KA| Kian A. JensenIB* Exploration and Consulting Services

42A85SE0117 Z . 11846 DENTON 010

ELECTROMAGNETIC SURVEY

for

KEEFER LAKE RESOURCES INC,

on the

DENTON PROPERTY

in

DENTON TOWNSHIP

PORCUPINE MINING DIVISION

DISTRICT OF COCHRANE

ONTARIO

by

Kian A. Jensen Consulting Geologist/Geophysicist

November, 1988

Kian A. JensenExploration and Consulting Service

42ABSSE8117 a.11846 DENTON 010C

Table of Contents

PageTitle Page i Table of Contents li Introduction l Location arid Access 2 Property 2 General Geology 5 Previous Exploration Activities 6 Geophysical Survey 7

Introduction 7 Electromagnetic Survey 7 Interpretation 8

Conclusions 10 Recommendations 10 Certificate Appendix

List of Figures

Figure 1: Location Map 3Figure 2: Claim Map and Property Location Map 4Figure 3: VLF-EM Survey Profile Map folderFigure 4: Fraser Filtering folder

Kian A. JensenExploration and Consulting Services

INTRODUCTION

During October and November, 1987 and early February, 1988, linecutting was completed on the majority of the Keefer Lake Resources Incorporated property. This report pretains to 23 contiguous unpatented mining claims in Denton Township.

A total of 22.05 miles of linecutting was completed to establish a total of 942 electromagnetic readings on 17.83 miles of north-south grid lines. The survey was completed from September 7, 1988 to November 9, 1988, by the author. The data reductions, drafting, interpretation and report were completed by the author from November 10 to 15, 1988.

The project area is located approximately 12.5 miles (20 km) west of the junction of Highways 101 and 144. The claims cover the area from the township line to the creek draining into Godon Lake in the southwestern portion of Denton Township, Porcupine Mining Division, District of Cochrane, Ontario.

The purpose of the survey was to identify the conductors parallel to the local stratigraphy and the known structural features and to identify favourable areas in drift cover portions of the property for gold mineralization.

KA| Kian A. JensenExploration and Consulting Services

LOCATION AND ACCESS

The 23 unpatented mining claims cover the area from the township line to the creek draining into Godon Lake in the southwestern portion of Denton Township, Porcupine Mining Division, District of Cochrane, Ontario as shown in Figure 1.

The project area is located approximately 12.5 miles (20 km) west of the junction of Highways 101 and 144. On the east side of Warran Lake, a logging road leads south to southeasterly through Keefer Township to the southwest corner of Denton Township and the project area. A four wheel drive vehicle would be required to travel the road for a short distance. Further access is either by four wheel vehicle or walking.

Additional access from Denton Township approximately l mile west of Cripple Creek. This road can be travelled by four wheel vehicle on the southern route to southeast of Godon Lake.

PROPERTY

The portion of the Keefer Lake Resources Inc. holdings covered by this report consists of 23 unpatented mining claims as shown in Figure 2, and consists of the following mining claims and recording dates:

P-949904 to P-949916 inclusively Denton Twp. Nov. 12, 1986 P-949920 to P-949929 inclusively Denton Twp. Nov. 12, 1986

KA| Kian A. JensenW* Exploration and Consulting Services

Figure 1: Location Map for Keefer Lake Resources Inc., Keefer and Denton

Townships, Porcupine Mining Division, District of Cochrane, Ontario.

947*37 i 947*3* f 947*39

947*40 l 947*41 '947848

947*43 l 947*44 947*49

,-^ 9499**9*9*84-, 9499X8 1\-— — J——— — --*-.-

947*49 l 947*90 '.^947 949923 949926 i 949989 J9SO03^.^^. .

947*64, 847063 947892 947*93 \947•—— — " ~"*P^""i/

9499221949921 1949920

947*61 1947*62 -. ..'...j* - *. j 194991* '949919. 9,9003*

1947*90 A 947892 947W3 l 947*94

947*99 l 947060947*97 ' 947*98 947*99

,' DENTON TOWNSHIP/KEEFER TOWNSHIP

LOCATION MAP OF KEEFER LAKE RESOURCES INCORPORATED

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(AC- t-*5'

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KA| Kian A. JensenExploration and Consulting Services

GENERAL GEOLOGY

The bedrock in the area consists of an early Precambrian metavolcanic-metasedimentary sequence and has been intruded by granitic rocks.

The rock units strike in a northeast to east direction. The oldest rocks appear to be pale colour ultramafic flows which are intercalated with metasediments. In isolated areas these rocks grade into a massive flow consisting of serpentinized peridotitic komatite. These rock are overlain by basaltic komatite and/or Mg tholeiites. The above rocks are succeeded upwards by Fe tholeiite, calc-alkalic basalt, intermediate to felsic metavolcanics and clastic metasediments.

The intermediate to felsic metavolcanics consist of tuffs, breccia and foliated to massive flows. This unit grades into metasediments and clastic metasediments. Within isolated areas the metasediments contain a zone of chert and magnetite iron formation.

The above lithological units are intruded by gabbroic to dioritic rocks. The felsic intrusives appear to have three stages, being: quartz diorite to tonalite, porphyritic granodiorite and a medium grained granodiorite.

Metamorphism in the area is of the greenschist facies. Rocks near the late intrusive have been altered to a epidote amphibolite to amphibolite facies.

Intruding all the above lithological units are north to northerly trending diabase dikes.

The structure in the area appears to be dominated by north northwest trending transverse faults, several are filled by the later diabase dikes. Several northeast trending shear zones are located in the southern portion of Godon Lake.

Kian A. JensenExploration and Consulting Services

PREVIOUS EXPLORATION ACTIVITIES

A detailed description of the exploration activities and the various properties up to 1938 is given in the O.D.M. Report Volume 47, Part 4 , t itled "Geology of the Keefer-Eldorado Area" by W.D. Harding and L.G. Berry.

From 1945 to 1947, A. Phillips trenched and diamond drilled a sericite-carbonate schist zone located about l mile southwest of Godon Lake. In 1961 Paymaster Consolidated Mines Limited conducted a ground magnetic and electromagnetic surveys in the area. Results of sampling of the trenches returned values up to 0.07 o.p.t. of gold.

During 1971, Texas Gulf Sulphur Company Inc. and Conwest Exploration Company Limited were joint venture partners on the Galata property. They conducted an airborne survey over portions of Keefer and Denton Townships.

In 1972, Falconbridge Nickel Mines Limited conducted a magnetic survey without locating any significant anomalies.

In recent years, Frank Galata has trenched many areas of Keefer and Denton Townships. Most of the sites are quartz or quartz-carbonate veining.

The present exploration program of Keefer Lake Resources Inc. is to define gold bearing target by means of geophysical surveys, geological mapping, trenching, and diamond drilling.

KA] Klan A. JensenViP Exploration and Consulting Services

GEOPHYSICAL SURVEY

INTRODUCTION:

The linecutting was conducted by Guy Thibault Exploration Services of Timmins, Ontario, from October to early November, 1987. The tie line 20+00 South was extented from the original 14 claim group located on the west side of Kosher Lake in Keefer Township. The east trending base line within the property covered by this report extends from 100+00 East to 140+00 East. North-south grid lines were established at 400 foot intervals and picketed every 100 feet. A base line was established at 0+00 North on the Keefer-Denton Township boundary from Line 60+00 East "B" to Line 140+00 East.

A total of 22.05 line miles of grid was established within the boundaries of the 23 mining claims.

On completion of the linecutting, the author conducted a VLF-EM survey over the north-south grid lines from September 7, 1988 to November 9, 1988, utilizing a Phoenix VLF-2 unit. The data reductions, drafting, interpretation and report were completed by the author from November 10 to 15, 1988.

ELECTROMAGNETIC SURVEY:

The electromagnetic base station was established on the existing grid in Keefer Township and the horizontal field strength (HFS) was adjusted to compare to the original survey. The transmitter station used for the survey was Cutler, Maine, with a frequency of 24.0 kHz. The base line and the tie lines were surveyed in a looping fashion at establish accurate control tie-ins for each grid line. The north-south grid lines were then surveyed with readings being observed every 100 feet.

The data was corrected for the daily fluctuations of the HFS and the tie-ins at the control stations.

The corrected data was plotted on a base map with a scale of l inch to 200 feet (1:2400) with the dip values being profiled as shown in Figure 3. The dip data was filtered by a low pass Fraser Filtering and contoured as shown in Figure 4.

Kian A. JensenExploration and Consulting Services

INTERPRETATION:

The VLF-EM survey located many anomalies which appear to form at least 14 trends and several smaller isolated anomalies.

1) L79E and L88E North boundary of mining claimsThis anomaly appears to be trending in a easterly direction

with an increase of the HFS from 90* to 200*. the central area of the anomaly is bisected by two suspected NNW trending diabase dikes. The cause of the anomaly may be sulphide mineralization which may have be remobilized by the dikes in a blackish fine grained graphitic (?) argillite.

2) L128E at 55N to L140E at 47NThis SE trending anomaly has an increase of 20* to 65* in

the HFS and may be due to a shearing of the granitic intrusive, the eastern portion is offset by a northerly to NNW trending diabase dike on Line 136 East.

3) L120E at 43+50NThis one line anomaly with an increase of 60* in the HFS

lacks further information due to the lake on the west side. It appears terminated by the NNW diabase dike between L120E and L124E. The cause of this anomaly may be shearing within the granitic intrusive.

4) L100E at 28+50N to L104E at 31+50NThis anomaly with an HFS increase from 110* to 130* and

trends in a NE direction is located on the north side of a slight magnetic anomaly. The cause may be due to a narrow diabase dike filling a shear zone. The northeastern portion is lacking due to the lake.

5) L108E at 17N to L112E at 17+50NL120E at 26+50NL128E at 28+50N to L140E at 24+50N

This anomaly trend which is associated with a magnetic low, has an increase in HFS from 200* in the western portion within the suspected metavolcanics to a 50* in the eastern portion within the granitic intrusive. The cause is probably related to shearing and sulphide mineralization within the metavolcanic tuffs and a continuation of the shearing within the granite. The three sections appear to be offset by NNW trending diabase dikes in the area of L120E and between L124E and L128E.

6) L128E at TL 23NThis anomaly is located on the east side of a NNW trending

diabase dike.

Kian A. JensenExploration and Consulting Services

7) L100E at 3N to L116E at 2+50NL120E at 8 + 50N to L124E at 7 + 75NL128E at 11+50N to L140E at 10+50N

This anomaly trend which is associated with a background to slightly low magnetic anomaly, has a HFS increase of 20(^ in the western part within the vocanic tuffs to a 2(^ within the granitic intrusive in the eastern part. The cause of the anomaly in the western part is probably due to shearing and sulphide mineralization within the volcanics. The eastern part may be due to either shearing in the granite or an overburden effect. It appears that there may be a branching of the anomaly just south of the Base Line on L112E. The trend is bisected by NNW trending diabase dikes near L120E and between L128E and L132E.

8) L116E at 4S to L136E at 3+50SThis weak trend has a HFS increase of about 3(^ and appears

to be related to the edge effects of the NNW trending diabase dikes.

9) L104E at 8-150S to L108E at 9 + 50SThis anomaly which has a HFS increase of 4(^ 7 is associated

with a magnetic high and may be due to a narrow chemical metasediment iron formation.

10) L100E at 16+50S to L112E at 15SThe trend has a HFS increase of 10(^ in the west to 45% in

the east. This is associated with a very high magnetic anomaly and may be due to sulphide mineralization or intense shearing within an easterly trending gabbroic intusive. This anomaly was also located by the recent airborne magnetic and EM survey by the O.G.s.

11) L112E at 11+50S to L128E at 14SThis trend generally has a HFS increase of 1(^ to 2(^ with

the exception on L116E which increases 7(^. It is associated with a high magnetic anomaly suspected to be a narrow chemical metasediment iron formation in the west and the NNW diabase dikes cause affect the interpretation in the eastern part. The portion of the anomaly on L116E may be a northerly faulted portion of anomaly No. 10.

12) L136E at 9+50SThis is associated with a very high magnetic anomaly which

is suspected to be related to a NNW trending diabase dike.

13) L120E at 17S to L132E at 18+50EThis anomaly is associated with a background to high magneic

trend associated with a. NNW diabase dike. The cause may be due to possible overburden effects and/or shearing.

14) L136E at 22+50S to L140E at 22+50SThis anomaly has an increase in the HFS by 5% to 10% and is

suspected to be related to the overburden effects.

Kian A. JensenExploration and Consulting Services

CONCLUSIONS

The VLF-EM survey was successful in locating 14 anomaly trends which are probably caused by either bedrock anomalies possibly due to either sulphide mineralization, structural features, possible remobilized sulphides associated with NNW trending diabase dikes or the effects of the overburden. Some of the structural features located by this survey were not that apparent from the previous total field magnetic survey.

The more prominent anomalies are suspected to be sulphide mineralization related to the general east-west shearing and the highest HFS of the individual trends are generally within the areas of metavolcanic bedrock.

It appears that anomaly No. 14 was previously detected by the recent O.G.S. airborne surveys.

The VLF-EM survey has revealled that the structural history is very complex and the author has attempted to connect the anomalies which have possible offsets by diabase filled faults.

RECOMMENDATIONS

Based upon the results of the present survey and the available information, the author recommends a limited amount of prospecting, and geological mapping of the property. The areas of importance for gold mineralization is in the vicinity of the magnetic lows in areas of suspected shear zones. The ultramafic intrusive may be host to base metal mineralization.

Based upon the results of the recommended work, minor trenching may be warranted and possibly a limited diamond drilling program.

Dated at Timmins, Ontario November 15, 1988

Respectf

Kian A. Consult in st/Geophysicist

Kian A. JensenExploration and Consulting Services

CERTIFICATE

With reference to my report on the Electromagnetic Survey on the Godon Lake Property of Keefer Lake Resources Inc. Dated November 15, 1988 ............

I, Kian A. Jensen, of the City of Timmins, Ontario, do hereby certify the following to be true and accurate to the best of my knowledge:

1) That I received an Honour B.Se. degree in Earth Science, Geology Major, from the University of Waterloo,

2) That I have been employed as a geologist and/or geophysicist by various exploration companies and consulting companies since 1978,

3) That I have been and still am a member in good standing in the following associations:

a) Society of Exploration Geophysicists - Associate, 1981b) Geological Association of Canada - Fellow, 1983

4) That I am the author of the corresponding report, and have been actively exploring and prospecting in the Timmins area since 1981,

5) That I have no interest directly or indirectly in the mining claims comprising the property described in this report or in the shares of any company or companies in this joint venture on this property or the surrounding properties, nor do I expect to receive any directly or indirectly.

Dated this15th of November, 1988Timmins, Ontario

Kian A. Jereeni*^.Se.Consulting Geologist/Geophysicist

Electromagnetic Unit

Lightweight, low battery drain, rugged, simple to operate

Two independent channels

Each channel may select any station between 14.0 and 29.9 kHz

Single crystal used for all frequencies

Locking clinometer provides tilt-angle memory

Superheterodyne detection and digital filtering provide extremely high selectivity and noise rejection

Military and time standard VLF transmitters are distributed over the world. These stations are used for geophysical EM surveying thus eliminating the need for a local trans mitter and permitting one-man operation.

To ensure that a station excites the prospec tive conductor, two stations at approximately right angles are used during a survey (see data on back).

The choice of 160 frequencies in the range 14.0 to 29.9 kHz permits the use of a local EM trans mitter when no suitable regular VLF station is available.

PHOENIX GEOPHYSICS LIMITEDGeophysical Consulting and Contracting. Instrument Manufacture. Sale and Lease.

Head Office: TORONTO 200 Yorkland Blvd., Wiltowdale, Ontario Canada M3J 1R5* Tel (.416)493-6350 Telex: 06 986856" Cable: PHEXCO TORONTO

VANCOUVER ?14 - 744 Well Mailings Street, Vancouver, B.C. Canada V6C 1 A8 let: (604) 669 1070

DENVER 5590 Havana St.,Denver, Colorado, 80239, U.S.A.Tel: (303) 371-2980 ' Telex: 00-450690

SpecificationsParomeJfeMeasured

Frequency Selection, Front Panel

Orientation and magnitude of the major and minor axe* of the ellipse of polarization.

Dual channel, front panel selectable (FI or F2) each with independent precision l O-torn dial gain control.

Frequency Selection, Internal : FI and fi can be selected by Internal switches within the ronae 14.0 to 29.9 kHz in 100 Hz Increments.

Detection And Filtering

Meter Display

Audio

Clinometer

Battery

Temperature Range

Dimensions

Weight

: Superheterodyne detection and digital filtering provide omuch narrower bandwidth and thus greater rejection ofInterfering stations and 60 cycle noise than conventionalreceivers.

: 2 ranges: 0 to 300 or 0 to 1000. Background Is typically set at100. Meter Is also used as dip angle null Indicator and batterytest.

: Crystal speaker. 2500 Hz used os null Indicator.

i +90 0 , + 0.5" resolution. Normal locking, push buttonrelease.

i One standard 9v transistor radio battery. Average lifeexpectancy - 1 to 3 months (battery drain Is 3 mA)

: -40" to * 60 0 C.

: 8 x 22 x 14 cm (3 x 9 x 6 Inches).

! 850 grams (1.9 pounds).

All of the established stations may be selected, or alternatively, alocal VLF transmitter may be usedwhich transmits at any frequencyIn the range 14.0 to 29.9 kHz.

VLF Station Frequency(kHz)

Bordeaux, France 15.1Odessa (Block Sea) 1 5.6Rugby, U.K. 16.0Moscow, U.S. S. R. 17.1Yosamai, Japan 17.4Hegalond, Norway 1 7 .6Molobor, Java 19.0Oxford, U.K. 19.6Paris. France 20.7Annapolis, Maryland 21.4Northwest Cope, Australia 22.3Lauluolel, Hawaii 23.4Buenos Aires, Argentina 23.6Cutler, Maine 24,0Seattle, Washington 24.SRome. Italy 27.2Aguada, Puerto Rico 28.5

Field DataThe results below illustrate the need for using two orthogonal stations when the strike of the prospective conductor is not well-known. The dip angle and amplitude data measured using station NLK In Seattle, Washington, show only a very weak anomaly associated with the two conductive sulphide zones at Cavendish, Ontario.

The results obtained using Cutler, Maine reveal a more prominent anomaly, but the best response was obtained using Annapolis, Maryland since the station lies almost due south and the transmitted electromagnetic field is thus maximum-coupled with the North-South trending conductors.

PHOENIX GEOPHYSICS LIMITED

VLF-RADIO EM SYSTEM LINE C CAVENDISH TEST AREA

J) WEST OIP,0e*ST DIP

5)NORTH DIP, SOUTH DIP

Station NS5 Annopolii, Md

Stolion NAACulltr, Moinl

Station NLK 8*ollH, WolNngKm

f x*—x Ministry of Report of WorkNorthern Developmentand Mines {Geophysical, Geological,i. bntlano

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ULof Survey(s)

Geochemical and Expenditures)

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Type of

VLF- (rClaim Holder(s)

Address

S u R*J e y o?.//*^900

Township or

rffOC,

-T CUPr'i Lir.oru;*? No.

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X 7"2.,Survey Company

ft- CC.NSUCX-Name and Address of Author (of Geo-Technical report)

p.p.

Jo- e.ny ,Date of Survey (frprn 61 t o)O7 09 ^31 O9 I Ipay l Mo. l Yr. j Day | Mp. | Yr.

, t- O c- (/COTotal Miles of line Cm

POMCredits Requested per Each Claim in Columns at rightSpecial 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

MOVlOBBft3tz4P** ''ft)

Airborne CBedEs/^ C \ \f

Note: Special provisions

to Airborne Surveys.

MINING LANDS SE

Geophysical

- Electromagnetic

- Magnetometer

- Radiometric

- Other

Geological

Geochemical

Days per Claim

L..-

Geophysical

- Electromagnetic !

- Magnetometer

- Radiometric

Days per Claim

- Other

Geological

eochemical4ID Days pe'

Claim

Electr oruagnctic

Magnetometer

Expenditures (excludes power stripping)

Mining Claims Traversed (List in numerical sequence)

Typ* of Work Performed

Performed on Claim(s)

Calculation of Expenditure Days Credits

Total Expendituresiot.il

tXiys C'ccfiis

InttructiontTotal Days Credits may be apportioned at the claim holder's choice. Enter number of days credits per claim selected In columns at right.

Date Recorded Holrii o/ Agent (Signatuiel

Certification Verifying Report of Work

Mining Oaim Prefix l____Number

RECORDEDi

NOV 1 O

1ol.ll mtmher of mini claims covered hy this report of work.

For Office Use OnlyTotal Days C'. Recorded

Date Approved as Recorded

l hereby certify that l have a persona! and intimate knowledge of the facts set forth in the Report of Work annexed hereto, having performed the woik or witnessed same during and/or after its completion and the annexed report is true.Name and Postal Address of Person Certifying

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1362 I85H2)

Ministry ofNorthern Development

MinesOntario

Technical Assessment Work Credits

Date

January 31, 1989

File

2.11846Mining Recorder^ Report ofWork Sl8806-50142

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Recorded Holder

Keefer Lake Resources Inc.Township or Area

Denton TownshipType of survey and number of

Assessment days credit per claimGeophysical

20flactrnmagnetir " days

Magnetnmator riayc

Radiometrir days

Other days

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

Geological days

Geochemical days

Man days Q Airborne O

Special provision Ixl Ground QJ

|~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.

Mining Claim* Asseoed

P 949908-09 949912-13 949915-16 949920 to 29 inclusive

i

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

10 days 15 days

P 949904-05-06 P 949907 949910 949911 949914

Yo credits have been allowed for the following mining claimsQ not sufficiently covered by the survey [D 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.

28 (85/12)

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

(416) 965-4888

Your File: W8806-50142 Our File j 2.11846

March l, 1989

Mining RecorderMinistry of Northern Development and Mines60 Wilson AvenueTimmins, OntarioP4N 2S7

Dear Sir:

RE: Notice of Intent dated January 31, 1989Geophysical (Electromagnetic) Survey on Mining Claims P 949904 et al in the Township of Denton.

The assessment work credits, as listed with the above-mentioned Notice of Intent, 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 Manaqor, Mining LandsMines 6 Minerals Division

Encls:

AB: se

cc: Keefer Lake Resources Inc. P.O. Box 72 160 King Cross Drive King City, Ontario LOE 1KO

cc: Mr. G.H. FergusonMining fit Lands Commissioner Toronto, Ontario

cc: Mr. Kian A. Jenson P.O. Box 37South Porcupine, Ontario PON 1HO

cc: Resident Geologist Timmins, Ontario

REFERENCES

AREAS WITHDRAWN FROM DISPOSITION

M.R.O.-MINING RIGHTS ONLY

S.R.O. -SURFACE RIGHTS ONLY

M.+ S. - MINING AND SURFACE RIGHTS

Daicnption Order No. Data Disposition Fil*

j) SLC n i,/70 F EB. 3(66 " * S. 171506

, OAN(H Jv-'-^ SIC

AND JOWSEY PARK RCSERVE 3. H, O

36/80 w 66/83 NOV. 18/83 M. B. O,

RESERVED FOR PUBLIC USE s.R.o.

X*.w. 9f/** s.*.*.

APPLICATION FOR CROWN LAND.

SAND AND GRAVEL

(6,) M.T.C.

(*2) M,T. C,

(jjj) M.T.C

W*) M T. C.

PIT 1417

PIT 1236

PIT 1470

PIT 1331

FILE 12*351

FILE 126531

UOEflS THIS TOWNSHIP LIL'S WITHIN THfc^JHUNlCIPALITYOF Tliti CITlf OF TIMMINS.

T.1PORTANT NOTICE

•I'll l S TDWNSUIP t'Oi;MS PART OK THE WAFBRBOARD FOREST

THE 1985/86 ANNUAL PLAN, ON FILE IN Tile: MINING RECORDER'S OFFICE, SHOWS THE ARKAS TO BE AFFECTED IH THL NtIXT VSAR.IF THIS PLAN AFFelCTS YOU, FURTHER INFORMATION MAY BE OBTAINED r ROM i

MR, MALCOM KILGOUR,UNIT FORESTER,

MINISTRY OF NATURAL RESOURCES,

896 R iverside Drive,Timmins . Ontario

Tali 705-267-7951

or4 Mr. Pierra Corbell,

Waferboard G roup

Tell 705-268-1462

42A05SE0M7 2.11846 DENTON 200i-

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REYNOLDS TWP. O UJ

LEGENDHIGHWAY 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 ORIGINAL SHORELINE MARSH OR MUSKEG MINES TRAVERSE MONUMENT

DISPOSITION OF CROWN LANDS

TYPE OF DOCUMENT SYMBOL

PATENT, SURFACE ft MINING RIGHTS..—-..........-. *

" .SURFACE RIGHTS ONLY.—......_........... O, MINING RIGHTS ONLY ..._................^ O

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

" .SURFACE RIGHTSONLY.-,............,......—. H

" .MINING RIGHTS ONLY...™.——————....—., yLICENCE OF OCCUPATION .._..—......—.........^ T

ORDER IN COUNCIL ..................................__ OC

RESERVATION ..———,..___......................._. ©

CANCELLED ___.......___—..—————............ ®

SAND 61 GRAVEL ...———..__..............—......... ©

NOTE: M INING RIGHTS IN P ARCELS PATENTED P RIOR TO MAY 6. 1913, VESTED I N ORIGINAL PATENTEE B Y THE PUBLIC LANDS ACT. R.S.O 1 970. CHAP. 380, SEC 03, BUBSEC 1.

SCALE: 1 INCH ^ 40 CHAINS

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TOWNSHIP

DENTON DEC * 11988

M.N.R. ADMINISTRATIVE DISTRICT

TIMMINSMINING DIVISION

PORCUPINELAND TITLES/ REGISTRY DIVISION

COCHRANEMinistryof LandNatural ManagementResources Branch

Ontario

Dili MARCH, 1985

G-3224

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