42A86NE9494 63.4536 DELORO 010

W* H er P

PUISSANCE CORPORATION

SUMMARY OF DIAMOND DRILLING PROGRAM, AND PLUGGER SAMPLING

DELORO TOWNSHIP, TIMMINS, ONTARIO

TOM GLEDHILL P.Bag. June 24, 1985

42A96NE8484 63.4536 DELORO 01OC

INDEX

I'ago No. Summary..................................... j

!nt roduft i on.... . ... . . . . . .. . . . . . .. . . . . . . . . . , 1

Gcnr ra l Geo l ogy ............,................ 2

Economic Mineralization..................... 2

1984 Pluggor Sampling....................... 2

1984 Diamond Drill Program.................. 3

Conclusion and Recommendations.............. 3

Maps - Diamond Drilling 19841*^50 foot sections ot D.D.II. , P-l to P-12 1"~SO foot plan of O.D.H.'s and detail geology

West ^ - East ^

Maps - Plugger Dust Testing - 1984Area l l" K) leiUArea 2 1" K) It-otArea 3 l" - 10 icct

PUISSANCE CORPORATION

SUMMARY UK DIAMOND DRILLING PROGRAM , AND PI.UGGKR SAMPLING

DELORO TOWNSHIP, TIMMINS, ONTARIO

SUMMARY

In an effort to evaluate a carbonate zone that, extends 4000 feet across the Deloro property of Puissance the zone was stripped of overburden. Two thousand feet of strike length from the western end was washed down to bedrock and over this area p lugger holes were- drilled at 5 foot centres on lines 10 feet apart. The dust from tills hole was then sent to an assay laboratory for fire assay. Following this program 11 diamond drill holes were drilled in the carbonate zone. One hole, P-12, was drilled into a zone 1600 feet south that: was described as porphyritic.

The plugger samples gave erratic high gold values and at the same time an unusual quanity of course native gold' was observed in quartz veins and fractures within the carbonate. Diamond drilling produced gold assays within this quartz fractured carbonate zone In holes P-l to P-6, and in hole P-8. At present there is no explanation for the absence of gold in P-7. Holes P-9, P-10 and P-11 do not/have gold assays and further work will be required here to confirm that the drill holes intersected the gold bearing quartz-carbonate zone. The values in the drilling are not high usually 0.02 ounces of gold per Con or less, but low values such as this are common when drilling of quartz-carbonate gold zones similar to this on of Puissance property. This zone is characteristic of the carbonate ore at Kerr Addison Virginiatown mine.

Three of the drill holes PT 1, P-2, P-4 and P-5 intersected a sulphide phase iron formation. Mere a gold intersection ran 0.317 oz/ton over 7.5 feet. This structure is small, and will require some detail drilling to develope a clearer picture* '

Considerable work was carried out in evaluating the assay techniques for this coarse gold. This will be the subject of a further report in 1985.

The wide distribution of coarse gold through the main carbonate (quartz-carbonate) zone, both in drilling and observation of out crop, leads to the conclusion that an extensive program of bulk sampling on surface should be undertaken in 1985.

-2-

PU1SSANCE CORPORATION l SUMMAKY OF DIAMOND DRILLING PROGRAM, AND PLUGGER SAMPLING

DELORO TOWNSHIP, TIMMINS, ONTARIO

INTRODUCTION

In order to map in detail and sample the carbonate zone that traverses the center of the Puissance Deloro property, ah exploration program was undertaken during the summer and lall of 1984. Previously ; the group had been surveyed with a magnetometer and electromagnetic equipment (V.I..P.). This was followed by geologic mapping. This report describes two programs from 1984, the plugger sampling o l the carbonate zone and subsequent diamond drilling. " "

GENERAL GEOLOGY

The major feature of the area, the Procupine - Destor Fault which lies 4000 feet north of the property and strikes northeast.

The rocks are interbedded volcanics tuffs and fragmental rocks. Minor amounts of sulphide phase iron formation were mapped. The formations are intruded by N-S diabase dykes averaging' about 30 feet in width. The regional strike is north 70 degrees. East with local variations. Seven carbonate horizons were mapped strike conformably across the claim group .and the formations are generally north dipping.

ECONOMIC MINERALIZATION

There are many occurrances of coarse gold across the main' carbonate zone. The carbonate unit is fractured or brecciated and the quartz veins that fill these fractures carry coarse particals of native gold.

1984 PLUGGER SAMPLING P*S* f*"/^W *'#t*S.###0* rV/^ftc 5)^,*V

The entire main carbonate zone was stripped and cleared. The western portion of the zone was washed down to bedrock. In this latter area plugger holes were drilled at five foot centres on lines 10 feet apart. The depths of these holes were 4 feet or the water table.

These zones were mapped in detail and are shown on the drill plane ( l"- 50 feet). The plugger sampling is shown on the plans A, fiand C (scale l" ^ 10 feet).

The gold assays of the plugger dust tend to be erratic. Evidence indicates that the sample size is too small and this results in erratic gold values. Similar coarse gold occurs at the Virginatown of Kerr Addison. Successful sampling of such gold deposits occurs when the sample is several tons.

l98A DIAMOND DRILL PROGRAM

K l ewen diamond drill holes,- P-1 to P-1 1 inclusive, were drilled in the main carbonate zones. Hole P-J2 was drilled to test a porphyritic zone. The holes P-1 to P-11 total 437'J leet while P-rl2 was797 feet.

The results of the holes P-1 to P-8 al l intersect the main carbonate zone. P-7 is the only hole to intersect the main carbonate zone and have no gold values. These are all located in the west end of the zone.

The holes P-9, P-10 and P-1 l may have intersected the main carbonate zone. They are located ODD (eel east of the other holes. There were no gold values in the ex(ensive assays. Further work is required to determine if these holes did intersect the main carbonate zone and i i the proper sections of the holes assayed. The surface outcrops of the main carbonate zone do contain coarse gold similar the western end of the zone.

The holes P-1, P-2, P-3, P-4 and P-5 intersected a sulphide phase of iron formation which usually give repeatable assay values. This is a relatively small structure and it may be possible to develop some economic tonnage with further drilling.

CONCLUSIONS AND RECOMMENDATIONS

Stripping the zone is useful in identifying the gold bearing unit. Plugger sampling gives values too erratic to employ in determining ore grade. Some of the coarse gold may not- have been lifted out of the holes in the sampling rout i ne.

Diamond drilling, like the stripping is useful to determine the size and attitude of the gold bearing structure but again the sample is relatively small.

Bulk sampling has been the only successful approach to testing and grading such an occurrance. A useful program would start with 20-50 ton character samples, perhaps 10 or more. This should then be followed with larger continuous run bulks of 100 to 1000 tons each.

June 24, 1985^

Respectfully submitted.

Tom Gledhill, B.A. P.Eng.

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Earth Resource AssociatesP.O. BOX 2150. TIMMINS. ONTARIO. P4N 7X8 CANADA

DIAMOND DRILL LOG

DRILLING COMPANY TRIANGLE DRILLING FOREMAN

CORE SIZE BQ . CORE STORED AT: Coreshack

~ PAGE 1^PROPERTY PU1SSA1KE

HOLE NUMBER P~ 1 '8424+70E/2450NGRID REFERENCE

TOWNSHIP1.Deloro CLAW.li.E.22iftii 0 - j -n 0

AZIMUTH ' ou DIP ANGLE

DIP TESTS 1 00 V-47 0 , 200V-480 , SOD 1 /-?'. 0

LOGGED BY Ken Lapierre DAj^Hoveiiib3r 2 , l iiiis

FOOTAGEO'-lj'b1"

13'b 11 --18'6

1

28 '6M

j

DESCRIPTION OF CORE

drill casing

IttTEftKEOIATE VQLCAtttC^-Carbonated (calcite) —— : ——————————————————— 13'6"-16'U U

-fine grained-undeterminable contacts-grey green colour ;-1X irregular trending caJcite stringers-Li ace fine grained pyrite

lC'0"-l6'6"-quartz .vein-50" to core axis 16'0"-18'6"-2tfliit' yrdiiiucJ pyrite-trace tourmaline

Si,\ji;ii guAKu vtiH SYS i tt j (so*) le'e'^zro"-gradational contacts 21'0"-23 I 6 U-1-21 calcite alteration aS'e^G'O"-5-8X rusty weather:.; banded material with magnetic quaUv.iGS 2o'u"-2u l d*t-trace chai copy r Re-IG-15% fine to r:.cciiu..i grained disseminated at.ii coalesced cii.'iredral tosubhedral pyrit\'.-3^.al ccriccntratlca up to 4i;*

-Ci mafjnrjLite prt;\i:,-J to lcv.'or conw-ici.

t

SAMPLE NUMBER

u3uo1

D3002

B3003B3004B3005bJOOb

PasAS?

O.UU2

trace

0.0360.0300.50'JO.Z^d

ft&hcc

U.Ucu

0.011

0.0560.0130.52i*U.i./

EARTH RESOURCE ASSOCIATES. DIAMOND DRILL LOG. PROPERTY P UISSANCE HOLE NUMBER p' 1

FOOTAGE

28'6"--~ 34'H 14

34' 11"—157*7"

v *

DESCRIPTION OF CORE

BANDED IKON i-OKMAllo.'i — Siliceous — Magnetite — Sulphide v 2Q^"-31'0"-unaetenninaDle contacts .31 0 ~33 6-magnetite bands(255t), 45" to core axis 33'6 -3u 0trace to 21 calcite alteration-IbX medium grained pyrite/pyrYhotite associated with calcite veinlets-3-5* disseminated, coalesced and stringers of pyrite associated within mag netite bands-Z-3% medium grained disseminated pyrite associated witn siliceous bands-minor concentration of volcanic material proximal to lower contact

* ,

INTERMEDIATE VOLCANIC — Carbonated (calcite) 36 1 Q"-38'b"-contacts: top- 850 to core axis 38 I 6"-41 I 0 B

bottom-200 to core axis-FAULT REUTEO 41'0"-45 I 0 I-pale green colour - -- , -' SIo^M'O"-fine grained . w u -^ u

-possible pillow selvages? 55'0u-o0 l 0 u-1-3X quartz/carbonate filled amygauies 60'0"-65'0"-trace calcite velnlets-450 to core axis w! 0"'70 !9!!-2t fine to medium grained disseminated pyrite 70'0'-75 I 0-moderate to highly carbonated-calcita J 75 I 0"-80'0"" ' - QO'O'^QS'O1*-

' - 85 1 O lt-90 l O"-90^0^^^"-

—————————————————————————— . ———————————————————————— —— 95'0"-10^0UlOO'O^-IOS'OlOb'O'MIO'O"

—————————————————————————————————————————————————————— MO'O'Mtfr^flIIS'O'-^O'O

—————————————————————————————————————————— - — ——— ————— : ————————————————— |?ninii.425'Q1 &U \J lt**f V——————————————————————————————————————————————————— t25l fr'M3eJ-S130*0 -135 0 - . . . 4 iTiinu -idn'nIO3 U, t*tu u———————————————————————————————————————————————— - —— •M01tiPl-14S10

————————————————————————————————————————— 44^1^ J.5QJL4

SAMPLE \UMBER

-fi3W7~-D3GQ8

r*^rt .\ 1^B3009

U301UB3011B3012B301303014

^63015-sa^te-DOU l/-flsete—83019-B3020—DJUtllB3Q??-—UwVCiC*

B3023 —U^/Wbw

1 B3024-83^25—i onn^cUJUtO

UJUi/1 mn?iU Jvcu*-B3029-^03030—' -ftlUVH—D.3Ui7 r^3032*- '4l.'Ui3-'l

Psi.-.A'fWSMck-&A&0.024.UL-U

tracetracetrace-trace-0.020tracetracetracetrace-*tracetracetracetrace0.0000.030Vi GUV*

tracetraceCI ul*s.

-&MQ— traceA, AltV t \J i i

•^ *^a t"*pLi ace4. f* 1— tt-trtro

-&AH0.0310.064

O.CQ20.001

EARTH RESOURCE ASSOCIATES: DIAMOND D RILL LOG. PROPERTY: Pt' ISSAf!CE HOLE NUMBER:

FOOTAGE

157*7"--171*6"

171*6"—194'5"

"**

DESCRIPTION OF CORE15U'0"-tbb I 0"———————————————————————————————————————————————————— 1fa5'0"-1GO'0 M160'0"-165 I 0"

INTERMEDIATE VOLCANIC — carbonatization (ankerite) 1bS'u"-170'0!!-contacts: top-20"to core axis-FAULT RELAitu 170^^-175 'O"

bo tt om-g r a d a 1 1 on a 1-green colour-fine to medium grained ankerite grains-trace to 13t quartz/carbonate filled an\ygdules-trace to IS fine grained subhedral disseminated pyrite,

ftANKEkllE/QuAKlZ/F-uCHSHl: ALTERATION ZONE 175'0"-177 6-undeterminable contacts-fine to medium grained ankerite grains-5-10X irregular trending quartz/carbonate stringers-trace-10i fuchsite alteration associated with stringers-1-21 fine to medium grained disseminated euhedral pyrite

-171 l 6u-172 l ir-quartz7ankerite7chlorite7fuchslte vein-100 to core axis-trace fine to medium grained pyrite associated within vein

.-177 l 8"-177'10u-quartz veinlet-450 to core axis 177'6"-180'0"

-non-mineralized

-178'5u -178 l 9"-quartz veln-300 to core axis-non-mineralized

v ISD'O-'iea'D"-182'6"-185'0U-3J fine to meriiur.i grained disseminated subhedral to euhedral 182'6"-1B5'0"pyrite

-185'7"-185 l ir-quartz veinlet-250 to core axis 185'0"-l{J7'b"51 calcite/fuchsite alteration associated with both contacts-trace pyrite

s

'SAMPLE NUMBERb3i)34B3035L)503oB3037D3038

B3039

9

B3040

B3041B3042

B3043

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0.01

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EARTH RESOURCE ASSOCIATES: DIAMOND DRILL LOG. PROPERTY:,, PUISSANCE HOLE NUMBER:

FOOTAGE

194 ' 5"—207*9"

207 '9 U~228 '8"

DESCRIPTION OF CORE ' ' . .

-186' 10M-187' r-quartz vein-300 to core 'axis-non-mineralized Wo"-lSO'0M

laO'Cr-ia^b"

-193'6 ll -194 l 2 ll -waU rock characterized by 70* siderite alteration VJH'o'-l^b'O"

-194 l 2 M-194'5 l'-quartz veln-30" to core axis-non-mineral izad

INTERMEDIATE VOLCANIC — Carbonatized — Chlorite — Ankerite 195'0 I1-197'6 11-undeterminable contacts-fine grained ankerite grains-grey green colour-1-3* irregular trending calcite stringers-no preferred orientation of chlorite grains '-trace-1% fine grained subhedral disseminated pyrite

.-198 l O"-198'4u-ankerite veln-400 to core axis w^-zotro-

iJOO'O^ZOJi'b 11

-202 1 ir-203'4H-quartz veinlet-25"to core axis ^o^'b^-^Ob'u"-trace fuchsite alteration-non-mineralized

-206'3H-206 l 6 M -quartz veinlet-300 to core axis i!Ub l U"-ilU7 l 6u-non-mineralized

ANKERITE/FUCHSITE/QUAftTZ ALTERATION ZONE , 207 I 6"-210 1 0 U-und^enip.Jnahle contacts-grey green to emerald green colour-30* quartz/ankerite/fuchsite stringers with apparent orientation-70-900 to core axis

SAMPLE NUMBER

B3044B3U45B304b

B3047

•*

B3U4BB3U49b3UbU

[53051

D3052

ftn&S^YS

traceU.U1Utrace

0.010

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trace

trace

EARTH RESOURCE ASSOCIATES: DIAMOND DRILL LOG. PROPERTY: P UISSANCE H OLE NUMBER: P-1/04

FOOTAGE

*

DESCRIPTION OF CORE

-zu/'iv-zub'^r-quartz/anKeme vein-30w,to core axis-non-mi nora li zed

-20U 1 7"-208 l 9u-quartz7ankerite7fuchsite veln-700 to core axis-trace pyrite

-209 l 5"-209 l 7M-quartz7fuchsite vein-500 to core axis-non-mineral i zed

-SlO'IV'-^ll'r-quartz/fucnslte vein-sir* to .core axis 210'0"-212 I 6 1'-trace pyrite associated with twth contacts

211 l 5"-2l) l 9 t' -quartz vein-450 to core AXIS ——————————————————————————-non-mineralized

-^ii: l i"-k:ii:'bt'-quartz7ankerite7fuchslte vein-50" to core axis-non-mi nora 1 i zea

; ' *

-ifi3'ii"-i;i3'3 i:-quartz7fuchslte velnlet-750 to core axis 212'6II-215 I 0M-non-mi nera li zea

-2i3 1 ir-2l4'3H-quartz7ankerIte7fuchsIte vein-undeterralnable contacts-trace fine grained pyrite associated with both contacts

215'0M-217 I 6"-2l7'6"-217 l 8"-quartz7ankerite vein-undeterminable contacts - .

-trace fine grained pyrite associated with both contacts siy'e^ao'o"-221 l 2"-226 I 4"-alteration zone characterized by ankerite caibonatizatlon 220 I 0"-222'6M

-contact?.: top-fuchslte/chlorlte stringers-FAULI KELATEO 222'6"-225 l O"bottom- * " " " " 225 I 0'-227'I51'

-preferred orientation of chlorite blebs-BO-85" to core axis

^gg?^-^?^-nicTiTrte7cntOTrt6 Stringers-85* to core axls-FAULT RELATED ————————————

V

SAMPLE NUMBER

B3053

B3054

B3055

D3056B305703058R3059

PaS

trace

-

0.010

trace

tracetracetraceO.U1U

AYS

EARTH RESOURCE ASSOCIATES: DIAMOND DRILL LOG. PROPERTY: PUISSANCE

PAGE ™

HOLE NUMBER: P-1/84

FOOTAGE

228*8"—327 "0"

DESCRIPTION OF CORE-226'7"-228'8"-wallrock characterized by abundant fuchsite a Iteration (60^) 227'6M-230'0"-25* ankerite alteration

-2ft pyrite stringers and disseminated pyrite

JNIERKLDIATE VOLCANIC — Carbonatized (ankerite)-undeterminable contacts-green to dark green colour-fine grain ankerite grains-i-zi irregular trending calcite stringers ,-trace disseminated pyrite

- .-22B l B--2i*O l Q'I-Nall rock characterized by ankerite patches and chlorite 230 IO tt-235'0"blebs - t235 I0"-240'0"

' . y———————————————————————————————————————————————————————— — — — — —— - — ; — n — —— — a ———

245 I 0"-2CO'0"li 14

250 I 0"-255'0U——————————————————————————————————— : —— — ———— — : —— 255'0"-260 I 0"

260'0"-265 I 0" -111 """H ~ ~- "H

265'0"-270 I 0"........ ..... .. .. ... M M

270'0"-275'U"II H

275 0 -2SO'0280 I 0M-285'0M285'0--290'011

295 I U"-3UU I 0M*

SAMPLE NUMBERB3060

63061K1U612B.30G2K 106 13B3063 —K1U614C3064K1D615B3065K10616B3066 —K10617B3tm? —K1061BB3068K10C19B30G9K 10620D^U/U

B3671B3072B3073 ——B3U/4

. ,-,,,..1

0.010

0.020

0.320

0.020

O.S50

'trace

0.010

0.080

0.010

0.010

Irdct.'0.0100.010trace0.010

^'^1 if

trace

trace

trace

trace

trace

trace

trace

trece

trace

EARTH RESOURCE ASSOCIATES: DIAMOND DRILL LOG. PROPERTY:.. PUISSANCE HOLE NUMBER: P-l/^FOOTAGE

*

DESCRIPTION OF CORE

-304'3M -304'G"-calcite7an!;eriteXfuchsite vein-450 to core axis 300'0"-305'0 11-trace fine grained disseminated pyrite

SOO'C'^SID'O"310'G"-315'0"

315 l O u-317'0"-ankeriteXciilorite stringers-450 to core axis-possibly FAULT .115*0" -320 I 0"RELATED

320'0 M -325 I 0 11325 I 0"-327'0U

.

END OF HOLE AT 327 FEET

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x

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S S 4"**y *^r

^fyfyf7\(i^)^t--^/?' t/ \ / v

SAMPLE NUMBER03075

U307603077

B307G

B3079esoao

•-

n ASSAYSPamour0.010

tracetrace

trace

tracetrace

P iP - R-

Earth ^esourcewAssociatesP.O. BOX 2150* TIMMINS. ONTARIO, P4N 7X8 CANADA

DIAMOND DRILL LOG

DRILLING COMPANY TRIANGLE DRILLING FOREMAN CORE SIZE BQ CORE STORED AT: Coreshack

,-^PAGE 1/

:RTY POUNCEHOLE NUMBER P-2/84

f GRID REFERENCE 24+705/2^211TOWNSHIP Deloro CLAIM M.E.22

AZIMUTH 1600 DIP ANGLE -620

DIP TESTS: 57* /600 LOGGED BY Ken Lapierre DATE November 6, 1984

FOOTAGE

fi'1 -15*0"

15*0"--15'7"

i*; 1 ?"—32*6"

DESCRIPTION OF CORE

-drill casing"- .

INTERMEDIATE VOLCANIC —— Carbonated (calcite) 15'0(1-17 I 61'-grounded material * *-contacts: top-undetertninable

bottom-550 to core axisfine to medium grained ,j * * •nrey oreen colour-2t fine grained disseminated euhedral to subhedral pyrite

MODERATE QUARTZ VEIN SYSTEM (60t)-Contacts :top-550 to core axis

bottom-600 to core axis-10-15* riolnmlt./ankpritP ajtratinn wfth prpff^rrAH nrlpntnt1nn-60eto core axis . -

— 10-15X volcanic (tiatprlal-5-101 fine to medium orained subhedral to euhedral disseminated and— Goaisced pyrite sseciated-wUh-c4rbonate alteration ———————————————————— ~

-Irfice to 2? fin^ cirnfn,?f1 Piihpdral disseminated pyrite within fjiinrt.?

-1Ji l 7w-17 l 6"-Vein system associated with bands -of -rusty weathered material,locally having magnetic qualities^rendtag.-6Q.FJa*. to -core -axis- , ,. ,.

17'6"-20'0"M M

SAMPLE NUMBER

B3081K10621

* ' -*

R308?K10622

ASSAYS Pgn^uf/Rpl 1

0.020

•~

n.rif.o

0.005

0.072

r;^

EARTH RESOURCE* ASSOCIATES: DIAMOND DRILL LOG. PROPERTY: PUISSANCE HOLE NUMBER: P-2/04

FOOTAGE

-

3Z 0 ~-57*0"

^*

DESCRIPTION OF CORE '20 '0"-22' 6"

——————————————————————————————————————————— . ——————— n ——— B ———. ————————————————————————————————————————— 22'6"-25'0"..

II M

-25MOII-26 I "-vein system associated with magnetite bands-650 to core axis 25 l O'-27'6"——————————————————————————— . —————— . ———————————————————————————————————————————————————————————————————————————— . ———————————————————————————— , ————————————— n —————————— ,, —————————

-29'0"-31 l 4"-Veln system characterized by volcanic mater la 1-700 to core axis 27'6 U- 30'o"-w quartz/carbonate filled amygdules-trace pyrite . 30'0"-32'6"

.INTERHEOIATt VuLuAfiit; — bericite — Pillowed?? - - - .

-contacts: top-bu w to core axisbottom-undeterminable

grey green to green colour-fine grained , . ;-trace-2X quartz/carbonate filled subrounded amygdules-mlnou amounts of chlorite blebs .-trace- li fine grained disseminated subhedral pyrite

-33'0"-37'7 M -wan rock characterized by chlorite blebs-bO-Bb" to core axis 32'611 -3b I 0"

-SS'S^SS 1 ? 11 -quartz/carbonate veln-300 to core axis 35 I 0U-40 I0"-non-mineral I zed

f *

^'^"-AS'S^-quartz/carbonate vein 40'0U-45'0"-non-mineralized 45 i O"-50 l O M

SD'O^-SB'O 1155*0" -57 'O 14

!

END OK HOLE Al b/ FttT——————————————————————————————————————————————————— : ——————————— J ———— -a ———————————————

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SAMPLE NUMBERB3083K10b23B3084K10624B3050K10625

183086KlUbiibB3087K1U627

B3088

B3009

B3090B3091B3092B3093

ParS-trace

O.OAO

0.020

0.010

O.O&O

,

0.010

trace

o.OlO0.0400.0200.010

mnO.Ottt

0.03:

O.G'li

U.UUi

U.Ub'

Earth Resource AssociatesP.O. BOX 2150, TIMMINS. ONTARIO. P4N 7X8 CANADA

DIAMOND DRILL LOG

DRILLING COMPANY TRIANGLE DRILLING FOREMAN CORE SIZEBQ CORE STORED AT: Coreshack

PROPERTY HOLE NUMBER P-3/24

' GRID REFERENCE 25+37K/2+50NTOWNSHIP -ELORO CLAIM"'E22

AZIMUTH 22?" DIP ANGLE-45 0

DIP TESTS: lOOV-45', 200V-455 3COV-44* 450^LOGGED BY Ken Lapierre DATE November 9 " '

1954.FOOTAGE0-5 '0"

5045 fO"

**

DESCRIPTION OF CORE-drill casing -

.-irrSKMSDIATS-tfAFIU VOLCANIC —— Chlorite —— Ankerite 5*0n-10'0"

contacts: undeterminable 10'0M -15'On-grey green colour 15 f 0^-20*0"-fine-medium grained ankerite grains-chlorite blebs-with apparent orientation-45" to core axis-2-3^ quartz/carbonate veins -0-45" to core axis-trace-1^ fine grained euhedral disseminated pyrite

-z } ' u"-OM rt -quartz/carbonate vein-50"to core axis 20*0" -25*0"-trace pyrite

-28 l 10"-29 l 2"-quartz7carbonate vein-20e to core axis 25 I 0"-3U ? 0"-trace pyrite

30 I 0"-35'0!' :-38'6"-39'0"-quartz veln-SO"to core axis " " — " "~"3'5 tOll -i'7T i*'-5^ pyrite/pyrrhotite stringers-80~to core axis . 37 I 6"-40 T Q T1

x-40'6n -42 l 3"-siderite alteration-possiblv FAULT KiSLATED WO"-42'6"1

-4.

SAMPLE NUMBER l

1

53094J3095J3096

J3097

woysW099J3100p3101

p 102

el**5

tracetracetrace

, t

0.030

0.020

0.030trace0.010

0.020

AYS

t'AGE

EARTH RESOURCE ASSOCIATES: DIAMOND DRILL LOG. PROPERTY: Puissance

PAGE 2

HOLE NUMBER: P-

FOOTAGE

45'0n -53*9"

-53'9n -57'?"

*

57'7n-232*0"

DESCRIPTION OF CORE

-43 'On -45'0" -wall .rock characterized by abundant ground W 6" -WO"-trace-25S disseminated subhedral pyrite

BANDED IRON FORMATION-contacts: top-undeterminable 45*0" -47*6"

bottom-700 to core axis 47 l 6"-50 t On-magnetite bands(35^)-70"to core axis 50 I 0"-52 I 6"-siliceous material(5Q#) , 52 '6" -55 'O"-carbonate? alteration (10^)-5-lO^s fine-medium grained disseminated/coalesced/stringers of pyrite associated with magnetite, siliceous materialand carbonate alteration

: i

STRONG QUARTZ VEIN "SYSTEM (75#) 55'0"-57 t 6t1-contacts: top-70*to core axis

bottom-40c to core axis-iron weathered bands with 5# pyrite/pyrrhotite/magnetite-5# carbonate alteration

1NTERM3DIATE VOLCANIC —— Calcite —— Pillowed??? 57'6"-60 f O"-contacts: top-40"to core axis 60'0"-65 I 0?

bottom-undeterminable ^5 1 011 -70 •O"-fine-medium grained Vd80"-75'0"

-?:rev creen to green 75 l 0n -80'0n-sliKhtlv-htehlv. carbonated 80 I 0"-85 1 0"-trace-39o subrounded quartz/carbonate filled amvedules' 85'0"-90 I 0"-trace calcite stringers 45-90' to core axis 90'0"-95 t O"-trace-2;^ fine-medium grained pyrite 95 f On -100 t O"

lUO t O"-105 l O"10J)'0"-11U'U"11U'U"-11^'U"115 f O n -120 f O n

————————— 120'0H -125 t O" 1

SAMPLE NUMBER8^103

B3104B3105B3106B3107

-*

B3108

B3109B3110B3111-B3112B3113B3114B3115B3116B3117B3118 |B3119B3120B3121B3122

BelfS^.YS0.02C

0.01C0.002trace0.044

0.003

0.01*tracetracetracetracetracet ra ctracetracetracet ra c i0.031tracetrac

"x - '

D\RTH RESOOTC5 ASSOCTVCS ASSOCIATES: DIAMOND DRILL LOG PROPERTY: Puissance HOLE NUMBER:•"OTAGE DESCRIPTION OF CORE '.

125*0" -130*0"130 'On -135'0"135*0"-140'0"140 f O"-145'0"I45 l0"-150'0nISO'On-WO"155 t O"-160'On160 '0" -165 '0"

.165 ' S"-169 '©"-quartz vein-5* to core axis 165 f O"-170'0M-2# tourmaline associated with both contacts-trace-255 fuchsite-2-3# pyrite

170'0"-175 t On175 '0H -180'OnHJU'U"-1B^'0"Ig5'0"-190'0"190 f O"-195'On

.197 f ll"-19S f O"- FAULT-55* to core axis . 195 fO"-197 '6"-5-10S& sulphides associated with both contacts 197 f o" -200*0"

.198'l"-199'0"-quartz vein-20*to core axis-5^ carbonate with both contacts-trace fuchsite alteration-3^ disseminated medium grained subhedral pyrite

200'0"-205'0"-208 t 4"-208'S"-ankerite alteration 2O5'U"-^iU'u''

-3/i quartz/feldsoar filled ainygdules-trace amounts of magnetite blebs-trace amounts of fuchsite blebs-trace fine grained disseminated pyrite

-209 ' 0" -209 ' 6" -a nkeri t e a Itera ti on-l)o magnetite blebs-trace-15o quartz aniyp,dules-trace pyrite

SAMPLE NUMBER

B3123B3124B3125H3126B3127B3128B3129B3130B3131

B3132B3133B3134B3135B3136B3137B3138

.

133139B3140

V" " Jel^AYStracetracetracetracetracetracetracetracetrace

tracetracebtat.*0.23itracttracttrace

tracet ra c*

EARTH RESOURCE ASSOCIATES. DIAMOND DRILL LOG. PROPERTY: Puissance . HOLE NUMBER: P-

FOOTAGE

?3?*n"-266*0"

•**

266*0"-344 '4"

DESCRIPTION OF CORE

.211'4"-2n*ll"-quartzXankerite veinlet-200 to core axis 210 '0" -21 5 '0"-trace pyrite

.215'0rt -2l8'0f1 -ankerite7dolomite alteration 215*0" -22o'0"-yfo quartz and quartz/feldspar filled araygdules-I0?b fuchsite blebs-trace-l/* magnetite blebs-2# medium grained disseminated pyrite-trace pyrite filled amygdules

,-221'6"-222'7"-abundant cal cite/magnetite alteration 220'Q"-225'0"

-trace-2^ quartz and quartzXf^W5par filled amvgdules22 5*0" -230 'On

INTiCRMEDIATE VOLCANIC —— Sericite —— Ankerite 230 I 0"-235 I 0TI .-undeterminable contacts ' 235 I 0"-240 I0"-fine grained 240*0"-245 I 0"green colour 245 f On -250*0"-slightly carbonated-minor amounts of chlorite blebs 250*0"-2^5*0tt i-trace disRpminnted fine grained subhedral pyrite 255 I On -^b0 1 0

260*0n-265'0n

ANKiirilT^/OUARTZ/i-UCHSITfi ALTERATION ZONa 265l O"-26? t 6"-contacts: top-250 to core axis-FAULT RELATED 267 ' 6" -270* O1'

bottorn-400 to core axis-FAULT RELATED 270*0'f -272*6n-fine-medium grained ankerite wains 272 f 6"-275'0"-Qli cht.Ty Pflrhnnst-.firt 2?S *Q".272*6"-S-1V* i rregular trending ouartz/ankerite strineers 277 *6"-2gO*0"-fiichRit.e a Iteration asfsociated with quartz stringers- ' 2^0 'Q" -2 82*6"gan^rplly MT-Wf tn core axis 282*fe"-285 '0"

-trace-!'* fine erained disseminated pyrite 285 t O"-287 f 6n-2^ fine grained pyrite associated with areas of fuchsite 287 t 6Tt -290'0"alteration 290* -292*6"

292*6"-295 f O"*

SAMPLE NUMBERB3141

B3142

B3143

B3144

B3145B3146B3147B3148

B31^BJ150B3151

B3152B3153B3154B3155B3156B3157B3158B3159B3160B3161B3162B3163

TrcCAVQBelfSWV strace

trace

3.034

trace

tracetracetracetrace

tracetracetrace

traceD. 015tracetracetracetracetracetracetracetracetracetrace

?

EARTH RESOURCE ASSOCIATES DIAMOND DRILL LOG. PROPERTY: -Puls ^ance HOLE NUMBER: f

FOOTAGE

339'6".428 '0"

DESCRIPTION OF CORE

-297'3"-297 f 6"-quartz vein-5Cf to core axis-non-mineralized 29*5* O". 207 'fi 11

-304 f 7"-305'0"-quartz vein-750 to core axis 2Q7'6"-1OO'0"-non-mineralized 300'0"-30?'6"

I02'fi".io*;'0"-306*10"-314*0" -SHEARING^' to cnre axis 305*0".307'6"

-quartz/ankerite/fuchsfcte alteration oriented 307 'fi" .310*0"parallel to shearing 31O'O" 312 '6n

- chlorite/fuchfiite al t**ration ^.ssQCiated with 312*6" -315*0"both contacts

-315*8"-317'0"-prfif(-rred nri flotation of quartz stringers and 3J5*O"-3l7'6'tfuchsite alteration-40 to core axis

.-317 l O"-322*On -25^ q'uartz stringers with preferred orientation- 117*6*1.320*0"

40*t.o core axis 320*0" -3 22*6"

-322 *0"-327'0" -abundant ground 172*^1.37510"-ground characterized by ankerite grains and 125*01.127 'fi"chlorite alteration-FAULT RELATED 327*6" .330*0"

330*0"-332*6n132*6" .335*0"335*0"-337',6"

-338 18 n^139 l 6" -fuchsite alteration 33 7*6" -3 40 fD"-3?o fine grained disseminated euhedral pyrite•-

INTERMEDIATE VCLGANlC —— Ankerite —— Fuchsite . 340 'O" -34*5*0"-contacts: top-40'to core axis l/^'on.i^O'O"

Dottom-gradational 350 "-355*0"-fine-medium grained ankerite grains 355*0^-360*0"-grey crrA^n C^l^nr-trace-15i fine grained pyrite

SAMPLE NUMBER

P31fi;

hnfi5B3166Rilfi?03168H11fi981170B3171

B1172- ,,

Tj ** ^ fj *b" f Mf

B3175R3176 .

B317SR317QB3180B3161

B11S2B31^3B3184.B3165

5-^-'91-••m |ASSAYS ii"Be'll

0.010

0,0400 0300.fi?Qtracetracetrae**

t- rg c**

trace0.010

tra^e

trac*1trace^* ra r* o

trace

trac^f" T*H f* O

tracetrace

** I

j

lj

i!

^IVHHMH

tEARTH RESOURCE ASSOCIATES: DIAMOND DRILL LOG. PROPERTYPuissance

PAW 6 HOLE NUMBER: P-3.Z&

FOOTAGE

4

*-* i

••-:

42^*0"-450*0"

.

DESCRIPTION OF CORE -362*0" -364 *0"-abundant fuchsite 360*0" -3^5 !0I(

365'0"-370'C"371 f l"-372'2"-abundant fuchsite-FAULT B2LATSD 370'0"-375 !0n372*2n -373 *0"-abundant coarse grained ankerite grains andchlorite alteration-FAULT RELATED376 '8n -377 "-fuchsite banding- 50* to core axis 17?'O".lrtft*O"

. - * ^dO'OW^dS'O**3S6*0"-366*V-fuchsite bandinK-35e to core axis 385 t O"-39b*0"i•38S t 8"-3^9 t3"-fuchsite banding-30' to core axis

-quartz stringers associated with both contacts-trace pyrite 390*0tl -395*0tf395* O" -400*0"410*4"-411 l O"-quartfrAnkerite7fuchsite veiii.^O'tio GO^** pxi s 40O'O"-^O*;'On405*0" -410*0"410 fO"-?4l5 f O"415'0"-420'0"420'0"-425*0"425 *0"-430 *0"MAFIC VOLCANIC —— Calcite —— Chlorite ^O*0n-^35*0"-undeterminable contacts 4-1-5*0" -440*0"-fine grained 440* O 11 -445*0"-dark green colour

-trace-1^ fine grained subhedral disseminated pyrite443'g"-444'3 w-auartz vein-W,tn cnre axis /,J,*;*pn -i'450* nn-6parii;iel chlorite stringers-30" to core axis-2^ fine grained pyrite associated with chlorite'stringers

j/^,END OF HOLS /T 450 FSST November Q, 1Q84. f/ V^Cftfafa7KtS*S* r ^^ ^ ^

SAMPLE NUMBER

B3186B31S7B31SB

B31S9B^IQOB3191

B319SB^19*B31QUB3195B3196B3197B3198B3199B3?00B1201B32"02

B3203

wASSAYS

1^11 tftracetracetrace

tracet,racftrace

traceCUDQOt- racetracetracetracetracetrace*-T*O f*P

tracetrace

trace-

!l

;

,,

Earth Resource AssociatesP.O. BOX 2150, TIMMINS. ONTARIO, P4N 7X8 CANADA

DIAMOND DRILL LOG '

DRILLING COMPANY TRIANGLE DRILLING FOREMAN CORE SIZE BQ CORE STORED AT: Coreshack

PAGE 1

PROPERTY PUISSANCE HOLE NUMBER P-4/64

GRID REFERENCE 25+3^/2+5011

TOWNSHIP Jiekjro CLAIM ^ AZIMUTH 2000 DIP ANGLE -'

DIP TESTS: 100'7-430 , 200'7430 , 300V450 , 400'745 LOGGED BY Ken Lapierre DATE November 12, -

FOOTAGE

fl-5'0"

MO"--5**?"

DESCRIPTION OF CORE

-nVill casing

INJFRMFOTATF VOLCANIC —— Ankerite 5 l U"-t0 1 0"

-undeterminable contact*-fine-medium grained ankerite arains-slightly to (pftdPrat.ely carbonated-chlorite blebs present-trace-?? ffn^ to mpdliim grained disseminated pyrite

-!2'0"-13'0"-abundant ground-possibly FAULT RELATED 10'0"-15'0"15'0 M-20 I O li

-?3'Q"-?4M"-wa!l rock characterized by ankerite carbonatization 20'0M -25 I 0 U-1X fuchsite alteration . . .-Mi pyrite --' '

-26 i r-26 l2 l'-quartz veinlet-65" to core axis 25 I 0"-30 I 0"Rhundant siderite alteration-trace pyrite

-30'0M -30'11 u-q"?rt7 vA!nlet-?S0 to core axis 30'0"-35'0"-minor arounts of ankerite, fuchsite altpfMt.ion with contacts-2X fine grained euhedral pyrite associated with hanging wall

-. .., .. ,., ......contact-...-.- . . — ..- - -,,.,,,,.. . ...... . .... .... ..—

— 3SlBa-36'10"-quartz voinlet^O0 to core axU ———————— ~. ——————————— 3S'0"-40'0"-3^ sjdprltp/ank^ritp alteration—^r?)rf* r fifl Jrnpv'i'f f n ^55^^ Jg^^irJ wlTh!fl V^l"^ 0 ^

SAMPLE NUMBER

B3204

-*

83205B3206B3207

B3208

D3209

iiO5*ri

BetfSftYS

trace

4

tracetracetract

tract

tree*

tree*

EARTH RESOURCE* ASSOCIATES: DIAMOND DRILL LOG. PROPERTY: Puissance HOLE NUMBER: P-f/a*^

FOOTAGE

~..

55' 3"—CCI O" ——— 00 O —

DESCRIPTION OF CORE

-51 pyrite associated with hangingwall rock proximal to veinlet

-36 '8"-37'1 "-quartz veinlet-200 to core axis31 pyrite at and proximal to both contacts of veinlet

-37 I 8M-37'9 M-FAULT-60 0 to core axis

-44'0"-44'4"-qiiartz vein-200 to core axis 40 1 0 M-45'0H-11 pyrite associated with both contacts and within vein

.-45'9M-46'2"-wall rock characterized by 31 pyrite stringers and 11

disseminated pyrite

-47 l O"-47 l ?"-quartz vein-600 to c^re axis-siderite alteration-21 pyrite- - -'-trare chalcopyrite

-*n'9"-ftf'3"-uall rork r.hararter i 7Pri hy SHEARED appearance 45 1 0 U-50'0 14

-"strptrhPd" ijiiartT/rarhnnatP f*4Jpd amygdnles-70o to nore axis

-phlnHtP altpratfnn l-trare-?! medium grained pyrite - f

5Q'0"-55'0"

SAWDE4)-WON-fORMATM)M — Siliceous — SulpWde - ...- . - ,- ;1

-magnPtitP hanrts{?nt)-dfi0 to rore axis

-51 ankerite/carbona'te alteration assorlatprt with mannpt.f'f.p tnnf.arts-51 pyrite/pyrrhotite alteration associated with magnetite and siliceous

bands— 55^4^56 '^-abtfndaftt-r-tfsty weather-ed-bands-50-600 to core axis —— . . ————— t ;:,"^ t ^ u —57 I 6"-60'0M

60 I 0"-62'6 M62'6"-65 l O"65 I 0"-67 I 6 U

SAMPLE NUMBER

B3211

t

B3212

B3213

83214832150321603217B321B

Beffl'

O.OOJ

trae

trace

0.0700.026tracetracetraca

1 M i111 \

ws

EARTH RESOURCE ASSOCIATES: DIAMOND DRILL LOG. PROPERTY:PAGE 3

HOLE NUMBER: p'^4*

^4FOOTAGE67*8"-

75 '0"

7b'0*—au 'O14

~*

80 "O"—155'0"

DESCRIPTION OF CORE

STRONG QUARTZ VEIN SYSTEM (85?) b7 l b"-XO'U'1-undeterminable contacts 70'0H-72 I 6 U——— siliceous material (85*) —————————————————————————————— 72 I 6"-75'0"-magnetite bands (4J)-30-50* to core axis-anker He/carbonate aiteration(St) associated with magnetite bands andwith vein material-5J pyrite/pyrrhotite mineralization associated with carbonate material

•.BANDED IRON FORMATION— Siliceous— Sulphide /^O^-^/'b"-undeterminable contact ;top 77'6U-80'0"bottom-45*to core axis

-magnetite bands (202) -65" to core axis-smoKey grey-grey green siliceous material (fcox)-lOi ankerite/carbonate alteration i - - -.-j)-iOi pyrite/pyrrhotite associated with magnetite contacts andcarbonate alteration -^ :

.

INTERMEDIATE VOLCANIC — Ankerite-contacts: top-45" to core axis

bottom- undeterminable-green colour-fine-medium grained ankerite grains-chlorite alterationtrace to 21 quartz/carbonate tilled amygduies-trace pyrite

-81Tl-B2 I 4 ll -ankerite7quartz vein-50" to core axis 8U'0"-85 I 011-itf chlorite alteration-51 pyrite

^82' lO'-SS 1 5"-ankeri te/quartz vein-undetenninable contacts - —— 1-5t chlorite alteration-5 J pyrite

SAMPLE NUMBER

B32190322063221

U3ZZZ83223

-*

8322^-

tracetrace0.014

trace0.006

'

trace

m

i PA^EARTH RESOURCE ASSOCIATES: DIAMOND DRILL LOG. PROPERTY: ..Puissance HOLE NUMBER: v'

FOOTAGE

155*0"--189*4"

DESCRIPTION OF CORE85 l O"-102 l O M-wall rock characterized by '3X amygdules B5'0"-S0'0 11-b-ioi ankerite grains with apparent orientation-700 to core axis 90'0H-95 I 0"

95 l O"-1oo'On—————————————————————————————————————————————————— |00 'Q"-105'0"-107'0M-118 l OM-wall rock characterized by calcite alteration iui)duM-nu'u"110 I 0M-115'0M

11b*0"-12U*U"1iJU'0"-12b l O"

-129'3"-129'9"-quartz7ankerlte vein-undeterminable contacts izb'u'MSO'u 11-21 chlorite alteration ---trace pyrite associated within vein and with both contacts——————————— x* —————————— !±!! ——— : ————————————————— 130'0*-135^rt

ISS'OMWO"140'0"-14b'U"inb iu"-ibo 1 u"

^ ibO'tr-iib'trANKERITE/QUARTZ ALTERATION ZONE

-contacts: toD-450 to core axis-possibly FAULT RaATEObottom-undeterminable

-fine to medium Q rained ankerite grains-qrey green colour-si Iqhtly carbonated-5-10* quartz/carbonate stringers with apparent orientation 45-60" tocore axis-trace fuchsite alteration locally associated with quartz/carbonate stringers-trace disseminated pyrite

-150'6"-158'iri -quartz7tourrnalineXcarbonate veJn-200 to core axis . 155'0"-160'0U-non-mineralizedt-159 l 8u-160 l O"-quartz7carbonate vein-400 to core axis

-non-mineralized

-162'0"-163 l Ou-wall rock characterised by abundant siderite ibu'u'--1o5 l u"

SAMPLE NUMBERb.^bB3ZZ603227B^?2fl —Vv/tvCiV

B3229B3230B3^31B3232B3233

B3234U323bUitJbU3237u3^3d

B3239

B3240

Bell^YStracetracetracetracetrace0.004tracetracetrace

traceO.OOUtracetracetrace

trace

trsci

EARTH RESOURCE ASSOCIATES: DIAMOND DRILL LOG PROPERTY: HOLE NUMBER:FOOTAGE

189*4"--207*6"

207*6"—231*8"

-

DESCRIPTION OF CORE-162'6"-163 l 9u-carbonate7quartz veinletrtS* to core axis

-trace fuchsite-21 f ine grained disseminated pyrite

16b'0"-170 l p-174 I 6"-175 l O"-carbonate7quartz vein-350 to core axis 120'0"-175 I 0-trace pyrite

175'0"-1UO'0-183'2"-184 l 3 ll -ankerite7quartzXblack chlorite velnlet-100 to core axis

-abundant fuchsite alteration associated with botn contacts-trace pyrite -

ii}0'0"-185 l C-187'4"-187 l 10"-quartz7ankerite vein-20" to core axis

-non-mineralized

INTERMEDIATE VOLCAMIC--Ankerite } 185 I 0"-100'C-undeterminable contacts 190'0"-195'(-fine to medluni grained anlerite grains ISS'O-^OOU-grey green colour . *-slightly carbonated-trace pyrite

--203'0ll-205 l 4 ll-wall rock characterized by siderite alteration zou'O-^ub'd

205'0M-2oT(|'-'

ANKERITE/FUCHSITE/QUARTZ ALTERATION ZONE-contacts: top-500 to core axis- FAULT RELATED

bottom-500 to core axis-FAULT RELATED-fine to medium drained ankerite grains-500 to core axis-local ly-chlorite blebs-500 to core axis-serpentine chlorite alteration-locally ^-5-IOt irreoular trending quartz and quartz/carbonate stringers-10* fuchsite alteration associated proximal to quartz and quartz/carbonatestringers-trace-1X pyrite -increase in pyrite concentration associated with fuchsite

* '

SAMPLE NUMBER

! li3Z411 U3242

' U3243

1 U3244

;,H B3245" B3Z4611 B3Z47

" 1W243u B3249

—— -^r- ———— . —

Bellas

tracetrace

trace

trace

tracttracttrace

trao-traa

*

P A P - F-:

rfST^,

l PAWEARTH RESOURCE1 ASSOCIATES: DIAMOND DRILL LOG. PROPERTY: Puissance HOLE NUMBER: P4A4

FOOTAGE

—— r-

*-A

231 '8"--337*0"

DESCRIPTION OF CORE '-2u7'ir'-^u'u"-preTrerre(i orientation or, anxente grains-50w to core axis- 207 1 6"-210'011FAULT RELATED ~

210'0"-212 I 6!-213'0"-214 l 3u-auartz vein-200 to core axis 212 I 6"-215'0U-non-mineralized

-213 l 3"-213 l 8ll-quart2 vefn-20* to core axis-non-mineralized

-216 l 9"-217 l O"-quartz7fuchsite vein-300 to core axis 215'0M-217 I 6"-trace pyrite associated with contacts*

-219'5"-219' 1 f "-quartz vein-400 to core axis 217 I 6"-220 I 0"-5X fuchsite alteration within vein-W chlorite alteration-trace pyrite "'*

-22Q l n"-2?2'Q"-waH rock characterized by abundant chlorite-posslbly 220^0U-222 I 6MFAULT RFI.ATFO

'

-???'0"-?29 l 8B-wall rock characterized by fine grained ankerite alteration W6II-P?S I 0Mand "stretched" chlorite blebs-500 to core axis

-227'1 M -??fl l 6"-cnre characterized by sandy/sllty material *WATER SEAM 225 I 0 M-227 I,6 11-highly carbonated 227'6"-230 l0 1'-229 l 8u-231 I 8"-wall rock characterized by 701, fuchsite alteration 23o'0"-232'6"

-301 irregular trending quartz/carbonate strinaers-trace pyrite

232'6"-235'0"

IMTFRMFnTATF Vni nANir.-^.nhlnrltP—— Untorft** 2^51)*^^^-rnntacts: top-50ft to core axis *K™ -^4b^bottom-undeterminable 245 I 0M-250'0"-fine to medium grained ankerite grains * 250'0"-25b'U"

SAMPLE NUMBERB3250

U3:iti1B3202

83253

03254

•9

B3255

D325&

DOOC7 PJ^O/ ——63258

B32BS

B3260

mst-B3263B32b4

Delefttrace

o.ooa0.276

0.012

0.012

' -

trace

trace

trace0.005

0.004

trace

tricetracetracetroce

Vs , /rech.

0.27;

-

EARTH RESOURCE'ASSOCIATES: DIAMOND DRILL LOG. PROPERTY: Pu j ssance HOLE NUMBER: p.

FOOTAGE

fc*

DESCRIPTION OF CORE

———— -green colour ——————————— : —————————————————————— ZSS'O^-MiO'ti"-trace quartz/carbonate filled amygdules 260' 3-265 "0"-trace Irregular trending carbonate stringers 2fi5 l n"-?70'nJI-trare pyrite 270 'O" -275 '0 M-

?7R'0'-?RO'0"?An*n"-9H^'n"285 '0" -290*0"290 I 0M-295'0"295 I 0"-300'0 11300 '0"-305* O 113n*j*n"-ain'ft 11310'0W-31^'0"315 I 0"-320 I 0"

-3?n'n"-tt7'n--in* rarhnnatP ^trlngpr-c *nrt vplnlAt^.aR* tn rnr* svU 320 1 0 M -3?5 I 0 M3?5 1 fl'-330'0M

" ' - "' - 330'0M -335 I 0"335'0"-337 I 0"

; - . ' j*

,.

. - -———— END OF HOLE AT 337 FEET ————————— '. ———————— : ———————————————————

f*

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SAMPLE NUMBER

D3265U32C6B3P67

.832^8B3?feQfi3?7083271B3272B3273B3274H3?75B3276B3277B3278Q3P7Q8326083281

L

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-

Earth Resource .AssociatesP.O. BOX 2150, TIMMINS. ONTARIO, P4N 7X8 CANADA

DIAMOND DRILL LOG

DRILLING COMPANY TRIANGLE DRILLING FOREMAN CORE SIZE BQ CORE STORED AT: Coreshack

PAGEi

PROPERTY HOLE NUMBER p'5 /84

GRID REFERENCE 25+41E/2+49NTOWNSHIP Oeloro CLAIM H- E - 22

AZIMUTH 1800 DIP ANGLE-450

DIP TESTS:100 '/-450 , 200'X-440 , 3QOV430 . 387V41 0 LOGGED BY Ken Upierra. DATE *ov. 15/84

FOOTAGE0-7 'O"

7*0"—63 '0"

*

63*0"—72 '0"

DESCRIPTION OF CORE

drill casing '--- .

INTivKMEDIATiS-MAFIC VOLCANIC —— Ankerite —— Calcite —— Chlorite 7'0"-10 I 01'-contacts: top-undeterminable . 10*On-15 f O"

bottom-bO* to core axis I5 fO"-20 f O"-fine to medium grained 20 f O"-25 f O"-grey green to green colour ' 25*Ofl ~30 f O"-tra ea pyrite 30*0??-35*0"^^^''-^y'U"

40*0"-45 f O"45 f O"-50*On

-52 T ll"-53 f O"-quartz veinlet-70a to core axis 50 f On-5Xf6"-non-mineralized 52*6n -55*0"

-54 t O t1 -54 1 3"-quartz vein- 70" to core axis 55 l Ott -57*6n-10jS pyrite stringers within vein-70*to core axis - -'

-56 ! 5"-63'2"-wall rock characterized by sheared appearance-contacts: top-70e to core aocis-FAULT RELATED 57'6rt -60*0n

^ botton-60*tp core fljrfp 60*0M .62*6"-"streched" qua r t z/ ea r bona t e filled amygdules- ' 62*6n -o5 f O"700 to core axis

STRONG QUARTZ VEIN SYSTEM (90#) 65*0"-67'6Tt——— contacts: top-^0" to core axis . ——————————— —— '- —————— 67'6"-2QIQn — —

Bottom-40* to core axis * 70'0"-72*6"

SAMPLE NUMBER

B3262B3283B3284B328^B3286B3287B^iJtiBB3289B3290B3291B12Q2

B3293

B3294B3i2sB329fc

B3297•300QO

B3299

Jel^SS^ch

tracetracetracetracetracetracetracetracetracetracetra.ce

trace

tracetracetrace

0.106n,r,3^O.o40

*

3.10^

EARTH RESOURCE'ASSOCIATES: DIAMOND DRILL LOG. PROPERTY: Puissance HOLE NUMBER: P-5/84

FOOTAGE

72*0"—69 to"

-,

89*0"--130*3"

DESCRIPTION OF CORE

-2-1 chlorite patches and stringers-2;., ankfn-it.fi a 1 t.erAt.i nn-j/j n;.Tfnetite material-2-5/* fine to EuxJium grained subhedral pvrite-coalesced ,disseminated, and stringers generally associated with alterationmaterial within vein

BANDED IRON FORMATION —— Siliceous —— Sulphide 72*6f'-75'0"-contacts: top-35-40* to core axis 75 I O tl -77 t 6n

bottom- 50* to core axis 77 1 6"-80 l O fl-magnetite bands (203) -60* to core axis 80*0" -82 '6"-smokey grey siliceous material (702) 82 t 6lf -85 f Otl-5i* ankerite alteration-2-5yJ pyrite/pyrrhotite-higher concentration of sulphides proximal to uppercontact

-trace chalcopyrite: .

-85*0". 86 "-fragmented appearance to Iron Formation 85 1 0"-87 t 6n-magnetite in the form of broken irregulartrending stringers

:. 87'6M -90 f OM

INTERVEDIATE-MAFIC VOLCANIC —— Ankerite —— Calcite- — Chlorite QO t O"-Q'i'OM t-contacts: top-50*to core axis 95*0n -100*0"

bottom-Kradational 100 fO" -105*0"-fine grained 105 f O"-110'0"-green colour, 110 f O"-115*0"chlorite alteration-highly carbonated-trace pyrite

.t

SAMPLE NUMBER

B3300B3301B3302B3303B3302*

•* i

33305

33306

333073330833309J 331033311

*iflhvs

0.010trace0.020trace0.010

trace

trace

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,

tEARTH RESOURCE ASSOCIATES: DIAMOND DRILL LOG. PROPERTY: Puissance HOLE NUMBER: P-

iFOOTAGE

11^'G".130*3"

130*3"-142*0'

—•*

ti\

DESCRIPTION OF CORE

, .INTr?-J2liIAToJ-lAnC VOLCANIC —— Ankerite n *J'0"-12n'O"contacts: too-sradational 120'0"-125 t Onbo t torn- 80* to core axis 125* O" -130*0"-fine to medium grained ankerite grains

-grey green to green-slightly carbonated-trace pyrite

-ANKEHITS/Q.UARTZ/FUCHS1TS ALTERATION ZCNiS 130*0n-132.*6"-contacts: top-30"to core axis-possibly FAULT RELATED

bottoin-20*to core axis , . . --medium grained ankerite grains— Ijo sid**r1t.ft glf. ft ra t- "i OP-grey green colour ^-5-lO^b quartz and quartz/carbonate stringers-2# fuchsite alteration generally associated withquartz and quartz/carbonate stringers and veins-trace pyrite .-3* fine grained pyrite associated with fuchsite

-132'0"-133'4"-area of abundant fuchsite alteratinn 132* 6" -13 5*0"-I33'0"-133*4"-carbonate7quartz vein-20- to core axis

-non-mineralized135*0f1 -137'6n137 * 6" -140*0"

-141 '0"-l42*0"-carbonat^Xqu?irt9'. v**in-2O*to co^** flxie 140'0"-142'6"-trace tourmaline— npn— "15,1^^3^3 1\ 7* fid

.*

SAMPLE NUMBER

R"?^12B3313B3314

B3315

.9

'

B3316

B3317B5318B3319

•-

g^"1

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•fiEARTH RESOURCE ASSOCIATE'S: DIAMOND DRILL LOG. PROPERTY: Puissance

PAG HOLE NUMBER: P-

FOOTAGEU2'0"-

165 'C"

165 fO" -210*9"

DESCRIPTION OF CORE*

INTaKKiiniATS VOLCANIC —— Ankerite 142'6"-145'0"-contacts: top-20* to core axis 145 I 0"-150'0"bottom-undeterminable 150 l On -155'0"

-grey green colour 155*0" -160*0"-medium graned ankerite grains 160*0" -165*0"-2-5;c quartz and quartz/carbonate stringers and veinlets-trace fuchsite alterationtrace pyrite

1"

ANKSK1TE/FUCHS1TH/QUARTZ ALT15KATICN ZONE-contacts : top-undeterminableboltom^eifto core axis-rAULT J:35LATaU-fine to medium grained ankerite grains—grey green to emerald green colour-10-15/6 irregular treding quartz stringers-10^ fuchsite alteration.trace-2jfe fine grained disseminated pyrite-increase in pyrite with increase in fuchsite alteration

-165 I0"-165 1 8"-fuchsite alteration associated wifch 4 quartz 165 t On-l67 f 6"veinlets 145* to core axis )

-tourmalin^! associated with quartz167*6" -170* Q"170*0" -172 '6"172* 6" -175 'O'1175 t On -177' 6"

* - 177 '6" -180*0"-180 ' 9" -1S3' 10" -FAULT-55" to core axis 180 f O M -182'6"-abundant serpentine-talc/chlorite alteration-^fuchsite alteration-traCe-lfj fine grained pyrite

-133'10n -192 f O"-20/* irregular trending quartz/carbonate strin gers and veiniets 182*6" -185 T0'

SAMPLE NUMBER

R^^2nB3321B3322B3323B3324

-j*

.

B3325

B3326B3327B332SB3329B3330B3331

B333^

BeAS^rS

t'.T'fl P P

tracetracetracetrace

trace

;race;race;race;raceirace;race

,race

EARTH RESOURCEASSOCIATES: DIAMOND DRILL LOG. PROPERTY: HOLE NUMBER: P-

FOOTAGE

-

**

210*9"-295*0"

DESCRIPTION OF CORE185*0"-187'6'!187*6". 190* C"190 *0" -192 '6"

- 192 '6"-194 '6' -abundant fuchsite alteration 192 l 6"-195 t O"

-194'6"-iyii*j"-v;all rock characterized by ankerite carbonatization-chlorite blebs-70' to core axis 195*0" -197*6"

197' 6" -200 'C"

-193 I 3 rt -2Gl l 7"-abundant rucnsite arteration-oO" to core axis 200*0"-202*6". . *

•2Gl'7"-*u6'y'-intermediate Volcanic 202 '6n -205*0"-abundant ankerite alteration

t•206*5 -208 '8" -abundant fuchsite alteration 205*0" -207* 6"— ti~av;e, pyx"i Le . - i

•207 t 10"-210 l u"-Intermediate Volcanic 207* 6" -210*0"

•210 '0" -210 !9" -abundant fuchsite alteration ~-1^ line grained pyrite

INTERMEDIATED FI C VOLCANIC —— Ankerite —— Chlorite ————————— 210*0H -212*6tt-contacts: top-60"to^core axis-KAULT HELATi!D 212*6tt -2l5*0''

bottom-70 to core axis 215 I On-220*0"-fine-medium grained ankerite grains 220*0n-225*0".grey green to green 225*0"-230 I0"-trace-1/i dissemunated pyrite 230*0" -23 5*0"

235 ? 0n -240*0" S240'0"-24i) l O"

.246 '10" -246 '5" -wall rock Characterized by fuchsite alteration 245 I 0"-250'0M-Ifi medium grained subhedral pyrite 250'0"-255'0"———————————————————————————————— n ————————————— 255 t O"-260*0**—

2^0!fin-265'0"————————————————————————— — ——————————— -s ——————— 265*0 -270*0" —

SAMPLE NUMBERB3333B3334B3335B3336

B3337B3338

B3339

3ellS?.YS0.01Ctrace0.016trace

tracetrace

trace1

B3340 fcrace

1BI341

B3342

B3343B3344B3345B3346B3347B33433349B3350B3351i3352Bn^—(J3354vm i

iracem

irace

,raceirace•raceirace•race.race,raceirace,race.race'.C04.race.race,

i

EARTH RESOURCE ASSOCIATES: DIAMOND DRILL LOG. PROPERTY: PuissancePAG

HOLE NUMBER: P. 57

FOOTAGE

zys'O"-— 3 11*9"-

311'9"-jtf/'O"

•**

i

:

DESCRIPTION OF CORE270 t6"-275'0"275'0"-250'Cn^0'0Tt -285'G rt285 fO" -290*0"290*0"-295'0"

ANKiiRiTci/guAKTZ ALTERATION ZONE 295*0" -300 'G"-contacts: top- 70' to core axis 300 f O"-305*On

bottoffi-60* to core axis 305 fO"-310 t O"-grey green-Pine grained '-10^ carbonate/quartz stringers. irregular trending

IMTiiKhEMATS-KAFIC VOLCANIC —— Calcite ; 310*O"-31^*O'-contacts: top-bO' to core axis 315 t O"-32b*Ot

bottom-undeterminabla 320*0" -325*0'-green colour 325 f'0 M -330 l O l-fine grained 330*0n -335 f 0f-chlorite blebs 335 ? 0"-?'40 | O I-trace a^iygdules 3^*0" -345*0'-trace-5;t ankerite alteration 345 f On-350 f Of-highly carbonated-calcite 350 l On-355*0T-trace dissemunated pyrite 355 l OM -360.tO'

3bO T On -3b5'0T3b5 t On -370*011370*0"-375 t Oh37i,'U"-3^0 fO"

- . 380*0" -385*0"385*0" -3^7*0"

END OF HOLE AT387 PEBTS i^ ^———————————————— tffy^tiKeMf ___

I J^ w TT 1 ft *^ *

SAMPLE NUMBERB3356B3357B3358B335983 3 60

B3361B3362B3363

'imAffB3365B3366B3367B33681*3369B3370B33?lBS372B3373B3374B3375B3376B3377B3378B3379

8eWA^ iO.OOjt ra C!tracttrac*trac(

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i

-

Earth Resource .AssociatesP.O. BOX 2150. TIMMINS ONTARIO. P4N 7X8 CANADA

DIAMOND DRILL LOG

DRILLING COMPANY TRIANGLE WULLIN5OREMAN CORE SIZE BQ CORE STORED AT: Coreshsck

PAGEv

PROPERTY TuiSSAKCi - HOLE NUMBER pfc./^

' GRID REFERENCE 24+422/2+51NTOWNSHIP Deloro CLAIM M. E . 2

AZIMUTH DIP ANGLE .90

DIP TESTS: 100 I 7-90 0 ,200V-890 ,300V880 ,400V870 ,471 1 / LOGGED BY Ken ^ ierre DATE NoV| 16M

FOOTAGE

0' —7 'o11

7*0"-50IQ'

56 f -6? f

DESCRIPTION OF CORE

-riri 1 1. casing '

. -

INTERMBniATS VOLCANIC __ Ankerite^-^"Chlorit0 7*0" 10*0"cont-p ctrS * top— undctenninsEbl.8 10*O*f 15*0**

bottom-6O* to core axis*-FAIJLT ^ELATSP 15*0"-20*0n—————— -grey green to green colour ————— - ——————————————— 20*0^-25*0" —————— -^fine-medium grained ankerite and chlorite grains ————— 25?)0tt *30*0n —

™ tracft1 pyrite "^O'O** ^S*O**————————— i- ————————————————————————————————————— JS'O^OtO*

^0*0 -45*0"4 l? t Ot*.SO*O1*

-5?*;n-56*0"-wall rock charactericed b h d/Tt b h d 50*0" I2 f (tlf——————— —— fragmented appearanoo-60* to Qoro axis-FAULT RELATBD^^"."??*^1 —————————— -moderate amount of sidorito alteration ——————————— : ————— ~

—"3— 55* pyrit**— 60* to cor^ axis ~.\ rt .MOnSRA-TE- .-QUARTZ VSIN SY&Tfl^ (45^) ——————— : ————— — - - - — -5 5JGH-57 '6*-———— cotvta-cts : top-undeterminable ——————————————————————— ' ———— : —

hotte™— 5* to core axis . .* ———— shear^Ufragmented material (4^ —————————————————— -- ———————— ————— -5^ ankerite alteration ————————————————————————————————————

-.1"T*a f* O— ^ 7-it/T*'? ^0

—— ,57'0"-6Q l Q"-sheared chloritic fragpcntod material ———————— 57'6n -60J O11 —

4

SAMPLE NUMBER

B3360B3361

. DOOftOOtfjo4033^3B33fl4B33S5 B3386B33&7B33^oiiiJdDj^&y

o o o ftr\ — OJJ'VO

-

B3392

n-j-iooOJJ7*-

*m^.

tracVA CJV*

trac-Hjraetrac

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EARTH RESOURCE ASSOCIATES: DIAMOND DRILL LOG. PROPERTY:.Puissance PAGE

P-6/8A HOLE NUMBER: 4kFOOTAGE62'3"--

74*2"

74*2"^107*0"

**

107*-170*'

DESCR,PT,ON OF CORE toW-M.*-' - .

BANDED IRON FORfVlATION —— S^\l **poue —— S^hi^e 6?'6"-65 f O"contact.*;: top-55*to core axis 65 t O"^67 t 6"hottom-60*to core axis 67 t 6n*70 l On-magnetite bands-35^ 76 l O"-72 t 6"-siliceous matfirlal-'JnjZ 79*ft"-7*;*n"-ankerite material-5-10^————— -5-10^ sulphidostpyritc/pyrrhotito?) oooociatod with ————— ———————————— magnetite bands and ankerite. — - ——————— — ———— - —— —————————-

TNTERMEnjAT55 VOLCANIC- _ Ankerite __ Chlorite 75 l0lt-^0 l 0fl-Contant.R: t.np.^O* t-.n rO T*** pyig ftntnw.ft^tO"bottom-undeterninable ^5 lO"-90 fOn-green to grey green ~- j . 90 l0t1 -95*0n~fine to niediuni grained ankerite ftrains 95 * Qn *- 100*0"fi oca ll.y chlorite blebs.^dVjO* to coris" axis ioO'0M w305 t OIt-trace amounts of quartz filled amygdnles 105 1 0tf -310 t011-trace pyrite 110*0" -115*0"*

IHTiJUMEDIATE VOLCANIC- — Col cite —— Ankorito —— Chlorite —— - ———— 115*0^-120^0". .... —— contacts-t— top-undeterminable- - .. ...,... 120 I 0"-125 I0"bottom-gradational 125*O"-130*O n-creen colour 130 "-135*0"-fine grained , ISS'O^-HO'O"-lo rally chlor-ihft hi phs apparent, nri pnt.at^ nn.*;n't.ft i;,ntn"-]45 th"core axis " I45 f0"-ll0 l 0"-trace pyrite . 1SO*0".1S?*O"——————————————————————————————————————————————————— 155tQn,16Qto"-———————————————————————————————————————————— I60*0n ^l65'0"———————————————————— : ——————————————————————— 165 ^"-170*0"

SAMPLE iNWtfR

B3394 'B3395B3396B3397R3^Qft

B3399R340053401J&402B34Q3B3404B3405B3406

-T3O 1 r\*3D J W f ——B3/J08B3409B3410B341183^3?B3413B3A14B3W—D341683417

ellA^YSn ni r3

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o 0520^6^t.ra^en.ni^

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.EARTH RESOURCE ASSOCIATES: DIAMOND DRILL LOG. PROPERTY: Puissance HOLE NUMBER: p.6

FOOTAGE170'-267'

"***

•i

267 'O rt -288*6"

DESCRIPTION OF CORE' - ' "

INTERMEDIATE VOLCANIC —— Ankerite —— Pillowed??? 170*0M .17^'p"-gradational contacts 175 '0"-!^^"-fine to medium grained ankerite grains 180 '0". 1^5*0"-trace to 2# chlorite alteration ] 1*5 ip"-! 90*0"-10^ ankerite carbonatization associated with 2S& chloriteblebs- 50^60" to core axis-possibly pillow selvaees???

-trace pyrite-trace-1^ disseminated jpyrite associated with ankerite and chloriteblebs-

-190 t 9n -191 t 5 n -wall rock charaotftrised hy flhunH flnt "hlorit* al- 190 f O"-195 '0"teration-55*to core axis-PAULT RELATSD"155 pyrite

195 t O"-200 l Ofl* - ? 200*dw -205*dn

205'0n -210 l 0n210 'On -215*0"215 ^"-ZZtTO"2ZO*O"-ZZ5 I 0"225*0" 230 '0"230 f On -235 t O"

236'2"-237 lO"-abundant ankerite, soft gouge.FAULT.lO^to core a3cis235'.2LO'0"240 l0n-245 t,0lt245 f On -250'0 1'250 fO"-255 f On255'0"-i!6U*0"260 t o"-265 f OTI

•V

[NTERMEDIATE-KAFIC VOLCANIC —— Calcite —— Chlorite 265 'O 11 - 270*0"-contacts: top-gradational 270 '0" -275 '0"

bottom-65 l'to core axis-FAULT RELATIiD-green colour-fine grained-highly carbonated-2^o ankerite grains

SAMPLE NUMBER i

8^418B3419B3420B3/421

B3422

B3423B3424B3^*25B3*26B3VZ?BjiiZBJ3429

B3430B3431

B3432B3433B3434B343JB3436

B3437B343B

ASSAYSAll W

tracetracetracetrace

trace

0.004tracetracetracetracetracetracetracetracet ra e etracetracetracetrace

;racetrace

;]s

-

m tEARTH RESOURCE ASSOCIATES: DIAMOND DRILL LOG. PROPERTY:, Puissonce

PAGE 4 HOLE NUMBER: P-f "•••••H*-——————— -—————— "M*————

FOOTAGE

287*6".362*6'

*

a

DESCRIPTION OF CORE

-trace pyrite

-278'0"-279'4"-silicified wall rock 275*0"-280'0"-trace feldspar alteration-282'6"-283'0"-quartz7ankerite veln-20"to core axis 280'0"-285'0"- tace pyrite

ANKERITil/QUARTZ ALTERATION ZONE - 285 f O" -287*6"-contacts: top-65* to core axis-FAULT KlSLATiSD 287*6"-290*0"bottom-20'to core axis-FAULT RELATED 290*0" -292* 6"-grey green colour 292*6"-295'0"-medium-coarse grained ankerite grains 295*0-300*0"-slightly carbonated , 300*0" -305*0"-10-15)1 irregular trending quartz/carbonate stringers 305*0"-310*0"-fuchsite alteration associated withbboth contacts 310'0"-315*0"-trace pyrite 315*0"-320*0"32, ,0"-325'0"325 fO"-330'0''

-331'7"-331*10"-Quarta vein-60*to core axis . 330*0" -335'0"-non-mineralized33S*0"-3^0 t O"- 4l'B"-342*4n-wall rock characterized by siderite alteration 340*0"-345*,0"345 1 (j** -3 50*0"354'l-354J 3"-quartzXcarbonate vein-70*to core axis 350*0" -355'0"-trace pyrite/luchsite with both contacts

-354'3"-354'5"-quartz carbonate vein-50* to core axis-trace disseminated pyrite

355'Ott -357'6"357'6"-360'0"

-359'0"-362'6"-abundant fuchsite alteration 360*0" -362*6"-trace pyrite

*

SAMPLE NUMBER

B3439

B3440

B3441B3442-B3443B3444B3445B3446B3447B3448B3449B3450

B3451B3452

B3453B3454B3455B3456

B3457B3458B3459

Bell8^

trac^

trace

tracetracetracetracetracetracetracetracetracetracetracetrace

tracetracetracetrace

tracetracetrace

iys

EARTH RESOURCE ASSOCIATES: DIAMOND DRILL LOG. PROPERTY; PuissancePAGE

HOLE NUMBER: P-

FOOTAGE362'6n -

393 , 9r

. .--' !--:'' . ' ';?l.'.^-.s ?e'.--'-

•-. . ----^ ' . .

.' .vi--'- ; .

;--:

^~ ' r - . '"

~"-f - .393*9"-

LLL.IL*•~-

DESCRIPTION OF CORE•v

INTERMEDIATE VOLCANIC? —— Ankerite-contacts: top-200 to core axis

bottom-gradational-grey to grey green colour-ankerite carbonatization-5^ chlorite/fuchsite blebs-50'to core axis-IJo quartz/carbonate veinlets-40-50* to core axis-trace fuchsl te associated with veinlets-1-25& pyrite associated with fuchsite -

-362 t 6"-370 l Ott -wall rock characterized by abundant fine grained362 l 6n-365 t O"ankerite(95^) - 365'0"-367 I 6"

-25^ fuchsite/chlorite blebs-50*to core axis 367 l 6"-370'0n-3/S fine grained subhedral pyrite-50*to core axis370'0"-372 f 6n372 t 6"-375 I On

375 fO"-380 l On380 t On -385 t O"385 1 0TI -390 f On

ANKERITE/QUARTZ/FUCHSIT15 ALTERATION ZONE 390 f O"-395'0"-contacts: top-gradational

bottom-60'to core axis- FAULT RBLATSD-grey green colour-medium grained ankerite and chlorite grains-slightly carbonated,15-20# quartz and quartz/carbonate stringers-5^ fuchsitevtalteration with veins-trace-2^ pyrite associated with fuchsite

-393 t 9"-400'G"-fuchsite alteration-40"to core axis 395^0" -397 '6"-1-2^ pyrite . 397'6"-400'0"

-402*0"-402 t 8"-fuchsite alteration- 50" to core axis 400 '0" -402' 6"-trace pyrite

SAMPLE NUMBER

B3460B3461B3462B3463B3464B3465B3466B3467

B3468

B3469B347U

B3471

3 el x r

tracetracetracetracetracetracetracetrace

trace

trace1tract

tract

AYS

t

t

EARTH RESOURCE'ASSOCIATES: DIAMOND DRILL LOG. PROPERTY: Puissance HOLE NUMBER: P-6/34

F'OOTAGE

•*-*

ji

DESCRIPTION OF CORE

-404'0-404 l 7 n -fuchsite alteration-50* to core axis 402' 6" -405*0"-23b pyrite associated with fuchsite

405 ' -409' 6"407'6"-410'0n4iO'0 H-4l2'6"4l2'6"-415 f O!l415*0^417*6"

-416 'llfl .419*2". quartz vein-50*to core axis (sub-par llel) 417 f 6n-420 f O"-non-mineralized

-420 *0"-422 "-quartz veining 420*0" -422*6"-Chlorite alteration-possibly FAULT RELATED

422 '6^-425 'O"425'0"-427 l 6n127'6"-430'0"

-430'0n -432 l 0"-fuchsite alteration -; 430 l O"-432 f 6"-1^ pyrite

-433 '0"-433 "-quartz vein-600 to core axis 432'6 tf -435'0"-non-mineralized

,-434 l O"-437 t O"-abundant irregular trending quartz strincers 435 f O"-437'6"

- trace fuchsite-trace-l;{ pyrite -

-437'0"-437'3"-quartz vein-50*to core axis 43?*6n-440 t O"-non-mineralized

11

-439 f C"-442'6"-abundant irregular trending quartz stringers 440'0n -442'6n- 442 f 6" -455 '0"-

SAMPLE NUMBERB3472

B3473B3474'83 475B3476B3477B3478

B3479

B3480B3481B3482B3483

B3484

,

B3485

B3486

B3487 d8348^

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tracetracetracetracetracetrace

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trace0.004trace0.008

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EARTH RESOURCE ASSOCIATES: DIAMOND DRILL LOG. PROPERTY: Puissance

7 HOLE NUMBER: P-6/fiA

FOOTAGE444 '4"-476'0"

**

-

i

DESCRIPTION OF CORE

INTERMEDIATE VOLCANIC-AnlrsH f. R 44*5 '0"-450'0"-contacts: top-600 to core axis-FAULT RELATE 450'0"455'Gn

bottom-undeterminable 455'0"-460'0"-srey sreen to green colour 460 '0" -465*0"-fine grained ankerite grains 465'0" -470 '0"-slightly carbonated 470*0" -475*0"-trace pyrite 475 ! 0n-476'0"

,-

~

'

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2ND OF HOLE AT476 FSST November 17, 19S4

.

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SAMPLE NUMBER

B348933490B3491B3492B3493B3494B3495

*

————

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0.032tracetracetracetracetracetrace

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PAGE '

Earth Resource AssociatesP.O. BOX 2150, TIMMINS. ONTARIO. P4N 7X8 CANADA

DIAMOND DRILL LOG

DRILLING COMPANY TOIANGLii DRILIJN(k)REMAN CORE SIZE BQ CORE STORED AT: Coreshack

PROPERTYHOLE NUMBER P-7/64

GRID REFERENCE 14+20E/0+40STOWNSHIP DELORO CLAIM

AZIMUTH ISO0 DIP ANGLE -

DIP TESTS: 100/43 o ,200/430LOGGED BY Ken Lapierre DATE December l,

1934..FOOTAGE0--12'0"

12'0" —64 '4"

•**

,

DESCRIPTION OF CORE-drill casing

liNlUilMELJlATli-MAFlC VOLCANIC —— Ankerite'/ —— Chlorite 12'0"-15 f On-contacts: top-undeterminable 15'0"-20'0"

bottom-6ooto core axis-fine grained-green colour - - - ,—slightly carbonated-locally chlorite blebs-60o ^o core axis ' '-1^ siderite alteration-2^ quartz/carbonate rilled amygdules-l)t irregular trending quartz/carbonate stringers-1-^yiJ line-medium grained subhedral pyrite

-22'0"-35 f O"-wall rock with apparent orientation-6QO to 20*0"-25'0h .tiVI'fi axis .

-23'2"-23'4"-two cross-cutting quartz veins-45o to core axis-5/0 line grained pyrite associated with both contacts

-26 V-26'y-quartz vein-^u to core axis 25'0"-30 I 0"-1^ pyrite associate with both conlacfcs

-3B'9"-3^*lu"-possible y KAULT-500 to core axis 30'0"-35'0"-chlorite/siderite alteration 35'0"-40'0"

4fc A ^ A A 4

SAMPLE NUMBER

064501G64502

•*

G64503

G64504

G64505064 506

Bf1f

trac^tract

trace

trace

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Vfi

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EARTH RESOURCE ASSOCIATES. DIAMOND DRILL LOG. PROPERTY: PuissancePAG

HOLE NUMBER: P-7/8,

FOOTAGE-

*

64 ? 4"-113*4"

.

*

DESCRIPTION OF CORE

39'0"-59'6"-wa-ll rock characterized by amygdules .ankerite 40 f O"-45 f O"-60O to core axis

-47 1 5"-47 t 7"-FAULT-800 to core axis 45'0"-50'0H-abundant chlorite/siderite alteration

50 1 0lt -55 l 0n-59 f 6"-64 t 4n-wall rock characterized by chlorite blebs-550 to 55 ^"WO"

core axis 60*0n -65 t 0n-59 t 7"-59'8n -quartz veinlet-90o ^o core axis

-1# pyrite associated with Contacts

ANKEKITE/QUARTZ/FUCHSITE ALTERATION ZONE —— Shearingcontacts: top-60O to core axis-FAULT RELATED

bottota-t)0o to core axis-FAULT RELATED-line-medium grained ankerite grains-grey green-emerald green colour '-25-30^ i quartz/carbonate and quartz stringers withapparent orientation-60" to core axis-parallel to shearing

-sheaf ing-600 to core axis-l-3jb fuchsite alteration-trace-l# fine grained pyrite

f64' 4" -99 '3 "-alteration zone characterized oy apparent 65 fO"-67 f 6"SHxiAKlNG-6U0 to core axis 67' o" -70 'O 11————— * ————————————————————— 70 to"-72'6"

y2'6"-75 l O"————————————— ? —— . —————————————————————————— . — 75100,77*6" —

77 f 6"-80'0nBU'U"-8ii l 6"82 1 6"-H5'0"8i)'U"-8V f 6"8V '6" -90 '0"90'0"-92'6"

A m * A m 4

SAMPLE NUMBER!

&4506.5

064507

G64508G64509G64510

•*

G64511G64Sl2064 5 13G6451tfG64515G64516G64517G64i*18064^19064520G64521

ellAfAYS j

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trace

tracetracetrace

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tracetracetrsree"trswtracetracetracetracetracetracetracem

i

-

EARTH RESOURCE ASSOCIATES. DIAMOND DRILL LOG. PROPERTY: Puissance

H pjlHOLE NUMBER: P-?/

FOOTAGE

113 '4" -207*0"

**

'

DESCRIPTION OF CORE

-93*3"-94'4"-FAULT-650 to core axifc 92*6"-95'0"-soft gouge-cataclastic material-CRAIG* S FAULT-probable

-99'3"-113 ! 4n-Alteration Zone characterized by. 95'0"-97 I 6"1) increase in ankerite alteration 97'6"-100 I 0"2) decrease in quartz and quartz/carbonate 100*0" -102*6"

stringers (5#) -irregular trending 102* 6" -105*0"3) no apparent shearing 105*0"-107 I 6"

107 '6" -110*0"100* On - 112* 6"112*6"-115*0"

INTERMEDIATE-MAFIC VOLCANIC —— Calcite —— Ankerite-contacts: top-60o to core axis-FAULT' RELATED

bottom-undetenninable-grey green to green colour '-fine grained-slightly-highly carbonated

. -l-3# quatrz/calcite filled amygdules-trace pyrite -

-Il4 t 4"-114 t 6"-abundant fuchsite-possibly FAULT RELATED 115*0"-120'p"-60O to core axis

-115 t 4"-H6 t O"-abundant fuchsite-possibly FAULT RELATED-60o .to core axis-trace pyrite

-116'0"-l44'C"-abundant ankerite patches 120 t On -125*0"-trace chalcopyrite, pyrite— locally 125*0^130*0"130'0"-135 t O"

SAMPLE NUMBERG64522

G64523064524G64525G64526064527064523064529064530- -.

G64531

*G64532G64533G64534

1=1

o -j AS6

trace

tracetracttracetracetracetracetracetrace

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trace

tracetracetrace

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mPAGE 4

EARTH RESOURCE ASSOCIATES: DIAMOND DRILL LOG. PROPERTY: Puissance HOLE NUMBER: P-

DOTAGE

*

DESCRIPTION OF CORE-135 1 3"-136'3"-BAm)ED IRON FOHMATION —— Siliceous —— Magnetite 135'0"-137'6n

-contacts: top-55o to core axisbottom-fcOw to core axis

-3^ pyrite associated qith quartz/carbonate/volcanic material

137' 6" -140*0"-144 1U"-207'0" -abundant calcite alteration and amygdules 140 f O"-l45*0"

-trace pyrite 145 fO^-150 f OfF 150 l O"-155'OnQ64lfrtiraCe 1J5'0"-160'0"U04^u ifftct i6o'0"rl65'0"

165 '0" -170 '0"170 '0" -175 '0"175*0" -180*0"180*0" -185*0"

i 185*0^190*0"190'0"-195 I 0"SKD OF HOLE AT 20? FRBT I^r^h^ l 19^ 1 195*0" -20080"

' 200*0"-205*0". 205*0"-207'0"

r*

,

J

/y \^/Cjtffwwzesjtju?

SAMPLE NUMBERG64535

G64536G64537G64539G645,^0064541G6454*G64543G6454.HG64545064*546G64547G64546G6454?G64550

BeW.Strace

tractracetracetracetracetracetracetracetracetracetracetracetracetrac*

,

j

Earth Resource AssociatesP.O. BOX 2150. TIMMINS. ONTARIO. P4N 7X8 CANADA

DIAMOND DRILL LOG

DRILLING COMPANY Triangle Drilling FOREMAN CORE SIZE BQ CORE STORED AT: Coreshack

PAGEPROPERTY PUISSANCE

HOLE NUMBER P-8/84 GRID REFERENCE 14---20E/2+20S

TOWNSHIP DELORO CLAIM ME29 AZIMUTH O.0 DIP ANGLE -450

DIP TESTS: LOGGED BY Ken Lapierre DATE December 2.1984

.FOOTAGE0'-7'0"

7'0"-92 '9"

^*

92 '9"-163'0"

DESCRIPTION OF CORE

-drill casinq

INTERMEDIATE-MAFIC VOLCANIC — Calcite 7'0"-10'0"-contacts: top-undeterminable 10'0M-15'011

bottom-250 to core axis-poosiblv FAULT RELATED 15 l O"-20 l O il-fine arained - ?0'0M-25'0 M-green colour * - ' 25'0M-30'0"-abundant alcite alteration 30*0^35^0"-1-2X chlorite? blebs 35 rO M -40 l O M-trace-tt quartz/calcite fillpri amygdule* 40'0lt-45'0"-trace pyrite " 45'0"-50 I 0 11

50 I 0"-55 I 0 11-55 l O tt -55 1 2M-quart7 vPin-4ri" to rnre ^^ 55'0"-fi0'0-

-non-mineralized gQ'O^-fii'O"65'0"-70 I 01'

-73'0"-75 l O u-abundant ground-possibly FAULT RELATED 7n*0*-7*:'nM7*i'0 M -ftn | n 11

80'0M-85'0"

,

INTERMEDIATE-MAFIC VOLCANIC— Ankpri to Qn'nH -95'0"contacts: top-250 to core axis-possibly FAULT RELATED 95 I 0"-100'0"

hot.t.om-?0e to core axis 100'0 M-105'0 1-fin*1 nrain^d ankerite carbonatl7atJon at inrrpatlna HHrtth*: inK*Oll -110 l O l-trace pyrite r 110 I 0 II -115 I 0 I

115'0"-120 I 0 I120'0 M-125'0 (

SAMPLE NUMBER

664551664552664553684554664555664556664557664558664559664560

GK456?664563

G645656154566GfidSfi?

GB4568664565G645 70664571664572664573G64574

Belt5?

tracetracetracetracetracetrace0.016tracetracetracetracetrarptracetracetraretracetrace

tracetrace..tracetracetracetrace0.002

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EARTH RESOURCE ASSOCIATES: DIAMOND DRILL LOG. PROPERTY: Puissance HOLE NUMBER: P-8/^

FOOTAGE

163'0"--173'0"-

173'0"--232 'b"

DESCRIPTION OF CORE

-125 I 0"-125'8"-8ANDEO IRON FORMATION — Si'liceous — Sulphide 125'0"-130'0"-wall rock characterized by abundant magnetite stringers and bands-contacts-30" to core axis: top

-10* to core axisrbottom-SI s iliceous material-20* magnetite-21 pyrite associated with magnetite 130'0M-135'0M

-129 l 8"-l3l'0"-quartz vein-200 to core axisISS'O-.-UO 1 !) 11140 lt)"-145 l OM1 45 '0M- 150*0"150'0M-155'0"155'0"-1Gfi'0"

,BANDED IRON FORMATION— -Siliceous — Sulohide " f 160'0"-165'0"

-contacts: top-200 to core axis 165'0"-170'0"bottom-300 to core axis 170I 0M-175'011

r70* siliceous material-ID-15% magnetite bands and stringers .;-dull green alteration within siliceous material-2-3X sulphides associated with magnetite

INibRMtDlATED-MAFIC VOLCANIC — Ankerite 175'0M-180'0M-contacts: top-300 to core axis 180 I0"-185 1 0"

bottom-200 to core axis ISS^^-^D'O"-fine-medium grained chlorite blebs? associated with ankerite 190*0M-195'0"altered areas 195 I 0"-200'0H

-grey green-green colour 200 I 0"-205 I 0"-H amygdules partially infilled wit.h pyrite 205'0U-210'0"-trace pyrite 210'0M -215'0"

215 I 0"-220'0"-2ifU 1 u i'-22ruH -quartz strInger-160 to core axis 220 "O" -225' O14

-trace tourmaline-abundant ankerite alteration proximal to stringer

SAMPLE NUMBER

GG4575

G64576

G64577G64578G64579G64580G64581

G64582G64583G64584

^ l ^ ASSAYS 3elFw.trace

trace

tracetracetracetracet rae*

tracetracetrace

G64585 traceG64586 paceG64587 traceG64588 traceG64589 traceG64590G64541G64592G64593G64594

:raceirace,race;race;race

EARTH RESOURCE'ASSOCIATES: DIAMOND DRILL LOG. PROPERTY; Puissance HOLE NUMBER:FOOTAGE

232'6"--30G 0

**

DESCRIPTION OF CORE '

—————————————————————————————————————————————————— 230'0"-232'6"AHKERITE/QUARTZ/FUCHSITE ZONE ————————————————————————————————— 232'6"-235'U"—————— -contacts: top-200 to core axis-FAULT RELATED —— : —————————————————————— —— — —— — —— bottom-200 to core axis*FAULT RELATED ——————————————————————————— IQ-15% quartz veins and striyers ——————— — — — ————————————————— ;————— St fuchsite alteration ———————— —— - —— — —————————————— ——— ——————— fine-medium grained ankerite grains ——————— : ————————————————————————— numerous faults ————— ——————— ———— —— ———————————————————————— -trACC pyrite — : ——————————— ; —————————————————————————————

-2'32'6 M -234'8" -abundant fuchsite alteration ——————————————————————— — - ———————————— 2t disseminated pyrite ———— ———— ———— - —— ————————————— -

- 232 '0H"232' 11 "-quartz veiu-400 tu core axis —————————————————————————————— —————— -trace tourmaline —————————— r-j —————————— -— ———————————

py i...

-232Mr-233'3"-10t quartz patches ————————————————————————————— : ————————————— — M, chalcopyrite —————————————————————— ————————————————————— U pyrite ————————————————————————— : —— - ——————— ' —————————— -trACC tourmaline ——— ' ———— - — —————————— - ——————————————

-234'7M -234'8''-quanz vcin-600 to core axis ———————————————— ; ———————————————————— -trace torma line/anker i te ———————————— — —————————— ; ——— ?r—

-tfdcs pyrite .-second quartz vein cross-cutting above quartz vein-200

———————— to core axis'-fuchsite associated willi second vein's contacts —————————COD 0 -to/ 0-230'10 t'-239'0"-quartz vein-600 to cure~axts ———————————————————— 237 '6*^240*0**

—————————————————————————————— : —————————————————— 240 '0 M - 242' 6"^^uartz^ve^n^jy^^to^core axis ^— t-^a^o nv/cit-Q- -Vrl tlt,C yyj-l-WS ———————————————————————————————————————————————————— ——————————————————————————————————————————————————————

*

SAMPLE NUMBERbb^ybG64596G64597

.

1

664598G64599

-664600--664604—

—— ———— . ggj^S^AYStracetraceU.042

-

&.OOGtrace

3.002

i

EARTH RESOURCE ASSOCIATES: DIAMOND DRILL LOG. PROPERTY:.-'uissance

4

HOLE NUMBER:

FOOTAGE

**

DESCRIPTION OF CORE ' -?44' l"-244'3u -Qtiartz vein 75 0 to core a y i"

-non-mineralized .. _ '. , ...,..—. , ,... ,. ... . . .

-?44 l 5"-?44'Rli -quartz vein-400 to core axis-non-mineralized

-?46'2 u-2^6 l 3 u -quartz vein-550 to core axis - 245*0 M 247'6**-21 tourmaline/fuchsite flU**r^tion-non-mi nera I i zed

-?dfi' iO"-947' 1 "-quartz/carbonate veln-300 to core axis-21 tormaline alt.prstlnn --non-mineralized '

— ?4.7'ftM — 247' 1 1 M -ouart2 vein-600 to cors axis ojmcn ocninn^f j v|*^ . -— - ^... ww — m w . v w****- i*f/ O o^U U

-non-mi nerall 7Prt* ' 250 I 0"-252 I 6"

-?53 l O M -?5? l 3''-quartz vein-500 to core axis 252 'S'^SS'O1'-non-rninerali?eri '

-254'6u-?54 l 11 u-qiiart7 vpfn-fiO0 tn Cnrp?xl?

———————— -non-mineralized (1 spec of chalcopyrite) —————— ——— ——————— ———

-255 l 1"-255'4 M -quart.7 vpin-750 to rnre axis 255 * Q"-2ST*"-trace tourmaline crystals-non -mineral i zed '~' '

.?Rfi'n"-?t;fi'?"-q, ! ARtT Vpin-7no t" c^re axis—. -^51 ankerite-alteration

V ' '

-?^7'4"-?fift l ?"-rrrK:c:-ri!tting qnart7 v^fnt 257*6 '-260*0 '-trs-P t.nnnnalinp ^It.prfltinn

V

SAMPLE NUMBER

G6460?

G646fV*WTUWW

664604G64605

G64606

G 646Q7

BellsBAYS

0.004

trace

tracetrace

O fkfl9 ^-UUt-

trace

iEARTH RESOURCE ASSOCIATES: DIAMOND DRILL LOG. PROPERTY: Puissance HOLE NUMBER: P-3/.

FOOTAGE

"~-*

DESCRIPTION OF CORE-zbd'-r-zbb'tr-anKerite/tourmaiine stringer-30" to core axis

-c-3 l 6 u-258 l y"-quartz vein-50* to core axis-b* tourmaline alteration-non-mineralized

-Zb9 1 4"-259'5"-quartz velnlet-500 to core axis-non-mineral i zed 260 l O"-262'6"

262 I 6"-265 I 0!1-2ob'u t'-ifbi: 4 b"-i-AULi-i!)v to core axis - 265'0"-267'6"

-CRAIG 1 S FAULT(probable) .-abundant ground-caving or hole (cemented)

-267 l 10 u-266 l 8u-quartz7carbonate vein-unoeterminabie contacts Z67'b"-Z70 I0"-2j tourmaHne alteration - i .-trace pyrite

; ' ' . r

-ij/i'i-.ij/z'b'-quartz vein-20" to core axis 270'0"-272 I 6"2X tourmaline patches .,... ...-.— .,.-zi pyrite proximal to contacts .

272'6"-275 l Ou' — . ———— 275^ ow.-27r^-Z7y*b"-ifBU'U"

————————————————————————————————————————————————— 280'.0M-282:t 6^-282'6 M -2yi l 2 ll-highIy chloritized wall rock-possibly PAUL! RELAIkl) 2B2 l 6 u -2bb'0 11

-bottom contact-soft gouge 285 1 0"-2U7 I 6"287'6M-2SO'0U

-29r4"-292'0"-quartz v^in-undeterminable Contacts 29U l O l'-292'b"-non-mineralized

-2yi'4 u -306'0"-wan rock characterized by apparent SHEARING-100 to core axis-151 quartz stringers parallel to snearing-iuv to core axis

#

SAMPLE NUMBER

G64608G64609G64610

bb4b11

G64612

G64613G64614664615G 64616G64617G64618GC 4619664620

Bel ^AYS

trace0.006trace

U.04Z-

0.006

tracetracetracetrace0.002tracetracetrace

EARTH RESOURCE ASSOCIATES: DIAMOND DRILL LOG. PROPERTY: PuissancePAG

HOLE NUMBER: P-8/

FOOTAGE

306 '0" ——457 '0"

i

DESCRIPTION OF CORE '

-234 4 -295 0 -quai tz vein-Sir to core axis 292 I 6"-295M-dnktifitt: alteration

———————— -non-fl::neralized ————————————————————————————— —— ————— —

-295'6 -295'10"-quan:z vein-unaetermlnable contacts 295'0"-297 l fi'4- -aj- j, r u -iM C.JJ W CJ/ U. -t.i oue pjri i te

-c9G 0 -3G6'0"-abundant quanz vein material -apparent orientation parallel 297'6M-300'0 Ito shearing— 10-20* to core axis 300 I 0I4-302'6I

-tra^e-U pyrite , 302'6"-305 I 0 I-trace chalcopyrite 3054 0M -310*0*

*

INTERHCDIATC-HAFIC VOLCANIC — Ankerite — Chlorite —————————————————— 310'0l'-315 t 0 t-contacts: top-200 to core axis-FAULT RELATED 315'0--320'o-

uuLiuin-unGeierminaDie ~ ( - 320 I 0 M-325'01'-finfi-mediuffl y f dined ankerite grains 325 I 0 M-330'0M-grey green tu green colour " -- """3^rO n-335*0'lii

——— -abundant chlorite stringer s* 10-20" to cui-e axis ——————————————— 33b'U*-340'0 '——— abundant ankerite -patches ———— - —————————— : —————— — —— 34{jio".345'oil——— .trace pyrite ——————————————— ————————— ——— — ————————— ————— trace amygdules —— ; ——————————— : —— —————— '- ——— ——————————————

• 334'4"-352'0H -highly siliciried-diikerite-talc-sheafed z6ne —————————— -34b'Uu-350'0—————————— FAULT REUTffl ————————————————————————————————— 350*0 M-3bb"U*

iJ*J\f - U O33 U'————————— contacts; top-100 to core axis —————————— : ———————————————— —————————————— bottotn-108 to core axis ————————————————————————————————— 5l4dteftsiides coiiiiion ——————— : ————————————— —— ———————— : ————————— -ti^ace-pyrite-^ ———————— ——————————————————————————

35b*0H -350'0"360 I 0"-365'0"365 i 0 u -370'0 u370 I 0"-375 I 0"375'0 M -380'0"380 I 0 U-365'0"385 l O"-390 t O"

SAMPLE NUMBER

" G64622

G64622

664623G64624G64625G64626

G64627664628G64629G64S30G64531bb4?3Z

G64633

1 ti64634tib4b3b

-

G64636G64637G64638G64639G646406^4641G.*b4642

Bel ASSAYS

trace

0.014

tracetracetracetrace

tracetracetracetrace0.030trace0.026

tracetrace

0.012O.Oubtrace0.024U.UU4tracetrace

9 0EARTH RESOURCE ASSOCIATES: DIAMOND DRILL LOG. PROPERTY: ,. Puissance

PAG? HOLE NUMBER: P-8J

FOOTAGE

t

**

-

DESCRIPTION OF CORE' 3yu'u"-3y5'U"——————————————————————————————————————————— 395 'Q ".400 "Q"

———————————————————————————————————————————————— 400'0"-405 I 0*—————————————————————————————— ; ————————————————— 405'0"-410'0"————————————————————————————————————————————————— 410'0M-415'0" ————————————————————————————————————— ———————————— 415iO"-420'0"-fl24'4"-424'7"-quartz voin-30p to core axis ————— ——— - ———— —— ——— 420 I OM25'0"

———————— H pyrite associated with contacts ———— - —— - — — — ———— ——— ——————————————— . ——————————————————————————————— 425'0"^430 I 0"'

-^33 l O M -433 M "-quartz voln-75* to core axis ———————————————— : ——— 430'0 M-435 I 0B— : ——————— trace pyrite associated with contacts ———————————————— : ————————————————————————— : ———————————————————— —————— — ——— ————— 4^5 t O'***AAQ l Qu•1^3 V "frU v———————————————————————————— ——————————————— - ————— 440'0*-445'0 1'

• 447' 0^-447 *8*-quartg-yein"200 to core axis —————————————————— 445*0^450 '0*———————— -3X fuchsite alteration —————————— ——————————— 450'0"-455'0"— — —————— trace pyrite — : ————————— . J . ——————— : — : —————————

-450'0*'-850'3l'-quartz vein-?400 to core axis —— ———————————————— r — 455*0 M-457*0*———————— -U pyrite associated with hanging wAll contact ————————————————

-452*4*-452'7"-quartz vein-Ze^-to core axis ——————————————————————— - —— ———————— -iJC-pyr4te associated with both contacts ————————————————————

^5jl*0M-453^g-wal4 rock characterized by abundant calcite/chlorite alteratiopn ——— ———,*.

- . -.•V '

t

———————— END-Of-WOtE-AT457-FESF ——————— DECEMBER 2, 1904. ————————————————

———————————————————— 7 ^ —— : —nKt?^ n'^&totAJ?—————————————————————————————————————— , f^4#7x {y \sja^^-'*'v ——

SAMPLE NUMBER654543Gfi46dAUWHO*f *f

G6A64SuUtUHv

G64646G64647-^64648-664649

RfiAfifiO —WVHvvV

G04051

fi6465g —QU*tv^lfc r*etcc9Go4o53 —G64654

-6f4tS5-

G64656

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"trace-"trace-

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trace

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'

Earth Rbsource -AssociatesP.O. BOX 2150. TIMMINS. ONTARIO. P4N 7X8 CANADA

DIAMOND DRILL LOG

DRILLING COMPANY Trian9 le Drilling FOREMAN

CORE SIZE BQ . CORE STORED AT: Coreshack

PAGEPROPERTY PUISSANCE

' . HOLE NUMBER P-9/84 GRID REFERENCE 38+20E/U20N

TOWNSHIP DELORO CLAIM ME 21 AZIMUTH 315 0 DIP ANGLE -45 0

DIP TESTS: 100V-450 f 200V-45 0 ,300V-450 ,400'X-430 , LOGGED BY Ken Lapieppe DATE Oec.9,198/"450

FOOTAGE 'O'*12'0"^

1 9 ' n "le U --89*3* —

***

. OQI*SH ———03 o --HH^ 0

DESCRIPTION OF CORE-uj ill ua^liiy

•v

INTCRMCOIATE^MAFIC VOLCANIC — Ankerite —————————————————————————— 12 l Ou-l6 i O" ~~--uiiUyLennliiable contacts ^S t Qu-tQ*Qu-yrey green to green colour 20 I 0I*-25'011-fine-medium grained anicerite grains ES'O^-SO'O"-13* dnktrite bLrii'yers— 300 to core axis ~ ' 30*0*-35 I 0U-appareat shearing— locally — 25* to core axis ' SS'OMO'O"-trace-1X pyrtte 40'0"-45 I 0"

, ' AS'O^SO'O"SO'O^SS'O11BS^-'-eD'O 11eo'o^es'o"

^iriM ^ iiu SS'O^O'O"-70 0 -70 4 -abunddiiL futhslte-possibly FAULT HELAltu 70 I0"-75 I 0"

-77 l Ou-79 l u"-wall rocK cnaracterized by fragmented appearance 75 I 0"-80'0M80 l O tt-85'0"

ANKERITE/QUARTZ/i-uUHSllfc ALltKATION ZONE 85'0 II -90 I 0"-contacts: top- 15* to core axis—l-AULT RELATED

bottom- 15C to core axis—FAuuT KtLATED-ftiedium grained ankerite grains-yrey green colour-IG-15% irregular trending quartz and quartz/carbonate stringers-trace fuchsite alteration-trace pyrite .

SAMPLE NUMBER

G64657G64658G64659G64660G64661G64662G64663G64664G64665G64666G64667G64668G64669

G64670G64671

G64672

8el!SS

tracetracetracetracetracetracetracetracetracetracetracetracetrace

tracetrace

trace

AYS*

S

——— j

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EARTH RESOURCE ASSOCIATES: DIAMOND DRILL LOG. PROPERTY: - Puissance

*HOLE NUMBER

FOOTAGE

**

,

DESCRIPTION OF CORE-yjV-yd 'li "-quartz vein-duu to core axis 90'0M -95'0"

-non-mineralized95'0"-100'0"100*0"-^^"

IID'ir-llb'O"-115 l O"-118 l O u-FAuLT-unaeterflUnabie contacts 115'0"-120'0"

-abundant cnlorite/serpentine-taic alteration

9420 l O"-122 l O H -wall rock characterized by 2X disseminated pyrite 'IM'O^IZS'O"t- 122^-1 22 ' 2"-quartz vein-850 to core axis

-non-mineralized

-124 l 4u-ii'5 l u'I-i-AUU--i5v to core axis } - . izs'O^lSO'O"-abundant "ground

130 I 0U-135'01'135'0M-140 I 0M

-144'10 ll-145 l 5tt-abundant sericite alteration 140'0"-145'0"

-14B'5"-147 "-abundant sericite alteration 145 I 0"-150 I 011-148'2 l( -l48 l 6"-quartz vein-8b0 to core axis

-non-mineralized150'0"-155'6"iSS'o^iso'o11160 'O"- 165*0"

-167'4M-167'8"-quartz vein-906 to core axis ISS'O^-^O'O"-non-mineralized^172*tr^1 94*2*^STRONG-QDA1?TZ VEIN SYSTEM(75T6) —————————————————————————————

-172'0"-172'4 ll-quartz vein-750 to core axis WOM-172'6"-non-mineral i zed172 l 6M-i;b'U 11

SAMPLE NUMBERG64673

G64674G64675G64676G646/7G64678

G6467S

G64680

G64681G64682G64683

G64684

G64685G646S6G64686G64688

G64689

G54690

Beli^trace

tracetracetraceu.uuztrace

trace

trace

tracetracetrace

0.002

tractracetracetrace

trace

trace

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EARTH RESOURCE'ASSOCIATES: DIAMOND DRILL LOG. PROPERTY: Puissance HOLE NUMBER: P-9/

FOOTAGE

•^*

'

i

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DESCRIPTION OF CORE

-I76 i sr-l78 1 5"-quartz vein-250 to core axis 175 I 0 M-177'6 M-trace chlorite alteration-trace tourmaline-trace pyrite

-ixy'5"-i7y'7"-quartz veln-650 to core axis 177 I 6"-180 I 0Mnon-mineralized

-I8i i 8"-ib8'4 t' -quartz veln-100 to core axis 180 I0"-182 I 6"-10* volcanic material . 182'6M-185 I 0"-W, tourmaline(patches ^crystals) 185'0II-187 I 6"-10* ankerite alteration 187'6 M-t90 l 011-trace rucnsite-trace pyrite-

-iyri"-l9l l 5"-quattz vein— 80" to core axis - f 1 90 I 0 U-192'6 U-non-mineralized

: ' f

-iyrbM-iyw-quartz vein— 800 to core axis-non-mineralizeo

-192'0II-192'1"-quartz vein— 80* to core axis .- . ... ...,...-non-mineral ired

-i c. a ~ \-yc. o -qua i ti veiniet— ou 10 core axis 192 o -195 UT-trace tourmaline-non-mineralized

W im'IAJtllli---* i nr~ n * * *j * **,l O-194'2"-quarLz vein— -85" to core AXIS " -- non-mineralized

-196 l 7"-iy; l b"-tuchsite alteration-FAULI— 30" to core axis IQS'O"-^?^ 14197'6 U -200'0"200'0"-205 I 0 M205'0M -210 I 0"aio'O^is'O"

SAMPLE NUMBERG64691

G64692

G64693654694G64695G64696

G64697

'

Ub4bytJ

G64699G64700G64701G64702G54703

Belff.AYS ^trace

trace

tracetracetracetrace

trace

trace

tracetracetracetracetrace

——i

EARTH RESOURCE ASSOCIATES: DIAMOND DRILL LOG. PROPERTY: Puissance HOLE NUMBER: P-9/84

FOOTAGE

^*

j

j

i

DESCRIPTION OF CORE215 I 0"-220'0"220'0 M -225'0 M225'0"-230 I 0"230'0"-235 1 0"

-^jy o -tay / -quartz vein~^sw to core axis 235 I 0"-240'0"-.tracfi lucliilLt:-non -ml nerd 1 imd

^dlT" "jllf?" Ana --t f L 14 * -ina x -i — — —— —-t^j j -c^j i - tjUdi Li/diikerite vein~7u to core axis 240 0 245'0"-iVjji-Tnlnerallzed

,-245'2"-245 l 65-quartz vein~4bw to core axis 245'0M-250 I 011

-4X touriiicil i ne-ilun-rnineraHzed

-252*10 -253'IO"-quartz -veinlet--16* to core axis -' 250 'O"-?^^ 1 o"tr*rn fttr+rirt 1 n/ li 14- *-**-J v-iri auc i uunb j Ltj/siaerne

-ti dCe pyrite . .

•254'r-255'0^quartzyankerite7ruchsileXtuurgialin.H veln-350 to C6re axis ———————————-ti 6C6 pjrrlLt;

255 'O11 -260 '0"-261'0"-202'0"-wall ro^ck characterized by SHEARED appea^nce-bU" to core axis 260 '0" -265*0"

-quartz/carbonate sLrlnyecs oriented parallel to Shearing 265 I 0"-2XO I 0 M-fuchsite alteration associated with both Contacts ' —— 270'D"-275 I-0"-yTuund present 275 'O11 -280*0*-trace pyrite 280*0"-285'0"

285 I 0"-290'0"290'0I4 -295 I 0"295'0H-300 I 0 U

-S^S^S^-SOS 40^uart/ vbin— 80" to cure axis —————————————————— 300'0 U-305'0"-non-mineral i zed - -

305'0M-310 I 0 11-3HJ4"-311'5'l-quai-t^-veiit"ey^-to core dxis —————————————————————— 310*U"-31i) l U''

-non-mineralized*

SAMPLE NUMBERG64704G64705G64706G54707664708

G64709

G64710

G64711

G64712G64713664714G74715G64716G64717G64718G64719G64720G64721

G64722Ub4Xk!3

8elfl?YS

tracetracetracetracetrace

0.020

trace

trace

tracetracetracetracetracetracetracetracetracetrace

tracetrace

-

EARTH RESOURCE ASSOCIATES: DIAMOND DRILL LOG. PROPERTY: , Puissance HOLE NUMBER:

FOOTAGE

'

i

DESCRIPTION OF CORE ' .-315 4 -316 G -qudi Lz veln--90 0 to core axis 315'0"-320'0"

-flon-ftilit6i'udl ized

-324'0"-324'9"-slderite alteration associated with quartz vein--856 to core 320 't)11 -325 'O11dXlS

e.u y -act \ -qiiai \,t vein — oo to core axis 325 0 -330 0-trace tourmaline crystals—trace pyrite

-331 '4 -33t'8M -quartzXankerite veln--30fr to core axis 330*0"335'0"———————— *non-rolneralized ————————————————————— —————————————335'0 II-340 I 0"

-340'2"-340 I8"-siderite alteration associated with quartz ve!n-800 to core axis340'0u-345'0"34b 4 U"-350'0"

' 350 '0"^^^".OCCIQ* ^crriiiii n MJi rf T i , at n flna i-n r^njia. i u4.. - - - -- j. i L.-J33 a -J33 li -quanz vein— ou w Core axis 3SS t) -360*0"-siderite alteration associated with both contacts

-359'7"-3GO l O"-qudrU vein— 20" to core axis ——————————————————————— ~ —————————— -trace tourmaline ———— ———— : ————— — —————— —————————————————— -non iiilneralized ———————— - —————————————————————————

seo'o^es'o"3bb'0"-370'0"-370'0H -370 l 9''-quartz-yelnlet-20n to cure axis ——————————————————— 3yU'U"-3;bjt O"

trace tourmaline present———————— -non-mineralized ————————————————————————————————— ; —

•^37e*tt4t^37t4tl "-quartz vein-irreQUlartrending-21 tourmaline patches t stringers

-377'0 H -383 l O"-abufidarit chlorite alteration - — - —————————— 375'0M-380'U"

384 '^i'-382-l JMrre9ular-tremtfng quartz veiir ———— ———————————————— 380 t O"-385'0" ———————— -3t tourmaline alteration ———— —————— — ———————————————————————————— -non-mineral i zed —————————————————— ? —————————————————

SAMPLE NUMBERG64724

G64725

G64726

G64727

G64728G64729664730664/31664732

G64733G64733G64735

G64/36

G64737

Belf^YS

trace

trace

trace

trace

tracetracetracetracetrace

tracetracetrace

trace

trace]

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PAP- RJ- .

EARTH RESOURCE ASSOCIATES: DIAMOND DRILL LOG. PROPERTY: Puissance9

HOLE NUMBER: P-9/84

FOOTAGE

-,

442*0"-— 517'0"

DESCRIPTION OF CORE385'0 U-390'0 U390 I 0"-395 I U 11

-395'4 -396' 1 "-quartz vein-2D 0 to core axis 395*0"-4CO I 0 R-non-mineralized

-395 l iO"-3y5'11 w -quartz vein— 90" to core axis-non-mineralized

-402 'Ou-402 "-quartz vei-n-20* to core axis 400 I 0M~405'011-trace rucnsite associated with both contacts-trace pyrite .

405'0"-410'0"410 I 0"-41J) I 0"

-419'0 l -420 l 0u-irregular tredlng quartz stringers 415'0M-420 I 0U-trace fuchsite-trace pyrite J

42u'u"-42b'U*4Zb',U--43U*U-430 I 0 M-435 I 0 I*

-43G 8 -437 2 -tjuoi lz veln~20 to core axis 43b*0"-4iJ7'b"-fUCIlS! Lfc/tuuriiial lne olterstlon

-439'0"-442'0"-abundant fuchsite alteratldn-FAULI KhLAIED 437'6U-440 I 0U-1-2X fine grained disseminated pyrite 440'0"-442'6"

- : -

INTERMEDIATE-MAFIC VOLCANIC — Anicerite 442 I 6 I4-445'011-contacts: top-150 Lo core axls-FAULTREtATEO ""

bultom-ufidetennlnable-fine-medium grained ankerite grains-gQfiy cirteri to green colour-lrdce-1I ilisseinlnnated pyrite -••— - — " "-trace chalcopyrite

-•446*yt^446'6"-quai*tz veinlet--?50 to core "axis ——————————————————— 445*0" •447*6"..,.!.v.. w. . *.~^ f

SAMPLE NUMBERG64738Iib4739G64740

G64741

G64742654/43G64744

- ,9

(ib474bGb4746(a64?47664748

*

G64749G64750

G64750

f* f A~1C*}G64752

BelT5^0.002tracetrace

0.014

tracetracetrace

- -tracetracetracetrace

tracetrace

trace

trace-

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" * PAG~7EARTH RESOURCE ASSOCIATES: DIAMOND DRILL LOG. PROPERTY: P-uissance HOLE NUMBER:

FOOTAGE

•^•^

];

DESCRIPTION OF CORE

-447 '; "-448 '^-quartz vein— 2ir to core axis 447 I 6 M-450'0 I-10* cnlorite/anserite alteration

-448' 7 u -449 "-ground— possibly FAULT KtLAitu

-449 '7"-451 M "-quartz vein— zir to core axis 450 lO"-452'6 y-non-mineral i zed

45Z'6U-455 I 0"-455 'O'^SSi1 1 "-quartz vein— w to core axis ASS'ff'-^STV1

-orecciated appearance— volcanic raaterlal-5X fuchsite alteration-trace pyrite

Asy'e^GO'o"-462 l 3"-462 l6"-quartz veinlet — 2u* to core axis 460'0"-465I 0"

"ankerite alteration associated with both contacts-trace pyr-ite

-464'2 M-464'10"-quartz vein— 200 td Co^6 axis-noiHninerdllztKJ —- —— -

465 l Ou-4Xu l U M——————————————————————————————————————————————— 470 I 0"-475'0 *

-479'4"-480 l O"-quartz vein—H)0 to core axis 475 l O M-4fiO I 0 11-10X chlorite alteration-31 pyi ILe dbsuCiated with buUi tOnLo^ts-Iracy clidkupyrile

480'0"-485'0"4Bb l U"-490 lO u

-490 1 2"-490MO u -quart2 vein— 15" to core axis AgO'O'^S'O"-trace pyrite

^S^^gw^FAttLT-IS0 tocore axis ————————— ! ————————————————————-abundant serpentine-talc/chlorite alteration

495 1 0 M-500'0"———————————————————————————— — — ——— — ———————— tinn'ftu-snti l n" — 'vuu u *j\jy v

SAMPLE NUMBERG54753

G64754

G64755G64756

664757G64758-*

bb47ijy665760^664761

G64762G64763G64764

G64765-^64766-

BelfSStrace

trace

tracetrace

tracetrace

tracetree etrace

tracetracetrace

trace-^trace

AYS*

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EARTH RESOURCE ASSOCIATES: DIAMOND DRILL LOG. PROPERTY: pu i ssance HOLE NUMBER:

FOOTAGE

*^

4

i

DESCRIPTION OF CORE

-507 l O"-507'3"-quart2 vein— 450 to core 'axis 505 I 0"-51Q'0"-trace tourmaline alteration-trace pyrite

-509'6 l'-509 l 7 ll -quartz stringer--500 to core^xis-3X pyrite associated with both contacts

510 l O"-R15 l n M515"0 M-517'0"

r

.*

-f - ' *

; ^

END OF HOLE AT 517 FEET DArwaher 9, 1Qftd

X /7/^J^ \LS

(-ifatyJfazse^A/?7

*

SAMPLE NUMBER

G64767

Gfid768G64769

-* 1

ASS Bell 1

— tfaen

trdC^traci

-

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PAGE0Earth Resource . AssociatesP.O. BOX 2150, TIMMINS. ONTARIO. P4N'7-X8 CANADA

DIAMOND DRILL LOG

DRILLING COMPANY Triangle Drilling FOREMAN CORE SIZE BQ CORE STORED AT: Coreshack

PROPERTY PUISSANCEHOLE NUN'BER P-10/84

GRID REFERENCE 36+23E/2+80NTOWNSHIP DELORO CLAIM ME 21

AZIK'JTH 1 30 0 D IP ANGLE .450

DIP TESTS: 100'7-450 ,200V-450 ,360V-450LOGGED BY Ken Lapierre DATE December 1 1, 1 984

FOOTAGEO-10'O"

10'0"—21'1"

21MV-25'8"

25'8"--58 '4"

DESCRIPTION OF CORE-drill casing

- .t *

INTERMEDIATE-MAFIC VOLCANIC — Ankerite-contacts: too-undeterminable

bottom-550 to core axis-medium grained ankerite grains-general lv oriented 550 to core axis-greyjjreen colour" '-trace pyrite

f

-10'0"-12 I Ol'-mInor amounts(15*) of siliceous fraamented material 10'0"-15'0"IS'O^O'O11

; ' ..IRON FORMATION — Magnetite — Non-banded ^n'o'-^^'O"-contacts: top-550 to core axis

bottom-500to core axis-both contacts characterized bv siliceous material T 51 pyrite/pyrrhotite mineral ization and trace amounts of chalcopyrite-95X massive magnetite

-Iron Formation characterized by an apparent "layering" appparance-500 to core axis

ACID FRAGMENTAL — Pyroclastic 25 I 0"-30 I 0"-contacts; top-500to core axis 3n | 0 M-^ I 0 1'hottom-5no tn rnpp ?vj?

-70S siliceous fraamented material— subrounded appearance withpreferred orientation — 500 to core axis

SAMPLE NUMBER

••*

G6477Q.664771

664772

RR47731 664774

ASSAYS Bell Wf

"

tracetrace*f*-k/*^

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* ^PAGE 2

EARTH RESOURCE ASSOCIATES: DIAMOND DRILL LOG. PROPERTY: ' Puissance HOLE NUMBER:

FOOTAGE

V y^'^S .-.

::V,-V vi'-" .'

; '.'? ; '' " : ".•s"; - ;- '

- . - , - - :

-SB9 **--143 '9"

•;*b '..y:-- ". -*..* . ' ';-- " -

-' *"' .. ' ; '

"" v ; ' s

-. -..,

DESCRIPTION OF CORE4

-tine grained fragments grade into coarser grained fragmentsat increasing depths

-fine grained chloritic matrix— slightly caroonated-1-5X pyrite/pyrrhotite associated witnin matrix

-SS'^-Syif-quartz vein— 500 to core axis SS'OMO'O"-non-mineralized— ————— - ————————————————— : ———————————————— 40'0"-45'0" —

4b'0M-bO'0"

-57'6"-57^7*l-quartz vein— undeterminable contacts bb'O'-bU'O"- non-mineralized

INItRMEOIATE-MAFIC VOLCANIC — Chlorite — Calcite-- rAnkerite 60'0II-65 I 0''-contacts! top-506 tocore axis 65'0H-70'0"———————— bottora-50e to core axis—FAULT RELATED . yu l u"-7b'0"-fine-medium grained" 75'0'"-80 I 0"-green colour . 80 l oM-8b l O"

- -locally, ankerite grains— 600 to core axis 85 I 0"-90 IU"-abundant chlorite alteration-trace pyrite

-95'3"-95'b"-quartz vein— 60" to core axis gS'O'-IOO'O* .-non-mineral ized

-95MO"-96'r-quartz v^eIn~4Uu to core axis-trace tourmaline alteration-non-mi ne're li zed

lOO'OMOS'O"-lOS'ffMts+tr^ratl rock characterized by "layered" appearance 105'0M-110 I 0"

-abundant cTffisrite/carbonate alteration HO'Ol4-lib l O"-highly carbonated

US'O" 120'U"-I24^64t -l24 1 7 l'-quartz veinlet—600 to core axis . 120'0"-125 I 0"

-non-mineralized

SAMPLE NUMBER

G64775

G64776G64777G647/8G547/9

G64780G64781Gb47teG64783G64784G64785

G64786G64787

G64788G64789G64790

664/91G54/92

Bel1s6'

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tracetracetracetracetracetrace

0.00?trace

tracetracetrace

tracetrace

Vr'S

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EARTH RESOURCE ASSOCIATES: DIAMOND DRILL LOG. PROPERTY: Puissance HOLE NUMBER: P-10/fi

FOOTAGE

Tw'y*---220'6"

-,-

•**

i

DESCRIPTION OF CORE

125 I 0"-130 I 0 U13U l U"-13b l U H13i)'U 4'-T4U'Ui'

ANKERITE/QUARTZ/FUCHSITE ALTERATION ZONh 140' "-US'O"-contacts: top-500 to core axis — FAULT kELAItu

bottom-undetenul liable-medium grained ankerite grains-g ey s**een colour -

. -ibi quartz fiquartz/ankerite stringers-tfdCti-1S fuclisiLti alterdtlon '-3X siderite alteration-trace pyrite

-147 -Wb^-quartz vein— 45" to core axis "' 145 I 0M-150 I 011-tt, tourmaline alteration-non-mineralized ,

-148 l 1 M-148 l 7"-quarLz velu— undeterminable contacts21 tourmaline alteration-trace fuchsite—trace p/rlLe

-150'9"^l52'2"-ruchsUe7clilurllB allerallon— SO0 to core axis ———— ————— 150'0"-155'QM———————— .FAULT ——————————————————————————————————————

-I53'0""151 f 0"^bundant siderite alteration —————————————————— 155'0"-160'0"^V

-156'6 ll -157 l 4 H -FAULT-4u i; to core axis-soft gouge present

-I65 l 8"-l66 l 0"-ankerite7quart2 veln—450 to core-arts— " ———————— JsV-^tr-————————— non-mi ngral i /.ed —————————— ——————— ———————————————————

*

SAMPLE NUMBERG64793tifaA/94fcb4795

664796

' J,'?.-, J,j,G6479/

ftfiA7Oft —WQi/yo

664799

^64800HG64801

—— ———— ASSAYS

Sell W.tracetracetrace

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trace

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EARTH RESOURCE ASSOCIATES: DIAMOND DRILL LOG. PROPERTY: Puissance HOLE NUMBER:

FOOTAGE

-"

!

[

f\f\f\ | f |1220'6' —1(\Tf\ aJO/ u

DESCRIPTION OF CORE

-167 l 6"-167 l 9 M-quartz velnlet — Q^ to core dxis-non-fflinerallzed

-t69'4l4 -169'7"-quartz vein--450 to core axis-lion-mineralized

-170'3"*170 l 8"-quartz vein— 40" lo core axis ———— : ——————————————— i70'O it -17S*0"

"LrdCe fuchsite alteration-non-mineralized .

-t75^54^17548l'-qaaptz vein— 50* to core axis 175'0"-1tfU'U"-21 tourmaline associated with both contacts-non- mineralized y

-183'0"-183'3"-quartz vein— 400 to core axis —— ; — ~ —————————————— 180'0"-185 t O"

———————— -tface-tourmailne ———————— —— ———— ————————— ————————

-non-mineralizedf

-187 l 6M -194'OSwall rock characterized by Increase inchlorlte alteration 185 I 0U -190'-011———————— and decrease-immkerite and quartz vetoing —— ———— ———— 190'0"-195'0"

-bottom contact:85e to core axis— FAULT RELATED with fuchsite/chlorite alteration

-198 I 0"-204'0B-10X quartz veining/fuchslte-slderlte alteration and 195'0"-200 I 0M... - .. -trace ovrite ——— — ————— - -- - - -- — ?On 1 ft ll-9inli I fiM -

vi u^v. pji l \,t C.WW W ~tWJ W

-^202^5"-202'7"^ctuarU /ankerite vein— 600 lu core axis —— —————— ——— ——————— ; —

- non-mineralized f- " 9nR'nu ?iA'nu

cUO U "clU U?in'nM ^iR'ft"civ U "t 10 UoiR'n1' ^on'n 11clD U "tell U

-if*TERMEatATe--WFI^-^eLeANtC— Ca 1 ci te^^Chtortte ————————————————— 22fr'0"-225'0^--J

-uridetenntnable contacts " ' " ~ ~ ' —————— 225'0"-230'0"

-fine grained 230 I 0"-235'0"

-green colour 235'0"-240 I 0"

SAMPLE NUMBER

G64802

6648U3

C$4804

G646Q5.6640 DO

664807r*r innn-fjo4ow8^-

rc A finnUU4ou9

G64010GG4811

G64612 ^-GM81^-

G64814G64815

——— ——— SeHS^YS

t ce

trace

trace-

tracetrace

trace^trace-

0.002rote• UUi

^trace~"tr^ce~tracetrace

———

i

EARTH RESOURCE'ASSOCIATES: DIAMOND DRILL LOG. PROPERTY: PuissancePAG^5

HOLE NUMBER: P-10/8-

FOOTAGE

*-*

*

i

i

DESCRIPTION OF CORE '-iilylily carbonated t 240 I 0 M-245 I 0"-2X calcite stringers— 45-90* to core axis 245'0M-250'0"-trace amounts of quart/ filled arnygdules 250 l O"-255'O k'-trace pvrite 255'0'f-260 l O"

260'0M-265 I 0U265*0"-270'0"Z70'0"-275'0"if7t)'0"-ifdO'0 B280 I 0 M-285 I 0"nf\Tf\u inif\" uil 1 i L 1 1 ,, 1 ,v J u nor j. r i TT-*:u/ u -dt/ u -wan lock characterized by 2i. calcite stringers 285'0"-290 I 0"-— : —————— -trace amounts of quartz filled — : ——— ————— ——————— 290 tO"-2a5) l O"295 1 0M-300'0"300'0"-305 I 0"305 1 0M-310 1 0 H310 I0M-315'0 11

- - - l . . 315 i O"-320'0"3ZO i O"-325 t Q"SZS'XJ^SSO'O"330'0"-335'0"335'0"-340'0"340'0"-345 1 0"345'0M-350'0"350'0H-355 I 0U355'0M-360 I 0-SbO'O'-abb'O"365'0"-367 I 0"

^

—————————— EKB-efMIOLC AT 307 FEET. ——— December 11, 1984 —————————————————'

,s J^^^^JUAJ

*

SAMPLE NUMBERG64816G64817G64818G64819G64820G64821G64822654823G64824G64825G64826G64827664828G6482966,4830G64831G64832G64823664834664835664836G64837G64838G64839G64840G64842

Belff.AYStrace0.002tracetracetracetracetracetracetracetracetracetracetracetracetracetracetracetracetracetracetracetracetracetracetracetrace

i-

Earth Resource -AssociatesP.O. BOX 2150. TIMMINS. ONTARIO. P4N 7X8 CANADA

DIAMOND DRILL LOG

DRILLING COMPANY Triangle Drilling FOREMAN CORE SIZE BQ CORE STORED AT: Coreshack

PAGE"!PROPERTY PUISSANCE

HOLE NUMBER P-11/84' GRID REFERENCE 38+OOE/8+OON

TOWNSHIP DELORO CLAIM ME20

AZIMUTH 160" DIP ANGLE -45 0

DIP TESTS (100*.200',300 l)-450 ,400 1 M80 ,500y-50 0 .600V-700V-490 ,WQO-V-460LOGGED BY Ken Lapierre December 16,1984.

•fOOTAGEU— lU'U"

10'0"*-— 182'0"

*

. -

DESCRIPTION OF CORE

-ami casing ^

INTERMEDIATE-MAFIC VOLCANIC — Chlorite — Calcite — Ahker^ite ——————————— lO'OMS'O" —-tuiiLdclii: topundetennlnable

bottora-undeterminable-hAUL'! RELAItU-fine grained

nj-nn.n j-nlnn/i . .................—....—...-l.........— yi ecu luiuui-11 irregular tieiidiny Cdcite strinyers"trace amounts of quartz/carbonate filled amygdules-trace pyrite

-18'3"-l8'6"-quartz veln—300 to core axis IS'O^O'O"-trace tourmaline-trace pyrite

-19M"-19 I 3 U -FAULT— 300 to core axis ' l ' '-abundant chlorite carbonate alteration

-21 T-2r4"-quart2 vein— undeterminable contacts ZO^-aS'O"-chlorite alteration-nun-mineralized

-22 l 2"-22'6"-quartz vein-r-2ow to core axis-5* cnlorite alteration"trace pyrite

SAMPLE NUMBER

664851

•*\

G64852

664853

Berths

trace

*

trace

trace

i

i

*.

i

SRTH RESOLDRTH RESOURCE ASSOCIATES: DIAMOND DRILL LOG. PROPERTY: Puissance HOLE NUMBER: P-11/84FOOTAGE

*~*

J

DESCRIPTION OF CORE.-23 '1 "-23 '4 "-quartz vein-undeterminable contacts

-non-mineralized '25 I 0M-30 I 0 M .3U'Uu-3t)*0''SS'OMO'O*W'OMS'O"

————————— ——————————————————————————————————————— 45'U"-5U'0U —————————————————————————————————————————————————— SO t OM.5S t0M —————————————————————————————————————————————————— 5S . 0..,60 i 0 i. ——

bO'0"-65'0"W'UU-70'U"/U'u'"-/})^"————————————————————————————————————————————————————— yS'O'-SO'O*1 ——80 I0"-85'011K) IUW-3U'0"

, 90 I 0"-95 I 0 11-95'3ll-95 l4H-carbondte;chlorite vein— /bu to core axis 95' O"- 100 'O"———————— -possibly FAULT RELATED ——————————————————————————— : —————————-2t pyrite ; '

100 I 0"-105 I 0U-1ub l uu-nb'u"-wan rocK characterized by soft medlura grained green grains- 105'0"-110'0"possibly chlorite ~ IWO'-HS'O"————————————— —————————————————————————— SiOx-jzo'O"-122'0M-122'5"-possibl hAULI -undeterminable contacts 120 I 0"-125 I01'-abundant chlorite alteration ™ ~ ~- " ~-IX medium coarse grained pyrite ~ •~"- - ~

IZS'OMSO'O"ISO'O^ISS'D"ISS'O'-UO'O"140 I 0"-14b l U tt-145 l 7"-147'0 ll -abundant ground-possibly FAULT RELATED" ~ ~ ' —————— 14b'U"-1bO'U H

-154 l 6 M-154 l 9"-quartzXcarbonate vein— 4utf to core axis 150 I 0M-155 I 0"155 I 0"-160'0U

' ' -T60*0"-165*0M ————————————————————————————————————————————————————— 5'0"-170'0"

SAMPLE NUMBER

G64854Gb48bb664856664857W)4bt)b664359tib4at)UG6486166486ZGb4b53G648646b486bbb4bbbB64B67G64868

664869664870 .664871664872664873

664874664875G648766648/7664878

664879664780664881j— r- j rvoo-6o4882 —

Ben^

tracetracetracetracetracetracetracetracetracetracetracetracetracetracetrace

tracetracetracetracetrace

tracetracetracetracetrace

tracetracetracFLI 111*1*

4YS

-•w-. - ^fx 4--^~N t* — N* * t t i i *EARTH RESOURCE^ASSOCiATES: DIAMOND DRILL LOG. PROPERTY: .Puissance HOLE NUMBER: P-11/^

FOOTAGE

182'0"-237 '5"

•••^

to/ o ~-3io'n* —W IV/ W

DESCRIPTION OF CORE-i7u'4"-i7U'd"-quartz veln-250 to core axis 170'0 I4 -175'0 1'

-trace pyrite

-177'0"-182'uM -increase in ankerlte/chlorite alteration m'O'-ieO'O"

ANKERITE/CHLORITE ALTERATION ZUNb 180 I 0 I4 -185'0 11-contacts: top-undeterminable-probably FAULT KhLAItU ISE'D^-^D'O"bottom-undeterminable 190 I0"-195'0'1-coarse grained ankerite grains oriented 70* to core ails 195 I0"-200 I 011

-possible SHEARING — 70* to core axis 200'0II-205 I 01'-60X cnlortte/serpentifle? alteration 205 I0"-210 I 0"-tt ankerite veining— cross-cutting and parallel to shearing 210'0"-215'0il-trace Siuui Ite altereitlori - , . ZIS'O'^ZO'O"—trace pyi Itii

' - )-222 l O M-224'0"-siderlte alteration replacing ankerite grains? 220 ' 0^-225 VO"

225 I0 M-230 I 011-232 l O tt -233 l O"-iidurite alteration replacing ankerite grains? 230'0"-235 I0U

INTERMEDIATE VOLCANIC — Ankerite ———————— ——————————————————— 235'0"-240'0M-UiiJeleniii nable contacts-fine graineU grey colour-sliyliLly carbonated - — -- :- - * ~-trace-1* disseminated pyrite " — ~

-240'8"-246 l O"-25 irregular trending quartz stringers 240*0 "-245 'O"* 245 I 0H-250'0U-247 I8"-247 I 11 "-quartz vein-4U0 to core axis ' ""

-non -mineral i zed250'0 M -255'0"

-2bb'6 ll -2bb 1 8"-quartz vein— 300 to core axis 255'0U -260 I 0 U-non-mineralized - -

*

SAMPLE NUMBERG64883

G64884

G64885G64886G64887G64888664889G64880G64891G64892

" -*

G64893G64894G6489S

G64896

G64897G64898

G64899G64900

•^ASSAYS

Bpll W.trace

trace

tracetracetracetracetracetracetracetrace

trace0.002trace

trace

tracetrace

tracetrace

PAP. r A?,

EARTH RESOURCE ASSOCIATES: DIAMOND DRILL LOG. PROPERTY: PuissancePAG

HOLE NUMBER: P-11/8F60TAGE

-,

Sjiu'u"—, 368 "0"

.508 U —M A rt i j* u412'6"

DESCRIPTION OF CORE-260'2"-260'10"-anKerite7quartz vein-undeterminable contacts 260 I0II-265'0"-z* pyrite stringers— 90" to core axis

-262 l8"-264'4"-2J pyrite stringers— 850 to core axis 265 1 0"-270'01'270 I 0"-275'0"-2X9 l !)"-282'0 1 '-waii rock characterized by fragmented siliceous material 275 I 0M-280 I 0'1-Si pyrite stringers— 700 to core axis 280 '0 "-285 'O"-b* pyrite associated with chloritic matrix285 lOM-290 l Oa290'0M-295'0"-297 J2u-zy7Mu"-quartz vein—undeterminable contacts 295 I 0"-300'011-z* pyrrhotite associated with 10* chlorite alteration•- '

-297 I 1uM-310 l u M-waii rocK characterized by pervasive fine grained calcite alteration300'0H-305 I 0"

- - . - / SOS'O'-SIO'O"-

•- - ' . ' --' 'FRAGf^!ENTAL — Calcite — Acid Pyroclastic 310'0"-315 I 0'1-gradationai contacts 315'0II-320 I 0*-grey green colour |sili j 320'0"-325'0"-fine grainerragmentsAgrade into coarse grained siliceous fragments 325 I0M-330 I 011at increasing depths 330'0II-335 I0"-pervasive calcite alteration within matrix 335 I 0"-340'0"-chlorite matrix 340 lO"-345 l O rt-trace-zi pyme/pyrrnotite associated within matrix 345iO"-350'0"SSO'O^-SSS'O"355 I 0 M-360 I 0M

. 360'0II-365 I 0UINTtRHEOIATE-HAFIC VOLCANIC — Calcite — Chlorite 365'0M-370 I 0"-contacts: top-gradationsl 370 I 0"-375 I 0Ubottom-uhdetenninable 375'0M-380 I 0"-fine grained grey green-green colour 380'0H-385'0"-pervasive calcite alteration . 385'0U-390 I 0"

-local lyjcaclte grains with preferred orientation— 600 to core axis 390 I 0U-395'0"-trace pyrite . 395'0"-400'0U

SAMPLE NUMBERGS4901

G64902G64903G649MG64905

G64906G64907G64908

664909G64910

G64911G64912G64913G64914G64915G64916G64917G64916G64919G64920G64921G64922G64923G64924G64925G54926G64927G64928

Pelfwtrace

tracetracetracetrace

tracetracetrace

tracetrace

tracetracetracetracetracetracetracetracetracetracetracetracetracetracetracetracetracetrace

*WS

ii

t t tEARTH RESOURCE ASSOCIATES: DIAMOND DRILL LOG. PROPERTY: Puissance

PAGe- 5 HOLE NUMBER: P-11/M

f8|:

m*(Q

fe

BfeiitW1ipfewp"it©^"'^jii**-*' 1i'Ut*

FOOTAGE

^.: ' - '

•ll^'fi*1

415*0"-

^ik.v-"w-:/..: -:C^v-\;:;;:,v -~®afa,fc^i'.

^474'0*. i

"••, ~ "" . - ~ f. -i.

"'-'j i.' '': ' ' ~" ' '

,,v,*-; -.-* :1 ' " ; - i.,,, .r - ' 7.*"

•#^-;.'01-.'"-'

|k^:;f,^.'; : -^..S -••'-••. ,. ; ~ '~. '

•- '* ' - ,i-^v:.'--

f -i - ,- ; . ,"*. i-

f

DESCRIPTION OF CORE400'0H-4l2'u"-decrt;dse In fdlcltt! pervasiveness 460 I 0M -405 I 0 Mr * **w *^ ^Wv V

405 0 -410 0QUARTZ/ANKCRITC/rUCHSITE VEIN ——————————————————————— : ——— 41Q'0"-412'6tl ~~~~

-contacts: top-60g to core axis 412'6I4-415'0"— ——————— : — bottom-600 lu core axis ——— ' ————————— ——————————————— - ——— trace tourmaline ————— —— ————— : ——— - —————————————— ———————-trace pyrite ——————————————————— r —— — — —————— - —— —— — ——..: ':. ' -i-- . . - . ' . . ^ . -

INTERMEDIATE VOLCANIC — Tuff?? ————————————————— ———————— 415'OM20 lOtt ————— contacts: top-60p lo core alls ——————————————— — ——————————— , —— :bottOiiHiiiiuti Lcnnl nabl e

-fine grained yrt-y green colour-U irregular treading quartz/ankerite stringers—— -trace-U pyrite . . —————————— - —— ————————— : —— : —————————

MM , u-422'0 -422 I 6"-quartz7ankerite vein-undeterminable contacts 420'0*l-425'0"- ——— — —— -trace pyrite —————— — — — — —— — — —— ——— - — — ————————

-428 '9^-420' 11 "-quartz/anker 1 le vein-undetenalnable contacts ——— — 425'0"-430*o" "~~~~~~~-2^6 pyrite dssociated with contacts

^SO'O'-flSS'O"-438lO ll -438l3l'-quartz velnlet-400 to core axis — ~~ ———— ~~~ ————— 435'0"-440'0M ————-trace-U pyrite associated along both contacts r'

44U I0"-445I0"445'0"-450'0 |J450 IOM55 I 0"

-457 '5"-457 "-quartz/carbonate vein~bbw to core axis 455 I0"-460'0M—— —————— -trace . toannallne ————————— ————————————— ————————————————— *trace pyrite ——————————————— ~~ ——————————————————

-461'6"-46riO"-quartz veinlet— 60* to core axis 460 I 0 U-465'U M

465'0 U -4?0 1 0"*

SAMPLE NUMBERG64929664930

G64931G64932

664933

- .,

664934

664935

664936664937

664938664939664940

664941

664942

G64943

—— /\oo

tracetrace

tracetrace

trace

'

trace

trace

tracetrace

tracetracetrace

trace

trace

trace

*\YS

j

i

ttEARTH RESOURCE ASSOCIATES: DIAMOND DRILL LOG. PROPERTY: Puissance HOLE NUMBER: P-11/t

FOOTAGE

474 '0"-510'9U

BlO'g"--742 '7"

DESCRIPTION OF CORE

-471 10"-47t l 4"-quartz vein— 300 to core axis 470'0"-475 I 0M-5* tourmaline/talc alteration-2i pyrite

ANKERITET/quartz/FUCHSITE ALTERATION ZONED 475'0"-480 I 0'4-contacts: top-undeterminable 480'0"-485 I 0"

bottom-700 to core axls-FAULT RELATED 485'OM90 I 011-Alteration Zone possibly within Tuffaceous Unit 490 I 0M-495'011-fine-rasdiumgrained , 495 I 0H-500 I 0'1

- -ggey green colour 500 I 0II-505'011-10* quartz and quartz/carbonate stringers— 45 -900 to core axis 505 I 0"-510 I 0"-fuchsite alteration associated with both fault related contacts 510 I 0"-515 I 0"-trace pyrite/chalcopyrite

——————————————————— —— ——————————————————— ————————————— : ————— : —————————————

MAFIC VOLCANIC — Chlorite — Calcite 515 I0W-520'011-contacts: top-70" to core axis— FAULT RELATED

bottom-75" to core axis— hAULl RkLAltt)-fine grained-green-oarK green colour-si igntiy to moderately carDonateo-IX irregular trending calcite stringers-trace pyrite ' '

-524'9 u-525'5"-quartz vein— 300 to core axis 520 I 0"-525 I 0"-S-tO.% ankerite alteration 525'0"-530'0"-2X chlorite alteration-trace tburmaline patches-fuchsite alteration associated with both contacts-trace pyrite associated with fuchsite

530 0 "-535' 0"B35 I 0II -540'0"540 1 0 I( -545'0"545 I 0"-550'U"

SAMPLE NUMBER664944

G64945664946664947664948664949664950664951664952

-j*

664953

-

664954664955

G64956G64957G64958bb4yby

Belli?"8

trace

tracetracetracetracetracetracetracetrace

*

trace

tracetrace

tracetracel;racetrace

i

|

EARTH RESOURCE ASSOCIATES: DIAMOND DRILL LOG. PROPERTY: Puissance

PACIW 7

HOLE NUMBER: P-11/84

FOOTAGE

4.4

l

i i

DESCRIPTION OF CORE

-bbrb-'-bbriP-epidote/calcite/quartz stringer— 250 to core axis 550'0"-555'0 U-rion-rninerallzed

555 1 0 I1 -560 I 0 I:550 I 0"-565'0"

-569'0"-bby'b"-quartz veinlet— 250 to core axis 565'0"-570'0'i-trace cnlorite/calcite alteration

-570'3"-570 1 7"-quartz vein— 3U". to core axis 570 I 0 M -575 I 0 H————————————— -?t BHntWPn*xTTP alteration ————————————————————————————————————————————

"1.10 rvnULiwUlvUsji 1 C albcluvlOn

-non-mineral i zed575 I0"-580'0"580'0"-585 I 0 U585 'tr -wu 'ir590'0"-595 1 0"535 I 0 U -600'0U

. - j 600 I 0H-605'0"bUb^^blD'O"eio'^-eis'O"sis^'-ezD'o11

————————————————— - —————————————————————————————— 620' 0^625*0"625 I 0"-630 I 0"630'0"-635'0"63b l O"-640'0 M640 I 0"-645'0"

————————————————————————————————————————————————— 645 t 0..,650 i QM650 1 0H -655'0H

^655 lO"-6SS*8*--yi loun(l— possibly FAULT RELATED ———————————————————— 6bb l O"-fcO'0"660'0"-665'0"

-669'10 u -670 l O"-quartz vvein— 70" to core axis 665'0"-670 I 0"-trace pyrite

670 "0" -675 "0"675'0U-680 I 0"6ao l O"-685 l O"585 l O"-690'O tl690'0"-695 I 0"byS 1 0"-7UU'U"

SAMPLE NUMBER

G64960

S64961G64962G64963

G64964

664965G64966tib4957664968G64969G64970G64971G6497G64973G64974G64975.664976G64977U64978G64979G64980G64981G64982G64983

G64984G64985G64986G64987G64988G64989

Belf^ftrace

tracetracetrace

trace

tracetracetracetracetracetracetracetracetracetrace0.0040.002tracetrace

~tracetracetracetracetrace

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i

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r

p

8EARTH RESOURCE'ASSOCIATES: DIAMOND DRILL LOG. PROPERTY: Puissance HOLE NUMBER: P-11/8*

FOOTAGE

-.

.

DESCRIPTION OF CORE

700'0"-705 4 0"/Ub'O'WIO'O"710 l O tl -715 l O"

-715 l O"-724'0"-wall rock characterized by 6-1US medium grained ankerite 715'0"-720'0"y. a ins 720 I 0"-725'0"

M-7ij 1 *71j 4 -cjUdj tz vein-undeterminable contacts-chlorite alteration———————— -non-ranreralized

-.71fi'n u 71K'1" nnai-i^T ua.tn- i 1 1 u 1 Ul 4. j. j.*-/ ID u -f iu i -quai ti vKiu-unuciieniiinaDie contacts_ ^ m -f t t

' *-non-nil ndrdjj zeu

-717'3"-717'6 l'-quartz vein— undeterwinable contacts-non-mineralized

; ~*- 'i :--718 11*-^19M M -quartz vein-^700 to core axis — ! "-chlorite alteration——————— -non-tnfneraitzed ——————————————— ————————— ——— - ————

-721 l 10 ll -722 l 3"-quartz vein-undetertdinable contacts^volcanic material within vein-trace pyrite " ~ •~'

725 l O tl -730'0 11-730'0 M -731 l 5"-quartz vein— GO0 to core axis - — - — JSQ^^SS1^"-105t volcanic material - -———————— -2X ankerlte-giteratton ——————————————— : ———————— ———————

— - - -non-mineralized "~ ~ - -- - - — - - -

-73t 0 -732*3 -quartz vein- — 70* to core axis-non-mineral 1 zed ' - — —- -

-73o 8 -735 9 M -Quartz veinlet-500 to core axis 735 'O11 - 740*0"

.

SAMPLE NUMBERG64990G64991G64992

.G54993G64994

G64995G64996

G64997

Wtracetracetracetrace

Ljtrace

*

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trace

*ws

i

EARTH RESOURCB ASSOCIATES: DIAMOND DRILL LOG. PROPERTY: Puissance HOLE NUMBER:FOOTAGE

T**C t *—

BIOM"

**

,

DESCRIPTION OF' CORE-7Jb1| b"-;c!b'8"-quartz vein— 45 0 to core axis

-nun-mineralized-739'lO"-740'0"^uartz vein— 70" to core axis —————————————————————————

-non -mineralized

-740'3"-74G 1 6 u -quartz7anKerite vein-50" to core axis 740 I 0"-745'0"-iiorHn ineraiized

ANKERITE/QUARTZ/FUCHSITT^CTERAI iOH ZONE — Chlorite —————————————————— : —————-contacts: top-75. to cora axis-FAULT RELATED————————— bottoffl-undeteriiiinable ———— —————————————————————————sued i urn-coarse grained ankerite grains-grey yreen colour-chlorite alt^rdliuit. increases at increasing depths-tO-15% quartz and quartz/ankerite Stringers-irregular trending-trace pyrite .

— 742 l 7"-743 t2it^fuchsite alterdliun associdted with fault related upper contact ———————-trace pyrite

'-745'0"-745 1 3"-fuchsite alteration 745'0"-760 I 0 U--74f^Jt^74f^l^-quartz vein— 4Be to core axis ———————— -. ————————— - ——— r- :

-non-mineral i zed-^74714ftit*-74ft i ^ u i.fiii^rt7 vufn-,9^0 tn t-ni'a avlc —————————————————— ———————————————————— i — —/•t/ IU —/to 3 —V^UOI \tL Vctll— — {.D LU LUl C QAlb

-nun-mineralized——————————————————————————~ -g, —————————————————————————————————— : ————————————————————————————————— - —————————————————————————

^49M^^5e4(T^irartz-ire1ntetFl 5^*^^25*-to-core-iaxts ———————————————————————-trace tourmaline-trace pyrite

-749'9"-75u'4"-quartz veinlet— W to core axis 7SO'0"-755 I 0"-non-mineralized

SAMPLE NUMBER

G64998

G64999

G65000

ASS Bell W

tract

.

trace

trace

— - I I l _ _

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—H

EARTH RESOURCE ASSOCIATES: DIAMOND DRILL LOG. PROPERTY: Puissance HOLE NUMBER: P-11ZJ4

FOOTAGE

•*-*

810*4"-849*6"

t\ M n i j~ li849 '6—— 854*6"-

,

DESCRIPTION OF CORE

-/td'd"-752 l 2 ll -quartz vein--300 to core, axis-tourmaiine/fuchsite alteration-non-mineralized

-/bl'8"-754 l O"-apparent SHEARING of wall rock— 600 to core axis-quartz/ankerite veins oriented parallel to shear planes-quartz vein oriented suoparauel to shear planes

-754'0 M-8uu l U"-Aiteration Zone characterized by abundant chlorite 755 I Q M-760 I 0"760'0M-765'011765 I0"-770 I 0 1'770'0 M -775 I 0"775'0"-780'0"780 I 0M -785 I 011785 I 0"-790'0 1'

* - - f 790 lO"-795* *795 l O y -800'0 M800iOll -805 l O"SOS^-SIC'D"810'0 II-815 I 01'

INTERMEDIATE VOLCANIC — Silicified — Calcite 815'0"-820 I 0"-contacts: top-undeterminable 820 I 0M-825 I 011

bottom-500 to core axis 825'0"-830 I 0 M-jrjnfe grained, grey green colour 830 I0"-835 I 0 M-21 i rregular trending calcite stringers 835*0II -840 I0"-trace pyrite 840 l O"-845'O tt

HIGHLY SILICEOUS IRON ^ORMAIIUN 845'0 M -850*0 U-contacts: top-Su** to core axis ' 850 I 0"-855'0 U

bottom-700 to core axis-85* siliceous material-5^ irregular trending magnetite stringers-5J chlorite/epidote? alteration - "~ -- — - —-5X pyrlte/pyrrhotite associated with alteration material andmagnetite~~t)ands '. "' ~ "

SAMPLE NUMBER

665001665002665003665004665005665006665007665008665009665010665011665012665013665014665015665016665017665018

665019665020

BelffAYS

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tracetrace

l

EARTH RESOURCE ASSOCIATES: DIAMOND DRILL LOG. PROPERTY: Puissance HOLE NUMBER: P-11/8

FOOTAGE

— 654' 6"-— roos*tf

*-*

DESCRIPTION OF CORE

-trace chalcopyrite

INTERMEDIATE VOLCANIC — silicified — calcite 855 I 0 II -860'0M-contacts: top-vuw to core axis 860 I 0M-865'0 M

bottom-undeterminable-fine grained, grey green colour-trace amounts of medium grained ankerite grains-lrace-2X quartz and .quartz/carbonate filled amygdules-136 irregular trending calcite stringers

. -trace pyrite1

-866'2M-866 l 9 ll-quartz vein-undeterminable contacts 865 I 0"-870 I 0"-n pyrite stringers associated with chlorite stringers

870'0"-875'0"- - . ; 875 I 0"-880'0"

-880 I 2 u -860 l 6u -quartzXcalcite velniet— 40" to core axis 880 I 0M-885 I 0"-trace pyrite

-889 l 3"-889'5"-quartz7carbonate vein— 450 to core axis 885 I 0M-890 I 0"-non-mineralized

ByU'0"-89b'0"895'0M-900'0"900'0 tl-905'0 i'905 I 0"-910'01'

-912 l 3"-912 l 8"-ground-poss!bly FAULT RELATED 910'0M-915 I 0"

-917 1 0 u -917'5'4 -ground-posslbly FAULT RELATED " ——— 915T0"-920 I 0"920'0M-925 I 0"

-yi:d i 4"-S2y'7 M -carbonate7chlorite vein— 25" to core axis 925'0"-930'0".

-934'9 M-934'10"-quartz veinlet— 50* to core axis 930'0"-935 I 0 (J935'0"-940'0"

-S4U'4 t'-940'9"-ground-posslbly FAULT RELATED 940'0"-945'0"945 I 0"-950'0"950 I 0"-955'0"

SAMPLE NUMBER

G65021G65022

G65023

665024G65025665026

G65027 -G65028G6S029G65030G65031G65032

G65033G65034G65035

665036G65037G65038G65039G55040

BeA*

tracetrace

trace

tracetracetrace

trace

tracetracetracetracetrace

tracetracetrace

tracetracetracetracetrace

W*YS*

!

ll

EARTH RESOURCE ASSOCIATES: DIAMOND DRILL LOG. PROPERTY: Puissance HOLE NUMBER:

FOOTAGE

--

-,

i

DESCRIPTION OF COREy 55*0 -96u'u"960 0 -965 '0'965 0 -970 0970 0 -975^0y?5'G"-y80'U"

—————————————————————————————————————————————————— 980^0" -955 '(T*985 0 -990 0990 0 -995 0yyVO"-100G'G

-*

•* H f '

f

——————— ENO-Qf-440Li-AT10QO FEE? ——————— December 1C. 19647 ——— ; ————————————

-' -

's ^Uws/y^fife^J^J ./' ' ^ "y/"-

*

SAMPLE NUMBER

G65U42665043G65044bbb04iiG65045G65047

— 6050481 G66049

. " '

•^eeA5?,

tractractractractractractractractrac

.

w — ——^YS

e6 'eeeee6

e s

i

-:

j

DIAMOND DRILL LOG

DRILLING COMPANY CORE SIZE BQ .

TRIANGLE FOREMAN CORE STORED AT: C oreshack

PAGEPROPERTY PUISSANCE

HOLE NUMBER P-12/84 GRID REFERENCE 15+OOE/16+OOS

TOWNSHIPDELORO CLAIM M.E. 3( AZIMUTH 1 500 D IP ANGLE -^5O

DIP TESTS:LOGGED BY Ken Lapierre DATE Dec.7Jan. /85

FOOTAGE

0-26'26'-

410'

DESCRIPTION OF CORE { split COre)

drill casingINTERMEDIATE TO MAFIC VOLCANIC- Calcite - Chlorite 26'- 30*

-undeterminable contacts 10'-35*-fine to medium grained 35'- 40'-grey green to green colour 40'- 45*-moderately to hiehly carbonated 45'- 50'-trace to 2# chlorite blebs-no preferred orientation 50'- 55*-trace amounts of irregular trending carbonate stringers 55'- 60'-trace fine grained subhedral disseminated pyrite 60'- 65*

65'- 70'-76'6"-76'7" -calcite veinlet -^5W to core axis 70'- 75'

-non-mineralized 75'- 80'80'- 85'85'- 90'

-9V8"-9VlO" -quartz vein -^0 to core axis 90'- 95'-non-mineralized

95'. 100'100 '-105*

-106'10"-107.'l" -carbonate veinlet -15U to core axis 105'-110'-non-mineralized

110 '-115'115'-120'

-122 '-130' -1# quartz/carbonate filled amvcdules 120 '-125'-subrounded 125 '-130'-1/8-to V^"diameter-non-mineralized

130 '-135'-

SAMPLE NUMBER

G65051^6^05?650536505465055650566505765058650596506065061650626506365064

650656506665067

65068650696507065071

65072

ASSAYS

DIAMOND DRILL LOG. PROPERTY: PUISSANCEPAGW2

HOLE NUMBER: P-12/^

FOOTAGE

t

DESCRIPTION OF CORE ^^ ^

135' -140 '140 '-145*145'-150'

-150'5"-150'6" -auartz/calcite veinlet -700 to core axis 150 '-155'-non-mineralized

155' -160 '160'-165'165' -170 '

-172'2"-172'5" -10# medium grained euhedral pyrite 170 '-175'175 '-180'180 '-185'

-187 '-188' -Fault Seam or possible sludge 185 '-190*190 '-195'195' -200'200'-205'

-209 '9"- 210' -Calcite vein -undeterminable contacts 205 '-210'-non-mineralized

210 '-215'21V-220'220 '-225'225 '-230'230 '-232 '6

-234'-247'6" -volcanic material characterized by 5-10# 232*6^-235'medium grained to coarse grained 235 '-237* 6subhedral to euhedral pyrite-disseminated 237'6"-240*and with preferred orientation -450 to core axis 240 '-242' 6

242 '6" -245'245 '-247 '6

-247 '6"- 2^0' -IRON FORMATION 247' 6"- 250*-5# pyrrhotite/pyrite/chalcopyrite-pref erred 'orientation 4510 to core axis

-contacts -45 to core axis250 '-252' 6

252'6"-255*255 '-260'260 '-265'

SAMPLE NUMBERG65073650746507565076

65077650786507965080650816508265083650846508565086^50 87

650886508965090650916509265093

1 65094650956509665097

1 6509865099

65100651016510265103

ASS————— *WS j

i

- DIAMOND DRILL LOG. PROPERTY: PUISSANCEPAG IR

HOLE NUMBER: P-12/

FOOTAGE

-^

410'-537'

DESCRIPTION OF CORE (split COre)

265 '-270'270 '-275'275 '-280'280 '-285'285 '-290'290 '-295'

-297 '-317' -moderate amount of ground 295 '-300*-possible FAULT ZONE 300 '-305*

305 '-310 '310 '-315*315' -320 '320'-325*325 '-330'330--335'335 '-340*

' 340'-345'345 '-350'

-355--356 1 -5-10# medium to coarse grained 350 '-355'-disseminated and 45O preferred orientation 355'-357'6'357'6"-360 (

-^60'-4lO' -w**!! rock characterized by a fine grained 360 '-36*5*tuffaceobs appearance " ~ 365 f -370'

-probable tuff? 370 '-375'375 '-380'380'-385'-385 '-390'390 '-395'395 '-400'400'-405'^05'-^10'

-INTERMEDIATE to MAFIC VOLCANIC - Ankerite - Chlorite - Fuchsite 410 '-415'-undeterminable contacts ^15 '-420'-grey to grey green colour if 20 '-425'-fine grained appearance 425*-430'-2-5^ chlorite blebs -apparent orientation 50 W to 70U 430 '-435'to core axis . 435 ' -440 '

SAMPLE NUMBERG65104651056510665107651086510965110651116511265113651146511565116651176511865119651206512165122651236*5124651256512665127651286512965130651316513265133651346513565136651376513865139

ASSAYS

j

i

: DIAMOND DRILL LOG. PROPERTY: PUISSANCEPAGE

HOLE NUMBER: P-12/8*

FOOTAGE

^

537'-590

590'-709

DESCRIPTION OF CORE ( split core)

-1 j fine grained fuchsite blebs- 50#-70# t) cere axis 440'-445'-minor amounts (up to 1#) of irregular trending 44-5' -450*quartz stringers 450 '-455'-trace to 2# fine grained disseminated euhdral 455' -460'pyrite 460 '-465'

465 '-470'470 '-475'475 '-480'480 '-485'485 '-490'490 '-495'495 '-500'500 '-505'505 '-510'510 '-515'515'-520'520 '-525'525 '-530!530 '-535'

-INTERMEDIATE to MAFIC VOLCANIC - Calcite - Chlorite 535 '-540'1 -undeterminable contacts 540 '-545'

-fine grained appearance 545*-550*-green colour 550 '-555'

555'-560'-highly carbonated 560' -565 f-trace mineralization 565 '-570'

570 '-575'575 '-580'580 '-585'585 '-590'

-MAFIC VOLCANIC - Ankerite - Chlorite 590 '-595'1 -undeterminable contacts 595'-600'

-medium grained ankerite grains (50-8055) 600 '-605'-chlorite alteration 605'-610'-trace pyrite mineralization 610 '-615'

615 '-620'

SAMPLE NUMBERG6514(G6514]G6514J6514;651446514J

ASSAYS

65l4fl6514?6514i6514*6515C651516515JI651536515M^1536515(!65157651586515S6516C65163651626516^651646516565166651676516865169651706517165172651736517465175 .

i

i/LX PAP - Ms-

V

PAGE

: DIAMOND DRILL LOG. PROPERTY: PUISSANCE HOLE NUMBER: P-12/84

FOOTAGE

^

709 '--UT

DESCRIPTION OF CORE UpVvWoreT)

620 '-625'625 '-630'630'-635*635 '-6*4-0'640'-645'645 '-650 '650 '-655'655 '-660'660' -665 '

-666 '-681' -wall rock characterized by fine 66 5 '-670'grained ankerite grains 670*- 675'

-2-4# quartz stringers - 30-50W to core axis 675'-680'-1-39& fine to medium grained subhedral to euhedraldisseminated pyrite associated with quartz and

wall rock ' 680 '-685'685 '-690'690/-695'695 '-700'700 '-705'

-INTERMEDIATE to MAFIC VOLCANIC - Ankerite - Chlorite blebs 70 5 '-710'

-undeterminable contacts 710 '-715*

-fine grained ankerite grains 415' -720'

-1-396 chlorite blebs - 50 0 to 70 o to core axis 720 '-725'-grey green colour 725 '-730 V

-trace to 1# fine grained pyrite mineralization 730 '-735'735 '-7^0'740'-745'

-?45 '8 "-745 '10" - quartz vein - ?0U to core axis 745 '-750*- non mineralized 750 '-755*

755'-760'760 '-765'765*-7?0'770 '-775'V75'-V80-

SAMPLE NUMBER

G65176G6517765178651796518065181651826518365184651856518665187

6518865189651906519165192651936519465195651966519765198651996520065201

652026520365204652056520665207

ASsWs

-: DIAMOND DRILL LOG. PROPERTY: PUISSANCE HOLE NUMBER: P-12/84

FOOTAGE

-*

DESCRIPTION OF CORE UpVtY cofe-l ' -

-78W-78V8" - quartz vein - *iO? to core axis 780 '-78 V- trace tourmaline- trace fine grained pyrite associated

with contacts785 '-790'790 '-795'

-796'9"-?96'10" - quartz vein -70 O to core axis 795'-797 1- trace tourmaline- trace ankerite patches- trace pyrite associated with contacts

.-

1END OF HOLE AT 797 FEET

!

f

—————————————————————————— J/ y# . ————————————

l^jStA/^tUf/Af(*r * *S J

•'

'

-

*

SAMPLE NUMBERG65208

G652096521065211

IP "- —— ' ASSAYS

42A06NE0404 63.4536 DELORO 0S0

PUISSANCE CORPORATION

GEOLOGICAL REPORTON

DELORO CLAIM GROUP DELORO TOWNSHIP, ONTARIO

June 24, 1985 TOM GLEDHILL, B.A. P.Eng.

PUISSANCE CORPORATION

GEOLOGICAL REPORTON

DELORO CLAIM GROUP DELORO TOWNSHIP, ONTARIO

SUMMARY

Mapping was carried out on a group of twelve claims in Deloro Township, Timmins, Ontario. The field observations were completed in the Spring .of 1984 by J.C. Kirwan. These notes are prepared based on Kirwan 1 s map. The group is mainly vertically dipping east-west striking volcanic related rocks.

The main carbonate z one conformable with the formations is fractured and filled with gold-bearing quartz. The gold is coarse." It is difficult to sample such a deposit except by bulk sampling. This was the routine employed by Kerr Addison at Virginatown.

Such a bulk sampling program is recommended.

''f-.

PUISSANCE CORPORATION

GEOLOGICAL REPORTON

DELORO CLAIM GROUP DELORO TOWNSHIP, ONTARIO

INTRODUCTION

A total of 12 claims was mapped in the spring of 1984. The field map was prepared by .#.C. Kirwan. This report is based on the writer's limited knowledge of the property, the observations in Kirwans's map and visits to the property to examine and evaluate the main carbonate zone.

GENERAL GEOLOGY

The major feature of the area is the Procupine-Destor Fault which lies 4,000 feet north of the property and strikes northeast.

The rocks throughout the property are carbonate rocks, intermediate volcanics, fragmental rocks, tuffs, iron formation and diabase. The iron formation and diabase have cross cutting relations to the bedded deposits. There is no explanation for the cross cutting nature of the iron formation.

The tops are north facings and are usually vertical or steeply north dipping. There is some dragging along the diabase dykes and minor distortion along cross faulting. The occurrance of gold associated with sulphide phase iron formation may be fault-related.

ECONOMIC GEOLOGY

The most interesting economic feature is the coarse gold associated with the quartz veining and fracture filling of the main carbonate horizon. This gold is difficult to establish a grade. Stripping and diamond drilling defines the zone but the small samples usually taken usually range from l to 20 Ibs. To be effective a bulk sample must be taken and it is recommended that character samples of 10-50 tons be taken and evaluated. This should the.n be followed by bulk sampling and/or miling of samples of 100 to 1,000 tons each.

i\ .CONCLUSIONS AND RECOMMENDATIONS ,- '

The gold values in the main carbonate zone are quite similar to other deposits that have proved economic. They are by nature erratic. A program designed to bulk sample these deposits is the best way to evaluate them.

A reconnaissance of the remaining 6 carbonate zones should be carried out initially employing geochemistry.

The failure to locate gold in the eastern drill holes in the main carbonate zone should be examined*

The gold in the iron formation should be tested at a laterdate. It has a potential for smaller tonnage.

t: An extensive bulk sampling program is reconunended in the

main carbonate zone. It should be started with samples up to 50 tons over selected areas. As the nature of the deposit is better understood, larger bulk samples should be taken.

Respectfully submitted,

June 24, 1985 P.Eng,Tom Gledhill, B. A.

i*.

, a

4aA86NE8484 63.4536 DELORO 030

PUISSANCE CORPORATION

DELORO TOWNSHIP CLAIMS,

ONTARI-0

SUMMARY ACCOUNT

by

John L. Kirwan

EARTH RESOURCE ASSOCIATES:P.O.Box 985,Centre Harbor, N.H. 03226,USA603 253-6107

P.O.Box 2150, Timmins, Ont. . . Canada , PAN 7X8May 23, 1984

l AKI H RLSOUKQ ASSCXJAItS JOHS l KIKWAN

DECLARATION

I, John Laurence Kirwan, of the Town of Centre Har bor, State of New Hampshire, United States of America, and of the City of Timmins, Province of Ontario, Canada, do hereby state:

1. that I am a practising Consulting Geologist with offices in Old Meredith Road, Centre Harbor, NH, USA 03226.

2. that I am President of Earth Resource Associates (John i L. Kirwan and Associates Limited) which was incorporated in the Province of Ontario in 1976.

3. that I have practised my profession as Geologist cont inuously since 1961 and as a Consulting Geologist cont- i nuously since 1972.

4. that I am a Professional Engineer of the Province of Ontario and of the State of New Hampshire and that my licence to practise is not under suspension or revocat ion in either juristiction. I am also a Fellow of the Geological Association of Canada and of several other professional and licensing bodies in Canada, the USA, England, Ireland and Brazil.

5. that I am a graduate with the Degree of Bachelor of Science in Geology and Mathematics from Carleton Univ ersity in Canada and with the Degrees of Master of Sci ence and Doctor of Philosophy from the University of London in England.

6. that I am familiar with the material contained in this report, having examined the original material myself, and with the property in question, having visited it on several occasions in the field, and

7. that I do not now have and do not anticipate receiving, any direct or indirect financial interest in the prop erty described in this report.

Respectfully submitted,

JOAVTI L. Kirwan

•\Kitl KISOUKi l -\ssv K l Ali K )t IN l Kim AS

PUISSANCE CORPORATION

DELORO TOWNSHIP CLAIMS

ONTARIO

by

John L. Kirwan

SUMMARY ACCOUNT

l INTRODUCTION

The Puissance Corporation of Toronto holds the mineral rights to 12 mining claims situated in the northeast quarter of Deloro Township, Porcupine Mining Area, District of Coch rane, Ontario, Canada. These claims comprise about 480 acres (based upon the nominal 40 acres per claim in Ontario) and occupy two offset, but contiguous, blocks of ground, the

l AKI f i KisOUKt !All^ IOHN i KlkU A\

more southerly of the two consisting of 8 patented claims ! and the more northerly (and westerly) consisting of 4 unpat- ented claims (see Figures l and 2, pages 3 and 4). ;

The patented claims are numbered as follows. The - number of acres in each claim was obtained from the original survey data of 1922, on file with the Land Registry Office \ in Cochrane, Ontario. No survey was located for claim ME20.J

ME 20ME 21ME 22

ME 23

ME 29ME 30ME 31ME 54

40.50 Acres41.25 Acres

44.75 Acres40.50 Acres42.50 Acres39.25 Acres37.25 Acres

and

Of these, the surface rights (but not the mining rights) were transferred to Dome Mines Limited for claims ME20, ME21, ME23, ME31 and ME54 on May 11, 1983.

The unpatented claims consist of the following:P-758009 P-75SQ1Q P-758011 and P-758012.

These were staked on April 10 and 11, 1983 and rec orded on April 18, 3983. On February 16, 1984 these were transferred to the Puissance Corporation. The original recording records for claims P-758009 and P-758010 stipulate1 that the mining rights only are conferred in the staking, whereas the records for claims P-758011 and P-758012 make no such restriction. Work reports have been filed with the Recorder's Office to maintain these claims in good standing until April of 1986, with additional work soon to be filed that will extend this time beyond that date.

AKI H l AW X l A! l K )H\ l klk\YA\

MINE PRODUCTION (g)

a Ba

3x106 - 31x10*

^1x106 A

Timmins

-tfT^

OGDEN

TISDALE

\ d

\*a a" y a 0 a l\

B:. \2-? N

DELORO

WHITNEY ^ . H 7

t/ ^ *^

*

\

— DPF : DESTOR- PORCUP1NE FAl

\ ZONE

\ 0 5

\ KM

PUISSANCE

Figure 2-Location ot tormer and presently producing mines, and the Desior-Porcupine Fault Zone in me Porcupine camp, Tne mining properties" are: \

Producing Mines \1 -Dome.2 -Mcintyre (Pamour Schumacher property i.3 -Hollinger i Pamour Timmins property t.4-Pamour #1.11 -Westfield Minerals t formerly Coniaurum; Pamour option l.19-Aunor (Pamour #3 Minei.20-Delmte. Former Producers5-Hallnor.6-Broulan Heef7-Hoyle8-Hugh Pain.9-Banner Porcupine (formerly Canusa).10-Uavidson-Tisdale.12 -Consolidated Gillies Lake.llt-Moneta.1-1 -Vipond.15-Paymaster Consolidated.16-Preston.17 -P'ulU-r Claim i Edwards rnaft).18 -Komfield building Corp. Ltd.(Buffalo Ankerite Mine: Pamour option).21 -Kenilworth.22-Desanlis23 -McLaren-Porcupme.24-Faymar.25 -Porcupine Lake.

* For simplicity, the traditional names of mining properties and prospects, as listed by Fergu-son f t a! ' IMHi and Cnrlsnn * )W7i. :m- usi-H__^__^___FIGURE l- Location of the Puissance Claims, Deloro Township, Ontario,

In Relation to the Gold Mines of the Timmins Area.(Base Sketch Map by the Ontario Geological Survey)

l AK'rl fslsOURi l K IAH^ |OH\ l KIKUAN

FIGURE 2- The Puissance Claims, Northeastern Deloro Township, Ontario.

l AKI M KlsOUkCl \ss( K IAl|s , KIK\\ \\

LOCATION, ACCESS

The Puissance claims are in the northeast quarter of Deloro Township about 6 miles (10 km) southeast of the Town of Timmins and about 4 miles (6 km) south of the Town of South Porcupine, but are within the Regional Municipality ofTimmins.

The ground is best reached from either Timmins or South Porcupine by means of a paved road known locally as the Back Road, which connects the two towns. From this road), at the old Buffalo Ankerite minesite, a dirt bush road known as the Faymar Road (which leads to the Faymar Mine) may be taken a distance of about rk m iles (2Vzkm) southward to where the Road to the Puissance claims begins. The Faymar Road is

4currently being rebuilt to accomodate redevelopment of the j old Faymar Mine. The Puissance road is now in the process of! rejuvenation to bush road quality, and travels eastward a j distance of about l'/? miles {2 1/? km) to the west part of the 'Puissance ground. j

iAlternatively, a road which travels southeastward fromi

the town of South Porcupine known as the Carshaw Road or Langmuir Road may be taken to the northern part of Shaw Towns- ship, from where a dirt road leads westward to a dam built |

!

by Dome Mines Limited about three quarters of a mile to the ! northeast of the Puissance ground. From here the ground may!bereachedonfoot. i' i

An old trail is marked on the claim map of Deloro Townr ship leading from the unpatented (Macioli) claims of the Puih ssance Corporation a distance of about 2 miles (3 km) north-; westward to a power line which crosses the Back Road at the old Paymaster minesite east of the Buffalo Ankerite. This trail is now too deteriorated and flooded to be of immediate use, but it might warrant restoration in the future.

Trails and roads east of the property are now no long-

I \KIH RI s()l Kt i \SM H l Ml K:K\\ \N

er in existence owing to flooding of the terrain caused by the building of the dam by Dome.

CHARACTER OF THE GROUND*

The claims are underlain by enormous expanses of bare rock separated by patchy areas of alder swamp. Mixed pine and spruce trees with intermingled tamaracks near the swamp areas alternate with deciduous trees, both in the swampy areas and on the northern claims where poplar and birch trees are common. The relief is low to moderate, being con trolled by hummocky areas of outcrop, except in the extreme east edge of the property where the ground gives way rapid ly to a broad water-filled swamp oriented north-south which is believed to be underlain by a major structural lineament known as the Burrows Benedict Fault. This is immediately j off the property, but two branch faults appear to cross the ;ground. j

ijGENERAL GEOLOGY j

The Destor Porcupine Fault which trends nearly due north' east, passes a little over half a mile (l km) north of the j claim group's northerly limit. This fault separates the rocks of the Timmins area into two main groups, the Tisdale, in whichsuch mineral deposits as the Dome, Hollinger and Mcintyre

i occur, and the Deloro, in which deposits such as the Faymar 'and McLaren at one time occur. Rocks south of this fault havenot received the attention they deserve until recently, whemthe high price of gold made several areas in which low grade!gold mineralization was known to exist, attractive. j

iThe rocks consist of gently north-dipping andesitic and

rhyolitic lavas with felsic and intermediate fragmental compf onents and metasedimentary rocks, including iron formation.These rocks have been intruded by stocks of granite and por-ji phyry and younger sheets of diabase oriented either north-

\klll RIX )LK( l \sxX l Ml ' ! is i kiKU AS

south or east northeast.

Except for the diabases, which are younger, the rocks are all of Archean (Precambrian) age and at least 2500 mill-j

tion years old.

GEOLOGY OF THE CLAIMS

Figure 3, page 8, is a sketch map made to show the general geology of the claims. It is compiled from:

a. a summary geological map made by Irvin Porcupine Mines in 1933. j

b. observations made by the writer in 1984, and 'c. interpretations of geophysical surveys also made in i

1984. jIt is not intended as a complete geological map as many iimportant geological parameters are missing as they have notyet been properly defined. [

The ground is underlain almost entirely by intermed iate lavas of Keewatin (Archean) age. These dip northward at an angle of about 45 0 and strike nearly due east-west. Within these lavas occur several layers of highly magnetic iron formation and at least one zone of non-magnetic iron formation. A layer of coarse volcanic fragmental rock crosses the property near the centre of the south claims.

Three bodies of granitic porphyry are shown and a near ly north-south-striking body of diabase is indicated, this latter being inferred from ground magnetic data. Three nearly north-south-striking faults are shown. That to the ' east, known as the Burrows Benedict Fault was compiled from! maps published by the Ontario Geological Survey. Two others, termed here the Powell Fault and the Mascioli Fault were deir- ived by interpretation of geophysical surveys. The inferred diabase dike probably occupies a fourth fault, also north- i south in orientation. l

______________________________________________ji \kllt Kl^( )L KC l \v.OUA!l^ i* "! IN , MKU AN

MILEO h-

IF IF IF

SCALE

II

II

IF

r \—— — 1

LJ.

Oa.

IF

LEGEND:

FRAGMENTAL ROCKS

DIABASE (Geophys- ically Indicated)CARBONATE ALTERATION! IRON FORMATION PORPHYRY

FIGURE 3- Geological Sketch Hap, Puissance Claims, Deloro Township. Includes geo physically indicated or interpreted material as well as compiled and observed data. Claims underlain by andesitic or basaltic rock, except as indicated above.

There are 2 sets of drill holes plotted: Holes 1-7 in the SW claim, and Holes 1-19 (of which the locations for Holes 6-9 are on Figure 4).

The Locations of Holes IR 1-IR 10 are shown in Figure 4.

\Klli RI SOI Rt l \V^(H l M l

The most interesting feature from a gold prospecting viewpoint on the ground is the occurance of several bands of carbonate alteration containing quartz veins and gold values. These bands are indicated on the accompanying Fig ure 3 by dotted lines whi*ch show the units trending across the southern (patented or Powell) claims in an east-west or northeast direction. Locally within the bands occur green layers of fuchsite mica, giving the rock a distinctive apple green colour on the fresh surface.

There are several general reports covering the Deloro Township area, including the present claims, though none shows the degree of detail shown on Figure 3. These are:

a. Ontario Department of Mines, 1938, The Porcupine Area, Map 47a,Scale, 2000 feet * l inch, to accompany report by M.E.Hurst (Vol. XLVII, Part 2).

b. Kirwan, J.L., 1968, Geology of the Precambrian Rocks in Part of the ; Porcupine Mining Area, Canada. Unpublished PhD Thesis, Univ- \ ersity of LOndon, 205 pp and portfolio of maps at 2640 feets l j inch. ;

c. Pyke, D.R., 1983, Geology of the Timmins Area, District of Cochrane,) Ontario Geological Survey, Report 219, 141 pages plus maps j and microfiche. j

These reports are of value for obtaining a general und'erstanding of the geological setting of the Timmins area andthe Puissance ground in Deloro Township in particular. i

HISTORY OF EXPLORATION ON THE PUISSANCE GROUND ,l

With the discovery of the Hunter Mine on the lake east of South Porcupine in 1908, a major gold rush came to what ; is now the Timmins area in 1909. During that year the disc-i overies included the Dome, Hollinger, Davidson, and McintyreMines as well as several other promising occurances were found.

l The patented claims cf the Puissance group were stakedon October 30th, 1909 by Herbert J. Dixon who recorded his claims on November 3rd, 1909 and transferred them on Dec-

iember 9, 1909 to F.A.Day who transferred them to Francis Pow,i ell on September 21st, 1910. The ground is therefore known!l AKIN KISOL KU \^OU\lls !OHS i KIKU \N

10

as the Powell claims (information from Ralph Allerston of Timmins, 1984).

The following information was extracted from File T-671 in the Assessment Files of the Ontario Geological Survey in Timmins.

Considerable trenching and pitting seems to have been done on the ground in the 1909-1911 period, for J.Obalski in 1911 reported on the claims as follows:"Three parallel veins have been found on this property but the princip al work has been done only on the No. l vein in the North and it is the only one that I have examined. This vein, or rather belt, runs East 10 degrees North and crosses the property for its entire length, three-quarters of a mile. The vein matter shows a considerable width at the surface reaching in places to 40' and 80'. Surface crosscuts ; have been blasted at quite regular intervals, and two vertical shafts i 6"z by 10' have been sunk about one-half mile apart on the hanging wall! zone at least 15' to the north of the surface outcrops. At a depth of' 50' crosscutting has been done in both shafts towards the south and has crossed through the same material as at the surface. These cross-; cuts have been extended respectively 36' and 26' from the shaft. |"By crushing and panning in many places along the surface outcrops, i good colors of gold are found. At the Shaft No. l there is an expos- : ure of native gold which is as spectacular as any other in sight in ; the Porcupine district. There is a quartz vein 3 to 4 feet in width ! and visible for 18' to 20' which is loaded with particles of gold and j remarkably rich specimens have been obtained therefrom. You will und-; erstand that I have not assayed these rich specimens because their | high value is apparent. I have taken a certain number of grab samples^ but intentionally at the places where there is no gold visible with a i view to knowing how the gold was distributed."WHITE QUARTZ AT THE SURFACE NEAR SHAFT No. l GREEN ROCK WITH SMALL VEIN OF QUARTZ END OF THE DRIFT, SHAFT NO.l AT DEPTH 50 FEET FIRST SURFACE TRENCH (1200 FT.W OF SHAFT NO.2) SECOND SURFACE TRENCH (600 FT. FURTHER EAST) THIRD SURFACE TRENCH (300 FT. FURTHER EAST) AVERAGE SAMPLE OF DUMP OF MATERIAL SAID TO COME

FROM THE ENTRANCE OF THE DRIFT CROSSCUT IN VEIN 600 FT. EAST OF SHAFT NO.2 ABOUT

3-4' DEEP BY 45' WIDE IN VEIN MATTER

0.06 Oz Gold/ton0.051.060.160.320.20

0.28

0.41"Another exposure of free gold has been found in the vicinity of the last trench. If we consider the above facts and the way they have been taken we come to the conclusion that gold has been disseminated in the vein in relatively fair amounts and besides is concentrated very likely in form of rich chutes in places.........."

•VKIH KiMKki KiKU \N

11

Mr. Obalski's report (the first and last parts of which are not reproduced here) contains a sketch map of the patented claims which shows the main alteration zone trend ing across the ground, connecting Shafts l and 2, and two other zones on claim ME29* as well as a large area of carb onate alteration in the northwest of claim ME54 which does not appear on later maps.

Mr. Ralph Allerston, of Timmins, former owner of the claims states in a summary given to the Ontario Geological Survey, "There are two short shafts on the property aboutone-half mile apart. Where the carbonate zone is much int-

i ersected by quartz veins gold values to the value of 0.7ounces have been indicated for a length in one section of : about 200 feet and over a width of four and a half feet". ;

In the 1919-1925 period considerable additional work was done on the ground by the Powell interests, including the explorat ion of the large quartz porphyry mass in the southwest of the claims and the discovery of a sulfide outcrop about 8 feet wide and 200 feet long that panned well in gold. This information is in a letter dated April 6, 1938 from Erie i Canadian Mines Limited. The sulfide outcrop was most likely the iron formation that was later drilled. The porphyry is rimmed by drill holes (see Figure 3) numbered XI thru X7 which nust have been put down at this time. Although their number suggests that some success was obtained, there is no information available at the present time as to what these holes intersected.

Irvin Porcupine appears to have acquired the ground

Throughout this report all values for gold have been converted from . dollars per ton to Troy ounces of gold per ton of rock, based on the l value of gold before 1935 of S20.00 per Troy ounce. The value in \ 1921, for example, was 520.67. Many companies continued to use the j old values after 1935 and even to tnis day, Dome Mines Limited, by quoting in pennyweights, continues to do so. It is not certain, how-' ever, what conversion factur should be used for Mr. Allerston's, whose original quote was "514.00". See below, page 14 for similar : figures quoted in the Financial POst._____________ ___j

l \KH i K: -i )l K( l \SM. x l \l i - ;' 'i *\ : - .i;\\ \\

12

before 1933, the earliest dates on the Irvin Porcupine maps in the Assessment Files in the offices of the Ontario Geol ogical Survey in Timmins. These maps show 19 drill hole locations,

a. into the gold-carbonate zone in the vicinity of the No.l shaft (Holes l, 2, 3, and 4),

b. into a curved, northwest-trending band of iron formation cut by quartz veins and assaying in gold, and

c. into the porphyry body in the southwest corner of the ground (Holes 15, 16, 17 and, into a second porphyry, Holes 18 and 19)

These holes are shown on Figure 3. For most of these drill holes, no log or assays are available. However, the geological map in File T67 shows some assays for the drill holes that went into the iron formation. These are:

(?) 0.89 over 2' within 0.39 over 6' 0.025 over 10 feet. 0.035 over 2 feet. Trace TraceTrace and Trace.

This, admittedly limited and undependable information would seem to indicate that only the southern part of the iron formation, near where it intersects the carbonatizec rocks, assays well in gold.

An assay sheet survives as part of interest shown in the ground by Erie Canadian Mines, Limited dated June 3rd, 1938 on Sylvanite Gold Mines stationery. Labelled "Powell Property DAC, Special F-E",it gives some assays: Tr, 0.02, Tr, Tr, Tr, 0.04, and 0.04. In a covering letter dated April 6, 1938, William Moot of Erie Canadian recites the history of the ground as obtained from a John Macpherson of Toronto who had worked on the ground when it was called the McKenzie Gold Mining Company. The presence of some very

i \RI i l K! M X Ki l \SM H l M l -^ K i f t\ ! KIKU '^

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HOLEHOLEHOLEHOLEHOLEHOLE

691011121314

J

13

high grade gold on the property is indicated,a. in the old, No. l, shaft,b. in ankerite dyke No. l, at many points along its strike, and.c. "about 100 feet east bf the porphyry-ankerite contact

and opposite the No. l or west shaft".

A report dated April 21, 1938, by D.A.Campbell for Erie Canadian describes the property, then in a state of wilderness and mentions that "a number of grab samples were taken but assay results were not of any value".

In 1939 Irvin Porcupine carried out more drilling, this time concentrating on the iron formation. Their drill holes, IR1 through IR10 are shown in Figure 4, page 14. Some assay results have survived:

HOLE IR1-

HOLE IR2-

HOLE 3R3-

SectiSecti

SectiSectiSecti

Secti

Secti

onon

ononon

on

on

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4 :

l :

NINITr0.0.0.Tr0.TrTrTr0.TrTr0.

Tr0.Tr

LL

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03

04

03

11

overovern

M

11

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II

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II

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II

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II

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33

193

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HOLE IR4- Section l

HOLE IR5- Section l

HOLE IR6-

"OLD 6" -

Iron Formation

Iron Formation

Iron Formation

0.114 " 9 1/* 1 Tr " 8'

T r " 4'

No assays given

No Assays Given.

Iron Formation

l \klH KI^H W l H M !N 1 KikU \\

14

a SHAFT No.l

200 f

SCALE: FEET

FIGURE 4- Locations of Irvin Porcupine Diamond Drill Holes IR1-10, Puissance Claims, Deloro Township. Shaft No. l is shown at Left for Location. See Also Figure 3: Holes 6-8 and 10 of an earlier set of drill holes are shown on both Figure 3 and Figure 4.

\kll )L

15

HOLE IR7- SectionSectionSection

"OLD 7" Section

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HOLE IR9: (Assumed

1:2:3:

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1:

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IRON FORMATION

IRON FORMATION

A quotation from the Financial Post (undated but to be found in the OGS File T67 already mentioned) will bring this historical section to a close: "Irvin carried out diamond drilling in 1939 with 200 feet of ore indicated averaging about 514.00 (either 0.7 or- 0.4 ounces of gold to the ton depending on whether S20 or S35 gold was being considered) across four and a half feet. In June, 1945, property leased to the Buffalo Ankerite Gold Mines Limited calling for expenditure of at least 550,000.00 within two years and the priviledge of forming new company. Buffalo Ankerite would own 75* of the capital and Irvin 25%". Nothing further, however, seems to have taken place with regard to this option.

In May, 1984, the writer visited the property and found Shaft No. 2 as well as much of the carbonate zone westward from this. At this time a total of 17 rock sample Si

j\Klt i k! M H Ki l \SM H MK'U

16

were taken for assay. Later, when Shaft No. l was found, 10 more samples were taken for assay, but the results from these 10 are not yet available. Assays from the 17 were:

e

6101- Quartz-Carbonate from trench E of Shaft No.2 0.1466102- Carbonate from trench on Cross Line 41E - trace6103- Fuchsite and quartz from line 40E at 2N trace6104- As above without Fuchsite 0.0186105- Quartz carbonate from Shaft No. 2 0.0206106- Quartz-carbonate rock from waste pile Shaft 2 0.0106107- Contact zone from above material trace6108- Waste pile, Shaft 2: Carbonate Rock trace6109- Fuchsite zone west of Shaft 2 trace6110- Iron Formation, Line 36E at 2+50N trace6111- Carbonate from XL34+90 @ 1+70N trace6112- Carbonate from XL 34+00 @ 1+OON trace6113- Carbonate, XL 31+00 at base line trace6114- Carbonate with 35!* Fuchsite, 29+00 @ BL trace6115- Quartz vein with minor Fuchsite 18+OOE IN trace6116- Carbonate from line 28+50E, 2+80N 0.0066117- Massive pyrite and carbonate trace

The above samples were "grab" samples taken where conditions permitted it. The trenches are all heavily grown in with trees and partly filled with earth, and the important carbonate rock deeply weathered so that it is, for the most part, obscured. The sampling and assaying does indicate that portions of the carbonated rocks assay well in gold, but the zone of carbonate rock and Fuchsite does not assay in gold in general. It will be necessary to bare these rocks by stripping and washing and geologically map and sample them, in order to determine the presence of gold in these rocks and its relationship with the lith ology and structure as well as the stratigraphic, intrusive, and metamorphic history.

l.Aki M KiSOUKt. I -\sSOl l All IONS l KIKWAS

17

MINERAL POTENTIAL OF THE PROPERTY

Interest in the Puissance ground has extended back in time to 1909 when the patented claims were first staked. It is one of the oldest properties in the Porcupine camp, and the interest in it is now, as it was in 1909, for gold. However, the presence of a coarse felsic fragmental rock on the property also indicates that the potential for mass ive sulfide mineralization (copper, zinc) also exists.

The indications for the presence of gold mineralizat ion, potentially in mineable quantities, are:

1. the presence of one {possibly as many as 5) horizons of carbonatized volcanic rock trending east-west across the ground and dipping northward. The main horizon, which is in places as much as 80 feet wide, contains quartz veining with which gold values are associated. Reported values from grab samples have assayed as high as 1.06 ounces of gold to the ton of rock, and a sample taken by the writer assayed 0.146. The possibility exists that this main carbonate zone, or one or more of the other reported zones, hosts a mineable gold deposit.

2. the existence of several small bodies of quartz feldspar porphyry. The contacts of porphyry bodies with the surr ounding country rock have long been recognized as the site for occurances of major gold deposits, particul arly in the Timmins-Noranda area. At least 10 drill holes are known to have been put into the north and east contacts of one of the Puissance porphyrys, but it is not known what encouragement was obtained.

3. the existence of a gold-bearing iron formation as well as several iron formations elsewhere on the property whose gold content is at present unknown. Drill indic ated values in the known iron formation range up to 0.13 ounces of gold per ton of rock along a drilled thicknessof 21 feet, as reported in drilling in 1939.

l -\KII1 KISOUKi l -\ss( H )\ t\ i kim

18

RECOMMENDATIONS

1. As soon as possible, the entire'ground held by the Puissance Corporation should be geologically mapped so as to determine the geological environment on the claims, to map the alteration zones and the porphyry bodies, to locate and trace the various iron formations, to define the felsic fragmental rockunits, and to serve as a framework for locating and following gold-bearing units and structures that are now known or will be found in the future. This geological mapping should be undertaken in two phases:a. reconnaissance geological mapping of the entire

claim group at a scale of l inch to 200 feet. ^""Estimated cost..........'.S 15,000

b. detailed mapping of zones of interest as they are exposed by stripping operations, at a scale of l inch to 100, 50 or 10 feet, as is appropriate for each one. For the Main Zone (see Recommendation 2) a scale of l inch to 50 feet is recommended, at an

Estimated cost of........S 10,000

2. The Main Zone of carbonate alteration should be exp osed for sampling, sampled, and assayed. To accomp lish this the following work will be necessary: a. restore the access road to the site. This has

already been accomplished to "trail" quality at a cost of............................,......S 18,000

b. remove the trees and bushes from a 20 acre strip of ground over the area of interest.

Estimated cost...........! 28,000c. remove the overburden from, clean out the various

trenches, and wash the rock. Because of unknown variables in the overburden the completed work cannot be priced.

Suggested budget.........S100,000

l AKI H KlSOUKi. l AV-CX l K)H\ l K.lk'UAN

20

will be apparent as the work progresses.Suggested budget.. 50,000

The above recommendations are designed to bring the property to a point where one or more gold-bearing bodies are indicated. Total cost of this phase is estimated at just under S500,000. As warranted by the results of this work, additional work will be recommended for the purpose of defining ore zones, determining tonnage and grade, and developing a mine, if warranted, on the site.

Respectful l y submitted,, ''vV

t *'

t

At Timmins, Ontario, May 23, 1984

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