MILLSTREAM MINES LIMITED j i!30 \ POTTER PROJECT - DIAMOND DRILL DATA ] ^ 1 SUMMER PROGRAM ^^^^^^^J DIRECTION. mama 601.5

Transcription

1 l" RECllr mxmmm START END mmmrnxwrnmrnm mm^^mimimm. MILLSTREAM MINES LIMITED j i!3 POTTER PROJECT DIAMOND DRILL DATA ] ^ 1 SUMMER PROGRAM ^^^^^^^J DIRECTION mama lim&m lalini lieirel ;:;:;;; : :::::;!:' ::::::::::;:B pt;:;;;;;;:;;:;:; : : :!;:'!:;: ^MmmmiiiMiiii :'lliil!^aloiii S961 S962 S963 S964 S965 S966 S967 7/3/96 7/14/96 7/21/96 7/26/96 8/5/96 8/8/96 8/12/96 7/13/96 7/2/96 7/25/96 8/4/96 8/7/96 8/12/96 8/13/96 75W 75W 45W 13W 13W 865W 16W 36 S 385 S 5 S 76 S 76 S 1 S 918 S MECH. PROBLEMS CLUTCH BROKEN GROUND MECH. PROBS CPLG. S968 8/13/96 8/14/ W 175 S ABANDON, BOULDER O/B S969 8/14/96 8/17/96 169W 725 N A9SE MUNRO 1 DRLLDATA.XLS

2 crv c ' *, H

3 l DAVE GAMBLE GEQSERVICES INC 7 First Street, Kirkland Lake, Ontario, P2N 1N3, Tel: , Fax: Project: MILLSTREAM MINES LIMITED Property: POTTER MINE PROJECT Twp/Claim: MUNRO TWP/ L 5395, L Hole No: S 96 1 MILLSTREAM MINES LIMITED DRILL RECORD Azimuth: 18 degrees Dip: 45 degrees Location: L7*5mW73*6mS Total Depth: 664.' ft. (32 Boxes) Started: July 3, Completed: July 13, Core Size: BQ Drilled By: Marathon Drilling Logged For: Millstream Mines Limited Logged By: Dave Gamble (Sept 8,1997) Tests: TD: 35' Dip: 4 deg. Az: TD: 65' Dip: 48 deg. Az: Purpose of Hole: To test a MaxMin M H.L.E.M. anomaly along strike from L 5 * 25 m W. Millstream Mines Limited personnel spotted and monitored the drilling of this hole during a summer, 1996 drill program. All drill hole information regarding the collar location, azimuth, inclination, date of drilling, anddrill contractor utilized, was supplied by Millstream Mines Limited personnel to DDG Inc who only carried out the logging of the drill hole S 96 1 in September, /^ Remarks 1 Results: The drill hole intersected a mafic pyroxenitic basalt flow ( or gabbro sill) and ultrajptft^fendotip basalt flow sequence. No samples were submitted for assay from this hole. 79.' 79.' 151.5' OVERBURDEN ^ X*^ ' V( tss^" ~ cjo^' i^ XoJc^ ^x"" BASALT FLOW PYROXENITIC ( medium to fine grained grey) s^ Medium grained interlocking texture of pale greenish plagioclase with pale buff tan brown to olive green fibrous to acicular pyroxene. Also dark greenish black equidimensional serpentinized olivine crystals The basalt flow is uniform massive to homogeneous throughout. Occasional isolated magnetite crystal grains and weak trace o<^% pyrrhotite locally. The medium grained crystalline texture is gabbroic looking in the thicker more massive medium grained parts of the flow. Contains several dark black fracture filled stringers at 91.5' and at 96.5' and at 1' at low angles TGA from 15 degrees To 3 degrees TGA. Unit is fractured at 35 deg. 55 deg. TGA. Becomes more fractured from ' 1 42' with dark green black chloritic linings, * or serpentine * or talc. Unit becomes finer grained crystalline gradually around 117' to a fine grained massive homogeneous grey basalt containing occasional 1 2 cm glomeroporphyritic knots of greenish white plagioclase crystals within a fine grained basalt groundmass. Magnetic susceptibility..2 c.g.s ^ap*ple lumber: Y* /^ / ^Arte. XT*" J^7 ^jf *Q 'ri ^ r C vc^g^r^ca u* ^^ **^~ :S *rv ^c,w "j,^*x^ Length S Cu Zn Ag 151.5' 157.5' BASALT U/M PERDOTITE FLOW BRECCIA A unit consisting of fine grained grey basalt (from above) and ultramafic basalt peridotite coarse fragments and /or blocks delineating the contact between grey basalt above and

4 Length Cu Zn Ag ultramafic peridotite below. Similar to a rubbly flow breccia. Upper contact appears as a fracture slip at 3 degrees TGA. Lower contact sharp at 15 degrees TGA and appears conformable ' 43.25' ULTRAMAFIC KOMATIITIC PERIDOTIC BASALT FLOW Upper contact sharp at 15 degrees TGA. The peridotite is dark green black, fine grained, slippery to feel, i.e. talcose to serpentinized. Several blocks of fine grained basalt equivalent to fine grained basalt from previous unit occurs at 176' 177', 186.5' 188.', 19.' 191.5', 199.' 2.25' as grey bleached xenoliths. Several glomeroporphyritic plagioclase clots up to 1 2 cm in size occur locally in the basalt xenolithic blocks. Contacts are generally irregular and unconformable to each other suggestive of a large fragment with irregular block boundaries. Unit is cut by numerous threadlike fractures filled with white calcite and green serpentine. The calcite threadlike stringers are fracture fillings and are irregular from deg. TGA to 4 deg. TGA. Several 5 mm veinlets of calcite occur at 175' 176' at 4 degrees TGA. Locally minor polysuturing is observed as dark green black serpentinized cooling features. Layering occurs locally where olivine cumulus lamellae or crude layering, now serpentinized occurrs, this fabric varies from 15 degrees 35 degrees TGA. The peridotite overall is massive, uniform dark green black, generally fine grained overall, locally evidence of polysuturing to polygonal fracturing, contains both white calcite fracture fillings and stringers to < 1/2 cm veinlets, also is extensively cut by pale green to dull green serpentine lined fractures. Magnetic susceptibility ranges from c.g.s. from 157.5' 36' with local increases at 36' to 7.8 c.g.s., and 7.5 c.g.s. from 36' 43.25'. Locally asbestos fibers occur as narrow < 1/8" fracture lined stringers occasionally throughout from 241' 346'. From 157.5' 346' numerous serpentine fractures from 2 degrees to 4 degrees TGA. Several 4 cm to 6 cm pale yellow green serpentine veinlets from 291' 292'. From 263.9' 264.3' a band of carbonitized bleached basalt at 45 degrees TGA. From 346' 43.25' a dark green to grey black peridotite with what looks like serpentinized layers to crudely formed spinifex, all possibly dark grey black serpentinized olivine. Also local polysuturing and layering at 367' at 45 degrees TGA. Lower contact sharp at 4 degrees TGA ' 664.' EOH BASALT FLOW ( as previous) Fine grained grey green basalt near contact to gradually becoming medium grained crystalline at 414', similar to unit at beginning of hole, gabbroic looking.

5 Length Cu ppm Zn ppm Ag ppm Au opt Massive, homogeneous, uniform basalt throughout to EOH at 664'., with occasional glomeroporphyritic 1 2 cm clusters or clots of plagioclase. Locally fractured, chlorite lined fractures at 15 degrees TCA at 474'. Green chlorite * calcite vein at 4 degrees TCA at 65.6' 66.', and at 631' ( 1" ) and 652' ( 1") at 4 degrees TCA. Magnetic susceptibility ranges from. 1. c.g.s. throughout unit, as follows: 43' 435',.2.4 c.g.s. 437'.7 c.g.s. 44' 477'..2 c.g.s. 481 '496'.5.8 c.g.s. 51 '56'.2.3 c.g.s. 51 1' 521'.7.9 c.g.s. 521 '556'..1 c.g.s. 561 '586'.4 1. c.g.s. 586' 664'..2 c.g.s. Broken core recovery 625' 627' and 66' 664'. Fractures in basalt, chlorite lined, thin at 4 6 degrees TCA, to EOH. EOH Note: There are 2 footage blocks marked 446', which are separated by 1' of core, therefore the hole is actually 1' longer i.e. EOH is 664' and all logging has been adjusted accordingly. x*"' ^* s ^^/ K /^^~P^?Z'

6 l DAVE GAMBLE GEOSERVICES INC 7 First Street, Kirkland Lake, Ontario, P2N 1N3, Tel: Fax: Project: MILLSTREAM MINES LIMITED Property: POTTER MINE PROJECT Twp/Claim: MUNRO TWP /L 5395 Hole No: S 96 2 MILLSTREAM MINES LIMITED DRILL RECORD Azimuth: degrees Dip: 45 degrees Location: L7*5mW73*85mS Total Depth: 75' ft. (39 Boxes) Started: July 14, Completed: July 2, Core Size: BQ Drilled By: Marathon Drilling Logged For: Millstream Mines Limited Logged By: Dave Gamble (Sept. 8,1997) Tests: TD: 365' Dip: 49 deg. Az: TD: 75' Dip: 48 deg. Az: Purpose of Hole: To test a MaxMin II HLEM anomaly along strike from L 5 * 25 m W. Scissor hole to S Millstream Mines Limited personnel spotted and monitored the drilling of this hole during a summer, 1996 drill program. All drill hole information regarding the collar location, azimuth, inclination, date of drilling, and drill contractor utilized, was supplied by Millstream Mines Limited personnel to DDG Inc who only carried out the logging of the drill hole S 96 2 in September, Remarks 1 Results: This hole intersected a layered mafic basalt pyroxenitic flow ( or gabbro sill ) and ultr^ftfscicwridotitic basalt flo H seqqence^jvlmor spinifex textured flow was noted over short intervals. A plagioclase porphyritic diorite dyke was encountered. No samples were submitted forass^ewfcahrc hole. 82.' ' V VV"" r. lp ' *1 it /.J O lc C/ v^ &J/ * r" ^ v ^^ 1 "lumber: ^^ ^^Jrf^^^ W, OVERBURDEN C*^' X^^^^"" ^ *J^ c^ <o<<ty 4^c/ ^^ * ^ BASALT FLOW PYROXENITIC V "^ V* y 7 Medium grained interlocking textured basalt, greenish grey in colour, contains interlocking s. X plagioclase and pyroxene and dark green black equidimensional serpentinized ^^^spf t olivine. Gradually becomes finer grained from 114' 14' as a fine grained massive basalt. ^J Possible chilled fine grained zone to a basalt flow with the central part of the flow taking on an intrusive or slower cooling crystalline texture of medium grained crystallinity and fine grained rapid chilling near the edges of the flow to a massive fine grained phase. Unit is fractured with chlorite lined fractures at 6 degrees TCA and several at low angles to the core axis at 15 degrees. Mag susceptibility..3 c.g.s. with locally higher values to.9 with locally isolated magnetite disseminations. Trace pyrrhotite locally. Lower contact sharp at 4 degrees TCA. Length Cu Zn Ag 14.' 162.5' ULTRAMAFIC KOMATIITIC PERIDOTITE BASALT Upper contact sharp at 4 degrees TCA. From 14.' 146.' spinifex texture with coarse blades of dark green serpentinized olivine no accurate fix as to layering i.e. variable orientations to the spinifex blades. Lower contact approximates 45 degrees TCA.

7 Length Cu Zn Au Ag 162.5' 439.5' BASALT FLOW ( as previous) Fine grained, medium grey green massive uniform basalt flow with occasional cream white to pale green plagioclase crystals and glomeroporphyritic plagioclase as 1 2 cm clusters or knots. Similar to fine grained basalt at beginning of hole. Unit is locally strongly fractures from 3 8 degrees TGA. Magnetic susceptibility...1 c.g.s. at '.2.3 c.g.s. at 21 8' 229'.62.1 c.g.s. at 231 '289'..2 c.g.s. at 294' 34' c.g.s. at 35' 32'..1 c.g.s. 32' 329' 1.' c.g.s. at 333'.1.5 c.g.s. 384' 394'..1 c.g.s. at 394' 41 9' c.g.s. 42' 428'..1 c.g.s. 43' 439.' Locally bleached with interstitial pervasive carbonate at 414.' 419.' Strongly fractured throughout, with broken core recovery 16' 22', 265' 344' moderately fractured, 344' 413' strongly broken, predominate fracture orientation 6 degrees TGA, also others at lower and higher angles to core axis. From 429' 439.5' bleached to light olive grey green, from 431 ' 438.5' strongly sheared broken zone, fault gouge 1" at 437', FAULT ZONE. Lower contact sharp at 55 degrees TGA * 479.5' FELDSPAR PORPHYRY INTERMEDIATE DYKE DIORITE Upper contact sharp at 55 degrees TGA. Uniform grey fine grained groundmass with 1/4* long x 1/1" wide euhedral lathes of white plagioclase imparting a uniform porphyritic texture. Also 1/16" and less dark greenish grey pyroxene euhedral crystals both as stubby cross sections and prismatic crystals. The groundmass is grey, slightly siliceous looking, probably intermediate or diorite composition. Lower contact is slightly scalloped approximately 45 degrees TGA, sheared and carbonate stringers at contact with underlying ultramafic unit. Magnetic susceptibility is. c.g.s. throughout.

8 Length Cu Zn Au Ag 479.5' 75.' EOH LAYERED ULTRAMAFIC PERIDOTIC BASALT, LEUCOBASALT, MASSIVE AND SPINIFEX TEXTURED FLOW SEQUENCE Fine grained, dark green black massive flow with darker black polysuturing cooling fractures. The flow unit is serpentized with remnant olivine equant 1 mm crystals completely serpentized to dark green black serpentine. Flow unit is cut locally by white calcite threadlike stringers and occasional white calcite veinlets most noticeable near upper contact from 479.5' 485'. Calcite veinlets 1" at 483.5' and 1" at 485 at 45 degrees TGA. Foliation fabric at 45 degrees TGA, locally strong fabric. Calcite veinlet 1 1/2" at 512.5' at 8 9 degrees TGA. Calcite veinlet 2" at 6 degrees TGA. Calcite veinlet 3" at 45 degrees Uct 8 degrees Let. Unit is weak to moderately fractured with serpentinized slips. Mag susceptibility varies from c.g.s. with the higher values reflecting slight increase in finely disseminated magnetite. Increase in fracturing and broken core from 532' 567'. Internal flow contact at 6 degrees TGA to a lighter grey green leuco basalt flow sequence with slight bleaching and broken ground from ' 583.'. From 589' 68' a flow agglomerate clasts 2 4' in size. Also some possible polysuturing. From 583' 673' massive fractured flow, some local polysuturing and serpentinized fracture slips. From 674' 677' fine bladed spinifex textured flow in grey green basalt. From 677' 686' fine grained massive flow as previous. Magnetic susceptibility..1 c.g.s. from ' 686'. From 686' 75' a massive dark green polysutured ( talc * serpentine filled polygonal fractures) flow sequence with magnetic susceptibility ranging from c.g.s. varying with disseminated magnetite content. Strongly fractured with serpentinizing slips. Locally broken over short intervals, strongly broken 734' 75' at EOH. EOH ^ /;, 7f^^2/^ X~~i5*^r^ s

9 l DAVE GAMBLE GEOSERVICES INC 7 First Street, Kirkland Lake, Ontario, P2N 1N3, Tel: , Fax: Project: MILLSTREAM MINES LIMITED Property: POTTER MINE PROJECT Twp/Claim: MUNRO TWP 1 L Hole No: S 96 3 MILLSTREAM MINES LIMITED DRILL RECORD Azimuth: 212 degrees Dip: 45 degrees Location: L4*5mW75*OOmS Total Depth: 64' ft. (33 Boxes) Started: July Completed: July 25, Core Size: BQ Drilled By: Marathon Drilling Logged For: Midstream Mines Limited Logged By: Dave Gamble (Sept. 8,1997) Tests: TD: 35' Dip: 46 deg. Az: TD: 599' Dip: 47 deg. Az: Purpose of Hole: To test a MaxMin d H.L.E.M. anomaly located on L 5 * 75 m W and under the east tailings area. Midstream Mines Limited personnel spotted and monitored the drilling of this hole during a summer 1996 drill program. All drill hole information regarding the collar location, azimuth, inclination, date of drilling, and drill contractor utilized, was supplied by Midstream Mines Limited personnel to DDG Inc who only carried out the logging of the drill hole S 96 3 in September, Remarks 1 Results: This hole intersected an ultramafic to mafic basalt flow sequence with minor flow agglomerate. Trace specks of pyrrhotite and chalcopyrite were observed locally along serpentized slips and in calcite fractures. From this hole 1 sample ( ) was submitted for Au, Ag, asi^r^nd returned insignificant values. 2.' 16.5' 16.' 4^fi ^xx.,,v. OkX^*" r^ff'l^ * t ^^ l c^jfc o^*y^ ^^ N.^T^ ^^^ OVERBURDEN c^cj^5x'.c^" ^r ULTRAMAFIC KOMATIITIC PERIDOTITE BASALT FLOW V ^ Massive, fine grained dark green black serpentinized peridotite flow with l&cally weak polysuturing with flow agglomerate short intervals. Fractured and slippery serpentized fracture slips at 45 degrees to 8 degrees TGA. From at 41.5' 43.25' slightly bleached grey green with fine bladed spinifex texture, mag susceptibility.2.4 c.g.s. in spinifex bleached section of flow. The massive flow varies from c.g.s. magnetic susceptibility with the variation due to variation of disseminated magnetite from 16.5' 16.'. Broken core recovered, fractured flow 14' 15.5'. Lower contact diffuse but delineated by a marked change in magnetic susceptibility and also colour change to leuco basalt flow, contact estimated at 6 degrees TGA. ^ample ftumber: Length Cu Zn Ag 16.' 64.' EOH BASALT FLOW SEQUENCE Medium to dark green in colour, not as dark as the greenish black peridotite but more of a grey green with local darker green sections. Flow is overall fine grained, massive in texture, uniform in appearance with short intervals of polysuturing to flow agglomerate 184' 187'. Magnetic susceptibility..1 c.g.s. throughout with local minor variations of c.g.s.

10 * Previous Length Cu Zn Au Ag from 154' 158'; 2.3' 2.5' c.g.s. from 214' 225', that represent a slightly more ultramafic differentiate in the leuco basalt sequence. The contacts are vague to diffuse but seem to approximate 3 degrees TGA, and again at 444' 452' with c.g.s., and again at 574' 586' with c.g.s.; Broken fractured core, serpentinized slips 122' 123'; 133' 134', 137' 139', plus trace cpy on polished slips, 141' 142', 24' 241' 252' 268' 313' 32', 349' 351', 36' 369' 397' 398', 462' 464'. From 25' 21' fine threadlike to stringers of quartz containing occasional splashes and specks of chalcopyrite and pyrrhotite. The flow continues to be fine grained with patchy minor 12 mm feldspar weakly porphyritic texture observed locally. Local calcite threadlike fracture fillings and minor stringer veinlets 269' 27' at 3 5 degrees TGA, 3.5' ( 1/2") at 45 degrees TGA; 321' ( 1/2") at 45 degrees TGA; at 323.5' ( 1") at 3 degrees TGA; 325.5' ( 1") at 5 degrees TGA; at 364.5' ( 1 1/2") at 15 degrees TGA; 393.5' ( 3" ) at 25 degrees TGA; Flow breccia agglomerate 43' 433', 515' 516', 52.5' 521.5', 531' 569' flow to flow agglomerate, massive to rubbly agglomerate. Trace chalcopyrite and pyrrhotite along fractures occur at 356', 397', 462' 496' 51', 512.5' 514.5', 516.5', 532', 537', 555.5', 575', in 1/16" calcite fracture filling at 3 degrees TGA. At 63.5' 64' EOH weak fine spinifex texture with internal flow contact at 45 degrees TGA. From 574' to 64' dark green black peridotite, serpentinized, seems to be leading towards more ultramafic sequence downhole. EOH. ^,..njyl/sf J^l^fi*^/^* S *^/'

11 DAVE GAMBLE GEOSERVICES INC 7 First Street, Kirkland Lake, Ontario, P2N 1N3, Tel: , Fax: MILLSTREAM MINES LIMITED DRILL RECORD Project: MILLSTREAM MINES LIMITED Azimuth: 19 degrees Started: July Logged For: Millstream Mines Limited Property: POTTER MINE PROJECT Dip: 45 degrees Completed: Aug. 4,1996. Logged By: Dave Gamble (Sept. 1,1997) Twp/Claim: MUNRO TWP/ L 53952, L Location: L 1 * 3 m W 17 * 6 m S Core Size: BQ Tests: TD: 375' Dip: 48 deg. Az: Hole No: S964 Total Depth: 86' ft. ( 46 Boxes) Drilled By: Marathon Drilling TD: 86' Dip: 47 deg. Az: Purpose of Hole: To test an area below and proximal to the pitted surface showing at grid coordinates 1 * 75 m W 1 9 * 6 m S. Millstream Mines Limited personnel spotted and monitored the drilling of this hole during a summer 1996 drill program. All drill hole information regarding the collar location, azimuth, inclination, date of drilling, and drill contractor utilized, was supplied by Millstream Mines Limited personnel to DOG Inc who only carried out the logging of the drill hole S 96 4 in September, Remarks l Results: This hole intersected a layered differentiated mafic pyroxenitic basalt to ultramafic peridotitic basalt alternating flow sequence. Several fault zones with accompanying bleaching, silicification and pervasive carbonization were encountered. An interflow grey siliceous sedimentary horizon locally pyritic was also intersected. From this hole 4 samples ( ) were submitted for Au, Ag assay and returned insignificant values. Numberjj Length Cu Zn Ag 9.5' 9.5' OVERBURDEN 537.' ULTRAMAFIC KOMATIITIC PERIDOTITIC TO LEUCOBASALT LAYERED DIFFERENTIATED FLOW SEQUENCE 9.5' 27.' BASALT FLOW pyroxenitic green Massive uniform fine to medium grained crystalline with 1/8' to 1/4" dark green talc/chlorite spots in fine grained part of the flow. The medium grained flow consists of a mottled texture of pyroxene and occasional plagioclase lathes. The overall colour is medium to medium dark green. Trace specks of chalcopyrite. Magnetic susceptibility..1 c.g.s. with a slight increase to.6 c.g.s. near lower contact. Lower contact 35 degrees TGA. 27.' 31.5' PERIDOTITIC BASALT FLOW dark green black. Massive, SO degrees TGA, dark green black serpentinized (olivine) peridotite flow, contains finely disseminated magnetite with mag susceptibility varying from c.g.s. Lower contact sharp and conformable to 1/8" serpentinized olivine 45 degrees TGA. The layering is delineated by 1/8" serpentinized black equant olivine layers with disseminated magnetite and with grey pyroxene. rf*

12 Length Cu Zn Au Ag 31.5' 118.5' BASALT FLOW ( as previous) pyroxenite green. Massive, uniform green basalt flow containing 1/4" rounded dark green spots ( talc * chlorite) in a fine grained groundmass. Minor carbonate stringer 35 degrees TGA 1/4" at 63.75'. Unit becomes gradually medium grained near gradational lower contact ' 137.' PERIDOTITE BASALT dark green black Upper contact is a gradational colour change from green to green black of a medium grained crystalline peridotite with disseminated magnetite and mag susceptibility e.g. s. and gradually tapering to lower readings near the upper gradual contact.9 c.g.s. and lower gradational contact 2.3 to.2 c.g.s. The presence of gradational peridotite to basalt is significant as it clearly illustrates the presence of an ultramafic to basalt differentiation trend. The high mag susceptibility readings are attributed to disseminated magnetite. 137.' 28.' BASALT FLOW ( as previous) pyroxenitic green magnetic susceptibility.1.2 c.g.s. throughout with gradual increase of.4 1. c.g.s. from 193' 28'. The lower contact is again a gradational contact delineated by a marked increase in magnetite contact and mag susceptibility below 28'. From 193' 28' are gradual increase in peridotite component again indicative of differentiating flow sequence. 28' 245' PERIDOTITE BASALT ( as previous) dark green black Black serpentinized olivine equant crystal grains (1/16") that form layers or striping at 5 degrees TGA. Interlocking grey pyroxene to weakly oikocrystic pyroxene occurs near lower contact from 237' 245'. Mag susceptibility varies from c.g.s. throughout unit with strongly disseminated magnetite. Lower contact sharp and 45 degrees TGA ' BASALT FLOW green pyroxenitic as previous, uniform massive fine grained with minor varitextured serpentinized olivine peridotitic/peroxenitic 5 degrees TGA at 278.6' 279.5' and at 28.5' 281.' containing weakly disseminated magnetite and serpentinized equant olivine grains. Magnetic susceptibility.1.2 c.g.s. throughout with gradual increase near lower contact from c.g.s. from 35' ' feet that is also corresponding to an increase gradually of serpentinized olivine towards actual lower contact. Lower contact 5 degrees TGA.

13 Length Cu Zn Au Ag ' ' PERIDOTITIC BASALT dark green black oikocrystic pyroxene as previous, uniform massive serpentinized peridotitic flow with 1 cm oikocrysts of grey pyroxene evenly distributed throughout. Strongly magnetic with disseminated magnetite with mag susceptibility ranging from c.g.s. Several yellow green serpentine veinlets occur at 337' ( 5 degrees TGA, 339' ( 1 degrees TGA, at 373 ( 3 degrees TGA, 384' ( 5 degrees TGA, 39' ( 5 degrees TGA. Minor basalt layer or fragment at 391 ' 391.5' 1/4" hematite red seam 6 degrees TGA. Lower contact sharp at 5 degrees TGA ' 46.' BASALT FLOW green pyroxenitic Pale green plagioclase pyroxenitic flow with magnetic susceptibility.2.4 c.g.s. Lower contact 4 degrees TGA. 46.' 537.' PERIDOTITIC BASALT FLOW dark green black as previous with grey 1 2 cm rounded oikocrystic pyroxene (and / or plagioclase) with black serpentinized olivine interstitial to the grey clots. At 433' start to loose the grey clots and unit becomes more of a speckled black equant serpentinized 1/16" olivine grains in a grey matrix of pyroxene and plagioclase that is fine grained. Magnetic susceptibility 46' 463' is c.g.s. Layering approximated 5 degrees TGA. From 463' 514' unit is speckled with equant 1/16" serpentinized olivine crystals that are black within a fine grained grey green groundmass. There tends to be clusters of serpentinized olivine forming a crude layering at 5 degrees TGA. Magnetic susceptibility c.g.s. 463' 495'. Several white calcite veins and stringers at ( 45 degrees TGA, 49' ( 1/2" and 8 degrees and 3 degrees TGA at 54.' ( 1 degrees TGA. From 59.5' an increase in thin white calcite stringers and veinlets. At 514' 514.3', a 4" mud gouge FAULT ZONE at 65 degrees TGA upper contact and 7 degrees TGA lower contact. From 514.3' 537.' CARBONATE ALTERATION ZONE that alters the ultramafic flow to strong buff tan coloured that is pervasively bleached with massive interstitial style of carbonate. Numerous threadlike stringers of calcite. Patchy talc rich rock still preserved to 537'. From 536' 537 last of talcose material at 55 degrees TGA with accompanying white

14 Length Cu Zn Au Ag calcite and minor quartz stringer veining..1 c.g.s. mag susceptibility. 537.' 538.' FAULT ZONE 537.' 538.' with mud gouge and fabric at 6 degrees TGA contains calcite and minor quartz broken stringers. 538.' 63 BASALT FLOW CARBONATE ALTERATION ZONE continues from the fault at 538' 568' that is extensively carbonate altered buff tan to grey green with numerous white calcite stringers. A number of calcite stringers and veinlets at 5 6 degrees TCA and several at low angles to core axis at 5 1degrees TCA. Locally trace to 1 7o disseminated pyrite. Mag susceptibility in alteration zone ranges from..1 c.g.s. The lower contact of the alteration at 568' approximates 5 degrees TCA. From 568' ' basalt flow is fine grained massive and uniform, contain threadllike white calcite fracture fillings predominantly at 5 6 degrees TCA. At 614.5' a 2" fine grained quartz vein 1 3 degrees TCA. At ' a contact of fine to medium grained flow that is also the start of pervasive silicification and bleaching discolouring the rock to pale apple green to pale olive green, possibly a mixture of epidote and quartz. At 634.5' 63 broken core fracture zone and possible FAULT at 6 75 degrees TCA.. c.g.s. mag susceptibility in alteration zone ' PERIDOTITE BASALT FLOW From 635' 655' continuation of bleached alteration zone from above and consists of a pale yellow green, sausseritized and silicified alteration zone. The bleaching has not obliterated several narrow spinifex textured intervals that occur 644.' 644.5' and at 649.' In addition to the overall bleaching quartz veins, stringers and vein breccia occur generally at 5 degrees TCA, locally throughout. At 636' 637.5' quartz vein breccia at 1 5 degrees TCA upper contact, and 45 degrees TCA lower contact. At 638.' ( 4") vein breccia 5 degrees TCA, 638.5' ( 65 degrees TCA, 64' ( 2") 45 degrees TCA, 642.5' ( 2") stringers, 643.' ' vein stringers and vein 45 degrees TCA. 649.' 65.5' veins and 5 degrees TCA. From 655' 712' unit is dark green, talcose with quartz threadlike stringers and several veinlets from 655' 5 degrees TCA. Quartz vein 55 degrees TCA. Below 667' 712' all stringers and veinlets are calcite with no quartz.

15 Length Cu Zn Au Ag Magnetic susceptibility in bleached alteration zone 635' 655' is. c.g.s. In the talcose dark green rock with quartz stringers the mag susceptibility is.1 c.g.s. As soon as calcite stringers begin the mag susceptibility rapidly increases from.2 c.g.s. to.4 c.g.s. over several feet, and the remaining part of the unit varies from.6 to 5.1 c.g.s. The unit is dark green black with a layering fabric of 5 degrees TGA at 74'. Lower contact sharp at 5 degrees TGA. 712.' BASALT FLOW green pyroxenitic ( as previous) mag susceptibility.1.3 c.g.s. throughout. Lower contact has been previously split for sampling, no accurate measurement but could be approximated at 5 degrees TGA. 736.' 822.' SILICEOUS GREY SEDIMENT Very fine grained, extremely hard siliceous, occasional thin beds of cherty material at 5 6 degrees TGA. The unit is medium grey in colour overall. Locally lighter grey granular in appearance but still extremely siliceous. A large part of this sedimentary horizon is fractured to a brecciated cherty siliceous unit with irregular shaped angular medium grey breccia that are densely packed to being clast supported, size of cherty breccia fragments 1" 3" with a darker grey 1/16" and less black pencil line matrix to the clastic population. Disseminated pyrite occurs from 736' 741' as finely disseminated < 1 mm pyrite flecks and grains. Locally several narrow bands or heavily disseminate pyrite to 4 Va over several inches. Calcite stringers and veins ' ( 3 degrees TGA and at 759.' ( 6 degrees TGA. Mag susceptibility.1.2 throughout. Crude bedding lamellae at 779' 78' at 6 degrees TGA. Lower contact broken to rubbly core recovered. Several intervals occur at 759' 775' and at 87' 812' appear like fine to medium grained tuff sedimentary material that are also strongly siliceous and hard that show granular variation are also included in this sedimentary horizon ' 741' 817' 741' 746' 822' ' 86' BASALT FLOW PYROXENITIC carbonate altered. Medium grained massive uniform flow pyroxenitic, bleached pale green by pervasive carbonate and cut by calcite stringers and veinlets at 2 9 degrees TGA. Also locally small patches of fuchsite associated with the calcite veinlets at 822.5' 824.' at 65 8 degrees TGA. Upper contact is broken by previous sampling but appears to 5 degrees TGA. Mag susceptibility. c.g.s. throughout to EOH ' 838'.1

16 Length Cu Zn Au Ag Calcite veins at 822' 65 9 degrees TGA at 827' 6 degrees TCA at 829.5' 83' at 2 degrees Uct and 5 degrees TGA, Let at 5 degrees TCA at 832' 4 degrees TCA stringers at 836.5' 7 degrees Uct 3 degrees Let at 842.5' ( 65 degrees TCA at 858.3' ( 2 1/2" 5 degrees TCA. EOH ^ x~ t X/ XX^v^x ^A^fc^^%^ X *Jt ^j

17 DAVE GAMBLE GEOSERVICES INC 7 First Street, Kirkland Lake, Ontario, P2N 1N3, Tel: , Fax: Project: MILLSTREAM MINES LIMITED Property: POTTER MINE PROJECT Twp/Claim: MUNRO TWP 1 L 53952, L Hole No: S 96 5 MILLSTREAM MINES LIMITED DRILL RECORD Azimuth: 19 degrees Dip: 6 degrees Location: L 1 * 3 m W 1 7 * 6 m S Total Depth: 724' ft. ( 39 Boxes ) Started: Aug 5, Completed: Aug. 7, Core Size: BQ Drilled By: Marathon Drilling Logged For: Millstream Mines Limited Logged By: Dave Gamble (Sept. 12,1997) Tests: TD: 38' Dip:57deg. Az: TD: Dip: Az: Purpose of Hole: To test an area below and proximal to the pitted surface showing at grid coordinates mw 1 9 * 6 m S. Millstream Mines Limited personnel spotted and monitored the drilling of this hole during a summer 1996 drill program. All drill hole information regarding the collar location, azimuth, inclination, date of drilling, and drill contractor utilized, was supplied by Millstream Mines Limited personnel to DOG Inc. who only carried out the logging of the drill hole S 96 5 in September, Remarks 1 Results: This hole intersected a layered differentiated mafic pyroxenitic basalt to ultramafic peridotitic basalt alternating flow sequence. Several fault zones with accompanying bleaching.silicification and pervasive carbonitization were encountred. Trace pyrite, pyrrhotite and occassional speck of chalcopyrite were noted. From this hole 5 samples ( ) were submitted for Au, Ag assay of which one sample also assayed for Pt, Pd. Assay results returned insignificant values ' 12.' ' 12.' 41.5' OVERBURDEN ULTRAMAFIC TO MAFIC KOMATIITIC LAYERED BASALT FLOW SEQUENCE PERIDOTITIC BASALT FLOW, medium grained green massive uniform flow, slightly darker greenish black serpentinized peridotitic flow from 9.' 12.'. Mag susceptibility.5.8 c.g.s. and increasing to c.g.s. from 9.' 12. '. Lower contact gradual approximately 5 degrees TGA. PYROXENITIC BASALT FLOW Medium to fine grained, green pyroxenitic flow with locally 1/4" dark green talc * chlorite rounded spots, locally white plagioclase intercumulus, lower contact sharp and 45 degrees TGA. Mag susceptibility.1.4 c.g.s. throughout. s S X From^ fo ^V rr ' c Jy ^ ( ^V /f? x^ ^y J* x /X. ^ ^,*5?,^ f Crs' 3? y ' P**/. T,xy cvv #^/ * 7 f f Length ^f Cu Zn Ag 41.5' 48.25' PERIDOTITIC BASALT FLOW Dark green black serpentinized peridotitic flow layer, contains trace pyrrhotite as fine disseminations and fracture fillings at upper contact. Lower contact is gradational over several inches and approximates 4 45 degrees TGA. Mag susceptibility c.g.s., strongly magnetic with disseminated magnetite. Locally varitextured with oikocrysts of pyroxene and poikolitic serpentinized olivine.

18 Length Pt Pd Au Ag 48.25' 153.5' PYROXENITE BASALT FLOW ( as previous) Massive uniform pyroxenite basalt flow fine to medium grained with locally 1/4" dark green talc * chlorite altered pyroxene spots and square stubby altered pyroxene crystals. Quartz * calcite vein 92.25' 4 degrees TGA. Trace pyrite * pyrrhotite * several flecks chalcopyrite along serpentinized fracture slips at 124', 129' 132' at 1 degrees TGA. Mag susceptibility..1 c.g.s. throughout. Lower contact gradational over several inches approximately degrees TGA ' 172.' PERIDOTITE BASALT FLOW ( as previous) Dark green black with black serpentinized 1/16" olivine * grey pyroxene fine to medium grained, layered 45 degrees TGA. Some lighter green sections representing local differentiation variations. Mag susceptibility c.g.s. throughout. Lower contact gradational again representing differentiation trends and approximates 35 degrees TGA PYROXENITE BASALT FLOW ( as previous) Uniform massive green fine to medium grained. Mag susceptibility..1 c.g.s. from 172.' 247.'. Trace specks pyrrhotite and chalcopyrite disseminated and occasionally along serpentinized slips 196' 21.. From 247.' 263.6' a mixed pyroxenitic basalt with minor peridotite component with green to dark green black local variations and mag susceptibility varying from c.g.s. Lower contact gradational over several 35 degrees TGA ' 21. (.1 co.ooi ND ' 314.1' PERIDOTITE BASALT FLOW Dark green black with 1/16" serpentinized equant olivine crystals and oikocrysts of grey pyroxene with serpentinized olivine in a poikolitic texture. Internal layering of 35 degrees TGA at 266' and 3 degrees TGA at 313'. Green serpentine fracture filling at 289.5' over 1" at 6 degrees TGA. Strongly magnetic with disseminated magnetite and Mag susceptibility c.g.s. throughout. Lower contact 35 degrees TGA ' 396.' PYROXENITIC BASALT FLOW Medium green, uniform massive fine grained with occasional dark green 1/4" clots and spots of altered pyroxene.

19 Length Cu Zn Au Ag Mag susceptibility..1 c.g.s. throughout and gradually increases from 384' towards lower contact from.1 to.4 to 4. c.g.s. again representing a gradation in the differentiation of a single flow with respect to colour and magnetite content. Lower contact is sharply defined by rapid increase in black serpentinized 35 degrees TGA to the peridotite flow unit below. The transition zone from clearly peridotite to pyroxenitic basalt is indicative of a differentiated flow sequence trending from ultra mafic to mafic suggesting stratigraphic tops are up hole or northwards. 396.' 496.6' PERIDOTITE BASALT FLOW ( as previous) Dark green black 1/16" equant serpentinized olivine crystals and oikocrysts of pyroxene medium grey, irregular embayed 1 2 cm pyroxene " oiks" that have a poikolitic texture of included black serpentinized olivine 1/16" equant sized crystals. Mag susceptibility c.g.s., strongly magnetic with disseminated magnetite. Layering 55 degrees TGA at 397.5', 4 5 degrees TGA at 399', 35 degrees TGA at 427', 55 degrees TGA at 474'. Throughout unit are 1/2" to 1" seams of fracture fillings of olive green serpentine, generally at conformable orientations to the layering 45 6 degrees TGA. From 47' 496.6' some of the olive green serpentine fracture fillings are crosscutting the layering fabric at 1 to 3 degrees TGA as well as paralleling the layered fabric. Lower contact 45 degrees TGA ' 59.' PYROXENITIC BASALT FLOW ( as previous) Medium to pale green, fine to medium green massive uniform flow cut by 1/4" and less calcite fracture fillings as stringers and veinlets at 3 degrees to 8 degrees TGA. Lower contact 35 degrees TGA. Magnetic susceptibility c.g.s. overall. 59.' ' PERIDOTITE BASALT FLOW From a dark green peridotite flow now talcose with abundant calcite threadlike fracture filled stringers and veinlets and veining at 35 5 degrees TGA and several late 1/4" calcite 2 3 degrees TGA. At 514.5' ( 1 1/2") calcite at 45 degrees TGA, at 516' ( 2" ) at 55 degrees TGA, 516.8' 517.' white calcite at 45 degrees TGA, at 517.' 519.' numerous white 1/4" 1 " calcite veinlets at degrees TGA, and at 52.9' 521.5' greenish white calcite laminated vein stringers at 45 degrees TGA. Mag susceptibility of carbonate * talc altered flow c.g.s.

20 Length Cu Zn Au Ag From 521.7' 573.' PERIDOTITIC BASALT ( as previous) Dark green black is colour with dark black serpentinized fractures, contains serpentinized equant olivine and oikocrysts of grey pyroxene with poikolitic olivine texture. Only several minor white calcite stringer fracture fillings and at ' a finely laminated white calcite stringer veinlet at 3 degrees TGA. Magnetic susceptibility c.g.s. throughout with finely disseminated magnetite. From 573.' ' talc carbonate altered peridotitic basalt flow. Broken core recovery 575' 581 ' with a possible fault fracture zone. Numerous white calcite stringers and veinlets throughout as previous at 59' 521.7'. Possible fault breccia 575' 577' but little actual fault or mud gouge recovered. From 581' ' talcose with dark green colour, fine grained, cut by numerous calcite 4 6 degrees TGA and some irregular fracture fillings. Lower contact is abrupt at 6 degrees TGA. Mag susceptibility c.g.s ' 647.' PYROXENITE BASALT FLOW Extensively bleached buff tan olive green ALTERATION ZONE from ' 597.' and cut by quartz stringers and veinlets. Quartz stringer vein 591.' 55 degrees TGA and from 592.5' 593.5' grey 5 degrees TGA with minor FAULT 5 degrees TGA at '. Quartz stringers and veinlets 6 degrees TGA at 596' 596.5'. Shear 3 degrees TGA at 597'. From 597' 618' mottled textured weakly altered pyroxenide basalt flow cut by quartz veinlets at 599' ( 3 degrees TGA. 61 ' ( 6 degrees TGA, 67.5' ( 1 1/2") 2 55 degrees TGA, ' ( 3 degrees TGA, 613' ( 3 degrees TGA' 614.5' ( 1 3 degrees TGA and ' ( 55 degrees TGA. The pyroxenite is weakly altered with mottled yellowish green brown epidote. Mag susceptibility.2.7 c.g.s. overall. From 618' 647' ALTERATION ZONE of pervasively silicified and sausseritized basalt to a fine grained fractured buff tan altered unit cut by quartz threadlike healed microfractures and several white quartz veinlets. Trace pyrite locally. Mud FAULT 8 degrees TGA at 64'over 2". Preserved spinifex texture locally at 645' 646.5'. Lower contact of bleached alteration zone at 45 degrees TGA delineated by laminated quartz stringers ' 623.' 633.' 643.' 623.' 628.' 638.' 648.' Nil Nil Nil Nil ' 724.' EOH PYROXENITE BASALT FLOW ( as previous) Dark green to medium green, talcose fine grained with quartz stringers and veinlets to 667', and from 667' 724' fracture fillings are calcite. Unit is generally massive uniform flow.

21 Length Cu Zn Au Ag Mag susceptibility..1 to 657'. and.1.3 c.g.s. to 724' with minor local variation up to.6 c.g.s. Spinifex finely bladed texture 656.5' 658.5' and 663.5' 664.5' and at 668.' and at '. Local bleaching 661.5' 664.5' to pale green, epidote * quartz veinlets at 55 degrees TCA.Local shearing 35 4 degrees TGA. Possible rounded 3" flow agglomerate 711' 713'. EOH /^pj S sjj&^ry /J Jfcf 'Tj&'ld^' Zr^f&^P /s jzy*?^ ^*^^ ' "W

22 Project: MILLSTREAM MINES LIMITED Property: POTTER MINE PROJECT Twp/Claim: MUNRO TWP/ L Hole No: S First Street, Kirkland Lake, Ontario, P2N 1N3, Tel: , Fax: MILLSTREAM MINES LIMITED DRILL RECORD Azimuth: 25 degrees Dip: 45 degrees Location: L 8 * 65 m W 7 1 * m S Total Depth: 681.' ft. (36 Boxes) Started: Aug 8, Completed: Aug 12, Core Size: BQ Drilled By: Marathon Drilling Logged For: Millstream Mines Limited Logged By: Dave Gamble (May 9, 1997) Tests: TD: 372' Dip: 42 Az: TD: 68' Dip: 43 Az: Purpose of Hole: To test a MaxMin II H.L.E.M. anomaly. Millstream Mines Limited personnel spotted and monitored the drilling of this hole during a summer/fall 1996 drill program. All drill hole information regarding the collar location, azimuth, inclination, date of drilling, and drill contractor utilized, was supplied by Millstream Mines Limited personnel to DOG Inc who only carried out the logging of the drill hole S Remarks 7 Results: The drill hole intersected an ultramafic komatiitic basalt flow sequence starting in an assemblage of serpentinized olivine+pyroxene+magnetite dunite to peridotite uniform massive flow sequence from 6.'22, and then into weakly polysutured massive pyroxene basalt flow sequence from ', and back into dunite to peridotite flow sequence as previous from '349.5'. From 349.5'681.' the hole intersected fine to medium grained crystalline pyroxene thick series of basalt flows or gabbro sill. Weakly disseminated and fracture controlled po + cpy occurs from 66.'681.' in a pyroxene 'gabbro' cumulate. From this hole 4 samples (1 sample previously taken not njhqbered, and 3 samples ) were submitted for Cu, Zn, Ag assay. 6.' 6.' 22 OVERBURDEN (Casing left in hole) ULTRAMAFIC KOMATIITIC DUNITE to PYROXENITE UNIFORM FLOW MAGNETITE RICH Dark green black olivine cumulate with oikocrysts of gray pyroxene encapsulating the dark black equant olivine crystals in a poikolitic texture. The olivine appears to be 13mny dark black equant crystals (serpentinized) within medium gray oikocrysts of pyroxene. *" The rock is slippery to feel, talcose, and contains disseminated magnetite, strongly ""s magnetic, ( c.g.s. mag susceptibility, usually c.g.s. throughout). Fractures are lined with a medium green talc/serpentine from 1 degrees to 6 degrees TCA. Local tension gash fillings of 13 mm asbestos fibers occurs as thread like fractures from ft. Several low angle 12 degrees 1/4 "1/2" fracture filled veinlets of pale green talc and serpentine occur at 4.', 43.', 48.7', 64.5' ( 1/4" 2"), 77.8' ( 2"), and at 79. ( 2") at moderate angles to the core axis of approximately 6 degrees TCA but can be variable. The pyroxene oikocrysts are variable in character from weakly diffuse 1/4"! /2" to well developed 1/2" to 1" with black olivine inclusions, poikolitic texture. More talc and serpentine green and white fracture fillings, 174"178" (could possibly be polysuturing) at 13 degrees TCA at 86.', 87.', 9.', 91.' 94.'. Locally asbestos occurs from 89.'99.' as minor fracture fillings. Massive uniform 12" coarse oikocrysts of pyroxene, gray in colour, with 12 mm black equant olivine crystal cumulate, fairly uniform flow throughout. Magnetite occurs as Samptfrx Numbyy /C~* "Jj kj^ fjf A *s ^ *, c ^"v^ /. *^T 2 s^vn ^ ^ i * &U/ JW ^7 gf y ' Length Cu Zn Ag

23 4 Length Cu Zn Ag intercumulus to the olivine and pyroxene crystals. Trace pyrite along several talc/serpentine slips occurs locally throughout. Talc and green serpentine fracture 5 degrees TGA, 1/4" fracture at 172.5'17, and at 176.5' 35 degrees TGA, and at 181.' 35 degrees TGA. Bleached epidote+clinozoisite (?) * quartz/carb vein at 35 degrees TGA 191.' 191.5'. At 2.'2.5' green serpentine laminated at 3 degrees TGA (as previous). At 24.5' 2" green serpentine finely laminated medium green at 35 degrees TGA. At " serpentine fracture filling at 5 degrees TGA. At 29.5' ' a bleached zone, fracture 2 degrees TGA, bleached pale green white epidote to clinozoisite * or quartz. From 212.'22 coarse pyroxene oikocrysts as previous, 1/2" 2" "oiks", and black olivine serpentinized 13 mm equant crystals. From 223.'22 black threadlike fracturing, weakly conductive as black talc or sooty graphite, possibly cooling fractures near contact, a form of weak polysuturing. Lower contact sharp but irregular to diffuse at approximately 7 degrees TGA ' BASALT FLOW Gray green fine grained crystalline, uniform to massive throughout. Weakly magnetic c.g.s. magnetic susceptibility, finely disseminated magnetite in areas of higher magnetic susceptibility readings. Broken core ' recovered. Possible flow banding at 237.' Narrow flow breccia rubble over several inches at 243.', rounded fine grained 1/4" basalt flow breccia fragments. Fine 12 mm dark gray talc/chlorite spots and flecks occurs locally throughout. From 257.'262.' flow is weakly pyroxenitic to pegmatoidal (medium grained pyroxene), and is darker green black and similar to preceding peridotite unit. Also evidence of several well developed polysutures locally. Similar textural variation of medium grained pyroxenite phase at 274.5' 27 From 277.5' ' weakly bleached with minor threadlike calcite fracture fillings and 1/4" calcite veinlets. lower contact 5 degrees TGA. Lower bleached contact,..3 c.g.s. magnetic susceptibility.

24 Length Cu Zn Ag ' 349.5' ULTRAMAFIC KOMATIITIC FLOW DUNITE to PYROXENITE MAGNETITE RICH At upper contact rubble flow breccia, layered and fragment orientation at 5 degrees TCA and is conformable to the contact. Appears to contain black threadlike talc fracture filling or possibly sooty graphite (conductive) as well as dark talc matrix component in the rubble to fracture top of this flow sequence. The rubbly nature extends from the contact at ' to approximately 29 where coarse grained 1/2"!" pyroxene oikocrysts (gray) and cumulus black 13 mm olivine (serpentinized) occur as a massive dark greenblack uniform massive flow. The magnetic susceptibility of the top of the flow varies from c. g. s., where as the massive flow ranges from c.g.s. throughout indicating the presence of finely disseminated intercumulus magnetite. This flow is similar to the flow at the beginning of the hole from 6.'22. Occasional bluegreen serpentine fracture fillings from 286.'291.', and at 322.', at 35 to 6 degrees TCA. The flow contains coarse grained poikolitic textured pyroxene with olivine inclusions and as well cumulus serpentinized olivine in an overall massive uniform flow. Form 34.'349.5' at end of interval the flow is fractured with fine dark gray threadlike fracture fillings that are weakly to moderately conductive, possibly fine sooty carbonaceous fracture fillings. Lower contact is sharp at 3 degrees TCA ' 681.' BASALT FLOW (as previous) or GABBRO SILL Generally fine grained gray green massive uniform basalt, (possibly gabbro sill); Magnetic susceptibility 4.3 c.g.s. from upper contact to 35, below this the mag susceptibility ranges from..1 c.g.s. with local variations up to 2.9 c.g.s. Some local variations in crystallization where medium grained pyroxene occurs, and as well minor dark green talc/chlorite spotting occurs. The finer grained material appears to contain pale green felted masses of actinolite. Local long intervals of fine to medium grained interlocking crystals, massive and uniform, either a coarse flow or gabbro sill, 4.' 427.' (.6 2. c.g.s.). Intervals of finely crystalline massive uniform flow with 1/8" to 1/4" dark green chlorite spotting from 427.'518.5' imparting an overall mottled texture (..1 c.g.s). White quartz vein breccia at 451.' ( 2") and at 459.5' and at 46.', irregular quartz and calcite patches and stringers. From 518.5'527.' dark gray black to green black pyroxenite, weakly oikocrystic, black thread like fracture fillings, strongly magnetic with disseminated magnetic c.g.s. throughout, also trace po, and black equant olivine cumulus, (part of a

25 Length Cu ppm Zn ppm Ag ppm differentiated uniform massive mafic to ultramafic flow sequence). From 527.'54.3', massive homogeneous gray green, uniform flow with chlorite spots as previous, (.1.8 c.g.s. mag susceptibility). From 54.3'54.6' a narrow 4" plagioclase cumulus layer with irregular contacts. White 14 mm long euhedral lathes of plagioclase, trace specks chalcopyrite. From 54.6'546.75' massive uniform gray green flow as previous with occasional chlorite spotting (.1.8 c.g.s.). From '549.75' dark gray black, to green black olivine pyroxenite, strongly magnetic (7.15. c.g.s), abrupt but diffuse contacts for these intervals in this differentiated flow sequence, (difficult to envisage this variation in a gabbro mass) Weak foliation fracture fabric at 3 degrees TGA delineated by black thread like fractures or polysuturing. From '566.' massive uniform flow as previous (.3.8 c.g.s.), several white calcite stringers/tension gash veinlets. From 566.'568.75' dark gray black olivine * pyroxene, diffuse looking cumulate with disseminated magnetite ( c.g.s). From '612.5', massive uniform, fine grained as previous. Minor white calcite threadlike stringers locally, trace flecks chalcopyrite (..1 c.g.s.). From 612.5'614.5' olivine pyroxenite phase as previous, similar narrow differentiated intervals, ( c.g.s. mag susceptibility). From 614.5'626.5' medium grained, mottled pyroxenitic interval, (.1, and up to 6.3 c.g.s. locally), 1/2" calcite veinlet at 62.'. At 626.5'627.5' sheared zone with calcite stringers at 45 degrees TGA. From 627.5'681.' mottled to good pyroxene cumulate with 2 mm x 5 mm interlocking prismatic gray green pyroxene lathes, gabbroic looking. From ' trace disseminated chalcopyrite i pyrrhotite as fine weak sulphide disseminations, also as sulphides cpy and po fractures linings at 672.' to 681.' Weak patch of disseminated pyrrhotite occurs at 65.' over 3". From 631.'633.' weak disseminated magnetite ( c.g.s.). The remaining part of hole is a medium grained pyroxenite,.1 c.g.s. mag susceptibility throughout. Good interlocking gray pyroxene cumulate to EOH Occasional calcite 1/4" stringer at 664.', 671.* 672.6'. Disseminated pyrrhotite and trace chalcopyrite from 66.'681.' as fine intercumulus disseminated droplet sulphide^arid as fine fracture fillings to EOH. EOH ^ j^f^fo ' ' 675.5' ' 675.5' 68.' 5.5' 4.5' Q.6% "/o

26 DAVE GAMBLE GEOSERVICES INC 7 First Street, Kirkland Lake, Ontario, P2N 1N3, Tel: , Fax: MILLSTREAM MINES LIMITED DRILL RECORD Project: MILLSTREAM MINES LIMITED Azimuth: 19 degrees Started: August 12, Property: POTTER MINE PROJECT Dip: 45 degrees Completed: August 13, Twp/Claim: MUNRO TWP 1 L Location: L 1 * 6 m W/9 * 18 m S Core Size: BQ Logged For: Millstream Mines Limited Logged By: Dave Gamble (Sept. 8,1997) Tests: TD: 33* Dip:48deg. Az: TD: Dip: deg. Az: Hole No: S 96 7 Total Depth: 34.' ft. (17 Boxes ) Drilled By: Marathon Drilling Purpose of Hole: To test an area directly below the pitted surface showing at grid coordinstes 1 * 75 m W 1 9 * 6 m S. Millstream Mines Limited personnel spotted and monitored the drilling of this hole during a summer/fall 1996 drill program. All drill hole information regarding the collar location, azimuth, inclination, date of drilling, and drill contractor utilized, was supplied by Millstream Mines Limited personnel to DDG Inc who only carried out the logging of the drill hole S 96 1 in September, Remarks 1 Results: This hole intersected a basalt flow sequence. Several pervasively bleached carbonate and silicified alteration zones associated with fault zones were encountered. Trace pyrrhotite and specks of chalcopyrite were observed, green carbonate fuchsite was also locally observed in the carbonate alteration zones with minor quartz, pyrite and trace chalcopyrite. From this hole 7 samples ( , and 5151 ) were submitted for Au, Ag, assay and returned insignificant results. 2.' OVERBURDEN Length Cu Zn Ag 2.' 34.' EOH BASALT FLOW The flow sequence varies from fine grained massive uniform medium green to medium grained crystalline textured green flow, indicative of more rapid cooling represented by fine grained crystallization in contrast to a slightly slower cooling represented by fine to medium grained crystallization. The flow sequence is cut by fine threadlike fracture fillings of quartz with minor local bleaching near the stringers, varying from 5 to 1 per foot of core varying from 3 degrees to 8 degrees TGA, with the more prominent stringers at 5 to 6 degrees TGA. Rusty fracture at 2' 21', and at 25' 28' at 1 degrees TGA, and also at 34' 35'. Occasional white carbonate stringers and tension gash fillings. Mag susceptibility of fine grained flow material..2 c.g.s. whereas the medium grained part of the flow can be up to 1.7 c.g.s. Becomes pervasively bleached at 42.' 42.5' and again from 48.' 64.5' as a buff tan strongly carbonitized ALTERATION ZONE with high ferrous calcite ( stains lilac using carbonate staining fluids). Also contains white calcite stringers carrying trace pyrrhotite specks, as well as trace disseminated pyrrhotite in the pervasively altered bleached section. There is also a patchy pervasive siliceous component that also contains fine epidote imparting a yellowish green colouration typical of sausseritization.

27 Length Cu Zn Au Ag The alteration zone is extensively microfractured with quartz threadlike alteration filled fractures throughout. Mag susceptibility. c.g.s. From 64.5' 34.' fine grained flow cut by numerous quartz stringers threadlike fracture fillings and occasional calcite vein stringers as well as a short extensively bleached sections, by predominantly silica * or calcite, * or epidote. Pervasively bleached silicification * sausseritization from 126.5' ' in fine grained flow sequence. From 148' 156.5' medium grained part of flow sequence with some pervasively bleached sections. The medium grained crystallinity is expressed predominantly by subhedral to anhedral cream white plagioclase in 1 2 mm crystal masses. The fabric of the veining stnngers and threadlike fracture fillings is variable from 3 degrees to 8 degrees TGA with again a number of predominant orientation 55 6 degrees TCA. Magnetic susceptibility is..1 c.g.s. and locally varying to.2 c.g.s. to EOH. At 163' 166' several silicified patchy zones to veins and stringers carry trace pyrrhotite and chalcopyrite. Locally several quartz stnngers degrees TCA at 168'. Also low angles to core axis at 193.5' 195.5' at 1 degrees TCA. Occasional pale mauve calcite stnngers, hematite dusting causing discolouration at 18'. Bleached ALTERATION ZONE, pale olive green, from 23.5' 254.' with FAULT ZONE 237' 238.5'sheared broken with mud gouge at 7 degrees TCA. Within the alteration zone is vibrant green carbonate fuchsite alteration 239' 248' and strong from 247' 248' with finely disseminated pyrite and trace chalcopyrite. From 249.' 33' medium grained flow to EOH. Cut by occasional quartz veinlet and stringer but not to the same extent as the fine grained flow part. Occasional quartz stringer carries trace to weakly speckled pyrrhotite at 283' 284'. Locally bleached buff tan 292.5' 294.5'. Medium grained flow to EOH. EOH ^ /ZT ^f*s?.x^^^*^kb S v ~S ' se er 163' 245' 292' 297' se er 65' 166' 248.5' ' 4.' 3.' 3.5' (ppb).1.1

28 Sheet 1 of 4 Project: MILLSTREAM MINES LIMITED Property: POTTER MINE PROJECT Twp/Claim: MUNRO TWP/ Pel 857 Patented Hole No: S 96 9 N 1/2 Lot 7 Con V 7 First Street, Kirkland Lake, Ontario, P2N 1N3, Tel: , Fax: MILLSTREAM MINES LIMITED DRILL RECORD Azimuth: 25 degrees Dip: 45 degrees Location: L 16 * 9 m W 7 7 * 25 m N Total Depth: 61.5' ft. (32 Boxes) Started: Aug 14, Completed: Aug 17, Core Size: BQ Drilled By: Marathon Drilling Logged For: Millstream Mines Limited Logged By: Dave Gamble (May 2,1997) Tests: TD: 575' Dip: 46 Az: TD: Dip: Az: Purpose of Hole: To test a MaxMin II H.L.E.M. anomaly. Millstream Mines Limited personnel spotted and monitored the drilling of this hole during a summer/fall 1996 drill program. All drill hole information regarding the collar location, azimuth, inclination, date of drilling, and drill contractor utilized, was supplied by Millstream Mines Limited personnel to DOG Inc who only carried out the logging of the drill hole S Remarks 1 Results: The drill hole intersected a pyroxenitic gabbro from 8.'369.' followed by a sequence of basalt brecciaagglomerate with a black carbonaceous matrix that grades into a graphitic conductive argillite horizon from 379.'42.'. The argillite contains up to 2*ft disseminated "buckshot" pyrite. Below the argillite unit a similar basalt brecciaagglomerate occurs and fines downhole (suggesting tops are to the south) into a hyaloclastite interval from 439.'53.5*. The basalt hyaloclastite tuffbreccia hosts pyrrhotite and trace chalcopyrite as thin seams, blebs, and disseminations and is similar to the unit seen near the mine sequence. Below the hyaloclastite unit is a sequence of uniform massive and polysutured basalt flows with narrow interflow breccia agglomerate with a carbonaceous matrix component. Locally disseminated and rounded blebs of pyrrhotite (up to 4Vo) with trace chalcopyrite occurs within the basalt sequence. The basalt flows and fragmentals within this hole appear to be part of a late differentiated stage (leucobasalt) of the ultramafic komatiitic basalt assemblage seen closer to the mine sequence. Using the criteria from the fining of the fragmentals the top facing direction for the volcanic stratigraphy is to the south at this location. From tws^hole a total of 1 3 samples (5 not numbered from previous sampling, and 8 from sample series ) were submitted for Cu, Zn, Ag assaying. /js 8.' 8.' 369.' OVERBURDEN (Casing left in hole) GABBRO Pyroxenitic gabbro, (..1 c.g.s. Magnetic susceptibility), medium green, fine to medium crystal grain size of gray green pyroxene and pale green white lathes of (.5 mm x 3 mm ) plagioclase in a medium green interlocking mosaic. Contains dark green spots of talc * or chlorite locally. Unit varies from a medium grained interlocking crystalline unit with well developed plagioclase microlathes to a mottled uniform texture locally. The mottling occurs where partially resorbed gray green pyroxene oikocrysts occur. At 11.' a 1/2" quartz 3 degrees TCA. Trace specks po and cpy at 17.'. 26.' and 29.' 31.*. At 33.25' there is an internal 7 degrees TCA delineating medium crystalline uniform textured gabbro to a local mottled textured gabbro. Po occurs as isolated disseminated specks locally throughout. At 5.' 1/2" quartzcarbonate 7 degrees TCA. From 5.' down uniform medium crystalline interlocking plagioclase lathes, uniform and massive. ^ j*6*?^ V V* X ^t ^ *v " v ^; cn^o^ *O clf^x y ^ ^ " ft *k r^c Ax iv^j ^r^ t Length Cu Zn Ag

29 4 Length Cu Zn Ag Minor calcite * or quartz stringers as fracture fillings and as minor threadlike stringers, the larger stringers occur at 13.' 5 degrees TGA); 19.' 3 degrees TGA); 11.' 4 degrees TGA); 116.5' 5 degrees TGA); 119.5' 85 degrees TGA); ' (1 8 degrees TGA); 143.M4 a series of 1/4'M" white calcite tension gash veinlets followed by broken core recovery ' with black graphitic 1 degrees TGA; ' 1/2" 8 degrees TGA); 188.* (1/8" and 1/4") intersecting calcite 3 degrees TGA. Conductive graphitic lined and polished slips 355 degrees and 1 degrees TGA. At 195.5' a calcite 8 degrees TGA hosts weak disseminated pyrrhotite (po), chalcopyrite (cpy) and sphalerite (ZnS). Start to see locally more blebs and specks of po * or trace cpy from 19.' downward especially associated with the weakly mottled gabbro variety, chlorite * or talc as 1/4" spots and irregular shaped patches again occur 198.' downward in the mottled varitextured gabbro. At 267.' 1 1/2" chlorite+calcite+quartz 35 degrees TGA with disseminated po * cpy. At 28.* 1/2" calcite + graphitic material with 55 degrees TGA. From 267.' downward varitextured to mottled gabbro contains several coarse grained pegmatoidal gabbro phases, coarse interlocking plagioclase lathes and pyroxene subhedral crystals. Calcite threadlike stringers as fracture fillings and occasional 1/4"! /2" calcite stringers also occur at 3 degrees TGA 1/8" 1/4" stringer; at 31.' 1/4" quartz calcite at 65 degrees TGA; at ' 7 degrees TGA); and from 32 numerous fine threadlike degrees TGA. Pyrrhotite occurs as disseminations and as fine droplets in some of the pegmatoidal gabbro phases. Unit becomes finer grained crystalline over the lower 2.', no interstitial carbonate, fine threadlike pale green micro fractures, possibly chlorite. Lower contact 354 degrees TGA. 369.' 379.5' BASALT BRECCIA AGGLOMERATE WITH ARGILLITE MATRIX Medium green basalt breccia agglomerate (1" 3") clasts, rounded to subangular to partially flattened, hosted in a black fine grained argillaceous siltstone matrix. There are black fine grained parts of the matrix that is sooty graphitic and conductive. At 384.'38 strong graphitic fault gouge. The flattening of the fragments and matrix weak foliation or layered fabric is 455 degrees TGA.

30 Length Cu ppm Zn ppm Ag ppm Au opt 379.5' 42.' From ' pyrrhotite rounded nodules W1/2" and finely disseminated po occurs with trace flecks of cpy. (.1.8 c.g.s. mag susceptibility) At 395.5' a 1 1/2" quartz vein and 5 degrees TGA with foliation fabric of enclosing 35 degrees TGA. From 392.8'395.5' clasts supported basalt agglomerate with minor fine threadlike black carbonaceous matrix. From 395.5'397.5' minor basalt breccia with heavily disseminated py as < 1 mm 'buckshot' pyrite 15 "/o overall. ARGILLITE GRAPHITIC STRONGLY CONDUCTIVE From 397.5'42.' Black very fine grained, jet black sooty argillite with abundant 1/4"! /2" pyrite rounded nodules, several elliptical nodules and with very thin calcite shadow structures enveloping the nodules. The black sooty argillite is strongly conductive"conductor". The unit hosts disseminated "buckshot" pyrite 13 mm as subhedral to euhedral pyrite. Threadlike and up to 1/4" white calcite stringers also occur. Within the argillite unit there are several clean pale olive green basalt tuff horizons from 4.'42.5' carrying IS2% disseminated py, and gray buff carbonate altered basalt from 413.5'414.75' carrying IS2% py, and from 415.5'417.5' and 418.'419.' again carrying 15y disseminated py. At 42.' is end of the massive dense fine grained graphitic argillite ' 41.' 42.' 413.5' 414.' 419.' 422.' 399.' 41.' 42.' 413.5* 414.' 419.' 422.' 42 4.' 2.* 1.' 11.5'.5* 3.' 3.' Q.2% D.5% D.2% Q.2% Q.2% Q.1% Q.46% D.7%.1 9^ D.8% * 439.' BASALT BRECCIA AGGLOMERATE From 42.* to approximately 439.' is a coarse basalt breccia agglomerate with rounded, irregular basalt agglomerate fragments as < 1/4" tuff and up to 1" and 3" basalt clasts within a fine grained argillaceous matrix. The fragment population tends to be clast supported. Locally contains disseminated po (14Vo) and trace cpy. Lower contact of coarse fragmental is somewhat gradational into more normal hyaloclastite tuff breccia below. From coarse breccia agglomerate grading into fine hyaloclastite it appears that the stratigraphy is fining southward indicating that stratigraphic tops are to the south. 439.' 53.5' HYALOCLASTITE BASALT TUFF BRECCIA Basalt mini pillow breccia, 1/4" pea size green fragments, fairly uniform throughout with occasional black argillite clast rounded and angular fragments from 451.'474.* and from 1"5" in size. At 442.' a 7 " rounded basalt fragment. Matrix is dark greenish

31 black, a fine dusting of basalt tuff * or black carbonaceous material. The hyaloclastite tuff breccia is similar to the mine sequence, appears densely packed to almost fragment supported. Minor argillite tuff chips 1/4" also occur locally. (..3 to.7 c.g.s. locally) Disseminated pyrrhotite as coarse splashes to rounded blebs and 1/2" pyrrhotite seam at 25 degrees TGA. Trace flecks of cpy also occur. The last 5.* is gradationally finer grained indicating that tops are downhole or south. Lower contact is 2 degrees TGA, but wavy irregular ' ' ' ' ' Length 5.5' Cu ppm Zn ppm Ag ppm Au opt 53.5' 528.' BASALT FLOW BRECCIA to BASALT FLOW From 53.5'59.' rounded breccia agglomerate (..1 c.g.s.) basalt fragments in a basalt matrix with several argillite fragments 1 1/2" at 56.' and 11" at 57.'. In addition minor argillaceous matrix to the basalt breccia agglomerate clasts. Grades into massive uniform fine grained medium olive green flow, (.2.5 c.g.s.). At 525.5'528.' broken core, sheared with 4" mud gouge at 527.' that is conductive. Minor white calcite stringers locally. Minor weakly disseminated and trace stringers of pyrrhotite. 528.' 549.5' BASALT FLOW BRECCIA AGGLOMERATE ( as previous) Coarse breccia agglomerate rounded fragments of basalt, minor black argillaceous matrix, fragments of amygdular and massive fine grained basalt flow. Splashes and coarse rounded blebs po (up to 4Vo po) and trace cpy locally, (..6 c.g.s. where po occurs) ' ' ' ' 2.' 4.5' D.2% 168 Q.2% 519 Q.5% 91 Q.5% ' 61.5' BASALT FLOW BRECCIA BASALT FLOW polysutured Green with delicate "lacy" looking pale green flow banded material probably quenched flow material and massive basalt flow. (.4 c.g.s. mag susceptibility). Some "frothy" looking to almost scoriaceous basalt within a basalt flow groundmass. Disseminated stringers po (5Xo) and trace cpy, grades into a narrow flow breccia with black argillaceous matrix and green basalt breccia fragments from 555.6' 557.'. From ' a polysutured basalt (.1.4 c.g.s.) fine grained flow and minor brecciated flow or polysuturing. Polysutures or polygonal fractures are filled with dark green talc and/or chlorite. Local coarse 1/4" blebs and rounded masses and minor swirls and disseminations of pyrrhotite and trace cpy associated polysutured flow to end of hole. (.1 jlz^.g.s) EOH S1#S^Y^ ' ' 61.5' 6.1' 6.5' 123 Q.4% 9.1 2X,.1

32 PLANIOCAUON OF DDH S961 MUNRO TOWNSHIP N IS * "X is! ) to Cfeirn Line i i j,s96 'S96 i L 53 f C&in (.//is ^ t"^^^ ***^.*1^ Road 95 (P) ( V LS97 /t r x PyKss ' Hill s96o; j i! ef '^ J * AZIMUTH 18 deg. COLLAR DDH S961 AZIMUTH 18 deg. l 45 deg. L 7 * 5 m W ms S961 3 uc" 4 ec i *, 5 S 4 r.., a u r* 4 U L 53 Claim line 3,,,,..._ a g u 946 (P)..3 K 4 i M i flfloq+sl Glomeroporphyritic Plagioclase 7S 15 3m f 1 '^ 1 1 ^^^ M^^^ Infoirrwtion on ocilion of th 1 * pnwidxt by MIMrnm Mines Ltd 1d, weak P Is 1d, weak Pis 1dMas Asb fracture fillings Fracturing 1b Mas Por Gbmeroporpyritic Plagioclase Fracturing EOH 664 ft. LEGEND Gabbro Argillite Ultramafic Komatiitic Basalt ^^ Fragmental Volcanics 3 IIB Hyaloclastite 2 HB TuffBrecciaAgglomerate Ultramafic Komatiitic Basalt 1 Layered Flow Sequence 1a Ultramafic Leuco Basalt flow Texture Qualifiers 1b Basalt Mas Massive, uniform flow 1c Pyroxenite Pis 1d Peridotite Sfx 1e Dunite Por Minerals Asb Asbestos ZnS Sphalerite Cpy Chalcopyrite Mgt Magnetite Polysutured flow Spinifex flow Plagioclase porphyitic Minor Interflow Breccia /Agglomerate o 2 so 1 2ft SCALE : 1:12 (1 Scale Imperial) DAVE GAMBLE GEOSERVICES INC MILLSTREAM MINES LTD DDH SECTION S961 L 7 * SOW m SECTION t Looking West) POTTER MINE PROJECT MUNRO TOWNSHIP Date: September, 1997 NTS: 32 G FIG. Scale: :12 Drawn Ref: S. G. Mill961.cdr

33 * x i * tt! PLAN LOCATION OF DDH S962MUNRO TOWNSHIP j1 '. rs 1! rsi 3 S 1 1 1,396C S96 ^...3 U r i u i L ( Clam "*** Road L 53 Claim L/ne a 7S g 4 U 1 Uie y 946 (P) l 3 w 15 ^ 1C.S977 x """ * ^c 1 3 g 4 ^ V, 1 HU S96OC E S 3m 3 r^ i x ^At, a i * w 1 N j COLLAR DDH S962 AZIMUTH deg. l 45 deg. L 7 * 5 m W 7 3 * 85 ms Looking East h Azimuth deg. i S962 1d Sfx Strong fractures 16' 22', 265' 344', moderately fractured 344' 413' at 6 deg. TGA Fracturing 1bMas o ' Information on DCBbon of tfiis Ddh provided by MiAttiesm M^IH LW. g Plagioclase Porphyritic Diorite 1d, Pis RECEIV j;;: i fen W. 11 GEOSCIENCE ASSr OFFICE EOH 75 ft. Fracturing 6 Diorite LEGEND 5 Hi Gabbro 4 Hi Argillite Ultramafic Komatiitic Basalt F r aa mental Volcanics 3 Bi Hyaloclastite 2 Hi Tuff Breccia Agglomerate Ultramafic Komatiitic Basalt 1 HI Layered Flow Sequence 1a Ultramafic Leuco Basalt flow Texture Qualifiers 1b Basalt Mas Massive, uniform flow 1c Pyroxenite Pis td Peridotite Sfx 1e Dunite Por Minerals Asb Asbestos ZnS Sphalerite Cpy Chalcopyrite Mgt Magnetite Polysutured flow Spinifex flow Plagioclase porphyitic Minor Interflow Breccia 'Agglomerate O 2 SO LP ^ 1 2 a SCALE : 1:12 (1 Scale Imperial) DAVE GAMBLE GEOSERVICES INC MILLSTREAM MINES LTD DDH SECTION 96 2 L 7 * S OW m SECTION ( Looking East) POTTER MINE PROJECT MUNRO TOWNSHIP Date: September, 1997 Scale: :12 WTS; 32 G Drawn Ret: S. G. Mill962.cdr FIG.

34 PLAN LOCATION OF DDH S963 MUNRO TOWNSHIP N 4 3 g 4 a IS! i i,,s96i fs96 IS ^ 1 1 s ".' is J 1 le S rs u 4 r s u 4. u L Cfcun LUoe y Road L 53 Claim I S fl S 4 U 946 t ] i Une 3!E 4 U.S97 yi t' B v^l 5 S 4 *: X 1 7 ^j i J ' HI/I s96o: j h i * 7 ^ j j S [gsi i U i ^ ^, V ^AS^n.a 8 4 K 1 * COLLAR DDH S963 AZIMUTH 212 deg. l 45 deg. Azimuth 212 degrees S Nil ppb Au t 1 oz /t Ag f o o Sfx 1d Fracturing at 14' 15' at 6 deg. TGA D m ^5^Z^^^^5^^^ ^^^^ 1 ItiterniBlioo en ocrtm of Site Wh provided by MiHtfrMm Mui*s Ltd RECEIVED O C BE8KNC EOH 64 ft REC OCT r o t GEOSCIENCr OFF, Diorite LEGEND i f 1a 1b 1c 1d 1e Minerals Gabbro Asb Asbestos Argillite ZnS Sphalerite Cpy Chalcopyrite Mgt Magnetite Ultramafic Komatiitic Basalt Fragmental Volcanics Hyaloclastite Tuff Breccia Agglomerate Ultramafic Komatiitic Basalt Layered Flow Sequence Ultramafic Leuco Basalt flow Texture Qualifiers Basalt Mas Massive, uniform flow Pyroxenite Pis Polysutured flow Peridotite Sfx Dunite Por Spinifex flow Plagioclase porphyitic Minor Interflow Breccia /Agglomerate o 2 so 1 2ft. SCALE : 1:12 (1 Scale Imperial) DAVE GAMBLE GEOSERVICES INC MILLSTREAM MINES LTD DDH SECTION S963 on Azimuth 212 deg. through collar at mw/5 + OOmS ( Looking West) POTTER MINE PROJECT MUNRO TOWNSHIP Date: September, 1997 Scale: 1 : 12 NTS: 32 G Drawn Ref: S. G. Mill963.cdr FIG.

35 PLAN LOCATION OF DDH S964 MUNRO TOWNSHIP 6S 78 SS l g ^ o. O) 9S 3 S 9E 8 1S us 3 8 * N *" 12S ETJ 13 t i Vi l "^ t** S c 4 r i fl L 539j 2 F d S96O^ffe S 984 " J/ " Iff ^(aim Line Js967 f r W/lQ/J lt'stcj i J h^ C* C"1 JL^T i V L i S 4 C Clat nllne *"W 5395i3 3 IS i 1 **L^ ^Jlr?**! n I SO Mom " InfcxTniition on locsbon of ffi fs Ddh pmvidtd by MHIstmm Mince Ltd. JS IO B N 4 * a ea r N j. o E" r 3" (D Azimuth 19 degrees COLLAR DDH S964 AZIMUTH 19 deg. l 45 deg. LIO + SOmW/T + SOmS 1dMas tbmas Is S964 IbMas 1d Mas Layering 5 deg. TGA 1bMas 1d Mas, weak Pyx oikocrysts, layering 5 deg. TGA 1d Mas, Layering 5 deg. TGA 1d Mas Pyx Oikocrysts IbMas 1d Mas Pyx Oikocrysts Carbonate Alteration Zone 514' 568' Bleached Silicified Alteration Zone ' 655' plus quartz SO deg. TGA 1d Mas Pyx Oikocrysts,layering 5 deg.tca 1d Mas Pyx Oikocrysts 65 deg.tca 6 deg. TGA IbMas Carbonate Alteration Zone Calcite stringers, no quartz 667' 712' Talcose 655'712' NilppbAut.1 Ag/5. 1, NilppbAu*.1 Ag/^ Carbonitized, calcite * fuchsite at 822' 824' IbMas EON 86. ft. IbMas Sfx 6 deg.tca 1d Mas, talcose Siliceous Grey Sediment cherty 5 deg. TGA 4 plus pyrite disseminations and in seams NilppbAu*.1 Ag/ Nil ppb Au *.1 oz /t Ag / Gabbro LEGEND Argillite l Siliceous Grey Sediment Ultramafic Ko m allitic Basalt Fragmental Volcanics Hyaloclastite Tuff Breccia Agglomerate ^^ Ultramafic Ko m at i i tic Basalt 1 H! Layered Flow Sequence 1a Ultramafic Leuco Basalt flow Texture Qualifiers 1b Basalt Mas Massive, uniform flow 1c Pyroxenite Pis Polysutured flow 1d Peridotite 1e Dunite Minerals Ash Asbestos ZnS Sphalerite Cpy Chalcopyrite Mgt Magnetite Sfx Spinifex flow Por Plagioclase porphyitic A A Minor Interflow Breccia /Agglomerate o 2 so 1 2 n. SCALE : 1:12 (1 Scale Imperial) DAVE GAMBLE GEOSERVICES INC MILLSTREAM MINES LTD DDH SECTION S964 on Azimuth 19 deg. Through collar at 1 * 3 m W/ 7 * 6 m S ( Looking West ) POTTER MINE PROJECT Munro Township Date; September, 1997 Scale: 1 : 12 NTS: 32 G Drawn Ref: S. G. Mill964.cdr FIG.

36 PLAN LOCATION OF DDH S965 MUNRO TOWNSHIP 6S 7S 8S ' 1 as ".g g 15 us 3 12S :* w*t* w g f D 3 1 d. ft I VI *ẉ 1 'b i S T i L ^965 i S9t 4 I li f L J/l C If 3 S c J t is967 7oetf "** ~^ *^^^w j R 4! Clat nline 2 la/m Una ^ D n I SO 3m g *ai 1 S966 f * CO l r l Tli w o E1 r 1 Azimuth 19 degrees COLLAR DDH S965 AZIMUTH 19 deg. l 6 deg. L 1 * 3 m W/ 7* 6 ms EW o c 1dMas S965 1bMas 1d Mas, Pyx oikocrysts 1 InfemvUon on fetation or this D* pnnndid by MlWnam Mints Ud. 1bMas co.1 Pt * <.1 Pd Nil ppb Au f;.1 oz /t Ag; 1d with layering at 45 deg. TGA tbmas Nil ppb Au * 1.1 oz /t Ag Nit ppb Au * 1.1 oz /t Ag / Nil p pfc Au * 1.1 oz /t Ag / Nil ppb Au f;.1 oz H Ag 1 Bleached Alteration Zone 618' 647', silicified,tquartz stringers xv A 3/ ^ i 1bMas y 397' at 55 deg. TCA Calcite stringere at f 399' at 45 deg. TCA 59'522'at 4 de TCA and at ^ J 427' at 35 deg. TCA 573' 589' at 4 deg. TCA ^ y if 474' at 55 deg. TCA * i/ Bleached Alteration Zone 589,75' 597' y 1bMas + Quartz stringers and veinlets. / jf 1 d Carbonate and talc altered ^y *y ib i* J^ Sfx / 7.X 1bMas,jr Sfx Jr. From 667' 724' calcite stringers only ^ a SIX EOH 724. ft. 1bMas 1d with layering at 266' st 35 deg. TCA and at 313'at 3 deg. TCA '^C/cr/i yt 1d Pyx oikocrysts with layering at 7 ^^***. fi/'** ^ s H 4 H 2 S i H 1a 1b 1c 1d 1e tsj^ ^^ifiefe Gabbro Argillite Minerals Asb Asbestos ZnS Cpy Mgt LEGEND Ultramafic Komatiitic Basalt Fragmental Volcanics Hyaloclastite Tuff Breccia Agglomerate Ultramafic Komatiitic Basalt Layered Flow Sequence ^1 '1 w Ultramafic Leuco Basalt flow TextU re Qualifiers Basalt Mas Pyroxenite Pis Peridotite Sfx Dunite Por Sphalerite Chalcopyrite Magnetite AA Massive, uniform flow Polysutured flow Spinifex flow Plagioclase porphyttic Minor Interflow Breccia /Agglomerate o ft SCALE : 1:12 (1 Scale Imperial) DAVE GAMBLE GEOSERVICES INC MILLSTREAM MINES LTD DDH SECTION S96 5 on Azimuth 19 deg. Through collar atlo + SOmW/Z + eoms ( Looking West) POTTER MINE PROJECT Munro Township Date: September, 1997 Scale: 1 : 12 NTS; 32 G Drawn Ref: s. G. Mill965.cdr FIG.

37 PLAN LOCATION OF DDH S966 MUNRO TOWNSHIP 6S 7S 8S i rtt S 9S J Ea. 1S S g 4 f o tu li V 3 c 4 T L* i ^ L L 539E 2 J^ s^ B 4 f 1 H!J c S367 tfoffi/ ^?: 539* 3 (P), 3 Clal tnune o 73 ISO 3m j ^^ III 1 4 m ' InfamwtJon an location of (his D* provided by MilsbMin Minos Lid. lalmune l^s^ 3 S41 1 ys966 g S 41 m i li i r o Azimuth 25 degrees COLLAR DDH AZIMUTH 25 deg. l 45 deg. LS + GSmWMO + OOmS 7" Asb 1d1c1e Mgt Acb 1d1c1e i in o to o * * CO O 1e1d Mas 1d1cle 3 Mgt (/^ a 1d Mas l b Mas 1 b Mas5 Note:Section Looking East LEGEND 45 EOH681.ft. Mgt Tr Cpy * Po Mgt Mgt 1 b Mas5 Ag; ppmcu4 17 ppmzn *.2 ppm ppm Cu * 22 ppm Zn *.2 ppm Ag ppm Cu * 24 ppm Zn f.2 ppm Ag W Cu *.1* Zn ; 5 IH Gabbro 4 Argillite Ultramafic Komatiitic Basalt Fragmental Volcanics 3 j B Hyaloclastite 2 Hi3 Tuff Breccia Agglomerate Ultramafic Komatiitic Basalt 1 OH Layered Flow Sequence 1a Ultramafic Leuco Basalt flow Textu re Qualifiers 1b Basalt Mas Massive, uniform flow 1c Pyroxenite Pis 1d Peridotite Sfx 1e Dunite Por Minerals Asb Asbestos ZnS Sphalerite Cpy Chalcopyrite Mgt Magnetite Polysutured flow Spinifex flow Plagioclase porphyitic Minor Interflow Breccia /Agglomerate O ft. SCALE : 1:6 (5 Scale Imperial) DAVE GAMBLE GEOSERV1CBS INC MILLSTREAM MINES LTD DDH SECTION S 966 on Azimuth 25 de g. Through collar at 8 * 65mW/1 * ms ( Looking East) POTTER MINE PROJECT Munro Township Date: June, 1997 Scale: 1 : 6 NTS: 32 G Drawn Ret: S. G. Mill966.cdr FIG.

38 PLAN LOCATION OF DDH S967 MUNRO TOWNSHIP 6S 7S 8S a Q. i3 I a ^ 1 w f S 98 e 1S S O 3 N L 539S 2 ""Iff *" J c 41, 1 ju4 1 L r S9S7 i4 539f.3 'a/m L/ne :^ ;S^G U. r Claim Line Azimuth 19 degrees COLLAR DDH AZIMUTH 19 deg. l 45 deg Nil ppb Au *.1 oz ; t Ag 1 4.' Nil ppb Au t.1 oz 11 Ag Nil ppb Au i.1 oz f t Ag; 4,' S967 Alteration Zone 48' 64.5' Carbonate + Silicification' 1bMas e CO 11S 125 g Jo u c T 1 S 4 C ^ X s S Clai nune K n Ol o a f 1 in M t ea j 1 Silicification t epidote 7i lid 3m 1 Infomuton on kraton of this Ddh pnawosti by Mllstreini Mines LM Quartz Stringers, Minor Calcite 64' 34' m Nil ppb Aut.1 Ag/3.' Alteration Zone23Q' 254 Fault, 7 deg. TGA Fuchsite, Calcite, Trace py, cpy "5151 Nil ppb Au; 3.5' Nil Au 4.1 oz 11 Ag f ' Nil Au *.1 oz 11 Ag f EOH 34. ft. NOTE SCALE: 1:6 LEGEND Gabbro Argillite Ultramafic Komatiitic Basalt Fragmental Volcanics 3 IB Hyaloclastite 2 RH Tuff Breccia Agglomerate ^^ Ultramafic Komatiitic Basalt 1 l:'^l Layered Flow Sequence 1a Ultramafic Leuco Basalt flow Texture Qualifiers 1b Basalt Mas Massive, uniform flow 1c Pyroxenite Pis 1d Peridotite Sfx 1e Dunite Por Minerals Asb Asbestos ZnS Sphalerite Cpy Chalcopyrite Mg t Magnetite Polysutured flow Spinifex flow Plagioclase porpnyitic Minor Interflow Breccia /Agglomerate o ft SCALE : 1:6 (SO Scale Imperial) DAVE GAMBLE GEOSERVICES INC MILLSTREAM MINES LTD ODH SECTION S967 on Azimuth 19 deg. Through collar at 1 * 6mW/ 9 * 18 ms ( Looking West) POTTER MINE PROJECT Munro Township Date: September, 1997 NTS: 32 G FIG. Scale: 1 : 6 Drawn Ref: S. G. Mill967.cdr