-

--

DErAI l MAGNETOi~f:.IER Arm Elf.CTROMAGflET I C SU RVEYS ON THE

ELL! OIT -35 {\IW ell FFORD-6 -~

t:llIOT r Ar~D CLI ~FOHD TOWtJSHI PS

LARDER LAKE r"rrHNG DIVISION

DISTRICT OF THIIS~'III~~GJ ONTARIO

FOR

TIGER GOLD EXPLORATION CORPORATION

t1ARCH 29.1 2005

PROVTNCTA1:""R"E"C 0 R DIN G OFFICE· SUDBURY

RECEIVED

----------------_._-

MISS WENDY K. WEllER

GEOTECH

TABLE OF CONTENTS

SUMHARY. . • ••

INTRODUCTION •.

LOCATION, AND ACCESS ..

PROPERTY HISTORY

REGIONAL GEOLOGY .

TOPOGRAPHY . • • .

. . . . . . . .

2005-E-3S MAGNETOMETER/ELECTROMAGNETIC SURVEYS.

OBSERVATION AND CONCL8sIONS ..

CONCLUSIONS.

REFERENCES •

TECHNICAL DATA •

ASSESSMENT DATA FORM •

CERTIFICATE. • ••••

MAPS

. . . . . . . . . . . . . .

LOCATION AND ACCESS (FIGURES la) and 1b) • • • • . ..

TABLE 1 - TABLE OF LITHOLOGIC UNITS FOR THE THACKERAY, ELLIOTT, TANNAHILL AND DOKIS TOWNSHIPS

GEOLOGICAL SETIING . . . . . . . . . . . . .•..

.il

· 1

· 1

• 2

• 2 I 3

· 3

· 3, 4

· 4, 5

· 5

6, 7

. . . 8

. . • 9

• . 10

1 a)

2 a)

• 2 b)

GROUND MAGNETOMETER SURVEY MAP NO.CE35/20Q~/~ag. . . . IN BACK POCKET

GROUND VLF-EM SURVEY - NAA PROFILED MAP NO.CE35/200Sj'l1 fIN BACK POCKET

SCHEDULE A ..•. WORK RECOMMENDATION .......•....• 1 a)

SUIi~ARY : i)

The report includes a Detail Magnetometer and Electromagnetic Surveys 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 conclusions based on the field surveys.

Technica1 data is provided at th~ back of this report. Field data is compiled on the accompanying plan maps CE35/2005/mag & CE35/2005/vlf found in the back of this report.

Due to the results of north/south winter survey, it has been decided to reverse the direction of the grid to be able to identify the north/south faults crossing the winter grid.

-1 a)-

WORK RECOMMENDATION SCHEDULE A

TIGER GOLD EXPLORATION CORPORATION 103 GOVERNMENT ROAD EAST, KIRKLAND LAKE, ON P2N 1A9

TELEPHONE (705) 567~300'

Michael Hanington. P.E., Mining Vice-president ofEx:ploration Tiger Gold Exploration Corporation 201 S. Greenfield #)0 Mesa. Arizona 85206 (480) 324-0910

March 2). 2005

Wendy Weller Geotech TIger Gold Exploration Corporation 103 Govcnunent Road East Kirkland Lake, ON P2N 1 A9

Dear Wendy,

RE. Ellion 35 Claims L·3013919 and L-4203546 Elliott Township

After reviewing the results of the magnetometer ami electromagoetie surveys OD the above noted property it is apparent, without question, th&t in·fill surveys running East and West are warranted and ahould be dODe at your first opportunity.

The nonhlsouth base line, and other appropriate refc:rence standards are of your choosing but picket lines should be turned off every 50 metcrl, 90 degrees East a.od 270 degrees West and S'LIltions mould be cut and measured f:Vety 25 meters.

If you have: any questions please call. Your attention to this is appreciated., thank you.

DETAIL MAGNETOMETER AND

ELECTROMAGNETIC SURVEYS ON THE ELLIOTT-35 AND CLIFFORD-6

ELLIOTT AND CLIFFORD TOWNSHIPS

LARDER LAKE MINING DIVISION

DISTRICT OF TIMISKAMING, ONTARIO

INTRODUCTION

There are 4 blocks (35 units) in the property. Claims L-4203510 and L-4203546 are composed of 12 units and located in Elliott and Clifford Townships.

Due to the results of the new north/south grid in Claim L-4203546, on March 8. 2005. a new east grid is being established using PLOOO of the north/south grid as the baseline.

The baseline has also been extended across claim L-4203510 in Clifford Township. for a total distance of 2400 meters. Picket lines are turned off at every 50 meters 90° east and stations are cut amd measured every 25 meters.

Weller.

Line cutting was performed by Tiger Gold Exploration Corporation.

The magnetometer survey was performed by Mr. John E. Perron.

The electromagnetic survey was performed by Miss Wendy K.

All drafting and contouring and report writing was done by Miss Wendy K. W~ller.

LOCATION AND ACCESS

The two claims that make up the E-35 Property have a common Doundary along the Elliott-Clifford Township line. The line has never D~en established by legal survey, and it's position on the ground is a oest estimate. Co-ordinates of 48 degrees 21 minutes north latitude and 79 degrees 50 minutes west 10ngtitude are located approximately central in the claims (NTS 320/5).

The E11iott-35 are in th~ Larder Lake Mining Oivision, and they are within the jurisdiction of the Kirkland Lake Resident Geolo­gist. Access is frow Kirkland Lake towards the east for 13 kilometers to the Harker-Holloway road (Highway 672). Follow 672 north for 24 kilom~ters to the claims. Highway 672 traverses across most of the property. Other access is available due to logging operations.

ONTARIO

-1 a)- LOCATION AND ACCESS FIGURE la) & 10)

CLIFFORD TWP.

N

(,)

w CIl w ::> a

INDEX WAp· 'CAL£: 1:1013780 Oa.18mllu)

ELLIOT\T TWP. I

CLIFFORD TWP.

~ AIR MA6NETIC DATA 't •• G.I.C., 1113

-'-'l

I I

--1-I i~c 'l I e

April 199~, w.K.W. . 320/0

I SCALE I: 20 000

f

I

-2-

PROPERTY HISTORY

1993 - Mr. R. K. Germundson - Geological Report on the A&A Mining Group, can be seen at the Regional Assessment Office.

1994 - Miss Wendy K. Weller - Detail Magnetometer ,and Electromagnetic Surveys on the A&A Mining ~laims, can be seen at the Regional Assessment Office.

REGIONAL GEOLOGY

The general area, which includes Elliott and Clifford Town­ships, is underlain by Archean Volcanic Suites belonging to the Abitibi Subprovince, Superior Province of the Canadian Shield. The volcanic rocks are intruded by a variety of related mafic to felsic stocks sills and dykes. Later Precambrian dykes of diabasic composition and texture trend in a north-westerly, northerly or northeasterly direction and have filled in along pre-existing structures (see Jansen, 1975 and 1978).

The genera 1 area can be defi ned as being hounded on the south by the Larder Lake Fault and on the north by the Oestor­Porcupine Fault, both regional, east-west trending structures along which are major gold mining camps such as Timmins, Harker-Holloway, Kirkland Lake, Virginiatown and Val O'or. A major east-west trend­ing syclinor;um is present between the two faults. The younger Slake River Group is flanked on the north and the south by rocks of the Kinojevis Group. (See Geological Setting). The southern contact between the two groups is much more structurally affected than is the northern contact.

Rocks of the Kinojevis Group are to a large extent composed of iron tholeiites. Such iron-rich composition is reflected in bands of high magnetic susceptibility alternating with bands of lesser magnetism. The weaker zones of magnetism outline sequences of sedi­ments and/or calc-alkaline volcanics. The contact with the overlying Btake River Group can be defined from air magnetic data, however a Zone of vertical gradation up to a mile wide mayor may not be pre­sent. Subtle magnetic variations which may represent economically significant features (Kimberlite pipes or alteration zones) can easi­ly be masked within the Kinojevis Group.

Blake River Volcanic Rocks are composed of calc-alkaline minerals. Massive and pillow flows occur in sequence with pillow and pyroclastic breccia and lapilti and ash tuff. Chemically they represent rhyolite, dacite, andesite and basalt. Rocks of the Blake River Group underlie the base metal camp of Noranda, Quebec. East­ern Clifford and Ben Nevis Townships have several base metal showings as well as rela tively more bed rock exposures then has the AM Group.

TABLE 1 . -2 a)- .

TABLE OF LITHOLOGIC UNlTS FOR THE THACKERAY, ELLIOTT, TANNAmLL. AND DOKIS TOWNSHIPS •.

PHANEROZOIC CENOZOIC

QUATERNARY PLEISTOCENE AND RECENT'

PRECAMBRIAN

nil; reworked till, esker land and gravel, varved clay, dune sand, alluvlulT' and peat,

UNCONFORMITY

MIDOLETO LATE PRECAMBRIAN (PROTEROZOIC) MAFIC INTRUSIVE ROCKS

Diabase and quartz diabase

INTRUSIVE CONTACT

EARLY PRECAMBRIAN (ARCHEAN) FELSIC JNTRUSIVE ROCKS . SYENITlC INTRUSIVE ROCKS ,

Equlgrinular and porphyritic cyenodlorlte, monzonlta, syenite, feldspar porphyry, pa~atlte and lamprophyrt

INTRUSIVE CONTACt

GRANITIC INTRUSIV'E ROCKS Quartz diorite, granodiorite, trondhJemlu, feldspar porphyry, and hybrid ~b '

INTRUSIVE CONTACT

MAFIC INTRUSIVE ROCKS Gabbro, quam gabbro, diorite, qulttl diorite, hornblende g3bbro, and

anorthosltlc vabbro •

INTRUSIVE CONTACT

VOLCANIC ROCKS RHYOLITIC AND DACITIC VOLCANIC ROCKS

Caic-Alkllln. Sulta M.alv. braccl., f1ow-bnccla, pyrocl.stlc bnccla, tuff, cryml tuft, amygda­

loldal, myolltlc .nd daclde rockl f.ldspar, and quartz porphyry, rhyolitic end dacltlc rock. '

Tholalltlc Suite .spharuUtlc tuff and tuff-breccra, and cherty tuff, rhyolitic and dacitic rocks

I

BASALTIC AND ANDESITIC VOLCANIC ROCKS Cafe-Alkalln. Suite

Mass/v., plllowld breccia, pyrocl.rtlc breccl., tuH and lapilll·tuff, amygda· lold.l, porphyrltlc feldspar b.sa"itlc and andes/tic rocks and greenschist and amphibolite '.cJ .. , meta-b.saltlc and met.-.ndesitic rocks

Tho/.lttle Suit. Black to dark grl.n, hlgh.fron, mau/v., pilloWed flow-top .brecc/e, pillow

bracel.,· hyalocl.stlc, varlolltlc .nd amygda/old,1 basaltic and and8sltlc ~k? and Interllow Mdlm.nU

Grey to green, hrgh-magneslum massive, pillowed, flow-top breccia, pillow­bncc/a, hy,loclastlc, porphyritIc ,.ldspaT, varlolitlc and amygdaloidal b.saltlc roclu end Intarllow sedlmenu

Geological Setting

o I ! t T miles)

x

r­III .,: • II

9 J

+ B -30_:A-t-I-_

Morrisette

-+ A·4 A

MA-20

Kirkland Lake o

+

-2 b)-

1: The New Bullonta

2: Holt- McDermott Mine

X: Sase Metals:!: Gold

- - Fault ± Diabase Dik~

'\

'\

x '

+ .,.-'--r -" ----...........",,- ,

aaU/hi:J \ +--• Virginiatown ':I,\.

<{"~

I

I • I

I

I : I

u' 1.11' c:J 1.11

:J o

• I

April, 1993

-3-

Little magnetic expression is present over the Blake River Group. Because of this circular and linear magnetic bodies are trace­able over great distances. Certain discrete circular features defined by higher magnetic susceptibility are known to be Kimberlites. The loci; of emplacement for kimberlites is structurally controlled (Brurrmer et al, 1992 and 1':'92). A cluster of seven kirnberl.ites Occurs between 10 and 19 kilometers south of the A&A Claims (see erummer, ~ .£!h and HcCl enaghan, 1993). .

«North-south trending structural elements have been identi­fied as important factors in the localization of Kimberlite bodies». (Barron, 1992). The Canyon-Esker Lakes Fault extends from north of The New Buffonta Property towards the south. It is overlain by the Munro Esker for at least 25 kilometers in Clffford, Arnold and Gauthier Townships, south from Highway 66. It crosses both the Destor~Porcupine and the Larder Lake faults. four pipes are located adjacent to it in Arnold Township. Kimberlite dykes also occur adjacent to major struc­tures.

To date, the search for Kimberlites has been related to selecting high magnetic, circular features from airborne data. Recall that Kimberlite pipes can be defined by relatively low magnetism, by no magnetic variation and with or without a conductivity expression. Similar scenarios can be developed for both gold and base metal models.

TOPOGRAPHY

The claim unit covers eight mining claims. There are three large exposed outcrop showings in this unit. A large c,"eek crosses the property with many small drainage creeks feeding into this creek. The vegetation ranges from pine, balsam, alder boggs to open timber cut areas. The BarricK hydro line runs north through the claim group.

2005 - .£35 ~GNETOMETER/ELECTROMAGNETIC SURVEYS

a) McPhar GP81 Proton Magnetometer

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 field using a current within a coil of wire. When the current is stopped, the protons precess about the earth1s magnetic field and in turn generata a small current in the wire. The fre­quency is proportional to'the earth's total magnetic field.

The instrument used for this survey was a HcPhar GP-81 Proton Magnetometer. More information about the survey and instrument can be found on the Technical Data form found in the back of this re­port.

b) Geonics EM-16

The VLF-EM metnod uses as a source, one of the main submarine

-4-

communication transmitters 1n the 15 to 25 kHz band found throughout the world.

VLF instruments are capable of picking up these structures that change the direction of the waves by using the tilt angle of the major axis of the polarization ellipse. The direction of tilt indi­cates the direction of the conductor.

The VLF easily illustrates the location of the upper limit 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 in this survey was a Geonics EM-16.

The two stations used were Seattle, Wash. 24.8 kHz and Annapolis, I~~ryland, 21.4 kHz .. More information about the survey and instrument can be found on the Technical Data Form in the back of this report.

OBSERVATION AND CONCLUSIONS

Magnetic Surve~ 2005:

The magnetic relief varied between 57,006 and 61,848 gammas (four thousand eight hundred and forty two gammas) 4,842 gammas.

The datumn was substracted at 57,000 gammas.

The field Map No. CE35/2005/mag can be found at the back of this report. The magnetic trend is northeast to east direction.

In this detailed survey there are many high magnetic circular ano­malies noted. On the west side of the Barrick Hydro line a low magnetic trend is interrupted by two large high magnetic bands (Iron-rich tholeiitic) There are four large overburdened outcrops throughout this grid, with three large creek ravines. (dr.ainage system to the Magusi River). In the south end of the grid (L-4205310) these ravines may indicate east/west smaller faults extending off the large north/so~th fault noted in the new north/south survey.

Electromagnetic Survey:

The field data is presented on a map at a horizontal scale of 1:2500, Map No. CE35/2005/vlf. Seattle, Washington was used in this survey.

Seattle, Washington showed 3 anomalies in the survey.

Q1 - Crosses PL600S 625E to PL1400S 495E. The topography of the area ranges from the west cliff face in the south end of the grid to flat black spruce bogg. The magnetic relief shows high magnetic anomalies which probably is iron-rich tholeiitic bands.

CONCLUSIONS

-5-

Q2 - Crosses PLIOOOS 360E to PL16S0S 310E. The topography of the area ranges from the steep south side of a large overbuden outcrop to crossing the two steep creek ravines in L-4203510. Also the magnetic relief shows a~~igh magnetic anomalie which is probably iron-rich tholeiitic bands.

Q3 - Crosses PLSOOS 700E to PL1200S 66SE. The topography of the area ranges from fl,at red pine, spruce to the east side of a smaller overburdened outcrop. The magnetic relief shows a high magnetic band (iron-rich tholeiitic bands).

Since there has not been a Geological Survey run over this ground in the past and due to the results of both the magnetic and electromagnetic sur­veys, a vertical loop EM unit should be run to further clarify the origins of the magnetic high and low systems.

A small stripping and trenching program to help clarify the origins of the electromagnetic conductors is being looked at.

Ma rch 29, 2005

Respectfully submitted,

Miss Wendy K. Weller Geotech

REFERENCES

Barron, Keith M.

Brummer, J.J., MacFayden, and Pegg, C.C.

-0-

- Geological Investigation of the New Buffonta Kimberlite, Garrison Town­ship, Ontario. For Gwen Resources Ltd. December, 1992.

D.A.- Discovery of Kimberl ites' in the Kirkland Lake Area. Northern Ontario, Canada. Part I: Early Surveys and the Surficial Geology. Exploration Mining Geology, Volume I, Number 4, pp. 339-350, 1992.

- Discovery of Kimberlites in the Kirkland Lake Area, Northern Ontario, Canada. Part II: Kimberlite Discoveries, Sampling, Diamond Content, Ages and Emplacement. Exploration Mining Geology, Volume It Number 4, pp. 351-370, 1992.

Geological Survey of Canada - Aeromagnetic Total Field Map, Blake River Syncline, Ontario; NTS 320/5, Map 20375 G, scale 1:20,000, 1993.

Jensen, loS.

McClenaghan, M. B.

Ontario Division of Mines

Ontario Geological Survey

- Map of Conductors and Apparant Conducti­vity of Overburden, Blake River Syncline, Ontario; NTS 32 0/5, Map 25057 G, Scale 1:20,000, 1993.

- Geology of Clifford and Ben Nevis Town­ships, District of Cochrane, Ontario. Division of Mines, GR 132, SSp. Accompan i ed by Map 2283, sca l"e 1 inch to 1/2 mile, 1975.

- Geology of Thackeray, flliott, Tannahill and Dokis Townships, Di!itrict of Cochrane, Ontario. Geological Survey Report 165, 71 p. Accompanied by Maps 2367, 2368, Scale 1: 31,680 (1 inch to 1/2 mile), 1978.

- Kirkland Lake Kimberlite Project Area Compilation, NTS 320/4, 5 and 42 A/1, 8. Geological Survey of Canada, 1993.

- Timmins - Kirkland lake Geological Compi­lation Series. Map 2205, 1972.

- Airborne Electromagnetic and Total Intensity Magnetic Survey, Kirkland Lake Area, Clifford Township by Questor Surveys Limited, Prelim Map P.22S3 Geophys. Ser., scale 1:20,000. February and March 1979.

Weller, Miss Wendy K.

-7-

- Airborne Electromagnetic and Total Intensity Magnetic Survey, Matheson­Black River Area, Elliott Township, by Questor Surveys LImited, Map 80609, Scale 1:20,000. March to ~uly, 1983.

- EM-1S, Operating Manual, Page 27.

- Detail Magnetometer and Electromagnetic Surveys on the A&A Mining Claims, 320/5, Clifford Township. Larder Lake Mining Division, District of Timiskaming, Ontario. October 1994

Technical Data: -s-Line (mi/km):_ ••• :?_:~ ... ~~_ ............... . No. of samples /stations: •• ~.!_~~~--.-._

ELECTROMAGNETIC SURVEY: Instrument: GEONICS EM-16

- ------·-VtttrrCAT-ARO·--·-·-Coil configura tion: _______ H_Q.~H9~It\1.--Method; FIXED TRANSMITTER --_._. ------------.;---_ ... _--- ... --Vertical scale: 1 INCH:: - 40~ ------ ------- .. _-- .. -.-._----

Line troversed= ..•••• _ •••• ______ • Line/picket spacing :_:~~::~t~ .. _. ____ .. -...... ..... -.. Opera tor:._ .. _~I.s_~_'!.~~Ql !!_ ~~1k~R

+ -------AccurocY:._: .. J~ ____ .. ___________ _ -.. _- ... Coil seporation: __ I~:~I_TY __________ ••

Parameters: INPHAS£ AND QUADRATURE ----_ .. ---- ---- -- .. _--_ .. ---- ....... Horizontal scale: 1:50000 . ------ .. --. ~--"--.--.- ...

Fre uen : CUTLER = 24.S kHz S a 'on: SEATTLE, WASHINGTON q cy ... ______________ ........... ___ .... t tl ____ ... __________ . _____________ _

Opera tion a I techn I q u e: __ ~~!~_~~!_r~~l.~~:. __ A~~3..~~Q!~~~_I~.K_E~. f~~I~g __ E~~_~ .. _~9~ __ ._ TO THE STATION • .. _ .. -........ _ .. _ ..... __ .. _ ....... ~ .... -_ .............. _._.--_ ....... -... -.- ...... _. -_ ... -_ ..... __ ..... .

. __ .. -... _-.. _- ._ ...... -... -.-. __ .... _. --....... ----- ..... -... -. __ ... __ ... _ .. -... __ ._ .......... __ .... . MAGNETIC SURVEY: Ope ra to r!_~:_.~: • .!:~~~.O.~ ... ____ ... ____ ... Instrument: MCPHAR GP .. 8 PROTON ... _ ... _--_ ............. _- ... -._-- + Ace ura cYt __ = ____ }._G.~~. __ .. ____ ...• _ ...

Bose station. BLOOO _._-_._----.. _-_ .... _ .. _-_. Diurnal method: CLOSED LOOPS BL TIE·INS ---.. _. __ ._---... __ .. _ .. Base station time: EVERY 60 MINUTES _ .. -.. _-_ ... -.---- ....... - Loco1ion Ivai u e: __ ~~~~.~._. _____ ••• __ .....

Contour interval: 50-100 GAMMAS ... -.-............. -......... _--. Dotumn subtracted: 57,000 GAMMAS .._--_._--_ .... _- ._ .... Contoured by: HISS WENDY K. WELLER .. _-... _ ..... _ .... __ .... _ ....... H · t I I 1 : 50000 or,zon a sca e ' •• ____ ._._ .••• _. __ •••.•. _

Opera tio no I tee hn i que : ••• ~.E.~?p_~.P.~~~_!!qy!!~ •.. ___ ... _. __ ._ .. _ ... __ ...... _ ...... __ ..... .. ............ _ ............ -.... -........... _ .................. _ .. _ ......... __ .. _._ .... __ ..... _ ... ---_ .. _-- _.-............ . .. _--.... -.. _. __ .. -.. --_ ... _-...... _--- _. -.......... -_. ---.... ------. -.... --..... - .. __ ... -.. _ ... _ .. -- ... _ .. _. INDUCED POLARIZATION SURVEY

Transmitter used: .. _ .. --.............. __ . __ . Receive r used :. ___ ............... __ •••• _ .. ---Method: --_ .. _ ...... _ ....................... _ ... -_. Freque ncy:. _____ ..... _ ... _ ..••..•.....•.......

On time: _ ..... -_ ... _ .... -_ .... -.. __ ...................... . Ron g e : ....... __ ._. __ ... _ .. _ ... _ .. ______ ..... __ ... _ Off time: "'--.... _ ....... ~ ...... _. -....... _ ... __ .... - De 10 y tim e :._ ... ___ .. __ . ___ .... __ . __ ._. __ .-... _. Power sou rce : _____ •• __ . ____ • __ •• __ .... __ .•. 0 u t put :_ ••••••••••.. __ •. ____ ....... _ .. _ .. ___ .- _ .. .

EI ec t rode or ra y : _________ ._. ____ •• ___ ._ E I ectrQ de spac ing:._ .• ____ •• ___ • __ ... _ .... .

Rea di ng s ta ken :_ •• __ ••. __ •..•• ____ . ____ . 0 the r dot a :_._ •. __ ._._. __ . ___ ........ _ •. -••.. Operational technique: __ .. ..... ... -. __ ...... _ ... _---- ---- ._ ... ---.. _ .. --_ .... __ ............. ---.-. --... --..... _ •... _ ............ --.... __ ........................... _ .... _. --_ .. -_ .... _- -_ ....... --..... _ ............... --... _ ... -....... _ ....... ,..-

.. -...... - ............................... _-.... _ ...... -........... --............................ _. -_ ........... _ .............. -... _ ............ __ ........... -_ ..... -..... ..

... _- ........ _- ..... _- -_ ...... -_ ... -.... -.... -.- ..... -. _.- ........ __ . -_ .. _--- ._-_ ....... ----. __ ... _ .... ---...... -- -_ ... _. -.. -.... ---

-9-

As'sessment Data Form Type of Work:

Pro s pee lin g : ... _. _ .. _ .......... _ ...... _ ...... _ .. • ••. • G e a 199 I c a II ... _ ..... _ .. . . . . . .. .... . . . . .. . . .. .

Ph y s Ica I' ••• _._.::~~_.~~::.r.~~~.~l~~ .. ~~~}!~~ N~. _ •• _ ••••••• _ ••••• _ ••••• _ •••.•.•...•.•••... _. " ..

Ge 0 physIco I ' .. ::.~~~~~~~~_~~~~: •• (.l_.~! ~!.I.~~L~~~_~~~~~I9t1~!~~ .?!~~Y~Y.~ ................. . G eo c hem i c a I : __ ~ .... _ •• _ •••• _ •• _ • _ • • • • . 0 rill i n 9 : •.• _ .................. _ • _ ........ ..

Assays/Analyses: __ ••••• _ •.••••• __ .•• Other work: ••. _ .....•.•.................

Recorded Holder:THE PERRON GOLD Survey ComDony: CORPORATIONI - AT 0

Name .• !Jg_E.R. ~_o~p_ ~~f!-P'~~UQ~. ~9FPQBl\norl~ame: .. T.I~~~.~O_L.~. ~:~.~~~~.~ ~~~ •• c.~~~?~ ... ~ .. N Address: 103 GOVERmofENi ;'O,!-J ~.~H. Addres s :._l.~~ .. ~~~~~~.E.N: .. ~O.~. E~~! ... .. -_ ................................ _ .................. . • ~!~~(~~.:'i.~.~~~~ l. 9~iI~~~q .~~'~ . .l~J .. ... _ ... _ .. ~ ~~~~: ... !g .~:::~~: .. QtITABJO. '" ~ ............... . Survey/Report Information: Star t of Via rk:.. _ MAR~~ .• ~!_.2_q~.. ....... End a f we:;-: : •• _~~~.:~ .~.~~ .. :?~~ ........ . Oroughflng Iime: •. ~~.~:~._:~.,.~:.:~~.,.2.~~~ r..;part· timc: .... MA~C~ .. ~?,.~~, ?o.o.~ ..... . Co m p Ie ti a n a f r e por t ' •• ~~~.~~.~?!. ?:.0p.5.. Aut h 0 r : ••• t~r.~L~!~~?~. :~:. :1~~~.~3 ..... ..

Work performed on claim(s) •.•• _ ........................... , ............................. . L-4203510, L-4203546" .. .

_ .......................... "' ........ '" '" ", ............ "' ................ -............ ." .... ", ........................... ", .......................... ,. .............. ,. ..

'" ..................... -.................................................................................................. .

...................... -................................................................................... "' .................. ..

--............ _ ...... __ ........................................................................................ ~ .. Work ap plied to claim(s).,~.~?~~~:~ :._L.-.9~.~~~~.,. _~:~~~~.5.~~. ~.-:~~~.~~~ .' •. ~~.~?~??~ 1 • • ~:~~q?60, L-980261, L-980262, L-980263, L-980264, L-980265, L-980266, L-980267 L-980270

................... _ ........... ~4 .................... __ .................... - ......... ~ ........................... , ,

.~.-.~~~~?~: .. _~:?_~?2.~~ , .. ~.:?~.~~~.~! .. ~~.9.~~~.5.~~. ~.-:~~9~.5.41 .. ~:~.~9.~??) .. ~ :~.&Q~?&~. L-:98D.3.5 7 ~. L-980358, L-980359, L-1239305, L-3003152. .. ............ . . -.............................. _.- ...... -...................... -...... -........................................................ ..

-_ ........ -..... --............................... -...... _ ...... --..................................................... . Pe~sons who performed work (supervisor first): ............................... ..

TIGER GOLD EXPLORATION CORPORATION ....................................... --.......... _ .......................................................................................................... ,. .......... ~ ..... . WENO'( K. WElLER AND CREW

................................ _ .............................................................. - ............................ * ....... .

JOHN E. PERRON .... --_ ............................... -..... _ ............................................. ~ ............. ~' .... .

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-10-

C E R T I FIe ATE

. I, Wendy K. Weller, of Virginiatown, Ontario, do h¢reby certify:

1) That I am a Geotech and reside at:

17 Hilltop Crescent, Box 252, Virginiatown, Ontario POK IXO .:

2) That I graduated from the Haileybury School of Mines as a certified Diamond Driller in 1982. a staking license for the past 17 years.

have had

3) That I was employed as a Diamond Driller for Heath and Sherwood for 1 year.

4) That I have been practising as a Geotech f(lIr a period of seventeen (17) years and I am qualified to write this report.

S) That I supervised and participated in this survey.

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