en 00 UJ ^ Lil O Lil CC Page: l of 14 *** Dip Tests *** Depth Azi. Dip Date Started: Date Completed: Date Printed: 29 Mar, 1999 Geology Sample No.

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1 QUEENSTON MINING INC Drill Hole: MU98- DIAMOND DRILL HOLE RECORD Property: MUNRO Collar loc from # Post L48 - 'N, 4'E Northing: 94. Easting: 1. Elevation: 11. *** Dip Tests *** Depth Azi. Dip Collar Azimuth (Grid). Collar Dip: (O Degrees Grid equals O degrees True) Hole Length: 9. Date Printed: 9 Mar, 1999 *** Dip Tests *** Depth Azi. Dip Date Started: Date Completed: Page: l of 14 DEC 4, 1998 DEC 1, 1998 Drilled by: BENOIT Core Size: NQ Material left in hole HX CASING Core Location: Upper Canada Site l Logged by: JD Schonfeldt Len SUMMARY LOG OVERBURDEN DIORITE CONTACT ZONE ULAMAFIC KOMATIITE FAULT ZONE BASALTIC KOMATIITE.8 8. ULAMAFIC KOMATIITE INTERFLOW MATERIAL ULAMAFIC KOMATIITE INTERFLOW MATERIAL "Sfl ULAMAFIC KOMATIITE ULAMAFIC KOMATIITE Q UJ ^ Lil O Lil CC en en en * ^ t UJ S w UJ UJLJ. oo ae UJ C (f) O UJ cs CO en D4NW.1948 GAUTHIER 1

2 Drill Hole MU98- Page: of 14 Len PY 1 AU AU1 AU ppb OVERBURDEN Hole collared to test a weak IP anomaly, feet, and represented by a section of well mineralz mafic/um flows, w/ cherty interflow material. Hx casing was reamed to 18. feet, NX casing was reamed to feet. Upon completion of the hole, NX casing was recovered. Attempts to recover Hx casing were unsuccessful DIORITE Collar in a unit of coarse grained, intrusive material, dioritic in origin. Core is grey black to white and speckled in appearance w/ large.cm sized plciy-t--uilau lelu piieaus suppuj-leu w/in et malic {amphibole *- biotite) matrix, w/ up to 1% qtz locally. This unit is weakly to strongly orange stained, mod to locally non mag, ankeritic w/in fine qtz stringers, and calcitic w/in late calcite fractures. Rx are extremely silicified, variably alt, and quite dirty containing numerous variably sized angular to sub rounded fragments to inclusions of what appears to be cooked up UM material, as well as a few larger rafts of potential host. Veining is well dev w/in this unit w/ numerous variably sized and oriented qtz veins, the larger of them O steep angles to ea. Mineralz is quite well dev w/ a l-% mix of fine and coarsely diss py, w/ lesser coarse py clusters/aggregates. Core is finely mafic fractured, and contains bands of bright orange stained material, often w/ sharp cts. These bands are interpreted to be an alt feature, as texture of the cleaner looking material persists through orange stained zones. A more detailed unit description follows Diorite. Dioritic material as above, w/ numerous wall rx inclusions, and orange stained alt material from 14.9 unitl /7 dtca 14. until /7 dtca, 147. unitl /7 dtca, and until Orange stained material in non mag w/ the remainder of the unit being weakly to mod mag. 1. until 1.6 a zone of narrow high angle light grey qtz veins, separated by slivers of host material containing l-% fine diss py. Basal ct for D 7 dtca, w/ some partially assimilated host material. Sulphides across the unit avg Ultramafic. A raft of strongly cooked up host, presumably of UM origins, although this is unclear. Core is grey black, weakly ank, mod mag, somewhat granular textured, mod silicified, and weakly veined w/ a few tiny qtz-carb veinlets, often w/ narrow(cm wide) bands of bleaching/alt outside veins. Tr accessory fine py adjacent to cts. Upper ct diffuse and partially assimilated. Basal ct better defined and shallow running along ea for approx 8 inches Diorite. Strongly orange stained alt dioritic material, w/ vague dioritic texture presurved. Core is fine grained, w/ tiny visible feld phenos, and some fine mafic fractures. Unit is not well veined, and mineralz w/ 11 fine and coarse py. Rx are non mag, silicified, and weakly ank w/in late carb stringers. Basal ct sharp ffl 77 dtca. 4 ^bbbb lib.u , , J.V.y ^ * * '

3 Drill Hole MU98- Page: of 14 Len PY t AU AU1 AU ppb Ultramafic. A raft of cooked up host, presumably UM's. Core is ankeritic, granular textured, amphibolitic, mod mag, silicified, not well veined and mineralz w/ tr-1% fine diss py. This unit is dark grey to black in colour, and has a well defined albeit irregular basal ct 8 7 dtca Diorite. Diorite the onset of the unit. Core is well veined w/ variably sized and angled qtz veins, the largest 1. inches 8 79 dtca, as well as numerous angular to sub rounded wall rx inclusions. Mineralz is well dev w/ l-!i fine and coarse diss py across the unit. Basal ct well 6 dtca Ultramafic. Another raft or inclusion of cooked up host material, presumably UM in origin. Core is weakly ankeritic, granular textured, mod mag, very weakly foliated approx 6 dtca, veined w/ the odd qtz-carb vein sweat, and one small lcm wide contorted qtz vein a 6 dtca, base of the unit. Mineralz is not well dev w/ tr py. Basal ct well defined albeit slightly 6 dtca Diorite. Diorite as 16.6 except that core is very well veined w/ qtz veins approx 1% of the core by volume. Core contains a few zones of stronger orange staining and a few angular fragm of wall rx. Mineralz is well dev w/ l-% fine and coarsely diss py, as well as a coarser py Calcite. Bx calcite vein, cts very irregular and shallow Diorite. Diorite as Core is grey to locally orange stained, coarse grained, mod to non mag in orange stained alt bands, silicified, weakly ank, and weakly calcitic w/ late calcite stringers. Rx contains numerous angular fragments of wall rx and are well raineralz w/ l-1i fine and coarsely diss py, as well a fine py clusters Core is very well veined w/ numerous variably sized and oriented qtz veins, the largest from 4.8 6/ dtca. Basal ct very irregular 9 6 dtca...9 Ultramafic. A sliver/inclusion of host/wall rx material, presumably UM in origin. Core is fine grained, mod mag, silicified, beige brown to black coloured, ankeritic mod well veined w/ a couple of high angle greyish qtz veins, and not well mineralz. This unit has a weak fabric, and contains rosettes of carb in the basal inches of the unit. Basal ct well defined albeit slightly 6 dtca Diorite. Diorite 174.7, except that core contain less of the orange fracture controlled staining as seen uphole, being predominantly grey toned. Aside from colour variations core is very similar, containing numerous wall rx inclusions, and l-% fine and coarsely diss py. 4.4 until 46.4 core bbuv a b Ot 1.St 1.*: 1.Ot 1.*: 1.*; l.ot 1.*: 1.*: 1.* 1.* 1.*; 1.* 1 -St -t 7% 1.Ot 1.Ot 1.*1 1.*i 1.*: 1.*; 1.*: 1.*f 1.*: 1.*r 1.*r 1 -t 1.*: 1 -*; l -*; 1.Ot 1.Ot 1.Ot 1.Ot 1.Ot 1.Ot -7t 1.Ot 1.Ot 1.Ot 1.Ot 1.Ot.7*:.St..St Q.% 1.*r 1..Ot

4 Drill Hole MU98-OS Page: 4 of 14 Len PY AU AU1 AU ppb is microbx, w/ fine dark grey high angle qtz veins, carrying l* very fine diss py. Wall rx inclusions are typically fine grained, ankeritic, and mod well mineralz. Veining is quite well dev w/ numerous variably sized and oriented qtz veins, the largest 1.4 until 1. 7/6 dtca. This vein is light grey in colour, and not well mineralz. Wall rx outside qtz vein is mineralz w/ S-% fine py clusters w/ lesser fine diss grains. Basal ct slightly diffuse w/ some partially assimilated material S 6 dtca * Ultramafic. Sliver of UM? host. Core is fine grained, ankeritic, mod mag, silicified, and amphibolitic, Rx contain some accessory fracturing, typically w/ some ueyi'ee: of jjieaciiiuy/dll ijitteuiiiy out from fractures. Mineraiz is modest. This unit is cut by numerous narrow dykelts of D high angles to ea. Basal ct slightly diffuse 9 6 dtca Diorite. Diorite in this area, is very dirty, and contains partially assimilated UM material, accessory py. Basal ct sharp dtca. quite dark in colour, as it Minimal veining, tr-1% fine Diorite. Continuing in dirty looking dioritic material, w/ numerous inclusions of wall rx, mainly UMs, w/ a couple of frags which appear to be mafic intrusive in origin as they contain fragments of what appears to be UM material. Most core in this section is quite dark and contaminated w/ partially assimilated host rx. Core contains a few orange stained alt bands, which appear fracture related, and is mineralz w/ l-% fine and coarsely diss py grains, w/ lesser fracture controlled seams. Veining is mod w/ the odd qtz vein, and numerous qtz-carb veinlets. Basal ct is unclear Sil. A unit of micro fractured, extremely silicified material. Core is very fine grained, dark grey in colour, veined w/ numerous qtz-carb veinlets to sweats. Unit is mineralz w/ i* very fine diss py. Unit may be an inclusion of cherty material, although this is unclear. Basal ct a bit diffuse, suggesting D may have partially assimilated unit Diorite. Dirty looking dioritic dtca. material as S 7.6. Basal ct slightly diffuse Ultramafic. A raft of strongly alt, cooked up host material. Core is grey to black coloured, fine grained, mod mag, ankeritic, mod silicified, and has a weak fabric 7 dtca. Core contains numerous variably sized and oriented qtz veins as well as a few narrow dykelets of D material, high angles to ea. Mineralz is modest w/ tr-1% fine and coarse py grains. Basal ct w/ 7 dtca Diorite. Dirty looking dioritic material as 7.6, w/ numerous wall rx inclusions

5 Drill Hole MU98- Page: of 14 Len PY i AU AU1 AU ppb and considerable partially assimilated host. Core is well veined and mineralz w/ 1-1 fine and coarsely diss py grains. Basal ct along BBC, but presumably O approx 7 dtca CONTACT ZONE Pale grey to locally beige toned UM affected by.the incipient style of alt. Core is fine grained, mod mag, silicified, foliated approx 7 dtca, mod well veined, w/ a few high angle qtz veins, of the light grey and milky white varieties. Mineralz is modest w/ 11 fine and coarse py. This unit can be best described as ct zone material as it is sandwiched between intrusives and enus aloud cui ali, IJ.UIIL fium auk Lo aliong pervasive! calcice ale. Basal ct mod well defined w/ 1-1 py seams 7 dtca. Basal foot of this unit spotted w/ rosettes of carb ULAMAFIC KOMATIITE FAULT ZONE Contact into a broad swath of UM rx, typically blue black to locally green toned and more chloritic/amphibolitic S top/margins, fine grained, foliated a 4 dtca, mod mag, soft, strongly pervasively calcitic, w/in matrix, and as discontinuous stringers in more blue black sections. Below approx 4. unit begins to look more like a flow sequence w/ chloritic tops/margins, relict spinifex textures, fine cooling cracks, and some flowy looking bx material w/in chloritic tops/margins. Neither veining nor mineralz is well dev. Core is cut by a variety of mafic intrusives. A more detailed unit description follows Calcite. A grungy looking, light grey coloured, granular textured unit of probable UM material, which is extremely pervasively calcitic. Not well veined or well mineralz. Basal ct quite well defined 6 dtca Mafic Intrusive. A dark grey, grungy looking, pervasively calcitic, mod mag, mafic intrusive dyke. Core is amphibolitic and contains a few irregular shaped UM inclusions. Neither veining nor mineralz is well dev. Basal ct ragged dtca Q.% Calcite. Strongly pervasively calcitic UM material as 61 dtca Basal ct quite Ultramafic. A mod blocky, blue black to locally brownish toned unit of UMs variably, locally affected by the incipient style of alt. Core is fine grained, soft, and mod mag in blue black sections. Granular textured, hard, and slightly more magnetic in brownish toned areas. Core is approx 6-7 dtca, not well veined, and effectively unmineralz, aside from brownish toned sections which typically hold tr-1% py. Basal ct w/ 7 dtca Fault Zone.

6 Drill Hole MU98- Page: 6 of 14 Len PY AU AU1 AU.. % ppb Ct along 9mm of gouge 8 7 dtca, followed by inches of granulated core. Downhole core is slightly more intact w/ fault gouge 9.9.cm 9 6 dtca, cm of gouge 7 dtca, mm 9 7 dtca, until 4. core is granulated w/ gouge 9 7/6 dtca, followed by BBC until basal ct which is quite strongly 6 dtca. Core is mod mag, pervasively calcitic, soft, fg, not well veined and not well mineralz Mafic Intrusive. A dark grey to black MI. Core is fine grained O cts and slightly coarser grained in central section of dyke. This unit is mod to strongly mag, pervasively calcitic, mod hard, amphibolitic, chloritic, and biotitic. Rx contain tr-% fine diss py, minimal veining, and numerous inclusions of UM wall rx. Unit is moderately blocky, and has an amphibolitic basal ct 9 49 dtca Fault Zone. Contact into blue black to dark green black, variably chloritic and amphibolitic unit of UMs. Core is very blocky, w/ rubbled, gouged and granulated core. Initial ct into 4 inches of dark green chloritic material, w/ fault 41. mm O 7 dtca, followed by intact core until until 4. core rubbled w/ fault gouge 4. l.lcm 9 7 dtca, followed by blocky core downhole until 4. were there is inches of granulated core w/ gouge. Below 4. core is blocky becoming extremely rubbled by 49. until 44. w/ gouge and strongly granulated core. Below 44. core is blocky w/ gouge a lcm 8 6 dtca. This unit is soft fine grained, weakly to mod mag, calcitic, not well veined and effectively unmineralz. Basal ct sharp 9 7 dtca Mafic Intrusive. A dark grey to black, fine to med grained, chloritic, biotitic, and amphibolitic mafic intrusive dyke. Core is mod hard, pervasively calcitic, mod mag, locally quite blocky, not well veined, and mineralz w/ tr-1% fine and coarse py. This dyke is quite dirty w/ numerous UM wall rx inclusions. Basal ct well defined 9 6 dtca Ultramafic. A grungy looking, chloritic zone of blue black to dark green amphibolitic UMs. Core is strongly calcitic, fg, weakly to mod mag, soft, talcy, and massive to locally foliated. Rx are not well veined and mineralz w/ tr coarse accessory py. Basal ct w/ tr gouge 9 77 dtca Fault Zone. Broken blocky core w/ fault gouge mm 9 7 dtca, cm dtca, followed by granulated core until 46.. Last inches of this unit are blocky w/ tr gouge 4 dtca. Host is a blue black, UM unit effectively unveined and unmineralz Ultramafic. Blue black, talcy, soft, fg, foliated, mod contorted, strongly calcitic, weakly to locally mod mag UM unit. Core is not well veined or well mineralz. Basal ct well defined 8 66 dtca.

7 Drill Hole MU98- Page: 7 of 14. Len PY AU AU1 AU ppb Mafic Intrusive. A granular textured, strongly pervasively calcitic mafic intrusive dyke. Core is mod mag, amphibolitic, chloritic, soft, unveined and unmineralz. Core is granular in central section w/ extremely fg, amphibolitic ct zones. Basal ct well defined 44 dtca Ultramafic fault gouge. Blue black UMs, fine grained, mod mag, calcitic, soft, talcy, mod blocky w/ fault cm a 46 dtca. Below gouge core is weakly foliated. Unit is not well mineralz or well veined Ultramafic Komatiite. Sharp ct into the first in a series of flowy looking UM material, dark green, fine grained, chloritic top/margin, w/ bx looking slightly paler coloured somewhat elongated fragments, w/in a chloritic UM matrix. Core is weakly biotitic, amphibolitic, weakly mag, fine grained, soft, unveined, and unmineralz. Core is mod blocky in this area w/ gouge mm e 4 dtca. Basal ct well defined 4 dtca Ultramafic Komatiite. Blue black to mod green toned, UM flow, slightly coarser grained central core, grading finer towards, bx flow top? 6 dtca. Mod mag, strongly calcitic, not well veined or well mineralz Ultramafic Komatiite. Massive UM material, grading finer grained, and more chloritic, and weakly bx towards basal ct w/ fgg, suggesting fault concentrated the top/margin of this flow. Basal ct w/ gouge/granulated core 68 dtca Fault gouge. Strongly gouged and granulated core, averaging between 6-7 dtca. Basal 7 dtca Ultramafic Komatiite. Blue black UM material, w/ somewhat of a flowy texture, displaying fine cooling cracks, relict spinifex textures, and some localized breccia. Core is moderately blocky, calcitic, amphibolitic, unveined, and effectively unmineralz. Basal ct well defined albeit 68 dtca, w/ veining Ultramafic Komatiite. Dark brown to green toned, amphibolitized UM flow. Core is mod mag, pervasively calcitic, fine grained, soft, and contains what appears to be relict spinifex textures, although this is unclear. Basal ct S 61 dtca BASALTIC KOMATIITE Light green grey to weakly bluish hued, flowy looking material, presumably *; 14 of basaltic affinity, although weak blue cast is similar to UM flows as seen * uphole. Core is silicified, strongly mag, local patchy pervasive calcite, w/ l.osr a few late calcite fractures, and some foliated(4 dtca) blue green calcite X-% 17

8 Drill Hole MU98- Page: 8 of 14 Len PY AU AU1 AU ppb patches/bands towards base of unit. Rx contain a few irregular shaped patches of amphibolitization. This unit reacts weakly to ank stain, is not well veined and mineralz w/ tr-1.% py as fine and coarse diss grains, and lesser fine py seams to clusters. Basal ct slightly irregular 67 dtca, w/ elevated py ULAMAFIC KOMATIITE Irregular ct into interflow material, to grey and beige INTERFLOW MATERIAL a sequence of thin UM flows intercalated w/ cherty probably representing the IP target. Core is grey blue toned near the base of unit, fine grained, and granular LGAUUJLCU Ij-Oiu d auiuiiy cdluile overprint. Rx die UKJU may, silicified, not particularly well veined, and well mineralz w/ -* py, as fine diss grains, and seams to streaks up to 4cm in size, holding local concentrations up to 1*. All core reacts strongly to Hcl. Details as follows J y * -* -*.uou b.8.1 Ultramafic Komatiite Interflow Material. This UM flows intercalated w/ beige grey cherty material, all of which has a strong calcite overprint and granular texture. Mineralz w/ -* py as diss grains and seams. Banding approx 4 dtca Chert. Beige to slightly grey toned, calcite overprinted chery interflow material. Granular textured, silicified, mod mag, mineralz w/ -* py. Basal ct mod well 1 dtca ULAMAFIC KOMATIITE INTERFLOW MATERIAL Very thiny laminated UM flows, intercalated w/ fine interflow material. UM material is dark brown to green, amphibolitized and chloritic, while interflow material is pale grey to blue green and considerably harder than UM material. The reaction to calcite is very site specific, w/ the interflow bands reacting strongly to Hcl, and the UM flows, reacting weakly w/in late calcite fractures. Core is well banded /foliated 4- dtca, is non to very weakly mag, not well veined and mineralz w/ l* fine and coarse diss py. The basal ct for this unit appears to a flow top bx, w/ fine fragments in a chloritic and amphibolitic 4 dtca * 1.* ULAMAFIC KOMATIITE A sequence of UM flows, flow bx and pillowed bx w/ pale blue grey, elongated UM fragments up to 1. inches in size in a brownish toned to dark green, chloritic and araphibolitic matrix. Core is mod mag, weakly ankeritic, weakly calcitic w/in some accessory late calcite fractures, not well mineralz w/ l* fine diss py, and weakly -4 dtca. Stretched to elongated fragments, and numerous zones of gouge suggests, that the ductility of this unit has made it a focal point for tectonic displacement, as it takes up the stress easier than some of the surrounding more competent units. Sequence is cut by a mafic intrusive as well. Details as follows *.9 1.* Ultramafic Komatiite.

9 Drill Hole MU98- Page: 9 of 14 Len PY AU AU1 AU ppb Foliated flow bottom to pillowed flow bx w/ elongated pale blue UM fragments in dark green to brown coloured, amphibolitized UM matrix. J.% fine diss py, mod mag, weakly ank, weakly cal in late fractures. Basal ct w/ gouge 9 7 dtca. 8. fgg, 1.7cm of 71 dtca. 8.4 fgg, mm of gouge s 6 dtca. 81. cm Of gouge and granulated core e 6 dtca. S1.7 lyy, i.iutu ox yuuye w 7 dtca. 8. fgg, mm of gouge 9 4 dtca cm Of dtca. 8.8 fgg, mm of gouge 9 7 dtca fgg, lcm of gouge 9 74 dtca fgg, l.lcm of gouge 4 dtca Fault gouge. Rubbled to gouged and granulated 7/7 dtca, w/ the basal ct slightly unclear due to BBC Mafic Intrusive. Fine grained, mod mag, pervasively calcitic, biotitic, amphibolitic, very dark green to black, mafic intrusive. Core is unveined, and not well mineralz. Basal ct sharp 9 1 dtca Ultramafic Komatiite Breccia. Pillowed to flow top bx w/ pale blue green elongated fragments in a dark green to brownish toned, chloritic, and amphibolitic matrix. Core is weakly ank, weakly calcitic w/in late calcite fractures, mod mag, soft, unveined and not well tnineralz. Basal ct 9 44 dtca ULAMAFIC KOMATIITE Broad swath of thinly laminated UM flows, w/ potential UM tuff horizons, although this is unclear. Core is dominated by the dark green to brownish and blue green thinly laminated UM material as seen earlier in this hole. Layering appears to be partially compositional and partially alt, as blue green to pale blue bands react weakly to ank, while the more brownish toned and dark green bands are strongly amphibolitized and pervasively calcitic, w/ some late calcite fracturing in all areas. Core is mod mag, fg, aside from the brownish toned sections which have somewhat of a granular texture, and quite soft, although locally the brownish strongly amphibolitized bands tend to be slightly harder than the blue green and pale grey blue bands. Layering/foliation is quite variable, ranging from 4-6 dtca. Rx contain l-!fc l-%

10 Drill Hole MU98- Page: 1 of 14 Len PY % AU AU1 AU ppb some mod well dev flow textures, are not particularly well veined, and not well mineralz, aside from the numerous intrusives that cut this unit and tend to hold the majority of the sulphides, typically w/ some py kicked out into wall rx adjacent to intrusions. This sequence is moderately blocky w/ numerous zones of gouged and granulated core. A more detailed unit breakdown follows Ultramafic Komatiite. Blue green foliated flow bottom? Foliation 9 4 dtca, and locally slightly contorted adjacent to basal ct. Not well veined or well mineralz. Basal ct sharp dtca Mafic Intrusive. Fine grained, and amphibolitic a margins, slightly coarser grained, granular textured central core. Dyke is strongly mag, pervasively calcitic, weakly biotitic, soft, not well veined or well mineralz. Basal ct sharp 8 7 dtca Ultramafic Komatiite. Brownish toned, amphibolitic UM material, w/ lessor banded blue green thinly laminated UM flow material. Core is soft, weakly to non mag, fg, locally pervasively calcitic, not well veined or well mineralz. Basal ct along BBC making ct unclear Fault Zone. BBC to granulated core w/ gouge 6 dtca Ultramafic Komatiite. UM flow, dominated by brownish toned, strongly amphibolitized, granular textured pervasively calcitic core. Strong pervasive calcite alt, has totally obliterated primary textures. Core contains a weak foliation -6 dtca, which becomes more pronounced towards basal ct. This section is unveined and unmineralz. Basal ct 9 6 dtca u i D.% Q.% Q.% Q.% XK D.% Q.%.7% 1.1: Q.% 1.1: Fault Zone. Broken blocky core w/ gouge 8 dtca Ultramafic Komatiite. Mod blocky. Blue green to pale blue grey, and variably brownish toned UM flow. Core is well banded/foliated dtca, w/ the blue grey green bands exhibiting a weak reaction to ank, and the more brownish toned sections reacting strongly to Hcl. Thinly laminated material is somewhat suggestive of tuffs, but strong calcite overprint make this unclear. Core is not well veined or well mineralz. Basal ct 44 dtca Mafic Intrusive. A granular textured, strongly pervasively calcitic, chloritic, strongly mag mafic intrusive dyke? Strong calcite overprint make minerology difficult to determine. Logged as a mafic intrusive, mainly due to sharp cts, and mag properties. Basal ct 9 46 dtca Ultramafic Komatiite.

11 Drill Hole MU98-OS Page: 11 of 14 Len PY AU AU1 AU NO. *r ppb UM flow material Basal ct 4 dtca fgg mm gouge S 4 dtca Ultramafic Komatiite. Thinly laminated UM flow material, blue grey to green grey, and variably brownish toned, and amphibolitic. approx 6 dtca, and locally slightly contorted. Ank in blue grey bands w/ some late calcite fractures, and pervasively calcitic w/in brownish toned bands. Core is not well veined or well mineralz. Basal ct 9 8 dtca. Oi/.O ^.OCUl Wi. i.du±u yuuge l* OO Uk.Cct Ultramafic Komatiite. A slightly more massive looking section, dominated by blue black UM flow material w/ poorly dev bx sections, somewhat suggestive of flow tops. Core is weakly ank, and weakly calcitic w/in some late calcite fractures, and the odd patch of pervasive calcite alt. Rx are mod to locally strongly mag, not well veined or well mineralz. Core contains lcm of 646. ffl 7 dtca. Basal ct w/ tr gouge 9 4 dtca Fault Zone. Broken blocky core w/ fault gouge from 647. until and O cm of gouge S 41 dtca Ultramafic Komatiite. Finely laminated UM flows as 617., except that there is more of the massive blue black UM material. Reaction to ank and calcite as above. Blue green to pale grey green thinly laminated material contains poorly dev flow top? bx. Rx are slightly less mag than unit Basal ct is diffuse, appearing slightly 8 dtca Felsic Dyke. A grey to weakly brownish toned, somewhat mottled looking, cooked up FD. Core is fg, mod mag, and finely calcite fractured, w/ local silica flooding outside fractures. Upper ct for this dyke is finely bx, basal ct w/ orange dtca. This intrusive is mineralz w/ l-% fine diss py grains, and is not well veined. Core contains some relict feld phenos, visible mainly adjacent to cts Ultramafic Komatiite. A narrow sliver of pale blue green to black UM host, sandwiched between intrusives. Core is weakly banded/foliated and contains some very vague bx material towards basal ct. Upper ct w/ amphibolitic margin. Core is non to very weakly mag, fg, and calcitic w/in the odd late calcite fracture. This unit is not well veined or well mineralz. Basal ct sharp dtca Felsic Dyke. Felsic dyke as above except that dyke is finely chlorite fractured, and quite dirty as it appears to contain some partially assimilated UM material. Basal ct sharp 4 dtca.

12 Drill Hole MU98- Page: 1 of 14 Len PY AU AU1 AU % ppb Ultramafic Komatiite. Sliver of host as Basal ct 4 dtca Felsic Dyke. A dark grey to blue grey, silicified intrusive w/ somewhat ghostly to remnant feld phenos, upper ct. This dyke is fine grained, weakly mag, unveined and not well mineralz. Basal ct sharp 6 dtca Mafic Intrusive. A fine grained, weakly calcitic, mod mag, calcitic, grey coloured mafic iiitiubive dyke. Cuie cuiilainb Liny amphibuleb, eta well as amphiboiitic fragments. Neither veining nor mineralz is well dev. Cts 8 7/4 dtca Ultramafic Komatiite. Blocky, blue grey UM host, sandwiched between mafic intrusives Mafic Intrusive. Mafic intrusive 676.9, except w/ more of the araphibolitized fragments and a stronger calcite overprint. 7/6 dtca Ultramafic Komatiite. Sliver of blue green to brownish toned, chloritic and amphibolitic host. Basal 8 dtca Mafic Intrusive. Mafic intrusive dyke as Basal ct dtca Altered Syenite. A dark grey to black, vfg, mod mag, silicified, alt syenite dyke. Core is very finely fractured, w/ fracturing tending to have 9 least some orange staining, which tends to highlight very tiny relict feld phenos. This dyke in non calcitic except for a weak reaction to Hcl w/in the odd late calcite fracture. Core is not well veined, and mineralz w/ tr fine diss py and tr chalcopy. Basal ct along BBC making ct unclear Fault Zone. BBC to variably gouged and granulated core 4 dtca Ultramafic Komatiite fault gouge. Variably blocky UMs dominated by brownish to dark green coloured, pervasively calcitic material. Core is soft, fg, weakly mag, weakly calcitic w/in late calcite fractures, and pervasively w/in the matrix of the brownish toned amphibolitic sections. Rx are not well veined or well mineralz, and contain a few zones of gouged to granulated core 8 7. mm gouge S 4 dtca, and from 77. until 77.8 gouged to granulated core 6 dtca. Basal ct well defined e 1 dtca Mafic Intrusive. A fine grained, to granular textured 8 base, dark grey to black, mod mag, pervasively calcitic mafic intrusive dyke. Core is flecked w/ tiny

13 Drill Hole MU98- Page: 1 of 14 Len PY AU AU1 AU. % ppb amphiboles and is quite dirty w/ numerous variably sized and shaped amphibolitic fragments. Basal ct well defined albeit slightly irregular 8 dtca Ultramafic Komatiite fault gouge. UM flows, dominated by finely laminated blue green flows w/ lessor brownish toned, granular textured, pervasively calcitic amphibolitic material. Core contains some bx flow top to pillowed bx material, w/ these areas tending to be the focal point for gouged to granulated core found in this sequence. Fault gouge 71. lcm 8 6 dtca, 71. mm dtca, mm cm of gouged/granulated core, lcm gouge 9 4 dtca, 9 7. uuii t* 7 uluci, and * 79. inches of varidbiy granulated core w/ gouge 4 dtca. Core in this area is not well veined or well mineralz. Basal ct is 4 dtca Altered Syenite. Dull grey to slightly purple hued, alt syenite dyke. Core is fine grained, silicified, non mag, finely mafic fractured, weakly calcitic w/in late calcite stringers, unveined and not well mineralz. Basal ct 9 68 dtca Ultramafic Komatiite. Core is a mix of finely laminated blue/green flows w/ bx flow tops, to pillowed flow tops, w/ increasing brownish toned, amphibolitic and pervasively calcitic material, in the downhole direction. Core is soft, weakly to locally mod mag, unveined and effectively unmineralz. Fault gouge occurrs cm 9 7 dtca, cm 76 dtca, lcm 8 6 dtca, and cm of 49 dtca. Basal ct along a zone of gouge 9 8 dtca Ultramafic Komatiite fault gouge. Fine grained blue black UM flows, w/ flow top bx, and bx pillowed flows. As seen earlier in the hole the bx sections appear to be the focal point for deformation as they are the most strongly gouged and granulated areas, presumably the path of least resistance- Core is strongly mag, weakly ankeritic, weakly calcitic w/in late calcite fractures, and not well veined or well mineralz. Sections of gouge occur 78. 6cm 9 6 dtca, cm of granulated core, 76. cm of gouge 8 6 dtca, cm 4 dtca, a cm gouge 7 dtca, followed by extremely granulated core until dtca. Downhole from 77. core is variably granulated, w/ gouge and and cm respectively and 7 dtca, and 778. cm granulated core lcm gouge 7 dtca, e 78.9 lcm 9 4 dtca, 784. inches of granulated core w/ mud, and 78. tr gouge 9 4 dtca. Below 791. core is very broken to locally rubbled until base of unit, w/ a slight increase in very coarse euhedral py. Basal ct along BBC making ct unclear Mafic Intrusive. Dark grey to black, fine grained mafic intrusive dyke. Core is mod to strongly mag, calcitic, amphibolitic, w/ tiny amphibolitized fragments, and a rather large, strongly amphibolitized upper ct zone down unitl 81.. This dyke is unveined, and contains tr-1% accessory fine py. Basal ct well defined albeit irregular 9 dtca. This dyke contains what appears to be

14 Drill Hole MU98- Page: 14 of 14 TO Len PY AU AU1 AU % ppb tiny remnant feldspars? Ultramafic Komatiite. Return to the sequence of UM flows,lacking the well dev flow top bx and bx pillowed flows, as seen uphole. Core is very blocky w/ gouge, granulation and unrecovered core. This unit is typically blue black w/ some of the brownish toned, more amphibolitic and calcitip material. Core is mod mag, fg, weakly ankeritic, and variably calcitic, w/ the blue black sections reacting mildly to Hcl in late calcite fractures, and the brownish toned sections being pervasively calcitic. This unit is effectively unveined and contains tr-1% py. Fault gouge mm 7 dtca, S 4.6 um of yz.sumidleu cure, w 49.7 l. luui of gouge 11 6 dtca, ist dtca, 8. 4cm of granulated core, 86. tr gouge, 89.8 lcm of granulated core, followed by fractured core until 86. w/ tr gouge on fracture faces lcm of gouge 6 dtca, 86.6 lcm of gouge 7 dtca, cm of gouge cm of gouge 7 dtca. Below 864. core is blocky w/ tr gouge throughout, until until 89.4 core is rubbled w/ feet unrecovered core in this area. Below 89.4 core is more massive, competent blue black to dark green toned UMs. Basal ct well defined 9 4 dtca Mafic Intrusive. Dark grey to black, fine grained, mod mag, calcitic mafic intrusive dyke. Core is slightly granular textured, flecked w/ tiny amphiboles, and contains amphibolitized fragments. Rx are mod silicified, unveined, and speckled w/ lli fine and coarse diss py. Basal ct 9 dtca, and sharp Ultramafic Komatiite. Blue black to dark green and brownish toned UMs. Core is mod blocky, unveined and not particularly well mineralz. Basal ct dtca Mafic Intrusive. Mafic intrusive dyke as , except w/ slightly more sulphides up to %. Basal ct 7 dtca Mafic Intrusive. Mafic intrusive dyke as Upper ct dtca, lower ct open. This dyke contains tr accessory py. 9. EOH.

15 \.^NS- \ * -K-- J - ^ TOWNSHIP - GAUTHIER

16

17 QUEENSTON MINING INC Drill Hole: MU98-6 DIAMOND DRILL HOLE RECORD Property: MUNRO Collar loc from tl Post L441-1'S, 19'W Northing: 8. Easting: 1. Elevation: 11. *** Dip Tests *** *** Dip Tests *** Depth Azi. Dip Depth Azi. Dip Collar Azimuth (Grid). Collar Dip: (O Degrees Grid equals O degrees True) Hole Length: 74.1 Date Printed: 9 Mar, 1999 Date Started: Date Completed: Page: l of 7 DEC 1, 1998 DEC 1, 1998 Drilled by: BENOIT Core Size: NQ Material left in hole NX casing, 7 rods and core b Core Location: Upper Canada Site l Logged by: JD SUMMARY LOG OVERBURDEN PORPHYRITIC SYENITE DIORITE DIABASE PORPHYRITIC SYENITE DIORITE PORPHYRITIC SYENITE DIORITE PORPHYRITIC SYENITE DIORITE PORPHYRITIC SYENITE DIORITE PORPHYRITIC SYENITE DIORITE DIORITE PORPHYRITIC SYENITE MAFIC INUSIVE PORPHYRITIC SYENITE DIORITE PORPHYRITIC SYENITE 1 rf* 1 Q LU^ Hi O Lil o: CD CD CD ~- 1 t LU ffi C/ LU LU u. LU C/ O LU C D4NW.1948 GAUTHIER

18 Drill Hole MU98-6 Page: of 7 Len PY AU AU1 AU ppb OVERBURDEN Hole was collared to test a shallow IP anomaly, never encountered. This hole became 167. feet and was subsequently abandoned. NX casing was reamed to 78.7 feet. Upon abandoning hole, attempts to remove steel were unsuccsessful, leaving 7 rods, 69 feet of NX casing, and the core barrel in the hole. No tropari tests were taken due to continuing magnetics of the hole PORPHYRITIC SYENITE DIORITE Collar in a locally blocky unit of very coarse grained intrusive material, dioritic to porph syenite in composition, as large (up to cm) plag and K spar phenos, approx -% mafic minerals(amphibole, chlorite, tr biotite), and less than 1(^ qtz. Core is grey to variably pinkish/orange toned, silicified, weakly mag, calcitic w/in late fine calcite fractures, effectively unveined, and not well mineralz w/ to tr sulphides. This intrusive is quite dirty containing numerous fragments, as well as few larger fragments/inclusions to roof pendants of wall rx. This dyke contains the odd zone of finer grained material, typically slightly pinker in colour, whether these represent other generations of dyke material, or zones of alt is unclear. Twinned plag phenos are rare, zoned K feldspars are quite common. A few of the larger phenos have milky white rims w/ opaque centres. Downhole this intrusive is extremely dirty, and considerably darker in colour w/ an increase in assimilated mafic and UM material. A few of the inclusions/intrusions have sharp cts, while others have irregular to diffuse and partially digested cts, suggesting some may be dykes, although the majority appear to be fragments, w/ partially digested and irregular cts. The fresher examples are light to dark grey in colour, w/ the pinkish orange staining as a function of hematization. Units of interest as follows Diabase. Fine to med grained, sharp well defined cts, suggesting dyke material, pervasive calcite alt make minerology difficult to determine. Core is mod hard, strongly mag, unveined, and effectively unmineralz. Possibly a diabase. 6/4 dtca Porphyritic Syenite Diorite. Diorite to ISp as collar. Core is becoming increasingly dirty downhole. Basal ct mod well defined, albeit slightly 6 dtca DIABASE Sharp ct into a dark grey to black coloured med grained intrusive rx, appearing to cut intrusive host. Core is quite hard, mod to strongly mag, quite blocky, weakly calcitic w/in late calcite fractures, and contains a network pattern of mafic mineralz and plag feld, w/ some degree of epidote alt. Core also contains a few inclusions of partially digested D host, as well as amphibolitized, angular to subrounded fragments. Core is slightly vuggy. Neither veining nor mineralz is well dev. Basal ct is sharp along BBC, but presumably 6 dtca.

19 Drill Hole MU98-6 Page: of 7 TO Len AU AU1 AU ppb PORPHYRITIC SYENITE DIORITE Return to the coarse grained intrusive material, as described the collar. Core becomes extremely dirty moving in the downhole direction w/ an increase in wall rx fragments, and partially assimilated country rx. Fragments contained in this intrusive are typically strongly cooked, especially near cts, w/ some better preserved material in the central sections of the larger inclusions. Neither veining nor mineralz is well dev. There are a couple of phases of the main intrusive in this area, typically finer grained, w/ both sharp and gradational cts. Units of interest as follows Mafic Intrusive. An inclusion w/ partially assimilated, diffuse cts, irregular 6/4. Inclusion is fine grained, dark grey to black, mod mag, calcitic, and contains tiny amphibolitized fragments. Neither veining nor mineralz is well dev Porphyritic Syenite Diorite. Diorite/porph syenite as described collar. Basal ct, slightly diffuse and irregular 7 dtca PORPHYRITIC SYENITE DIORITE Irregular ct into an extremely dirty section of dioritic? material. Core is quite variably w/ orangish red toned, recognizable diorite w/ large phenos as described above, and extremely cooked up dark grey to black material containing remnant feldspar phenos, contained w/in a predominantly mafic matrix, w/ some dioritic material preserved suggesting core is dioritic in origin and containing increased levels of assimilated wall rx. Core is very blocky to locally rubbled mod mag, silicified, and calcitic. The basal feet of this section contains some fingers of bright orange fine grained material, w/ sharp cts, suggesting this is another phase of the same intrusion. Neither veining nor mineralz is well dev. Basal ct very irregular PORPHYRITIC SYENITE DIORITE Extremely dirty dioritic/porph syenite material as above, except that inclusions, as well as partially digested material appears UM in origin. Inclusions typically have diffuse, irregular cts, fine grained, weakly mag, weakly calcitic, and mod hard, often softer in the central part of inclusion w/ the cts being more silicified. This section of core contains a couple of vein like slivers of fine grained, bright orange D material, interpreted to be another phase of the main intrusive body, as they have well defined sharp cts. Neither veining nor mineralz is well dev PORPHYRITIC SYENITE DIORITE Extremely dirty porph syenite/dioritic material, as above, less the UM !*; component, w/ the inclusions appearing more mafic. Core continues to % 7 contain, dykelets of fine grained bright orange material, interpreted to be a finer grained phase of the main intrusive body. Some of the included

20 Drill Hole MU98-6 Page: 4 of 7 Len AU AU l AU ppb material, in this area appears to be amphibolitized basalt, or possibly mafic intrusive, being calcitic, mod mag, and strongly amphibolitized, locally containing amphibolitized fragments, but typically lacking well defined cts, and often being partially mixed w/ lsp/ host. Below 7. core contains a couple of narrow milky white to light grey qtz veins, w/ associated accessory py up to U.% in wall rx adjacent to veins. Downhole from 8. core is predominantly cooked up, partially digested mafic material, w/ fewer windows of recognizable lsp/ intrusive. Core is mod to strongly broken/blocky, not well veined, and effectively unmineralz. Below 8. mafic material, appears to be partially digested basalt, being fine to med grained, mod mag, amphibolitized, calcitic w/in late calcite fractures, and the odd pervasive calcite patch. Basal ct a bit 6 dtca PORPHYRITIC SYENITE DIORITE Below 44.6 core is more porph in appearance, containing large tabular feldspars w/ diffuse margins in a somewhat finer grained dioritic looking matrix, of mainly grungy chlorite and amphibole w/ a slight increase in qtz content. Core is mod blocky, calcitic w/in late calcite fractures, weakly to mod mag, and mod silicified. Core contains some partially assimilated mafic material as well as a mafic intrusive dyke. This unit is mod blocky, unveined and not particularly well mineralz. The matrix of this unit is dark green to black, while the larger feldspars are typically slightly orangish pink stained, and often exhibiting good zoning. Units of interest as follows Porphyritic Syenite Diorite. Porph syenite/diorite as above, w/ some partially assimilated mafic material. Not well veined or well mineralz. Basal ct mod 7 dtca... Mafic Intrusive. Dark grey to black, granular textured, non to weakly mag, mod silicified, finely calcite fractured, mafic intrusive dyke. Core contains tiny amphiboles as well as the odd amphibolitized fragment. Rx are not well veined or well mineralz. Basal ct quite sharp O 8 dtca Porphyritic Syenite Diorite. A cleaner looking section as 44.6, except w/ fewer inclusions and less partially digested mafic material. Basal ct is grad DIORITE PORPHYRITIC SYENITE A section of core dominated by med grained, grey dioritic looking material, w/ some inclusions of mafics, as well as sections containing partially assimilated mafic material, and a few finer grained, bright orange coloured pulses of what is interpreted to be a finer grained phase of the main intrusive body. This sequence is mod blocky, mod mag, weakly calc in late cal fractures, mod silicified, not well veined or well mineralz. Dioritic looking sections contain tr lime green epidote alt. Mafic inclusions are granular textured, mod mag, and pervasively calcitic. Neither veining nor mineralz is well dev w/in this sequence. Units of interest as follows O

21 Drill Hole MU98-6 Page: of 7 Len PY AU AU l AU ppb Diorite. A more dioritic looking zone of intrusive material, presumed to be a finer grained phase of the main intrusive body. Core is mod blocky, silicified, mod mag, grey, grading to orangish pink hued towards base, not well veined or well mineralz. This section is quite clean containing only a couple of wall rx inclusions, and l band of fine grained, bright pink/orange coloured material w/ diffuse cts. Neither veining nor mineralz is well dev in this area. Grad basal ct Porphyritic Syenite Diorite. An extremely dirty looking sequence of core w/ sections of finer grained, dioritic looking material as 79.6, and coarse grained material, similar to that logged O 44.6, both of which hold inclusions of mafic material, and contain sections slightly darker in colour which appear to contain some partially digested wall rx, as well as a few bands of fine grained, bright orangish pink core typically w/ diffuse cts, interpreted to be a finer grained phase of the main intrusive body. Core is mod silicified, mod mag, weakly calcitic w/in dyke material, and slightly more calcitic w/in mafic inclusions, as well as being mod blocky, unveined, and not well mineralz. Basal ct mod sharp 9 dtca MAFIC INUSIVE PORPHYRITIC SYENITE A sequence of core dominated by a large mafic intrusive dyke, which appears to cut main D/1SP intrusive. Core is fine to med grained, strongly mag, weakly calcitic w/in late calcite fractures, and mod silicified. Rx contain tiny amphiboles, irregular shaped amphibolitized fragments, a few slightly larger fragments of what appears to be amphibolitized basalt, as well as a few sections containing tiny remnant feldspar phenos, suggesting MI has partially digested some D/1SP material. This unit also contains a couple of inclusions? of recognizable D/1SP host. Veining is negligible, mineralz is modest w/ a sprinkling of fine py up to J.% locally. Upper ct is sharp 9 dtca, basal ct is diffuse 6 dtca, and appears partially digested DIORITE PORPHYRITIC SYENITE Return to the dirty sequence of dyke material, as seen earlier in the hole. Core is extremely variable in this area, being a mix of med grained dioritic looking material as 79.6, coarser grained porph syenite looking material as S 44.6, as well as numerous inclusions of wall rx, also quite variable including MI, V7 and 4U. In addition to the numerous inclusions in this unit dyke material contains numerous slightly darker coloured zones which appear to contain some partially digested mafic/um material. Core also contains a few orange red dykes? of what appears to be true syenite, possibly another phase of the main intrusive body, although this is unclear, as cts can be both sharp and gradational. These orange red fine grained sections, as well as a slightly greyer coloured one, contain X-% py locally, as fine diss grains and lesser fracture controlled seams. A more detailed unit description follows Diorite Porphyritic Syenite , *.*.* C^.Bif.: S"

22 Drill Hole MU98-6 Page: 6 of 7 TO Len AU AU1 AU ppb An off white to cream and slightly orange stained unit, containing large plag/k feldspar phenos, tightly packed w/ little mafic matrix. Core is silicified, weakly mag, and not well mineralz or well veined. This unit contains a few mafic/um inclusions. Basal ct unclear Porphyritic Syenite Diorite. An orange red coloured unit of porph syenite as described earlier in the log, w/ a couple of finer grained pulses of bright orange red material, presumed to be another phase of the main intrusive. These bright orange red sections contain tr-1% py, w/ the remainder of the unit basically devoid of py. Core contains a couple of mafic inclusions, as well as some partially digested wall rx. Basal ct is well defined albeit very irregular to ragged , Q.% Ultramafic Mafic Intrusive. An inclusion of what appears to be UM material, which has been intruded by a mafic intrusive from. until.. UM material is blue black quite soft, non mag, granular textured, and pervasively calcitic. Mafic intrusive is slightly harder, weakly mag, granular textured, pervasively calcitic, and contains a couple of small inclusions of UM material. Neither veining nor mineralz is well dev. Basal ct 6 dtca Diorite. A med grained phase of more dioritic looking material, as Core is slightly pinkish stained, silicified, mod mag, calcitic w/in late calcite fractures, and mod dirty w/ a few mafic inclusions, as well as some partially digested mafic material. Core is not well veined or well mineralz. Basal ct quite sharp, albeit 6 dtca Syenite. A bright orange phase of fine grained material, presumed to be related to the main intrusive body. Core is silicified, non to very weakly mag, finely mafic fractured, calcitic w/in late calcite fractures, not well veined and mineralz w/ l* fine diss py. Basal ct 4 dtca Porphyritic Syenite Diorite. Core in this area is extremely variable as 6., w/ alt unit of coarse grained porph syenite, finer grained diorite, mafic inclusions, partially digested mafic material, and a couple of fine grained, bright orange bands which look like true syenites. Core is quite blocky in this area. Basal ct along BBC making ct unclear Diorite. Grey to orange toned dioritic partially digested material. phase as e.6. Basal ct diffuse w/ some Porphyritic Syenite Diorite. Core is extremely variable as 6., w/ alt units of coarse grained porph syenite finer grained diorite, mafic inclusions, and partially digested mafic material. Basal ct quite sharp 8 dtca Diorite.

23 Drill Hole MU98-6 Page: 7 of 7 Len PY AU AU1 AU * ppb Diorite? A fine grained phase of grey coloured silicified, material presumed to be related to the main intrusive body, although this is unclear. Core is calcitic w/in late calcite fractures, non mag, flecked w/ mafics, silicified and slightly glassy in appearance. This unit is mineralz w/ l-% py as fine diss grains, and lesser fracture controlled seams. Basal ct well defined albeit irregular dtca Ultramafic. An inclusion? of blue black UM material. Core is fine grained, granular textured, pervasively calcitic, non mag, and soft. This unit is mod well veined w/ contorted/boudined dark grey qtz veins, and mod well mineralz w/ a X-% mix of fine and coarsely diss py. Core contains a few somewhat ghostly feld phenos suggesting UM is locally partially digested by /lsp host. Core contains a weak foliation as well. Basal ct mod well 7 dtca Basalt. An inclusion of presumably basaltic material containing what appears to be vague variolitic material adjacent to the top ct. Below this point core is extremely calcitic, and amphibolitized making ID difficult. Basal ct diffuse and partially digested Porphyritic Syenite Diorite. Core is a mix of coarse grained, porph syenite material, finer grained dioritic looking material, and numerous inclusions of mafics, as well as slightly darker coloured D/1SP which appears to contain some partially digested mafic material. Neither veining nor mineralz is well dev. Mafic inclusions are pervasively calcitic, and strongly amphibolitic making it difficult to determine whether fragments are mafic intrusive or amphibolitized basalt. Basal ct diffuse and partially dtca Porphyritic Syenite Diorite. An extremely coarse grained section of dyke material, as above except that this sections contains well dev plag/kspar feld phenos up to mm across, w/ local examples of twinning in plag phenos, and zoning in the typically larger kspars. Core is off white to pinkish red stained, weakly to mod mag, silicified, and calcitic w/in late calcite fractures. Core is mod dirty w/ a few mafic inclusions, and a few slightly darker coloured areas, which appear to contain some partially digested mafic material. Neither veining nor mineralz is well dev EOH.

24 TOWNSHIP GAUTHIER ^

25 s. l- \ \ \ 7i L- s loo- - / a \ l L V t Vfr t- L 1" O O H O 8 /N Sc^U l- T ) g o -\- too -M f ' 1 S

26 QUEENSTON MINING INC Drill Hole: MU99-7 DIAMOND DRILL HOLE RECORD Property: MUNRO Collar loc from #4 Post L991-64'S, 6'E Northing: 1. Easting: 6. Elevation: 111. *** Dip Tests *** Depth Azi. Dip Collar Azimuth (Grid). Collar Dip: (O Degrees Grid equals O degrees True) Hole Length: 797. Date Printed: 9 Mar, 1999 *** Dip Tests *** Depth Azi. Dip Date Started: Date Completed: Drilled by: Core Size: Material left in hole Core Location: Logged by: Page: l of 19 Jan, 1998 Jan 14, 1999 BENOIT NQ HX, NX CASING UPPER CANADA SITE M. McGill SUMMARY LOG Len PY Ir S* AU AU1 WT*. AU ppb OVERBURDEN ACHYTE PORPHYRITIC SYENITE BRECCIA PORPHYRITIC SYENITE PYRITIC SILICIFIED ZONE PORCELAINOUS QUARTZ CARBONATE VEINING SILICIFIED ZONE PORCELAINOUS QUARTZ CARBONATE VEINING ACHYTE BRECCIA ACHYTIC LAPILLI TUFF FELSITE BRECCIA CO Q UJ ^^ ^*- III LU DC en CD eg, Si SI i UJ CO UD WC UJ u. OO "X. UJ CJ to o UJ C PORPHYRITIC SYENITE BRECCIA l PORCELAINOUS QUARTZ CARBONATE VEINING FELSITE BRECCIA FELSITE PORCELAINOUS QUARTZ CARBONATE VEINING FELSITE PORCELAINOUS QUARTZ CARBONATE VEINING DEBRIS FLOW PORCELAINOUS QUARTZ CARBONATE VEINING D4NW.1948 GAUTHIER

27 Drill Hole MU99-7 Page: of 19 NO. Len PY AU AU1 AU ppb OVERBURDEN Hx casing was driven to 88.6 feet and NX casing was reamed to 18. feet (1.6 feet into bedrock) through sand and gravel. O to feet- boulders, to 86.6 feet- coarse sand; 86.6 to 16.6 feet- boulders. A successful tropari test was taken at 797 feet- az 7/-1 degrees. Casing is in the hole ACHYTE PORPHYRITIC SYENITE BRECCIA The hole collars in a pale rusty-reddish to pale pink-purple to brownish mottled unit which most probably consists of several flowy to quasi-intrusive phases into which has been introduced a coarse lapilli-sized fragmental ccmjjoiieiil. The eulixe xucx. mauu Iieia subsequently been intensely altered, brecciated and riddled with very fine carbonate and siliceous micro-veinlets; this tends to further mask the protolith(s). These rocks are thought to represent a 'near-vent' flowy/pyroclastic area invaded by shallow alkaline intrusive bodies which accompanied a larger trachytic volcanic center. Fragments of intrusive and volcanoclastic material appear to be caught up in the intrusive components. These intrusives in turn may be intercalated with true pyroclastic materials. The intrusive components include rocks which might be logged as felsites and others which are very much like porphyritic syenites. The type examples of both of these phases are seen at McBean and Anoki. The former rocks are very fine grained, siliceous/albitic, and contain very fine carbonate metacrysts or possibly feldspar phenos. They tend to be greyish to pale purplish to pale pink in colour and may have a a fine cataclastic texture developed in the groundmass. The latter rocks tend to more reddish to orange-toned and consist of a rather siliceous or albitic aphanitic matrix in which are suspended sub-rounded pale milky white to slightly greyish feldspar and occasionally quartz phenos. Both rocks carry fine diss py grains and are generally non-magnetic. Measurements of magnetic susceptibility are quite low ^1.). Definitive examples of trachyte flow material in this section are difficult to differentiate from other rocks which have a more 'intrusive' character. Fragments or 'xenoliths' are generally angular to sub-angular and range from 1/8 inch up to several inches across. Several varieties are found; some are clearly lithic fragments of porphyritic syenite, while others appear almost cherty and are typically darker in colour (grey shades). Some fragments have a fine grained, slightly speckled appearance quite like some of the carbonated felsites logged elswhere. Other dirty white grains or blotches are granulated areas of carbonate and qtz, and or metacrysts of the same. Some of this material appears to be derived from nearby veins while other examples are in-situ metasomatic features. Although these fragments appear fairly discreet megascopically, closer inspection reveals that the boundaries of these features are somewhat fuzzy and not well defined. This may be a result of the generally strong alteration in the rocks. Fine veining/threads of qtz and carbonate are generally xcutting these 'fragments'. There are also examples of metacrysts which appear to post date the 'fragments.'. The rocks are quite hard and likely silicified or albitic. Locally weak U lib , J.U %.*:.*1 1.*.* 1.Oil.*t.1! 1.%.*r 1.*.*.%.Otr 1.%.S** 1.* 1.* 1.Otr.Sir 11.*.Sir 1.Sir 1.* 1.* 1.Olr.Sir 1.S*..*,.Sk 1..Olr,.Sti 1..*

28 Drill Hole MU99-7 Page: of 19 Len (ft ) PY % AU AU1 AU ppb hematitic alteration washes through the system. A good deal of pervasive and vein carbonate has overprinted the rocks,- very minor amounts of calcite lie in late fractures, while the bulk of the carbonate is dolomite t - ankerite. There is probably some moderate to strong potassic alteration in the system also. The rocks are lightly mineralised with very, finely disseminated py and traces of chalcopyrite. Very small amounts of specular hematite are also present. Some slightly higher concentrations of sulphide can be found in and around some of the 'fragments'. The bjtecciated/spolueu appecu.eiice is ci i.tssuit of coeixse tind fine scale tectonic deformation, primary porphyritic textures and/or spotty textures resulting from metacrysts and larger patches of alteration material. Several episodes of alteration and brittle deformation have affected these rocks; little in the way of ductile fabrics are present. Weak jointing at high angles persists throughout the unit. RQD values vary from moderatly high to very low. More details follow in the break out Felsite Breccia. A pale purple-brown coloured rock with a weak porphyritic texture is present down to about 16 feet. A greyish matrix supports pale white feldspar phenocrysts and probably carb metacrysts ranging from an 1/8 to a 1/4 inch across. Below this a more prominent spotted texture develops. The rocks are riddled with very fine scrappy carb and silica filled fractures, mostly at high core angles. Locally xcut by high angle cataclastic zones - inches thick. Weakly sericitic in part, with traces of fuchsite. Locally blocky and broken up with some strong rusty gossan developed around late, low angle slips and joints( especially between 17 and 1). Weakly mineralised with very fine grained py which appears as random disseminations and small patches of the same. There is some very subtle fracture control of the py locally. Fine cataclastic textures are developed in the groundmass down to 16. Below this, the matrix is more aphanitic to massive and resembles a felsite in which very prominent, dirty white carbonate clots and smaller metacrysts have grown. The largest of these have locally collesced into patches several inches across; in some cases this material infills areas around larger fragments of the hostrock. Most metacrysts larger than about 1/ inch in diameter have a fine internal cataclastic texture developing, much like the groundmass in the rocks above 16 feet. Moving towards 148, the rocks slowly become more and more deformed until a coarse breccia develops at around 147. A few sub-rounded xenoliths of slightly more orange coloured?intrusive material appear below 1 feet. Weakly ankeritic and non-magnetic in this interval Slip. A strong rusty slip Ms DTCA Porphyritic Syenite. Brecciated, chaotic, high angle contact into a pale orange to greenish-grey ZO J.J S i.b i LC.1 LC ; % 11.% % : %.1;.*4.1 1.% ) uuu?

29 Drill Hole MU99-7 Page: 4 of 19. TO Len PY % AU AU1 AU ppb weakly speckled unit. Similar to 'porphyritic syenites'and some of the more leucocratic 'diorites' logged at McBean. A more massive, porphyritic intrusive which is relatively fresher and less disrupted than the rocks immediately above. Well populated with 1/8 inch diameter subhedral feldspar phenos and lesser carb metacrysts throughout. Xcut by fine wispy and locally disrupted carb and silica threads and rare veinlets up to 1/4 thick. Most veining lies at high angles, although a clustering around the -4 degree orientation is visible in places. A few sub-rounded xenoliths ranging from 1/ to inches across have been caught up in the unit; these are more numerous moving downhole and are generally of either a dark grey cherty composition or a more orange coloured intrusive similar to those seen in rocks alcove. A few tixauiplcb o! palcuy ofl-while edib-qlz vein material are also present. Continuing quite hard and non-magnetic. Weakly hematised down to about 16. Fine carb/qtz threads xcut the rocks randomly but to a lesser extent than rocks immediately above. Some of the xenoliths are xcut by the veining while others are not. Slightly blocky coring with one narrow rusty zone at around 1 feet. Moderately mineralised with very fine disseminated py; this is present both in the matrix and in some of the fine veining Ms Lapilli Tuff Breccia. Opening along a moderately sharp contact at approximately 4- DTCA into a grey to weak orange coloured, coarsely speckled to splotchy textured section. This interval appears to be a coarse breccia or possibly a fine agglomerate consisting of fragments of greyish and pale orange coloured (porphyritic) intrusive material, mixed in with generally smaller subangular cherty fragments. The size of the constituents, their angularity and relative amounts by volume in the section vary considerably from place to place. Varying amounts of veining and the growth of?later carb metacrysts has produced a very busy texture in the groundmass. The amount of carbonate alteration and veining/microfracturing in general has increased considerably compared to the overlying unit. Fragments are xcut by the veining in many cases. A very hard, siliceous and strongly carbonated interval which is dusted with very fine grained pyrite. Some crude fracture control of the sulphide is evident here and there; as well, slightly greater amounts rim or fill some of the fragments. Locally weakly sericitic with a pale olive coloured variety. Non-magnetic and weakly hematitic moving downhole. Blocky, broken up and rusty from 178 to a *1 11.*.*1 1.*.*1 1.st.*1.1;.* 1 1 i.sk.*.ut *1.*r.*r.; 1..*r 1. ^ 1. ^ 1..*r 1..Olr 1..*! 1. ^..Sir.*r 1.. %..*: *k % Ms Porphyritic Syenite. A short section of orange coloured, relatively fresh looking intrusive (or possibly a trachyte flow). Similar to the unit above at 148, but with crisper feldspar phenos barely supported in a greyish aphanitic matrix. Variably hematised but not strongly so. coarsely brecciated top contact and more anonymous lower contact. Cut by several high angle pale grey qtz veins/stringers and a later, finer, lower angle set of qtz-carb threads. Neither vein set carries any sulphide. The host carries some ghostly inclusions (almost totally assimilated?) which are locally slightly more

30 Drill Hole MU99-7 Page: of 19 Len PY AU AU1 AU. % ppb altered (weak sericite) and carry slightly more very fine diss py as compared to the host. Both lithic and cherty fragments can be seen; they are sub-angular and range from 1/4 to /4 of an inch across. A hard and non-magnetic section which carries small amounts of very fine py Trachyte Breccia. Entering a pale orange, fine breccia or possiljly a coarse lapilli tuff or micro-agglomerate. This area consists of a grainy/porphyritic? matrix in which a large number of angular to sub-angular fragments are suspended. The matrix resembles the unit immediately uphole; a collection of fairly clean feldpar grains (K-feldspar?) barely supported themselves in a pale orange, feldspathic yiouiiuuidbs, bul willi a uuji.e uibjoiiileux'bi'ok.eii aspect. FragmenLS of chert?, lithic (porphyritic) material, (variations on the host phases seen so far in the hole), and pieces of carbonate/qtz vein? and alteration material are littered throughout. The entire mass has subsequently been cracked and shifted about, allowing fine threads of carbonate and silica to xcut the existing components and in some cases fill in and around larger tectonic fragments. Mm to cm scale brecciation and fine cataclasis is visible throughout. A to 4 degree set of qtz stringers appears to post date the tectonic effects and the finer, high angle veining. Weakly mineralised with very fine py,- elevated concentrations occur in and around some of the fragments and may be fractured controled at a mm scale locally. Weakly ankeritic and very hard with no magnetic response Ms Porphyritic Syenite. Opening into a more intrusive-looking phase across a brecciated, somewhat arbitrary contact zone. A very strongly granulated, more heavily veined foot zone occurs at the beginning of the interval. The rocks then become texturally quite like ISp units logged at McBean, with the addition of carbonate and silica overprinting in the form of numerous fine scrappy stringers, gashes and patches/metacrysts. The rocks are a dirty grey colour with some faint orange patches and very hard. Cloudy, but recognizable -4 mm feldspar phenos are supported in a very siliceous, aphanitic matrix. Small fragments of dark grey cherty and more orange-toned lithic material are scattered throughout the unit. Rounded patches of carbonate material ranging from 1/4 to inches across are variably developed throughout and impart a coarse speckled texture to the rocks. Low angle, bone white patches of very fine grained carbonate and silica are developed locally; these are typically somewhat linear, (parallel to the core axis) and often have tiny ladder (tensional) veins developed perp to the GA. These features are generally not mineralised and are xcut by much finer, high angle silica veinlets. Non-magnetic and modestly mineralised with very fine diss py and traces of chalcopyrite. Some fragments are more strongly pyritic both internally and along margins Ms Trachyte Breccia. Returning to another section of spotted to speckled, pale orange to brownish

31 Drill Hole MU99-7 Page: 6 of 19 Len PY AU AU1 AU ST ppb breccia or brecciated flow. Quite similar to the unit above at 18, but with more numerous and prominent clasts and patches of carbonate, which range from 1/8 to l inch across. Some of these features are metacrysts, while others appear to be fragmented vein material. In addition, other sub-angular lithic and grey cherty fragments are scattered throughout the unit. All of these components are cut by very fine, high and low angle carb and siliceous stringers, although the intensity of veining is less than that seen in the unit immediately above. Very thin reaction rims are beginning to develop around many of the clasts in this unit also. A few small examples of the bone white-porcelain type vein material are present. Continueing very hard and non-magnetic. Probably weakly hematised in part. A blocky, locally jji.~ojs.cu-up becliuii wllii stsve-tai iia^zuw, rualy corridors about, weak slips. Weakly mineralised with very fine diss py; greater concentrations are found rimming and inside of some of the cherty and carbonate patches. Weakly sericitic in part. Some very tight late slips offset fragments and the matrix in several spots MS.1... Ms Trachyte. Opening into a bright orange, coarsely speckled unit with well defined, slightly fuzzy, high angle contacts. Probably a thin, porphyritic flow sandwiched between two breccia/flow units. Contains numerous 1/ to l inch diameter, subhedral phenocrysts of altered (carbonate and sericite)?sanadine and a lesser number of smaller felspathic phenos. These are set in a bright orange-red aphanitic matrix, which is locally cataclasticly deformed on a mm scale. Weakly mineralised with only traces of very fine py. Xcut by a few low angle carb-qtz threads. Very hard and non-magnetic Porphyritic Syenite. A pale orange interval with some characteristics of the breccia at 8 and the 'intrusive' at 18. A blocky and broken up interval xcut by several 1/ to l inch thick pale milky barren qtz veins and a rusty, possibly faulted zone at 46. (Similarly rusty and broken up for the first feet of the section). The rocks are weakly and uniformly speckled throughout suggesting an intrusive origin. Small feldspar phenos make up the bulk of the speckling. Small cherty and lithic fragments are scattered throughout, although these are not as numerous as in overlying units. Some of these fragments have weak reaction rims and small strain shadows. Contains several small bone-white gash type veins and several dirty white carbonate clots/metacrysts. A very few tiny angular fuchsite fragments are also present. Generally weakly mineralised, with greater amounts of diss py in and around some of the fragments and alteration features. Fine carb and silica threads at high angles cut all components; these are poorly mineralised. A very hard, weakly hematised unit. The rocks become finely brecciated and bleached approaching the lower contact Lost core. A rusty, broken up section with some very fine pebbles; this suggests a high

32 Drill Hole MU99-7 Page: 7 of 19 Len PY AU AU1 AU % /T ppb angle fault may have cut the core here Felsite Breccia. Opening into a pale grey-green, weakly speckled interval which resembles a felsite filled with numerous small sub-angular fragments of pale grey chert, dirty white carbonate and a lessor number of lithic fragments. A few larger (- inches across) bone-white carbonate patcheg are present in the upper feet of the interval. The matrix is rather cloudy due to the large amount of fine pervasive carbonate and sericite in microfractures and narrow brittle deformation corridors. Invaded by many slightly thicker stringers of carb and silica at 4 to 8 DTCA. A poorly mineralised section with traces of veiry xiiie py Porphyritic Syenite. Returning to a small section similar to the rocks at 4. Pale orange with a weak speckled appearance. This area carries a slightly greater number of 1/8 inch thick high angle pale grey (barren) qtz-carb and carb stringers, which are late features. A few very fine, stringy, -4 degree fracture systems with very slightly coarser py are developed in one or two locations. Locally blocky with rusty joints at 6.7 and Felsite Breccia. Contact into a short interval of pale greyish, weakly speckled possibly intrusive material much like the rocks at 49. Continuing more strongly veined as per the overlying section. Fragments in this area are becoming slightly larger, and the amount of porcelain vein material is increasing. A very pale grey, discreet cherty-siliceous vein cuts the unit 6 DTCA at ; this feature is slightly brecciated along the margins and it carries very pale brownish carbonate inclusions/rafts. No sulphide is carried in the vein proper, however a weak halo of fine py is developed along the margins. The rocks here have a weak reaction to ankerite stain and are very hard and non-magnetic. Slightly more strongly mineralised in the matrix here, with slightly heavier py evident as very fine rims around some of the fragments Ms Porphyritic Syenite. Returning to another section much like rocks at 18. Pale orange with abundant fine, well defined feldspars in the matrix and in small rounded lithic fragments. Some small, angular, greyish cherty fragments are present but they are less common than in the units immediately above. Two inch thick veins xcut the core; a very pale orange high angle siliceous cataclastic zone S 7.9 and a pale grey to slightly glassy qtz-carb vein 74.. The latter vein lies at DTCA and consist of cm scale interlocking qtz and carbonate grains. One mm py grain is present in the vein. A modestly mineralised section containing very fine diss py in the matrix and slightly greater amounts in and around some fragments. The interval is bounded by rather fuzzy, high angle contacts Felsite Breccia.

33 Drill Hole MU99-7 Page: 8 of 19 Len PY AU AU1 AU. % ppb A predominantly dirty greenish-grey section of heavily carbonated and intensely brecciated intrusive? with many fine stringers and gashes and microfractures throughout. Remnant porphyritic textures are visible in portions of the matrix. Larger (- inch) dark grey chert?xlithic fragments are conspicuous in the interval, along with an increasing number of low angle, dirty white carbonate/qtz patches and metacrysts. The rocks are locally weakly sericitic and quite cloudy. Fine h,igh angle qtz stringers cut most of the clasts and flatter veins; fine internal brecciation is developed in many clasts and patches of carbonate. Some areas of the interval have been riddled with very fine grained, buff coloured, almost cherty stringers and or similar patchy alteration. This has subsequently been deformed leaviiiy vej.y xiiie ualauici&lic LeALUxeB in uiciiiy pdita ul Lhe interval. Very hard and moderately mineralised with very fine py and a few small specks of chalcopyrite. Veining, especially later ages, is generally barren, although a few examples with fine chalcopyrite and?galena are present. As in other areas, fragments and some fracture-fillings and or patchy alteration carries slightly more sulphide. A small interval of pale orange ISp lies at 98.4 to A slightly blocky section with one very narrow rusty zone (around a slip?) at MS Trachyte Breccia. Opening into a bright orange-red interval with some strong similarities to the rocks at 8. A coarsely spotted rock which contains sub-angular cherty and lithic fragments. Some of the larger, darker fragments appear to be lithic (porphyritic) fragments as opposed to cherty compositions. 1/ to 1. inch diameter grey-blue phenocysts of possibly altered leucite are also present. Other paler coloured, off white carbonate patches may be metacrysts or possibly vein fragments. These components are supported in a feldspar-rich, medium-grained matrix. The core is xcut by an increasing amount of low angle pale white porcelain-like silica-carbonate fracture-fillings which are typically cracked by very fine perpendicular ladder veinlets. Younger, high and low angle pale grey qtz stringers cut most of the other components- The amount of veining is slowly increasing moving downhole through this unit. Continueing very hard and most probably more strongly altered by potassium in this area. Some of the larger?leucite phenos and other metacrysts have small K-feldspar metacrysts growing on top of the earlier carbonate alteration, suggesting that much of the present texture in this unit is metasomatic. A rusty, broken up section of core lies at 1 to 1.8. The amount of fine pyrite in both the matrix, fragments and in some of the very fine, low angle fractures is higher in this section than in similar rocks uphole. As is seen above, the clasts tend to be slightly more heavily mineralised and often show some fine internal fracture controlled py. In some cases, fragments are larger in this interval than in preceeding units; some examples reach - inches across. Non-magnetic and very hard Ms Felsite Breccia.

34 Drill Hole MU99-7 Page: 9 of 19 Len PY AU AU1 AU.. % ppb Opening into another variation on the finely brecciated intrusive/flow theme. This example is predominantly a pale grey to grey-green, finely spotted rock with a psuedo-porphyritic texture. As in other areas, this phase carries a variety of small pale orange felsic and greyish cherty fragments, suspended in a granular, feldspathic matrix. A few fragments might be of sedimentary origin in this example. The pale white, low angle 'porcelain veins' are present in variable amounts, becoming somewhat less common moving downhole. These features are slightly thicker, however, as compared to examples uphole. Locally some areas are slightly more reddish-orange and resemble the trachyte breccias described above. Other zones have a coarser spotty appearance where larger metacryst of carbonate axe developed. Slightly lalei 1/ iiiuu Lhick. CcLLJJ-qLz veiiiiei- cai, Lhe ullic in a random fashion; these lie at -4 DTCA and are generally barren. Very fine low angle threads of qtz and carbonate xcut some areas in the unit,- these sit at - degrees and suggest that a weak 'vein fabric 1 might be developing locally. The rocks are more disrupted/brecciated in the upper parts of the unit; they become more massive and coarsely granular moving towards 6. A modestly mineralised unit with very fine diss py distributed throughout the matrix. Small amounts of py occur in some of the fragments, however most veining carries little if any sulphide. One exception is a very fine greyish metallic (galena?) in several fine qtz-carb stringers below 8. Some very subtle sericitic alteration begins to appear in the lowermost parts of the unit,- some very tiny flecks of fuchsite are also present. Locally quite blocky with rusty or limonitic joints Ms Trachyte Breccia. Gradational contact into the typical pale orange, finely speckled phase with a pronounced coarse blotchy/veined texture. The normal medium-grained feldspathic matrix is invaded by brecciated vein remnants and discreet blocks of pale white, finely fractured fine grained porcelain-like carbonate-qtz vein material; moving downhole more and more of the vein material occupies the core, until in the last 6 inches it disappears and is replaced by a rusty gossaned zone surrounding an 8 inch section of blocky, broken core. A weak set of - degree carb-qtz stringers xcuts the host and heavy veining. Modestly mineralised with most of the very fine py lying in the matrix and around some of the smaller 'fragments'. Gradational, high angle lower contact Felsite Breccia. Fairly sharp contact into a pale grey, variably brecciated phase. Rocks here resemble porphyritic felsites logged in some McBean holes with the addition of a strong siliceous overprint. The matrix carries faint -4 mm pale white feldspar phenos, carb? fragments and rafts of 'porcelain vein 1 material along with a lot of fine spotty to cloudy carbonate alteration material. Abundant high angle qtz and carb threads/microfractures xcut the unit randomly. Locally offset along 8-9 degree, razor sharp siliceous slips. Very hard and non-magnetic. Weakly mineralised with very fine diss py and traces of chalcopyrite; most is sprinkled throughout the matrix. Low angle porcelain veins and patches/rafts of the same become more voluminous moving

35 Drill Hole MU99-7 Page: 1 of 19 Len PY t AU AU1 AU ppb downhole. wispy vein-like corridors of strong cataclastic deformation (sub-mm scale) criss-cross the unit at variable core angles and become more numerous moving downhole. The matrix material becomes more intensely brecciated below 8; pale dirty white carbonate and siliceous/cherty alteration fluids fill in the voids and themselves become cataclastically deformed. Veining and zones or planes of deformation become more flatly orientated moving towards Ms Cherty Breccia. A laij-ly Buciip COiiLacL au eippiuaiitidlely DTCA uyeus Liiib pale pinkish-grey breccia zone. This unit may represent the result of further alteration and deformation of the overlying unit. Most of the rock in this interval is a finely cataclastic, cherty to granular phase which contains predominantly small (1/4-1/ inch across) angular pieces of a slightly darker grey, strongly siliceous phase and lesser pale orange lithic fragments (more so towards 411). Very hard and non-magnetic. Xcut by a few scattered to 4 degree 1/8 inch qtz stringers. Becoming progessively more pyritic moving towards 411. Most of the sulphide is sprinkled throughout the matrix, but a few small wispy lenses are also present. Very weak reaction to ankerite stain. Very sharp lower contact at 1 DTCA Ms Ms PORPHYRITIC SYENITE PYRITIC SILICIFIED ZONE Opening along a pale milky qtz vein into a pale orange to dark metallic olive green interval of strongly silicified and sulphide-rich rocks. The protolith in most of the interval appears to be a syenite porphyry or a porphyritic trachyte, much as described above. This phase has been intensely silicified and then brecciated at sub-cm scales and - inch diameter size fractions. The voids are filled with a pale greyish cherty phase which is locally crushed and cataclastically deformed on a mm scale. This in turn is strongly dusted with fine grained pyrite and some minor chalcopyrite. Locally the dusting develops into massive pyrite as small clots, patches and lenses within the silicified areas. Fine qtz and carb-qtz stringers/gashes lying at 4- degrees xcut all other components. More details are in the break-out Quartz vein. A pale milky white, 1-1/4 inch thick qtz vein cutting the core 9 DTCA defines the top contact of the sulphide-rich interval. The vein carries small flecks of chalcopyrite, pyrite and a bluesh, soft metallic mineral. It also contains several larger patches of the former sulphide with some closely associated anhedral?galena. The vein margins are sharp and are bounded by an 1/16 to 1/8 inch thick,?later dark grey qtz rind vein which comes in contact with the wallrocks. A dirty brownish alteration halo penetrates several mm into the hostrock from this outer 'shell vein'. The ' * 4.% 7.* 6.* 7.*r.% 7.* 4.%.* 1.%.*.* 8.(Hi IQifc 8.Oil.!*.Sil 7.* 1*1;

36 Drill Hole MU99-7 Page: 11 of 19 Len PY AU AU1 AU.. li ppb vein material is slightly mottled to cloudy and contains several small spidery carb-filled cavities with discreet qtz crystals in them Chert. A short interval of very pale buff-brown coloured chert lies between the above noted qtz vein and the underlying sulphide-rich section. This unit has been internally brecciated and re-cemented and then cracked again creating a tiny stockwork of dark silica-filled fractures; one set of fractures loosely parallels the vein contacts and the other lies perp to the core axis. The result is a crude cm scale 'brick-work' texture overprinting the earlier brecciation/crushing. A poorly mineralised section with traces of very fine py. Bouiiucd by a fiuely LiecuidLtiu, somewhat ragged lower contact which lies at approx 4 DTCA. This contact may be parallel to the vein contact. Non-magnetic Pyritic Silicified Zone. A pale reddish to greenish, sulphide-rich section. Good examples of the pale orange, porphyritic protolith are visible as to inch diameter patches amongst zones of dusty, patchy and semi-massive sulphide. The sulphide-rich areas occupy ls-% of the core and represent in total about -1 % of the rock volume. Small splashes of chalcopyrite are visible along fractures perp to the CA, as are very tiny fracture-fillings of a blueish metallic (?galena). The section is locally cracked and riddled with fine - degree (locally arcuate) qtz stringers; these are late and post date the main sulphide event. Some late brecciation also accompanies the veining and breaks across patches of sulphide. A few dirty white patches of finely broken-up, 'porcelain type' vein material are present in the uppermost portions of the interval- Non-magnetic with low MS values (.8-.1) Porphyritic Syenite Breccia. A blotchy, pale grey to dirty orange coloured section of coarsely brecciated host rock with small amounts of fine patchy py scattered throughout. The grey siliceous fluid which has invaded the host phase is clearly visible in portions of this interval. Locally the core is finely broken up and crushed but no faulting or shearing is evident. Small fragments and rafts of porcelain vein material are found at around 4 feet. At least two generations of -4 degree pale glassy grey stringers xcut the breccia. A set of low angle, scrappy gashes also cuts the unit. The rocks become lighter in colour as a pale buff coloured fluid invades the lowermost 8 inches of the interval,- this is finely brecciated also, irregular, convoluted lower contact zone Pyritic Silicified Zone. Returning to a strongly pyritic section, much like the rocks at 41. A more intensely brecciated interval with more micro-fracturing and disruption of the alteration material. Brecciation occurs at several scales ranging from sub-cm up to several cm fragments. Pale orange with a greenish cast down to 44, then becoming more grey-green and slightly more heavily veined. S-1% pyrite with lessor amounts in part. Non-magnetic with a moderate RQD. Slightly ragged, irregular lower contact at approx 8 DTCA.

37 Drill Hole MU99-7 Page: 1 of 19 TO Len PY * AU AU1 AU ppb Ms PORCELAINOUS QUARTZ CARBONATE VEINING Contact into a zone of pale bone white vein or exhalite? material, very similar to veins and fragments of the same noted higher in the hole. This interval consists of of about 9% vein material and %, to inch pale orange fragments of trachyte or syenite porphyry- These xenoliths are representative of rocks seen earlier in the hole and are well preserved with the addition of very fine chloritic rinds or reaction rims. Small brownish flecks of presumably the same material are scattered throughout. The host material is d fine yraineu, vaiiably yidiiuidl qlz duci carbonate rich phase which may be derived from a microcrystalline exhalitive silica deposit (chalcedony?). It has been subsequently cracked, carbonated, finely brecciated, and xcut by fine pale grey siliceous stringers and very fine irregular chloritic-filled fractures and cm scale knots. The matrix of the vein material is poorly mineralised. Very fine diss py is developed along and about some of the fine chloritic fracturing, especially towards the lower contact of the section. Non-magnetic and very weakly reactive to ankerite stain and cold HCl. A broken-up interval with a low RQD value. Strongly brecciated and veined at the high angle lower contact Q.% Ms SILICIFIED ZONE Opening into a strongly silicified corridor consisting of several phases, all of which are barely recognizable through the tectonic and metasomatic overprints. Fine scale brecciation (and possibly shearing)is developed in most of these units, but later alteration has effectively rewelded the rocks into very hard, massive, yet strongly veined siliceous breccias. Most components are riddled with fine threads, gashes and stringers of silica and carbonate. Microfracturing is variably developed throughout. The lower - feet of the section is invaded by irregular porcelain type veining and the basal contact is located where this veining becomes the dominant component. More details follow in the breakout *.* 1.Sir 6.. *fc 4.*..*..S\ Porphyritic Syenite Breccia. The initial phase in this section opens as a recognizable orange-coloured porphyritic rock which quickly becomes a more dirty brownish, mottled to speckled/spotted material as the amount of silicification and veining increases. Strongly veined with many very fine fractures and a lesser number of 1/8-1/4 inch thick low angle, 'porcelain type' veins. Dark grey cherty fluids have invaded the rocks and filled in around fragments of the original rock type. Modestly mineralised with very fine diss py; this is generally restricted to the matrix. The unit concludes at an anonamous, high angle lower contact Ms Cherty Sediments. A pale mossy green coloured interval is present down to 46. The unit is

38 Drill Hole MU99-7 Page: 1 of 19 Len PY AU AU1 AU ppb strongly brecciated, speckled and cut by a 1/8 inch thick, low angle cherty vein for about 1 inches. It then evolves into a layered or foliated rock which although intensely siliceous and cherty appears to have been a mafic tuff? or dirty greywacke? originally. The layering/foliation lies at - DTCA. The unit becomes almost gritty approaching 46, where a wispy conformable carb stringer seperates the 'freshest' part of the unit from a more cataclastic, 'mobile' (sheared?) horizon.. The lower contact is sharp and similarly aligned at about DTCA. A non-magnetic unit with a pronounced sericite? overprint. The rocks contain very little sulphide except for the lowermost - inches which carries a small amount of very finely disseminated pyrite Ms Silicified Breccia. Sharp contact into a dirty pink to dark greyish breccia of indeterminate origin. The uppermost 8 inches has a pale buff appearance and may be weakly sericitic in part. A subtle low angle fabric is developing in this area and there is some semblance of folding in the matrix. Moving downhole, the rocks become a dirty pinkish shade and are finely brecciated or fractured. Hairline chloritic fracture-fillings/rims surround the pieces of hostrock. The pink area becomes darker grey in colour around 46 and the breccia texture becomes coarser and less defined. As well, the amount of sulphide increases dramatically so that the rocks begin to resemble the pyritic silicified zones noted at 41 and 41. Fine grainy to dusty pyrite, one small spot of chalcopyrite and several very small specks of a grey metallic (galena?) are present in and around the most heavily mineralised area. A low angle, very dark grey, cherty, disrupted veinlet cuts across the pyritic zone as do a weak set of high angle, fine qtz threads. These later features are generally devoid of sulphide. A non-magnetic interval Veined Felsite. This last breakout is based on a increasing amount of 'porcelain type 1 veining evolving within a light grey toned matrix. The groundmass resembles a porphyritic felsite texturally. This has been later broken into several subunits by high angle cherty deformation corridors and cm scaled breccia zones. The later veining is highly disrupted and broken-up itself, with rafts and twisting branches becoming more voluminous moving towards 47. Small amounts of chlorite are beginning to develop around these veins in the midst of the deformed matrix. The matrix in this unit is modestly mineralised with very fine diss py; in contrast the veining is very weakly mineralised if at all. Non-magnetic Ms PORCELAINOUS QUARTZ CARBONATE VEINING Opening into a zone of approximately 8% by volume of dirty bone white vein material which encloses rafts and smaller fragments of a dark grey cherty breccia (locally graphitic-ex 48.)and slightly bleached pale orange trachyte or syenite breccias. The former host is visible down to about 48. Below this the fragments are generally trachytic/syenitic. A very strongly 9 S *

39 Drill Hole MU99-7 Page: 14 of 19 TO Len PY % AU AU1 AU.PPb disrupted interval where both the veins and the clasts are broken, criss-crossed by numerous fine qtz stringers and riddled with numerous microfractures. Cataclasis on a mm scale is ubiquitous. Fine pinkish to greenish (epidote?) cherty fluids have invaded and surrounded fragments of vein material and the host rocks in several spots. These fluids are also internally brecciated at a mm to cm scale. Portions of the interval are weakly altered with a pale greenish sericite and a very dark grey chlorite which stains parts of some brecciated areas and surrounds smaller fragments. Slightly more ankeritic in this area as compared to rocks tested uphole. Generally weakly mineralised with very fine py in the host rocks (with some very fine fracture control) and along fine chloritic/sericitic fractures developing iii duu a-luuiiu biecuid zuiiea. Tidcea of di fidkey blue mecailic are visible in some of these areas(molybdenite?) The common high angle, fine qtz stringers are not normally mineralised. A non-magnetic interval. Locally rubbly to crushed over l inch stretches in the lowermost 8 feet of the unit,- little evidence of faulting accompanies these breaks D.% Ms ACHYTE BRECCIA Gradational contact into a strongly silicified, muddy, finely brecciated unit with some similarities to trachyte breccias logged uphole. This example is more heavily altered and broken up internally, leaving very little primary texture intact. The unit begins as a cherty, dark grey rock with some fine speckling (carb metacrysts) after which a more crushed, brittle texture is developed. This crackle texture grades into a more massive verysiliceous, weakly hematised area which bottoms out along a razor sharp, 8-9 degree contact (slip or fault?). Rather weakly veined with high angle hairline qtz stringers. Small flecks of chalcopyrite occur in several of these late features. The matrix is modestly mineralised with a dusting of very fine diss py, as per similar units uphole. Non-magnetic D.% X.% Ms Faulted contact? ACHYTIC LAPILLI TUFF Opening into a distinctive fragmental along a very sharp, high angle contact. The abrupt change at 6.7 suggests a faulted and or dyked-out contact,- slicks are not visible, however very narrow, high angle cherty slips ('siliceous breaks') are present on the hangingwall of the contact within inches of the change. Some evidence of a narrow, pale grey-green cherty/siliceous vein? or tiny dyke? remains on the footwall side of the interface also. The direction of offset is unknown, however the abrupt change in the style of deformation and alteration across this contact suggests a significant movement has occured. The rocks are a medium olive green with a coarsely spotted appearance; sub-rounded, pale orange clasts of porphyritic trachyte/syenite are suspended in a coarse gritty matrix which is strongly sericitic and possibly weakly epidotised? locally. Almost all of the clasts show some weak cloudy to dusty alteration. In contrast to many of the 'flowy-fragmental' units described uphole, this unit is relatively undeformed and not silicified until one approaches the basal contact Sli.S*,.** 1,.* 1..St.,t

40 Drill Hole MU99-7 Page: 1 of 19. Len PY AU AU1 AU ppb The matrix is heavily carbonated but texturally still argues for a tuffaceous protolith. Higher in the unit the matrix is finer and more ashy in character; this changes to more of a crystal tuff? moving towards. Other fragments in various states of assimilation/alteration? are present; these include dark grey cherty fragments, smaller very pale orange-buff lithic clasts without phenocrysts, and other pale greenish?mafic or sedimentary? fragments. Examples of the latter are generally more ghostly (more altered?). Fine irregular, scrappy carb veining is present in small amounts, along with a few pale grey, high angle qtz stringers. Overall the amount and intensity of veining is modest compared to rocks noted uphole. Below about., the character of the unit changes. Silica enters the system along wilh liciyiueulti a milax Lu Lue unueilyiiiy uriil, and the encire rock mass becomes chaotic, brecciated and more strongly veined and microfractured. A non-magnetic and weakly mineralised section. Slightly more very fine py occurs in the groundmass below and immediately below the upper contact. The veining is generally barren. Reaction to cold HCL is negligible and to ankerite stain very slight Ms FELSITE BRECCIA A slightly more massive character signals the approximate beginning of a pale grey, weakly porphyritic interval. Similar to other IF units logged above. Strongly silicified and ankeritic with a moderate amount of very fine fracturing and 1/8 inch thick -6 degree carb-qtz veining. One raft of porcelain type vein material is caught up in the section. Non-magnetic and well mineralised with very fine disseminated py throughout the matrix. Locally finely brecciated and weakly sericitic about fine wispy vein/breccia material. Moderately sharp, coarsely brecciated basal contact at 4 DTCA * l.st 9 O 4.4. Ms PORPHYRITIC SYENITE BRECCIA Contact into a dark brownish unit with an orange cast. A weakly porphyritic section with comparitively little tectonic (brittle) deformation. Strongly silicified and slightly more veined moving downhole. Fairly massive initially, suggesting a possible intrusive origin. Subsequently grading into a more fragmental-like rock with an increasing amount of small carb fragments and metacrysts? A large, dark grey, well mineralised rounded clast lies at 9.; it is compositionally much like the unit immediately above. Around this clast are fine breccias developed in what may be dilatant zones. Around 41, the fragmental texture begins to acquire a weak foliation a about 4 DTCA. At 41. to 4. is a wispy, foliated/finely laminated interval of pale buff to off-white cherty exhalite?? is developed. Internally, the lamini are finely granulated suggesting some shearing may have occured parallel to the layering. Weakly mineralised with small amounts of diss py. The layering lies at 4- DTCA. The major unit concludes along a sharp contact DTCA Q.%.* D.% Chert.

41 Drill Hole MU99-7 Page: 16 of 19 Len PY % AU AU1 AU ppb Ms PORCELAINOUS QUARTZ CARBONATE VEINING Opening into a broad section of pale white to cream coloured vein material which has effectively engulfed and largely replaced an interval of pale orange trachyte/syenite breccia. Quite similar to the unit described at 47. Small (inch scale) fragments and larger (1-, feet) scale rafts of the hosting? trachyte are scattered throughout the section. Approximately 81; of the unit is vein material. Most of the clasts are sub-angular to angular and many are xcut by a set of fine, high angle silica veins which are presumably late features. The matrix material has a fine grainy aspect and contains numerous Small L AdyuieiiLti uf aliyhlly whiter CdxboiidLt: (meldcryscs?} which suggests widespread brittle deformation exits throughout the groundmass. Overall, a poorly mineralised unit where very small amounts of fine diss and fracture-controlled py is found in some of the trachyte fragments. A few pale grey to white qtz veins, typically 1/4 to 1/ inch thick, carry small amounts of a soft grey metallic (molybdenite?) especially towards the lower contact. Below 6, the host components have a strongly bleached appearance and the rocks in general are more severely deformed and crushed. A blocky interval with numerous small crushed and broken zones; these do not appear related to faulting or other local breaks. Non-magnetic and variably ankeritic with little response to cold HC Trachyte Breccia Ms Ms Ms Ms , * i TK Q.% FELSITE BRECCIA Coarsely brecciated contact into a very dark grey to purplish, heavily veined phase; a variation on the felsite breccia theme. This example carries scattered rounded fragments of the typical pale orange porphyritic trachyte breccia in a strongly silicified, variably porphyritic, slightly muddy matrix. Many fine carb flecks and small metacrysts clutter the groundmass along with variable amounts of fine dusty/patchy to semi-massive pyrite. The interval locally resembles the rocks at 41 where the amount of sulphide is greatest. The rocks are riddled with fine carb and qtz stringers and in S.% S.% e.% Q.%.1r.*

42 Drill Hole MU99-7 Page: 17 of 19 TO Len PY AU AU1 AU ppb general the amount of veining and microfracturing is increasing moving towards 64. Much of the veining lies at about 4- DTCA. Irregular boudinaged and disrupted 'porcelain type' veining begins to invade the host at around 649. and becomes more intense moving downhole. Weak sericitic? alteration is developing locally; more so in brecciated and veined areas. Most veining carries very little sulphide. Continueing non-magnetic Ms FELSITE PORCELAINOUS QUARTZ CARBONATE VEINING Opening into a section of greyish-purple, weakly porphyritic felsite, similar Lo the above unil, bul which haa been iuvddeu by ; porcelain type : vein material. About 7% of the interval is vein material. A very strongly disrupted, cracked up and variably brecciated zone xcut by several generations of fine siliceous (white and pinkish toned) and carbonate-rich stringers. The off-white dominant veining has been strongly deformed suggesting that at least strong episodes of brittle deformation have affected these rocks. Weakly mineralised with small amounts of very fine py; this is generally restricted to fragments of felsite. Weakly sericitic locally. Much of the interval is broken up into 4-6 inch long pieces, resulting in low RQD values for the interval Ms as B J. l l (J.S* 1.*1 1.*;.*.:*..UU FELSITE Continueing in a dark grey, finely speckled, fairly massive section of recognizable felsite. A very hard, strongly veined interval without the orange xenoliths seen in units above. Numerous very fine stringers, microfractures and fine carb metacrysts overprint the siliceous groundmass. A few larger carbonate and 'porcelain type' veins roll across the rocks at all angles with some clustering at around 4- DTCA. Locally brecciated in the upper parts of the section with some weak sericite? alteration which accompanies later carbonate and siliceous fluids. Weak alteration halos of the same are developed around some of the larger qtz and carbonate veins. A sharp, 4 degree buff yellow (alteration?) contact occurs at 716.9; below this the rocks are finely brecciated and slightly lighter toned. Wether this is an alteration front, a tectonic front or a change in lithology is unclear. All rocks below the contact are weakly sericitic and contain recognizable clasts again. Another similar interface occurs at 718, with a similar tiny buff coloured rind. Rocks below this feature are again slightly more sericitic and they continue to be finely brecciated. Most of the unit is moderately to well mineralised with fine dusty and patchy py; much of this sulphide occurs in the matrix with some very fine fracture control evident in places. Most of the veining carries little if any sulphide !* 1. %..* 1..* 1.. %..*. % *. s** % Si* Ms PORCELAINOUS QUARTZ CARBONATE VEINING Opening into a mostly pale white interval very similar to the unit at 4.. The unit begins along a coarsely brecciated zone of buff coloured cherty-looking fragments suggestive of an exhalite type of protolith. The

43 Drill Hole MU99-7 Page: 18 of 19 Len PY * AU AU1 AU ppb remainder of the section consists of approximately 9% vein material and % small angular rafts and fragments of pale orange porphyritic trachyte/syenite; the largest of these is generally smaller than those seen in similar units above. The matrix is comparitively more granulated to locally brecciated and is cut by numerous fine pale pink-orange gashes and stringers. Very fine chlorite wisps and crenulated fracture-fillings surround some of the brecciated vein material. Very weak sericite or chlorite washes are developed in some of the more heavily disrupted areas also. Poorly mineralised with small amounts of very fine py in some of the trachyte fragments and associated with some of the chloritic fracture fillings. Traces of a soft blueish metallic are present in the lowermost lo feet of tile Sci.Liuu(iiiulybueiiii.e?). Non-magnecic and xcuc by the cypicai nign angle qtz stringers which post date most of the other veining and alteration. The rocks react very weakly to ankerite stain and not at all to cold HC1. A locally blocky to broken up section with slightly better RQD values overall than the unit at Ms DEBRIS FLOW Opening along a ragged, angular contact into a pale grey to dirty olive green-toned interval with a weak speckled appearance. A psuedo-fragmental rock, distinct from the breccias/flows already logged in this hole. This phase might be better thought of as a micro-agglomerate or polymict lapilli tuff consisting of various sizes and compositions of sub-rounded fragments up to about inches across. Most clasts lie in the 1/4 to 1/ inch diameter class; all components are supported in a coarse sand-sized cataclastic matrix of qtz grains and very finely brecciated lithic clasts. Variations in the amounts of different types of clasts and the amount of alteration is reflected in the overall colour of the rocks. The upper 1-14 feet is a more greyish tone and consists of predominatly felsite fragments in a more siliceous matrix; this area looks quite like some of the felsite breccias noted above. Below 778, an increase in the amount of pale orange trachyte/syenite fragments changes the overall character of the unit. Other fragments include several varieties of dark grey chert, pale orange jasper? clasts, small bits and pieces of carbonate and qtz vein? material and possibly clasts of sediment or mafic volcanic material. A few tiny fuchsitic clasts are also present. A weak overprint of wispy and pervasive sericite invades the section below 778. Very fine qtz and carb stringers xcut the unit at high and low core angles. Locally slightly thicker (1/ inch) porcelain type veins cut the unit. Microfracturing is more strongly developed in the upper half of the section. Very hard and strongly carbonated within the fine groundmass components. Non-magnetic and weakly ankeritic at best. Strongly altered with a buff-toned?carbonate wash down to about 767 from the upper contact. Modestly mineralised with very fine py,- most of this is found in the matrix within clasts and to a lesser extent following fine fracture patterns. The lowermost feet of the unit consist of pale yellowish to buff coloured wispy chert? fragments? cut apart by the typical porcelain type of vein material * 1.% 1.Olr 1.% *1.*r.*

44 Drill Hole MU99-7 Page: 19 of 19 Len PY % AU AU1 AU ppb Ms Ms PORCELAINOUS QUARTZ CARBONATE VEINING Returning to a short segment of material much like the rocks at 7 above. Some pale grey later? qtz is invading portions of the pale white matrix, suggesting more deformation and alteration of this feature moving downhole. A few small trachytic fragments are present in the lowermost 6 inches of the core. Weakly mineralised End of Hole 797. feet.

45 l.^ns^ \ TOWNSHIP, K-- * - GAUTHIER i W } IM ^ \ 1147 nri ^! Scale 1: FMt

46 l- V 'zoo 7??.'

47 QUEENSTON MINING INC Drill Hole: MU99-8 DIAMOND DRILL HOLE RECORD Property: Munro Collar loc from #1 Post L4198-6'S, 1'W Northing: 118. Easting: 4. Elevation: *** Dip Tests *** *** Dip Tests *** Depth Azi. Dip Depth Azi. Dip Collar Azimuth (Grid). Collar Dip: (O Degrees Grid equals O degrees True) Hole Length: Date Printed: 9 Mar, 1999 Date Started: Date Completed: Page: l of Jan 19, 1999 Jan 6, 1999 Drilled by: BENOIT Core Size: NQ Material left in hole HX Si NX CASING Core Location: Upper Canada Site l Logged byi^. F. Ploeger Len AU AU1 AU ppb SUMMARY LOG. 7. CASING ACHYTE LAPILLI TUFF ACHYTE TUFF MAFIC TUFF ACHYTE END OF HOLE Q UJ ^ UJ o LLJ GC en CO eg - 1 t UJ en ea lu * UJ u. CJO UJ u U) UJ cs D4NW.1948 GAUTHIER 4

48 Drill Hole MU99-8 Page: of 8 TO Len AU AU l AU ppb. 7. CASING The overburden as noted by the drillers included boulders from. - 8.' and. - 7.', and coarse sand from 8. -.'. This hole was collared to test a higher grade corridor in the Esker zone. Hx casing was reamed to 49. feet, NX casing was reamed into bedrock 7. feet. Adverse ground conditions S 4. and 64.1 feet required two separate cement jobs. Upon completion of hole attempts to remove casing were unsuccessful ACHYTE LAPILLI TUFF Overall, this appears to be a tracytic tuff that contains various facies/ phases that range from gritty to lapilli to pseudoleucitic. The entire unit is well foliated to - TGA, therefore all the fragments/ lapilli and the pseudoleucite phenocrysts as well as the matrix grains are stretched imparting a streaky lensoid character to the rock. The overall colour is medium grey with local tinges of blue, green, creamy brown and pink depending on the degree of alteration and the facies. Pseudoleucitic phases contain medium to dark blue grey streaks averaging about 1/ inch which appear pseudorhombic in cross section. The core is cut by approximately Hi dull white ankerite veinlets while the matrix is fairly well carbonatized along foliation planes and microfractures with ankerite. The pyrite/ sulphide content is trace overall with occasional enrichment to t over narrow widths. The trachyte tuff facies are all moderately magnetic (averaging about gammas) with weaker responses in more highly altered sections where it appears that the magnetite may have been converted to pyrite. The dominant facies/ phase changes are described separately below Gritty/ Lapilli Tuff- The core starts with a section of gritty to lapilli tuff. It is foliated and streaky as described above and creamy medium grey in colour. It contains about % dull white ankerite stringers roughly parallel with the fabric but locally divergent. The sulphide content is about D.% or less at the start. The fragments/ lapilli occur as dark grey and creamy lighter grey streaks to about l inch. The matrix is fine grained and well foliated Pseudoleucite Trachyte- There is a subtle change whereby dark grey streaks that are assumed to constitue remnant flattened (7:1) and altered pseudoleucite phenocrysts begin to appear. Although deformed, they resemble similar phenos that were relogged in an old Inco hole where the deformation could be traced from pristine phenos through to well sheared ones. When viewed in cross section, the character of the phenos is more euhedral (rhombic?) in appearance. On average, they constitute about 1* of the host with locallized weaker and stronger concentrations. The matrix is gritty and sheared and contains finer grained sections. The leading 4 feet from ' include about l-% disseminated sulphides in the matrix and along foliation planes. This interval is also slightly more altered to a medium pink grey colour and is cut by approximately % irregular dull white ankerite veining. The first 1' of this section also contains a number of porous oxidized slips ', about D.% pyrite is associated with a weak , ,

49 Drill Hole MU99-8 Page: of 8 Len PY AU AU1 AU % ppb network of fabric parallel white and pink carbonate veinlets. The interval is moderately magnetic overall Gritty Tuff- This interval reverts back to a fine to gritty tuff similar to the start of the hole. It is medium grey with creamy grey streaks defining the foliation/ shearing about TGA. Locally there are hints of possible lapilli size fragments and stretched pseudoleucite phenos. The tuff contains trace sulphides and is moderately magnetic Pseudoleucite Tuff- The host becomes pseudoleucitic as described above through a fuzzy contact. The matrix changes to a medium brown grey colour and the phenos seem to emerge as darker bluish grey lenses forming an average of about % of the rock. Overall, the interval is fairly uniform in appearance and contains trace sulphides. However, at about 6.', the colour begins to lighten to medium to pale creamy brownish grey approaching a 1. inch white and pink carbonate k-spar(?) vein 41.'. The altered zone is also slightly enriched in pyrite, averaging approximately Q.% but ranging up to UT adjacent to the vein. There is a second similar 1/ inch 4. which has very little sulphide associated with it. The pseudoleucitic zone continues intermittently to 46.' where the host becomes dominantly tuffaceous. This interval is moderately magnetic except for the altered section where it decreased, again reflecting the possible conversion of magnetite to pyrite Fine Tuff- This section reverts to a gritty to fine tuff with minor local lenses of pseudoleucitic trachyte to 6 inches. Overall it is medium grey with a streakiness imparted or caused by foliation of the gritty medium to fine grained host. The dark grey blue pseudoleucitic phenos occur in a creamy pinkish brown matrix. The colour change of the matrix may represent a primary compositional change or an effect of alteration. The interval is well about TGA and contains 4% dull white carbonate veinlets and trace sulphides Pseudoleucite Trachyte- This segment comprises pseudoleucite trachyte similar to that described above with pseudoleucites stretched to a 6:1 ratio within a strong shear fabric about 4 +/- TGA. The matrix, which is creamy brownish grey in colour,hosts lot streaky bluish grey phenos. Overall, the interval is moderately magnetic with trace sulphides and approximately % carbonate veining which is concentrated in zones. At 77.', there are a series of narrow (1/8 inch) white and pink carbonate veinlets amounting to % over 6 inches with about % sulphides roughly parallel with the fabric. Similarly at 81.', there is a 4 inch section of dull white porcelainic carbonate with % accompanying sulphides. There are two strongly oxidized/porous rusty slips/ faults with minor ground core at 84. and 89.'. They trend at about TGA and the degree of oxidation indicates a strong pervasive ankerite alteration. Between the two oxidized 88.', is a 6 inch creamy white carbonate vein at TGA. It divides a mildly bleached pale pinkish brown grey sheared and mineralized (%)

50 Drill Hole MU99-8 Page: 4 of 8 TO TO Len AU AU l AU ppb pseudoleucite tuff from a more massive porphyritic phase containing orange pink leucite phenos in a purple grey groundmass (spotted trachyte) hosting about D.% sulphides. This unit continues through the second rusty zone to 9.'. It contains about % fine gashy white carbonate threads and ends along a hazy contact parallel to the fabric. The dark blue grey pseudoleucitic trachyte unit continues to 4.' where it grades into the following mixed unit ACHYTE TUFF This interval comprises a mix of the pseudoleucitic facies of trachyte tuff described above as well as mafic and finely bedded/ laminated phases Spotted Trachyte- The zone starts with % lenses of spotted trachyte hosted in foliated medium buff grey to faintly blue grey pseudoleucitic trachyte tuff. The phenos in the matrix of the host are very faint and barely discernible from the remainder of the matrix. The main spotted trachyte lenses comprise orange pink anhedral clots of carbonate (and K-spar?) which are pseudomorphic after leucite and, for whatever reason, were altered differently and were more resistent to deformation than the blue spotted type. Perhaps these were narrow fingers of flows of slightly different chemical composition. The interval is moderately magnetic and contains trace to D.% finely disseminated sulphides. Individual spotted trachyte lenses are up to l foot thick Gritty Tuff- This interval is dominated by gritty fine to medium grained tuff that contains sections of finely banded, very fine grained tuff. The fine banding parallels the strong about 4 TGA. The fine grained matrix contains small clasts that comprise carbonatized/ carbonate grains and pale and dark grey lensoid streaks to 1/ inch that may represent sheared clasts of variable composition. Overall, the tuff is medium grey with trace sulphides and a moderate magnetic signature. A section from 4. to the end is more medium creamy pinkish grey coloured which represents pervasive ankerite alteration along the fabric planes. There is a corresponding increase in sulphide content to about Q.%. The trailing feet are slightly coarser fragmental, the clasts again resembling carbonate fragments, and culminate in about 6 inches of very finely bedded tuff and possibly cherty tuff. At 4.', there are several oxidized slips parallel to the fabric MAFIC TUFF ACHYTE A leading section of altered tuff that appears intermediate in composition, is followed by the bulk of the unit which is comprised of mafic tuff with very little textural or compositional divergences. However, there are local variations in the streaky carbonate alteration features that define the foliation/ fabric as well as in the degree of pervasive carbonatization. The unit averages trace sulphides and is moderately magnetic throughout except in the more strongly carbonatized sections where the magnetite appears to have been converted to pyrite. The less altered portions of the mafic tuff

51 Drill Hole MU99-8 Page: of 8 Len PY % AU AU1 AU ppb are dark grey to black in colour whereas the carbonatized sections are medium to light grey. There is a a subtle and gradual change in the carbonate from ankerite/ dolomite to calcite down hole This is the leading mildly to moderately altered, medium to light grey, moderate to weakly foliated ( about 4 TGA) fine grained mafic tuff. In addition to blue staining indicating that ankerite is the dominant carbonate mineral, there is a slight fizz in the pervasive matrix carbonate indicating the start of an overall decrease in the intensity and composition of the carbonate alteration. Locally, from 46. to 46.' and to 469.', the rock becomes finely laminated/ banded about 4 TGA. There are additional very narrow slivers that are similarly banded. The sulphide content is trace overall with slight enrichment to D.% around late ragged gashy dull white and pinkish orange veinlets and creamy lighter grey more massive, pervasively altered sections such as from ', ' and '. The latter interval is well carbonatized (ankerite dolomite) containing % massive to broken dull white to pink veins. At 466.', there is a small splash of chalcopyrite in a 1/4 inch carbonate veinlet Mafic Tuff - The bulk of this section comprises homogenous mafic tuff which marks the change from ankerite to calcite as the dominant carbonate mineral in veins and pervasive alteration. Overall, it is dark grey to black, with very minor local dark green grey shades, moderately magnetic throughout, moderately well pervasively calcite altered with whispy faint to moderate streaks of dull/ pale grey calcite which define a weak fabric about 4 TGA. There are occasional zones containing poorly formed dull white calcite metacrysts that resemble small clastic grains or phenocrysts. Throughout the tuff, there is is to trace sulphides and Ut late quartz calcite veining. The rock is fairly homogenous as described with no major divergences until about 69.' which marks the start of a series of apparent mafic flows that are described in more detail below. At the start of the interval, there is about 4.' of moderately altered medium pink grey to dull grey tuff which averages approximately l* finely disseminated sulphides/ pyrite. The sulphides are centered on and around dull grey pink alteration bands to inches that contain late ladder type carbonate quartz gash veinlets. Beyond this point, the tuff becomes homogenous as described, calcitic, moderately magnetic ( gammas), dark grey and unmineralized Mafic Flow- There is an apparent change through an indistinct contact into a more massive fine grained mafic unit, possibly a flow although there are no flow contact features. The whispy calcitic features along the foliation planes are absent and the host becomes massive textured and dark green grey coloured. The interval contains about 1% random gash veins and patches of dull white to pale grey calcite f+dolomite?) and quartz with trace pyrite and chalcopyrite. Compositionally, there appears to be no change. The rock is a fine grained mix of chlorite and

52 Drill Hole MU99-8 Page: 6 of Len PY *r AU AU1 AU ppb calcite (and possibly amphibole). The only apparent difference between the mafic tuff and the flow is the massive nature of the latter. It may be a function of the veining, which if predeformation, may have made the host more competant and therefore more resistent to subsequent deformation; or, there may have been a primary lithological difference in rock competance with the veining being a later feature in the more competant lithology This section of the mafic tuff contains dull grey spots and streaks that resemble lapilli or pseudoleucite streaks but which are actually calcite clots and metacrysts that have formed along the foliation planes. The remainder of this interval is typical mafic tuff as described Mafic Flow- At this point, there is another change to a more massive mafic flow as at 69.'. The leading contact appears to follow a ragged l inch calcitic veinlet S about 4 TGA and the trailing contact seems to end abruptly at the end of a carbonate chlorite altered section at 6 TGA. The unit ranges from fine to medium grained indicating that it may be comprised of several different flows with flow contacts at the grain size changes. The overall colour is medium to dark olive green grey with the colour changes reflecting subtle increases in alteration (pervasive calcification). The slightly coarser grained portions of the unit contain local minor visible amphibole grains and round spots about l mm in size, of carbonate, feldspart?) and chlorite pseudomorphed after olivine!?) or possibly infilling amygdules. The flow is mildly fractured with highly irregularly shaped calcite quartz stringers amounting to about 1% infilling the fracture planes. Ocassionally, these veinlets or confined alteration zones are overprinted with later ladder type calcite veinlets. Very minor traces of chalcopyrite and a black metallic mineral are associated with the alteration and stringer zones. This interval is moderately magnetic as well. At 7.', the cut core contains a small speck of chalcopyrite nested in a silver blue mineral that resembles molybdenite or altiate Mafic Flow- This is a somewhat more tenuous fine grained massive mafic flow(?) unit. It is similar in appearance to the first zone at 69.' but contains a weak foliation overprint in places that is accented by calcite metacrysts(?) and weak whispy calcite along the foliation planes. The contacts of the flow are indistinct and it contains less then 1\ secondary carbonate quartz veining Mafic Flow- This is another fine grained massive mafic flow unit similar to the preceeding ones. The leading and trailing contacts are tenuous but seem to be oriented parallel with the fabric. It is uniformly a medium grey colour with a slight greenish tinge and very subtle lighter patches where it was more pervasively calcified. The fine grained texture results from very minute greenish amphibole(?) laths in a lighter grey calcitic groundmass. The interval is moderately magnetic and contains trace sulphides associated mainly with approximately %

53 Drill Hole MU99-8 Page: 7 of 8 Len PY AU AU1 AU % ppb dull grey and creamy pink calcitic patches and veinlets Mafic Flow- This is another massive looking section with indistinct contacts and UT fine calcite spotting. In addition, there are % dull grey randomly oriented calcite stringers and trace sulphides. The unit is moderately magnetic Porphyritic Mafic Flow?- This section appears to be porphyritic but lacks clear cut contacts. The porphyritic texture is due in part to calcite spotting but there is also an apparent primary component of similar sized (1/16 inch) white feldsparf?) phenocrysts. There is a dramatic drop in the magnetic signature from highs of -4 gammas to. gammas across the contact. The unit contains trace sulphides and the contacts and internal fabric trend at about TGA Mineralized Zone- At this point, there is an abrupt drop in the magnetic signature from about gammas to. gammas and a corresponding increase in the sulphide content from trace to an average of about J.%; local concentrations range up to % over 1- feet. The sulphides, pyrite with subordinate (trace) chalcopyrite and arsenopyrite, occur as disemminations and as streaks and veinlets to 1/8 inch wide. The host is mafic tuff as described above with blebs, lenses, patches and whispy streaks of calcite parallel with the foliation fabric. This fabric, unlike in previous intervals, begins at about 4 TGA and flattens internally to TGA. The calcite is pale pinkish grey in contrast with the dark grey/ black matrix. The pyritic zone begins to weaken at a strong carbonate vein with ragged chloritic fractures at '. Vein contacts are irregular at / TCA. By 8.', the sulphide content begins to become irregular/ spotty Weakly Mineralized Zone- There is a gradual decrease in the sulphide content from l to D.% and a comlimentary increase in magnetite from. to 8 gammas throughout this interval. In general, the fabric and veining directions become variable, ranging from the normal angle of 4 TCA to meandering along TCA. The host is dark grey to black mafic tuff containing the calcitic features as described previously. Sulphides occur as disseminated grains and isolated streaks. A quartz carbonate (calcite and ankerite) /7 TCA cuts the unit at 87.8' ', is a carbonate rich zone (%) comprised of dull grey calcite that meanders along TCA and forms the dominant constituent, and, pale creamy pink and white calcite/ quartz veins and patches that are concentrated mainly around 88.O'. Associated with the veining is % pyrite and chalcopyrite with very fine spacks of VG s 879.9'. The remainder of the interval exhibits features and textures typical of the mafic tuff with fabric orientations returning to the trend of approximately 4 TCA. There is no distinctive structure or feature that terminates the mineralized zone Mafic Tuff- The interval reverts to mafic tuff averaging trace sulphides except as noted. At 9., 98., 91. and 94.8', there are 1- inch pale pinkish grey alteration zones that

54 Drill Hole MU99-8 Page: 8 of 8 Len AU AU1 AU ppb roughly parallel the fabric and contain up to % disseminated sulphides each. Others that have similar textures and colours are not mineralized. 96. to 98.' is fine grained and resembles the massive mafic flows described earlier in the log. The interval is cut by (^ pale pink irregular calcite stringers and patches with several small splashes of chalcopyrite. The contacts appear wavy at about 6 TGA. The host then reverts back to the mafic tuff with trace sulphides overall but very minor localized (1/ inch) zones of D.% Mafic Flow- This is a massive fine grained flow unit that contains % randomly oriented 1/4 inch calcite stringers which occasionally exhibit minor sulphitic halos amounting to trace overall. The contacts of the interval are indistinct. The flow is uniformly medium grey in colour with a slight pink tinge at the start and it is more highly magnetic then previous flows ranging up to 6 gammas. Following this flow, there is a return to mafic tuff as described Mafic Flows- This appears to be a series of or massive flows with minor tuffaceous interflow material. It begins and ends along indistinct contacts with fine grained massive zones and includes a center section that is medium grained and mildly foliated. The center section is speckled with white calcite along the foliation planes. The core angles of the tuff preceeding the flow are about TCA, whereas internally, they flatten to TCA and end wandering along TCA. The magnetic signature of the flow is comparable to that of the surrounding tuff and it also contains only trace sulphides. Between 17. and 18.', there are several sections of broken core over short intervals probably resulting from areas of multiple nested carb chlorite slips at low (1- degrees) angles TCA. At 177.8', there is a inch pale pink calcite vein at TCA Mafic Flow- This is another massive fine grained mafic flow, but in this instance, it appears to exhibit possible flow contact features such as at 11. and 116.' where there are subtle whispy changes in the colour tones. The magnetic signature is gammas (moderate) and there are trace sulphides. Between 117. and 111.' there is about 7% dull white quartz patches and veining at high (about 6 TCA) angles TCA. The quartz is accompanied by minor calcite, chlorite and traces of pyrite, chalcopyrite and molybdenite(?) This interval comprises 9% dull grey calcite and white quartz with trace sulphides at 4 TCA Mafic Flow- This is the last fine grained mafic flow unit in the hole. It is similar in character to all the others and contains % dull grey calcite veining with trace sulphides END OF HOLE

55 TOWNSHIP GAUTHIER CiouCw ^ ii Se.-, ^

56

57 Northern Ontario MMttyof Development and Mhos Declaration of Assessment Work Performed on Mining Land Ion M() and M(), R.S..11 Transaction Number (office use) /1 Assessment File* Research Imaging D4NW.1948 GAUTHIER 9 section* 9() and 66() of the Mining Act. Under Motion 8 of the Mining Act, this mt work and correspond with the mining land holder. Question* about this collection ent and Mines, rd Floor, 9 Ramsay Late Road, Sudbury, Ontario, PE 6B. Instructions: - For work performed on Crown Lands before recording a claim, use form 4. - Please type or print in ink. 1. Recorded holder(s) (Attach a list if necessary) Name QUEENSTON MINING INC. Address SUITE 11 16, 111 RICHMOND ST. W. TORONTO, ONTARIO MH G4 Name Address Client Number 1819 Telephone Number Fax Number Client Number Telephone Number Fax Number. Type of work performed: Check (S) and report on only ONE of the following groups for this declaration. Geotechnical: prospecting, surveys, r\71 Physical: drilling stripping, n Rehabilitation D flksavs and wnrfc under section 18 frens^ * J trenchina and associated assavs "-1 Work Type Office Use DIAMOND DRILLING Date* Work Prom P"*""* D.y 4 Month 1 Y~r 98 D.y 9 Mon* Y-r99 Global Portioning Syctern Data (if available) wrahip/area GAUTHIER, TCOK * LCDCL TWP6. MorG-PlanNumber G-11.G-719&G69 Commodity tal S Value of Work Claimed NTS Reference.. Q Please remember to: - obtain a work permit from the Ministry of Natural Resources as required; - provide proper notice to surface rights holders before starting work; - complete and attach a Statement of Costs, form 1; - provide a map showing contiguous mining lands that are linked for assign! - include two copies of your technical report. '. Lif. Mining Division ^ l*i liul^ io^k Resident Geologist District J^({ i k la nd. da^. Person or companies who prepared the technical report (Attach a list if necessary) Name DAVE SCHONFELDT, MURRAY McGILL, ft FRANK PLOEGER PROJECT GEOLOGISTS Address c/o QUEENSTON MINING INC, PO Box 996, Kirkland Lake, Ontario PN L1 Name BENOIT DIAMOND DRILLING LTD. Address 17O1, RUE L'HYDRO, C.P. 81, VAL D'DOR, QUEBEC Name SWASTIKA ASSAY LABORATORIES Address P.O. Box 1, SWASTIKA, ONT. POK 1TO Telephone Number (7) Fax Number (7) Telephone Number (819) Fax Number (819) Telephone Number (7) Fax Number (7) Certification by Recorded Holder or AGENT l, WAYNE BENHAM, do hereby certify that l have personal knowledge of the facts set forth in (Print Name) this Declaration of Assessment Work having caused the work to be performed or witnessed the same during or after its completion and, to the best of my knowledge, the annexed report is true. Signature of Recorded Holder or Agent Date Agent's Address QUEENSTON MINING INC.. TORONTO, ONTARIO 41 (/97) Telephone Number (416) 64-1 RECEIVED Fax Number (416) i MAY GEOSCIENCE ASSESSMENT OFFICE

58 . Work to be recorded and distributed. Work can only be assigned to claims that are contiguous (adjoining) to the mining land where work was performed, at the time work was performed. A map showing the contiguous link must accompany this form. MMng Claim Number. Or if wort* wee done on other eligible mining land, show in thte column the location number indicated on the claim map. 1 TB787 L991(W^ CLM 81 ^ LEASE 1679 fiooot li'i L. 117 Number of Claim Untts. For other mining tend, 1st t-. m rtmnm m raclbtbb. 16 ha 7 c b ha 8 ha Value of work performed on thie claim or other mining land. 6,8 S6,9 S76,96 oc Value of work applied to this claim. N/A, Value of work signed to other mining claims. 14, S4, Bank. Value of work to be distributed at a future date,8 S.9 S76,96 4 L. 1 1 S, L $, 6 7 L. 1 L S se.ooo 8 L S, 9 L S, 1 L 17 1 S, 11 L S 1 L S, Column tals 1 S1,6 S4, S4 S79.6 I.. WAYNE BENHAM,, do hereby certify that the above work credits are eligible under (Print Full Name) subsection 7 (1) of the Assessment Work Regulation 6/96 for assignment to contiguous claims or for application to the claim where the work was done. Signature of Recorded Holder or Agent A in Writing Date 6. Instructions for cutting back credits that are not approved. Some of the credits claimed in this declaration may be cut back. Please check {/) in the boxes below to show how you wish to prioritize the deletion of credits: GO 1. Credits are to be cut back from the Bank first, followed by option or or 4 as indicated. D. Credits are to be cut back starting with the claims listed last, working backwards; or D. Credits are to be cut back equally over all claims listed in this declaration; or D 4. Credits are to be cut back as prioritized on the attached appendix or as follows (describe): Note: If you have not indicated how your credits are to be deleted, credits will be cut back from the Bank first, followed by option number if necessary. For Office Use Only Received Stamp Deemed Approved Date Date Notification Sent RECEIVED Date Approved tal Value of Credit Approved 41 (/97) MAY GEOSCIENCE ASSESSMENT OfFlCE Approved for Recording by Mining Recorder (Signature).194 *~ \J

59 Ministry of Ministere du Ontario Northern Development Developpement du Nord and Mines et des Mines Geoscience Assessment Office 9 Ramsey Lake Road June 1,1999 6th Floor Sudbury, Ontario QUEENSTON MINING INC. PE 6B RICHMOND SEET WEST TORONTO, ONTARIO Telephone: (888) MH-G4 Fax: (877)67-1 Visit our website at: Dear Sir or Madam: Submission Number:.1948 Status Subject: Transaction Number(s): W Deemed Approval We have reviewed your Assessment Work submission with the above noted Transaction Number(s). The attached summary page(s) indicate the results of the review. WE RECOMMEND YOU READ THIS SUMMARY FOR THE DETAILS PERTAINING TO YOUR ASSESSMENT WORK. If the status for a transaction is a 4 Day Notice, the summary will outline the reasons for the notice, and any steps you can take to remedy deficiencies. The 9-day deemed approval provision, subsection 6(7) of the Assessment Work Regulation, will no longer be in effect for assessment work which has received a 4 Day Notice. Allowable changes to your credit distribution can be made by contacting the Geoscience Assessment Office within this 4 Day period, otherwise assessment credit will be cut back and distributed as outlined in Section #6 of the Declaration of Assessment work form. Please note any revisions must be submitted in DUPLICATE to the Geoscience Assessment Office, by the 1 response date on the summary. If you have any questions regarding this correspondence, please contact Lucille Jerome by at lucille.jerome@ndm.gov.on.ca or by telephone at (7) Yours sincerely, ORIGINAL SIGNED BY Blair Kite Supervisor, Geoscience Assessment Office Mining Lands Section Correspondence ID: 18 Copy for: Assessment Library

60 Work Report Assessment Results Submission Number: 1948 Date Correspondence Sent: June 1, 1999 Assessor: Lucille Jerome General Comment: Transaction Number First Claim Number wnship(s) l Area(s) Status Approval Date W GAUTHIER Deemed Approval June 1, 1999 Section: 16 Drilling PDRILL Correspondence to: Resident Geologist Kirkland Lake, ON Assessment Files Library Sudbury, ON Recorded Holder(s) and/or Agent(s): Wayne Benham TORONTO, ONTARIO, CANADA QUEENSTON MINING INC. TORONTO, ONTARIO Page: 1 Correspondence ID: 18

61 u Ontario ARNDL Ministry of Natural Resources l 1 Ministry of. Northern Development and Mines no INDEX TO LAND DISPOSITION k M.N.R. ADMINISATIVE DISICT PLAN KIRKLAND LAKE G-II Victoria ' IfH1 *L T MINING DIVISION TOWNSHIP LARDER LAKE GAUTHIER UNO TITLES/REGISY DIVISION TIMISKAMING Jf-U rv ^F l Wfie: T ^^ T l 1 Seal* 1: loot 1 MttTM i l t&l 1 1 FMt 4 7 MOO 9 1 Contour Interval 1 Metro* AREAS WITHDRAWN FROM DISPOSITION MRO - Mining Rights Only SRO- Surface Rights Only M H- S - Mining and Surface Rights l S / \ 969 l &6JO SYMBOLS e \\xr4111 /'i ( i [7! Dal* DI*po*Jtlon Flrt BARRI.CK POWER LINE Road allowance; surveyed... shoreline.., - J 999,f ll,*71 Ontor TOWNSITE STAKING RESICTED S.S. (B) MINING ACT -Boundary wnship, Meridian, Baseline. IEO4 l \ s DMcrlptton (APPUCATJON PENDMO UNDER PUBLIC LANDS ACT) Lot/Concession; surveyed... unsurveyed r Parcel; surveyed unsurveyed Right-of-way; road..,... railway utility... H X m ;o Reservation Cliff, Pit, Pile... fa Contour...,..,.,... Interpolated. Approximate Depression. 4 r Control point (horizontal)...,...,.. A H ^ "O Flooded land...f...i.. --vc-~-i-i-:-i-i-z Mine head frame..., a Pipeline (above ground)... Railway; single track,... -* ' *double track... -" H 1 ~ abandoned... Road; highway, county, township... access... trail, bush...,...,... Shoreline (original)... Transmission line...,...:...:..^,.. Wooded area... -" -^i V 9 ^ i 69^, \I96 J j 71///I741 DISPOSITION OF CROWN LANDS 1464 /6Z 8 6I Patent Surface 4 Mining Rights Surface Rights Only Mining Rights Only \J x""^, THE INFORMATION THAT APPEARS ON THIS MAP HAS BEEN COMPILED FROM VARIOUS SOURCES, AND ACCURACY IS NOT GUARANTEED. THOSE WISHING TO STAKE MIN ING CLAIMS SHOULD CON SULT WITH THE MIN&G RECORDER, MINISY, OF NORTHERN DEVELOP MENT AND MINES, FOR AD DITIONAL INFORMATION ON THE STATUS OF THE LANDS SHOWN HEREON..e o Lease Surface ft Mining Rights...,...,...,..,..,...B Surface Rights Only.-...,....H Mining Rights Only....V....B Licence of Occupation... w....t Order-in-Council...,....OC o o t Cancelled Reservation....~...,...,...^4 T ^ Sand it Gravel....,...^J *u"' 118*41 NOTICE OF FORESY ACTIVITY THS TOWNSHP l AREA FALLS WITHIN THE TjWljSKAMtN^MANAGEMENT tfmf x ANO'MlY 8E~SUBJECT, TO FOMsY~6PERATK*S. THE MMR UNIT FORESTER FOR THS AREA CAN BE CONTACTED AT: j*^ T, P.O. 8X 19 I SWASTIKA, ONT. POK ITO ARCHIVED JULY 8, 199 CO in * 1 H ARCHIVED AUGUST 8/97. rq CIRCULATED JANUARY,199 ML Map base and land disposition drafting by Surveys and tapping Branch, Ministry of Natural Resources. \ The disposition of land, location of lot fabric and parcel boundaries on this index was compiled for administrative purposes only. C l c