Journalof Radioanalyticalandl{uclearChemistry, I.'o1.211, iVo.3 (2000) 559 566 On the transition from tin-rich to antimony-rich Europeanwhite soda-glass trade beads for the Senecas of Northeastern North America M. L. Sempowski,l A. W. Nohe,l J.-F.Moreau,2 I. Kenyon,3 K. Karklins,4 S. Aufreiter,S R. G. v. Hancock5.6 I llochester ll'[useum & ScienceCenter, Rochester, Jrlev l'ork 14603, USA :Depurtnen|de.ssctenc'e'shttmaine.set|aboratoired'archdologie,(JniversitddtQuebecdChicotttimt,Chicou|imi.oudbec',CrlnQr1(],(;71|2l 3 Ontario Heritage Foundation, Toronto, Ontario, Canada, M5C IJ3 a Parks Cqnada, Onlario Service Cenlre, Ottau,a, Ontario, Canada, KtA 0Nl5 5 .St.tltf'pOXl: Reactor Facilrq, ancl Department of Chentical Engineering and Applied Chemistrt,, LJniversih,of 'l'orctnto, 'l-oronlo, Ontario, Canqda. M5S 3E5 6SI't)tt.P()K|.'-)|:ttt't|t|.l'ttttt!I)epur|t (RcccivcdNovember 22, 1999) ltltasbcenshtlrrtrthatscvcralrrtodiljcatiorrsoccurrcd,overtIrespanofthel7thtol9thcenturies.intheagcntsuscdtoopacilil:-iurtlpcan-tnac rvhitc sttda-glitss beadsthat vv'ere transmitted as trade goods to northeastern North Amerrca.l-rn was used at thc beginnrngof thc lTth cclttun fbllorved bi'Sb latcr in thc century. and then by As during the 18th and l9th centuries. In an attempt to dellne more closelythe transitionliorn Srr- rich to Sb-rrchr.r'hite bcads.lvc analyzed 198 white glass beadsliom a number o1'archaeological sites in ruvestern New York State Chcrnrcal analr"sis sltousthat thc arrivalol'Sb-rvhite soda-glass trade beads began in this regionduringthe periodfionr approximately A l) 1625-16-10. ancl that tho haclcornplctclv rcplaccd Sn-rvhite beads by A.D. 1675. Specific beadchemistries link a number of'the archaeolos.ical sites. Introduction -fypological classifications of European glass trade beads of many different shapes, colours, and decorations. recovered I}om North American archaeological sites,have been of great imporlance to archaeologists. KIoo and KIDD's 1970 classification sche'nre.l expanded by KnnrltNs.2 has become the standard fbr easternNorth America.3 While specific rnulti-coloLrred glass bead typeshaveproven to be useful tirne-rnarkers fbr the datingof archaeological sites of the European contact era in noftheastern North America, single-coloured glasstrade beads, commonly found on thesesites,have proven more difficult to date on the basis of appearance alone. Chernical analvses of turquoise blue beads, however, have greatll'refined their use as chronological markers by indicatingchangesin chemical compositionover time.a 7 Prelirninary elemental analyses of white glass trade beads recovered from archaeological sites in southern Ontario, Canada suggest similarpotential. They demonstrate that early l Tth centurySn-rich drawn glass beads werereplaced sonletime late in that century by Sb- rich glass beads. rvhichcontinued to be produced into the l9th centur),. Arsenic-rich glass beads appeared by the late l8th cc-ntury and were in use into the 2Oth centur.v''. arrd Ir-rich rvhite glass beads were madeduring the latc lgth andearl\, ?Oth centuries.8 [Jnfbrtunately. while we have identified the general terlporal parameters for the Sn-white to Sb-white glass bead transition, it was impossible to provide more precise dates because of the annihilation and dispersal o1' much of the nativepopulation frorn southern Ontarioby the rniddleof the 17th century. Therefore, in an attempr to document the transition more closely,198 white glass beads from two parallel series of Seneca Iroquois sites in western New York State (see Fig. l) were analyzed. Archaeological context of the beadsamples The bead samples derived ftoni fifteen Seneca Iroquois siteswhich were occupied frorn the late l6th throughthe early l Sth centuries in western New York (seeFig. l). Duringthis period, therewere two distinct groupsof Seneca, each occupying a separate village in close proximity to the other, plus one or more srnall associated villages. Like other northern lroquoian people,the Seneca abandoned their villages and moved approximately every l5 to 20 years. usually to a new site only a few rniles away. The result is two parallel sequences of village sites - an eastern and a western series. The Seneca were the first Iroquoian group whose sequential moyements during the peri0d irnrnediately following E,uropean contact were traced archaeologically,g-12 and these early formulations have undergone only slight rnodifications since thattime.li I5 Furthennore, the unusual continuitl, o1'thesequence of- Seneca sitesfor the early historic period has rnadeit a benchmarkfor cornparative studies of archaeological assemblases from other areas. 0)i6 573I :000{;st)17 00 (' .'(J00 . lkutle m iut Kioclo. Budupest ,1 kudt miai K tudo. l) udupe st K|uver .lcadentit PubIi.shers, Dordrec ht
8
Embed
On the transition from tin-rich to antimony-rich European white soda-glass trade beads in northeastern North America
This document is posted to help you gain knowledge. Please leave a comment to let me know what you think about it! Share it to your friends and learn new things together.
Transcript
Journalof Radioanalyticalandl{uclearChemistry, I. 'o1.211, iVo.3 (2000) 559 566
On the transition from tin-rich to antimony-rich European white soda-glasstrade beads for the Senecas of Northeastern North America
M. L. Sempowski , l A. W. Nohe, l J.-F. Moreau,2 I . Kenyon,3 K. Karkl ins,4 S. Aufrei ter ,S R. G. v. Hancock5.6I llochester ll'[useum & Science Center, Rochester, Jrlev l'ork 14603, USA
:Depurtnen|de.ssctenc'e 'sht tmaine.set |aboratoi red'archdologie,(Jnivers i tddtQuebecdChicot t t imt,Chicou| imi .oudbec' ,Cr lnQr1(] , ( ;71|2l
3 Ontario Heritage Foundation, Toronto, Ontario, Canada, M5C IJ3a Parks Cqnada, Onlario Service Cenlre, Ottau,a, Ontario, Canada, KtA 0Nl5
5 .St.tltf'pOXl: Reactor Facilrq, ancl Department of Chentical Engineering and Applied Chemistrt,, LJniversih,of 'l'orctnto,
'l-oronlo, Ontario, Canqda. M5S 3E5
6SI ' t ) t t .P()K| . ' - ) | : t t t ' t | t | . l ' t t t t t ! I )epur| t
(Rcccivcd November 22, 1999)
l t l t a s b c e n s h t l r r t r t h a t s c v c r a l r r t o d i l j c a t i o r r s o c c u r r c d , o v e r t I r e s p a n o f t h e l 7 t h t o l 9 t h c e n t u r i e s . i n t h e a g c n t s u s c d t o o p a c i l i l : - i u r t l p c a n - t n a c
rvhitc sttda-glitss beads that vv'ere transmitted as trade goods to northeastern North Amerrca. l-rn was used at thc beginnrng of thc lTth cclttun
fbllorved bi'Sb latcr in thc century. and then by As during the 18th and l9th centuries. In an attempt to dellne more closely the transition liorn Srr-
rich to Sb-rrch r.r'hite bcads. lvc analyzed 198 white glass beads liom a number o1'archaeological sites in ruvestern New York State Chcrnrcal
analr"s is s l tous that thc arr ival o l 'Sb-rvhi te soda-glass t rade beads began in th is region dur ing the per iod f ionr approximately A l ) 1625-16-10. ancl
that tho haclcornplctc lv rcplaccd Sn-rvhi te beads by A.D. 1675. Speci f ic bead chemistr ies l ink a number of ' the archaeolos. ical s i tes.
Introduct ion
-fypological classifications of European glass trade
beads of many different shapes, colours, and
decorations. recovered I}om North American
archaeological sites, have been of great imporlance to
archaeologists. KIoo and KIDD's 1970 classi f icat ion
sche'nre. l expanded by Knnr l tNs.2 has become the
standard fbr eastern North America.3 While specific
rnulti-coloLrred glass bead types have proven to be useful
tirne-rnarkers fbr the dating of archaeological sites of the
European contact era in noftheastern North America,
single-coloured glass trade beads, commonly found on
these sites, have proven more diff icult to date on the
basis of appearance alone.
Chernical analvses of turquoise blue beads, however,
have greatl l ' refined their use as chronological markers
by indicating changes in chemical composition over
t ime.a 7 Prel i rn inary elemental analyses of whi te glass
trade beads recovered from archaeological sites in
southern Ontario, Canada suggest similar potential. They
demonstrate that early l Tth century Sn-rich drawn glass
beads were replaced sonletime late in that century by Sb-r ich glass beads. rvhich cont inued to be produced into
the l9th centur) , . Arsenic-r ich glass beads appeared by
the late l8th cc-ntury and were in use into the 2Oth
centur.v ' ' . arrd I r - r ich rvhi te glass beads were made dur ing
the latc lgth and ear l \ , ?Oth centur ies.8
[Jnfbrtunately. while we have identif ied the general
terlporal parameters for the Sn-white to Sb-white glass
bead transi t ion, i t was impossible to provide more
precise dates because of the annihi lat ion and dispersal o1'
much of the native population frorn southern Ontario by
the rniddle of the 17th century. Therefore, in an attempr
to document the transition more closely, 198 white glass
beads from two parallel series of Seneca Iroquois sites in
western New York State (see Fig. l) were analyzed.
Archaeological context of the bead samples
The bead samples derived ftoni f ifteen Seneca
Iroquois s i tes which were occupied frorn the late l6th
through the early l Sth centuries in western New York
(see Fig. l ) . Dur ing th is per iod, there were two dist inctgroups of Seneca, each occupying a separate vil lage in
close proximity to the other, plus one or more srnall
associated vi l lages. Like other northern l roquoian
people, the Seneca abandoned their villages and moved
approximately every l5 to 20 years. usually to a new site
only a few rniles away. The result is two parallel
sequences of vil lage sites - an eastern and a western
series. The Seneca were the first Iroquoian group whose
sequential moyements during the peri0d irnrnediatelyfollowing E,uropean contact were traced
archaeological ly,g-12 and these ear ly formulat ions have
undergone only s l ight rnodi f icat ions s ince that t ime. l i I5
Furthennore, the unusual cont inui t l , o1' the sequence of-
Seneca sites for the early historic period has rnade it a
benchmark for cornparative studies of archaeological
assemblases from other areas.
0 ) i 6 573 I : 000 { ; s t ) 17 00(' .'(J00 . lkutle m iut K ioclo. Budupest
,1 kudt m iai K tud o. l) udupe s t
K|uver .lcadentit PubIi.shers, Dordrec ht
M [- SF-MrcWSKI Ct AI.: ON THE TRANSII'ION FROM TIN-RICH'IO AN'IIMONY-RICI-I f:LIROPE,\N \\'Ht I'I1 SOI)A-GI-,\SS
scale
1 0 m i l e s
Hudson River
Lake Onlar io
BochesterL a k e E r i e
{{
II
Mohawk River
((iiIItt
//\ _ - _
((
Est i rnates of occupat ion dates fbr the indiv idual s i tes
in the two series are somewhat more problematic, but af'elv kcy historic events and changes in assemblages of
European ntanuf"actured goods have permitted
approximat ions of beginning and ending dates for eachpair of contenlporary sites. While furlher refinements are
rnevi table. the present sequence and chronology of
Seneca sites appears to be close to the mark, with errors
l ikely to be within 5 to l0 year margins. Dur ing theperiod under study' here, the Seneca were acquiring
lruropean-lltade glass beads, along with other types of
rlanulirctured goods. in trade or exchange either with
Iluropean rtrerchants, prirnarily the Dutch, or from other
conducted at rnost of the Seneca vil lage sites have, in
turrr. yielded good-sized glass bead samples, which arenor.r' housed and available for study at the RochesterMuscunr & Science Center. The white glass beadsselcctcd lterc are lrorn fifteen sites, representing sevenl-5- to 20-y 'car t i rne per iods.
tt
Exper imenta l
In two separate test ing phases conducted rn 199_5 and
1997, 198 white glass beads of varying r lanulacrure
(cored and uncored, drarvn and lvound), sizes, and
shapes were analyzed non-destructivelrr,, usinrl
instrumental neutron activation analysis at the Slowpoke
Reactor Facil ity of the [Jniversity of Toronto.l6 -l-hese
beads had to be neutron- i r radiated as l i t t le as possible in
order to minimize the bui ld-up of radioact iv i tv l iorn12256 (hal f - l i fe 2.75 days) and f iorn l2asb
thal{ ' - l i l -e 60.9
days) in the Sb-r ich beads. so that they could be returned
to t l ie Rochester Museunr & Science Center rv i th in a
reasonable amount of t ime.
Beads of mass 5- I 0 rng were first cleancd
ultrasonically, as required. They were stored individuall l,,
in 1.2 ml polyethylene vials, were i r radiated ser ia l ly tbr
f i ve minu tes a t a neut ron f lux o f 1 .0 .1012 n .cm l .s l .
Genesee A l b a n y
E ive l
N E W
l i t g I M a p o t ' N u t ' Y o r k S t a t c s h o w i n g t h e S e n e c a r c g i o n ( = n . l ) . 1 5 7 0 - 1 7 1 0 ) . K c 1 t o S e n e c a s i r e s . l A c l a r l s . l ( ' u l b c r t s o n . l l r a r n .J ( ' an re ron .5 l )u t ch I l o l l o rv .6 l ]ac to ry Ho l lo rv :7 Fug le . { J [ . i n ra ,9 War ren , 10 Corn ish . l l l ] os le r M i l l s . l r P t l re r I I pusc : I3 S tcc les
l ' l l v {enz is : l 5 Dann . l 6 Marsh : l 7 Roches te r . l unc t ion : l 8 Bough ton H i l l ; l g l l ea le :20 Sn l ,de r -McClu re
IIIrIrNN
_s60_s60
M I,. SF.N4I'O\\'SKI Ct AI.: ON THE TRANSI'TION FROM TIN-RICH TO ANI'IMON\'-RIC]H EUROPEAN WHII'F, SODA-GI,.\SS
[: ' ive to seven minutes after irradiation, the induced
radioactivity was counted for f ive minutes using a hyper-
pure germanium detector-based gamma-ray spectro-
meter. This produced analytical concentration data for
Co, Sn, Cu, Na. Al , Mn. Cl and Ca. The samples were
recounted for f ive to thirty-three minutes the next day to
measure the concentrations of the longer-l ived
radioisotopes of Na, As, Sb and K. The sodium
nleasurenlents were used to l ink both counts. Elemental
concentrations were calculated using the comparator
method. based on elemental standards. Beads of larger
masses were irradiated at suitably lower neutron fluxes
to make just enough radioactivity for reasonable
chern ica l ana lyses .
Resul ts and discussion
In v iew of the goal of def in ing the Sn-r ich to Sb-r ich
transition pcriod of white glass beads in western New
York Statc. throueh the non-destructive chernical
analysis of beads from fifteen archaeological sitesranging in time llom the late l6th century to rhe earl1,l Sth century, 188 drawn white soda-glass beads wereidentif ied from the sample collection. They represenr thefocus of this paper. The remaining l0 beads consisted o1-wound potash-glass beads (see below). Although rhenumbers of relevant beads are relatively small (188). it isclear that, as in Ontario, drawn white soda-glass beads
from western New York were opacified solely with Sn in
the late l6th and early lTth centuries, and were opacified
solely with Sb by the late l Tth century.
Table I shows that the Warren. Cornish and floslel
Mif fs s i tes (A.D. 1625-1640) exhibi t thc f . i rsr Sb-r ich
beads. I t a lso shows that the Dann and Marsh si tes (A.D.
1655-1615) y ie lded the las t o f the Sn- r ich beads.
Table ? summarizes the transition from Sn-rich to
Sb-r ich beads in temporal s l ices of approximately l5 ro20 years for both sequences of Seneca sites. Comparison
of the numbers of beads at the eastern and western
I 'able I . t. isting of East Seneca and West Seneca sites.
vvith a summary of the opacifiers used in the whitc glass beads fbund thercirr
Teble 2. Opacifier sumntary by period and by East and West Seneca subunits
West East Total sb, %Pcr iod SnSbSbSn
= 1 5 9 0 - 1 6 r 0
= 1 6 1 0 - 1 6 2 5
= 1 6 2 5 1 6 1 0
= I 610 165-j
=165_ j t675
= 1 6 7 0 - 1 6 8 7
= 1 6 9 0 - 1 7 1 0
'l-ruttsil iort
00
27
IIjj
I 3
00
00
00
00
II
BB
99
l 0
l 6
t8
88
55
t 5
55
22
00
00
2222
00
00
t 0
00
I 7
3 7
00
2 7
88
) z
1 6
1 0
t 5
00
00
00
00
1 1
88
26
17
l 5
15
00
00
t l
63
1 0 0
1 0 0
521 9
5 7
56r56r
46 44 3 5 6464 8 r 1 0 7
M. M. L. L. SEMPOWSKI SEMPOWSKI et et aI.: aI.: ON ON THE THE TRANSMON TRANSMON FROM FROM TIN-RICH TIN-RICH TO TO ANTMONY-RICH ANTMONY-RICH EUROPEAN EUROPEAN WHITE WHITE SODA-GLASSSODA-GLASS
Seneca sites during the "ffansition period" between A.D.
1625-1640 and A.D. 1655-1675 indicates only slight
differences between the two sequences, in terms of the
relative proportions of white beads opacified with Sn
and Sb, respectively. In the western sequence, we find 19
Sn-rich beads and 18 Sb-rich beads [Sn/Sb:1.1], while
the eastern series manifests 22 Sn-rich beads and 27
Sb-rich beads [Sn/Sb:0.8]. Furthermore, as indicated in
the last column of Table 2, the relative percentage of
white beads opacified with Sb (Sb-rich beads) increases
steadily at all sites, over the course of the transition
period.
Ll'est Seneca c onnections
The revised site sequence for the western Seneca
group has the'following order: Adams -+ Brisbane? -+
Dutch Hollow -+ Lima -+ Power House -> Dann -->
Rochester Junction -+ Snyder/McClure.l5 This sequence
is partially confirmed by chemically matching white
Sn-white or Sb-white glass beads (see Table 3).
The chemical profiles of 6 Sn-rich beads link Power
House with Dann, and those of 3 Sb-rich beads link
Dann with Snyder/McClure.
East Seneca c onnections
Similarly, the proposed site sequence for the East
Seneca people is: Tram -> Cameron + Factory Hollow-+ Warren -) Steele + Marsh -+ Boughton Hill.l5
Table 4 indicates that 11 Sn-white beads link Warren
with Steele, while a tenuous 2 Sb-white glass beads link
Marsh with Boughton Hill.
West and East Seneca connections
Early interactions (A.D. 1610-1625)between the twogroups of Seneca are also confirmed by a set of 12
chemically matching Sn-white glass beads from Dutch
Hollow (west) and Factory Hollow (east) (Table 5).
Similarly, later (A.D. 1655-1710) interactions may be
evidenced by 4 Sb-rich beads that appear to link Marsh(east; A.D. 1655-1675) to Boughton Hil l (east; A.D.
1670-1687) to Snyder/McClure (west; A.D. 1690-1710)(Table 5). Finally, in what appears to be a pt,zzling
temporal anomaly, 4 Sn-rich beads link the early (A.D.
1590-1610) site of Cameron (east) with the much later (A.D.
1655-1675) Marsh site in the same sequence (Table 5).
Table 3. West Seneca connections
sb.ppmppm
AS,
ppm
Na,o,/^o,/^
cl,%%
Sn,
ppm
Mn, K,
ppm %
AI, CA,
Y o %
Power House - West
6',1
70
7 l
Dann - West
80
84
At4
Dann - West
A0s
A06
I 640-l 655
5920 2.2
4800 2. r
5 l l 0 1 . 9
l65s-r675
6580 2 .1
5100 2 .0
6660 <0.8
1655-167 s
463 3.7
531 4.2
1690-1710
527 3.7
1 . 1 8
t . t 2
t . t 4
1 .0s
l . l 6
r .04
r .4 1 .47
1.8 1 .20
2.2 t .32
0.30
0.26
<7t <80
<67 <78<67 <63
t2 .0
12.2
1 2 . l
<38 <100
<56 <64
<38 <86
I 1 . 6
t2 .2
1 0 . I
6 .7
7 . 1
7.3
s0000
36s00
47200
3 1 s 0 0
49600
4 1 1 0 0
<780 <82
39300
40500
40600
0.87
0.90
1 . 9
1 . 5
l . l
7.2
6.7
7.4
t .29
L38
1.22
0.3s
<870 <82
<830 <85
Snyder/McClure - West
A80 t 0.84
Notes:
Beads labeled "A"
were analyzed in 1995. The remainder were analyzed in I99iBead labeling: r: round; c : circular; t: tube.
562
M. L. SEMPO'WSKIet aI.: ONTT{ETRANSMONFROMTIN-RICHToAIITMoNY-R.ICHEURoPEANrInrInsopa.GL4,SS -
Table 4. East Seneca connections
Na,
%%
CI,
%%
AI, CA,
% %Mn, K,ppm %
Sn,
ppm
As,ppm
Sb,ppm
Cameron - East
447 447 rr
A48 t
A49 t
Marsh - East
A03 t
Wanen - East
3 0 c
3 l c
3 2 c
3 3 c
3 4 c
4 2 c
Steele - East
6 2 r
6 3 r
6 4 c
6 5 c
6 6 c
Marsh - East
0 l r
Boughton Hill - East
429 429 tt
0.620.6s0.75
0.34
0 .31
0.33
0.33
0.76
0.73
0.71
0.69
0.73
0.83
0.78
0.79
0.73
0.77
0.76
0.79
0.83
J . t
4.0
4.6
4.3
6.5
6 . 1
6.0
5.6
7.0
8.2
6 .8
6.2
6.5
6.9
6.5
4.2
4 .1
0.63
0.67
0.68
0.63
0.70
0.67
0.76
0.78
0.66
0.73
0.68
0.70
0.66
0.62
<73.<85
<63
<80
<63<73
<77
<59
<64<56<56
<68
<74
1590-1610
1060 2. r
875 3.3
859 2.6
1655-1675
1010 2.9
r625-1640
4040 3.9
3630 4.34850 4.84270 5.043t0 4.84280 3.6
I 640-1655
4620 4.94370 4,94380 4.94340 4.64870 5.1
16s5-1675A
3770 <0.5
16'10-t687
3680 <0.6
6.3
6.0
s.9
6.2
7.4
7.2
7 .6
7 .7
7.6
8.8
7.2
7.6
7.4
7.9
6.7
7.3
<120
< l l 0
<180
130200
135000
152000
144600
36s00
41600
3 5 1 0 0
41600
36000
34400
3s700
45400
4r600
29600
36100
(goo
<740
<50<50<60<60<83
<76 <1700
140 <36<45 <41
I 10 <59<55 <48
t20 <46
<27 14500
<34 14800
Table 5. West and East Seneca connections
Sn,ppm
As,ppm
Sb,ppm
Mn, K, Nap p m % %
CI,
%%
AI, CA,
% %
Dutch Hollow- West
1 6 c
1 7 r
l 8 r
2 0 r
2 l c
2 2 r
2 3 r
2 4 r
Factory Hollow - East2 5 r
2 6 r
2 7 r
2 8 c
Marsh - East
402 402 tt
Boughton Hill - East
M 7 r
/.28 /.28 rr
Snyder/Iv1cClure - West
465 r
0.69
0.72
0.75
0.69
0.75
0.75
0.72
0.73
0.72
0.78
0.78
0 .81
0.83
0.72
0.90
0.93
4.6
5.2
4.7
4.6
5 . 1
5 . 1
4.0
4.6
4.7
4 .1
4 .1
4.2
s.6
5 . 1
5 . 1
5.9
0 .81
0,74
0.80
0.73
0.75
0.70
0.87
0.69
0.67
0.69
0.66
0.72
0.68
5.3
5.6
4.8
5.2
5.3
4.5
5.6
4.4
5.7
5.0
4.2
4.3
2.7
<0.6
<0.6
1 . 5
7 . 1
7.3
7 .7
7.0
7.7
7.7
7.5
I . )
7.5
7 .8
7.2
7.2
8.5
6.7
7.2
8.0
0.57
0.60
r6r0-t625
4380
43s0
42304230
4340
2760
3480
4550
3 130
16lo-162s
44804480
4570
4230
4600
1655-1675
2870
1670-1687
2810
25202520
1690-1710
29202920
126000
133000
122000122000
t27000
132000
124000124000
136000
1 1s000
132000
134000
13 1000
137000
<890
<690
<820
<960
<87 <87t70 <72180 <64<62 <59t20 <55<59 136
<73 <71<67 <61
130 <50180 <51<61 <62
<75 <75
110 16400
72 10400
<34 15400
<37 155000.59
563
M. M. L. L. SEMPOWSKI SEMPOWSKI Ct Ct AI.: AI.: ON ON THE THE TRANSITION TRANSITION FROM FROM TIN-RICFI TIN-RICFI TO TO A}ITMO].ry-RICI{ A}ITMO].ry-RICI{ EUROPEAN EUROPEAN WHITE WHITE SODA-GI.ASSSODA-GI.ASS
These small glimpses of inter-village interactions are not
unexpected, given the spatial proximity of the two
sequences of villages, the probable pattern of prescribed
inter-marriage between the groups, and the well known
phenomenon of reciprocal gift exchange which existed
between two such closely associated Iroquoian groups.17
Bead mandacture, shapes, and chemistries
To the west and north of the Seneca region, Sb-rich
glass trade beads do not occur on sites dated before A.D.
1650.8 Since the peoples of Ontario tended to be within
the French trading sphere throughout this entire period, it
appears that Sb-rich beads were acquired from the Dutch
sphere which'predominated in New York from the early
lTth century. Thus, Dutch bead-making houses appear to
have been at least the initial source of the Sb-rich beads
which began occurring on Seneca sites between =1625
and 1640. The timing of this transition in white bead
production is consistent with historical and
archaeological evidence suggesting alterations in Dutch
glass bead production at precisely this time. Following
almost two decades during which the Van Tweenhuysen
and other independent Dutch trading companies had
competed for North American markets, the States
General approved the Dutch West India Company's
request for a monopoly on trade in New Netherlands in
162l.18 The company did not actually begin operating
until 1623, and built Fort Orange near present day
Albany in 1624, essentially curtailing the activities of
their many Dutch competitors and taking control of the"Indian trade" in New Netherlands. As the new company
assumed control of trade with the Mohawk and other
New York Iroquois, changes in glass bead suppliers, or
at least a reduction in their overall number. would be
expected. The monopoly might also have resulted in
some changes in bead manufacturing techniques. A
reduction in the quality and variety of beads available is
suggested archaeologically in the Seneca area by the
disappearance of the more complex, and elaborately
made, striped "polychrome" beads, and their
replacement by simpler monochrome types which would
have been less expensive to produce.l5,l9 ;utr BAART's
investigations on Dutch bead factory sites also supports
the observation that such changes occurred in
Amsterdam bead production at around this time (BRnRr,
personal communication to Charles WRAy, 1982).
The shift from Sn to Sb as the opacifier used in the
manufacture of white drawn soda-glass beads may
represent one such change. An analysis of the form and
shape of the beads involved in this transition helps to
elucidate the possible rationale underlying it. First, the
transition seems to have begun primarily in the
manufacture of solid (uncored) circular white beads,
while that of cored circular white beads, which were
composed of only a thin layer of opacified glass
surroundingaclear glass core, continued to use Sn as the
opacifier. As shown in Table 6, this pattern of Sb-rich
uncored beads and Sn-rich cored beads persists
throughout the transition period, although the number of
exceptions increases over time. Indeed, by A.D. 1655-
70,the majority of cored and uncored beads of all shapes
(tubular, rounded, oval and circular) were being
opacified with Sb. Nevertheless, a significant number of
cored beads (both circular and tubular) continued to be
produced with Sn as the opacifier. By the last quarter of
the 17th century, however, the shift appears to have been
complete; cored and uncored white beads of all shapes
were opacified with Sb, and Sn-rich beads appear to
have been completely replaced.
Table 6. Opacifier summary by period, bead form, and bead shape
SbSn
Form:
Shape:
Uncored
C R O / B
Cored
C R O/B TUncored
C R o/BCored
T C R O / B
22
II
22
33
34
49
33
5 -
; ;
; ;6 8
l 0
JJ
l 0
30
23
53
55
33
55
l 3
II
11
aaJJ
nn
JJ
l 3
JJ
66
22
33
t 1
55
44
55
99
t 4
l 5
I 5
t 0
9 -
3 9
II
55
55
1590-1610
1610-1625
1625-t640
1640-1655
I 655-l 675
1670-1687
1690 -1710
Transition
TotalsII
3 1 0
Key to bead shape: T - tubular, C - circular, R - rounded, O/B - oval/barrel.
s64
M. M. L. L. SEMPOWSKI SEMPOWSKI Et Et AI.: AI.: ON ON THE THE TRANSITION TRANSITION FROM FROM TIN-RICH TIN-RICH TO TO ANTIMONY-RICH ANTIMONY-RICH EUROPEAN EUROPEAN WHITE WHITE SODA-GTI,SSSODA-GTI,SS