32D04SE900) 2.15168 MCFADDEN 010

GEOLOGICAL REPORT

ON THE

WRIGHT PROPERTYMCGARRY AND MCFADDEN TOWNSHIPS

LARDER LAKE MINING DIVISIONDISTRICT OF TIMISKAMING

ONTARIO CANADA

January, 1994 Brian WrightGeological Technician

32D84SE90ei 2.15168 MCFADDEN 01C5C

TABLE OF CONTENTS

PAGE

Introduction..,........,.......................,............................,........................... l

Location, Accessibility........................................................................ l

Climate, Local Resources.................................................................... 2

H i story of the Claim Block ................................................................. 5

Regional Geology................................................................................... 10

Property Geology.......,.......................................................................... 11

Present Work Program ...............................................,....................... 15

Discussion of Results.................................,.......................................... 15

Structures and Mineralization ........................................................ 17

Recommendations for Future Exploration .................................. 18

Conclusions............................................................................................... 19

Bibliography............................................................................................. 20

Declaration.........................................................,..................................... 21

FIGURES/ TABLES/ MAPSFigure 1: Location Map .................,................. 3Figure 2: Claim Location ............,.................... 4Figure 3: Superior Province .......................... 7Figure 4: Abitibi Greenstone Belt,.............. 8Figure 5: Regional Geology ............................ 9Figure 6: General Geology.............................. 12Figure 7: Structure, Geology, Deposits...... 14

Map 1: Geological Map ..................... In Back Pocket

INTRODUCTION

Brian Wright and Associates currently hold a number of claims in

McGarry and McFadden Townships, Larder Lake Mining Division. A

geological mapping over the entire property and stream sediment

sampling program on claim 1180059 was completed during the

spring Si summer of 1993- This report will detail observations made

during this program and recommend future exploration programs to

be carried out on the property.

LOCATION. ACCESSIBILITY.

The claim block is located in the south-east portion of McGarry

Township and the north-central portion of McFadden. Larder Lake

Mining Division, District of Timiskaming, Ontario, Canada (figure l ).

Access to the property is by means of Highway * 66 approximately 5

kilometers east of Virginiatown then south on the Raven Lake Access

road to approximately 800 meters from the claim boundary of claim

unit 1180047. Other access routes to the property include an

overgrown logging road that crosses the entire property, various

a.t.v. and snowmobile trails that have been cut in the area, and

water access in available via Larder Lake.

LIST OF CLAIMS

The work was performed on the following claims : 1180047. 1180048.1180049.1180050,1180052.1180053.1180056. 1180057. 1180058. 1180059. 1187131.

CLIMATE. LOCAL RESOURCES

Climatic conditions are typical for this part of Northern Ontario.

Temperatures range from - 45 degrees Celsius to * 35 degrees

Celsius.

Water resources are available within the property. Mining supplies

and skilled human resources are available in Kirkland Lake and

surrounding communities.

The topography of the claim group is dominated by north-east

trending ridges made up of mensa and cuestas bounded by steep

terraced rock bluffs which rise 50 to 230 m above the level of Larder

Lake.

Timber in the area consists of Jackpine, poplar, birch and balsam.

Black spruce and tag alders occur in swamp poorly drained areas.

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HISTORY OF THE CLAIM BLOCK

Despite being within a half a mile of a major gold mine (the Kerr

Mine ) the property has been overlooked in the past and little if any

exploration work has been completed on the property. The history of

the area in the vicinity of the present claim block is well documented

at the Ministry of Northern Development and Mines branch office in

Kirkland Lake. Table l outlines the chronological history of the claim

block and the adjacent properties.

Table l : History of the Property and Adjacent Properties

Year Company and Work Completed

1937 Highridge Mining Company Ltd. and Wesley Gold Mines

Limited controlled the property immediately north of the

present claim block. A total of 13 surface diamond drill

holes on their property were completed totaling 10,352

feet. The thickness of the Cobalt sediments above the

Archean volcanic basement was between 210 feet and

670 feet. All holes were drilled into the Northeast Arm

Shear Zone, Of importance is the fact that Hole * 6

penetrated the overlying Cobalt sediments and

intersected gold mineralization in the underlying volcanic

terrain that forms part of the shear zone. The gold

mineralization was logged as being associated with a well

mineralized quartz/carbonate-rich chloritic carbonatized

schist. This underlying mineralized schist yielded 0.18

opt gold across 19 feet including 0.29 opt across 8.2 feet.

1943 Larder "U" Island Mines Ltd. and Great Larder Gold Mines

controlled the property immediately west of the present

claim block. Prospecting, mapping, trenching and

diamond drilling were completed on their property. All

diamond drilling was confined to the Northeast Arm

Shear Zone. The thickness of the Cobalt sediments was

between 200 and 500 feet. Of importance is the fact that

hole * 3 penetrated the overlying sediments and

intersected anomalous gold values. The gold

mineralization was logged as being associated with a talc

carbonate schist. Also of interest is hole * 2 which

intersected gold mineralization in the Cobalt sediments

yielding up to 0. l opt gold across 2.0 feet,

1980-81 Placer Development Ltd. held a large portion of the

present claim block. Prospecting, mapping, geochemistry,

airborne radiometric survey, and diamond drilling were

completed on their property, a total of 4 drill holes

totalling over 3000 feet were completed east of the

current claim block. The thickness of the Cobalt

sediments above the underlying Archean volcanic

basement was between 670 to 960 feet.

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ArchtanMaiachtwin d*ibut {not ihownl

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lyeniK 10 Miiwv* \o gn*( \jic quarrr d-cxitt , to

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B 8*. 8b, 3'akf River r,rouo BcRiver tUPP*' Fm . T,*d*i* G'Ou

7 7*. 7b, Kinoievii Group, 7c Kinoievn Gfoup,(M.tfdt* Fm.. Tiid*le Giouol

6 6^* LJ'der Lake Gipup. 6ft StoughtonRoqor*THHK* Group. 6e Loy**r Fm, TadjliGroup

l &C Porcupine Group

lo*wr Supergroups4 4* Stttd Group. -1b Hunter Mint Group. 4c

Upp*sr Fm., Deloro Group 3 ^j Cii^crinc Group, 3c Middl* Fm.. Deloro

Group 3 3i Ajbewtwc Group. 2c Lower Fm. Otlo'o

Group 1 \t Pacaud luMi

'l fflfri to Kitkljnd La^t Am. V)Uth limb o( ivnchnonum IJtnttn 1973C. 19731."b rel*M 10 Kukljnd L^h* Aff*. ocrV* limb o' lynclmo'ium Umwn 1 976. I978b|.

"*e reftri to Timmini A'ei IPv^e. 15801.

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1984-93 Mr. R. A. MacGregor holds the property immediately

northwest of the present claim block, several geophysical

programs were completed on his property. Sporadic

surface sampling yielded negligible gold values.

1991-93 Mr. Brian Wright staked the present claim block.

Work completed to date includes prospecting, stream

sediment sampling and geological mapping of claim

1180059 at a scale of l inch to 200 feet ( see back

pocket).

REGIONAL GEOLOGY

The regional geology has been adequately described by John

Hamilton in his 1986 Masters thesis as a " belt of Archean volcanic

and sedimentary rocks that form a northeast trending Subprovince

of the Superior Province of the Canadian Shield (M.E.R.Q. -

O.G.S.. ). It stretches for about 800 km across northern Ontario and

Quebec (figure 3 ). The Abitibi belt is bounded to the north by the

Opaticametasedimentary gneiss belt ( Card et al., 1981 ). and to the

south is covered by Huronian sedimentary rocks (figure 4 ) . The

western and eastern boundaries are the Kapuskasing Structural zone

( Percival and Card, 1985 ) in Ontario and the Grenville Province in

Quebec, respectively.

The western portion of the Abitibi belt that borders the Kapuskasing

Structural Zone is characterized by synclinal cusps, asymmetrical

linear belts and small outliers of volcanic and sedimentary rocks

which occur marginal to and suspended in large batholithic

complexes composed of quartzo-feldspathic gneisses and granitoid

rocks. Eastward in the Timmins - Kirkland Lake area volcano-

sedimentary supracrustal rocks dominate over granitoids. In the

central part of this area, the supracrustal rocks appear to be

distributed in a large basin, generally referred to as the Blake River

Synclinorium which is bounded by two major east-west trending

fault zones (figure 5 ). A similar broad anticline cored by the Round

Lake Batholith occurs to the south of the Larder Lake Break. Further

to the east, in Quebec, the belt of supracrustal rocks of the Abitibi

Belt widens and has been subdivided by Dimroth et al., into three

large geotectonic subdivisions called the internal Zone. External Zone,

and the Foreland ( Bellecombe Belt ) Zone. The Blake River

Synclinorium is included within the the Internal Zone ".

" Jensen ( 1978a ) has outlined two major volcanic cycles in the

Kirkland Lake district. Rocks of the older volcanic cycle are restricted

to the outer regions of the Blake River Synclinorium, occupying the

core of the Lake Abitibi Anticline in the north and the rim of the

Round Lake Batholith in the south. The upper volcanic cycle

dominates the central portion of the Blake River Synclinorium. The

entire stratigraphic section of the two major cycles is interpreted to

be at least 50 km. in thickness ( Jenson and Langford, 1983 ).

PROPERTY GEOLOGY

The geology of the claim group has been documented as being

entirely covered by Cobalt sediments of Proterzoic age. Mr. R. A.

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Felsic Intrusives

Timiskaming Sediments

Trachyte

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* Kerr Addison mine

SLA Spectacle Lake Anticline

BLS Beover Lake Syncline

MacGregor's property, located immediately to the west of the present

claim block, is also underlain by rocks of the Cobalt Group, Mr.

MacGregor, 1990 states that" The Cobalt Group consists of fine

grained greenish to greenish-grey greywackes to coarser grained

greenish to brownish arkoses to polymetalic heterolithic

conglomerates. The greywackes were observed to carry very fine

mud clasts in places. The arkoses are sand sized to coarser grading

almost to micro conglomerates in places. The conglomerates stand out

because of their variety and large clast sizes. Pink to whitish

granites, porphyries and greenish volcanics predominate, but bedded

siltstone, iron formation and greywackes were also noted. The

contact between the coarse conglomerate and finer grained

greywacke arkose appears to be quite sharp although many of the

contacts are obscured by overburden. The rocks appear to dip gently

to the east." The actual thickness of the Cobalt sediments on the

property has not been determined but drilling on nearby properties

would indicate a range between 200 and 700 feet.

Structurally, the claim block has been documented as being

underlain by a major northeast trending fault called the Milky Creek

Fault (Thomson. 1949 ) . Hamilton ( 1986 ) describes this fault or

secondary splay as part of a larger parallel system of shears referred

to as the the Northeast Arm Shear Zone (figure 6 ) . The Northeast

Arm Shear Zone continues northeastward off the property where it

sinistrally offsets the Larder Lake Break in the vicinity of the the

Kerr Mine. It also continues southwestward off the the property into

Hearst Township where it hosts several gold deposits. The

economically attractive gold deposits in the area are almost always

spacially associated along the Larder Lake Break or with secondary

splays off the main break (figure 7 ). These structures in all

probability, acted as conduits where the mobilization of gold bearing

fluids would migrate into structurally porous areas and could

eventually concentrate into significant gold bearing environment.

Other structures of interest on the property include two circular

depressions that may be the weathered expressions of kimberlite

pipes.

PRESENT WORK PROGRAM

The present work program of mapping and prospecting was designed

with the following objectives; To locate any possible Archean

windows on the property as reported by local prospectors

( Mandzuik 1980 ) . To determine possible Archean structures that

have a expression through the Cobalt cover. To investigate the

possibility of gold within the Cobalt formation. The entire claim

block was mapped at a scale of l inch to 200 feet with 400 foot line

spacing. A total of 10 stream sediment samples were collected and

are to be analyzed for kimberlite indicator minerals ( results pending

) . The results of this program are presented in the geological map

inclosed in the back pocket.

DISCUSSION OF RESULTS

The program did not provide the results anticipated but a more

complete understanding of the geology of the property was obtained.

The reported occurances of Archean rocks on the property could not

be located. These occurs were reported by the man who had logged

the area in the 1920's and it is possible that these rocks could be

flooded by beaver ponds. The probability that the Archean rocks

may have been float or do not exist on the surface of the property

seems to be the most likely scenario.

The Huronian rocks have been deposited under low energy

conditions and do not appear to be sorted well enough to concentrate

heavy minerals to produce paleoplacer deposits.

The stream sediment sampling failed to produce any indicator

minerals for diamonds but further work in this area is warranted.

A total of 10 samples weighting approximately 25 kilograms each

were hauled out of the bush and 5 were sent for analysis . Three

samples that were taken downstream from the suspected kimberlite

consisted of clay and were washed away in the screening process and

no concentrate was recovered. Two samples taken up ice from the

target did produce a concentrate but no indicator minerals were

recovered.

The completed program did not produce immediate results but the

location and structures on the property require further detailed

exploration. The best chance for an economic deposit to be

discovered is in the Archean Formations underlying the Huronian

rocks.

TABLE OF FORMATIONS Recent and Pleistocene

- peat- clay ; fine grained greenish-blue to grey in color- glacial till; sand and boulders

Keweenawan mafic intrusive rocks- olivine diabase- lamprophyre

Huronian Supergroup Coleman Formation

- argillite ; fine grained grey to greenish gray in color massive with little signs of bedding

-arenite : medium grained .grey in color, graded bedding and cross-bedding common, quartz rich with accumulations of pyrite

- greywacke; fine grained , grey to brownish in color, thinly bedded

- pebble conglomerate ; large boulders up to 2 feet in diameter of mafic to felsic origin, poorly sorted, various colors

Archean- felsic to mafic volcanic and intrusive rocks

STRUCTURES AND MINERALIZATION

During the current mapping program the presence of a large parallel

fault and shear system was indicated or detected. The Milky Creek

Fault is evident in places along a large escarpment trending N 50 E

that more or less cuts the property in half. The movement or

displacement of this fault could not be determined from surface , To

the east of this fault a larger escarpment with up to 700 feet of

vertical distance occurs. This ridge has been previously called part of

the Milky Creek Fault System but appears to match up with the

Southwest McFadden Fault that has been identified to the south and

west of the property. To the west of the Milky Creek Fault there are

three parallel lineaments that may be the surface expression of some

underlying fault or shear system.

The present program did not detect any veins over six inches in

width but several veinlets were detected but were not considered

significant. A slight pinkish ( possible feldspar) alteration was

present with these veinlets.

RECOMMENDATIONS FOR FUTURE EXPLORATION

The prospecting and mapping failed to find any Archean windows on

the property or defined drill targets for gold mineralization. To

define possible gold targets on the property a systematic exploration

program has been proposed. The establishment of a grid system at

400 foot spacing, on the property will require 30 miles of linecutting.

Upon completion of the linecutting the property will be mapped at a

scale of l inch to 200 feet. Prospecting with a beep mat to locate any

possible near surface conductors should establish if any Archean

windows are present on the property. Geophysical surveys

recommended to be completed are a ground magnetometer survey

and a Maxi-Probe E.M. survey to locate any deep seated structures or

mineralization. Completion of this program should establish targets

for follow up diamond drilling.

Should the results of the indicator mineral sampling prove

encouraging a R. C. drilling program over the 2 possible kimberlite

targets is recommended.

CONCLUSIONS

The property is located in a favorable environment to host economic

mineral deposits but work completed to date has been insufficient to

establish drill targets. Further exploration on the property is justified

and should be implemented as soon as possible.

BIBLOGRAPHY

Assessment Office. Ministry of Northern Development and Mines Kirkland Lake. Ontario

Baker. J.W... 1957, Kerr-Addison Mine: Structural Geology of Canadian Ore Deposits: Canadian Institute of Mining and Metallurgy, v. 2,

392-402

Brummer J.J. et al ., 1992 Discovery of Kimberlites in the Kirkland Lake Area: Exploration Mining Geology, v. l No. 4 pp 351-370

Card, K.D. et al . , 1981, Progress Report on Regional GeologicalSynthesis, Central Superior Province, Paper 81-la, pp 77-93.

Dimroth, E. . et al . , 1982, Evolution of the South-Central Part of the Archean Abitibi Belt, Quebec, Part l : Stratigraphy and Paleogeographic Model : Canadian Journal of Earth Sciences, 19pp. 1729-1758

Jensen, L.S, and Langford, F.F. , 1983, Geology and Petrogenesis of the Archean Abitibi Belt in the Kirkland Lake Area, Ontario, O.G.S. Open File Report 5455

Hamilton, J.V. . 1986, The Structural and Stratigraphic Setting of Gold Mineralization in the Vicinity of Larder Lake Southcentral Abitibi Greenstone Belt, Northeast Ontario: Master of Science Thesis - Queens University Unpublished Report pp. 1-156

Hodgson C.J, . et al. , 1991, Gold Deposits and the Tectonic Frameworkof the Abitibi Greenstone Belt Larder Lake Area. O.G.S.

Open File Report 5782

Lovell H.L. , 1970. Lake Timiskaming Rift Valley O.D.M. , M. P. 39

Thomson. J.E. , 1949, Geology of Hearst and McFadden Townships Ontario Department of Mines, Annual Report, V. pt. 5. pp 1-53

DECLARATION

I, Brian james Wright, of the Town of Kirkland Lake, Province of Ontario, Canada, do state:

1) that I am a geological technician and my mailing address is Box 691 Kirkland Lake, Ontario, P2N 2K3.

2) that I received my education from the Haileybury School of Mines, Haileybury, Ontario.

3) that I have been practicing my profession continuously since 1983 and that I am qualified to submit this report.

4) that my report on the Wright Claim Block in McGarry and McFadden Townships, Ontario, is based on work carried out and supervised by me and on review of published and unpublished information on the property and surrounding area.

October 2, 1993'Wf/

Brian Wright Geological Technician

January 24, 1994

Mr. B. Wright P.O. Box 691 Kirkland Lake, Ontario P2N 1X6

Dear Sir,

RE: McFadden Twp Samples

5 Samples were submitted as follows:

NOS 23502 23503 235062350823509

Samples were all screened to produce a -20 +60 mesh fraction. Samples 23506, 23508, 23509 were entirely fine grained clay and all material passed the -60 mesh screen.

The -20 + 60 mesh fractions for sample 23502, 23503 were pre- concentrated using heavy liquids to produce a heavy concentrate {all minerals heavier than S. G. 3.1) to examine microscovpically. No kimberlitic mineral grains were observed from the concentrates examined from these two samples. Our invoice to you is as follows.

5 Samples washing - screen@ $50 = $250

2 Samples Dry Mag Seperate = ^250 4 Samples fractions Heavy = ^180

Liquids. 4 Microscopic Examinations

@ $25 = $100 TOTAL COST = $780.00

Please Remit at your earliest convenience.

Yours truly,

A. L. Barker Vice President

Suite 1414 IK l University Avenue

Guardian Tower Toronto. Out.. Canada

MSII 3M7(416) 359-9282

Kax(4l6) 367-5269

BELL-WHITE ANALYTICAL LABORATORIES LTD.P.O. BOX 1 87, POJ 1KO

HAILEYBURY, ONTARIO TEL: 672-3107 FAX: (7O5) 672-5843

Qkrttfirat* 0f AnalgfitaNO. 0692

SAMPLE(S) OF: Rock ( 5

DATE: September 10, 1990

RECEIVED: September 1990

SAMPLE(S) FROM:Mr. Brian Wright, Bratt Resources

Sample #

12345

Oz. gold

0.046 0.016 Trace 0.002 0.040

N ACCORDANCE WITH LONG-ESTABLISHED NORTH AMERICAN CUSTOM. UNLESS IT IS SPECIFICALLY STATED OTHERWISE GOLD AND SILVER VALUES REPORTED ON THESE SHEETS HAVE NOT BEEN ADJUSTED TO COMPEN SATE FOR LOSSES AND GAINS INHERENT IN THE FIRE

ASSAY PROCESS

BELL-WHITE ANALYTICAL LABORATORIES LTD.

32D84SE9001 2.15168 MCFADDEN 300

Ontario

Ministry ofNorthern Developmentand Mines

Ministere du Developpement du Nord et des Mines

February 21, 1994

Geoscience Approvals Office 933 Ramsey Lake Road 6th Floor Sudbury, Ontario P3E 6B5

Telephone: Fax:

(705) 670-5853 (705) 670-5863

Our File: 2.15168 Transaction #: W9380.00247

Mining RecorderMinistry of Northern Developmentand Mines4 Government Road EastKirkland Lake, OntarioP2N 1A2

Dear Sir/Madam:

Subject: APPROVAL OF ASSESSMENT WORK CREDITS ON MINING CLAIMS L1180059 ET AL IN MCGARRY b MCFADDEN TOWNSHIPS

The deficiencies in the original submission have been rectified.

The assessment work credits for Geology, Section 12 of the Mining Act Regulations, have been approved as outlined on the original submission.

The approval date is February 11, 1994.

If you have any questions regarding this correspondence, please contact Lucille Jerome at (705) 670-5855.

Yours sincerely,

Ron C. GashinskiSenior Manager, Mining Lands Section Mining and Land Management Branch Mines and Minerals Division

-LJ/jl Enclosures:

cc: Resident GeologistKirkland Lake, Ontario

'Assessment Files Library Toronto, Ontario

rvilnlstry ofNorthern Development

Ontario

Report of Work Conducted After Recording Claim

([Q Mining Act

Number

Personal information collected on this form Is obtained under the authority of the Mining Act. This Information will be used for correspondence. Questions about this collection should be directed to the Provincial Manager, Mining Lands, Ministry of Northern Development and Mines, Fourth Floor, 159 Cedar Street, Sudbury. Ontario, P3E 6A5. telephone (705) 670-7264. i ^ i X ^S

Instructions: - Please type or print and submit In duplicate. *~ * " ^"^- Refer to the Mining Act and Regulations for requirements of filing assessment work or consult the Mining

Recorder.- A separate copy of this form must be completed for each Work Group.- Technical reports and maps must accompany this form in duplicate.- A sketch, showing the claims the work is assigned to, must accompany this form.

Recorded Holders) Client No.

P.O . rt^vilng Division

/fe*//^/Township/Area M or Q Plan No.

GMinfnfl

t J" c*

,

G 32 /rWork Performed

From: /?*""X? i f i

To: OC -f-*ft

Work Performed (Check One Work Group Only)Work Group

Geotechnical Survey

Physical Work, Including Drilling

Rehabilitation

Other Authorized Work

Assays

Assignment from Reserve

Type

bt*OMO)\^ t^Jrlicdo/L MlvPAal ^fJM0flV(^

^ ___ j^X **^ 1 \ f ^J i

RECEIVED

* OCT06 1993 .T *;MINING LANDS BRANOI 1

t J

Total Assessment Work Claimed on the Attached Statement of Costs 236? 16Note: The Minister may reject for assessment work credit all or part of the assessment work submitted if the recorded

holder cannot verify expenditures claimed in the statement of costs within 30 days of a request for verification.

Persons and Survey Company Who Performed the Work (Give Name and Address of Author of Report)Name Address

P.O. /lv* /9/ •.^g-y X**

(attach a schedule If necessary)

Certification of Beneficial Interest * See Note No. 1 on reverse side

l certify that at the time the work was performed, the claims covered in this work report were recorded in the current holder's name or held under a beneficial interest by the current recorded holder.

Date Recorded Holder or Agent (Signature)

Certification of Work Reportl certify that l have a personal knowledge of the facts set forth in this Work report, having performed the work or witnessed same during and/or after Its completion and annexed report Is true.

Name and Address of Pereon Certifying

Certified By (Signature)

Deemed Approval Date

'^ Date Notice for Juhendmems Sent

Date Approved f

d3 OC1 H PPI .ll 100241 (03/81)

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Not

e 2:

If

wor

k ha

s be

en p

erfo

rmed

on

pate

nted

or

leaa

ed la

nd,

plea

ae c

ompl

ete

the

follo

win

g:

l cer

tify

that

the

rec

orde

d ho

lder

had

a b

enef

icia

l Int

eres

t In

the

pate

nted

or

leas

ed la

nd a

t the

tim

e th

e w

ork

was

per

form

ed.

Sign

atur

eDa

te

WORK COMPLETED

Geological mapping

Sampling

STATEMENT OF COSTS

DAYS RATE TOTAL

45 days S 250.00 SI 1250.00

4 days S 250.00Helper! 150.00 S1600.00

lDOCUMENT No '9380* 00241

Report Writing

Map Preparation

Room 81 Board

12 days S 250.00 S 3000.00

6 days S 250.00 S 1500.00

4 months S 500.00 S 2000.00

*, Transportation 96 km./day x 49 days x 0.35/km. S1646.00

Consulting Fees S 2000.00

Supplies S 500.00

Assaying Gold samples S 120.00

Assaying indicator samples Results pending

Total to date

Certification Verifying Statement of Costs

l hereby certify:that the amounts shown are as accurate as possible and these costs were incurred while conducting assessment work on the lands shown on the accompanying Report of Work form.

that as A(Recorded Holder, Agenl. Position In Company)

to make this certification

Attestation de l'*tat des coQts

J'atteste par la prdsente :que les montants indiques sont le plus exact possible et que ces depenses ont 6te engagees pour effectuer les travaux devaluation sur les terrains Indiques dans la formule de rapport de travail cl-|olnt.

am authorized Et qu'ft litre de je suis autorisd(tttulalra enreglstre'. representant, posit occupa dans la compagnle)

faire cotte attestation.A.

OfttAMftl) Nota : Dam cetle formule. tonqu'il deslgne

REFERENCESAREAS-WITHDRAWN FROM DISPOSITION

M.R.O. -j MINING RIGHTS ONLY

S.R.O. - SURFACE RIGHTS ONLY

M.+ S. - MINING AND SURFACE RIGHTS

Datcription Order No. Dtt* Deposition FHe

67) Surface Rights Withdrawn from ^ Stoking, ^action 36/80 ord*r N

, Surface and MininStaking, section 3

i Rights Withdrawn from ./BO order No,1 " "* s

j7\ Surface and Mining Rights Withdrawn from -^Staking, section 36/80 order Mn U/ i m**

j Surface and Mining Rights Withdrawn from Stoking, section 36/80 order NoV-Hlli 0/57/87 Opens Part of W/38/Sb

0/63/87 Opens Part of W/38/85 0-L4*-*o NR nurr or ww/ee

Surface and Mining Rights Withdrawn^f/om Staking, section 36/80 order N 0/64/B7 Opens Part of W/8/86O L4/S9 OPENS P*RT OF W8/86

3) Surface and Mining Rights Withdrawn -'Stoking, section 36/80 order No.bt

m

PART E^ RE OPENED BY

D^) Surface omLMIning Rights Withdrawn from ^Staking, section 36/80 order NokOiZti.

PWT © REOPENeo w W*0*" "O. O-LKJ/89 NR PART g) REOPENED BY ORDER NO. t)-LW89 NR

*g\ Surf ace and Mining Rights Withdrawn from ^Staking, section 36/80 order Nokft/fti -

0/33/86 Opens Par! of W/9/86 0/65/67 Opens Port of W/9/86O-Lee-90 NR OPEN8 PMTT OF W9/8C, MOV CI/90

0-L32-9O NR OPENS PART Of W8/86

DECEMBER (4, 1990

THE INFORMATION THAT APPEARS ON THIS MAP HAS BEEN COMPILED FROM VARIOUS SOURCES, AND ACCURACY IS NOT GUARANTEED. THOSE WISHING TO STAKE MIN ING CLAIMS SHOULD CON SULT WITH THE MINING RECORDER, MINISTRY OF NORTHERN DEVELOP MENT AND MINES, FOR AD DITIONAL 4NFORMATION ON THE STATUS OF THE LANDS SHOWN HEREON.

MCGARRY TWP.

L ^Larder \

LA3jptjtf^2\is.j.l.-ls --lo-ns.or' V/p !

Hannigan Bay

1186537

r̂ **|MllB6536 - p

RATTRAY TWP.ARCHIVED

ai/ o-c.

LEGEND

HIGHWAY AND ROUTE No.

OTHER ROADS

TRAILS

SURVEYED LINES:TOWNSHIPS. BASE LINES, ETC.LOTS. MINING CLAIMS, PARCELS, ETC.

UNSURVEYED LINES:LOT LINESPARCEL BOUNDARYMINING CLAIMS ETC.

RAILWAY AND RIGHT OF WAY

UTILITY LINES NON-PERENNIAL STREAM

FLOODING OR FLOODING RIGHTS SUBDIVISION OR COMPOSITE PLAN RESERVATIONS ORIGINALSHORELINE MARSH OR MUSKEG MINES TRAVERSE MONUMENT

DISPOSITION OF CROWN LANDS

TYPE OF DOCUMENT SYMBOL

PATENT. SURFACE S MINING RIGHTS™...—..*..— *

" .SURFACE RIGHTS ONLY...————._.T.r...... 9

" .MINING RIGHTS ONLY ^...................w. Q

LEASE, SURFACE A MINING RIGHTS-..——..—.—— M

" .SURFACE RIGHTS ONLY._.....^......™...-.. B" , MINING RIGHTS ONLY-..——,.—^......fc——. Q

LICENCE OF OCCUPATION .__....................1..— TORDER-tN COUNCIL ............................,....™ OC

RESERVATION . ...M......._......——..-..........— ©CANCELLED ...—....................,.............™ ®SAND 4 GRAVEL ..........._............m ......"...

NOTE: MINING RIGHTS IN PARCELS PATENTED PRIOR TO MAY 6, 1913, VESTED IN ORIGINAL PATENTEE BY THE PUBLIC LANDS ACT. R S.O. 1970, CHAP. 380. SEC 63. SUBSEC 1

SCALE: 1 INCH = 40 CHAINS

L C C JC4

FEET10OO 2OOO 4OOO 6OOO 8OOO

O 2OO* METRES

1000li KM;

2000{2 KM)

TOWNSHIP

MCFADDENM.N.R. ADMINISTRATIVE DISTRICT

KIRKLAND LAKEMINING DIVISION

LARDER LAKELAND TITLES/ REGISTRY DIVISION

TIMISKAMING

MinistryofNatural

Ontario

LandManagement

Branch

Dati JANUARY 1985Number

6-3215

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