GEOLOGICAL SURVEY

ON THE

KARAT-14

CLIFFORD TOWNSIDP

LARDER LAKE MINING DIVISION

DISTRICT OF COCHRANE, ONTARIO

FOR

TIGER GOLD EXPLORA TION CORPORATION

JUNE 23, 2006 MISS WENDY K. WELLER

GEOTECH

2.32532

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TABLE OF CONTENTS

TABLE OF CONTENTS

SUMMARY

INTRODUCTION

LOCATION AND ACCESS

PROPERTY HISTORY

REGIONAL GEOLOGY

ECONOMIC GEOLOGY

TOPOGRAPHY

OBSERVATION OF FIELD RESULTS

CONCLUSIONS

REFERENCES

ASSESSMENT DATA FORM

CERTIFICATE

MAPS

LOCA TlON AND ACCESS (FIGURES la)

TABLE 1 - TABLE OF LITHOLOGIC UNITS FOR THE CLIFFORD

AND BEN-NEVIS TOWNSHIPS

GEOLOGICAL SURVEY MAP NO. K14/2006/geo

2

2

3

4

5

5

5,6

6

7

7,8

8 no ';I

10

11

5a)

5b)

In back pocket

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SUMMARY:

The report includes a Geological 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 conclusions based on the field surveys.

Technical data is provided at the hack of this report. Field data is \,;umpiied on the

8 accompanying plan maps K14/2006/geo, found in the back of this report.

INTRODUCTION

GEOLOGICAL SURVEY ON THE

KARAT-14 CLIFFORD TOWNSHIP

LARDER LAKE MINING DIVlSIN DISTRICT OF COCHRANE, ONTARIO

4

There is 1 block (fourteen units) in the group. Claim 4209407 is located in Clifford

Township, Larder Lake Mining Division.

On June 3, 2006 a Geological Survey of the K-14 group was started (4209407). The

K -14 Group has an extensive new east/west grid from the winter and spring of 2006. For the

plJTp(l~ of this report the 200G "'linter grid, claim posts and claim lines were used as tie-in

points for creeks, ponds, outcrops, vegetation boundaries and glacial eskers for this survey.

There are two small outcrop showings in the block of 14 near and the north/west 400meter

claim line post (west of the number 2 comer post) and the west boundary claim line (between

the #3 and #4 comer posts) along the Esker Provincial Park boundary and the claim block.

Geological Survey was contracted out to Miss Wendy K. Weller.

All drafting and contouring and report writing was done by Miss Wendy K. Weller.

5

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LOCATION AND ACCESS

The Karat Fourteen Group is found in the north central half of Clifford Township,

east/west of Highway 672.

The Karat Fourteen Group is found in the Larder Lake Mining Division, and they are

within the jurisdiction of the Kirkland Lake Resident Geologist. Access is from Kirkland

Lake towards the east for 13 kilometers to the Harker-Holloway road (Highway 672). Follow

672 north for 34.4 kilometers.

PROPERTY HISTORY

At present time, the Karat 14 Group is a new block of unpatented mining claims that is

presently being worked on by Tiger Gold Exploration Limited.

May 26,2006 Magenetometer and Electromagnetic Survey of K-14 (North section)

REGIONAL GEOLOGY

The Clifford Township, 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 general area can be defined as being bounded on the south by the Larder Lake

Fault and on the north by the Destor-Porcupine Fault, both regional, east-west trending

5355000N

UTM Zone 17 lSOOOm grid

LOCATION AND ACCESS MAP

585000E

FIGURE la)

(

590000E

PAGE Sa)

2

Clifford and Ben Nevis Townships

Table 1 T;\I3LE OF L1TIIOLOCIC L"~ITS FOR TlIE CLIFFOI\I)-BE~ ~E\'IS .\RE.\,

CE~OZOlC

Ql·,\TER);.\RY

Recent

Pear, ;Ilhl\'illlll,

Pleislocene

eLI,,'I, ,;Illd, rill ,Illtl d,l\'.

C'!lC d ll/(}Tmily

PREC:\~fBRL\:'-l'

~llDDI.E TO I..\TE PREC\'IBRI.\:'" (PROTEROZOIC I

~!.\FIC I~TR l','iI\'E ROCKS

E.\RLY PREC.\~IBRI.\:'" (;\ROfE;\~)

FELSIC I:"'TRL"Sln: i,OCKS Gr:lnnd;nnlf', qli,lrtl. d',/,r:r,', dll'rttf', '~1'1l1!(', !1·ld,p.lr pnrphyr~' .tnd

qll.trt/.(,·ld"p.lr pllrpll\ rv

{rleru\!: r' c"'1!lld

MAFIC TO I~TER~!E[)IATE INTRL'SIVE ROCKS

/rrlrllril'e conlflcl

\'OI.C,\:\'IC ROCKS

Felsi .. Volcanic Ro,'ks

Hhyot!,I"i!.· ,lilt! rll\ol,t.·, .\1.1."1\1', /I"w·",,', ""', l<lff.IH,·('ci.I, Iliff and Iapilli·lllff.

Intermediale Volcanic Rocks And,·,il.: alld dacitl': .\(.I\,i\('. pdlowl'.!, /low."rl·,cia. Iliff. ,Irt:dlite,

~rafic Volcanic Rocks

3.1>alr: '\f.ls,i\~, pillowed, f1o\\.I,r,·r('ia, tllfT·hr,·ccia,

5 b)

6

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 synclinorium 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. 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 tholeites. Such

iron-rich composition is reflected in bands of high ma,gnetic 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 economical1y significant

features (Kimberlite pipes or alteration zones) can easily be masked within the Kinojevis

Group.

Blake River Volcamc Rocks are composed of calc-alkaline minerals. Massive and

pillow flows occur in sequence with pillow and pyroclastic breccia and lapilli 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 Elliott Groups.

ECONOMIC GEOLOGY

For the Blake River Group, a megacauldron has been defined which occupied what is

now the central part of the Blake River Synclinorium. Within such a large feature, the sense

of vent vs.proximal vs. distal positioning becomes rather vague. The three will have

completely inter-fingered with each other through time. In general, base metal deposits form

in proximal to vent areas. Stratiform gold deposits are likely to be found in distal regions.

Clifford Township is known for gold occurrences, they are located along margins of

alkaline rocks (Jensen, 1978). Alteration is present in shear zones, and fractures which

contain quartz, epidote, calcite, chalcopyrite, pyrite and specular hematite.

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TOPOGRAPHY

The claim unit covers fourteen mining claims. Highway 672 crosses the south/west

section of the group. The topography of the area ranges from flat black spruce swamp to the

south/west. In the north/east section one very deep long narrow (northeast/southwest) glacial

esker is located east of highway 672. A large drainage creek crosses back and forth on PL 000

from the Baseline to 075E, this large creek crosses the entire south west section of the grid

(between the 400 meter and 500 meter mark of the picketlines). All drainage creeks and

beaver ponds along the creek system are encompassed by glacial eskers and large alder

swamps. The creeks and beaver ponds are part of the drainage system for the Magusi Basin

to the south/east. There are many small timber access roads crossing the block on the

nurth/east end of the b'fOUP.

The relief over this block of claims does not exceed 30 to 40 meters. Over three quarters of

this group is part of the Munroe Esker System, (sand, bJfavel and till).

2006 K14 (FOURTEEN MINING CLAIMS)

GEOLOGICAL SURVEY

OBSERVATION OF FIELD RESULTS

A-Pillow Lava Deposits (2b) within the magnesium-rich sequences are of basalt

composition.

Description: Dip angle 182 debJfees - 180 debJfeeS

Fresh face- dark to light green

Weathering colour - dark green

8

Salvages - ranges from I inch to 2 inches in thickness, quartz filled with

epidote stringers, pillows tightly packed together, locally phenocrysts of plagioclose

up to 1-2 cm. in dimension are concentrated in the pillows outer limits.

~Flow Top Breccia /Pillow Breccia (2c) within the magnesium-rich sequences are ofbasaIt

composition.

Description: Colour - dark b'Teen to black, Weathering colour - dark brown, fine grained,

intense fracturing - 55 degrees to 58 degrees

Irregular patches of epidote with spider quartz stringers, non mab1Jletic

CONCLIJSIONS:

At present time the new north/south grid is being completed for the purpose of running the

mab1Jletometer and electromagnetic surveys over targets from the winter program.. When all

information is completed a stripping program is being considered for the small outcrop

showing in Hl~ K-iO Group.

JUNE 23, 2006

Respectfully submitted,

Miss Wendy K. Weller

Geo-Tech/AGENT

PERRON GROUPS

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REFERENCES

Weller, W.K. Detail magnetometer and electromagnetic Surveys

Clifford Township, District of Cochrane, Ontario.

March 27, 2006

Ontario Division of Mines Timmins - Kirkland Lake Geological Compilation Series, Map

2205, 1972.

Ontario Geological Survey Airborne Electroma!:,'11etic and Total Intensity Magnetic

Survey, Matheson-Black River Area, Elliott Township,

by Questor Surveys Limited, Map 80609, Scale

1:20,000. March to July, 1983.

ASSESSMENT DATA FORM

Type of Work:

Prospecting:

Physical: GEOLOGICAL SURVEY

Geochemical:

Assay/Analyses:

Cost of Work: $2,289.00

Recorded holder:

Name:

Geological: K-14 GROUP CLIFFORD TWP.

Drilling:

Other Work:

Dollars applied: $2,289.00

Survey Company:

Name: TIGER GOLD EXPLORA TION

CORPORATION

TIGER GOLD EXPLORATION CORPORATION

Addre<;<;' 103 Government Read East Kirkland Lake, Ont. P2N 1 A9

Survey/Report Information:

Address. 103 Government Road bast Kirkland Lake, Ont. P2N lA9

Start of work: June 3/06 End of work: June 9/06

Drafting time: June 21,2006 Report time: June 21, JUNE 23,2006

Completion of report: JUNE 23,2006

Author: MISS WENDY K.WELLER

Work performed on claims: L-4209407

Work applied to claim(s):

L-30038J6, L-3006739,

Persons who performed work (supervisor first):

TIGER GOLD EXPLORATION CORPORATION

WENDY K. WELLER

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CERTIFICATE

I, Wendy K. Weller, of Virginia town, Ontario, do hereby certify:

1) That I am a Geotech and reside at:

17 Hilltop Crescent Box 252 V irginiatown, Ontario POK lXO

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2) That I graduated [wm lh~ Hai1cybury School of Mines as a certified

Diamond Driller in 1982. I had a staking license for the past 19 years.

3) That T was employed as a Diamond Driller for Heath and Sherwood for

1 year.

4) lbat I have been practicing as a Geotech for a period of nineteen (19)

years and I am qualified to write this report

5) That I supervised and participated in this survey.

Date d f wendy{WeIler

Geotech/ Agent

3006664

--~' ." ., :.

11 - - "A .t·"-·"

-1'1 "' -- --,' , 14

" ,: . , ~-~')~_~ __ -- ~'L _ . . -.4,_

;' \. ).,,, _ HICK LAYER OF /~ ' - -- """ - -;'-' .... '") "-" __ ,, ~--____;;A--'\. \ f ;. - -- - .. - - A --

, 1 --- -- -)--.' -~). r· ~ OUTWASH SAND,

'GRAV~~, DUNE SAND

JACK PINE REPLANT AREA

4209407

••

THICK SPRUCE,PlNE"POPLAR

BI RCH (SECOND GROWTH) -

BOGG

\

\

\

~ _ __ ~ ___ ~ __ -+~~ _ _ -.~ _ _ _ ~~ ____ ~ ____ ~r-_~~~L-_~~~~-P~ ______ ----~--~~~

4400N

J 1 ~ ______ ~ _ ___________________ ~ __ ~ ______________ ~ __ ~~~-+~~ __ +-~~~~~ __ ~~~ __ ~~~~~~150N

_-7 · .. . . ~

JACK BOGG

. SYMBOLS ~

-~C 1 aim Lin e - - C 1 aim Po s t !if

line Post Q

Esker Park Boundary

Traverse Line » < ---

Vegetation Boundary, ----? Pinei Pine ReplantH Spruce--l}­

Birch f\1l poplad), Alder~

Beaver pondsc:.~ Creek -' : ~_" .. i

Highway 672/ Access _:

Ou tc rop ---; Showi ngs ,--::/} ,. 1 L ~ ,

LEGEND

Cenezoic

Pleistocene

Gravel, Sand & Dune Sand

Early Precambrian

~le t a VO 1 can i c s

2b) pillow lava magnesium rich sequences

2c) flow top breccia/pillow breccia

K-14 GROUP

GEOLOGICAL SURVEY

CLIFFORD TOWNSHIP

Report by W. K. Weller

Date: June 23, 2006

Map No. K14/2006/geo

Scale: 1:5000 meters ,(."'C'." ( ) le e r.... 2 t..·t~ , ....

\,~:--: -==--=t:-\ -==-~lt:===t

,. .. ~.' .....

2.32582