LITHOLOGY REPORT - Detailed -

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1 (m) (m) Lithology Sample # Length Casing Minor Interval: A Casing above ground (Air) G Casing through gravel or overburden (Ground) c Interbedded greywacke; siltstone; mu LC Moderately bedded but highly disturbed, weakly to moderately foliated throughout with a weak, local, spaced crenulation. Strongly fractured throughout. 5-10% quartz-carbonate veining throughout dominantly quartz stringers with trace carbonate. Trace py occurs in foliation planes throughout. Local minor faulting occurs as small mm- to cm-scale faults with trace to minor fault gouge. Lower contact is sharp. --- KP samples ( core removed) LC LC FLT weakly graphitic mostly filled with gouge, some associated lost core BD F 40 weak to strong foliation CRN 10 weak spaced crenulation (can't see saddles) FLT Fault filled with gouge including 20cm lost core FLT Fault filled with angular fragments trace gouge and 20cm lost core BD May-13 8:18:50 AM Page 1 of 22

2 (m) (m) Lithology Sample # Length FOL 20 weak to moderate foliation FLT small fault filled with minor fault gouge and quartz FLT small cm-scale fault with minor gouge BD FOL 60 moderate foliation with trace py in foliation planes FLT possible fault, no visible gouge. Filled with small angular fragments BD FOL 35 moderate foliation CRN 50 weak, spaced cleavage LC 30 sharp lower contact Qtz/Carb Variably angled veins throughout. Glassy to oxidized quartz veins mm- to cm-scale. Milky white to glassy veinlets with trace carbonate in fractures mm-scale. Minor Interval: a a a Lost Core Small zone of lost core in fault. fault with 20cm lost core Fault with 20cm lost core Lost Core Lost Core a Massive, light grey, medium- to coarse-grained. Sharp contacts. --- KP samples ( core removed) 16-May-13 8:18:51 AM Page 2 of 22

3 (m) (m) Lithology Sample # Length LC 45 bedding parallel lower contact c Interbedded greywacke; siltstone; mu Locally well bedded, zone of strong silicification masking bedding and fabrics. Locally foliated. Moderately quartz veined associated with increased silicification. Gradational lower contact. Alteration Maj.: SIL CHL GRU ACT GRA GAR HEM Comment P WM Weakly to moderately silicified throughout, associated with milky quartz veining BD FOL 20 moderate foliation LC gradational lower contact Qtz white to glassy, foggy looking (possibly recrystallized) quartz veins with trace carbonate. At variable angles to core axis a Phyllitic mudstone Dark grey to black, fine-grained, soft. Strongly foliated often obscuring bedding. 5-10% qtz/carbonate veined throughout. Lower contact is gradational. 16-May-13 8:18:51 AM Page 3 of 22

4 (m) (m) Lithology Sample # Length FOL 15 strongly foliated BD 40 moderate confidence, bedding obscured by strong foliation LC gradational lower contact Qtz/Carb white to milky quartz veins with minor calcite apparently bedding parallel a medium-grey, massive, medium-grained. Trace glassy quartz veins. Lower contact is gradational / / / / / / / LC gradational lower contact c Interbedded greywacke; siltstone; mu LC light to medium-grey. Dominantly well bedded cm-scale with some dm-scale 1a beds ~20% mud locally up to 50%. Weakly foliated throughout with local intense fabrics and occasional spaced crenulation. 5-10% glassy to milky quartz veinlets throughout with occasional larger veins including one qtz-ep vein with aspy along rims and fractures. Trace pyrite throughout, dominantly along foliation planes occasionally within quartz veinlets. Small zone from m where foliation is strong to intense with no apparent increase in veining, contains 1-2% py + aspy along fabric and bedding planes, possibly due to increased mud content (?). Lower contact is slightly gradational but parallel to bedding /F / 0.5/F / / / / Minor medium-grained sub- to euhedral 13GR GR GR GR GR GR GR GR May-13 8:18:51 AM Page 4 of 22

5 (m) (m) Lithology Sample # Length arsenopyrite rimming a quartz vein and within fractures in vein. Pyrite occurs replacing arsenopyrite in the same setting /F / 0.3/F / / / / fine-grained pyrite clustered in pods and stringers in fractures parallel to bedding and fabrics. Trace fine- to mediumgrained aspy in fabric planes /F / / / / / / Fine- to medium-grained pyrite along fracture and fabric planes GR GR GR GR GR GR BD FOL 15 moderately foliated BD BD FOL 15 Strongly foliated, can't see saddles due to grain size inconsistencies and veining BD BD FOL 5 moderately foliated BD FOL 15 strongly foliated BD FOL 15 moderately foliated YD1 40 poor graded bedding indicates possible younging downhole BD LC 30 30/075 slightly gradational Qtz ~2cm thick glassy quartz vein with 30-40% epidote (?). Vein at low angle to core axis and undulating. Aspy + py in along rims and in fractures in vein. 16-May-13 8:18:51 AM Page 5 of 22

6 (m) (m) Lithology Sample # Length Qtz/Carb Undulating, strongly broken and fractured vein with 20-30% oxidized orange-yellow mineral? Does not react with acid. No visible sulphides Qtz/Carb Minor glassy quartz veinlets and stringers at variable angles to core axis with trace carbonate along fractures. Minor Interval: a Lost Core mechanical breakage and spun core, 0.5m missing from run. Not sure exact position of lost core a 13GR Grey, coarse-grained greywacke. Contains abundant quartz laths and is strongly sillicified as well as weakly to moderately carbonatized. 1-2% aspy occurs disseminated throughout the unit. Unit may be a 4va although no obvious contacts can be found. Contains a quartz/carb/ep vein near the top of the unit. Lower contact is slightly arbitrary based on bedding and grain-size. Alteration Maj.: SIL CHL GRU ACT GRA GAR HEM Comment P S Strong to intensely silicified throughout with moderate calcite alteration. Alteration decreasing downhole P WM Weakly to moderately silicified with trace carbonate alteration throughout. Decreasin downhole /F / 1.5/DI S / / / / fine- to medium-grained subhedral aspy disseminated throughout as well as rimming veins and within fractures. Trace pyrite occurs along fractures in veins as well LC 20 13GR GR May-13 8:18:51 AM Page 6 of 22

7 (m) (m) Lithology Sample # Length Qtz/Carb Low angle to core axis, slightly undulating. Smokey to glassy quartz with up to 10% ep, 15-20% calcite, likely some other carbonates as well (brownish pink, soft mineral doesn't react with HCl). Contains aspy and py along rims and in fractures c Interbedded greywacke; siltstone; mu 13GR Light to medium-grey, fine- to coarse-grained, ~20-30% mud beds, cm- to dm-scale beds. Weakly to moderately foliated throughout depending on grain size. Fabric often difficult to measure due to width of beds. 5-10% quartz veinlets and carbonate stringers throughout. Trace pyrite contained in fabric planes and fractures throughout. Local aspy associated with minor quartz veining and fracturing. Lower contact sharp. --- KP samples ( m) 13GR GR GR /F / 1/CG / / / / Coarse-grained sub- to euhedral aspy crystals in very fine calcite filled fractures and along quartz vein margins. Pyrite along fracture and fabric planes BD FOL 35 weak foliation BD YD2 45 graded bedding indicates younging downhole BD FOL 20 weak to moderate foliation FLT 40 small fault filled with gouge and minor angular fragments BD FOL 15 very weakly foliated BD May-13 8:18:51 AM Page 7 of 22

8 (m) (m) Lithology Sample # Length FLT 45 small fault filled with gouge FLT 45 small fault filled with gouge BD BD FOL 15 moderate foliation YD3 50 graded bedding indicates younging downhole BD FOL 20 weak to moderate foliation LC 50 bedding parallel Qtz mm- to cm-scale quartz veinlets with minor carbonate stringers Qtz/Carb zone with increased white to glassy quartz veins with calcite along margins and in fractures as well as very fine/wispy calcite filled fractures with aspy a Light to medium-grey, massive, medium- to coarse-grained. Local silica flooding with minor calcite filled <mm-scale fractures. Trace pyrite in fractures throughout. Lower contact is gradational. Alteration Maj.: SIL CHL GRU ACT GRA GAR HEM Comment P M Weak to moderate silica flooding LC gradational lower contact c Interbedded greywacke; siltstone; mu Medium- to dark-grey, fine- to coarse-grained. ~20-30% mud, mm- to cm-scale bedding occasional dm- 16-May-13 8:18:51 AM Page 8 of 22

9 (m) (m) Lithology Sample # Length 50 scale greywacke beds. 1-5% quartz/carbonate veining throughout. Weakly to moderately foliated dominantly in the mud rich beds. Local trace pyrite in fractures and fabric planes. Lower contact is sharp YD3 55 graded bedding indicates younging downhole BD LC 50 sharp lower contact a light-grey, medium-grained, silicified greywacke. Fractured rubbly sections throughout. Trace veinlets throughout, trace pyrite in fractures. Sharp lower contact FOL 25 weakly to moderately foliated LC 40 sharp lower contact Qtz/Carb Patchy to massive glassy quartz with 5% calcite along rims and in fractures c Interbedded greywacke; siltstone; mu medium to dark grey, well bedded with 30-40% mud beds. Bedding cm-scale locally foliated. Local brecciation with carbonate veinlets occurs, with a few faults. Trace py occurs along fractures and in fabric planes. Lower contact is gradational. 16-May-13 8:18:51 AM Page 9 of 22

10 (m) (m) Lithology Sample # Length YD3 40 graded bedding indicates younging downhole BD FLT 40 series of thin gouge filled fault planes parallel to bedding BX small zone of weak brecciation BX small zone of weak brecciation FLT section with multiple narrow fault filled with fault gouge LC gradational lower contact a 13GR Light grey, massive, medium- to coarse-grained with <5% wisps of mud. Locally brecciated by white/pink carbonate veinlets. Small fault zone at 207m. Lower contact is sharp but irregular marked by a large quartz vein BX Minor brecciation due to pink/white calcite veinlets FLT 50 fault zone with ~15% gouge, and 20-30% quartz LC Sharp but irregular lower contact Qtz/Carb Patchy to massive, glassy quartz with minor calcite along rims and fractures Carbonate white/pink calcite weakly brecciating host Carbonate small white/pink carbonate veinlets fracturing unit throughout. 16-May-13 8:18:51 AM Page 10 of 22

11 (m) (m) Lithology Sample # Length Qtz/Carb Broken glassy to smokey quartz veins in fault zone with minor calcite Qtz/Carb glassy to smokey quartz with minor calcite Quartz veins 13GR Glassy to smokey quartz with 10-20% very large ankerite (white/yellow, reacts very weakly with acid when powdered), trace-1% aspy strongly associated with ankerite. Sharp but irregular contacts /Ri / 0.5/C m G / / / / LC sharp but irregular lower contact Coarse-grained, euhedral arsenopyrite occuring in a large quartz vein strongly associated with large coarse-grained ankerite crystals. Fine-grained trace pyrite along the contacts of the vein Qtz/Carb Glassy to smokey quartz with 10-20% very large ankerite (white/yellow, reacts very weakly with acid when powdered), trace-1% aspy strongly associated with ankerite. Sharp but irregular contacts c Interbedded greywacke; siltstone; mu 13GR Light to medium grey, well bedded cm- to dm-scale, ~10-15% muddy beds. Locally weakly foliated. Locally veined, tr py in fractures. Lower contact is gradational. 13GR GR GR GR GR May-13 8:18:51 AM Page 11 of 22

12 (m) (m) Lithology Sample # Length BD BD FOL 25 very weakly foliated BD YD3 50 graded bedding indicates younging downhole FOL 25 very weakly foliated BD YD3 45 graded bedding indicates younging downhole BD FOL 20 weakly foliated (can't see saddles) LC gradational lower contact Qtz/Carb glassy to milky quartz with 10% calcite along fractures associated with ~1% pyrite Qtz glassy to milky quartz Qtz Low angle to core axis, slightly undulating ~ 3cm wide. Trace carbonate along fractures Qtz Low angle to core axis, undulating ~2cm wide, 5-10% epidote Qtz Glassy quartz with minor epidote, one vein but possibly folded? Not a consistent orientation da Sulfide bearing silicate iron formation 13GR (UIF) Dark green, strongly chlorite altered. Contains a quartz vein with 10-20% py + aspy + po m - 3 flecks/specks of VG associated with spotty carbonate alteration. Lower contact is gradational where quartz vein is in irregular contact and contact is masked by carbonate alteration. Alteration Maj.: SIL CHL GRU ACT GRA GAR HEM Comment P I Strong to intense chlorite alteration throughout. Moderate spotty carbonate alteration from 244.7m near a vein. 13GR May-13 8:18:51 AM Page 12 of 22

13 (m) (m) Lithology Sample # Length /F 0.5/F 0.5/F / / / / Quartz veining with fine-grained pyrite and aspy throughout, local trace po / / / / / / / 3 Large flecks/specks of VG in chlorite, associated with minor carbonate alteration near vein LC gradational lower contact Qtz/Carb smokey quartz with 5-10% calcite, strongly sulphidized Quartz veins 13GR White to glassy quartz with trace carbonate. Contains 5-10% large patches of strong chlorite (likely inclusions of host) with aspy and po associated. Sharp but irregular contacts. Alteration Maj.: SIL CHL GRU ACT GRA GAR HEM Comment PCH S Patches of strong to intense chlorite in qua vein, likely inclusions from host rock / 0.2/F 0.5/C G / / / / Coarse-grained, euhedral aspy locally contained within chlorite inclusions in quartz vein as well as minor po in fractures in chlorite and vein LC sharp but irregular lower contact Qtz White to glassy quartz with trace carbonate. Contains 5-10% large patches of strong chlorite (likely inclusions of host) with aspy and po associated. Sharp but irregular contacts. 13GR May-13 8:18:51 AM Page 13 of 22

14 (m) (m) Lithology Sample # Length d Silicate iron formation 13GR (UIF) Green-grey, moderately to well bedded cm-scale; with 20-30% clastics, 5-10% chert and trace magnetite beds. Minor quartz veining and 1-2% po + aspy. With a minor mudstone unit at the bottom. Lower contact is sharp. --- KP samples ( m, ) / 0.8/F 0.2/F / / / / Medium-grained euhedral arsenopyrite along fractures proximal to quartz veining. Fine-grained pyrrhotite strongly filling fractures proximal to quartz veining as well as locally disseminated in unit BD LC 50 sharp lower contact Qtz Sharp but irregular contact, white to smokey quartz with trace carbonate along margins and in fractures. No apparent mineralization associated with his vein Qtz/Carb white to greenish, recrystallized quartz vein with ~20% calcite in veinlets and patches. Vein contains po filled fractures and is associated with a concentration of aspy and po in fractures and host proximal to vein. Minor Interval: c Massive mudstone; argillite Dark grey to black, fine-grained, massive. Sharp contacts. 13GR GR GR GR May-13 8:18:51 AM Page 14 of 22

15 (m) (m) Lithology Sample # Length c Oxide Iron formation 13GR Dark green/grey, well bedded mm- to cm-scale with dm-scale greywacke beds. Trace po locally replacing magnetite. units make up about 20-30% of the zone with sharp contacts parallel to bedding. Locally veined with one vein rimmed by po and aspy. Sharp lower contact. --- KP Samples ( m) / 0.5/DI S 0.1/F / / / / Local fine-grained po disseminated in IF units. Coarse-grained aspy strongly associated with fractures and rimming of a carbonate/qtz vein GR GR GR GR GR GR GR GR UC 50 sharp upper contact of minor unit LC 50 sharp lower contact of minor unit BD UC 50 sharp upper contact of minor unit FOL 30 weakly foliated LC 45 sharp lower contact of minor unit UC 35 sharp upper contact of minor unit LC 50 sharp lower contact of minor unit UC 40 sharp upper contact of minor unit LC 40 sharp lower contact of minor unit LC 40 sharp lower contact Qtz white to glassy, recrystallized quartz Carb/Qtz white calcite with 40% glassy quartz, rimmed by po and c.g. Aspy. Minor Interval: c Massive mudstone; argillite Dark grey to black, massive, fine-grained. Sharp contacts 16-May-13 8:18:51 AM Page 15 of 22

16 (m) (m) Lithology Sample # Length a a a Dark grey, medium-grained, massive. Sharp contacts Dark grey, medium-grained, massive. Sharp contacts Dark grey, medium-grained, massive. Sharp contacts. (Middle Mudstone) d Silicate iron formation 13GR Dark green/white/grey, interbedded silicate iron formation with many greywacke units. No bedding present in silicate iron formation, contacts with greywacke minor units are sharp and mostly parallel to each other. Trace po is located throughout the IF units. SIF is weakly to moderately chlorite altered. One larger quartz vein occurs with few small veinlets. Lower contact is sharp. Alteration Maj.: SIL CHL GRU ACT GRA GAR HEM Comment P WM weakly to moderately chloritized PCH M 20% patches of chlorite in quartz vein P W weakly chloritized P WM weakly to moderately chloritized P W weakly chloritized / 0.2/DI / / / / / S / 0.2/DI / / / / / S / 0.2/DI / / / / / S / 0.2/DI / / / / / S / 0.2/DI S / / / / / LC 35 lower contact of minor unit 13GR GR GR GR May-13 8:18:51 AM Page 16 of 22

17 (m) (m) Lithology Sample # Length UC 30 upper contact of minor unit LC 35 lower contact of minor unit UC 40 upper contact of minor unit LC 40 lower contact of minor unit UC 40 upper contact of minor unit LC gradational lower contact UC 40 upper contact of minor unit BD LC 40 lower contact of minor unit LC 35 lower contact Qtz white to glassy quartz vein with 20-30% patches of chlorite. Contacts are sharp but irregular. Minor Interval: a a a a a a Dark grey, massive, medium-grained. Dark grey, medium-grained, massive. Quartz veins White to glassy quartz with ~20% chlorite. Dark grey, massive, medium-grained. Dark grey, medium-grained, massive. Dark grey, medium-grained, massive. Dark grey, medium-grained, massive. 16-May-13 8:18:51 AM Page 17 of 22

18 (m) (m) Lithology Sample # Length c Interbedded greywacke; siltstone; mu 13GR Dark grey to black, well bedded, mm- to dm-scale. Up to 70% bedded mud. Strongly to intensely foliated with a moderate to strong crenulation often obscuring bedding % carbonate veinlets occur throughout, dominantly parallel to bedding. Lower contact is gradational. --- KP UCS sample ( m) 13GR GR GR GR BD CRN 45 weakly to moderately crenulated FOL 15 strongly foliated BD 25 Can't see bedding, measured off veinlets observed to be bedding parallel in unit FOL 40 intensely foliated CRN 35 strongly crenulated BD FOL 25 intensely foliated (can't see bedding) CRN 60 strongly crenulated FOL 30 intensely foliated (can't see bedding) BD FOL 20 strongly foliated CRN 40 weakly crenulated BD FOL 25 strongly foliated LC gradational lower contact 16-May-13 8:18:51 AM Page 18 of 22

19 (m) (m) Lithology Sample # Length a Phyllitic mudstone 13GR Dark grey to black, strongly foliated, weakly to moderately crenulated. Two small shears filled with chlorite-carbonate and fragments of mud. Lower contact is sharp. --- KP UCS sample ( m) GR GR GR CRN 55 weakly crenulated FOL 25 strongly foliated SHR cm wide shear filled with fine-grained chloritecarbonate and mm- to cm-scale angular mud fragments SHR 15 ~3cm wide shear filled with fine-grained chlorite and carbonate with 5% angular mm- to cm-scale mud fragments LC 30 sharp lower contact d Silicate iron formation 13GR Dark green, intensely chlorite altered. Unit begins with a larger quartz vein. 1-2% po with trace aspy disseminated throughout 2d. Lower contact is gradational. Alteration Maj.: SIL CHL GRU ACT GRA GAR HEM Comment P I Intensely chlorite altered throughout / 1/DIS 0.1/C / / / / Few crystals of aspy, no apparent G association. Fine-grained disseminated po throughout LC gradational contact 16-May-13 8:18:51 AM Page 19 of 22

20 (m) (m) Lithology Sample # Length Qtz White to glassy quartz with trace carbonate along fractures c Interbedded greywacke; siltstone; mu 13GR Medium-grey, well bedded mm- to cm-scale, little to no mud. Locally chlorite altered proximal to a vein. Lower contact is gradational. Alteration Maj.: SIL CHL GRU ACT GRA GAR HEM Comment HL MS Chlorite alteration proximal to vein BD LC gradational contact Qtz White quartz with trace carbonate in fractures. Angle is approximate, contact is slightly irregular. Clear chlorite alteration halo c Oxide Iron formation 13GR Top of unit is slightly sheared and chlorite altered. Light-medium grey/green, mm- to cm-scale bedded throughout. ~5-10% chert, 30-40% magnetite beds. Weakly grunerite altered throughout with one small zone slightly fractured with amphibole alteration present. Trace po + aspy. Lower contact is sharp. Alteration Maj.: SIL CHL GRU ACT GRA GAR HEM Comment PCH WM Local alteration consisting of patches of fin crystalline calcite, fine-grained chlorite localized to Fe-rich beds and acicular to radiating amphiboles very locally P W weakly grunerite altered throughout 13GR GR GR GR GR GR May-13 8:18:51 AM Page 20 of 22

21 (m) (m) Lithology Sample # Length Moderately amphibole altered consisting o pale green acicular to radiating crystals of amphibole. Possibly replaced by carbonate although no reaction with acid. Zone is weakly fractured throughout, possible caus of alteration (?) P W weakly grunerite altered throughout / 0.2/DI S 0.1/C G / / / / Few grains found of medium- to coarsegrained aspy, no apparent association with fractures/veins etc. Fine-grained po locally disseminated in magnetite beds SHR Possible shear zone filled with 40-50% quartz, 10-20% calcite and 5% chlorite FLT 55 small mm-scale fault filled with fault gouge BD BD LC 45 sharp lower contact Qtz/Carb Quartz-carbonate filling possible shear zone Qtz patchy quartz with chlorite alteration halos GR GR GR c Interbedded greywacke; siltstone; mu 13GR Light to dark grey, fine- to very-coarse grained. Dominantly greywacke with up to 30% mudstone locally. Trace py in fractures. Quartz veinlets (<cm-scale) occur at variable angles to core axis throughout although often parallel to bedding. Strength of fabric is dependant on mud content. --- K.P. UCS Sample ( m) EOH = 345.3m 13GR GR GR May-13 8:18:52 AM Page 21 of 22

22 (m) (m) Lithology Sample # Length YU2 35 graded bedding indicates younging uphole BD FOL 25 weakly foliated BD BD FOL 20 strongly foliated 16-May-13 8:18:52 AM Page 22 of 22

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