SILVERSIDE-64

MAGNETOMETER Mil) ELECTROMAGNETIC SURVEYS 2002

THACKERAY AND GARRISON TOWNSHIPS

LARDER LAKE MINING DI VI SI Of J

DISTRICT OF COCHRANE, ONTARIO

FOR

TIGER GOLD EXPLORATION CORPORATION

MISS WEHDY K. WELLER

GEOTECH

OCTOBER 2, 2002

32D05NW2136 2.24288 GARRISON 010

TABLE OF CONTENTS

SUMMARY. . . . . . . . . . . . . . . . . . . . . . . . . . i)

INTRODUCTION . . . . . . . . . . . . . . . . . . . . . . . l

LOCATION AND ACCESS. . . . . . . . . . . . . . . . . . . . l

PROPERTY HISTORY . . . . . . . . . . . . . . . . . . . . . 2

GENERAL GEOLOGY. . . . . . . . . . . . . . . . . . . . . . 2

TOPOGRAPHY . . . . . . . . . . . . . . . . .. . . . . . . . 3

INSTRUMENTATION. .....................3,4

PRESENTATION AND DISCUSSION OF RESULTS ..........4,5

OBSERVATIONS AND CONCLUSIONS . . . . . . . . . . . . . . . 5

ASSESSMENT DATA FORM . . . . . . . . . . . . . . . . . . . 6

TECHNICAL DATA . . . . . . . . . . . . . . . . . . . . . . 7

BIBLIOGRAPHY . . . . . . . . . . . . . . . . . . . . . . . 8

CERTIFICATE . . . . . . . . . . . . . . . . . . . . . . . 9

MAPS AND TABLES

LIST OF CLAIMS - FIGURE la). . . . . . . . . . . . . . . . la)

CLAIM LOCATION MAP - FIGURE ib). . . . . . . . . . . . . . ib)

LOCATION MAP - FIGURE le). . . . . . . . . . . . . . . . . le)

TABLE l - TABLE OF LITHOLOGIC UNITS - FIGURE Id) . . . . . 2a)

TABLE 2 - SCHEMATIC DIAGRAM - FIGURE le) . . . . . . . . . 2b)

GROUND VLF-EM SURVEY MAP SS/2002/vlf . . . . . . IN SACK POCKET

GROUND MAGNETOMETER SURVEY 98 - MAP SS/2002/mag IN BACK POCKET

SUMMARY i)

The report includes a Magnetometer and an Electromagnetic survey as required by The Ministry of Northern Development and Mines for assessment work purposes.

The report includes an introduction to the property, property history, general geology, field observations and con clusions based on the field surveys.

Assessment and Technical data forms are provided at the back of the report. Field data is compHed on the accompany ing plan maps also found in the back of this report.

SILVERSIDE-64

MAGNETOMETER AND ELECTROMAGNETIC SURVEYS 2002

THACKERAY AND GARRISON TOWNSHIPS

LARDER LAKE MINING DIVISION

DISTRICT OF COCHRANE, ONTARIO

INTRODUCTION

The mining claims

claim group consists of sixty-four (64) unpatented eight (8) of which are included in this report.

On August 23, 2002, the start of a recut and two man chaining in the 1998 north/south grid was started. The picket lines are 100 meters apart and stations every 25 meters. Recut contracted to Alain Pariscoat. The two man chaining was performed by Gwen Resources Ltd. Magnetometer sur vey was done by Mr. John Perron, one vlf station, maps and reports were done by Miss Wendy K. Weller.

The line spacing is approximately 100 meters and the sta tions were cut and measured every 25 meters.

Tie line 300 South was re-established and read.

Ownership of the aforementioned unpatented mining claims has been attested to by Gwen Resources Ltd., and was not indepen dently ascertained by the writer.

LOCATION AND ACCESS

The Silverside-64 Grid is located north and south of east-west boundary of Thackeray and Garrison Townships.

the

The Silverside-64 Grid is in the Larder Lake Mining Division, and they are within the jurisdiction of Kirkland Lake Resident Geologist.

Access is from Kirkland Lake towards the east for 13 kilometers to the Harker-Holloway road (Highway 672) north for 25 kilometers to logging road #49 than 13 kilometers north/west to Silverside-64 Grid.

(See figures Ib) and le).

-l a)-

HORK PERFORMED ON THE FOLLOWING CLAIMS THACKERAY TOWNSHIP

FIGURE la)

L-789865

L-789866

L-792322

L-792323

L-792324

L-792328

L-792329

L-792330 8 CLAIMS

-l b)-CLAIM LOCATION MAP GARRISON/THACKERAY TOWNSHIPS FIGURE lb .)

r—

. — ^ . ——J-T - '——-rT-—— —— —— f- W —— ~TT it IT , , L '' ~

K ^'J 758868 ^

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H l.

'-t-^-i/.-'.'^/^^ A7j — i _ l T" (803343 J803S4a |e03S47 1792313 l"" 14— .-— — . _ . ,

J ...., i .~ rS23O1 TOJVU; "742307 'T-O^HI " 7B25H ' 792320 ( 792X6 ( ""07 j 7,2312 ( 782313 ( 792323\"2JMj — — f- — -t---t-— -r--t— J — 4 —

——— L- — -r- — —-, "2302 TVZJ03 I79J3O8 '792311 "2318 |7923,*' 7,2324 jV*"7 '

7*2303 (792304 792309 ' 792310 , 7,23,7 1 792318 'p2J2J I \L ||4I2 ---J ' -J. J. -2- tt

j 1211408 j lil HOT l]'5"— -j- —

1.1047511 l

T92332 |792339f 82i* 2 j ^^S^ j 73*327

792333 7933Mj7*234J l 792348 f 7JM42

1 L '

7923341782337(7933*4 792347 73**4,--f--;-^-—— .""33 7J23MI7V2343 1 ""4* 73AS40

i 1 1—— —1 — ~" 1 — —— — \ —

| *7348\ j 1047303 10473C8 j

104rS10 . i 1 *4n*\f— — -J-f- - t---|--;,.iPH4n^ r i ' i r' ^ ' ' 'WvJ f ] 1O47S|J 1,047/513 1W75t * 10*7513 1 \1 | 04/313 | 1,0475,8 ,1 1 __ L L -J- --l— - i~ —— i1 1 J ' 1 '1 1048998 L/g 1 1047000 1 1C*700, 1047749

— ~— ——— —— ——— ——— l \--~A- ——~ r ---f ---j----

J104f7003

l ——— 1 ^~MOSOM9 ' i /T 1 ' 'vi

f~ ~ ~ -J J ^-^ J1C30120 | ^~~"^~TlD ———t\ 1 ^-TL tV-' /'A I1048IIO | 1048111 ,\\ ^

1047004 1047D05 | 1C470O6 1047753

U-|-f-—— -I0477S4 l 1047753 10*7732 |-j __ in7 !10477J9 104T718 1047757 10*7758

f-'Vk L-.i..,4j-^J\^t^4-- T,..1,05012, \^\ 1 1 l ( i f1 ' 1| ^ X .1048HJ ,10A81,2 1047785 1

1\ \.l 1047783 "1047782 1047781

104 V'

1 10SOI25 10S01 22 toaogo 10440M i34aoM | 104ao87 ' 10*8006 ' 1048104 l ^ '' ll O II [1047931 I0478JO Jl0477M 1 1047757 '~~(— - H- - ----J ——— I — ..j— - ^ — . K —-4 ——— i ——— J^. —— __| 1(W77M20 i "0301^^ 1 uy0 1 2 J | 1G4 AOQ7 IfldftfVftrfl IA^LAAAC ^ 104AO04 l 1 ^-' t/v^^ ll j l ill 104ao" | I047"? - — f- — — 4- — — 4- -t- -- ^ J T-j — i _ i 1

T IO'1*M5 i 1M'3— l r -h----1 - -t- ^ ' ' ~f i 'T'"'"\ ' *- -

1

1

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1

-1

1

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J31

1

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1

——

4

^

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THACKERAY

-i c)-

Location Figure

-2-

PROPERTY HISTORY

1985 - Kerr Addison Mines Ltd. Magnetometer 4 Electromagnetic Surveys

1986 - Kerr Addison Mines Ltd. Induced Polarization Survey

1997 - Magnetometer S Electromagnetic Surveys September 3, 1997

1997 - Magnetometer 4 Electromagnetic Surveys December 22, 1997.

Ownership is attested to by Deak Resources Ltd. of 103 Government Road East, Kirkland Lake, Ontario, and was not independently ascertained by the writer.

GENERAL GEOLOGY

L. S. Jensen (O.G.S. Report 165) states that the predominate underlying bedrock is mainly basaltic and andesitic volcanic rocks of the Tholeiite Suite.

((Volcanic rocks of Thackeray Township appear to have been deposited on the northern flanks of volcanics)).

tuffs.Tholeiitic volcanic rocks are a sequence of lava flows and

The tholeiitic sequence is composed of three rock types; low Iron, magnesium-rich tholeiitic basalt, Iron-rich basalt and tholeiitic rhyolite. (Shown in Figure "Id) Table l - Table of Lithologic units).

a) FauU:

L. S. Jensen (O.G.S. 165) states ((lineaments are long linear valleys and depressions partly filled with alluvium and occupied by streams. These lineaments represent narrow shear zones or faults.)) As shown on Table 2 - Figure le) the north/west fault goes through the Thackeray Creek System.

b) Munro Esker:

The Thackeray Creek System is located in the center of the Munro Esker. The Munro Esker is a vast area of Glaciofluvial well sorted strata of medium and coarse-greenish sands, gravel large erratics. Due to the errosions of the Munro Esker, the rela tionship between faults, and the net-slips of faults cannot be determined accurately.

-2 a).

TAQLE 1

JIGURE Id)

TABLE OF LITHOLOGIC UNITS FOR THE THACKERAY, ELLIOTT, TANNAHILL. AND DOKIS TOWNSHIPS.

PHANEROZOIC CENOZOIC

QUATERNARYPLEISTOCENE AND RECENT

Till; reworked till, eskar sand and gravel, varved clay, duno sand, alluvium and peat

UNCONFORMITY

PP.ECAMOTUANMIDDLE TO LATE PRECAMBRIAN (PROTEROZOIC)

MAFIC INTRUSIVE ROCKSOlabaia nnd querti dlabaia

INTRUSIVE CONTACT

EAHLY PRECAMBRIAN (ARCHEAN) FELSIC INTRUSIVE ROCKS

SYENITIC INTRUSIVE ROCKSEquigranular and porphyritic tyanodlorlta, monzonlt*, fyenlta, feldipor

porphyry, peoffiatlta and lamprophyre

INTRUSIVE CONTACt

GRANITIC INTRUSIVE ROCKSQuartz dlorlta, granodlorlia. trondh|amlt*. faldipar porphyry, and hybrid

roehi

INTnUSIVE CONTACT

MAFIC INTRUSIVE ROCKSGabbro, quartz gabbro, dlorlta, quartz dlorlts, hornblende gabbro, nnd

anorthosite flabbro

INTfiUS1VG CONTACT

VOLCANIC ROCKSRHYOLITIC AND OACITIC VOLCANIC ROCKS

Cala-Alkilln* SullaMaiilv* bracci*, flow-breccia, pyroelaitla braeela, tuff, eryitgl luff, imygda-

laldal, rhyolltlc and daelllo rocki faldipar. and quartz porphyry, rhyolltlc and doeltlc roc l* t

Thofellilc SullaSphorulltle tuff and tuff-breccia, and charty tuff, rhyolltlc and dacltlc rccki

HASALTIC AND ANOESITIC VOLCANIC ROCKS Calc-Alknllna Sulla

Maiilvo, plllownd braeela, pyroclflltla brocola, tuff and Inpllll-luff, omygda- laldol, porphyritic faldipar bnialtle and andailtle rocks and grgentchln nnd amphibolite faclei, mota-bnioltlc and maia-ande:ltlc rocks

Tholollilc SulioOlnck lo dark greon, high-Iron, monlvo. plltowtd flow-top breccia, pillow

braccla, hyaloclaitle, variolitic and amygdaloidal baialilc and andciliic rocki and Intarflow Mdlmonti

Groy lo green, hlflh-maonaslum manlva, pillowed, flow-top breccia, pillow- brerclo, hyoloclaitlc, porphyritic faldipar, variolitic ond hninlllo rocki nnd InlorTlnw inrllmonli

SUC 1365'

o

•n*—*CT)

O

l

F.rjuie 16-Schemaiic duQfarn showing the main slnjctutal relationships in the map-atea.

-3-

TOPOGRAHY

Throughout the grid north and south of the baseline, there are many old and new beaver pond systems feeding into Thackeray Creek.

The vegetarion ranges from jack pine replant on the glacial esker (in the north/west side of the group) to thick alder and poplar swamps in the east side of the grid.

INSTRUMENTATION

Magnetometer Survey:

This system uses a backward motion of spinning protons of a hydrogen atom within fluid of hydrogen and carbon. These spinning magnetic protons are caused to have two opposite poles by applying a magnetic fluid using a current within a coil of wire. This frequency of precision is proportional to the earth's total magnetic field.

This Instrument 1s read directly 1n gammas which is the absolute value of the earth's total field for that station.

The diurnal variation was monitored by closing each loop at any secondary check station, at a grid line, baseline intersection. Diurnal corrections were applied by linear distribution of any observed variation over the time between base stations.

Electromagnetic Survey:

The VLpnEM method1 uses as a. source, several of the main sub marine communications transmitters in the 15 to 25 kHz band found throughout the world,

The submarine communication radio waves travel In a si^jlo mode parallel to the surfaces of the e.irth along the earth-air inter- ace.

VLF instruments are capable of picking up any structures that change the direction of the waves by measuring the tilt angle being zero on flat ground, but when a conductor is present, the tilt angle will acquire a finite value. The direction of tilt indicates the direction of the conductor.

Calculations of such parameters as depth, depth extent, dip and width of the conductors is very minimal.

The VLF easily illustrates the location of the upper "M^K

-4-

of dipping structures which can be seen or plotted as VLF profiles as areas of greatest change in tilt angle per unit of distance.

The instrument used for this survey was a Geonics EM-16 Unit. The sensitivity of this unit is l* for the inphase and l* for the quadrature. The operating frequency for the EM-16 from 15-25 kHz and the station is made by plug-in units.

Further information on the VLF and the magnetometer can be found in the back of this report on the Technical Data and Assessment forms.

PRESENTATION AND DISCUSSION OF RESULTS

i) Magnetometer Survey 1998:

The field data is presented on Map No. SS/2002/mag at a scale of 1:2500 meters, found in the back of this report.

The magnetic data is illustrated as isomagnetic con tours, contour intervals 50 to 100 gammas, on a map of corrected magnetic values recorded at each station.

The magnetic relief ranges from 57,444 gammas to 58,283 gammas, difference of 839 gammas.

The magnetic trend is in a north/east direction. Thereis not much of a difference in the magnetic relief this usuallymeans no or very slight difference in the host rock in the area.

i i) Electromagnetic Survey:

The field data is compiled on the Map No. SS/2002/vlf at a scale of 1:2500 meters, found at the back of this report.

It was decided to use the Seattle, Washington station in the survey, due to the direction of the old picket lines.

In this survey 4 distinctive contacts were found:

Ql - Crosses PL600E 724N to PL700E 765N.The area is wet thick alder swamp. This contact is in the same direction as the magnetic trend for the area. The quadrature is negative.

Q2 - Crosses PL600E 075N to PL700E 121N.The area is poplar, alder swamp. The contact is found along the south edge of a large magnetic low that crosses three quarters of this section of grid. The quadrature is positive.

03 - Crosses PL800E 400N to PL/OOOE 500N.The topography of this section of grid is a steep ravine

-5-

running in the same direction as the contact. This contact may possibly be a northeast fault off the main Canyon Fault that runs North/South along Thackeray Creek System.

Q4 - Crosses PL1000E 200E to PL1200E 250N.This contact is also found along the south edge of the large magnetic low system that crosses the property. Also this contact could be caused by water.

OBSERVATIONS AND CONCLUSIONS

At the present time the rest of the 1998 grid is being re-cut and two man chained. Due to the amount of blodown and very heavy growth around the alder swamps the old picket lines were re-turned and followed as closely as possible to the original lines.

Both magnetometer and VLE-EM Surveys will be completed in the next month.

Respectfully submitted,

October 2, 2002 Miss Wendy K. WellerGeotech

-6-

Assessment Data FormType of Work.-Prospecting:............................... Geolpglcal'.Physlcah LINE CUTTING AM CHAININGGeophysical: ELECTROMAGNETIC ^ STATION) AND MAGNETOMETER SURVEY

Geochemical:......-.......-..-.......

Assays/Analyses:..,................. Other

Cost of Work:..!4;.2.^;.0.0......... Dollars Applied :..s4.237.oo

Recorded Holder: Survey Company:Name:.GWEN. .RESOURCE^ LTD ../PERREX. R.ES...INC Ma m 6 r

Address t.lO^ .GO^V ERNME^T JO/^ MS JA- ^ Address :. 103. -GO-V ERNNEN T^ f-OAp^EA S T^,

KIRKLAND LAKE, ONTARIO P2N IA9 . K. [ ^.LAf!?..L.A.^ E.' OjNTAP.IO P2.N IA9

S u r'v e y 7 Re p'o'rt" TnTo'r'm a fi on :Start of work:.AUGUST 23A .200Z-,....... Enct of work\.5 E.p™.B.|R.?.0A..2.Q??......

Draughting lime:..s.E.PT.2jJ..30J..^oOZ. Report' timG--.^EPT -.3pA ^pCT. l, j()02

Completion of r e po r t -... OCTOBER^, ^ 2002 AU t hor:...Mi.ss .'.JEHOY^K^ WELLER ...,

Work performed on claim(s)...............................................................

.. .L "7.?? 6.^ .L.:!l9.8.6.6. ! A: Ll2.3.2?^ .L\7?^^^

Work applied to claim(s) ...L-735604, L-735605, L-735606","L-735607i"l"-"735608, 1-736*844, [-7*36845, L-736846,

" "I" 7368477"!"- 736*848'," "C- 784869"" U-784872 "'

Persons who performed work (supervisor first):. ~!1" E !LR.E.59.UJ?? E.S LTO -

WENOY K. WELLER

JOHN E.^.^

ALAIN PARISCOAT

-7-

Technical Data:Line (mi/km):.. A3?.^!...:.-.-— — ~- Line traversed:......-— ...—.

No. of samples/stations-.........??.6...- Line/picket spacing:.,}.0.0,/.2.5..1?.

ELECTROMAGNETIC SURVEY: 0 Perator:. N.D.Y..^..w.E.L .L LR......

Instrument-. GEONICS EM' 16""" ^ .,

Coil configuration:....HORiZQNTAi...... Coil separation:.. ..I.NFINJJY

Method L.Ml0.-!^.!^.1!™-...--...... Parameters:J.f.^^

Vertical^7a7ed".^..;.LA0.:.........'. Horizontal scale-..2J?.OM

Operational technlque:...AkUiLEM!^^EAST 90 0 TO STATION

MAGNETIC SURVEY: .,... .....v

lnstrument:..J'iCPHAR^GP--8^^^^^^^M- Accuracy;....

Base station..._,. ?.L.90pE^^^M . Diurnal

Base station time^.i0..'!1.^!.^...._.. Localion/value;.

Contour interval :....5.?..G.iM.^L........ Datumn subtracted-

Contoured by:...WENDLl--.w.E LL.E?......... Horizontal s ea l e-......1..:. 2 L0.0.

Operational technique:......s. s.0.Lp5.E..M.0.u.!IL.^

INDUCED POLARIZATION SURVEY

Transmitter used........................ Receiver used:......

Method:........................................ Frequency............

On time:..................................... Range:..........,.........

Off time;...................................... Delay time:.............

Power sou ree:............................. Output ;..................

Electrode array.1........................ Electrode spacing^.

Readings taken:.......................... Other data;..........

Operational technique:,.

-8-

BIBLIOGRA'PHYFile No. KL-1374 - Kerr Addison Mines Ltd.

(iKerr-Garrison Property))

Garrison and Thackeray Townships

L. S. Jensen - Ontario Geological Survey, Report 165,

Geological of Thackeray, Elliott, Tannahill, and Dokis Townships, District of Cochrane, Ontario

by L. S. Jensen

Wendy K. Weller - Silverside-64 (Thirteen Mining Claims)

Magnetometer and Electromagnetic

Surveys 1997

Thackeray'S Garrison Townships

LARDER LAKE MINING DIVISION

DISTRICT OF COCHRANE, ONTARIO

September 4, 1997

Wendy K. Weller - Silverside-64 (Fifteen Mining Claims)

Magnetometer and Electromagnetic Surveys 1997

Thackeray S Garrison Townships

Larder .Lake Mining Division,

District of Cochrane, Ontario

December 22, 1997

s Wendy K. Weller - Silverside-64 (Sixteen Claims)Magnetometer S Electromagnetic Surveys 1998Thackeray and Garrison TownshipsLarder Lake Mining Division,District of Cochrene, OntarioFor Alexander H. Perron 'May 11, 1998

Wendy K. Heller - Silverside-64 - 9 ClaimsMagnetometer S Electromagnetic Surveys 2002 Thackeray S Garrison Townships Larder Lake Mining Division District of Cochrane, Ontario September 23, 2002

-9-

CERTIFICATE

I, Wendy K. Weller, of Kirkland Lake, Ontario, do hereby

certify:

1) That I am a Geotech in Training and reside at:

71 Second Street, Apartment //2, Kirkland Lake, Ontario.

P2N IR6,

2) That I graduated from the Haileybury School of Mines as

a certified Diamond Driller in 1982. I have had a staking

licence for the past 12 years.

3) That I was employed as a Diamond Driller for Heath 4 Sherwood

for l year.

4) That I have been practising as a Geotech Trainee for a period

of twelve (12) yrs.and I am qualified to write this report.

5) That I supervised and participated in this survey.

Date ' —————— ^ndy K/^Welle/Geotech

ONTMIO MINISTRY OF NORTHERN DEVELOPMENT AND MINES

Work Report Summary

Transaction No: W0280.01529

Recording Date: 2002-OCT-02

Approval Date: 2002-OCT-15

Client(s):

140281 GWEN RESOURCES LTD.

181187 PERREX RESOURCES INC

194505 STARMIN MINING INC.

Survey Type(s):

LC

Status: APPROVED

Work Done from: 2002-AUG-23

to: 2002-SEP-30

MAG VLF

Work Report Details:

Claim#

L

L

L

L

L

L

L

L

L

L

L

L

L

L

L

L

L

L

L

L

735604

735605

735606

735607

735608

736844

736845

736846

736847

736848

784869

784872

789865

789866

792322

792323

792324

792328

792329

792330

Perform

soSO

sosososososososososo

S230

S415

5665

S372

S260

S562

S774

S959

54,237

External Credits:

Perform Approve

soSO

sososoSO

sosososoSO

SO

S230

S415

S665

S372

S260

S562

S774

S959

54,237

SO

Applied

S193

S400

S400

S400

S400

S400

S400

S400

S400

S400

S400

S44

SO

SO

SO

SO

SO

SO

SO

SO

S4.237

Applied Approve

5193

5400

5400

5400

5400

S400

S400

5400

S400

5400

5400

S44

SO

SO

SO

50

SO

SO

SO

SO

54,237

Assign

SO

SO

so50soSO

SO

soSO

SOSOSO

S230

5415

5665

5372

5260

5562

5774

5959

54,237

Assign Reserve Approve Reserve Approve Due Date

0

0

0

0

0

0

0

0

0

0

0

0

230

415

665

372

260

562

774

959

54,237

SO

SO

SO

SO

SO

SO

SO

SO

SO

SO

SO

SO

SO

SO

soSO

sosoSO

SO

50

SO 2003-OCT-03

SO 2003-OCT-03

SO 2003-OCT-03

SO 2003-OCT-03

SO 2003-OCT-03

SO 2003-OCT-03

SO 2003-OCT-03

SO 2003-OCT-03

SO 2003-OCT-03

SO 2003-OCT-03

SO 2003-OCT-22

SO 2002-OCT-22

SO 2003-FEB-21

SO 2003-FEB-21

SO 2003-MAR-14

SO 2003-MAR-14

SO 2003-MAR-14

SO 2003-MAR-14

SO 2003-MAR-14

SO 2003-MAR-14

SO

Reserve:SO Reserve of Work

SO Total Remaining

Report*: W0280.01 529

Status of claim is based on information currently on record.

32D05NW2136 2.24288 GARRISON

2002-Oct-16 01:44 Armstrong-d

900

Page 1 of 1

Ministry ofNorthern Developmentand Mines

Date:2002-OCT-15

Ministere du Developpement du Nord et des Mines Ontario

GEOSCIENCE ASSESSMENT OFFICE 933 RAMSEY LAKE ROAD, 6th FLOOR SUDBURY, ONTARIO P3E 6B5

PERREX RESOURCES INC. 103 GOVERNMENT ROAD EAST KIRKLAND LAKE, ONTARIO P2N 1A9 CANADA

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

Dear Sir or Madam

Submission Number: 2.24288 Transaction Number(s): W0280.01529

Subject: Approval of Assessment Work

We have approved your Assessment Work Submission with the above noted Transaction Number(s). The attached Work Report Summary indicates the results of the approval.

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.

If you have any question regarding this correspondence, please contact STEVEN BENETEAU by email at steve.beneteau@ndm.gov.on.ea or by phone at (705) 670-5855.

Yours Sincerely,

Ron GashinskiSenior Manager, Mining Lands Section

Cc: Resident Geologist

Gwen Resources Ltd. (Claim Holder)

Assessment File Library

Perrex Resources Inc. (Claim Holder)

Perrex Resources Inc. (Assessment Office)

Starmin Mining Inc. (Claim Holder)

Wendy Kathleen Weller (Agent)

Visit our website at http://www.gov.on.ca/MNDM/LANDS/mlsmnpge.htm Page: 1 Correspondence 10:17638

IM1HKN DEWLOFHEItl

6*n*r*l Inform*tlon.tnd Llmltttlorwn .M*Mn*MDIIHrtkwl,ltliy *HDM PKMPH ttrwgtl (M tocri.LIM* TRkl H Kt|*by O Me l, w. H* Mtl

MINING LAND TENURE

MAP

uCI

M

lo00

to o o

Date; Time of Issue Aug 7 2002

TOWNSHIP/ AREA

THACKERAY

11:37 K Eastern

PLAN

0-3220

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PLAN

0-3638

ADMINISTRATIVE DISTRICTS l DIVISIONSMining Dlvl*bn Ltrd*rLtk* Lund Tlttoi/R.glttry Division COCHRANE Ministry of Natural ReEOLtrces District KIRKLAND LAKE

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