershed stretches

from the height of land near Thunder Bay, east of Rainy River into the Lake of the Woods

and runs northwards towards the Winnipeg River. Dams are located on the mouth of the

Rainy River and he ad of the Winnipeg River, at the far north end of the Lake. l discussed the

effect of fluctuating water levels caused by these dams in relation to the water levels in sorne

depth in Chapter II. Changes in the water levels of the Lake of the Woods are indicated on

the rock surfaces. The water level in the summer of 2001 [the year that fieldwork was carried

out] was approximately 75 centimetres higher than the norm. This meant that the

watermarks on the cliffs on the sites recorded in 2001 were the highest yet recorded.

Section 3: What methods were used?

(a) Examination of maps from different periods

To find new sites and to re-examine old ones, l modified the techniques traditionally

used by archaeologists. l needed to know the history of the investigation of each site, and

whether previous archaeologists had investigated such matters as whether offerings existed at

these sites. However, before recording the sites, they had to be located - a serious challenge

given that only a dot on al: 40 000 map indicated a site. Ali the while, l attempted a

preliminary analysis of the data. l quickly learnt that the most recent charts were inevitably

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'idealizations;' tourists and fishing boats who relied on them were often found marooned in

the middle of nowhere complaining about 'uncharted reefs' that had mysteriously appeared.

Furthermore, the scenery in this region generally looks the same, so one easily becomes lost

in the middle of Lake of the Woods.

Archaeologists working in the twenty-first century should realise that they use maps

made during the second part of the twentieth century. Due to changes in the water level, the

shorelines on these maps are different from those observed and recorded on maps made by

different people travelling through the Lake of the Woods sin ce La Vérendreye arrived there

to establish Fort Charles (Burpee 1927). The twenty-first century archaeologist searches for

rock images in a twenty-first century landscape but most of these images were created during

previous centuries, when the landscape was possibly physically quite different. It is possible

that islands in that landscape once formed part of the main shorelines but became islands as

a substantial rise in water level flooded low lying lands. Sites could have been fartheraway

from the water's edge. Rock images may be found in caves that are no longer immediately

beside water. Yet, archaeologists view pictograph sites that are not immediately adjacent to

water as anomalies.

The archaeologist can resolve this problem if he remembers that the water levels

have risen and the shape of that Lake have changed. Therefore, archaeologists should

examine the maps created by White and Meyer between 1913 and 1916, (1916) and make a

visual comparison between them and the modern 1:8 000, 1 :250 000, and 1 :40 000 maps of

the region. The detailed literature review of the Canadian Shield established that pictograph

sites are invariably found on pro minent rock faces, prominent outcrops, and along the shores

of islands, but not in areas of muskeg. Archaeologists traditionally believe pictographs to be

found in places that are orientated east or west, on granitic rocks, and always in association

with water. In locating new sites, 1 kept these key points in mind and examined maps of

1 :250 000, 1 :80 000 and 1 :40 000 for changes in elevation and for geologïcal information. 1

identified every part of the lake where the contour lines were close together on maps, since

these might represent steep cliff faces rather than where reefs, muskeg and swamps existed. 1

established the effect of changes in depth of the water, the nature of the bottom of the

different parts of the lake (whether it was rock or mud), and graduaI changes in water depth

and compared the shorelines of the landscape. The comparison of the different maps

enabled me to estimate how the shape of the land probably had changed when the water

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levels were raised. l needed to carefully examine modern maps to determine the relative

proximity of the elevation lines along the shore edges of each and every landform. Rising

water flooded shallow areas, submerging low-profile archaeological sites, and low-Iying rock

images sites.

Surveying the shorelines and cliff faces revealed many rock faces as potential site

locations, like those depicted in figure 4.1 below, in the area north of the Aulneau Penin sula

and south of the Barrier Islands. The physical features associated with sites invariably include

ledges, overhangs, or large cracks or crevices. Previous archaeologists clearly established the

association between these features and images.

Figure 4.1: Examples of cliff faces examined for pictographs during 2001.

Archaeologists in northern Ontario traditionally have found sites by examining large

expanses of cliff faces on rocky shores of lakes and rivers, where the rock surface faced east

or west and was immediately adjacent to water, or the rock surface plunged direcrly into

water. They also relied upon information gained from local informants. Dewdney's notes,

held by the Royal Ontario Museum, show clearly that he relied upon informants to find sites

in the Lake of the Woods and throughout the Canadian Srueld.

Two new sites were discovered near already known sites, indicating that previous

archaeologists did not always systematically examine the vicinity of known sites. DhKm-20,

in figure 4.2 below, a new site found in 2001 is located on the opposite headland from where

Dewdney recorded DhKm-18 in 1960. DiKm-49 was found in 2001 in a cave berund DiKm-

3, wruch Dewdney recorded in 1953.

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Figure 4.2: DhKm-18 (an "old" site) and DhKm-20 (a "new" site).

Attempting to find new sites in this landscape involved using the services of a team

of professional divers. The divers examined thirteen specifie cliff areas that we suspected

were completely or partial1y submerged sites. The list is as fol1ows:

1) the rock face at the base of and around DgKl-2 in Sabaskong Bay.

2) the rock face at the base of and around DgKl-1 in Sabaskong Bay

3) the rock face at the base of and around DgKl-17 in Sabaskong Bay

4) the rock face at the base of and around DgKl-19 in Sabaskong Bay

5) the base and the length of the cliff face from just south of DhKm-4, including

DhKm-l and north of this site in the southern part of Whitefish Bay.

6) the entire length of the base of the rock face at the base of the headland near the

entrance of Atikaminike Bayon the eastern side ofWhitefish Bay.

7) the base of the rock face upon which DhKm-3 exists

8) the rock face at the base of and around DiKn-l on Hayters Peninsula

9) the entire rock face south of and at the base of the cliff on which DiKm-3 exists

10) the base of the cave where DiKm-49 exists

11) the entire rock face south and north of DiI<Jn-51 and the base of the cave cal1ed

DiI<Jn-50 on Horseshoe Island

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In other cases, the divers also wanted to investigate sorne submerged cliff faces

which they thought had potential for pictographs, so I could deterrnine whether they were

sites or not. The map in figure 4.3 indicates where underwater investigations took place.

Aubeau hoin1mla Wh·.

1h'Im~

Pit:tognph Sitefi Areas investigated underwmer

Figure 4.3: A map of where the diving took place.

Several of these divers, who dove professionally in the Lake of the Woods, had

encountered sorne of these rock faces while working. Diving in this region is important. The

Lake of the Woods is used as place to train and certify divers for diving under the ice in the

win ter, since sorne areas of the Lake do not have strong currents. Sorne of the Lake is free of

ice during the winter because of fast currents, including sorne areas where pictographs are

located or are covered only by thin ice. The divers conducted this reconnaissance work under

the terrns of my archaeologicallicence issued by the governrnent of Ontario. A diver below

the boat, beside the cliff face, used an underwater camera pointed at the rock surface. While

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~ ..

viewing a TV screen of what was on the rock surface below the water level, l indicated to

another diver at the surface where l wanted the camera pointed. The te am a1so searched

underwater for artefacts, caverns, piles of rocks, or anything not geological in nature at the

base of each cliff face.

Although we checked places where we or the divers thought sites might exist, we

found none.

The divers inspected the base of the cliff face of eight known pictograph sites:

DhKm-4, DhKm-5, DiKm-3, DgKl-2, DgKl-1, DgKl-17, and DgKl-19. Offerings above

water existed at all of these sites, ranging from tobacco at DhKm-4, DgKl-1, and DiKm-3, to

clothes, smallliquor botdes and tobacco at DgKl-2 and DhKm-1. Occasionally, we noted a

striking difference between the offerings left at the site and those found below it. The next

chapter presents and discusses these offerings.

(b) Methods for collecting data

We used exacdy the same methods for recording data both at known sites and at

newly discovered sites. l devised the forms after reading numerous field reports of rock

image sites and the guidelines published for the creations of collections of architectural

drawings (Porter 1994). Pictograph and petrog1yph sites are large three-dimensional

structures in the landscape, like buildings. Therefore, studying how arcrutects collected,

recorded and archived information became a logical step. l used Form A to record

information on the physica1 structure of the rock surface and the information required

according to the terms of my archaeological licence from the Ontario Government

(Appendix 3). l devised Form B to record the images as a whole unit rather than separately

(Appendix 3). Confidentiality issues arose as a consequence of the licence requirements by

the Government of Ontario to conduct archaeological surveys or fieldwork in the Province.

l am responsib1e for keeping the particulars of the locations of the site(s) found under this

licence confidential and not allowed to publish or release to the public, in any format, the

particulars of the locations of these site(s). l must supply, however, detailed information

concerning the locations of site(s) to the Ontario Ministry of Tourism, Culture and

Recreation on Archaeological Site Record Forms or the Archaeo1ogical Update Forms. Prior

to recording each site, either l or my assistant 1eft tobacco, a common practice among

archaeologists in this region.

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Form A recorded the location and the physical context of each site. The Borden

number must be included, likewise, the names of the recording archaeologists and the date of

record. Form A contains similar information ta that required by the official Borden form

each archaeologist licensed by the Ontario government submits after the completion of

fieldwork. The foilowing information must be included for ail sites: the Borden number,

recorder's name, date, preferred site name, other names, name of township, concession,

county or district, location, access, and settlements. l developed both forms prior to

conducting fieldwork, but modified them after physicaily examining the first few sites.

If an official name does not exist, the archaeologist should try to ascertain from

inhabitants of the region if a local name exists. Two sites, DiKm-SO and DiKm-Sl, are on

the southwestern shores of an island thought by local inhabitants to resemble a horseshoe

and, therefore, cailed Horseshoe Island. However, trus name, like that of Tamarack Island to

the north of it, is not recorded on the 1 :40 000 map.

l will present the information obtained about DgKl-2, in the photograph in figure

4.4, to illustrate the information coilected in Forms A and B.

Figure 4.4: Overview of DgKl-2 taken in 2001.

DgKl-2 was examined several times. The first date indicates the first examination; the

second, the divers' expedition to determine whether offerings existed below the surface of

the water, and the trurd date indicates when W. A. Ross, the regional archaeologist and l

examined the paintings and the offerings. He wished to see for rumself the new paintings and

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the large quantity of offerings present at this site in comparison to the other sites found in

the Lake of the Woods.

Borden Number DgK1-2 Recorder M. Bell & A. Coison Date IJuly 4/01, August 5/01, August 24/01 Place Name The Three Caverns Pictograph Site

(Pastershank 1989) Alternate Site Names None Previous Site Names Dewdney's Site # 198 (August 20d 1964)

We recorded the current place name as well as prevlous place names to enable

archaeologists to track each site by name or Borden number. The Borden number was

provided for a known site. Until l obtained a Borden number from the Ontario Ministry of

Culture and Communications, l left this section blank when recording each of the new sites.

The next categories enable the archaeologist to indicate the precise geographic

location of the archaeological site in question. The spatial co-ordinates category records

longitude and latitude. After fieldwork at the end of the day, l added additional data: NTS

grid location, and site elevation.

Figure 4.5: Physicallocation of DgK1-2 in Sabaskong Bay, Lake of the Woods.

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The "geographical notes" section enables the recording of further information about

the topographie setting of the area. The archaeologist here identifies the local name, if one

exists, of the place where a site exists.

Geographie Notes It lies on a rock of land whieh is on the main route to Sabaskong Indian Reserve IR 35D on Crow Portage Bay, main channel from Splitrock Narrows to Sabaskong Bay. It is opposite island with a private eamp (no name) and near the turning to be taken to the Nestor Falls government dock.

Information about present day nearby settlements must be gathered so that the

archaeologist can if, she so wishes, consider whether sites always occur in the vicinity of

specifie types of settlements. The word 'near' implies that site is within 6 miles, or

5.21385744 nautical miles, or 9.6506404 kilometres by boat from either the nearest

settlement or reserve. The journey would only take up to 15 to 20 minutes by boat to qualify

as 'near'.

Present Day Nearby Settlements It is near the entrance to the harbour of Indian Reserve 35D and the township of Nester Falls

It is important to state whether the landmass is a peninsula, an island, a narrows, or

mainland and to record its name.

ILand Masses IPeninsula - Sabaskong Peninsula

Since it is possible that not ail the pictographs can be recorded from a boat, l

included the space "Access" to record the method of visiting these sites. DgKI-2 was one of

several sites that could be recorded partially by standing on the rock ledge immediately in

front of sorne of the images.

Access

The archaeologist must supply information concerning the regional drainage of the

water system in the geographical region in question.

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,---------:----------------~ ,------------------------

Regional Drainage Water Systems (direction of Crow Portage to Sabaskong Bay to Little flow) Traverse Bay to Big Narrows to Kenora to

Winnipeg River to Nelson River System to Arctic Ocean.

1 think that the archaeologist should attempt to determine the uses of the adjacent

body of water and speculate about the period of said use in years. The uses of the body of

water can relate to the presence of fish, waterfowl, ungulates and how the land in the vicinity

of the site is currently used for recreational purposes. This commentator stated that the water

has been used for travel (communication), the transport of people and goods, recreation and

fishing (both personal and commercial). A time frame of three hundred years plus was given

for the period of use of this body of water, sin ce this covers the historie period from when

European observers first arrived in this region.

Uses of Body ofWater Communication, transportation, fishing, recreation, wild rice?

Period of use for body of water (in years) 300+

The presence of water on the number of sides must be noted at the site to allow the

archaeologist to indicate whether there are paintings on multiple sites of a rock face or only

one side.

IPresence ofWater (on # of sides) Il side

The type of body of water next to or nearby the pictograph site must also be identified (i.e.

lake, river, stream, channel or ocean) and its name given.

IBody of water surrounding/ adjacent to site ILake - Crow Portage Bay

The archaeologist should indicate whether the water freezes or not during the win ter,

whether possibilities existed that the water level fluctuated at the site, what and/or who

caused these fluctuations, when they occurred that year, and whether major changes had

occurred in the water level and for what reason.

Freeze/Partially freeze in winter Water Level Fluctuation (yes/no) Cause of water level fluctuation

Freeze Yes Dams, lncrease ln precipitation, artificial control of water levels by Lake of the Woods Water Control Board.

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Extent of Fluctuation ~inches Eer annuml Estimate of Average of75.96 cm /6"- 2' Control ofWater Levels by whom/what? Lake of the Woods Water Control Board -

dams Season ofWater Level Fluctuation Spring/ early summer. Major Changes in Regional Water Level (in Rise ln water level ln 1888 caused by years) building of Rollerway in northern part of the

Lake of the Woods -123 years ag9

It is important to indicate the number of water levels visible on the rock and their height

relative to the current level. If there is only one visible it must be the current one.

IVisible Water Levels (number, height) Il (currentl

The location of the pictograph(s) must be recorded, i.e. whether the paintings occur on cliff

faces or in caves.

Location (cliff faces / rock outcro s/ caverns/ out of water

Cliff face

The final category in this section, "general notes," allows recording of any additional

information that the archaeologist thinks should be collected.

1 General Notes INone

Form B's first three categories are the same as Form A's, since the Borden number

of the site, the name of the archaeologist and the date when this site was examined should be

noted. l devised Form B to consider the sites and the images as a whole unit rather than as

separate units. l recorded the rock face with images as single large unit rather than as

separate units to avoid smaller groupings being arbitrarily imposed by the archaeologist on

the images. l first described and recorded each rock face in terms of its physical attributes.

Then l described the images present.

On Form B the archaeologist also indicates the units used for any measurements

taken, i.e. metric or imperial. He assesses the type of rock. Information from the

archaeologist, and subsequently from geological maps, may be distinguished by names beside

the information recorded.

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Figure 4.6: Field drawing of DgK1-2 by M. Bell in 2001.

Type of rock Granite. Ice and water eroded Archean granite (Mining, G. V. and Sharpe, D. R. 1991 Surficial geology, Rat Portage Bay, Ontario: Geological Survey of Canada Map 1770A Scale 1: 100 000)

The contextual approach reqwres that additional information about rock types

gleaned from geological maps of the region must be added later. The number of cliffs or

caves and their height must be indicated.

Number of cliff(s) 1 Height of top of cliff(s) from present day 13.73 metres water level Number of visible water lines 1 fcurrent) Height of top of cliff(s) from visible water line 13.73 metres

The height of the cliff from the present day water line must be recorded. The information

for caves is different since these paintings were not created on the surface of a cliff face. The

number of caves must be counted. The distance from the roof of the cave to the present day

water level, as weil as the height of the cave must be measured. The former measurement

may seem odd for caves, but two were found in close proximity to water. High water levels

could cause the water to enter the inside of these caves. The width of the cave must also be

measured.

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The vegetation at the top of the cliff faces, on the side and/or at the surface and base

of the cliff and the cave should be recorded. The archaeologist must determine whether

vegetation over paintings hinders their visibility from the water, and whether it contributes to

the graduaI deterioration of the cliff face and images. The type of vegetation must be noted,

because it is possible that it has been removed or changed over time.

Vegetation of tOE of cliff~s) Birch, jack pine, juniper, sedges Vegetation on side 1 surface of cliff( s) Birch, white pine, bracken fem, grass, rock

tripe, lichen Vegetation on base of cliff(s) None -water

Since the presence or absence of features such as ledges, overhangs and large cracks,

crevices, and deep holes is important for finding pictographs, they should be described if

they are present, particularly if they exist close to each other as weIl as the paintings.

Rock overhangs Yes = 1 (big one - 2 metres deep) Proximity of rock overhangs to one another NIA Proximity of rock overhangs to paintings Above painting§, sorne on overhang Large cracks Yes = 3 diagonal, 1 horizontal Proximi!f of large cracks to one another Refer to photograph Proximity of large cracks to paintings Through 1 beside Large crevasses Yes = 1 large horizontal Proximity of crevasses to one another NIA Proximity of crevasses to paintings Above paintings Rock shelfl shelves Yes = 1 very big one at base of cliff Proximity of rock shelfl shelves to one another NIA Proximity of rock shelfl shelves to paintings Below paintings Rocks present at base of cliff(s) Yes and they are very big

As mentioned, l removed several categories initially devised prior to conducting

fieldwork. lnitially, archaeologists were required to record the specific orientation of the rock

surface at different parts of the cliff face. l initially amalgamated these readings into a single

category called orientation, implying that a reading be taken giving the orientation of the rock

at the location of the paintings' site. l found applying this category very difficult in the field,

even though l had devised it because several archaeologists (e.g. Pastershank 1989; Rusak

1991) had noted that sorne sites face particular compass directions.

Number of angles of painted face + location 15 (base, middle, to )

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Orientation of angles (NSEW) 1 = 180 (S), 2 = 180 (S), 3 = 90 (E), 4 = 101 (E), 5 = 139 (SE), 6 = 120 (SE), 7 = 99 (E), 8 = 150 (SE), 9 = 140 (SE), 10 = 100 (E), 11 = 120 (SE), 12 = 120 (SE), 13 = 160 (SSE), 14 = 130 SE, 15 = 189 SW)

In the case of caves, the orientation of the cave opening should be recorded.

A category exists in which the archaeologist notes whether offerings were made at

the site, both under and ab ove water. These must be recorded in the same category

regardless of where these offerings occur.

Offerings Yes = I<ids' and adults' clothes (pants, skirts, t-shirts, socks, chenille sweater, Bannel clothes - sorne old, sorne new) , dried food stuff, bandages, earring (mother of pearl with porcupine quills and silver and blue beads), earring - plastic heart (never in pairs), tobacco, empty tobacco container ("Copenhagen Tobacco"), beer bottle glass, clear glass, "Prayer Sticks" ( 26 bundles of 12, 12 cm long by 12.5 - 17 cm wide, tied together with white cotton string, half of each stick painted blue and the other half painted red, large diameter sticks always tied together and small diameter sticks always tied together - never mixed, 1 bundle of 12 in the left-hand cave, refer to field sketches and digital and manual photographs).

More offerings were left on the rock bench under overhang when we came back later to record more photographs; modern paintings also visible at site. Returned August 5th 2001 with a team of divers who discovered the rocks immediately below and the vicinity around the rock art site. They discovered that it was a mud bottom and that there was a pile of rocks but no offerings were evident, only a Mountain Dew soft drink can, a man's bicycle and another cavern below the water level to the right and 2.14 metres below the surface of the water.

The methods of recording the site must indicate the techniques used.

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[MethodS of Recording Digital images, photographs (colour), field notes, field drawin

Place details concerning the weathering of the rock surface, exfoliation, any white mineraI

deposits, rock tripe as weil as lichen encroachment and growth, or any oddities used in the

creation of these images in a final section, "general notes."

General Notes -- ----_.-

None of the images identified by Pastershank 1989 can be identified with exception of the two handprints because 0

white mineraI deposits over the surface of the rock. However, new images exist in modern red paint most probably created using a spray cano One of the paintings-an animal shape overlies the ochre smear under the large overhang, while two of the new motifs are beside the ochre under the overhang. The fourth new image at this site differs sin ce it is an outline of an animal shape in red spray paint, which is hoilow. It was not painted using a paintbrush but a spray can like the other new images. However, it differs in location since it not above or nearby the offerings under the rock overhang but on the side of the overhang exposed to the elements and it is difficult to see. Exfoliation resent.

AIl of the field data were entered into Excel spreadsheets to keep an electronic record

of this information, and to establish quickly and easily whether patterns emerged.

(c) Image analysis of potential sites in the field

We examined potential pictograph sites to determine whether ledges, overhangs,

large cracks, crevasses, or deep holes existed. Often it was doubtful whether a site existed or

not because of the difficulty in distinguishing pale ochre from a pink coloured granite

surface. To establish reliably whether the 'redness' seen was just the colour of the rock or

ochre, l employed photographic tools. The red/orange patches on the photograph below is

not ochre but orange coloured lichen.

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Figure 4.7: Red/orange lichen on the western end ofCrowrock Island.

The travel time involved and the weather forecast must be considered to determine

the best time of day to take photographs of the sites and surrounding areas. We used a Sony

Cybershot DSC-S70 digital camera to confirm whether a pictograph site existed. Each

evening, we downloaded TIFF files and conducted preliminary analyses of potential and

known pictograph sites using Photoshop 6.0. By employing the enhancement tools available

in this software, we could establish whether what we suspected, from examining the site in

the field, might be faint ochre was in reality an image or a collection of images. By

controlling the colour ranges from a part of a weIl known site caIled DjKn-l, visible in figure

4.8, where the red ochre was very strong, we could identify images that had either faded or

become obscured by the visible white mineraI washes.

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Figure 4.8: Part of DjKn-l used as the control me.

However, these enhancement tools could not detect images existing below lichens growing

on the surfaces of the cliffs themselves.

Once we had discovered that very faint images existed, we returned to the site in

question to survey and record them. We discovered that in-depth photography using manual

cameras demonstrated how the different images related to each other and to the surface on

which they lay. The digital camera was less valuable in this aspect of the work, since the size

of the file and relatively small quantity of memory, together with the distance between sites,

meant that using manual cameras was easier. Furthermore, despite aIl the advances in digital

technologies, it was still difficult to fully control the lenses and the aperture. The camera

settings provided by the manufacturer dictated the extent that one could collect raw data in a

digital format. Digital cameras must develop to broaden the use of lenses.

Image files obtained from the digital camera were recorded as TIFF files and burned

onto CD-ROMs each evening. The images were recorded as Tagged Image File Format,

which provides the purest form of image currendy available. This format allows the use of

the new techniques developed by the Intelligence, Agents and Multimedia Group directed by

Professor Wendy Hall, at Southampton University, who advised me on this aspect of my

research. TIFF files are compressible, retrievable, and stable. JPEG image fùes, in

comparison, lose data when compressed. TIFF fùes can be used in a non-proprietary format

with the viewing programme not being controlled by a single vendor. The final advantage is

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that this format is extensible; hence it can evolve over time to meet the changing needs of

different users and does not require new software for viewing files. The Kodachrome slides

produced with the manual cameras were scanned, saved as TIFF files and burned into CD­

ROMs. Two copies were made of each CD-ROM.

Section 4: The method used for describing shapes and how does one consider time

Time, the age and the shape of the images are interrelated because the physical

outline of an image changes as it gets older. An image should not be considered static with

regards to its physical shape since its physical outline changes over time. Time must always

be considered since neither the rock nor the images are static entities. However, none of

these images can be dated using absolute chronometrie techniques.

Unfortunately exfoliation, fading of the images, deposition of white mineraI deposits,

and lichen and rock tripe growth and encroachment affect the images. Each must be

discussed.

(a) Exfoliation.

Exfoliation of the rock surface occurs because the rock surfaces upon which the

images exist are affected by more than the fluctuating water level of the Lake as discussed in

chapter II. Rusak (1992a: 25) strongly asserted that pictograph sites in White Otter Lake, a

lake east of the Lake of the Woods, were "in a po or state of preservation" since in sorne

places the rock had exfoliated "to a depth of several milimeters". She concluded that this

occurred when dams to the north- and southwest artificial1y raised the water level. The

Shevlin-Clarke logging company constructed these dams in 1912 to aid the transport of logs

down Turtle River from White Otter Lake. However, extreme temperatures also contribute.

Exfoliation occurs when granite starts a hydration process in which the rock breaks, splits,

and peels as a result of expansion in salt crystals and/or water present in smal1 cracks in the

rock surface.

Mean temperatures range between 12.5°C to 14°C in summer, and -17°C to -12°C in

winter. This region experiences a maximum period of between forty and sixty frost-free days.

Snow accumulation in the Boreal Forest is higher than in the neighbouring Great Lakes-St.

Lawrence Forest. Snow coyer can last for six months.

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Taylor, Meyers and Wainwright (1975: 88) argued that freeze-thaw, often called frost

action, caused exfoliation of the rock surface at sites. Essentially, the outer layer of the rock

expands and contracts with the dramatic changes in tempe rature s, causing small cracks.

Moisture accumulates in these cracks. Over time, this moisture freezes, expands, and thaws

causing the rock surface to become weaker and break away from the main body.

However, the question exists whether pictograph sites which have paintings near the

water level would also be affected by the movement of ice during the winter and spring

breakup. Two views exist regarding this question. Sorne argue that the growth rate and

stability of ice is different depending on where the ice is situated in the lake. Bays would have

more stable ice sheets than channels because the water in a channel has a high velocity

(Layman pers comm. October 2002). Water flows faster and more efficiently in channels

than in bays; hence bays provide a "more conducive environment" for the growth of an ice

sheet (ibid.). Those pictographs existing on cliff faces in protected bays are more likely to be

affected by the movement of ice sheets than those sites that exist on rock surfaces beside

channels. This is because the ice will shift more times than in the bay and take a longer

period of time to increase in volume. The second opinion is that ice in bays and other

current-free areas can bec orne ice sheets but during break-up and freeze-up it does not shift

much unless it is broken. This is because the ice just sits there and either just builds or melts.

The rare exception to this rule could occur at break-up during a strong wind if bays were

relatively sheltered from all but one direction. Therefore, bays that had cliffs that faced the

prevailing wind, which is northwest, but were otherwise relatively sheltered would be free of

ice. In areas where a strong current exists then ice is swept through the channel, piles up, and

becomes huge pack jams that rub and grind against each other and the shoreline. Free

flowing ice floes still moves along the shore.

(b) White mineraI deposits

Groundwater leaches mineraIs identified as potassium, calcium, sodium, silicon, and

aluminium from the soil and cracks in the interior of the rock. Sorne of this water flows over

the paintings during the spring thaw or after heavy rainfall (Taylor, Meyers and Wainwright

1975: 88). Sorne of the groundwater evaporates as it runs down the rock face leaving an

"insoluble minerai deposit 'skin' on the rock surface" (ibid.). Taylor, Meyer and Wainwright

maintained that, initially, this deposit is invisible but as it repeatedly accumulates it becomes

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white. No one has established the deposition rate at which these white mineraI deposits

accumulate.

Taylor, Meyer and Wainwright argued that the creator of images couid essentially

place images on these white mineraI deposits rather than directly on the rock surface. To

establish the structure of the pigments on the sites in question, they examined several

samples using a scanning electronic microscopy. Chapter III includes a discussion of this

work. Wainwright and Taylor (1977: 31) also used scanning electron microscopy to establish

the structure of the pigment of two samples from two sites. Analysis of the cross-sections of

the two samples revealed distinct, almost parailel layers (ibid.). Wainwright and Taylor

posited that a chemical or a physical process separated the original pigment into distinct

Iayers. They concluded that the pigment must have migrated within the deposit because the

the samples had been taken from images that appeared not to have been repainted.

(c) Lichen and rock tripe growth and encroachment

Taylor, Meyers and Wainwright (1975: 89 asserted that lichen and algae probably

increased the rate of decay of rock images. Lichens do not con tain chlorophyll as most plants

do. Instead they consist of symbiotic fungal and algal cells (Blackmore and Tootill 1984:

209). They live in areas where other plants cannot survive and grow very slowly.

Several species of lichen grow on the surfaces of rock in this region, including

Xanthoria elegans, or rock orange lichen Oohnson, Kershaw, MacKinnon and Pojar 1995: 338).

It appears in places where there is a vast quantity of calcium and nitrogen. Although often

found in conjunction with cliff-dwelling birds' nests (ibid.), 1 did not find any birds' nests

upon examining the pictograph sites where this lichen grew. Xanthoria elegans grows rapidly,

but its growth rate apparently depends on its habitat. It has been used to date surfaces.

Two types of rock tripe, a type of leaf lichen, were found. Umbilicaria vellea, or

Forested rock tripe (ibid.: 351), grew at the majority of sites. Umbilicaria muhlenbergzï, or Plated

rock tripe, also grew at sorne sites. Umbilicaria vellea occurs in conjunction with sorne

moisture seepage. Both occur on acidic rocks in shaded or open places. The

Ojibwa/ Chippewa used both plants as a soup for sick people or made a syrup from them

which was eaten to expel tape worms.

The average lichen arguably grows only 1mm a year (Blackmore and Tootill 1984:

209). McCarthy (1999) critically evaluated ail of the models used in lichenometry. He defined

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lichenometry as the technique which utilises measurements of the thalus diameter to generate

the minimum estimate for the amount of time that "colonized surfaces [of rock] have been

exposed and stable" (ibid.: 379). McCarthy critically examined the biological basis for several

of the assumptions that have been used to interpret lichen-size age data. He (ibid.: 384-385)

concluded that the majority of the lichenographic ages could not be verified. They had not

been produced by methodologies that used widely accepted biological principles. He argued

the importance of considering the species, habitat, density, and space availability as well as

how growth had been affected by other events.

Section 5: Assessing age

Once these images are created and a site exists, it is highlighted as a locale of

importance in both the physical and mentallandscape of regional residents. The moment in

which these images were created is important but very difficult to determine. 'Conventional'

artefacts, once discovered during an excavation, are argued to represent fragments of time at

which specific events occurred. Images, once placed upon the surface of a rock face, become

integrated into the region's time sequence. They do not just represent one instance of time.

Since they can be revisited, reused and repainted, they become part of the mental and

physical record of the geographic region in which they exist. Images often are superimposed

or manipulated, especially if a known group of images is used as mnemonics or vocabulary.

Audiences can use and understand older images in conjunction with those created by

subsequent image creators. Moreover, audiences of these images change and can react

differently to both the images and their locations. The deposition of an item, called an

'offering', acts as evidence of such a reaction. Interaction between images and the people

who subsequently view them is difficult to mark, or delineate, in terms of specific known and

identified time events. The presence or absence of offerings at a site acts as a good indicator

of whether the images present are still being used; of whether they are still part of the mental

landscape of a current cultural group. Subsequent creators of newer images might also draw

upon meanings implied by placing new images on older images for new audiences.

These rock image sites experience seasonal climatic changes, as well as fluctuations in

water levels and temperatures. The sites and their images continually undergo changes that,

though difficult to evaluate on a daily basis, become evident over long periods of time. They

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change in size, and perhaps disappear as a consequence of rock exfoliation, or mineraI

deposition and/ or plant growth over the images.

Section 6: Description of a shape

It is important that the archaeologist should describe, not interpret, the evidence

when recording a rock image site. This operation involves thinking very carefully about how

one describes images, since any description will affect subsequent analysis. She must not

impose any interpretation based upon physical shape. Anyone concerned with the

methodological and theoretical issues relating to the study of rock image sites must describe

the shape of an image objectively, and in detail. Images can be organised and discussed by

their shape. A rock image must be considered as a shape to reduce the possibility of investing

the description with meaning during the recording stage. It is vital to understand the physical

outline, form, and structure of an image before discussing its context or meaning.

Considerable care must be employed when choosing the vocabulary to describe the shape or

form of an image in order to avoid inadvertently or prematurely ascribing meaning(s). A

shape's form should be referenced and nothing more. Meaning must be ascribed at a

different and later level of analysis.

The precise size of an image should not be considered. It is difficult to establish

whether size was an important issue from a detailed examination of the ethnographie record

of the indigenous peoples. The current size of an image may depend upon uncontrollable

elements, su ch as the deposition of mineraIs upon the rock surface, exfoliation, and plant

growth. Nevertheless, the archaeologist should note whether a shape is large or small after

describing it with respect to the other images at the site. Hence, stating that a small, long,

horizontalline or short, vertical rectangle existed is possible.

The arbitrary division of the images painted upon the surface of a rock into parts

must be avoided. Sites, regardless of whether previous archaeologists originally described

them in several parts, were described again, since the archaeologist must only describe, not

interpret, the data.

Ail the images were described from the left- to right-hand side of the site, using ail

the digital and manual photographs that l had of each site. Since describing the images from

left to right prevents the sites from being subdivided into sections, terms such as face and

panel become redundant. If a site is physically broken into sections because images spread

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across related or nearby rock surfaces (which occurs at DhKm-18, DhKm-4, DgKm-2,

DhKm-50, DgI<1-17, DgI<l-19, DgI<l-l, DhKm-5, DgI<l-2, DiKq-2, DjKq-23, DiKn-1,

DgI<l-2, DhKn-1, DjKn-1, and DhKm-1), the archaeologist must not rein force these

divisions by describing the images in groups bounded by their physicallocation. It is possible

that these subdivisions were not important to the creator of the images.

While describing the shapes, the notion of continuous time also must be considered.

It is important to note uncontrollable elements that affect the size of images over time:

exfoliation, lichen or rock tripe encroachment, and white mineraI deposits.

1 had to consider carefully the vocabulary that 1 used. 1 drew upon the work of ]aritz,

an art historian interested in the every-day life and the material culture of the general

populace, and not the aristocracy, of the Middle Ages to help me think about how to

describe the images. His research data consisted of medieval paintings of every-day life,

forcing him to undertake highly detailed descriptions of complex images. Standards for

describing an image do not exist, as ] aritz and Schuh (1992: 144-145) observed. Despite the

fact that many proposals exist, none of these standards is widely accepted by the academic

community who describe and deal with images as potential sources of information. They

offered five reasons for the lack of standards:

1. formaI language could not easily discuss the specifies of an image,

11. different interests and consequently different approaches existed for different art

historians,

111. there are considerable gaps in "certain areas of terminological research" (ibid.:

145),

IV. there exists a "fear of losing flexibility and openness by using a system of strict

standards", and

v. the different techniques used by academics who need to analyse varying amounts

of pictures for their research (ibid.).

]aritz and Schuh offer suggestions for creating standards which 1 think are reasonable, given

that the images they considered were European, while the ones 1 was describing belonged to

a different cultural tradition.

Therefore, 1 decided to use a vocabulary that implied as little meaning as possible,

and that described only the physical outline of an image. My goal attempted not to permit

any supposition concerning poorly preserved or ambiguous figures. A technique must be

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used to de scribe these images, even ones that are terribly faint. When describing a shape, one

should consider its present form and nothing more. Smears, blobs, and spots exist and must

be treated as described.

It is impossible to describe a stick figure without reference to terms such as arms,

legs, horns, ears, head, and body. The key point is that a stick figure should not be called an

anthropomorph, or a hum an or spirit figure. These words could be misconstrued at a later

date. The image could be interpreted as the representation of a human being, when, in reality,

its painter intended it to represent something other than a human.

l examined the TIFF flle of each site using Adobe Photoshop 6.0 while the images of

each site were being described. This enabled me to examine areas of rock surface that had

white mineraI deposits perhaps coating over the red images. Occasionally, this revealed

hitherto undetected "new" images at long-known sites such as DiKp-1, as shown in the

photograph below in figure 4.9.

Figure 4.9: DiKp-1 in June 2001 annotated by Cols on in 2002 to indicate locations of previously unknown images.

This photograph has not been altered. Red images clearly exist above the area where images

described by Ashdown (1973), Lawson (1885) Dewdney (1959), Reid (1976) and Molyneaux

(1975) were traditionally known to exist.

Presupposition must be avoided concerning poorly preserved or ambiguous figures.

Finding the precise edges of each image was not easy. Zooming into the TIFF flle of each

site and using the various tools available in Adobe Photoshop 6.0 such as hue/saturation,

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desaturate, brightnessj contrast and colour balance tools aided my search (see Appendix 2 for

examples of what each tool does to a selection of the images from DiKp-1). However, l also

empIoyed VIPS, an image processing package4. This software highlighted the problems of,

and assisted in describing poorly preserved or ambiguous figures. It also highlighted several

features that aided their written description, as l will discuss below.

Section 7: The tools used to aid the analysis of the data

Several computing tools were crucial in undertaking data analysis. KLEIO lAS, a

database management system, Adobe Photoshop 6.0, and Vasari Image Processing, both for

image manipulations, served as the main software tools. l used the database tool to link

information about rock image sites with photographs of the sites. The image manipulation

tools aided my search for patterns in images and groups of images.

(a) KLEIO lAS

KLEIO lAS enabled me to connect my written descriptions of each image with its

electronic record.5 Originaily designed for medieval specialists, the software had a Latin

command language, with documentation in German. An English-Ianguage version became

available in 1993; l used the latter version. The software allows the researcher, usuaily an

historian, to enter information in a structure that reproduces that of the original document.

This preserves valuable information about the document, while ailowing the selection of a

method of organizing the data after the data-gathering process. It is possible to minimise

coding or mark-up on the digital record of a source prior to analysis, preserving features of a

document that may sustain conflicting interpretations.6

KLEIO lAS can manage different types of documents, induding image files. The

programme stores ail records in a manner that preserves context among records, but these

can be defined as logicaily equivalent for processing (1993: xiv) (see Appendix 4). The most

abstract group of sources must be at the top of KLEIO IAS's hierarchical structure, and the

most concrete group of information at the bottom.

4 More than a simple set of routines it is an image processing framework which is used in student projects and PhD research at Southampton University (http://www.vips.ecs.soton.ac.uk/ 26th November 2004).

5 The image ftles were produced in the TIFF format, a non-proprietary ftle format compatible with most image processing software. 6 KLEIO usually runs under UNIX, not Windows.

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Three levels of information exist: documents, groups, and elements. Documents are

the highest level of information and can be organised into groups that are abstract groupings

of information in the document. The term, 'documents,' corresponds to the type of

information being described. The historian designer used this term to imply that, at this level,

information be provided as to the document type examined, such as census records, parish

records, or paintings. Documents consist of groups which correspond to rows or records in

other traditional database systems. Each group in KLEIO lAS has a specified relationship

with others in the database specified by the user. This relationship can be quite complex,

since several groups may be dependent upon a higher group, and the same group name may

be used elsewhere in the database. Groups are related to each other in a hierarchical fashion.

Each group of information contains elements pertinent to that group. Elements are the

smallest unit of information that KLEIO lAS can access. lt is possible for these groups to

contain identically named elements, allowing these related elements to be 'implicitly joined' if

the system suspects that the user might bene fit in considering both elements as of the same

type (ibid.: xv). Elements can consist of any number of specified entries, or any type of

specified information.

KLEIO lAS offers a collection of basic algorithms to deal with data. This enables

assumptions about the data to be included in the database independently of the data itself.

Thaller (in Woollard and Denley 1993: xvi) argues that these algorithms constitute a form of

expert system that makes use of context-sensitive data. This system provides a detailed set of

basic database operations, such as data retrieval and report generation. The researcher can

move easily, therefore, through highly complex structures, and obtain results to complex and

unwieldy queries. He may even join different databases.

The file that specifies the structure of my data defines eight databases, of which l

have needed to use only four (see the file in Appendix 4). Each database contains a specific

type of data, and each is subdivided into several parts. The data file con tains all the site

information collected in the field, including information gathered in forms A and B, and the

textual description of each image from each site. The image flle contains the images

themselves. This flle also references the textual descriptions in the data file. Hence the user

can query the database either from the textual records or from the images.

l wrote and stored all of the image descriptions in KLEIO lAS. l also stored the

information collected as to the contextual details about the sites and their physical features in

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KLIEO lAS. The database contains all the information gathered in the two forms, A and B,

and the detailed descriptions of each image that existed at known pictograph sites in the Lake

of the Woods.

(b) Image analysis using Adobe Photos hop 6.0 and VIPS

1 conducted a preliminary analysis of the image files while collecting site data in 2001.

The analysis, done with Photoshop 6.0, revealed that a limited range of motifs appeared in

the rock image sites. It also increasingly provided sorne insight into the way in which human

beings perceived a physical shape. Close examination of each image revealed that perception

of its precise physical shape could depend upon the viewer rather than upon the presence of

red ochre. 1 confirmed this by using a second image processor, Vasari Image Processing

Software [VIPS],7 which is used by a number of world-class museums and galleries. The

National Gallery in London England uses it for most of its imaging research.8 A large

number of research projects analysing large images also have employed VIPS (Martinez, et.

al. 2002, Martinez 1991). 1 loaded the image files collected during my 2001 fieldwork season

onto a server to process them using this software.

Each shape, each graphic shape in red ochre, in each TIFF file, was extracted with a

'slider' tool built by Dr. Kirk Martinez. Image processing software assumes that the image

photographed was on a flat surface perpendicular to the camera, and not upon a slanted or a

curved surface. The slider allows for sorne control of images that do not meet these

requirements. It permits me to process each graphic shape independently. In fact, none of

the images at each site occurs on flat surfaces truly perpendicular to the camera. For this

reason, the colour saturation of each image is uneven. Preliminary image analysis conducted

in the field had already indicated this. It became clear that the different angles of each rock

face had an effect on the quality of the image obtained.

On the image of a given site, graphic shapes may rest on surfaces that are at different

angles to one another. If all the graphic shapes are processed at the same time, using the

same settings, results differ for each of the visible red shapes on a given image. The slider

enables me to change and alter the hue saturation levels according to each individual ochre

shape rather than for a group of shapes. The slider also assists in writing descriptions of

7 The VIPS software was developed by Dr John Cupitt and Dr Joe Padfield (The National Gallery, London) and Dr Kirk Martinez University of Southampton (http://www.vips.ecs.soton.ac.uk). 8 VIPS runs under UNIX.

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graphic shapes. However, l find turning the graphic shapes into black and white images the

most useful technique for the description of the shapes themselves. The software reveals that

shapes often have indistinct edges. It highlights the role that the human eye and brain play in

the process of recognizing images.

Conclusion:

Although these software tools were complex and technically challenging, they

enabled me to examine systematically the textual and visual data that l had collected, and to

gather the maximum amount of information possible about these pictograph sites.

Section 8: Vocabulary used to describe each type of image found

l attempted to use a nested classification for describing these images. The images

were described from the perspective of an individual standing or sitting in a canoe

immediately in front of the site and the image in question. The angle or the slant of a line

was not obtained because it was not in reality straight once it was examined using VIPS.

Furthermore the slant would also depend on the angle of the photograph taken. All the

photographs were taken using the water level as a horizontal baseline.

The question obviously arises as to how l would describe a shape such as the following:

+ x l described this shape as two short lines, one horizontal, and one vertical, crossing at a ninety

degree angle. It is not necessarily, or even probably, a 'cross,' as it is frequendy designated in

the literature of the rock images of the Canadian Shield. Since the creator of this image was

not necessarily someone who held the J udeo-Christian concept of a cross, no good reason

exists for it to be labelled as a cross. Interpretation is embedded in that word. If it is

diagonally depicted it should be still described as two short lines crossing each other at a

ninety degree angle, or, possibly, diagonally.

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l designated this shape as a series of horizontal short lines one above the

other with two vertical lines at either end of the horizontal lines. It should not be called a

"ladder", a "Midewiwin ladder" or a "lattice" and the short horizontal lines should not be

termed "rungs".

l described this shape as a series of short horizontallines one above the other.

Neither should it be labelled as a "ladder", a "Midewiwin ladder" " or a "lattice" and the

short horizontal lines should not be termed "rungs". If the short lines do not occur in close

proximity to each other they should not be considered as a unit.

Both of these images should be called diagonal lines

and no comment should be made regarding the angle. Any comments made as to the angle

may be linked to interpretation.

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l term both of these shapes triangles even if they

occur in conjunction with other images such as stick figures where there is a temptation to

refer to them as 'hats', especially if they are on the 'heads' of stick figures. The commentator

must record whether the shape is hollow or not.

s t , n • S .3 !~

Ali these shapes are of creatures. Images that have vertical rather than horizontal bodies

should also be recorded as creatures. If the creature has short lines sticking upwards on the

head they should be recorded as ears, horns or antlers. The commentator must record

whether the shape is hollow or not.

A shape loosely categorised as 'bird' differs from that loosely categorised as 'turtle' or

'creature' because of its different physical outline. The curved, downward pointing, usually

horizontal, perhaps vertical or even diagonal lines emanating from either side of the central

body of the shape distinguish that loosely categorised as 'bird' from 'creature'. The lines

emanating from either side of the shape's central body should be termed "a wing." At one

end of the body shape, a small triangle should exist; one of the triangle's points labelled

'head,' another, 'beak'. Occasionally attached at the opposite end of the shape to which the

small triangle is attached, one may find either a larger triangle or rectangle, or two diagonal

lines. This larger attribute should be called the "tail."

Shapes loosely categorised as creatures, in contrast, have a maximum of four short

verticallines from only one side of a central part of the shape, or no lines at aIl. This central

shape will probably have a smaller round, or oval shape, referenced as a 'head,' attached at

one end. A short line, termed as a 'tail,' may be attached to the other end of this central body.

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Images such as these must be

called birds. The commentator should note whether the image is hollow and the direction in

which the beak on the head is pointed. The number of short verticallines on the underside

of the curved horizontalline must be counted integral to this shape. If the centre of the bird

is hollow, the commentator should state whether anything is represented in the hollow

interior of the shape.

Images such as these must be called turtles.

Turtles' usually have four short lines, called 'legs,' emanating in four directions from the

outside edge of the shape. Extended into the shape's body, these lines would, in theory, cross

in its centre. The head and the tail of the 'turtle' exist at opposite ends of the shape, each

between two 'legs'. The commentator should note whether the shape is hollow or solid, and

the direction the head points. If the centre of the turtle is hollow, the commentator should

note any representation within.

If a shape resembles any of the four shapes above, the

commentator should record this shape as a crescent. State whether it is vertical or horizontal,

and whether its points face left or right if it is vertical. If the crescent is horizontal, the

commentator must additionally comment whether the points face downward or upward.

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One should not describe this shape as a boat or a canoe, as it often is in the Hterature of the

Canadian Shield.

, JI J This shape must be described as a combination as a group of

vertical or horizontal Hnes, and noting the number of Hnes. A recording would read as

foliows: "group of four or five vertical or horizontal Hnes." One should not use the

frequently used term 'taliy marks.'

ci _,#$ tr

Loosely categorise this shape as 'parallel lines.' Note

whether this shape appears vertical, diagonal or horizontal. Note whether the Hnes touch

each other at ali (as in ex ample at right of above figure). Do not use the frequently used term

'taliy marks.'

m Lb

Cali this shape a line and state whether it is horizontal or

vertical.

(

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l call this shape a right hand print if the thumb is on the left, and a left if the thumb is on the

right hand side. However, the thumb may have faded or never been represented, in which

case, use 'hand print.' It must be recorded whether the shape is hollow or not. The person

using this term must realise that using the term hand print does not necessarily imply that the

image painters painted a hand with ochre and pressed it on the rock surface.

These shapes are examples of

different types of stick figures. Do not use the terms: anthropomorph, human being,

stickman or stick man, since these imply more specific meanings of some type and/or

impute gender. Difficulty in describing these shapes arises, since the words: leg, arm, head,

body, and, possibly, horns, immediately imply assumptions about the different parts of the

stick figure to the reader. The option exists to describe them as "a collection of four short

lines that are diagonal, vertical, and horizontal with a spot at one end." However, this would

make searching for this shape very difficult when and if recovering it from a large database.

Therefore, l decided to use the terms leg, arm, head, body, and, possibly, horns, or ears.

Comments must be made regarding the presence or absence of legs, arms, etc., and whether

they are depicted upward or downward. It is important to also note if the body or the head is

hollow or not. If the head has short vertical lines on the outside then these should be

recorded as either horns or ears, and a note should be taken if short lines are attached to the

end of each arm.

This shape can only be described as a star. The number of points should be

counted and note should be made of whether it is hollow or not.

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o l called this shape a square. One should not comment about the precise

angle of any of its corners. Again, one should record whether the shape is hollow or not.

This shape must be called a

zig-zag and note whether it occurs diagonally, verticaIly, or horizontally. It must not be

designated as a 'power line' or by some other word with a similar meaning. Such problematic

terminology, although frequently found in the rock image literature of the Canadian Shield,

meshes interpretation with the description of the images in question. Occasionally, a round

filled in circle is attached to one end of the zig-zag. One or two short curved lines attached

to the outside edge of an solid circle, or 'he ad,' could be called horns.

l called these shapes rectangles. No comment

should be made about the preClse angle at any corner. The commentator must record

whether the shape is hollow or not as weil as whether it is vertical or horizontal.

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This shape is a smear and could be called an ochre

wash on the surface of a rock. Smears come in various sizes and shapes, such as oval,

oblong, and round. These shapes cannot be placed in any category described above. They

could be, and are, larger than blobs.

-­• .. These shapes are examples of blobs. They usually exist if the

ochre has either faded, exfoliated off the surface of the rock face, or has become

indistinguishable because of the accumulation of white mineraI deposits. They vary in size,

since they exist once a shape no longer has distinguishable edges that can be clearly

delimited, identified and described. Blobs vary in shape, appearing round, oval, oblong, small,

large, horizontal, vertical and diagonal. Dots are small blobs. The key points are that they

cannot be placed in any of the above categories, and they are always smaller than smears.

Section 9: Possible relationships between rock image sites and other archaeologïcal

sites

Previous archaeologists concerned with these pictograph sites have not considered

the possibility that relationships may exist between the pictographs and any neighbouring

archaeological sites. A large number of archaeological sites from a specific archaeological or

historic time period possibly may exist in the immediate vicinity of a pictograph site or

groups of pictograph sites. This would be an interesting issue to consider and comment

upon. However, this is clearly impossible to undertake using the map below, which

represents the current state of archaeological knowledge.

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Figure 4.10: Map indicating location of other known archaeological sites to pictograph sites.

Some of the Borden quadrants in the map above are blank, indicating that sites either

have not been found, or that the Ontario Govemment does not have this information.

Assertions as to possible relations between conventional archaeological sites and pictograph

sites can be made only after archaeologists have established and examined in detail ail of the

sites in this region.

Conclusion:

A careful examination of the twenty-seven sites of the Lake of the Woods, using

Forms A and B, and technical software, provided me with a vast quantity of detailed

information concerning the context of each site, the physical features of the rock surface, the

large quantities of offerings both below and above the water line, and detailed descriptions of

the images. This information provided the basis to start a thorough examination of the

pictograph site images in the Lake of the Woods. l could now employ first, the culture­

historical approach in Chapter V, secondly, the contextual approach in Chapter VI, and,

finaily, one of the approaches concemed with meaning in Chapter VII. Through employing

each approach in sequence, l may achieve the four goals of my the sis to Ca) identify the

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possible vocabulary of images, (b) determine whether combinatory rules exist, (c)

reconstitute the life history of each site, and (d) ascertain whether the images can be related

to other images outside rock image sites ta determine if this can provide information about

the meaning(s) of the rock images.

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Chapter V: Culture-History Approach:

This chapter is concerned with the culture-historical approach, which permits

analysis of the form, date, and location of the images, and supplies archaeologists with the

basic data that they need to perform higher-Ievel operations. They must concentrate on

assembling detailed information about each individual site, and consider each image as a

separate entity at this level. Seven sections exist in this chapter.

Deterioration over time affects the shape, existence, and groupings of images. The

first section considers the clarity and the blurring of images caused by either, or a

combination of, exfoliation, lichen and rock tripe encroachment, and the deposition of white

mineraI deposits. The second section is concerned with the distribution of the images

throughout the Lake of the Woods. It establishes the minimum number of images per site,

the large st number of images per site, and the smallest number of images per site. The third

section considers the rock image style of the images of the Lake of the Woods in comparison

to how previous archaeologists have considered style in Northern Ontario. The fourth

section examines the ethnographic information regarding the components of the paint, and

how it was applied to the surface of the rock. Unfortunately, information does not exist as to

the type of implements and techniques used to create images. The fifth section examines the

ethnographic literature of this region regarding the large quantities of gifts such as tobacco

which were often given to supernatural beings to obtain supernatural bene fit, especially in a

ritual context. The sixth section of this chapter discusses the wide range of objects, called

offerings, above and below the water level. This is because several sites had a very large

number of offerings, including tobacco, clothing, liquor bottles, and coins. This was quite

unexpected based on the previous literature from this region and elsewhere in the Canadian

Shield. The seventh section of this chapter considers how it might be possible to date these

images since direct dating techniques cannot be used.

Section 1: Blurring loverlay discussion and darity of images.

A detailed examination of the rock image sites in the Lake of the Woods reveals that

many of the images suffer from exfoliation of the rock's surface, rock tripe and lichen

encroachment, or the accumulation of white mineraI deposits (please see Appendix 5).

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I~

Exfoliation is not evident at DhKm-20, DhKo-l, DiKm-49, DiKm-4, DjKr-23, and

DhKm-19. It is difficult to establish whether exfoliation has taken place at DgKm-l, DhKm-

5, and DiKq-10. Exfoliation of the rock's surface may have occurred at the microscope level

and be invisible to the naked eye. Exfoliation is present at several sites: DiKm-50, DgKI-l,

DiKp-l, DiKm-51, and DjKn-l. Severe exfoliation has caused many images to be unclear at

fifteen pictograph sites: DkKn-6, DgKm-2, DkKn-7, DiKn-l, DiKm-3, DhKn-l, DjKr-23,

DhKm-3, DhKm-l, DhKm-4, DhKm-3, DhKm-18, DgKl-2, DgKl-19, and DgKI-17

(xq716, xq717).

Figure 5.1: DkKn-6 in 2001.

Exfoliation can be so severe sometimes that it affects the entire pictograph site rather

than just a few of the images. Ail four images at DkKn-6 in figure 5.1 above are so severely

exfoliated that they can be described only as four oblong blobs of various sizes. However,

images can still be identified to sorne degree at other sites, as is the case with DhKm-l,

DhKm-18, and DhKn-1. The images loosely termed 'creatures' evident in figure 5.2, below,

are visible even though they suffer from exfoliation. Sometimes relatively large pieces of rock

can break off from the surface of the rock face.

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Figure 5.2: The different shapes of 'creatures' at DhKn-1 in 2001.

The photograph in figure 5.3 demonstrates that the first two images, on the left hand

side, to be described at DhI<m-4 are severely damaged because the surface of the rock had

fallen off once it had turned into flakes (xq728). Hence the first image can be described only

as an almost closed oval shape with pointed base and ten straight diagonallines coming out

from edges of the oval, while the second can be described only as a group of lines crossing

each other at ninety degree angles.

Figure 5.3: Overview of DhKm-4 in Whitefish Bay in 2001.

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Twelve pictograph sites: DgKI-19, DgKI-17, DgKI-2, DgKm-l, DgKm-2, DhKm-l,

DhKm-5, DhKn-l, DhKo-l, DiKm-3, DiKm-50, and DiKn-l have smears and

concentrations of ochre affected by a combination of exfoliation, lichen and rock tripe

growth and white mineraI deposits. Eighteen smears and one concentration of ochre exist

(xq740 and xq741) in the Lake of the Woods. DhKm-l, in figure 5.4, typifies a site where

exfoliation has had a considerable effect on the majority of its images (xq735, xq716, and

xq717). Exfoliation probably has caused a large number of the images to become paler and

more difficult to see in the bright sun. Figure 5.4 reveals that a few images were affected by

lichen and rock tripe encroachment as weil as by white mineraI deposits.

Figure 5.4: DhKm-1 has images affected by exfoliation, white mineraI deposits and rock tripe and lichen encroachment in 2001.

It is evident in figure 5.5 below, a photograph of the same site, that exfoliation probably has

played a larger role than lichen or mineraI deposits in causing these images to be pale.

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Figure 5.5: The exfoliated images at DhKrn-1 in 2001.

Figure 5.6, a photograph of another part of DhKm-l, indicates that this long vertical smear

is affected by rock tripe encroachment and some white mineraI deposits and not just by

exfoliation, causing further lack of clarity.

Figure 5.6: The smear at DhKrn-1 in 2001.

Lichen has adversely affected some of the images at fifteen pictograph sites: DgKl-l,

DgKl-19, DkKn-6, DhKm-l, DhKm-20, DhKm-18, DhKm-3, DhKo-l, DiKm-49, DiKm-

51, DiKn-l, DkKn-7, DiKp-l, DjKn-l, DhKm-5 (xq724). It has started to affect images at

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DgKl-17, DjKr-23, DgKm-2, but it does not affect images at DgKl-2, DiKm-4, DhKm-4,

DgKm-1, DiKq-10, DhKm-19, and DiKm-50.

Rock tripe has not affected images at DgKl-2, DiKm-4, DhKm-3, DhKm-4, DgKm-

1, DiKq-10, DhKm-18, DhKm-19, and DiKm-SO, but is has affected sites DkKn-6, DkKn-

7, DhKm-1, DhKo-1, DhKm-5, DiKp-1, DgKl-19, DgKl-17, DjKr-23, DiKm-51, DjKn-1,

DiKn-1, and DgKm-2.

Figure 5.7: The upper part of DiKn-1 in 2001.

Figure 5.7 above, depicting part of DiKn-1, further il1ustrates how lichen and rock

tripe often obscure images at pictograph sites. Rock tripe appears with lichen at five sites

including: DiKm-3, DiKn-1, DgKl-19, DhKm-18, and DjKn-1 (xq722 and xq723).

White mineraI deposits are a common occurrence in relation to sorne of the images

at several of the pictograph sites: DgKl-1, DgKl-2, DgKm-1, DhKm-1, DhKm-3, DhKo-1,

DhKm-20, DiKm-3, DiKm-51, DiKp-1, DiKq-10, DjKr-23, and DhKm-5 (xq725 and

xq735). The accumulation of white deposits was so severe at DiKq-10, seen in the two

photographs below, that it was almost impossible to see and identify the images.

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~ ..

Figure 5.8: Severe deposition ofwhite mineraI deposits at DiKq-10 in 2001.

This locale, at Picture Rock Point, was designated as a site by Dewdney in 1960, who

cailed it Site # 95 (Dewdney and Kidd: 44). This site is on either side of the corner of the

block of granite in figure 5.8 above. It is the best ex ample in the Lake of the Woods where

white mineraI deposits have severely affected the images, since it is very hard to see the rock

images without using VIPS/ip and Adobe Photoshop 6.0. Examination of other sites that

have white mineraI deposits demonstrates that these deposits are often unequaily distributed

across cliff faces. Of interest concerning this site is that very little rock tripe growth and

lichen encroachment affects the images in comparison to the surface of the rock that lacks

these red images. Occasionaily paintings are superimposed on white mineral deposits

occurring over earlier images, as observed at DhKm-5 and DhKm-3.

Several images at DhKm-3 in the photographs, figure 5.9, below suffer from the

deposition of white mineraI deposits. Others suffer from exfoliation as weil as rock tripe and

lichen encroachment.

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Figure 5.9: AIl of the images at DhKm-3 in 2001.

White mineraI deposits exist both under and over some of the red images ln the three

photographs of DhKm-3 presented above in figure 5.9.

Close examination of photographs reveals that the accumulation of white mineraI

deposits has affected the images at DhKm-3, DiKm-3, DhKo-l, DiKp-l, DiKn-l, and

DhKm-5. These shapes can be described by carefully using the VIPS software. This software

was useful in establishing whether images were superimposed over white mineraI deposits

which in turn obscured other red images. DhKm-5 is an example of a site where red images

are superimposed over each other and are affected by white mineraI deposits.

My examination of the photographs of this site using VIPS/ip reveals that images

have been created at DhKin-5 several times over an unknown period. The different colours

indicate that images have been painted over other images. The white images in the black

background in A22 are the same red images affected by white mineraI deposit in A1. Once

the image file is loaded into VIPS the slider turns all the red pixels selected in the Al box

into white pixels and every other colour into black pixels. Ali the red pixels, regardless of

whether they are below or superimposed on white mineraI deposits, will become white

pixels, shapes among the black pixels in the box called A22 in figure 5.10.

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Figure 5.10: Screenshot of sorne of the red images be10w the white mineraI deposits.

Figure 5.11: If this screen shot is compared with the screen shot above it is c1ear that the accumulation of white mineraI deposits at DhKm-5 is not uniform.

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It is possible to establish whether red(s) was superimposed upon another red are a, or

whether the pale red/pink areas are covered in white mineraI deposits in the are a of red

pixels in box A7, by comparing it with the red pixels in the box A2. When l moved box A7, l

isolated a shade of red coloured pixels different to the one that l had selected in the previous

screenshot, to see whether other images that are not easily visible existed on the same surface

isolated in box A2. If white images in box A22, which are in reality red, are compared

(figures 5.1 0 and 5.11) it is clear that superimposed images exist at the same place and are

affected by the white mineraI deposits. This deposition is not uniform, and it does not coyer

the entire image. It does cause images to become paler, and to "disappear" underneath it.

Image analysis of the TIFF files using software such as VIPS and Adobe PhotoS hop 6.0

indicates the fragility of the sites and their images together with their changing nature. It also

demonstrates the key role of the human eye in recognizing the images themselves.

The human eye and the brain play a major role in the identification of individual

images. This role is most clearly evident if a specifie image has been isolated from its context

upon the surface of the rock using the VIPS software, and is viewed against a black

background away from its original context. It becomes evident that these red images were

not solid blocks of red upon a grayish granite surface, sin ce the edges of a group of white

pixels that once constituted the red image were not clearly delineated and the centre of an

image was not solid white.

l used various tools available to try to mathematically remove the white pixels

deemed 'noise' and attempted to make the image in question become solid.

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Figure 5.12: Screenshot showing what occurs to the same images using different tools when 1 mathematically tried to remove the white pixels deemed 'noise".

l realised, by doing so, that my eyes and brain were 'filling in the gaps'. Essentially the

brain and the eye of the observer make decisions as to the precise edges of each image. The

part played by the human being in identifying the shape of an image increases when the

edges of superimposed images must themselves be estimated.

Conclusion:

Unfortunately, many of the images have been affected by exfoliation, white mineraI

deposits, and the accumulation of rock tripe and lichen. This means that the images that l

described no longer had their original distinct clear edges, and many had been destroyed.

Many of the images that l did describe were nearing the end of their liEe-cycle, creating

severe problems for those attempting to describe them. Image analysis using Adobe

PhotoS hop and VIPS indicated the fragile nature of these images, the sites, and their

changing natures. Use of this software highlighted the considerable role played by the human

eye and brain in the identification and subsequent description of these images.

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Section 2: Distribution of images

It is generally assumed that a vast range of images was produced at these sites.

However, relatively few images exist. A total of three hundred and eighteen images were

recorded with an average of eleven images per site and a minimum number of one. The map

below in Figure 5.13 indicates the number of images at each site.

Dhkm-S - 37

~~~ ~29 DKo-1 -28 DhKm-l 17 DIKn-l - 16 DIKr-1 - 14 DQKI-17 -'" 13 Dil<:ctlO = Il DhKn-l ~ 10 IOoKI ~=9 'D,I<I - 8 DYr-23 = 8 Dql<m-l=7

Lake of the Woods

Figure 5.13: A map of the Lake of the Woods area showing the numbers ofimages at each site.

Two sites had more than thirty images: DhKm-s and DhKm-3. Only three sites have

between twenty and twenty-nine images: DiKm-3, DhKo-l, and DjKn-1. Six sites have

between ten and nineteen images: DhKn-l, DiKm-l, DiKp-l, DgKI-17, DhKm-l, and

DiKq-l0. The rest of the sites have fewer than ten images: DkKn-6, DgKm-l, DhKm-18,

DhKm-4, DiKm-4, DgKI-2, DkKn-7, DgKl-19, DgKI-l, DiKm-20, DiKm-19, DiI<m-sO,

DiI<m-sl, DiKm-sO, DiKm-49, DhI<m-20, DgI<m-2, and DjKr-23.

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Conclusion:

Most of the images are in the eastern portion of the Lake of the Woods. Relatively

few sites exist in the southern and the northern portion of the region. Two sites exist in the

northwestern portion of the region but sites do not exist in the southwestern region, possibly

because the geology is differem and the area is swampy, sandy, and full of muskegs and bogs.

Indeed, the soils in this region are wetlands, called organic mesisols. This region is mesic

woody forest. The soils in the western portion consist of sand deposits, stratified sand and

glacial deposits over calcareous till with peat over undifferentiated deposits (Soil Research

Institute 1964). Sand and gravel bars as weil as beaches were created by the deposition of

materials on the shores and margins of glacial lakes. Peat and alluvial deposits are

commonplace (Kanivetsky 1979) whilst the Precambrian shield is visible in sorne parts of the

southern region of the Lake of the Woods where the overlying drift is less thin and less than

9.14 metres (Kanivetsky 1978). The southern and western part of the Lake of the Woods was

probably the most severely affected as the water levels were artificially raised from 1888

onwards (please see Chapter II for this discussion). Indeed, the divers told me they suspected

that habitation sites were flooded when the water levels were raised, as they had seen stone

rings, probably fireplaces, that are now below the current water level.

Section 3: Analysis of rock image style in relation to Northern Ontario and adjacent

areas.

Style is important for archaeologists because different styles are aften equated with

different ethnic groups, while similarities are interpreted as evidence of close interaction.

Given the physical size of the Lake of the Woods region, is it perhaps surprising that it has

produced not only such a small number of images, but also such a small range of shapes.

This makes it difficult ta undertake detailed comparisons of the shapes found in this region

in relation with elsewhere in Narthern Ontario and adjacent areas. However, comments can

be made regarding the stylistic qualities of the images found in 2001 in comparison to how

previous archaealogists have considered style in Northern Ontario.

As discussed in Chapter III, Grant (1967: 20) had defined the general style of the

images as being "painted (naturalistic)" . According ta Grant this style of paintings

predominated in the Northern Woodlands and it "continued westward" across the prairies of

western Canada as far as the Columbia-Fraser Plateau (ibid.). He maintained that sorne

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"simple abstract elements" existed but they were subordinate to the naturalistic style (ibid),

and that this style of painting occurred in areas "dominated by a nomadic hunting economy".

It appears that Grant did not consider that stylistic differences might exist in regions within

the Canadian Shield. It is also difficult to as certain the qualities of an image that was deemed

as "naturalistic" by Grant so one can either reject or use this term for the images of the Lake

of the Woods. Furthermore, problems could exist if one considers his statement that

paintings were usually in red but occasionally in white or black pigment. Indeed, the majority

of the images recorded in 2001 were painted in red ochre yet some of the newly discovered

paintings had been created in modern red, blue, white, green, and black spray paint. It is also

clear that neither blobs nor smears were considered as images by Grant. Initially, Dewdney

had not considered images such as smears, blobs, or ochre washes as images, but he appears

to have subsequently accepted that smears could be images. However, it is likely that he

would have recorded the other images if he believed that they "fitted into" the categories in

his table in figure 3.44, discussed in Chapter III.

The images in the Lake of the Woods can be divided into groups according to whether

they have either hollow or solid centres, or do not have solid or hollow centres because these

shapes are either individuallines, or are created from connected lines. Rajnovich (1981 b: 286)

described the images she examined at sites in Deer Lake, some of the most northerly sites in

northwestern Ontario, as having similar centres. She identified four styles of images, aIl of

which had different centres. The images l examined in 2001 are similar to three of the four

types of morphs Rajnovich identified. The images that l discovered Rajnovich possibly might

describe as "finger lined, or stock morphs," "open or outlined morphs," and "closed

morphs." She argued that the lines of the "open or outlined" images possibly denoted

"internaI organs," and she noticed that this stylistic feature was common to many of the

images created by the Cree and the Ojibwa during the twentieth century. Her observation is

pertinent for the newly discovered images that exist at DhKm-20 in the Lake of the Woods

especially since the painter provided a date of 1982.

Eighteen smears and seventy-seven blobs were found in the Lake of the Woods.

Indeed, Rajnovich (1980b, 1980c, 1980d, 1981a, 1981b, 1981c, 1987, 1994) did not consider

a shape called a "blob" or a "smear" to exist. Rusak, who was trained by Rajnovich, argued

that smears and ochre washes were images. She (1992b: 124) concluded, after the first year of

a two year field survey of White Otter Lake, that smears and ochre washes were placed there

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intentionally sin ce they always occurred in conjunction with the five physical features that

exist with images at pictograph sites on cliff faces. She argued that the presence of these

images at such a large number of pictograph sites in White Otter Lake confirmed that these

places held considerable significance in the world view of the Algonquian-speaking peoples.

Rusak, like Pastershank (1989), viewed them as individu al images in themselves, while

Rajnovich (1981b) perceived washes as a part of an image. Otherwise none of the other

archaeologists who examined pictographs sites in Northern Ontario, such as Smith (1981),

Pelleck (1981), Pastershank Rajnovich (1989) and Rusak (1992a), discussed the style of the

images at pictograph sites.

The images in the Lake of the Woods are generally similar to those found at other

pictograph sites that l examined elsewhere in Northwestern Ontario prior to working in the

Lake of the Woods. The photographs below, figures 5.14, 5.15, and 5.16, are of three

pictograph sites recorded in 1992 on the Turtle River System, northeast of the Lake of the

Woods in N orthwestern Ontario. The shapes in figure in 5.14 include stick figures, the

principal shape in figure 5.15 is a smear, and the main figure in figure 5.16 is a stick figure.

Figure 5.14: DIJn-l from Harmon Lake Figure 5.15: DjKp-l0 on Moberly Lake

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Figure 5.16: DjJp-1 on Moberly Lake.

Once l had described and grouped the images from the Lake of the Woods

according to type it was clear that the largest number of images could be described as 'blobs'.

Indeed, there were seventy-seven different types and sizes of shapes called 'blobs' (xq349)

and eighteen 'smears' (xq326). The large number of smears and blobs of different shapes and

sizes indicates that the passage of time has affected these images. As l argued in the previous

chapter, a shape should not be considered as static and timeless since its outline changes over

time.

Smears have various sizes and shapes: such as oval, oblong and round. Blobs exist

where the ochre has either faded or exfoliated from the surface of the rock face and spots are

small blobs. Furthermore, the vocabulary and the level of detail at which these images are

described has influenced the number and the range of each type of shape. This means that it

is possible to classify the images differently, and, consequently, l could easily demonstrate

that the very vocabulary used heavily influenced the possible outcome of any d,iscussion of

perceived style. A nested hierarchy of types seems to leave the most options open with

respect to classification.

For example, if all the extremities of a shape such as creature were to be ignored, it

would be possible to simply describe the shape as a 'creature.' Unfortunately, this gives the

impression that all the twenty-three shapes that are 'creatures' are the same 'creature.' It is

not always possible to identify the species of the creature based on its appendages. However,

if one closely examines the photographs of the images, takes into account the appendages,

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~.

~.

and whether or not the image is hoilow, this could mean that ail twenty-three images are

slightly different. The twenty-three 'creatures' were at DjIZn-l, DiKp-l, DiKm-3, DhKo-l,

DhIZn-l, DhKm-5, DhKm-3, DgI<J-l, DgI<J-2, and DgI<J-17. Occasionaily sorne sites had

more than one image of a 'creature' (xq382). If the shapes of 'creatures' were classified in

considerable detail, the images would be as foilows (see also Appendix 6):

a)

b)

c)

d)

e)

f)

g)

h)

i)

j)

k)

1)

m)

creature, facing left, with head with large horns or ears, tail, two legs visible - one

back and one, solid - DgI<J-l

creature, facing right with he ad with large horns or ears, tail, two legs visible - one

back and one front, solid - DgI<J-l

creature, facing left with two clear legs with a third leg, tail and horns or ears, hoilow

- DgI<J-17

creature with head, with horns or ears or antlers and a back and a pair of front legs

facing right, solid - DgI<J-2

creature with long horns or ears, facing right, one back leg and one front leg and

curved tail, solid - DhKm-3

creature, vertical does not face left or right, with four legs, a tail, and a he ad and two

horns or ears, solid - DhKm-3

creature with head, facing left, one back and one front leg, with two horns or ears

superimposed upon pale images - DhKm-5

creature with horns or ears facing left since long tail pointing downwards on right

hand side of animal, four legs visible (front legs are less visible). Head is also less

visible, solid - DhKm-5

creature, facing left with faint outline of he ad with horns or ears and a short tail,

solid - DhKm-5

creature, facing left, head with horns or ears and tail but no clearly defined legs, solid

-DhKm-5

creature, facing le ft, with horns or ears but no clearly defined legs and tail, solid -

DhKm-5

creature, body is horizontal line with horns or antlers, no legs, facing right, solid -

DhIZn-l

creature, horizontal body is a line with head with horns or antlers, no legs, faces left,

solid - DhIZn-l

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n) circular creature with head, facing right, with two horns or ears attached to head,

two legs and two arms, solid - DhKo-l

0) creature with head, facing right, short tail, one back leg with two digits and one front

leg with unknown number of digits, solid - DhKo-l

p) creature with two horns or ears, only front part of body and head facing left, no rear

body, legs or tail, hollow - DhKo-l

q) creature, facing left, long horizontal with pointed mouth with dots down the middle

of the creature beginning behind head, top of creature have triangles on top side and

horizontal series of short lines, hollow - DhKo-l

r) creature facing right with two horns or ears pointing up , one front and one back leg,

solid - DiKm-3

s) diagonal creature, but vertical with no legs but a tail with a point, two legs raised

upwards and a head, with two horns or ears - DiKm-3

t) creature with horns or ears on its head, a curved tail, and two legs with feet, facing

left, solid - DiKp-l

u) creature, cross section, facing right, with a rack of horns or antlers, and a tail, four

short diagonal legs, solid - DjKn-l

v) creature, horizontal cross section of body, facing left, with horns or ears or antlers

indicated by small round hollow bubble ab ove filled in head of hollow creature with

antlers, one back leg and one front leg - DjKn-l

w) creature, horizontal cross section, facing right with two back legs and two front legs

are visible as is a he ad with horns or ears. The creature has a long tail measuring

approximately half of the length of body - DjKn-l

As indicated above there are twenty-three definitions of 'creatures.' All of the images

are quite different from each other. Indeed, it may appear as if two of the 'creatures' are the

same; however, neither image is the same since the interior of one is hollow and the interior

of the other is solid (xq752, xq755, xq754, and xq753).

The same problem occurs with the type of shape called 'stick figure' (xq382b). Using

a single word rather than undertaking a detailed description of each image provides a false

impression of the types of images, their complexity, and individuality. A short description

glosses over the differences evident in the pictograph sites of this region.

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.~.

Indeed, although even the largest group of image cal1ed 'blob' may sound simple,

these images are in reality quite different from each other. Although in these cases, the

differences reflect the different images the blob evolved from, and the different natural

processes affecting its evolution, rather than different products of human endeavour. The

shapes of the pictographs found at rock image sites in the Lake of the Woods can be more

general1y categorised as fol1ows (see Appendix 7):

a) seventy-seven different types of 'blobs' (xq349)

b) eighteen different types of 'smears' (xq326)

c) five types of shape cal1ed 'unidentifiable shape' (xq744) and one area at DgI<J-19 that

also contains pairs of vertical lines and spots of smal1 concentrations of ochre

(xq745)

d) two types of shape cal1ed 'diagonal stick figure' (xq382b)

e) fifteen types of shape cal1ed 'vertical stick figure' (xq358a, xq382b)

f) two types of shape cal1ed 'upper torso of vertical stick figure' (xq358c)

g) twenty-nine loosely categorised types of shape cal1ed 'hand print' (xq328, xq328a,

xq328b, and xq333), eleven are right 'hand print' shapes (xq328b) and seven are left

'hand print' shapes (xq328b)

h)

i)

j)

k)

1)

five vertical types of shape cal1ed 'vertical zig-zag' (xq321)

t:wo types of shape cal1ed 'diagonal zig-zag' (xq321)

one type of shape cal1ed 'horizontal zig-zag' (xq321)

t:wo types of shape cal1ed 'one vertical and one horizontal short line that cross each

other at ninety degrees' (xq336 and xq336a)

two types of shape cal1ed 'square, created by two vertical and two horizontallines of

equallength' (xq746)

m) three types of shape cal1ed 'turtle' (xq382 and xq362)

n) two types of shape cal1ed 'bird' (xq335)

0) one type of shape cal1ed 'horizontal crescent with points facing upwards' (xq332,

xq350, and xq348) (see figure 1.2 in Chapter I)

p) seven types of shape cal1ed 'horizontal crescent with points facing upwards with

vertical lines attached to topside' (xq332, xq348, and xq 350) (see figure 1.2 in

Chapter 1)

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.~

q)

r)

s)

t)

u)

v)

w)

x)

y)

z)

two types of shape called 'horizontal crescent with points facing downwards' (xq348a

and xq348) (see figure 1.2 in Chapter 1)

two types of shape called 'horizontal crescent, points facing downwards with vertical

lines on bottom side' (xq 350 and xq348) (see figure 1.2 in Chapter 1)

ten types of shape called 'horizontal line' distinguished by the following qualities:

wide, narrow, long and short (xq338)

eight types of shape called 'diagonal line' distinguished by the following qualities:

wide, narrow, long and short (xq747)

eleven types of shape called 'vertical line' distinguished by the following qualities:

wide, narrow, long, short and with a forked end (xq339)

four types of shape called a 'two parallellines' (xq 347 and xq749) which are either

diagonal, vertical or horizontal

rune types of shape called a 'group of three diagonal parallel short lines' (xq346)

two types of shape called a 'group of four diagonal short lines' (xq342)

two types of shape called a 'group of six short horizontallines' (xq343)

two shapes called 'three lines joined together at one end' (xq324)

aa) four types of shape called "curved lines" distinguished by the following qualities:

vertical, horizontal, diagonal, narrow, long, short (xq324)

bb) two types of shape called "three vertical and diagonallines attached to each other at

the lower end of each line" (xq510)

There are many images that occur once.

Porty one of the shapes in the Lake of the Woods are hollow (xq752). They are

found at the following sites: DgKl-17, DgKl-2, DhKm-18, DhKm-20, DhKm-4, DhKm-3,

DhKo-1, DiKm-3, DiKm-4, DjKn-1, and DjIZn-1. Other images had 'solid', 'infilled' or

'filled in' centres. By accident three different terms were used to describe the same concept

because the description of the images took place over a month. Essentially such images had a

solid centre and there were no obvious holes inside the shape. This is the only time when 1

changed the vocabulary that 1 used to describe the shapes of images from the pictograph

sites of the Lake of the Woods.

One hundred and flfty-one shapes have solid centres (xq755, xq754, xq753) and they

were at the following sites: DgKl-1, DgI<J.-2, DhKm-1, DhKm-19, DhKm-18, DhKm-20,

DhKm-3, DhKm-5, DhIZn-1, DhKo-1, DiKm-3, DiKm-4, DiKm-50, DiIZn-1, DiKq-10,

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DjKn-l, DjKr-23, DkKr-6, DgKl-19, DiKp-l, DiKm-51, and DkKr-7. The centres of two

images are unclear at two different sites, DjKn-l and DjKr-23 (xq756). Eighteen sites (DgI(l-

1, DgI(l-17, DgI(l-2, DhKm-l, DhKm-l, DhKm-20, DhKm-3, DhKm-4, DhKm-5, DhKo-

1, DiKm-3, DiKm-4, DiKm-51, DiKn-l, DiKp-l, DiKq-l0, DjKn-l, and DjKr-23) have

ninety-three images that cannot be classified as having solid or hollow centres because these

shapes are either individuallines or are created from connected lines (xq757).

Lines that are connected to each other can constitute another shape. Therefore lines

(xq325 and xq324), horizontal lines (xq337 and xq338), vertical lines (xq339 and xq337a),

diagonallines (xq747 and xq747a), triangles (xq370a), rectangles (xq748), squares (xq746) and

circles rarely exist as individual shapes since they are mostly parts of other shapes (xq751 and

xq751a). The image below was described as: rectangular box shaped image with round circle

on one end of the lowest of the four v shaped lines that cross the middle of the rectangle.

The top end of the rectangle is closed by the first of the vs (xq748) in figure 5. 17 below.

Figure 5.17: Close up of a rectangle with the circle and the diagonallines from DhKm-3 in 2001.

Shapes often exist inside other shapes. This makes it difficult to determine whether a

shape is hollow, solid, or unclear. Sorne shapes just contain lines, while others incorporate

other shapes. Three shapes have lines in their centre at DhKm-3 (xq753), while images other

than lines exist in one image from DhKm-18 and in five images from DhKm-3 (xq759).

Completely recognizable images such as stick figures were found to exist inside other shapes.

At DhKo-l there were two vertical stick figures inside other shapes (xq 515). Here a vertical

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stick figure exists inside a rectangle that is narrow and has open gaps at the right and left

ends. This hollow rectangle, visible in figure 5.18 below, contains a vertical stick figure with

two arms down and two legs and verticalline that crosses inside of the right hand end of the

rectangle (xq748, xq358b, and xq358a).

Figure 5.18: The rectangle with the stick figure at DhKo-l in 2001.

Conclusion:

Every attempt was made to objectively describe the images at these sites. Many of the

images in the Lake of the Woods, as described in depth, are unique. Hence, a large number

of different types of image also exist at only one site. Images are either hollow or solid, and

may be constituted of several shapes, such as the example in the photograph above.

Furthermore, if images are described more generally as 'creature' or 'zig-zag', it is easy to

establish that the range of images is small and there are large numbers of the same type of

shape. A nested hierarchy of types clearly leaves the most options open with regard to

classification.

Section 4: The techniques used to make paintings

Ethnographie information concerning the type of implements and techniques used to

create images does not exist. Pohorecky (1968: 106) posited that paint was applied to the

surface of the rock either with fingers or simple brushes. It is likely that fingers were used to

apply paint to the surface of the rock.

Fortunately, some ethnographie evidence exists as to paint components. At least

some paint was made from ochre and isinglass. Isinglass comes from the air bladder of the

sturgeon, a fish commonly found in this region of North America. Jones (1980: 48) reported

that, in 1972, he was told bya Swampy Cree informant from Norway House, Manitoba that

an old man had told mm "that ochre was mixed with sometmng from a sturgeon to make a

painting or rock paintings." Jones (ibid.) argued that this was the "only direct evidence of the

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connection between ochre pigment and the use of isinglass (or sorne other substance) from

sturgeon as a rock painting binder." Skinner (1911:23) observed in 1908 that the East Cree

men put a mixture of red ochre and isinglass on their legs which would not wash off and

must be le ft to "wear away." He also described a Northern Saulteaux legend from Martens

Falls Post on the Albany River, Ontario, where isinglass was described as coming from

sturgeon (Skinner 1911: 171). Stevens (1971:89) related a legend collected from the Ojibwa

from Sandy Lake, Ontario, where an old shaman gave a young man "a powerful glue that

had been made from a marrow of a sturgeon backbone." He used this glue on his feet and

hands and it allowed him to climb up to the top of sorne steep cliffs where the Thunderbirds

lived. James Isham in his "Observations and Notes on Hudsons Bay, 1743" reported that:

the Glue the Natives saves out of the Sturgeon is Very strong and good, they use itt {sic] in mixing with their painting, which fixes the Colours so they never Rub out

(Rich 1949: 169).

Dewdney (Dewdney and Kidd: 1967: 21) stated that B. Amos Ratt, an informant

from La Ronge in Northern Saskatchewan, had told him that "he had taken earth from a

deposit on the Churchill River" and had "reddened" it by "bringing it to a white heat in a

frying pan. Amos said that he subsequently mixed this "earth" with oil rendered from white

fish gut and used the substance "to waterproof his log cabin and paddles."

Densmore (1974:370) discovered that the reddish substance that "rose to the surface

of certain springs" in one of the regions where she conducted fieldwork, was collected, dried,

and baked in a fire. According to Densmore it "became hard like a stone". This substance

was subsequently powdered and the fine red powder was kept. Tt was mixed with grease to

produce paint "that was reddish but not vermillion," and which, Densmore, stated was used

on arrows, faces, and bodies. She argued that this "scum" contained iron oxide and the

powder was referred to as ochre. This is interesting information but it is unclear where it

came from, since Densmore conducted the fieldwork for this publication at several

reservations in Minnesota, including White Earth, Red Lake, Cass Lake, Leech Lake or Mille

Lac, the Lac Court Oreilles Reservation in Wisconsin, and the Manitou Rapids Reserve in

Ontario (ibid.: 281).

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.~ ...•

Conclusion:

Very little ethnographie evidence exists as to how the paint was made for the images

and how it was prepared and applied. However, a few reports do exist from different parts of

the Canadian Shield, from the Cree and the Chippewa but not from the Lake of the Woods,

eoncerning the paint's eonstituents. It is likely that it was made from oehre and isinglass.

Unfortunately, ethnographie information do es not exist eoncerning the type of implements

used to ereate images on the surface of the rock face.

Section 5: Discussion of the offerings left at sites

Ethnographie literature of this region indieates that gifts sueh as tobaeeo eould be

given to supernatural beings to obtain supernatural bene fit, espeeiaily in a ritual eontext.

Both Hilger (1936: 20) and Densmore (1974 [1928]: 325) observed that the Midé always

offered tobaeeo when gathering plants for medieinal uses.

Warren (1984 [1885]: 79) observed that giving something, like tobaeeo, to an eIder

when genuine information was sought from them, was "an invariable eustom" of their

religious beliefs. He noted (ibid.: 64) that if Indians wanted to address Kitehemanido this

address was always aeeompanied "by a sacrifice of tobaeeo or other article deemed preeious

by the Indian." Warren (ibid.: 287 and 337) observed several instances where tobaeeo was

also used as a gift item to prevent war or aggression. He deseribed several instances where

gift giving was part of negotiation as a means of preventing warfare (ibid.: 284, 365, 369, 371,

and 375). In one instance, Warren wrote that Monsieur Cadotte, a fur trader, gave presents to

the Dakota of tobaeeo and clothing as a means of preventing warfare.

Coleman (1947: 83) wrote that tobaeco had great power and eonsequently was a

eommon offering to ail the manitous. She noted that putting tobaeco on the ground or upon

the surface of water was eommonplace and that it "was often placed beside the dead for their

use on their long journey." Coleman, in an earlier published work (1929: 54) stated that those

who were siek and wanted to be eured by a specifie rock, owned by a pers on, and known to

cure the siek, brought it blankets, tobaeeo and other gifts to obtain favour. Her informant,

Mrs. Fairbanks, added that the person who owned the specifie rock took the gifts.

Over a century later, Pufahl learned from his informants at the Eagle Lake Reserve,

near the pietograph sites he was studying, that these sites were saered to the local indigenous

eommunity and "routinely receive[d] offerings of tobaeeo" (1990: 19). Smith (1995:33)

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argued that the use of tobacco was a sign of respect between humans and the manitous, and

asserted that it was common practice to offer either loose tobacco or tobacco in the form of

cigarettes to the EIders. However, if tobacco was buried it protected the individual buried

from the Thunderers (ibid.: 72). Tobacco was also either strewn into the water, smoked

before a trip or offered to Mishibeshu (ibid.: 119-120). She noted that Hilger had observed

that this was common practice between 1930 and 1940.

Offerings above water have always been sought by archaeologists who have

examined pictographs. Fox (1974), Dewdney and Kidd (1962 and 1967), Lambert (n.d.),

Pastershank (1989) and Reid (1975 and 1976) examined pictograph sites in the Lake of the

Woods for previous offerings. Therefore, it was important for us coilect this type of

information as weil. Neither of the two caves held anything that could be cailed an offering

(xq 124b). Fifteen sites in total, including the two cave sites, did not have any offerings:

DgKl-19, DgKm-1, DiKm-49, DiKm-50, DiKm-51, DgKm-2, DhKm-18, DhKm-19,

DhKm-4, DiKm-3, DiKp-1, DjKn-1, DjKr-2, DkKn-7, and DkKn-6 (xq 124 and xq007).

Since the range of offerings was vast, it was important that they should be split into

types according to whether they were tobacco, money, liquor botdes, chinaware, clothes, or

anything else.

Twelve sites had tobacco and items that were termed as offerings: DiKm-4, DhKo-1,

DhKm-20, DgKl-17, DiKn-1, DhKn-1, DjKr-23, DgI<l-1, DgI<l-2, DhKm-1, DhKm-3, and

DhI<m-5 (xq124). They are marked by the letter "0" on the map in figure 5.19 below.

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~, r

Lake of the Woods

10 20 l 'Km.

DkKn-ii

Figure 5.19: Sites where offerings were found in 2001.

Tobacco was the common offering at rune of the sites, including one of the newly

discovered sites: DhKm-20, DhKm-5, DhKm-1, DgI<J-2, DjKr-23, DhKn-1, DgI<J-1, DgI<J-

17, and DiKn-1, either in the form of 100 se tobacco or cigarettes. Dewdney found it at

DiKm-4 and DiKm-3 in 1960 and Pastershank at DgKl-2 and DgI<J-1 in 1989. The letter

"T" on the map in figure 5.20 indicates at which sites tobacco was found as an offering.

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Lake of the Woods

Figure 5.20: Sites where tobacco was found as an offering in 2001.

Coins, money, were found as offerings at several sites: DiKm-4, DiKn-1, DjKr-23, DhKm-1,

DgKl-17, and DhKm-S. This is indicated by the letter "M" on the map in figure 2.21 below.

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Lake of the Woods

Figure 5.21: Sites where money was found as an offering in 2001.

Clothing of various types was found at several sites including DhKm-3, DhKm-l,

DiKn-1, and DgKl-2 (xq007 and xq124). Both Fox (1974) and Molyneaux found similar

offerings stuffed into a cleft in the rock surface of DhKm-l in 1974 (figure 5.22).

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Figure 5.22: Offerings discovered by Fox in 1974 at DhKm-1.

Dewdney found clothing at a number of sites, including DiKm-3, DiKm-4, DhKm-

1, DhKm-4, DhKm-5, and at DjKq-2 while conducting fieldwork between 1958 and 1964.

The offerings found at DiKm-3 changed in type between 1959 and 1960. Dewdney visited

the site in 1959 and found what he called a "prayer raft"; a year later on July 17th 1960 he

found a wide range of objects: 32 painted sticks in deep water, one cigarette, one yellow T­

shirt, a girl's blouse, a small girl's flannette dress, a very small T-shirt, and a pair of freshly

laundered blue jeans which had worn out at the knees. Clothing of various types were found

at five sites in 2001 including: DhKm-3, DhKm-1, DgKl-2, DiKn-1, and DgKI-17 as

indicated by the letter "C" on the map in figure 5.23.

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.~.

Figure 5.23: Sites where c10thing was found as offerings in 2001.

Small alcohol and beer bottles were found at DhKm-l, DiKn-l, DhKo-l, and DgKl-

2. The locality where this type offering was found is indicated by the letter "L" on the map

below in figure 5.24.

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~ Lake of the Woods

o 10 20 ~l& , ___ ,,,,,"-_, Km ..

DkKn,7

Figure 5.24: Sites where alcohol bottles were found as offerings in 2001.

At DgI<J-17, DhKm-3, DhKm-1, DgI<J-2, DjKr-23, and DhKn-1, 1 found objects

le ft as offerings that differed from everything else found. The objects left as offerings

included bullets, feathers, chinaware, a hand-blown glass bottle, a small ceramic bowl, and

bundles of prayer sticks. Dewdney had found offerings of chinaware and enamelware at

DhKm-18, DhKn-1, and DiKn-1. During his 1960 field season he also found bundles of

prayer sticks at DhKin-5, DiKm-3 (figure 5. 25), DjKq-lO (figure 5.26), DhKm-18, and

DiKm-4. Dewdney collected one of a number of bundles, or ceremonial sticks, from

DhKm-18, which he called Site # 104. They consisted of a number of barked poplar sticks

that had been cut squarely at each end and tied together. Five large dots were painted along

one side of each stick. Two of these dots were near either end of each stick while one was at

the centre of each length. The two outer dots were green, and the three central ones were

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red. He also described the ceremonial offerings that he found at DiKm-3, Site # 28, as being

thirty-four sticks held together by grey yarn at one end. The sticks were held parallel with

each other with one strand on each side of the stick. Three red dots were painted along one

side of each stick: one was painted at each end and one was in the centre. Both ceremonial

bundles are held by the Ethnological Collections at the Royal Ontario Museum.

Figure 5.25: Offerings that Dewdney found at DiKm-4 called Site # 93, Annie Island in 1960.

Figure 5.26: Offerings that Dewdney found at DjKq-10 called Site # 95, Picture Rock Point in 1960.

Several sites (DiKn-l, DgI<l-2, DhKm-l, DhKm-3, and DgI<l-17) had very large

number of offerings, consisting of several types of offering, including tobacco, clothing,

alcohol bottles, and coins. This size of the offerings was quite unexpected based on the

previous literature from this region and elsewhere in the Canadian Shield.

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. ,r-' ...

Professional divers also searched the bases of cliff faces for possible submerged

offerings at some of the pictograph sites that l examined. While DiKn-l, DhKm-3, and

DgI<1-2 had offerings only ab ove the water level, large quantities of offerings were also

found below the water level at DhI<in-l and DgKl-17.

At DiKn-l five piles of tobacco and cigarettes as well as a snuff box lid were found

in the various cracks in the cliff face (figure 5.27). Three sample-size Crown Royal whisky

bottles were found as well as several unidentifiable alcohol botdes, some clothing, and some

coins (three 25 cent pieces dated 1977, 1989, 1995; one 1 cent coin dated 1989, and one 10

cent piece dated 1994) .

Figure 5.27: The lower part of the DiKn-1, Hayter's Point in 2001.

Two of the Jack Pines growing close together above the same paintings were found

with clothing hanging in the branches. A dress shirt and a towel were found at base of both

the trees and a cloth was tied around one of the trees.

A large range of offerings was found beneath the paintings on the rock bench at

DhKm-3. Tobacco, two cowrie shells hidden in the sedge bush that grew there, a piece of

red cloth, and a faded red cap with the words "Sail Caribbean" embroidered on it were also

found here.

Large quantities of offerings were found above the water level at DgKl-2, including

twenty-seven bundles of wooden dowels. Each dowel was approximately twelve centimetres

long. Bence each bundle measured 12 centimetres in length and between 12.5 and 17

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centimetres in width. Each bundle consisted of twelve dowels painted in red and blue paint

and tied together with white cotton twine (see figure 5.28 below). Twenty-six of these

bundles were found at the entrance of one of the two caves that are integral components of

this rock image site. The site is comprised of a large rock bench and an overhang that

protects both the images and the offerings le ft there.

Figure 5.28: The largest pile of the offerings found at DgKl-2 in June 2001.

One bundle was found at the entrance to the second and rear cave. A large variety of

offerings were also found here, including a large pile of used children's and adult clothing

(trousers, shirts, T-shirts, socks, a chenille sweater, flannel clothes, bandages, an empty

tobacco container with the label "Copenhagen Tobacco," broken clear glass, beer bottle glass

and several single earrings made from plastic and from porcupine quills and silver and blue

beads).

DgKI-2 was visited several times and the pile of clothing appeared larger each time

we returned. About $40.00 worth of tobacco had been left in a large pile beneath the

paintings. Additional offerings had been placed on the rock bench each time we returned.

Yet such offerings were not discovered at the base of this cliff site when it was examined on

August 5th 2001 by the team of divers. The immediate vicinity of the site below the water

level was explored and divers found some garbage, some rocks, as weil as another cave to the

right and 2.14 metres below the surface of the water at the site. Garbage found at the base of

the site included a Mountain Dew soft drink can and a man's bicycle. But objects that could

be classified as offerings including medicine bundles, ceramics, glassware or china plates were

not found at the base of this site.

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DhKm-1, one of a cluster of five sites in the southern part of Whitefish Bay, was

unique in that it had vast quantities of artefacts below the surface of the water at the base of

the cliff in addition to just above the surface of the water in a crack/ cleft in the cliff face.

Above the water level a wide range of offerings was found, including clothing such as

socks, shirts, jeans, a jersey shirt, and a polyester sport shirt in a wide range of colours. Ali

this clothing was stuffed in the crevices (see figure 5.29) and the cracks of this site, with

numerous sample-size alcohol bottles, coins, tobacco, an empty small-size soft drink bottle,

and a towel.

Figure 5.29: Offerings stuffed in the crevice at DhKm-1 in 2001.

Under the water, a wide range of objects was also found, including moccasins, large

quantities of fabric and leather clothes of different styles and different periods. These formed

a huge pile, leaning against the cliff face at a depth of 15.85 metres. Other objects found

included a plate with the maker's mark of Alfred Meaken Royal Ironstone China, England,

which had Queen Victoria's crown, lion, and unicorn on the base. It resembled the bowl

below (figures 5.30 and 5.31) from the water near the pictograph site, DiKm-50, on an island

locally called Horseshoe Island, located north of this site but also in Whitefish Bay.

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Figure 5.30: The Bowl near DiKm-50

Figure 5.31: The Marker's Mark

A glass bottle, which could not be securely dated, was also found at the base of the cliff

where DhKm-1 existed (figures 5.32 5.33, 5.34, 5.35, and 5.36). The glass bottle was hand

finished at its neck but its base was evidently blown into a mould. When the bottle was open

it smelled of juniper. It contained le ad shot and had a cork top covered with hand-tooled

metaI.

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Figure 5.32: The Vial

Figure 5.34: Close-up of Top Figure 5.35: The Lead Shot

Figure 5.36: The Vial Opening

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The glass bottle lay about 1.52 to 1.83 metres away from a section of ceramic pot, also at

15.85 metres below the surface of the water (figures 5.37, 5.38. 5.39, 5.40, 5.41, 5.42, 5.43

and 5.44).

Figure 5.37: Outside of Pot

Figure 5.38: Inside of Pot

Figure 5.39: Side view of Pot

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Figure 5.42: Surface of Pot

Figure 5.43: Base of Pot

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Figure 5.44: Rim of Pot

The pot was dated on the basis of its similarity to those found amongst the grave

goods during Kenyon's excavation of the five Armstrong Mounds (1986: 12-16), which he

ascribed to the Late Laurel period and argued were constructed about 1,000 years ago. Ross

also dated this pot, based upon a careful examination of the photographs above, as being

from the period between 1400 AD. and 800 AD. (Ross pers. comm. August 2001). Meyer

disagrees with this interpretation because he identified it as belonging to the Duck Bay

complex of the Rainy River composite dated by Lenius and Olinyk (1990: 84) as being from

the period between 1100 A D. and 1350 A. D. (Meyer pers. comm. September 2006).

Kenyon (1986) concluded that the principal purpose of the five mounds was to indicate

sacred places and verify territorial occupation. He postulated that large numbers of people

gathered at the mounds in either the spring or the fail, since sufficient food resources were

only available at those times of year. Kenyon found a large number of small ceremonial

ceramic vessels in these mounds (ibid.: 112-116).

By recording what the divers found, it is possible to consider that at least some of

these sites may have a longer life history than previously expected.

DgKl-17 is located on Cyclone Point, Sabaskong Bay, and offerings were found

under the water at the base of the cliff as weil as above water. Tobacco and coins were found

above water in crevices. The divers found a variety of objects underneath the water,

including a bundle of red and white painted wooden dowels, a collection of srurts located

about 6.10 metres from the site, amongst large boulders, and a broken plate dating to the

nineteenth century with the maker's mark of Alfred Meaken. It was found directly beneath a

rock image site.

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Conclusion:

Not ail the pictograph sites had offerings when they were examined in 2001.

Although the images at these sites are not great in number, it is clear from the vast range and

quantity of offerings that the physical locations and the paintings are and were important.

Ethnographic evidence was provided as to the importance of offerings in this region

(Densmore 1974 [1928]; Hilger 1936; Coleman 1947; Warren 1984 [1885]; Smith 1995; and

Pufahl 1990). Yet offerings left above water are always investigated by archaeologists who

examine pictograph sites in the Lake of the Woods (Fox 1974; Dewdney and Kidd 1962,

1967; Lambert n.d., Pastershank 1989; Reid 1975, 1976). Hence offerings of any type and

size were sought for when these sites were examined in 2001.

Sixteen pictograph sites did not have offerings of any type and two of these sites

existed in caves. This group included DgKI-19, DgKm-1, DiKm-49, DiKm-50, DiKm-51,

DgKm-2, DhKm-18, DhKm-19, DhKm-4, DiKm-3, DiKp-1, DjKn-1, DjKr-2, DkKn-7,

and DkKn-6. Offerings were found at only one of the newly discovered sites on a cliff face

cailed DhKm-20. A wide range of offerings were found at the remaining eleven sites, where

offerings invariably consisted of either one or a combination of items including tobacco,

chinaware, clothing, and alcohol bottles. However, substantial quantities of offerings were

found at DgI(l-17, DhKm-3, DhKm-1, DgI(l-2, DjKr-23, and DhKn-1. These offerings

included builets, feathers, chinaware, a hand-blown glass bottle, a smail ceramic bowl, and

bundles of prayer sticks. However, this range of objects was not unusual since Dewdney had

found offerings of chinaware and enamelware at DhKm-18, DhKn-1, and DiKn-1 and

prayer sticks at DhKm-5, DiKm-3, DjKq-2, DhKm-18, and DiKm-4 in his 1960 field

season.

Large quantities of offerings were found during the 2001 field season both above and

under water at several sites. The presence of the offerings underwater enables one to posit

that these sites and not just the images have had considerable importance for a long period

of time, possibly in the case of DhKm-1 back to at least 900 AD. It would have been

interesting to establish what was at the base of ail of the pictograph sites in the Lake of the

Woods, but as 1 stated in Chapter IV it was only possible to rely upon the services of the

divers when they were free and not involved in rescue work elsewhere in the Lake of the

Woods.

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Section 6: Discussion of dates

Dating these images is very difficult, because the local indigenous Algonquian­

speaking peoples do not permit the removal of pigment samples necessary to accommodate

direct dating techniques from the sites. This is unfortunate because the dating of small

samples of pigment would provide secure dates for different images. Such information

would provide researchers with the ability to establish the first time that a place was used as a

pictograph site. If a series of dates was established for a collection of sites in a specifie

geographic region it might be possible to determine whether a sequence of styles existed in a

region and if different styles of paintings at a site were concurrent or sequential. Dewdney

(1970a) realised that considerable potential existed in the new techniques being explored at

the time, since his colleagues worldwide were trying to correlate the style of an image with

finding a way of providing a secure date for it. Dewdney (1970a) suggested that future

pictograph studies ought to include taking samples of the paint of these paintings as well as

the rock substrate on which the paintings existed. He argued that it was important to do this

research as well to be as objective as possible regarding the description of the images

themselves. Dewdney argued that advances in Scanning Electron Microscopy or analysis

using lasers might aid in establishing the date of the paintings.

But the difficulties in dating the paint has not meant that researchers were not

interested in the paint. During the early 1970s, researchers were concerned with questions

regarding the conservation of the paints utilised for creating these red images, conservation

of pictograph sites themselves in the Canadian Shield, and discovering new and different

ways of examining them were dealing with paint samples from pictograph sites (Myers and

Taylor 1974; Taylor, Myers and Wainwright 1974,1975; Wainwright 1990,1997; Wainwright

and Taylor 1977). Unfortunately, although Wainwright and his colleagues undertook

analytical work on paint samples taken from various sites in the Canadian Shield, this

research did not continue.

Several solutions for dealing with this problem of establishing a date for these images

can be proposed, given that samples of the pigment cannot be removed and dated. One

solution would be to use independent evidence of when these images were created. The site

may have been in use and rock images created both before and after the specifie objects were

left or abandoned there. The other kinds of artefacts left at sites can often be dated but they

only indicate that the site was visited by people who traveled through this region at a

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particular time. An examination of these objects provides the archaeologist with a time frame

during which the site was visited. Perhaps the physical locale itself and not just the images

were considered important for a period of time. Another solution to this problem might be

to establish the time period during which rock images may have been created by examining

the rate of deterioration of such images using photographs and drawings of the sites that

were made by archaeologists who had previously recorded these sites. The final solution is to

consider the stylistic changes that have occurred with regards to the images at these sites.

The images at the site that l already knew of prior to conducting fieldwork resemble those

found elsewhere in Northern Ontario. However, a considerable number of modern images

were found, either with datable information or stylistic features that en able archaeologists to

determine their age.

It is possible to consider three questions:

(a) Is there independent evidence of when these paintings were created?

(b) Is it possible to calibrate the rate at which white mineraI deposits accumula te,

rock tripe and lichen grow and spalling occurs?

(c) Have the images present at pictograph sites changed stylisticaIly over time?

The first question seeks to obtain calendar dates. The second question seeks to

resolve the question of the age of these images using relative dating since it seeks to calibrate

the rate at which these processes develop. The third question also uses relative dacing to

establish the rate at which the stylistic changes have occurred. AlI three solutions require

detailed examination of aIl the documentation on the pictograph sites in the Lake of the

Woods.

Unfortunately, it was impossible to ob tain a complete set of aIl the recordings, slides,

and photographs of each site. Sorne of this material is not in the public domain because it

has not been published, other examples remain in the safekeeping of archaeologists for their

own future research, and sorne of this information has been lost or it is impossible to

de termine where it may be kept. Slides also decay over cime, frequently regardless of the care

and expense taken to preserve them. Most of the colour decays and the film turns red. This

creates problems if one is attempting to ascertain the changes in images that were created

from red ochre because it is difficult to determine whether the red that is visible is that of the

slide film or of the image in question. The photographs of each site taken in 2001 will be

compared with the first photograph taken of the site and any subsequent photographs. l will

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present as much of trus visual information as possible to establish any visible changes over

time. Twenty-seven pictograph sites will be examined for trus study. It may be odd to include

the sites that were only discovered in 2001 since only one set of documentation exists.

However, the paintings at ail of the sites in trus group were different since sorne were created

sorne time ago in ochre, others were painted in modern spray paints with a date, others were

created using modern paint over older ochre images, and one site solely consisted of an

image in modern spray paint. It is important to include these "newly" discovered sites since it

enables the trurd question of whether the images have changed stylistically over time to be

considered.

DgKl-1:

It is unclear from Dewdney's notes, held by the New World Archives at the Royal

Ontario Museum, whether it was this site or Site #198, in figure 5.45, that Dewdney heard

about from an informant caIled S. C. o. Linklater, who in turn had been told about the site

by Bob Arcrue from Morson, Ontario, on May 29th 1963.

Figure 5.45: Setting of Site # 197.

Dewdney caIled DgKl-1 # 197 in 1965 (see figures 5.46 and 5.47) and recorded it at the same

time as DgKI-2, caIled Site # 198, wruch exists nearby. It is clear from two photographs

below that he did not see the red image on the rock on the left of the cliff face. Dewdney

clearly indicates in the tides of the slides of these photographs reproduced below that there

are only two faces. However, today there is a red image that exists to the left of rus Face 1

which is also to the le ft of the vertical white mineraI deposit. Trus observation is supported

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by the images in his field drawing of the site in figure 3.21. Wh en viewing his photographs, it

is important to remember that the redness of the slides reflects the fact that the slide film is

old and decaying.

Figure 5.46: Face 1 Site # 197 by Dewdney in 1964.

Figure 5.47: Face 2, Site # 197 by Dewdney in 1964.

Pastershank in 1989 examined the same site but argued that this site had three faces rather

than two. Dewdney's Face 1 became her Face 2 and his Face 2 became her Face 3 (figure

S.48).

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Figure 5.49: Face 3 of DgK1-1 by Pastershank in 1989.

Lichen and rock encroachment has not occurred but the red shapes have faded between the

cime when the images were photographed by Dewdney in 1964 and Pastershank in 1989 in

figures 5.48 and 5.49.

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Figure 5.50: Photograph of DgKl-2 in 2001.

By 2001, the vertical white mineraI deposit near the diagonal red line on the left hand side

had increased in size in figure 5.50. The paintings, on the left hand side, now suffer from

lichen encroachment but rock tripe is not a problem. The rock surface where the two

creatures exist on the le ft hand side of the site have begun to crack and exfoliate, but

otherwise the images appear to be in a similar condition to what they were in 1989.

DgKl-2:

Dewdney made it clear in his book published with lZidd in 1967 that Site # 198 is the

same as DgKl-2 since he identified two finger drags next to a smear (Dewdney and lZidd

1967: 110) in figure 5.51.

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Figure 5.51: Face 1 of Site # 198 by Dewdney in 1964.

Dewdney stated, in field records held by the New World Collection at the Royal

Ontario Museum, that "over the hole the roak [rock] is well smeared". Yet he did not record

this smear in his field drawing of Site # 198, even though the smear over the hole clearly

appears in Dewdney's photograph above, in figure 5.51, but not in his recording of the site in

figure 3.21. The fact that he ignored the smear, in figure 5.52, perhaps reflects his belief,

when he recorded this site, that smears did not constitute images, as discussed earlier in this

chapter.

Figure 5.52: "Cave" at Site # 198 in 1964 by Dewdney.

Unfortunately, given the deterioration of the photograph above (figure 5.52), taken by

Dewdney in 1964, it is impossible to establish how quickly the images, as opposed to this

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slide film, are decaying. Pastershank, with her crew in 1989, recorded the site again, and

designated the part recorded by Dewdney in 1964 as Face 1 since the paintings that were

evident had obviously increased in number (figure 5.53). She subdivided this site into eight

faces, which she designated with roman numerals. By 1989, smears were obviously accepted

as legitimate shapes causing an increase in the size of the site. Each face was determined by

the presence of identifiable images. Pastershank identified four hand prints and suspected

that a fifth existed, as weil as three finger strokes on the central part of the red smear that

covered Face II (figure 5.54). She noted that the rock surface was crumbling and spailed and

that "mineraI seepage" was evident both above and to the sides of the red ochre smear. She

also observed (1989: 59) that smail colonies of lichen had started to grow throughout this

part of the rock face.

Figure 5.53: Pastershank's Face 1 by Pastershank in 1989.

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.~.

Figure 5.54: Faces II, III and IV by Pastershank in 1989.

In 2001, my crew and 1 discovered four new images at DgKl-2. Three of these were

superimposed over older images that Pastershank had recorded in 1989 as evident in figure

3.25. But unfortunately, almost ail the images Pastershank had identified, except for two

recognisable handprints and some parailel lines, were very pale and next to impossible to

distinguish. The disappearance or fading of the images recorded by Pastershank in 1989

could be a consequence of the exfoliation of the images, possibly in conjunction with the

deposition of mineraIs. Mineral deposition often causes a white deposit to form on images

painted using ochre. The new paintings found in 2001 were created using some modern paint

instead of ochre. The new paintings exist both on top of and beside paintings described by

Pastershank (1989), and large quantities of offerings were discovered in the 2001 field

season. Three of these new images, an animal, a six pointed star and a quarter crescent

moon, were superimposed on older paintings as weil as direcdy on the rock surface that

Pastershank (1989: 54-63) had described, recorded and photographed. The fourth new image

was created, not on any of the designated Faces, but was placed beside the area cailed a "site"

by Pastershank. This image (figure 3.26) is radicaily different from any of the new images

since it is hoilow rather than solid.

None of the new images were affected by rock tripe and lichen encroachment, large

quantities of white mineraI deposits or obvious signs of exfoliation. But, it is clear that the

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images that Pastershank had recorded in 1989 are paler, most probably as a consequence of

white mineraI deposits rather than exfoliation or lichen and rock tripe encroachment.

DiKm-3:

Dewdney recorded this site, now called DiKm-3, as Site # 28 on August 15th 1953

(figure 3.10). Dewdney found this site as the result of a letter dated 3/7/1946 from a

gentleman called Alfred Kundert from Madison, Wisconsin. He had written to the Travel

and Publicity Bureau in Toronto to inform them that he and a friend of his, called Mr. W. W.

Lauterback of South Bend in Indiana, had found a pictograph site in Whitefish Bay. Kundert

enclosed some coloured drawings and slides and wrote that the site was approximately three

miles out of Sioux Narrows. The letter from Alfred Kundert was subsequently forwarded by

the Travel Bureau to Kenneth I<idd, who subsequently sent it to Dewdney (Dewdney's

notes, New World Archives, Royal Ontario Museum). Dewdney' field recording in figure

3.10 and his photographs below in figures 5.55 and 5.56 show that white mineraI deposits

have accumulated and lichen and rock tripe encroachment is a problem.

Figure 5.55: Setting from distance of Site # 28, Sioux Narrows by Dewdney in 1953.

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Figure 5.56: Face 2 and 3 of Site # 28 by Dewdney in 1953.

The rock tripe is growing verticaily across the pictographs. Many of the images remain clearly

visible but they are affected by the accumulation of white mineraI deposits on the rock

surface as weil as by lichen and rock tripe in figure 5.56. In 1991 I visited the site while on a

fishing trip and I took the photograph in figure 5.57.

Figure 5.557: Close-up of DiKm-3 taken in 1991.

When the photograph in figure 5.57 is compared to Dewdney's photograph in figure

5.56 it is clear that lichen and rock tripe growth and the accumulation of white mineral

deposits have increased since 1959 but at a slow rate. It is impossible to establish whether

exfoliation has occurred. It would therefore be expected that, if the photographs taken in

1991 (figure 5.57) and 2001 (figure 5.58) were compared, changes would have occurred with

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respect to the accumulation of white mineraI deposits, rock tripe and lichen encroachment as

well as exfoliation. But very few changes have occurred.

Figure 5.58: Close-up of DiKm-3 taken in 2001.

DhKn-1:

Dewdney first recorded this site on August 19th, 1960 as Site # 106 (figure 3.11). In

his notes, Dewdney indicated that S. C. O. Linklater had informed him of the site's existence.

ln turn, Jim Comegan from Morson, Ontario, had told Linklater about the site on May 29th,

1963. Comegon reported that he could see the images from the water: "figures are mosdy

marking and pictures. It seems to me 1 saw a picture of a turtle" (Dewdney's notes on file at

New World Collection, ROM).

Lichen growth was a problem at this site and it appears that Dewdney removed it by

"sponging" some of it off. He noted that some of the species of lichen on the images could

not be removed, so he speculated about how it had affected the images. Dewdney

interpreted the image on Face 1 as a "horned snake sturgeon" (Dewdney's notes on file at

New World Collection, ROM). Unfortunately, 1 could not find the colour photographs or

slides that he stated were "excellent." Dewdney did not discuss the presence of lichen and

rock tripe growth for Face 2 in his notes but 1 did find a photograph of Face 2 of this large

site, and none seems to have been present. This could be because Dewdney removed it.

When the photograph below (figure 5.59), taken by Dewdney, and his field drawing (figure

3.11) are compared to one another, it is clear that he did not record the large red smear that

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. ~.

existed above the turtle and creatures, and only part of the smear that existed below these

Images .

Figure 5.59: Face 2, Site # 106 by Dewdney in 1960.

Dewdney wrote in rus notes, that the rock face of thls part of the site was "extremely rough"

and that the red in rus watercolour below (figure 5.60), made from rus rice paper and red

paint, rus field recording, was "not reliable," since "it should be a rustier red." Furthermore,

Dewdney has not recorded the smears evident in his photograph above.

Figure 5.60: Site # 106, Sabaskong-Obabikon Channel, Watercolour reproduction of Face II by Dewdney.

Dewdney did not comment on the accumulation of wrute mineraI deposits, lichen, or

plant growth of any type on the rock's surface, or on possible exfoliation of the rock.

Molyneaux examined and photographed trus site in 1974 for a project he conducted in

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conjunction with the Department of Anthropology at Trent University. l was able to obtain

a copy of the report on this project. He was principally concerned only with the first group

of paintings at this site, in particular the "very large lizard-like representation" that he

measured as being over 4.5 metres (15 feet) in length (1974: 11). Molyneaux assessed Site #

106 as suffering from "granular exfoliation" which preceded the creation of the paintings

(ibid.). The site was also deemed to show evidence of "minor encroachment of lichen

colonies" (ibid.).

The site was photographed in 2001 and compared with the photographs above from

1960, figure 5.59, and 2001, figures 5.61 and 5.62, revealed that exfoliation has occurred,

since the images are paler in 2001 than they were in 1960. Lichen and rock tripe

encroachment is a problem for sorne of these images but it is difficult to establish the

accumulation of white mineraI deposits.

Figure 5.61: Close-up ofleft hand part of DhKn-1 in 2001.

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Figure 5.62: Close-up of right hand part of DhKn-1 in 2001.

DhKm-1:

It is evident that in Dewdney's field drawing (figure 3.7) of Site # 92 A and Site # 92

the two sites DhKm-1 and DhKm-4 were combined. Dewdney found and recorded both in

1960, but he classified them as one site. He also did not record the encire site. Dewdney's

Face l is DhKm-4 while rus Face II and III are part of DhKm-1, as evident in figure 3.13,

Chapter III. DhKm-4 is not immediately adjacent to DhKm-1, as Dewdney's field drawings

of both sites imply. However, why Dewdney only recorded the images from part of DhKm-

1, wruch he cailed Site # 92, is unclear. Indeed, the sites are more than a few metres apart

from each other as the annotated photograph in figure 3.12 indicates. Dewdney did not

record ail the images, and he missed an image now classified as a smear as indicated by the

annotated photograph in figure 3.13, and Dewdney's photograph of the site below in figure

5.63.

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Figure 5.63: Setting "the hole" at Devil's Hole Site # 92 by Dewdney in 1960.

Sorne red vertical images are visible on the left hand of the photograph above as is

the red smear in the area that Dewdney did not record. Ali of the images are quite bright. It

is difficult to determine the level of exfoliation. Lchen and rock tripe clearly has not affected

them and white mineraI deposits are not superimposed over these images.

Figure 5.64 Setting with W. F. and offerings beside Site # 92 by Dewdney in 1960.

It is difficult to de termine the physical status of the images of DhKm-1 in figure 5.64

since the photograph is very bright and perhaps suffering from age. Fox examined the site in

September 1974 (1974: 3) and did not describe the images that he found, since he was more

concerned with the offerings left in the large cleft at the site. If the photograph below (figure

5.65), taken in 1974, is compared with figure 5.66, taken in 2001, it is clear that the water

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level was considerably higher in 2001 than it was 1974. Unfortunately, it is very difficult to

de termine from figure 5.65, taken by Fox, the physical state of the images recorded by

Dewdney fourteen years before. It is evident that the smear that he ignored is wide and

relatively unaffected by lichen and rock tripe encroachment. Yet, it is impossible to

determine whether white mineraI deposits have started to accumulate and exfoliation of the

rock surface is present.

Figure 5.65: DhKm-1 taken in September 1974 by W. Fox.

Fox used the Borden number rather than Dewdney's number of Site # 92, since the

site was reported by Herbert Bergman on 13th September 1973 under the Ontario Heritage

Act as a separate site from Dewdney's Site # 92A. Molyneaux (1974) stated that many of

these images were smears (ibid.: 9) and that "extensive exfoliation" had occurred at this site

(ibid.: 8). Images previously described no longer were visible, which implied for Molyneaux

that they were applied on areas of rock now exfoliated. He asserted that the high water line at

this site hindered the accumulation of mineraI deposits and the growth of lichen and rock

tripe, but that contact with water may "have contributed to the "fading" of the paintings"

(ibid.).

Lambert, in his (1985) unpublished study of some of the pictograph sites, made the

mistake of considering some of the paintings of DhKm-1 as part of DhKm-4 (figure 3.14),

despite Reid (1976) having reported in May 1975 that the two sites were separate entities

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with their own Borden numbers. It is difficult to determine why Lambert was confused since

he would have known that Reid had already designated DhKm-1 as a separate entity from

DhKm-4. lndeed it is clear from rus own records, that Lambert (n.d.) knew of Dewdney's

1973 publication and had probably seen Dewdney's 1960 field drawings of DhKm-4 and

DhKm-1 (figure 3.7).

Lambert argued that that the images suffered from fading since they were directly

exposed to the sunlight and "repeated wasrung by water action". He argued that the

deposition of white mineraI deposits was the biggest problem for this site as a whole, while

lichen development was the heaviest in relation to the right hand images that he recorded

(ibid.: 68). He recorded that precipitate, which can be identified as wrute mineraI deposit, was

"apparent in the highest elevations" (ibid.) wruch presumably means it existed at the top of

the rock face in question. Although Lambert recorded other smears at trus site he did not

record the smear that Dewdney also missed. Lambert (n.d.: 85) argued that panel iv existed

below the horizontal crack and that it was "highlighted by the ochre smear" that he identified

on the rock surface on either side of this "fissure." Despite this drawback, the rest of the

paintings he identified as existing in 1985 were still present in 2001, visible in figure 5.66.

Figure 5.66: DhKm-1 in June 2001.

It is difficult to clearly see some of these images as a consequence of the rock tripe

and lichen encroachment in conjunction with exfoliation. White mineraI deposits are also

problematic for some of the images in conjunction with lichen and rock tripe encroachment.

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Comparison of the images, in the photographs taken in 2001 and the field drawings by

Lambert in 1985, reveals that the deposition of white mineral deposits for sorne images and

exfoliation for others has caused them to be paler than they were when Lambert recorded

them.

DhKo-l:

Dewdney published his drawings of this site in 1960 (figure 5.69), nine years after

Kathleen Campbell photographed it (figure 5.68). Dewdney used drawings of the images at

this site, instructions on how to find it, and a sketch map showing its location in the Lake of

the Woods that he had found in an archaeological file held by the National Museum of

Canada, Ottawa. He transcribed the letter that accompanied the drawing and the sketch map.

It stated that the pen and ink sketch map and the drawing below (figure 5.67), were made by

Howard T. Thompson on 9 November 1936. The text beside the drawings of the images

stated that they were "deer, fish, sun passage, devil. It is hard just to remember to the point.

Of course the body and the legs are just straight lines". Thompson was a guide in the Lake of

the Woods from Minahico, Ontario. He wrote that the site, or "Indian inscriptions" as he

called them was first found in 1910, but the physicallocation of the site was known by all the

boat captains who worked in the Lake of the Woods prior to this date. He noted that he did

not know who the authors of these images were, although he had questioned many of the

local Indian guides about these pictographs at Painted Rock Island. No one had been able to

give him any information about these images.

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Figure 5.67: Thompson's Drawings of the images at the pictograph site.

Dewdney also recorded this site and his field drawing (figure 5.69) supports

Thompson's field description of the rock on which the paintings were found. Thompson had

described the rock face as "a square rock projecting out from a cliff'. Unfortunately,

Thompson did not describe the physical condition of the images, although he had described

sorne of the images present at this site. Therefore, it is impossible to draw any conclusions as

to the level of lichen and rock tripe accumulation from his information. Yet, given that

Thompson described the site in the manner that he did, it is possible to posit that the images

he described were not affected by lichen and rock tripe.

This site was first photographed in 1951 by Kathleen Campbell who was the lndian

Health Nurse for the Lake of the Woods region and travelled to the indigenous and the

white communities in the area. She always took her camera with her and photographed

things that she found interesting (K. Campbell pers. comm. 2001). She had thought that the

photograph below in figure 5.68 was not very good and so she returned to the site a few

weeks later to get a better photograph. However, she discovered that the red images had

been covered in religious slogans such as "Jesus saves" (K. Campbell pers. comm. October

2005). Her photograph indicates that the images were severely affected by lichen and rock

tripe encroachment as weil as black deposits that have mn down from the top of the rock

face. If this is compared with Thompson's field drawing of 1936, inconsistencies are evident.

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Severai of the images that he described in words and drew were, by 1951, probably covered

in lichen and rock tripe as weIl as by vertical black stains. Small plants grow in the crevices of

the rock surface.

Figure 5.68: DhKo-1 by K. Campbell in 1951.

When CampbeIl's photograph above is compared with Dewdney's field drawing

below (figure 5.69) and his photograph (figure 5.70), it is clear that there are inconsistencies

between the images captured in Dewdney's photograph below and those in CampbeIl's

photograph featured above. Larger numbers of images are evident in Dewdney's field

drawing than appear in CampbeIl's 1951 photograph because Dewdney removed the lichen

growing on the images. lndeed, he stated that the site "was extensively overgrown with

lichen" (Dewdney and Kidd 1967: 46) and he used his sponging technique to rem ove the

lichen which was "fairly easy to scrub off" (ibid.). Dewdney wrote on rus field drawing below

that lichen had obscured sorne of the images but he did not state that he removed it so that

he could see the images below. However, Dewdney stated in the 1967 publication (Dewdney

and Kidd 1967: 46) that sorne of the images had suffered from weathering. Nevertheless,

both CampbeIl's 1951 and Dewdney's 1960 photographs demonstrate that white mineraI

deposits had accumulated on the surface of the rock beneath the images and possibly on the

images themselves.

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pu;<lio.h ç",~s·s,""~n "'.iN>

t",,~«lir i"I0.,.~~t..' 6tnF ....

5It""#/OB' Pail1tetll<ock /sl<7acf s()vtll of Spa/' Rock /s/crncf, wl<e ofrlie Woods

"

Figure 5.69: Dewdney's field recording of Site#108 undertaken on August 20 August 1960.

Dewdney's photograph of the site, below, confirms his sketch of the site's rock

formation he provided as well as the images he found and described above. The photograph

below (figure 5.70) is rather blurry, and sorne distance from the site but it was the only slide

of this site in Dewdney's collection held by the ROM. Unfortunately, both the distance and

the blurriness makes it difficult to determine the extent to which the lichen and rock tripe

encroachment, accumulation of white mineraI deposits, and the level of exfoliation affect the

paintings. Dewdney removed sorne lichen and rock tripe to increase the number of images

visible, and a photograph was not taken of the site prior to the lichen removal. Therefore, he

took the photograph after he removed the lichen. However, it does indicate that the

"vandalism" observed by Molyneaux in 1974 was present in 1960. Molyneaux, in 1974, stated

that a large grey patch existed to the left of the paintings (1974: 12) at this site. Yet, whether

this grey patch covered the religious slogans described by K. Campbell as existing at the site

in 1951 is unknown sin ce neither Dewdney nor Molyneaux mentioned the presence of any

religious slogans when they described the images at this site.

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Figure 5.70: Dewdney's photograph of Site#108.

Molyneaux appears to have obtained a Borden number for this site in 1974, and

called it DhKo-1. His project was conducted in conjunction with the Department of

Anthropology at Trent University. He examined DhKo-1 again in 1981. He published a

section of the site in Archaeology in 1987. Unfortunately, it is impossible to determine when

the photograph in figure 5.71 was taken. However, its existence permits some comments on

a few of the images at this site.

Figure 5.71: Section of DhKo-l taken hy Molyneaux.

Very little lichen is present on these red images. Yet, his report from 1974 described

the rock's surface as being "covered with a heavy mineraI deposit but the paintings appear to

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be superimposed on this altered surface" (ibid: 12). Exfoliation was classified as "minor",

while the lichen was described as being in "colonies obliterating large sections of the

paintings" (ibid.). Molyneaux argued vandalism had occurred to the left of the images at this

site because of a large grey patch that according to Molyneaux had caused images to be

"obliterated by paint' , (ibid.). He concluded that the "extensive biological growth,"

presumably the large quantity of lichen, in conjunction with its physicallocation "in a heavily

used passage" in the Lake of the Woods caused the site to be "relatively uns table and in need

of protection" (ibid: 13).

The site was photographed in 2001 (figure 5.72), and when the photographs from

1951 (figure 5.68) and 1960 (figure 5.70) are compared it is evident that someone has

removed lichen and rock tripe. Otherwise it would have been impossible to see the images

that Dewdney recorded and photographed, sin ce it is likely that the lichen and rock tripe

would have covered them over. It is possible to argue that this site suffers from sorne lichen

encroachment and the accumulation of white mineraI deposits. Rock tripe encroachment has

started to occur, but whether exfoliation has occurred is very difficult to establish (figure

5.72).

Figure 5.72: Overview of DhKo-1 in 2001.

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;--..

DiKm-4:

Dewdney recorded Site #93 on July 15th 1960 (figure 5.73).Joe Major from Morson,

Ontario, reported this site to S. C. O. Linklater. The image was described as a "figure about

two feet above water" (Dewdney's notes in New World Collections, ROM).

an 'bf'krirNj S Île '1

,><

\. f V ! \

) 1 \

\

) \ )

(':.~) ,&,-tif':

".

,,'

,,'

!ll/fr,"r tÜ,,"1l. .wat"/2r"

I~vq{

IM'j 1)': Ij.~

CtU:tt$TOPlifR pEWDNEY

Figure 5.73: Dewdney's Site# 93 which he called an "offering site" inJuly 1960.

Figure 5.74: Setting of Site # 93 hy Dewdney in 1960.

Dewdney stated (Dewdney and Kidd 1967: 53) that the images at this site were

difficult to find since the rock face had vertical lines of black lichen as in figure 5.74. He

stated that he almost did not find the paintings because the rock's surface was "was streaked

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with black lichen whose edges were scalloped ln rhythm with the undulations of the

pictographs" (ibid.).

Figure 5.75: Jerry Corpine at Site # 93 by Dewdney in 1960.

The images in figure 5.75 taken in 1960, visible behind the gendeman, are unaffected

by white mineraI deposits, exfoliation, and rock tripe and lichen encroachment.

Molyneaux recorded this site in 1974. In his field report, Molyneaux observed that

the site was "partially covered by a white mineraI deposit" and there was evidence of slight

"exfoliation near the head of the figure" (1974: 6). He also observed that lichen grew near

the images but had not encroached upon the images themselves.

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Figure 5.76: DiKm-4 by Molyneaux. Figure 5.77: DiKm-4 by Pelshea in 1978.

Four years later Molyneaux (1979) examined the site again. A photograph of trus site

was published with an article in Rotunda, the magazine of the Royal Ontario Museum, in

1980. Although this photograph (figure 5.76) is black and white and not colour, it is possible

to conclude that these images do not suffer from lichen or rock tripe encroachment or the

deposition of white mineral deposits. However, wrute mineraI deposits do exist on trus rock

surface below the images, as is evident in Dewdney's photograph of 1960, above (figure

5.75). The images have not changed a great deal when trus photograph is compared to

Dewdney's, taken twenty-four years earlier. It is impossible to conclude anytrung secure

regarding the level of exfoliation of the rock surface, since it is difficult to conclude whether

the surface of rock is spalled. Molyneaux (ibid.: 7) implied in his article that rus photograph

of DiKm-4, in figure 5.76 above, was taken during the field season of 1973 when the water

level was low. Pelshea photographed the site in 1978 (figure 5.77). It is clear from rus

photograph that the images did not suffer from the accumulation of white mineraI deposits,

rock tripe or lichen, or exfoliation. If rus photograph is compared with Molyneaux's, possibly

taken in 1973 (figure 5.76), it is clear that the images are still quite distinct and that little

evidence exists of the accumulation of wrute mineraI deposits and exfoliation on the images.

However, lichen encroachment has started to occur at the right hand side of the 'v' at the top

end of the vertical zig-zag. Rock tripe encroachment has not started to grow.

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('.

Figure 5.78: DiKm-4 taken in 1991. Figure 5.79: DiKm-4 taken in 2001.

l took the photograph above (figure 5.78) in 1991, when l went on a fishing trip in

Whitefish Bay. By this time, the orange lichen at the top of the zig-zag image had begun to

encroach. White mineraI deposit was underneath the images. The black lichen on either side

of the images has not affected them and exfoliation is not a problem. If this photograph is

compared with Pelshea's 1978 (figure 5.77) and Dewdney's 1960 photographs (figures 5.74

and 5.75), it is evident that little has changed.

If the photographs taken in 1991 (figure 5.78), and 2001 (figure 5.79) are compared,

one can see very little difference between the two. Hence, it is possible to conclude that the

lichen and the rock tripe colonies have not radically increased in size. But there has been an

increase in white mineraI deposits. Even so, rock tripe and lichen, white mineraI deposits and

exfoliation are not a serious problem for the images at this site. Lichen encroachment is

present at the right end of the 'v' of the vertical zig-zag and rock tripe has begun to grow on

the rock surface to the left of the vertical stick figure. This rock tripe is not evident in the

photograph l took ten years earlier.

DhKm-3:

Dewdney recorded this site as Site#69 on 8th August 1959. He did not provide any

information as to the conditions of the images on his drawing in figure 5.80.

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#69 P,dure Roe/; J,jond Wliifdf5h 8°il,Lake of the Woo,," Au.g8-59

FaceI

I[.-7Sm

FCI~J1l

CHR.ISTOPHER. DEWDNe:Y

Figure 5.80: Dewdney's field drawing of Site # 69 called Picture Rock Island undertaken on 8 August 1959.

Dewdney argued that the pigment was "indissolubly bonded to the rock - for how

long is anybody's guess" (Dewdney and Kidd 1962: 55). He subdivided the images at this site

into three Faces. The turtle, which he designated as belonging to Face 1 (figure 5.81),

suffered from lichen encroachment (ibid: 54).

Figure 5.81: Face 1 of Site # 69 in Whitefish Bay, Lake of the Woods taken by Dewdney in 1959.

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Figure 5.82: Face II of Site # 69 taken by Dewdney in 1959.

Dewdney did not provide any comments regarcling Face II (ibid.); however, it is

evident from the photograph above that large quantities of white mineraI deposits were

superimposed over many of the red images in figure 5.82. It is clifficult to determine whether

exfoliation was a problem but it is clear that lichen existed on the left hand side of the images

in the area between Face l and Face II. Whether this affected images is unknown.

Dewdney clid comment that sorne of the images on Face III were fainter than others

in this section of the rock image site (ibid.: 55). l was unable to find a photograph taken by

Dewdney of this part of the site when l examined his collection of slides held by the Royal

Ontario Museum. However, l found a watercolour of these images that he created (figure

5.83).

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Figure 5.83: Water colour reproduction of Face III of Site # 69 by Dewdney in 1959.

Molyneaux recorded this site in 1974. He published a black and white photograph of

this site in Rotunda in 1980 (figure 5.84). Since it is so smaIl scale and dark it is very difficult

to establish any fine details regarding the images. However, if they are compared with the

same images in Dewdney's photograph taken in 1959 it is clear that many of the images have

strongly defined edges. Unfortunately, because this photograph is black and white, it is hard

to establish whether the images near the lichen and rock tripe are encroached on at aIl. It is

also hard to determine whether the accumulation of white mineraI deposits has increased

since Dewdney photographed these images in 1959.

Figure 5.84: Black and White photograph of DhKm-3 taken by Molyneaux.

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Pelshea photographed this site in 1978 (figure 5.85). Sorne of the images were clearly

affected by white mineraI deposits. Lichen has grown on the right hand side, or Face III as

Dewdney termed it. The extreme left hand side of the pictograph site is not visible.

However, the lichen visible on the left hand of the photograph, in figure 5.85, was also

present at this site, as it was in 1959 when Dewdney recorded it.

Figure 5.85: The images at DhKm-3 taken hy Pelshea in 1978.

If figure 5.85 is compared to Molyneaux's photograph, in figure 5.82, it appears as if

the images on the white mineraI deposits in the middle of the rock face are paler in Pelshea's

photograph. It is impossible because of the angle in which the photograph was taken as weIl

as the level of exfoliation to deterrnine whether the lichen and rock tripe have increased in

quantity. The three photographs below taken for my doctoral research indicate the physical

status of the images in 2001 (figures 5.86, 5.87, 5.88)

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Figure 5.86: Left hand side of DhKm-3 taken in 2001.

The images on the far left are the most severely affected by lichen. It was impossible to

de termine whether images exist below the large vertical swath of black and light green lichen

on the rock in the middle of the photograph. The white evident on the surface of the rock is

mineraI deposit. The photograph in figure 5.86 demonstrates that there are large numbers of

faint pale red images superimposed on the white mineraI deposits. These faint images are

clearer than the paler images on the rock surface that are not covered in white mineraI

deposits (indicated in figure 5.87). These very pale images are present in Pelshea's 1978

photograph but Dewdney did not record them in his drawing or his photograph from 1959.

Figure 5.87: Annotated section of DhKm-3 by Colson taken in 2001.

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Although paler than those superimposed over the white mineraI deposits, they are, perhaps,

contemporaneous in age because they are the similar physical proportions. In the far right,

evident in the third photograph (below in figure 5.88), it might be expected that there are

images in the area between the white mineraI deposits yet none exists here. The images

evident in the photograph below are only affected by white mineraI deposits, sorne of them

to the point that they are fainter than their neighbours. Lichen or rock tripe does not exist

here. Unfortunately, it is difficult to establish whether exfoliation of the rock surface at this

site is a problem.

Figure 5.88: Right hand end of DhKm-3.

DhKm-4:

Dewdney recorded this site as Face 1 of Site # 92 A on J uly 15th 1960 in figure 3.7. It

is important to remember that Face l is DhKm-4 and Dewdney's Faces II and III are parts

of DhKm-1 which is sorne metres away, as evident in figure 3.12. Dewdney stated in his

1962 publication that the images at Site # 92 A were "merely smears, except for one small

abstraction" (Dewdney and Kidd 1962: 52). On the paper that accomparued his field

sketches of the images he stated that these images were "very faint". This conclusion is

supported by his photograph below (figure 5.89).

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Figure 5.89: Face 1- Figure a & b, Site # 92 A taken by Dewdney in 1960.

Dewdney took the photograph above while recording these images using rice paper

and red paint. However, he wrote and recorded on his field drawing of the site that the

images were exfoliating away from the surface of the rock face marking the places beside the

images where other images were "flaking" or had exfoliated away. It is possible that because

he did not think that smears of ochre were paintings, possibly half of the site was not

recorded.

Molyneaux reported that the images existed in the areas of the rock face which were

exfoliated "thereby indicating that the paintings were applied after the exfoliation" (ibid.). He

asserted that the high water line at this site hindered the accumulation of mineraI deposits

and the growth of lichen and rock tripe but that contact with water may "have contributed to

the 'fading' of the paintings" (ibid.).

Ten years later, Lambert in 1985 observed that the images were fading and that the

rock face suffered from "extensive spalling" (ibid.: 66). Furthermore, "generalized lichen

growth" on the right hand side of the rock face "further obscures" the images (ibid.). He

concluded that the fading of the images was a consequence of two factors: direct sunlight

and repeated "washing by wave action" (ibid: 68).

Sixte en years later 1 examined this site and the photographs below were taken

(figures 5.90 and 5.91). The red images are faint and the surface of the rock suffers from

severe exfoliation. Lichen and rock tripe encroachment exist both above the images, and

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. ~.

between them on the right hand side of the images in the photograph immediately below,

and the Ieft hand of the second photograph below .

Figure 5.90: Left hand side of DhKm-4 in 2001.

Figure 5.91: Right hand side of DhKm-4 in 2001.

Exfoliation is the largest problem for these images since the lichen and rock tripe does not

directly affect them. The deposition of white mineraI deposits is difficult to establish since

exfoliation appears to be the more pressing issue for the images at this site. Whether or not

wave action contributes to the deterioration of these images is, as Lambert (n.d.), Molyneaux

(1974) and Dewdney in 1960 suspect, a question that is impossible to answer.

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DhKm-5:

Dewdney recorded DhKm-5 as Site # 105 on August 19t\ 1960. His field drawing

below (figure 5.92) indicates that the rock on which these images occurred was granite but he

made no comment regarding the white mineraI deposits, any exfoliation, or lichen and rock

tripe encroachment.

60"-

"I~~ .. b.oo,,·

, , ,

!! Aj~

,t;:\;::" ,;, i

"

.' in,ulh t­"lwv.:

Sire "'/05" • sOUTIl of' :tJev;/'s ]3er'! Whi1'et'(rh Ba,! LaKe of fllt?: /A'/oOq,

Figure 5.92: Dewdney's field drawing of Site # 105 undertaken on 19 August 1960.

Dewdney was fascinated by the large creatures, which he termed "bison," at this site

(Dewdney and Kidd 1962: 52, 1967: 54). He asserted that the bison appeared to be "more

alive" (ibid.) than a similar image that he had recorded at a pictograph site on the Bloodvein

River north of the Lake of the Woods. Dewdney was clearly impressed with these images

since he mentioned them again in his 1970 article in the magazine Artscanada, where he noted

that this site existed "within an easy two days' paddle" from the prairies (1970: 21). Very little

lichen or rock tripe has started to grow on the surface of the rock and accumulation of white

mineraI deposits has occurred. Whether exfoliation is a problem is difficult to establish

because the only photograph of this site that l could find in the ROM is not a close up shot

(figure 5.93).

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Figure 5.93: Close view of Site # 105 taken by Dewdney in 1960.

Molyneaux observed that a "white to yellowish deposit" covered approximately forty

percent of the site (1974: 7). He noted that "minor flaking" occurred in the lower part of the

site and that exfoliation was "slight". Molyneaux commented that the lichen growth at this

site was sporadic but that it existed on "the major fractures" in the surface of the rock (ibid.).

In 1978, Pelshea photographed the site in figure 5.94. Unfortunately, he did not

provide any comments concerning the physical state of these images as regards exfoliation,

the accumulation of white mineraI deposits, and lichen and rock tripe growth and

encroachment.

Figure 5.94: Closer view of DhKm-5 by Pelshea in 1978.

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Although it is clear from the photograph that lichen and rock tripe are not encroaching on

the images it is difficult to establish the level of exfoliation. These images do suffer from the

accumulation of white mineraI deposits which are heavier below the images than ab ove them

Molyneaux undertook a photographie study of five pictograph sites in Whitefish Bay

in 1979, including DhKm-5. In 1987 he published a photograph of this site, in figure 5.95, in

the journal Archaeoiogy. However, 1 am unsure when he took the photograph; hence it is

impossible to compare with Pelshea's photograph taken in 1978 or Dewdney's photograph

taken in 1960. The bright colours evident may be the effects of its appearing as a colour print . . ln a magazlne.

Figure 5.95: Molyneaux's photograph of DhKm-5.

ln 1985, Lambert examined DhKm-5. He observed in his unpublished notes that the

images at this site were not as faded as those at DhKm-4 but that they had suffered from

"much more interference from a red/orange underpainted background" (ibid: 87).

Presumably he means that the images that are visible were superimposed over older

pictographs that are overlain by white mineraI deposits, causing the red to appear as

red/orange. Only one image was faded at this site, according to Lambert (ibid. 88), and no

comment was made about any exfoliation or lichen and rock tripe encroachment.

1 recorded this site in 2001 (see figure 5:96 below). The site consists of two parts,

although the smal1 section depicted in figure 3.40 was included as part of this site at a later

date, after the main body of the site had been recorded by Dewdney in 1960, Reid in 1975,

Molyneaux in 1975 and 1979, Pelshea in 1978, and Lambert in 1985. 1 first saw this part of

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DhKm-5 when l visited the site in 1991 with Rusak, an archaeologist who at the time was

conducting fieldwork in the White Otter Lake/ Turtle River system (1992a). She pointed out

that DhKm-5 consisted of not just the rock face recorded but an additional part to the left of

the main rock surface. The precise year and date in which this part of the site was found and

established as part of DhKm-5 is unknown, and older photographs have not been found. So,

l cannot compare what this smaller part of the site was like with the photograph taken in

2001 in (figure 3.41). However, Rusak told me in 1991 that only one image existed here

which was identified a crescent. Analysis using VIPS and Adobe PhotoShop has

demonstrated that other images are not present in the immediate vicinity of this image. The

image is clearly not affected by lichen or rock tripe growth, although it exists within close

proximity to such growth. Rock spalling has not occurred on a large scale, such as that

evident at DhKm-4, but white mineraI deposits clearly exist on the surface of the rock. The

photograph of the principal part of DhKm-5 below shows that the odd colour of images

results from their being painted on white mineraI deposits and by further accumulation of

white deposits (figure 5.96). The reddish orange or pale red arguably indicates that some of

the images may have been superimposed on white deposits. Yet, their paleness could also be

a consequence of accumulation of deposits over them. This means that the edges of some of

the images have become difficult to determine. Lichen and rock tripe encroachment on the

images has commenced and will gradually obliterate these images. It is difficult to establish

whether exfoliation is a problem as a consequence of the accumulation of white mineraI

deposits on every surface.

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.~ ..

Figure 5.96: Photograph of DhKm-5 taken in 2001.

DiKp-1:

Dewdney recorded this site, his Site # 70, on 12th August, 1959 (figure 5.97). His

recording indicates that there were only five images here.

Site #70 - Sumer Channe/-Lake of the Woods Aug.!259 (P'tro9/yphs at 5rte#1!

shown elscw/?f're)

~ CL'" "LANO ~

~N~eÇ -rv~~Sht-~/ .......... e

At)~NEAI.I PfNINSLJLA (pdn)<jIYrj,~

SCALI': 2"~11n Z":;. 1-61{",

,.

CtUt,1 STQPlifR DLWDNIY

Figure 5.97: Dewdney's field drawing of Site # 70 in Sunset Channel undertaken on August 12, 1959.

His drawing of the Images supports Lawson's (1885: 657) drawing of the images

(figure 3.3), which was published in the American Naturalist. Lawson did not make any

comments about the accumulation of white minerai deposits, lichen or rock tripe

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encroachment, or exfoliation. It is equally impossible to tell whether the addition al images

visible in 2001 to the right and above the ones that Lawson recorded were present at the

time that Dewdney recorded them since a photograph is unavailable. If Lawson's drawing in

figure 3.3 is compared to the photograph taken in 2001 (figure 5.100), it is evident that more

red images exist now It is possible that Lawson recorded the images that he did since no

others were present.

Dewdney discovered the location of this site through Mallery's descriptions, who in

turn had relied on Lawson (Dewdney and Kidd 1962: 42, 1967: 44). Dewdney was the first

person to take a photograph of the site but, unfortunately, 1 have not been able to obtain a

copy of it at the ROM. Therefore it is impossible to make any comments as to the lichen and

rock tripe encroachment, deposition of white mineraI deposits, exfoliation, or vandalism.

Molyneaux and his colleagues (1975), a te am from the Canadian Conservation

Institute and the Department of Anthropology, Trent University, sought to document in

detail fifteen pictograph sites in the Canadian Shield in terms of physical conditions such as

moisture access, seepage deposit formation, seepage deposit flaking, exfoliation and

biological growth. In the course of this work a photograph of the site was taken (figure 3.44).

This team assessed each site in this study to establish its physical condition with regard to

these criteria. Topographical maps illustrating site locations and scale drawings of the

pictographs were also recorded for each site. It is evident from reading his report that

Molyneaux only considered the images on the face that both Dewdney and Lawson had

recorded. 1 have annotated the photograph taken in 1975 to indicate the images that

Molyneaux did and did not consider (figure 5.98).

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Figure 5.98: DiKp-1, Sunset Channel, 25thJuly 1975 annotated by A. Colson in 2001

It is possible to see that there are red images on the block of rock below the rock

overhang as weil as faint oval blobs on the wrute mineraI deposits. Molyneaux and rus

coileagues commented on the physical state of the images they recorded. They argued that

"minor spalling" (ibid.: 3), exfoliation, was only a problem for one of the images and had not

occurred elsewhere. Lichen growth was considered not to be a problem for the group of

images under consideration, although it is now clearly a problem for those images on which

he did not comment. The lichen was identified as "Xanthoria elegans" (ibid.) (underlining is

Molyneaux's). Wrute mineraI deposits were also found elsewhere on the site but not on the

images under consideration. Molyneaux and rus coileagues observed that "deposit flaking

was light and evenly distributed over face" and that it had occurred prior to the rock being

used for painting (ibid.). Defacement of the images was deemed not to have occurred here.

Today, lichen is encroacrung on the images. White mineraI deposits are problematic

for sorne of the images, since sorne of the images that were not noticed by Molyneaux and

his coileagues in 1975 are partially obscured. Although they were not recorded, it is possible

to see them. It is very difficult to establish whether exfoliation of the rock surface has

occurred at trus site from trus photograph.

In May 1975, Reid obtained a Borden number for trus site: DiKp-1. The photograph

which he took in 1975 (figure 5.99) demonstrates the presence not just of the group of

images already observed and discussed by Molyneaux in the same year, Dewdney in 1959 and

Lawson in 1885, but of the other images.

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Figure 5.99: Photograph of DiKp-1 taken by C. S. Reid in May 1975.

The key difference between this photograph and Molyneaux's is that it is easier to see the

images sin ce the sunlight was not shining directly on the rock's surface thus partially

obscuring them. Very little lichen growth has occurred on the main section of the site that

everyone was concerned with. The accumulation of white mineraI deposits is a problem for

the remaining images above and to the right of the images that are the centre of this

photograph. This site was photographed again when l conducted my doctoral fieldwork in

2001 (figure 5.100).

Figure 5.100: Photograph of DiKp-1 taken in June 2001.

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.I~-

If the photograph taken by Reid is compared with the photograph above taken in 2001,

visible lichen encroachment has occurred between 1975 and 2001 at several places. This

photograph has been annotated and presented again below to show where the lichen has

begun to grow in comparison with Reid's photograph. The hatched areas in figure 5.101

highlight the areas that were affected by lichen growth or encroachment.

Figure 5.101: Lichen growth and encroachment as marked by A. Cols on in 2001.

By 2001 the site clearly suffered lichen growth and encroachment but whether rock spalling,

rock tripe encroachment, and white mineraI deposits have increased since this site was first

discovered is difficult to establish because only two photographs can be examined. It is also

impossible to establish whether the number of images has increased at this site. However it is

evident that several images that were recorded in 2001 were present in the photographs taken

by Reid and Molyneaux in 1975 if the photograph below (figure 5.102) is examined.

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Figure 5.102: The areas containing missing images at DiKp-1 indicated by Colson.

This site is affected by lichen and rock tripe encroachment. Sorne exfoliation has occurred as

weIl as the accumulation of white mineraI deposits.

DgKm-1:

The only photograph available was taken in 2001 (figure 5.103). There is a large

quantity of rock tripe and lichen surrounding the area where the red images are present. It is

difficult to establish whether exfoliation has occurred. White mineraI deposits are already

affecting the images.

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Figure 5.103: DgKm-1 in Splitrock Bay taken in 2001.

DgKl-17:

Pastershank recorded this site in 1989, and subdivided it into three parts designated

Faces l, II and III. Two informants, Ron Kelly and Ron Seymour, who lived on the nearby

Sabaskong Bay reserve, told her of its existence (pastershank 1989: 63). She described Face 1

as having "a heavy population of lichen" and presumed that the area which was painted

"appeared to be unnatural, possibly cleared prior to use by the artist" (ibid.). Mineralization,

which was not described as regards its colour, was judged to be "moderate" throughout the

site and a precipitation of some sort existed "along the north-and-south extent of the Face"

(ibid.). Unfortunately, l have been un able to obtain ail of the photographs taken; l only

obtained a photograph of part of the rock face that she designated as Face 1 (figure 3.37).

Pastershank described several shapes as existing on the rock face she called Face l, including

"two faint, small, horizontally aligned horned-anthropomorphs with their arms extended

straight out" (ibid.). A smear was identified to exist to the left of these shapes and a right

hand print existed to their right. Face II had a small smear which was described as located

above a "horned hollow cervid in a running pose" and "five sets of three finger strokes"

existed below it (ibid.). This area of the rock surface was surrounded by lichen on ail sides,

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which also partially covered some of the images that suffered from "a small degree of

mineralization" (ibid.: 65). l suspect that the term mineralization can be defined as white

mineraI deposits. Pastershank described Face III as perpendicular to Face II and as having

several sets of three finger strokes so heavily encroached by lichen that some were difficult to

see.

Figure 5.104: Left hand part of DgK1-17. Figure 5.105: Right hand part of DgK1-17

If the photographs above (figures 5.104 and 5.105), taken in 2001, are examined, it is

impossible to identify or determine the precise location of the shapes that Pastershank called

"horned anthropomorphs" (ibid: 63), the small smear and the right hand print. This is

probably because they have been severely affected by exfoliation. It is possible that the

quantity of lichen has increased, but the photograph taken by Pastershank in 1989 does not

show much of the lichen present in figure 3.37. Since it is impossible to undertake a

comparison of the photograph of the right hand part of the site taken in 2001 with the

photographs of the whole site taken by Pastershank in 1989, very little can be concluded as

to lichen encroachment, exfoliation, rock spalling, and the deposition of any white mineraI

deposits. However, white mineraI deposits have been deposited on these images; although

they are similar to those described in 1989, they are paler. Exfoliation is a problem, and

lichen, not rock tripe, has begun to develop on the images at this site.

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DgK1-19:

Dewdney knew of this site's existence based on a sketch map that glVes the

latitudinal and longitudinal information and the black and white photograph below (figure

5.106); his notes confirm its identification. Unfortunately, he did not provide a date for when

he discovered its existence. He also did not examine the site or give it a number.

Figure 5.106: Cyclone Point (unknown photographer and unknown date).

It is very difficult to conclude a great deal from this image. This is because this figure is a

digitized version of a photograph that was photocopied. l examined the original photograph

but l was unable to draw any conclusions regarding the physical status of the images and the

effects of exfoliation, deposition of white mineraI deposits, and lichen and rock tripe

encroachment.

Pastershank recorded this site in 1989. She did not use Dewdney's information to

find this site, but rather, was informed of it by Ron Kelly and Ron Seymour of Sabaskong

Bay (pastershank 1989: 63).

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Figure 5.107: DgK1-19 by Pastershank taken in 1989.

Both lichen and rock tripe had begun to encroach on these faint shapes, which were also

suffering from exfoliation. The pale white colour evident in the photograph ab ove, figure

5.107, suggests that white mineraI deposits were probably affecting the visibility of the ochre

shapes there.

Figure 5.108: DgK1-19 photographed in 2001.

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.~.

When the photographs from 2001 and 1989 (figures 5.1 07 and 5.108) are compared,

lichen and rock tripe encroachment of the shapes has clearly occurred. The red shapes have

been affected by the increased accumulation of white mineraI deposits and exfoliation.

DiKq-10:

Dewdney recorded Site # 95 in 1960, and for many years it was known as the

pictograph site on Picture Rock Point or Dewdney's Site # 95. According to his field notes,

he established that the water was deep at this site. It also seems likely from his field notes

that he thought this site might be a good place to take paint samples because it had a thick

lime crust. He did not suggest a dating technique that could be used, stating only that "sorne

picts [pictures were] obscured as consequence of the thick lime coating" (Dewdney's field

notes for Site # 95 in the S. Dewdney Collection, New World Archives, Royal Ontario

Museum, Toronto). Indeed, the white mineraI deposit on the rock face is clearly visible from

afar in the photograph below (figure 5.109).

Figure 5.109: Annotation by Cols on of Site # 95 taken by Dewdney in 1960.

Dewdney recorded additionai information, but it is difficult to understand his notes.

A Borden number was obtained for this site once l completed my fieldwork in 2001.

Unfortunately, l do not have a copy of Dewdney's record of the images. However, he

observed that the images were painted on "a thick, rough encrustation of lime, and, with

exception of the human figure, are obscure" (Dewdney and K.idd 1962: 42, 1967: 44).

Unfortunately, a photograph of this site was not found among Dewdney's papers, and l was

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only able to find a slide of the site in its physical setting (figure 5.109). Therefore, it is

impossible to compare the photographs taken by Dewdney in 1960 with those taken in 2001.

It is evident from the photograph, below (figure 5.110) that the shape Dewdney identified

cannot be found. The accumulation of white mineraI deposits has caused problems for the

viewer evident in that the shapes that Dewdney recorded can no longer be identified. It is

only possible to determine that a large number of blobs, a short vertical line, a faint

unidentifiable shape, and two shapes called "three vertical and diagonallines attached to each

other at the lower end of each line" exist at this site.

Figure 5.110: Left hand side and right hand side ofDiKq-10 in 2001.

It is difficult to establish whether exfoliation has occurred, but it is clear that the

accumulation of white mineraI deposits is severe. It is also clear that lichen and rock

encroachment is not a problem for the images at this site.

DjKr-23:

Dewdney recorded this site as Site # 94 in Portage Bay, in the western portion of the

Lake of the Woods, on 18th July, 1960. Dewdney asserted that deep water existed at the base

of the site, but did not make any other comments about the site and its relationship to the

rest of the cliff face. Unfortunately, l could not find a photograph that illustrated the site's

physicallocation on the cliff face. In the photograph below (figure 5.111), taken by Dewdney

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ln 1960, it is clear that very little lichen or rock tripe encroachment has occurred on the

shapes at this site. White mineraI deposits are not present. It is difficult to determine whether

exfoliation has occurred at this site because of the distance of the photographer from the

Images.

Figure 5.111: "Setting of Site # 94 with P.D." Photograph taken by Dewdney in 1960.

Figure 5.112: Annotated setting of DjKr-23 in 2001 by Colson.

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The photograph ab ove (figure 5.112), was taken in 2001 when the water level was higher.

The rocks visible in Dewdney's 1960 photograph are beneath the surface of the water in

figure 5.111.

Figure 5.113: DjKr-23 in July 2001.

If the photograph of the site from 2001 (figure 5.113), is compared to Dewdney's

1960 photograph (figure 5.111), some interesting conclusions can be drawn. It is evident that

the lichen has increased in quantity in comparison to what was there in 1960 and that it has

begun to encroach on the shapes at this site. Rock tripe has also begun to grow on the right

hand edge of the cliff face. It is difficult to assess whether exfoliation has occurred sin ce

1960 because Dewdney did not describe the shapes in either of his publications with Kidd

(Dewdney and Kidd 1962 and 1967). Accumulation of white mineraI deposits has not

occurred to the extent that it is evident to the naked eye.

l obtained a Borden number for this site in 2001.

DhKm-18:

Dewdney recorded Site # 104 in Whitefish Bay, in the eastern portion of Lake of the

Woods, on 19,h August, 1960 (figure 5.114). Dewdney argued that little was "too notable

about this site" other than the shape that he identified as a thunderbird, which was larger

than any thunderbirds that he had recorded elsewhere (Dewdney and Kidd 1962: 51; 1967:

53).

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017

'offert/Nj sife/)

#;73 An/lle/,-!clI7d, WlJikfis/18atj

5i/;z#/O"f

f)cvlhB",! 5 MT!; end of [.i/(Jife!l:S1; .Bal!

wk<Z"or1't!eUVoaS-

<111 ôlferiFl'l sif,z "

Figure 5.114: Dewdney field drawing of Site # 104 undertaken on 19 August in 1960.

Figure 5.115: Setting of Site # 104 taken by Dewdney on left and annotated by A. Colson on the right.

Dewdney identified the thunderbird at trus site as existing in the green lichen in the

photograph above (figure 5.115). It is difficult to determine from this photograph precisely

where it is and its size in relation to the rest of the cliff face. It is also difficult to establish the

quantity of rock tripe, lichen, and exfoliation given the angle of the photographer to the rock

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surface. lt is equally impossible to estimate the level of accumulation of white mineraI

deposits. Dewdney called this site "an offering place" because he found offerings here.

Offerings were left below the shape and the "ceremonial sticks" as he called them are

currently held in the Ethnological collection of the Royal Ontario Museum. Chinaware and

enamelware were also found by Dewdney, according to the Borden form for this site. The

physicallocation of this site is easier to determine if one examines the photograph in figure

5.116, which illustrates someone in the process of recording the shape using rice paper and

red paint. The offerings that Dewdney found are evident at the base of the gentleman's feet.

Figure 5.116: Devil's Bay Site # 104 taken hy Dewdney.

Dewdney found the bird shape when he visited the site for the second time, according to

Dewdney and Kidd (1962 and 1967), since the glare when he first visited it reduced visibility.

Lambert, in July 1985 (n.d.: 98-102), found two more images. He argued this oversight

probably had occurred since lichen obscured "large portions of the two newly recognised

figures" (ibid.: 100). Lambert argued that the shapes he found in 1985 were "likely similar to

that seen 25 years before was exacerbated by glare, or sorne other kind of environmental

influence" (ibid.: 99). He argued that the faintness and fading of the images meant that the

archaeologist concerned should just photograph and not trace them. Lambert asserted that

the pitting and weathering of the rock's surface fortunately only occurred on the edges of the

painted surface. Rock spalling was not a problem, although something called "min or

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cracking" was occurring on the peripheral are as of the cliff face (ibid.). The largest problem

for Lambert was the growth of the dry brown-green lichen that encroached on the three

shapes. Yet its "lower margin," which is presumably where the lichen encountered the water,

was apparently "regulated by the high-water 'scour-line' "(ibid.).

This site was examined again in 2001 (figures 5.117, 5.118, and 5.119). The three

shapes discussed by Lambert were still barely visible, but two other shapes were also

identified in the immediate vicinity of the first three.

Figure 5.117: Bird identified by Dewdney and Lambert beside the two vertical stick figures identified in 2001.

Figure 5.118: Smear at DhKm-18 in 2001.

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Figure 5.119: Oblong blob at DhKm-18 in 2001.

Lichen, but not rock tripe, encroachment was a severe problem in 2001 (figures

5.116, 5.118, and 5.119). The accumulation of white mineraI deposits is probably occurring,

but it is not evident at the moment. Exfoliation is more severe for these images than

anything else.

DiKm-51:

Dewdney recorded this site on Horseshoe Island in Whitefish Bay, Site # 270, in

figure 5.120 either in 1966 or afterwards, since Dewdney and Kidd (1967) did not list those

sites that are numbered above # 264 (Dewdney and Kidd: 185). His field notes stated that

the shapes here were very faint and that Francis Tom, who appears to have come from

Whitefish Bay Indian Reserve, called one of the shapes at this site "a medicine snake" (Field

Notes, New World Archives, Royal Ontario Museum). Dewdney described the shapes as

being typically "very rough" (ibid.). He observed that the rock face itself had a "southwest

orientation" (ibid.). This is an unusual observation since Dewdney did not typically note the

directional aspect of the rock face upon which these shapes exist in this region. Dewdney

also observed that lichen grew upon the surface of the shapes at this site. However, he did

not undertake a field drawing of the images at this site in the manner he had done for

previous sites.

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Figure 5.120: Close up of Site # 270 Horseshoe Island in Whitefish Bay by Dewdney.

Lichen and rock tripe encroachment clearly affected the red shapes in the photograph above,

in figure 5.120, taken by Dewdney. Rock tripe was encroaching on the shapes on the right

hand side of the site. The paleness of the shapes is indicative that exfoliation is a problem. It

is possible that Dewdney excluded the shapes from the right hand side of the site because he

did not consider smears as parts of sites until sometime in the late 1960s. The photograph

below, in figure 5.121, was taken in 2001 by E. Campbell, the volunteer on my fieldwork.

Figure 5.121: DiKm-51 taken in 2001.

This site including the smear is larger than Dewdney seems to indicate, as seen ln the

photograph taken in 2001 which is annotated in figure 5.122.

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Figure 5.122: Annotated by Colson in 2001 of DiKm-51 taken in 2001.

When the annotated photograph of Dewdney's below (figure 5.123) is compared to the

photograph above taken in 2001 (figure 5.121) the site is slightly larger on the right hand

side. Lichen and rock tripe encroachment of the images has occurred. The blueness of the

slide has occurred because the sky is overcast.

Figure 5: 123: Annotated by Cols on in 2001 of DiKm-51 taken by Dewdney.

It is evident from the Borden records held by the Ontario Ministry of Tourism,

Culture, and Recreation that this site was forgotten since no one obtained a Borden number

for it under the Ontario Heritage Act. It was "found" again when 1 conducted my fieldwork

in 2001. If the photograph above (figure 5.121), is compared to Dewdney's possible 1966

photograph (figure 5.120), visible lichen and rock tripe encroachment has occurred on

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;-- ..

images. The shapes have faded but they are still evident to the naked eye. The accumulation

of white mineraI deposits and exfoliation is also evident.

DkKn-7:

Lambert examined this site in July 1985 in his unpublished study. This site, like

DkKn-6 and DjKn-1, is in Blindfold Lake which was connected, prior to the construction of

the dam, to the Lake of the Woods via a series of rapids. He (n.d.) obtained the Borden

number under the Ontario Heritage Act and stated on the Borden form that the site was not

recorded or noted by Dewdney and Kidd 1967. Neither was it known by local residents in

Blindfold Lake, which is connected to the Lake of the Woods. A photograph does not exist

but he (n.d.: 63) argued that weathering in conjunction with lichen encroachment had either

"completely erased or obscured the paint." He asserted that the surface of the rock face was

severely eroded and suffered from "numerous small pits and fissures" which predisposed the

surface of the rock to lichen growth.

Figure 5.124: DkKn-7 in 2001.

Lichen and rock tripe was evidently a huge problem for this site in 2001, as seen in

figure 5.124. The surface of the rock is indented with small fissures and pits. The red shape

discussed by Lambert in 1985 is still present but it seems to have suffered from exfoliation. It

is not apparently suffering from any obvious accumulation of white mineraI deposits.

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DkKn-6:

Dewdney (1958, 1963, 1968, 1970a, 1970b, 1970c, 1971, 1975a, 1975b, 1977, 1979a,

1979b) and Reid (1974, 1976, 1977, 1979, 1988) did not examine this pictograph site.

Lambert examined this site the same year, July 1985, as he did DkKn-7, also in Blindfold

Lake. He argued that the detail of the shapes he saw were hard to distinguish as a

consequence of weathering on the surface of the rock. Furthermore, the rock was covered

with white mineraI deposit which was in turn "overlain by extensive but patchy growths of

lichen" (ibid.: 58). Lambert argued that, although lichen encroachment had started to occur,

it did not affect three of the five shapes that Lambert had identified. l examined this site as

part of my fieldwork in 2001. The five shapes identified by Lambert in 1985 were only

identifiable as four oblong blobs in figure 5.125 below. One of the shapes identified by

Lambert had disappeared.

Figure 5.125: DkKn-6 in 2001.

The disappearance of the fifth shape was probably caused by a combination of

factors. The photograph above illustra tes that lichen growth and encroachment is a huge

problem. Rock tripe has also begun to grow amongst the lichen. lt is also possible that

exfoliation has aided the destruction of the four shapes that are currencly barely visible.

DhKn-2:

This image, cal1ed Site # 107, existed on the south end of the Channel between

Obabikon Lake and Obabikon Narrows and was called the Obabikon Narrows

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Lichenoglyph (figure 5.126). Dewdney located it at the same time that he found DhKn-1

thanks to information S. C. O. Linklater had supplied to him. Bob Archie from Morson,

Ontario, informed Linklater of its existence and noted its physical location as well as the

following brief description as "a figure of a sort of head. The moss grows all around the

figure. The pictograph is on a boulder about 5 or 6 feet above the water line." (New World

Archives, Royal Ontario Museum)

, .

. ' 7'''''-WdU.­

"7usfIJ ,/j60

SITe #107 -adc,ign scropad outof/tch.rn on boa/der O,fockrt"d with offènil'l>

in Obabli:a NarroWf .North ofOba",l<a /Ja''{,

soorn of AUIIlf?aU P€ni'l,l/Ia,

Lak.< of' tne U'RJOq<.

Figure 5.126: Dewdney's field drawing of Site # 107 in Obabika Narrows undertaken on August 19 1960.

Molyneaux and his team from the Trent University examined the lichenoglyph and

concluded that "deterioration by means of lichen encroachment was inevitable" (1974: 10).

Indeed, photographie analysis of this shape indicated that lichen growth had "obliterated"

many of its specific details (ibid.).

During my 2001 doctoral field work we attempted to find the image drawn by

Dewdney. We could not find it despite spending several hours searching. It can only be

presumed that the lichen had grown so much that the image no longer exists.

DjKn-1:

Dewdney recorded this site, called "the Blindfold Lake Site", as Site # 29 in 1958.

Figure 3.18 indicates the precise location of the offerings that Dewdney found in 1959 as

well as few of the images. However, other photographs of this large site were not found in

the Dewdney collection in the Royal Ontario Museum. The photograph in figure 3.19 is of

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part of this site, and was originally published in Dewdney and Kidd's publication (Dewdney

and !<idd 1962: 27 and 1967: 29). It was not found in the New World Archives held by the

Royal Ontario Museum. Despite only having one photograph in figure 3.19 it is evident that

the site suffered from exfoliation and that lichen grew on the rock's surface before 1962. It is

impossible to determine whether the whitish colour visible in the photograph was caused by

the accumulation of white mineraI deposits.

In 1974, Molyneaux and the Trent University team examined this site and argued that

the rock shelf, evident in Dewdney's photograph in figure 3.18, was used for leaving

offerings. This data, Molyneaux argued, indicated an "active, contemporary belief in the

sacred qualities of the site" (1974: 14). A deposit that varied in colour from "pale reddish

brown to white" was described as existing over many of the shapes. Molyneaux observed

that "deposit flaking" occurred and apparently caused the "pigment loss" (ibid.); perhaps

Molyneaux is stating that the shapes were exfoliating off the surface of the rock face.

However, he had observed that, although several small areas of exfoliation existed, there was

evidence that this had occurred before the shapes were created. Stress fractures also existed

in the rock itself but Molyneaux argued that they did not cause erosion of the rock's surface.

Lichen colonies were found "in spring seepage areas" (ibid. 15) and had started to encroach

on sorne shapes, but Molyneaux concluded that lichen encroachment was not an extensive

problem for this site. Vandalism was evidently a problem for Molyneaux since he found

sorne names and initiaIs painted on the rock face "100 feet to the right of the site" (ibid.).

Molyneaux published a photograph (figure 5.127) of part of this site but it 1S unclear in which

year he took it. He implied in his article that he took it after the dry winter of 1973.

Figure 5.127: Part of DjKn-1 taken by Molyneaux.

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Reid examined this site in 1975 and assessed it as having "high representability and

high interpretability" (ibid.: 14). Unfortunately he did not provide a photograph of this site;

hence it is difficult to establish the physical status of the shapes, the amount of lichen and

rock tripe encroachment, the deposition of white mineraI deposits, as weil as the possible

rate of exfoliation. In 1978, Pelshea took photographs of this site (figures 5.128 and 5.129).

The red is very bright in both pictures. Lichen, rock tripe and white mineraI deposits were

present on the images when Pelshea photographed this site.

Figure 5.128: Pelshea's photograph of the left hand side of DjKn-l taken in 1978.

If the ab ove photograph is compared to Dewdney's photographs taken in 1959

(figure 3.18 and 3.19), it is impossible to undertake a detailed comparison since Dewdney's

photograph only covers a smail portion of the images. The water level was higher in 1978

than in 1959, since the lowest image on the left hand side in Pelshea's photograph (figure

5.128), is doser to the water level than it was in Dewdney's 1958 photograph (figure 3.18).

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Figure 5.129: Pe1shea's photograph of the right hand side of DjKn-1 taken in 1978.

Unfortunately, it is difficult to de termine precisely how much higher the water level

was when Pelshea recorded the site in comparison to when Dewdney recorded it in 1969.

Exfoliation is evidently still an important issue, as is the deposition of white mineraI deposits.

The quantity of lichen and rock tripe has evidently increased since 1959 when these images

were first photographed.

Lambert argued in 1985 that, prior to conducting field work at this site, he had

observed that Dewdney's drawings and photographs were not identical and showed

differences from the site as Lambert recorded it in 1985. Whether this i5 a valid statement

remains impossible to establish, since Lambert's photographs of the entire site were

impossible to obtain. He (n.d.) concluded that microscopie erosion was inevitable "because it

was a natural process" (ibid: 26) but that no evidence existed of rock spalling (ibid: 27). He

asserted that two types of white mineraI deposit existed. One type on1y existed in the central

portion of the cliff face of Face 1, and it was so thick that it had obscured portions of three

shapes (ibid.). The second type was thinly overlaid over all of the shapes. Broad areas of

lichen existed on the top half of what Lambert termed Face 1 and "obscured sorne painted

areas" (ibid) and probably sorne shapes.

This site was photographed in 2001 and has three parts (figures 5.130, 5.131, and

5.132).

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Figure 5.130: Part of DjKn-l in June 2001.

Lichen and rock tripe encroachment is evident at the top of this part of DjKn-1 in

figure 5.128. The images are severely affected and in sorne instances impossible to identify

clearly. The site is also evidently affected by the accumulation of white mineraI deposits in

the centre and this has caused sorne of the images to become faint. Exfoliation is also a

problem at this site. The high water mark is clearly evident at this site.

Figure 5.131: Part of DjKn-l in June 2001.

The shapes in figure 5.131 are not as affected by lichen or rock tripe encroachment

as those in figure 5.129. White mineral deposits clearly superimpose sorne of the shapes.

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Exfoliation is evident underneath the shapes, as Lambert had noticed earlier. The two large

cracks are evident as Lambert (n.d.) observed, but it appears that further exfoliation is not

evident.

Lichen and rock tripe encroachment is evident on the red hand print in figure 5.132

below. This image was found and identified as part of the site although it does not exist

beside the other parts of this site but higher up the same cliff. It is likely that exfoliation is

present but it is difficult to determine the quantity at this part of the site.

Figure 5.132: Part of DjKn-1 in June 2001.

DiKn-1:

Dewdney recorded this site as Site # 91A and B on 15 July 1960 (figure 3.16). It is

found on Hay ter Penin sula, on the eastern portion of the Aulneau Peninsula. Unfortunately,

a close-up photograph of the site and rus drawing of the entire site could not be found and l

only found the photograph below (figure 5.133) in Dewdney's papers held by the ROM.

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Figure 5.133: Setting from a Distance of Site # 91A and B taken by Dewdney.

Dewdney divided trus site into two parts, which he called A and B. Part A was the Iower part of the site wrule Part B was the upper part of the site. He was particuiarly interested in a shape called "a checker-board," which he argued couid be a "weaving texture" (Dewdney and Kidd 1962: 50; 1967: 52). Figure 5.134 shows this image.

Figure 5.134: "Face lB figure c + d" by Dewdney in 1960.

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Figure 5.135: "Face lA fig a + b" by Dewdney in 1960.

It is clear from the photograph ab ove (figure 5.133) that exfoliation is quite severe

and that evidence exists of rock tripe and lichen encroachment. White mineraI deposits are

not as clearly evident here as at sorne sites.

Figure 5.136: DiKn-l in June 2001.

This site was photographed and examined in 2001 (figure 5.136). It is evident that it

suffers from severe lichen and rock tripe encroachment and that many of the images are

severely exfoliated. Exfoliation rather than the accumulation of white mineraI deposits is

more of a problem at this site. It also means that the images are very difficult to identify.

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Indeed it is difficult to see some of the shapes that Dewdney photographed in 1960 (figures

5.135 and 5.136, since they have been so severely exfoliated (figures 5.137 and 5.138).

Figure 5.137: Blob beside exfoliated area at DiKn-1 in 2001.

The 'checker-board' that Dewdney identified in 1960 beside the blob in the photograph

above has disappeared due to severe exfoliation of the rock's surface.

Figure 5.138: Dewdney's "Face lA fig a + b" at DiKn-1 in 2001.

It is evident if the photograph above (figure 5.138) is compared with the photograph in

figure 5.135 that the images viewed by Dewdney in 1960 are still visible but they are affected

by lichen encroachment and exfoliation of the rock's surface. It is clear from the photograph

below (figure 5.139), that lichen and rock tripe encroachment has severely affected the

shapes Dewdney identified in 1960.

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Figure 5.139: Red images are visible although partially hidden by the lichen and rock tripe in the upper half of DiKn-1 in 2001.

If the photograph below (figure 5.140) which is a close-up of this part of the site is

examined, it is clear that the red shapes in the upper part of DiKn-l, which Dewdney called

Part B, are impossible to identify.

Figure 5.140: Shapes ab ove the main collection of shapes at DiKn-1.

Lichen and rock tripe are clearly so severe that it is impossible to identify any images.

It is only possible to state that red images are present.

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DjKn-2:

Dewdney did not examine this site but, Lambert argued (n. d.: 52) that he had

established its existence from Dewdney and Kidd's (1975) publication of their original (1963)

book. Lambert noted that Dewdney had mentioned this site while he described the existence

of Site # 29 or DjKn-1. Reid (1976: 25) observed that the site was in good condition but

some danger existed that it might be vandalised since it was so weil known to the general

public.

Lambert reported (n.d.: 52) that rumours existed as late as the 1970s that this site was

destroyed since someone had fired at it using a shot gun. Lambert examined the site to

ascertain whether it had been used for target practice. He ascertained that weathering and

rock spalling had affected the shapes at this site rather than gun fire. Lambert also concluded

that white mineraI precipitate and lichen was not present at this site. In 2001, l heard the

same rumour about gun fire having affected this site. However, l was not able to find this

site when l searched for it.

DhKm-20:

A Borden number has been obtained since this site was discovered in 2001 during

my fieldwork. Unlike most of the other sites in the Lake of the Woods this site is possible to

date since it was dated by the author. The shapes at this site (figure 5.141) are quite unusual

and were created using modern paints in red, blue, and white.

Figure 5.141: DhKm-20 in June 2001.

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These shapes were painted by R. Bird and the images are dated 1982. The date is

painted in red paint below the lower front part of the fish shape. Hence these images were

nineteen years old. The red shape, above the fish shape, is affected by lichen encroachment

on its Ieft hand side while the white and blue fish shape is affected by white mineraI deposits.

These images are not affected by rock tripe encroachment. It is difficult ta establish whether

the images are affected by exfoliation since it is possible that it has started to occur on the

edges of the images but evidence of it occurring is hard to determine with the naked eye.

DhKm-19:

This site was also discovered during 2001 and a Borden number obtained for it. It

exists on the south-east facing shore of Turtle Lake a few metres from red channel marker

S44. It, too, was created with modern green and black paints but, unlike the shapes at

DhKm-20, these shapes are not dated or signed (figure 5.142). Neither the style nor the form

suggests the same author created the images.

Figure 5.142: DhKm-19 in 2001.

This image is not affected by the accumulation of white mineraI deposits or exfoliation. It is

also not affected by lichen or rock tripe encroachment.

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DgKm-Z:

This new site was found near to DgKm-1 during 2001. A Borden number was

obtained for it. It (figure 5.143) lies southwest of Sand Bay in a small, unnamed bay.

Figure 5.143: DgKm-2 in July Z001.

Six shapes exist here. They suffer from exfoliation, and probably from spalling,

which may explain why these images are smears. White minerai deposits cause problems for

these images but fortunately the lichen and rock tripe encroachment exists above the images.

DiKm-49:

This site, found in 2001, is inside a granite cave immediately behind DiKm-3. The

site is on an island southwest of Return Point, north-northeast of Three Sisters islands, in

Whitefish Bay. Two lines are present on the ceiling of this cave, both are visible in figure

5.144 below.

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Figure 5.144: DiKm-49 in June 2001.

These two lines are near the entrance of the cave, hence the sunlight visible on the

right hand side of the opening. The shapes on the ceiling are affected by lichen but not by

rock tripe encroachment. Accumulation of white mineraI deposits and exfoliation are not a

problem.

DiKm-50:

This site, in a cave, lies a few metres south of DiKm-51 (initiaIly caIled Site # 270 by

Dewdney) in Whitefish Bay. It is located on the southwest facing shore of the lower arm of

the second, large, horseshoe-shaped island just south of the Three Sisters Islands. This cave

site was discovered in 2001 and a Borden number was obtained for it. The photograph

below (figure 5.145), indicates that the shape here is a large smear which exists on the ceiling

of the cave. Unfortunately, exfoliation is a problem causing the image to faIl off the ceiling.

This could be accentuated by water coming into the cave through an opening near the

water's edge.

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Figure 5.145: DiKm-50 in June 2001.

Neither the accumulation of white mineraI deposits, nor rock tripe and lichen encroachment

threaten the images in this cave.

Conclusion:

Direct dating techniques cannot be used as stated in the beginning of this section,

rendering it difficult to date ail the images at these sites. However, the deposition of white

mineraIs, lichen and rock tripe encroachment, and exfoliation of the rock surface take place

over time, destroying or causing the images to fade (see Chapter V, section 1). The offerings,

especiaily the artefacts left at sites, can be dated but they only indicate that the site was

visited by people. It is possible the rock images were created there both before and after

artefacts were left there. It is also possible to date by association sorne of the sites since

independent evidence is available. Clearly, this question of the age of the images is important

and therefore three questions were asked at the ons et of this section:

(a) Is there independent evidence of when these paintings were created?

(b) Is it possible to calibrate the rate at which white mineraI deposits accumulate,

rock tripe and lichen grow and spalling occurs?

(c) Have the images present at pictograph sites changed stylisticaily over time?

The discussion of the images and the drawings of these sites and their images

illustrates that it is relatively easy to evaluate the age of sorne of these sites and to answer

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question (a). lndeed, DhKm-20 was identified as a pictograph site in 2001 but it was created

by an individual who left his signature, "R. Bird," and he or she provided a date of 1982

below the right hand corner of the front of the fish (figure 5.146).

Figure 5.146: DhKm-20 created by R. Bird and signed in 1982.

The four modern red spray paint images present at DgKI-2 were painted at DgKl-2 after

Pastershank recorded the ochre images in 1989 and before 2001 when land my crew

recorded the site. The three solid images, superimposed over older ochre images that

Pastershank had recorded in 1989, are visible in Figures 5: 147 and 5.148.

Figure 5.147: Two of the modern solid spray painted images at DgK1-2.

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Figure 5.148: The third modern image which is solid at DgK1-2.

The fourth modern image created from spray paint was a hollow shape existing to the Ieft of

the older ochre image in figure 5.149 below.

Figure 5.149: The modem hollow spray painted image at DgK1-2.

A vast quantity of offerings, wruch kept on growing in quantity throughout the

summer of 2001, were found at DgKl-2. l established that some of the new images here were

connected to a court case regarding charges of incest in one of the reserves in the Lake of

the Woods. However, l have been asked by W. A. Ross, who was the regional archaeologist

in 2001, not to provide any more details regarding the images and why they were created

(Ross. pers. Comm. July and August 2001). Unfortunately, none of the offerings Ieft at trus

site had anytrung that could be securely dated.

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The image present at DhKm-19, discovered in 2001 (figure 5.150), was painted using

modern spray paints but unfortunately it cannot be dated using independent evidence. Prior

to its being recorded in 2001 no-one had either recorded it or reported its existence to

Ontario MÎnistry of Culture and Communications. However, more can be concluded about

this image with respect to its style in the answer regarding question (c).

Figure 5.150: Modern spray paint image at DhKm-20.

Independent evidence must include objects that can be dated to specific time

periods, such as offerings found either below or above the surface of the water at pictograph

sites. The presence of the offerings underwater enables one to posit that these sites, and not

just the images, have had considerable importance for a long period of time, possibly, in the

case of DhKm-1 back to at least 800 AD. This statement can be made because objects, called

o fferings , were found below the surface of the water immediately beside the cliff on which

the paintings exist (See Appendix 5 of this chapter). Offerings were also found above water

level in 2001 but it is the offerings under the surface of the water that provide the strongest

indicators of the length of time this place has been considered as important to one or more

groups of people. A small ceramic pot (see figures 5.37 to 5.44) was found at the base of

DhKm-1 at 15.85 metres below the surface of the water. It was dated on the basis of its

physical similarity to those found amongst the grave goods during Kenyon's excavation of

the five Armstrong Mounds (1986: 12-16), which he ascribed to the Late Laurel period and

argued were constructed about 1,000 years ago. Ross also dated this pot, based upon a

careful examination of the photographs above, from the period between 1400 and 800 A.D.

(Ross pers. comm. August 2001). A small hand-blown glass bottle dated to the nineteenth

century was found about 1.52 to 1.83 metres away from the ceramic pot, also below the

surface of the water (see figures 5.32 to 5.37). Meyer disagrees with this interpretation

because he identified as belonging to the Duck Bay complex of the Rainy River composite

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dated by Leruus and Olinyk (1990: 84) as being from the period between 1100 A. D. and

1350 A. D. (Meyers pers. comm. September 2006). The divers also found a large pile of

clotrung leaning against the cliff face at the same depth as the pot and glass bottle. A wide

range of objects was found, including moccasins, large quantities of fabric and leather clothes

of different styles and different periods. They also found a wrute cruna plate with a brown

design, which had the maker's mark of Alfred Meaken Royal Ironstone China, England,

wruch had Queen Victoria's crown, lion, and unicorn on the base (see figures 5.30 and 5.31).

Evidently, DhKm-l has a vast range of evidence that provides a strong indication of the

considerable length of time it has been used. Dewdney's observation of the offerings in 1960

and Fox and Molyneaux's descriptions of the offerings in 1974 also confirm that trus site has

been continually used for a long period of time (see Appendix 5).

A chipped bowl was found under the surface of the water near the pictograph site

DiKm-50, on an island locally called Horseshoe Island, located north of trus site but also in

Wrutefish Bay. It was found at an underwater fireplace that was 2.44 cm (8 feet) away from

DiKm-50 (see Appendix 5). DiKm-50, the cave site on Horseshoe Island is also a few metres

south of DiKm-51 wruch is a pictograph site on a cliff face first recorded by Dewdney in

1970. It is possible that trus fireplace could have been used prior to the raising of the water

level since the crupped bowl was found below the freeze level. However, a broken plate was

also found with the same design and the same maker's mark at the base of DgKl-17, in

Sabaskong Bay. Given that trus plate was found at the base of DgKl-17 and another at

DhKm-1 (see figures 5.30 and 5.31), it is possible to argue that the physical places where the

paintings now exist have been considered important since the nineteenth century. Indeed,

the presence of the china plate at DgKl-17 enables the archaeologist to provide a date for the

possible use of trus site as a place of significance in the landscape. Dewdney cleady knew of

this site but did not record it, although he had an undated black and wrute photograph of it

(figure 5.106) as well as a sketch map as to how to find it in rus notes. It was first recorded by

Pastershank in 1989 but she found it because she was informed of its existence by Ron Kelly

and Ron Seymour, from the nearby reserve.

Coins are not as useful indicators in comparison to plates, bowls, and pots as to the

length of time that a physical locale used for a long period although many were found at

DiKn-1, DjKr-23, DiKm-4, DhKm-5, and DhKm-1. Indeed, a quarter dating from the reign

of George V as well as an American Penny was found at DhKm-1. Otherwise all the coins

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were Canadian. It is difficult to rely on coins as datable objects although they have dates on

them because these coins could have been in circulation for a considerable length of time

before they were left as offerings.

Another method of determining when a physicallocale was first used as a pictograph

site is to examine the records made by previous archaeologists. All of them have recorded

the presence of objects, which are offerings. These were found by Pastershank in 1960 by

DgKl-1, DgKI-2 but not at DgKI-17 and DgI<l-19 (Appendices 1 and 4). However, by 2001

offerings were found at DgKl-1, DgI<l-2, DgI<l-17 but not DgI<l-19. It could be argued that

DgKl-1 and DgI<l-2 were still being used but it is unclear when they started to be used. It is

clear from the offerings at DgKl-17 left below the water level indicate that it has been used

for some time since the offerings found contained a broken plate that dated from the

nineteenth century. Dewdney found and recorded offerings at DhKm-1, DhKm-5, DhKn-1,

DiKn-1, and DjIv-23 in 1960, and offerings were found at these sites in 2001. Dewdney also

recorded offerings at DhKm-18, DiKq-10, DjKn-1, DiKm-3, DiKm-3, and DjKn-1, but

offerings were not present in 2001. He did not record the presence of offerings at DhIZrn-3

and DhKo-1 when he recorded both sites but offerings were found there in 2001. Although

a considerable body of information was collected by Dewdney and subsequent archaeologists

regarding offerings, they did not provide any information that enables these items to be

identified within a specifie time period. Very litcle evidence exists as to when these red

images were first created. Indeed, Dewdney, who first recorded many of the sites, relied on

reports of these sites from informants. But none of these informants gave any indication of

the length of time these sites had existed prior ta report. Lawson, a geologist, was the first

pers on to record and describe a pictograph site in the Lake of the Woods, DiKp-1, in 1885

(see figure 3.3). Dewdney, although he was not the first person to photograph DhKo-1, did

establish that this site was known about as early as 1910. He found this site using a sketch

map (see figure 5.67) and a sketch of the images provided in 1936 by a guide, H. T.

Thompson, who maintained that the site was first found in 1910 but was known by all the

boat captains who worked in the Lake of the Woods prior to this date.

If it were possible to take a sample of pigment from a site it might be possible to date

the superimposition of paintings over painting and white mineraI deposits. However, none of

the sites can be examined using this type of analysis. But it does lead us to consider the

answer ta question (b). It was very difficult to answer this question. Critical comparison of

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field drawings, photographs and the associated reports and slides indicate that care should be

taken regarding any assertions concerning the accumulation of white mineraI deposits as weil

as growth of the lichen and rock tripe over images if they are considered crucial in calculating

the possible age of a site. Information from previous studies is useful, since it assists in

establishing the rate at which lichen and rock tripe encroach, exfoliation occurs and white

mineraI deposits accumulate at rock image sites in the Lake of the Woods. But it must be

remembered that measuring lichen and rock tripe encroachment is particularly problematic

since both can be removed relatively easily from sites as the photographs of the images of

DhKo-1 demonstrate.

Several researchers studied the micro-stratigraphy of the surface of the rock face in

which the pictographs exist. Although these studies were discussed in Chapter III it is

important to highlight the key points. Taylor, Myers and Wainwright (1974) examined seven

samples of paint from the Agawa pictograph site in Ontario, and from a site on Lac

Wapizigonke, Québec to determine its formation and composition. They intended to

establish the causes of the natural deterioration of pictograph sites in the Canadian Shield,

prior to devising any conservation treatments. However, they (ibid.: 40) concluded that the

pigment was "firmly attached to and intimately mixed with the [white] mineraI deposit in a

sandwich structure" instead of adhering to the surface of the rock. The white deposit found

on these cliffs coats the images and provides a "protective coating from the leaching action

of the rain and erosion by wind" (ibid.) as weil as preventing the pigment from dissolving

away. Taylor and his coileagues argued that the graduaI accumulation of this white mineraI

deposit on pictographs led to "the 'faded' appearance" of many of the images. Essentiaily

paintings were becoming obscured over time and the paintings eventuaily "disappear[ed]".

They (ibid.: 41) proposed that it might be possible to utilise the thickness of the

white mineraI deposit upon the surface of the pigment to estimate a date. However, they

abandoned this ide a because too many variables affected the rate at which this deposit

accumulated. It was unknown whether the rate of accumulation of white mineraI deposits

was continuous or had changed over time and whether it was influenced by other factors

affecting the surface of a cliff face, such as crack formation. Other factors that should be

discovered are the exfoliation of the rock's surface, lichen and rock tripe growth and

encroachment.

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Myers and Wainwright's (1977) study of samples from over 30 sites m the

Similkameen Valley and the Canadian Shield, confirmed Taylor and his colleagues' (1974)

conclusion. lndeed, Myers and Wainwright (1977: 31) asserted that the pigment was

"embedded in the deposit before and after the paintings were made". Wainwright and

Taylor's (1977) study using scanning electron microscopy determined the structure of the

pigment of two paint samples. One was taken from a painting on Lac Wapizagonke, Quebec,

and the other was removed from a painting at the Bon Echo site on Mazinaw Lake in

Ontario. Their results were important, although only two samples were examined, since they

demonstrated severallayers of pigment may exist at pictograph sites which appeared to have

been painted oruy once.

It is possible to condude that dating the images usmg the stratigraphy of the

pigments on the surface of the rocks is not very useful to my discussion but it darifies the

precise relationship of the pigment to the white mineraI deposit on the surface of the rock.

Another avenue of research for dating these images would be to consider the rate at

which lichen and rock tripe encroachment occurs, and whether either plant can be dated. It

is a commonly established fact among those who have examined pictograph sites in Québec

and Ontario that lichen and rock tripe occurs on pictograph sites (E.g. Arsenault 1998: 26-

27, Arsenault et. al. 1995: 46-47; Dewdney and Kidd 1962: 5-6 and 1967: 5-6; Molyneaux

1974 and 1974). Molyneaux (1974, 1975) reports that lichen and rock tripe affected the

pictograph sites of the Lake of the Woods but he did not draw any conclusions as to whether

different quantities of lichen and rock tripe exist on rock faces that face particular

orientations.

Neither did Dewdney specifically state whether the direction of a site may have

influenced the growth of lichen. However, he wrote that "fuzzy green lichen" grew on sites

"on which the sun never shines" (Dewdney and Kidd 1962, 1967: 6). However, Vaillancourt

(2003: 11) used this reference to support the view that north facing rock faces with images

are "habitually covered in lichen." She also based her conclusion on the following references:

Rajnovich (1994: 11), Arsenault (1998: 26-27) and Arsenault and his colleagues (1995: 46-47),

to substantiate her daim. However, none of these archaeologists made such a daim.

Arsenault and his colleagues (1995: 46-47) commented at sorne length on the orientation of

rock faces that had pictographs but they did not state that north facing faces had lichen.

Arsenault, later, (1998: 26-27) stated that sites predominately faced south, southeast and

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south west, although sorne faced north and west. Once again he did not specifically state that

lichen was found on north-facing rock faces with pictographs.

Dewdney (Dewdney and Kidd 1962: 6 and 1967: 6) claimed that it was north facing

cliff faces that did not experience sun that had "green fuzzy lichen" (ibid.) but he did not

clearly establish that north facing sites had lichen. Furthermore, the text that Vaillancourt

(2003: 11) quoted from Rajnovich did not support this opinion. It is impossible to draw the

conclusion that sites that face north have the largest quantity of lichen and rock tripe since

only one site, DiKo-l, faced north and it is clear from the photographs examined that the

lichen and rock tripe has been removed repeatedly.

Establishing the orientation of five pictograph sites in the field was difficult sin ce the

compass would not function at DgKm-2, DhKm-3, DhKm-l, DhKm-S, and DhKm-18 due

to the iron content of the rock upon which the paintings exist. However, it is possible to

establish their orientation using a compass and a map. Both cave sites must be excluded

from this examination since the paintings are inside the cave and the physical structure of a

cave site is different to that of the pictograph sites on cliff faces. Furthermore, each cave

examined can be entered and exited from two directions. Both sites, when compared are also

radically different. If appendix 5 is examined, it is clear that six sites are oriented towards the

southeast: DgKl-2, DjKn-l, DhKm-S, DiKp-l, DhKm-19, and DiKq-l0. DkKn-7, DhKm-

18, DiKm-3, and DgKm-2 face southwest while DgKm-l, DiKm-4, DgKl-17, and DgKl-l

face east. DhKm-20 faces northeast and DhKn-6 face northwest. DhKo-l faces north and

two sites, DgKl-19 and DhKm-l, face in a direction between east-southeast and east. DiKn-

1 faces a direction that lies between south-southeast and southeast and the face of DhKm-S

is orientated in a direction between southeast and east. One site, DhKn-l, faces west­

southwest. DjKr-23 faces south-southeast while DhKm-4 faces in a direction between south

and south-southwest. DiKm-Sl faces in a direction between south and south-southwest.

These results, with the exception of the three sites that face north and northwest, confirm

Dewdney's (Dewdney and Kidd 1962: 6) general statements regarding the orientation of the

surface of paintings discussed in Chapter III. The physicallocation and the orientation of the

pictograph sites on cliffs in the Lake of the Woods cannot support Reid's (1980) observation

discussed in Chapter III. Therefore Rajnovich (1980b: 34)'s claim that south-to-east facing

rock walls were selected as places to paint pictograph, discussed in Chapter III, is equally

difficult to consider. A connection may exist between the orientation of the site and the

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~ ..

presence of exfoliation. Unfortunately, it is difficult to establish whether exfoliation exists for

DhKo-1 and DhKm-20. Exfoliation has occurred at DkKn-6 which faces northwest (see

Appendix 5). Appendix 5 demonstrates that only five of the ten sites that face directions

between south and east are affected by exfoliation. It is difficult to establish whether

exfoliation has occurred at DhKm-5, DjKr-23, and DgKI-1 while exfoliation does not appear

to occur at DiKm-4 and DhKm-19. Yet ali seven sites that face between south and west­

southwest suffer from exfoliation

Appendix 5 illustrates that the three sites facing north, northeast and northwest

suffer from lichen growth. Fifty percent of the sites that directly face east or southeast suffer

from lichen growth and encroachment. Ali sites oriented between south and east have

images that suffer from lichen growth and encroachment. Ali four sites that face southwest

also suffer from lichen growth, but the images at DhKn-1 and DhKm-4, which face south­

southwest and west-southwest, do not suffer from lichen growth. Why both sites are similar

in this respect is unclear since the physical location of the images at each site is different.

However, both of the se sites suffer from severe exfoliation. Neither suffer from rock tripe

encroachment. This is bizarre, especialiy since DiKm-51, which faces a direction between

south and south-southwest, suffers from exfoliation as weli as rock tripe encroachment.

Rock tripe encroachment should be considered next since it often occurs ln

conjunction with lichen. It occurs at two of the three sites that face in a northerly direction.

Rock tripe does not grow at DhKm-20, a new site, but it occurs at DhKn-6 and DhKo-1,

two older previously known sites. However, lichen growth occurs at ali three sites. The lack

of rock tripe at DhKm-20 may be because rock tripe takes a longer period of time to

establish itself in comparison to lichen. Rock tripe does not occur on any of the sites that

face east, or on four of the six sites that face southeast. The two southeast facing sites where

it does occur are DiKp-1 and DjKn-1. Both sites were among the first to be recorded and

discovered in the Lake of the Woods region. (Lawson recorded the images of DiKp-1 in

1885 and Dewdney recorded the images of DjKn-1 in 1958, whereas he recorded the

majority of the sites he examined in this region in 1960 or later.) The other sites that face

southeast were recorded from 1960 onwards until 2001. The five sites that face directions

between south and east, excluding those that directly face southeast, ali have rock tripe

affecting the images. It is clear that the images at DjKr-23, facing south-southeast, have not

yet been encroached on by rock tripe. Appendix 5 shows that the seven pictograph sites face

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directions between the west and the south. However, only two of these sites, DiKm-3 and

DiKm-51, are affected by rock tripe.

Appendix 5 makes it clear that all three sites that face in a northerly direction suffer

From the deposition of white mineraI deposits. It is clear that only two of thirteen sites facing

From an easterly to a southeasterly direction do not suffer From the deposition of white

mineraI deposits. Neither DhKm-3 nor DhKm-19 appear to suffer From exfoliation.

Appendix 5 also indicates that the majority of sites facing between south-southeast and west­

southwest do not suffer From an accumulation of white mineraI deposits. Only two sites in

this category suffer From an accumulation of these deposits: DiKm-3 and DgKm-2.

Correlations exist, since white mineraI deposits, lichen and rock tripe always occur on

sites that face a direction between east and southeast, such as DhKm-5, DhKm-1 and DgKl-

19. Rock tripe sometimes occurs here. Sites that face southeast will most probably suffer

From exfoliation, the deposition of white minerai deposits, and, possibly, From rock tripe and

lichen. The relatively large number of sites in this group provides me with the ability to draw

some simple conclusions regarding the possible sequence of processes that occur at a site

after images have been created there. It is impossible to establish the precise date of image

creation at each site but sorne observations can be made if the recording date of each site is

used as a base line.

DiKp-1 was first recorded in 1885. By 2001, it suffered From exfoliation, the

deposition of white mineraI deposits, and lichen and rock tripe encroachment. Dewdney first

recorded DjKn-1 in 1959. In 2001, it suffered From lichen and rock tripe encroachment,

exfoliation and the deposition of white mineraI deposits. DhKm-3, recorded in 1958 by

Dewdney suffered, in 2001, From all of the same problems as DjKn-1 except for the growth

of rock tripe. Dewdney recorded DiKq-10 in 1960. It suffered From the deposition of white

mineraI deposits, but not From rock tripe and lichen encroachment. Unfortunately, it is

difficult to establish whether exfoliation was a problem when Dewdney recorded it.

Although DgKI-2 was first recorded in 1989, it suffered From the deposition of white

mineraI deposits and exfoliation by 2001. Lichen and rock tripe were not evident at this site.

DhKm-19, one of the newly discovered sites with new images, belongs to this group, and in

2001 it did not suffer From anything. Ali of the sites except for DhKm-19 suffered From the

accumulation of white mineraI deposits. It is difficult to establish whether exfoliation is the

second process that occurs at site since it is hard to evaluate its presence at sites if has just

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commenced. However, it is clear that lichen grows at sites before rock tripe. An additional

problem is whether rock tripe and lichen encroachment occurs over white mineraI deposits.

Clearly a sequence exists for sites that face southeast but unfortunately it is impossible to

calculate the rate of each process and when each one commences.

An interesting possibility is a correlation between the presence of blobs and

exfoliation, existence of white mineraI deposits, lichen and rock tripe encroachment and the

orientation of the rock face. The most common shape is a 'blob,' and seventy-seven different

types were identified to exist at the pictograph sites. However, a correlation does not exist

between the level of exfoliation, existence of white mineraI deposits, lichen and rock tripe

encroachment and a large proportion of blobs at these pictograph sites. Examination of

Appendix 5 indicates a relationship exists between the orientation of the site with the

number of blobs.

It is clear from Appendix 5 that the strongest relationship between orientation and

blobs exists for DiKn-1, DhKm-5, DgKI-2, DjKn-1, DhKm-3, DiKp-1, DhKm-19, and

DiKq-10. These sites face between east-southeast and south-southeast. A weaker correlation

is evident in Appendix 5 for those sites on cliffs that face southwest. Two of the four sites in

this group severely suffer from a large number of blobs. Unfortunately, it is difficult to

determine why only two of the four sites have blobs. It is likely this could be related to the

age of the images at each site. It is clear that not only does the rate of these processes differ

from one site to another (see Appendix 5) but Dewdney (an amateur researcher) and

subsequent archaeologists may have been interfering with this process by removing the

lichen and the rock tripe to establish the range and nature of the images at each site.

Dewdney indicated that he removed the lichen with a wet sponge from surface of the images

at several sites so that he could better see and record the images (for example Dewdney and

K.idd 1962: 6).

Another problem that complicates establishing the age of a site is that different

archaeologists have disagreed as to what was an image (please see Chapter III for a

discussion of why images such as smears were not considered to be images and the effect of

this decision.).

The accumulation of white mineraI deposits is influenced by the quantity of soil at

the top of the cliff, the number of times it rains during the year and the physical structure of

the rock itself. However, sin ce ground water sporadically seeps down the rock face, mainly

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,-r-...

during the spring and fall period, it is possible that faint images are older than the bright

ones.

An interesting alternative to resolving the possible age might be to examine DhKm-

20, a pictograph site whose surface suffers from exfoliation, lichen encroachment and white

mineraI deposits but not rock tripe. The red shape at the top of this site is affected by lichen

encroachment and the fish shape below is affected by white mineraI deposits. However,

none of the images is affected by exfoliation or by rock tripe encroachment although it is

present nearby. It also has a date of "1982", faces northeast and has no blobs. The site was

only 20 years old when l examined it in 2001. It is possible that these images have not started

to noticeably decay because they are not created from ochre paints.

If the orientation and the new sites are examined in conjunction with one or two of

the four problems that affect sites, interesting observations may be made. It seems likely that

lichen growth or the accumulation of white mineraI deposits are probably the first problems

to occur. The other issues just exacerbate the problem. Since lichen was removed on the

older sites by previous archaeologists, it is impossible to posit the precise rate at which

encroachment might occur.

So, what can be concluded? It can be argued that many pictographs are probably

older than 50 years. Wainwright and his colleagues during the 1970s pushed the date

backward with their observation that the pigments migra te , a process that would take sorne

time. However, image analysis of the rock surface aided me to establish that, although lichen

encroachment had occurred at the earliest documented site in Lake of the Woods (DiKp-1),

paler images, which Lawson (1885), Dewdney (1960), Molyneaux (1974) and Reid (1974) clid

not record, exist at this site. None of these adclitional, paler, and hence possibly older, images

were observed or cliscussed although the principal group of images had been examined in

considerable depth (see pages 330-335). Today, it is still possible to identify the images first

recorded in 1885 by Lawson, later by subsequent researchers, and only one of the images is

paler, since it has been affected by the accumulation of white mineraI deposits. Fourteen

images were identified at this predominately southeast facing site, of which two were faint

unidentifiable shapes and five were blobs. The blobs were not identified by previous

researchers and probably were not cleaned of lichen, if the surface of the main group was

cleaned. Hence, it is possible to posit the argument that lichen grows slowly on southeast

facing surfaces.

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It is difficult ta assess the quantity of mineraI deposits left on the rock surface, but it

is likely influenced by the depth of soil on the top of the cliff face, rather than in the rock

itself since relatively little or no white mineraIs were found on the paintings that occur on the

roof of both caves. Perhaps because cliff faces are vertical, rather than horizontal, water drips

straight down from the top of the cliff carrying with it mineraIs which get caught in

microscopie irregularities on the rock face. DiKm-50 was affected only by exfoliation while

DiKm-49 was affected only by lichen. None of the images at either site was new. The images

at both sites were mostly likely affected by wave action and changing water levels since they

both have sorne water close to their base. It is very hard to account for the rate of exfoliation

because of other influential factors such as the changing water levels, and ice formation in

different channels.

It is difficult to answer question Cc) regarding stylistic developments because changes

in how archaeologists have considered images, such as smears, has led to sites like DgKl-2,

DhKm-4 and DhKm-l becoming clearly defined, others recognised as being larger, and, in

the case of DhI<m-4 and DhI<m-l, as being separate sites. However, whether this has

affected the recognition of additional images at sites such as DiKp-l is difficult to determine.

It is clear that the use of new computing software has enabled images that were difficult to

see on sites such as DhI<m-3 and DiKp-1 to be more visible. Other than commenting on the

difference in the centres of the ochre images, very little can be concluded regarding the styles

of the ochre images. This chapter has already established that the ochre images in the Lake

of the Woods resemble those found throughout this part of Northern Ontario. However, the

images painted in modern paint, discovered and recorded in 2001, differ both From images in

ochre and between themselves as regarding their style and colours.

The images in the Lake of the Woods are different. Sorne were created in ochre,

sorne were painted in modern spray paints with a date, sorne were painted in modern paint in

several colours, and sorne were created using modern paint over ochre images after 1989.

The new modern images at DhKm-20 were painted in red, white, and blue paint. The fish

shape was created in blue and white with red spots either side of a horizontal white line

which runs the length of the fish shape. These shapes bear a strong resemblance to those

created by the artists who are considered members of the Woodland School of Art

spearheaded by Norval Morrisseau.

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(\

Time affects both the physical size and condition of an image and can totaily alter the

style in which the image was originaily created. Ultimately, the image cailed a blob exists

regardless of the original style of the images. If an image was hoilow or constructed of lines,

its shape might become unrecognizable faster than if it were solid. But ail these images with

different centres are found co-existing in the same geographical region (see Rajnovich

1981b).

Ideaily specific styles of images could be dated, enabling stylistic sequences to be

established, and providing the archaeologist with the tools to determine the order in which

the sites were painted. Such information would en able the archaeologist to consider and

confirm speculations regarding whether images were placed in groups, or one at a time

ultimately creating the effect of a group of related images (see Rajnovich 1980b). Indeed,

secure dates for specific styles enables the archaeologist to establish the time sequence in

which images may have been superimposed on one another if images were repeatedly over

painted at sites. Secure dates for specific styles of different images would sanction the

archaeologist to contrast and establish any offerings left at a site that could be dated with the

style of the images at the same sites or groups of sites.

A detailed examination of the previous field recordings of each site reveals that

considerable developments and changes have occurred in the techniques used to record

these sites (see pages 136 to 161 of Chapter III). Any changes in the size of the same images

could reflect these developments rather than anything else. Furthermore previous

archaeologists have differed in their opinion as to the importance and recognition of

different images (as evident in Chapter III). However, a detailed critical comparison of the

field drawings, photographs, and reports was difficult to conduct, since it was impossible to

obtain a complete set of information.

Conclusion for the chapter:

This chapter has presented and discussed the information that should be coilected in

the culture-historical approach. Ail the information discussed in this chapter is summarised

and presented in Appendix 5. Many of the sites are affected by the deposition of white

mineraI deposits, exfoliation of the rock's surface, lichen and rock tripe growth and

encroachment. Hence, large numbers of images are blurred, obscured, and almost destroyed.

Ail the images probably once had clear, distinct edges but they are ail ultimately becoming

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blobs before they are completely destroyed. These images have, like the rock surface on

which they exist, a life-cycle. All of these processes cause difficulties for anyone describing

these images. Analysis of the images using Adobe PhotoShop and VIPS indicated the fragile

nature of the images, the sites, and their changing nature. It also demonstrated the major role

played by the human eye and the brain in the identification of the individual images.

Relatively few sites exist in the southern and the northern portion of the Lake of the

Woods region. Two sites exist in the northwestern portion of the region but sites do not

exist in the southwestern region. This is possibly a consequence of the fact that the geology

is different, the land is lower than elsewhere in Lake of the Woods, and hence this part of the

lake was probably the most severely affected as the water levels were artificially raised from

1888 onwards. It is therefore difficult to determine whether trus distribution is connected to

the fact, raised in Chapter II, that in the early seventeenth century the Algonquian-speaking

peoples seasonally resided in the eastern portion of the Lake of the Woods and only

gradually took control of the western portion as the Assiniboine srufted westwards in the

middle of the eighteenth century (Heidenreich in Harris 1987: Plate 37).

Section 2 of trus chapter established that a total of three hundred and twenty-four

images were recorded. The average number of images per site is twelve and the minimum

number of images per site was one. DhKm-19, DiKm-SO, and DhKn-6 have only one image

while DhKm-S has the largest number of recorded images, trurty-seven. Deposits of white

mineraIs, lichen and rock tripe encroachment, and exfoliation of the rock surface takes place

over time and results in the destruction or fading of images. These images, or shapes, are

neither static nor timeless. A relatively small range of image types is found among preserved

images. However, given that these images are on rocks exposed to the elements and start to

deteriorate and often begin changing shape soon after they were created, it is impossible to

establish the full range of combinations of images that once may have been present. The few

types of images found to exist in the Lake of the Woods are a, contrasts sharply with the

popular belief that a relatively large vocabulary of images was in use.

Section 3 of trus chapter demonstrates the great difficulty 111 classifying and

describing any image and that the level of description given to an image affects its analysis. It

is possible to classify the images differently, and the vocabulary used heavily influences the

possible outcome of any discussion of perceived style. It is important to take the middle road

between the "splitter" and the "lumper" approach when describing images. A nested

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hierarchy of types leaves more options open with respect to classification. The presence of a

large range of different shapes that occur only once causes me to speculate that a

considerable number of people probably moved through this region and used these images

to convey information. It suggests that these images were part of the larger vocabulary of

signs used by everyone and not solely the product of specialised religious practitioners, such

as the Midé. This makes it more likely that each image was created independently and was

understood separately from the other images at a pictograph site. Tt is possible that the

organization of images and the combination of images does not reflect any particular set of

rules, other than the fact that individuals used the same place over a period of an unknown

time. Perhaps the variability in the form of images reflects a lack of standardization. It is also

possible that this variability also reflects the fact that the images changed over time.

It is impossible to precisely determine either the implements used to apply the paint

or its ingredients. Tt is possible to posit that fingers were probably used to apply the paint.

Ethnographic evidence supports the ide a that iron ore, ochre, was used and possibly isinglass

from the air bladder of the sturgeon, a fish that lives in this region of North America.

Not ail the pictograph sites had offerings when they were examined in 2001. The vast

range and quantity of offerings Ieft at the sites suggest that the physicai locations and the

paintings were and are important. Most of the offerings that have survived were Ieft in cracks

or crevices or dropped into the water in front of sites. Ethnographic evidence provided

additionai support regarding the importance of these offerings (Densmore (1974 [1928]),

Hilger (1936), Coleman (1947), Warren (1984 [1885]), Smith (1995), and Pufahl (1990).

Dating these images remains a problem, since direct dating techniques cannot be

used. The presence of datable offerings at a few of the sites provided an indicator of the

length of time, or periods in time, in which these sites have been used. But they did not

provide a strong indicator of the age of the images. Indeed, it remains impossible to establish

the precise date at which ail but the most recent of these images were created. Dewdney,

who first recorded many of the sites, relied upon reports of the sites from informants who

often did not give any indication of the length of time these sites were believed to have

existed prior to them being "discovered."

It was very difficult to use lichen growth as a measure of age since the rate of growth

appears to differ from site to site and it is impossible to establish how many visitors,

researchers, and archaeologists foilowed Dewdney's practice of removing the lichen that

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coyer many of these paintings. This prevents establishing a baseline for each site that would

ailow archaeologists to determine which images existed first and which ones were

subsequently added.

Whether the images present upon the pictograph sites have changed over time is

impossible to determine. The great variability of images suggests that doing this stylisticaily

will be difficult if at ail possible. This method is problematic given the incomplete

documentation regarding these sites in combination with the changing methods used to

record them.

Although it is impossible to establish the exact age of each site, it is possible to

conclude from the presence of blobs at sites throughout the Lake of the Woods that some of

the images were created some time ago. VlPS software and the Adobe Photoshop 6.0

provided me with the ability to establish whether additional paler images existed beside the

readily visible images. Both highlighted the fact that it was important to look beyond the

areas of the surface of the rock that had strong, clearly defined, red images since paler images

could exist elsewhere on the rock surface. The presence of both the pale and the dark red

images in ochre as weil as the modern spray painted images indicates that these places were

and are being used.

Observations regarding the distribution of different shapes, different combinations

of shapes, the association between the five required physical traits with images and any other

possible patterns wiil be examined in the next Chapter.

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Chapter VI: Contextual Approach

This approach connects the culture-historical information discussed in the previous

chapter with the distribution of the images found at each site and the natural features of each

site. The previous chapter applied the culture-historical approach to the data collected in

2001 and established the range of the images, their possible age, and their location. A nested

hierarchy of types was believed to leave the most options open. Individual images were not

static but changed over time, since they were subject to the accumulation of white mineraI

deposits, lichen and rock tripe encroachment, and exfoliation of the rock surface.

This chapter applies the contextual approach to consider a broader set of

associations and relationships regarding the generallocation of the site, between the images

and rock surfaces, and among the images themselves. At this level l offer low-Ievel

generalisations from my data and do not search for explanations of what these data might

mean. This chapter also considers previous research regarding these same issues. The first

section discusses the physical location and physical features of the sites in the Lake of the

Woods, the second section considers the relationship between the images and the rock

surfaces, and the final section examines the images themselves and considers whether

relationships occur between each shape. (The same data was also examined for clusters using

SPSS and the results were presented as dendrograms in Appendix 16.) Shapes occur on cliff

faces and inside caves; however, this difference in location is only important for section two

which deals with the issues concerning the images and the rock surfaces.

Section 1:

(a) Possible correlation between the geology, the geomorphology, and the type of

land mass on which the sites exist.

Fieldworkers accept that pictograph sites occur on granitic cliff faces throughout the

Canadian Shield. This belief about their physicallocation has fundamentally affected the way

in which archaeologists have surveyed them. This supposition presumes that the geology and

the geomorphology of each locale, of each site, is the same. It also presumes that the

landscape is the same.

Chapter V established that the Lake of the Woods sites were on Pre-Cambrian

granite on the northern and eastern portion of the Lake of the Woods, but the geology and

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geomorphology of the sites are quite complex (see Appendix 8). If the geology of ail of these

sites is examined, it is evident that twenty-five of the sites are on rocks identified as

hornblende, gabbro, diorite, periodite, or serpentine (see Appendix 8). DiKp-1 and DhI(m-

19, in contrast, were found on schistose volcanic rock with smail amounts of iron bearing

sediments. Considerable quantities of volcanic rocks and younger sediments, according to

Tanton (1939), also occur at both sites.

Most of the sites described in Appendix 7 share the same general geomorphology.

Twenty-four are in areas where more than eighty percent of the rock is outcrop composed of

ice eroded Archean granite with patches of thin drift and scattered boulders. The

geomorphology of DjKn-1, DkI<n-6, and DkI<n-7 is not the same as that of the other

twenty-four sites, although they have the same geology as the majority of the sites (Appendix

8).

A strong correlation cannot be established between the geology and geomorphology

of these sites. Nether is there a strong correlation between the geomorphology, geology, and

the type of landmass of each site (see Appendices 8).

(b) Possible correlation between the main travel routes and the physicallocation of

the sites

It is important to consider whether the physicallocation of each site is connected to

mam tracks, or travel routes, through the region; and the significance of any such

relationship. These tracks, the recommended routes indicated by either red continuous or

discontinuous lines on the charts produced by Fisheries and Oceans Canada, indicate the

safest route though the islands, reefs, and shailows from the twentieth century onwards.

These thoroughfares are used by sailors and boatmen, as discussed in Chapter IV, to travel

safely through this lake. These routes ailow relatively inexperienced people with little

knowledge or no knowledge of the region to move from one part of the lake to another.

These routes use the deepest part of every region of the lake and avoid lee shores (shores

facing the prevailing winds).

Although these routes may weil be the best ones for motorised boats, they are not

necessarily as suitable for canoes or sail boats. Travelling by canoe or by sail requires a

different range of techniques and methods. Both types of vessels are affected differently by

the wind, the water, small local rapids, strong local currents, and changes in the weather.

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People travelling by canoe would have preferred travelling in areas protected by islands and

large land masses, since the water and wind action would have been reduced. Historically this

region was explored by canoe and not by motor boat, although people travel through this

region by motor boat today.

Canoeists crossed the Lake of the Woods using routes protected from strong winds

and open water where wave action would have been strong enough to easily swamp and

capsize canoes. This could explain why two routes existed through this region from the fur

trading posts in the Rainy Lake region southeast of Lake of the Woods to Rat Portage at its

north end. One route went through Whitefish Bay, east of the Aulneau Peninsula to Rat

Portage. The second, longer route ran west of Aulneau Peninsula via the Big Traverse, which

is the large body of open water in the southwest portion of the Lake of the Woods. Those

who visited and created these rock image sites knew how to manoeuvre and travel in and

around as weIl as through the Lake of the Woods. Chapter V established that the majority of

the sites are located in the northern and eastern portion of the lake and it is clear from

marine maps of the region that they are not always near the modern major thoroughfares.

Chapter V established that two sites were known prior to Dewdney's recordings of

the 1960s: DhKo-1 and DiKp-1. Lawson first recorded DiKp-1 in 1885 (1885), and,

although DhKo-1 was first recorded in 1936, aIl the boat captains who worked on Lake of

the Woods in 1910 knew of it. Neither site is beside a main track used by motorised boats

(see Appendix 9). But both sites were visited, otherwise no one would have reported their

presence to individuals such as Dewdney. Campbell's observation, discussed in Chapter V,

that she found religious slogans over the images at DhKo-1 when she revisited the site in

1951 confirms that previous knowledge.

The introduction of motorised boats in the 1870s changed the method of travel

through this region; now it could be travelled and explored without total reliance on

manpower and dependence on marine weather conditions. In 1872, the first motorised boat,

a small steam launch or tug with a "3 or 3 % feet draft," (1.07 metres) left from Hungry Hall,

the Hudson's Bay Company post on the mouth of Rainy River, and crossed the southern

part of the lake to Northwest Angle Inlet on the southwest si de of the Lake of the Woods

(International Joint Commission 1917: 195). Two more boats built by the Canadian

Government especially for this route (ibid.) repeated this journey in 1873. The government,

mining and lumber companies, and private individuals built and launched boats of different

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/- ...

sizes and types from 1876 onward for transporting freight and passengers, for towing logs,

and for the fisheries. How the raised water levels affected the co mm on travel routes in the

region is impossible to determine, but they were affected.

Some sites lie beside or near the main modern thoroughfares through the lake. lt is

possible that the physical location of new sites such as DhKm-19 and DhKm-20 may be

connected to several changes in the routes, the type of boat, the physical location of the

previously known sites, and possibly even the changes in the water levels discussed in

Chapter IV. However, these links cannot be established.

(c) Possible correlation between the local reserves, the offerings left, and the sites

The presence of offerings could be linked to the proximity of Indian reserves to sites

in the Lake of the Woods. Trurteen, or 48%, of the pictograph sites are close to an Indian

reserve (xq091). Using maps of 1:250 000, 1:80 000 and 1:40 000, and assuming that

Algonquian-speaking peoples left the offerings that archaeologists found, l established wruch

reserves were closest by boat to each site. The reserves in trus area were set up after the

Algonquian-speaking peoples signed Treaty #3, the North West Angle Treaty, in October

1873. If pictograph sites were located near reserves, then offerings should be present. The

word 'near' implies that site is within 6 miles, or 5.21385744 nautical miles, or 9.6506404

kilometres by boat from the nearest reserve. The journey would only take between 15 to 20

minutes by boat. The data in Appendix 9 indicated that DgKI-17, DgKl-2, DgKl-1, DjKr-23,

DhKn-1, DiKm-4, and DhKo-1 are located near an Indian reserve and had offerings in

2001. But DgKm-2, DhKm-19, DgKl-19, DgK.m-1, and DiKq-10, are also near a reserve,

but they had no offerings in 2001. Although, DhKm-20, DiKn-1, DhKm-1, DhKm-3,

DhKm-5, and DhKn-1 were not near a reserve, offerings were discovered at these sites in

2001. DiKm-50, DiI<m-51, DiI<m-49, DiI<m-3, DkKn-6, DkKn-7, DjKn-1, DhI<m-4,

DhI<m-18, and DiKp-1 are not near a reserve and offerings were not found in 2001. It was

not always necessary for a site to be near a reserve for offerings to be found in 2001; and the

reverse is also true.

lt is possible to determine whether offerings were found at these same sites in the

past by previous archaeologists, as the literature of this region shows. Appendix 9 illustrates

that on1y nine of the twelve sites that had offerings in 2001 were found with offerings when

they were first recorded. The group of nine sites includes: DgKl-1, DgKl-2, DhKn-1, DjKr-

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23, DhKm-1, DhKm-S, DiKn-1, DjKn-1, and DiKm-4. Only five of these sites are near a

reserve. Information in Appendix 9 indicates that previous archaeologists found offerings at

DiKq-10, DhI<m-18, DjKn-1, and DiI<m-3. No offerings were found at these sites in 2001

(see Appendix 9). DhKo-1, DhI<m-3, and DgI<J-17 did not have offerings when they were

first discovered but only DgI<J-17 and DhKo-1 are near a reserve. Information in Appendix

9 demonstrates that only DgI<J-1, DgI<J-2, DhKn-1, and DjKr-23 of the sites that were near

reserves had offerings both when they were first recorded and in 2001. DiKq-10, which is

near a reserve, no longer had offerings when it was recorded in 2001. DhI<m-18, which is

not near a reserve, had offerings when it was first recorded but not in 2001. No reserves

were located near five of the sites that had offerings in 2001 and when they were first

recorded. This group includes: DhI<m-1, DhI<m-S, DiKn-1, DiKm-3, and DiI<m-4 (see

appendices 9 and 16).

The physical proximity of a pictograph site to an Indian reserve does not influence

offerings, as shown in the records of both previous archaeologists and my fieldwork in 2001.

(d) Land mass, orientation of the sites and the presence of offerings

Reid (1980) and Rajnovich (1980b) considered the type of land mass on which the

sites were found and the orientation of sites' surfaces to be related to each other. They

claimed that pictograph sites were usually on either straight shorelines or coastlines that were

not broken into parts by bays, islands, or points. Reid (1980) based his observation on the

physical location of pictograph sites in the West Patricia region, north of the Lake of the

Woods. Unfortunately, this daim is problematic for the Lake of the Woods for sorne of the

previously known sites such as DiKn-1, DhI<m-18, DgI<J-1, DiI<m-3, DgI<J-19, DiKq-10,

and DgI<J-17 are on the shorelines of points of land. Both Reid and Rajnovich contended

that the creators of the images chose these places specifically for the orientation of the cliff

face in specific directions.

Appendix 9 indicates that both of the sites in caves, DiKm-SO and DiKm-49, are on

islands. Eight of the twenty-five cliff sites were found on islands, eight sites on the Aulneau

Peninsula and eleven sites on the mainland.

The variable of directionality was added to establish whether correlations occur

between the land mass of the sites and orientation of the rock surfaces. The sites in caves

cannot be induded in this discussion since they have two entrancesj exits and paintings are

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inside the caves. Previous archaeologists Dewdney (Dewdney and Kidd 1962: 6), Reid (1980)

and Rajnovich (1980b: 34) observed that pictograph sites on cliffs tended to face towards the

east to south and occasionally west and the south (see discussion in Chapter III).

Subsequently, archaeologists such as Lambert (1983: 19-20), Pastershank (1989: 49 & 71),

and Rusak (1992a: 23) noted the compass bearing of the rock surfaces on which pictographs

survive. The data collected for the cliff sites in the Lake of the Woods, in Appendix 10,

indicates a strong correlation between sites on islands and either an east to south-south-east,

or an east to east-south-east orientation.

These findings only partially support Rajnovich's (1980b: 34) argument that south-to­

east facing cliff walls were selected because the light conditions were "best for creating and

seeing paintings." Rajnovich asserted that a body of water had to exist immediately beside a

site so as to increase its "dramatic value" (ibid.), but pictograph sites in the Lake of the

Woods do not always occur beside water. Appendix 10 data reveals that there is no

correlation between the orientation of such sites and the land mass (please see Chapter N

for the definition of this term) on which they are located.

Data concerning the presence of offerings at the twenty-seven sites in 2001 was

added to determine whether there are any correlations between the specific orientation of the

rock surface and of the land mass. Correlations do not exist between the orientation of a site,

the land mass on which it exists, and the presence of offerings in 2001.

Reid (1980) did not qualify his observation with physical measurements or with an

example as to what "a straight shoreline" was. l did not consider the type of shoreline in my

research. l think that this type of observation is too subjective, sin ce it depends on the

opinion of the archaeologist in question.

(e) Possible correlations between the number of images at sites, vegetation, water

levels, the water beside the cliff face and the caves:

The belief held by previous archaeologists that pictograph sites always occur on cliff

faces immediately beside water probably has affected survey methods. Major important

variables include the accessibility to the images on the cliff faces and in the caves, the

vegetation in the immediate vicinity of the images, and the current water level. The physical

position of the images probably is connected to the height of the water level when the

images were created, especially where the painter had to sit in a boat while painting them.

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The availability of a flat surface devoid of lichen and rock tripe could have influenced the

physicallocation of the images on the rock surface, and the number of images.

Information in Appendix 11 dissolves Pohorecky (1968: 103)'s statement that ail the

pictographs were readily observable from a canoe. Two cave sites were found, and only the

images in DiKm.-49 were visible while stiil sitting in a boat in a spot accessible only during

the abnormaily high water levels of 2001. The images at DiKm.-50 were only visible once we

crawled inside the cave after leaving the boat. Ail of the pictograph sites on cliffs in the Lake

of the Woods were only accessible by some form of boat (xq097, xq096, xq016, and xq017).

However, shailow water at the base of several cliff sites, and a high water level meant that it

was impossible to examine and record the pictographs at DjKn-l, DkKn-7, and DkKn-6

using our motorboat, so a canoe was used instead (xq097). In 2001, twenty-one of the

twenty-seven sites had water at the base of the cliffs (xq206, xq 133, & xq145) (see Appendix

16). These sites are: DgKm-l, DhKm.-l, DgKl-l, DgKl-17, DgKl-19, DgKl-2, DgKm-2,

DhKm.-4, DhKm.-5, DiKm-3, DiKm-4, DiKm.-51, DiKn-l, DiKp-1, DiKq-10, DjKr-23,

DjKn-1, DhKo-1, DiKm.-49, DiKm.-50, and DkKn-7. Sorne of the images at these sites had

to be examined by standing on rocks in front of, or beside, the site as weil using a boat:

DiKm-50, DiKm-49, DhKn-1, DhKm.-19, DiKn-1, DhKm-3, DgKl-2, and DjKn-1 (xq096

& xq097). However, sorne of the sites known prior to 2001 did not have water at their base

and consequently did not meet Pohorecky's (ibid.) requirement that sites always occur

immediately beside water. DhKm-3 and DhKn-l did not have water at their base. Ail of the

sites discovered in 2001 required a boat for access, but additional hiking or climbing was

necessary to reach the images at DiKm-50, DhKm-20, DhKm.-19, and one part of DjKn-1.

Previous archaeologists possibly forgot that water levels change from season to

season, year to year, and over longer intervals. Indeed, the water level in 2001 was

approximately 76.20 cm (2.6 feet) higher than the level considered normal. As discussed in

Chapter II, the water level does not remain static because it is controiled by the International

Joint Commission and therefore the images can be directly affected by the fluctuating water

levels. It is clear from a visual comparison of DhKm.-1 in the photograph in figure 5.66 with

the photograph in figure 6.1 that the water level affected the images more in 2001 than in

2003. The water levels were higher than average in July 2001 and considerably lower in late

August 2003 when the region experienced a severe drought. The high water marks on the

surface of the rock are visible in the photograph below (figure 6.1).

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Figure 6.1: DhKm-1 photographed August 27th 2003

Rajnovich's (1980b: 34) assertions regarding the physicallocation of the sites adjacent

to water and the close proximity of the images to the water imply that ail cliffs are the same

height and shape. Yet, the data presented in Appendix 11 indicates incredibly varied cliff

heights. Equally evident was the range of physical features found at each cliff face, especially

after careful examination of the data in Appendices 11 and 12. This data will be discussed

later in this chapter.

The difficulty of securely dating these sites contributes to the problem in asserting

that pictograph sites always occur in conjunction with water. If the water level of Lake of

the Woods had not been artificially raised in the past, sorne of the sites such as DiKm-3,

DhKm-20, DhKm-19, DiKm-4, DiKn-l, DiKm-49, DiKm-SO, and DgKm-l might have

had less water at their base than they did in 2001 or at times when the levels are now

considered normal. Therefore, a canoe or a boat was not used either to see or to create the

images at these sites because an individual could have stood on dry land. It is possible to

draw this conclusion because the water was shallow at the base of these sites. The

presence or absence of water at the base of cliff sites and caves affects the range of plants

found at their base. Dewdney (Dewdney and I<idd 1962, 1967), Pastershank (1989),

Lambert (n. d.), and Rusak (1992a) invariably noted only whether rock tripe and lichen

growth affected the images and the physical status of the site. They did not comment on

plants growing on the top, sides, or on the rock surface near the paintings (xq137 and

xq208). Many sites suffered from rock tripe and lichen encroachment, but the 2001 crew

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identified moss, harebells, gooseberries, raspberries, and bracken ferns growing in the small

crevices near paintings (xq137 and xq208). Few previous archaeologists have considered

plants at the base of painted cliff faces. The growth of plants at the base of a cliff provides a

weak indication of previous water levels. If water levels shift dramatically, plants such as

water lilies are unable to grow. Plants that have started to grow in the small cracks and

crevices at the base of cliffs die, either because they lack water as the water level falls, or are

drowned by rising water. Therefore, l recorded the vegetation on the top, the side(s), the

surface, the base of the cliffs, and both of the caves (xq133, xq134, xq137, xq138, xq207, xq

211, xq 210, xq 209, xq 208, and xq 206).

Several sites had both plants and water at their base, as seen in Appendix 11. Water

was not always immediately present below the paintings, since plants, in conjunction with

rocks, were often present. Although l noted water, sorne plants also grew at the base of

DjKn-1, DhKo-1, DkKn-6, DhKm-18, and DkKn-7. Water lilies thrived at the base of part

of DjKn-1; but sorne raspberry bushes rose from rocks at another part of the same site.

Water lilies floated on the surface of the water at DkKn-6. A small pin cherry tree and a

raspberry bush grew in cracks at the base of the cliff face at DhKm-18. DkKn-7 overlooked

a raspberry bush and sorne water lilies.

Four sites have images on cliff faces that were not directly beside water: DhKn-1,

DhKm-20, DhKm-3, and DhKm-19. Rock and a wide variety of plants were found at the

base of these cliffs. DhKn-1 had white pine, spruce, birch, juniper, pale corydalis, goosefoot,

harebells, dogbane, rough avens, northern bush honeysuckle, bear berry, alum root, vetch,

columbine, various grasses, bracken fern, rock tripe, as weil as lichen. A juniper bush, pale

corydalys, sedge, and moss flourished at the base of DhKm-3 amongst the large rock fall and

a wide variety of fully grown trees. Bracken fern, moss, and rock tripe grew on DhKo-1,

which also had water at its base. DhKm-19, (figure 5.142), discovered in 2001, contained an

image painted immediately ab ove a rock ledge large enough to stand on with ease, and

covered in small poplar trees, harebells, sedges, gooseberries, raspberry bushes, northern

bedstraw, alum root, and lichen. The images could seen either from a boat, or while standing

on the ledge.

Correlations between the number of images present at sites and the method of

viewing these images cannot be established since the method of viewing and creating the

images depends on changing water levels. Pohorecky's (ibid.) statement regarding pictograph

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sites is problematic in the Lake of the Woods region, sin ce two sites were found inside caves.

Water existed at the base of cliffs of twenty-one of the twenty-seven sites examined (xq206,

xq 133, and xq145) and at the base of both caves. However, plants caused difficulties in

viewing the images from a canoe for eight of the twenty-five sites on cliffs. Hence

Pohorecky's daim that images were readily visible from a canoe and could be recorded from

a boat is inaccurate. He did not state if the other physical features su ch as large cracks, large

crevices, overhangs, holes and benches, which previous researchers induding archaeologists

have argued are important, impeded the visibility of these images. The presence of these

features will be examined later in this chapter.

Rajnovich's (1980b: 34) daims that sites were immediately beside a body of water and

were chosen for their ability to reflect light on the images are flawed if applied to the sites in

the Lake of the Woods. Rajnovich (ibid.) also left unconsidered the possibility that lichen and

rock tripe affected the visibility and the shape of the images. It is evident from Chapter V

that both lichen and rock tripe was a problem for many of the sites.

Both Pohorecky's (1968: 103) and Rajnovich's (1980b: 34) propositions become

awkward given the water level changes in the region discussed in Chapter II. Both

archaeologists have presumed that water levels at sites have remained static and enabled

viewers in a boat to see these images easily. Changes in the water level are and were

inevitable. A change in water level affects not just the accessibility of the person viewing and

recording images but the vegetation present, the relationship of the water to the images and

the site itself.

The following two dendrograms used the Euclidean distance method (Table 6.1) and

the Pearson correlation method (Table 6.2) and demonstrate that a weak relationship,

perhaps differing insignificantly, exists between the sites and the different features such as

the type of land mass, access to sites by boat, proximity to lndian reserves, offerings left

nearby the images in 2001, vegetation at base, proximity ta site and the number of cliffs if

the site was on a cliff face. "Presence - absence" tables were constructed using the

information discussed in Chapter VI with a "1" indicating a presence or "0" indicating an

absence (see Appendix 16).

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CAS E Lallel DiRq-l0

DgRrn-2

DgRl-19

DgRrn-l

DgRl-17

DjR"-23 DgRl-l

DgRl-2

DbKJn-19

DkRn-6

Dkl<11-7

DbKJn-4

DiRrn-3

DiRrn-51

DiRp-l

DbKJn-1

DbKJn-5

DiRrn-4

DbKJn-18

DhRm-20

DbKJn-3

DhRo-l

DiRn-l

DhRn-l

DjRn-l

DiRrn-50

DiRrn-49

Rescaled Dist811ce Cluste" Combine o 5 10 15 20 2S

IJum +---------+---------+---------+---------+---------+ 22

25

4

20

1

2

23

14

15

8 17

21 13

6

9

18

10

24

7

19

12

11

16

26 27

Table 6. 1: Hierarchical Cluster Analysis - dendrogram using Average Linkage (Between Groups) using Euc1idean distance method to establish whether a re1ationship exists between the sites and the different features.

CAS E LaIle1 DiRq-1O

DqRrn-Z

DqRl-19

DgRrn-l

DhRm-19

DgRl~17

DjR"-23

DgRl-1

DgRl-2

DkRn-6

DkRn-7

DbKJn-4

DbKJn-18

DiRrn-3

DiRrn-51

DiRp-l

DbKJn-1

DbKJn-5

DiRn-l

DiRrn-4

DhRo-l

DiRrn-50 DiRrn-49

DhRn-l

DbKJn-3

DbKJn-20

DjRn-l

Rescaled Distance Cluste:t: Combirle o 5 10 15 20 25

IJUlll. +---------+---------+---------+---------+---------+ 22

25

4

5 23

20

l

2

14

lS

8

10

17

21

13

6

9

12

18

19

26 27

11

7

24 16

Table 6. 2: Hierarchical Cluster Analysis - dendrogram using Average Linkage (Between Groups) using Pearson correlation method to establish whether a re1ationship exists between the sites and the different features.

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(f) Possible correlations between the physical features of the rock surface of

pictograph sites

Previous archaeologists, basing their daims on ethnohistorical and anthropological

sources, have asserted that key features of cliff faces are prerequisites for paintings in the

Canadian Shield (Rajnovich 1994: 11; Rusak 1992a: 23; Vastokas and Vastokas 1973: 47-54).

Caves will not be induded in this examination since their physical structure is radically

different. The key features of rock image sites on cliffs indude: deep holes, large cracks, large

crevices, rock overhangs, and rock benches or ledges. l examined the pictograph sites on

cliffs to ascertain the presence of these physical features at each site presented in Appendix

12. Not all sites possessed every physical feature deemed "crucial", or "required" by previous

archaeologists, as data in Appendices 12 and 13 reveal. Sites often had a minimum of two of

the five physical features, sorne of which occasionally affected the paintings themselves.

Each physical attribute is examined in sequence.

(i) Deep holes:

DgKI-2 and DkKn-6 had the physical feature called a "deep hole" in 2001. It remains

undear from the literature reviewed in Chapter III whether the size of the hole is important.

The key idea is that it is deep and part of the site. The hole at DkKn-6 is smaller than the

holes at DgKl-2. DgKl-2 contained two holes above the water level, with an additional,

smaller hole at the back of the larger hole indicated in the photograph below (figure 6.2).

Divers who assisted me found a third hole to the right and 2.13 metres underneath the

surface of the water. The annotated photograph below indicates that these holes acted as

openings to two caves.

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Figure 6.2: Annotated photograph by Cols on of the holes which are called caves at DgKl-2 in the rock above the water level.

Figure 6.3 depicts the interior of the large cave at DgKl-2 indicated above in figure 6.2. An

adult could move about inside this cave.

Figure 6.3: Inside the cave at DgKl-2

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Figure 6.4: Map of the pictograph sites that have deep holes in 2001

The map (figure 6.4) indicates the physicallocation of sites with this feature using the letter

"H" beside the Borden number. Both sites are in the eastern portion of the Lake of the

Woods.

(ii)Large cracks:

The second prerequisite is the "crack". Twenty-three of the twenty five sites had

large cracks (xq132). The distribution of these sites in the Lake of the Woods is indicated in

figure 6.5 by the letter "C" beside the Borden number. DgKl-l and DhKm-19 have small

cracks (xq132). Large cracks affected paintings at sixteen of the pictograph sites: DgKl-2,

DgKl-17, DgI<J-19, DhKm-1, DhKm-3, DhKm-5, DhKm-20, DiKp-1, DgKm-2, DiKm-3,

DgKm-1, DhKo-1, DiKq-10, DjKr-23, DiKm-51, and DiKn-1 (xq 144 and xq215).

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~

? 'P 2~ Km. -1~ DkKn7 c

Big TnYCrRe Day

Figure 6.5: Map of pictograph sites with large cracks in 2001

(iii) Crevices:

Archaeologists previously argued that crevices are particularly important. DhKm-1 's

large crevice, or cleft as it was sometimes called, was named the "Devil's Hole" by Dewdney

(Dewdney and Kidd 1962: 51; Dewdney and Kidd 1967: 53) and he described it as "a deep,

almost horizontal fissure, averaging five inch es in width." Fox (1974: 3) described the same

feature as a cleft stuffed with bundles of clothing. In 2001, l found it packed with the vast

quantities of offerings described in Chapter V.

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Figure 6.6: Map of pictograph sites with crevices in 2001

However, six sites on cliffs: DgI<J-l, DhKm-20, DkKn-6, DiKm-3, DhKm-4, and DiKq-l0

do not have large crevices (xq230 and xq131). The map in figure 6.6 uses the letters "CR to

illustrate the location of the nineteen sites with crevices. This group includes Dgl<J-2, DgI<J-

17, DgI<J-19, DhKm-l, DhKm-3, DhKm-S, DhKm-18, DhKn-l, DiKp-l, DgKm-2,

DgKm-l, DhKm-19, DhKo-l, DiKm-4, DjKn-l, DjKr-23, DkKn-7, DiI<m-Sl, and DiKn-l

(xq230 and xq131). Crevices run through the area of the rock which is painted at seven of

these sites: DhI<m-l, DhKm-3, DhKm-18, DhKn-l, DhKo-l, DjKr-23, and DiKn-l (xq230

and xq131).

(iv) Rock overhangs:

Previous research also presumed rock overhangs to be associated with images

occurring at cliff faces. Fourteen of the twenty-five cliff sites had rock overhangs: DgI<J-l,

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DgKl-2, DgKl-17, DgKl-19, DhKm-l, DhKm-3, DhKm-5, DhKm-18, DhKm-20, DhKn-l,

DiKp-l, DkKn-6, DgKm-2, and DiKm-3 (xq234 and xq213).

Figure 6.7: Map ofpictograph sites with overhangs in 2001

Eleven pictograph sites lack rock overhangs: DgKm-l, DhKm-4, DhI<m-19, DiKm-4,

DiKq-l0, DjKn-l, DjKr-23, DkKn-7, DiI<m-51, DhKo-l, and DiKn-l (xq234 and xq213).

Figure 6.7 indicates the physicallocation of sites with overhangs using the letter "0" beside

the Borden number. Sites with this physical feature are predominantly on the eastern portion

of the Iake.

Overhangs above images couid affect their preservation. However, 1 found little

correlation between the presence of rock overhangs and the number of images especially

blobs (see Appendix 12). The rock overhangs were above the paintings at eight of the

fourteen sites: DgKl-l, DgKl-17, DgKl-19, DgI<m-l, DhI<m-3, DhI<m-5, DhI<m-18, and

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DhKm-20. Paintings occurred both on and above rock overhangs at DgKl-2 and DgKm-2.

Images were found on and below overhangs at DiKp-1, ab ove and adjacent to the overhang,

at DhKm-1 and on the overhangs at DiKm-3 and DhKn-1.

(v) Rock shelves, benches, and ledges:

One physical feature, the rock shelf, bench, or ledge juts out horizontally either at or

near the base of the painted vertical area of the rock surface. No rock ledge graced four of

the sites: DhKm-20, DiKp-1, DiKm-3, and DiKm-4 (xq147 and xq146). The remaining

twenty-one had this feature: DgKI-1, DgKl-2, DgKl-17, DgKl-19, DhKm-1, DhKm-3,

DhKm-4, DhKm-S, DhKm-18, DhKn-1, DKkn-6, DgKm-2, DgKm-1, DhKm-19, DhKo-

1, DiKq-10, DjKn-1, DjKr-23, DkKn-7, DiKm-S1, and DiKn-1 (xq147 and xq146).

This feature varies in size. Sometimes shelves are large enough to stand on, su ch as

that at DhKm-19, or merely to hold onto, as is the case of those at DkKn-6, DkKn-7, and

DgKI-17. However, those at DhKm-3, DiI<m-S1, and DjKn-1 were large enough to sit on,

while the benches at DgKl-2 and DhI<m-3 were large enough for people to walk on and to

examine the images (xq147 and xq146). The map (figure 6.8) below, illustrates the location of

Lake of the Woods sites with this feature with the "S" beside them. No pattern registers

regarding their occurrence in this region.

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Figure 6.8: Map ofpictograph sites with rock shelves, or benches or ledges in 2001

Conclusion:

Only one cliff pictograph site, DgKI-2, contained ail the physical features that

previous archaeologists such as Rajnovich (1994: 11) and Rusak (1992a: 23) considered

prerequisites. Only DgKI-2 and DkKn-6 had the feature cailed a hole. The information in

Appendices 12 and 13 demonstrates that not ail the sites had ail the features. The

dendrograms in Appendix 16 confirm this weak relationship. Nine sites had four of the five

"required" prerequisites: DgKI-19, DgI<J-17, DhKm-l, DhKm-3, DhKm-5, DhKm-18,

DhKn-l, DkKn-6, and DgKm-2. Eight sites had three of the five required physical features:

DgKm-l, DhKo-l, DjKn-l, DjKr-23, DkKn-7, DiKm-51, DiKn-l, and DiKm-4. Seven

sites had oruy two of the five required prerequisites: DiKm-3, DhKm-20, DiKq-l0, DiKp-l,

DgI<J-l, DhKm-4, and DhKm-19.

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The information regarding the presence of offerings at sites in 2001 was compared

with the number of physical features present at a site to determine if the number of the

physical features related to ritual activities, indicated by the presence of offerings. If the

information in Appendix 14 is compared with that on offerings in Appendix 11 this indicates

that a site with ail the "required" five physical features very likely acquired offerings. DgKl-2,

as discussed ab ove, was the only site that had ail five required physical features and objects

cailed offerings in 2001. Only two sites that had two of the five required physical attributes

had offerings in 2001. The information in Appendix 14 indicates that only three of the nine

sites that had four of the five required physical attributes had offerings in 2001. Only four of

the eight sites that had three of the five required physical attributes had offerings in 2001. It

can be posited that, as the number of required physical features decreases, sites are less likely

to have offerings (see Appendix 14).

(g) Possible correlations between the five prerequisites and rocks at base of sites:

None of the archaeologists other than Rusak (1992a, 1992b) have coilected

information regarding the presence of rocks at the base of pictograph sites. For sorne

unknown reason Rusak (1992a) coilected this information for ail of the sites surveyed for the

White Otter Lake Pictograph Project in 1991. She did not state why she recorded this

information. l coilected the same to determine the reason behind her decision. Seventeen of

the twenty-five pictograph sites on cliffs had rocks at their base: DgKl-2, DgKl-19, DhKm-3,

DhKm-S, DhKm-18, DhKm-20, DhKn-l, DiKp-l, DkKn-6, DiKm-3, DgKm-l, DiKm-4,

DjKn-l, DjKr-23, DkKn-7, DiKm-Sl, and DiKn-l (xq240 and xq237).

Rocks are not found at the base of eight pictograph sites that occur on cliff faces:

DgKl-l, DgKl-17, DhKm-l, DgKm-2, DhKm-4, DhKm-19, DhKo-l, and DiKq-l0 (xq237

and xq240). Large rocks were found partiaily above the water level at DhKm-3, DjKn-l,

DhKm-18, DjKr-23, DhKm-20, DiKm-4, and DiKm-3 (xq237). Sorne were large enough for

an adult stand on, ailowing closer examination of images at DiKm-4, DiKm-3, and DhI<m-

20. Red, blue, and white paint drops were on the surface of the large granite rocks

immediately in front of DhKm-20 (xq237). DgKI-19, DgI<m-l, DhKm-S, DiI<m-Sl, and

DjKr-23 had mostly submerged rocks. At DgKl-2, DiKp-l, and DkKn-6 rocks were below

the water level.

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Figure 6.9: Map ofpictograph sites with rocks at their base in 2001

A geographical pattern is not evident in figure 6.9, a map depicting the seventeen

pictograph sites on cliffs and the two sites inside caves that had rocks at their base.

This information was compared with the presence of the five physical features

recorded in Appendix 15. DgI<J-2 has rocks at its base. Two thirds of the sites that had four

of the five required physical features also have rocks at their base. Ail of the sites except for

DhKo-1 which had three of the five required physical features also had rocks at their base.

However, only three of the seven sites that had rocks at their base had two of the five

required physical features. Although it is unclear why Rusak (1992a) recorded the presence of

rocks at sites, a correlation exists between the presence of the five physical features and rocks

at the base of the cliffs at each site (see Appendix 15).

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Caves:

Both caves found in the Lake of the Woods contradict the commonly held beliefs

regarding the physical location of pictograph sites. Images were painted on the ceilings of

each cave. The cave sites also have some of the same physical features as cliff sites: crevices,

cracks, and rock shelves, overhangs but no holes. Neither cave is a hole. The range and

nature of the vegetation was determined for inside each cave and the rocks found on the

floor of each cave were recorded. Each cave possessed two different entrancesj exits.

Both sites were close to the water. The pictograph site DiKm-49, was behind DiKm-

3, and the images were visible and recorded from a boat. Water covered the floor of DiKm-

49 but at lower water levels during the beginning of the twentieth century, the floor may

have been dry (xq207 and xq134). One entrancej exit to DiKm-50, on the shoreline of

Horseshoe Island, opened at the waterline in 2001.

Figure 6.10: DiKm- 50 on Horseshoe Island, Whitefish Bay

The photograph in figure 6.10 was taken looking downward through DiKm-50 towards the

water's edge. The black marks on the side of rocks in the base of the cave in figure 6.11

below indicate that water entered the cave and stayed for a period of time there. In 2001,

water lay at the base of the cave's mouth.

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Figure 6.11: The black marks on the rock's surface.

Rock at the base of the caves:

Large rocks were not found at the bottom of DiKm-49 and DiKm-50 but rock

chips, sand, and gravel were found on the floor of DiKm-49 (xq 238 and xq239). Rocks were

found inside the cave, DiKm-50, along the edge where the sides meet the overhang and rock

chips, fine gravel and sand layon the floor of the cave.

Vegetation:

DiKm-49 and DiKm-50 did not have any vegetation on their floors. The range of

plants found was smaller inside caves. DiKm-49 had mosses, rock tripe, and lichen growing

on its walls, while DiKm-50 did not have any plants on its surface (xq135 and xq211). This

was possibly because water frequendy entered and washed through the cave. The water level

was very close to the entrancej exit, hence, the surface of the rock was devoid of any type of

plant life (xq135 and xq211). DiKm-49 had lichen on its ceiling, while the ceiling of DiKm-

50 was completely bare (xq136).

Cracks:

Both caves have cracks. DiKm-49 existed because of two vertical cracks in the

granite, causing a wide crevice to occur, while the two diagonal cracks in the ceiling created a

"tunnel" which mns from the cave, outside to the top of the cliff ab ove DiKm-3 (xq218).

DiKm-50 did not have any large cracks since it is an erratic, or large boulder, perched on the

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bedrock beside the shoreline. Fine cracks were found through the paintings on the ceiling of

DiKm-50 and smaIl cracks existed beside the paintings in DiKm-49 (xq228, xq214, xq226.

xq216, and xq225).

Crevices:

Crevices are apparent in the interior of DiKm-50 along the edges where the sides

meet the overhang caused by the erratic which constituted the ceiling. The ceiling sat

perched on large rocks that rest directly on the bedrock. The bedrock formed the back and

sides of the cave since it sloped down towards the base in a wide 'V' shape with little ridges

in the floor. The floor graduaIly sloped upwards towards the back and the roof of the cave

(xq220 and xq143).

Rock shelves or benches:

Rock shelves were only found at one of the entrances to DiKm-50 (xq148 and

xq149).

Since only two sites are found inside caves in this region it is very difficult to do

mu ch other than compare one with the other.

Summary for Section 1:

Significant correlations cannot be established between the geology and

geomorphology of these sites, even though Chapter V established that granite was the rock

of choice for the people who created the pictograph sites. Likewise there is little correlation

between the geomorphology, geology and the type of landmass of each site, between the

main tracks, thoroughfares, and the physical location of the pictograph sites in the Lake of

the Woods, or between the physical proximity of the pictograph sites to lndian reserves and

the presence of offerings recorded, either in the past by previous archaeologists, or in 2001.

Approximately one third of the sites are located on islands. There was little correlation

between the orientation of a site, the land mass where it occurs, and the presence of

offerings in 2001. Archaeologists have maintained that deep holes, large cracks, large

crevices, rock overhangs, and rock benches or ledges were "crucial" to the presence of

paintings on cliff faces. However, only one site, DgKl-2 encompassed ail these features and

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frequently pictograph sites were found with only two of the five required physical features.

As the number of required physical features decreased at a cliff pictograph site, offerings

were Jess likely to be found in 2001 (see Appendix 16). A weak correlation exists between the

presence of these five physical features and rocks present at the base of the cliffs. Caves had

a different physical structure, although they shared sorne similar physical features with sites

on cliff faces. Cave sites had crevices, cracks, rock shelves, overhangs, but not holes. DiKm-

50 is the gap between the erratic, or large boulder, that lies perched on the bedrock beside

the shoreline. DiKm-49 exists because of a large space caused by a vertical crevasse which is

parallel to and behind the edge of the cliff where DiKm-3 exists. Its roof is a pile of rocks

precariously balanced on top of the large gap. This initial comparison provides the

groundwork for the examination of sites inside caves. Pictographs in caves should be

considered rare. Another pictograph site, DcJh-45, was found in a cave in Confederation

Park in downtown Thunder Bay in 2001 (Bell pers. comm. 2001). It had a similar physical

structure to those found and recorded in 2001 in the Lake of the Woods. DcJh-45 occurs

within a series of granite cliffs bordering a dry riverbed (Ross pers. comm. October 2001).

Hopefully, future fieldwork will provide more examples elsewhere in the Canadian Shield.

Section 2:

This section deals with the relationship between images and rock surfaces. The

images will be considered as a group rather than as individu al entities. Caves had only

straight lines and smears; cliff faces had other images, but the physical difference between

sites in caves and on cliff faces will not be considered in this section. This is because it is

important to see whether the site's physical structure could influence the number of images

present.

Only one archaeologist had considered the relationship of images to their physical

surroundings on the rock's surface. Rusak (1992b: 124) observed that smears occurred at all

but two of the pictograph sites that were recorded in 1991 in White Otter Lake (see Chapter

III, page 169), but the correlation is weaker for the sites of the Lake of the Woods since

eighteen smears exist at eleven of the twenty-seven sites: DgI<J-17, DgKl-19, DgI<J-2,

DgKm-1, DgKm-2, DhKm-1, DhKm-5, DhKn-1, DhKo-1, DiKm-50, and DiKn-1 (xq326).

DgKl-17, DgKm-1, DhKm-1, DhKn-1, DhKo-1, and DiKm-3 have more than one image

that was identified as a smear.

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(a) Number of images at sites and the geographicallocation of the site.

A site had on average eleven images, as concluded from Chapter V. But no

geographical pattern emerged for the number of images per site. Figure 5.13 indicates that

DhKm-3 and DhKm-5, each having more than thirty images, were situated in Whitefish Bay

in eastern Lake of the Woods. DiKm-3, DhKo-l, and DjKn-l, which had between twenty

and twenty-nine images, were located in different parts of the region. Of the six sites having

between ten and nineteen images, DiKn-l and DhKm-l also were found in Whitefish Bay.

Yet, DiKn-l was located in the northern, and DhKm-l in the southern part of Whitefish

Bay. The remaining sites in this group are found in different parts of the region. Sites that

have fewer than ten images were predominately in Whitefish Bay: DiKm.-4, DhKm.-18,

DiIZm-51, DhIZm-20, DiIZm-49, and DiIZm-50. DgKl-2, DgKl-l, DgIZm-l, DgIZm-2, and

DgKl-19 in Sabaskong Bay, to the south and east of Whitefish Bay, had fewer than ten

images. One site, DhIZm-19, had less than ten images and was in Turtle Lake, which lies

between Whitefish Bay and Sabaskong Bay. The remaining two sites with fewer than ten

images, DkKn-6 and DkKn-7, are in Blindfold Lake, which is connected to Lake of the

Woods. Unlike the other site in the western portion of the Lake of the Woods, DjKr-23

possessed fewer than ten images.

(b) Number of images present and the number of the physical features present at cliff

sites.

It is clear that a weak link occurs between the number of images present at a site and

the number of physical features previous archaeologists argued were required to be present

(see Appendices 5, 6, 10). For instance, DgKl-2, although it had ail the "required" features,

had fewer than ten images. On the other hand, DhIZm-3 and DhKm.-5, each with more than

thirty images, had only four of the five physical features. DiKm.-3, DhKo-l, and DjKn-l had

between twenty and twenty-nine images, but DhKo-l and DjKn-l had only three of the five

features while DiKm-3 had only two. Six sites had between twenty and twenty-nine images.

Of those, DhKn-l, DgKl-17, and DhIZm-l had four of the five required physical features,

while DiKn-l had only three. DiKp-l and DiKq-l0 only had two of the five physical

features. DhIZm-18, DhIZm-19, DkKn-6, and DgIZm-2 had four of the five physical features

but they had less than ten images. DgIZm-l, DiKm.-51, DiIZm-4, DkKn-7, and DjKr-23,

which had three of the five "required" physical features, had less than ten images. DgKl-l,

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DhKm-4, DhKm-20 and DhKm-19 also had fewer than ten images per site but they had

only two of the five physical features.

(c) Number ofimages and presence of offerings in 2001.

Likewise, there is no clear correlation between the number of images and offerings.

Only DhKm-3 and DhKm-S, which had more than thirty images, also had offerings above

the water level. DhKo-1 was the only site of the three with between twenty and twenty-nine

images that had offerings that were ab ove the water level. Four of the six sites with between

ten and nineteen images had offerings in 2001: DhKn-1, DiKn-1, DgKI-17, and DhKm-1.

Offerings were also found below water level at DhKm-1 and DgKl-17. Five of the sixteen

sites that had fewer than ten images had offerings in 2001: DgKI-2, DiKm-4, DgKI-1,

DhKm-20, and DjKr-23.

(d) Number ofimages at sites and the number of diffs used.

l looked for a connection between the number of sites and number of cliff faces with

images at each site. But the results indicate no relationship. Only one cliff face was found to

have images at each site except at DhKn-1 and DiKn-l. DhKn-1 and DiKn-1 each had

between ten and nineteen images on two cliffs. DjKn-1 had between twenty and twenty-one

images on three cliffs.

Summary for Section 2:

The geographical location of the site bore no influence on the number of images

present at a site. The number of images is independent of a site's physical characteristics. The

number of images is not related to the presence of offerings in 2001. No relationship

occurred between the number of images and the number of cliff faces used at each site.

Images were painted on the ceilings of both caves.

Section 3:

This section examines the various sorts of images at different sites, and whether any

relationships exist between them. Although previous archaeologists observed that specific

images occurred at sites (discussed in Chapter III), the vocabulary used affected the

discussion of these images. Conway (1978) had posited that pairs of canine morphs occurred

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r--..

with an open-armed morph, which he identified as Orion and Canis Major. He did not

provide any guidelines for identifying these images.

Lambert's (n.d.) conclusions regarding the distribution of images in the Lake of the

Woods, Bloodvein and the Winnipeg River area depend on his classification of images,

which involved suppositions of meaning in the description of the images. It is impossible to

establish whether the "canoes and anthropomorphs" he had identified at DhKm-4, DhKm-

1, DhKm-18, DhKm-5, DkKn-7, DkKn-6 and DjKn-1 were more prevalent than images he

called 'creatures.' He argued that there was a higher incidence of "canoes and

anthropomorphs" in the Winnipeg River region, which includes Lake of the Woods, than in

the Bloodvein region, where shapes he called 'creatures' were more prevalent. Lambert's

(n.d.) classification system is subjective and based on definitions of words from Webster's

International Dictionary. It is very difficult to establish what the shapes that Lambert called a

"canoe" looked like. They might be what l would call a horizontal crescent with points

facing upwards. Perhaps the image that Lambert termed as an "anthropomorph" is what l

would loosely categorise as a stick figure. Unfortunately, he did not provide any additional

information regarding details that could be crucial to the individu al nature of these images.

Rajnovich (1980b: 35) maintained that a "canoe" shape often occurred with another

"canoe" having a slightly different shape, which she attributed to the differences in each

"canoe's" occupants. It is likely that she interpreted the shape called a crescent as a canoe but

this is only speculation on my part. Pastershank and Rajnovich observed that pairs of images

frequently occurred at sites (pastershank 1989; Rajnovich 1980b, 1980d). This is an

interesting observation but previous archaeologists' description of shapes depended on their

own systems of classification, and, inadvertently, meaning was ascribed to these shapes,

lmages.

The combination of shapes considered in this section follows the order in which

section 3 of Chapter V discussed the more generally categorised shapes. A nested hierarchy

of types leaves the most options open with respect to classification. The geographical

distribution of each image will also be noted so as to establish any presence of specific image

concentrations.

Each shape will be analysed according to the sequence described in Chapter V. Each

shape was grouped in Chapter V according to loosely defined groups of the same type so in

this chapter they will be referred to as 'birds', or 'creatures', 'zig-zags', and soon. Each shape

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will also be examined as to its geographical distribution within the Lake of the Woods. Each

shape wiU be examined to establish whether shapes occurred with similar others at the same

site or combined with different images, as Conway (1978) had argued. But it is possible for

shapes also to occur alone, as Rajnovich (1980b: 34) had speculated. The presence of the sole

shape of a turtle at D hIZm -19 confirmed her speculation.

(a) Smears

Eighteen different types of smears occur at eleven pictograph sites, including DgKl-

17, DgKl-19, DgKI-1, DgKl-2, DgIZm-1, DhIZm-1, DhIZm-5, DhKn-1, DhI<o-1, DiIZm-50,

and DiKn-1 (xq326) (Appendix 10). If sites with smears were compared to those with blobs

only DgKl-17, DgKI-19 and DiIZm-50, or 27.27% of this group, had smears but not blobs.

Smears differ from blobs in that they are larger. It is likely that they were placed on the rock

intentionaUy, whereas blobs are more probably a result of taphonomic processes. The line in

figure 6.12 connects aU the sites that have smears and shows that smears existed at sites in

the southern and the southeastern portion of the lake.

Figure 6.12: Sites with smears.

Smears did not always occur with shapes loosely categorised as creatures, because

'creatures' only occurred at six of the ten sites which had smears (xq382). Smears also did not

always occur at sites with shapes loosely categorised as 'crescents' (xq348), as 'zig-zags'

(xq321), or 'stick figures' (xq 382b). It is clear that a weak correlation exists between the sites

and the shape loosely categorised as a 'smear'. This weak link between the images and the

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r~----

sites is confirmed by the dendrograms obtained using the Euclidean distance method (Table

6.3) and the Pearson correlation method (Table 6.4).

Rescaled Distance C1uster Combine CAS E o 5 10 15 20 25

Label Mum +---------+---------+---------+---------+---------+ DgKm-2 18 -DiKm-50 19 -DgKl-19 5 -DhY..n-l 10 DgKm-2 17 -DgKm-l 6 -DhKo-l 15 -DhKo-1 16 -DgKl-2 2 -DiKm-3 13 -DiKm-3 14 -

DhKn-1 11 -DiKn-l 12 -DhKm-1 8 -DhKm-5 9 -DgKl-17 4

DhKm-1 7 -DgKl-17 3 -

Table 6.3: Hierarchical Cluster Analysis - Dendrogram using Average Linkage (Between Groups) using Euc1idean distance method to de termine the nature of the relationship between smears and sites

CAS E Label

DhKo-1 DhKo-l DgKl-2 DiKm-3 DiKm-3 DgKl-17 DhKm-1 DhKn-l DiKn-l DgKl-17 DhKm-l DhKm-5 DgKm-2 DiKm-50 DgKm-2 DhKn-l DgKl-19 DgKm-1

Rescaled Distance Cluster Combine o 5 10 15 20 25

Mum +---------+---------+---------+---------+---------+ 15 16

2

13 14

4

7

11

12 3

8

9

18

19 17 10

5 6

--

---

-

-----

Table 6.4: Hierarchical Cluster Analysis - Dendrogram using Average Linkage (Between Groups) using the Pearson correlation to de termine the nature of the relationship between smears and sites

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(b) Blobs

Blobs are caused by taphonomic processes and reflect the passage of cime. The tine

in figure 6.13 connects ail the sites that have blobs. This map also indicates that the majority

of the sites had blobs and that there were relacively few sites that did not have blobs. It is

important to remember that blobs are the decayed remains of shapes that once had clearly

defined edges.

Figure 6.13: Sites with blobs

Twenty of the twenty-seven sites had blobs: DgKl-2, DgKl-l, DgI<l-19, DgKm-l,

DgKm-2, DhKm-18, DiKq-l0, DhKm-3, DhKm-5, DhKn-l, DhKo-l, DiKm-3, DiKm-51,

DiKn-l, DjKr-23, DiKp-l, DkKn-6, DkKn-7, DjKn-l and DhKm-l (xq 349). There are

seventy-three different types of 'blobs' (xq349). Ail of them are different from each other

(see Appendix 16). Eight additional types of blobs did not occur on their own because they

were connected either to another blob or to a short tine (see Appendix 16). Hence three­

quarters of the sites had at least one blob. Seven sites, or one quarter, did not have blobs:

DgI<l-17, DhKm-4, DiKm-4, DhKm-19, DhKm-20, and DiKm-49 (xq 349). It is clear from

the map above that sites throughout the Lake of the Woods have blobs. Nine sites had blobs

and smears: DgI<l-2, DgKm-2, DgKm-l, DhKm-l, DhKm-3, DhKm-5, DhKn-l, DhKo-l,

and DiI<n-1. Ten sites had only blobs and not smears: DgKl-l, DhKm-18, DiKm-3, DiKm-

51, DiKp-l, DiKq-l0, DjI<n-l, DjKr-23, DkI<n-6, and DkI<n-7. Blobs are the most

common type of shape in this dataset. Eight sites which had one or more shapes loosely

categorised as 'creatures' (xq382) also had blobs. These sites were DgI<l-l, DhKm-3, DhI<n-

1, DhKo-l, DiKm-3, DiI<tD-51, DiKp-l, and DjI<n-1. Eight sites that had shapes loosely

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classified as 'stick figure' shape also had blobs (xq382b): DgKm-1, DhKm-18, DhKm-3,

DhKn-1, DhKo-1, DiKm-3, DiKn-1, DjKn-1, and DhKm-l. The shapes loosely classified as

'zig-zags' occurred with the shapes cailed blobs at four sites: DhKm-3, DiKm-3, DiKp-1,

DhKm-1 (xq321). Shapes loosely categorised as 'crescents' occurred with blobs at ten sites:

DgKl-1, DgKl-2, DhKm-3, DhKm-5, DiKm-3, DiKm-51, DiKn-1, DiKp-1, DjKn-1 and

DhKm-1 (xq348). Blobs also occurred at the sites where the left and right hand print shapes

occurred: DiKm-3, DjKn-1, DhKm-5, and DgKl-19 (xq328, xq328a, xq326b). It is clear that

a weak link exists between the blobs and the sites and this is confirmed by the dendrograms

in Appendix 16.

(c) Unidentifiable shapes

This shape is similar to blobs in that their physical shape is affected by taphonomic

processes if they were created using ochre based paint. A blob created in ochre paint usuaily

is either oval, rectangular, or round and suffers from deterioration caused possibly by the

accumulation of white mineraI deposits, weathering and erosion of the rock surface.

However, one of these images was painted using modern spray paint which was very faint

and hence the edges of the image were not clearly defined and it was difficult to describe or

identify parts of the shape. Five types of shape were found at: DgKl-2, DhKm-18, DiKp-1,

and DiKq-l0 (xq744), while one area at DgKl-19 contains pairs ofverticallines and spots of

smail concentrations of ochre (xq745). These shapes were found in conjunction with blobs at

DgI<J-2, DiKq-10, and DiKp-1 (xq349), and with a smear at DgI<J-2 (xq326). The area that

contains pairs of vertical lines of spots and smail concentrations of ochre at DgI<J-19

occurred in conjunction with a smear. The line in the map figure 6.14 connects ail the sites

that have unidentifiable shapes and demonstrates the geographical distribution of these

images. Sites in the northwest and the southeast portion of the lake had these images.

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Do,

Figure 6: 14: Sites with uniclentifiable shapes

(cl) 'Stick figures'

Twenty-one types of shape cailed 'stick figure' (xq358a, xq382b) exist. Several

different physical types occurred since fifteen of these shapes were different types of vertical

stick figures (xq382a), two diagonal stick figures (xq382b), and two cailed 'upper torso of

vertical stick figure' (xq358a) (for examples see Appendix 7). Some of the stick figures are

not physicaily the same shape (see absence and presence table in Appendix 16). The shape

cailed 'upper torso of vertical stick figure' will be discussed in the next section. The stick

figures were identified at nine pictograph sites: DgKm-l, DhKm-l, DhKm-18, DhKo-l,

DiKm-3, DhI<:m-3, DiI<:m-4, DiKp-l, and DjKn-l (xq382b). These sites had on average two

stick figures per site.

The vertical stick figures were at DhKn-l, DgI<:m-l, DhKm-l, DhI<:m-3, DiKn-l,

DhKo-l, DiI<:m-4, DiKp-l, and DjI<n-l (xq382a) in the map in figure 6.15. Figure 6.15

indicates that vertical stick figures occurred at sites in the eastern, northeastern and southern

portions of the lake. Only DiI<:m-3, in Whitefish Bay in the eastern potion of the region, had

shapes classified as diagonal stick figures. The line in figure 6.15 connects ail the sites that

have a shape cailed a vertical stick figure regardless of its various physical attributes.

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Figure 6.15: Sites with vertical stick figures.

Diagonal stick figures are only found with vertical stick figures at DiKm-3 (xq382b).

None of the vertical stick figures resemble each other at DhKo-1 and one occurred inside a

rectangle, in figure 5.18, while another was inside a shape identified as a square (xq382b).

The combination of a stick figure inside another shape does not show up elsewhere in the

Lake of the Woods. Three of the vertical stick figures at DhKm-3 and DjKn-1 are unique.

Both of the vertical stick figures at DjKn-1 had hollow centres, as did the stick figure at

DiKm-4. One of the vertical stick figures at DhKo-1 had a hollow body similar to an

isosceles triangle, while the second vertical stick figure at this site had a hollow rectangular

body. One of the vertical figures at DhKm-3 also had a hollow rectangular body but the stick

figure that also had a rectangular body at DhKo-1 is different. The dendrograms in

Appendix 16 indicate that a weak relationship exists between the stick figures and the sites.

(e) 'Upper torso of vertical stick figure'

Two shapes of the 'upper torso of vertical stick figure' were found at DiKn-1 and

DgKm-1 (xq382b) (see Appendix 7). This shape is found with blobs (xq349) at both sites,

although the shape called 'upper torso of vertical stick figure' appears at DgKm-1 with three

vertical stick figures. As shown in figure 6.16 below, DiKn-1 is in the northern part of

Whitefish Bay while DgKm-1 is in Sabaskong Bay in the southeastern portion of the Lake of

the Woods.

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Figure 6.16: Sites that had the shape of the 'upper torso of a vertical stick figure'

(f) Hand print

Twenty-six hand prints (xq328, xq328a, xq328b, xq333) were recorded at DgKl-2,

DhKm-3, DgKl-19, DhKm-5, DiKm-3, and DjKn-1 (xq328, xq328a and xq328b), for an

average of 4.3 shapes of hand prints per site at which they occurred. Hand prints were also

present at sites in the eastern, southeastern, and northeastern portion of the lake (figure

6.17). The line in figure 6.17 indicates that these sites existed in the eastern portion of the

reglOn.

Figure 6.17: Sites that had the shape ofhand prints.

It was difficult to identify right or the left hands in instances where only four digits

were clearly visible and the thumb was frequently missing. Eleven are right 'hand print'

shapes (xq328b) and seven are left 'hand print' shapes (xq328b) (see the absence and

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presence table for hand prints in Appendix 16). The seven left hand print shapes were

identified at DgKl-19, DjKn-1, DhKm-5, and DiKm-3 (xq328, xq328a, and xq328b). Eleven

right hand print shapes were identified at DgKl-19, DjKn-l, DhKm-S, DhKm-3, and DiKm-

3. Both right and left hand print shapes occurred at DiKm-3, DjKn-1, DhKm-5, and DgKl-

19 (xq328, xq328a, and xq326b). The map in figure 6.18 charts their geographical location

and the line indicates that the sites occur in the eastern, southeastern, and northeastern

portions of the lake. However, a weak relationship exists between the hand prints and these

sites (see Appendix 16).

Figure 6.18: Location of sites that had both a left and a right hand print shape.

It is also possible that, if right hand print shapes existed, a left hand print shape was

originaily present. Shapes loosely categorised as 'crescents' (xq348) did not occur with right

and le ft hand print shapes. Shapes loosely categorised as 'zig-zags' did not occur at the same

sites as left and right hand print shapes (xq321). Shapes of the right hand print and the left

hand did not always occur with shapes loosely termed as 'creatures' once the detailed

descriptions of these shapes are considered (xq382).

(g) 'Zig-zags'

Eight types of shape loosely categorised as 'zig-zags' occur at DiKp-1, DiKm-4,

DiKm-3, DhKm-3, and DhKm-1 (xq 321). The term 'zig-zag' is misleading since it implies

that the shapes are exactly the same as indicated by the data in the presence - absence table

in Appendix 16). Although ail of these shapes are found in Whitefish Bay in the eastern

portion of Lake of the Woods, none of these shapes was identical (see Appendix 16). A

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horizontal zig-zag was at DiKp-l, two diagonal zig-zags at DiKm-3 and DhKm-3, five

vertical zig-zags at DhKm-l, DiKm-3, and DiKm-4. DhKm-3 and DiKm-3 had two zig­

zags, one vertical and one diagonal. None were identical, since a few of them had horns or

ears, and heads. Three zig-zags, at DhKm-3, DiI<::m-3, and DiI<::m-4 (xq365), had forked

ends, but the 'zig-zags' at DiI<::m-3 and DiI<::m-4 were vertical, while the zig-zag at DhI<::m-3

was diagonal with a forked end that consisted of three short lines. The two vertical zig-zags

at DiI<::m-3 and DiI<::m-4 differed in that the zig-zag at DiI<::m-3 had a head with horns or ears

(xq365). The information in appendix 10 reveals that none of these shapes is the same. 'Stick

figures' (xq323) were also evident at the same sites. 'Zig-zags' are not found with hand print

combinations, hand print shapes (xq328, xq328a and xq328b), or 'crescents' (xq348).

(h) 'Creatures'

The group loosely categorised as 'creatures' has the most variety of types in this

dataset. However, ail of them are different (see Appendices 6, and 16). Twenty-three shapes

identified as 'creatures' were examined at ten sites: DjKn-l, DiKp-l, DiKm-3, DhKo-l,

DhKn-l, DhI<::m-5, DhI<::m-3, DgKI-l, DgKI-2, and DgKl-17 (xq382, xq752, xq755, xq754,

and xq753). Each 'creature' bearing site had approximately two such shapes. The map below

indicates that these images existed at sites in the southern, eastern, and northwestern parts of

the lake (figure 6.19). The line connects these sites.

Figure 6.19: Sites with creatures

Eight, or one third, of these shapes faced right, while thirteen, or half, of the

'creatures' faced le ft (xq382). The creatures that faced left were at DgKI-l, DgKl-17,

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DhKm-S, DhKo-1, DiKp-1, DjKll-1 and DhKll-1, while those that faced right were at

DiKm-3, DgKl-1, DgI<1-2, DhKm-3, DhKo-1, DjKn-1, and DhKn-1. Three shapes of

creatures faced neither 1eft nor right at DhKm-3, DiKm-3, and DhKo-1. The sites that have

creatures facing right together with creatures facing left (DgKl-1, DhKo-1, DjKll-1, and

DhIZn-1) are located east, northeast and south of the Aulneau Peninsula. Seven had hollow

centres, at DhI<m-3, DhKo-1, DjK-1, and DgK1-17. Three of the four 'creatures' at DhKo-1

were hollow; two faced left and two faced right. DhI<m-3 had two 'creatures.' One was

vertical, hollow, and faced neither 1eft nor right, while the other had a solid centre and faced

right. The creature shapes at DjIZn-1 were hollow but two of them faced right while the

other faced left. The sole hollow creature at DgI<l-17 faced left. Creatures often had horns or

ears. Nine sites located throughout the lake contained such images: DgI<l-l, DgI<l-17,

DhI<m-3, DhI<m-S, DhIZn-1, DhKo-1, DiI<m-3, DiKp-1, and DjIZn-1 (xq382), DjKr-23

and DiKq-10 in the northwestern portion of the lake were devoid of such examples. The

dendrograms in Appendix 16 indicate that a weak correlation exists between the shape called

'creatures' and the pictograph sites. 'Creature' shapes do not always exist with stick figures

(xq382), with hand print shapes (xq328, xq328b, and xq328a), or with crescents (xq348).

(i) 'Crescents'

These shapes possibly have been called 'canoes' by previous archaeologists. Thirteen

different shapes were categorised as 'crescent' at DgI<l-l, DgI<l-2, DhKm-S, DiKm-3,

DiI<m-S1, DiIZn-1, and DjIZn-l (xq348). These sites are in the eastern part of the Lake of

the Woods. These shapes had solid centres, but several different types of crescents were

identified (xq 348) (see Appendix 16 and figure 1.1). Occasionally, sorne of the shapes

loosely categorised as cres cents occurred on their own. Sometimes they occurred together.

Bach combination of images was unique. Six 'horizontal crescent with points facing upwards

with verticallines attached to topside' were found (xq332, xq348, and xq 350). Three of these

crescent shapes had the same shape; two existed at DgI<l-l and one existed at DiIZn-1 (see

Appendix 16 and figure 1.1). Ail three could be described as a horizontal crescent with points

facing upwards with three short verticallines attached to the topside of the crescent (xq348).

DgI<l-2 was in Sabaskong Bay and DiIZn-l in the northern part of the Whitefish Bay. Both

were located in the eastern and southern portion of the region. DhI<m-S and DiI<m-S1 each

had a horizontal crescent with points that faced downwards (xq348a and xq348). Both of

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these sites were ln Whitefish Bay. There are two 'horizontal crescent, points facing

downwards with verticallines on bottom side' (xq 350 and xq348) at DjKn-1. The images

were not identical, since one of the shapes had three short verticallines, the other, four short

vertical lines attached to the underside of the horizontal crescent. The dendrograms in

Appendix 16 indicate that a weak correlation exists between the sites and the shapes calied

'crescents'.

The 'crescent' does not appear with 'stick figure' (xq348, xq382b and xq382a), or

with the hand print shapes (xq328, xq328b, and xq328a).

(j) 'Turtles'

Three shapes can be described as turtles at DhKm-3, DhKm-19, and DhKn-1

(xq382 & xq362). (A discussion of what differentiates the shape of a turtle from the shape of

a 'bird' or a 'creature' is in Chapter IV.) The turtles at DhKn-1 and DhKm-19 were solid and

painted using ochre while the turtle shape at DhKm-3 was holiow. While ali three shapes

were termed as "turtles" ali of them were different (see Appendices 7 and 16). Both turtles at

DhKm-3 and DhKn-l were painted using ochre. The painter employed modern spray paints

at DhKm-19 (xq327 & xq362). Turtle shapes made with ochre always occurred with ochre

'creatures', while turtle shapes created in modern paints existed on their own (xq327 &

xq362). The creatures at DhKm-3 were a solid creature facing right, and a holiow one facing

neither right nor left (xq382). The creatures at DhKn-l were solid, and two of them faced

left. These 'creatures' at DhKm-3 and DhIZn-l had either horns, ears, or antlers. Both of the

turtle shapes painted in ochre occurred with a shape of a 'stick figure' at DhKm-3 and

DhIZn-l (xq382b). Each of these vertical stick figures had two arms and two legs (xq382b).

Each site is in a different part of the lake. DhIZn-l was in Sabaskong Bay, DhKm-3

was in Whitefish Bay, and DhKm-19 was in Turtle Lake, located between these two parts of

Lake of the Woods. Ali three sites were in the southeastern portion of the Lake. The turtle in

modern paint at DhKm-19 did not occur with any other shape, supporting Rajnovich's

(1980b: 34) speculation that shapes could exist on their own as weli as with other shapes at

sites. However, the ochre turtle shape at DhKn-l occurred in conjunction with a vertical

stick figure, various 'creatures,' and several smears. This is in comparison to the red ochre

turtle shape at DhKm-3, which occurs with a larger range of shapes.

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(k) 'Birds'

Two shapes loosely categorised as 'birds' are found at DhKm-3 and DhKm-18 in

Whitefish Bay in the eastern portion of the Lake of the Woods (xq33S). Both shapes of birds

appear in conjunction with vertical stick figures (xq382b). Despite both shapes called 'birds'

occurring at DhKm-3 and DhKm-18 in conjunction with other shapes, neither shape had

the same physical description (see Appendix 16).

(1) 'Group of three diagonal paraUe1 short tines'

Shapes described as 'a group of three diagonal parallel short lines' (xq346) are found

only at DgKl-17, in Sabaskong Bay in the southeastern portion of the Lake. Nine types of

shape exist. They occur with only one 'creature' (xqS02).

(m) 'One vertical and one horizontal short tine that cross each other at ninety

degrees'

Eleven types of the shape called 'one vertical and one horizontal short line that cross

each other at ninety degrees' occur at five sites (xq336 & xq336a), but they can be subdivided

into two general groups (see Appendix 7). The shape in figure 6.20 called 'one vertical and

one horizontal short line that cross each other at ninety degrees' occurred nine times at

DhKo-1, DjKn-1, and DjKr-23 (xq336).

Figure 6.20: An examp1e of a shape caUed 'one vertical and one horizontal short line that cross each other at ninety degrees'.

It is clear from the map in figure 6.21 below that this shape is found at sites in the

northeastern, northwestern, and southern portion of the Lake of the Woods. The line

connects these three sites together.

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Figure 6.21: Sites with 'one vertical and one horizontal short line that cross each other at ninety degrees'

This shape is not found with 'stick figures' (xq382b), 'crescents' (xq348), 'creatures'

(xq382), 'zig-zags' (xq 321), or hand print shapes (xq328, xq328b, and xq328a).

The second type of this shape, which was slightly different, was described as 'one

vertical and one horizontal short line cross each other at ninety degree angle with short lines

at the end of each of the vertical and horizontallines'.

Figure 6.22: An example of a shape called 'one vertical and one horizontal short line that cross each other at ninety degrees with short lines at the end of each of the vertical and horizontallines'

Two examples of this shape were observed, at DiKp-1 and at DhKin-3 (xq366a) in

the northern and the eastern portion of the region. A comparison of figure 6.21 with figure

6.23 demonstrates the radical difference in the geographicallocation of each type.

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~ .. Figure 6.23: Sites with the shape called 'one vertical and one horizontal short line cross each other at ninety degree angle with short tines at the end of each of the vertical and horizontallines'

This particular shape is found with 'zig-zags' and 'stick figures' at both sites. The

stick figures were vertical and had two arms down and two legs (xq382a). But neither of the

zig-zags were the same, since the zig-zag at DiKp-1 was horizontal while the zig-zag at

DhKm-3 was either diagonal or vertical (xq321 and xq365). The shape called 'one vertical

and one horizontal short line cross each other at a ninety degree angle, with short lines at the

end of each of the vertical and horizontal lines' is found with 'creatures' at DiKp-1 and

DhKm-3. Both shapes were solid, had curved tails, either ears or horns on their heads, a

back and a front leg, but the shape at DiKp-1 faced left and the creature shape at DhKm-3

faced right. The shape called 'one vertical and one horizontal short line cross each other at

ninety degree angle with short lines at the end of each of the vertical and horizontal lines'

existed in conjunction with 'crescents' (xq348) or with the shape called hand prints (xq328,

xq328b, and xq328a) (see Appendix 16).

(n) 'Group of four diagonal short lines'

Two types of shape called a 'group of four diagonal short lines' (xq342) co-existed at

DhKm-5 and DhKm-3 with 'creatures' (xq382). Both sites are in the southern part of

Whitefish Bay in the eastern portion of the Lake of the Woods.

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Figure 6.24: Sites with groups of four diagonallines

The shapes of the creatures were different (see Appendix 16). The shape 'group of four

diagonal short lines' did not occur in conjunction with shapes loosely categorised as

'crescents' (xq348), 'stick figures' (xq283b), or 'zig-zags' (xq321). It occurred twice with right

hand print shapes, at DhKm-3 and DhI<.in-S (xq328, xq328b, and xq328a), but not at the

other sites that also had right hand print shapes; therefore, it cannot be argued that right

hand print shapes occurred with the shape called 'a group of four diagonal short lines'.

(0) 'Group of six short horizontallines'

Two shapes called a 'group of six short horizontal lines' (xq343) were observed at

DhKo-1 and DhI<.in-3 in the southern and the eastern portion of the Lake of the Woods.

They oruy occurred with 'creatures' (xq382), and vertical 'stick figures' (xq 382a). One of the

vertical stick figures at DhI<.in-3 (xqS11) was exactly the same as one at DhKo-1, except that

it was not inside a hollow square (xqS1S).

(P) 'Two paralle1lines'

Four examples of 'two parallel lines' (xq 347 & xq749) which were alternatively

diagonal, vertical, or horizontal were identified at DhI<.in-4, DgKl-1, DiI<.in-3, and DjKn-1

(xq347). These sites are in the eastern, southeastern, and northeastern portions of the Lake

of the Woods. None of these shapes was identical because one of the lines in the vertical

version of this shape just touched the middle other vertical line at DjKn-1 (xq347) (see

Appendix 16).

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(q) 'Three Hnes joined together at one end'

One shape called 'three lines joined together at one end' was painted at DiKp-l and

DiKm-3 (xq324). DiKm-3 is on an island east of the Aulneau Penin sula in Whitefish Bay and

DiKp-1 is on an island north of this peninsula. Both sites therefore were in the eastern and

northern portion of the region (figure 6. 25).

Figure 6.25: Sites with shapes called 'three Hnes joined at one end'

This shape occurred with 'stick figures' at both sites (xq382b). The stick figures were not

identical since the stick figure at DiKm-3 was diagonal while the stick figure at DiKp-1 was

vertical (xq382b). It also occurred with 'zig-zags' at DiKp-1 and DiKm-3 (xq321), but

examination of the detailed description of each zig-zag shows that the zig-zags were different

(xq321) (Appendix 16). The zig-zag at DiKp-1 was horizontal with a round head that had

two horns while the zig-zags at DiKm-3 were long, diagonal, with a pointed end and a head,

or vertical with a round head with horns and a forked tail (xq321). The shape 'three lines

joined at one end' did not occur with 'crescents' (xq348), or with hand print shapes (xq328,

xq328b, and xq328a).

(r) 'Group of four diagonal Hnes'

This shape is at DhKm-3 and DhKm-S (xq342) in the eastern portion of the lake.

Both groups of four diagonallines occurred with the shape loosely categorised as a 'creature'

(xq382). Only one of the creatures at DhKm-3 vaguely resembled those of DhKm-5. The

shape at DhKm-3 had long horns or ears, faced right, had one back leg and one front leg, a

curved tail and was solid (xqS11). AIl the other shapes of creatures at this site were hollow.

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Ali the creatures at DhKm-5 (xq513) were solid and faced le ft; otherwise, they differed. This

shape did not occur with 'crescents' (xq348), 'stick figures' (xq323), 'zig-zags' (xq 321), or

hand print shapes (xq328, xq328a, xq328b).

(s) 'Group of six horizontallines'

The shape called 'a group of six horizontallines' is found at DhKm-3 and DhKo-l

(xq 343), in the eastern and southern parts of the lake. This shape occurred with vertical

'stick figures'. If the precise description of each stick figure is examined at DhKm-3 and

DhKo-1, neither shape was exactly the same (xq382b) (see Appendix 7). This shape was also

found with 'creatures' (xq382) but neither the 'creature' nor the vertical stick figure was

similar. This shape did not occur with 'crescents' (xq348), 'zig-zags' (xq321), or hand print

shapes of either type (xq328, xq328a, and xq328b).

(t) 'Group of nine short lines'

The shape 'a group of nine short lines' appears at DhKm-5, DiKm-3, and DiKn-1

(xq344). These sites are in Whitefish Bay in the eastern portion of the Lake of the Woods.

None is exactly the same shape (see Appendix 7). The shapes at DiKn-1 were vertical while

at DiKm-3 and DhKm-5 they were horizontaL Furthermore, the ninth horizontal short line

in the shape at DiKm-3 was very faint.

(u) 'Square, created by two vertical and two horizontallines of equal shape'

Five examples of this shape are found only at DhKo-l (xq746) in the southern

portion of the lake (see Appendix 7). Four of these squares were exactly the same, while the

fifth had a short vertical stick figure with two legs and two arms in the bottom left corner of

the square.

Summary for Section 3:

The large number of blobs (xq349) and five types of 'unidentifiable shape' (xq744)

reflect that the pictograph sites are undergoing change from use, reuse, and natural attrition.

It is impossible to establish the full range of combinations of images. Smears are larger than

the blobs. Their physical size suggests, as discussed in Chapter IV, that they resulted as a

consequence of someone placing a wash of ochre on the rock surface, since they are often

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larger than other shapes such as creatures, zig-zags, and crescents. They could also reflect the

passage of time as a large image may have faded, exfoliated from the surface of the rock face,

or become indistinguishable because of the accumulation of white deposits.

Shapes such as smears, blobs, and unidentifiable shapes cannot simply be ignored as

they once were. Dewdney (1958-1964) and Lambert (n.d.) were perhaps mistaken in ignoring

them and not perceiving them to be indicators of pictograph sites. Perhaps these images

were not perceived to be interesting or informative, by either archaeologist, from the

interpretive perspective but these are not valid reasons to exclude them. By 1991 Rusak

(1992b) had recognised them as being significant shapes at pictograph sites. The smears,

blobs, and the unidentifiable shapes reflect that people used these rock surfaces to express

something and the images they created have just altered with the passage of time. This

conclusion is supported by the presence of a large number of shapes that occur only once

(Appendix 7). Examples of several of these images are visible in figures 5.17 and 5.18. Sites

such as DjKn-l, DhKm-3, DhKo-l, DiKm-3, and DiKn-l had a large number of these

uniquely occurring shapes. It must also be remembered that many of the varieties of shapes

called 'creatures', 'zig-zags', 'crescents', 'hand prints', 'stick figures', 'birds', and 'turdes' also

only occur once or twice once they are examined and described in depth (Appendices 6, 7,

and 16).

It is possible to consider combinations of various shapes. Right hand print shapes

exist if a left hand print shape is present (xq328, xq328a, xq326b). Shapes that are hands that

are left and right co-exist with 'creatures' at DiKm-3, DjKn-l, DhKm-5, and DgKl-19

(xq382). Vertical 'stick figures' only existed with hand print shapes at DjKn-l and DhKm-3

(xq382a, xq382b, and xq323). The four sites with creatures facing right and left are: DgKl-l,

DhKo-l, DjKn-l, and DhKn-l (xq382). While the sites DiKm-3, DhKo-l, DhKm-3, DiKp-

1, and DjKn-l have 'creatures' and stick figures, only DhKo-l has 'creatures' with horns,

ears, or anders (xq382b) with 'stick figures' that had horns, ears, or antlers (xq382). Two

crescent shapes whose points face downwards exist at DhKm-5 and DiKm-51.

Ochre turtles are at DhKm-3 and DhKn-l 'creatures' as well as the same type of

stick figure which if it is described in detail is a 'vertical stick figure with two arms and two

legs' (xq382b). The shape 'one vertical and one horizontal short line cross each other at a

ninety degree angle with short lines at the end of each of the vertical and horizontal lines'

existed with vertical 'stick figures' and 'creatures' at DiKp-l and DhKm-3. Two types of

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shape cailed a 'group of four diagonal short lines' (xq342) exist with 'creatures' at DhKm-S

and DhKm-3.

Two types of shape cailed a 'group of six short horizontal lines' (xq343) exist at

DhKo-l and DhKm-3 with 'creatures' and vertical 'stick figures' (xq382a). The shape cailed a

group of four diagonallines occurs at DhKm-3 and DhKm-S (xq382) with 'creatures' that

have either horns, ears or antlers. The shape cailed a group of four diagonallines at DhKm-3

and DhKm-5 is associated with right hand prints and a 'creature' (xq382). Both of these

'creatures' have either horns, ears, or antlers.

Two shapes were painted by themselves at a site. A turtle shape existed on its own at

DhKm-19 and a smear on its own at DiKm-SO. The existence of these individual images

supports Rajnovich's (1980b: 34) speculation that images could occur on their own as weil as

with other images at sites. Rajnovich (1980b: 35) also observed that paired images sometimes

occurred but only one pair of images was discovered at one site in the Lake of the Woods at

DgI(l-l. Here two shapes existed side by side which were described as a horizontal crescent

where three short vertical lines attached to the topside of the crescent (xq348). It is very

difficult to uncover combinatory 'rules' because of the smail dataset that 1 have at hand and

since many of the shapes have decayed beyond recognition becoming blobs. Indeed, the

most frequent shape identified is a blob (see Appendix 16).

Were the images created by professionals, specialists in these images amongst the

Algonquian-speaking community, or by amateurs? The creators of these images were

professionals in the sense that it is likely that they were trained in the creation and the use of

the images. This is a difficult question to answer with regard to the images created in ochre.

Yet, the shapes at DhKm-20 and DhKm-19 in modern paints so strongly resemble those

created by the members of the Woodland School of Art, founded by Norval Morrisseau

during the mid twentieth century, that the painters of these images were professionals or

inspired by professionals. This assumption is supported by the presence of the signature of

the painter and the date at the base of the images at DhKm-20. Unfortunately, it is

impossible to make any assertions regarding the ochre images since evidence does not exist

regarding their authors.

Sorne images occur in sorne geographical regions of the Lake and not others. Blobs

clearly occurred throughout the entire lake but smears were mainly found at sites in the

southern, eastern, and southeastern portion of the lake. The largest number of different

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shapes were found in the eastern portions of the lake. Here seven different shapes existed: 'a

group of nine short lines,' 'a group of four diagonal short lines,' 'a group of four diagonal

lines,' 'birds', 'crescents', and 'zig-zags, but diagonal zig-zags were only on DiKm-3 in the

same region of the lake. Two shapes are evident throughout the eastern, southeastern, and

the northeastern portion of the Lake of the Woods. These shapes are 'two parailellines' and

the 'hand print'. Two shapes existed in the northern and eastern portion of the lake, the

'three lines joined at one end' and 'one vertical and one horizontal short line cross each other

at ninety degree angle with short lines at the end of each of the vertical and horiz0!l-tallines.'

Two shapes existed in the southern and the eastern portion of the lake, 'a group of six short

horizontal lines,' and 'a group of six horizontal lines.' Two shapes occurred only in the

southeastern region of the Lake of the Woods: 'a group of three horizontal short lines', and

'turtles.' 'Unidentifiable shapes' existed at sites in the northwest and the southeast region of

the lake. 'Creatures' occurred in the southern, eastern and northeastern portions of the lake.

Hand print shapes occurred throughout the southeastern, eastern and the northeastern

portions of the region. The shape 'one vertical and one horizontal short line that cross each

other at ninety degrees' is found throughout the northeastern, northwestern, and southern

portion of the lake. The 'upper torso of vertical stick figure' occurred twice at sites in the

eastern and the southeastern portion of the Lake. The shape cailed 'a square, created by two

vertical and two horizontallines of equal shape' occurred in the southern portion of the lake.

As discussed in Chapter V there were many shapes that only occurred once and they were

predominately at rock image sites in the southern, southeastern, and eastern portion of the

lake. Only a few of the shapes occurred elsewhere in the region and they were either at

DjKr-23 in the northwest or DjKn-l in the northeastern parts of the lake. Only two

pictograph sites, DjKr-23 and DiKq-l0, existed in the western and the northwestern potion

of the lake. Petroglyph sites tend to be more numerous in the northwestern and northern

region of the lake. When the northeastern region was examined it is important to remember

that DjKn-l was the only pictograph site where the images were not ail described as blobs.

Sorne shapes appear in sorne parts of the lake and not in others. Perhaps sorne of the images

in the northeastern and northwestern pictograph sites occur in the petroglyph sites of the

northeastern and the northern part of the Lake of the Woods. This speculation can only

confirmed once these sites have been examined and the images described in the same

manner which the pictograph sites were examined.

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Conclusion:

This chapter sought to discover any relationships between the physical existence of

the sites in the larger landscape, the physical features of the rock's surface and the images

themselves. It was important ta establish any correlations and patterns ta provide a solid

basis for considering the meaning of these images.

Pictograph sites in caves and on cliffs should be perceived as different physical types,

Slnce each has their own characteristics. For other purposes, they must be examined

together. The lack of detailed correlation between the geology, the geomorphology in the

immediate vicinity of the sites and the landmass implies that another reason existed for using

images. The results provided do indicate that granite cliffs did not need to have large or small

crevices, cracks and holes for painting to take place. These results are supported by the

dendrograms presented in Appendix 15. The creators of these images perhaps had another

important reason in mind, such as some type of supernatural connection. In section II, 1

established that a link did not exist between the images and the rock surfaces, between the

number of images at sites and the type of land mass, the number of the physical features

present at cliff faces, whether offerings were found in 2001, and the number of cliffs used at

each site. The lack of positive correlations between the number of images and these other

features, especially o fferings , is interesting, since it suggests that other factors and reasons

explain why offerings were found at some of the sites in 2001.

Section III examined the images to determine any relationsrups between them. The

widespread distribution of the blobs (xq326) and of the five types of 'unidentifiable shapes'

(xq744) throughout the geographical area containing pictograph sites indicates that the sites

have been used for a long period of time because these shapes are produced by decay. The

large number of individu al images occurring once, such as those in figures 5.16 and 5.17, the

large variety of 'creatures,' 'stick figures,' 'zig-zags,' 'crescents,' 'hand prints,' 'turtle,' and

'bird,' and the large number of blobs, suggested that the people who used these images had a

large repertoire of forms from which to draw. These shapes reflect that people have used

these rock surfaces to express sometrung, and that time has passed since they were initially

created. The presence of a large number of unique images supports this idea.

The number of similar images within the large number of shape types is relatively

small and makes it difficult to identify combinations of specific shapes. The number of

shapes at a site ranges from one to trurty-seven. DhKm-19, DiIZm-50, and DkKn-6 had only

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one shape, while the largest site, DhKm-5, encompassed thirty-seven images. Blobs were the

most common type of shape. Combinations appeared if shapes were loosely described but, if

the shapes in question were described in detail, relatively few image combinations existed at,

and between, sites. This information is confirmed by the analysis and the dendrograms

presented in Appendix 16. A very weak correlation occurs between the physical location of

the sites, its physical attributes, and the shapes that occur in large numbers: 'creatures', 'zig­

zags', 'cres cents', 'blobs', 'smears', 'parallellines', 'birds', 'turtles', 'hand print', and the shape

called 'three horizontallines'.

Sorne images occur in sorne parts of the lake and other types in other parts of the

lake (see Appendix 16). Blobs are decayed images, and their widespread prevalence

throughout the lake demonstrates that blobs rather than smears may be more important

indicators of the passage of time. Smears were found at pictograph sites in the southern,

eastern and southeastern portions of the lake. This difference in geographical distribution

between the two shapes suggests that perhaps sorne smears were placed intentionally at sites

and do not always reflect the passage of time. The largest number of shape types occurred in

the eastern portion of the lake, where seven different shapes are found: 'a group of nine

short lines,' 'a group of four diagonal short lines,' 'a group of four diagonal lines,' 'birds,'

'crescents,' and 'zig-zags.' Diagonal zig-zags were found only on DiKm-3 in the same region

of the lake. 'Creatures,' which constitutes the large st number of any type, were painted in the

southern, eastern, and northeastern portions of the lake.

l will consider the meaning of these patterns and observations in the next Chapter,

where l use the homological approach to consider how to establish the meaning of these

patterns, and their relationship to other images outside the Lake of the Woods rock image

sites.

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Chapter VII: Approaches Concerned with Meaning.

This chapter discusses the meaning of the sites, and of the images themselves, in

relation to their physical location. l explored the ide a of considering the images individually

or as a group forming a narrative, with an aim to determine whether the images at pictograph

sites should be viewed as iconic or as narrative. l undertook a detailed examination of four

birch bark scrolls, using the same techniques l applied to the pictograph sites, to establish

whether images were understood as groups or individual elements. The birch bark scrolls

served as an illustration to counterpoint the rock image sites because the Algonquian­

speaking peoples made and used both.

The first section briefly discusses the two approaches considered use fuI for

establishing meaning, and establishes which is the most appropriate for analysing the images

on the pictograph sites. Section two provides a detailed examination of four birch bark

scrolls whereby l applied the same methods and techniques of analysis using the culture­

historical, contextual, and homological approaches. The goal of this small study was to

establish whether the images of the birch bark scrolls are similar to those of the rock image

sites, and if they provide dues as to how the images of the pictograph sites can be discussed.

Section three discusses efforts to consider rock image combinations as stories.

Present day indigenous Algonquian-speaking peoples are interested in these images.

Some of the images at several of the sites have been re-interpreted. This indicates that those

who currently live in this region have integrated these archaeologically and historically

important places into their mental and physical landscape. The fourth and final section of

this chapter discusses the notion that new images have been added to the graphical

vocabulary of the pictograph sites. Seven shapes were painted using modern paint but four

of the new images in modern paint were new vocabulary in the Lake of the Woods rock

image sites.

Section 1: The two useful approaches concerned with meaning

The literature reviewed in Chapter III indicated that archaeologists are more

interested in assigning meanings or explanations to the images themselves or to groups of

images than in studying rock image sites and their relationships. The majority of

archaeologists working on rock image sites of the Canadian Shield, in the vicinity of the Lake

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of the Woods, have resorted to the homological approach. However, as argued before, there

are two use fui approaches for establishing the meanings of these images: the homological

and the analogical approaches. They can be employed individuaily or in combination.

Therefore, it is important first to briefly outline again and reiterate what each approach

implies for the user.

(a) Analogical approach:

The wide spread use of the analogical approach, associated with New Archaeology or

the processual approach, was a reaction by positivists against the culture-history approach

during the 1960s. Those who foilowed this method of analysis argued that behaviour was

predictable from mate rial culture because of the many uniform connections between the

various components of socio-cultural systems, material culture, and human behaviour. As

Lyman and O'Brian (2001: 303) observed, the use of general comparative analogies required

application of the theory of orthogenesis. Yet general comparative analogies were not new in

the 1960s since they as weil as homologies, (specifie historical analogies), had been used to

examine the archaeological record of North America during the late nineteenth and the first

part of the twentieth century (ibid.: 304).

Biologists defined analogies as similar features of different species that do not have

close evolutionary relationships. Similarities have resulted from natural selection operating to

adapt different species to a similar environment (Abercrombie, Hickman & Johnson 1985:

20). An archaeological analogy in the narrow sense is a likeness or partiallikeness assumed to

exist as a consequence of convergent development under comparable conditions.

Interpretation using analogies ailows scholars to use strong cross-cultural regularities

between behaviour and material culture in systemic contexts to attribute behavioural

correlates to mate rial remains recovered from archaeological contexts. Binford maintained

that ethnographie analogies are useful sources of middle-range generalisations (Binford 1977:

288). An analogical interpretation is based on the existence of strong functional correlations

between specifie behavioral aspects and specifie aspects of material culture. Given such a

correlation, the presence of similar material culture in the archaeological record ailows an

archaeologist to presume that similar or associated behaviours existed in the pasto Watson,

LeBlanc and Redman (1971: 51) argued that analogies provided archaeologists with the

"richest sources of hypothesis" available.

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/~.,

What types of bridging arguments do scholars use for justifying an analogical

interpretation? Those who adopt an analogical approach conclude that it is only worth

employing univers al regularities in human behaviour. They presume that correlations exist

between past and present day cognitive and behavioural capabilities of human beings. If

similar behavioural characteristics can be established between specifie aspects of material

culture and behaviour in the modern (present day) world, they can be extended to cover the

same or similar aspects of material culture in the archaeological record (Binford 1981).

Scholars adopting analogical approaches use universal generalisations rather than concepts

specifie to individual cultures or historically related cultures. It is impossible to include the

idiosyncratic facets of an historical tradition if one considers only universal correlations

relevant. This approach utilizes the results of different developments that, because of

functional correlations, are similar regardless of their cultural origins or the environmental

setting within which they developed.

Does the analogical approach have anything to contribute to the Lake of the Woods

data? Related to a positivist and universalising view, this approach does not provide an in­

depth understanding of culturally specifie meanings, including any changes in meanings.

Perhaps sorne universals exist with respect to meaning because human beings have had the

same neural network since the Aurignacian period, but the development of human

physiology, ideas, and objects is subject to numerous, unpredictable changes through time.

Univers ais seem more prevalent in human behaviour than in belief systems. This makes

using an analogical approach and discovering culturally idiosyncratic belief systems in the

archaeological record difficult. Meanings and the reasons attributed to artefacts clearly

depend on the ethnie, social, cultural, religious, and geographical identities of the people

involved. Scholars also must be aware of the dangers of extrapolating general analogies from

specifie bodies of ethnographie evidence without considering the specifie contexts within

which that evidence was created or applied. This approach could be useful if drawing on a

similar body of data produced by the Algonquian speaking peoples proved impossible.

Fortunately, a large body of data is available for analysis from which correlations can be

drawn between the images used elsewhere on objects made by the Algonquian-speaking

peoples, the images on the birch bark scroIls, and those on pictograph sites.

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(b) Homological approach:

An archaeological homology is a similarity in two or more cultures that occurs as the

result of a shared historical origin unobscured by cultural drift or adaptation to different

cultural environments. Archaeological homologies differ from those in biology, because they

can result from both diffusion and common descent. In biology, reproductive isolations

mean that homologies can occur only among species that are descended from a common

ancestor. Consequendy, homological similarities imply evolutionary relations among

organisms (Abercrombie, Hickman, & Johnson 1985: 145). Scholars establish interpretations

using homologies by demonstrating and tracing cultural continuities through time in a single

cultural tradition or a series of historically related cultural traditions. Interpretations

employing homologies frequendy also resort to the direct historical approach. This approach

identifies parallels between culturally specific beliefs and their material expressions du ring the

early historical period and employs material culture to trace these beliefs back into prehistoric

times. The bridging arguments for establishing homologies between beliefs or behaviour and

material culture, and between the present and the past are culturally specifie. Homologies,

asserted Watson, LeBlanc, and Redman (1971: 50), were advantageous in regions with strong

cultural continuity, and where the same techniques and implements were utilised for a long

period of time. Written records, oral heritage, and ethnographic materials, always combined

with archaeological data from successive periods, are probably the strongest types of

evidence to be used when devising bridging arguments (frigger 1995: 452). Scholars exploit

these materials to establish which beliefs were present in specific cultures.

The direct historical approach connects archaeology with other disciplines, providing

information concerning the practices and beliefs of either specific societies or groups of

historically related societies. By relying on a wide variety of evidence, archaeologists can

attempt to establish continuity in the practices and beliefs in question. The homological

approach allows in-depth analysis of a specifie group and its material culture. It permits

archaeologists to consider what human beings might have thought about in the past and the

meaning of specifie symbols and objects. It may be possible to determine that similar images

used in a variety of different mediums held similar meanings. Yet, continuity of form does

not necessarily imply continuity of meaning. Meaning, too, can change, especially since icons

tend to be polysemie.

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Archaeologists using homological interpretations must have a detailed understanding

of the skills required to use archaeological, historical, and ethnographie materials from the

region in question. These materials are multidisciplinary in nature. Those taking this

approach must verify how entrenched beliefs are established in cultures and how susceptible

they are to evaluation in terms of that culture. Any archaeologist using the homological

approach must be aware of different cultural perspectives and acknowledge that using the

direct historical approach is neither straightforward nor simple. Material symbols may

continue to be used but their meaning is not necessarily inert. Material symbols can acquire

new meanings and become an example of what Davis (1992: 25) called an "iconographie

disjunction." Continuity or discontinuity in beliefs over time is not correlated in a simple

manner with material culture. An example of such a symbol is the swastika which has had

several radically different meanings to different peoples.

It is important to choose which approach to use. Since 1 am more interested in this

group of images' symbolism and meaning than in inferring technological processes,

subsistence patterns and numerous aspects of social and economic behaviour, the

homological approach is more appropria te. This approach is also more advantageous in

regions such as the Lake of the Woods, where cultural continuity is strong.

This approach places a heavy reliance on written materials to create bridging

arguments. Unfortunately, this study suffers from a fundamentallack of detailed historical or

ethnographie information regarding the meanings of the images that occur on cliff faces and

inside caves.

Many analysts maintain that specifie places in the landscape were used as pictograph

sites. Rajnovich (1994: 34) argued that according to the Ojibwa these images often occur on

specifie rocks in the landscape in which the medicine manitous, or spiritual grandfathers are

thought to live. Vastokas and Vastokas (1973: 47) observed that "aIl remarkable spots in the

country" were believed to be the "favourite haunt of the spirits." Physical features, such as

"boulders, rock hills, and outcroppings with unusual dimensions or character, such as clefts,

holes, or crevices," served as dwellings for manitous and mythological creatures (ibid.: 48).

Hallowell (1936: 47), Jones (1981a: 72), and Wheeler (1977b: 710) argued that the Ojibwa

believe that, after consulting manitous that lived in the rock, shamans created the images,

either to record a vision que st or as lessons to others. The rocks marked the places where

holes or openings penetrate the surface of the Earth, which consisted of several layers,

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through which supernatural beings could pass from one world to another. These holes

served as meeting places connecting the four distinct, horizontally-Iayered worlds of the

Algonquians: sky, earth, underwater, and underground (Hallowell 1992: 74; Grim 1983: 77;

Rajnovich 1994: 35; Vastokas and Vastokas 1973: 53-54).

Ethnographic evidence from the Severn River, north of Lake of the Woods, enables

one to argue that the rock image sites are places in the landscape where the shaman(s) in the

community went to obtain advice, or medicine. Chief Thomas Fiddler, a shaman from the

Severn River are a, reported learning through a dream how to get medicine to help people.

He returned to the same hill that his shaman grandfather, Jack Fiddler, went into, to obtain

medicine from the cave dwellers (Fiddler and Stevens 1995: 196). He reported that Jack

Fiddler went every spring to the same rock in a place called Rathouse Creek, near Trout

Lake, to con suIt the Cliff Dwellers regarding herb medicine (Fiddler & Stevens 1995: 47-48).

Perhaps individuals consulted the manitous, or left offerings to the memegweccios, also

known as may-may-gwashi or memenowéciwak, who live in rocks beside water (Coleman

1937: 42; Flannery 1931: 4, 7, 16-17; Hallowell1992: 64).

Redsky (1972: 36), an Ojibwa elder from Shoal Lake, argued that the pictographs

were not made from paint but from the blood of the godly hands of the may-may-gway-shi

as he termed them. These small hairy spirits lived in the cliffs alongside the lakes where the

paintings are found. Lambert (1983: 109), an archaeologist, observed that Redsky's statement

contradicted an earlier one he made in the same publication that he believed the pictographs

were a result of human agency. Despite the apparent contradiction in Redsky's (1972) work,

he argued that individuals, usually shamans, went to consult other beings, such as manitous,

to obtain medicine, help or other forms of aid. The offerings that continue to be made as

gifts to spirits at the pictograph sites suggest that these places are still important to the local

indigenous peoples. Clearly, specific places in the landscape were important to the

indigenous people who created these images.

Dewdney (Dewdney and Kidd 1964: 8-9) based claims concerning the importance of

the physical features of the cliff image sites on information from informants. His informants

spoke of small hairy creatures called may-may-gway-shi who "lived behind waterside rock

faces, especially those where cracks or shallow caves suggest an entrance" (Dewdney and

Kidd 1962: 13-14). He discovered that "specifically gifted Ojibwa shamans had the power to

enter the rock" to "exchange tobacco" for what Dewdney termed "potent rock medicine"

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r----...

(ibid.: 14). Dewdney (1979b: 336) insisted that an 1mage group should be examined in

conjunction with its location and that a site could be considered in relation to its local

environment.

Vastokas and Vastokas (1973: 48) argued that crevices and holes were the "dwelling­

places of the manitous and mythical creatures su ch as the Maymaygwayshi". Hallowell (1992:

64) gave another name to these creatures, memenowéciwak, which perhaps reflects a

dialectical difference. They lived on the earth, and pictographs were attributed to them.

These creatures "were familiar to everyone," but only encountered on rare occasions. They

had a human form, lived in rocky escarpments, travelled in canoes, and occasionally stole

fish, for which they had a fondness, from Indians. When they met humans, they hung their

heads to hide "a soft part to their no se, only a hole" (ibid.).

Vastokas and Vastokas (1973: 100) argued that the crevlces at the site of the

Peterborough petroglyphs led to the underground, therefore, crevices and, by default, cracks,

provide another way of accessing these four worlds. Previous archaeologists argued that

holes at pictograph sites formed an "entrance," "natural entrance" (Rusak 1992a: 36, 54),

"grotto" (Lambert 1985: 21; Rusak 1992a: 23), or openings to the four layered Algonquian

worlds described by Hallowell (1992: 74) and Vastokas and Vastokas (1973: 45-48). The

continued presence of offerings at sorne of the sites suggests that sorne of these sites were

and are considered important places in the physicallandscape despite the passage of time.

Although it is possible to establish that the Algonquian-speaking peoples created

these images, it requires the examination of a considerable quantity of evidence. The

Algonquian speaking peoples, as discussed earlier in Chapter II, have a sophisticated

knowledge and understanding of how to read, use, and manipulate images using a wide

variety of objects, induding beads, quills, moose hair, and bitte n, or etched, into birch bark,

for different audiences. These images are confined to portable objects, unlike the images on

rocks, so they could be carried by people, in bands, as they migrated from one part of Lake

of the Woods to another, from hunting place to gathering place, and from person to person

over time and space. Images were an important means by which the Aigonquian-speaking

peoples communicated information and ideas, regardless of the materials used to create

them. Detailed examinations of the imagery, as discussed in Chapter II, reveals that creators

manipulated different types of shapes and materials for specifie audiences. The rapidity with

which the floral ornamentation developed and spread supports this idea.

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The key difference between the pictograph sites and these images on portable objects

is: pictograph sites remain statie points of contact between different members of the same

group, different groups, bands, and between the different worlds of the Algonquian belief

system, whereas images on portable objects are not static points of contact. These images

and the objects on which they exist have changed and have been manipulated over time by

different audiences.

Specific places were chosen, but the important features that qualified a physicallocale

as a potential pictograph site remain unknown. If specifie features were important for the

presence of images it is clear that archaeologists have not yet identified them. Furthermore,

and unfortunately, the body of ethnographie evidence is used not only to posit the possible

presence of images at particular places in the landscape but also to substantiate the presence

of the images themselves. Essentially, the same body of information is being used both as a

source of information to find the sites and their images, and also to interpret them. Yet the

data presented in Chapter VI demonstrates that archaeologists' efforts to establish what

might have caused particular places to be chosen have been unsuccessfuL

The correlation between the paucity of offerings in 2001 with the paucity of physieal

features at pietograph sites is difficult to explain. Perhaps offerings are left at the sites that

are known to be pictograph sites in the generally available literature. Indeed, offerings were

not found at the "newly discovered" sites. It is difficult to establish why this has occurred

since it is impossible to establish what the missing factors, if any, may be in choosing a

location for a pictograph site. It does suggest, however, that the offerings present in 2001

resulted from individual rather than collective behaviour. Individual behaviour also might

explain the paucity of the individu al physical features at sites. It is possible to support this

proposition from the artifacts collected at the base of the DhKm-1 below the water level, as

discussed in Chapter V.

Yet a connection exists between images on portable objects and static entities in the

landscape because the Midé, ritual and medicinal specialists, were key members of

Algonquian society. The Algonquians created and used images to communicate information

on a range of portable objects, while the Midé used a specifie group of images on birch bark

scrolls. Various ethnographie sources indicate that the pictograph sites were places where the

sacred and profane worlds met, and where the Midé, or shaman, could go to seek help and

consult the spiritual grandfathers.

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.r--.

The strong similarity of the images found on the statie and portable objeets used by

ail, and those ereated by the Midé, strongly suggests that it would be a use fuI endeavour to

examine several examples of the images on bireh bark. Sorne of the images on bireh bark

seroils number 1 and 3, examined later in this chapter, bear a strong resemblance to those of

the pictographs. However, other images on both these seroils and on scroils number 2 and 4

are radieaily different, and have no resemblance to the images of the pietograph sites. A brief

examination of the four scroils indieates several arrangements for the images on them, but

the precise rationale behind the arrangement is difficult to establish, as l demonstrate in

section 2 below. Consequently, the meaning of the images on birch bark seroils is obscure.

This suggests an equal difficulty in deterrnining the arrangement of the images on pietograph

sites.

The biggest problem in pictograph image analysis remams the paueity of written

material on their precise signifieance. It is impossible to eomprehend either the signifieance

of the images or their intent. This problem has impeded arehaeologists' attempts to establish

both the meaning of the individual shapes, and the possible meanings of shapes oeeurring in

various eombinations with other shapes at different pietograph sites. Sorne have posited the

possible eonnection between the shapes created by the Midé on bireh bark and those existing

on the surfaces of rocks CV astokas and Vastokas 1973; Dewdney and Kidd 1962 and 1964). l

use an examination of bireh bark seroil images as a counterpart, or an illustration, of possible

results regarding images on the pietograph sites.

Two questions exist: do the images at pictograph sites represent a specifie

voeabulary? Or did shamans who knew a specialized vocabulary create these images?

Previous researchers have observed differences in the types of images.

Vasto kas (1984) defined two functional types of images, which she cailed iconic and

narrative. The images were either read as a group of multiple images, therefore, as texts with

meaning, or they were read as individual images, as iconography with meaning. Vastokas

(1984: 430), in her article on birch bark seroils (diseussed in Chapter 11), defined narrative

compositions as multiple motifs organised in a "more perceptuaily scattered disposition

ailuding sequence and movements to the eye aeross the surface of pictorial ground." She

(ibid.) argued that profile images denoted motion, while frontal views indieated action.

Narrative art forced the observer to detect the greater visual complexities of the composition

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(ibid.: 431). She concluded that the birch bark scrolls were "narrative visual wholes" to be

interpreted in terms of their form and context.

Coleman (1947), Copway (1851), Schoolcraft (1851), and Landes (1968: 172)

differentiated between types of images used for information. Images were used in two

contexts which can be termed the sacred and the profane.

Dewdney (1970: 22), on the other hand, identified three types of writing: secular,

tutorial, and visionary. The images on pieces of birch bark left as trail messages at portages to

provide useful information to those who followed, are an ex ample of secular writing.

Tutorial writing enabled an initiate to learn by rote the traditions and practices of the

Midewiwin from the teacher, the Midé. These images occurred on the Midé scrolls and those

who had been initiated into the Midewiwin Society "read" them as mnemonics. Images such

as a dream symbol, obtained from a person's dream guardian during their puberty dream,

acted as an example of visionary writing (ibid.).

Those images used in a social rather than a religious context may have changed most

radically in their physical appearance. The literature reviewed in Chapter II reveals that

relatively unchanged images belonged to the religious life of the Algonquian-speaking

peoples. Here images served as mnemonics in a variety of scenarios, designed to convey

information over several generations to specific individuals called Midé.

Schoolcraft's (1851: 351), Coleman's (1947: 63), Dewdney's (1970: 22-23, 1975: 12-

13), Warren's (1984 [1885] 89), Densmore's (1974[1929]), and Hoffman's (1883: 139) articles

gave examples of images likely used in the profane world and which, hence, underwent sorne

level of physical change and shifts in meaning as discussed in Chapter II. Images and

indentations used to mark the totem of the individu al buried were placed on grave markers,

or on treaties between indigenous peoples and Europeans, on objects to measure the number

of generations past, on headboards of bark canoes, on copper plates, as a "signature" which

was recognised over a geographical area, and on personal objects. Hunters, trappers, and

travellers used images to indicate information about boundaries, trails, and notices of

different sorts. Everyone over a wide geographical area recognised and understood this

group of images, therefore the origins and meanings of this group of images were not

shamanic.

It is hard to de termine whether images at pictograph sites were made at the same or

at different times. Images made at the same time may tell a story, or the images may have a

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meaning which is only understood by individuals. If images were made at different rimes,

then the implications for the meaning of these images is impossible to establish.

Very few image combinations occur repeatedly at any pictograph sites. The large

number of blobs indicates that many images have decayed, and that sufficient time has

passed for them to have deteriorated beyond recognition.

The variability of the images at the different sites depends on how professionaily

these images, and the sites, were produced. If a shaman produced these images, there would

be litde variety in the specialized vocabulary used. Yet, it is impossible to establish the length

of time over wruch professionals may have created these images. If the patterning of these

images at the individual sites is deliberate, then perhaps these images are designed to teil a

story.

A few sites, DiKm-4, DhKm-3, DhKo-1, and DhKn-1 have been re-interpreted

since 1990, using information provided by elder members of the Ojibwa Oackson 2000), who

also have interpreted images on birch bark scroils. The images are used to teil a story, but it

is impossible to teil whether the story is ancient, or whether it reflects the manner in which

the site and images have become part and parcel of the modern Ojibwa's cultural and mental

landscape.

The images on pictograph sites cannot be dated using absolute dating techniques.

Their style does not provide any indication of whether they were made either at the same or

at different rimes. The presence of the blobs, discussed at length in Chapter V, in

combination with the large number of blurred and exfoliated images suggests that the rock

surfaces were used repeatedly. Therefore, interpreters should treat the images as having

individu al meanings, and avoid considering a coilection of them as a group.

However, the question of treating a group of images at a site as telling a story

remains. Images considered as a story should have the same funcrion as those on birch bark

scroils. Therefore, l decided to conduct an examination of several birch bark scroils and their

images to establish the range of images, and to uncover any image combination on each or

between scroils. l compared these results to the rock image sites to determine whether birch

bark scroil images were used in the same manner, and, hence, have the same type of meaning

as those on rock image sites.

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Section 2: An examination of four bireh bark serolls.

1 obtained two song seroils, one of medicinal information, and one about an

historieal event. Eaeh seroil was unique. 1 tried to obtain similar seroil types, but aehieving

this goal proved impossible. What 1 eould suecessfuily ob tain with minimal bureaucratie fus s,

teehnieal issues and problems dietated the seroil type studied. The diffieulties of digitizing

black and white photographs or plates of varying qualities limited the number of seroils used

in this analysis. It was important to examine these images in original bireh bark form, and not

as transcriptions or redrawings.

The first seroil, seroil number 1 (figures 7.1 and 7.2), is a digitized file of a black and

white photograph taken by Jacqueline Rusak and 1 in September 1993 of the Massacre Seroil,

held by Lake of the Woods Museum, in Kenora, Ontario. The figure below shows half of the

seroil. The seroil had been bent in half and eould not be opened without risk of breakage, so

two photographs were taken.

Figure 7.1: The left hand part of seroll number 1.

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Figure 7.2: The right hand part of seroll number 1.

l successfuIly digitized the black and white print ln Densmore's (1910: 100)

publication on song scralis (see figure 7.3 and 7.4). Both scrolis were produced fram a black

and white print, not a photograph. l will cali figure 7.3 scrali number 2, and figure 7.4 scrali

number 3.

Figure 7.3: One of the serolls that Densmore photographed.

Figure 7.4: One of the serolls that Densmore photographed.

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Both seroils (figures 7.3 and 7.4) are part of a large study with good information

regarding their eontext and the meaning of sorne of the images. Both are held by the

Ameriean Bureau of Ethnology at the Smithsonian Museum.

Dewdney photographed and published the fourth and final seroil (figure 7.5) ln

1970 (1970c: 27& 28).

Figure 7.5: The seroU published by Dewdney in 1970.

Nlistakes ean oeeur when these images are traced, despite every effort on the part of

the reproducer. A detailed eomparison of Dewdney's (1975) drawing of the seroil on medieal

plants, from the Ethnology Department of the Royal Ontario Museum (figure 7.6), with the

original photograph (figure 7.5) published in 1970 (1970c) reveals that fundamental

differences exist in the shapes of the images. 7

7 Careful comparison of each figure in the photograph with Dewdney's tracing ab ove shows that Dewdney missed features of several of the images. These mistakes are inevitable when images on a scroIl or document are copied by hand or traced. This demonstrates the importance of obtaining a photograph of the actual scroIl or a digital version, a tiff flle. Fulford (1990), in an article examined earlier (see Chapter II) realised that problems often occur in the transcription of images on birch bark scroIls. It was impossible, he maintained, to provide definitive transcriptions and translations of the Hoffman material (ibid.: 128). He re-transcribed and re­translated the chants that Hoffman (1891) had compiled before reworking the entire corpus to develop glosses to improve the flow, or to supply better connections between the word and the pictographs. Fulford decided to do this beeause he saw inherent problems of Hoffman's informants' poetie use of language and Hoffman's own inadequaeies. In the end, Fulford (ibid.: 127) concIuded that the reproductions of the scroIls were generally accurate.

Despite great efforts, the diffieulty in improving the quality of digitized images of published bireh bark scroIl photographs beeame evident. The impossibility of using an original bireh bark seroIl also limited my research.

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. /" ..

Figure 7.6: Dewdney's tracing of the seroil in figure 7.5.

The annotated photograph below (figure 7.7) indicates rune differences between

Dewdney's drawing and the original photographed. A numbered blue box outlines each area

where lines are missing between the original and Dewdney's drawing. Dewdney did not draw

the verticalline, which could be a crease, running through the middle of the scroil. A narrow

vertical blue rectangle highlights this region of Dewdney's reproduction .

Figure 7.7: The nine differenees between the Dewdney's drawing and the original seroil.

(a) How were the seroils examined?

l used the same method and techniques to describe and analyse the scroil images as

employed for the pictograph sites. The same sequence of theoretical approaches used to

describe and analyse the pictograph images was applied to the images on the birch bark

scroils. Therefore, l first described images on the birch bark scroils using the methods

discussed at length in Chapter N. l examined the images using the techniques and methods

used for the rock image sites discussed in Chapter V. l sought scroil image combinations as

discussed in Chapter VI for the rock images. It was important to apply the same procedures,

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methods, and techniques to another group of images ereated and used by the Algonquian­

speaking peoples. As the images of the pietograph sites in the tiff files had been deseribed

from left to right, ail of the images on the seroils were deseribed from left to right. This

approaeh was taken sin ce ail image files examined using KLEIO lAS must be deseribed from

left to right (see Chapter IV). This also foilows Hoffman's (1891: 267) observation as to how

the images eailed pietographs were read: the seroils eould be read from left to right, or right

to left and sometimes some seroils used both styles. Coleman (1947: 79) noticed that the

seroils belonging to the Midé in northern Minnesota were read from left to right. Vennum

(1978: 761) argued that migration seroils, used by the Midewiwin, were read from left to

right, since the Otter traveiled from the east to the west (ibid.). The eontextual information

for bireh bark seroil numbers 1, 2, and 3 was purposely ignored when deseribing the images;

l used it only in applying the eontextual approaeh. Very little eontextual information existed

for seroil number 4.

(b) Culture-Historie al Approaeh:

The images of the four seroils are etehed on the surface of the bireh bark. None is

eoloured in. The physieal state of the seroils eould not be eonsidered beeause photographs

were used for this study and the originals could not be eonsulted.

There are one hundred and nine images in total (xq414), averaging 27.25 per seroil.

Twenty-two of the one hundred and nine shapes have hoilow interiors (xq430). Five of these

shapes are on seroil number 1, eight on seroil number 2, while the remaining nine shapes are

on seroil number 3. Seroll number 4 has no hoilow shapes. Twenty-three shapes, found on

ail four seroils, have hoilow interiors with lines. There are eight shapes on seroil number 1,

seven on seroil 2, five on seroil 3, and three shapes on seroil number 4. Only three shapes, ail

on the seroil number 2, had centres that deseribed as partiaily hoilow (xq431). The remainder

of the shapes deseribed were made up of lines, and, therefore, eould be deseribed as having

neither hoilow, hoilow with lines, nor partiaily hoilow centres.

The images present are as foilows:

1) Five types of shape eailed a 'creature,' found only on seroil 1, exist in this dataset (xq419).

2) There are four types of 'bird' (xq422), ail on seroil number 1.

3) There is only one 'turtle' (xq423), and it is found on seroil number 4.

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4) 'Two parallellines' do not exist (xq420). However, the shape called 'two parallel vertical

lines' occurs four times, found only on scroll number 1.

5) 'A line of dots' occurs four times on scrall number 4. It does not occur alone, only in

conjunction with other images such as cireles, lines, and the turtle.

6) 'Cirele' appears forty-one times (xq426). Only six of these cireles exist without other

cireles, lines, squares, or rectangles, four were found on scrall number 2, and two on scroll

number 4. The remainder of the cireles are attached to other cireles, rectangles, squares

verticallines, horizontallines and diagonallines.

7) The 'zig-zag' does not exist on its own. It does occur in conjunction with other shapes

such as rectangles, horizontal, and diagonallines on scroll number 1 and 4. The zig-zag shape

is vertical on scrall number 1 and in the shape on scroll number 4.

8) There are ten shapes that have a 'rectangle' as one of their components. There is no such

shape that consists only of a rectangle. Rectangles occur only with other shapes such as

vertical, horizontal, diagonal lines, and cireles (xq418). They occur as components three

times on scrall number 1 and 4 and twice on scrolls number 2 and 3.

9) The 'square' type of shape was found twice (xq427): on scrall number 1 containing six

verticallines, and with a 'creature' on it; and on scrall number 3 with a cirele, horizontal, and

verticallines.

10) Two 'stick figures' were found, each as part of a larger shape (xq428) together with

cireles. One stick figure occurs on each of scrall numbers 2 and 3. However, only the top

half of the stick figure is evident on scrall number 3.

11) There are two shapes called "long diagonal line with short diagonal lines on each side"

on scrall 2 (xq433).

12) Six shapes called 'short diagonalline,' alliocated on scroll number 2 (xq432).

13) Three shapes called a 'very short diagonalline' are etched on scrall number 2 (xq432). A

similar type of shape, shorter than the other lines of the same type, 'a short diagonal line,'

appears on the same serail.

15) Only one 'one long verticalline' shape exists, found on scroll number 4 (xq434).

16) There are four 'triangle' shapes (xq435). One triangle is on each of scralls 2 and 3, while

the remaining two triangles are on scrall number 4. None appears alone and ail have lines of

different types.

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Ali other shapes only occur once, and are composed of a combination of vertical,

horizontal, and diagonallines (xq432), rectangles, and circles.

It is very difficult to comment upon the style of the scroUs. However, it is possible

that the two scroUs (numbers 2 and 3) coUected, discussed, and published by Densmore

(1910) show more similarities between each other, while scroU (number 4) published by

Dewdney (1970b) and scroU number 1, photographed in 1993 by Rusak, are similar in style.

However, the physical arrangement of the images on scroUs number 1 and 4 are quite

different. The shapes on scroU number 1 are distributed around the edge while those of

scroU number 4 do not share this stylistic characteristic.

Comparison of the images found on bireh bark serolls and on the roek image sites

Comparison of the above list of shapes with the list in Chapter V (page 268) reveals

that shapes caUed blobs are absent from the birch bark scroUs because of different

taphonomic conditions. Like pictograph sites, birch bark scroUs had 'creatures,' 'birds,' 'stick

figures,' and 'turtle' occurring on their own. The scroUs also had shapes caUed 'rectangles,'

'zig-zag,' 'squares,' and 'triangles,' but none of these occurred separately like those on the

rock image sites. The largest number of shapes for the four birch bark scrolls is the group

called 'circles,' but only six of them occur alone. The large st number of images in a group

occurring on the pictograph sites were the blobs.

The next largest group of shapes on birch bark scroUs were 'creatures.' Five types of

'creature' occur on the birch bark scroUs while twenty-three shapes loosely categorised as

'creatures' were identified on the pictograph sites. The 'creatures' on the birch bark scroUs

are considerably more complex than those of the rock image sites (see Appendix 17).

Furthermore, aU the 'creatures' occur on a single scroU, number 1, while the twenty-three

types of 'creature' occur on approximately a third of the twenty-seven rock image sites.

'Birds' occurred both on birch bark scroUs and at rock image sites. The birch bark

scrolls had four types of 'bird' shape while the rock image sites had only two types of 'bird'

shapes. One of the bird shapes, on birch bark scroU number 1, is very similar to the bird

shape on DhKm-3. However, the bird shape on the birch bark scroU is immediately beneath

another image which does not occur above the bird shape at DhKm-3.

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~ ..

Although both the bireh bark serails and the roek image sites had the 'turtle' shape,

none of these images had the same physieal shape.

Although the bireh bark serails had a 'zig-zag', it did not oeeur on its own but with

other shapes such as rectangles, horizontal, and diagonallines on scrail number 1 and 4.

The shape loosely categorised as 'stick figure' also occurred on two of the birch bark

scroils this shape was always part of another shape, a circle (xq 428).

Otherwise, twenty-three of the one hundred and nine shapes on the scroils were hoilow

while only forty-one of the three hundred and eight shapes of the pictographs were hoilow

(xq752). Hoilow shapes were found on ail four of the birch bark scroils (see Appendix 17),

but hoilow images did not occur on ail of the pictograph sites. The hoilow shapes on the

birch bark scroils were drawn as hoilow while those of the roek image sites may not have

always been hoilow. Sorne of these shapes may have beeome hoilow because of exfoliation,

the deposition of white mineraI deposits, lichen and rock tripe encroachment. On the other

hand, none of the images on the birch bark scroils were solid like those of the rock image

sites. Images on birch bark seroils could not be rendered solid in the same manner as those

of the sites without etching a hole in the bark. Although these images could not be described

as solid, they either had lines or other shapes in their centres.

There were twenty-five types of shapes on the rock image sites and sixteen types of

images occurred on the birch bark scroils. The birch bark scroils had a number of images not

found on the rock image sites including: 'short diagonalline,' 'very short diagonalline,' 'one

long verticalline,' 'circles,' 'long diagonalline with short diagonallines on each side,' and the

'two parailel verticallines' shape.

The average number of images per pictograph site was eonsiderably lower than the

number of images on the birch bark scroils: 11 to 27.25. Colour use illustrates another major

difference: colour is an important feature of the rock image sites, but it is entirely absent

from the images on the birch bark scroils. Indeed, the colour and type of paint prove to be

key indicators that sites are being reused. No such clear indication of reuse of the birch bark

scroils is indicated. The range and type of images found on the birch bark scroils and the

rock image sites are quite different. This eould indieate that each group of images belongs to

a different set used to communicate different types of ideas. Birch bark seroil images are

more eomplex than those of rock image sites. The person 'reading' and using the images on

the bireh bark relied on a specialized knowledge: one knew and understood the sequence in

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which they were used. l discuss the information for the two scroIls coIlected by Densmore,

which indicates that readers required special knowledge to understand birch bark scroIl

images in the homological approach later in this chapter.

(e) Contextual Approaeh:

The smaIl number of common (see Appendix 17) and the variety of unique shapes in this

dataset make it difficult to establish whether any combination of shapes occurs in aIl of the

different scroIls.

The eontext of the information on the seroIls:

SeroIll:

Very little contextual information exists regarding this scroIl. The dark verticalline in

the centre of the scroIl is a crease. Dewdney did not examine this scroIl although he spent a

considerable quantity of time researching and examining the birch barks found in the Lake of

the Woods region for his (1975) book on birch bark scroIls. Neither does he mention it in his

(1970b) article that published the photograph of birch bark scroIl number 4, nor in the book

he co-authored with Kidd (1962 and 1967).

Serolls 2 and 3:

Both of these black and white photographs were published in Densmore's (1910)

publication on the song scroIls, coIlected during 1907, 1908 and 1909 from the Chippewa

lndians of White Earth, Leech Lake, Red Lake reservation in Minnesota, and from a

Chippewa who lived in the Bois Fort reservation in Minnesota. Her study was discussed in

Chapter II. Densmore (ibid.: 96) argued that the word "medicine" referred to any substance

by which results "are supposed to be mysteriously attained." The scroIls have images which

she (ibid.: 96-106) connected with rare medicines. Densmore transcribed the title and words

of each of the songs on the scroIls as carefuIly as possible using an interpreter and the image,

the mnemonic was obtained and published in conjunction with the musical score of the song

sung, the words, and the harmonic analysis of the song. Densmore (ibid.: 96) stated that aIl

of the songs were sung by the shaman caIled 0' deni' gûn. She asserted that the songs were

examples of songs sung at the dance that either foIlowed an initiation or at lodges during the

evenings that preceded the ceremony. Densmore noted that only those who had purchased

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the right to sing them could sing the songs. 0' déni' gûn, the shaman who sang these songs,

was, Densmore diseovered, "one of the most powerful medicine men on the White Earth

reservation" (ibid.). Unfortunately, it remains unclear who exaetly provided her with this

information on the seroils. Dewdney did not examine or mention either of these seroils in

his (1975) book on bireh bark seroils.

Scroll4:

Very little is known of the eontext in whieh the images on this seroil were ereated.

Although the photograph of this seroil was published by Dewdney (1970b) in eonjunetion

with a detailed discussion of several pictograph sites in the Canadian Shield, Dewdney made

little comment about the birch bark scroil, the photographs of whieh were also published.

Dewdney (1975: 141) asserted that this scroil was a "pharmaceutieal song seroil." How he

arrived at this conclusion is unclear. Dewdney stated that this seroil was one of several seroils

given to the Royal Ontario Museum by Francis Fisher, who was one of the last Midé from

the English River region of the Canadian Shield (Dewdney and K..idd 1967: 13). Dewdney

(1975: 147) found it while examining the large woven medicine bag whieh had been given to

him, possibly during the summer of 1960, "for safe storage in the Royal Ontario Museum"

after the death of its owner. Dewdney did not examine this seroil either in his (1975) book

on the bireh bark seroils or in his book with I<.idd published in 1962 and 1967. It is

surprising that he did not comment on this seroil. It would have been interesting to know

how Dewdney would have considered it, given the six categories of seroils, in his (1975: 21-

22) publication, based on variations in themes he had identified: (a) origin seroils, (b)

migration eharts, (e) master ri tuaI and seroils, (d) ghost lodge and sky degree, (e) deviant

seroils, and (f) en..igmatie seroils; and given his further assertion that the principal funetion of

the bireh bark seroil was mnemon..ie.

(cl) Meaning:

What do these images mean? Ideaily one would use the homologie al, and the direct

historieal approaeh, and construet bridging arguments between written data regarding the

physieal shape of images, their mean..ing, and the images themselves. This eould work

effeetively for the two seroils, number 2 and 3, since Densmore (1910) eoileeted a vast

quantity of useful information on the images on these seroils. Yet, since very little

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information exists regarding the images' mearungs on serolls 1 and 4, stating anything

eonerete about these images, or verifying any recent interpretations and readings given to the

images of both these serolls remains diffieult.

Vennum (1978) stated that any interpretation and understanding of a group of

images on bireh bark serolls ean only oeeur if one is capable of drawing upon a large body of

evidence related to eaeh partieular seroll and its specifie images. Detailed information must

exist; otherwise any conclusions beeome tentative. Vennum drew extensively upon work

eondueted by Blessing (1963) and his informants, who analysed the migration type of serolls

of the Mille Lae reservation. Vennum (1978: 788) asserted, based on Blessing (1963: 93-94),

Hoffman (1891: 290) and Densmore (1910: 26), that the images, whieh were mnemonies,

"were less generalized and their meanings seeretly guarded."

Landes (1968: 172, 224) had established that, if images were used on bireh bark

seroIls, only the shaman who ereated the seroll knew the specifie meaning of the images. The

"partieular message" of a seroIl, or, essentially, what the pietographs meant, was probably

impossible to establish unless the owner, who was also probably its maker, labelled or

translated eaeh figure. Hoffman (1891: 191-193) stated that a candidate eould learn the

meanings of these images only after paying his fee and preparing himself through fasting and

tobacco offerings. The Midé used serolls as mnemonic devices to remember the words of

their chants, for the instruction of new members, to record oral traditions, and to perform

correct ceremonial procedures.

Hence, each seroll and its associated images should be examined in conjunction with

a body of data that is seeurely connected with the seroll in question. It therefore makes sense

to eonsider the data at hand about the images on each scroll.

SeroU 1:

It is diffieult to know what the images on the scroll ealled the Massaere Scroil may

be. It would be really useful to know when the seroll was made, who made it, to whom it

may have belonged before it was obtained, and why it was obtained. The text on the baek of

the black and white photograph, in Jacqueline Rusak's handwriting, states that an Ojibwa

elder, whose name is unknown, interpreted the seroll as depicting the murder of La

Vérendreye's son, his eompanions, and Jesuit missionaries while they were holding couneil.

Their deeapitated bodies were found in a circle. However, various useful pieces of

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.r'.

information are unavailable regarding this explanation: the name of the elder who gave this

interpretation, the elder's status within the Ojibwa eommunity, whether the elder was Midé,

and the name of the elder's reserve.

This seroIl and its images were utilised by Reid (1979) in an attempt to date several

images at a number of petroglyph sites at the Lake of the Woods. Reid (ibid.: 250) relied on

an undoeumented interpretation by James Redsky, a Midé from Shoal Lake on the western

side of the Lake of the Woods, whieh was perhaps the same reserve or different to that of

the unnamed elder. It is impossible to establish from Reid's (1979) article how and whether

eaeh image was interpreted by Redsky beeause Reid did not clearly indieate whether he

eoIleeted this information. However, he (ibid.) did provide sorne information that Redsky

provided to him about sorne of the images on this seroIl

Redsky interpreted the bird-like shapes as a 'paisq'. He argued that this word eould

be roughly translated as "bird of omen" and that this image oeeurred three times on the

seroIl. Reid eonsulted Baraga (1992 [1878]: 354), a Roman Catholie missionary who ereated

the first Cree/Ojibwa and English dietionary, and learned that the word was 'peskwe' whieh

meant 'a kind of owl'. Reid (ibid.) observed that the paisq symbol for Redsky identified

"tragedies or undesirable events," If the "wings" are upward to form a "Y," the event was a

future one. If the wings were down the event had happened, and it eould not be avoided. If

the wings were to the side, as in the seroIl then the event was taking place. Redsky, Reid

(1979: 250) observed, interpreted the seroIl as "purporting to show the massacre of Father

Aulneau, La Vérendreye's son, and their eompanions in the Lake of the Woods."

Serolls 2 and 3:

The information gathered by Densmore (1910) on seroIls 2 and 3, provides more

signifieant clues to these images. She published sorne of the mnemonies, eaIled the song

pietures, for sorne of the shapes on these seroIls. She (ibid.: 97-106) provided the song

pieture that triggered the singing of eaeh song, the Ojibwa words and their translation, the

score of eaeh song, its tide, and her analysis of eaeh. Her information enabled eaeh image,

eaeh mnemonie, visible in both photographs to be identified as the ones whieh triggered the

songs to be sung. Both seroIls are presented, in figures 7.8 and 7.12 below, annotated with

white numbers and aeeompanying information so that sorne of the songs ean be identified.

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Figure 7.8: Seroll number 2 annotated by Cols on from left to right in 2005.

The shapes numbered 12, 13, 14, 15, 16, 17 are part of one song picture, in figure 7.9 below,

identified by Densmore (ibid.: 100) as the song called the "Song of Good Medicine".

SONG-:rJCT'Clt.L~,.'~' •. ~ dO·

reat.hürs are Sf,~(··n Hf:;\r

the 11lde'wlnl'11!.

Figure 7.9: Mnemonie for the Song of Good Medicine.

The shapes numbered 18, 19, 20, 21, 22, 23, 24, 25, 26 are another song picture, in figure

7.10, called the "Song of the Crab Medicine Bag" (ibid.: 102).

SONG l'TCT1Jl\E NO. 85.

The drawing Tepre­sents a Mîde' bag witlJ t'NO mi'gls be­sido il.

Figure 7.10: Mnemonic for the Song of the Crab Medicine Bag.

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The shapes cailed 28, 29, 30, 31, 32, 34 are part of another song picture, in figure 7.11 below,

discussed by Densmore (ibid.: 103) as constituting the "Song of the Fire-Charm".

fo'ONG PIGTURE NO. S6. The fiames are seen ascending froID a cl rcle of ftre.

Figure 7.11: Mnemonic for the Song of the Fire-Charm. SeroU 3:

Figure 7.12: SeroU number 3 annotated by Cols on in 2005.

It is possible to undertake the same procedure for scroil number 3 using Densmore's

information; it is evident that shapes 7, 8, and 9 are part of the song picture for the "Song of

the Owl Medicine" in figure 7.13 below.

SONG PICT"URE NO. 88. The Mïde'winl'nl', tIle man and l1is \Vife, are see-n in the wigvram,from which the owl is flying.

Figure 7.13: Mnemonic for the Song of the Owl Medicine.

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,------"

The shape on seroil number 3 known as number 10 ean be identified as the song picture for

the "Song of Starvation" (ibid.: 1 04) in figure 7.14 below.

SONG PICTURE NO. X7.

Figure 7.14: Mnemonic for the Song of Starvation.

The shapes numbered 11, 12, 13, and 14 on bireh bark seroil number 3 are identifiable as

integral eomponents of the song picture eailed "Song of the Man who Sueceeded" (ibid.: 98)

in figure 7.15 below.

SONG PICTURE NO. 82.

Figure 7.15: Mnemonic for the Song of the Man who Succeeded.

Scro1l4:

Unfortunately, it is impossible to state anything except that Francis Fisher, who had

been a Midé in the English River region of the Canadian Shield prior to his death sometime

after the summer of 1960, used this seroil. It is impossible to comment on any of the shapes

deseribed (see figure 7.16).

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Figure 7.16: ScroU number 4 annotated by Cols on in 2005.

(e) Conc1uding comments:

Differences in description between those who knew the song pictures and those with

little or no knowledge of how they should be used together must exist. Without the privilege

of knowing what these images mean, images are subdivided and dealt with in a manner that

could ultimately obscure their significance. It is very difficult to assign meaning to individual

birch bark scrolls. This may not matter since Vennum (1978) believes the researcher can

examine these images and scrolls in great depth only if he can draw on a large body of

ethnographically relevant information. If the body of relevant evidence for each scroll does

not exist, then considering these birch bark scrolls as documents, as Vastokas (1996: 55)

advocates, becomes problematic. It becomes impossible for the historian to ask the pertinent

questions of them: who made the scroIl, who created the images, why were they created, for

what purposes, and what was the date that the scroll was made. However, should this body

of evidence exist, it is still impossible to successfully provide a date for the document, the

scroll.

Section 3: Efforts to treat rock image combinations as stories.

It is very difficult, if not impossible, to determine whether the images on birch bark

scrolls have shifted in meaning. Examination of the images on the scrolls number 2 and 3,

collected by Densmore, indicates that images sometimes occurred together, although this

was unclear without examining the drawings of several of the songs. Additional information

on the images indicated the songs enabled one to identify which images occurred together.

However, at some of the pictograph sites in the Lake of the Woods where collections

of images exist, some of the images have been given new meaning, and they are considered

as connected, as stories. This contradicts the results discussed in Chapter VI, where it was

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concluded that definite patterns did not exist between the different images, despite using a

nested classification. The images on the pictograph sites in the Lake of the Woods do not

have a commemorative strain, but new meaning may have been attached to them at five sites:

DhKm-3, DiKm-4, DgKm-l, DhI<n-1, and DhKo-1. Each site is examined in sequence to

demonstrate how new meaning has been applied to the images at site.

(i) DiKm-4:

This site was interpreted by Ann Seymour, the Director of the Lake of the Woods

Ojibway Cultural Center in Kenora in 1990 (Anonymous 1990a: 10). The annotated

photograph, in figure 7.17, isolates each of the images to clarify which image Seymour

discussed. She stated that the images at this site indicated that "someone took a long and

difficult joumey that lasted a month. The snaky line denotes the journey and the crescent

beside the encireled he ad denotes the moon - a month." It was coneluded by the writer of

this short article, who spoke to Ann Seymour, that the journey taken was "a happy story"

and that the "Cirele of Heaven on the pictograph tells us that the journey was successful"

(ibid.).

Figure 7.17: The shapes at DiKm-4 according to Ann Seymour.

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(ii) DhKm-3:

This site has been named the Grand Medicine Society (Anon. 1990b: 3). Seymour

also interpreted several of the images at this site. She asserted that the turtle was "Miknik"

the messenger or translator between the spirits (manitous or manido) and the people (ibid.).

A similar statement from Seymour exists in Rajnovich's (1994) publications as weil as the fact

that the turtle was the translator because they spoke many languages (Seymour in Rajnovich

1994:36). Seymour argued that the spiritual aspect of the turtle was indicated by the two

horizontallines across its back. She interpreted the shape between the lattice and the turtle as

a snake and "offered the suggestion that the snake was somebody's name" (Anon 1990b:3).

The lattice for Seymour depicted the degree to which the painter of the rock image site

belonged sin ce the lattice was the sign of the Midewiwin Society (Seymour in Rajnovich

1994: 32). The shapes that Seymour described are indicated in figure 7.18 below.

Figure 7.18: The turtle, snake, and the first lattice discussed by Seymour at DhKm-3.

Redsky, from Shoal Lake, on the western side of the Lake of the Woods, was apparently

asked for his opinion of these images. He interpreted the turtle shape as Miknik "the

messenger" and argued that the lattice figure was the sign of the Midewiwin. The snake

shape was interpreted as possibly the "Great Spirit and Lightening" (ibid.). The photograph,

in figure 7.19, illustrates the rest of the images interpreted at this site by Seymour.

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Figure 7.19: The thunderhird, Hne, handprint, lattice, and the human figure with hands raised upwards at DhKm-3 identified hy Seymour.

The writer of trus text stated that another lattice figure occurs with a figure that Seymour

described as "a human figure with hands raised" (ibid.). Seymour interpreted the hand print

to the right of trus image "as signs for the death of a warrior." The bird visible in figure 7.19

she interpreted as a thunderbird, and the zig-zag shape connected to it as a communication

line or a "power line to the heavens" (ibid.).

(iii) DgKm-1:

This site, in figure 5.99, has been used in a land daims proposaI for an area of land in

the Sabaskong Bay area (Ross pers. Comm. August 2001). No additional statements have

been obtained as to how any of the images at trus site have been interpreted.

(iv) DhKn-1: An eIder at Manitou Rapids, a reserve to the southeast of the Lake of the Woods,

interpreted the images here (Reid pers. comm. 2005). Their interpretation was subsequently

published in a guidebook to the Lake of the Woods although it was not acknowledged in the

publication Qackson 2000: 112). The images, in figure 7.20, were described as follows: a

turtle wruch is symmetrically faced on either side by two serpentine figures. One of these

serpentine figures is described as having antlers while the other has horns.

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Figure 7.20: An annotated photograph of part of DhKn-1 demonstrating the images discussed.

To the left of both of these figures is another creature identified as a serpent which has an

open mouth, ears, and three long flippers.

(v) DhKo-1:

An altemate interpretation of the images was given to some of the shapes at DhKo-1

on Picture Rock Island (figure 7.21) in the same guide book as the interpretation for DhKn-1

(ibid.).

Figure 7.21: An annotated photograph of DhKo-1.

The creature shape in figure 7.21 has been interpreted as a sacred bear, possibly representing

a "powerful Midé leader" (ibid.). This image is "connected by a series of rectangular forms

with paths between some" but, unfortunately, it is difficult to determine what this means.

Several of the shapes were described as lodges, while one of the figures nearby was identified

as a human figure. Since a drawing demonstrating these speculations was not provided, it is

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impossible to ascertain the precise location of the lodges and the human figure. A horned

figure exists in the centre of the site, and to the lower le ft right hand of it, another image, a

"horned serpent-sturgeon" that has projecting spines along its back.

Conc1uding remarks:

The above discussion clearly demonstrates that people ascribe meaning regardless of

whether they created the images or whether or not they can rely on written or dated oral

information. It was impossible to establish the meanings of the new images at DhKm-19 and

DhKm-20, and the new images placed on the older images at DgKI-2. One person's signing

of the new images at DhKm-20 suggests that the rock image sites were given meaning by

one individual, rather than a group of people, and do not have meaning beyond the

individual. However, the new meanings given to other images at the sites discussed in this

section indicates that these images have been integrated into the lives of sorne of the people

who currently live in the region.

Section 4: The continuing importance of the images and sites.

Similarly, specifie places are still important to the native peoples who live and work in

the Lake of the Woods. Perhaps new shapes have been added to the graphie vocabulary

because newer and very professionallooking images were found in 2001 at DgKl-2, DhKm-

19, and DhKm-20. There were seven shapes painted using modern paint, but only four of

these are new to the vocabulary evident in the dataset of the Lake of the Woods. Both of the

shapes at DhKm-20 were new but the shape at DhKm-19 was one of the three turtles

located in this region. Otherwise, ail of the newer images are radicaily different from the

images elsewhere. At DgKI-2 four new images are in modern red, painted over and beside

oIder images created using ochre:

1) a creature with head, with horns or ears or antlers and a pair of front and

back legs, facing right

2) star

3) unidentifiable shape, hoilow body outlined by lines

4) vertical crescent with points facing right

Ail of these images except for the third image listed above were superimposed on an older

ochre smear which is visible in figure 4.4. Dewdney first recorded this site in 1964, at which

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time these images were not present. These new images were also absent when Pastershank

recorded the site in 1989. Although these are new images, theyare similar to the older images

at other sites. These new modern images, however, differ from the other new images at

DhKm-19 and DhKm-20, sites unknown to archaeologists prior to 2001. Ali the images at

both of these sites were made without ochre, using modern paint.

An individu al named R. Bird signed and dated as "1982" the red, blue, and white

images at DhKm-20 (figure 5.141). These images strongly resemble those images in paintings

and art objects created by members of the New Woodland School of Art. This School was

founded by Norval Morrisseau who drew on Ojibwa beliefs and traditions. This movement

developed in the late 1960s in Northwestern Ontario and, according to Trevelyan (1989: 188),

"came of age" in 1983, when the Art Gailery of Toronto mounted an exhibition of the works

made by members of this group.!

Trevelyan explored several ideas but one of them in particular should be considered.

She (ibid.: 198) argued that art was a vehicle for the transmission of new ide as and she also

posited that the development of this school was a response to a cultural crisis among the

native community.

The image of the turtle at DhKm-19, in figure 5.160, is readily identifiable as a turtle

painted in black and green paint. It does not bear as strong a resemblance as those images in

DhKm-19 to the works of New Woodland School of Art. It is possible to argue that these

new images are probably professional; they bear a strong resemblance to those found in the

artworks of this school of art.

Conclusion:

The results of the analysis of the four birch bark scroils indicate that it is impossible

to ascertain the identity of particular songs, mnemonics, without a body of data that is

reliably connected to the birch bark scroils in question. However, this study did suggest,

based on stylistic differences in the types of images, that the images on the pictograph scroils

probably had different functions and uses. 1 have already disagreed with Vastokas' (1996: 55)

1 Morrisseau's colleagues included Daphne Odjig,Jackson Beardy,Joseph Sanchez, Eddy Cobiness, Alex Janvier, and Carl Ray. These individuals have influenced two generations so that the works of Arnoo Angeconeb, Shirley Chee Choo, Blake Debassige, Don Ningewance, Leland Bell, and Carl Bearn are known internationally beyond the region north of Thunder Bay, Ontario.

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opinion that birch bark scroils should be considered as documents unless there is detailed

ethnographic description. Her suggestion that these scroils should be considered as "cultural

expressions" is valid.

However, as with the images of the pictograph sites, describing these images must be

undertaken with considerable eare and thought because it is dearly very diffieult to deseribe

an image. It is very easy to be subjective, rather than objective about them and to gloss over

minute details.

It is evident from the comparison of Dewdney's drawing of the scroil (1975: 141) and

its photograph (1970b) that he made nine transcription errors. Mistakes in tracing inevitably

occur, and the cultural perspective of the individual describing the shapes must be

acknowledged.

Vastokas makes two interesting points, both of which are difficult to sustain. She

posited that, as records of Aboriginal history and an historical source of "writing without

words," scroils acted as "representations" of events that took place over time and space

(ibid.:). Vastokas (ibid.: 56) advised establishing "pictorial conventions" but, unfortunately,

she did not provide any dues as to how to undertake this task.

It would have been useful if she had articulated precisely how she thought this goal

could be aehieved. l am forced to argue, based upon my small sample of the four birch bark

scroils, that very little can be achieved regarding the meanings of these images without a

substantial body of ethnographic information historicaily connected to the scroils. Vastokas'

(1996) paper is important, and her ideas are theoreticaily good but they represent an ideal

researeh situation that is rarely aehievable.

The red images on the pietograph sites indieate that the Algonquian-speaking peoples

used, and stiil use, different shapes for expression, but establishing the fuil range of image

combinations is impossible. Meanings of the images on the rocks are not readily obtainable,

and common sense is no guide; it depends on intuition. Their meaning cannot be ascertained

without verbal intuition. Since the number and type of images is so smail, and the people few

in number, the groups of Algonquian-speaking peoples probably were too small to have had

several specialists using different types of images. The wide range of shapes, the differences

in the range of shape type used, in eonjunetion with the physical differences between rock

image sites and those of bireh bark seroils, suggests that graphie voeabulary was not only a

product of speeialized image makers but was widely shared. It is possible to eondude that

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the images on the pictograph sites had meaning attributed to them at the individual level

rather than the group level.

Although it is impossible to ascertain the meaning of the images and the pictograph

sites, the continued practice of leaving offerings at sites such as DhKm-l proves that the

physical location of these sites held, and holds, considerable importance for sorne of the

people of this region. What les son do we learn from the examination of birch bark scroils for

those of the pictograph sites? First, these images are combined in a manner obscure to

someone uninitiated in the graphic vocabulary involved. The images of the scroils are more

complex than those of the pictograph sites. Second, only drawing on a detailed body of

ethnographie, eontextual literature direetly eonneeted to the images and the seroils in

question made establishing the eombination and meanings of the images possible. The body

of information required to identify and even start to grasp the meaning of the pictograph

images has been lost and forgotten. Perhaps those who may have used it never coilected it,

since the coilection of information regarding images the Midé made possibly was perceived

as more important. The third les son is that the role of the creator or creators with regard to

the images of the pictograph sites has been forgotten. The lite rature appears to lay too much

emphasis on subsequent twentieth century observers, espeeially on the viewpoints of

archaeologists. Finaily, care must be taken with regard to using ethnographic, and

archaeological sources for establishing the meaning of these images and the sites.

Sorne level of choice probably existed for the selection of a location and the images

used for a pictograph site, explaining why so few of the pietograph sites that had images had

ail of the five "required physieal features" (see section 1, Chapter VI). The "required physical

features" were likely unimportant in the creation of images (see Appendix 15). The images

probably were created over a long period of time by individuals and not by ritual specialists.

Hence, the importance of these features has either changed, shifted, or been mistaken.

Regardless, of their current significance it is the fact that they exist that is important. These

images are weil known by the archaeologists, the anthropologists, and the art historians and

by the local indigenous peoples. Essentiaily, everyone is talking, reading or conversing with

each other. Therefore, the information that images should occur with five specific physical

features has become an established fact, and so offerings are left where a large proportion of

the five features are present in conjunction with images. The present day indigenous

Algonquian-speaking peoples are interested in these images. Sorne of the images at several of

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the sites have been re-interpreted. Those who currently live in this region have integrated

these archaeologically and historically important places into their mental and physical

landscape. The presence of the images in modern paint on older ochre images, and new

images at new places in the landscape suggests that images are still used as a means of

communication, and that they are integral to gaining an understanding of the archaeological

and rustorical record, and of the present day.

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('

Chapter VIII: There is no Holy Gran: An Obsession with Meaning.

Introduction:

Wright (1981) described the Subarctic as a forbidding landscape challenging to its

pre-contact human occupants. As l argued in Chapter II, successful occupation of this region

requires a comprehensive understanding of its seasonally dynamic ecology, water

transportation routes, seasonal climatic extremes, and a host of hidden dangers, risks, and

opportunities. To interpret the placement of archaeological sites of different functions across

the landscape, the investigator must understand the complexity of past land use, the regional

geography' s physical nature, and the everyday challenges past occupants faced. The

archaeologist must become personally immersed in the site's physical geography and context

since, in the now more heavily populated Lake of the Woods, many of these considerations

are integral components of the process of conducting archaeological field investigations.

To travel, live, and work in the boreal forest requires a high level of technical skill,

intra-group co-operation, self-reliance, and understanding of the physical environment in all

its complexity. Even during the height of the summer, sudden weather changes, and relative

isolation require 'bush skills,' awareness of one's surroundings, and teamwork. Careful and

thorough preparation must precede any expedition to a site, even in the first years of the

twenty-first century. As a outsider from the twenty-first century with the advantage of

technology, one still must make compensations and have the challenge of maintaining a keen

awareness of how it might have been in the pasto

An archaeological field investigation, even one serviced by a large motor boat,

requires careful preparation and a wary respect for the dangers associated with travel on

waters such as Lake of the Woods. Three people might be required for such research treks:

one to operate the motor and drive the boat, another to navigate the safest course through

intricate channels, and the third to serve as a general lookout. The water surface must be

constantly scanned for deadheads [floating or semi-submerged logs], the next navigation or

hazard buoy, for tell-tale signs of submerged reefs, and especially, swimming bears, moose

and other hazards. Even short journeys require a careful review of the charts before setting

out, preparation of equipment, and consideration of weather conditions expected over the

course of the day. Such considerations would be even more critical for travellers in small

canoes.

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r--..

As we travelled, we "read" the lands cape so as to de te ct the precise location of a

pictograph site. Our preparation enabled us to identify tell-tale signs. This is especially

difficult when travelling through a lands cape that can look surprisingly undifferentiated to

even an experienced traveller on the lake; becoming lost was never difficult. The charts,

although recent and glossy, are "idealizations." Ultimately, not getting lost depended much

on our ingenuity and ability to find destinations represented by nothing more than dots on

small-scale maps.

To travel at 35 kilometres an hour on Lake of the Woods is to live life in a blur. The

different greens of the coniferous and deciduous trees blend in with the greys of the granite.

Rapidly changing weather conditions can obscure distant landmarks, and make it difficult to

traverse the intricate channels and travel corridors through the lake. At the same time, the

water's surface can change rapidly From a dear turquoise, dark grey, to a deep blue,

depending on the douds, the wind and the rain. The dear distinctions between different tree

species varieties become ever more evident, the granite's strata increasingly marked as we

slow to a haIt. The intricate mosaic of leaves becomes identifiable as a myriad of plants, and

startling contrasts in the colour intensities of the granite rock surfaces emerge as individual

outcrops. As we advance toward our shoreline of interest, and slow the boat's engine until

we almost drift, it becomes easier to examine the rock's surface and to search its physical

features for any traces of red pigment concentration: the pictographs themselves.

An important observation, arising as a consequence of my fieldwork and analytical

work, relates to how archaeologists deal with the sites and images. The action, especially by

archaeologists, of offering tobacco at ail the places with paintings implicitly implies that aU

the sites have, and had, the same meaning for aU of the local indigenous peoples. This

assumption must be questioned, especially since offerings were not found at aU of the sites

examined. It is possible that tobacco left may have blown or washed away. It is equally

possible that not aU places with paintings may have had the same enduring spiritual meaning

among local Aboriginal residents that sorne of them appear to have today. It may be that

offerings are le ft at different sites under different circumstances. Whether the archaeologist

finds offerings there or not may be entirely coincidental timing between his visits and other

individuals visiting and using the site.

Were and are these rock paintings always considered spiritual? Or are the places and

not the painting spiritual? Leaving tobacco at aU of the sites presumes that aU of the places,

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or the paintings, have and have had the same meaning(s). It is possible that these images

and/ or the rocks on which they exist once had a spiritual significance but, unfortunately, the

oral tradition documenting that character has been lost in the face of acculturation, or is

impossible to securely establish.

Ethnographie literature exists concerning the practice of offering, or giving, tobacco

in exchange for information in a wide a variety of scenarios (see Chapter V), but secure links

between the offering of tobacco with sites do not exist in the literature for this region until

the early twentieth century (Colman 1947; Hilger 1936). Only towards the end of the

twentieth century did Pufahl establish through his informants at the Eagle Lake Reserve,

near the pictograph sites he was studying, that the local indigenous community considered

these sacred sites that "routinely receive[d] offerings of tobacco" (1990: 19). Five years later,

Smith (1995: 33) argued that the use of tobacco was a sign of respect between humans and

the manitous and maintained it was common practice to offer either loose tobacco or

tobacco in the form of cigarettes to EIders.

Now, it is common practice amongst archaeologists to make an offering of tobacco

once the images at a site are distinguished but before recording the site. A pinch of tobacco

is taken out of the packet of loose tobacco and scattered on the surface of the water

immediately in front of the images, or left in a crack or crevice in the rock face in the

immediate vicinity of the images. This is to pay respect to the spiritual character of the site in

line with instructions from Aboriginal EIders. But not ail pictograph sites had evidence of

previous offerings of tobacco when they were examined in 2001. This might be because the

archaeologists left the tobacco on the surface of the water, rather than in a cleft in the rock.

Or it might be that tobacco left by other people, such as local Algonquian-speaking peoples,

had decayed, blown or washed away.

My crew and l always sprinkled tobacco onto the surface of the water but other

archaeologists do different things with the tobacco. When l first started fieldwork in

Northwestern Ontario, Rusak, Pastershank, and Reid (pers. comm. June 1991) advised me to

leave such offerings at sites. Rusak invariably left some tobacco either on the water's surface,

or in a crack, or crevice when she did fieldwork (ibid.).

Regardless of this practice, the vast range and quantity of o fferings , including

tobacco, suggests that some of the physicallocations and/or paintings stiil remain places of

visitation. Some groups of people other than archaeologists are leaving, and have le ft, these

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offerings. Anthropologieal and ethnographie writings establish that gifts of objects such as

tobacco or other articles are often given to supernatural beings to obtain spiritual benefit,

especially in a ritual context. Archaeologists argue that the offerings found at sites and

discussed since 1885 suggest that each possesses sorne ritual significance. Archaeologists

examining pictograph sites in the Lake of the Woods (Fox 1974; Dewdney and Kidd 1962,

1967; Lambert n.d., Pastershank 1989; Reid 1975, 1976) always seek objects left as offerings

ab ove water.

It is impossible to establish however, the precise nature of these red images, the

pictographs. It is unclear whether they held any religious symbolic significance. It is possible

that the paintings were simply used as forms of communication.

Therefore this practise of leaving offerings by archaeologists may be something of an

'invented tradition'. After all, these archaeologists are not usually indigenous Algonquian

speakers. Their actions may arise from a reading of ethnographic sources, or perhaps the

advice of previous archaeologists. Essentially circularity exists here since the archaeologists

were told (or believed) that painting sites are spiritual places. The action of leaving offerings,

such as tobacco, is a means of paying respect to the Ancients [the antecedents of the current

indigenous peoples] and honouring and respecting the beliefs of contemporary traditional

believers. In actuality, the archaeologists have been blinded by their actions to possible other,

and more secular meanings, of the rock paintings.

Invented traditions are, of course, nothing new. In introducing a well-known

collection of essays on the subject, Hobsbawn (2003: 9) identified three types of 'inventions,'

all of which seem to have emerged in the wake of the indus trial revolution, coinciding with

the dawn of modern archaeology. He identified these overlapping 'inventions' as:

a) those established or symbolizing social cohesion or the membership of groups, real or artificial communities, b) those establishing or legitimising institutions, status or relations of authority, and c) those whose main purpose was socialization, the inculcation of beliefs, value systems and conventions of behaviour.

(Hobsbawn 2003: 9)

From this powerful observation he later argued that:

the study of invented traditions cannot be separated from the wider study of this history of society, nor can it expect to advance much beyond the mere discovery of such practices unless integrated into a wider study

(Hobsbawn 2003: 12) Leaving tobacco as an offering, the archaeologist ascribes an importance that may

not exist to the site. Archaeologists may be creating a tradition by continually depositing

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tobacco at pictograph sites, especially at those that are newly discovered. We cannot establish

the precise significance of the places where the images occur, and we cannot securely ascribe

a meaning to them. Meanwhile these sites, their images, and the invented traditions are

probably being inexorably incorporated into the lives of the sorne of the local Aigonquian­

speaking peoples.

It is very difficult to quantify the level to wruch these sites are used today. It may be

that only a few people from a few reserves use and know of a few sites in sorne parts of the

region. Indeed, the presence of new images at previously known pictograph sites and the

existence of newly discovered sites with images not made using ochre demonstrates that

these images and their sites are being utilised and integrated.

What has been going on here?

My fieldwork was carried out in 2001. The number of images extant on a site bore

little relationship to the presence of offerings. A site could have a large number of images yet

no offerings. The physical proximity of a pictograph site to an Indian reserve also had no

influence. There also was no relationship between the orientation of a site, the landmass on

which it was located and the existence of offerings. Yet the fewer the number of those

"required" physical features present at a pictograph site located on a cliff site, the less the

likelihood of offerings being found. By liberally distributing tobacco are we not manipulating

our own evidence? We are not referring to the artefacts, rather to the relationsrup between

the individuals looking at the site. By following the advice of archaeologists to leave tobacco,

a researcher acknowledges the dignity, legitimacy, and value of that 'other world' to wruch

the site may belong. The archaeologist arguably enters by the act of 'exchange' since no

information can be obtained without the prior offering of tobacco. A complex bridging

argument is involved so that we can assume that the Algonquian-speaking peoples who

currently occupy the region have a long rustory of association with the sites.

Are we perhaps being hoodwinked by the fact that the sites contain 'pictures' or 'art'?

That is after all what the sites are called, in both the popular and academic literature.

Regardless, the principal artefact examined in trus the sis is an image. Images are neither

flakes, nor pot-sherds, nor bones. Images are vectors of information, like lithics, bones, and

ceramics. Each has its unique methods by wruch it can be described and subsequently

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analysed. The image is a form of communication, and deserves the same consideration, at the

same time as the tool, the bone, and the pot-sherd. AIl must be considered as equaily

important, and possibly even integral to each other's context.

Perhaps the problem is that we do not know the stage at which images were utilised

as forms of expression or as a means of simple communication. It may be that images have

been mislaid or ignored because the emergence of lithics, ceramics, and bones can be more

easily cross-referenced, subsequently documented and incorporated into the archaeological

record. In order to carry out a rigorous examination of an archaeological phenomenon, we

must draw upon increasingly large bodies of disparate data. This is especiaily true of an

image, which is perhaps best understood as a multimedia event, with different multiple

sources, multiple meanings, and sequenced approaches required. Such approaches are

inherent to the application of a range of digital technologies.

This is not surprising, for, as a draft recent report of the Cyber Information

Committee established by the American Council of Learned Societies argues,

a critical mass of information is often necessary for understanding both the context and the specifies of an artefact or event, so that often a very large datas et of multimedia content-image, text, sound, moving image, audio-is required. Humanities scholars are often concerned with how meaning is created, communicated, manipulated, and perceived through discourse. Recent trends in scholarship have broadened the definition of what faIls into the category of discourse, and many scholars formerly comfortable working only with texts now turn regularly to architecture and urban planning blueprints, art, music, video games, ftlm and television, fashion illustrations, billboards, dance, videos, gesture, graffiti, food, rituals, as weil as blogs. While difficult to achieve, the value of critical mass or functional completeness is easily demonstrated. The Shoah archive has a signal authenticity in large part because it is so comprehensive. The tale of what happened to one or two familles, in one or two villages, in one or two countries, during the Holocaust is worth recording and disseminating-but how much greater is the knowledge we gain from the completeness of the record.

(The Draft Report of the American Council of Learned Societies' Commission on Cyberinfrastucture for Humanities and Social Sciences 5 November 2005: 27)

The need for academic rigour is paramount with any object, especiaily with images, and it is

attainable in this digital age.

Images are important sources of information, vectors that, as noted in the quotation,

have been abandoned in favour of text or script. If we continue to charge ahead because we,

as humans, want to know their 'meaning' without using a disciplined, quantitative and

qualitative approach, we will achieve very little. By the same token, each of these data related

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~ ....

to an Image can be stored in digital format now, and, therefore, can be manipulated

according to well-defined and standardised rules and practices, often formally documented,

e.g., by the IEEE. We can go some way to understand and to document the contexts of

images and how both have changed.

Images are such important vectors of information that some, like the Swastika, or

Madonna, are swamped with different contexts, and with evidence pointing to different

points of view. Others of the very distant or not so distant past ean laek such compelling

detail. The image known as the "Marlboro Man" is a powerful ieon invoking the mythical

Ameriean eowboy and masculine trademark. This image assisted in establishing Marlboro as

one of the world's best-selling cigarette brands (MacKenzie Ward pers comm. 1991). The

image known as the Swastika has a long history, a variety of contexts, and many implicit

meanings throughout the world. Someone could use the word 'Madonna' and think that

everyone knew implicitly they were referring to Leonardo da Vinci's painting ealled the

'Dreyfus Madonna' held by the National Gallery in Washington, De. Yet, it is equally

possible that one could think of a photograph of the pop star called Madonna. Indeed, the

manner in which images are utilised can differ extraordinarily from century to century, and

between cultures and peoples.

Iconographic disjunctures are probably commonplace. In today's world if someone

cannot read text, they will probably rely on pictures or diagrams to help them 'read' and

understand, as mu ch as possible, about these images. Images are very powerful in the

manner in whieh they ean convey a vast amount of information without words. As human

beings we want to 'read' images, establish their meanings and understand them.

To understand the image, the pictograph, as a source of information reqwres a

different way of thinkingl. It involves drawing on all of the disciplines that use images as

sources of information: art history, new art history, anthropology, and history, not just

archaeology. Eaeh uses images in a fundamentally different manner. Yet, the study of rock

images has fallen to the domain of archaeology because they are found on the surface of

rocks, and not on clothes, eanvases, portable objects, or paper documents loeated in archives

or collections.

1 1 cali, as 1 argued in Chapter 1, the images on rock faces shapes not morphs unlike my predecessors Rusak (1991 b), Pastershank (1989), Rajnovich (1987& 1994), Reid (1979), Lambert (1983, 1985, n.d.), Dewdney (Dewdney and Kidd 1962).

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Any comprehensive interpretation of visual evidence necessitates crossmg

disciplinary boundaries and dealing with different perspectives. This perspective is defined

and exists in the manner by which an individual perceives and organises the world according

to (a) the way in which the individual has been educated and (b) the way in which the culture

that they belong to organises and perceives this world. Every individual is trained and

educated to organise information into categories so that new ideas, concepts, perceptions,

beliefs, essentially information, can be processed, used and stored in manageable units.

Evidence, whether visual, oral or written, can be interpreted, manipulated, and used in a

variety of ways. Each scholar, regardless of discipline, has a number of generic questions to

ask of documentary evidence. Each discipline employs its own techniques to gather

information, draw on disparate types of information, ask a distinct set of questions, and,

perhaps, arrive at different conclusions.

So, the tobacco is scattered and work can begin. It now remains to summarise the

remaining three sections of this chapter. The first is the summary of the findings and a

discussion of whether the goals established at the beginning of the the sis were achieved; the

second section considers the theoretical and methodological implications of this thesis; and

the third and final section considers further research.

Section 1:

The goal of this the sis was to conduct a systematic, detailed, and thorough

examination of the images of the pictograph sites in the Lake of the Woods region to (a)

as certain a possible vocabulary of images, (b) determine whether combinatory rules exist, (c)

establish the life history of each site, and (d) learn whether the images can be related to other

images outside rock image sites and discover whether this can help provide information

about meaning.

As addressed m the conclusion of Chapter II, the information required to

contextualise the pictograph sites in the Lake of the Woods derives from a variety of

disciplines. Considerable agreement exists about the climatic changes and geomorphologic

history of the region. However historians and archaeologists find it difficult to agree about

who has ever lived there, in part, because each discipline uses different types of evidence to

tackle this problem. Our understanding of the archaeological record of the boreal fore st is,

unfortunately, a "rather nasty, messy, and simplistic culture-history" (Hamilton pers. comm.

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October 2000) and the paucity of work conducted in this region compared to others in

North America is probably a consequence of the physical isolation, vegetation coyer, the

harsh climate, and the sedimentary depositional environment. Unfortunately, the inadequate

archaeological data from the boreal forest region, in conjunction with the scanty historical

references to the individual groups who lived in this region prior to contact, at contact, and

during the early historic period, inhibits scholars from identifying the terri tories of various

groups. The problems resulting from different names for the same groups could perhaps be

resolved by the careful use of historical documents and the identification of synonymous

designations.

However, during the early seventeenth century, the Siouan-speaking Assiniboine

resided seasonally on the western half of the Lake of the Woods and continued to do so until

the middle of the eighteenth century (Heidenreich 1987: Plate 37). Throughout this period

Algonquian-speaking peoples lived in the eastern portion of the Lake of the Woods and

gradually took control of the region as the Assiniboine moved westwards (Heidenreich and

Noël: Plate 40). From a letter written by La Vérendreye in 1736, scholars know that Siouan­

speaking peoples were in the region at the same time as the Algonquian speakers. Since the

early part of the eighteenth century, the Assiniboine were allies of the Cree against the Sioux,

although the Assiniboine are linguistically closely related to the Sioux (DeMallie & Miller

2001: 572). It also, so far as discussed in Chapter II, has proved impossible to determine

which specific groups of Algonquians, Cree or Ojibwa, lived in the region between Lake

Superior and Lake Winnipeg. Both groups shared a similar symbolic system. No solid

evidence exists as to whether the Cree or the Ojibwa created the images at the pictograph

sites of the Lake of the Woods region. It is easier to conclude generically that the

Algonquian-speaking peoples made the se images, than to try to ascertain whether one culture

or the other created them. It is possible to posit that the Algonquian-speaking rather than the

Assiniboine-speaking peoples created them, since the rock images in the Lake of the Woods

strongly resemble those of sites elsewhere in Northwestern Ontario where groups of

Algonquian-speaking peoples are known to have resided (This question was considered in

considerable detai! in Chapter II.). The rock images created by the Assiniboine are very

different from those created by Algonquian-speaking peoples in Northwestern Ontario (e.g.

Keyser and I<lassen 2001; Keyser 1977; Greene 2001). Chapter II also clarified that the

Algonquian-speaking peoples used groups of different images for different purposes than the

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Assiniboine. The physicallocation of sites in the Lake of the Woods also fits into the general

Algonquian pattern of where rock image sites occur in Northwestern Ontario. 1 argued from

culture-historical data, for using general Algonquian cultural data to interpret the rock

images. This warrants using the AIgonquian ethnographic data to interpret the meaning(s) of

these images, and, hence, justifies using homologies for considering the meaning of the

images which occur in Lake of the Woods.

First Goal:

The first goal of establishing a possible vocabulary for the images, unfortunately, was

not achieved. Chapter III revealed that scholars disagreed on a classification scheme for

describing these images. Description of the images is highly subjective, and the vocabulary

used influences interpretation. Each researcher tends to use his/her own system. Images

often were interpreted rather than described, and, so, 1 decided to think very carefully about

how to record them.

As 1 argue in Chapter IV, the archaeologist should first describe, not interpret the

evidence. This operation involves thinking very carefully about how one describes images,

since any description affects subsequent analysis. It entails not imposing any interpretation

based on their physical shape. The rock image shape must described objectively and in detail.

Images can be organised and discussed by their shape. As 1 argued in Chapters IV

and V, this task is crucial since we lack an understanding of the grammar, punctuation,

sequence of painting episodes, degradation, and the information loss regarding painting

episodes. A rock image must be considered primarily as a shape because this reduces the

possibility of investing description with meaning during the recording stage. Understanding

an image's physical outline, form, and structure before discussing its context or meaning is

vital for archaeologists. When describing a shape, reference its form and nothing more.

Meaning is something to be ascribed at a later stage, using either the analogical or the

homological approach, or a combination of both (see Table 1.1 in Chapter 1).

The discipline inherent in the use of digital technologies plays a vital role lU

marshalling the evidence when this method is employed.

Chapter V discussed and applied the culture-historical approach to this data, and

established the total range of images, drawing on the insights provided in using digital

technologies.

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Image analysis usmg software, discussed at length in Chapter IV, such as Vasari

Image Processing Software (VIPS) and Adobe Photoshop 6.0 indicated the fragility of the

sites and their images, as weil as their changing nature. Adobe Photoshop 6.0, an image

manipulation software package, revealed that a limited range of motifs appeared in the rock

image sites. It also provided sorne insight into the way hum an beings perceive a physical

shape. Close examination of each image revealed that perception of the precise physical

shape of an image could depend on the viewer, rather than on the presence of red ochre.

The VIPS software permitted me to examine each image individually, and confirmed this

observation. The software revealed that shapes often lacked clear, sharply defined edges. It

highlighted the role that the hum an eye and brain play in the process of recognizing images.

The creator did not deliberately blur the shape's boundaries to impart an 'effect'. Post­

depositional image degradation, a component of site taphonomy, is creating 'visual tricks' on

the analyst.

This role is most clearly evident when usmg a procedure described in detail in

Chapter V. U sing the VIPS software, a specific image could be isolated from its context on

the surface of the rock and viewed against a black background, divorced from its original

context. The edges of a group of white pixels that once constituted the red image were not

clearly delineated, and the centre of an image was not solid white; the images were not solid

blocks of red on a grayish granite surface. The VIPS software also helped to establish

whether images were superimposed over white mineraI deposits which, in turn, were

superimposed over other red images at sites such as DhKm-5.

We do not understand the graphic grammar, punctuation, the degree of degradation,

or the sequence of painting episodes. This work emphasises the need for sequence,

objectivity, and the requirement for multiple tools [cross-referencing], and has powerful

implications for a discussion of analytic techniques routinely employed in the analysis of

lithics, bones, sherds and images. Above ail, it emphasises the need for rigour in achieving an

understanding of images as a means of communication.

A total of three hundred and eighteen images were recorded; an average number of

eleven images per site. The deposition of white mineraIs, lichen, and rock tripe

encroachment, and exfoliation of the rock surface that have taken place over time has caused

the images either to fade or be destroyed. These images, or shapes, are not static and

timeless. Given that the images are on rocks exposed to the elements, they start to

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deteriorate and begin changing shape soon after they are created. Consequently, it is

impossible to establish the full range of combinations of images once present. The narrow

range of image types found in the Lake of the Woods area contrasts sharply with the popular

belief that a relatively large vocabulary of images was used.

It is very difficult to classify and describe any image, and the level of description

given to an image dramatically affects the way in which it can be analysed. It is possible to

classify the images differently. The vocabulary used will influence heavily the outcome of any

discussion of perceived style. It is important to take the middle road between the "splitter"

and the "lumper" approach. A nested hierarchy of types, sequentially examined, probably

provides the most options with respect to subsequent classification. l tried to take a middle

road between the "lump ers" and the "splitters" but large numbers of loosely categorised

types of images e.g. 'creatures' in conjunction with a relatively small quantity of images in the

entire datas et made identifying combinations of specific image types problematic. If aIl the

extremities of a shape such as 'creature' were ignored, it would be possible to simply describe

it as a 'creature.' But this gives the impression that aIl the twenty-three shapes that are

'creatures' are physically the same shape. However, if one closely examines the photographs

of each image (see Appendix 6) and takes into account the appendages and whether or not

the image is hollow it is clear that aIl twenty-three images are slightly different

Second Goal:

The second goal was to determine whether combinatory rules can be established for

the images. l applied the contextual approach after the culture-historical approach to the

information in Chapter VI ta consider this question. It is important to establish whether

correlations occurred and patterns existed amongst the various pieces of data to provide a

solid basis for considering possible meanings. It was crucial to discover any different

relationship types between the physical existence of the sites in the larger landscape, the

physical features of the rock's surface and the images themselves so as to provide a solid

basis enabling the identification of their meaning

The pictograph sites in caves and on cliffs should be perceived as different physical

types, since each has its own characteristics. But for their other characteristics they were

examined together. Granite is generally used for sites but the lack of strong correlation

between the geology, the geomorphology in the immediate vicinity of the sites and the

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~-

landmass suggests that other reasons may have influenced the choice of a particular place.

Sites occurred on islands and on the mainland but not necessarily immediately beside water,

although water is present in close proximity. The fluctuations in water levels demonstrate

that it is not simply the Images that experience time and change. The rock surfaces

themselves have a history.

None of the sites, whether on cliffs or ln caves, has exactly the same physical

structure. These differences may or may not affect the location of the images. Individuals

such as Conway and Conway (1990b), Dewdney and Kidd (1962 & 1967); Lambert (1983,

1985, n. d.), Rajnovich (1989 & 1994), Rusak (1992a), Vastokas and Vasto kas (1973) drew on

a range of ethnographic and anthropological sources including (Coleman 1937; Fiddler and

Stevens 1995; Landes 1968; Wheeler 1977a, n. d.) to identify the key features of rock image

sites on cliffs: deep holes, large cracks, large crevices, rock overhangs, and rock benches or

ledges. These features were considered by previous archaeologists as prerequisites for the

presence of images. Only one of the twenty-five pictograph sites found on a cliff, DgKl-2,

had ail the physical features that should be present according to previous archaeologists.

Granite cliffs did not need to have sorne large or smail crevices, cracks and holes for

paintings to exist. However, those that drew on ethnographic and anthropological sources in

an attempt to establish the factors ind.icating the presence or absence of images at sites

should be applauded for their efforts, since this was a necessary step in the quest for the

identification of the specific origins of the sites. However, a proposition based on such shaky

grounds is likely to be unsound. Perhaps there is no obvious reason why specific places were

chosen. The answer exists in a body of information either lost in the past or now impossible

to obtain. Although it is fascinating to entertain the notion that sorne sites were secular while

others were sacred, this proposition cannot be considered given the evidence at hand.

A strong relationship could not be established between the images and the types of

rocks. A relationship does not occur between the number of images at sites and the type of

land mass, the number of the physical features present at cliff faces, whether or not offerings

were found in 2001, and the number of cliffs used at each site. Images existed on the ceilings

of both of the caves encountered, but do two caves constitute a representative sample from

which to derive a generalization? The lack of positive or negative correlations between the

number of images and these other features, especiaily o fferings , suggests that other factors

may explain why offerings were found at sorne of the sites in 2001. In retrospect, it would

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have been useful if l had built a component into my research design that documented how

many localities with the physical criteria (granite cliff, caves, cracks, crevices, or holes, etc.)

do or do not contain rock paintings.

It was clearly important to de termine any relationship between the images, shapes,

themselves. l used 'shape' instead of the term morphs.

The widespread nature of the blobs (xq326), and the five types of 'unidentifiable

shapes' (xq744) throughout the geographical area containing pictograph sites indicates that

the sites have been used over a long time period. Essentially, these pictograph images may

have become indistinguishable because images change shape as they weather, fade, and,

perhaps, are reused. The large number of individual images that only occur once, the large

number of variations of different shapes loosely categorised as 'creatures,' 'stick figures,' 'zig­

zags,' 'crescents,' 'hand prints,' turtle,' and 'bird,' as well as the large number of blobs, or

decayed images, suggested that the people who used these images, shapes, knew how to

exploit them as a graphic vocabulary to express whatever they wanted to communicate.

Unfortunately, it is impossible to establish the full range of combinations of images.

However, smears, blobs and unidentifiable shapes cannot be ignored as they were in the pasto

Dewdney (1958-1964) and Lambert (n.d.) were mistaken in ignoring smears and not

perceiving them to be indicators of pictographs. Perhaps these archaeologists did not

perceive such images to be interesting or informative from the interpretive perspective;

hardly a valid reason to exclude them. Although these images are smears, they are still

images. Fortunately, there was a change in perception regarding these shapes prior to Rusak's

(1992b) survey of the White Otter Lake pictograph sites. Otherwise, the smear as a legitimate

analytic category may have been ignored for an even longer period of time. These shapes

demonstrate that people used these rock surfaces to express something, and that significant

time has elapsed since they were originally created. This ide a is supported by the presence of

a large number of images that occurred only once and are discussed in Chapter V.

The large number of types of images, shapes, that were loosely categorised as a type,

such as 'creature,' or 'zig-zag,' in conjunction with a relatively small quantity of images in the

datas et makes identifying combinations of specific image types difficult. Images were

identified as being loosely categorised as a type of shape. As l argued in Chapters IV and V,

it is evident that the vocabulary and the level of detail at which these images were described

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!~

in the earlier archaeologicalliterature has influenced the number and the range of each type

of shape.

It is possible to classify the images differently. Consequently, demonstrating that the

very vocabulary used has heavily influenced the possible outcome of any discussion of

perceived style becomes straightforward. 1 concluded that a nested hierarchy of types left

more classification options open. For example, if ail the extremities of a shape such as

creature were to be ignored, it would be possible to simply describe the shape as a 'creature.'

Unfortunately, this gives the impression that ail the twenty-three shapes that are 'creatures'

are the same. It is occasionaily impossible to identify the creature's species based on its

appendages. However, if one closely examines the photographs of the images and takes into

account the appendages and whether or not the image is hoilow, this could mean that aIl

twenty-three images are slightly different.

Only twenty-seven sites are currently reported; the fewest shapes per site occurred at

DhKm-19, DiKm-50, and DkKn-6, where only one shape existed. The site with the largest

number of images, thirty-seven, was DhI<:m-5. Blobs were the most common type of shape.

The lack of combinations is not the result of the method used to describe the images

since the differences in the physical shapes of each images were not ignored or glossed over.

These differences are important and the descriptive vocabulary used should be selected

carefully since it affects any discussion of the perceived style. Combinations appeared to exist

when the shapes were loosely described as belonging to a particular group or type of images

(see Appendices 6 and 7). However, but when the shapes in question were described in detail

it became abundantly clear that relatively few shape combinations existed at, or between,

sites (see Appendix 16).

Some images existed in some parts of the lake but not in others (see Chapter VI,

particularly Appendix 16). The widespread prevalence of blobs throughout the lake suggests

that blobs rather than smears may be more important indicators of the passage of time.

Smears occurred at pictograph sites in the southern, eastern and southeastern portion of the

lake. This difference in the geographical distribution between the two shapes supports the

ide a that perhaps some smears were placed intentionally at sites and do not always reflect the

passage of time. Smears might be deliberately executed and not a function of taphonomy

primarily because they, unlike blobs, are not 'randomly' distributed. The largest number of

loosely defined groups of shape types occurred in the eastern portion of the lake where

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seven different shapes existed: 'a group of nine short lines,' 'a group of four diagonal short

lines,' 'a group of four diagonallines,' 'birds', 'crescents', and the shapes loosely categorised

as 'zig-zags'. 'Creatures' constitute the largest number of any shape type and existed in the

southern, eastern, and northeastern portion of the lake. Most of the images are in the eastern

portion of the Lake of the Woods. Relatively few sites exist in the southern and the northern

portion of the region. Two pictograph sites exist in the northwestern portion of the region

but pictograph or petroglyph sites are not present in the southwestern region, possibly

because the geology is different and the area is swampy, sandy, full of muskeg, and bogs (see

Chapter II and V). The petroglyph sites tended to be more numerous in the northwestern

and northern region of the lake. Perhaps sorne of the images in the northeastern and

northwestern pictograph sites occur in the petroglyph sites of the northeastern and the

northern part of the Lake of the Woods. Confirmation of this speculation can only occur

once these sites have been examined and the images described in the same manner as the

pictograph sites were examined.

The homological, rather than the analogical approach was applied in Chapter VII to

establish whether rules existed. Even though the sites could not be dated using absolute

dating techniques, l chose this approach since cultural continuity between the pre-contact

and post-contact past is a strong possibility in this region, and the same techniques and

implements have been employed for a long period. It was established in Chapter II that the

Algonquian-speaking peoples have been using several image types as a means of

communication.

This approach makes connecting archaeological information with that derived from

other disciplines possible, so as to obtain information concerning the practices and beliefs of

either specifie societies, or groups of historically related societies. By relying on a wide variety

of evidence, archaeologists can attempt to establish continuity in the practices and beliefs in

question.

This approach enabled the in-depth analysis of a specifie group and its material

culture, permitting archaeologists to consider what human beings might have thought about

in the past, and the meaning of specifie symbols and objects. Trigger (1995: 452) argued that

written records, the oral heritage, and ethnographie materials always combined with

archaeological data from successive periods, are probably the strongest types of evidence to

be used when devising bridging arguments. Although this approach poses substantial

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technical challenges, namely in the use of generic approaches to data, scholars should exploit

these materials to establish which beliefs might be present in specifie cultures. It is important

to determine whether similar images used in a variety of different media held similar

meanings. However, continuity of form does not necessarily imply continuity of meaning.

Meaning can also change, especially sin ce icons tend to be polysemie.

The presence of a large range of different shapes that occur only once (discussed in

Chapters V and VII), causes me to speculate that a considerable number of people probably

moved through this region and used these images to convey information. The Lake of the

Woods, as l have repeatedly argued, is, and was, an important part of a primary

transportation corridor that bisects the continent from east to west and from north to south.

The lack of an apparent pattern in these images possibly reflects the diversity of form, a

variety of functions, unknown but of considerable time depth, and a varied ethnie

authorship. It suggests that these images were part of the larger vocabulary of signs used by

everyone and not solely the product of specialised religious practitioners such as the Midé.

This makes it more likely that each image was created independently and understood

separately from the other images at a pictograph site. It is possible that the organization of

images at sites were believed to have supernatural power, and the combination of images

does not reflect any particular set of rules, other than the fact that individuals, maybe

families, used the same place over an unknown period of time. Perhaps the variability in the

form of images reflects a lack of standardisation. More likely, this variability also reflects a

combination of facts that either the images physically changed over time, or that the artists'

choice of shape, icon or shape changed through time or situational context.

Yet these images probably belong to a group for which little ethnographie data exists,

as l established in Chapter II. This, in comparison with the quantity of information for the

two groups of images (the floral image and those utilised by the Midé), indicates that we

really do not have a strong sense of the combinatory rules we seek. One of the largest

problems with the rock images sites is that there is no base line on which we can build our

analysis. Perhaps we, as archaeologists, are unable to see the pattern(s) because we lack the

intellectual context of symbolic meaning and sufficient knowledge or understanding of all the

taphonomic issues.

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Third Goal:

It would be a considerable breakthrough to establish each site's life history. This is a

reasonable goal but, unfortunately, it was not achieved. Absolute dating of these sites would

have been useful especiaily where the images were superimposed and badly exfoliated.

Unfortunately, direct dating techniques cannot be used. The presence of datable offerings at

DhKm-1, DgKI-17, and nearby to DiKm-S1 and DiKmSO provided some indication of the

length of time over which these sites have been used. This evidence did not provide a strong

indicator of the age of the images. It remains impossible to establish the precise date at

wruch ail but the most recent of these images were created. Nevertheless, some of the new

shapes couid be given approximate ages. The new shapes in modern paint were

superimposed on ochre between 1989 and 2001 at DgKl-2 because Pastershank did not

record them in 1989, and l found them in 2001. It is possible to date the shapes in red, blue,

and white modern paint of DhKm-20 because their creator conveniently provided a date of

1982. These images strongly resemble those images found in paintings and art objects

created by the members of the New Woodland School of Art, founded by Norval

Morrisseau, who drew on Ojibwa beliefs and traditions. Whether these images reflect the re­

use of a place for spiritual purposes by an Aboriginal person, or someone of unknown

cultural affiliation mimicking a widely recognised modern artistic tradition is impossible to

establish. Trus is because it is difficult to reconstruct cultural continuity in the recent past in

trus region.

Otherwise, Dewdney, who first recorded many of the sites, relied on informants,

who often gave no indication of the length of time such sites were believed to have existed.

Lichen growth and encroachment were unreliable indicators, since the rate of growth appears

to differ from site to site, and it is impossible to establish how many archaeologists foilowed

Dewdney's practice of removing the lichen covering many of these paintings. Trus prevents

determining a baseline that would make it possible to know wruch images initiaily existed,

and wruch were subsequently added at each site.

It is also impossible to consider whether the images present upon the pictograph

sites have changed over time. The great variability of images suggests that doing trus

stylisticaily, if at ail possible, will be chailenging. Despite tremendous efforts l found that trus

method was problematic given the incomplete documentation regarding these sites, and the

changing methods used in recording them renders application of this method flawed.

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It is possible to conclude from the presence of blobs at sites throughout the Lake of

the Woods that some of the images have some antiquity. VIPS software and Adobe

PhotoShop 6.0 provided me with the ability to establish whether additional, paler images

existed beside those that were readily visible. Both highlight the importance of looking

beyond the areas of the surface of the rock that had strong, clearly defined red images, since

paler images could exist elsewhere on the rock surface. Furthermore, the presence of both

the pale and the dark red images in ochre, as weil as the modem spray painted images,

indicates that these places were, and continue to be, used.

Perhaps it is possible to date the constituents of the paints, as discussed in Chapters

II and V, but samples could not be removed. It is impossible ta determine either the

implements used to apply the paint or its ingredients. Fingers were possibly used ta apply the

paint of the images found and recorded before 1989. The ethnographie evidence discussed in

Chapter V supports the idea that iron ore, ochre, was used and possibly isinglass from the air

bladder of the sturgeon, a fish that was prevalent in this region of North America. However,

newer images discovered and recorded in 2001 were painted using modem spray paint in red,

green, black, white, and blue.

Clearly, a shift has occurred in the paint and technique used to create the images.

Fourth Goal:

The final goal was to consider whether the images can be related ta other images

outside rock image sites, and if this can help provide some information about meaning. It

should be clear, from Chapter II, that previous researchers have agreed that these images are

polysemie in nature and that the images were used to convey information to other people.

Previous researchers concurred that the images of the pictograph sites are similar to those on

birch bark scroils made by the Midé ritual specialists. Everyone has posited that a detailed

investigation of the images on birch bark scroils, the ethnographie record, and the

pictographs might provide some answers as to the meanings of the images found on the rock

faces. For this reason l applied, in Chapter VII, the same sequence of philosophical

approaches, with their own questions and techniques, to the images of four birch bark

scroils, each of which was produced for different purposes. However, earlier researchers

made evident that an unknown number of images were used by the Algonquian-speaking

peoples who were not ritual specialists (Coleman 1947; Landes 1968; Schoolcraft 1851;

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Copway 1851; Dewdney 1975). Unfortunately few of these images exist. Perhaps sorne were

used by Roy, an Ojibwa trader, between 1835 and 1839 (Fulford 1992). Over a hundred years

later Landes (1968: 172) observed that images were familiar to ail Ojibwa hunters, trappers,

and traveilers, who used them to indicate boundaries, trails, notices of different sorts, and on

grave markers. Coleman (1947: 63) had observed, while doing her fieldwork, that the totem

of a deceased individu al was placed upon a grave market.

The results of the analysis of the four birch bark scroils reveals the impossibility of

ascertaining the identity of particular songs, mnemonics, without a recorded body of data

reliably connected to the birch bark scroils in question. However, this study indicated that

the images on the pictograph scroils were used differently. Very few of the images on the

birch bark scroils and the rock image sites are the same. Comparison of the images on the

sites and those of the birch bark scroils reveals little similarity. Comparison of the images

found on the birch bark scroils without contextual documentation and those on the rock

image sites indicates that it is impossible to establish what meaning they held for either their

creators or the people who subsequently observed them. The meaning of the images on the

surface of these rock faces cannot be determined. At the same time, since so few of the

images on the birch bark scroils and the sites are similar, sorne level of choice probably

existed in the mind of the creator of the images, in both place selection in the landscape, and

image selection. It is likely that the creator considered each image as an individual entity and

not as a story. Nonetheless, groups of images at sites are currently being reinterpreted as a

"story," rather than as individual entities (see Section 3 of Chapter VII).

If we view images as individual entities, we can explain why so few of the pictograph

sites that had images had ail of the five "required physical features." Few sites had the

"required features" (crevices, benches, holes, overhangs, cracks) because the variables that

archaeologists have deemed crucial were not important for the creation of images. Such

images were probably created over a very long period of time by individuals and possibly not

by ritual specialists. Relatively few offerings were found in 2001 at sites that had relatively

few of the five physical features, possibly because, at one time, these features were

unimportant. They have subsequentlY become important. It is likely that the significance of

these sites has either changed, shifted, or been mistaken over time. At present, their

importance is not only weil known by archaeologists, anthropologists, and art historians but

also by the local indigenous peoples. People, regardless of whether white or native, read

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books and articles written by art historians, archaeologists, and anthropologists.

Consequently they learn about the importance given to these sites by the practitioners of

each discipline, and the conversations each has with their respective native informants.

Information about these sites is being recycled and exchanged.

Ethnographic information and date able archaeological evidence support the idea that

specific places in the landscape were important in the pasto The presence of new images on

older images at DgKl-2 indicates that physical places in the landscape continue to be

important, despite the numerous changes within Ojibwa and Algonquian societies over the

last two or three hundred years. The discovery of the two sites with new images, DhKm-19

and DhKm-20, suggests that people still use the landscape as more than a place to travel

through, hunt, or live in, but it is still difficult to establish that specific connection with the

spiritual realm. But it is impossible to establish, however, the precise nature and significance

of these images and the pictographs. It is unclear whether they held any religious symbolic

significance. It is possible that the paintings were simply used as forms of communication.

Section 2: The Theoretical and Methodological Implications of this Thesis

Theoretical Implications:

Theories are considered useful in explaining regularities, but a really useful theoretical

framework also will aid the explanation of the variability evident in the data. Theory is

intertwined with method. The theoretical framework archaeological researchers use affects

the way in which they interpret the pasto Therefore, prior to conducting any new research, an

archaeologist must establish the theoretical approach that each of their predecessors used in

their studies. Previous frameworks affect the way data is collected [fieldwork] and

subsequently analysed. Once completed, it is important to establish whether these

philosophical approaches have affected the methodological approaches. Different theories

require different methods, in both fieldwork and analysis.

In the introduction to this thesis, l argued that archaeologists currently use five

different interpretive approaches. Unlike scholars from other disciplines, archaeologists

usually lack textual data. Textual data is often produced within a particular perspective, and

the investigator can be carry forward that perspective to a greater or lesser extent. These five

interpretive approaches, culture-historical, contextual, intuitive, analogical, and homological,

are used to infer human behaviour and meaning from archaeological data. Each prescribes

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.~.

the types of questions applied and determines the levels of understanding obtained about

whichever form of archaeological evidence is being considered. The same data must be

examined in sequential order using these different approaches, if the potential quantity and

quality of information gained is to be increased.

The different, but complementary theoretical approaches should be employed in a

definite order. My critical review of the previous research conducted on the rock image sites

of the Canadian Shield, specifically the Lake of the Woods, in Chapter III concluded that the

intuitive approach, (narrative, constructivist, or so-called 'humanist'), must be avoided

because of the problems that arise. 1 think it is imperative for scholars to articulate to others

the method through which conclusions were reached. Readers should not be subjected to the

unstated premises of the author, but shown precisely how an interpretation was processed. If

an archaeologist intends to establish the meaning of these images in a more rigorous and

persuasive fashion, the analogical or the homological approaches should be adopted (see

Table 1.1). As argued in the text, archaeologists should use the following sequence of

approaches: culture-historical, contextual followed by either the homological and analogical

approaches or a combination of the latter two.

Methodological Implications:

The first and most obvious methodological implication of this thesis is that images

must be considered as sources of information in the same way as traditional archaeological

artefacts [perhaps canonical] of the lithic, the bone, and the pot-sherd. Lithics, pot-sherds,

and bones do not occur with neither handbooks nor manuals on how to examine them.

Images should be included as an integral part of any archaeological survey and excavation if

they occur in the geographical region together with "conventional" archaeological sites.

Scholars involved in archaeological research should realise that images, although they are not

like "conventional" archaeological artefacts, still cannot be ignored, or treated in a cavalier

fashion. Researchers called "rock art specialists" must in turn be aware of the importance of

'canonical' archaeological techniques, procedures and approaches. It is vital that both groups

consider an image as a source of information and understand its physical outline, form, and

structure before discussing its context or meaning. Once again, 1 stress the importance of

using the theoretical and analytical approaches in a definite sequence.

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The second methodological implication is that images cannot be adequately

described using numbers. This is weil understood among those attempting to create adequate

metadating conventions for the description of varied bodies of information. (e.g. ]aritz &

Schuh 1992; Rose 2001; Saouter 1998). Otherwise a 'flat' uniformity is achieved at the cast of

losing distinguishing characteristics. Considerable care must be employed when choosing the

vocabulary to describe the shape or form of an image to avoid inadvertently or prematurely

ascribe meaning(s). This is why l described each shape using a small set of clearly delineated

vocabulary (see Chapter IV). The same vocabulary was re-used repeatedly. Once a shape is

carefuily described, it must be written up, preferably in a database of some type (I used

KLEIO lAS), in a referenced, cross referenced, and searchable form. Ascribing meaning

occurs at a different and [much] later level of analysis. Classifying and describing any image is

very difficult, since the level of description given to an image affects the way in which it can

be analysed. It is possible to classify the images differently, and the vocabulary used will

heavily influence the possible outcome of any discussion of perceived meaning. The

vocabulary and the level of detail has had an impact on both the number and range of each

shape type. Therefore, prior to describing the images, the vocabulary used must be carefuily

considered and discussed. The vocabulary used must not be discipline-specific. It is also

important to take the middle road between the "splitter" and the "lumper" approach when

describing images. l found that a nested hierarchy of types le ft the most classification options

open. The precise size of an image was ignored because these images have changed shape

from the onset of their creation. It was noted whether an image such as a line was longer,

shorter, wider, or narrower than the average size of the image at each site so as to provide an

indication of its size. The image shape was dependant, perhaps, on the amount of paint at

hand. It is difficult to establish importance of image from a detailed exarnination of the

ethnographie record of the peoples who lived in this region. The current size of an image

depends upon uncontrollable elements, such as the deposit of mineraIs upon the rock

surface, exfoliation, and plant growth. Nevertheless, it should be noted subsequent to its

description whether a shape is large or smail with respect to the other images at a site.

However, the precise dimensions of the shape need not be ascertained because, during my

analysis of these images, it became clear that the size of an image was unimportant. It is

possible to state simply that a shape called a smail long horizontal line or short vertical

rectangle existed.

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It is crucial to describe systemically the images from one end of the painted area to

the other without arbitrarily subdividing the images, shapes, into groups defined by rock

fissures or dis crete perceived spatial clusters. Describing the images in smaller, arbitrary parts

may be easier in the field, but this arbitrary subdivision of sites into parts called faces and

panels gives rise to numerous problems, as discussed in Chapter III. l described the images

at a site from left to right to prevent subdivisions suggested by cracks and crevices in the

rock face. l discuss the fieldwork methods and techniques l employed in my 2001 field

season in Chapter IV. Any short cuts taken during fieldwork inevitably leads to problems

during the analysis stage. Finally, the methodology used to describe and decipher rock images

must be extended in stages, sin ce there is no existing narrative that contextualises it.

Section 3: Further research - What should be done next and which way should the field go?

Rock images must be taken seriously as sources of information; symbolism, and

communication; as important human expressions. The original meanings their creators

applied cannot be established or verified. This should not imply that images be "forgotten,"

left unexamined, and unconsidered as part and parcel of the archaeological record of a given

geographical region. Images must be considered as another archaeological source, like a

lithic, a bone, or a pot-sherd, otherwise the problems that l have discovered in their

description and analyses in Chapter II will persist. Images admittedly require the analyst to

think of the archaeological site not just as a two-dimensional, but as a three-dimensional

entity. The examination of these images, the se archaeological artefacts, requires "thinking out

of the box" to a greater degree than usual and often entails dealing with larger quantities of

information, possibly employing techniques borrowed from other disciplines. It might also

require that the archaeologist acknowledge that it might never be possible to determine their

original intended meaning(s). This should not deter archaeologists from examining images

and regarding them as integral to the understanding of the regional archaeological record.

There are several other serious questions that remain for contemplation - they have

been exposed rather than resolved. Sorne argue that the use of digital technologies will 'solve'

formerly unsolvable problems. That might sometimes be the case but, without rigorous

methodological procedures, much will be lost in digital transcription. If we are to examine

the images using powerful technologies, and if we are to have any hope of relating them to

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hum an experience, then we must have both the infrastructure, and develop our own tools, or

combine a number of methodological tools for use in conjunction with each other. My

experience would suggest that we need to be free of disciplinary restrictions when choosing

tools. It goes without saying that theoretical frameworks must be thoroughly invoked prior

to using any digital tools. The advent of digital technologies has meant, of course, that there

is the possibility that access via digital surrogates to damaged, faded or partial images may

yield further insights. There is also the remote possibility that an examination of other

circumpolar sites using the homological approach might yield sorne insight, but only to the

site in question, and only after the data has been approached with equal rigour.

A secure grasp of 'sophistication' requires a rigorous intellectual base. This, in turn,

requires an understanding of the intertwining of theory and practice. There is simply no

point in collecting data for its own sake, however intrinsically fascinating, or however 'fun'

the field experience. While such experience is a process in itself, it is inherently

impressionistic, and should not be confused with rigorous research. Rigorous research has its

own delights. On the other hand, theory which has not been grounded in rigorous

archaeological practice and secure data is equally problematic.

This gets us back to 'invented traditions' and perhaps archaeologists, unwittingly or

not, have assisted in the creation of many such traditions. Their practices establish them as

members of a specific community. When scattering tobacco at a site, they are affirming

themselves as potential keepers of important information pertaining to the images. They,

possibly unwittingly, aid in the construction of identities for the peoples of the region, and

their relationship to their pasts. By rigorously adhering to systematic exposition, examination,

and analysis of the rock images of Lake of the Woods, we have established that we remain

ignorant of the role these images played in the lives of peoples in the distant pasto Whatever

role they play today is an entirely different concern.

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Appendix 1: Summary of the information available on the pictograph sites prior to 2001

Borden Number DiKm-3 Alternative Site # 28 (Dewdney August 15th 1953); Return Point Names: Photographs - Yes - Reid (1975); Dewdney (1953); Molyneaux (1979) were they taken? Measurements Dewdney (1953) - Face l = 50 cm (h), Face III = 100 cm /1 m (h); taken by each Reid - 2 metres square iperson Method( s) of Ashdown (1973) - written description and map; Dewdney (1953)-recording used written descriptions, drawings, photographs;

Reid (1975) recorded accessibility, possible cultural affiliation, significance, condition/ endangerment, assessed "representability, interpretability" of site, obtained Borden number for site under Heritage Act, photographed and mapped site. Molyneaux (1979) - photographs

Location of field Ashdown (1973) - unknown notes Dewdney (1953) - New World Archives, Royal Ontario Museum,

Toronto, Ontario; Reid (1975) Ontario Ministry of Citizenship, Culture and Recreation, Thunder Bay, Ontario; Molyneaux (1979) in possession of the author and Ontario Heritage Foundation

Published works Ashdown, J. H. 1973. A Contemporary Explorer's Chart to the Lake of the where site Woods. Kenora: Royal Yacht Club of the Lake of the Woods. referred to Dewdney S. and K. Kidd. 1962 Indian Paintings of the Great Lakes.

Toronto: University of Toronto Press. Dewdney S. and K. Kidd. 1967. Indian Paintings of the Great Lakes. 2nd

Edition Toronto: University of Toronto Press. Reid, C. S. 1976. Environment, Man and MC!)'mC!)'gwC!)'shi: The Dimensions of Past Human Cultural Impact in the Lake of the Woods Area; Regional Archaeologist, Historical Planning and Research Branch, Northwestern Region, Lake of the Woods Planning Area Molyneaux, B. L. 1979 The Whitqish BC!)' Pietograph Pro/eet. Report to the Ontario Heritage Foundation. No licence.

Scholar's name, J. H. Ashdown (traveller) - 1973; Selwyn Dewdney (artist) - 1953 profession, (August 15); C. S. "Paddy" Reid (archaeologist) - 1975; Brian date(s) of study Molyneaux (archaeologist) - 1979 Location, Dewdney (1953) north west shore of an island in Whitefish Bay, number of faces about 3 miles SSE of Sioux Narrows. He subdivided it into three recorded, etc Faces. Noted current water level in relation to the images he recorded.

Reid (1976: 29) accessed by boat to Whitefish Bay, culturally affiliated to Northern Hunters and Fishers, of probable religious significance, good condition, site well known and published in tourist guides. (ibid.: 14) assessed as having "high representability and high interpretability" .

Rock type? Not stated Offerings Dewdney - clothing items deposited at this site (Dewdney -list in present? Field Book 2), "residue of a "prayer raft" found here - now in the

Royal Ontario Museum" in their Ethnological Collections.

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Borden Number DiKm-4 Alternative Annie Island, Annie Island Pictograph Site, Site # 93, Annie Island Names: (Dewdney J uly 15,h 1960) Photographs - Yes - (Dewdney 1960); Molyneaux (1974, 1979) were they taken? Measurements Dewdney (1960) - a little over 60"; Reid - 2 metres square; taken by each Iperson Method( s) of Ashdown (1973) - written description and map; recording used Dewdney Guly 1960) - field reproductions, written description,

photographs; Molyneaux (1974) - photographie documentation of site, description of erosion of site vis-à-vis future protection or conservation Pelshea (1978) - field reproduction, slides; Molyneaux (1979) - photographs Reid (1976) recorded accessibility, possible cultural affiliation, significance, condition/ endangerment, assessed "representability, interpretability" of site, obtained Borden number for site under Heritage Act, photographed and mapped site;

Location of field Ashdown (1973) - unknown notes Dewdney (1960) - New W odd Archives, Royal Ontario Museum,

Toronto, Ontario; Reid (1975) Ontario Ministry of Citizenship, Culture and Recreation, Thunder Bay, Ontario. Pelshea (1978) unknown where field notes etc located but photographs in Ontario Ministry of Culture, Tourism and Recreation, Thunder Bay, Ontario. Molyneaux (1974) possession of the author Molyneaux (1979) in possession of the author and Ontario Heritage Foundation

Published works Ashdown, J. H. 1973. A Contemporary Explorer's Chart to the Lake if the where site Woods. Kenora: Royal Yacht Club of the Lake of the Woods. referred to Dewdney S. and K. Kidd. 1962 Indian Paintings if the Great Lakes.

Toronto: University of Toronto Press. Dewdney S. and K. Kidd. 1967. Indian Paintings if the Great Lakes. 2nd

Edition Toronto: University of Toronto Press. Molyneaux, B. L. 1974. Trent University Rock Art Research Pro/ect Summary Report. 1974 Field Season. Department of Anthropology, Trent University. Reid, C. S. 1976. Environment, Man and Mqymqygwqyshi: The Dimensions ifPast Human Cultural Impact in the Lake if the Woods Area; Regional Archaeologist, Historical Planning and Research Branch, Northwestern Region, Lake of the Woods Planning Area. Molyneaux, B. L. 1979 The Whitifish Bqy Pictograph Prqject. Report to the Ontario Heritage Foundation. No licence

Scholar's name, Ashdown (explorer) - 1973; Selwyn Dewdney (artist) - 1960 Guly profession, 15); C. S. "Paddy" Reid (archaeologist) -1976; Victor Pelshea date(s) of study (archaeologist) - 1978; Brian Molyneaux (archaeologist) - 1974,

1979.

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Location, number West side of Annie Island in southern end of Whitefish Bay; of faces recorded, Dewdney (1960) - 48" above watet; one solitary figure; etc Molyneaux (1974:6) single painting that he argued was "the most

expressed shamanic motif in the rock paintings of the Canadian Shield." Reid (1976: 29) accessed by boat to Whitefish Bay, culturally affiliated to Northern Hunters and Fishers, of probable religious significance, good condition, site weIl known and published in tourist guides. (ibid.: 14) assessed as having "high representability and high intefJ.:>retabili!y".

Rock type? Granite Offerings Dewdney (1960) - an "offering" site. In: Dewdney and Kidd (1967: present? 54) discovered "another deposit of dothing, prayer sticks, and

tobacco, aIl as fresh as if they had been put there yesterday."

Borden Number DhKm-4 Alternative Devil's Bay l Pictograph (Lambert n.d.); Site # 92 (Dewdney 1960) Names:

This site was originaIly part of DhKm-1 according to Dewdney's drawings ofDhKm-1. This fact caused problems for Lambert in 1985 sin ce he combined the recordings, description, and analysis of DhKm-1 with DhKm-4.

Photographs - Yes - Dewdney (1960), Lambert (n.d.), Reid (1976), Molyneaux were they taken? f1974 , 1979) Measurements Dewdney (1960) - Face l = 2 feet taIl by 72 inches long; taken by each pers on Method( s) of Ashdown (1973) - written description and map; recording used Dewdney (1960) - written descriptions, drawings, photographs;

Molyneaux (1974) - photographie documentation of site, description of erosion of site vis-à-vis future protection or conservation Reid (1976) - recorded accessibility, possible cultural affiliation, significance, condition/ endangerment, assessed "representability,

/~, interpretability" of site, obtained Borden number for site under Heritage Act, photographed and mapped site. Molyneaux (1979) - photographs Lambert (n.d.) - written description, photographs, dot-for-dot recording;

Location of field Ashdown (1973) - unknown notes Dewdney (1960) - New World Archives, Royal Ontario Museum,

Toronto, Ontario; Molyneaux (1974) - unknown Reid (1975) Ontario Ministry of Citizenship, Culture and Recreation, Thunder Bay, Ontario; Molyneaux (1979) field notes in possession of the author and Ontario Heritage Foundation Lambert (n.d.) - unknown where field notes and photographs located but Borden forms available from Ontario Ministry of Citizenship, Culture, and Recreation.

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Published works Ashdown, J. H. 1973. A Contemporary Explorer's Chart to the Lake of the where site Woods. Kenora: Royal Yacht Club of the Lake of the Woods referred to Dewdney S. and K. Kidd. 1962 Indian Paintings of the Great Lakes.

Toronto: University of Toronto Press. Dewdney S. and K. Kidd. 1967. lndian Paintings of the Great Lakes. 2nd

Edition Toronto: University of Toronto Press. Lambert, P. J. n.d. The Northwestem Ontano Rock Art Pro/ect: The 1985 Results and Regional Overoiew. Unpublished report for Northwestern Region Conservation Archaeology Report. No number. Molyneaux, B. L. 1974. Trent Universiry Rock Art Research Pro/ect Summary Report. 1974 Field Season. Department of Anthropology, Trent University. Reid, C. S. 1976. Environment, Man and Mqymqygwqyshi: The Dimensions of Past Human Cultural Impact in the Lake of the Woods Area; Regional Archaeologist, Historical Planning and Research Branch, Northwestern Region, Lake of the Woods Planning Area. Molyneaux, B. L. 1979 The Whiteftsh Bqy Pictograph Prqject. Report to the Ontario Heritage Foundation. No licence

Scholar's name, J. H. Ashdown (traveller) - 1973; Selwyn Dewdney (artist) - 1960; C. profession, S. "Paddy" Reid (regional archaeologist) - 1975; Brian Molyneaux date( s) of study (archaeologist) - 1974, 1979; P. J. Lambert (archaeologist) - 1985

(August) Location, number Dewdney (1960) Whitefish Bay, Lake of the Woods. (Dewdneyand of faces recorde d, Kidd 1967: 53) west shore of the - Face l = 3' (above water?). etc Molyneaux (1974) - no comments about images.

Reid (1976) on Lake of the Woods, north side of entrance to Devil's Bay, Access by boat; southern end ofWhitefish Bay; Reid (1976: 30) accessed by boat to Whitefish Bay, culturally affiliated to Northern Hunters and Fishers, of probable religious significance, good condition, site well known and published in tourist guides, (ibid.: 14) assessed as having "high representability and high interpretability".

Rock type? Dewdney (Dewdney and Kidd 1967: 53) granite outcrop Offerings None present?

Borden Number DhKm-l Alternative Dewdney's # 92 A (1960), Names: Devil's Hole (Reid 1976)

This site was originally part of DhKm-4 according to Dewdney's drawings ofDhKm-4. This fact caused problems for Lambert in 1985 since he combined the recordings, description, and analysis of DhKm-1 with DhKm-4.

Photographs - Yes - colour slides- Dewdney (1960); Fox (1974); Molyneaux were they taken? f1974); Reid (1976); Lambert (1985) Measurements Lambert (1985) taken by each pers on

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Mcthod( s) of Dewdncy (1960) - writtcn descriptions, drawings, photographs; recording used Ashdown (1973) - written description and map.

Fox (1974) - field notes, photographs; Molyneaux (1974) - photographie documentation of site, description of erosion of site vis-à-vis future protection or conservation Reid (1976) recorded accessibility, possible cultural affiliation, significance, condition/ endangerment, assessed "representability, interpretability" of site, obtained Borden number for site under Heritage Act, photographed and mapped site. Lambert (1985) written descriptions, tracings, photographs

Location of field Ashdown (1973) - unknown notes Dewdney (1960) - New World Archives, Royal Ontario Museum,

Toronto, Ontario; Molyneaux (1974) - unknown Fox (1974) - copies of slides and field notes sent to me by W. A. Ross, Regional Archaeologist, Ontario Ministry of Citizenship, Culture and Recreation, Thunder Bay, Ontario - were lost but were found. Reid (1975) Ontario Ministry of Citizenship, Culture and Recreation, Thunder Bay, Ontario; Lambert (n.d.) - unknown where field notes and photographs located but Borden forms available from Ontario Ministry of Citizenship, Culture, and Recreation.

Published works Ashdown,]. H. 1973. A Contemporary Explorer's Chart to the Lake rifthe where site Woods. Kenora: Royal Yacht Club of the Lake of the Woods referred to Molyneaux, B. L. 1974. Trent University Rock Art Research Prqject

Summary Report. 1974 Field Season. Department of Anthropology, Trent University. Reid, C. S. 1976. Environment, Man and Mqymqyqwqyshi: The Dimensions rifPast Human Cultural Impact in the Lake rifthe Woods Area; Regional Archaeologist, Historical Planning and Research Branch, Northwestern Region, Lake of the Woods Planning Area Lambert, P. J. n.d. The Northwestern Ontario Rock Art Pro/ect: The 1985 Results. Unpublished report. Ontario Conservation Archaeology Report. Northwestern Region No number. Ontario Ministry of Citizenship and Culture.

Scholar's name, ]. H. Ashdown (traveiler) - 1973; W. Fox (archaeologist) - 1974; profession, Brian Molyneaux (archaeologist) - 1974, 1979; C. S. "Paddy" Reid date( s) of study (regional archaeologist) - 1976 Location, number Dewdney (1960) Whitefish Bay, Lake of the Woods. of faces recorded, Fox (1974) none recorded just photographed site and recorded etc details as to offerings found.

Lambert (n.d.) - Face II and III = 36" above water; Molyneaux (1974) - no comments Reid (1976: 29) accessed by boat to Whitefish Bay, culturaily affiliated to Northern Hunters and Fishers, of probable religious significance, still in use by local Ojibway, good condition, site weil known and published in tourist guides. (ibid.: 14) assessed as having "high representability and high interpretability".

Rock type? Not stated

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~, (

Offerings present?

Borden Number Alternative Names: Photographs -were they taken? Measurements taken by each Iperson Method( s) of recording used

Location of field notes

Published works where site referred to

Scholar's name, profession, date(s) of study Location, number of faces recorde d, etc

Rock type? Offerings present?

Borden Number Alternative Names:

Dewdney (1960) found clothing which he termed offerings. Molyneaux (1974: 9) wrote that site found "immediately north of Site 92, these pictographs occur in relation to a very large crevice, the "Devil's Hole". Although there are scattered paintings, predominately smears of pigment, the focal site of this site is this "hole". During the 1974 field season, articles of clothing were discovered in the crack, presumably left as offerings." Fox (1974) found offerings ofbundles of clothingwhich were stuffed into a cleft in the rock surface of DhKm-1

DhKm-18 Site # 104 or Devil's Bay (Dewdney August 19th 1960), Devil's Bay III (Lambert n.d.), Yes - Dewdney (1960); Lambert (n.d.)

12" tall (Dewdney 1960)

Dewdney (1960) - written descriptions, drawings, photographs; Lambert (n.d.) written description, photographs, dot-for-dot recording; Dewdney (1960) - New World Archives, Royal Ontario Museum, Toronto, Ontario; Lambert (n.d.) - unknown where field notes and photographs located but Borden forms available from Ontario Ministry of Citizenship, Culture, and Recreation. Dewdney S. and K. Kidd. 1962 Indian Paintings if the Great Lakes. Toronto: University of Toronto Press. Dewdney S. and K. Kidd. 1967. lndian Paintings rfthe Great Lakes. 2nd

Edition Toronto: University of Toronto Press. Lambert, P. J. n.d. The Northwestern Ontario Roek Art Pro/eet: The 1985 Results and Regional Overview. Unpublished report. Ontario Conservation Archaeology Report. Northwestern Region No number. Ontario Ministry of Citizenship and Culture. Selwyn Dewdney (artist) - 1960; P. J. Lambert (archaeologist) - 1985 (August)

On west side of Devil's Bayon the south side of the Aulneau Peninsula; Dewdney (1960) - Devil's Bay south end ofWhitefish Bay, 96" above water, 49 degrees 14.6' / 94 degrees 4.6' but ocly one image recorded of a hallow winged bird. Not stated Dewdney (1960) - an "offering" site since offerings left below images and collected the ceremonial sticks as he called them and they are currendy held in the Ethnological collection of the ROM. Also Chinaware and enamelware according to Borden form for this site.

DhKm-5 Site # 105 (Dewdney August 19th 1960); Devil's Bay (Molyneaux 1974); Devil's Bay II (Lambert n.d .. )

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Photographs -were they taken? Measurements taken by each

1 pers on Method(s) of recording used

Yes - Dewdney (1960); Lambert (n. d.); Reid (1976), Molyneaux

(1974, 1979) -----c~~~~-~---Dewdney (1960) 3.5 feet and 36" (two sections);

Dewdney (1960) - written descriptions, drawings, photographs; Lambert (n.d.) written description, photographs, dot-for-dot recording; Molyneaux (1974) - photographie documentation of site, description of erosion of site vis-à-vis future protection or conservation Reid (1976) recorded accessibility, possible cultural affiliation, significance, condition/ endangerment, assessed "representability, interpretability" of site, obtained Borden number for site under Heritage Act, photographed and mapped site. Molyneaux - photographs. (1979)

Location of field Dewdney (1960) - New World Archives, Royal Ontario Museum, notes Toronto, Ontario;

Reid (1975) Ontario Ministry of Citizenship, Culture and Recreation, Thunder Bay, Ontario. Lambert (n.d.)- unknown where field notes and photographs located but Borden forms available; Molyneaux (1974) not known Molyneaux. (1979) - field notes in possession of the author and Ontario Heritage Foundation

Published works Dewdney S. and K. Kidd. 1962. Indian Paintings rf the Great Lakes. where site referred to

Toronto: University of Toronto Press. Dewdney S. and K. Kidd. 1967. Indian Paintings rfthe Great Lakes. 2nd

Edition Toronto: University of Toronto Press. Lambert, P. J. n.d. The Northwestern Ontario Rock Art Pro/ect: The 1985 Results and Regional Overview. Unpublished report. Ontario Conservation Archaeology Report. Northwestern Region No number. Ontario Ministry of Citizenship and Culture. Molyneaux, B. L. 1974. Trent University Rock Art Research Prqject Summary Report. 1974 Field Season. Department of Anthropology, Trent University. Reid, C. S. 1976. Environment, Man and Mqymqygwqyshi: The Dimensions rfPast Human Cultural Impact in the Lake rfthe Woods Areaj Regional Archaeologist, Historical Planning and Research Branch, Northwestern Region, Lake of the Woods Planning Area. Molyneaux, B. L. 1979 The Whitefish Bqy Pictograph Pro/ect. Report to the Ontario Heritage Foundation. No licence.

Scholar's name, Selwyn Dewdney (artist) - 1960 ; C. S. "Paddy" Reid (archaeologist) -profession, 1976; Brian Molyneaux (archaeologist) - 1974, 1979; P. J. Lambert date(s) ofstudy j(archaeologist) -1985 (August) Location, number South of Devil's Bay in Whitefish Bay; Lake of the Woods, of faces recorde d, Dewdney (1960) - 48" above water and 3.5' above water etc Molyneaux (1974: 7) not record images but commented that there

were "at least two representations of Bisons on this site, a very rare motif in the Shield area".

Rock type? Not stated

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Offerings present?

Borden Number Alternative Names: Photographs -were they taken? Measurements taken by each

1 pers on Method(s) of recording used

Location of field notes

Published works where site referred to

Scholar's name, profession, date(s) of study

Dewdney - an "offering" site, Offering found below paintings that consisted of prayer sticks and Dewdney and his crew "carefully lifted one corner of the neady piled clothing to find it was all clean and in good repair. No attempt been made to foist off second-rate articles on the mysterious healers" (Dewdneyand Kidd 1967: 55)

DhKn-l Site # 106 (Dewdney August 19th 1960), Obabikon Bay (Molyneaux 1974: 11). Yes - Dewdney (1960); Reid (1976)

Dewdney (1960) - Face 1= 15'16", Face II = 50' long by 2" wide; Molyneaux (1974: 11) - none but speculated that "lizard-like" representation" was over 15 feet long. Reid (1976) - 2 metres square Dewdney (1960) - written descriptions, drawings, photographs; Molyneaux (1974) - photographie documentation of site, description of erosion of site vis-à-vis future protection or conservation Reid (1976) recorded accessibility, possible cultural affiliation, significance, condition/ endangerment, assessed "representability, interpretability" of site, obtained Borden number for site under Heritage Act, photographed and mapped site Dewdney (1960) - New World Archives, Royal Ontario Museum, Toronto, Ontario; Reid (1975) - Ontario Ministry of Citizenship, Culture and Recreation, Thunder Bay, Ontario; Molyneaux (1974) - unknown Dewdney S. and K. Kidd. 1962. Indian Paintings if the Great Lakes. Toronto: University of Toronto Press. Dewdney S. and K. Kidd. 1967. Indian Paintings if the Great Lakes. 2nd

Edition Toronto: University of Toronto Press. Molyneaux, B. L. 1974. Trent Universiry Rock An Research Pro/ect Summary Repon. 1974 Field Season. Department of Anthropology, Trent University. Reid, C. S. 1976. Environment, Man and Mqymqygwqyshi: The Dimensions if Past Human Cultural Impact in the Lake if the Woods Area; Regional Archaeologist, Historical Planning and Research Branch, Northwestern Region, Lake of the Woods Planning Area. Molyneaux, B. L. 1981 Archaeological Fieldwork Report: Licence Number 80-F-0383. Department of New World Archaeology. Toronto: Royal Ontario Museum. Selwyn Dewdney (artist) - 1960; Brian Molyneaux (archaeologist) -1974,1979; C. S. "Paddy" Reid (regional archaeologist) -1976.

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Location, number On the west side of Miles Bayon the south side of the Aulneau of faces recorde d, Peninsula; Dewdney (1960) - Obabikon Narrows (north end of etc Obabikon Bay, Face 1= 22' above water - "serpent", Face II = 18'6"

ab ove water. Molyneaux (1974: 11) wrote that paintings were divided into "two groups, with the most significant motif being a very large lizard-like representation that is over 15 feet in length." Reid (1976: 30) accessed by boat to Miles Bay, culturally affiliated to Northern Hunters and Fishers, of probable religious significance, good condition, sorne fading. (ibid.: 14) assessed as having "high rep_resentability and high interpretability".

Rock type? Molyneaux (1974: 11) granite Offerings Dewdney (Dewdney and Kidd 1967:45) stated that deep cleft existed present? between ledge and "rock wall that almost filled with dirt and rubble.

Lying on the ground were ancient, weathered overcoat and various rags that had rotted beyond recognition".

Borden Number DhKo-l Alternative Site #108 (Dewdney August 20th 1960); Painted Rock Island Names: 1 (Molyneaux 1974); Painted Rock (Reid 1976) Photographs - Yes - Dewdney (1960); Reid (1976); Molyneaux (1974, 1981) were they taken? Measurements Reid (1976) - 1.5 metres square taken by each [person Method(s) of Dewdney (1960) - written descriptions, drawings, photographs, field recording used reproductions (paintings traced by standing on log held by ropes),

"vigorously sponged off' the lichen (Dewdney and Kidd 1967: 46) to record images. Molyneaux (1974) - photographic documentation of site, description of erosion of site vis-à-vis future protection or conservation Reid (1976) recorded accessibility, possible cultural affiliation, significance, condition/ endangerment, assessed "representability, interpretability" of site, obtained Borden number for site under Heritage Act, photographed and mapped site. Molyneaux (1981) - unknown

Location of field Dewdney (1960) - New World Archives, Royal Ontario Museum, notes Toronto, Ontario;

Molyneaux (1974) - unknown Reid (1975) Ontario Ministry of Citizenship, Culture and Recreation; Thunder Bay, Ontario. Molyneaux (1981) -unknown

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Published works Dewdney S. and K. Kidd. 1962. Indian Paintings if the Great Lakes. where site Toronto: University of Toronto Press. referred to Dewdney S. and K. Kidd. 1967. Indian Paintings if the Great Lakes. 2nd

Edition Toronto: University of Toronto Press. Molyneaux, B. L. 1974. Trent University Rock Art Research Pro/ect Summary Report. 1974 Field Season. Department of Anthropology, Trent University. Reid, C. S. 1976. Environment, Man and Mqymqygwqyshi: The Dimensions if Past Human Cultural Impact in the Lake if the Woods Area; Regional Archaeologist, Historical Planning and Research Branch, Northwestern Region, Lake of the Woods Planning Area. Molyneaux, B. L. 1981 Archaeological Fieldwork Report: Licence Number 80-F-0383. Department of New World Archaeology. Toronto: Royal Ontario Museum.

Scholar's name, Selwyn Dewdney (artist) - 1960 (August 20); Brian Molyneaux profession, (archaeologist) - 1974, 1981; C. S. "Paddy" Reid (regional date(s) of study archaeologist) - 1976. Location, number On north side of Painted Rock Island on the south side of the of faces recorded, Aulneau Peninsula; Dewdney (1960) - part obscured by lichen, 7 etc feet ab ove water, south of Splitrock Island, ledge = approximately

12 feet above water, exposure of face = 3 degrees east of north, crack in face of rock. Molyneaux (1974: 12) wrote "although many of the paintings are indistinct, there are several particularly fine examples of shamanic figures". Molyneaux (1981) - unknown Reid (1976: 30) accessed by boat to Painted Rock Channel, culturaIly affiliated to Northern Hunters and Fishers, of probable religious significance, still in use by local Ojibway, good condition, weIl known and published in tourist guides. (ibid.: 14) assessed as having "high representability and high interpretability".

Offerings Dewdney (1967 publication with Kidd) no offerings present present? Rock type? Molyneaux (1974: 12) granite

Borden Number DgK1-17 Alternative Cyclone Point Pictographs #1 (Pastershank 1989) Names: Photographs - Yes - Pastershank (1989) were they taken? Measurements Pastershank - 35 metres (h) by 36 metres (w) -check that this site? taken by each person Method(s) of Pastershank (1989) dot-for-dot field recording of site, field recording used reproductions, field notes, photographs. Location of field Pastershank (1989) Ontario Ministry of Culture and Recreation, notes Thunder Bay, Ontario. Published works Pastershank, G. 1989. An Archaeological Surot})! if Sabaskong Bqy, Lake where site if the Woods. Ontario Conservation Archaeology Report #13, North-referred to western Region. Kenora: Ontario Ministry of Culture and

Communications.

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Scholar's name, Georgine Pastershank (archaeologist / biologist) - 1989 profession, date( s) of study Location, number Southeast corner of Sabaskong Penin sula on Cyclone Point, on well-of faces recorde d, travelled water route from Splitrock Narrows into northeast arm of etc Sabaskong Bay, bedrock ledge; Pastershank (1989) - Face l = an

addition al 5-4 metres past a southward bend - Face II = 7 metres from eastern start of cliff - 21 degrees from vertical, Face III = 7 metres from eastern start of cliff.

Rock type noted? No, just fact that site exist on bedrock Offerings None observed

1 present?

Borden Number DgKl-19 Alternative Cyclone Point Pictographs #2 (pastershank 1989). Names: Photographs - Yes - Pastershank (1989) were they taken? Measurements taken by each Iperson Method( s) of Pastershank (1989) dot-for-dot field recording of site, field recording used reproductions, field notes, photographs, Location of field Pastershank (1989) Ontario Ministry of Culture and Recreation; notes Thunder Bay, Ontario Published works Pastershank, G. 1989. An Archaeological Survry 0/ Sabaskong Bqy, Lake where site 0/ the Woods. Ontario Conservation Archaeology Report #13, North-referred to western Region. Kenora: Ontario Ministry of Culture and

Communications. Scholar's name, Georgine Pastershank (archaeologist / biologist) - (1989) profession, date( s) of study Location, number Located on same bedrock as DgKl-17 only 18 metres west. of faces recorde d, Designated by Pastershank (1989: 67) as separate sites based upon etc different styles, elevations and hues of pigments used which

Pastershank argued indicated the two sites were not contemporaneous. Pastershank (1989) One Face divided into two panels that exist because of a "perpendicular, south-facing hiatus of bedrock, nine-centimetres-wide" (ibid.: 69).

Rock type noted? No, just fact that site exist on bedrock Offerings None observed

1 present?

Borden Number DgKl-2

Alternative Site # 198 and Sabaskong Bay II (Dewdney August 20d 1964); Three Names Caverns Pictograph Site (pastershank 1989) Photographs - Yes - Dewdney (1964); Reid (1976), Pastershank (1989) were they taken?

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Measurements of Pastershank (1989) - entire site measures 48 metres (h) by 18 metres rock art section (w). Pastershank (1989) - Face II = 290 cm by 107 cm, Face VII = (height by width) 27 cm long iftaken Method( s) of Dewdney (1964) - written descriptions, drawings, photographs. recording used Reid (1976) recorded accessibility, possible cultural affiliation,

significance, condition/ endangerment, assessed "representability, interpretability" of site, obtained Borden number for site under Heritage Act, photographed and mapped site. Pastershank (1989) dot-for-dot field recording of site, field reproductions, field notes, QhotograQhs.

Location of field Dewdney (1964) New World Archives, ROM, Toronto; Reid (1975) Notes Ontario Ministry of Citizenship, Culture and Recreation; Thunder

Bay, Ontario. Pastershank (1989) Ontario Ministry of Culture and Recreation, Thunder Bay, Ontario

Published works Dewdney S. and K. Kidd. 1962. Indian Paintings of the Great Lakes. -where site Toronto: University of Toronto Press. referred? Dewdney S. and K. Kidd. 1967. Indian Paintings of the Great Lakes. 2nd

Edition Toronto: University of Toronto Press. Reid, C. S. 1976. Environmen~ Man and Mqymqygwqyshi: The Dimensions ofPast Human Cultural Impact in the Lake of the Woods Areaj Regional Archaeologist, Historical Planning and Research Branch, Northwestern Region, Lake of the Woods Planning Area. Pastershank, G. 1989. An Archaeological Surory of Sabaskong Bqy, Lake of the Woods. Ontario Conservation Archaeology Report #13, North-western Region. Kenora: Ontario Ministry of Culture and Communications.

Scholar's name, Selwyn Dewdney (artist) - 1964; C. S. "Paddy" Reid (regional profession, archaeologist) - 1976. Georgine Pastershank (archaeologist / date(s) of study biologist) - (1989) Location, number Dewdney (Dewdney (1964) only records existence of one face called of faces recorded, Face l by Pastershank (1989), in Dewdney and Kidd (1967: 110) etc states that "only the finger draggings of a smeared area qualify it as a

pictograph site; but they are associated with a low shallow cave where a large lens of rock softer than the prevailing dark, schistose one that has weathered out". Reid (1976: 30) accessed by boat to Sabaskong Bay, culturally affiliated to Northern Hunters and Fishers, of probable religious significance, good condition, well known and published in tourist guides. (ibid.: 15) assessed as having "high representability and high interpretability" . Pastershank (1989) On east side of Sabaskong Peninsula at south end of NE arm of Sabaskong Bay; at the base of the cliff within the rock shelter = 3 tiny roof-laminated caverns; pictographs are generally west facing but N end of rock shelter bends to make a S-facing panel; 7 faces Face l = on N wall (grotto = 18 cm below paintings; Face II = within rock shelter, Face III = within rock shelter, down and to the left of II, Face IV = within rock shelter, Faces V - VI - VII = on bending section of overhang of rock shelter,

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Rock type?

Offerings present?

Dewdney (Dewdney and Kidd 1967: 110) dark schistose with larger lens of softer rock whlch has weathered out in low shallow cave

~~

Dewdney (1964) - none Pastershank (1989) - fresh tobacco in small crack 53 cm below figure (Morph 10) on Face II

Borden Number DgKl-l

Alternative Names Photographs -were they taken? Measurements of rock art section (height by width) iftaken Method(s) of recording used

Location of field Notes

Published works -where site referred?

Scholar' s name, profession, date(s) of study

Site # 197 and Sabaskong Bay l (Dewdney August 2nd

Sabaskong Bay Pictograph Site (pastershank 1989) Yes - Reid (1976), Pastershank (1989)

1964); The

Dewdney (1964) - written descriptions, drawings, photographs; Reid (1976) recorded accessibility, possible cultural affiliation, significance, condition/ endangerment, assessed "representability, interpretability" of site, obtained Borden number for site under Heritage Act, photographed and mapped site. Pastershank (1989) dot-for-dot field recording of site, field reproductions, field notes, photographs. Dewdney (1964) New World Archlves, Royal Ontario Museum, Toronto, Ontario; Reid (1975) Ontario Ministry of Citizenship, Culture and Recreation; Thunder Bay, Ontario. Pastershank (1989) Ontario Ministry of Culture and Recreation, Thunder Bay, Ontario Dewdney S. and K. Kidd. 1962. Indian Paintings rf the Great Lakes. Toronto: University of Toronto Press. Dewdney S. and K. Kidd. 1967. Indian Paintings rfthe Great Lakes. 2nd

Edition Toronto: University of Toronto Press. Reid, C. S. 1976. Environment, Man and Mqymqygwqyshi: The Dimensions rfPast Human Cultural Impact in the Lake rfthe Woods Area; Regional Archaeologist, Historical Planning and Research Branch, Northwestern Region, Lake of the Woods Planning Area. Pastershank, G. 1989. An Archaeological Survry rf Sabaskong Bqy, Lake rf the Woods. Ontario Conservation Archaeology Report #13, North­western Region. Kenora: Ontario Ministry of Culture and Communications. Selwyn Dewdney (artist) - 1964; C. S. "Paddy" Reid (regional archaeologist) -1976; Georgine Pastershank (archaeologist / biologist) - (1989)

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Location, number Dewdney (1964) only records existence of two Faces; Dewdney and of faces recorde d, Kidd 1967:110) argues "paintings either side of angular rock. On the etc le ft are two likely bears -regardless of the long ears on the one - and

their tracks, and to the right are canoes and tally marks. Bears and tally marks frequently appear on the Miday scroIls, but never in this kind of configuration. l would judge that both groups are by the same hand." Reid (1976: 30) accessed by boat to Sabaskong Bay, culturally affiliated to Northern Hunters and Fishers, of probable religious significance, good condition, weIl known and published in tourist guides. (ibid.: 15) assessed as having "high representability and high interpreta bili ty" . Pastershank (1989: 51-54) divided this face into three Faces. Situated in central southern most area of a first small jutting protrusion from the north west of Sabaskong Peninsula (ibid.: 51). Most northern of aIl the pictograph sites in Sabaskong Bay.

Rock type? Dewdney (Dewdney and Kidd 1967: 110) schistose

Offerings present?

Borden Number

Alternative Names Photographs -were they taken? Measurements of rock art section (height by width) iftaken Method( s) of recording used Location of field Notes

Published works - where site referred?

Scholar's name, profession, date( s) of study Location, number of faces recorde d, etc Rock type noted?

Offerings Ipresent?

Pastershank (1989: 51) observed that "crack in the bedrock at juncture between Face 1 and Face II that presently being used as a tobacco offering ledge. This crack is located 80 centimetres diagonaIly from the morphs.

DkKn-7

Blindfold Lake Pictograph; Rushing River IV Pictograph Site

Yes -Lambert (.n.d.)

Lambert (n.d.) written description, photographs, dot-for-dot recording Lambert (n.d.) - unknown where field notes and photographs located but Borden forms available from Ontario Ministry of Citizenship, Culture and Recreation; Lambert, P. J. n.d. The Northwestern Ontario Rock Art Pro/ect: The 1985 Results and Regional Overview. Unpublished report. Ontario Conservation Archaeology Report. Northwestern Region No number. Ontario Ministry of Citizenship and Culture. P. J. Lambert (archaeologist) - 1985 Ouly)

One of several sites on Blindfold Lake. Lambert (n.d.) stated on Borden form that not noted by Dewdney and Kidd 1967 and not known by local residents Not stated

Not stated

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Borden Number DkKn-6

Alternative Blindfold Lake Pictograph; Blindfold Site II, Rushing River III, Names Rummery Site Photographs - Yes -Lambert (n.d.) were they taken? Measurements of rock art section (height by width) iftaken Method( s) of Lambert (n.d.) written description, photographs, dot-for-dot recording used recording; Location of field Lambert (n.d.)- unknown where field notes and photographs located Notes but Borden forms available from Ontario Ministry of Citizenship,

Culture and Recreation; ~-- - --- -- - --- --- -- --- -------------

Published works Lambert, P. J. n.d. The Northwestern Ontario Rock Art P,o/ect: The 1985 -where site Results and Regional Overview. Unpublished report. Ontario referred? Conservation Archaeology Report. Northwestern Region No

number. Ontario Ministry of Citizenship and Culture. Scholar' s name, P. J. Lambert (archaeologist) - 1985 Guly) profession, date( s) of study Location, number One of several sites on Blindfold Lake of faces recorded, etc Rock type noted? Not stated

Offerings Not stated present?

Borden Number DjKn-l

Alternative Rushing River l, Site # 29 (Dewdney 1958); Blindfold Lake Names (Molyneaux 1974: 14); The Blindfold Lake Pictograph (Lambert n.

d.) Photographs - Yes - Dewdney (1958); Molyneaux (1974); Reid (1976); Lambert were they taken? ICn.d) of Face l and Face II; Rusak 1993 Measurements of rock art section (height by width) iftaken

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Method( s) of Ashdown (1973) - written description and map recording used Dewdney (1958) - written descriptions, drawings, photographs;

Molyneaux (1974) - photographic documentation of site, description of erosion of site vis-à-vis future protection or conservation Reid (1976) recorded accessibility, possible cultural affiliation, significance, condition/ endangerment, assessed "representability, interpretability" of site, obtained Borden number for site under Heritage Act, photographed and mapped site. Lambert (n.d.) written description, photographs, dot-for-dot recording; Rusak (1991) photographs and dot-for-dot recording

Location of field Ashdown (1973) - unknown Notes Dewdney (1958) - New World Archives, Royal Ontario Museum,

Toronto, Ontario; Molyneaux (1974) unknown Reid (1975) Borden forms, Ontario Ministry of Citizenship, Culture and Recreation; Thunder Bay, Ontario; Pelshea (1978) unknown where field notes etc located. Lambert (1985) - unknown where field notes and photographs located but Borden forms available from Ontario Ministry of Citizenship, Culture and Recreation, Thunder Bay, Ontario. Rusak (1993) field recordings, field notes in Ontario Ministry of Citizenship, Culture and Recreation, Thunder Bay, Ontario, photographs unknown

Published works Ashdown, J. H. 1973. A Contemporary Explorer's Chart to the Lake if the -where site Woods. Kenora: Royal Yacht Club of the Lake of the Woods referred? Dewdney S. and K. Kidd. 1962 lndian Paintings if the Great Lakes.

Toronto: University of Toronto Press. Dewdney S. and K. Kidd. 1967. Indian Paintings if the Great Lakes. 2nd

Edition Toronto: University of Toronto Press. Molyneaux, B. L. 1974. Trent University Rock Art Research Prqject Summary Report. 1974 Field Season. Department of Anthropology, Trent University. Lambert, P. J. n.d. The Northwestern Ontario Rock Art Pro/eet: The 1985 Results and Regional Overview. Unpublished report for Northwestern Region Conservation Archaeology Report. No number. Reid, C. S. 1976. Environment, Man and Mqymqygwqyshi: The Dimensions ifPast Human Cultural Impact in the Lake if the Woods Area; Regional Archaeologist, HistorÏcal Planning and Research Branch, Northwestern Region, Lake of the Woods Planning Area

Scholar' s name, J. H. Ashdown (traveller) - 1973; Selwyn Dewdney (artist) - 1958; profession, Molyneaux (1974); C. S. "Paddy" Reid (regional archaeologist) -date( s) of study 1976; Victor Pelshea (archaeologist) - 1978; P. J. Lambert - 1985

(July); Jacqueline Rusak (archaeologist) - 1993

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Location, number Molyneaux (1974:14) stated that the range and the strong colours of of faces recorde d, the paintings at this site "makes it a significant site in the area." etc Reid (1976: 29) accessed by boat or from dirt road from Highway

17, cultural1y affùiated ta Northern Hunters and Fishers, of probable religious significance, good condition and covered by high water in summer months. (ibid.: 14) assessed as having "high representability and high interpretability"

Rock type noted? Not mentioned

Offerings present?

Borden Number

Alternative Names Photographs -were they taken? Measurements of rock art section (height by width) iftaken Method(s) of recording used

Location of field Notes

Dewdney wrote that offerings were found at this site Molyneaux (1974: 14) wrote that the rock shelf at this site was "used for the deposition of offerings, indicating an active, contemporary belief in the sacred qualities of this site".

DiKp-1

Site # 70 (Dewdney Aug 12th 1959); Sunset Channel; 25thJuly 1975 l(Molyneaux 1975 for the TRAP study), Cliff Island Yes - Reid (1976), Molyneaux (1975)

Dewdney (Aug 12th 1959) - 50 cm (h);

Ashdown (1973) - written description and map Dewdney (1959) - written descriptions, drawings, photographs; Reid (1976) recorded accessibility, possible cultural affiliation, significance, condition/ endangerment, assessed "representability, interpretability" of site, obtained Borden number for site under Heritage Act, photographed and mapped site. Molyneaux (1975) assessed to establish the condition regarding moisture access, seepage deposit formation, seepage deposit flaking, exfoliation, and biological growth. Site its physical condition with regard to these criteria. Site location recorded, scale drawings of the images, general site data and condition and description of undertaken. Ashdown (1973) - unknown. Dewdney (1959) - New World Archives, Royal Ontario Museum, Toronto, Ontario; Molyneaux (1975) TRAP Project. Field notes possession of the Canadian Conservation Institute Reid (1975) Borden forms, Ontario Ministry of Citizenship, Culture and Recreation, Thunder Bay, Ontario.

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Published works Ashdown, J. H. 1973. A Contemporary Explorer's Char! to the Lake of the -where site Woods. Kenora: Royal Yacht Club of the Lake of the Woods referred to? Dewdney S. and K. Kidd. 1962 Indian Paintings of the Great Lakes.

Toronto: University of Toronto Press. Dewdney S. and K. Kidd. 1967. Indian Paintings of the Great Lakes. 2nd

Edition Toronto: University of Toronto Press. Lawson, A. C. 1885. Ancient Rock Inscriptions on the Lake of the Woods. American Naturalist XIX (7): 654-657. Reid, C. S. 1976. Environment, Man and Mqymqyqwqyshi: The Dimensions ofPast Human Cultural Impact in the Lake of the Woods Area; Regional Archaeologist, Historical Planning and Research Branch, Northwestern Region, Lake of the Woods Planning Area. Molyneaux, B. L. 1975. CCI/TRAP Pictograph Condition Inspection Survey. Ottawa: Canadian Conservation Institute.

Scholar's name, A. C. Lawson (geologist) - 1885; Selwyn Dewdney (artist) - 1959 profession, (August 12);]. H. Ashdown (traveIler) - 1973; C. S. "Paddy" Reid date( s) of study (archaeologist) - 1975 Location, number On south side of Cliff Island, Sunset Channel, north on Aulneau of faces recorded, Peninsula, near DiKo-2. etc Reid (1976: 29) accessed by boat to Sunset Channel, culturaIly

affùiated to Northern Hunters and Fishers, still in use by local Ojibway, good condition, weIl known and published in tourist guides. (ibid.: 14) assessed as having "high representability and high interpretability"

Rock type noted? Not mentioned

Offerings Not mentioned present?

Borden Number DhKm-3

Alternative Site # 69 (Dewdney August 8th 1959) Names Photographs - Yes, Dewdney (1959), Reid (1976), Molyneaux (1979), were they taken? Measurements of rock art section (height by width) iftaken Method( s) of Dewdney (August 8th 1959) - written descriptions, drawings, recording used photographs.

Reid (1976) recorded accessibility, possible cultural affiliation, significance, condition/ endangerment, assessed "representability, interpretability" of site, obtained Borden number for site under Heritage Act, photographed and mapped site. Molyneaux (1979) -Photography

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Location of field Dewdney (1959) - New World Archives, Royal Ontario Museum, Notes Toronto, Ontario.

Reid (1975) Borden forms, Ontario Ministry of Citizenship, Culture and Recreation, Thunder Bay, Ontario. Pelshea (1978) unknown where field notes etc located. Molyneaux (1979) in possession of the author and Ontario Heritage Foundation

Published works Dewdney S. and K. Kidd. 1962. Indian Paintings if the Great Lakes. -where site Toronto: University of Toronto Press. referred to? Dewdney S. and K. Kidd. 1967. Indian Paintings if the Great Lakes. 2nd

Edition Toronto: University of Toronto Press. Reid, C. S. 1976. Environment, Man and Mqymqygwqyshi: The Dimensions ifPast Human Cultural Impact in the Lake iftbe Woods Area; Regional Archaeologist, Historical Planning and Research Branch, Northwestern Region, Lake of the Woods Planning Area. Molyneaux, B. L. 1979 The Whitefish Bqy Pictograph Pro/ect. Report to the Ontario Heritage Foundation. No licence.

Scholar' s name, Selwyn Dewdney (artist) - 1959; C. S. "Paddy" Reid (archaeologist) profession, - 1976; P. J. Lambert (archaeologist) - 1985; Victor Pelshea date(s) of study 1 (archaeologist) - 1978; Brian Molyneaux (archaeologist} - 1979. Location, number Dewdney (1959) Three Faces subdivided by bands of white mineraIs of faces recorde d, on rock surface. Site on Picture Rock Island in Whitefish Bay. On etc cliff face but immediately beside water.

Reid (1976: 30) Southern end ofWhitefish Bay; accessed by boat to Whitefish Bay, culturally affiliated to Northern Hunters and Fishers, of probable religious significance, good condition, site weIl known and published in tourist guides. (ibid.: 14) assessed as having "high representability and high interpretability".

Rock type noted? Not stated

Offerings Dewdney (1959) no offerings present present?

Borden Number DgKm-l

Alternative names Splitrock Bay (Reid 1976)

Photographs - Yes, (Reid 1976) were they taken? Measurements of rock art section (height by width) iftaken Method(s) of Reid (1976) recorded accessibility, possible cultural affiliation, recording used significance, condition/ endangerment, assessed "representability,

interpretability" of site, obtained Borden number for site under Heritage Act, photographed and mapped site.

Location of field Reid (1975) Borden forms, Ontario Ministry of Citizenship, Culture Notes and Recreation, Thunder Bay, Ontario

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Published works Reid, C. S. 1976. Environment, Man and MqymqyglJJqyshi: The Dimensions

-where site rifPast Human Cultural Impact in the Lake rifthe Woods Area; Regional referred? Archaeologist, HistorÏcal Planning and Research Branch,

Northwestern Region, Lake of the Woods Planning Area. Scholar's name, C. S. "Paddy" Reid (archaeologist) - 1976 profession, date( s) of study Location, number Reid (1976: 31) accessed by boat ta Splitrock Bay, culturally affiliated of faces recorde d, ta Northern Hunters and Fishers, of probable religious significance, etc good condition, site well known and published in tourist guides.

(ibid.: 15) assessed as having "high representability and high interpretability".

Rock type noted? Not stated

Offerings Not stated 1 present?

Borden Number Dewdney Site # 94 - no Borden number

Alternative names

Photographs - Yes, Dewdney (1960) were they taken? Measurements of rock art section (height by width) iftaken Method(s) of Dewdney (1960) - written descriptions, drawings, photographs. recording used Location of field Dewdney (1960) - written descriptions, drawings, photographs; Notes Published works Dewdney (1960) - New World Archives, Royal Ontario Museum, -where site Toronto, Ontario. referred? Scholar's name, Selwyn Dewdney (artist) - 1960 profession, date( s) of study Location, number of faces recorded, etc Rock type noted?

Offerings Offerings in a crack below site (Dewdney and Kidd 1967: 44) 1 present?

Borden Number DiKn-l

Alternative names Hay ter Peninsula, Dewdney # 91

Photographs - Yes, Dewdney - (15th July 1961), Molyneaux (1979), Reid (1976) were they taken?

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Measurements of rock art section (height by width) iftaken Method( s) of Dewdney (1961) - written descriptions, drawings, photographs; Reid recording used (1976) recorded accessibility, possible cultural affùiation,

significance, condition/ endangerment, assessed "representability, interpretability" of site, obtained Borden number for site under Heritage Act, photographed and mapped site. Molyneaux (1979)

Location of field Dewdney (1961) - New World Archives, Royal Ontario Museum, Notes Toronto, Ontario;

Reid (1975) Borden forms, Ontario Ministry of Citizenship, Culture and Recreation, Thunder Bay, Ontario Molyneaux (1979) - photographs

Published works Dewdney S. and K. Kidd. 1962. Indian Paintings rif the Great Lakes. -where site Toronto: University of Toronto Press. referred? Dewdney S. and K. Kidd. 1967. Indian Paintings rif the Great Lakes. 2nd

Edition Toronto: University of Toronto Press. Molyneaux, B. L. 1979 The Whiteftsh Bqy Pictograph Prrject. Report to the Ontario Heritage Foundation. No licence. Reid, C. S. 1976. Environment, Man and Mqymqygwqyshi: The Dimensions rifPast Human Cultural Impact in the Lake rifthe Woods Area; Regional Archaeologist, Historical Planning and Research Branch, Northwestern Region, Lake of the Woods Planning Area.

Scholar's name, Selwyn Dewdney (artist) - (15th July 1961); Brian Molyneaux profession, (archaeologist) 1979; C. S. "Paddy" Reid (archaeologist) - 1976; date(s) of study Location, number Dewdney (1961) Northeast tip of Hay ter Peninsula at north entrance of faces recorde d, to Whitefish Bay, Lake of the Woods. Three Faces each subdivided etc into parts (a) and (b) because a group of paintings existed above

ledge and group of paintings immediately beside water's edge. Rock type noted?

Offerings Dewdney (Dewdney and Kidd 1967: 52) wrote that found "no present? prayer sticks; but an odd chine [china] cup and other odds and ends

were visible in a horizontal crack nearby".

Borden Number DjKn-2

Alternative names Route Bay (Lambert n.d.), Rushing River III

Photographs - Yes, Reid (1976); Lambert (n.d.) were they taken? Measurements of rock art section (height by width) iftaken

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Method( s) of Lambert (n.d.) written description, photographs, dot-for-dot recording used recording;

Reid (1976: 14) recorded accessibility, possible cultural affiliation, significance, condition/ endangerment, assessed "representability and interpretability" of site, obtained Borden number for site under Heritage Act, photographed and mapped site.

Location of field Lambert (n.d.) unknown where field notes and photographs located Notes but Borden forms available from Ontario Ministry of Citizenship,

Culture and Recreation; Published works Lambert, P. J. n.d. The Northwestern Ontano Rock Art Project: The 1985 -where site Results and Regional Overview. Unpublished report. Ontario referred? Conservation Archaeology Report. Northwestern Region No

number. Ontario Ministry of Citizenship and Culture. Reid, C. S. 1976. Environment, Man and Mqymqygwqysht~· The Dimensions rfPast Human Cultural Impact in the Lake rfthe Woods Area; Regional Archaeologist, Historical Planning and Research Branch, Northwestern Region, Lake of the Woods Planning Area.

Scholar' s name, C. S. "Paddy" Reid (archaeologist) - 1976; P. J. Lambert profession, (archaeologist) - 1985 Guly) date(s) of study Location, number Reid (1976: 25), accessed by boat or 500 yards through bush from of faces recorde d, dirt road, culturally affiliated to Northern Hunters and Fishers, of etc probable religious significance, good condition, and sorne danger of

defacement as well known. (ibid.: 14) assessed as "high representability and high interpretability"

Rock type noted? Not stated

Offerings Not stated 1 present?

Borden Number Dewdney's Site #95 - no Borden number

Alternative names Picture Rock Point; Site # 95 (Dewdney 1960)

Photographs - Yes, Dewdney (1960) were they taken? Measurements of rock art section (height by width) iftaken Method( s) of Dewdney (1960) - written descriptions, drawings, photographs; recording used Reid (1976: 13) recorded accessibility, possible cultural affiliation,

significance, condition/ endangerment, assessed representability and interpretability" of site, obtained Borden number for site under Heritage Act, photographed and mapped site.

Location of field Dewdney (1960) - New World Archives, Royal Ontario Museum, Notes Toronto, Ontario.

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Published works Dewdney S. and K. Kidd. 1962. Indian PaintingJ qfthe Great LakeJ. - where site Toronto: University of Toronto Press. referred? Dewdney S. and K. Kidd. 1967. Indian Paintings 0/ the Great Lakes. 2nd

Edition Toronto: University of Toronto Press. Reid, C. S. 1976. Environment, Man and Mqymqygwqyshi: The Dimensions 0/ Past Human Cultural Impact in the Lake 0/ the Woods Area; Regional Archaeologist, Historical Planning and Research Branch, Northwestern Region, Lake of the Woods Planning Area

Scholar' s name, Selwyn Dewdney (artist) -1960; C. S. "Paddy" Reid (archaeologist) -profession, 1976; date( s) of study Location, number Dewdney (1960) Western Peninsula. Reid (1976: 26) by boat to of faces recorded, western Peninsula culturally affiliated to Northern Hunters and etc Fishers, Major pictograph site, still in use by local Ojibway. Fair

condition because local bigots splashed paint when Ojibway use became known. (ibid.: 13) assessed " as high representability and high inteq.,retability"

Rock type noted? Not stated

Offerings Dewdney and Kidd (1967: 44) "found offerings on water lapped present? ledge: neatly folded clothing and a towel, topped by a little pile of

tobacco."

Borden Number No Borden number

Alternative names Site # 270 (Dewdney 1967) on Horseshoe Island

Photographs - Yes, Dewdney (1967) were they taken? Measurements of rock art section (height by width) iftaken Method(s) of Dewdney (1967) - photographs; mentioned in a notebook recording used Location of field Dewdney (1967) - New World Archives, Royal Ontario Museum, Notes Toronto, Ontario. Published works None -where site referred? Scholar's name, Selwyn Dewdney (artist) -1967 profession, date(s) of study Location, number Dewdney - Horseshoe Island, Whitefish Bay of faces recorded, etc Rock type noted? Not stated

Offerings Not stated 1 present?

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Appendix 2: What sorne of the Tools of Adobe PhotoShop 6.0 can reveal.

This appendix has severai screenshots taken while utilising the different toois

available in Adobe Photos hop 6.0. Each illustrates what happened to the image of DiKp-

1 when examined to establish the edges of the images, including any that may have faded.

The image below of DiKp-l was loaded into Adobe:

Figure Appendix 2.1: DiKp-l

Figure Appendix 2.2: The tiff file called DiKp-l as seen once loaded in the software.

It was subsequently examined, once it had been zoomed in using the tool called hue and

or saturation and the following screenshot resulted.

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Figure Appendix 2.3: The shapes visible using the desaturate tool.

It is clear in the screenshot above that the desaturate tool highlights the presence of red

pigment on the surface of the rock.

Figure Appendix 2.4: Manipulation of the colour red using the red colour channel.

Here colour is removed ta see whether the edges of the red shapes can be determined.

The brightnessj contrast tool was the next tool to be used. The screenshot below (figure

appendix 2.5) is the same tiff before it was manipulated using the brightness and contrast

tool.

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Figure Appendix 2.5: The tiff when it was being manipulated.

The screenshot below (figure appendix 2.6) can occur once with the manipulation of the

brightness/ contrast tool. The red image on the rock surface becomes very visible since

the tool highlights the differences.

Figure Appendix 2.6: The colour is removed.

The screen shot below (figure appendix 2.7) is what the tiff fùe of DiKp-l might look

like if the levels of the red channel of the colour balance tool are manipulated and either , reduced or increased beyond its level when the fùe was imported into the software.

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~ ..

Figure Appendix 2.7: The image me during the process ofusing the red colour channel.

The red colour channel is very useful as the screenshot below (figure appendix 2.8)

illustrates since the redness of the ochre images becomes highlighted and emphasised

distinguishing itself From the red of the granite.

Figure Appendix 2.8: The colours are being manipulated using the red colour channel.

The green colour channel is useful as the screenshot below (figure appendix 2.8)

demonstrates since the red images are highlighted.

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.r---. Figure Appendix 2.9: The use of the green colour channel.

The green colour channel is equally as useful as the red colour channel but it is clear if the

figure below is compared with the one above that a small decrease in the green colour

causes the red images on DiKp-l to have clearer outlines (see figure appendix 2.10).

Figure Appendix 2.10: The images have clearer edges.

The blue colour channel was subsequently used to examine these red images and to

determine whether they were clearer or harder to distinguish by altering the quantity of

blue in the tiff flle.

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Figure Appendix 2.11: The images have clearer edges.

The figure above illustrates the shapes of the pictographs at the maximum level of colour

saturation using the blue colour channel. While the figure below shows what occurred to

the same images when the levels of blue were considerably reduced.

Figure Appendix 2.12: The same images.

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Appendix 3: A Blank Copy of Form A and Form B for Sites on CHffs and Caves.

Form A for Both CHffs and Caves:

Borden Number Recorder Date

Place Name Researcher's site number Alternate Site Names Previous Site Names Spatial Co-ordinates (lat/long) NTSmap Elevation Geographic Notes Present Day Nearby Settlements Land Masses Access Regional Drainage Water Systems (direction of flow) Uses of Body ofWater Period of use for body of water (in years) Presence of Water (on # of sides) Body of water surrounding/ adjacent to site Freeze/Partially freeze in winter Water Level Fluctuation (yes/no) Cause of water level fluctuation Extent of Fluctuation (inches per annum) Control ofWater Levels by whom/what? Se as on ofWater Level Fluctuation Major Changes in Regional Water Level (in years) Visible Water Levels (number, height) Location (cliff faces/rock outcrops/ caverns/ out of water) General Notes

Form B for Pictographs on Cliff Faces:

Borden Number

Recorder Date Units of measurement Type of rock Number of cliff(s)

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Height of top of cliff(s) from present day water level Number of visible water lines Height of top of cliff(s) from visible water line Vegetation of top of cliff(s) Vegetation on side/ surface of cliff(s) Vegetation on base of cliff(s) Rock overhangs Proximity of rock overhangs to paintings Large cracks Proximity of large cracks to paintings Large crevasses Proximity of crevasses to paintings Rock shelf/ shelves Proximity of rock shelf/shelves topaintin~s Rocks present at base of cliff(s) Offerings Number of angles of painted face + location (base, middle, top) Orientation of angles (NSEW) Methods of Recording General Notes (exfoliation, white mineraI deposit, lichen and rock tripe encroachment)

Form B for Pictographs inside Caves:

Borden Number

Recorder Date Units of measurement Type of rock Number of cave(sl refer to field drawing Height of cave from p~esent day water level Number of visible water lines Height of top of cave from visible water line Width of cave Vegetation of to~ of cave Vegetation on side/ surface of cave Vegetation on base of cave Rock overhangs Large cracks Proxirnity of large cracks to paintings Large crevasses Proximity of crevasses to paintings Rock shelf/ shelves

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Rocks present at base of cave Offerings Orientation of cave opening(s) Method(s) of recording General Notes (exfoliation, white mineraI deposit, lichen and rock tripe encroachment)

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Appendix 4: The Mod File used by Kleio lAS

Below is the physical structure of the data in the DAT file. The structure of the data

represents the logical relationship between the parts of the data. The structure starts out with

the most abstract level at the top, and becomes more concrete. The elements must be

identified first.

data base name=design;first=i;overwrite=yes;write=structure element name=assigned_no;image=digital;type=image element name=access;write="access_to_site" element name=alcname;write= "alternative_name" element name=annotation;write="interesting .. jnfo_re_tale" element name=author;write="author_oCtale" element name= bhosadsi;write="body _oC watecsurrounding/ adjacencto_site" element name=birchbark;write= "birchbark" element name= bark_contxt;write=" contexC oCbirchbark" element name=bordenn;write="borden_number" element name=claimed_status;write=" specific........geographical_region" element name=colour;write="colour" element name=date;write="date_oCfield_recording" element name=date_info_collected;write="date_information_collected" element name=exfoliat;write= "exfoliation"; element name=extent;write="extent_of_fluctuation" element name=fielinfo;write="fieldnotes" element name=format;write=" format" element name=freefw;write="freeze/partially_freeze_in_winter" element name=gen_notes;write=" general_notes" element name=geo~not;write="geographical"notes" element name=group_belon~to;write="group_tale_belon~to" element name= hcavprwl;write= "heighC oCtop _ oCcavern_from_presencday _ wateclevel" element name=hcliprwl;write="heighcoCtop_oCcliffs_from_present_day_wateclevel" element name=holefluc;write="maintenance_oCcurrencwater" element name= horeflec;write="water_reflection_on_rocks( clifConly)" element name=id element name=idprofyr;write=" scholar' s_name,_profession_and_date( s L oCstudy" element name= l_crevas;write= "large_crevasses" element name= landmass;write="land_masses" element name= larcraks;write= "large_cracks" element name=lac1ong;write="latitude_and_longitude" element name= location;write= "location_ oCimages" element name=maintyr;write= "maintenance _ oCcurrent_ water_leveCyears" element name=majchhol;write="major_changes_in_regionaCwater_levels_years" element name=mater_used;write="materials_used_to_create_image" element name=meascav;write="measurements_of_cavern_if_taken" element name=measclif;write="measurements_oCclifCiCtaken"

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element name=meth_rec;write="methods_oCrecording" element name=scrollid;write= "birch_bark_scrolLidentity _num ber" element name=n_cavern;write="number_of_cavern" element name=n_cliffs;write="number_oCcliffs" element name=n_tclvwl;write= "heighcoCclifCfrom_ visible_ watecline" element name=n_ vwlin;write= "number_oC visible_ water_lines" element name=no_angle;write="number_oCangles"; element name=no _story _pub;write=" numbec oCstories_published" element name=offering;write=" offerings" element name=offnoted;write="offerings_noted" element name=ori~ed;write="original_edition" element name=ori~pdate;write="originaLpublication_date" element name=ori~pub;write=" original_publisher" element name=ori~title;write="originaLtitle" element name=page;write+ "page_to_page" element name=personid;write="identity_oCperson" element name=phychart;write=" physical_ characteristics" element name=pLname;write= "place_name" element name=prealtname;write="previous_alternative_name" element name=predpeop;write=" presencday _peoples" element name=predsett;write= "presencday _settlements" element name=preduse;write="period_oCuse_in_years" element name=prehosid;write= "presence_oC water-numbecoCsides" element name=primary _editor;write= "primary _editor" element name=projname;write= "projeccname" element name=prxpaint;write=" proximity _ oCrock_ overhangs_to paintings" element name=prxrochg;write="proximity_oCrock_overhangs_to_one_another" element name=pub_ work;write="published_ work" element name=px_cre;write="proximity_oCcrevasses_to_another" element name=px_lc;write="proximity_oClarge_cracks_to_one_another" element name=px_lcpai;write="proximity_oClarge_cracks_to_paintings" element name=rcprcsh;write="rocks_on_clifCshelf/ shelves" element name=regdrsys;write=" regionaLdrainage_ water_systems" element name=rocbacav;write="rocks_acbase_oCcavern(s)" element name=rocbacli;write="rocks_acbase_oCcliff(s)" element name=rockfall;write="rock_fall" element name=rocovhgs;write="rock_overhangs" element name=rocprecre;write=" rocks_presencin_ crevasses" element name=rocshelf;write"rockshelf' element name=roctacli;write="rocks_actop_oCcliff(s)" element name= roctocav;write = "rocks_at_top_oCcavern(s )" element name= season;write=" season_ oC waterlevel_fluctuation" element name= second_editor;write=" secondary _editor" element name= second_pdate;write=" secondary _publication_date" element name= second_pub;write=" secondary _publisher" element name=shape;write="shape_oCtopos" element name=tiffnums;write="tifCftle_numbers" element name=type_ data;write="type_oCdata_recorded"

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element name=typerock;write=ltype_oCrock" element name:=urut_m;write=" urut_ of_measurement" element name=useofho;write= "uses_oCbody _oC water" element name=vegbcav;write:= "vegetation_acbase_oCcavern( s)" element name=vegbcli;write= "vegetation_acbase_ ° Ccli ff( s)" element name=vegsscav;write:="vegetation_on_side/ surface_oCcavern(s)" element name=vegsscli;write:= "vegetation_on_side/ surface_oCcliff( s)" element name:=vegtcav;write:="vegetation_actop_oCcavern"; element name=vegtcli;write="vegetation_actop_oCcliff(s)" element name=visiwale;write="visible_ wateclevels"; element name=why;write=" cause_of_ water_leveLfluctuation" element name=projname;write="project_name" element name=persorud;write= "identity _ oCperson" element name:=date;write=" date_oCfield_recording" element name= bordenn;write= "borden_number" element name=urut_m;write="urut_of_measurement" element name=measclif;write="measurements_oCclifCiCtaken" element name= fielinfo;wri te=" fieldnotes" element name=pub_ work;write="published_ work" element name=idprofyr;write=" scholar' s_name:>-profession_and_date( s L oCstudy" element name=phychart;write="physicaLcharacteristics" element name=typerock;write="type_oCrock" element name=offnoted;write="offerings_noted" element name=shape;write=" shape_oCtopos" element name=mater_used;write="materials_used_to_create_image" element name=centre_ oCimage;write=" centre_ oCimage" element name=shape;write="shape_oCtopos" element name=mater_used;write="materials_used_to_create_image" element name=centre_oCimage;write="centre_oCimage" element name=shape;write="shape_oCtopos" element name=mater_used;write="materials_used_to_create_image" element name=centre_oCimage;write="centre_oCimage" element name=projname;write=" project_name" element name=personid;write="identity_oCperson" element name=tiffnums;write="tifCfùe_numbers" element name= bordenn;write= "borden_number" element name=date;write=" date_ oCfield_recording" element name=pl_name;write="place_name" element name=alt_name;write=" alternative_name" element name=pre_name;write="previous_name" element name=lac1ong;write="latitude_and_longitude" element name=geo~not;write="geographical"notes" element name=predsett;write= "presencday _settlements" element name=predpeop;write= "presencday _peoples" element name= landmass;write= "land_masses" element name=access;write=""access_to_site" element name=regdrsys;write=" regionaLdrainage_ water_systems" element name=useofho;write="uses_oCbody _oC water"

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r--..

element name=preduse;write="period_oCuse_in_years" element name=prehosid;write= "presence_ oL water-number_ of_sides" element name= bhosadsi;write= "body _oL watecsurrounding/ adjacent_to_site" element name=maintyr;write="maintenance_oCcurrencwater_leveLyears" element name=holefluc;write="maintenance_oCcurrencwater" element name=why;write="cause_of_water_level_fluctuation" element name=extent;write="extencof_fluctuation" element name=season;write=" season_ oC waterleveLfluctuation" element name=majchhol;write="major_changes_in_regional_water_levels_years" element name=visiwale;write="visible_ wateclevels" element name= location;write= "location_ o Limages " element name=projname;write="project_name" element name=personid;write=" identity _ oCperson" element name=date;write=" date_oCfield_recording" element name=tiffnums;write="tifCfile_numbers" element name= bordenn;write= "borden_number" element name=unit_m;write="unit_of_measurement" element name=typerock;write="type_oCrock" element name=n_cavern;write="number_of_cavern" element name=cavprwl;write= "heighC oCtop _oC cavern_from_presencday _ water_level" element name=n_ vwlin;write="number_oC visible_ water_lines" element name=n_tcavwl;write= "height_ oCcave_from_ visible _ watecline" element name=vegtcav;write="vegetation_actop_oCcavern" element name=vegsscav;write= "vegetation_on_side/ surface_oCcavern(s)" element name=vegbcav;write= "vegetation_acbase_oCcavern( s)" element name=rocovhgs;write=" rock_ overhangs" element name=prxrochg;write="proximity_oCrock_overhangs_to_one_another" element name=prxpaint;write= "proximity _oCrock_ overhangs_to paintings" element name=larcraks;write="large_cracks" element name=px_lc;write= "proximity _ oClarge_cracks_to _ one_another" element name=px_lcpai;write="proximity_oClarge_cracks_to_paintings" element name= Lcrevas;write= "large_crevasses" element name=px_ cre;write= "proximity _oC crevasses_to _another" element name=rocshelf;write"rockshelf' element name=rocbacav;write="rocks_acbase_oCcavern( s)" element name=roctocav;write="rocks_at_top_of_cavern(s)" element name=rcprcsh;write= "rocks_on_clifCshelf/ shelves" element name=rocprecre;write=" rocks_presencin_crevasses" element name= offering;write = "offerings" element name=oritangle;write="orientation_oCangles" element name=rockfail;write=" rock_fail" element name=exfoliat;write="exfoliation" element name= gen_notes;write=" generaLnotes" element name=projname;write="project_name" element name=personid;write= "identity _oCperson" element name=date;write="date_oCfield_recording" element name= bordenn;write= "borden_number" element name=unit_m;write= "unit_ of_measurement"

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element name=meascav;write="measurements_oCclifCiCtaken" element name=fielinfa;write="fieldnates" element name=pub_ work;write= "published_ work" element name=idprofyr;write=" scholar' s_name,_profession_and_ date ( s LoCstudy" element name=phychart;write="physicaLcharacteristics" element name=typerock;write="type_oCrock" element name=offnoted;write="offerings_noted" element name=shape;write="shape_oCtopos" element name=mater_used;write="materials_used_to_create_image" element name=centre_oCimage;write="centre_oCimage" element name= shape;write= "shape_oCtopos" element name=mater_used;write="materials_used_to_create_image" element name=centre_oCimage;write="centre_oCimage" element name=id element name=format;write="format" element name=date_info_collected;write="date_information_collected" element name= second_pdate;write=" secondary _publication_date" element name=author;write="author_of_tale" element name=primary _editor;write= "primary _editar" element name=type_ data;write="type_oCdata_recorded" element name=page;write+"page_to_page" element name=annotation;write="interestingjnfo_re_tale" element name=group_belong_Jo;write="group_tale_belong_Jo" element name=claimed_status;write=" specific~eographicaLregion" element name=id element name=m_content;write="myth_content" element name=scene;write="scene" element name=people element name= sex;write=" sex_ oCdepicted_person" element name=m_pname;write="name_oCpersons_in_myth" element name=m_associated_characteristics;write="associated_characteristics_in_myth" element name=m_status;write= " status_oCperson_my th" element name=m_clothing;write="clothingjn_myth" element name=m_scene;write=" scenes_in_myth"; element name=action element name=setting element name=person;write="person" element name=id element name= format;write = " format" element name=date_info_collected;write="date_information_collected" element name=author;write="author_oCtale" element name=primary _ editor;write= "primary _editor" element name=type_ data;write="type_oCdata_recorded" element name=page;write="page_to_page" element name=annotation;write=" interestingjnfo _re_tale" element name=group_belong_Jo;write="group_tale_belong....to" element name=claimed_status;write=" specific~eographicaljegion" element name=id

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element name=form_oCobject element name=collection element name=archive element name=ori~collect;write="original collector" element name=why element name=collected_date element name=author element name=visible element name=group_belon~to element name=claimed_status element name=materials_used_to_construct_object element name=shape;write=" shape_oCtopos" element name=mater_used;write="materials_used_to_create_image" element name=centre_oCimage;write="centre_of_image" element name=shape;write="shape_oCtopos" element name=mater_used;write="materials_used_to_create_image" element name=centre_ oCimage;write=" centre_ of_image" element name=o_content;write="oraLevidence_content" element name=o_scene;write="scenes in_oraLevidence";order=multiple element name=o_people;write="people_in_oraLcontent" element name=o_sex;write="sex_oCdepicted_characters";type=category;category=gender element name=o_pname;write="name_oCperson" element name=o_associated_characteristics;write="associated_characteristics_o" element name=o_status;write="status_of_person_oral" element name=o_clothing,o_status; element name=o_action;write="oraLsituation" part name=i;write="image";

position = number;arbitrary=rock_art,birchbark,second_data part name=rock_art;arbitrary=rock_face,cave_face part name=rock_face;arbitrary=rphy _cont,rcuc work,rprev _ work,rimage part name=rphy_cont;write="rock_face_physical_context";

position=projname,personid,tiffnums,bordenn,date, pl_name,alt_name,prealtname,pre_name,laclong,geo~not,predsett,

predpeop,landmass,access, regdrsus,useofuo,preduse,prehosid,bhosadsi,freefw,maintyr, holefluc,why,extent,season,majchhol,visiwale,location

part name=rcur_work;write="rock_face_currencwork"; position=projname,personid,date,tiffnums,bordenn,unicm,typerock, n_ cliffs,hcliprwl,n_ vwlin,n_tclvwl,vegtcli, vegsscli,vegbcli, rocovhgs,prxrochg,prxpaint,larcraks,px_lc,px_lcpai,rocshelf, l_crevas,px_cre,pxcrepai,rocbacli,roctacli,rcprcsh,rocprecre, offering,no_angle,oritangle,rockfall, exfoliat,meth_rec,gen_notes

part name=rprev _ work;write= "rock_face_previous_ work"; position=projname,personid,date,bordenn,photos,units_m,measclif, meth_rec,fielinfo,pub_work,idprofyr,phychart,roc_typr,offnoted

part name=rimage;write= "images_ on_ clifCface" ;arbitrary= supertopos, topos part name=supertopos;

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position::::bordenn,shape,colour,matecused,centre_oCimage part name=topos;

position:::: bordenn,shape,colour,matecused,centre_ oCimage part name::::cave_face;

arbitrary::::cphy _cont,ccur_ work,cprev _ work,cimage part name::::cphy _cont;write::::" cavephysicalcontext";

position::::projname,personid,tiffnums,bordenn,date, pCname,alt_name,prealtname,pre_name,laclong,geo~not,

predsett,predpeop, landmass,access,regdrsys,useofuo,preduse,prehosid,bhosadsi, freefw,maintyr,holefluc,why,extent,season,majchhol,visiwale,location

part name::::ccur_ work;write::::" cave_currenc work"; position::::projname,personid,tiffnums,date,bordenn,unit_m,typerock, n_cavern,hcavprwl,n_ vwlin,n_tcavwl,wid_cav,vegtcav,vegsscav, vegbcav,rocovhgs,prxrochg,prxpaint,larcraks,px_lc,px_lcpai,rocshelf, l_crevas,px_cre,pxcrepai,roc bacav ,roctocav ,rcprcsh,rocprecre,offering, oriopcav,exfoliat,meth_rec,gen_notes

part name::::cprev _ work; write::::" cave_previous_ work"; position::::projname,personid,date,bordenn,photos,units_m,meascav, meth_rec,fielinfo,pub_work,idprofyr,phychart,roc_typr,offnoted

. . n' . ft part name::::C1mage;wnte:::: 1mageS_ln_cave ; arbitrary::::supertopos,topos;

part name:::supertopos; position::: bordenn,shape,colour,mater_used,centre _ oCimage

part name:::topos; position::: bordenn,shape,colour,mater_used,centre_ oCimage

part name:::: birchbark;write= "birchbark"; arbitrary:::: bark_ contxt,supertopos,topos

part name::: bark_contxt;write:::" contexC oCbirchbark"; position::::id,tiffnums,form_oCobject,collection,archive,ori~collector,

why,collected_date,author,visible,group_belon~to,claimed_status,

materials_used_to _construcC obj ect; part name:::supertopos;

position:::scrollid,shape,colour,mater_used,centre_oCimage part name:::topos;

position:::scrollid,shape,colour,mater_used,centre_oCimage part name:::second_data;

position:::number; arbi trary::: myth, oral_ evidence

part name:::myth; position:::id,format,ori~title,date_info_collected,ori~ed,

ori~pub,ori~pdate,second_pub,second_pdate,narrator,

primary _editor,second_editor,no _story _pub,type_ data,page, annotation,group_belon~to,claimed_status;

part:::m_content part name:::m_content;write::: "myth_ content" ;arbitrary:::people,m_scene;

position::: id part name:::people;

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position = sex,m_pname,m_associated_characteristics,m_clothing,m_status; part name=m_scene;write="scenes_in_myth";

position = id,action,setting; part name=oraLevidence;

position=id,format,orig....title,date_info_collected,orig....ed,orig....publisher, orig....pdate,second_pub,second_pdate,narrator,primary 3ditor, second_editor,no_story_pub,type_ data,page,annotation,group_belong....to, claimed_status; part=o_content

part name=o_content;write="oral_evidence_content";arbitrary=° _people,o_scene; position=id

part name=o_people;write="people_in_oral_content"; position = ° _sex,o _pname,o _associated_ characteristics,o _clothing,o _status;

," ' 1 'd " part name=o_scene;wnte= sceneS_ln_ora _ev! ence ; position = id,o _action,o _setting;

exit name=design

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') )

Appendix 5: Lichen, Rock Tripe, Exfoliation. and White Mineral Deposits in conjunction with Site Orientation.

This appendix presents the information for all the sites regarding the presence or absence of lichen, rock tripe, exfoliation and white

mineraI deposits in conjunction with site orientation. This will be used to determine whether correlations exist and whether anything can be

concluded regarding their age. Information on the number of blobs and the total number of images is aiso presented. This information will

be used to establish whether correlations exist between it and the orientation of the site. Information is presented regarding the offerings in

2001 and previous offerings. This will help to establish the Iength of time that the physicailocation of a pictograph site has been perceived

to be important.

1-178 1 small degrees (S), 2 blob,4

1

Pastershank DgKl- - 259 degrees small

8 images Yes - tobacco in 1989-Yes Yes No Yes (SSW), 3- blobs

tobacco 1

194 degrees, along side each other

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') ')

Yes = children' sand adults clothes (trousers, skirts, t-shirts, socks, chenille

sweater, flannel clothes - sorne old, sorne new), dried food stuff, bandages, earring

(mother of pearl with porcupine quills and silver and blue beads), earring - plastic

1 = 180 (S), heart (never in pairs), tobacco, empty

tobacco container ("Copenhagen 2 = 180 (S),

Tobacco"), beer bottle glass, clear glass, 1 3 = 90 (E), 4

"Prayer Sticks" (26 bundles of 12, 12 cm = 101 (E),5

1 small long by 12.5 - 17 cm wide, tied together = 139 (SE),

6 = 120 blob,4 with white cotton string, half of each stiek

(SE), 7 = 99 small painted blue and the other half painted red,

(E),8 = 150 blobs large diameter sticks always tied together

alongside and small diameter sticks always tied Pastershank DgKl-

No Yes No Yes (SE), 9 =

and 9 images together - never mixed, 1 bundle of 12 in in 1989 -2 140 (SE), 10

attached to the left-hand cave, refer to field sketches tobaeco = 100 (E), 11

each other, and digital and manual photographs). More = 120 (SE),

12 = 120 1 offerings were left on the rock bench under

(SE), 13 = unidentifia overhang when came back later to record

160 (SSE), ble shape more photographs, modern paintings also

1 14 = 130

visible at site. Returned August 5th 2001 with a team of divers who discovered the

(SE), 15 = rocks immediately below and the vieinit)'

1 189 (S\'V) around the rock image site. They 1

discovered that it was a mud bottom and i

that there was a pile of rocks but no i offerings were evident only Mountain Dew 1 soft drink can, a gendeman's bicycle, and

another cave to the right and 2.14m (7 feet)

1 below site un der water.

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') ')

Tobacco, money (coins) - on shelf/ crevasses. August 5/01 = (with

divers) Medicine sticks found under water in same bundles = 12 sticks tied together

with string, red and blue just like site

DgKl- 1 -109 immediately opposite Nestor Falls - are a

None 17

Yes Yes No Yes degrees (E)

No blobs 13 images couple of feet below the water level but not recorded

immediately beside/below rock art site; Broken plate but can't find other part -same maker's mark as Horseshoe Island pot - Alfred Meaken; child's fishing rod;

i

collection of shirts about 6.1 m (20 feet) among large boulders below the water level

4 - Angle 1 on left when facing cliff -

1 blob and continues to

area of the right to

pairs of Angle 4 (at

vertical DgKl-

base). 1 - 90 lines and None

19 Yes Yes Yes Yes degrees (E),

spots of 6 images No

recorded 2 - 93

degrees (E), small

concentrat 3 - 90

ions of degrees (E),

ochre 4 -162 degrees (SSE)

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\ ')

2 blobs,

1

horizontal oval blob with two

DgK short

None Yes Yes Yes Yes 81 (E) vertical 17 images No m-l

lines recorded

sticking up on top

right hand side

June 12/01 - multiple articles of clothing (socks, shirts, jeans, jersey shirt, polyester sport shirt, aIl colours) - aIl above water level , stuffed in crevasses and cracks as

weIl as numerous sample-size alcohol bottles, coins, tobacco, empty small-size soft drink bottle, toweL July 22/01 (with

2 blobs, divers) - Yes = ceramic pot, glass bottle

horizontal (bottom blown into a mould, containing

Dewdneyin oval blob

lead drop shot, neck of bottle hand-1960-

with two finished - no seam at top, cork with hand-

clothing. tooled top, has a smell when opening

DhK 110 degrees short

container - juniper smell, on bottom 25%, Molyneaux

m-l Yes Yes Yes Yes

(ESE) vertical 17 images

wedged in groove in rock about 1.52 - 1.83 in 1974-

1

lines m (5-6 feet) from pot), lots of coins in the

clothing; sticking up Fox 1974-

on top rock (George V quarter, American penny),

bundles of right hand

plate made by same company as bowl from clothing;

new Horseshoe Island site - Alfred side

Meaken, Royal Ironstone China, England, Queen Victoria's crown, lion and unicorn) (AC). Huge pile of miscellaneous clothing, different styles and different periods to the depth of 15.85 m (52ft) from the surface of

the water. lncluded fabric and leather clothes, moccasins, pile leaning against cliff

1 face.

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\ )

Stick, peeled, which looks !ike beaver stick but ends are a bit weathered so hard to be 100% sure - 3/4" diameter and 1/5' long. Tobacco between 2 and 3. Two cowrie

shells = one 7.5 cm - other 5 cm (hidden in sedge). One pie ce of red clotho One cap

DhK Yes Yes No Yes

150 degrees 10 blobs 33 images

(red) embroidered "Sail Caribbean" - None m-3 (SE) deteriorating cloth, very faded, not recently recorded

left (probably over 1 year old). Ali on rock shelf. Soil under areas 2 and 3 has been

disturbed recently (by stick?) and between a bush at north-east edge, also under large cowrie shell and one small area of moss 6

inches.

1 = 200

DhK degrees

None m-4

No Yes No No (SSW), 2 = No blobs 5 images No recorded

182 degrees (S)

10 different types of

Difficult to blobs,l

estab!ish group of

Dewdney in 1

because of blobs of

1960 found DhK Yes accumulatio Yes Yes 120 degrees different

37 images Yes - coins (coin) on 2ledges, tobacco on 2

m-5 (ESE) sizes, 1 ledges, decayed fruit - food prayer

n of white sticks and mineraI

round none later

cleposits blob with short !ines

sticking out either

sicle

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î ')

1 blob, one faint

unidentifia ble shape, a group of Dewdney in 1

DhK 230 degrees small 1960 found '

m-18 Yes Yes No No

(SW) blobs and 6 shapes No prayer

! lines that sticks and cross each none later

other at 1

ninety degree angles

Left side = Dewdney in

250 degtees 1960 found overcoat DhKn

No Yes No No (WSW),

2 blobs 10 images Yes - Right side = feather Oarge bird),

and various -1 Right side = partially smoked cigarette weathered

240 degrees and rotten

(WSW) "rags" ,

y es = in the various cracks in the cliff face Dewdney in righ t cliff - tobacco (5 piles), cigarettes, snuff can lids, 1960 found

119 (SE); left 8 blobs, 1

3 sample-size Crown Royal botdes, alcohol chinaware DiKn-

Yes Yes Yes No cliff - 1 Oeft)

collection 16 images botdes, clothing, money (25 cents = 1977, and other

1 = 132 (SE), 1989, 1995; 1 cent = 1989, 10 cents = oddsand 2 (right) = ofblobs

1994). 2 Jack pine ttees up top with gifts on ends. 164 (SSE) them - dress shirt, towel (on gtound), cloth Nothing 1

tied around tree. found later 1

1 -142 1

degtees (SE), 2 faint 2 - 164 unidentifia

DiKp-Yes Yes Yes Yes

degtees ble shapes, 14 images No No 1 (SSE), 3- 5 different

150 degtees types of 1 (SE), 4 - 140 blobs

degtees (SE)

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DkKn Yes Yes Yes

-6

DkKn Yes Yes No

-7

DjKn-Yes Yes Yes

1

DiKm Yes Yes Yes

-3

DiKm No No No

-4

Difficult to

DhKo establish

Yes whether Yes -1

this has occurred

Difficult to It has

establish begun to

DjKr-Yes whether

grow but it 23

this has does not

occurred affect the

images

Yes

No

Yes

Yes

No

Yes

No

\ )

Page 548

322 (NW)

222 degrees (SW)

1 = 140 (SE), 2 =

142 (SE), 3 = (SE)

WSW-225 degrees

90 degrees-East

Almost due north,4 degrees

4 (1 being highest of

the 4, 4 being the

lowest).1 = 148 (SE), 2 = 178 (S), 3 = 164 eSSE),

4 = 160 eSSE)

)

4 blobs 4 images No No !

!

1 blob 1 image No No

Dewdney in 1958 and

8 blobs 36 images No Molyneaux

in 1974 recorded offerings

Dewdney in :

5 blobs 29 images No 1953 found a "prayer

raft" Dewdney in 1960 found

No blobs 4 images Yes-2 pieces of money (silver) on rocks at clothing,

base of cliff underwater tobacco and prayer sticks.

3 blobs and 1 spikey

Yes - beer bottle glass under moss in blob with 29 images None

seven lines vertical crevasse

sticking out

2 blobs and two

small round

Dewùney

blobs one 8 images Yes = money, builets (33), tobacco - ail found

immediatel located in crevices offering in

1960 yon top of the other

Page 576: An obsession with meaning: a critical examination of the pictograph sites of the Lake of Woods

\, ~

2 (base) 1 = 200 degrees

No None DiKin

Yes Yes Yes Yes (SSW) , 2 = 1 blob 6 images -51

182 degrees (S)

Dewdney Difficult ta

found establish 2 (base) 1 =

No clothing, DiKq-

No whether No Yes 148 (SE), 2 7 blobs 11 images towel and 10

this has = 120 (ESE) tobacco in

occurred 1960 Not DhK

No No No No 1 - 154(SE) No blobs 1 image No applicable m-19

Difficult ta establish 1 (base of

Yes - tobacco, something in water tao deep Not DhK Yes whether No Yes cliffface) 54 No blobs 4 images

ta reach applicable m-20 this has degrees (NE)

occurred 236 degrees Not DgK

Yes Yes Yes Yes 4 blobs 6 images No applicable m2 (SW)

Not DiKm No Yes No No 214 (SSW) No blobs 1 image No

applicable -50 NNW, another

opening at back leads up

Not DiKm Yes No No No ta top of No blobs 2 images No

applicable -49 DiKm-3

openingup and facing

WSW

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,r--..

Appendix 6: The Different Types of the Shape Loosely Categorised as a 'Creature'.

The photographs below are of each shape identified as a 'creature' at the sites where

this type of shape existed.

DgKl-l:

Ca) creature, facing left, with head with large horns or ears, tail, two legs visible - one back

and one, solid

(b) creature, facing right with head with large horns or ears, tail, two legs visible - one back

and one front, solid

DgKl-17: Ca) creature, facing left with two clear legs with a third leg, tail and horns or ears, hollow.

DgKl-2:

Ca) creature with he ad, with horns or ears or anders and a back and a pair of front legs facing

right, solid

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DhKm-3:

(a) creature with long horns or ears, facing right, one back leg and one front leg and curved

tail, solid

(b) creature, vertical does not face left or right, with four legs, a tail, and a head and two

horns or ears, solid

DhKm-5:

(a) creature with horns or ears facing left since long tail pointing downwards on right hand

side of animal, four legs visible (front legs are less visible). Head is also less visible, solid

(b) creature with head, facing le ft, one back and one front leg, with two horns or ears

superimposed upon pale images

Page 552

Page 579: An obsession with meaning: a critical examination of the pictograph sites of the Lake of Woods

(c) creature, facing left with faint outline of head and a short tail, solid

(d) creature, facing right, head with horns or ears and tail but no clearly defined legs, solid

(e) creature, facing left, with horns or ears but no clearly defined legs and tail, solid

DhKh-l:

(a) creature, body is horizontalline with horns or antlers, no legs, facing right, solid

(b) creature, horizontal body is a line with head with horns or antlers, no legs, faces left, solid

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Page 580: An obsession with meaning: a critical examination of the pictograph sites of the Lake of Woods

DhKo-l:

(a) circular creature with head, facing right, with two horns or ears attached to head, two legs

and two arms, solid

(b) creature with head, facing right, short tail, one back leg with two digits and one front leg

with unknown number of digits, solid

(c) creature with two horns or ears, only front part of body and head facing left, no rear

body, legs or tail, hollow

(d) creature, facing left, long horizontal with pointed mouth with dots down the middle of

the creature beginning behind head, top of creature have triangles on top side and horizontal

series of short lines, hollow

Page 554

Page 581: An obsession with meaning: a critical examination of the pictograph sites of the Lake of Woods

DiKm-3:

(a) creature facing right with two horns or ears pointing up, one front and one back leg, solid

(b) diagonal creature, but vertical with no legs but a tail with a point, two legs raised upwards

and a he ad, with two horns or ears

DiKp-l:

Ca) creature with horns or ears on its head, a curved tail, and two legs with feet, facing left,

solid

DjKn-l:

(a) creature, cross section, facing right, with a rack of horns or antlers, and a tail, four short

diagonal legs, solid

Page 555

Page 582: An obsession with meaning: a critical examination of the pictograph sites of the Lake of Woods

(b) creature, horizontal cross section of body, facing le ft, with horns or ears or antlers

indicated by small round hollow bubble above filled in head of hollow creature with antlers,

one back leg and one front leg

(c) creature, horizontal cross section, facing right with two back legs and t:wo front legs are

visible as is a head with horns or ears. The creature has a long taï! measuring approximately

half of the length of body

Page 556

Page 583: An obsession with meaning: a critical examination of the pictograph sites of the Lake of Woods

Appendix 7: Examples of the Different Types of Shapes in Each Group.

Several examples of the different types of each shape are provided below ta demonstrate

that the shapes have ta be discussed as types because they are often physically different ta

each other.

a) seventy-seven different types of 'blobs' (xq349)

Three examples of these:

- DkKr-6, - DjKr-23, - DkKr-7

b) eighteen different types of 'smears' (xq326)

- DhKn-l

, ,- DgKl-2

-DgKm-2

Page 557

Page 584: An obsession with meaning: a critical examination of the pictograph sites of the Lake of Woods

c) five types of shape called 'unidentifiable shape' (xq744) and one area at DgKl-19 that

also contains pairs of vertical lines and spots of small concentrations of ochre

(xq745)

- DgKl-2 - DiKq-l0,

- DiKp-l d) two types of shape called 'diagonal stick figure' (xq382b)

- DiKm-3, - DiKm-3

e) fifteen types of shape called 'vertical stick figure' (xq358a, xq382b)

- DjKn-l, - DhKo-l, -DgKm-l

f) two types of shape called 'upper torso of vertical stick figure' (xq358c)

Page 558

Page 585: An obsession with meaning: a critical examination of the pictograph sites of the Lake of Woods

- DgKm-l, - DiKn-l

g) twenty-nine loosely categorised types of shape called 'hand print' (xq328, xq328a,

xq328b, and xq333), eleven are right 'hand print' shapes (xq328b) and seven are left

'hand print' shapes (xq328b)

- DgKl-19, - DjKn-l, - DiKm-3

h) five vertical types of shape called 'vertical zig-zag' (xq321)

- DhKm-l, - DhKm-3, - DiKm-4

i) two types of shape called 'diagonal zig-zag' (xq321)

- DhKm-3, - DiKm-3

j) one type of shape called 'horizontal zig-zag' (xq321)

Page 559

Page 586: An obsession with meaning: a critical examination of the pictograph sites of the Lake of Woods

- DiKp-l

k) two types of shape called 'one vertical and one horizontal short line that cross each

other at ninety degrees' (xq336 and xq336a)

- DjKn-l, - DhKm-3

1) two types of shape called 'square, created by two vertical and two horizontallines of

equallength' (xq746)

- DhKo-l, - DhKo-l, - DhKo-l

m) three types of shape called 'turtle' (xq382 and xq362)

- DhKm-5, -DhKn-l, - DhKm-19

n) two types of shape called 'bird' (xq335)

-DhKm-3, -DhKm-18

Page 560

Page 587: An obsession with meaning: a critical examination of the pictograph sites of the Lake of Woods

0) one type of shape called 'horizontal crescent with points facing upwards' (xq332,

xq350, and xq348) (see figure 1.2 in chapter 1)

p) seven types of shape called 'horizontal crescent with points facing upwards with

vertical lines attached to topside' (xq332, xq348, and xq 350) (see figure 1.2 in

chapter 1)

q) two types of shape called 'horizontal crescent with points facing downwards' (xq348a

and xq348) (see figure 1.2 in chapter I)

r) two types of shape called 'horizontal crescent, points facing downwards with vertical

lines on bottom side' (xq 350 and xq348) (see figure 1.2 in chapter 1)

s) ten types of shape called 'horizontal line' distinguished by the following qualities:

wide, narrow, long and short (xq338)

- DhKo-1, - DiKm-3,

t) eight types of shape called 'diagonal line' distinguished by the following qualities:

wide, narrow, long and short (xq747)

- DjKn-1, - DgKl-1, -DjKn-1

u) eleven types of shape called 'vertical line' distinguished by the following qualities:

wide, narrow, long, short and with a forked end (xq339)

L....-~....J - DhKo-1, -DhKo-1, - DjKn-1

v) four types of shape called a 'two parallellines' (xq 347 and xq749) which are either

diagonal, vertical or horizontal

Page 561

Page 588: An obsession with meaning: a critical examination of the pictograph sites of the Lake of Woods

- DgKl-l, - DiKm-3, - DjKn-l

w) nine types of shape called a 'group of three diagonal parallel short lines' (xq346)

- DgKl-17, - DgKl-17,

- DgKl-17

x) two types of shape called a 'group of four diagonal short lines' (xq342)

-"'-~::...J - DhKm-5, - DhKm-3

y) two types of shape called a 'group of six short horizontallines' (xq343)

- DhKo-l, - DhKm-3

z) t:wo shapes called 'three lines joined together at one end' (xq324)

Page 562

Page 589: An obsession with meaning: a critical examination of the pictograph sites of the Lake of Woods

.r·

- DiKm-3, - DiKp-l

aa) four types of shape called "curved lines" distinguished by the following qualities:

vertical, horizontal, diagonal, narrow, long, short (xq324)

- DhKm-20 - several examples here, -DhKm-l a

vertical curve beside an area of ochre that is severely exfoliated

bb) two types of shape called "three vertical and diagonallines attached to each other at

the lower end of each line" (xq510)

There are many images that occur once and here are these shapes.

- DiKn-l, DhKm-3, - DhKm-4

-DhKm-3, -DhKm-4,

- DhKm-l

Page 563

Page 590: An obsession with meaning: a critical examination of the pictograph sites of the Lake of Woods

- DhI<.in-5, - DiI<.in-3, - DjKn-l,

- DjKn-l

Page 564

Page 591: An obsession with meaning: a critical examination of the pictograph sites of the Lake of Woods

(

~'

Appendix 8: The Geology, Geomorphology, and Type of Landmass of Each Site

This appendix indicates that, although the rock on wruch these pictograph sites

existed is defined as Archean Early Precambrian the specifie geology and geomorphology is

different (Barnett, Henry and Babuin 1991; Davies 1983, 1985; Kaye 1981; Minning and

Sharpe 1991a, 1991b, 1991c; Trazer 1943). This appendix also demonstrates that no

correlations exist between geology and the geomorphology and the type of landmass on

which these sites prevail.

Archean Early More than eighty

Precambrian but rock percent of the rock can

is identified as be identified as rock

DgKl-1 hornblende, gabbro, outcrop wruch is ice Mainland - Sabaskong

diorite, periodite, and eroded Archean granite Peninsula

serpentine. None of with patches of trun drift and scattered

them is the same age. boulders.

Archean Early More than eighty

Precambrian but rock percent of the rock can

is identified as be identified as rock

DgKl-2 hornblende, gabbro, outcrop wruch is ice Mainland - Sabaskong

diorite, periodite, and eroded Archean granite Peninsula

serpentine. None of with patches of thin drift and scattered

them is the same age. boulders.

Archean Early More than eighty

Precambrian but rock percent of the rock can

is identified as be identified as rock

DgKl-17 hornblende, gabbro, outcrop wruch is ice Mainland - Cyclone

diorite, periodite, and eroded Archean granite Point

serpentine. None of with patches of trun drift and scattered

them is the same age. boulders.

Archean Early More than eighty

Precambrian but rock percent of the rock can

is identified as be identified as rock

DgKl-19 hornblende, gabbro, outcrop wruch is ice Mainland - Cyclone

diorite, periodite, and eroded Archean granite Point

serpentine. None of with patches of trun drift and scattered

them is the same age. boulders.

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Archean Early More than eighty

Precambrian but rock percent of the rock can

is identified as be identified as rock

DgKm-l hornblende, gabbro, outcrop which is ice

diorite, periodite, and eroded Archean granite

Mainland

serpentine. None of with patches of thin

them is the same age. drift and scattered

boulders.

Archean Early More than eighty

Precambrian but rock percent of the rock can

is identified as be identified as rock

DhKm-l hornblende, gabbro, outcrop which is ice Mainland -Aulne au

diorite, periodite, and eroded Archean granite Peninsula

serpentine. None of with patches of thin

them is the same age. drift and scattered

boulders.

Archean Early More than eighty

Precambrian but rock percent of the rock can

is identified as be identified as rock

DhKm-3 hornblende, gabbro, outcrop which is ice Island - unnamed

diorite, periodite, and eroded Archean granite island

serpentine. None of with patches of thin

them is the same age. drift and scattered

boulders.

Archean Early More than eighty

Precambrian but rock percent of the rock can

is identified as be identified as rock

DhKm-4 hornblende, gabbro, outcrop which is ice Mainland - Aulneau

diorite, periodite, and eroded Archean granite Peninsula

serpentine. None of with patches of thin

them is the same age. drift and scattered

boulders.

Archean Early More than eighty

Precambrian but rock percent of the rock can

is identified as be identified as rock

DhKm-5 hornblende, gabbro, outcrop which is ice Mainland - Aulneau

diorite, periodite, and eroded Archean granite Peninsula

serpentine. None of with patches of thin

them is the same age. drift and scattered

boulders.

Archean Early More than eighty

Precambrian but rock percent of the rock can

is identified as be identified as rock

DhKm-18 hornblende, gabbro, outcrop which is ice Mainland - Aulneau

diorite, periodite, and eroded Archean granite Peninsula

serpentine. None of with patches of thin

them is the same age. drift and scattered

boulders.

Page 566

Page 593: An obsession with meaning: a critical examination of the pictograph sites of the Lake of Woods

More than eighty Archean Early

percent of the rock can Precambrian but rock

be identified as rock Mainland - Aulneau

is identified as outcrop which is ice

DhKn-l hornblende, gabbro, eroded Archean granite Peninsula

diorite, periodite, and with patches of thin

serpentine. None of drift and scattered

them is the same age. boulders.

More than eighty Archean Early

percent of the rock can Precambrian but rock

be identified as rock Mainland - Aulneau is identified as

outcrop which is ice Peninsula - Hay ter DiKn-l hornblende, gabbro,

eroded Archean granite Peninsula diorite, periodite, and

with patches of thin serpentine. None of

drift and scattered them is the same age.

boulders.

Archean Early More than eighty Precambrian, schistose percent of the rock can

volcanic with some be identified as rock small quantities of outcrop which is ice

Island - Cliff Island DiKp-l sediments that are iron eroded Archean granite

formation. Y ounger with patches of thin sediments possibly drift and scattered

exist here. boulders.

Archean Early Precambrian but rock

Glaciofluvial deposits of is identified as

sand and gravel measure Mainland DkKn-6 hornblende, gabbro,

between one and three diorite, periodite, and

metres in depth. serpentine. None of

them is the same age. Archean Early

Precambrian but rock Glaciofluvial deposits of

is identified as sand and gravel measure

Mainland DkKn-7 hornblende, gabbro, between one and three

diorite, periodite, and metres in depth.

serpentine. None of them is the same age.

Archean Early Drift and rock

Precambrian but rock consisting of till and

is identified as stratified deposits that

Mainland DjKn-l hornblende, gabbro, measure between one to

diorite, periodite, and three metres thick in

serpentine. None of depressions.

them is the same age.

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More than eighty Archean Early

percent of the rock can Precambrian but rock

be identified as rock Island - Unnamed is identified as

outcrop which is ice island across from DiKm-3 hornblende, gabbro,

eroded Archean granite Tamarack Island diorite, periodite, and

with patches of thin serpentine. None of

drift and scattered them is the same age.

boulders. More than eighty

Archean Early percent of the rock can

Precambrian but rock be identified as rock

is identified as outcrop which is ice

Island - Annie Island DiKm-4 hornblende, gabbro, eroded Archean granite

diorite, periodite, and with patches of thin

serpentine. None of drift and scattered

them is the same age. boulders.

More than eighty Archean Early

percent of the rock can Precambrian but rock

be identified as rock Island - Picture Rock

is identified as outcrop which is ic~

DhKo-l hornblende, gabbro, eroded Archean grarute Island

diorite, periodite, and with patches of thin

serpentine. None of drift and scattered

them is the same age. boulders.

More than eighty Archean Early

percent of the rock can Precambrian but rock

be identified as rock Mainland - Penin sula -

is identified as outcrop which is ic~

DjKr-23 hornblende, gabbro, eroded Archean grarute Western Peninsula

diorite, periodite, and with patches of thin

serpentine. None of drift and scattered

them is the same age. boulders.

More than eighty Archean Early

percent of the rock can Precambrian but rock

be identified as rock Island - U nnamed is identified as

outcrop which is ic~ island but locally called DiKm-51 hornblende, gabbro,

eroded Archean grarute Horseshoe Island diorite, periodite, and

with patches of thin serpentine. None of

drift and scattered them is the same age.

boulders. More than eighty

Archean Early percent of the rock can

Precambrian but rock be identified as rock

Mainland - Peninsula-is identified as

outcrop which is ice DiKq-l0 hornblende, gabbro,

eroded Archean granite Western Peninsula diorite, periodite, and

with patches of thin serpentine. None of

drift and scattered them is the same age.

boulders.

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Page 595: An obsession with meaning: a critical examination of the pictograph sites of the Lake of Woods

Archean Early More than eighty Precambrian, schistose percent of the rock can

volcanic with sorne be identified as rock

DhKm-19 small quantities of outcrop which is ice Mainland - Aulneau

sediments that are iron eroded Archean granite Peninsula formation. Y ounger with patches of thin sediments possibly drift and scattered

exist here. boulders.

Archean Early More than eighty

Precambrian but rock percent of the rock can

is identified as be identified as rock

DhKm-20 hornblende, gabbro, outcrop which is ice Mainland - Aulneau

diorite, periodite, and eroded Archean granite Peninsula

serpentine. None of with patches of thin drift and scattered

them is the same age. boulders.

Archean Early More than eighty

Precambrian but rock percent of the rock can

is identified as be identified as rock

DgKm-2 hornblende, gabbro, outcrop which is ice

Mainland diorite, periodite, and

eroded Archean granite

serpentine. None of with patches of thin drift and scattered

them is the same age. boulders.

Archean Early More than eighty

Precambrian but rock percent of the rock can

is identified as be identified as rock

Island - Unnamed DiKm-50 hornblende, gabbro,

outcrop which is ice island but locally called

diorite, periodite, and eroded Archean granite

Horseshoe Island serpentine. None of

with patches of thin drift and scattered

them is the same age. boulders.

Archean Early More than eighty

Precambrian but rock percent of the rock can

is identified as be identified as rock

DiKm-49 hornblende, gabbro, outcrop which is ice Unnamed island across

diorite, periodite, and eroded Archean granite from Tamarack Island

serpentine. None of with patches of thin drift and scattered

them is the same age. boulders.

Page 569

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'î 1

) /

Appendix 9: Possible Correlations between the Type of Track. Reserves. Offerings in 2001 and before. and Type of Site.

This appenclix presents the data regarding the type of track (routes taken by boat inclicated on charts by the Department of Oceans

and Fisheries), whether the route may or may not exist nearby a site, the presence or absence of reserves nearby, whether offerings were

present in 2001 and before, and whether the site exists on a cliff or in a cave. The word 'near' implies that site is within 6 miles, or

5.21385744 nautical miles, or 9.6506404 kilometres by boat from the nearest reserve. The journey would only take up to 15 to 20 minute by

boat.

DgKl-1

Known­reported on May

29 th 1963 but first recorded by

Dewdney in 1964

5 minutes from South track

that runs through

Sabaskong Bay

Sabaskong Bay lndian Reserve 35

D

Yes - tobacco

Page 570

Pastershank in 1989 - tobacco

Cliff

Page 597: An obsession with meaning: a critical examination of the pictograph sites of the Lake of Woods

') )

Yes = children's and adults clothes (trousers, skirts, t-shirts, socks, chenille sweater, flannel clothes - some old, some new), dried food stuff, bandages, earring (mother of pearl with porcupine quills and

silver and blue beads), earring - plastic heart (never in pairs), tobacco, empty tobacco container ("Copenhagen Tobacco"), beer

Known - first bottle glass, clear glass, "Prayer Sticks" (26 bundles of 12,12 cm

recorded by long by 12.5 - 17 cm wide, tied together with white cotton string,

Dewdney in Sabaskong half of each stick painted blue and the other half painted red, large

1964, then 5 minutes from

Bay Indian diameter sticks always tied together and smalt diameter sticks always

Pastershank in DgKl-2

Pastershank in South track in

Reserve 35 tied together - never mixed, 1 bundle of 12 in the left-hand cave,

1989 - tobacco Cliff

1989 but found Sabaskong Bay

D refer to field sketches and digital and manual photographs). More

in 2001 with new offerings were left on the rock bench under overhang when came

images back later to record more photographs, modern paintings also

visible at site. Returned August 5th 2001 with a team of divers who discovered the rocks immediately below and the vicinity around the rock image site. They discovered that it was a mud bottom and that

there was a pile of rocks but no offerings were evident only Mountain Dew soft drink can, a gentleman's bicycle, and another

cave to the right and 2.14 m (7 feet) below site under water. Known- by

Dewdney but he Yes - tobacco, money (coins) - on shelf/crevices. August 5/01 =

did not record it. It was first

(with divers) - Medicine sticks found under water in same bundles -

recorded by 5 minutes from Sabaskong 12 sticks tied together with string - red and blue just like site

DgKl-Pastershank in South track in

Bay Indian immediately opposite Nestor Falls - are a couple of feet below the None recorded Cliff

17 1989 but Sabaskong Bay

Reserve 35 water level but not immediately beside/below rock art site; broken

informed by Ron D plate but can't find other part - same maker's mark as Horseshoe

Kelly and Ron Island pot - Alfred Meaken; child's fishing rod; collection of shirts

Seymour, from about 6.1 m (20 feet) among large boulders below the water level

nearby reserve Known by

Dewdney but he 5 minutes from

Sabaskong DgKl- did not record.

South track in Bay Indian

No None recorded Cliff 19 Recorded by

Sabaskong Bay Reserve 35

Pastershank in D 1989

---

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') ! ')

Known - first 5 -10 minutes Sabaskong

DgKm-recorded by Reid

from South lndian No None recorded Cliff 1 track in Reserve

in 1975 Sabaskong Bay 45F

June 12/2001 - Yes = multiple articles of clothing (socks, shirts, jeans, jersey shirt, polyester sport shirt, all colours) - all ab ove water level , stuffed in crevices and cracks as well as numerous sample-size

alcohol bottles, coins, tobacco, empty small-size soft drink bottle, towel. July 22/2001 (with divers) - Yes = ceramic pot, glass bottle

Dewdneyin 5 minutes from

(bottom blown into a mould, containing lead drop shot, neck of 1960 - clothing. Known - first bottle hand-finished - no seam at top, cork with hand-tooled top,

DhKm- recorded by main track

None has a smell when opening container - juniper smell, on bottom Molyneaux in

called East 1974 - clothing; Cliff 1 Oewdney in Track through

nearby 25%, wedged in groove in rock about 1.52 - 1.83 m (5-6 feet) from Fox 1974-1960

Whitefish Bay pot), lots of coins in the rock (George V quarter, American penny), bundles of

plate made by same company as bowl from new Horseshoe Island clothing;

site - Alfred Meaken, Royal lronstone China, England, Queen Victoria's crown, lion and unicorn). Huge pile of miscellaneous

clothing, different styles and different periods to the depth of 15.85 m (52ft) from the surface of the water. lncluded fabric and leather

clothes, moccasins, pile leaning against cliff face.

Yes - Stick, peeled - looks like beaver stick but ends are a bit weathered so hard to be 100% sure - 3/4" (1.88 cm) diameter and

10 minutes 1/5' (15.24 cm) long. Tobacco between 2 and 3. Two cowrie shells Known- first from main = one 7.5 cm - other 5 cm (hidden in sedge). One piece of red

DhKm- recorded by track called None clotho One cap (red) embroidered "Sail Caribbean" - deteriorating None recorded Cliff 3 Dewdney in East Track nearby cloth, very faded, not recently left (probably over 1 year old). Ali on

1959 through rock shelf. Soil under areas 2 and 3 has been disturbed recently (by a Whitefish Bay stick chewed by a beaver?) and between bushed at north-east edge,

also under large cowrie shell and one small area of moss 14.4cm (6 inches) from it.

Known -first 5 minutes from

main track DhKm- recorded by

called East None

No None recorded Cliff 4 Dewdney in Track through

nearby 1960

Whitefish Bay

Page 572

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') ")

Known -fu:st 5 minutes from

Dewdneyin main track

DhKm- recorded by called East

None Yes - coins (coin) on 2 ledges, tobacco on 2 ledges, decayed fruit - 1960 found Cliff

5 Dewdney in Track through

nearby food prayer sticks and 1960

Whitefish Bay none later

Known -first 5 minutes from

Dewdneyin main track

DhKm- recorded by called East

None No

1960 found Cliff

18 Dewdneyin Track through

nearby prayer sticks and 1960

Whitefish Bay none later

Sabaskong

10 minutes Bay Indian

Dewdneyin Reserves

Known - first from main

35H & 32 1960 found

DhKn-recorded in 1960

track called C&the Yes - Right side = feather Oarge bird), partially smoked cigarette

overcoat and Cliff

1 South Track various by Dewdney

through lndian

weathered and Reserve on

Sabaskong Bay Obabikon

rotten "rags"

Bay

1 0 minutes of Y es = in the various cracks in the cliff face tobacco (5 piles), Dewdneyin 1960 found

Known- main track None

cigarettes, snuff can lids, 3 sample-size Crown Royal botdes, aIcohol chinaware and

DiKn-1 recorded in 1960 called East nearby

botdes, clothing, money (25 cents = 1977, 1989,1995; 1 cent = other odds and

Cliff by Dewdney Track through 1989, 10 cents = 1994). 2 Jack pine trees up top with gifts on them -

Whitefish Bay dress shirt, towel (on ground), cloth tied around tree. ends. Nothing

found later

5 minutes from

Known - first the alternative

DiKp-1 field drawing by track called the None

No No Cliff Lawson in 1885

east-west route nearby above Aulneau

Peninsula.

DkKn-6 Known in 1985 Not near main None

No No Cliff by Lambert track nearby

DkKn-7 Known in 1985 Not near main None

No No Cliff by Lambert track nearby

---- -

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\) ~ /

Known-Dewdneyin

recorded by Not near main None 1958 and

DjKn-l No Molyneaux in Cliff Dewdney in track nearby 1974 recorded 1958

offerings

Reported in 20 minutes from main

1946 but first track called None

Dewdney in DiKm-3 recorded by

East Track nearby No 1953 found a Cliff

Dewdney in through

"prayer raft" 1953

Whitefish Bay At least 20

Known- first minutes from Dewdneyin

DiKm-4 recorded by main track None Yes-2 silver coins on rocks at base of cliff that were under the 1960 found

Cliff Dewdneyin called East nearby surface of the water clothing, tobacco 1960 Track through and prayer sticks.

Whitefish Bay 10 minutes

from Lake of the alternative Woods

Known - drawn route through Indian

DhKo-by Howard T. area and 20 Reserve 35

1 Thompson on minutes from and Lake Yes - beer bottle glass under moss in vertical crevice None Cliff

1

the 9th South track in of the November 1936 Sabaskong Bay Woods

and 10 minutes Indian from Main Reserve 35]

track 10 minutes

Known-from main

Lake of the DjKr-

Dewdney first track called

Woods IR Yes = money, bullcts (33), tobacco - alliocatcd in crevices Dewdney found

Cliff 23 recorded in 1960

North-South 31B

offering in 1960 track through Big Narrows

Page 574

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') ')

Known-first 5 minutes from

DiKm-recorded by main track

None 51

Dewdneyin called East nearby

No None Cliff 1966 or track through

afterwards ~'hitefish Bay 10 minutes

Known-from main

Lake of the 1 Dewdney found DiKq-

Dewdney first track called

Woods IR No clothing, towel

Cliff 10 North-South and tobacco in

recorded in 1960 track through

31B 1960

Big Narrows Sabaskong

Less 5 minutes Bay Indian

New - found in from main Reserve

DhKm- 2001 but track called and

19 paintings in South Track Sabaskong No Not applicable Cliff

modern paint through Bay Indian Reserves

Sabaskong Bay 35H and 32

C New - found in 5 minutes from

DhKm-2001 but with main track

None 20

date of 1982 but called East nearby

Yes - tobacco, something in water too deep to reach Not applicable Cliff paintings in Track through

modern paint %itefish Bay

New - found in 5 minutes from

Sabaskong main track

DgKm- 2001 but called South

Indian No Not applicable Cliff 2 paintings in Reserve

ochre Track through

45F Sabaskong Bay

New - found in 5 minutes from

DiKm- 2001 but main track

None 50 paintings in

called East nearby

No Not applicable Caye

ochre track through %itefish Bay

Page 575

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")

20 minutes New - found in from main

DiKm- 2001 but track called None No Not applicable Caye

49 paintings in East Track nearby ochre through

Whitefish Bay

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"j )

Appendix 10: Indian reserves, offerings in 2001 and before, type of site, type oflandmass, and orientation of sites.

This appendix presents the data required ta discuss whether a correlation exists between the physical proximity of the pictograph

sites to the nearby reserves and the presence of offerings recorded either in the past or in 2001. It also enables the data regarding the type of

site, its land mass, and orientation to be examined and compared.

DgKl-l

DgKl-2 Sabaskong Bay lndian Reserve

35D

Yes - tobacco

Yes = children's and adults clothes (pants, skirts, t-shirts, socks, chenille sweater, flannel clothes - some old, some new), dried food stuff, bandages, earring (mother of pearl with porcupine quills and

silver and blue beads), earring - plastic heart (never in pairs), tobacco, empty tobacco container ("Copenhagen Tobacco"), beer bottle glass, clear glass, "Prayer Sticks" (26 bundles of 12, 12 cm long by 12.5 - 17 cm wide, tied together with white cotton string,

half of each stick painted blue and the other half painted red, large diameter sticks always tied together and small diameter sticks

always tied together - never mixed, 1 bundle of 12 in the left-hand cave, refer to field sketches and digital and manual photographs). More offerings were left on the rock bench under overhang when came back later to record more photographs, modern paintings

also visible at site. Returned August 5th 2001 with a team of divers who discovered the rocks immediately below and the vicinity around the rock image site. They discovered that it was a mud

bottom and that there was a pile of rocks but no offerings were evident only Mountain Dew soft drinks can, a gentleman's bicycle, and another cave to the right and 2.14m (7 feet) below site under

water.

Page 577

Pastershank in 1989 - tobacco

Pastershank in 1989 - tobacco

1 = 180 (S), 2 = 180 (S), 3 = 90

(E),4 = 101 (E), 5 = 139 (SE), 6 = 120 (SE), 7 = 99

(E), 8 = 150 (SE), 9 = 140 (SE), 10 = 100 (E), Il = 120

(SE), 12 = 120 (SE), 13 = 160

(SSE), 14 = 130 (SE), 15 = 189

(SW)

Cliff

Cliff

Sabaskong Peninsula

Mainland

Sabaskong Peninsula

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') î /

Yes - tobacco, money (coins) - on shelf/crevices. August 5/01 = (with divers) - Medicine sticks found under water in same bundles

Sabaskong Bay - 12 sticks tied together with string - red and blue just like site

Mainland -DgKI-Indian Reserve

immediately opposite Nestor Falls - are a couple of feet below the None recorded 1 - 109 degrees (E) Cliff Cyclone 17

35D water level but not immediately beside/below rock art site; broken

Point plate but can't find other part - same maker's mark as Horseshoe Island pot - Alfred Meaken; child's fishing rod; collection of shirts about 6.1 m (20 feet)among large boulders below the water level

4 - Angle 1 on left when facing cliff -continues to the

DgKl-Sabaskong Bay right to Angle 4 Mainland Indian Reserve No None recorded (at base). 1 - 90 Cliff - Cyclone 19

35D degrees (E), 2 - 93 Point degrees (E), 3 - 90

degrees (E), 4 -162 degrees (SSE)

DgKm-Sabaskong

Indian Reserve No None recorded 81 (E) Cliff Mainland 1 45F

June 12/01 - Yes = multiple articles of clothing (socks, shirts, jeans, jersey shirt, polyester sport shirt, all colours) - all above water level , stuffed in crevices and cracks as well as numerous

sample-size alcohol bottles, coins, tobacco, empty small-size soft drink bottle, towel. July 22/01 (with divers) - Yes = ceramic pot,

glass bottle (bottom blown into a mould, containing lead drop shot, neck of bottle hand-finished - no seam at top, cork with Dewdney in 1960 -

DhKm-hand-tooled top, has a smell when opening container - juniper clothing. Molyneaux Mainland -

1 None nearby smell, on bottom 25%, wedged in groove in rock about 1.52 - 1.83 in 1974 - clothing; 110 degrees (ESE) Cliff Aulneau

m (5-6 feet) from pot), lots of coins in the rock (George V Fox 1974 - bundles Peninsula quarter, American penny), plate made by same company as bowl of clothing;

from new Horseshoe Island site - Alfred Meaken, Royal Ironstone China, England, Queen Victoria's crown, lion and unicorn) (AC). Huge pile of miscellaneous clothing, different styles and different

periods to the depth of 15.85 m (52ft) from the surface of the water. Included fabric and leather clothes, moccasins, pile leaning

against cliff face.

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Yes - Stick, peeled -looks like beaver stick but ends are a bit weathered so hard to be 100% sure - 3/4"(1.88 cm) diameter and

1/5' (15.24 cm) long. Tobacco between 2 and 3. Two cowrie shells = one 7.5 cm - other 5 cm (hidden in sedge). One piece of

Island -DhKm-None nearby

red clotho One cap (red) embroidered "Sail Caribbean" -None recorded 150 degrees (SE) Cliff unnamed

3 deteriorating cloth, very faded, not recendy left (probably over 1 year old). Ali on rock shelf. Soil under areas 2 and 3 has been

island

disturbed recendy (by a stick chewed by a beaver stick?) and between bushed at north-east edge, also under large cowrie shell

and one small area of moss 6 inches from it. .

DhKm- 1 1 = 200 degrees Mainland -

4 None nearby No None recorded (SSW) , 2 = 182 Cliff Aulneau

degrees (S) Peninsula

DhKm- Yes - coins (coin) on 2ledges, tobacco on 21edges, decayed fruit-Dewdney in 1960 Mainland -

5 None nearby

food found prayer sticks 120 degrees (ESE) Cliff Aulneau

and none later Peninsula

DhKm-Dewdney in 1960 Mainland -

18 None nearby No found prayer sticks 230 degrees (SW) Cliff Aulneau

and none later Peninsula Sabaskong Bay

Indian Dewdney in 1960 Left side = 250 Reserves 35H Mainland -

DhKn-and 32 C and Yes - Right side = feather (large bird), partially smoked cigarette

found overcoat and degrees (WSW), Cliff Aulne au

1 the Indian

various weathered Right side = 240 Peninsula

Reserve on and rotten "rags" degrees (WS\X~

Obabikon Bay

Yes = in the various cracks in the cliff face tobacco (5 piles), Dewdney in 1960

right cliff - 119 Mainland -cigarettes, snuff can lids, 3 sample-size Crown Royal botdes,

found chinaware and (SE); le ft cliff - 1 Aulneau

DiKn-1 None nearby alcohol botdes, clothing, money (25 cents = 1977, 1989, 1995; 1 other odds and ends.

(left) = 132 (SE), 2 Cliff Peninsula cent = 1989, 10 cents = 1994).2 Jack pine trees up top with gifts

Nothing found later (right) = 164 - Hay ter

on them - dress shirt, towel (on ground), cloth tied around tree. (SSE) Peninsula

1 - 142 degrees (SE), 2 - 164

Island -DiKp-l None nearby No No

degrees (SSE), 3 -Cliff Cliff

150 degrees (SE), Island

4 - 140 degrees (SE)

Page 579

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DkKn-6

DkKn-7

DjKn-1

DiKm-3

DiKm-4

DhKo-1

DjKr-23

DiKm-51

None nearby

None nearby

None nearby

None nearby

None nearby

Lake of the Woods Indian Reserve 35 and

Lake of the Woods Indian

Reserve 351

Lake of the Woods IR 31B

None nearby

No

No

No

No

Yes-2 silver coins on rocks at base of cliff that were under the surface of the water

Yes - beer bottle glass under m05S in vertical crevice

Yes = money, bullets (33), tobacco - alliocated in crevices

No

Page 580

)

No

No

Dewdney in 1958 and Molyneaux in

1974 recorded offeri~

Dewdney in 1953 found a "prayer

raft"

Dewdney in 1960 found clothing,

tobacco and prayer sticks.

None

Dewdney found offering in 1960

None

322 (NW) Cliff

222 degrees (SW) Cliff

1 = 140 (SE), 2 = . 142 (SE), 3 = (SE) 1 Cliff

WSW-225 degrees

90 degrees - East

Almost due north, 4 degrees

4 (1 being highest of the 4,4 being the lowest). 1 =

148 (SE), 2 = 178 (S), 3 = 164 (SSE),

4 = 160 (SSE)

2 (base) 1 = 200 degrees (SSW), 2 = 182 degrees (S)

1

Cliff

Cliff

Cliff

Cliff

Cliff

Mainland

Mainland

Mainland

Island -Unnamed

island acro5s from

Tamarack Island

Island -Annie Island

Island -Picture Rock Island

Mainland -Peninsula - Western Peninsula

Island -Unnamed island but

locally called

Horseshoe Island

Page 607: An obsession with meaning: a critical examination of the pictograph sites of the Lake of Woods

DiKq- Lake of the 10 Woods IR 31B

Sabaskong Bay Indian Reserve

DhKm- and Sabaskong 19 Bay Indian

Reserves 35H and 32 C

DhKm-20

None nearby

DgKm-Sabaskong

Indian Reserve 2

45F

DiKm-50

None nearby

DiKm-None nearby

49

'\ )

No

No

Yes - tobacco, something in water too deep to reach

No

No

No

Page 581

''j

Dewdney found clothing, towel and

tobacco in 1960

Not applicable

Not applicable

Not applicable

Not applicable

Not applicable

2 (base) 1 = 148 Mainland -Peninsula

(SE), 2 = 120 Cliff - Western

(ESE) Peninsula

Mainland -1 - 154(SE) Cliff Aulneau

Peninsula

1 (base of cliff Mainland -face) 54 degrees Cliff Aulneau

(NE) Peninsula

236 degrees (SW) Cliff Mainland

Island -Unnamed island but

214 (SSW) Cave locally called

Horseshoe Island

NNW, another Island -

Unnamed opening at back

island leads up to top of

Cave DiKm-3 opening

across from

up and facing Tamarack

WSW Island

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'') / )

Appendix 11: Data regarding the type of access to the pictograph site, vegetation at base of site, water levels, and the number of

cliffs used.

This appendix presents the data regarding the type of access to images at each site, the vegetation at the base of each site, the water

level at each site in 2001, the number of cliff faces used, and the total number of images present. It is important to indicate the water level

because it should not be assumed it is the same at each site.

Boat and foot since it was possible to climb on the .

DgKI-2 k b h' f f Present water level None- but rock and water 13.73 m 9 Images roc enc ln ront 0

site

DgKl-17 Boat Present water level None - water 4.572 metres 1 13 images 1 1

DgKl-19 Boat Present water level None - water 6.096 metres 6 images

DgKm-1 Boat Present water level None - water 4 metres 7 images

)hKm-1 Boat Present water level None - water 7 mettes i 17 images 1 1bmnm

From ledge to top of cliff is ' applicable Boat and foot since an . b h 1 d 1 12.19 metres. Ledge has to be 1 because site

DhKm-3 individual had to climb Present water level Jumpedr us ,pa e dCory ka ys, reached by climbing steep cliff 33 images not k f se ge, moss an roc d f . 1 liff . d' 1 up roc ace. compose 0 vertJca c Imme late y

faces and large boulders. adjacent to water

DhKm-4 Boat Present water level None - waler 1.25 metres 5 images

DhKm-5 Boat Present water level None - water 6.096 metres 37 images

Pin cherry, raspberry and DhKm-18 Boat Present water level b 30.48 mettes 6 shapes

water at ase

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White pine, spruce, birch, juniper, pale corydalis, goosefoot, harebells,

Boat and foot because dogbane, rough avens, DhKn-1 site is not immediately Present water level northern bush honeysuckle, 5 - 6 metres 10 images 2

beside water's edge. bear berry, alum root, vetch, 1

columbine, grasses, bracken fern, rock tripe, lichen and

rock

DiKn-1 Boat Present water level None - water 1 = 3.05 metres - 3.66 metres,

16 images 2 2 = 9.14 metres

DiKp-1 Boat Present water level None - water 7 metres 14 images 1

At lowest point = 40 cm from

DkKn-6 Boat - canoe Present water level Water lilies on surface of water surface. At highest

4 images 1 water point = 60 cm from water

surface

DkKn-7 Boat - canoe Present water level Water lilies on surface of

1.39 metres 1 image 1 water at base of cliff

Water lilies on surface of 1 = 2-3 metres, 2 = 5 metres,

DjKn-1 Boat - canoe and foot Present water level water, raspberries and 36 images 3 rock(bottom of cliff no. 3)

3 = 30.48 metres

DiKm-3 Boat Present water level None - water 3.5 metres 29 images 1

DiKm-4 Boat Present water level None - water 5.33 metres 4 images 1

DhKo-l Boat Present water level Bracken fern, moss, rock

2.79 metres 29 images 1 tripe with water

DjKr-23 Boat Present water level None - water 20 metres 8 images 1

DiKm-51 Boat Present water level None - water Approximately 27.45 metres 6 images 1

DiKq-l0 Boat Present water level None - water 15 metres 11 images 1

DhKm-19 Boat and land (foot

Present water level None - water 4 metres 1 image 1 access)

- ------ -

Page 583

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~) ')

Balsam fir, white spruce, juniper, raspberry,

gooseberry, pale corydalis,

DhKm-20 Boat Present water lever climbing false buckwheat on

18.29 metres 4 images 1 rock she!f immediately

be!ow paintings and mosses, lichens on rock face which

just water

DgKm-2 Boat Present water lever None -water 4-5 metres 6 images 1

not applicable because Not DiKm-50 Boat/foot Present water lever None because water present exit/ entrance immediate!y 1 image applicable

beside water because cave

not applicable because Not DiKm-49 Boat/canoe Present water lever None because water present exit/ entrance flooded with 2 images applicable

water because cave

Page 584

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Appendix 12: Do an the sites have the necessary physical features for pictographs?

This appendix is designed ta quickly establish correlations between the five prerequisites required by sorne previous archaeologists

for the presence of paintings. It is clear that only one site, DgKl-2, has aIl the five key features, or prerequisites. Each of these prerequisites

is cornbined with the number of blobs, total number of images, as weIl as the rocks at the base of cliff faces.

DgKl-1 1 Cliff Yes (above Yes (below 1 No

1

No 1

No 1

1 small blob, 4 small blobs along 8 images No

paintings) paintings) side each other

Yes (paintings Yes 1 small blob, 4 small blobs

DgKl-2 1 Cliff above feature Yes (below

(through Yes (above

Yes alongside and attached to each 9 images Yes (above &

and paintings paintings) paintings) below water) on feature)

paintings) other, 1 unidentifiable shape

DgI<l- Yes (ab ove Yes Yes

Yes (adjacent 1 Cliff (adjacent (through No 1

No blobs 1

13 images 1 No 17 paintings)

paintings) paintings) paintings)

DgKl- Yes (ab ove Yes Yes

Yes (through 1 blob and area of pairs of

Yes (ab ove & 19

Cliff paintings)

(adjacent (through paintings)

No verticallines and spots of small 6 images below water)

paintings) paintings) concentrations of ochre

DgKm-Yes (feature Yes

Yes (adjacent 1

1

Yes (above & Cliff ab ove No (through No 11arge oval blob 7 images

1 ltings) paintings)

paintings) below water)

Yes (feature Yes Yes Yes (above & 2 blobs, horizontal oval blob with

DhKm- 1 above & Cliff

adjacent to (through (through through No two short verticallines sticking

1 17 images 1 No

paintings) paintings) paintings) paintings up on top right lund side

DhKm- Yes (above Yes (below Yes Yes (ab ove & 1

1

Yes (above 3

Cliff paintings) paintings)

(through through No 10 hlobs 33 images water)

paintings) paintings

DhKm-Cliff No 1 :~~_~~~~e Yes (above

No 1

No 1

No blobs 5 images No 4 ......... : ......... : ..... ,.... .... \

Page 585

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î î

Yes (below Yes 10 different types of blobs, 1

DhKm-Cliff

Yes (ab ove & amongst (through

Yes (adjacent No

group of blobs of different sizes, 37 images

Yes (above 5 paintings) paintings) 1 round blob with short lines water) paintings) paintings)

sticking out either sicle

Yes 1 blob, one faint unidentifiable DhKm-

Cliff Yes (ab ove Yes (below (between & Yes (through

No shape, a group of small blobs and

6 shapes Yes (above

18 paintings) paintings) adjacent paintings) lines that cross each other at water) paintings) ninety degree angles

DhKn-Yes (paintings

Yes (below Yes (below Yes (through Yes (above 1

Cliff found on paintings) paintings) paintings)

No 2 blobs 10 images water)

1

overhangs)

Yes (below Yes

Yes (through ,

DiKn-l Cliff No (through No 8 blobs, 1 collection of blobs 16 images Yes (above

paintings) paintings)

paintings) water) :

Yes (several ,

overhangs -paintings Yes

Yes (adjacent 2 faint unidentifiable shapes, 5 Yes

DiKp-l Cliff below No (through No 14 images (underwater overhangs and paintings)

paintings) different types of blobs only)

paintings on feature)

DkKn- Yes (below Yes (below Yes Yes

Cliff (adjacent No Yes 4 blobs 4 images (underwater 6 paintings) paintings) paintings) onl1')

DkKn-Yes (ab ove Yes

Yes (adjacent Yes (above 7

Cliff No & adjacent (adjacent paintings)

No 1 blob 1 image water)

paintings) paintings)

Yes (below Yes (above Yes (adjacent

Yes (above DjKn-l Cliff No

paintings) paintings) & below No 8 blobs 36 images

water) paintings)

DiKm-Yes (paintings Yes

Yes (above & 3

Cliff on the No (through No No 5 blobs 29 images below water)

overhang) paintings)

DiKm-Yes

Yes (adjacent Yes (ab ove & Cliff No No (adjacent No No blobs 4 images

4 paintings)

paintings) below water) --- ---- -

Page 586

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DhKo- Yes (below Yes

Yes (through 3 blobs and 1 spiky blob with Cliff No (through No 29 images No

1 paintings) paintings)

paintings) seven lines sticking out

DjKr- Yes (below Yes

Yes (through 2 blobs and two small round

Yes (ab ove & Cliff No (through No blobs one immediately on top of 8 images

23 paintings) paintings)

paintings) the other

below water)

DiKm-Yes (above Yes Yes (ab ove &

Yes (ab ove & 51

Cliff No & below (through below No 1 blob 6 images below wa ter)

paintings) paintings) paintings)

DiKq-Yes

Cliff No No (through No No 7 blobs 11 images No 10

paintings) 1

DhKm-Cliff No

Yes (below No

Yes (above No No blobs 1 image No

19 paintings) paintings)

DhKm- Yes (ab ove Yes (ab ove

Yes (ab ove & 20

Cliff paintings)

No & through No No No blobs 4 images below water)

paintings)

Yes (paintings

DgKm-above the Yes -check Yes

Yes (ab ove 2

Cliff overhang and with field (through paintings)

No 4 blobs 6 images No on the notes paintings)

overhang) cave -

DiKm-Cave

cave - not cave - not cave - not cave - not not No blobs 1 image

cave - not 50 applicable applicable applicable applicable applica applicable

ble cave -

DiI<Jn-Cave

cave - not cave - not cave - not cave - not not No blobs 2 images

cave - not 49 applicable applicable applicable applicable applica applicable

ble

Page 587

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.~ ')

Appendix 13: Sites grouped according to the number of physical attributes present.

This appendix demonstrates that only one site had aU Eve of the physical attributes argued by previous archaeologists as important

for the presence of paintings at pictograph sites on cliffs. The table below clearly indicates that the most sites have only four of the Eve

physical attributes considered prerequisite: deep holes, large crevices and cracks, rock overhangs, rock benches, and rock ledges. Rocks at

the base of cliffs and caves are not considered as one of the prerequisites since only Rusak (1992a) recorded and considered this features as

important.

DgKl-2 DgKl-19 DhKo-l DiKm-3

DhKm-3 DgKm-l DgKl-l

DhKm-5 DiKm-51 DhKm-4

DhKm-18 DiKn-l DhKm-20

DhKn-l DiKm-4 DhKm-19

DkKn-6 DkKn-7 DiKp-l

DgKl-17 DjKn-l DiKq-l0

DgKm-2 DjKr-23

DhKm-l

Page 588

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Appendix 14: Sites grouped according to number of physical attributes present plus offerings.

Data in this appendix demonstrates any correlation between the presence of the physical attributes and the presence of offerings in

2001. The table indicates that the presence of the five physical attributes did indicate that offerings were present in 2001 (those sites that

have offerings are in italics). The cave sites DiKm-49 and DiKin-50 are not included in this table because not ail the physical prerequisites

are associated with caves. Furthermore neither site had offerings.

DgKl-2 DgKl-19 DhKo-1 DiKm-3

DhKm-3 DgKm-l DgKI-1

DhKm-5 DiKm-51 DhKm-4

DhKm-18 DiKn-1 DhKm-20

DhKn-1 DiKm-4 DhKm-19

DkKn-6 DkKn-7 DiKp-l

DgKl-17 DjKn-l DiKq-l0

DgKm-2 DjKr-23

DhKm-1

Page 589

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'1 !

-)

Appendix 15: Sites grouped according to number of physical attributes present and with rocks at base of cliff face.

This appendix demonstrates that only one site had ail five of the physical attributes argued by previous archaeologists as important

for the presence of paintings at pictograph sites on cliffs, and that most sites have only four of the five physical attributes. The sites with

rocks at their base are in italics. Rocks do not exist in the cave site called DiKm-49 but they do occur at the base of DiKm-50 but neither

site is included in this table because this table is concerned with the sites on cliff faces.

DgKI-2 1

DgKI-19 DhKo-l DiKm-3 1

DhKm-3 DgKm-1 DgKJ-l

DhKm-5 DiKm-51 DhKm-4

DhKm-18 DiKn-1 DhKm-20

DhKn-1 DiKm-4 DhKm-19

DkKn-6 DkKn-7 DiKp-1

DgI<l-17 DjKn-1 DiKq-l0

DgKm-2 DjKr-23

DhKm-l

Page 590

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Appendix 16: The "presence and absence" tables and the dendrograms from the Pearson correlation and the Euclidean distance method to consider the re1ationship between the physical attributes of the sites, the different sites and the images, and the relationship between the sites and sorne of the largest shape types.

The information entered in the tables below was subsequently examined using SPSS to confirm the existence of clusters. Through

SPSS clusters were analysed and the relationship between the different sites and image types was investigated. The sequence of information

foilows that of the chapter. The relationship between different aspects of the sites, the relationship between the physical attributes of the

sites, and finaily the relationship between sites and some of the largest shape types identified in Chapter V.

a) The data presented below was used to create the foilowing dendrograms, and to indicate the weak relationship, perhaps differing

insignificantly from randomness, between these sites and the different features such as to the type of land mass, access to sites by boat,

proximity to lndian reserves, offerings left nearby the images in 2001, vegetation at base, proximity to site and number of cliffs at a site if

the site was on a cliff face.

In the "type of site" column, number 1 designates a cliff, while 0 means that the site is a cave. In the "land mass" column, '1' stands

for mainland and '0' indicates an island. The 'l'in the "access" column indicates a site accessible only by boat, and the '0' indicates that the

images could be reached by foot as weil as boat. The '1' under "proximity to lndian reserve" shows that an lndian reserve existed near the

site in 2001, while a '0' indicates no proximate reserve. As discussed in Chapter VI the word 'near' implies that site is within 6 miles, or

5.21385744 nautical miles, or 9.6506404 kilometres by boat from the nearest reserve. The journey would only take up to 15 to 20 minute by

boat. The 'l'in the "offerings le ft at sites in 2001" column indicates that offerings were found there in 2001, while '0' indicates that no

offerings were found. The 'l'in the "vegetation at base" column indicates that plant matter grew at the base of the site, while the '0'

indicates that vegetation was not present at the base of the site. The '1' under "proximity of main track to site" indicates that the site was

close by to an officiaily charted water route, and the '0' indicates that it was not. The 'l'in the "number of cliffs" column indicates images

occurring on one cliff face, while '0' shows that multiple cliff faces were used. A '-9' placed in this column shows paintings occurred inside a

cave rather than on a cliff face.

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-_.- -------

proximity offerings proximity

Borden latitude longitude

geographical type land acces to Indian left at sites

vegetation at of main numberof number range of site mass s Base track to c1iffs

reserve in 2001 site

DgKl-1 49 09' 15" 94 56' 32" Sabaskong Bay 1 1 1 1 1 0 1 1 DgKl-2 49 06' 48" 93 57' 18" Sabaskong Bay 1 1 0 1 1 0 1 1 DgKl-17 4905' 48" 93 58' 12" Sabaskong Bay 1 1 1 1 1 0 1 1

DgKl-19 4905' 54" 93 58' 00" Sabaskong Bay 1 1 1 1 0 0 1 1 DgKm-1 49 05' 39" 94 04' 51" Sabaskong Bay 1 1 1 1 0 0 1 1 DhKm-1 49 14' 54" 94 04' 00" Whitefish Bay 1 1 1 0 1 0 1 1 DhKm-3 4917' 42" 9403' 39" Whitefish Bay 1 1 0 0 1 1 1 1 DhKm-4 49 14' 30" 9404' 00" Whitefish Bay 1 1 1 0 0 0 1 1

DhKm-5 4914' 0" 9404' 48" Whitefish Bay 1 1 1 0 1 0 1 1 DhKm-18 4914' 31" 9404' 33" Whitefish Bay 1 1 1 0 0 1 1 1

nr Obabikon DhKn-1 4912' 12" 9416' 0" Bay 1 1 0 1 1 1 1 0 DiKn-1 4925' 18" 9413' 06" Whitefish Bay 1 0 1 0 1 0 1 0 DiKp-1 4928' 24" 9430' 24" Sunset Channel 1 0 1 0 0 0 1 1 DkKn-6 4939' 45" 9417' 09" Blindfold Lake 1 1 1 0 0 0 0 1 DkKn-7 4939' 45" 9417' 09" Blindfold Lake 1 1 1 0 0 0 0 1

DjKn-1 4940' 03" 9414' 36" Blindfold Lake 1 1 0 0 0 1 0 0 DiKm-3 4922' 42" 947'36" Whitefish Bay 1 0 1 0 0 0 1 1 DiKm-4 4920' 30" 9403' 51" Whitefish Bay 1 0 1 0 1 0 1 1

Painted Rock DhKo-1 4912' 06" 9429' 36" Channel 1 0 1 1 1 1 1 1

DjKr-23 4930' 54" 9451' 54" Portage Bay 1 1 1 1 1 0 1 1 DiKm-51 4921'12" 9407' 36" Whitefish Bay 1 0 1 0 0 0 1 1 DiKq-10 4929' 51" 9448' 54" Bishop Bay 1 1 1 1 0 0 1 1

DhKm-19 4910' 57" 9408' 03" Turtle Lake 1 1 0 1 0 0 1 1 DhKm-20 49 14' 30" 9404' 12" Whitefish Bay 1 1 1 0 1 1 1 1 DgKm-2 49 06' 06" 9404' 24" Sabaskong Bay 1 1 1 1 0 0 1 1 DiKm-50 4921' 12" 9407' 36" Whitefish Bay 0 0 0 0 0 0 1 -9

DiKm-49 4921' 12" 9407' 36" Whitefish Bay 0 0 1 0 0 0 1 -9

Page 592

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Hierarchical Cluster Analysis - Dendrogram using Average Linkage (Between Groups) using Euclidean Distance Method Rescaled Distance Cluster Combine

CAS E 0 5 10 15 20 25 Label Num DiKq-10 22

DgKm-2 25

DgKl-19 4

DgKm-1 5 --' 1-

DgKl-17 3

3 DjKr-23 20

DgKl-1 1

DgKl-2 2

DhKm-19 23 1

1 DkKn-6 14

Tl-DkKn-7 15

DhKm-4 8

Di'Km-3 17

3 DiKm-51 21

DiKp-1 13

DhKm-1 6 J ~ DhKm-5 9

DiKm-4 18

DhKm-18 10 ===rt-r-DhKm-20 24

DhKm-3 7

DhKo-1 19

DiKn-1 12

DhKn-1 11

DjKn-1 16

DiKm-50 26

DiKm-49 27

Page 593

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/

Hierarchical Cluster Analysis - Dendrogram using Average Linkage (Between Groups) using Pearson Correlation Method Rescaled Distance Cluster Combine

CAS E o 5 10 15 20 25 Label Num DiKq-lO 22

DgKm-2 25

DgKl-19 4

DgKm-l 5

DhKm-19 23

DgKl-17 3

DjKr-23 20

DgKl-1 1

DgKl-2 2

DkKn-6 14

DkKn-7 15

DhKm-4 8

DhKm-18 10

DiKm-3 17

DiKm-51 21

DiKp-1 13

DhKm-1 6

DhKm-5 9

DiKn-1 12

DiKm-4 18

DhKo-1 19

DiKm-50 26

DiKm-49 27 J DhKn-1 11

DhKm-3 7

DhKm-20 24

DjKn-1 16

Page 594

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b) The table below indicates a weak relation between the site and the five required physical features considered necessary for the presence

of a pictograph site. The following dendrograms confirm this weak relationship.

A '-9' indicates cave sites without cliffs. The '1' indicates the presence of a feature at a site, while the '0' points to its absence. --- -- ---------- -- _ .. _- ----- -- ------ -- -- --_ ....... _-

Site Latitude Longitude Geographical Type of

Overhang Shelves Cracks Crevices Roles Rocks at

Range Site Base

DgKl-l 49 09' 15" 94 56' 32" Sabaskong Bay 1 1 1 0 0 0 0

DgKl-2 49 06'48" 93 57' 18" Sabaskong Bay 1 1 1 1 1 1 1

DgKl-17 49 05'48" 93 58' 12" Sabaskong Bay 1 1 1 1 1 0 0

DgKl-19 49 05' 54" 93 58' 00" Sabaskong Bay 1 1 1 1 1 0 1 J DgKm-l 49 05'39" 94 04' 51" Sabaskong Bay 1 1 0 1 1 0 1

!

DhKm-l 4914' 54" 94 04'00" Whitefish Bay 1 1 1 1 1 0 0 1

DhKm-3 49 17' 42" 9403' 39" Whitefish Bay 1 1 1 1 1 0 1

DhKm-4 4914' 30" 9404' 00" \Xlhitefish Bay 1 0 1 1 0 0 0 ,

DhKm-5 4914' 0" 9404' 48" Whitefish Bay 1 1 1 1 1 0 1 1

DhKm-18 4914' 31" 9404' 33" Whitefish Bay 1 1 1 1 1 0 1 DhKn-l 4912' 12" 9416' 0" nr Obabikon Bay 1 1 1 1 1 0 1 i

DiKn-l 4925' 18" 9413' 06" Whitefish Bay 1 0 1 1 1 0 1

DiKp-l 4928' 24" 9430' 24" Sunset Channel 1 1 0 1 1 0 1

DkKn-6 4939' 45" 9417' 09" Blindfold Lake 1 1 1 1 0 1 1

DkKn-7 4939' 45" 9417' 09" Blindfold Lake 1 0 1 1 1 0 1

DjKn-l 4940' 03" 9414' 36" Blindfold Lake 1 0 1 1 1 0 1

DiKm-3 4922' 42" 947'36" Whitefish Bay 1 1 0 1 0 0 1

DiKm-4 4920' 30" 9403' 51" Whitefish Bay 1 0 0 1 1 0 1 Painted Rock

DhKo-l 4912' 06" 9429' 36" Channel 1 0 1 1 1 0 0

DjKr-23 4930' 54" 9451' 54" Portage Bay 1 0 1 1 1 0 1

Page 595

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DiKm-51 4921' 12" 9407' 36" Whitefish Bay 1 0 1 1 1 0 1

DiKq-l0 4929' 51" 9448' 54" Bishop Bay 1 0 0 1 0 0 0

DhKm-19 4910' 57" 9408' 03" Turtle Lake 1 0 1 0 1 0 0

DhKm-20 4914' 30" 944' 12" Whitefish Bay 1 1 0 1 0 0 1

DgKm-2 49 06' 06" 9404' 24" Sabaskong Bay 1 1 1 1 1 0 0

DiKm-50 4921'12" 9407' 36" Whitefish Bay 0 -9 -9 -9 -9 -9 -9

DiKm-49 4921'12" 9407' 36" Whitefish Bay 0 -9 -9 -9 -9 -9 -9

Page 596

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Hierarchical Cluster Analysis - Dendrogram using Average Linkage (Between Groups) using Euclidean Distance Method Rescaled Distance Cluster Combine

CAS E 0 5 10 15 20 25 Label Num DiKm-50 26

DiKm-49 27

DgKl-2 2

DkKn-6 14

DiKm-3 17

DhKm-20 24

DgKm-1 5

DiKp-1 13

DiKm-4 18

DjKr-23 20

DiKm-51 21

DiKn-1 12

DkKn-7 15

DjKn-1 16

DhKm-18 10

DhKn-1 11

DgKl-19 4

DhKm-3 7

DhKm-5 9

DhKm-1 6

DgKm-2 25

DgKl-17 3

DhKo-1 19

DhKm-19 23

DhKm-4 8

DiKq-10 22

DgKl-1 1

Page 597

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Hierarchical Cluster Analysis - Dendrogram using Average Linkage (Between Groups) using Pearson Correlation Method Rescaled Distance Cluster Combine

CAS E 0 5 10 15 20 25 Label Num DiKm-3 17

DhKm-20 24

DgKm-1 5

DiKp-1 13 ~ DiKm-4 18

DhKm-4 8

DiKq-10 22

DhKm-18 10 -DhKn-1 11 -DgKl-19 4

DhKm-3 7 -DhKm-5 9 -DhKm-1 6

DgKm-2 25

DgKl-17 3

l J

DjKr-23 20 -DiKm-51 21 -

DiKn-1 12

DkKn-7 15 -

DjKn-1 16 - -

DhKo-1 19

DhKm-19 23

DgKl-2 2

DgKl-1 1

DkKn-6 14

DiKm-50 26

DiKm-49 27

Page 598

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Ali of the image shapes that had large numbers of same type were re-described using either the number 'l'or '0'. The "presence­

absence" tables presented below used information ruscussed in Chapters V and VI. The '1' indicates the presence of a feature for each

shape while the '0' indicates its absence.

However, because they lack the descriptive precision of words, numbers inadequately describe the attribute of a shape. SPSS was

employed to conduct cluster analysis if the image shapes group was large enough. However, such analysis becomes impossible in cases

where the shape sample size is too smali. It should also be remembered that the dataset, containing only three hundred and eighteen images,

is very smali.

c) The 'zig-zag':

------- ~----- ~~ -

Borden Latitude Longitude Geographical Range

Zig-horizontal vertical diagonal he ad

ears or forked number zag horns end

DhKm-l 49 14' 54" 94 04'00" Whitefish Bay 1 0 1 0 0 0 0 DhKm-l 49 14' 54" 94 04' 00" Whitefish Bay 1 0 1 0 0 0 0 DiKp-l 4928' 24" 9430' 24" Sun set Channel 1 1 0 0 1 1 0 DiKm-3 4922' 42" 9407' 36" W'hitefish Bay 1 0 0 1 1 1 0 DiKm-3 4922' 42" 9407' 36" W'hÏtefish Bay 1 0 1 0 1 1 1 DhKm-3 4917' 42" 9403' 39" Whitefish Bay 1 0 1 0 0 0 1 DiKm-4 4920' 30" 9403' 51" W'hÏtefish Bay 1 0 1 0 0 0 1

bent four bent five bent three bent Bent seven bent eight times

time times times twice times 1 0 0 0 0 0 0 1 0 0 0 0 1 0 0 0 0 0 0 0 1 0 0 0 0 0 0 1 0 0 0 0 0 0 1 0 0 0 0 0 0 1

Page 599

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The dendrogram below, using hierarchical cluster analysis and Euclidean distance, indicates that the correlation is qui te weak between the

sites and the shape loosely categorised as a 'zig-zag.'

Hierarchical Cluster Analysis - Dendrogram using Average Linkage (Between Groups) using Euc1idean Distance Method Rescaled Distance Cluster Combine

CAS E 0 5 10 15 20 25 Label Num

DhKm-3 6

DiKm-4 7

DhKm-1 1

DhKm-1 2 ~ DiKm-3 5

DiKp-1 3

DiKm-3 4

Hierarchical Cluster Analysis - Dendrogram using Average Linkage (Between Groups) using Pearson Correlation Method Rescaled Distance Cluster Combine

CAS E o 5 10 15 20 25 Label Num +---------+---------+---------+---------+---------+

DhKm-3 6

DiKm-4 7 ]

DiKm-3 5

DhKm-1 1

DhKm-1 2

DiKp-1 3

DiKm-3 4

Page 600

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'\ -') !

d) The 'turtle':

--------- ----------_._------ -- ---_ ... _-- - -- -- -

Borden Geographical centre ochre

Latitude Longitude horizontal vertical diagonal tail he ad legs of number Range

image paint

DhKm-3 4917' 42" 9403' 39" Whitefish Bay 0 1 0 1 1 1 0 1 49 12' 12" - 94 16' nr Obabikon

DhKn-l 0" 9416' 0" Bay 0 1 0 1 1 1 1 1 DhKm- 49 10' 57" - 9408'

19 03" 9408' 03" Whitefish Bay 0 1 0 1 1 1 1 0

This group eannot be examined using SPSS beeause there are only three types of this specifie shape.

e) The 'bird':

head head

Borden Latitude Longitude

Geographical horizontal vertical diagonal

Tail wings with

with number Range outspread

beak up beak to

the right

DhKm-3 4917' 42" 9403' 39" Whitefish Ba~ 0 1 0 1 1 1 0 DhKm-18 4914' 31" 9404' 33" Whitefish Bay 0 1 0 0 1 0 1

Head !

with centre of ochre beak to image paint the le ft

0 1 1 0 0 1

This group eannot be examined using SPSS beeause there are only two types of this specifie shape.

f) The 'hand print':

Page 601

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The number '-9' indicates that exfoliation, lichen or rock tripe encroachment, and white mineraI deposits rendered impossible

establishing whether the shape was either hollow or solid.

Borden latitude longitude

geographical right left unknown vertical horizontal diagonal fingers thumb ochre

centre number range paint

DgKl- 49 05' Sabaskong 19 54" 93 58'00" Bay 0 1 0 1 0 0 1 1 1 1

DgKl- 49 05' Sabaskong 19 54" 93 58'00" Bay 1 0 0 1 0 0 1 1 1 1

DhKm- 49 17' 3 42" 9403' 39" Whitefish Bay 1 0 0 0 0 1 1 1 1 1

DhKm-5 49 14' 0" 9404' 48" Whitefish Bay 0 0 1 0 1 0 1 0 1 1

DhKm-5 4914' 0" 9404'48" Whitefish Bay 0 0 1 0 0 1 1 0 1 1

DhKm-5 4914' 0" 9404'48" Whitefish Bay 0 0 1 0 0 1 1 0 1 1

DhKm-5 4914' 0" 9404'48" Whitefish Bay 0 0 1 0 0 1 1 0 1 1

DhKm-5 4914' 0" 9404'48" Whitefish Bay 0 0 1 0 0 1 1 0 1 1

DhKm-5 49 14' 0" 9404'48" Whitefish Bay 0 1 0 1 0 0 1 1 1 1

DhKm-5 49 14' 0" 94 04'48" Whitefish Bay 0 0 0 1 1 0 1 0 -9 1

DhKm-5 4914' 0" 9404' 48" Whitefish Bay 0 1 0 1 0 0 1 1 -9 1

DhKm-5 4914' 0" 9404' 48" Whitefish Bay 0 0 1 1 0 0 1 0 -9 1

--------

Page 602

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DhKm-5 49 14' 0" 9404' 48" Whitefish Bay 1 0 0 1 0 0 1 1 1 1

DhKm-5 4914' 0" 9404' 48" Whitefish Bay 1 0 0 l 0 0 1 1 -9 1

DhKm-5 4914' 0" 9404' 48" Whitefish Bay 1 0 0 1 0 0 1 1 1 1

Blindfold DjKn-l 4940' 3" 9414' 36" Lake 0 0 1 1 0 0 1 0 0 1

Blindfold DjKn-l 4940' 3" 9414' 36" Lake 0 1 0 0 1 0 1 1 0 1

Blindfold 1 DjKn-l 4940' 3" 9414' 36" Lake 0 1 0 0 0 1 1 1 0 1

Blindfold DjKn-l 4940' 3" 9414' 36" Lake 1 0 0 1 0 0 1 1 0 1

Blindfold DjKn-l 4940' 3" 9414' 36" Lake 1 0 0 1 0 0 1 1 1 1

Blindfold DjKn-l 4940' 3" 9414' 36" Lake 1 0 0 0 0 1 1 1 0 1

Blindfold DjKn-l 4940' 3" 9414' 36" Lake 1 0 0 1 0 0 1 1 0 1

DiKm- 4922' 3 42" 9407' 36" Whitefish Bay 0 1 0 1 0 0 0 0 1 1

DiKm- 4922' 1

3 42" 9407' 36" Whitefish Bay 0 1 0 1 0 0 0 0 1 1 1

DiKm- 4922' 3 42" 9407' 36" Whitefish Bay 1 0 0 1 0 0 0 0 1 1

DiKm- 4922' 3 42" 9407' 36" Whitefish Bay 1 0 0 1 0 0 0 0 1 1

Hierarchical cluster analysis was undertaken using this data, resulting in the following dendrograms. The dendrograms below, labelled (i)

and (il), confirm a very weak correlation, and perhaps differ insignificantly from randomness between the site and the shape called a 'hand

print.'

Page 603

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Hierarchical Cluster Analysis - Dendrogram using Average Linkage (Between Groups) using Euclidean Distance Method Rescaled Distance Cluster Combine

CAS E 0 5 10 15 20 25 Label Num

DiKm-3 25

DiKm-3 26

DiKm-3 23

DiKm-3 24

DhKm-3 3

DjKn-1 21

DgKl-19 1

DhKm-5 9

DjKn-1 19

DjKn-1 22

DhKm-5 15

DjKn-1 20

DgKl-19 2

DhKm-5 13

DjKn-1 17

DjKn-1 18

DhKm-5 7

DhKm-5 8

DhKm-5 5

DhKm-5 6

DhKm-5 4

DjKn-1 16

DhKm-5 11

DhKm-5 14

DhKm-5 10

DhKm-5 12

Page 604

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'\ ) )

Hierarchical Cluster Analysis - Dendrogram using Average Linkage (Between Groups) using Pearson Correlation Method Rescaled Distance Cluster Combine

CAS E o 5 10 15 20 25 Label Num

DhKm-5 7 -DhKm-5 8 -

DhKm-5 5

DhKm-5 6 -DhKm-5 4

DjKn-1 16

DiKm-3 23

DiKm-3 24

DgKl-19 1

DhKm-5 9

J 1

~

1

J DhKm-3 3

DjKn-1 21 1

DiKm-3 25

DiKm-3 26 J DjKn-1 19

DjKn-1 22 J DhKm-5 15 -DjKn-1 20 -DgKl-19 2

DhKm-5 13 -DhKm-5 11

DhKm-5 14

DhKm-5 10

DhKm-5 12 ~ DjKn-1 17

DjKn-1 18

Page 605

Page 632: An obsession with meaning: a critical examination of the pictograph sites of the Lake of Woods

~\, ! )

g) The group loosely categorized as 'paralle1lines':

---- --- _ .. _----

Borden Latitude Longitude

Geographical diagonal vertical horizontal

touch each other in ochre paint

number Range the middle

DhKm-4 4914' 30" 9404' 00" Whitefish Bay 0 1 0 0 1 DgK1-1 49 09' 15" 94 56' 32" Sabaskong Bay 0 0 1 0 1 DiKm-3 4922' 42" 947'36" Whitefish Bay 1 0 0 0 1 DjKn-l 4940' 3" 9414' 36" Blindfold Lake 0 1 0 1 1

The small number of this shape types prevents conducting any hierarchical cluster analysis.

h) The 'crescents':

The number '-9' indicates that white mineraI deposits, exfoliation, or lichen and rock tripe encroachment rendered impossible

establishing whether there were three or four lines present. (Table continued on next page)

Borden Latitude Longitude Geographical Range vertical horizontal diagonal

points face number left

DgK1-2 49 06' 48" 93 57' 18" Sabaskong Bay 0 0 0 0 DgK1-1 49 09' 15" 94 56' 32" Sabaskong Bay 0 1 0 0 DgK1-1 49 09' 15" 94 56' 32" Sabaskong Bay 0 1 0 0

DhKm-5 49 14' 0" 9404' 48" Whitefish Bay 0 1 0 0 DhKm-5 4914' 0" 9404' 48" Whitefish Bay 0 0 1 0 DiKn-l 4925' 18" 9413' 06" Whitefish Bay 0 1 0 0 DiKn-l 4925' 18" 9413' 06" Whitefish Bay 0 1 0 0 DjKn-l 4940' 03" 9414' 36" Blindfold Lake 0 1 0 0 DjKn-l 4940' 03" 9414' 36" Blindfold Lake 0 1 0 0 DjKn-l 4940' 03" 9414' 36" Blindfold Lake 0 1 0 0

~:Km-5L 4921'12" _J>4Q7'l§" .. ~

Whitefish B~ _ 0 1 0 0 -- -- ~ ~-

Page 606

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)

points face points face points face four vertical three vertical four vertical three vertical ochre centre

right up down linestop linestop lines down lines down paint

1 0 0 1 0 0 0 0 0

0 1 0 1 0 0 0 1 1 0 1 0 1 0 0 0 1 1 0 0 1 1 0 0 0 0 1 1 0 0 1 0 0 0 0 1 0 1 0 1 0 1 0 0 1 0 1 0 1 -9 -9 0 0 1 0 0 1 1 0 0 -9 -9 1 0 0 1 1 0 0 1 0 1 0 1 0 1 0 1 0 0 1 0 0 1 1 0 0 0 0 1

Hierarchical Cluster Analysis - Dendrogram using Average Linkage (Between Groups) using Euc1idean Distance Method

Label

DhKm-5

DiKm-51

DjKn-1

DiKn-1

DjKn-1

DgKl-1

DgKl-1

DgKl-2

DhKm-5

DiKn-1

DjKn-1

CAS E

Rescaled Distance Cluster Combine

o 5 10 15 20 25 Num +---------+---------+

4

11

9

6

10

2

3 1---

1

5

7

8

Page 607

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) ')

The dendrogram above, obtained using Euclidean distance, indicates a weak correlation between sites and 'crescent' shapes. The

dendrogram below, using Pearson correlation, confirms this finding.

Hierarchical Cluster Analysis - Dendrogram using Average Linkage (Between Groups) using Pearson Correlation Method

Rescaled Distance Cluster Combine

CAS E 0 5 10 15 20 25 Label Num

DiKn-1 6

DjKn-1 10 J DgKl-1 2

DgKl-1 3 J DhKm-5 4

DiKm-51 11 J DjKn-1 9

DiKn-1 7

DgKl-2 1

DhKm-5 5

DjKn-1 8 ~ h) The group loosely categorized as 'creatures':

The number '-9' indicates that a 'creature' faced up rather than left or right. This table continues on the next page.

Borden facing facing 1 back 2

1 front Latitude Longitude Geographical Range horizontal vertical back number left right leg

legs leg

DgKl-l 49 09' 15" 94 56' 32" Sabaskong Bay 1 0 1 0 1 0 1 1

-- ---

Page 608

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DgKl-l 49 09' 15" 94 56' 32" Sabaskong Bay 1 0 0 1 1 0 1 DgKl-17 49 5' 48" 93 58' 12" Sabaskong Bay 1 0 1 0 0 1 1 DgKl-2 49 06'48" 93 57' 18" Sabaskong Bay 1 0 0 1 1 0 0

DhKm-3 49 17' 42" 9403' 39" Whitefish Bay 1 0 1 0 1 0 1 DhKm-3 49 17' 42" 9403' 39" Whitefish Bay 0 1 -9 -9 0 1 0 DhKm-5 4914' 0" 9404' 48" Whitefish Bay 1 0 1 0 1 0 1 DhKm-5 4914' 0" 9404' 48" Whitefish Bay 1 0 1 0 0 1 0 DhKm-5 49 14' 0" 9404' 48" Whitefish Bay 1 0 1 0 0 0 0 DhKm-5 49 14' 0" 9404' 48" Whitefish Bay 1 0 1 1 0 0 0 DhKm-5 4914' 0" 9404' 48" 'X'hitefish Bay 1 0 1 0 0 0 0 DhKn-l 49 12' 12" 9416' 0" nr Obabikon Bay 1 0 0 1 0 0 0 DhKn-l 4912' 12" 9416' 0" nr Obabikon Bay 1 0 1 0 0 0 0 DhKo-l 49 12' 06" 9429' 36" Painted Rock Channel 0 0 0 1 0 1 0 DhKo-l 49 12' 06" 9429' 36" Painted Rock Channel 0 0 0 1 1 0 1 DhKo-l 4912' 06" 9429' 36" Painted Rock Channel 0 0 1 0 0 0 0 DhKo-l 49 12' 06" 9429' 36" Painted Rock Channel 1 0 1 0 1 0 1 DiKm-3 4922' 42" 9407' 36" Whitefish Bay 1 0 0 1 1 0 1 DiKm-3 4922' 42" 9407' 36" 'X'hitefish Bay 0 1 0 0 0 0 0 DiKp-l 4928' 24" 9430' 24" Sunset Channel 1 0 1 0 1 0 1 DjKn-l 4940' 03" 9414' 36" Blindfold Lake 1 0 0 1 0 1 0 DjKn-l 4940' 03" 9414' 36" Blindfold Lake 1 0 1 0 1 0 1 DjKn-l 4940' 03" 9414' 36" Blindfold Lake 1 0 0 1 0 1 0

,

----- --------- ----

2 backlegs 1 front leg 2 front legs centre of head centre body tail horns/ears ochre paint

0 1 0 1 1 1 1 1 0 1 0 1 1 1 1 1 1 1 0 1 0 1 1 1 0 0 1 1 1 1 1 0 0 1 0 1 1 1 1 1 1 0 1 1 1 1 0 1 0 1 0 1 1 0 1 1 1 0 1 1 1 0 0 1 0 0 0 1 1 1 1 1 0 0 0 1 1 1 1 1 0 0 0 1 1 1 1 1

Page 609

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0 0 0 1 1 0 1 1 0 0 0 1 1 0 1 1 1 0 1 1 1 0 1 1 0 1 0 1 1 1 0 1

0 0 0 1 0 0 1 1 0 1 0 0 0 1 1 1 0 1 0 1 1 1 1 1 0 0 0 1 1 1 1 1 0 1 0 1 1 1 1 1 1 0 1 1 1 1 1 1 0 1 0 0 1 1 0 1 1 0 1 1 1 1 1 1

Hierarchical cluster analysis conducted on this data led to the undertaking of two different correlation types. The Euclidean distance

analysis generated the first dendrogram. The second dendrogram used Pearson's correlation to establish correlations between sites and

'creature' shapes.

Page 610

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Hierarchical Cluster Analysis - Dendrogram using Average Linkage (Between Groups) using Euc1idean Distance Method Rescaled Distance Cluster Combine

CAS E 0 5 10 15 20 25 Label Num

DjKn-l 21

DjKn-1 23

DhKo-1 14

DhKn-1 12

DgKl-2 4

DhKm-5 8

DgKl-1 2

DiKm-3 18

DhKo-1 15

DhKm-3 5

DiKp-1 20

DgKl-1 1

DhKm-5 7

DhKo-1 17

DjKn-1 22

DhKm-5 10

DhKm-5 11

DhKm-5 9

DhKn-1 13

DhKo-1 16

DiKm-3 19

DgKl-17 3

DhKm-3 6

Page 611

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Hierarchical Cluster Analysis - Dendrogram using Average Linkage (Between Groups) using Pearson Correlation Method Rescaled Distance Cluster Combine

CAS E 0 5 10 15 20 25 Label Num

DjKn-l 21

DjKn-1 23 J DhKo-1 14

DhKn-1 12

DgKl-2 4

DhKm-5 8

DhKm-3 6

DiKm-3 19

DgK1-1 2

DiKm-3 18 J DhKo-1 15 f--

DhKm-3 5 -DiKp-1 20

DgK1-1 1 -DhKm-5 7

DhKo-1 17

DjKn-1 22 1

DhKm-5 10

DhKm-5 11

DhKm-5 9

DhKn-1 13

j r---

1 L DhKo-1 16

DgKl-17 3

Page 612

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) )

The dendrograms above, obtained using hierarchical cluster analysis and Euclidean distance and Pearson correlation, prove a weak

correlation between the sites and 'creatures.'

i) The 'stick figure':

The number '-9' indicates that a 'stick figure' faced up instead ofleft or right. (The table continues on the next page).

Borden 2 legs lleg can't see legs due 1

number Latitude Longitude Geographical Range vertical horizontal diagonal

down down to lichen, rock

tripe, exfoliation

DgKm-l 49 05' 39" 94 04' 51" Sabaskong Bay 1 0 0 1 0 0 DgKm-l 49 05' 39" 94 04' 51" Sabaskong Bay 1 0 0 0 1 0

,

DgKm-l 49 05' 39" 94 04' 51" Sabaskong Bay 1 0 0 1 0 0 DgKm-l 49 05' 39" 94 04' 51" Sabaskong Bay 1 0 0 1 0 0 DhKm-l 49 14' 54" 94 04'00" Whitefish Bay 1 0 0 1 0 0 DhKm-3 49 17' 42" 9403' 39" Whitefish Bay 1 0 0 1 0 0 DhKm-3 4917' 42" 9403' 39" Whitefish Bay 1 0 0 1 0 0 DhKm-3 4917' 42" 9403' 39" Whitefish Bay 1 0 0 1 0 0 DhKm-18 4914' 31" 9404' 33" Whitefish Bay 1 0 0 0 0 1 DhKm-18 4914' 31" 9404' 33" Whitefish Bay 1 0 0 0 0 1 DhKn-l 49 12' 12" 9416' 00" nr Obabikon Bay 1 0 0 1 0 0 DiKp-l 4928' 24" 9430' 24" Sunset Channel 1 0 0 1 0 0 DjKn-l 4940' 03" 9414' 36" Blindfold Lake 1 0 0 0 0 0 DjKn-l 4940' 03" 9414' 36" Blindfold Lake 1 0 0 1 0 0 DiKm-3 4922' 42" 947'36" Whitefish Bay 0 0 1 1 0 0 DiKm-3 4922' 42" 947'36" Whitefish Bay 0 0 1 1 0 0 DiKm-4 4920' 30" 9403' 51" Whitefish Bay 1 0 0 1 0 0 DhKo-l 4912' 06" 9429' 36" Painted Rock Channel 1 0 0 1 0 0 DhKo-l 4912' 06" 9429' 36" Painted Rock Channel 1 0 0 1 0 0 DhKo-l 49 12' 06" 9429' 36" Painted Rock Channel 1 0 0 1 0 0 DhKo-l 4912' 06" 9429' 36" Painted Rock Channel 1 0 0 1 0 0

Page 613

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') )

1 1 arm

both both larm upand no hollow solid stick solid hollow horns

Fingers ochre paint down

arm 1 arm

arms arms body body body head he ad arms

down or ears

up down

up

0 0 0 1 1 0 0 1 1 0 0 0 1 1 0 0 0 0 0 0 0 1 1 0 0 0 1 0 0 1 0 0 0 0 0 1 1 0 0 0 1 0 0 1 0 0 0 0 0 1 1 0 0 0 1 0 0 0 0 0 1 0 0 1 1 0 0 0 1

0 0 0 0 0 1 1 0 0 1 0 0 0 1

0 0 0 0 0 1 1 0 0 1 0 0 0 1

0 0 0 0 0 1 0 1 0 0 0 0 0 1

0 0 0 0 1 0 0 0 1 1 0 1 0 1 0 0 0 0 0 1 0 0 1 1 0 0 0 1

0 0 0 0 0 1 0 0 1 1 0 0 0 1 0 0 0 0 0 1 0 0 1 1 0 0 0 1

0 0 0 0 0 1 1 0 0 1 0 0 1 1

0 0 1 0 0 0 0 0 1 1 0 0 0 1

0 0 1 0 0 0 0 0 1 1 0 0 0 1

0 0 0 0 1 0 0 0 1 1 0 0 0 1 0 0 0 0 0 1 1 0 0 1 0 0 0 1 0 0 0 0 0 1 0 0 1 1 0 0 0 1

0 0 0 0 0 1 0 0 1 1 0 0 0 1

0 1 0 0 0 0 0 1 0 1 0 1 0 1

0 0 0 0 0 1 1 0 0 1 0 0 0 1

Examining through hierarchical cluster analysis both of the dendrograms below (Euclidean distance and Pearson correlation), demonstrates

only a weak correlation between the sites and the 'stick figure.'

Page 614

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Hierarchical Cluster Analysis - Dendrogram using Average Linkage (Between Groups) using Euclidean Distance Method Rescaled Distance Cluster Combine

CAS E o 5 10 15 20 25 Label Num +---------+---------+---------+---------+---------+

DiKm-4 17 -DhKo-l 21 -DhKm-3 6

DhKm-3 7 -DjKn-1 13

DgKm-1 4 -DjKn-1 14

DgKm-1 3 - -DhKo-1 18 - r---DhKo-1 19 -DhKm-1 5

DhKn-1 11 - 1--

DiKp-1 12 -DgKm-1 1

DhKm-18 10

DhKm-3 8 '-----

DiKm-3 15

DiKm-3 16 ~ DgKm-1 2

DhKm-18 9

DhKo-1 20

Page 615

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Hierarchical Cluster Analysis - Dendrogram using Average Linkage (Between Groups) using the Pearson Correlation Method Resca1ed Distance C1uster Combine

CAS E o 5 10 15 20 25 Label Num

DiKm-4 17 -

DhKo-l 21 -DhKm-3 6

DhKm-3 7 -DjKn-1 13

DhKo-1 18 -DhKo-1 19 -DhKm-1 5

DhKn-1 11 -DiKp-1 12 - - r---DgKm-1 1

DhKm-18 10

DhKm-3 8

DgKm-1 4 -DjKn-1 14

DgKm-1 3 - -DiKm-3 15

DiKm-3 16

DgKm-1 2

DhKm-18 9 1

DhKo-1 20

Page 616

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'1 / ')

j) The 'smear':

The number '-9' indicates that exfoliation, white mineraI deposits, lichen or rock tripe encroachment made it impossible to establish

whether the shape was either hollow or solid.

Borden Latitude Longitude Geographical Range centre of shape red ochre number

DgKl-2 49 06'48" 93 57' 18" Sabaskong Bay -9 1

D~Kl-17 49 05'48" 93 58' 12" Sabaskong Bay -9 1

D~Kl-17 49 05'48" 93 58' 12" Sabaskong Bay -9 1

DgKl-19 49 OS' 54" 93 58' 00" Sabaskong Bay 1 1

DgKm-l 49 OS' 39" 94 04' 51" Sabaskong Bay 1 1 DhKm-l 4914' 54" 94 04' 00" Whitefish Bay -9 1

DhKm-l 4914' 54" 94 04' 00" Whitefish Bay -9 1

DhKm-5 4914' 0" 94 04' 48" Whitefish Bay -9 1

DhKn-l 49 12' 12" 9416' 0" nr Obabikon Bay 1 1

DhKn-l 4912' 12" 9416' 0" nr Obabikon Bay -9 1 DiKn-l 4925' 18" 9413' 06" Whitefish Bay -9 1

DiKm-3 4922' 42" 9407' 36" Whitefish Bay -9 1

DiKm-3 4922' 42" 9407' 36" Whitefish Bay -9 1

DhKo-l 4912' 06" 9429' 36" Painted Rock Channel -9 1 DhKo-l 4912' 06" 9429' 36" Painted Rock Channel -9 1

DgKm-2 49 06'06" 9404' 24" Sabaskong Bay 1 1 !

D~Km-2 49 06'06" 9404' 24" Sabaskong Bay 1 1 DiKm-50 4921'12" 9407' 36" Whitefish Bay 1 1

.

Both of the following dendrograms using hierarchical cluster analysis (Euclidean distance and Pearson correlation) reveal a weak correlation

between the sites and the shape loosely categorised as a 'smear.'

Page 617

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'î / ')

Hierarchical Cluster Analysis - Dendrogram using Average Linkage (Between Groups) using Euc1idean Distance Method Rescaled Distance Cluster Combine

CAS E 0 5 10 15 20 25 Label Num

DgKm-2 18

DiKm-50 19

DgKl-19 5

DhKn-1 10

DgKm-2 17

DgKm-1 6

DhKo-1 15

DhKo-1 16

DgKl-2 2

DiKm-3 13

DiKm-3 14

DhKn-1 11

DiKn-1 12

DhKm-1 8

DhKm-5 9

DgKl-17 4

DhKm-1 7

DgKl-17 3

Page 618

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Hierarchical Cluster Analysis - Dendrogram using Average Linkage (Between Groups) using the Pearson Correlation Method

Label

DhKo-1

DhKo-1

DgKl-2

DiKm-3

DiKm-3

DgKl-17

DhKm-1

DhKn-1

DiKn-1

DgKl-17

DhKm-1

DhKm-5

DgKm-2

DiKm-50

DgKm-2

DhKn-1

DgKl-19

DgKm-1

CAS E

Rescaled Distance Cluster Combine

o 5 10 15 20 Num +---------+---------+

15

16

2

13

14

4

7

11

12

3

8

9

18

19

17

10

5

6

-

Page 619

25

Page 646: An obsession with meaning: a critical examination of the pictograph sites of the Lake of Woods

î ')

k) The 'blob':

The number '-9' used in the "centre of shape" field indicates that exfoliation, white mineraI deposits, lichen or rock tripe

encroachment rendered it impossible to establish whether or not the shape was solid. There are seventy-three different types of 'blobs'

(xq349) as weil as a number of radicaily different blobs which only occur once. (The table continues on the two pages.)

Borden Latitude Longitude

Geographical centre of oval vertical horizontal

rectangular round

red number Range shape joblong ochre

DgKl-2 49 06' 48" 93 57' 18" Sabaskong Bay 1 0 0 0 0 0 0

DgKl-19 4905' 54" 93 58' 00" Sabaskong Bay -9 0 0 0 0 0 1

DgKm-l 49 05' 39" 94 04' 51" Sabaskong Bay -9 1 0 0 0 0 1

DhKm-l 4914' 54" 94 04'00" Whitefish Bay 1 -9 0 0 0 0 1

DhKm-l 4914' 54" 94 04'00" Whitefish Bay 1 -9 0 0 0 0 1

DhKm-3 4917' 42" 9403' 39" Whitefish Bay 1 -9 0 0 0 0 1

DhKm-3 4917' 42" 9403' 39" Whitefish Bay 0 0 0 0 0 0 1

DhKm-3 4917' 42" 9403' 39" \'V'hitefish Bay 1 1 0 0 0 0 1

DhKm-3 4917' 42" 9403' 39" Whitefish Bay 1 0 0 0 1 0 1

DhKm-3 4917' 42" 9403' 39" Whitefish Bay 1 0 0 0 0 0 1 1

DhKm-3 4917' 42" 9403' 39" Whitefish Bay 1 0 0 0 0 1 1

DhKm-3 4917' 42" 9403' 39" Whitefish Bay 1 1 0 0 0 0 1

DhKm-3 4917' 42" 9403' 39" Whitefish Bay 1 0 0 0 0 1 1

DhKm-3 4917' 42" 9403' 39" Whitefish Bay -9 0 0 0 0 0 1

DhKm-5 4914' 0" 9404' 48" Whitefish Bay 1 1 0 0 0 0 1 , ,

DhKm-5 49 14' 0" 9404' 48" \'V'hitefish Bay -9 1 0 0 0 0 1

DhKm-5 4914' 0" 9404' 48" Whitefish Bay -9 1 0 0 0 0 1 1

DhKm-5 49 14' 0" 9404' 48" Whitefish Bay -9 1 0 0 0 0 1

DhKm-5 49 14' 0" 9404' 48" Whitefish Bay -9 1 0 0 0 0 1

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DhKm-5 4914' 0" 9404' 48" Whitefish Bay -9 1 0 0 0 0 1

DhKm-5 4914' 0" 9404' 48" Whitefish Bay -9 1 0 0 0 0 1

DhKm-5 4914' 0" 9404' 48" Whitefish Bay -9 1 0 0 0 0 1

DhKm-5 4914' 0" 94 04' 48" Whitefish Bay 1 1 0 0 0 0 1

DhKm-5 4914' 0" 9404' 48" ~'hitefish Bay -9 0 0 0 0 1 1

DhKm-18 4914'31" 9404' 33" ~'hitefish Bay -9 1 0 0 0 0 1

DhKn-1 49 12' 12" 9416' 0" nr Obabikon Bay -9 0 0 1 0 0 1

DhKn-l 4912' 12" 9416' 0" nr Obabikon Bay 1 0 0 0 0 1 1

DiKn-l 4925' 18" 9413' 06" ~tefish Bay 1 0 0 0 0 0 1

DiKn-l 4925' 18" 9413' 06" Whitefish Bay -9 0 0 0 0 0 1

DiKn-l 4925' 18" 9413' 06" Whitefish Ba~ 1 0 0 0 0 0 1 ,

.

DiKn-l 4925' 18" 9413' 06" Whitefish Bay -9 0 0 0 0 0 1

DiKn-l 4925' 18" 9413' 06" Whitefish Bay 1 0 0 0 1 0 1 1

DiKn-l 4925' 18" 9413' 06" Whitefish Bay 1 0 0 0 0 0 1

DiKn-1 4925' 18" 9413' 06" Whitefish Bay 1 0 0 0 0 0 1

DiKn-l 4925' 18" 9413' 06" Whitefish Bay 1 0 1 0 0 0 1

DiKp-l 4928' 24" 9430' 24" Sunset Channel 1 0 0 0 1 0 1

DiKp-l 4928' 24" 9430' 24" Sunset Channel 1 0 0 0 1 0 1

DiKp-l 4928' 24" 9430' 24" Sunset Channel 1 0 0 0 0 1 1

DiKp-l 4928' 24" 9430' 24" Sunset Channel 1 0 0 0 0 1 1

DiKp-l 4928' 24" 9430' 24" Sunset Channel 1 0 0 0 0 1 1

DkKn-6 4939' 45" 9417' 09" Blindfold Lake 1 1 0 0 0 0 1 .

DkKn-6 4939' 45" 9417'09" Blindfold Lake -9 0 0 0 0 0 1

DkKn-6 4939' 45" 9417' 09" Blindfold Lake -9 0 0 0 0 0 1

DkKn-6 4939' 45" 9417' 09" Blindfold Lake -9 0 0 0 0 0 1

DkKn-7 4939' 45" 9417' 09" Blindfold Lake 1 0 0 0 1 0 1

DjKn-1 4940' 03" 9414' 36" Blindfold Lake 1 0 0 0 0 0 1

DjKn-l 4940' 03" 9414' 36" Blindfold Lake -9 0 0 0 0 0 1 ---

Page 621

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') î

DjKn-1 4940' 03" 9414' 36" Blindfold Lake -9 0 0 0 0 0 1

DjKn-1 4940' 03" 9414' 36" Blindfold Lake 1 0 0 0 0 0 1

DjKn-1 4940' 03" 9414' 36" Blindfold Lake -9 0 0 0 1 0 1

DjKn-1 4940' 03" 9414' 36" Blindfold Lake 1 0 0 0 0 1 1

DjKn-1 4940' 03" 9414' 36" Blindfold Lake 1 0 0 0 0 0 1

DiKm-3 4922' 42" 9407' 36" Whitefish Bay -9 0 0 0 0 0 1

DiKm-3 4922' 42" 9407' 36" Whitefish Bay 1 0 0 0 0 0 1

DiKm-3 4922' 42" 9407' 36" Whitefish Bay -9 0 0 0 0 0 1

DiKm-3 4922' 42" 9407' 36" Whitefish Bay -9 0 0 0 0 0 1

DiKm-3 4922' 42" 9407' 36" Whitefish Bay -9 0 0 0 0 0 1

DiKm-3 4922' 42" 9407' 36" Whitefish Bay 1 1 0 0 0 0 1 Painted Rock

DhKo-1 4912' 06" 9429' 36" Channel 1 0 0 0 0 0 1 Painted Rock

DhKo-1 4912' 06" 9429' 36" Channel 1 0 0 0 0 0 1

DjKr-23 4930' 54" 9451' 54" Portage Bay 1 1 0 0 0 0 1

DjKr-23 4930' 54" 9451' 54" Portage Bay -9 1 0 0 0 0 1

DiKq:-10 4929' 51" 9448' 54" BishopBay 1 0 0 0 0 0 1

DiKq-10 4929' 51" 9448' 54" Bishop Bay 1 0 0 0 0 1 1

DiKq-10 4929' 51" 9448' 54" Bishop Bay 1 0 0 0 0 1 1

DiKq-10 4929' 51" 9448' 54" Bishop Bay 1 0 0 0 0 1 1

DiKq-10 4929' 51" 9448' 54" Bishop Bay 1 0 0 0 0 1 1

DiKq-10 4929' 51" 9448' 54" BishopBay 1 0 0 0 0 1 1

DiKq-10 4929' 51" 9448' 54" Bishop Bay 1 0 0 0 0 1 1

DgKm-2 49 06' 06" 9404' 24" Sabaskong Bay 1 0 0 0 0 0 1

DgKm-2 49 06' 06" 9404' 24" Sabaskong Bay 1 1 0 0 0 0 1

DgKm-2 49 06' 06" 9404' 24" Sabaskong Bay 1 0 0 0 0 1 1

DgKm-2 49 06' 06" 9404' 24" Sabaskong Bay 1 0 0 0 0 0 1

Page 622

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~

Sorne exceptional types of blob cannot be placed in this spreadsheet:

1) DgKl-1 - severallarge blobs alongside each other and connected, impossible to establish centre because of white mineraI deposits/red

ochre

2) DgKl-2 - four small blobs alongside each other, solid centres/very strong ochre

3) DhKm-1 - horizontal oval blob with two short verticallines sticking up on top right hand side, solid centre but pale/red ochre

4) DhKm-3 - small round blob which has a curve in it and points downwards, solid centre/red ochre

5) DhKm-5 - group of blobs of different sizes, touching each other, possibly solid centres but this is difficult to establish because of white

mineraI deposit/ pale red ochre

6) DhKn-1 - round blob which has short lines sticking out on either side, possibly solid but difficult to establish this because of white

mineraI deposits/ red ochre

7) DhKo-1 - spikey blob with seven lines sticking out, solid centre /red ochre

8) DiKn-1 - collection of blobs squashed next to each other, impossible to establish centre because of severe lichen growth/ strong red

ochre

9) DjI<r-23 - small round blobs one immediately above the other, possibly solid centre but difficult to determine because image badly

exfoliated and unclear/red ochre

Since 'blobs' had the large st number of types, it was examined using SPSS. The first dendrogram below, (on the next page) (i), used

the Euclidean distance and demonstrates a weak link between the sites and this shape. The second dendrogram, (turn over the page at the

end of dendrogram i) (ii), obtained using the Pearson correlation, confirms this observation. However, it remains important to remember

that blobs are the decayed remains of shapes that once had clearly defined edges.

Page 623

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'~ ')

(i) Hierarchical Cluster Analysis - Dendrogram using Average Linkage (Between Groups) using Euc1idean Distance Method Rescaled Distance Cluster Combine

CAS E 0 5 10 15 20 25 Label Num +---------+---------+---------+---------+---------+

DgKm-2 70

DgKm-2 73

DhKm-3 10

DhKo-l 60

DiKq-10 63

DiKm-3 54

DhKo-1 59

DjKn-l 49

DjKn-l 52

DiKn-1 34

DjKn-l 46

DiKn-1 30

DiKn-l 33

DiKn-1 28

DiKn-1 35

DiKq-10 69

DgKm-2 72

DhKm-3 11

DiKq-10 67

DiKq-10 68

DiKq-10 65

DiKq-10 66

DjKn-l 51

DiKq-10 64

Page 624

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DiKp-1 39 -

DiKp-1 40 -DhKn-1 27

DiKp-1 38 -

DhKm-3 13 -DgKl-2 1

DjKr-23 61 -DgKm-2 71 -DhKm-3 8 -DkKn-6 41 -DiKm-3 58 -DhKm-5 15

DhKm-5 23 -DhKm-3 12 -DhKm-3 7

DiKp-1 37 -DkKn-7 45 -DhKm-3 9 r---

DiKn-1 32 -DiKp-1 36 -DhKm-1 5 -DhKm-3 6

DhKm-1 4 -DhKm-18 25

DjKr-23 62

DgKm-1 3

DhKm-5 21

DhKm-5 22

Page 625

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î

DhKm-5 19

DhKm-5 20

DhKm-5 17

DhKm-5 18

DhKm-5 16

DiKm-3 56

DiKm-3 57

DgKl-19 2

DiKm-3 53

DiKm-3 55

DjKn-1 47

DjKn-1 48

DkKn-6 43

DkKn-6 44

DiKn-1 31

DkKn-6 42

DhKm-3 14

DiKn-1 29

DjKn-1 50

DhKn-1 26

DhKm-5 24

Page 626

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(ii) Hierarchical Cluster Analysis - Dendrogram using Average Linkage (Between Groups) using Pearson Correlation Method Rescaled Distance Cluster Combine

CAS E 0 5 10 15 20 25 Label Num

DjKr-23 61

DgKm-2 71

DhKm-3 8

DkKn-6 41

DiKm-3 58

DhKm-5 23

DhKm-5 15

DhKm-3 12

DiKp-1 37

DkKn-7 45

DhKm-3 9

DiKn-1 32

DiKp-1 36

DiKq-10 69

DgKm-2 72

DhKm-3 11

DiKq-10 67

DiKq-10 68

DiKq-10 65

DiKq-10 66

DjKn-1 51

DiKq-10 64

DiKp-1 39

DiKp-1 40

Page 627

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'j -)

DhKn-1 27

DiKp-1 38

DhKm-3 13

DgKm-2 70

DgKm-2 73

DhKm-3 10

DhKo-1 60

DiKq-10 63

DiKm-3 54

DhKo-1 59

DjKn-1 49

DjKn-1 52

DiKn-1 34

DjKn-1 46

DiKn-1 30

DiKn-1 33

DiKn-1 28

DiKn-1 35

DgKl-2 1

DhKm-3 7

DhKm-1 5

DhKm-3 6

DhKm-1 4

DhKm-18 25

DjKr-23 62

DgKm-1 3

DhKm-5 21

DhKm-5 22

Page 628

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DhKm-5 19

DhKm-5 20

DhKm-5 17

DhKm-5 18

DhKm-5 16

DiKm-3 56

DiKm-3 57

DgKl-19 2

DiKm-3 53

DiKm-3 55

DjKn-1 48

DjKn-1 47

DkKn-6 44

DkKn-6 43

DkKn-6 42

DiKn-1 31

DiKn-1 29

DhKm-3 14

DjKn-1 50

DhKn-1 26

DhKm-5 24

Page 629

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'î ')

m) Possible re1ationship between sites, various physical features, and groups which have large quantities of shapes.

This table contains the information required to establish a possible connection between a site, the five required physical features,

and the shapes which occur in large numbers: 'creatures,' 'zigzags,' 'crescents,' 'blobs,' 'smears,' 'parallellines,' birds,' 'turtles,' 'hand print,'

and 'three horizontallines.' An '-9' indicates cave sites without cliffs.

Site Latitude Longitude Geographical Type of

Overhang Shelves Cracks Crevices Roles Rocks at

Range Site Base

DgK1-1 49 09' 15" 94 56' 32" Sabaskong Bay 1 1 1 0 0 0 0 DgK1-2 49 06'48" 93 57' 18" SabaskonKBay 1 1 1 1 1 1 1 DgK1-17 49 05' 48" 93 58' 12" Sabaskong Bay 1 1 1 1 1 0 0 DgK1-19 49 05' 54" 93 58' 00" Sabaskong Bay 1 1 1 1 1 0 1 DgKm-l 49 05' 39" 94 04' 51" Sabaskong Bay 1 1 0 1 1 0 1 .

DhKm-l 4914' 54" 94 04' 00" Whitefish Bay 1 1 1 1 1 0 0 1

DhKm-3 4917' 42" 9403' 39" Whitefish Bay 1 1 1 1 1 0 1 DhKm-4 49 14' 30" 9404' 00" Whitefish Bay 1 0 1 1 0 0 0 DhKm-5 49 14' 0" 9404' 48" Whitefish Bay 1 1 1 1 1 0 1 1

DhKm-18 4914' 31" 9404' 33" Whitefish Bay 1 1 1 1 1 0 1 DhKn-l 4912' 12" 9416'0" nr Obabikon Bay 1 1 1 1 1 0 1 DiKn-l 4925' 18" 9413' 06" Whitefish Bay 1 0 1 1 1 0 1

DiKp-l 4928' 24" 9430' 24" Sunset Channel 1 1 0 1 1 0 1 DkKn-6 4939' 45" 9417' 09" Blindfold Lake 1 1 1 1 0 1 1 DkKn-7 4939' 45" 94 17' 09" Blindfold Lake 1 0 1 1 1 0 1 DjKn-l 4940' 03" 9414' 36" Blindfold Lake 1 0 1 1 1 0 1 DiKm-3 4922' 42" 947'36" Whitefish Bay 1 1 0 1 0 0 1 DiKm-4 4920' 30" 9403' 51" Whitefish Bay 1 0 0 1 1 0 1

Painted Rock DhKo-l 4912' 06" 9429' 36" Channel 1 0 1 1 1 0 0 DjKr-23 4930' 54" 9451' 54" Portage Bay 1 0 1 1 1 0 1 DiKm-51 4921'12" 9407' 36" Whitefish Bay 1 0 1 1 1 0 1 DiKq-l0 4929' 51" 9448' 54" Bishop Bay 1 0 0 1 0 0 0

DhKm-19 4910' 57" 9408' 03" Turtle Lake 1 0 1 0 1 0 0 DhKm-20 49 14' 30" 944' 12" Whitefish Bay 1 1 0 1 0 0 1 DgKm-2 49 06'06" 9404' 24" Sabaskong Bay 1 1 1 1 1 0 0

- --

Page 630

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9407' 36" Whitefish Bay -9 -9 9407' 36" Whitefish Bay -9 -9

(Table continued below because of the large number of attributes)

Hand ParaUel Group of Three

Zig-Zag Creature Print Smear Blob

Lines Bird Turtle Horizontal Cres cent

Lines

0 1 0 0 0 1 0 0 0 1 0 1 0 1 1 0 0 0 0 1 0 1 0 1 0 0 0 0 1 0 0 0 1 1 1 0 0 0 0 0 0 0 0 1 1 0 0 0 0 0 0 0 0 1 1 0 0 0 0 0 1 1 1 0 1 0 1 1 1 0 0 0 0 0 0 1 0 0 0 0 0 1 1 1 1 0 0 0 0 1 0 0 0 0 1 0 1 0 0 0 0 1 0 1 1 0 0 1 0 0 0 0 0 1 1 0 0 0 0 1 1 1 0 0 1 0 0 0 0 0 0 0 0 0 1 0 0 0 0 0 0 0 0 0 1 0 0 0 0 0 0 1 1 0 1 1 0 0 0 1 1 1 1 1 1 1 0 0 0 0 1 0 0 0 0 0 0 0 0 0

0 1 0 1 1 0 0 0 0 0 0 0 0 0 1 0 0 0 0 0 0 0 0 0 0 0 0 0 0 1 0 0 0 0 1 0 0 0 0 0 0 0 0 0 0 0 0 1 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 1 1 0 0 0 0 0 0 0 0 1 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0

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) î /

The following dendrograms were obtained through hierarchical cluster analysis of this data. The dendrograms below, (on the next few

pages) labelled (i) and (ii), confirm a very weak correlation and perhaps differ insignificantly from randomness between the site, various

physical attributes at each site, and the shapes that occur in large numbers: 'creatures,' 'zigzags,' 'crescents,' 'blobs,' 'smears,' 'parallellines,'

birds,' 'turtles,' 'hand print,' and 'group of three horizontallines.'

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.'j ) ')

Hierarchical Cluster Analysis - Dendrogram using Average Linkage (Between Groups) using Euclidean Distance Method

CAS E Label Num

6

25

19

5

4

9

2

11

12

21

15

20

10

14

3

13

18

22

24

8

16

23

17

1

7

o 5 10

J

J

.. -

Rescaled Distance Cluster Combine 15 20 25

1 -

1

1

~ l-

I--

-

1-.. -

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'\ 'î

Hierarchical Cluster Analysis - Dendrogram using Average Linkage (Between Groups) using Pearson Correlation Method Resca1ed Distance Cluster Combine

CAS E o 5 10 15 20 25 Label Num DiKq-10 22

DgKm-2 25

DgKl-19 4

DgKm-1 5

DhKm-19 23

DgKl-17 3

DjKr-23 20

DgKl-1 1

DgKl-2 2

DkKn-6 14

DkKn-7 15

DhKm-4 8

DhKm-18 10

DiKm-3 17

DiKm-51 21

DiKp-1 13

DhKm-1 6

DhKm-5 9

DiKn-1 12

DiKm-4 18

DhKo-1 19

DiKm-50 26

DiKm-49 27 J DhKn-1 11

DhKm-3 7

DhKm-20 24

DjKn-1 16

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'\ ;

'~ /

Appendix 17: The "Presence and Absence" Tables for the Images of the Birch Bark Scrolls.

The smail number of results for each of the largest types of shape precludes any statistical analysis from being conducted using

SPSS. For each of these tables a "1" indicated the presence of a feature while a "0" indicated its absence. This is because there is not a

sufficient quantity of data on which to perform cluster analysis. However, the table below indicates that the 'creature' which occurred only

on birch bark scrail number 1, were not exactly the same.

The table below for indicates that the 'bird' shapes on birch bark scrails were not exactly the same and that they occurred only on birch

bark scrail number 1.

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) )

The table below presents the information on the shape called 'two parallel verticallines', which only occurs on birch bark scroll1.

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~ .. !

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