2.21391

42A09SE2036 2.21391

DDH No: KDS-00-01

MUNRO 010

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DAVE GAMBLE GEOSERVICES INC. 70 First Street, Kirkland Lake, Ontario, P2N 1N3 , Tel: 705-567-4381, Fax: 705-567-3801

MILLSTREAM MINES DRILL RECORDProject: POTTERDOAL WEST PLUNGEProperty: KIDSTON 1 DYMENTTwp/Claim: MUNRO TWP ; L 1 225282Hole No: KDS -00-01

Azimuth: 000 deg.Dip: - 50 deg.Location: LO * 75 mW 1 Z * 83 mSTotal Depth: 479.0 m

Started: AUG 25, 2000Completed: SEPT 01, 2000Core Size: NQDrilled By: Bradley Bros.

Logged For: MLSM 1 OG J.V.Logged By: DAVE GAMBLETests: TD: 50 m Dip: -50.50 deg Az: 002.5 deg.

TD: 200m Dip: -49.75 deg Az: 001.0 deg. TD: 350 m Dip: -49.50 deg Az: 006.0 deg. TD: 479 m Dip: -49.00 deg Az: 005.5 deg.

Purpose of Hole: To test Quantec's Real Section I.P. Anomaly between L 0+00 mW and L 1+00 mW centered near base line 0 + 00 mS, and also to test for the westerly down plunge and depth extension of the Cu-Zn mineralization from the Potterdoal mine area and below the short ddh's drilled by Granges Inc. in 1992.

Remarks l Results: The hole encountered a komatiitic volcanic flow succession consisting of olivine cumulate peridotite, spinifex textured flows, interflow breccia, and leuco-komatiitic variolitic pillowed basalt flows from 4.3-349.73 m. From 344.73-361.68m a hyaloclastite unit, similar to the mine hosting sequence at the Potter Mine was encountered. The upper 0.77 m contained 5 0V, by volume of coarse nodular to framboidal Po rimmed by Py in a weak graphitic fine grained argillaceous matrix to the He. Also within this He unit 15"/o by volume nodular Po + Py occurs from 357.85- 359.50m and again at 360.42-361.65m. From 361.68-451.80 m pillowed variolitic basalt flow sequence was encountered with coarse stringer Po + trace splashes Cpy from 362.70-369.34 m in a fractured to brecciated flow interval.

From 451.8-458.73 m a second hyaloclastite unit was encountered but contained only minor Po + Py as blebs, disseminations and nodular to framboidal sulphides locally. From 458.73-479.00 (EOH) a layered, locally graded fine to coarse clastic sedimentary sequence with fining up hole indicates stratigraphic tops to the south. The sedimentary sequence consists of black, graphitic, weakly conductive argillite, siltstone to clean granular sandstone, minor laminated grey mudstone to chert, and becoming very coarse conglomeratic towards the bottom of the hole with coarse boulders of chlorite amygdular and massive basalt set in a fine granular clastic matrix. The black argillaceous beds are host to coarse nodular pyrite, pyrite seams, and finely disseminated pyrite. At 465.10-465.70 m a very fine grained finely laminated mudstone to chert contains pyrite lamellae and several coarse splashes of red-brown ZnS. At 473.0-474.0 heavily disseminated pyrite with coarse stringers of red brown ZnS occurs in the fine clastic sedimentary matrix of the coarse conglomerate was also intersected. Fourteen intervals were saw cut and assayed for Cu-Zn-Co-Au-Ag.

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4.30

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4.30

19.75

Description

OVERBURDEN (CASING LEFT IN)

KUFS - KOMATIITIC ULTRAMAFIC FLOW SEQUENCE4.3 - 10.5 m PERIDOTITE FLOWDark grey green olivine cumulate peridotite flow with equant 1-2 mm olivine cumulate crystals. Cut by dark green black serpentinized polysutures. Locally fine micro spinifex locally. Broken core 95 - 10.5 m.

10.5 - 11.3 m SPINIFEX FLOWUpper contact sharp @ 40 deg. TGA. Coarse bladed dark green olivine spinifex

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DDH No: KDS-00-01 Sheet of 18

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19.75

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70.02

Description

blades in a medium grey-green groundmass. Fine bladed spinifex at upper contact rapidly progressing to coarse bladed spinifex, tops up hole or to the south.

11.3 - 16.6 m PERIDOTITE FLOW Dark grey black serpentinized olivine cumulate flow, with dark grey black lacy serpentinized microfractures with intervening dark to medium grey olivine cumulate equant crystals. Broken core 13.5 - 14.0 m. Occasional dark green serpentinized polysuture. Lower contact sharp at 70 deg. TCA. defined by grey bleached lower 20 cm with calcite and minor quartz veining.

16.6 - 16.8 m FLOW TOP BRECCIA "A1"Fractured komatiite basalt, flow top breccia zone of light to medium grey fractured fine grained basalt flow breccia,

1 6.8 - 1 9.5 m SPINIFEX FLOW SEQUENCE From 16.8 - 17.0 m Fine random spinifex flow. From 17.0 - 19.0 m Coarse bladed spinifex flow. From 19.0 -19.1 m Foliated skeletal olivine spinifex. Contact at 50 deg. TCA. From 19.1 - 19.5 m Peridotite olivine cumulate flow. Lower contact at 60 deg. TCA.

1 9.5 - 1 9.75 m INTERFLOW BRECCIA Good rubbly basalt flow breccia. Upper and lower conformable contacts at 60 deg. TCA. Note: From 16.6 - 19.75 m spans a complete komatiitic flow sequence cycle from an "A1" through to "A1" flow breccia intervals characterized by internal flow layers from A1 to A2 to A3 to B1 to B2 to A1 forming a flow cycle. This flow sequence suggests that the flow faces uphole or the flow top facing stratigraphically to the south.

BASALT FLOW SEQUENCE - LEUCO KUFS To TBS (LOW MgO KOMATIITIC BASALT To THOLEIITIC BASALT FLOW SEQUENCE). From 19.75 - 23.0 m BASALT FLOW - Fine-grained random spinifex pyroxene or prismatic amphibole (tremolite) in a medium grey to light olive green groundmass. The basalt flow contains light grey 1-3 mm coalescing variolites and a chloritic pillow selvage at 20.55 m. Cut by dark green chlorite filled fractures. Fractured bleached basalt flow top breccia with dark green chloritic matrix and fracture fillings. Broken core from 20.0-20.5 m. From 23.0 - 27.7 m. BASALT FLOW - Medium grey, hard, massive uniform basalt flow (leuco KUFS to TBS tholeiitic), with fine light buff to pale green pyroxene spinifex or bladed prismatic amphibole (tremolite) crystals throughout.

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Description

From 27.7 - 30.5 m BASALT FLOW, equant 1 mm dark green chloritized pyroxenecrystals viewed on end or as cross sections of bladed prismatic crystals, and also as 1 cmbladed prismatic crystals in the long axis that impart a spinifex like texture as prismaticcrystal lathes in a medium to light buff tan to pale grey to light olive green ground massmosaic making up the basalt flow (either low MgO komatiite or tholeiitic basalt).

From 30.5 - 31.0 m BASALT FLOW TOP BRECCIA FRACTURED - Internal basalt flowbreccia to flow top breccia, medium grey-green, fractured basalt flow with dark greenchloritic matrix and chlorite filled fractures. At 29.76 - 29.81 m calcite and quartz veinlet at85 deg. TGA.

From 31.0 - 37.0 m BASALT FLOW, medium to light grey buff to pale grey green.massive leuco KUFS to TBS basalt flow with fine microspinifex" or bladed prismaticamphibole ( tremolite).Cut locally by calcite plus quartz fracture filled stringers containing trace Py-Po (pyrite andpyrrhotite). At 31 .0 a 2 cm quartz * calcite vein at 90 deg. TGA.

From 37.0 - 38.1 m BASALT FLOW, with 1 mm cross sections of dark green chlorite afteramphibole or pyroxene imparting a spinifex type texture of prismatic crystals or blades andalso with foliated skeletal bladed or foliated prismatic crystals at 55-65 deg. TGA.Cut locally by quartz filled fractures. At 37.4 - 37.5 m quartz * vibrant green fuchsite filledfractures at 70 deg.

From 38.8 - 43.4 m BASALT FLOW, microspinifex* texture with tremolite or amphibolesin a medium green to olivine green massive flow.At 38.8 - 39.4m the basalt flow is bleached to buff tan and weakly fractured.Cut by quartz plus calcite veins at 39.12 - 39.19 m at 80 deg. TGA, and at 39.25 - 39.30 mat 80 deg. TGA, and calcite * chlorite plus locally fuchsite stringers from 39.30 - 39.9mcarrying Po plus trace specks of Cpy.The bladed tremolitic amphibole is microspinifex textured-like and seems to graduallydecrease by 43.4 m.

43.4 - 53.19m BASALT FLOW, PYROXENITE CHLORITE AMYGDALOIDAL, LEUCOKUFS TO TBS, Medium grey - olive green fine-grained texture, massive to homogeneousflow with 1 mm dark green chlorite round amygdules. Locally ghost like remnant spinifexbut there appears to be much more clinopyroxene. There also appears to be weak lathe-like to diffuse lath-like plagioclase, a leuco low MgO komatiitic basalt flow or possibly a Mg- tholeiitic basalt flow.

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Quartz + calcite vein at 44.75 -44.8 m at 50 deg. TGA with chloritic borders plus Postringers to fine seamlets Po.At 52.77 m Calcite plus quartz stringers with dark green chlorite, irregular shaped carryingseveral 2 mm splashes of red brown sphalerite (ZnS) and trace chalcopyrite (Cpy).Locally throughout weak to trace Po along fractures, trace Py also occurs.

At 53.19 - 53:76 m FOLIATED ZONE (SHEAR), pale green Mg chlorite competentfoliation fabric at 70 deg. TGA, trace Po near lower 80 deg. TGA contact. This penetrativefoliation fabric is similar to a foliated tectonic "shear zone".

53.76 - 62.35 m BASALT FLOW CHLORITE AMYGDALOIDAL, (as previous). Pale grey- green massive, homogeneous fine-grained flow with 1 mm dark green chlorite flecks andchlorite amygdules.

62.35 -62.47 m Quartz-calcite 1-3 cm stringers at 20 deg. TCA.

62.47 - 62.60 m Foliation fabric at 50 deg. TGA of light green Mg chlorite plus minorcalcite and quartz stringers.

62.60 - 66.3 m BASALT FLOW, medium grained mottled texture, cut by calcite stringers,locally pervasive interstitial carbonate.Lower flow contact sharp at 60 deg. TGA.

66.3 - 70.02 m BASALT FLOW, Fine grained to very fine grained aphanitic pale grey -green bleached upper contact. Cut by calcite stringers and dark green chlorite fracturefillings.At 66.7 - 67.0m INTERPILLOW BRECCIA. At 67.0 m edge of pillow with scattered lightgrey variolites that within several cms have coalesced to form a massive core to thepillow. At 67.9 - 68.0 m several 1 - 2 cm large quartz and dark green chlorite calciteamygdules.At 66.85 m a 3 cm calcite vein at 40 deg. The basalt is very dense, hard compact flowunit.At 66.1 5 - 68.6m there are 0.5 to 1.5m isolated to coalescing light grey buff variolites.At 68.3 - 68.5 m a sinuous grey glassy 1 cm quartz stringer at 15 deg. TCA with calciteborders.At 69.3 - 69.6 dark green wispy to patchy chloritized basalt, cut by calcite stringers.

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DDH No: KDS-00-01 Sheet of 18

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70.02

70.66

71.70

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70.66

71.70

73.63

Description

NOTE: The basalt flow sequence may be the basal part of the low MgO komatiite sequence with the upper part of the flow characterized by spinifex texture, weak and then progressing to coarse bladed spinifex at the top of the flow cycle.

BASALT VOLCANICLASTIC BRECCIA - LEUCO KUFS to TBS Upper contact sharp but wavy with irregular minor embayments at 5 deg. TGA. Angular 1 cm to 10 cm basalt breccia fragments, lacks rounding suggesting low degree of transport. The breccia unit generally consists of underlying flow fragments but also contains other compositional fine-grained basalt fragment types from pale apple green to buff tan to spinifex textured fragments in contrast to the light olive to pale army green of the enclosing basalt flow. The breccia population represents 7Q1k by volume with a medium olive to army green basalt flow matrix. This basalt breccia unit is generally clast supported. Lower contact sharp locally jagged from 20 - 30 deg. TGA. Near the lower contact a long lenticular basalt breccia fragment exhibits 'in situ' fracturing and brecciation indicating low transport and immature sorting.

BASALT FLOW - LEUCO KUFS to TBS Fine-grained, buff olive green, massive uniform, source material for most of the above overlying volcaniclastic breccia. The flow unit is cut by fractures, some are dark green chloritic and some are calcite filled. Trace Po occurs in the fractures and in the calcite * chlorite fracture fillings. Lower contact sharp but wavy, irregular at 5 to 15 deg. TGA.

BASALT VOLCANICLASTIC BRECCIA - LEUCO KUFS to TBS Similar to breccia at 70.02 - 70.66 m with coarse angular to subrounded 2 - 10 cm basalt breccia fragments. Breccia is 7007o by volume to SO1!*! matrix. Multilithic breccia population of various basalt types. Generally the most abundant breccia clasts are fine-grained medium olive green basalt flow rocks that are also the enclosing host flow rocks, as well as medium green breccia clasts, spinifex textured clasts, and dark grey calcareous to carbonaceous clasts also occur in a fine medium olive green flow matrix. The breccia is generally clast supported. This unit is probably a slump breccia or flow front debris flow. The breccia unit is cut by calcite stringers, contains local pervasive interstitial calcite. Several large * 1 5 cm basalt flow breccia clasts near the lower contact suggests a coarse base to less coarse fragment size gradation uphole overall indicates a possible top facing lo the south.

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DDH No: KDS -00-01 Sheet of 18

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76.63

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232.10

Description

Calcite vein 2 cm thick at 10 deg. TGA from 72.95 - 73.20m. Trace Po * Py in calcite stringers. Lower contact sharp but wavy irregular with basalt flow embayments. Contact approximates 15 deg. TGA.

BASALT FLOW - LEUCO KUFS to TBS (as previous)76.63 - 96.90 m BASALT FLOW, a continuation of fine grained basalt flow, medium olivegreen, cut by calcite * quartz fracture fillings, trace Po and some dark green chloritealteration bordering some fractures.At 78.3 - 78.5m a calcite * quartz stringer 2 cm thick with Po splashes and trace Cpy.At 83.12 - 83.33 m quartz * calcite + chlorite 10 cm vein at 30 deg. TGA.At 84.7 - 84.96 m calcite chlorite veinlet 3 cm at 1 0 deg. TGA.At 85.68 - 85.75 m basalt flow breccia, angular fine grained basalt flow top or pillowbreccia. Dense compact bleached tan coloured basalt. Irregular to jagged contact. From85.75 - 86.8 m VARIOLITIC PILLOWED BASALT FLOW, Pale tan 1-2 mm isolatedvariolites that rapidly coalesce to form pillow cores. Clearly defined pillow selvages andinterpillow breccia.From 86.8 - 96.65 m BASALT FLOW, as previous fine-grained, massive, uniform, cut byoccasional chlorite lined fracture and calcite stringer, trace Po splashes along somestringers and fractures.Occasional dark green chlorite amygdules.At 89.5 - 89.7 m quartz - calcite vein at 40 deg. TGA with trace Po near edge of vein infractures. From 95.5 - 95.9 m fractures with Po plus trace Cpy.

96.65 - 96.90 m BASALT FLOW TOP BRECCIAUpper contact sharp but wavy irregular at 70 - 90 deg. TGA. Rubbly flow top that graduallychanges to spinifex textured flow.

96.90 - 97.25 m SPINIFEX FLOWDark grey komatiitic basalt spinifex textured flow. The dark green finely bladed randomoriented spinifex blades are in a medium grey groundmass. The spinifex texture graduallydisappears below 97.25 m grading into a massive medium grey green fine grained flow.

97.25 - 104.35 m BASALT FLOW, the flow contains medium to light grey variolites at97.5 - 97.6 m and is cut by chlorite filled fractures locally. The variolites representpossible pillow core edges. At 99.5 - 99.75 m excellent dark green chlorite interpillowselvages and interpillow quenched textured primary flow basalt hyaloclastite.

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At 100.? rf* 9ood ''O"' Srey vanohtes and from 100.3 - 104.35 m weak to fine spinifextextured **™ ^salt.At 104 34 fine variolites.At 102,14- - 102.18 m quartz calcite vein at 50 deg. TGA and agan at 102 28 m a 1 cmvein at 5/V Oeg- TGA.

104.35 - f 22.02 BASALT FLOW SEQUENCEAs prevkWS. fine grained massive flow cut locally by chlorite filteJ fractures plus trace Po At 106. ft rf* good pillow selvage and good marginal to pillow cort isolated variolitesprogress*** to massive coalesced variolites for the core of the p*ow. Locally f**** chlorite amygdules. Good pillow margin at 1 1 1 .6 mLocally to* *"i Puartz * chlorite veinlets @ 40 deg. TGA.From 11** m -117,15 m dark green chlorite 1 -2 mm spotting mparting a fine 'pepper* like textiM* to tne medium green basalt flow.

From If/ -15 - 1 22 -02 m BASALT FLOW, fine grained, medium green, with occasionaldark gr*** amygdules throughout. Trace Po along fractures and near occasional calcitefilled fraO**6 - Trace specks Cpy with the Po.At 122. 0/' f"1 sharp low contact at 50 deg. TGA .

1 22.02 - If*-3 m BASALT PILLOWED FLOW. Medium grey to grey green, fine grained basalt pi***"*1 flow Dark 9reen chloritic selvages with well developed primary interpillow hyaloclart**6 p'"ow edges exhibit light grey variolites that rapidly coalesce from the pillowmargins V' * massive pillow core.

At 126.5 ** mterpillow selvage contains fine calcareous argillite as patchy to wispyinterpillW*edimenl -From 12* -7 - 127.07m a good interval of interpillow hyaloclastite pillow breccia containingrounder) 4Wanfc that are round concentrically zoned hyaloclastite basalt quenched textured basall gtc****5 The matrix contains fine 1 - 3 mm white intergranular quartz There is alsodark grry W Wa(* Palchy to wispy argillite as minor intersedimentary material. Theglobular M-salt shards tend to be pale apple green cores and successive concentric ringsappear ir. fc* darker green in colour. Lower contact wavy irregular and approximates 40deg. TO

127.07 - 12*-30 m BASALT FLOW, as previous, pillowed flow with light grey variolites,dark gnu"'' chloritic pillow selvages. Lower contact wavy at 60 deg TGA.

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DDH No: KDS -00-01 Sheet 8 of 18

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128.30 -134.8m BASALT FLOWPale to light olive green, tremolitic to weak spinifex textured flow. Massive, uniform, finegrained, hard dense flow.At 129.32 - 129.56 m Quartz -i- minor calcite stringers and patchy vein, lower contact sharpat 30 deg. TGA.At 131.45 - 131.6 m quartz * calcite (3cm) veinlet at 25 deg. TGA.At 131.8 - 132.1 m quartz -i- calcite stringer vein at 10 deg. TGA.At 133.4 -134.1 quartz * calcite stringers.Lower contact sharp at 60 deg. TGA.

134.8 - 135.25 m INTERFLOW BASALT BRECCIAUpper contact sharp at 60 deg. TGA.Rubbly flow breccia competent with weak fabric at 50 - 60 TGA. Occasional spinifextextured flow fragments.Lower contact sharp at 50 deg.' TGA.

135.25 - 150.65 m SPINIFEX FLOWFrom 135.25 - 143.0 m Good coarse bladed olivine spinifex flow. Dark green olivinespinifex blades in a medium grey fine grained ground mass.At 136.8 m swirling textured spinifex with chevron type swirling olivine blades.From 140.5 - 143.0 m gradually lightening to medium green with gradual diminishing ofspinifex bladed texture.From 143.0 - 150.65 m medium green flow with microspinifex light green blades ofprobably tremolite, locally patches of variolites, and some darker green pyroxene or olivinebladed spinifex. Overall gradual lightening in colour and gradual change from coarsespinifex at top of interval to more massive less spinifex towards and at bottom part of flowsequence.Locally cut by occasional quartz * calcite stringers. At 144.3 - 144.48 m several 1 to 3 cmquartz + dark green chlorite veinlets at 45 deg. TGA.Lower contact sharp at 40 deg. TGA.

150.65 - 151.80m BASALT FLOWMedium to light green, fine grained, massive variolitic pillow flow. The variolites are palegreen.Lower contact sharp at 40 deg. TGA.

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^^^HHHBK!OES^

, Description

151.80 - 151.95 m INTER-FLOW To FLOW TOP BASALT BRECCIAA thin interval of 40 deg. TGA stretched to partially flattened interflow basalt brecciafragments. Upper and lower contacts are conformable at 40 deg. TGA.

151.95 - 156.30 m BASALT FLOWMedium green variolitic patches, fine microspinifex texture, possibly tremolitic, contains 1mm dark green chlorite pepper-like flecks or spots. Generally a massive uniform flow unit.minor quartz stringers, trace Py along fractures. Lower contact sharp at 45 deg. TGA.

156.30 - 1 67.25 m SPINIFEX FLOWCoarse bladed olivine, dark green spinifex in a medium grey-green fine grainedgroundmass. Occasional dark green chlorite amygdules. Very coarse spinifex bladestowards lower part of interval suggesting blades fine uphole or tops to the south.Sharp abrupt lower contact at 70 deg. TGA.

167.25 - 168.5 m BASALT FLOWFine grained medium olive green, locally cut by quartz * minor calcite stringers. From168.5 - 169.8 m medium grey patchy coarse crystalline cpyx, minor spinifex textured flowwith a gradual lower contact from medium to coarse crystalline or spinifex crystallinetextured flow.

From 169.8 - 183.0 m BASALT FLOWFine grained texture, medium grey-green generally massive uniform, locally microspinifextextured as pale green blades ( possible tremolite). Cut by quartz veinlets at 174.85 -174.90 m. at 50 deg. TGA and by quartz stringers from 175.0 - 176.0 m.Locally chlorite filled fractures. At 181.7 - 182.5 m fine pale green lacy fracture filled bypale green chlorite * quartz.

183.0 - 183.4 m INTERFLOW BASALT FLOW To FLOW TOP BRECCIARubbly basalt with fragments from underlying basalt flow. Cut locally by quartz * calcite0.5 cm veinlets at 45 deg. TGA.Lower contact sharp at 40 deg. TGA.

183.4 - 188.5 m SPINIFEX FLOWCoarse bladed spinifex textured flow dark green spinifex blades in a medium greygroundmass mosaic. Locally pale green trace fuchsite. Locally cut by stringers of quartz *calcite.From 188.0 - 188.5 m broken core with Fault Gouge from 188.4 -188.5 m at 35 deg TGA.

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DDH No: KDS -00-01 Sheet 10 of 18

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232.10

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318.90

Description

188.5 - 223.7 m BASALT FLOW Medium grey-green, fine-grained massive uniform flow.Contains fine 1 mm dark green chloritic specks and also 1 - 3 mm dark green chloriteamygdules.Also appears to contain pale green to cream white interlocking plagioclase that isgradational at 198.0 - 200.9 m.Locally variolitic at 197.6 m.Cut by quartz * calcite veinlets at 192.4 m (1cm) at 40 deg. TCA and at 199.0 (4 cm) at 50deg. TCA, with trace Po * Cpy. Trace Po along fractures.At 200.86 - 200.95 m Quartz vein at 45 deg. TCA with trace Po.At 202.85 m, a 1 cm quartz vein at 25 deg. TCA with chloritic borders.Basalt Flow from 201.0 to 203.0 m becomes progressively finer grained.Basalt Flow locally contains chlorite 1 mm to 5 mm amygdules.Trace Po along widely spaced fractures with quartz fracture filled stringers.At 207.25 m a 2 cm quartz veinlet at 55 deg. TCA.At 210.6 a 2 cm quartz veinlets at 20 deg. TCA. with trace splash Po.At 213.77 and 213.88 m two quartz veinlets at 35 deg. TCA.At 218.1 - 218.3 m quartz * calcite stringer with dark green chlorite.At 222.13 - 222.42 m quartz * calcite stringers at 10 deg. TCA.From 219.5 - 223.7 m Fine grained basalt flow with tremolite to microspinifex type texturelocally. Lower contact sharp at 50 deg TCA.

223.7 - 227.5 m SPINIFEX FLOWDark green olivine spinifex blades and equant olivine in a pale olive green fine grainedgroundmass.Upper contact sharp at 50 deg. TCA.Lower contact abrupt with rapid change from spinifex to fine grained flow. Broken core atlower contact.

227.5 - 232.1 m BASALT FLOWFine grained massive uniform pale to medium grey green. Locally cut by chlorite fractureswith minor quartz * calciteLower contact sharp at 45 deg. TCA.

PERIDOTITE FLOW - KUFSFrom 232.1 - 237.35 m Medium to dark green massive uniform locally serpentinizedpolysutures, an olivine cumulate, gradually becoming darker green, a gradational

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DDH No: KDS - 00-01 Sheet 11 of 18

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318.90

319.10

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319.10

320.35

Description

increase in dark green downhole. At 234.3 - 234.4 and at 234.77 - 234.85 m two small pegmatoidal coarse grained pyroxenide dyklets at 45 deg. TGA with coarse grey prismatic cpyx. At 237.2 - 237.25 m fractured broken Fault Zone at 50 deg. TGA. From 237.25 - 318.90 m Dark green olivine cumulate with equant 1-3 mm olivine crystals in a serpenfinized groundmass. The unit is polysutured with dark green serpentine fillings and light vibrant green serpentine polysutures or fracture fillings locally. Intercumulus grey cpyx occurs as the groundmass for the equant olivine crystals.

From 255.5 - 299.3 m fibrous 1 mm and less serpentine asbestos occur along occasional widely spaced tension fractures. Strongly magnetic with finely disseminated magnetite and magnetic susceptibility readings from 4.0 c.g.s up to 9.4 c.g.s. The magnetite is a product of serpentinization of olivine producing serpentine -i- magnetite.

At 260.1 m layering at 55 deg. TGA. At 300.5 m layering at 35 deg. TGA and at 307.6m at 50 deg. TGA.

Fractured core at 302.0 - 303.5 m along a serpentinized polysuture at the end of a drill run at 311.0 m.

From 311.0 - 318.9 m the peridotite flow unit becomes finer grained crystalline and gradually becomes a lighter olive to army green, leuco-peridotite.

Lower contact is sharp at 60 deg. TGA.

INTERFLOW BASALT FLOW TOP BRECCIA (LEUCO KUFS to TBS). A narrow flow breccia interval defining the above peridotite to more leucocratic komatiitic basalt flow below. The unit is compact and is characterized by angular olive green komatiitic basalt flow breccia fragments, a flow top breccia. Lower contact is sharp but with wavy irregular surface at 50 deg. TGA.

BASALT FLOW (LEUCO KUFS To TBS) Medium green, microfractured with trace Po, locally finely variolitic, fine grained, leuco - komatiite flow. Internal flow contact at 320.1 at 65 deg. TGA. From 320.1 - 320.35m pale grey green and becoming fine grained aphanitic near lower contact. Minor calcite stringers * quartz. Lower contact sharp at 65 deg. TGA.

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DDH No: KDS -00-01 Sheet 12 of 18

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320.35

340.43

321.68

323.35

324.17

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320.43

321.68

323.35

324.17

326.10

Description

INTERFLOW TUFF SEDIMENTUpper and lower contacts conformable at 65 deg. TGA. A narrow interval of finely laminated dark grey to black 0.5 cm layers of argillite with 1 mm seams or thin lamellae of Po * Py. Between the argillaceous layers is medium to darker green fine basaltic tuff/sediment. At and near the upper contact fine quench textured basalt occurs as grey-white porcellaneous to perlitic wispy lamellae to quenched textured hyaloclastite.

BASALT FLOW - (LEUCO KUFS To TBS). As previous, pale to medium olive green fine grained basalt flow cut by fine calcite * quartz filled microfractures carrying trace Po. Possible fine variolites and pillow selvage indicating basalt pillowed flow. Lower flow contact sharp at 45 deg. TGA.

PYROXENITE GABBRO DYKEMedium grey-green, fine-grained from upper chilled contact gradually becoming medium grained by 322.20 m. The rock consists of grey-green to green-brown stubby cpyx and dark green hornblende amphibole prismatic needles on the long crystal axis and stubby 1 - 2 mm dark green on short axis in a n interlocking groundmass of cream white plagioclase. Chilled fine grained lower contact zone but only over 10 cm. The pyroxenite dyke has a symmetry of chilled contacts, upper contact is approximately 45 deg. TGA, while the lower' contact approximates 60 deg. TGA.

BASALT FLOW - as previous LEUCO KUFS To TBS Fine-grained, medium grey-green, weakly variolitic. At 323.47 m quartz vein breccia irregular to patchy veinlet at 40 deg. TGA. Lower contact sharp but locally jagged to irregular at 50 deg. TCA.

PYROXENITE GABBRO DYKE (As previous) Fine-grained chilled margin and becoming more coarse to medium grained in the central part and becoming fine-grained and chilled towards the lower contact. Upper contact sharp jagged at 50 deg. TCA, lower contact sharp but irregular embayed approximately 55 deg. TCA. The medium-grained central part or core to the dyke is composed of an interlocking mosaic of grey-green to green-brown cpyx as stubby equant crystals, amphiboles as dark green prismatic needles of hornblende in an interlocking cream white plagioclase ground mass. The symmetry of upper and lower chilled margins is more suggestive of a dyke like rock than a possible flow rock.

Sample Number:

From: To: length (m)

Au ppb

Ag Ppm

Cu ppm

Zn ppm

Co ppm

DDH No: KDS -00-01 Sheet 13 of 18

Metres From:

326.10

349.73

Metres 'To:

349.73

361.68

Description

From 325.6 - 326.10 m is the fine grained chilled lower contact where as the upper contact is chilled over 10 to 15 cm only before rapidly becoming a medium-grained interlocking crystalline textured unit.

BASALT FLOW - VARIOLITIC PILLOWED - LEUCO KUFS TO TBS Fine grained, medium to dark green with pale cream green to buff coloured variolites that range from i-2 mm up to 1-2 cm in size. The variolites tend to coalesce forming large masses of pale cream green basalt pillow cores. Small isolated variolites occur especially along the margin and near the pillow edge. The interpillow selvages are thin, exhibit quench textured basalt shards as primary flow hyaloclastite. Orientation of selvages at the beginning of the interval range from 50 - 60 deg. TGA and locally contain trace Po plus occasional speck Cpy. Minor quartz * calcite stringers also cut the basalt with trace Po trace Cpy. The interpillow hyaloclastite is generally a pale to medium green and is a good contrast to the pillow edges. The pillow edges generally contain isolated 1-2 mm variolites.

The pillow cores are microfractured. contain dark green chlorite, occasional quartz i calcite stringers and trace specks to small blebs of Po * Py. From 344.0 - 347.1m irregular quartz veinlets to stringers * minor calcite and dark green . chlorite as tension fracture fillings. The lower contact is buff tan to pale grey-green bleached over the lower 0.5 metre, with possibly some perlitic quartz lined healed microfractures. Throughout the pillowed flow sequence fine 1 mm and less dark green chlorite amygdules are locally observed. Lower contact sharp at 65 deg. TCA.

HYALOCLASTITE - TBSUpper contact sharp at 65 deg. TCA. From 349.73 - 350.5 50"A coarse framboids to nodular Po rimmed by nodular Py. The matrix to the sulphides consists of basalt equant to angular shards with argillite chips and coarse patches to fragments. Fine argillaceous matrix also occurs. The basalt shards are palagonitized as pale green quench textured fine grained aphanitic chilled basalt rims to the darker green shards. Occasional coarse basalt fragment 2-3 cm as part of the fragment population. At 350.5 - 350.75 m a rounded fragment of medium grained pyroxenide gabbro or basalt similar to the dyke material seen further up hole. Upper contact sharp at 45 deg. TCA whereas the lower contact is 35 deg. TCA in the opposite sense, and this is interpreted to be a volcanic boulder or breccia fragment.

Sample Number:

1881

From:

349.73

To:

350.50

length (m)

0.77

Au ppb

7

Ag ppm

0.3

Cu ppm

148

Zn ppm

994

Co ppm

45

DDHNo: KDS - 00 - 01 Sheet 14 of 18

MetresFrom:

361.68

.MetresTo:

451.80

Description

From 350.75 - 351 .0 m Hyaloclastite with a coarse pale green 15 cm basalt fragment.

At 351.0 -351. 17 m Argillite layer at 35 - 40 deg. TGA. From 351.17 - 359.56 m, thehyaloclastite consists of a uniform sequence of "pea-sized" basalt equant shards, pale greyto grey green, with argillite accidental chips and fragments - a reworked or mass flowdeposit. This unit is very similar to the mineralized mine sequence hyaloclastite at thePotter Mine'to the south. There are also local short intervals of matrix calcite imparting alayered fabric at 45 deg. TGA at 353.10m. Occasional rounded grey 1 cm calcareousmudstone to calcareous argillite fragments also occur.

Occasional coarse bleb of Po at 356.0 m and from 357.85 - 361.68 m coarse blebs andnodular to framboids of Po * Py, 15"A by volume.

From 359.56 - 360.17 m, 360.24 - 360.36m, and 360.38 - 360.42m are coarse pale greenbasalt flow blocks.

From 360.42 - 361 .68 m the He contains several 3 to 8 cm rounded basalt accidentalfragments, coarse splashes Po + Py nodules to framboids and coarse seams at 360.60 - 360.70 m.

From 361.42 - 361.68 m the unit contains a high "/o of argillite as matrix.

Overall there appears to be a coarse fragment gradation from coarse fragments and basaltboulders at the base, and becoming uniform throughout much of the interval, with the toppart of the unit characterized by argillaceous matrix with sulphides.

The lower contact is sharp at 65 deg. TGA.

BASALT VARIOLITIC PILLOWED FLOWAs previous pale grey-green massive to microfractured pillow cores, variolitic near pillowrims, and medium green thin interpillow selvages. Cut locally by thin fracture filled calcitestringers.

From 367.20 - 369.34 m the basalt is a fractured flow and laced by Po coarse stringersand with minor Cpy splashes and blebs. Some of the flow material is quench textured withpalagonitized ultramafic groundmass and bleached with perlitic-like fractures. Thesulphides as stringers represent 1 S 'fa by volume. The section looks like a fractured flow toslump breccia or flow breccia unit that is characterized by a fragmented to fragmental

SampleNumber:

18821883

1884 1885

188618871888

From:

357.85358.85

360.42 361.00

367.20368.00368.80

To:

j

358.85359.50

361.00 361.65

368.00368.80369.34

length(m)

1.000.65

0.58 0.65

0.800.800.54

Auppb

72

2 nil

17nil10

Agppm

0.30.3

0.1 0.2

0.30.41.3

Cuppm

147173

126 152

221748

2020

Znppm

121115

141 135

1160484417

Coppm

4142

41 59

3980

271

DDH No: KDS -00-01 Sheet 15 of 18

Metres From:

Metres To:

Description

appearance and cut by sulphide stringers and fracture fillings. The lower contact is abruptat 60 -65 deg. TGA.

369.34- 380.63 BASALT FLOW SEQUENCE - LEUCO KUFS (low MgO KOM) To TBS.From 369.34 - 371.55 m BASALT FLOWMedium grey-green, massive flow. At 370.4 - 370.55m interpillow hyaloclastite as selvagematerial. From 370.55 - 371.55 m fractures pillow core with chlorite calcite linedfractures.From 371.55 - 372.5 m SPINIFEX FLOW PILLOWEDGood spinifex textured flow with dark green random spinifex blades in an army to olivegreen groundmass, possibly a pillow.

From 372.5 - 374.55 m BASALT PILLOWED FLOWArmy-green komatiitic basalt with dark green chlorite * serpentine j; argillite as filledpolysutures and interpillow selvages.

From 374.55 - 374.66 INTERPILLOW BASALT FLOW BRECCIA.

At 374.87 - 374.94 m calcite vein and interpilllow breccia at 50 deg. TGA.At 375.6 interpillow selvage at 15 deg. TGA with good well defined chilled pillow edgemargins.From 375.6 - 380.63 m dark green chloritic 1 - 2 mm amygdules.The interpillow selvages are dark green with a black argillaceous component with trace toweak finely disseminated Po. This unit is a good example of pillowed komatiitic basalt flowmaterial.

From 380.63 - 398.45 m BASALT PILLOW FLOW - PILLOW BRECCIAA thick sequence of dark olive green and medium grey green mini-pillows with roundedameboid shapes, chilled margins set in a black argillaceous interpillow sedimentary matrixto basalt pillow breccia matrix . Some pillows are broken with 1-2 cm variolites that areclearly dissected by brecciation at 387.0 m.Within the argillite matrix to the mini pillows and pillow breccia is weak disseminated Po.At 386.81 - 386.95 m calcite vein at 35 deg. TGA with trace flecks Po * Cpy.At 387.62 - 387.72 m calcite vein at 50 deg. TGA with flecks and disseminations of Po withtrace Cpy.Locally in the pillow breccia sequence there is quenched textured interpillow basalthyaloclastite with the argillaceous matrix. Some of the mini basalt pillows exhibit

Sample Number:

From: To: length (m)

Au ppb

Ag ppm

Cu ppm

Zn ppm

Co ppm

DDH No: KDS -00-01 Sheet 16 of 18

Metres From:

451.80

458.73

Metres To:

458.73

479.00 EOH

* Description

concentrically zoned multiple chill to quenched margins. Lower contact abrupt and sharp at 65 deg. TGA.

398.45-451.80 BASALT VARIOLITIC PILLOWED FLOW Medium grey-green basalt flow with 1-3 cm variolites that are light or grey-green in colour at the start Of the interval. Locally weak chlorite 1-3 mm amygdules and occasional calcite filled amygdules at 422.0 m. At 403.15 - 403.60m calcite vein with minor argillaceous sediment at 30 deg TGA, and a calcite-chlorite vein at 405.47 - 405.65 m at 35 deg. TGA. Well developed interpillow selvages start at 404.8 with minor argillite interpillow sediment * trace Po. The interpillow selvages are usually chloritic, darker green than the pillows and tend to be thin rarely exceeding 2-3 cm thick. The edge of the pillow usually exhibit 1 mm fine isolated variolites along the chilled pillow edge. The core of the pillows can be fractured, with trace Po, and as well contain weak amygdules of green chlorite and rarely calcite'. At 419.84 - 420.25 m a quartz * calcite * dark green chlorite stringers and veinlet at 25 deg. TGA. The pillows appear to be 1.0 to 1.5 m in size, although some smaller pillows also occur as determined by the frequency of the interpillow selvages. At 442.06 - 442,14 m a selvage with calcite stringers at 35 deg. TGA. From 444.0 - 451.8 m increase in calcite filled amygdules and fine fracture filled calcite stringers. Lower contact sharp at 50 deg. TGA.

HYALOCLASTITE - TBS as previousMedium green, pea-sized basalt equant shards with angular to subrounded accidental argillite chips and fragments 1-2 mm up to 1.5 cm as 'rip-ups' within this transported mass flow deposit. The argillite accidental fragments and clasts appear to have come from the argillite unit directly below. The matrix of the hyaloclastite contains void filling white calcite in the interstices to the fragment population and appears to be the primary matrix cement for this HC unit. From 457.5 - 458.73 m fine argillite also contributes to the He matrix. From 452.0 - 452.7 m several large framboids or nodules and blebs of Po occur in the He in association with fine black argillite matrix. The lower contact is sharp but undulating at 40 deg. TGA.

SEDIMENTARY SEQUENCE: ARGILLITE - SILTSTONE - SANDSTONE - CHERT- CONGLOMERATE From 458.73 - 459.40 MASSIVE SULPHIDES as pyrite nodules SO1* (vol) in an argillite

Sample Number:

1889

1890

From:

452.00

458.73

To:

452.70

459.40

length (m)

0.70

0.67

Au ppb

nil

nil

Ag Ppm

0.2

0.3

Cu Ppm

147

86

Zn ppm

167

435

Co ppm

53

29

DDHNo: KDS-00-01 Sheet 17 of 18

Metres From:

- Metres To:

A. Description

matrix. Mostly Py with some fine disseminated calcite and calcite shadows. Nodules up to4-5 cm and coalescing forming massive seam-like sections.From 459.40 - 460.0 m ARGILLITE, black, weakly conductive, weak disseminated pyrite.From 460.0 - 460.4 MASSIVE SULPHIDE as coarse pyrite nodules to disseminated pyritein beds 2-3 cm thick with calcite shadows, also several small pyrite layers and seams to460.7m. v-From 460.8 - 461.7 m SANDSTONE, pale yellowish green clean granular sandstone,finely layered at 55 deg. TGA with grain gradation fining up hole with 1 mm granulartexture that fines up hole indicating stratigraphic tops face to the south.From 461.7 - 462.5 ARGILLITE, black argillaceous fine grained sediment with finelydisseminated weak pyrite.From 462.5 - 464.0 m SANDSTONE, yellowish grey green pale in colour sandstone,siliceous granular textured sediment as previous.From 464.0 - 464.2 ARGILLITE, as previous.From'464.2 - 471.0 GREY AND BLACK LAYERED ARGILLACEOUS SLUMP BRECCIAA medium grey slump textured soft sediment deformation unit with medium grey and blackargillaceous sedimentary disrupted sedimentary layered fragments in a poorly to disruptedlayered sedimentary dark grey to black argillaceous matrix.At 465.1 - 465.7 m CHERT TO FINELY LAMINATED GREY MUDSTONEA series of fine-grained finely laminated cherty siliceous sediments with fine lamellae of pyrite and occasional splash of ZnS. Intervening beds between the cherty layers are granular and grade or fine up hole. Layering at 40 to 45 deg. TGA. From 467.83 - 468.63m increase layers of finely disseminated pyrite. Sedimentary layering at 469.0 m at 30deg. TGA, at 470.2 m at 40 deg. TCA.From 468.63-471 .0 GREY AND BLACK LAYERED ARGILLACEOUS SLUMP BRECCIAA slump breccia or soft sediment deformation unit with intervening dark black to greyalternating sedimentary layering.From 471.0 - 479.0 m EOH. CONGLOMERATE, A boulder fragment population isprimarily made up of large 10 - 50 cm fine grained bleached light grey basalt blocks androunded breccia blocks. The basalt boulders are generally very fine grained and massiveand occasionally contains fine 1-2 mm calcite amygdules. The matrix to the basaltfragments and blocks is fine grained grey to black argillaceous sediment.From 473.0 - 474.0 m heavily disseminated Py occurs within the fine granular clasticsedimentary matrix and locally with strong 1 cm to 5 cm long x 1 cm thick red brown ZnS.From 474.0 - 479.0 at EOH the sedimentary matrix to the basalt breccia clasts and blockscontains fine to coarse nodules and framboids of pyrite. At 478.8 - 478.95 m calcite vein at40 deg. TCA in argillaceous pyritic sediment.From bottom of the hole (EOH) to top of this sedimentary sequence there is also a large

Sample Number:

1891

1892 1893

1894

From:

460.00

465.10 467.83

473.00

To:

460.70

465.70 468.63

474.00

length (m)

0.70

0.60 0.80

1.00

Au ppb

7

127

10

Ag ppm

1.1

0.8 0.1

0.4

Cu ppm

130

42 45

535

Zn ppm

716

3140 104

18400

Co ppm

30

17 22

48

DDH No: KDS -00-01 Sheet 18 of 18

Metres From:

, Metres To:

Description

scale fining from coarse conglomerate with large breccia fragments or boulders of basaltgrading into a soft sedimentary slump breccia sequence, and further grading from coarseto finely layered fine granular clastic sedimentary units that is characterized by sandstone,siltstone, grey mudstone and black argillite with locally finely laminated chert or greymudstone. The overall grain gradation of the fine clastic sediments fining up hole isconclusive and supportive evidence that the sedimentary sequence fines uphole and thatthe sedimentary sequence faces and stratigraphically tops to the south.EOH

Sample Number:

From: To: length (m)

Au ppb

Ag ppm

Cu ppm

Zn ppm

Co ppm

ONTARIO MINISTRY OF NORTHERN DEVELOPMENT AND MINES

Transaction No: W0180.30100

Recording Date: 2001 -MAY-11

Approval Date: 2001-JUL-23

Work Report Summary

Status: APPROVED

Work Done from: 2000-AUG-25

to: 2000-SEP-09

Client(s):

128504

Survey Type(s):

DYMENT, LESLIE MICHAEL

ASSAY PDRILL

Work Report Details:

Perform Applied Assign Reserve Claim* Perform Approve Applied Approve Assign Approve Reserve Approve Due Date

L 1225282 S39.256 339,256 SO SO SO O 339,256 339,256 2005-JUN-30

339,256 339,256 SO 30 SO SO S39.256 339,256

External Credits:

Reserve:

30

339,256 Reserve of Work Report*: W0180.30100

S39.256 Total Remaining

Status of claim is based on information currently on record.

42A09SE2036 2.21391 MONRO 900

2001-Aug-09 09:51 Armstrong-d Page 1 of 1

Ministry ofNorthern Developmentand Mines

Date: 2001-JUL-23

Ministere du Developpement du Nord et des Mines Ontario

GEOSCIENCE ASSESSMENT OFFICE 933 RAMSEY LAKE ROAD, 6th FLOOR SUDBURY, ONTARIO P3E 6B5

LESLIE MICHAEL DYMENT BOX 66Swastika, ONTARIO POK1TO CANADA

Tel: (888) 415-9845 Fax:(877)670-1555

Dear Sir or Madam

Submission Number: 2 .21391 Transaction Number(s): W0180.30100

Subject: Approval of Assessment Work

We have approved your Assessment Work Submission with the above noted Transaction Numbers). The attached

Work Report Summary indicates the results of the approval.

At the discretion of the Ministry, the assessment work performed on the mining lands noted in this work

report may be subject to inspection and/or investigation at any time.

If you have any question regarding this correspondence, please contact BRUCE GATES by email at bruce.gates@ndm.gov.on.ea or by phone at (705) 670-5856.

Yours Sincerely,

Ron Gashinski

Supervisor, Geoscience Assessment Office

Cc: Resident Geologist

Leslie Michael Dyment (Claim Holder)

Assessment File Library

Leslie Michael Dyment (Assessment Office)

Visit our website at http://www.gov.on.ca/MNDM/LANDS/mlsmnpge.htm Page: 1 Correspondence 10:16174

PROVIMTU.1. HHIHG

MINING LAND TENURE

MAP

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Dale/Time of Issue Apr 25 2001

TOWNSHIP/AREA

MUNRO

U:21h Eastern

PLAN

M -0376

ADMINISTRATIVE DISTRICTS / DIVISIONSMining Division Larder Lake

Lxnd Titles/Registry Division COCHRANE

Ministry of Natural Resources District KIRKLAND LAKE

TOPOGRAPHIC LAND TENURE

Ei M.,,.,.LJ d*..!1 !: n-flf **

UcwiH al (letup,

QQ ,a ,

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LAND TENURE WITHDRAWALS

IMPORTANT NOTICES

LAND TENURE W ITHDRAWAL DESCRIPTIONS

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JiMS

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SE C l ION 1PUH2 HJ1.W. 1MJJ ?1'JJ0J

IMPORTANT NOTICES

SURFACE TRACE - PLAN V IEW

400mS SOOmS

DDH KDS-00-01

200mS 100mS OOOmS 100mN 200mN 300mN 400mN _______l________l________l________i

LO*75mW

KDS-00-01 EOH 479.0 m

SURFACE TRACE - PLAN V IEW

DRILL HOLE CROSS SECTION Q * 75 m W

400mS 3QOmS 200mS 10OmS

L O f 75 m W

OOOmS 100mN 200mN 300mN 400m N

1 l

WARDEN TOWNSHIPClaim Line

PLAN LOCATION OF DDH KDS-00-01 ALSO SHOWINGPREVIOUS DDH'S GRANGES 'PD' SERIES, CANAMAX 'AM' SERIES

LEGEND

Diabase Dyke Feldspar Porphyry Dykes

IBM Tholeiitic Basalt Dykes—— Gabbro——"Disseminated Sulphide——Massive Sulphide—— Sed. Seq. Argillite to Conglomerate ^ Tholeiitic Hyaloclastite HC—*—- Tholeiitic Basalt Flows TBS ^—Komatiitic Volcanics KUFS

A A A Spinifex Textured Flows •3 fi-bx^ Interflow Breccia

r~\ P illowed Flows

O SO 2Otl

DAVE GAMBLE GEOSERVICES INC70 First Street. Kirkland Lake, Ontario P2N1N3 Tel 705-567-4381 Fax 705-567-3801

MILLSTREAM MINES LTD.POTTERDOAL WEST PLUNGE PROPERTY

DDH KDS-00-01Surface Trace and Cross Section

along 0+ 75 m W (Looking West)MUNRO TOWNSHIP

Dare: SEPT2000

Scal* Scale B arNTS: 42A

Drawn Ret: kds0001 cdrFIG KDS0001

42A09SE2036 2.21391 MUNRO 210 9 *M391