SUMMARY RPT ON THE PUKASKWA R PROP … o i l geochemical survey was also conducted using 100m spaced flagged ... with minor amphibolite grade metamorphism ... 40 to 50 degrees to the

l l l l l l l l l l l l l l l*

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S. 13*74 CAMP i-AKE 010

2.13074

NORANDA EXPLORATION COMPANY, LIMITED (no personal liability)

Summary Report on the

PUKASKWA RIVER PROPERTY MISHIBISHU AREA

N.T.S. 42C/4

NORTHWESTERN ONTARIO DIVISION

HEMLO, ONTARIO October, 1989

Russell Reid Geologi st Hemlo District

61.

TABLE OF CONTENTS

Page

1.0 Introduction......................................... l

2.0 Location and Access.................................. l

8.13974 CAMP LAKE

l l l l l l l

3.0 Property Description................................. l

l 3.1 Disposition Status.............................. l3.2 Joint Venture Status............................ l

l 4.0 Previous Work........................................ 2

H 5.0 Regional Geology..................................... 3

m 6 .0 Property Geology..................................... 4

7.0 Structural Geology................................... A

l

l

l

l

l

8.0 Conclusions.......................................... 6

l l l l l l l l l

Figure l Regional Location Map

l Figure 2 Property Location Map

Figure 3 Property Claim Map

l

l

l

l

l

l

l

l

LIST OF FIGURES

LIST OF MAPS

Map l Geological Compilation Map Scale 1:5000

l l l l l l l

1.0 INTRODUCTION

Geological mapping of the property was undertaken throughout

the summer of 1989; this is a report on the work covering the

western half of the property. The program was centered on the

Mishibishu Deformation Zone, and used a newly cut grid (lines at

125m spacing) as control.\

2.0 LOCATION AND ACCESS

— The Pukaskwa property is located in the western part of the

™ Sault Ste. Marie Mining Division, within Homer Township, Camp

l Lake and David Lakes areas; approximately 60km west of Wawa,^* *

Ontario. Access to the property is achieved by helicopter from

m t he Cameron Lake or Macassa Creek base camps located along the

Central Crude road which extends south from the Magnacon Mine

road.

l3.0 PROPERTY DESCRIPTION

l 3.1 Disposition Status

M The Pukaskwa property consists of 274 contiguous unpatented

claims located in the David Lakes, Camp Lakes and Homer Township

l areas of the Sault Ste. Marie Mining Division. All claims are

currently held in good standing.

l 3.2 Joint Venture Status

m A n option agreement was signed between Noranda Exploration

Company, Limited and Caribbean Resources Limited dated June l,

l 1933 giving No r ex t '\e s ole right to earn into the 274 original

ll

l l l l l l l l l l l l l l l l l l Figure l: Location mao

l lclaims of the property to 51^. Noranda is the operator of the

Bork programs on the project.

l .0 PREVIOUS WORK

l Recent exploration of the Pukaskwa River property began with

an airborne geophysical survey conducted by Aerodat for Caribbean

Besources Co. in 1986.

• During 1987 and early 1988, Caribbean Resources Co.

"onducted ground VLF-EM and soil geochemical surveys, and

Geological mapping of the eastern Devil Lake portion of the

property at a scale of 1:5000. A follow-up diamond drilling

Rrogratn comprised of sixteen holes was performed.*

. Following signing of a joint venture option agreement

between Noranda Exploration Company, Limited (no personal

Bliability) and Caribbean Resources Corporation dated June l,

1988, a SOOra line-spacing control grid was cut over the western

•two-thirds of the property not covered by the 1987 surveys. A

ws o i l geochemical survey was also conducted using 100m spaced

flagged grid lines west of L130E. A reconnaissance prospecting

•program of the property and 1:5000 geological mapping between

L90E and L110E was conducted during the fall of 1988.

I . The 1989 chronology of events for the Pukaskwa River

property is as follows:l

l

l

l

April to June - 125m spaced wing lines cut to complementexisting control grid from L60E to L130E; and cut from LO to L35E on the Devil Lake portion of the Mishibishu Deformation Zone.

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LOCATION MAPPUKASKWA

11 ' .012 34

MILES

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mineralization are more concentrated. These are oriented sub-

parallel to the local stratigraphy, both of which wrap around the

large felsic intrusive bodies.

Metamorphism has generally been recorded as mid to upper

greenschist facies, with minor amphibolite grade metamorphism

evident near granitic intrusions.

\

6.0 PROPERTY GEOLOGY

The Pukaskwa property is underlain by a sequence of mafic

to intermediate volcanics with intercalated felsic pyroclastic

units and interflow sediments along the north. The central zone

is underlain by intermediate volcanic units, poorly sorted

polymictic conglomerates, wackes and arkose with minor

subarkosic wacke and argillaceous units. The southern portion of

the property is underlain by a thick sequence of arkosic

sandstone and arkose, with subordinate polymictic conglomerates,

intermediate tuffaceous units, and minor reworked felsic tuff.

The property has experienced low to medium grade greenschist

facies regional metamorphism, with lower amphibolite grade

metamorphism observed proximal to felsic intrusive bodies.

7.0 STRUCTURAL GEOLOGY

The dominant structural feature on the Pukaskwa property is

a series of synformal fold axes trending approximately N75 to

N80E, plunging shallowly to the east, within the Mishibishu

Deformation Zone. The precise location of the major fold axis is


unknown due to parasitic synf orm/ant i forma l pairs developed

within the se diment a ry lvol can i c package, and sub-parallel

shearing developed along the axial planes of the folds.

The Mishibishu Deformation Zone is flanked to the north and

south by east-trending, steeply dipping (65 to 70 degre'es)

reverse thrust faults. Both show a significant vertical (dip-

slip) displacement, north-side up, with less dextral (right -"hand)

strike-slip displacement as indicated by lineation measurements

proximal to the faults and trending about N010 to N065, plunging

40 to 50 degrees to the east. The northern fault has developed a

50 to 100m zone of footwall brecciation and associated quartz

veining and flooding within the mafic volcanic flows and tuffs,

exposed from L90E to L130E, north of TL95N. No sulphide

mineralization was noted. The southern fault is a narrow zone (3

to 25m wide) separating the dominantly conglomerat e/wacke

sequence to the north from the arkosic se diment ary l f e l s i c to

intermediate volcanic sequence to the south. The fault is

relatively 'dry', characterized by talcose to locally graphitic

fault gouge with minor quartz veining and minor (l to 2X) and

sulphide mineralization.

Possibly co-eval to the development of the above thrust

faults is the development of normal faults and associated open

fold structures trending approximately northwest. One such

cross-s t ructure is well exposed in the Champagne trenches near

baseline 20,DOON at 20,150E. Geological mapping has defined

similar structure throughout the property based on foliation data


and lineation trends. The northwest trend of the cross-

structures is sub-parallel to the fold axis of the regional Kink

Lake Anticline, located to the southwest of the property; and

indicates they may be related to the large-scale folding of the

Mishibishu Greenstone Belt.

8.0 COHCLOSIONS s

Gold mineralization of the Pukaskwa property is dominantly

controlled by its structural (tectonic) history. The following

is a summary of tectonic events leading to the development andi

emplacement of the auriferous quartz veins and structural zone

presently known to occur within the Mishibishu Deformation Zone:*

(1) Isoclinal folding of the volcanic/sedimentary sequence about

an east-northeast trending fold axis with numerous parasitic

s yne l in e l a n t i c l i ne pairs developed within the sediments.

Shearing and dilation along the axial planes of the folds

may have occurred, initiating the development of the

Mishibishu Deformation Zone.

(2) Tight reverse (thrust) faults developed trending eastward

flanking and at a low angle to the existing axial plane.

Re-mobilization and hydrothermal alteration within the shear

zones may have occurred. Post-faulting dilation and quartz

veining of the shear zones is indicated.

(3) Northwest trending, normal cross faulting and associated

open folding of the property produced an en echelon

(disjointed) structural trend, hosting quartz veins. The


frequency of cross-fault offsets increases markedly from

west to east across the property. This development of the

northwest cross-structures may be co-eval to the reverse

faulting of event two.

The exact period of gold introduction into the area is presently

unknown. However, development of the structural host environment

initiated during the synclinal folding of the Mishibishu

Greenstone Belt, and additional hydrothermal alteration and

dilation of the zone occurred during subsequent tectonic events;

any of which may have introduced the auriferous fluids or re-

mobilized mineralization to its present locale.* m

Respectfully submittedNoranda Exploration Company, Limited(no personal liability)

Russe 11 ReidGeologistHemlo District

RR/rab

l l l l l l l l l l l i l l l l l l l

2.13074 CAMP LAKE O2O

2. 13074


Report of Work GROUND MAGNETIC SURVEY

on the PUKASKWA PROPERTY

N.T.S. 42/C 13 Northwestern Ontario Division

Hemlo District January 17, 1990

Tim Walmsley Geophy si ci st

l

STATEMENT OF QUALIFICATIONS

I, Timothy J. Walmsley of the City of Thunder Bay, Province of Ontario, do hereby certify that:

1. I am a geophysicist, residing in Thunder Bay, Ontario.

2. I am a graduate of Queens University, with a B. Se. Engineering, Geophysics (1987).

3. I have been actively engaged in geophysical exploration since 1987.

4. I was personally responsible for the interpretation of the geophysical data described in this report.

Timothy Walmsley Geophysk


48Ce4SEeet4 2 .13874 CAMP LAKE 020C

TABLE OF CONTENTS

1.0 Introduction.............

2.0 Location (t A ccess........

3.0 Geology..................

4.0 Personnel................

5.0 Instrumentation..........

5.1 Magnetometer Survey.

6.0 Discussion of Results...

6.1 Magnetometer Survey

6.2 Detailed Survey....

7.0 Conclusions.............

8.0 Recommendations.........

Page

. l

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2

, 2

, . 2

2

, 2

2

3

3

3

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LIST OF ATTACHMENTS

Scale

B Figure l Location Map............................. 1:45,000

* Figure 2 Claim Sketch............................. 1:45,000

lLIST OF MAPS

l Map l Total Field Magnetics - Readings.............. 1:2,500

Map 2 Total Field Magnetic Contours................. 1:5,000.

l

l

l

l

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l


1.0 INTRODUCTION

During the months of May d J une, 1989, a Total Field

Magnetic survey was completed over the Mishibishu Lake

Deformation Zone (MDZ) within the Pukaskwa property. The

objectives of the geophysical surveys were to assist geological

mapping, and to delineate magnetic zones.


The Pukaskwa property is located in the western part of the

Sault Ste. Marie Mining Division, (Camp Lake and David Lakes

areas) approximately 60km west of Wawa, Ontario (Figure 1).

Access to the property is best achieved by helicopter from the

Cameron Lake or Macassa Creek base camps. These camps are

situated along the 16km Central Crude road which extends south

from the Magnacon Mine road.

The property consists of 274 claims optioned from Caribbean

Resources in June of 1988.

Between July and September of 1988 a control grid was cut

with both tie lines and wing lines spaced at 500m. In April of

1989 cutting began on additional wing lines, limited to coverage

of the MLDZ, and spaced at 125m stations. A total.of 113km of

line has been cut at this time.

igiira 1: Location snap

lllllllllllllllll,

l


3.0 GEOLOGY

The area is underlain by met avo l cani c e and met as ed itnent ary

sequences of the Mishibishu Lake belt which are intruded by

swarms of diabase dikes. The MLDZ extends across the length of

the property striking070 - 090degrees.

4.0 PERSONNEL

The magnetic survey was carried out by M. Andrychuck and E.

Van l i e shout, both employees of Noranda Exploration Company,

Limited.

5.0 INSTRUMENTATION


A Scintrex MP-3 proton precession magnetometer was utilized

on the survey. Measurements of the earth's total geomagnetic

field (accuracy of .1 nTs) were taken at 12.5m stations and at 5m

stations locally. Diurnal corrections were made by integrating

recorded time, magnetic variations on a fixed base station with

the raw field data.

6.0 DISCUSSION OF RESULTS


A total of 59.8km of total field magnetic data was acquired

in the central portion of the property. There is approximately

6000 nTs variation in the magnetics, however, most values range

from 58,700 to 59,000 nT.

Within the survey area narrow discrete magnetic features in

excess of 59,100 nT and as high as 61,900 nT are defined and are

interpreted to map magnetite bearing diabase dikes. In addition,

similar negative magnetic features less than 58,500 nT and as low

as 55,200 nT are interpreted to represent reversely polarized

diabase dikes. Five major dikes (D1 - D5 i n c l. ), all striking

approximately WNW, are identified in the survey area. A sixth

dike (D6), located at 7900N striking 085 degrees, as interpreted

from a magnetic linear.

6.2 Detailed Survey

A detailed survey was performed over the VG Showing

involving 5-Okm of 10m mag.

The magnetic survey delineated the diabase dike which lies

just 25m west of the showing. It also showed clearly the extent

to which the chargeability anomalies are associated with the

dikes.

7-0 CONCLUSIONS

The magnetic survey proved a very useful mapping tool.

Unfortunately there were very few magnetic stratigraphic units.

8.0 RECOMMENDATIONS

Continuation of magnetic surveying is highly recommended as

results are most useful in aiding the mapping of stratigraphy and

s t rue ture.

Respectfully submittedNoranda E xp^Tb r a t i on Company, Limited(no persiyn/Q liability 1)

Tim Walmsley Geophysi cist Hemlo District

TW/mb


2.13074 CAMP LAKE030

2. 13074


Report of Work INDUCED POLARIZATION SURVEY

on the PUKASKWA PROPERTY

N.T.S. 42/C 13 Northwestern Ontario Division

Hemlo District January 17, 1990

Tim Walmsley Geophy si ci s t

STATEMENT OP OUAUFICATIONS

I, Timothy J. Walmsley of the City of Thunder Bay, Province of Ontario, do hereby certify that:

1. I am a geophysicist, residing in Thunder Bay, Ontario.

2. I am a graduate of Queens University, with a B. Se. Engineering, Geophysics (1987).

3. I have been actively engaged in geophysical exploration since 1987.

4. I was personally responsible for the interpretation of the geophysical data described in this report.

Timothy Walmsley Geophysic


42C84SE88M 8.13074 CAMP LAKE 030C

TABLE OF CONTENTS

Page

1.0 Introduction........................................... l

2.0 Location Se Access...................................... l

3.0 Geology................................................ 2

4.0 Personnel.............................................. 2

5.0 Instrumentation..............................-.....'..... 2

5.1 Induced Polarization/Resistivity.................. 2

6.0 Discussion of Results.................................. 3

6.1 Induced Polarization/Resistivity Survey........... 3

6.1.1 Resistivity................................ 36.1.2 Chargeability.............................. 4

6.2 Detailed Survey................................... 4

7.0 Conclusions............................................ 5

8.0 Re commendat ions........................................ 5


Figure l

Figure 2

Map l

Map 2

Map 3

Map 4

LIST OF ATTACHMENTS

Location Map,

Claim Sketch

Scale

l :45,000

1145,000,

LIST OF MAPS

Apparent Resistivity Values..

Total Chargeability Values...

Apparent Resistivity Contours

Total Chargeability Contours.

1:5,000

1:5,000

l :5,000

l :5,000


1.0 INTRODUCTION

During the months of May S June, 1989, Induced

Polarization/Resistivity surveys were completed over the

Mishibishu Lake Deformation Zone (MDZ) within the Pukaskwa

prope rt y.

The objectives of the geophysical surveys were to assist

geological mapping, and to delineate resistive polarizable zones

related to silicified sulphide mineralization which may be

associated with economic gold mineralization in the area.


The Pukaskwa property is located in the western part of the

Sault Ste. Marie Mining Division, (Camp Lake and David Lakes

areas) approximately 60km west of Wawa, Ontario (Figure 1).

Access to the property is best achieved by helicopter from the

Cameron Lake or Macassa Creek base camps. These camps are

situated along the 16km Central Crude road which extends south/'fromtheMagnaconMineroad.

The property consists of 274 claims optioned from Caribbean

Resources in June of 1988.

Between July and September of 1988 a control grid was cut

with both tie lines and wing lines spaced at 500m. In April of

1989 cutting began on additional wing lines, limited to coverage

of the MLDZ, and spaced at 125m stations. A total of 113km of

line has been cut at this time.

l l l l

X

SUPERIOR

Figure 1: Location mao

PUKASKWA NATIONAL

"" " " w** .f,*.'.,,,, *


3.0 GEOLOGY

The area is underlain by metavolcanic rocks and

metasedimentary sequences of the Mishibishu Lake belt which are

intruded by swarms of diabase dikes. The MLDZ extends across the

length of the property striking 070 - 090 degrees.

4.0 PERSONNEL

The IP/Resistivity survey was contracted to Mertens S

Ma c Ne i l of Guelph, Ontario.

5.0 INSTRUMENTATION

5.1 Induced Polarization/Resistivity

The IP/Resistivity survey was carried out using the IPX-IB

transmitter with 2.5kw generator made by Phoenix Limited and an

I PR-8 receiver manufactured by Scintrex Limited. A gradient

array configuration was utilized with a nominal current electrode

separation of 1km and a potential electrode spread of 25m.

Selected lines were also run utilizing a dipole-dipole array with

an 'a' spacing of 25m. The current "on/off" time was 2 seconds

for both surveys. The primary voltage measured during the "on"

current cycles is a function of the electrical resistivity of the

ground. The calculated resistivity R is: R K*V/!, where V is the

'on 1 time voltage, 'I' the "on" time 'current and 'K' is a

geometric constant determined by the relative positions of the

current and potential electrodes.

The secondary voltage, measured in time intervals during


"off" current cycles, is a function of the pol a rizabil i t y of the

ground. In all cases, the chargeability measured by the IPR-8 is

the mean value of the transient voltage over a selected time

interval which is:

1) normalized for the length of the integration interval

2) normalized for the primary steady state voltage

3) normalized for decay curve shape

4) normalized for number of pulses

The units of the quantities measured are therefore

dimensionless and are normally expressed in "millivolts per

volt".

6.0 DISCUSSION OF RESULTS

6.1 IP/Resistivity Survey

A total of 88km of gradient array IP/res i stivity surveying

was completed on the property over the MLDZ.

6.1.1 Resistivity

The apparent resistivity ostensibly defined trends

that parallel lithologic and structural strike. The data showed

only isolated correlation between topographically low areas and

low resistivity features. Thus, the apparent resistivity values

are for the most part reflecting lithologic features.

The resistivity data displays a fair degree of variability

with most values ranging between 4,000 ohtn-m and 15,000 ohm-m.

Local features displaying resistivities in excess of 45,000 ohm-m

and less than 700 phm-m are observed. The intermediate to high


resistivity areas have been observed to map the siliceous units

(felsic volcanics and clastic metasediments) . Low resistivity

features are associated with lithologies exhibiting higher

degrees of sulphidization (ie. S-10%), as well as conductive

fault/shear systems.

The inconsistency of the resistivity data, due primarily to

the effect of topography and paleo-infilling, disallows any

detailed lithologic interpretation. However, assuming a

siliceous Magnacon type deposit is the exploration target, then

the resistivity data should prove useful in locating siliceous

zones of significant enough size to host an economic ore body.

6.1.2 Chargeability

The gradient array induced polarization survey defined

numerous chargeability features trending parallel to geology at

080 - 085 degrees. The survey data defined underlying weak to

moderately polarizable lithologies with an average background

chargeability between 15 - 20 mV/V. Anomalously high

chargeability zones (^0 mV/V) generally coincide with lower

resistivity areas. However, smaller, more moderate chargeability

anomalies (25-30 tnV/V) do occur in areas of high resistivity as

we ] l .

6.2 Detailed Survey

A detailed survey was performed over the V.G. showing

involving 3.3km gradient IP/resistivity and 1.5km of dipole-

dipole IP/resistivity.

Both the dipole-dipole and the gradient data returned only

background levels of chargeability and resistivity over the

showing. The lack of recognition of the V.G. - hosting Quartz-

vein by these methods can clearly be attributed to the vein's

smal l s i ze.

7.0 CONCLUSIONS

Resistivity seemed to be successful at identifying siliceous

areas of significant size.

There seems to be evidence to support that the majority of

significant chargeability anomalies are the result of magnetite

within and re concent rat i on of sulphides along the diabase dikes.

Thus the defined anomalies must be carefully screened or

erroneous conclusions can be drawn.

8.0 RECOMMENDATIONS

It would appear that most of the defined chargeability

amonalies are associated with diabase dikes and thus magnetic

coverage is essential to help screen anomalies. It is also

apparent that more information is required to assist target

selection and thus spectral IP should be used if further

surveying is to be undertaken.

Respectfully submittedNoranda E^plor/ation Company, Limited(no p e &sam al liability)

Tim Walmsley Geophysici st Heml o Dist pa c t

oH

ntario

Ministry ofNorthern Developmentand Mines g ^ l 3 O f 4

Geophyslcal-Geologlcal-Qeochemlcal Technical Data Statement

File.

TO BE ATTACHED AS AN APPENDIX TO TECHNICAL REPORTFACTS SHOWN HERE NEED NOT BE REPEATED IN REPORT

TECHNICAL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETC.

Type of Survey(s) Magnetometer, I.P., Restivity

Township or Area G-3765——-——————^-—Claim Holder(s) Noranda Exploration Company, Limited

Survey Company Noranda Exploration d Mertens S MacNell

Author of Report Tim Walmsley————————-—————^ Address of Author P-O- Box 2656, Thunder Bay, Ontario

Covering Dates of Survey.

Total Miles of Line Cut—(linecutting to office)

SPECIAL PROVISIONS CREDITS REQUESTED

ENTER 40 days (includes line cutting) for first survey.ENTER 20 days for each additional survey using same grid.

Geophysical—Electromagnetic————Magnetometer——^

DAYS per claim

—Radiometric. I.P.

-Other-Restivity

Geological-—Geochemical.

20

AIRBORNE CREDITS (Special provision credit* do not apply to airborne lurveyi)

Magnetometer. .Electromagnetic(enter dayi per claim)

DATE:.Author of Report or Agent

Res. Geol.. .QualificationsPrevious Surveys

File No. Type Date Claim Holder

837 (85/12)

MINING CLAIMS TRAVERSED

r.,MHA.f*..,..prefix) (number)

1028335

1028360

1028361

10283^7'

1028369 o 51028343

........i.o.2.?.3.?..1...............^.2.?.3.4.?.....,

........^9.?.S?7.?.....-.:',..i-.:v.M^^::M.,,,,10283.73...........,..^8.3.8.Q.....

,...UfiWa7^.*n,,.*4MWW..^ .....,..lteS27.s..:: ?.L;..;'..;.AQ2fi3W.....

1028329 1028388

TOTAL CLAIMS. 50

M

l

Continued on attached sheet

GEOPHYSICAL TECHNICAL DATA

GROUND SURVEYS - If more than one survey, specify data for earh typ* of survey.. ' . , : j V t : : ,: - :,

Number of Stations. Station interval ——Profile scale,.-——.

-Number of Readings ,JLine

Contour interval.

UInstrument Scintrex MP-3

Accuracy — Scale constant —0-1 "teDiurnal correction method Automated - Computerized E.g. Unit

Base Station check-in interval (hours)————————..——..™^——Base Station location and value ___________________——™.

InstrumentELECTROMAGNETIC Cîl r^nfigl'ratinn

f.n\\ ^separation t

Arriirary

Method: D Fixed transmitter D Shoot back D In line Frequency. . ,. ..,.,,. ,.. ———————————— , —— . — : — — .,

1 (ipecify V.L.F. itation)Paranr'tTs mMsurpH

D Parallel line

Instrument.Scale constant,Corrections made.

Base station value and location.

Elevation accuracy.

InstrumentMethod [S Time Domain Parameters - On time — 2 sec

- Off time 2 sec

- Delay time —65 PIS

CD Frequency Domain — Frequency ____ _ Range——————,—

— Integration time 790 PSPower 2.5 Kw generator

Electrode arrayElectrode spacing. Type of electrode . stainless steel stakes

•'Ifiing Claims (continued)

SSM.1028389

1028390

1028395

1028396

1028397

1028398

SELF POTENTIALInstrument

Survey Methnrl

flnrrertinns marie

Ranoe

-,. . . ..v-.-, . w . . - 1

I ••••.•Ki.;;:L-;iv;;i ii-Av j: : " .' '.: - i !îftlfim ^-'Js,, j .,-!,,, J ;: j-..:. ' *

1 ••*' i ^' "' ""-': ' ' ' ' '''''""' ": ' fi "" " ' -.'ri'i.i' ,, * '- '.. ,

/i;.'^..!^,/-!.',,,,.'.^^';! '

RADIOMETRIC

Instrument.Values measured.Energy windows (levels). Height of instrument—— Size of detector————— Overburden———————

.Background Count.

(type, depth Include outcrop map)

OTHERS (SEISMIC, DRILL WELL LOGGING ETC.) Type of survey———————————————————————Instrument ,———-^—^——-—-—....—.——-...———-. Accuracy——--——.^——-——-.—-——-,.—-—-—-—^-

/ifcvr

Parameters measured.

Additional information (for understanding results).

AIRBORNE SURVEYS Type of survey(s) ———— Instrument(s) —————

Accuracy.(specify for each type of survey)

Aircraft used.Sensor altitude.

(jpecify for each type of lurvey)

Navigation and flight path recovery method.

Aircraft altitude.Miles flown over total area.

.Line Spacing ,, .,..

.Over claims only—

GEOCHEMICAL SURVEY - PROCEDURE RECORD

Numbers of claims from which samples taken.

Total Number of Samples. Type of Sample.

(Nature of Material)Average Sample Weight——————— Method of Collection————————

Soil Horizon Sampled. Horizon Development. Sample Depth———— Terrain—^^——^—

Drainage Development——————————— Estimated Range of Overburden Thickness.

ANALYTICALMETHOQgValues expressed in: percent D

p. p. m. Op. p. b. d

Cu, Pb, Zn, Ni, Co, Ag, Mo, As,-{c1rcle): . , . .,: . ,. ' :. - ' i'" 1 ''!.'."'

Others___________^_____(.'..j.,.———Field Analysis {___

Extraction Method. Analytical Method. Reagents Used.

.tests)

Field Laboratory AnalysisNo. f__________

SAMPLE PREPARATION(Includes drying, icreening, crushing, aihing)

Mesh size of fraction used for analysis————,

Extraction Method. Analytical Method. Reagents Used__

Commercial Laboratory (. Name of Laboratory.—. Extraction Method—. Analytical Method —— Reagents Used ____

.tests)

General. General.

Ontario

Ministry ofNorthern Developmentand Mines

Ministere du D6veloppement du Nord et des Mines

June 19, 1990

42Ce4Sieei4 Z . l3*74 CAMP CAKE

Mining Lands Section 880 Bay Street, 3rd Floor Toronto, Ontario MSS 1Z8

Tel: (416) 965-4888

Your File: W9005.032,033,034 Our File: 2.13074

900

Mining Recorder ,Ministry of Northern Development b Mines875 Queen Street EastP. O. Box 669SAULT STE. MARIE, OntarioP6A 2B3

Dear Sir:

Re: Notice of Intent dated May 18, 1990 for a Geophysical (Magnetometer and Induced Polarization) and Geological Surveys submitted on Mining Claims SSM 1028355 et al in David Lakes, Camp Lake and Homer Township.

The assessment work credits, as listed with the above mentioned Notice of Intents, have been approved as of the above date.

Please inform the recorded holder of these mining claims and so indicate on your records.

Yours sincerely

W. R. CowanProvincial Manager, Mining LandsMines St Minerals Division

i:zm Encl:

cc: Mr. W. D. TiernanMining s Lands Conmissioner Toronto, Ontario

Noranda Exploration Company THUNDER BAY, Ontario

Resident Geologist WAWA, Ontario


Technical Assessment Work Credits

Mav 18. 199Q

fit*

2.13074Winino Recorder* Report of

ftdOO'5-03?

Recorded Holder

Noranda Exploration Company, LimitedTownship or Area

David Lakes. Camp Lake. Homer TWP.Type of survey and number of

Assessment days credit per claim Mining Claims AssessedGeophysical

Electromagnetic.

Magnetometer.

Radiometric —

20

Induced polarization.

Other—————.——-

.days

-days

.days

.days

.days

SSM 1028355 to 358 Incl. 1028361 to 364 incl. 1028368 to 371 1ncl. 1028374 to 377 1ncl. 1028328 to 332 Incl. 1028336 to 338 1ncl. 1028341 - 342

Section 77 (19) See "Mining Claims Assessed" column

Geological ————————————————————days

Geochemical —————-^——————————days

Man days |~~j

Special provision O

Airborne

Ground

(~1 Credits have been reduced because of partial coverage of claims.

Q Credits have been reduced because of corrections to work dates and figures of applicant.

Special credits under section 77 {16) for the following mining claims

15 days Magnetometer SSM 102833510 days Magnetometer SSM 1028359 - 360, 1028372-373, 1028339 5 days Magnetometer SSM 1028340, 1028343

No credits have been allowed for the following mining claimsl ) not sufficiently covered by the survey insufficient technical data filed

The Mining Recorder may reduce the above credits if necessary in order that the total number of approved assessment days recorded on each claim does not exceed the maximum allowed as follows: Geophysical -80; Geologocal -40; Geochemical -40; Section 77(19) -60. . -



Oat*

May 18. 1990

FM*

2.13074Mining Recorder^ Report Of Work No.W9005-033

Recorded Holder

Noranda Exploration Company It.rt.Townihlp or Area ' "

David Lakes, Camo Lake, Homer Two.Type of survey and number of

Assessment days credit par claimGeophysical

Inrliirnripnliirl^tlOO. 17.6 ftayt

Section 77 (19) See "Mining Claims Assessed" column

Genlngir.al rtay.

Geochemirsl . , .,,.. rfayt

Man days [3 Airborne Q

Special provision fXl Ground 5D

Q3 Credits have been reduced because of partial coverage of claims.

Q Credits have been reduced because of corrections to work dates and figures of applicant.

Mining Claim* Assessed

SSM 1028355 to 364 i net. 1028368 to 377 Incl. 1028328 to 332 incl. 1028335 to 343 incl. 1028346 to 348 incl. 1028380 to 383 Incl. 1028386 to 390 inch 1028395 to 398 incl.

Special credits under section 77 (16) for the following mining claims

NOTE: Induced Polarization and Resistivity Surveys are assessed as one survey when the information for both surveys is gathered at the same time.

No credits have been allowed for the following mining claims[~j not sufficiently covered by the survey Q insufficient technical data filed

The Mining Recorder may reduce the above credits If necessary in order that the total number of approved assessment days recorded on each claim does not exceed the maximum allowed as follows: Geophysical - 80; Geologocal - 40; Geochemical - 40; Section 77(19) - 60.



AMENDED

Oat*

May 18, 1990

FM*

2.13074Winino Recorder* Report of"W05-034

Recorded Holder

Noranda Exploration CompanyTownship or Area

David Lakes,

Limited

Camp Lake, Homer Twp.Type of survey and number of

Assessment day, credit per claimGeophysical

Other.,,.. ,.,,

Section 77 (19) See"

Geologies!

Geochemical

Man days (~1

Special provision fiTI

dayt

da ve

dayi

days

Mining Claims Assessed" column

20

da vi

Airborne Q

Ground f")

Q Credits have been reduced because of partialcoverage of claims.

l~l Credits have been reduced because of correctionsto work dates and figures of applicant.

Mining Claims AnetMd

SSM 1028380 10283861028394 102832810283351028355102835810283611028368801313 -801320,801306 -801351 -801344 -

to 383 to 391to 399 to 333to 349- 356-359to 364to 377

314801327

307352345

1ncl 1nd1ncl 1nclincl

1nc?1ncl

*

t

*

*

*

*

Special crediu under section 77 (16) for the following mining claims

15 days Geological SSM 1028334, 1028357, 102836010 days Geological SSM 1028385, 1028393, 1028400 to 405 1nc1. 1028354

1028378, 1095698, 801337, 8013385 days Geological SSM 1028384, 1028392, 1028327, 1028365, 1028367, 1095697

No credits have been allowed for the following mining dalms

[^ not sufficiently covered by the survey Q insufficient technical data filed

SSM 1028353, 1031056, 1122249, 1028366

The Mining Recorder may reduce the above credits if necessary in order that the total number of approved assessment days recorded on each claim does not exceed the maximum allowed as follows: Geophysical - 60; Geologocal - 40; Geochemical - 40; Section 77(19) - 60.

Ministry ofNorthern Development

Ontario

Mining ActReport of Work(Geophysical, Geological and Geochemical Surveys)

Instructions- Please type or print.- Refer to Section 77, the Mining Act tor assessment work requirements

and maximum credits allowed per survey type.- If number of mining claims traversed exceeds space on this form,

attach a list.- Technical Reports and maps In duplicate should be submitted to

Mining Lands Section. Mineral Development and Lands Branch:Type of Survey(s)

Magnetic SurveyRecorded Holder(s)Noranda Exploration Company,AddressP.O. Box 2656, Thunder Bay,Survey CompanyNoranda Exploration Company,

Limited

Ontario P7B 5G2

Limited

Mining DivisionSaultSte. Marie

2/3V7**

Township or Area fG-3765 v g . 376? (COau

Prospector's Licence No. *~~A 34387

Telephone No.807-623-4339

Name and Address of Author (of Geo-Technical Report)Tim Walmsley, P.O. Box 2656, Thunder Bay, Ontario P7B 5G2

Date of Survey (from d to)QJh 05 i 'W 1 IP i -06 i W-

•)

Credits Requested per Each Claim in Columns at right Mining Claims Traversed (List in numerical sequence)Special Provisions

For first survey:

Enter 40 days. (This includes line cutting)

For each additional survey: using the same grid:

Enter 20 days (for each)

Man Days

Complete reverse side and enter total(s) here

Airborne Credits

Note: Special provisions credits do not apply to Airborne Surveys.

Geophysical

- Electromagnetic

- Magnetometer

- Other

Geological

Geochemical

Geophysical

- Electromagnetic

- Magnetometer

- Other

Geological

Geochemical

Electromagnetic

Magnetometer

Other

Days per Claim

20

Days per Claim

Days per Claim

Total miles flown over claim(s).Date Recffri&d Holder or Agent (Signature)

February 5/90 ^^fcx^^ vj^QL/^Li^-ceCertification Verifying Report of Work

Mining ClaimPrefix

SSM

Number

1028355102835610283571028358102835910283601028361102836210283631028364^1028368102836910283701028371102837210283731028374

Mining ClaimPrefix

SSMNumber

T02837510283761028377^10283281028329 '102833010283311028332 .1028335

-fc

-Ri

10283361028337102833810283391028340

Mining ClaimPrefix

S8M

^-G

FEE

)C9Jpt r

Total number of mining claims covered by this report of work.

Number

102834110283421028343

0 R D E

9 1990

3*-

D

\ hereby certify that 1 have a personal and intimate knowledge of the facts set forth in this Report of Work, having performed the work or witnessed same during and/or after its completion and annexed report is true.Name and Address of Person Certifying

Ronna F. Tergie, P.O. Box 2656, Thunder Bay, Ontario P7B 5G2Telephone No.

807-623-4339

For Office Use Only

Total Days Cr. Recorded

636

362 (69/06)

Date Recorded

f J. 1/1* .Date Approved as Recorded

Mining Recorder *

Provincial Manager, Mining Lands

t&Z?/'/^-' ^s/ut^? '

Date C*rtm*jpSy (Signature) .

Received Stamp

1 \

V

R. E dm!TV E D 'AM^ F3 '91590' ' 1

.

'Ministry ofNorthern Development and

Ontario

Report of Work Mining Act (Geophysical, Geological and Geochemical Surveys)

Instructions- Please type or print. -- Refer to Section 77, the Mining Act tor assessment work requirements


attach a list.- Technical Reports and maps in duplicate should be submitted to

Mining Lands Section, Mineral Development and Lands Branch:Type of Survey(s)

Induced Polarization ' Rest lvl tyRecorded Holder(s)Noranda Exploration Company, LimitedAddressP.O. Box 2656, Thunder Bay, Ontario P7B

Mining Division Township or Area fSaultSte. Marie G-3765 v ^.37^ ( U.

2. j ?0 -7 #5G2

Jau.Prospector's Licence No,A 34387Telephone No. 807-623-4339

Survey CompanyMer tens St MacNeil Guelph, OntarioName and Address of Author (of Geo-Technical Report)Tim Walmsley, P.O. Box 2656, Thunder Bay , Ontario P7B 5G2 01 05 89 1 30 06

Day | Mo. | Yr. j Day l Mo.89

1 Yr.-Credits Requested per Each Claim in Columns at right Mining Claims Traversed (List in numerical sequence)

Special Provisions

For first survey:



Enter 20 days (for each)

Man Days

ep.Vig,l(0erQ R Q

FEB 9 1990

Receipt No ,, ,

Airborne Credits


Geophysical

- Electromagnetic

- Magnetometer

Geolog cal

Geochemical

Geophysical

E D- Ma; letometer

-Oth r

Geolog :al

Electromagnet c

Magnetometer

Other

Days per Claim

~20~~

'20

Days per Claim

Days per Claim

Total miles flown over claim(s).Date Recorded Holder or Agent (Signature)February 5,1 99' )J// .f 7 '

Certification Verifying Report of Work

Mining ClaimPrefix

SSM

,. .

Number

1028355102835610283571028358102835910283601028361102836210283631028364 ^102836810283691028370102837110283721028373

1028374

Mining ClaimPrefix

SSM

Number

10283751028376102837710283281028329'102833010283311028332102833510283361028337

1028338

1028339102R340

1028341see accac

Mining ClaimPrefix

SSM

led smTotal number of mining claims covered by this report of work.

Number

102834210283431028346102834710283481028380102838110283821028383102838610283871028388102838910283901028391^

bee

50

1 hereby certify that 1 have a personal and intimate knowledge of the facts set forth in this Report of Work, having performed the work or witnessed same during and/or after its completion and annexed report is true.Name and Address of Person Certifying ^Ronna F. Tergie. P.O. Box 2656, Thunder Bay, Ontario P7B 5G2

Telephone No.807-623-4339

Date ,. .^^February 5,1990 CertJIfed By (Signature)

Received Stamp

For Office Use Only

Total Days Cr. Recorded

Date Recorded

Date Approved as Recorded

Mining Recorder

Prfcvjfeial Manager, Mining Lands

RECEIVED

A.M. p i.

1362 (89/06)

wSSM.1028396

ing Claims (continued)

1028397

1028398

Ministry of f J -"Northern Development

aocTMines Ontario

DOCUMENT No

-— - Report of WorkAct '(Geophysical, Geological and Geochemical Surveys)

Instructions- Please type or print.- Refer to Section 77, the Mining Act for assessment work requirements


- attach a list. - -- Technical Reports and maps In duplicate should be submitted to

Mining Lands Section, Mineral Development and Lands Branch:Type of Survey(s)

Geological SurveyRecorded Holder(s)

-Npr-anda -Exploration Company,. Lim1 fed . . ... -AddressP.O. Box 2656, Thunder Bay, Ontario P7B 5G2

Mining Division

Saul t- Ste. Marie

Township or Area @Qt*i4 David Lake Areat.

H&rto* s- J jjJsLProspector's Licence No. f

A 34387Telephone No.807-623-4339

Survey CompanyNoranda Exploration Company, LimitedName and Address of Author (of Geo-Technical Report)Russel Reid, P.O. Box 2656, Thunder Bay, Ontario P7B 5G2

Date of Survey (from i to) 01 05 89\ 1 30 07 89

Credits Requested per Each Claim in Columns at right Mining Claims Traversed (List in numerical sequence)Special Provisions

For first survey:



Enter 20 days (for each)i -, " ' 4;l J

Man Days : l-" "'~"~ -

Geophys cal

- Electromagnetic

- Magnetometer

- OtherGeological "" " ~~ "'"

Geochemical ^ ,J

Geophysical .J L..*^r|^~Wo'"tVrj'rjr,nV~ J-~'"'"

I FEB 9 1990

Receipt No. . ——— .— — . ——— — — — -Airborne Credits


E'D'^- Mag

-Othf

Geologli

omagnetic

etometer

il

liical

Electromagnetic

Magnetometer

Other

Days per Claim

20 '

Days per Claim

Days per Claim

Total miles flown over claim(s).Date Record/^! Holder or AgentfSlgnature)

February 5/90 c -tt-xÛLJ .-^Cu^XÛ-e.Certification Verifying Report of Work

Mining ClaimPrefixSSM

-...,

Number1028380102838110283821028383 '

.1028384 ~.

.1028385 :~.1028386 .1028387102838810283891028390102839110283921028393102839410283951028396

Mining ClaimPrefix

SSM

•~— - -

Number10283971028398102839910284001028401 ,1028402 '102840310284041028405^.102832710283281028329102833010283311028332

Mining ClaimPrefixSSM

•r 1 - - :

. ".'-'J-

:..v~-

. - '..-

see attached sheetTotal number of mining claims covered by this report of work.

Number102833310283341028335102833610283371028338102833910283401028341102834210283431028344102834510283461028347

91'

1 hereby certify that 1 have a personal and intimate knowledge of the facts set forth in this Report of Work, having performed the work or witnessed same during and/or after its completion and annexed report is true.Name and Address of Person Certifying

Ronna F. Tergie, P.O. Box 2656, Thunder Bay, Ontario P7B 5G2Telephone No.807-623-4339

For Office Use Only

DateFebruary 5,1990Received Stamp

cxvR 60 E 1 VE D

1362 (89/06)

Mining Claims (continued)

SSM. 1095697

1095698^

1031056.-^

1122249*---

801313

801314•—---

801320

801327

801306

801307 ^^

801351

801352^^

801337

801338*^

801344

801345

Noranda Exploration Company, Limited(no personal liability)

P.O. Box 2656, 960 Alloy Drive Thunder Bay, Ontario P7B 5G2

norandg______2.13074

Telephone (807) 623-4339

February 5, 1990***CL

Mining Lands Section ^ ff/ t^ 3rd Floor /fo, ^ "(i 880 Bay Street ^ Toronto, Ontario "/ty M5S 1Z8

Dear Sir:

Enclosed please find (in duplicate) maps and reports for mining claims SSM.1028328 et al in the area of David Lake for I.P. survey, magnetometer and restivity.

Yours truly,


Ronna F. Tergie Claims Co-ordinator Northwestern Ontario Division

,encl. reports (2) S maps -TOT

technical data sheet

c. c. file 2009

Noranda Exploration Company, Limited(no personal liability)

P.O. Box 2656, 960 Alloy Drive Thunder Bay, Ontario P7B 5G2

noranda Telephone (807) 623-4339

QFebruary 5, 1990

Mining Lands Section 3rd Floor 880 Bay Street Toronto, Ontario MSS 1Z8

Dear Sir:

Enclosed please find maps and reports (in duplicate) for geological survey for mining claims SSM. 1028380 et al in the David Lake Area.

Yours truly,


Ronna F. Tergie Claims Co-ordinator Northwestern Ontario Division

/rftencl. reports (t maps (2)

c.c. file 2009

1h ,i

|ARE A3 V

M. R. O

S.R.O.

M. -i- S,

-

'ITHD-

-SL'F:."

-M If J. 1

JOT* S -^

ACE KI^TSOMLY

'•3 A," '"^ '" ' ^ - ' "~ P ' '~ ':~~~~ t

F J a

NOTES

LAND UNDER TnE WATERS OF LAKE WITHDRAV/N FROM STAKING BY CR2E5 DATED 50 A'RIL 19:2.

COUNCIL

THE SL'BDlV!SJC\ OF THE TOWNSHIP OF HOMER IN LOTS AND CCNCESS10NS WAS PARTIALLY ANNULLED 27 FEBRUARY, !985.

R E C E ( V E

2.13674 CAMP LAKE 200 TE OF'TSSUT]

i ~ rjo.

PUKASKWA

PARK

CL 2526' - T , ..

•^ * "X \ \ L\ '..^'y.—-*r^^—

:03I046 l ' 031044 ' I Q3I039 l

l l

ALL ISLANDS WITHIN 2 MILE LIMIT

ARE PART OF NATIONAL PARK

031040-.110310 J8 .031030

1032216 , 1032219 l 03 I032E2IV032 '71

• 032222l032l74

1032101 IC3208B^ • •~

HIGHWAY AND R O',

OTHER R OADS

TR AILSSURVEYED LIMES:

TCV.NSK'PS. BAS

UNSL'RVEYEO LiM LOT LT.ES . PARCEL B OL1 *-3"r.'if.MNG CL-:V.s

UTILITY L INES

SC't -Pr ~- E\"*!" - S .

SUH DIVISION OR C

MINES

TRAVERSE WON'L)V

" " ~'

E FLA.N

TYPE OF U.GCU.'.:E' PATENT, SURFACE s

.SURFACE R.

\3 R IGHTS

"5 D-^LY..'...

D'.LY ......

LEASE, SURFACE S. V

" .SURFACE FiG

" .MINING RIGH"

LICENCE OFOCCUPA'

ORDER-IN-COUNCJL .

RESERVATION ———

CANCELLED .___

SAND Se GRAVEL __

CNLY

\^Y..

SYMBOL g

......... O S~™- ©

e.-. o ?— B i—. Q— V—. OC

©

E: WINING RIGHTS 1913. VESTEC I LANDS ACT. F

:.s PATEN~E~-PH:OR TO K*.AL PATENTEE Bf T^.E c~

CHAP. 380, SEC. 5I-. SU

SCALE: 1 INCH = 40 Zr-.Al

FEETO TOOO 2OCC 60OC SHOO

o 200METRES

2000 (2 KM

DATE OF ISSUE

SEP **'B89

SAUIT STE MARIE MINING BECCPOrffS OFFICE

T r. i -; M c 'j f T l b v.' . i o 11 i r

r V .f

l SAULT SS r- r i ' ' -i - .-i -

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ND

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DATE OFISSUE

.-•SAULT STE. MARIE MINING RECORDER'S OFFICE

LEGEND.HIGHWAY- OTHER -

.TRAILS

NO r'

FC

ta

RIGHT'

-NON-PEREti.^VAj. STREAM.

FLOODING OR

WINES

TR A V E.

T**

DISPOSITION OF CROWN LANDS

-TYPE OF DOCUMENT"

PATENT SUflf MfNlNC RtCHT'S i-J-v

" BIGHTS QNi.S^;^^LEASE,SUBFACE St MINING ''

CANCEtLtD -' "^

NOTE, M ;NING fltGHT^.tN CANCELS..~i9ia -VESTED IW ORIGINAL

^ ^ —— T L***D* *CT.' F* .S O 19XJ."BY THE'"*U6L 1C'

38O; SEC. 6' "

SCALF V l INCH *'40 CHAINS.- "i V; --V V

, O' 4OOO . ' 8000:- '

1000 .li K Ml" !

2OOO' - '- , r'f i -. t •,(2*V*-""V-- ' '-' '\ : '^

AREA

DAVID: LAEM.N.R. ADMINISTRATIVE DISTRICT

MINING DIVISION ' - - " .,

SAULT STE; -' MARJE7;.LAND TITLES/ REGISTRY D1VISI.ON

THUNDER BAY ; - :

Ministry of,NaturalResources

Ministry of - :- Northern Development and Mines '

Ontario

DECEMBER, 1986, Numbtr

G "y ^^/•s r** -3765

MATTHEWS SHOWING - SIGNIFICANT ASSAY DATA

SAMPLE No. EASTING NORTHING ANALYSIS (g/t)

15310-D 15319-J 15319--K 15319-L15325-C

117+50 E 86+80 N117+50 E 86+80 N117+50 E 86+80 N117+50 E 86+80 N117+50 E 86+81 N

V . VJ

SAMPLE No.

15329-115330-C15330-D15335-M

EPT-1- 7 EPT-4-18 EPT-4-19

EASTING

102+90103+00103+00103+20

103+25 103+50 103+50

EEEE

E E E

NORTHING A

88 + 6088 + 8588+8588+70

88+72 N - 88+69 N - 88+70 N -

NNNN

88+73 88+70 88+71

N N N

ANALYSIS (g/t)

IAL PARK

SHOWING

V-2o"ooV| X \

2.13074Mapl

PROJECT:. PUKASKWASurw*y*d by:.,...........,............ DoteDrown by:........ ...............—.Scale ..I.:N.tS ' 42C/4 noranda

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LEGEND

FELSIC PLUTONIC ROCKS

DIABASE DYKE

EARLY INTRUSIVE ROCKS ( SYNVOLCANIC) o) Felsic Quartz Feldspar Porphyryb) Gabbro

CHEMICAL SEDIMENTS- SULPHIDE IRONSTONE

CLASTIC SEDIMENTSa) Poly mie tic Conglomerateb) Wackec) Arkose, Siltstone Rudstone

FELSIC VOLCANICSaJFlowbJTuffc)Crystal Tuffd)Breccia

INTERMEDIATE VOLCANICSa)FlowbJTuffc) Crystal Tuffd) Breccia

MAFIC VOLCANICSa)Flowb) Tuffc) Crystal Tuffd) Breccia

PUKASKWA NATIONAL PARKGeological ContactFaultShear Zone

Ddh. Locations

Trench Locations

Anomalous G rab Sample Location

Mishibishu Deformation Zone

Quartz Vein

Quartz Strlngws

PyriteArsenopyrlt*Silicification

Hematizatton

^0950 ON

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loWSfyS". "l

-êrj&sUmlt of Detailed Ma iplng Sep,

f o 23 fa l *

MATT

HEWS

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SIGN

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ASSA

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SAMP

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STIN

G NORTHING

ANALYSIS (g

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117+

50 E

86+80

N15319-J

1531

9-K

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