DET AI L MAGNET0i1ETER AND

ELE.CTROMAGnETIC SURvEYS ON THE

ELLIOTT--35

ELLIOrr TOWNSHIP

LARDER LAKE f'lINING DIVISION

DISTRICT OF TIHISJ~HING.I ONTARIO

PROViNCIAl. RECOROING Of"FICE • SUOBURY

RECEIVED

APRIL 4.1 2005

FOR

i1 I SS WENDY K. t/ELLER

GEOTECH

SUMf4ARY. • • • .

INTRODUCTION • •

LOCATION, AND ACCESS.

PROPERTY' HISTORY •

REGIONAL GEOLOGY .

TOPOGRAPHY • • . . •

TABLE OF CONTENTS

200?-E-3S MAGNETOMETER/ELECTROMAGNETIC SURVEYS. .

OBSERVATION AND CONCLUSIONS. •

CONCLUSIONS.

REFERENCES •

TECHNICAL DATA .

ASSESSMENT DATA FORM • • . .

CERTIFICATE. • • • • • • •

MAPS

LOCATION AND ACCESS (FIGURES la) and lb)

TABLE 1 - TABLE OF LITHOLOGIC UNITS FOR THE THACKERAY.

.i)

· 1

· 1

• • 2

· . 2. 3

· 3

· 3, 4

. . . . 4. 5

· 5

· 6, 7

· . 8

· 9

· • 10

1 a)

ELLIOTT, TANNAHILL AND DOKIS TOWNSHIPS. . 2 a)

GEGLOGICAL SETIING . • . . . . . . . . . . • • . . .. 2 b)

GROUND MAGNETOMETER SURVEY MAP NO. E3S/20Q&/~a9 • . IN BACK POCKET

GROUND VLF-EM SURVEY - NAA PROFILED MAP NO. E35/200Sjlf.lfIN BACK POCKET

WORK RECOMMENDATION •.••..•.•.•.••.••....• i a)

SUM14ARY: i)

Th'e report includes a Detail Magnetometer and E1 ectromagnetic 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.

Technical data is provided at the back of this report. Field data is compiled on the accompanying plan maps E-35/2005/mag and E-35/2005/vlf, found in the back of this report.

_i a)-

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

TELEPHONE <7Q5} 567-3001

Michael Hanington. P.E., Mining Vicc-presidcot of Exploration TIger Gold Exploration Corporation 201 S. Greenfield flO Mesa.. Arizona 85206 (480) 324-0910

March 21, 2005

Wendy Weller Gcotech Tiger Gold Exploration Corporation 103 Government Road East . Kirkland Lalc:e, ON P2N 1 A9

Dear Wendy,

RE: Elliott 35 Claims L·3013919 and L-4203546 Elliott Township

SCHEDULE A -----

After reW=wins the results of the magnetometer and dec:tromagnetie surveys 00 the above noted property it is apparent, 'Without question, that in-till surveys running East and West arc warranted and should be dODl) It your fim opportunity.

The nonhlsouth bue line, and other appropriate reference standards are of your choosing but picket liMs should be turned offcvery 50 mdcrs, 90 degrea Ea.:st and 270 degrees West and stations should be cut and measured every 25 meters.

If you have any questions please call. Your attention to this is appreciat~ thank you.

SiDaJf·

t,~-;.~.-;P Tiger Gold Exploration Corporation

DETAIL MAGNETOMETER AND

ELECTROMAGNETIC SURVEYS ON THE

ELLLIOTT-35

ELLIOTT TOWNSHIP

LARDER LAKE MINING DIVISION

DISTRICT OF TIMISKAMING, ONTARIO

INTRODUCTION

There are 4 blocks (35 units) in the property. Claim L-4203545 is ~om~os~d of 5 units and is located in Elliott Township.

Due to the results of the north/south grid on L-4203545, on February 7, 2005, a new west grid was established using PL1600E as the new baseline.

Picket lines were turned off at every 50 meters, 360 degrees north and 180 degrees south and stations were cut and 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 ooundary along the Elliott-Clifford Township line. The line has never open established by legal survey, and it1s position on the ground is a best estimate. Cb-ordinates of 48 degrees 21 minutes north latitude and 79 degrees 50 minutes west longtitude are located approximately central in the claims (NTS 320/5).

The Elliott-35 are in th~ Larder Lake Mining Division, and they are within the jurisdiction of the Kirkland Lake Resident Geolo­gist. Access is fro~ Kirkland Lake towards the east for 13 kilometers to the Harker-Holloway road (Highway 672). Follow 672 north for 24 kilometers 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) & lb)

LAKE A II Tllt·'-=:=!I

(..)

·UJ CD UJ :J o

· N · · I NDEX MAP' SCALE hIOI'7eO (1-. US mil .. )

ELLIOT\T TWP. ,

~ r---" I I Lt~3

I ' :

1-. CLIFFORD

TWP.

AIR MACUIETIC DATA 'r •••.•. C •• I'tl

A,rll1993 w.K.W.. 320/15

SCALE I: 20 000

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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 Claims, 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 jntruded 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 general area can be defined as being hounded on the south by the Larder Lake Fault and on the north by the Destor­Porcupine Fault, both regional, east-west trending structures .10ng which are major gold mining camps such as Timmins, Harker-Holloway, Kirkland Lake, Virginiatown and Val D'or. A major east-west trend­ing syclinorium is present between the two faults. The younger Blake 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 ;s 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 Blake 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 lap,lli 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 relatively more bed rock exposures then has the A&A Group.

•

TABLE 1

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TABLE OF LITHOLOGIC UNITS FOR THE THACKER A Y, ELLIOTT TANNAHILL. AND DOKIS TOWNSHIPS. . t

PHANEROZOIC CENOZOIC

QUATERNARY PLEISTOCENE ANO RECENT'

PRECAMBRIAN

Till; reworked till, esker sand and gravel, varved clay, dune sand, alluvium and peat.

UNCONFORMITY

MIDDLE TO LATE PRECAMBRIAN (PROTEROZOIC) MAFIC INTRUSIVE ROCKS

Dlaba,. and quartz diabase

INTRUSIVE CONTACT

EARLY PRECAMBRIAN (ARCHEAN) FELSIC JNTRUSIVE ROCKS . SYENITIC INTRUSIVE ROCKS .

Equlgranular and porphyritic: lVenodlorlte, monz:onlte, syenite. feldspar porphyry, pegmatlt. and lamprophyr.

INTRUSIVE CONTACt

GRAN ITIC INTRUSiVe ROCKS Quartz diorite, granodiorIte, trondhjemIte, feldspar porphyry, and hybrid

rocb .

INTRUSIVE CONTACT

MAFIC INTRUSIVE ROCKS . Gabbro, quertz gabbro, dIorite, quartz dIorIte, hornblende gabbro. and

enonhotltlc Uabbro .

INTRUSIVE CONTACT

VOLCANIC ROCKS RHYOLITIC AND DACITIC VOLCANIC ROCKS

Calc-Alkaline Suite Meulva breccia, flow-breccla, pyroclastic breccia, tuff, crystal tuff, amygda­

loldel, rhyolitic and dacltlc rock.t feldspar, end quartz porphyry, rhyolitic and dacltlc rocks .

TholeIItic Suite .Spherulltlc tuff and tuff-breccla, and cherty tuff, rhyolitic and dacidc rocks . I

BASALTIC AND ANDESITIC VOLCANIC ROCKS Calc-Alkaline Suite

Massive, pillowed breccia, pyroclastic breccia, tuff and lapilll-tuff, amygda­loldal, porphyritic feldspar basa'rtle and andesltlc rocks and greenschist and amphibolite facie., meta-basaltlc and meta-andesitic rocks

Thol.lIdo Suit. Black to dark g .... n, hlgh.·lron, manlv., pilloWed flow-top .breccla, pillow

breccia,' hyaloclastlc, varJolltlc and amygdaloldel basaltIc end andesItlc rock~ and Interflow sedIments

Grey to green, hlgh-magneslum massive, pillowed, flow-top breccia. pillow­breccia, hyaloclsstlc, porphyritic feldspar, varlolitlc and amygdaloidal basaltic rocks and Interflow sedIments

Geological Setting

[ f miles! o ! ,

x

.

r-1\1 '1t' .-1/1

9 J

+ 8-3~ .............. _

Morrisette

-+ A-4 A

MA-20

Kirkland Lake o

+

-2 b)-

1: The New Buflonta

2: Holt- McDermott Mine

X: Base Metals:!: Gold

- - Fault :!: Diabase Dike

\

\

\

x .

+

I

I • I·

I

I : I

u ' 1.1.1' en

• I

I

• r I _0-r-' ----...... ,*"""",.., I j

-~-,. \ +' -- 6"~ . ...! \ ----Ki'" Gauthier \ I .

/-• Virginiatown :-., .... ~'j).\)

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 locii of emplacement for kimberlites is structurally controlled (Brummer et al, 1992 and 1~92). A cluster of seven kimberlJtes occurs between 10 and 19 kilometers south of the A&A Claims (see Brummer, ~ cit. and McClenaghan, 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 Cafford, 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. Kimbe~lite 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 creek 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 - .E35 I>\l.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 earth's magnetic field and in turn generate 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 McPhar 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) Geon;cs EM-16

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

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

VLF instruments are capable of picking up these structures that ch~nge trye direction of.the.waves by using the tilt angle of the maJor aX1S of the polar1zatlon 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-I6.

The two stations used.were Cu~ler, Maine, 24.0 kHz and Annapolis, I~ryland, 21.4 kHz.- More lnformatlon about the survey and instrument can be found on the Technical Data Form in the back of this report.

OBSERVATION AND CONCLUSIONS

Magnetic Survey 2005:

The magnetic relief varied between 57,013 and 60,111 gammas (three thousand and ninety eight gammas) difference of 3098.

The datumn was substracted at 57,000 gammas.

The field Map No. E35/2005/mag can be found at the back of this report. The magnetic trend is northeast to east direction.

In this survey there are four high magnetic circular anomalies noted. These circular anomalies may possibly be Kimberlite targets that should be tested by geochemical survey,

As shown in the first north/south survey a north/south fault shows in the same direction as the magnetic trend.

There was one small overburdened outcrop noted in the southwest half of the new grid.

Electromagnetic Survey:

The field data is presented on a map at a horizontal scale of 1:2500, Map No. E35/2005/vlf. Seattle, Washington was used in this survey.

Seattle, Washington showed 3 anomalies in the survey.

Q1 - PL050S 100W to PL4N 165W. The topography of the area ranges from flat jackpine bogg to the south slope of a overburden large outcrop. The quadrature is negative.

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Q2 - PLOSOS 1628N to PL4S 128W. The topography of the area is a wet low lying pine bogg.

Q3 - PLlS0S 415W to PL4S 435W.

CONCLUSIONS

The topography of the area is a small overburdened outcrop. The contact is running northeast direction.

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.

Apr; 1 4, 2005

Respectfully submitted,

Miss Wendy K. Weller Geotech

REFERENCES

Barron, Keith M.

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

Brurrmer, J.J., MacFayden, D.A.- Discovery of Kimberlites· in:the Kirkland and Pegg, C.C. Lake Area, Northern Ontario, Canada.

Part I: Early Surveys and the Surficial Geology. Exploration Mining Geology, Volume It Number 4, pp. 339-350, 1992.

- Discovery of Kimber-lites ·in the Kirkland Lake Area, Northern Ontario, Canada. Part II: Kimberlite Discoveries, Sampling, Diamond Content, Ages and Emplacement. Exploration Mining Geology, Volume I, 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, L.S.

McClenaghan, M. B.

Ontario Division of Mines

Ontario Geological Survey

- Map of Conductors and Apparant Conducti­vity of Overburden, Blake River Syncline, Ontario; HTS 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 re 1 inch to 1/2 mile, 1975.

- Geology of Thackeray, Elliott, Tannahill and Ookis Townships, District 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/I, 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.2253 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 July, 1983. ,

- EM-16, 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

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Technical Data: Lin e (mi Ikm):~.!~:.~ •.... ~! .... __ ....... _ ..... _ No. of sam pies /stations! __ .5.11 _______ _

Line traversed~

Line/picket spaci~~~~~~!~~~~~~.~.~~~-_-~_~-~ ELECTROMAGNETIC SURVEY: Ope ra to r:. ___ ~.I..s_~l!.s~Q! -~!-~g!-bgK ____ _ Instrument: GEONICS EM-16

- --------VElttTCAt'-ARO---·---Coil configura tion: _______ HJ1~g9tHBi. __ _

+ A c cur ac Y: __ :_J~ _____________________ _ Coil separati on : __ I~~~_I_r.:: __________ • __

Method: FIXED TRANSMITTER ------ ---------._-;--_._. --_ ... ---Vertical scale: 1 INCH = - 40%

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

Parameters: INPHASE AND QUADRATURE _.- ------- ---------_._----- -.-Horizontal scale: 1:50000 ------ --_ .... ------. ---.-

Fr eq u en cy : ... ~~!:_~.:_~~:_~_~~.: ._ .. _____ . St a t ion: • __ ~E~~~~~ :!.A.s_H_I..N.GI.9~. ____ •• _

Operation a I tech n I q u e: __ ~~!~_~~!_r~~LN_~:. ___ ~~~_~s~Q!~~~ _!~K..E~_.f_~S!~~_~2~I_~_~9~ ___ _ TO THE STATION • .. _--_ ... _-._-_ .... ----._- _._- --.-.-~- ----------- ..... _----........ ---------_ .. _ ... ------------ .... _ ... -----.. ---

.. _._----.. _- --_.-_._ .. --_ ... -.. _--- .... _._--_ ...... --_ .. .-----_._-.---.. -...... _ ... _._-._----- -..... _------ .. MAGNETIC SURVEY: Opera tor, J. E. PERRON ... _--------... --_. ------ -_ .. --. _ .. -Instr ume nt : __ ~~!..~~~_~~:~_~~~I.q~ __ . _____ _ + Ae c u racYt __ = ____ ] __ G_~~ ______ o_ • ______ _

Base s tat io n ._~.l:~.9 ___________ . _______ _ Diurnal met hod: CLOSED LOOPS BL TIE-INS ---_.-. __ .. _--------_ .. Bose station time: EVERY 60 MINUTES. ... _---_._-_ ...... __ ._-_.- Location Ivalue: BLOOO --------------- ------... -Contour interval: 50-100 GAMMAS -_._ .. ------_. --------_. Datumn subtracted: 57,000 GAMMAS -...... -----_ ...• -_ ... -... _ .. Contou red by :_~:.~~ __ ~_~~?_~_~:._~~~_~~~ ___ ._ Horizontal sea Ie ·J.:.!QQ9_q _______________ •• Ope ra t ion a I tee hn i que : ___ ?_E~?9_~_f_~~~!!qy_~~ __ •. ______________ . ______ .... _. __ .. ____ .... _

._-.-........ ---- ......... -...... _ ... -_ ..... __ ...... --..... ----- -_ ..... -------._-_ .. _-_._._---.---_."" ... --_. -_. ---- _ .. __ . --_. __ ._----_. -.. _ ...... _-- -.. _---_.- .. -------_ .... ---_ .......... -_ .. -.. _----- --_._--.. -.. _- .... -INDUCED POLARIZATION SURVEY

Transmitter used: .. -- ---... _-_ ...... _ .. --..... _. R ece j ve r used : ____ . _____ ... _____ "_ .. ___ .. __ _

Method: _ .. _- ... -.... _--_ ............ _-- .. -.. _ .. -.. -_. _ .. -- Fre que n cy ! ________ • __ . ___ .. __ a __ • ____ a ••••• _.

On time: -- _ ... _ .. -.... --......... --.......... -.... _ .... _ .. - Ra n g e :_._ ..•. ___________ . ___ .. _______ ., ___ . ____ ... __

Off time: --_ .... _ .... _ ..... _- -_.- -- .. -.. _-_ ... -.. - De lay tim e : ______________ . _________________ • ___ .

Power source: ---------.----- --- --- -- --_ .. -- Out put :_. _____________________ .. _. ________ . __ ...

EJ e c trod ear ra y : _____________________ ._ E 1 ec t rQ d e spac ing: _______________________ 0.

Rea ding s tak en ! ___________ • ___ ___ _ _ _____ Ot her d a t a : ___ • _____________________________ .

Operational technique: ------_. -------.... -.. _-_ .. _-- ---- --_ .. ----------_ .. _-_ .. ---- -- ----_ .. ------ ---._-- ---_ .. ---- _ .. _- ----._-- .-..... _- _ .. _- ... _--_ .. _------- .. --_. -----........ -. ----_. ------- .. -.- --_ .. _ ...

-... --. ---. ----- -._--............. _ ........ "'.- -- .... --... -.. -. _ .... -....... - .... __ . --.............. __ .. _._-..... _-- --- -,..- -.. _-- ---- -- -___ a. -.. --... _- -- .. --- -_ .. _- --------_ .... _---- .. -_ .. _- ----- .. -.. --------_ .. -_._-... ---- ---------"- _ .. _ .. --._---------_ ..... ----

AS'sessme"nt Data -9-Form .

Type of Work:

Prospecting: ....... _........................ Geologlcal ' •.••.•.••.....•...........•.•.....

. Ph y sica II_ •••• _.~~~~ •• ~~T!_~ ~~.~l~~ .. ~~~.r!!~ N~. _ ........................... _ ••••.. _ ••••...• '" ..

G e a p hy sica I '. ~~.::~~~~~.~~~~ ~ •• <,l_.~~~!.I.~~ ~. ~~~ .~~~~~IQtl~I~~. ?Y~Y~J.s .................. . . .

G e a c hem i c a I : __ ... _ • _ ••••• _ ._ ••••• _ .. • .. 0 ri It i n 9 : ..• _ ............. ,: .... __ .......... .

Assays/Analyses:._ •••••.••..••• _.... 0 thcr work: ••.•..•..•...................

Cos t 0 f '110 r k: $6,972.00 ------- .................... . . .

Recorded Holder: THE PERRON SurveIl Comoanv: • GOLD CORPORATIt1NI ",

No mc.~~~~~. ~9~~. ~:~~9~!:~~9~ .. ~9F?P~JJ.9NJ~ arne: .!.I~~.R .• G.O.L.~. ~~:.~~~~.~ ~~~ .. c.~~:?~~~ :~.'! Addres S: 103 GOVEP.N~!2~li i=.O'!O E.~5 r I Addr e s s: 103 GOVERNMENT ROAD EAST, -............................ _ .............. _.. ........ -- ...... -....... - ..... -......... -.......... . . ~l~.:~~~.:~.O._~~~~!. 9~II ~~~q .~~~. }~J .. ......... _ ... ~ ~~~~::'!g .~~:~~! .. QtITABlO. '" ~ ............... . Survey/ Report Information: Start of 'ilor:~: MARC~ 17,2005 .. - - ........... --_ ........ . End 0 f work : ..• M.~~~.~. ?~ .... 20Q5 •••••....

Oraugh tlng tim e : •. ~:.~~~ ... ~~.~~ •. ?9-~~ ... . Rep 0 r t· tim c : •. ~PR.I ~ .. ~ ~ ~.' .. 20~5 ........ .

Completion of repor' .• ~~~.I.~.~: .. 2.~~~ .. . Author: ~HSS ~!EN~J'( K. ~":LLE:.l . ........ .. .. .. .. ...... .. .. .... ...... .. ... .. .. .. .. .. . .. .. .. .. .. .

Work performed on cloilii(st ........................................................... .. L-4203545 . .

......................... __ ................................................ -........................ -................ ~ ..... ..

.. ................................................................. ....... .... ................ ............... ~ ................ .

............ .. <II .... " ...................................................... _ ........................................................................ * ...................... " .................... ..

--.. -- ....... -..... -_ .. _--- .............................. -................................................... ,. .. ~ .......... " Work ap plied to C!oim(sL~.:?~'::~~:.'. .L .. -.~~9~.~~ ~. ~:~~q~~L, .. ~:J5lq~~.~.:I. h:-9.80.333.,. ...... . L-980334, L-980337, L-980338, L-980339, L-980340, L-980341, L-980342, L-980345,

..................................... ~ ............................. -................................. " .................. " ........... . L-980346, L-980347, L-980348, L-980349, L-980350, L-980359 .

......... ,. .. ~., ..... '" ... _ •• we ••• ""... .. ................ 4O .... 4O .. " ...... _ ,. ,. ..... _ ........... ,. ...... " .... " ........ :. ........... ,. .. '" .......... ~ ••• , ....... .

........ ..... ... ... -...................... -_ ..................................................................... " ......... " ................ '" .. ~ ... " " ........ ~

.----:-.. -... -....... -............................................................. -................................... " ~ ...... ,

Persons who performed work (supervisor fir51): ................................ . TIGER GOLD EXPLORATION CORPORATION ............................... _- ................................................................................... " .................... . WENO" K. WELLEI~ ,

............... _ ........... _._ ... _ ............................... "' ......... - ................................... .o ....... oO~ ....... ~ .. " •••

JOHN E. PERRON <o .. ~ ............................................ _ .............................................................. "'~~,. ...... <P ••

ALAIN PARISCOAT AND CREW .... . ...................... _ ......................................................................... -.. " .............. "' .. ~.- .............. .

.................................... ,. .............. ,.. .. _ .................. '"'_ ........ _ .................. <O ................. ~ ............. ..

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C E R T I FIe ATE

I, Wendy K. Weller, of Virginiatown, Ontario, do hereby 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. I have had a staking license for the past 17 years.

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 for a period of seventeen (17) years and I am qualified to write this report.

5) That I supervised and participated in this survey_

W&ldY :WEier Geotech

•

I •• f' , •• 4. . -,

, . , . , . •

I •

. ..

•

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i

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Claimline-- Creek ('1.f

/

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INSTRUMENTATION

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LARDER LA KE MINING DIVISi;ON

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