: Other [ j. Footage. 100m. (O Pa m. (D Pa m. (D Pa m

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1 52006SE KAWASHE LAKE 00 DIAMOND DRILLING AREA: KAWASHE LAKE REPORT NO: 33 WORK PERFORMED FOR: St. Joe Canada Inc RECORDED HOLDER: Same as above [xx] : Other [ j Claim No. Hole No. Footage Date Note Pa 868 MN m July/86 (O Pa 866 MN m July/86 (D Pa 868 MN m July/86 (D Pa 860 MN m July/86 (D NOTES: () #W , filed in Oct/88

2 DIAMOND DRILL RECORD HOLE LOCATION LATITUDE ELEVATION STARTED MN OOW July 6, 986 Muskeg Lake Property LENGTH DEPARTUR AZIMUTH 00m 6+30N 2050 DIP July 7, METERS Om 50m 00m DIP AZIMUTH FOOTAGE DIP AZIMUTH MOLE Mq86 REMARKS LOGGED BY A. H. Vogt NQ ' ^ O LANGfllOGES RON 366t CASING DESCRIPTIVE LOG finegrained, weakly foliated (CAA foliation = 52 ) dark green coloured minor banding between 3.30 and 3.38m with JsotMd.de of cherty, greenish and grey silica and **lt disseminated pyrite magnetic susceptibility 200 strong carbonatization in the flow immediately adjacent to the underlying quartzfeldspar porphyry FELDSPAR PORPHYRY DYKE or Apophysis: pinkishred to greenishgrey strongly silicified with quartz pseudcmorphs after feldspar phenocrysts (zoning of feldspar recognizable, feldspar phenocrysts up to 0.5cm) Upper Contact at CAA = 90O Lower Contact at CAA ^ 67O magnetic susceptibility to 500 irregular fractures filled with quartz and associated with sulphides (euhedral to anhedral pyrite) ; pods and stringers with magnetite and tourmaline (?) overall sulphide content ~ls QuartzFeldspar Porphyry Mafic Volcanic Flow "N Chilled Marcrin f QuartzFeldspar Porr lL^ ^ ^^^\\^k\ ^ MaficVolc #47 ^ ^ ^^^^ 3y ^S silicafilled fracture with associated disseminatec pyrite is "retracted" at the contact lyry mie i si di th 47 'X, IDES f, \ Mpfpfacrp 'V7 /T ' **x/ j Uow Lica: "i lied i ractur* ;semii lated pi rite i: 2 con act 4.84 * * n ^ r^ '. " F ' C 'i r\j \^ 6.39 TAL ^ ^ ^7 4 with ; "retn.55 z, :ted" Au ASSAYS ted at * ASS R E OZ/N 3SSVEf CFFK AY24 C E l OZ/N T ~''. ES c ^OC""* V E D ji i i 0* I

3 3 0 5 *o 07 t o* ecc O* CO *U 8 cc g 5 DIAMOND DRILL RECORD F M ^ M H : intercalation of banded, carbonatized mafic flow carbonatized close to the contact with the overlying quartz feldspar porphyry f ine to mediumgrained weakly foliated minor fracturing with calcitequartz infillings magnetic susceptibility = 200 MAFIC DYKE: irregular contacts, partly parallel to Core Axis hornblende laths up to 4mm calcite schlieren fine to msdiumgrained (grain size increasing down hole; mmsized feldspar matacrysts and chlorite clots) partly banded weak to moderate foliation traces of sulphides along foliation planes partly fractured with quartzcalcite infillings : banded; CAA = 59O : minor shear zone with associated traces of sulphide and minor biotitization CAA = : fine, irregular banding (CAA. = 720) crosscut by calcitefilled fractures and calcite schlieren traces of sulphides biotitization magnetic susceptibility = 200 ^^ */ banding; fine, microfolded bands offset by calcite :} filled fractures, biotitization magnetic susceptibility = : brecciation; calcite infilling : calciteepidotequartz vein CM = ^i^ NAME OF PROPERTY. HOLE \ SOCPM tots ^^m ^ i ja&c H TAL 0.67 ". AU ASSAYS i \ b ^mm 0, * ^^ O t 'M MM

4 i DIAMOND DRILL RECORD NAME OF HOLE Muskeg Lake Property MN8684 SHEET 3 of 5 XSULPM IOCS neterage TAL AU t. ASSAYS Ol/ron OZ U i S o o bu 0 l0 z C d 45.0: * AMPHIBOLITIZED mediumgrained, massive l2nmsized chlorite clots :^) irregular quartzcarbonate structures with inclu : C sions of chlorite schlierens :) MAFIC INTRUSIVE (Dyke or Apophysis) : contact 320 CAA porphyritic texture with nrasized hornblende and biotite crystals in dark green to black matrix; no preferred orientation of hornblende laths fractures filled with calcite in parts strong carbonatization diffuse Lower Contact with incorporation of f ragments/xenoliths of amphibolitized mafic flow medium to finegrained with moderate foliation fractured" with calcite infillings : strongly fractured MAFIC INTRUSIVE (Dyke or Apophysis) : similar to m strong carbonatization : contact subparallel to Core Axis Lower Contact O CAA finegrained, weak foliation; minor fracturing : broken core : incipient Banded Iron Formation with fine, slightly folded and disrupted bands; calcitefilled frac tures; cut off by the contact to the underlying intrusive CAA. 3 biotitization 4742 s tefic Pod ; with o lcite \ \""*"^r;3 7 5 " *r LYJauw 8u^ \\w\\\\ ~Z^\\ \ \ \ \ \ Volemie Fl( )w Foliation 5.0 ^^^^^ \ivum\\\ ^?s' : : i"*v*. :N ^u Carbor atized biotit s porp intrus ion S VTV Ss."i "~ " ' P^^ Com ^ ^ ^ i V'V " fi."^ :V:" * *. act l...l, homolende lyriti im^*m^f mm*mm mm^mf

5 DIAMOND DRILL RECORD NAME OF PROPERTY Muskeg Lake Property^^^ HOLE NO MN8684 SHEET NO 4 of 5 5 ** O *D O O* iot tn UJ 0 O o: O I 5. 2! 5. 6* 52.2] 52.7: 53. 0( OC 62. 6S 62.9 MAFIC INTRUSIVE (Dyke or Apophysis) : similar to m and m strong carbonatization BANDED IRON FORMATION (SulphideRich) : contact parallel banding of Banded Iron Formation mmfine bands of sulphides (pyrite, pyrrhotite) alternating with siliceous, calcitic,, chloritic bands CAA. banding 80O magnetic susceptibility up to 35,000 bands slightly to strongly folded to totally disrupted FELDSPAR PORPHYRY: zoned feldspar phenocrysts up to 0.5cm in dark grey matrix contact parallel banding of Banded Iron Formation BANDED IRON FORMATION: similar to m but only traces of sulphides banding CAA. = 69O finegrained, moderately foliated slightly fractured partly banded : banded (70O CAA) : mediumgrained section with chlorite clots and feldspar metacrysts gradual transition no obvious contact BANDED IRON FORMATION: rrmfine banding, slightly folded magnetic susceptibility to.500 calcitic, chloritic, siliceous bands pyrrhotite occupies narrow fissures parallel to the banding traces of chalcopyrite ~^ sulphides fragment of mafic flow incorporated into the Banded Iron Formation CM = 800 X SOtfM IOCS M i mmmmm necerage TAL x AU ASSAYS x OZ W ; ' O*. W ^ K*

6 DIAMOND DRILL RECORD NAME OF property ^jljskeg Lake Property HOLE MN8684 SHEET. * SULPM IOCS TAL \ AU ASSAYS t OZ/N ozroh. ', V *o *6 s o* io* c/) K i oz MAFIC VOLCANIC FIX*?: similar to m fine to mediumgrained banded sections fractured with mainly calcite infillings minor biotitization around some of the fractures partly strong carbonatization moderately to strongly foliated : irregular pod of silica, calcite, feldspar cut by a younger, calcitefilled fracture subparallel to the Core Axis ,08: banding CAA = : banded and strongly carbonatized flow abundant bands of calcite : greyquartz vein : banding (CAA = 62O) and strong carbonatization : quartz vein CAA ^ 80O : banding CAA = 79O.v.. minor offset by small fractures : banding offset of the bands by calcitefilled fractures subparallel to the Core Axis : zone of intermittent banding h to lorn wide calcitequartz veinlets with traces of pyrrhotite and chalcopyrite CAA = 6568 minor biotitization as envelopes of some of the veinlets : quartz (calcite) vein CAA = 650 END OF HOLE ro*m i ^H mmmm mmmm mmmm

7 "I. DIAMOND DRILL RECORD Muskeg Lake Property NAME OF PROPERTY 96m o c un rawooj.0* i nr A'TION, AT,T,,nr 8+OOW ELEVATION ^TARTFO July 2, 986 LENGTH ^"' ll nfparthrf 8+65N AZIMUTH 205 ot p 45 r.nismim July 3, 986 METERS Om 96m DIP 45" 43" AZfMUTH 205" FOOTAGE DIP AZIMUTH HOLE MN8689WFr NO i pf 6 REMARKS ^^ ^ ^ LOGGED BY A.H VOCft to *2 *6 O O cc O 3 8 ec O C CASING/OVERBURDEN ' DESCRIPTIVE LOG finegrained, feldspar metacrystic /' well foliated, small feldspar crystals aligned parallel to the.' "*. foliation intensity of foliation increases down hole ^ moderately chloritic slightly fractured with calcite infillings; mmwide chloritized haloes around fractures minor biotitization associated with fractures pyrite on fracture planes \ /. locally weak silicification and sericitization \A CAA foliation at 6.50m 67" CAA foliation at 8.20m : strong biotitization "MYLONITE": light brownishgrey silicification and strong sericitization intensely foliated with CAA of foliation ^ 67 0 rare bluishgrey quartz eyes stretched quartz lenses aligned parallel to foliation : core in core box probably disorganized fragments of strongly sericitized "mylonite" and highly magnetic (Magnetic Susceptibility up to 65,000 SI Units x 0~ ) with mmwide bands of magnetite alternating with calcitic, siliceous and chloritic bands contact at 0.45m between banded formation and underlying "mylonite" x, r^^ ^ "' Mp f" P 35* p" ~'^"^N " '^"v " '~ f ~,.^. ^^ \ 'V/jY" '~* ' * : :'/ \w >>~~^. ^^\ ^L^.? : tjj^* Yo X ''/\ ^C^ "C~t i!, : Oi /v TAL X 'r ; E s i l S AU X ~ '" ASS5 ASSAYS ff V' P c n i ~ OZ/N ~ '~O''~?~^ 5SV,E^ OFc i^" AX 24 ^ ^ \ OZ/N ^ ~ AU SI'?"" F'LE'3 363 ^ v e D Y ; l i i S ; * m i mmmm B i mmmm i M BHP

8 DIAMOND DRILL RECORD NAME OF PROPERTY Muskeg Lake MO, R MN8689 SHEET NO 2 of 6 X SOLPH, IDES "TTeTerage" AU ASSAYS O Z M O Z M "MYLONITE" UPPER MARKER HORIZON: stronger siliceous, less sericitic than m light brownishgrey to dark grey well foliated CAA = 67" finely banded with siliceous and sericitic bands quartz lenses and quartz eyes small clots with garnet surrounded by siliceous halo BANDED IRON FORMATION, Oxide Facies: Upper Contact irregular at ± right angle to Core Axis; cross cutting the foliation in the "mylonite" banding CAA ^ 65" mmwide magnetiterich bands alternating with siliceous, calcitic and chloritic layers minor epidote pyrrhotite and pyrite at fissures parallel banding and dissemina ted; overall sulphide content 2/6; partly limonitic magnetic susceptibility up to bands mostly complexly folded MAFIC VOLCANIC TUFF: finely layered CAA = 670 pyrrhotite and traces ofchalcopyrite along bedding planes and traces, partly limonitic mmwide quartz and calcite veinlets transitional Upper Contact sharp Lower Contact with CAA ^ 48" AMPHIBOLnTZED coarsegrained clots of partly to completely chloritized hornblende up to 0.4cm in diameter massive chloritic partly weakly sericite or epidotealtered groundmass fractured with calcite infillings and associated chloritic haloes around the fractures at approximately 7.2m transition into a well foliated amphibolitized mafic volcanic flow chloritic clots stretched to lenses parallel to the foliation CAA foliation at 7.50m ~ 75" io

9 ^. ; j^jf^ s 5(D O zg s CO tu ^ 8 W i! DIAMOND DRILL RECORD aphanitic to finegrained; feldspar metacrystic fine (<mm) clots of chloritized hornblende approximately 2'fc chloritic matrix well foliated; CAA of foliation = 65" slightly fractured with calcitic infillings and chloritic haloes. around fractures : dark : grey, silicified with mmsized feldspar metacrysts in aphanitic matrix mmquartzcalcite veinlet at CAA = 2" : finely banded intercalation with CAA = 60 0 biotitization : finely banded intercalation contact parallel to foliation = CAA 65" calcitic bands :" ; i : broken core f * : quartz vein parallel to foliation bluishgrey quartz with pyrite flakes along partings AMPHIBOLITIZED similar to m massive to well foliated medium to coarsegrained clots of partly to completely chloritized hornblende up to 0.5cm in diameter fine feldspar metacrysts locally weak sericitic alteration chloritic matrix partly strongly fractured with calcite infillings decreasing grain size and increasing intensity of foliation down hole CAA foliation at 34.50m = 66" ' : Feldspar Porphyry Dyke JUpper.and Lower Contact CAA ~ 42" 205& zoned feldspar phenocrysts with an orange MO. l NAME OF PROPERTY HOLE MN8689 t SUtPH tots mmmm Muskeg Lake Property SHEET MO 3 of 6 TAL Au x x ASSAYS O Z, N.. O l row L

10 DIAMOND DRILL RECORD NAME OF PROPERTY Muskeg Lake Property tint and up to lcm in size in a dark grey. siliceous matrix pyrite disseminated and on fracture planes biotitization in flow at the Upper Contact transition into an aphanitic to finegrained mafic flow similar to m intensely foliated; chloritic fine feldspar metacrysts aligned parallel to the foliation CAA foliation = 65O minor grey quartz veining disseminated pyrite and discontinuous bands of pyrite along small fissures parallel to the foliation slightly fractured with calcitic infillings locally carbonatization WO. HOLE a SULPM IOCS MN8689 ^^^r ^ 4 of 6 SAMRL.E rnom TAL SHEET. AU ASSAYS x 0. 0 M : abundant calcite wisps parallel foliation biotitization, foliation CAA^ 64" e c a c ft Z l l n H 5 c C QUARTZ VEIN: Upper and Lower Contact CAA = 65" white to light grey quartz.....^ pyrite, pyrrhotite and chlorite along partings in the quartz fragment of carbonatized flow surrounded by calcite in the quartz vein "MYLONITE" LOWER MARKER HORIZON: intense foliation CAA foliation = 67" dark grey colour strong silicification, moderate sericitization : change in colour to a light yellowishgrey strong sericitic and less siliceous quartz veining parallel foliation CARBONATECHLORITE SCHIST: Upper Contact parallel to foliation CAA = 62" strongly foliated with abundant wisps of calcite parallel to foliation mmm mmmm mmmm 0.46 l.oo

11 DIAMOND DRILL RECORD NAME OF PROPERTY.. Muskeg Lake Property HO, P N0 MN8689 SHEET. 5 of 6 MO. SUtPM IOCS neterage TAL AU * x ASSAYS or, W O Z. M decreasing amount of carbonate down hole : pervasive carbonatization and biotitization deformation intensity decreased as compared with the overlying "mylonite" ^fc ^^^ i S o 0 V) Hs oz5 t transitions to a sheared amphibolitized mafic volcanic flow finegrained, fine feldspar metacrysts variable amount of fine chlorite clots well foliated, partly banded feldspar metacrysts and chlorite clots stretched parallel to foliation frequent calcitequartz veinlets : dark grey quartzcalcite structure contacts parallel to foliation CAA = 65" weakly magnetic BANDED IRON FORMATION: magnetic susceptibility up to 5,000 CAA of banding alternating siliceous, magnetite rich, chloritic, minor calcitic bands : pyrrhotite, pyrite, traces of chalcopyrite along fissures parallel to banding and along crosscutting fractures overall sulphide content 205^ " AMPHIBOLITIZED finegrained with increasing grain size down hole to mediumgrained flow clots of chloritized hornblende fine feldspar metacrysts well foliated few quartz veinlets intercalations of finegrained mafic flow; * ~.~ MMH

12 DIAMOND DRILL RECORD NAME OF PROPERTY Muskeg Lake Property HOLE MN8689 SHEET NO 6 Of 6 XSOLPH IOCS neterage TAL x Au i ASSAYS O I. N O2 W j CARBONATIZED gradual transition from overlying amphibolitized mafic volcanic flow strong carbonatization in the form of abundant calcite wisps strongly chloritic talcy aphanitic to finegrained partly fine feldspar metacrysts chloritic well foliated with CAA of foliation = 65 0 small intercalations of amphibolitized mafic volcanic flow with mmsized clots of chloritized hornblende fractured with calcitic infillings, locally strong carbonatization with calcitic wisps related to small shear zones weakly silicified and sericitized weak biotitization associated with calcite filled fractures locally fine banding CAA ^ 75" : milkywhite quartz vein with CAA of 75 " chlorite and minor sericite along partings : siliceous structure CAA = 57" with epidote, garnet, strongly silicified halo END OF HOLE CD *o O io H I in UJ e tr 0 Z.J r

13 DIAMOND DRILL RECORD NAME OF PROPERTY MN8694 HOLE LOCATION LATITUDE ELEVATION STARTED Muskeg Lake Property LENGTH 53.6m 2+OOW 6+60N July 7, 986. AZIMUTH 205 July 8, METERS Om 50m 00m 53m DIP AZIMUTH FOOTAGE DIP AZIMUTH HOLE ^MN8694 REMARKS Jfe Pajari LOGGED BY A. H. Vogt Q LI *lo DESCRIPTI ON SUMMARY LOG CASING/OVERBURDEN MAFIC VOLCANIC FLOW FELDSPAR PORPHYRY DYKE "AMPHIBOLITIZED" MAFIC VOLCANIC FLOW MAFIC VOLCANIC FLOW "AMPHIBOLITIZED" MAFIC VOLCANIC FLOW MAFIC VOLCANIC FLOW "AMPHIBOLITIZED" MAFIC VOLCANIC FLOW /. '4, S ^ N Mpfprapp \ ".5 ' ". to P/NS x,\.w J 7c:v. Q '~* Tftc,'{ ffr ' t ''J' ^'n~ ;,! '/'l' j Q /, \^\ s'/^t^'\\^ ^Jjr ^^^"^ TAL l ^ y Z IT i! i!( T: i; i Au x ASSi ASSAYS r. i R E OZ/N JAU SU~' SStV'EN CF C ';C AY 24 C E? OZ/N 388 V E D EY i i flo *O ~ BANDED IRON FORMATION : magnetiterich banded iron formation : tuff/tuffite facies. FELDSPAR PORPHYRY DYKE BANDED IRON FORMATION MAFIC VOLCANIC FLOW BANDED IRON FORMATION MAFIC VOLCANIC FLOW END OF HOLE AZ Z O O 2 O d O Vi taj S cc 0 Z J M t

14 DIAMOND DRILL RECORD NAME OF PROPERTY Muskeg Lake Property MN8694 LENGTH 53.6m HOLE. LOCATION LATITUDE ELEVATION STARTED 2+OOW July OFPARTURF 6+60N AZIMUTH FINISHED July 8, METERS Om 50m 00m 53m DIP AZIMUTH FOOTAGE DIP AZIMUTH HOLE REMARKS No Pajari LOGGED BY A.H. Vogt GAS ING/OVERBURDEN DESCRIPTIVE LOG & s,rv?r M#* t" (* YA O P TAL Au ASSAYS K K OZ/N OZ/N aphanitic to fine grained locally feldspar metacrystic weakly to well foliated slightly fractured with calcite and quartz infillings; minor offset along these fractures pillow margins indicated by stretched (parallel to foliation) amygdules : zone with irregular quartz veining and minor brecciation. associated silicification, sericitization chloriteepidotecalcite, clots of garnet traces of pyrite CAA approximately 55O 4844 tr similar to m CAA = 680 CAA foliation at 5.50m = 6 CD *0 to (O o shear zone CAA = 05 0 abundant wisps of calcite and rare lenses of quartz parallel to foliation biotitization 2 Z g o i to UJ 8 cc O 2 <.j CAA foliation at 2.00m = 65O : strongly foliated with quartz and calcite bands parallel to foliation CAA foliation = 55O pyrite on fissures parallel to foliation at the contact with the feldspar porphyry dyke

15 DIAMOND DRILL RECORD NAME OF PROPFPTV Muskeg Lake Property HOLE NO ^MN8694 SHEET t, SOLPH IOCS neterage TAL, Au ASSAYS X or/ M 0 M FELDSPAR PORPHYRY DYKE: Upper Contact CAA = 65O Lower Contact CAA = 58 0 ID5% feldspar phenocryst in a dark grey to bleached light grey and pinkishred matrix strong silicification cmsized feldspathic clots in the silicified matrix fractured with ^ wide quartz veinlets silicification associated with these quartz veinlets disseminated pyrite, anhedral to euhedral, concentrated at the Upper and Lower Contact ^vl.% "AMPHIBOLITIZED" mediumgrained; foliated composition essential chlorite and feldspar equigranular textural appearance rare clots of chloritized hornblende chloritic matrix slightly fractured with calcite and quartz infillings and traces of pyrite CAA foliation at 24.00m = 52O j transition (decreasing grain size) into: J *o 54O ^ f o 2 g 0* f W Ut 8 o: aphanitic to fine grained well foliated pyrite on fracture planes slightly to locally intensely fractured : quartzcalcite vein associated with minor shear zone CAA = : grey quartz vein CAA = 44 0 transition to:. H

16 DIAMOND DRILL RECORD NAME OF Muskeg Lake Property MO, F K.,. MN8694 SHEET NO 3 of "AMPHIBOLITIZED" similar to m locally biotitization around fractures : quartz structure Upper Contact irregular with CAA 62 Lower Contact s CAA 48O white to light grey quartz traces of pyrite, pyrrhotite and chalcopyrite at the Upper and Lower Contact transition into: similar to' m partly feldspar metacrystic CAA foliation at 37m = 65O.06.2: milky white to light grey quartz vein CAA SULPH IOES riecerage TAL 0.30 t Au ASSAYS OZ/W OZ M : epidoterich structure with traces of sulphides CAA = 5 CD (O *6 to O t s fo : at m fine, slightly folded banding CAA approximately 45O nest with garnet : foliation and fine banding with CAA = 60O chloritic lenses stretched parallel to foliation, in strongly carbonatized, weakly silicified flow : fine banding with CAA changing from 53O to 20O down hole banding offset along small fractures : fine banding CAA = 620 OT UJ 0 LANQRIC transition into: *mtm*^f*m IMaB WHOM

17 DIAMOND DRILL RECORD NAME OF Muskeg Lake Property MOI F s.r. MN8694 SHEET 4 of 6 MO. SO L PH, IOCS necerage TAL ^ Au ASSAYS * o i, W O I W "AMPHIBOLITIZED" " similar to m partly sericitic altered : light grey quartz vein CAA 500 Foliation at 7.00m = 65O B y : ~ ' increasing foliation (crenulation foliation) towards the contact with the underlying Banded Iron Formation BANDED IRON FORMATION: : mm to cmwide magnetite, siliceous, chloritic, calciterich bands partly complexly folded CAA of banding 70O to 82O magnetic susceptibility to 20,000 pyrrhotite, pyrite, traces of chalcopyrite along small fissures and in small pods overall sulphide content S4% S4% ,:, : fine tuff /tuffite strongly calcitic possible contact metamorphic overprint' FELDSPAR PORPHYRY DYKE: 4842 s~ S i i 2 z 8o t( V) Ul ^^U? L.! ^^ Upper Contact: irregular intrusive contact Lower Contact CAA = 77O 207. feldspar phenocrysts, up to 0mm in size, in grey, siliceous matrix bleaching and silicification around small fractures disseminated pyrite 7. BANDED IRON FORMATION: similar to m finegrained; bluishgreen tint; partly feldspar metacrystic weakly foliated partly strong carbonatization associated with bleaching of the

18 DIAMOND DRILL RECORD NAME OF PROPERTY HOLE Muskeg Lake Property MN8694 SHEET 5 of 6 X SULPH, IOCS Hete*"^".0(3^ TAL * Au * ASSAYS OZ/H OZ W flow to a light green slightly to locally intensely fractured with quartz and calcite infillings and chloritized haloes BANDED IRON FORMATION: magnetic susceptibility up to 5,000 CAA of banding 80 to 850 alternating mmwide magnetiterich siliceous, chloritic and calcitic bands partly complexly folded locallized minor pyrrhotite and pyrite along fissures parallel to the banding and along fractures similar to m : partly banded strongly fractured with calcitequartz t epidote infillings partly strong carbonatization locally intensive biotitization feldspar metacrystic well foliated partly bleached and weakly silicified and sericitized CAA foliation at 07m = 50O : intensely fractured with quartzcalciteepidote infillings biotitization Foliation at.00m CAA = 65 O : finely banded CAA of banding 73076O banding offset along calcitef illed fractures traces of pyrrhotite intensive biotitization locally pervasive carbonatization minor light grey quartz veining 4850 tr

19 DIAMOND DRILL RECORD NAME OF rnorrpty Muskeg Lake JProperty ^ HOLE MN8694 SHEET NO 6 of 6 X SULPH IDES SAMRLE neterage TAL i Au ASSAYS t. O Z/ W O Z W : strong carbonatization minor quartzcalcite veining biotitization. CAA foliation at 28.50m = 60O : intensive fracturing; network of fine epidote and 4 calcitefilled fractures with small pods of pyrite, pyrrhotite, traces of chalcopyrite locally biotitization as halo around fractures : shear zone at CAA ~ 7O abundant wisps of calcite and + quartz biotitization : alternating chloritic, calcitic and bands of greenish chert CAA of banding = 6lo : quartz vein with milky white to bluishgrey quartz CAA = 770 chlorite along partings in the quartz small seams of chlorite at the Upper and Lower Contact CAA foliation at 50m " 62O END OF HOLE CO to 5to o o " o* LANGRIOGES mm**mm m^m* MBM^

20 ' DIAMOND DRILL RECORD NAME OF PROPERTY Muskeg Lake Property HOLE LOCATION LATITUDE ELEVATION STARTED MN lOOW July 8, 986. LENGTH DEPARTUR E A7 IMUTH nw i^wrn 56m 6+06N D(p 45" July 9, 986 METERS Om 56m DIP AZIMUTH 205" FOOTAGE DIP AZIMUTH HOLE MN8695^ECT REMARKS No Pajari LOGGED BY A.H. Vogt CASING/OVERBURDEN MAFIC VOLCANIC FLOW ' OESCRIPTI ON SUMMARY LOG AMPHIBOLITIZED MAFIC VOLCANIC FLOW MAFIC VOLCANIC FLOW BANDED IRON FORMATION: : tuffaceous facies : magnetiterich, siliceous iron formation : tuffaceous facies 4835 x, * MpfPT3lX Yo TAL.08 ASSAYS 56 K OZ/N OZ/N p W!C OHC LOO:OA:, S SURVEY LES rp.cc C M V i!j t. ***~l t JM I ^"* MAY S3 R.E C E! V i :. D FELDSPAR PORPHYRY DYKE BANDED IRON FORMATION AMPHIBOLITIZED MAFIC VOLCANIC FLOW END OF HOLE x^ot /Y^ r^/ f? r ~ ^^ " '' /. ^ \ s?o /.cv',, "*"~ D f T^, \ ~~ r ^~ n'' \ r; : X^ 'r 'f.,. c':,v" ^2 Vo y^ 2/ \3 ' L. j i o V) Uf 8 cc o

21 DIAMOND DRILL RECORD NAME OF PROPERTY HOLE. MN8695 LOCATION LATITUDE 24+OOW ELEVATION STARTED July 8, 986 Muskeg Lake Property LENGTH 56m DEPARTURE 6+06N AZIMUTH f^j J DIP r.n.smfn July 9, 986 METERS Om 56m DIP 45" 45" AZIMUTH 205" FOOTAGE DIP AZIMUTH HOLE MNrSfi^l25sHEET REMARKS NO Pajari LOGGED BY A. H, CASING/OVERBURDEN DESCRIPTIVE LOG SULPH % IDES Mft^pTatrp TAL K AU K ASSAYS OZ/N OZ/N ~ M"** * MAFIC VOLCANIC FLOW, Chloritic: aphanitic to finegrained partly fine feldspar metacrysts; alternating feldspar metacrystic with aphanitic/ finegrained flow weakly to well foliated slightly to locally intensely fractured with calcite and quartz infillings and associated minor biotitization 'VL/S fine (^Imm) chlorite clots '~ locally banded : fragment of finegrained, weakly anphibolitized mafic volcanic flow CAA foliation at 5.00m = 60" : calcite f i lied fractures and calcite wisps associated with patchy biotitization.75.76: cmwide quartzcalciteepidotechlorite veinlet CAA s 50" S : fine banding and strong foliation CAA = 69 s to 72 calcite bands partly carbonatization io AMPHIBOLITIZED f tt, p CO u/ a ^ g s <.j fine to mediumgrained l3rnm sized chloritized hornblende clots and laths fine feldspar metacrysts chloritic matrix massive to weak foliation weakly fractured with calcite and quartz infillings intercalation of finegrained mafic flow ' romm mmmm*rr

22 DIAMOND DRILL RECORD NAME OF PROPERTY Muskeg Lake Property HOUE MN8695 SHEET NO 2 Of 3 at 25.2: ^cmwide veinlet with epidote and minor calcite CAA rr 08" i SULPH IDES FltOM ne ter age TAt x AU ASSAYS \ OZ/W O l. M transition into MAFIC VOLCANIC FLOW, Chloritic: finegrained, partly feldspar metacrystic weak to well foliated slightly to strongly fractured with calcitequartzepidote infillings chloritized and biotitized alteration haloes around fractures CAA foliation at 30m = 65" CAA foliation at 36m = 66" : calcite (quartz) vein CAA = 63 0 Upper Contact CAA s 66 0 Lower Contact traces of pyrrhotite.,...r :. S 5 K s f vt ut 9W o BANDED IRON FORMATION: : finely banded tuff 7 tuffite CAA banding ~ 82" calcite bands. ~ strong biotitization, traces of pyrrhotite : Magnetite Iron Formation mm to onwide magnetite, magnetiterich siliceous. chloritic and calciterich bands CAA of banding ~ 78* 84" locally complex folding of the bands pyrrhotite and pyrite occupy small fissures paral lel to the banding traces of chalcopyrite, overall sulphide content "/ :. tuff/tuffite similar to m FELDSPAR PORPHYRY DYKE: Upper Contact irregular intrusive contact pink, zoned feldspar phenocrysts, imm to 2mm in size, in a dark grey; siliceous matrix disseminated pyrite and pyrite along small fractures Q.5%, euhedral to anhedral pyrite tr po ~* *# py MH f

23 DIAMOND DRILL RECORD NAME OF PROPERTY Muskeg Lake Property M, F ^ MN8695 SHEET. 3 of 3 " i ~ :.. r haloes of silicification and bleaching around small fractures mm to cmsized xenoliths of Banded Iron Formation Lower Contact CAA = 80" SILICEOUS BANDED IRON FORMATION: finely banded siliceous layers with disseminated pyrite and flakes of chlorite, some calcite bands CAA banding 77" intercalated finegrained flow or tuff traces of chalcopyrite pyrrhotite along small fissures strongly chloritic AMPHIBOLITIZED (with intercalation of fine grained MAFIC VOLCANIC FLOW) : fine to mediumgrained clots of chlorite up to 3rom in diameter fine feldspar metacrysts chloritic matrix massive to weakly foliated slightly fractured with calcite and guartz infillings intercalation of mafic flow partly finely banded : pervasive carbonatization foliation at CAA = 72" grading down hole into a finegrained, well foliated mafic volcanic flow with rare clots of chlorite END OF HOLE XSULPH IOCS neterage TAL x AU x ASSAYS OZ, N t *~ OZ N to *D 0 ^ f l l w UJ g o:. f M^MM mmmmm mammi '

24 i ONTARIO GEOLOG:CAL S ASSESSMENT FILES OFFICE KAY REC EIVED QQ H* M, ree.

25 CLAIM # *PA *PA *PA *PA *PA *PA *PA *PA88677 PA PA PA PA PA PA PA PA PA PA PA PA PA9253 PA9254 PA9255 PA9256 PA9257 PA9258 PA9259 PA925 PA PA PA PA92543 AREA WORK DAYS CREDITED TAL 37 DAYS

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27 "V. \ \ r e5(2(33 ' i* 9079/85235 '85t242 l,. w I8G89O6 ~s a i. L ' " R W8689I " " ~" ~~^ I::'::::::^ ~ ^^" ~ ~" ^T ~" "3""^ l ~ ~ T L \ ^ _ 87268lo * J l l~ ~ ' " 4.^ ^ /yj ISA fi Fy J UyUyC/t l~ vn c t f l \ T^"^ l ' l 8U9I2 J87266T;.i ~~\T,,c r~^f^~^htf7w it?!?^ 87^692 l J73t493 l l B72695,' \

28 Ministry of Report j DOCUMENT No. Northern Development and Mines, i., i of Work!..,~~^ W8803' Ontario r ^~ ki E Min Name and Address of/recorded Holder St. Joe Canada Inc. KAWASHE LAKE T Smte 00, 20 Adelaide St. F.. r Summary of Work Performance and Distribution of Credits Total Work Days Cr. claimed /33d for Performance of the following work. (Check one only) [~ Manual Work Mining Claim Prefix Number Attached Schedule l Work Days Cr. Toronto. OniaHn Mining Claim prefix Work Days Cr. Prefix Mining Claim Number Work Days Cr. rjshaft Sinking Drifting or other Lateral Work. [^Compressed Air, other Power driven or mechanical equip. [ j Power Stripping r^j Diamond or other Core drilling Land Survey AU the work was performed on M,nin9 daim.sh pa86 ^ pa860 Required Information eg: type of equipment, Names, Addresses, etc. {See Table Below). ^ fctbie. G 3.GO& Attached: Schedule 2 Under relief fran forfeiture /3^0oiyj /J f f L Certification Verifying Report of Work Date of Report May 0, 988 hereby certify that have a personal and intimate knowledge of the facts set forth in the Report of Work annexed hereto, having performed the work or witnessed same during and/or after its completion and the annexed report is true. Name and Postal Address of Person Certifying David Molloy, Exploration Manager, St. Joe Canada Inc (As above) Table of Information/Attachments Required by the Mining Recorder Date Certified May 8, 988 Certified I Typo of Work Specific information per type Other information (Common to 2 or more types) Attachmen/s' Manual Work S Shaft Sinking, Drifting or other Lateral Work Nil Names and addresses of men who performed manual work/operated equipment, together Work Sketch: those arc required to show Compressed air, other power driven or mechanical equip. Type of equipment extent of work in relation to tho Power Stripping Diamond or other core drilling Type of equipment and amount pxponde.d, Note: Proof of actual cost must bo submitted within 30 days of recording. Signed core log showing; footage, diameter of core, number and angles of holes. Names and addresses of owner or operator together with dates when drilling/stripping done. Work Sketch (as above) in duplicate Land Survey Name and address of Ontario land surveyor. Nil Nil

29 SCHEDULE 2 Diamond Drilling Conducted By: Midwest Drilling 80 Cree Crescent Winnipeg, Manitoba R3J 3W. "?r\y 9 r :.' 4' w Claim f PaS68 Pa868 Pa866 Pa.860 Hole # MN8694 MN8684 MN8689 MN8695 Start July 7/86 July 6/86 July 2/86 July 8/86 Finish July 8/86 July 7/86 July 3/86 July 9/86 Dip/Azimuth 45/205 45/205 45/205 45/ m 00.0m 96.0m 56.0m Credits Avail TCTAL DAYS AVAILABLE TAL DAYS UNUSED CREDITS NB: Previous credits from Cla±m 868 Additional Credits applied for Previous credits from claim 866 Additional credits applied for Previous credits from claim 860 Additional credits applied for O? O