42A89SWe885 8.5320 BEATTY 010

VLF GEOPHYSICAL ELECTROMAGNETIC

SURVEY

CLAIM L 578332

BEATTY TWP., ONTARIO

by

JOHN T. WARD, P.Eng,

RECEIVED

.- -

MINING ̂ AM&S' SiCTION

December 31, 1981.

ABSTRACT

A Crone VLF electromagnetic survey was completed on Claim L578332 Beatty Twp by the writer in the fall of 1982. Very weak electromagnetic responses obtained in the central south half of the claim lend support to the presence of possible fault structures indicated by the 1981 magnetic survey of the claim by the writer.

ADDENDA

A Geonics EM 16 VLF electromagnetic survey was completed using the same VLF station on the same lines April l, 1983 to upgrade the data. The resurvey included 3 extra lines decreasing survey line spacing to 200 feet.

INDEX 42A09SW0085 2.5320 BEATTY 010C

PAGE

ABSTRACT

PROPERTY LOCATION, ACCESS l

GEOLOGY, PREVIOUS WORK l

GEOPHYSICAL SURVEY 2

INTERPRETATION 2

CONCLUSIONS AND RECOMMENDATIONS l

CERTIFICATION k

FIGURES

1) KEY MAP Scale l" = 1/2 mile

2) RADEM VLF SURVEY, TILT ANGLES, MINIMUM FIELD STRENGTH Scale l" r 100'

3) GEONICS VLF SURVEY 96 GRADIENT AND PHASE ANGLE IN DEGREES Scale l" s 100'

4) GEONICS VLF SURVEY AND EMI6R RESISTIVITY TEST. FRASER CONTOURS, APPARENT RESSISTIVITY OHM METRES AND RESISTIVITY PHASE IN DEGREES Scale l" r 100'

VLF GEOPHYSICAL ELECTROMAGNETIC SURVEY

CLAIM L578332 BEATTY TWP., ONTARIO

PROPERTY, LOCATION, ACCESS

Claim L578332, situated in Beatty Township, Larder Lake Mining Division is an unpatented mining claim recorded in the name of Dohn T. Ward, 9 Willamere Drive, Scarborough, Ontario and covers the SE l/* S 1/2 of Lot 2, Concession 1.

The property south boundary is paved highway 101, seven miles east of the town of Matheson and is accessible by automobile year round.

The claim is totally covered by thick mossy muskeg with extremely sparsely scattered small tamarck and black spruce.

GEOLOGY, PREVIOUS WORK

Beatty Township was mapped by J. Satterly and H.S. Armstrong in 1945 and reported in the 56th Annual Report O.D.M. Vol. LVI part VII 19*7. Although no outcropping exists on the claim it is expected that the property is underlain by

Archean metasediments, (arenite, argillite, feldspar porphyry, lamprophyre) and possibly intermediate volcanics. Gold mineralization in the general area has been found in fault structure related quartz veining.

The. property was surveyed magnetically by fluxgate magnetometer in 1975 by Canadian Johns Manviile Co. Ltd. however the 20 gammas sensitivity was not sufficient to allow mapping of bedrock structure. A vertical coil 1000 H~ E.M. survey at the same time was also too insentivie to detect fault structures. Canadian Dohns Manviile also carried out biogeochemical testing of the surrounding claims in 1972 but no suitable vegetation for their tests existed on

the claim covered by this report.

A detailed l gamma sensitivity total field magnetic survey was completed by the writer in 1981 which indicated the presence of a N 20 0 W fault cutting centrally

through the property.

-2-

^GEOPHYSICAL SURVEY

This survey was completed using a Crone VLF RADEM system on lines cut at 200 foot intervals and picketed at 100 foot intervals. Survey station spacing was 50 foot intervals along lines spaced at 400 foot intervals.

Tilts angle readings were taken facing southward perpendicular to the NAA station direction. Total field maxima and minima were both taken and recorded at each station. Readings were recorded at 800 units background and later converted to percent total field strength through multiplication by the constant

0.125. Results are presented on a scale of l" - 1 00 feet.

On March 31st 1983 and April 1st 1983 the above survey was repeated using a G comics EM 16 system repeating the same stations and adding three additional detail lines. This work is further discussed in a report (File No. L578332) by the writer dated June 6th, 1983 describing a VLF survey of claim L578332 using the VLF station Maryland over 50 foot station intervals along 200 foot interval east- west traverses. Test traverses with Geonics EM16R system were carried out on lines 1W and 4N March 31st, 1983 to demonstrate that such work is feasable using steel electrodes through the snow into frozen ground.

INTERPRETATION

The tilt angles are extremely low and verification with other electrical type surveys was required to give confidence in interpretability of the data. At 12+75 north line 1W the presence of a subsurface narrow very weak conductor is indicated by the RADEM, EM 16 and EM16R surveys. A roughly 500 foot wide zone of lower resistivity (40 ohm metres against a host rock background of 80 ohm metres) is also indicated striking north 70* westerly through the centre of

claim L578332 by:

1) lower apparent resistivities on EM16R TEST LINES,

2) 2596 to 5096 Minimum field strength RADEM nulls

3) weak EM16 reverse guadrature conductor axis responses along the north-east side from 10+OON line 1W to 11+25N line 13W and along the south side from 5+OON line IW to 5+75N line 5W and from 5+OON line 9W to 5+75N line 13W.

-3-

IDisplacement of conductivity responses is clearly evident at the N20 0 west trending fault interpreted magnetically to transect the property (see assessment file report by writer April 1982).

CONCLUSIONS AND RECOMMENDATIONS

Although the VLF tilt angles were no larger than the usual noise level of VLFsurveys they showed coincidence between surveys and survey instruments. The *-a. '^-o^o

to 5096 minimum signal strengths at the tilt angle nulls of the RADEMsystem showed coincidence with a 500 foot wide 5096 decrease in apparent resistivity indicated by two EM16R test traverses later run on March 31st, 1983. Displacement of the weak reverse quadrature EM16 axes by the 1982 magnetically interpreted fault indicates that these weak VLF responses are bedrock related.

It is recommended that EM16R survey work be compleJ0cW**4he fall of 1983 to fully map all conductive features of the property.

December 31, 1982 Amended 3une 3rd, 1983

4.

CERTIFICATION

I hereby certify that all the work covered by this report was

carried out by myself and under my direct supervision. I further

certify that I have been engaged in geophysical mineral exploration

in Canada for most of the last 33 years as a geophysicist, contractor

and consulting engineer.

Former employment includes the position of Senior Geophysicist -

Barringer Research, Rexdale; Geophysicist - Derry Michener S Booth

Consulting Geologists; Geophysicist - Patino Mining Ltd., and that of

Self-Employed Consulting Engineer^j for the past 9 years.

December 31,1981. JOHN T. WARD, P.Eng.

CRONE GEOPHYSICS LIMITED

3607 WOLFEDALE ROAD, MISSISSAUGA, ONTARIO, CANADA.

Phone: 270-0096

FIELD STRENGTH meter

BATTERY test and "STEADY" or "KEYED" signal switches

INCLINOMETER

FIELD STRENGTH range switch

VOLUME CONTROL ON-OFF switch

STATION SELECTOR switch

BATTERY COMPARTMENT (inside)

CONDUCTOR DIRECTION ARROW SPEAKER

This is a rugged, simple to operate, ONE MAN EM unit. It can be used without line cutting and is thus ideally suited for GROUND LOCATION OF AIRBORNE CONDUCTORS and the CHECKING OUT OF MINERAL SHOWINGS. This instrument utilizes higher than normal EM frequencies and is capable of detecting DISSEMINATED SULPHIDE DEPOSITS and SMALL SULPHIDE BODIES. It accurately isolates BANDED CONDUCTORS and operates through areas of HIGH HYDRO NOISE. The method is capable of deep penetration but due to the high frequency used its penetration is limited in areas of clay and conductive overburden.

The DIP ANGLE measurement detects a conductor from a considerable distance and is used primarily for locating conductors. The FIELD STRENGTH measurement is used to define the shape and attitude of the conductor.

SPECIFICATIONS

Source of Primary Field: VLF Communication Stations 12 to 24 KHz

Number of Stations: 7 switch selectable

Stations Available: The seven standard stations are Cutler, Maine, 17.8; Seattle, Washington, 18.6; Collins, Colorado, 20.0; Annapolis, Md., 21.4; Panama, 24.0; Hawaii, 23.4; England, 16.0. Alternative stations which may be substituted are: Gorki, Russia, 17.1; Japan, 17.4; England, 19.6; Australia, NWC, 22.3 KHz.

Check that Station is Transmitting: Audible signal from speaker.

Parameters Measured and Means:(1) DIP ANGLE in degrees, from the horizontal of the magnetic component of the VLF field. Detected by minimum on the field strength meter and read from an inclinometer with a range of 800 and an accuracy of V4 0.

(2) Field Strength (total or horizontal component) of the magnetic component of the VLF field. Measured as a per cent of normal field strength established at a base station. Accuracy 2% dependent on signal. Meter has two ranges: O 30096 and O 60096. Switch for "keyed" or "F.S." (steady) signal.

(3) Out of Phase component of the magnetic field, perpendicular in direction to the resultant field, measured without sign, as a per cent of normal field strength. This is the minimum reading of the Field Strength meter obtained when measuring the dip angle. Accuracy 296.

Operating Temperature Range: - 200 to +110 0 F.

Dimensions and Weight: 3.5" X 7.5" X 10.5" 6 Ib.

Shipping: Foam lined wooden case shipping wt. 15 Ib.

Batteries: 2 of 9 volt: Eveready 216, Burgess 2U6, Mallory M-l604Average life expectancy 3 weeks to 3 months dependent on amount of usage.

Units Available on a Rental or Purchase Basis. Contract Services Available for Field Surveys.

CRONE GEOPHYSICS LIMITED3607 WOLFEDALE ROAD. MISSISSAUGA. ONTARIO, CANADA L5C 1V8

TELEPHONE: (416) 270-0096 CABLE: CRONGEO, TORONTO TELEX: 06- 961260.

Australian Branch: 244 Newbridge Road. MOOREBANK. N.S.W. 2170 Telephone: (02) 602-0937. Telex: 71-22922

INSTRUCTIONS FOR OPERATION OF THE RADEM VLP-EM RECEIVER

(1) Transmitter Stations

The VLF Communication Broadcast stations are positioned throughout the world. At present, 13 of these stations broadcast steadily except for maintenance periods usually of 1/2 to 1/3 days per week. The RADEM receives any 7 of these stations with selection by means of a switch. The usable range of the stations varies widely with power and transmission conditions but is usually between 1000 and 5000 miles. Two types of signals are broadcast "keyed" (on and off) and "frequency shift" (FM) .

A station should be selected that is located in the same direction as the regional strike. For example, if the geological strike is east-west then a station located east or west of the operator should be used. If in doubt of the geological strike two orthogonal stations should be read.

(2) Field Measurements

(a) Dip Angle of Resultant Field

This is the angle of inclination, measured from the horizontal in degrees, of the direction of the resultant VLF field. The VLF field is normally horizontal (O 0 dip) . The dip angle measurement is independant of the strength of the field and the gain setting of the RADEM receiver. When plotted on a profile the dip angles usually form a cross-over pattern above the conductor as with the standard vertical loop EM method.

To measure the dip angle the RADEM is first held with the instrument face horizontal and rotated until a null is obtained (visual minimum on the field strength meter and audio null) .

February 1977

Crone Geophysics Limited Radem

2

direction of the VLF field. The RADEM is then held vertically and tilted from right to left until another null is obtained. The instrument is held steady in this null position and the dip angle read from the in clinometer. Note that the arrow in CRONE points to wards the conductor if the arrow points north the dip angle is recorded as say 10 0 N. In making the dip angle measurement the Normal-K switch must be in the NORM position.

(b) Out-Of-Phase Measurement (Usually Not Measured)

The secondary field from a ground conductor often is not in the same phase as the primary field/ therefore the resultant field will have an out-of-phase component.

To measure the out-of-phase component as a percent of the normal primary field the volume control of the amplifier must be set up as a standard. This is achieved at a base station in a normal area. The Field Strength range switch is placed in the O - 300 position. The RADEM held with the face horizontal and the body ro tated until a maximum Field Strength reading is obtained. In this position the Volume control is adjusted until the meter reads "100". The Volume control is left at this setting until the base station is read again usually one to several hours later. The Out-Of-Phase reading is the minimum position of the Field Strength meter when the dip angle of the resultant field is being measured. It is read at the same time as the dip angle is being read with the RADEM in the vertical null position.

The Out-Of-Phase measurement is sensitive to a lower order of conductivity than the dip angle measurement. For this reason it is often not recorded unless very poor conductors are being sought.

(c) Horizontal Component of the Field Strength

This is simply the strength of the field in the horizontal plane. It is the maximum reading obtained from the Field Strength meter when the instrument is rotated in the horizontal plane. It is therefore at right angles to the null position. It is usually read after the dip angle measurement simply by holding the RADEM horizontal, the CRONE arrow pointing at right angles to the operator, and adjusting position for maximum reading in the horizontal plane.

Crone Geophysics Limited Radem

If the signal is keyed the Normal-K switch is moved to the "K" position for the field strength reading. It must be returned to the normal position for dip angle measurement.

The field strength of VLF stations drifts with time. This drift is particularly severe during sunrise and sunset periods. A base station should be established in a normal area and the RADEM adjusted to a Horizontal Field Strength of "100" on the "O - 300" scale by means of the volume control pot. This base or subsidiary base station should be read every one to two hours as in a magnetic survey.

Eraser's Method

Reference: Geophysics, Volume 34, No. 6, December 1969, "Contouring of VLF-EM Data"

This is a simple operation on the dip angle readings that more clearly defines anomalous areas. It requires a consistent reading interval usually 50' or 100'. It produces a survey in which the conductors are contoured much the same as a Horizontal Field Strength survey although lacking the detail possible with the Field Strength measurement.

Example of Field Sheet

Station Out-Of- Dip Angle Reading Field Strength Remark Phase-% Degrees Time Drift Corr.

lON-Base10+50NUN11+50N12N12+50N13N13+50N14N14+50NilON-Base

2200046600

002N6N

12N22N20N8NIS

12S

10010099

101102118185263247164

114

9:00:02:04:06:08:10:12:14:17:20

10:10

00

-1-1-2-2-2-3-3-4

-14

10010098

100100116183260244160

100

LakeLake

Road

X 1 Over

Crone Geophysics Limited RADEM VLF

- 4 -

Station Shut-Down Timetable, March 1982.

CUTLER, MAINE 17.8K Hz - Every Monday 1200 to 2000 UT (If holiday falls on Monday, maintenance will be performed on preceding Friday.)

SEATTLE, WASHINGTON 24. 8K Hz - Thursday 1600 to 2400 UT (During Daylight saving time 1500 to 2300 UT)

LAULUALEI, HAWAII 23.4K Hz - MaintenanceWednesday and Thursday 1700 to 0500 UT.

ANNAPOLIS, MARYLAND 21.4K Hz - Every Tuesday 1200 to 2000 UT.

NORTH WEST CAPE, AUSTRALIA 22.3 K Hz - Every Monday 0000 to 0800 UT.

RUGBY, ENGLAND 16.OK Hz - Everyday, 1300 to 1400 UT.

YOSAMI, JAPAN 17.4K Hz - First Thursday andFriday of month 2300 to 0900 UT, every other Thursday and Friday 2300 to 0700 UT.

List of Available Stations on the RADEM unit

Eastern S. Time

7 am to 3 pm

11 am to 7 pm

12 am to 12 pm

7 am to 3 pm

7 pm to 3 pm

8 am to 9 am

6 pm to l am

Code Letter

CMSWAMHEOFEMSODNCHNYJTJBA

Station and Location

Cutler, MaineSeattle, WashingtonAnnapolis , MarylandLaulualei, HawaiiBordeaux, FranceRugby, EnglandMoscow, RussiaOdessa (Black Sea)Exmouth, AustraliaHelgelend, NorwayYosami , JapanTokyo , JapanBuenos Aires , Argentina

Frequency

17. 8K Hz24. 8K Hz21. 4K Hz23. 4K Hz15. IK Hz16. OK Hz17. IK Hz15. 6K Hz22. 3K Hz17. 6K Hz17. 4K Hz20. OK HZ23.6K Hz

Call Sign

NAA NLK NSS NPM NWU CBR UMS EWB NWC JXZ NOT JG2AR

Temperature Effect

Temperature drift may cause the field strength meter to null well below the zero mark. This should be corrected by the screw adjustment below the "Normal" switch on the front panel. Adjust with the volume control pot at 0.

Batteries: Two of #216 Eveready 9 Volt - Life: 20 Hours continuous.

crt. 5/4/82

Report of Work(Geophysical, Geological, Geochemical and Expenditures)

Type of Survey(s)

J c:^ CNj

Th M. -The M m"

Cia7rrTHolder(s)

Address^c ATy fi ; C: ^ C

s.saae BEATTY(Township or Ar

' M '4

900

Prospector'i Licence No.

S K"60

urvey Company

_ ^ _ , .Name and Address of Author (of CSeo-Technical report)

T -

Date of Survey (from S to)

Day j Mo. j Yr. j Day J Mg^J^Yr.

SO/^^LC/Y

Total Miles of line Cut

Credits 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 and enter total(s) here

Airborne Credits

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

Geophysical

- Electromagnetic

- Magnetometer

- Radiometric

- Other

Geological

Geochemical

Geophysical

- Electromagnetic

- Magnetometer

- Radiometric

- Other

Geological

Geochemical

Electromagnetic

Magnetometer

Radiometric

Days per Claim

J2 (J

Days perClaim

Days per Claim

Mining Claims Traversed (List in numerical sequence)

Expenditures (excludes power stripping)Type of Work Performed

Performed on Claim(s)

Calculation of Expenditure Days Credits

Total ExpendituresTotal

Days Credits

4- 15

InstructionsTotal Dayi Credits may be apportioned .at the claim holder's choice. Enter number of days credits per claim selected in columns at right,

Mining ClaimPrefix

LNumber

fT7B ? J l

\" L. A U l

1 HDE

1 \M7 ift i9ll'

Expend. Days Cr.

20

) E UHVNt.1 D

wp.nHi

^ ."-

u/

i/191

2|^.i 'j*

Mining ClaimPrefix

MINIM

KU

12*PM

3i*jii!

NumberExpend. Days Cr.

C W Iff-i-Ar fc kJ

OCT 2 9 1982

G LAND^ ^ft•^ mmt v i ̂ i^,^ 4*7 KB \

/'

TIOo

Total number of mining * claims covered by this J report Of work.

Date .

c J. f ? ALRecorded-HokJer or Agent (Signature^

tt L 7 i I'ti^-Certification Verifying Repotrof Work

l hereby certify that l have a personal and intimate knowledge of the facls set forth in the Report of Work annexed hereto, having performed the work or witnessed same during and/or after its completion and the annexed report is true.

Name and Postal Address of Person Certifying

' c c' *Oiite Cfl't'fiert Certified by (Signature)

b g

Ontario

Ministry of Natural Resources

GEOPHYSICAL - GEOLOGICAL)- GEOCHEMICAL TECHNICAL DATA STATEMENT

FUe.

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) Township or Area Claim Holder(s^

V LF gu

T- WAftO

Survey Company ^o Author of Report -S&

P fS

WAitC? f - &/J c*

Address of Author toft \

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.

DAYS per claimGeophysical

—Electromagnetic—^.^

—Radiometric.-Other————Geological.

AIRBORNE CREDITS (Special provision credits do not apply to airborne surveys)

Magnetometer. .Electromagnetic, . Radiometric

DATE:

(enter days per claim)

SIGNATURE:.Author of Report or Agent

Res. Geol.. . Qualifications jPrevious Surveys

File No. Type Date Claim Holder

MINING CLAIMS TRAVERSED List numerically

(prefix) (number)

TOTAL CLAIMS.

837 (5/79)

GEOPHYSICAL TECHNICAL DATA

GROUND SURVEYS — If more than one survey, specify data for each type of survey

Number of Stations ——— Station interval 5""O Profile scale _______

//b

Contour interval.

.Number of Readings 3-46

.Line sparing -4 &O

Instrument.Accuracy — Scale constant. Diurnal correction method.Base Station check-in interval (hours). Base Station location and value ———

g

Instrument V

Coil configuration Coil separation ——

Z o* t/AJF/A/ 1 TG.

AccuracyMethod: Frequency

2. 0

Parameters measured.

TODETFixed transmitter

A//4/Q lO Shoot back ICkz-____

d In line D Parallel line

(specify V.L.F. itation)

C ^

o

Instrument, Scale constant.

Corrections rriade'

Base station value and location .

Elevation accuracy.

Zo1— 1H^Ni— i X

5oo,QwyDQ2

s^HjjKcrDf!

Instrument -^^—————— Method D Time Domain Parameters — On time -——

-Off

f l Frequency Domain _ Frequency ______ Range '————

— Integration time.

Power.Electrode array — Electrode spacing . Type of electrode

SELF POTENTIALInstrument_________________________________________ Range.

Survey Method _____________________________________________

Corrections made.

RADIOMETRICInstrument.——.Values measured.Energy windows (levels) -—^.——---—^———-.—....—..—.^—^..^-.—.—-—-—--.---—--.—- Height of instrument___________________________Background Count. Size of detector__________________________________________

Overburden —.—————.——————(type, depth - include outcrop map)

OTHERS (SEISMIC, DRILL WELL LOGGING ETC.)

Type of survey———————————————————————Instrument —^——-—————^———————^^—^——— Accuracy____________________________Parameters measured.

Additional information (for understanding results).

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

Instrument(s) —————(specify for each type of survey)

Accuracy__________________(specify for each type of survey)

Aircraft used.——-———————————.-—^..—-————————™

Sensor altitude-Navigation and flight path recovery method *

Aircraft altitude _______________________________ LineMiles flown over total area ________________________ 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.

ANALYTICAL METHODSValues expressed in: per cent

p. p. m. p. p. b.

Dn n

Cu, Pb,

Others—

Zn, Ni, Co, Ag, Mo, As,-(circle)

Field Analysis {.Extraction Method. Analytical Method- Reagents Used——

Field Laboratory AnalysisNo. ———^——-——

SAMPLE PREPARATION(Includes drying, screening, crushing, ashing)

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)

.tests)

.tests)

GeneraL General.

Ministryo) Order of 2a!ural the MinisterResources

The Mining Act

Room 6450, Whitney Block Queen's Park Toronto, Ontario M7A 1W3 416/965-1380

In the matter of mining claims: Recording Office File #338

L 578332

in the Township of Beatty

John T\ WardOn consideration of an application from the recorded holder,.—under Section 77 Subsection 22 gf The Mining Act, l hereby order that the time for filing reports and plans in support of_____Electromagnetic____.______^assessment work recorded on December 18, 1Q 82.be extended until and including December 31 19 82. .

December 10, 1982Date

copies:' Mr. J.T. Hard9 W til am ere Drive Scarborough, Ontario Ml M 1W5

Mining Recorder Kirkland Lake, Ontario

SignatuVe'of Director, Land Management Branch

Ontario

Ministryof Geotechnical Natural Report

Approval

Fil

Mining Lands Comments

^-,-Y-. ( '.,? js/tf/ytf ;

Fo: Geophysics

Comments

roved Wish to tee again with corrections *,1To: Geology - Expenditures

Comments

[~] Approved ) l Wish to see again with correctionsDate Signature

LJTo: Geochemistry

Comments

t l)L'J/.

Date Signature

Q Approved LjWish to see again with corrections

To: Mining Lands Section, Room 6462, Whitney Block. (Tel: 5-1380)

Ministry of GeotechnicalSeTLs Report

Ontario Approval

Mining Lands Comments

vy'A,

To: Geophysics

Approved pfwith to see again with corrections

To: Geology - Expenditures

Comments

Approved |~| Wish to see again with correctionsDate Signature

To: Geochemistry

Comments

|"~) Approved f~l Wish to see again with correctionsDate Signature

l [TO: Mining Lands Section, Room 6462, Whitney Block. (Tel: 5-1380)

1593 (81/10)

1983 01 07

Mining RecorderMinistry of Natural Resources4 Government Road EasP.O. Box 984Kirkland Lake, OntaHP2N 1A2

Dear Sir:

He have received repofts and maps1 (Electromagnetic) survey sub|liwi Provlslons (credlt f o ~ Mining Claim L 578332

This material will bestatement of assessment work credi

Yours very truly,

E.F. AndersonDirectorLand Management Branch

Whitney Block, Room Queen's Park Toronto, Ontario M7A 1W3 Phone: 416/965-1380

DWrsc

cct John T. Ward 9 WHlamere Drive Scarborough, Ont M1N l*

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NOTES

400* Surface Rights Reservation along the shores of all lakes and rivers.

or

LEGEND

PATENTED LAND

PATENTED FOR SURFACE RIGHTS ONLY

LEASE

LICENSE OF OCCUPATION

CROWN LAND SALE

LOCATED LAND

CANCELLED

MINING RIGHTS ONLY

SURFACE RIGHTS ONLY

HIGHWAY 6 ROUTE No,

ROADS

TRAILS

RAILWAYS

POWER LINES

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