42I05SE2002 2.20660 VALENTINE 010

GEOP

RECEIVEDOCT 30 2000

GEOSCIENCE ASSESSMENT OFFICE

VSlLALkkPORl"on a

MAGNETOMETER AND VLF-EM SURVEYon the

CORAL RAPIDS PROPERTYKILMER, VALENTINE, HAMLET A PITT

TOWNSHIPS, PORCUPINE MINING DIVISIONfor

DON MCKINNON A c- r* u 'U

Submitted by: Steve AndersonVISION EXPLORATIONOctober 27,2000

42IOSSE2002 2.20660 VALENTINE 010C

TABLE OF CONTENTS

PageIntroduction................................................... lLocation and Access......................................... 2Personnel...................................................... 2Previous Work................................................ 3General Geology.............................................. 3Claims............................,............................. 3Work Program................................................ 4Magnetometer Survey........................................ 4VLF-EM Survey............................................. 5Results......................................................... 6Recommendations and Conclusions....................... 6Certificate..................................................... 7

FIGURES

Location Map................................................ Figure # lRegional Location and Geology Map.................... Figure #2Claim and Grid Sketch.................................... Figure #3

MAPS

Magnetometer Map......................................... Map #1VLF-EM Map.............................................. .Map #2

INTRODUCTION

The following report will deal with the results of a magnetometer and VLF-EM survey carried out on the Coral Rapids Property. The property is held by Don McKinnon and is made up of 11, contiguous, unpatented block mining claims (l 16 units), located in Kilmer, Valentine, Hamlet and Pitt Townships, Porcupine Mining Division, Districts of Cochrane, Ontario. This work was carried out on a contract basis by Vision Exploration and took the form of a flagged- line program, which was followed up with magnetometer and VLF-EM surveys. A total of 30. l km. of grid lines were established and surveyed during the month of October 2000.

The purpose of this program was to extend existing grid (surveyed in 1999) provide additional ground geophysical data that would aid in the geological interpretation of the area.

55-

3C-

PROVINCE OF ONTARIOFI* l

.C li ant: MCKINNON PROSPECTINGProparig: CORAL RADIOS PROPERTY

Till.;

LOCATION MAP

EXPLORATIONTIMMINS ONTARIO

LOCATION AND ACCESS

The Coral Rapids Property straddles the Township line between the southeast portion of Kilmer Township and southwest portion of Valentine Township, Porcupine Mining Division, Districts of Cochrane, Ontario. The property is situated approximately 140-km. north from the town of Smooth Rock Falls, Ontario. The Ontario Northland Rail Line runs in a north-north easterly direction through the central portion of the block while the Abitibi River runs along the claim group's eastern boundary.

Access to the work area was gained by taking Hwy 634 north from the town of Smooth Rock Falls for 75km to Fraserdale. From Fraserdale, Ontario Hydro maintains an all weather gravel road, which runs north for another 55km to their Otter Rapids generating station. It should be noted that Ontario Hydro occasionally locks the gate at the Otter Rapids Dam, limiting access. Arrangements were made for the gate to remain open for the duration of this work program.

From Otter Rapids the Property was accessed by way of an ATV by going north along the Ontario Northland Rail Line for 10 km. This provides access to the central portion of the claim group.

Accommodations in Fraserdale and Otter Rapids can be arranged through Ontario Hydro. These rooms are very expensive and are based on availability. As no rooms were available at the time, accommodations for this work program were arranged in Smooth Rock Falls.

PERSONNEL

The people directly involved with this work program were all employed by Vision Exploration and are as follows.

Steve Anderson... ...................................Timmins, OntarioDonny McKinnon.................................... Timmins, OntarioSteve Poison........................................ ..Timmins, OntarioDannyBrazeau.......................................Timmins, OntarioRob Todoravich.................................... ...Timmins, OntarioJody Brazeau.......................................... Timmins, Ontario

Steve Anderson supervised all work.

REGIONAL LOCATION MAP

CORAL RAPIDS PROPERTY

PREVIOUS WORK

The focus of this work program was to extend an existing flagged line grid that was established in 1999. This grid was surveyed using the same parameters as the 1999-work program. The current data set was then merged with the 1999 data.

GENERAL GEOLOGY

The geology of the area is shown by OGS, Mines and Mineral Division Map 2506 (Figure #2) to be underlain by sediments, specifically limestone, dolostone, shale and gypsum.

CLAIMS

The Coral Rapids Property is made up of 11 contiguous, unpatented block mining claims (116 units) located in Kilmer, Valentine, Hamlet and Pitt Townships, Porcupine Mining Division, District of Cochrane, Ontario. All are currently recorded in the name of Don McKinnon. The claim numbers are as follows:

CLAIMS # OF UNITS TOWNSHIP

1223523 3 KILMER1223530 6 VALENTINE1223531 15 VALENTINE1223532 16 KILMER1228039 3 VALENTINE1228205 l VALENTINE1228206 16 KILMER1228214 10 VALENTINE1228684 16 KILMER1228693 16 KILMER1223526 14 HAMLET/PITT

KILMER TOP

RAPIDS X LONG RAP** **" RE3CTVC

CLAIM AND GRID SKETCH CORAL RAPIDS PROPERTY

SCALE: luFIGURE #3

'/s

PITT TWP

WORK PROGRAM

The first stage of this work program involved extending a previously established (1999) grid to the north and south. A flagged-line grid was set up with the base line running at 15 degrees Az. and cross lines at 115 degrees Az. The line interval was set at 100 meters, with a 25 meters station interval. A total of 30. l km. of chained and flagged grid lines were established.

The grid was then surveyed with Magnetometer and VLF-EM, using a 25-meter reading interval, resulting in 28.5 km of magnetometer and VLF-EM coverage. These parameters are the same as what was used in 1999. This data was then merged with the 1999 data providing a single map with continuous coverage.

The following is a brief description of the geophysical methods and parameters used.

MAGNETOMETER SURVEY

A GEM GSMT-19 Proton Precession magnetometer was used to carry out the magnetometer survey. The instrument is synchronised with a GEM GSMT-19 recording base station to help eliminate magnetic diurnal variation. This should ensure an accuracy of less than 1.0 Nt.

The Proton Precession method involves energising a wire coil immersed in a hydrocarbon fluidThis causes the protons in the proton rich fluid to spin or precess simulating spinning magnetic dipoles.When the current is removed the protons precess about the direction of the earth's magnetic field,generating a signal in the same coil which is proportional to the total magnetic field intensity. In thisway, the horizontal gradient of the earth's magnetic field can be measured and plotted in plan form withvalues of equal intensity joined to form a contour map.

This presentation is useful in correlating with other data sets to aid in structural interpretation. Individual magnetic responses can be interpreted for dip, depth and width estimates after profiling the

data.

The following parameters were employed for the survey:

Instrument - GEM, GSMT-19 Proton Precession MagnetometerReading Interval - 25mLine Interval - 100mDiurnal Correction Method - GEM GSMT-19 Recording Base StationData Presentation - Data posted and contoured plan map

-1:5000 scale- Contour interval: 20 nano-teslas

VLF- EM SURVEY

A Geometrics EM-16 VLF instrument was used to survey the entire property. Both the In- phase (dip angle) and Quadrature values were recorded at 25m intervals.

While VLF stands for Very Low Frequency, it is for mineral exploration purposes a very high frequency compared to other commonly used Electromagnetic Surveys. The commonly used frequencies are in the order of 18-20 kilohertz. The VLF-EM technique employs fixed transmitter stations located at various places around the world to facilitate navigation. Because of this, one has a limited choice as to what transmitter station that can be used, depending on distance from and azimuth to the transmitter station.

For this survey, Cutler Maine (NAA) was used. It has an operating frequency of 24.0 KHz and an azimuth of approximately of 110 degrees TN from the property. Very briefly, the transmitting station emits a concentric, circular wave pattern, expanding about the transmitter dipole. Being thousands of miles away from the transmitter, we deal with the tangent of this wave pattern, which in this case would have a direction normal to the azimuth of 110 degrees. Thus any conductors having a general EW strike direction would be intersected by this signal which induces a signal in the conductor which in turn opposes the primary signal from the transmitter station. This elliptically polarizes the resultant field enabling detection of the conductor using a receiver coil to determine the attitude of the resultant field at various points along the grid lines.

The resultant field dips away from the conductor axis on both sides of the conductor producing a crossover on the conductor axis. For an EW conductor, a true crossover would occur where the field dips south and changes to a north dip as you progress from south to north. For this survey, a +A system is used where a (*) dip angle means the field is dipping to the south (indicating anomaly is to north) and a (-) dip angle means the field is dipping to the north (indicating anomaly is to South). This is the case only if all readings were taken facing north as per this survey.

The quadrature values, while not useful alone, can help distinguish between bedrock conductors, which generally have a smaller out-of-phase response than overburden or short wavelength conductors can. Also, the polarity of the quadrature is diagnostic, i.e.; if the polarity follows or is the same sense as the In-phase it gives more credibility to the conductor. Reverse quadrature often indicates overburden responses.

The following parameters were employed for the survey:

Instrument - Geometrics EM-16 VLF Transmitter Station - Cutler Maine (USA)

- Call symbol NAA Frequency - 24.0 kFIzAzimuth to station - approx. 110 degrees TN Reading Direction - All reading taken facing north Reading Interval - 25m Line Interval - 100m Data Presentation - Data posted and profiled plan map

-Scale-1:5000- Profile scale l cm = 1007o

SURVEY RESULTS

The geophysical program conducted on the extension of the 1999 Coral Rapids Grid was successful in outlining a number of features that are of interest.

The main purpose of this program was to test the southern extension a magnetic high outlined in 1999. This feature does not appear to extend to the south with the main bull-eye high occurring on L700S at 350W.

The 2000-work program revealed the presence of two one line magnetic lows. These bulls-eye features are located on LI 100S/1375W and L BOOS/1875 W, with the later remaining open to the Southwest. Both these zones are approximately 400Nt below background,

Two magnetic highs were outlined. The first is a one-line bulls-eye that occurs on L1000S at 1950W and is roughly 150Nt above background. The second is similar in amplitude but extends from L600N/150W to L1000N/300W.

As with the 1999 survey the VLF-EM survey conducted did not show any significant responses. This may be due to poor station coupling for the line angle used as well as extreme overburden conditions. Due to the fact that the VLF station Annapolis has been shut down, Cutler or Seattle are the only station available.

RECOMMENDATIONS AND CONCLUSIONS

The geophysical programs carried out on the Coral Rapids Property were successful in outlining a number of isolated magnetic anomalies that could be further tested.

As the James Bay lowland have be the focus of diamond exploration for a number of years and continues to be explored. Kimberlite pipes have been shown to show up as magnetic highs and lows or may have no magnetic signature. As a result, isolated magnetic features such as the ones outlines by this program have been the starting points for grass-roots diamond exploration.

Due to the areas potential for hosting Kimberlite pipes, the anomalies outlined by this program should be further tested to determine the source of their response.

CERTIFICATION

I, Steve Anderson of Timmins, Ontario hereby certify that:

1. I hold a three-year Technologist Diploma from Sir Sandford College, Lindsay, Ontario, obtained in May 1981.

2. I have been practising my profession since 1979 in Ontario, Quebec, Nova Scotia, New Brunswick, Newfoundland, NWT, Manitoba Saskatchewan and Greenland.

3. I have been employed directly with Asamera Oil Inc., Urangellschaft Canada Ltd., Nanisivik Mines Ltd., R. S. Middleton Exploration Services Ltd., Rayan Exploration Ltd and am currently an owner of Vision Exploration.

4. I have based conclusions and recommendations contained in this report on knowledge of the area, my previous experience and on the results of the fieldwork conducted on the property during 2000.

Dated this 27th day of October 2000 it Timmins, Ontario.

APPENDIX A GEM GSM-19 MAGNETOMETER

GEM GSM-19

INSTRUMENT SPECIFICATIONS

MAGNETOMETER l GRADIOMETERResolution:Accuracy:Range:Gradient Tolerance:Operating interval:

input/Output: Power Requirements:

Power Source:

Battery Cha/ger:

Operating Ranges:

Storage Temperature: Display:

Dimensions:

VLFFrequency Range: Parameters Measured:

Resolution:Number of Stations: Storage:

Terrain Slope Range: Sensor Dimensions: Sensor Wefeht:

0.01 nT (gamma), magnetic field and gradient0.2 nT over operating range.20,000 to 120,000 nT.Over 10,000 nT/m3 seconds minimum, foster optional. Readings initiated from keyboard,external trigger, or carriage return via RS-232-C.6 pm weatherproof connector, RS-232C and (optional) analog output12 V, 200 mA peak (during polarization), 30 mA standby. 300mA peakin gradiometer mode.Internal 12 V, 2.6 Ah sealed lead-add battery standard, others op tional An Boemal 12V power source can also be used Input 110 VAC, 60 Hz. Optional 110/220 VAC, 50/60 Hz. Output dual levef charging. Temperature: -40 *C to -1-60 *C Battery Voltage: 10.0 V minimum to 15V maximum. Humidity: op to 90* relative, mn condensing. -50"CtD*650C

LCD: 240 x 64 pixels, or a x 30 characters. Built in heater for opera tion bdow -20"C Console: 223 x 69 x 240mm. Sensor itaffc 4 x 450mm sections. Sensor 170 x 71mm dia. Weight Console 2.1 kg. Staff 0.9kg, Sensors 1.1 kg each.

15 - 30.0 kHz.Vertical In-phase and Out-of phase components as percentage of totalfield.2 components of horizontal fieldAbsolute amplitude of total field.0.1*.Up to 3 at a time.Automatic with: time, coordinates, rnagnebc field/gradient, stope, EMfield, frequency, m- and out-of^phase vertical and both horizontalcomporMtnii for each jetecbcd sbiuon.O--90* {entered manuafty),14x 15x9on. (5.5x6x3 inches).

APPENDIX B GEOMETRICS EM-16 VLF

VLF EM(."LANt VYAVt; fcM INSIKUMfcNIS.

EMI6On* of the most popular md widory used electromagnetic Instrumi* ttwEMls VLf receiver makes the ideal reconnaissance EM. This can be anritaM to m field reliaMfty, operational sanpHcny. compactness and mutual compatibly with oiner reconnaissance instruments such as portable magnetometers and rada*etric delee ton.

The VLF method at EM surveying, pioneered by Geonics. has proven a be a simple economical means o* mapping geological structure and lauH tracing. Tin applications are many and varied, ranging Irom direct detection of massive sufpntii conductors taine indirect detection ol precious metals and radioactive deposits.

Pie EU1 G is the only Vlf Instrument that measures the quad-pnaaas well u trie in phase secondary Md. This has the advantage of providing a additional piece of data for a more comprehensive interpretation and also afaws a mor* accurate determination o* the Ult angle.

The secondary fields are measured as a ratio to (he primary (idd caking the measurement independent of absolute field strength.

The EM16 Is Uie only VLF receiver that can be adapted ta mmswt VLf resistivity.

SpecificationsMEASURED QUANTITY In-phasc and ojiad-pnase components of wrtcal mag

netic Held as a percentage of horizontal pieiary NtJd. (i.e. tangent of the tilt angle and ellipticity)

SENSITIVITY la-phase : tt 507. Quad-phase:! 40?.

RESOLUTION 1V.

OUTPUT Mijaiigbyaudtolane.ln-phaseindicatoniwinecnan- \at fefinomelef and quad-phase (row a gtafated df*

iPI WSNB FREaUENCY 1S-Z5 kHz VLF tadto Band. Station setKM done by means ri pbg-huMts.OnrtW Swilcn. battery lest push button, staflei selector ewflc*. eudto voueiw comrot, quadrature dH, meter.

POWER SUPPLY ( dhposaok* 'AA'

DIMENSIONS 42iMx9cm WCtCHT lnstnmentt.0ka

SMpping :S.Skg

RESISTIVITY METER

EMI6/I6RThe EM16R is a simple, button on tttacnment to the EM 16 converting it to a direct reeoUnf lemin reeistMry meter. The EM18B interfaces i pair of pottn- tiii HtctrodB to rtie EM 18 eneMIng the meeturement of the ratio of, and iht {thin angle between, the horizontal electric and meenetie fields of the plan* wave propagated by distsvt VI F radio transmitters.

The EM16R is direct reading in ohm-meters of apparent ground resistivity. If ihe phase angle is 45*, the resistivity reading is the true value and ihe earth is uniform to the depth of exploration (i.e. a skin depth). Any departure from 45* of phase in dicates a layered earth. Two layer interpretation curves are supplied with eacn in strument to permit an interpretation basid on a twe layer earth model.

This highly portable resistivity meter makes an Ideal tool lv quick geological map ping arid has been used successfully for a variety of applications.

e Detection at massive and disseminated sulpmda deposits Overburden conductivity and thickness measurements Permafrost mapping Detection and delineation ol industrial mineral deposits Aquifer mapping

Sp6ClfiC3tiOnS "wu ATTACHMENT

MEASURED QUANTITY

RESISTIVITY RANGES

PHASE RANGE

RESOLUTION

OUTPUT

OPERATING FREO.UENCY

Apparent Resistivity of the ground in ohm meters Phase angle between Ex and Ky in degrees 10- 300 onm meters 100- 3000 ohm-meters 1000 - 30000 ohm-meters 0-90 degrees

INTERPHOBE SPACING PROBE INPUT IMPEDANCE

DIMENSIONS

WEIGHT

Phase : O.S*Nut by audk* font, fteststtvtty and phase angle read tow graduated dWs.15-25 kHz Vlf Radio Sand. Sultan selection by means f rotary s***.10BMIM

100 MO m paralef wfth 0.5 ptechrads1*x1t.5xtOen. (KtachedteskteolEUK)1J kg (tocajdkn prates and catte)

Ontario Ministry ofNorthern Developmentand Mines

Declaration of Assessment Work Performed on Mining LandMining Act, Subsection 65(2) and 66(3), R.S.O. 1990

Number (office use)

issment Files Research Imaging

)rity of subsections 65(2) and 66(3) of the Mining Act. Under section B of the 3d to review the assessment work and correspond with the mining land holder. ining Recorder, Ministry of Northern Development and Mines, 6th Floor,

42I05SE2002 2.20660 VALENTINE

900Instructions: - For work performed on Crown Lands before recording a claim, use form 0240.

- Please type or print in ink.

1. Recorded holder(s) (Attach a list if necessary) o s\Name

Telephone NumberAddress i

f Fax Number

Name

Address

Client Number

Telephone Number

Fax Number

2. Type of work performed: Check ( ^ ) and report on only ONE of the following groups for this declaration.

n RehabilitationGeotechnical: prospecting, surveys, assays and work under section 1 8 (regs) D Physical: drilling, stripping,

trenching and associated assaysWork Type

Dates Work Performed

xL

Office Use

Commodity

Total S Value of Work Claimed

TV, Toth | Vear

NTS Reference

Global Positio System Data (If available) Township/Ar

M̂ot

Mining Division

or G-Plan Number d - Resident Geologist District

Please remember to: - obtain a work permit from the Ministry of Natural Resources as required;- provide proper notice to surface rights holders before starting work;- complete and attach a Statement of Costs, form 0212;- provide a map showing contiguous mining lands that are linked for assigning work;- include two copies of your technical report.

3. Person or companies who prepared the technical report (Attach a list if necessary)Name

-E*f iTelephone Number76*- -772 7L

Address

r V# , lFax Number ^

Name

Address

"RECEIVED

Telephone Number

Fax Number

i, , do hereby certify that l have personal knowledge of the facts set(Print Name)

forth in this Declaration of Assessment Work having caused the work to be performed or witnessed the dame during 1 or after its completion and, to the best of my knowledge, the annexed report is true.

DalT

DO

pjTelephone Number Fax Number

0241(02/98)

5. Workjo.be recorded and distributed. Work can only be assigned to claims that are contiguous (adjoining) to^ the mlrrtrVfl iflhd w^we work;wasvp*eltormeWfct'the time work wad performed. A map showlftg^the contiguous llnkfc? 'rnu8t: acijrnpany' trilsjo/m.j l-M:,'- r •^•\ ~ A /^/^''^#^S~"

Mining Claim Number. Or It work was done on other eligible mining land, show In this columrf the location rtufnber inoicaVed oh'jHe cialW fnaf).

eg

eg

eg

1

2

3

4

5

6

7

8

9

10

11

12

; 13

14

15i

TB 7827

1234567 . :

1234568

/22^^-3/2.7^^2-

n 1 fa/ Qy1 ̂ Z-C? (9O\

(ZJ^^l f/2.Z^"T^^h~)ftl.ob

Number of Claim Units. For other mining land, list hectare*.

16 ha

12

2

f/

It,

tt

k

-lk ————

,.,'

Column TotalsR ' -i-

Value of work performed on this claim or other mining land.

S26, 825

0

S 8, 892

^/2? {T2/yfc,t/23^2/77

yy /(^

Value of work applied to this claim.

N/A

124,000

S 4,000

&V&/5

b^bO

Value of work assigned to other mining claims.

S24,000

0

0

^/z?^ !

2y^*T

/j y f@f)

Bank. Value of work to be distributed

, at a future date. ,

K' ' " ' "''

S2.825 ~*

or

54,892

1* ' ' - .--H ;

2//^2 /99/0

7 /nItf/?

i.v-

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s 0 W , do hereby certify that the above work credits are eligible under.'do - n1 tec -.f.rdv (Print FuH Nam*) : .,- . r;

subsectlori 7 (1) of the Assessment Work Regulation 6/96 for assignment to contiguous-Claims or for application to

the claim where the,,work was done;) ^rSignet Agent Authorized in Writing

W~ J_____

6. Instructions for cutting-tack credits that are not approved.

Some of the credits claimed In this declaration may be cut back. Please check ( ^ ) in the boxes below to show how

you wish to prioritize the deletion 6fCredits: Eh lrCrWlt8~are7to-Be:cut back from the Bank first, followed by optlorr 2 or 3 or 4 arirnJlcated. ~, t

. . . D. 2. Credits are to be cut back starting with the claims listed last, working backwards; or Y. Credits are to be cut back equally over all claims listed In this declaration; or

4. Credits are'to Be cut back as priori

r)

Noterlf you have Trot Indicated how your credits are tt

zed on the attached appendix or as follows (describe):

RECEIVEDOCT 3 o

GEOSCIENCE ASSESSMENT -iha Halatai-OEElQBe mill ha

h-?!' 'TO'"1 '" \'' t:~ ~- T,

t back from the dank first,

ForiOffleeilReceived Stamp

Approved for Recording by Mining Recorder (Signature)

0241 (02M)

Ontario Mnlttry ofNorthern Developmentand Mines

Statement of Costs for Assessment Credit

Transaction Number (office use)

Personal information collected on this form Is obtained under the authority of subsection 6 (1) of the Assessment Work Regulation 6/96. Under section 8 of the Mining Act. this information Is a public record. This information will be used to review the assessment work and correspond with the mining land holder. Questions about this collection should be directed to a Provincial Mining Recorder. Ministry of Northern Development and Mines, 3rd Floor, 933 Ramsey Lake Road, Sudbury Ontario P3E 6B5.

Work Type

FlflcD ^ )}U 0 ^

Mt^^^t^ SLSVU-^ULF^ PA .^fvt/-*-,f wtt\ ̂ y" rC 'df^o^\

C- Si

Unit* of workDepending on the type of work, list the number of hours/days worked, metres of drilling, kilometres of grid line, number of samples, etc.

3^.7/0^23. -f A^

Associated Costs (e.g. supplies, mobilization and demobilization).

Transportation Costs

Food and Lodging Costs

n F- f* F i w F piOCT302000

Calculations of Filing Discounts: GEOSCIENCE ASSESSMENT

-. - . -. ' .' ;.'! :'Cost Per Unit ' * ^

of work

91 n^/kt^tf /2 f/jzt^* /? i C/k^

r

lue of Assessment Work

^oMotalCost

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H* /K

1. Work filed within two years of performance is claimed at 100*^ of the above Total Value of Assessment Work.2. If work is filed after two years and up to five years after performance, it can only be claimed at 500Xo of the Total

Value of Assessment Work. If this situation applies to your claims, use the calculation below:

TOTAL VALUE OF ASSESSMENT WORK x 0.50 s Total S value of worked claimed.

Note:- Work older than 5 years is not eligible for credit.- A recorded holder may be required to verify expenditures claimed in this statement of costs within 45 days of a

request for verification and/or correction/clarification. If verification and/or correction/clarification is not made, the Minister may reject all or part of the assessment work submitted.

Certification verifyingucosts:

l, ^A^A^-e^ Mwl'OV'SO^ . do hereby certify, that the amounts shown are as accurate as may reasonably(please print full name)

be determined and the costs were incurred while conducting assessment work on the lands indicated on the accompanying

Declaration of Work form as(recordeo1

cibotdrf.

l am authorized to make this certification.agent, or state company position with tigning authority)

0212 (O3/97)

5^rvi ^

JCT 272000 a

PORCUPINE MINING DIVISION^

Ministry ofNorthern Developmentand Mines

December 4, 2000

DONALD MCKINNON BOX 1130 TIMMINS, Ontario P4N-7M5

Ministere du Developpement du Nord et des Mines Ontario

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

Telephone: (888) 415-9845 Fax: (877)670-1555

Dear Sir or Madam:

Subject: Transaction Number(s):

Submission Number: 2.20660

StatusW0060.00433 Approval

We have reviewed your Assessment Work submission with the above noted Transaction Number(s). The attached summary page(s) indicate the results of the review. WE RECOMMEND YOU READ THIS SUMMARY FOR THE DETAILS PERTAINING TO YOUR ASSESSMENT WORK.

If the status for a transaction is a 45 Day Notice, the summary will outline the reasons for the notice, and any steps you can take to remedy deficiencies. The 90-day deemed approval provision, subsection 6(7) of the Assessment Work Regulation, will no longer be in effect for assessment work which has received a 45 Day Notice. Allowable changes to your credit distribution can be made by contacting the Geoscience Assessment Office within this 45 Day period, otherwise assessment credit will be cut back and distributed as outlined in Section #6 of the Declaration of Assessment work form.

Please note any revisions must be submitted in DUPLICATE to the Geoscience Assessment Office, by the response date on the summary.

If you have any questions regarding this correspondence, please contact JIM MCAULEY by e-mail at james.mcauley@ndm.gov.on.ea or by telephone at (705) 670-5880.

Yours sincerely,

ORIGINAL SIGNED BYLucille JeromeActing Supervisor, Geoscience Assessment OfficeMining Lands Section

Correspondence ID: 15476

Copy for: Assessment Library

Work Report Assessment Results

Submission Number: 2.20660

Date Correspondence Sent: December 04, 2000 AssessorJIM MCAULEY

Transaction First ClaimNumber Number Township(s) l Area(s) Status Approval Date

W0060.00433 1228693 VALENTINE, KILMER Approval November 29,2000

Section:14 Geophysical MAG 14 Geophysical VLF

At the discretion of the Ministry, the assessment work performed on the mining lands noted in this work report may be subject to inspection and/or investigation at any time.

Correspondence to: Recorded Holder(s) and/or Agent(s):

Resident Geologist Steve AndersonSouth Porcupine, ON TIMMINS, ONTARIO, CANADA

Assessment Files Library DONALD MCKINNON Sudbury, ON TIMMINS, Ontario

Page: 1

Correspondence ID: 15476

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KILMERW R R ADMIHHTMmE DIITRtCT

COCHRANE

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PORCUPINE

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ant* no

Mhwtry of Mravtry ofMatura* Northern PavBtapmantBooources andMnea

G-3524

42I05SE2002 2.20660 VALENTINE 210

-**T;

TOPO LEGEND

SHORE LINE

ROAD

HYDRO LINE

CLAIM POST ASSUMED

CLAIM POST LOCATED

CLAIM LINE

LOT AND CONCESSION LINE

RAIL LINE

LEGEND

INSTUMENT: GEONlCS EM-l 6 VLF

PARAMETERS MEASURED: IN-PHASE AND QUADRATURE

READING INTERVAL: 25M

PROFILE SCALE: l cm - l O*

STATION: CUTLER MAINE NAA-24.0 KHZ.

ALL READINGS TAKEN FACING NORTH

42I05SE2002 2.20660 VALENTINE 220

VALENTINE TOWNSHIPTOWNSHIP

TOPO LEGEND

SHORE LINE

ROAD

HYDRO LINE

CLAIM POST ASSUMED

CLAIM POST LOCATED

CLAIM LINE

LOT AND CONCESSION LINE

RAIL LINE

a,.*: MCKINNON PROSPECTINGLEGEND

CORAL RAPIDS PROPERTYINSTRUMENT: GEM GSM-19 PROTON PRECESSION MAGNETOMETER

PARAMETERS MEASURED: EARTH'S TOTAL MAGNETIC FIELD (NANO-TESLAS)

READING INTERVAL: 25 M

CONTOUR INTERVAL: 20 NANO TESLAS

DIURNAL CORRECTION METHOD: RECORDING GEM BASE STATION

DATUM SUBTRACTED: 58000 nT

POSTED AND CONTOURED MAGNETOMETER DATA .

Townehip:KILMER ^— VALENTINE EXPLORATION

TIMMINS ONTARIO

42I05SE2002 2.20660 VALENTINE 230