32D04NWD204 2 15846 ARNOLD 010

N.T.S.: 32 D/4

RPT. NO. S-95-1

Latitude:48 14

Longitude: 79 49

2.1584 6

EXPLORATION REPORT ON

MAGNETOMETER AND VLF-EM SURVEYS

HOWARD LAKE PROPERTY

THE KIRKLAND LAKE AREA

ARNOLD TOWNSHIP

LARDER LAKE MINING DIVISION

ONTARIO

F.J. SHARPLEY

RECEIVED

FEB6 -1935

MINING LANDS BRANCH

JANUARY 1995

32004NWQ204 2 15846 ARNOLD 01 OC

TABLE OP CONTENTS PAGE

SUMMARY

1.0 INTRODUCTION . . . . . . . . . . . . . . . . . . . . . . 6

2.0 PROPERTY . . . . . . . . . . . . . . . . . . . . . . . 6

2.1 Claims 62.2 Location and Access 72.3 Topography 7

3.0 EXPLORATION HISTORY . . . . . . . . . . . . . . . . . . 8

4.0 GEOLOGY . . . . . . . . . . . . . . . . . . . . . . . . 9

4.1 Regional Geology 94.2 Property Geology 9

5.0 MINERALIZATION . . . . . . . . . . . . . . . . . . . . 10

5.1 Regional Mineralization 105.2 Property Mineralization 11

6.0 CURRENT WORK CARRIED OUT . . . . . . . . . . . . . . . 12

6.1 Line Cutting 126.2 Magnetometer Survey 126.3 VLF-EM Survey 13

7.0 DISCUSSION OF RESULTS . . . . . . . . . . . . . . . . 14

7.2 Magnetometer Survey 147.3 VLF-EM Survey 15

8.0 CONCLUSIONS AND RECOMMENDATIONS . . . . . . . . . . . 17

9.0 REFERENCES AND SELECTED BIBLIOGRAPHY . . . . . . . . . 18

10.0 CERTIFICATE OF QUALIFICATIONS: F.J. SHARPLEY . . . . 20

Appendix I: LIST OF FIGURES page 21

Figure 1: Figure 2: Figure 3: Figure 4: PLAN l PLAN 2 PLAN 3

Location MapClaim MapTopographic MapAirborne Magnetic Map (OGS Map 81327)Topography and ClaimsMagnetic Survey, Readings and ContoursVLF-EM, NLK-Profiles and ReadingsVLF-EM, NLK-Fraser Filter Contours

1:5000 1:5000 1:5000 1:5000

Appendix II INSTRUMENT SPECIFICATIONS 22

LIST OF MAPS IN POCKET

PLAN l - Topography and ClaimsPLAN 2 - Magnetic Survey, Readings and ContoursPLAN 3 - VLF-EM, NLK-Profiles 6 Readings

VLF-EM, NLK-Fraser Filter Contours Compilation-Magnetic Survey, Color Contours St VLF-EM

1:2500 1:2500 1:2500 1:2500 1:5000

SUMMARY

The Howard Lake Property consists of 4 non-patented Mining claim

units located in Arnold Township of the Kirkland Lake area of the

Larder Lake Mining Division of Ontario. The property lies within

the Archean Blake River Basin, six km north of the Victoria Creek

gold discovery in the Abitibi Subprovince of the Superior

Province of the Precambrian Shield.

During the period fro* December 1994 to January 1995, the MDF

Syndicate carried out line cutting, magnetometer and VLF-EM

surveys on the property to investigate interesting airborne

magnetic features for gold and kimberlite potential.

Several weak to strong VLF-EM anomalies have been encountered on

the Howard Lake Property. These conductors are targets for gold

mineralization that may represent structures emanating off the

Murdoch Creek - Kennedy Lake Fault. They may represent westward

extensions of the Broker's Fee Fault Zone where gold is

associated with sulphides in a zone that is two km to the east.

The main magnetic feature is a weak isolated twin peaked ground

magnetic anomaly occurring on the central part of the grid over a

strike length of 300 metres and a width of 100 metres with an

amplitude of 160 to 180 gammas above background. This magnetic

intrusion is probably of mafic or kimberlitic in composition.

5

A program of geological Mapping and geochemical humus sampling is

recommended to evaluate several VLF-EM conductors for gold

potential. Till sampling of the glaciofluvial deposits on the

west side of the grid and gravity or resistivity surveys is

recommended to determine if this magnetic feature on the central

part of the grid is a kimberlite of possible economic interest.

1.0 INTRODUCTION

Line cutting and geophysical surveys have been completed on the

Howard Lake Property, Arnold Township in the Kirkland Lake area,

Larder Lake Mining Division, Ontario. The geophysical ground

program was designed to investigate the oval shaped airborne

magnetic anomaly for gold and kimberlite potential.

The field work was carried out during December 1994 and January

1995.

2.O PROPERTY

2.1 Claims

The Howard Lake Property consists of 4 contiguous, non-patented

mining claim units in Arnold Township in the Larder Lake Mining

Division of Ontario.

The claims are numbered as follows:

L-1189757: 4 units - Arnold Township (Map No. M.321)

The claims total 160 acres or 64.75 hectares and are registered

as follows:

7

D.M. Cameron 33 1/3 percent interest

M. Caron 33 1/3 percent interest

Seal River Exploration Limited - 33 1/3 percent interest

The claims were recorded on February 3,1993.

2.2 Location and Access

The property is located 13 km northeast of Kirkland Lake, Ontario

in Howard Lake in the central part of Arnold Township. Access is

from Kirkland Lake for 8 km east on Highway 66 to the Esker Lake

Road (Highway 672); north for 10 km to the Howard Lake Road;

east-northeast for 3 km to the lake.

2.3 Topography

The property is about 40 percent in Howard Lake which is part of

the Misema River. The topography on land is mainly wet shoreline

with alders and cedar. On the western and eastern edges of the

claim the topography rises to 50 feet above the shoreline of the

lake. The forest cover is mainly birch, spruce, poplar, cedar and

alders.

The climate is typical of northern Ontario with snow cover and

cold weather from mid November until May.

8

Cottage lots cover the island in the lake and the western shore

of Howard Lake on the southern part of the claim.

3.0 EXPLORATION HISTORY

An airborne magnetic and electromagnetic survey with lines spaced

at 200 metre intervals of the Kirkland Lake Area was carried out

by the O.G.S. in 1979; Arnold Township is covered on Map P.2259.

The Arnold and Katrine Townships were mapped by W.A. Hogg for the

O.D.M. in 1962 on a scale of one inch to one half mile (Map

2061); O.D.M. Geological Report No. 29 (Hogg 1964).

There is no record of mineral exploration on the property.

4 . O GEOLOGY

4.1 Regional Geology

The Howard Lake Property lies on the south-central flank of the

east-west trending Blake River Basin and seven miles north of the

east-west trending Larder Lake Fault Zone. The west-northwest

Victoria Creek Shear Zone is four miles to the south. The

northeast trending Murdoch Creek Fault is one mile to the west.

The area is part of the Abitibi Subprovince of the Superior

Province of the Precambrian Shield. The Blake River Basin within

the area of interest consists of undifferentiated intermediate

volcanics intruded by syenite, diorite, gabbro and kimberlite.

4.2 Property Geology

The Howard Lake Property lies on the south-central flank of the

Blake River Basin. The rocks consist of undifferentiated

intermediate volcanics consisting of massive and porphyritic lava

flows striking east-west and dipping steeply (ODM Map 2061-Hogg

1962). Gabbro and diorite intrusives occur in the area.

To the west of the property the Murdoch Creek-Kennedy Lake Fault

strikes northeast.

10

Glaciofluvial deposits occur on the west side of the property.

5.0 MINERALIZATION

5.1 Regional Mineralization

The types of gold deposits in the area are as follows:

Archean Lode Gold Deposits:

(1) Larder Lake Type: mainly mafic-ultramafic volcanic contact

(a) Quartz-Veins in Carbonate: (Carbonate Ore)

(b) Disseminated Pyrite: (Flow-Ore)

(eg) Kerr Addison

(2) Kirkland Lake Type:

(a) Quartz-Veins mainly in syenite.

(b) Quartz-Breccia mainly in syenite

(eg) Macassa

(3) Victoria Creek Type:

(a) Disseminated Pyrite in felsic tuff (Gauthier Group),

(eg) Sudbury Contact

11

Kimberlite Intrusions in the area are as follows:

(1) C14 (diamondiferous) - 4 km north of Howard Lake

(2) A-2 Pipe: - 4 km northwest of Howard Lake

(3) AM-47 Pipe: - 4.5 km west of Howard Lake

(4) A-4 Pipe: - 5 km southwest of Howard Lake

The northwest striking Quinze Dam Fault is 4 km west of Howard

Lake. The area falls within the Timiskaming Structural Zone

(L.T.S.Z.).

5.2 Property Mineralization

There is no record of mineralization on the property.

Two kilometres to the east gold is associated with the Broker's

Fee Fault striking east-west. Gold and chalcopyrite, pyrite

mineralization is associated with quartz veining in carbonatized

intermediate agglomerate with graphite.

12

6.0 CURRENT WORK CARRIED OUT

6.1 Line Cutting

During the period from December 28,1994 to January 18,1995 a

total of 4.8 line kilometres of picket line was cut with a chain

saw by M.C. Exploration Services Inc. of Timmins, Ontario. The

lines are spaced at 100 metre intervals and the stations at 25

metre intervals. Approximately 40% of the lines are on Howard

Lake (Plan 1).

6.2 Magnetometer Survey

The magnetic data was collected with an EDA OMNI IV PPM 350

proton procession magnetometer which measures the absolute value

of the earth's magnetic field to an accuracy of t/- l gammas. The

magnetic survey was carried out by M.C. Exploration Services Inc.

on January 20,1995. A single operator was used with the sensor

mounted on an aluminum pole to remove it from surface geological

noise. Readings were taken at 12.5 metre intervals.

Magnetic diurnal variations were monitored by establishing an EDA

OMNI IV PPM 400 base station magnetometer, which recorded

readings every 30 seconds as the survey was being conducted. The

data from both magnetometers was then dumped with a computer and

base corrected values were computed. Readings were taken along

13

grid lines spaced at 100 metre intervals with readings at 12.5

metre intervals along the line. Approximately 4.8 line kilometres

of data were recorded in this way.

Corrections to the magnetic field values recorded during the

field survey were made using the approximate time and diurnal

change information. The values were then plotted on the computer

by M.C. Exploration Services Inc. at a scale of 1:2500 and

contoured at 10 gamma intervals. The base value used is 57000

gammas.

6.3 VLF-EM Survey

The VLF-EM survey was carried out using a Geonics EM-16

instrument to measure the secondary component produced by the VLF

transmitter station at Seattle (NLK-24.8 KHz). Measurements of

the in-phase and quadrature values were taken every 12.5 metres

along the survey lines spaced at 100 metres on the grid. A total

of 4.8 line kilometres of data was collected by M.C. Exploration

Services Inc. of Timmins, Ontario on January 20,1995.

The results are plotted in profile at a scale of 1:2500. A

conductive response is indicated in a change of gradient from a

positive to negative proceeding in a north direction, as shown on

the map. The Fraser filter values were calculated for the in-

14

phase profiles. The values were plotted and contoured at 10 unit

intervals. The results are compiled by M.C. Exploration Services

Inc. using a computer and shown on maps at a scale of 1:2500.

7.0 DISCUSSION OF RESULTS

7.2 Magnetometer Survey

A weak isolated twin peaked ground magnetic anomaly occurs on

claim L-1189757 between lines 2+OOE to 5+OOE at from 0+25S to

0+75N over a strike length of 300 metres and a width of 100

metres with an amplitude of 160 and 180 gammas above background

(Plan 2). This anomaly corresponds with the airborne magnetic

anomaly over a diameter of 600 metres and an amplitude of 30

gammas.

The anomaly is partly in Howard Lake and part on the west shore

of Howard Lake in wet swamp.

7.3 VLF-EM Survey

Several east-west trending VLF-EM anomalies encountered on the

Howard Lake Property varying from weak to strong are as follows:

15

Anomaly A:

A strong east-west trending VLF-EM anomaly occurs on the southern

flank of the magnetic anomaly over a strike length of 450 metres

from the western boundary of the property to near the eastern

boundary of the property at approximately 1+50S to 2 + 25S from

line 1+OOE to 5+OOE. A possible faulted eastern extension of the

anomaly occurs on lines 6+OOE and 7+OOE at 2+75S (Plan 3). The

anomaly is partly in Howard Lake and partly on the west shore of

Howard Lake.

Anomaly B:

A strong east-west trending conductor occurs on the southern

flank of the magnetic anomaly over a strike length of 550 metres

from the western boundary of the property to near the eastern

boundary of the property (Plan 3). The VLF-EM conductor is partly

in Howard Lake and partly on the western shore of Howard Lake.

Anomaly C:

A weak to moderate conductor trending east-west occurs on the

northern flank of the magnetic anomaly from line 1+OOE to 5+OOE

at 1 + 75N to 1+OON (Plan 3). The anomaly is partly in Howard Lake

and partly on the west shore. A possible faulted weak eastern

extension of the VLF-EM anomaly occurs on lines 6+OOE and 7+OOE

at from 0+00 to 1+OON. This eastern extension is partly in Howard

Lake and partly on the eastern shore of Howard Lake.

16

Anomaly D:

A weak VLF-EM conductor trending east-west occurs in the

northeastern part of the property from line 5+OOE to 6+OOE at

2+OOE (Plan 3). This conductor is partly in Howard Lake and

partly on the eastern shore.

17

8.0 CONCLUSIONS AND RECOMMENDATIONS

Several weak to strong VLF-EM and magnetic zones have been

encountered on the Howard Lake Property. The VLF-EM conductors

are targets for gold mineralization that may represent structures

emanating off the Murdoch Creek Fault Zone. They may represent

extensions of the Broker's Fee Fault Zone, 2 km to the east that

has gold and sulphide association.

The main magnetic feature 300 metres by 100 metres is located on

the central part of the grid between lines 2+OOE to 5+OOE at from

0+25S to 0+75N appears to be caused by a magnetic intrusion of

mafic or kimberlitic composition. This property lies within an

area of a kimberlite field.

Geological mapping and geochemical humus sampling over the VLF-EM

conductors on the east and west shore of Howard Lake would help

to determine the gold potential.

Till sampling of the glaciofluvial deposits on the west side of

Howard Lake and a gravity or IP resistivity survey would help to

determine if the magnetic body is kimberlitic.

Respectfully submitted,

F. J. Sharpleyey

9.O REFERENCES

18

EMR (1981)

GSC (1993)

GSC (1993)

GSC (1993)

GSC (1993)

Jensen L.S. (1983)

ODM (1962)

ODM (1971)

ODM (1979)

OGS (1978)

Topographic Map: 32D/4 Larder Lake 1:50,000

Map C25049G CarteMap of Apparent Conductanceof Bedrock ConductorsBlake River Syncline, OntarioScale 1:50,000

Map C25050G CarteMap of Apparent Conductanceof Bedrock ConductorsBlake River Syncline, OntarioScale 1:50,000

Map C20369G Carte Magnetic Anomaly Map (Residual Total Field) Blake River Syncline, Ontario Scale 1:50,000

Map C20370G Carte Magnetic Anomaly Map (Residual Total Field) Blake River Syncline, Ontario Scale 1:50,000

and Langford F.F.Geology and Petrogenisis of theArchean Abitibi Belt in the Kirkland LakeArea, Ontario; O.G.S.-O.F.R.-5455.

Preliminary Geology Map No. P.178 Arnold Township, District of Timiskaming 1:15,840

Geological Compilation Map: ODM Map 2205 l"* 4 miles: 1:253,440

Kirkland Lake Data SeriesArnold TownshipPreliminary Map P.894(Rev): 1:15,840

Quaternary GeologyKirkland Lake AreaLarder Lake Mining DivisionPreliminary Map P.2479 t P.2492; 1:50,000

19

OGS (1979)

OGS (1982)

OGS (1962)

OGS (1979)

OGS-GSC (1959)

OGS-GSC (1951)

1994

(1986)

Quaternary Geology Larder Lake Area District of Timiskaming Preliminary Map P.2290 Scale: 1:50,000.

Map P.2480Drift Thickness Series Drift Thickness of the Larder Lake Area Scale 1:50,000

Map 2061Arnold and Katrine Townships,Geological Report No. 29,Timiskaming DistrictW.A. HoggScale 1:31,680

Preliminary Map P.2259 Kirkland Lake Area; Arnold Twp; Airborne Electromagnetic Survey; Total Intensity Magnetic Survey. District of Timiskaming

Aeromagnetic Maps 7084G - l"- 4 miles

Map 289G (Rev): Aeromagnetic Map Kirkland LakeTimiskaming District, Ontario Scale 1:50,000

Map 47G: Aeromagnetic Map Larder LakeDistrict of Timiskaming Scale 1:63,360

Claim Map: M.321: Arnold Township

Airphotos: 1:20,000 86-4808-02-71..75 86-4807-02-36..39

20

10.0 CERTIFICATE OF QUALIFICATION

I, Frederick Javes Sharpley of the City of Burlington, Province

of Ontario, do hereby certify:

1) That I aa a consulting geologist and reside at 2372 Sinclair

Circle, Burlington, Ontario, L7P 3C3.

2) That I graduated fro* the University of Saskatchewan,

Saskatoon, Saskatchewan, holding a degree of Bachelor of Arts,

Geology (1959).

3) That I aa a Fellow of the Geological Association Of Canada.

4) That I have practised my profession as a Mineral exploration

geologist for a period of 35 years.

5) That I personally was involved with the technical supervision

of the work and the report.

6) That I have a financial interest in the Howard Lake Property

in Arnold Township, Ontario.

\ Burlington Ontario

January 27,1995. F.J. Sharpley

21

APPENDIX I:

LIST OF FIGURES

ARNOLD TP. PROPERTYHOWARD LAKEKIRKLAND LAKE AREALOCATION MAPLARDER LAKE MINING DIVISIONARNOLD TOWNSHIP, ONTARIO

F.J.SHARPLCY

ARNOLD TP PROPERTY TOPOGRAPHIC MAP ARNOLD TP., ONTARIO BLAKE RIVER BASIN

SCALE: 1150.000

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22

APPENDIX II:

INSTRUMENT SPECIFICATIONS

The PPM-350 is the latest addition to EDA's OMNIMAG*™ series of magnetometers and gradiometer*. It fe engineered to provide users with the latest state-of-the-art advances hi microprocessor technology. Including many features that are unique In the field.

Major benefits and features Include:* Significant Increase In productivity*lowered survey costs* Automatic diurnal correction* Programmable grid coordinates* Highly reproduceable data* Ergonomfc design* Simplified fieldwork* QxTiputer-compatible

t

jcificationsDynamic Range SensitivityStatistical Error Resolution Standard Memory Capacity Absolute Accuracy"

Display Resolution -Capture Range

'Display-

3radient Tolerance "sensorm *

-Sensor Cable-Dperating Environmental Range

^ppwer Supply

-Battery Cartridge Life

-Weight and Dimensions fcStrurr^tOxiscteorJy

- lead Add Battery Cartridge. Sensor

System Complement

18.000 to 93.000 gammas±0.02 gamma0.01 gamma1383 data blocks or readings± 15 ppm at 230C.50 ppm overthe operating temperature range '0.1 gamma±25*, relative to ambient field strengthofbststoredvalue Custonvdeslgned. ruggedized Iquid crystal display with an operat Jig temperature range from -35DC1C to

5.000 gammas per meter Optimized miniature design.

- Magnetic cleanliness k consistent with thespedfiedabsoluteaccuracy Remains flexible In temperature range; Indudestow strain connector -SS^C to *550C; 0-100* relative humidity; weather-proof Non-magnetic rechargeable sealed lead add battery cartridge or belt; or. Disposable tT cen battery car-t ridge or belt ^ 2.000 to 5.000 readings, depending upon ambient temperature ana rate of readings3.4 kg. 238 x 150 x 250 mm1.2 kg. 56 mm diameter x 200 mm Electronics console; sensor with 3-meter cable, sensor staff ; power supply; harness assembly; operation manual.

EDA Is a pioneer In the development of advanced geophysical systems and has created many innovations that Increase field productivity and tower survey costs.EDA's OMNIMAG series consists of the PPM-350 Total Held Magne tometer. PPM400 Base Station Magnetometer, and the PPM-500 Vertical Gradiometer. Contact us now f or details.

f ''

i:t D A iwtnimefitt fc*. llhorncVfe Park dive

1C9

toUSA O A instrument* toe.i t

4S0681DVI

VLF Electromagnet!" Unit

Pioneered and patented exclusively by Geonics Limited, the VLF method of electromagnetic surveying has been proven to be a major advance in exploration geophysical instrumentation.

Since the beginning of 1965 a large number of mining companies have found the EM16 system to meet the need for a simple, light and effective exploration tool for mining geophysics.

The VLF method uses the military and lime standard VLF transmissions as primary field. Only a receiver is then used to measure the secondary fields radiating from the local con ductive targets. This allows a very light, one-man instrument lo do the job. Because of the almost uniform primary field, good response from deeper targets is obtained.

The EM16 system provides the in-phase and quadrature components of the secondary field with the polarities indicated.

Interpretation technique has been highly developed particularly lo differentiate deeper targets from the many surface indications.

Principle of OperationThe VLF transmitters have vertical antennas. The magnetic signal component is then horizontal and concentric around the tiansmitter location.

SpecificationsSource of primary field

Transmitting elation* used

Operating frequency rang*

Parameters measured

Method of reading

Scale range

Readability

Reading timeVLF transmitting stations.

Any desired station frequency can be supplied with the instrument m the form of plug-in tuning units. Two tuning units can be plugged in at one time. A switch selects either station.

About 15-25 kHz.

(1) The vertical in-phase component (tangent of the tilt angle of the polarization ellipsoid).(2) The vertical out-of-phase (quadra ture) component (the short axis of the polarization ellipsoid compared to the long axis).

m-phase from a mechanical inclino meter and quadrature from a calibrated dial. Nulling by audio tone.

In-phase ± 150*: quadrature ± 40*. Shipping weight

10-40 seconds depending on signal strength.

Operating temperature range —40 lo SO* C.

Operating controls

Power Supply

Dimensions

Weight

Instrument supplied with

ON-OFF switch, battery testing push button, station selector, switch, volume control, quadrature, dial ± 40*. inclinometer dial ± ISO*.

6 size AA (penlight) alkaline cells. Lite about 200 hours.

42 x 14 x 9 cm (16 x 5.5 x 3.5 in.)

1.6kg(3.5lbs.)

Monotonic speaker, carrying case, manual of operation. 3 station seleclc plug-in tuning units (additional fre quencies are optional), set of batlerir

4.5kg(10lbs.)

.Figure?

l IMITFD Designers 4 manufacturers LIIVIIICL7 of ge0physiCal instruments

f.u!;5idia ry o!

2Thorncliffe Park DriveToronto/Ontario/CanadaM4H 1H2Tel: (416) 4751821

Ontario

. .Report of Work Conducted*** ** j. *** *After Recording Claim

MMngAct

M*!A — — -**-a i Jin aa ahft*-*-^ K a* iBa a i Jarl **t MfcA fftx-M alai ni •lnw ocMocuon snouNi DO OHVCMG 10 mv t*rawincMi Sudbury. Ontwio. P3E 6A5. tataphone (705) 670-7264.

Hljil^n i jJ fclrtj^haaai ff^^*^Ml*MMM**^ — ̂ JMwimry ov nonnoni UBVMOpnwni •no^MMV^^MM^M^B^MM^M ^^^B^dldUKA — *- —- -*

^-..—jfc. ••|n — — . 4 KA ^^— -*— — Qj, a a *rounn r nor, i9v wKMf onvot,

Instructions: - Please type or print and submit in duplicate.- - Refer to the Mining Act and Regulations for requ

Recorder. ,- A separate copy of this form must be completed- Technical reports and maps must accompany thfc- A sketch, showing the daims/the work is

.2.1584 6

32O04NWO2O4 2.15846 ARNOLD 900

* — * Jt * *

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Work Performed (Check One Work Group Only)Work Group

l/ Geotechnical Survey

Physical Work, IndurJaig Drilling

Rehabiitation

Other Authorized Work

Assays

Assignment fixunReserve

Type

/fao/ltffrm^Te/' ISL.F-fW ate/ Line Cv'fttnoJ f

RECEIVED

FEBG -1895

MIMtri'J- Lfilir*'- BRANCH

Total Assessment Work Claimed on the Attached Statement of CostsNote: The Minister may reject for assessment work credit aN 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.

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

flrt- 2*1 Of/ foStCO'/o J t Of/

(atiach a schedule If necessary)

Cai lineation of Deneflclal Interest * See Note No. 1 on reverse side

For Office Use OnlyTotal Value Gr. Recorded

^344,0.

Received Stamp

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S**Value of

MMMTMfltfork Done this Claim

Mf

Credits you are claiming in this report may be cut back. In order to minimize the adverse effects of such deletions, ptoase indicate from which claims you wish to priorize the deletion of credits. Ptoase mark (*) one of the following:1. IB Credits are to be cut back starting with the claim listed last, working backwards.2. D Credits are to be cut back equally over all claims contained in this report of work.3. D Credits are to be cut back as priorized on the attached appendix.

In the event that you have not specified your choice of priority, option one will be implemented.

Hotel: Examples of beneficial interest are unrecorded transfers, option agreements, memorandum of agreements, etc., with respect to the mining claims.

Note 2: If work has been performed on patented or teased land, ptease complete the following:

l certify that the recorded holder had a beneficial interest in the patented or leased land at the time the work was performed.

Signature Dsto

Ministry ofNorthern Development

OntarioMinisteredu DoVeloppeffiont du Nord ei des mines

Statement of Costs for Assessment CreditEtaft des coOts aux fins du credit d'evaluation

Mining Act/Loi sur tes mines 1584 6PeraonaJ infonnabon cokected on this term is obtained under the authority of the MMng Act This information w* be used to maintain a record and ongoing status of the mining daim(s). Questions about this cofection should be directed lo the Provincial Manager, Mmmgs Lands, MifMStry of Northern Development and Mines. 4th Floor. 159 Cedar Street. Sudbury. Ontario P3E 6A5. telephone (705) 670-7264.

Les renseignements personnels contents dans la presente formule sent recueMs en vertu de la Ld sur toe mhw* et serviront a tenir a jour un registre des concessions minieres. Adrasser toute question sur la collece de ces renseignements au chef provincial des terrains miners, ministere du Devetoppement du Nord et des Mutes. 159. rue Cedar. 4* etage. Sudbury (Ontario) P3E 6A5. telephone (705) 670-7264.

1. Direct Costs/Gouts directs

Type

and ConeuManfe

Location de

Description

Labour Main-d'oeuvreField Supervision Supervision sur te terrain

TypeLtne "fr

Type

Type

Amount Montant

rfoo

Total Direct Costs Total des couts directs

Totals Total global

2. Indirect Costs/CoOts indbects** Note: When claiming RehabiMaJion work Kfin tare not

Pour le rembouraement des travaux de rehabiMaten, les coOla mdvects ne sort pas admisstoles en tent que travaux d'evaluation.

Type

Transportation

Food flnd Lodging

D68cnpbonType

Amount Montant

l

Sub Total of Indirect Costs Total partJel des eouts hndlrects

t (not jraelir than 20* of Direct Coats)

Total Value of (ToM of Otact end

Totals Total global

Note: The recorded holder will be required to verify expenditures claimed in this statement of costs within 30 days of a request for verification. If verification is not made, the Minister may reject for assessment work al or part of the assessment work submitted.

: tetituWre enregstre seratenu de verifer les depsraesdernandeas dans le present etat des couts dans tes 30 jours suivant une demande a cet effet. Si la verification n'est pas eftectuee. to ministre paul rejetertout ou une partie des travaux d'evaluation presentto.

HMng Discounts

1. Work filed within two years of completion is claimed at 10OTb of the above Total Value of Assessment Credit.

Remises pour depot

1. Les travaux deposes dans tes deux ans suivant tour achevamant sort rembourses a 100 to de ta vateur Mate susmenbormee du crtdl devaluation.

2. Work filed three, four or five years after completion is claimed at 50* of the above Total Value of Assessment Credit. See calculations below:

Total Value of Assessment Credit Total Assessment Claimed

x 0.50

2. Les travaux deposes trois. quatreoucinq ans apres tour achevement sort rembourses a 50 H de la vaJeur totale du credit d'evaluation susmentiorme. Voir tes calculs ci-dessous.

Vtfeur toMe du crtdH d'evaluMionx 0.50

Certification Verifying Statement of Costs

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

that as(Recorded Holder. Agent Position in Company)

to make this certification

Attestation de I'etat des coOts

J'atteste par la presente :que tes montants indiques sent te plus exact possible et que ces depenses ont ete engagees pour effectuer tes travaux d'evaluation sur tes terrains indiques dans la formule de rapport de travail ct-joint.

l am authorized Et qu'i titre de . je suisautoris6(Hulaire enregistre. repntoentant. poste occupe dans la compagnw)

faire cotte attestation.

0212WVU91) Nota : Dans cette formute. kxsqu'il designe des to masculin est utiNse au sens neutre

VMiUB OF A88B88MBMT WORK PERFORMED OH MIMIMO CLAIMS

MAY 08, 1995FILE NUMBER 2.15846TRANSACTION MO. W9580.00040

CLAIM NUMBER VALUE OF ASSESSMENT WORKDOME OH THIS CLAIM

L-1189757 93,480.00

TOTAL 93,480.00

OntarioMinistry ofNorthern Developmentand Mines

MinistereduDeveloppement du Nord et des Mines

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

Telephone: (705) 670-5853 Fax: (705) 67O-5863

May 10, 1995 Our File: 2.15846 Transaction /: 9580. 00040

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

Dear Mr. Spooner:

RE: APPROVAL OF NOTICE OF REDUCTION ISSUED FOR ASSESSMENT WORK REPORTED OH MINING CLAIM L-1189757 IN ARNOLD TOWNSHIP.

As discussed with Mr. Sharpley by phone on May 29, 1995, he will receive full assessment credit for the report and only be reduced by the value of the line-cutting, magnetometer and VLF survey performed on the island (0.4km). Accordingly, this resulted in a $180.00 reduction from the original submission.

Assessment work credits have been approved as of May 08, 1995 as outlined on the attached distribution of work form. The credits have been approved under Section 14 (Geophysical) of the Mining Act Regulations. Please contact the Mining Recorder in order to redistribute the allowable assessment credits.

If you require additional assistance in this matter please contact Steven Beneteau at (705) 670-5858.

ORIGINAL SIGNED BY:

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

SBB/jl Enclosure:

cc: Assessment Files Office s Sudbury, Ontario

Resident Geologist Kirkland Lake, Ontario

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THE INFORMATION THAT APPEARS ON THIS MAP HAS BEEN COMPILED FROM VARIOUS SOURCES, AND ACCURACY IS NOT 'V* '*NTEED THOSE

IG TO STAKE MIN- CLAIMS SHOULD CON-

WITH THE MINING HtCOHUEH, MINISTRY OF NORTHERN DEVELOP MENT AND MINES. FOR AD DITIONAL INFORMATION ON THE STATUS OF THE LANDS SHOWN HEREON

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COPY OF THIS MYLAR ARCHIVED APR.08/92

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Rir.urs WirHORAWN FROM STAKING StC f ION 43 ORDER (HSOI97O) NONR W 12/73

-61 AKtN4,**e(lt,f. Jb/HU order MO ORDER NO r 54/Ofl OPl-.NS

SURFACE t MINING RICH l S WITHDRAWN FROM ST AKINO.s.cllon Ib/HO OROFK NOW/33/88NR 0-07/881 OPENS W-35/B8NH

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FEB G -1995

MINING LANDS BRANCH

6.15846

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Claim Post Location

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RECEIVED

FEB G - 1995

MINING LANDS BRANCH

Total Field Magnetic Contours

evel 1; 10nT from 57590 to 57840nT

evel 2; 1 OOnT from 57600 to 57800nT

57000nT Base Subtracted

Data Range; 57584 to 57844nT

200 samples with a mean of 57740nT

^Jise Station ; South of brid m bush

57750 NanoTet.la Keferenc.e Field

INSTRUMENTS

OMNI IV PPM - 350, portable unit

OMNI IV PPM 400, base station unit

PLAN 2

Scale 1 2bOOO 50 100 150

M c.

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MD F SyndicateMagnetic SurvHoward Lake C^r

NTS: 52 D 7 SW L(]rder Lake Mining Division[ xploration Scrvu^;:* Iru, Jcin 995

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FEB 6 -

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VLf- Anomaly Axis —Q

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FEB G -1995

MINING LANDS BRANCH

LEGEND

KRASER l ILUR PKODUCIS

Contour Intervals. Level 1, 10%. from O to ]QQ7e, level ?; 100%, from O to 1005S

168 culculoted samples Duta Range, -1J1 to

Seatle, Jl^ . 6 kHz

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Larder Lake Mining DivisionM. C. Exploration Services Inc. Jan. 1995