Geology and Rock Geochemistry Enigma Massive Sulphide Property

Geology and Rock Geochemistry Enigma Massive Sulphide Property, Wilson Creek New Denver, Southern British Columbia North 50o 05’ 33”; West 117o 23’ 29” UTM Zone 11 472000E, 5549000N NTS map sheet 82K/03 Slocan Mining Division

R.I. Thompson, Ph.D., P.Eng. RIT Minerals Corp., 10915 Deep Cove Rd., North Saanich, B.C.

For

Property Operator: Kootenay Gold Inc. 550-999 W. Hastings Street Vancouver, B.C. V6C 2W2 Property Owner: T. Kennedy of Kimberley, B.C.

Table of Contents 1.0 Summary p 6 2.0 Introduction p 8 3.0 Property Description and Location p 9 4.0 Accessibility, Climate, Local Resources, Infrastructure, Physiography p 10 5.0 Exploration History p 11 6.0 Geological Setting p 11 6.1 Local Geology p 15 6.2 Property Geology p 16 7.0 Deposit Type p 20 8.0 Mineralization p 24 9.0 Exploration p 31 10.0 Sampling Method and Approach p 32 11.0 Sample Preparation, Analyses and Security p 32 12.0 Data Verification p 33 13.0 Adjacent properties p 33 14.0 Mineral Processing and Metallurgical Testing p 33 15.0 Mineral Resource and Mineral Reserve Estimates p 34 16.0 Other Relevant Data and Information p 34 17.0 Interpretation and Conclusions p 34 18.0 Recommendations p 35 19.0 References p 37 20.0 Statement of Costs p 39 21.0 Statement of Qualifications p 40

Figures

Figure 1: Digital elevation map showing location of the Enigma Property astride Wilson Creek p 9 Figure 2a: Regional Geological context of the Enigma Property. The belt of dark green rocks is the remnant of the upper Triassic-lower Jurassic back-arc basin p 12 Figure 2b: Regional Geological context of the Enigma Property. p 13 Figure 3: Regional stratigraphic cross section (not restored) showing the relative distribution and thickness of Upper Triassic-lower Jurassic strata (dark green) relative to older successions p14 Figure 4: Geological map of the Enigma Property showing a detailed distribution of lithofacies and location of measured stratigraphic sections p16 Figure 5: Typical sooty, carbonaceous mudstone with euhedral pyrite crystals. The pyrite is interpreted as authigenic; pressure shadows filled with fibrous quartz adjacent to some cubes indicate crystal growth prior to deformation p 17 Figure 6: Typical flaggy character of planar-bedded calcareous siltsone of the Upper Triassic Slocan Group on the Enigma Property p 18

3 Figure 7: Augite porphyry typical of sill textures encountered within the massive sulphide-bearing assemblage p 18 Figure 8: Hornblende-phyric sill present in the massive sulphide-bearing assemblage in stratigraphic section no. 2 (ref. Fig. 17a) p 19 Figure 9: Oblique view of asymmetric chevron anticline. Hammer is oriented along fold axial plane -- sense of vergence is to the right (south). This fold style is characterized by planar limbs and narrow hinges p 20 Figure 10: Inverted cross laminations illustrating the stoss side of a ripple truncated by an overlying laminated sandstone p 21 Figure 11: Part of massive sulphide lens, unknown width, within mudstone breccia host (ref. stratigraphic section no. 3 for location and details of setting) p 22 Figure 12: Mudstone breccia consisting of flinty mudstone and sill clasts in a mudstone matrix p 22 Figure 13: Massive sulphide zone from stratigraphic cross section no. 2 illustrating its deeply weathered and fractured appearance. The zone is 8 m wide p 23 Figure 14: Massive sulphide layer 30 cm wide within zone illustrated in figure 13 p 23 Figure 15: Deeply weathered and fractured massive sulphide zone with mineralized mudstone breccia showing fresh surfaces on samples of mineralized mudstone breccia extracted from shallow excavation. See figures 17a and 17b for details of stratigraphic position and relations p 24 Figure 16: Stratigraphic cross section no. 1 measured along the lower west side of Wilson Creek (ref. Fig. 4 for location). Measured thicknesses from top are in meters and indicated on the right side of the representative column. The succession is interpreted to be overturned, in which case it decreases in age from north to south. Since the bedding is near vertical, the section is best viewed when laid on its side with the top on the left p 25 Figure 17a: Stratigraphic cross section no. 2 measured along the upper west side of Wilson Creek (ref. Fig. 4 for location). Measured thicknesses from top are in meters and indicated on the right side of the representative column. The massive sulphide zone is 8 m wide, from 470 m to 478 m p 26 Figure 17b: Detailed description of the 8 m wide massive sulphide zone depicted in figure 17a. Figures 13 to 15 are examples of lithologies occurring within this zone p 27 Figure 18: Stratigraphic cross section no. 3 measured along the upper east side of Wilson Creek (ref. Fig. 4 for location). Measured thicknesses from top are in meters and indicated on the right side of the representative column. Massive sulphide-bearing zone is 60 m thick from 343 m to 403 m; lenses of massive sulphide in mudstone breccia were collected from a 10 wide zone between 343m and 344m. The measured zone of mudstone breccia from 295m to 403 m is considered very prospective for massive sulphide lenses. Figures 11 and 12 illustrate massive sulphide and breccia textures p 28 Figure 19: Stratigraphic cross section no. 4 measured along the lower east side of Wilson Creek (ref. Fig. 4 for location). Measured thicknesses from top are in meters and indicated on the right side of the representative column p 29

4 Fig. 20: A schematic diagram illustrating a possible genetic relationship between sill intrusion, brecciation and mineralization. Mafic sills intrude semilithified (water saturated) mudstone near the seabed. The combination of heat and pore water creates phreatic-like reactions with water turning to vapor which escapes to the sea floor, and disrupting the mudstone on its way. Meanwhile, circulation of fluids created by the temperature differential between the heat source (sill complex) and the cool surrounding sediments, focuses fluid flow and with it the transport and deposition of suphide minerals, either as replacements or as layers on the sea floor p 31

Tables

Table I: Description of mineral title cells comprising the Enigma Property.

Appendices

Appendix 1: Listing of analytical results for rock samples taken on the Enigma property: samples are identified by unique numbers that are referenced to special coordinates provided as UTMs in zone 11

Appendix 2: Map showing sample locations and numbers.

5 Summary

The Enigma Property (herein referred to as the Property) is owned by T. Kennedy (100%) of Kimberly, British Columbia. Kootenay Gold Inc., a Vancouver- based company, is the operator of the property.

Kootenay Gold Inc. engaged RIT Minerals Corp. in 2008 to undertake a geological evaluation of the property (including field mapping) and to prepare a report that integrates geological and geochemical data bases.

The Property consists of 3 mineral tenures located on Wilson Creek which empties into Slocan Lake at the hamlet of Rosebery, located 7 km north of New Denver, British Columbia.

Seven days were spent in the field, mapping, measuring stratigraphic sections, and investigating specific sulphide mineral occurrences. This work was done in concert with detailed prospecting and rock sampling by S. Kennedy, T. Kennedy and C. Kennedy, a family of prospectors from the town of Kimberly B.C. (hereafter referred to as the Kennedy’s).

Pyrrhotite-pyrite-chalcopyrite-sphalerite massive sulphide lenses (Fig. 1) in mudstone breccia (Fig. 2) are known from at least two localities within a 70-300 m thick stratabound mineralized succession on the Property. The succession is homoclinal, steep north-dipping (overturned), having a strike length of at least 4000 m – open at both ends. Disseminations, stringers and veinlets of pyrrhotite and pyrite with subordinate chalcopyrite and sphalerite are ubiquitous within the mineralized succession. Host lithologies consist of mafic sills (augite porphyry; diabase), carbonaceous mudstone, mudstone breccia, siltstone and carbonaceous limestone.

Breccias consisting of aphanitic, flinty (sill) clasts in a mudstone matrix suggest intrusion of magma into semi-consolidated, saturated sediments proximal to the sea floor were

6 accompanied by phreatic-like subsurface eruptions. The association: augite porphyry, breccia, and pyrrhotite- chalcopyrite-rich massive sulphide within a mineralized stratabound succession is consistent with Besshi-type massive sulphide deposits, a class of strata-bound deposit that occurs in thick sequences of clastic sedimentary rocks and intercalated mafic to intermediate volcanic rocks and (or) sills.

The Property is part of an Upper Triassic-Lower Jurassic (Slocan-Rossland) back-arc basin; as such it is the same age as the Windy Craggy Besshi-type massive sulphide deposit in northwestern British Columbia, the world’s largest such deposit boasting 297 Mt of ore grading 1.4% Cu and 0.3% Zn (north zone only).

Copper-Zn-Pb metal ratios mimic average compositions of Besshi-type massive sulphide deposits world wide: variable Cu/Zn with little or no Pb. Presence of Mn-rich spessartine garnet (coticule) is also characteristic of Besshi-type deposits. Sericite and (or) muscovite, epidote (after augite), mariposite (Ni-Cr mica), biotite, scorodite, and quartz- carbonate veining are all consistent with this deposit class.

The combination of strike length, widths of mineralization, and massive sulphide exposed at surface, make Enigma a property of merit.

In Japan (Besshi mining district, Shikoku Japan), the United States (Ducktown District, Tennessee) and Africa (Matchless amphibolite belt, Namibia), belts of prospective rocks have strike lengths measuring 10’s to 100’s of km; in each case several mines occur along the strike of each mineralized belt. By analogy, Enigma may be part of such a belt, representing an under-recognized class of mineral deposit and a new exploration target in Upper Triassic-Lower Jurassic rocks of southeastern British Columbia.

7 sulphide-bearing outcrops seem appropriate follow-up strategies. The combination of near-by infrastructure, straight forward reliable access, and a structurally simple, steep- dipping planar target, make for excellent diamond drilling prospects.

1.0 Introduction RIT Minerals Ltd. was retained by Kootenay Gold Inc., a British Columbia company, to produce a geological map of the Enigma Property (herein referred to as the Property), and to undertake an independent review of mineral showings, and available geological and geochemical databases and reports.

This report includes a description of the general geological setting of the Property, a description and analysis of the geological mapping and evaluation carried out by the author, a review and assessment of the exploration work done by Kootenay Gold Inc., and an assessment of the merits of the property. Historical records for the area were obtained from The Geological Survey of British Columbia’s online inventory of mineral occurrences and assessment reports (GSB MINFILE and GSB MapPlace).

The author is familiar with the Property having spent 7 days during June of 2008 mapping and evaluating it. The author is also very familiar with the geology of the region, having been responsible for regional mapping and geological compilation in the Vernon (82L) and Lardeau (82K) map areas during the period 1993 – 2006 (e.g. Thompson et. al., 2006 and references therein).

Metric units are used throughout and monetary values are quoted in Canadian currency.

8 3.0 Property Description and Location

The Property is roughly centered at: North 50o 05’ 33”; West 117o 23’ 29”; UTM Zone 11 472000E, 5549000N within NTS map sheet 82K/03. The mineral tenures straddle the Wilson Creek drainage, which flows south and drains into Slocan Lake at the hamlet of Rosebery (Fig. 1).

Figure 1: Digital elevation map showing location of the Enigma Property astride Wilson Creek. The deeply incised river courses are surrounded by rugged systems of alpine ridges. Accommodation and basic living necessities are available in New Denver; however, Nakusp is the nearest source of supplies adequate for an exploration program.

The town of New Denver is 7 km to the south, on the eastern shore of Slocan Lake; the town of Nakusp is 34 km to the northwest on the eastern shore of Upper Arrow Lake. Access is by all weather paved road (Highway 6) from New Denver north 7 km to Rosebery, and then approximately 8 km by logging roads, either side of Wilson Creek.

The Property comprises 3 mineral tenures containing approximately 1500 hectares (Table I). The mineral cell titles were acquired online and as such there are no posts or lines marking the location of the Property on the ground.

Tenure No. Name Owner NTS Date Area 561730 ENIGMA 134308 (100%) 082K 2011/sep/15 497.499 561983 ENIGMA 2 134308 (100%) 082K 2011/sep/15 497.5 561984 ENIGMA 3 134308 (100%) 082K 2011/sep/15 456.108 Owner 134308 - T. Kennedy Table I: Description of Enigma Property mineral titles.

4.0 Accessibility, Climate, Local Resources, Infrastructure, Physiography The Property is accessible using 2 major logging road systems that follow both south and north sides of Wilson Creek from the hamlet of Rosebery on Highway 6, 7 km north of New Denver. These are good quality gravel roads. Accessory roads, some decommissioned (with culverts replaced by water bars), are accessible by 4 wheel drive vehicle and (or) ATV, dirt bike, mountain bike or on foot.

Nakusp is the nearest major supply centre where material and services adequate to explore the property can be found. Infrastructure resources are excellent and readily available. The Property is within a few km’s of the hydroelectric grid; and the region has a long history of mining, hence personnel with heavy equipment, exploration and mining experience are available. The climate is benign, with agreeable Spring-Summer-Fall seasons and a temperate winter that sees relatively limited snow accumulations at lower levels, although accumulations may be substantial at elevation. Work in subalpine and

10 alpine regions is seasonal, limited to June through mid October; at lower elevations the field season extends from late April until early November.

The Property occupies the moderately steep, rugged slopes of Wilson Creek; tributary streams are moderately to deeply incised with seasonal water flow. Elevations range from 600m to 1800 m. Tree species are dominated at lower elevations by Western Hemlock (Tsuga heterophylla) and Engelmann Spruce (Picea engelmannii) with some Interior Douglas Fir (Pseudotsuga Menziesii var. glauca); Subalpine Fir (Abies lasiocarpa) and Engelmann Spruce dominate at higher elevations; Western Redcedar (Thuja plicata) and Sitka Alder (Alnus crispa) occupy moist, shaded areas, avalanche shoots and steep stream beds; logged areas have been replanted with Lodgepole Pine and a scattering of Engelmann Spruce.

Outcrop is sparse, except along road banks and in some creek beds.

5.0 Exploration History To the best of the author’s knowledge, there is no exploration history for massive sulphide occurrences in the Wilson Creek area.

6.0 Geological Setting The Property is contained within Upper Triassic and Lower Jurassic clastic, volcaniclastic and volcanic rocks comprising an arc and back-arc assemblage that extended the length of the Cordillera from Yukon to southern California. In southern British Columbia the assemblage covered a vast region from present day Kamloops east and south to Rossland, British Columbia (Figs. 2 and 3). Regional lithofacies patterns

Figure 2a: Regional Geological context of the Enigma Property. The belt of dark green rocks is the remnant of the upper Triassic-lower Jurassic back-arc basin.

Figure 2b: Regional Geological context of the Enigma Property.

Figure 3: Regional stratigraphic cross section (not restored) showing the relative distribution and thickness of Upper Triassic-lower Jurassic strata (dark green) relative to older successions. feature carbonaceous clastic strata and rare limestone (Slocan Group) beneath and interfingering with clinopyroxene-phyric volcanic rocks and sills spanning calc-alkaline and tholeiitic varieties but including alkaline varieties as well. Analyses of detrital zircons from sandstone facies within the Slocan Group, yield strongly negative εNd values, suggesting derivation of sediment from an evolved continental source like the North American craton (Unterschutz, 2002); conversely, detrital zircons sampled from volcaniclastic rocks near flows and breccias of the Nicola and Rossland Groups yield positive εNd values, an indication that the volcanic component of the back arc basin was derived from juvenile crustal sources. Hence, it appears that there was a broad Late Triassic to Early Jurassic clastic basin (Slocan Group) which occupied most of Vernon (82L) and Penticton (82E) map areas and formed part of the outer self to the ancient pacific margin of North America; it was fringed by volcanic belts: the upper Triassic Nicola Group on the west, and the Lower Jurassic Rossland group on both the west and the east.

14 During the Upper Jurassic, the arc and back arc, together with subjacent assemblages, were deformed, uplifted and intruded, first by Upper Jurassic (~160-180 Ma) diorite, later by Cretaceous (~70-90 Ma) granodiorite and granite, and most recently by small felsic Tertiary (~50 Ma) stocks and sills.

Mountain building was protracted (180-50 Ma) with the net effect in the west Kootenays of producing a convex east, curvilinear belt of tightly folded and faulted strata called the Kootenay Arc (Fig. 2). The Property is located about 10 km west of the Kootenay Arc structural trend where folds are generally open and trend east-west; faults are steep- dipping with relatively small displacements.

6.1 Local Geology Geology in the vicinity of the Property (Fig. 4), at the northern end of Slocan Lake, is dominated by the Upper Triassic and Lower Jurassic Slocan Group, a succession of carbonaceous mudstone, sandstone and limestone deposited into a back-arc basin having restricted circulation. Contacts between litho types are, for the most part, sharp and planar; low angle cross stratification is common within sandstone beds, and grading may be present; limestone beds are carbonaceous and uniformly fine-grained and silty. The sandstone beds are interpreted as sediment gravity flows (turbidites) deposited within the distal portion of a much larger turbidite fan. Presence of euhedral pyrite crystals in black carbonaceous mudstone, in copious quantities in some beds, suggests the basin was anoxic and sulfur-rich.

There are three nearby intrusions: 1) epidote-biotite quartz monzonite, quartz diorite and granodiorite of the Jurassic Snowslide and Wragge Creek stocks which extend from the mouth of Wilson Creek west, across Slocan Lake; 2) biotite-hornblende quartz monzonite of the Mount Carpenter Stock located at the mouth of Carpenter Creek on its north side as one enters New Denver; 3) agerine-augite leucogranite and leucoquartz monzonite belonging to offshoots of the Jurassic (~180 Ma) Kuskanax Batholith located at the head of Wilson Creek; and 4) feldspar porphyry dikes, sills and plugs scattered throughout the area.

The Slocan succession reacted to deformation as a multilayer, forming long, straight- limbed open to closed folds having narrow hinges (chevron style). Fold trends are east- west with limb dips varying between 20 and 75 degrees; however, as one proceeds eastward, toward the Kootenay Arc fold belt, fold trends rotate into a northwest-southeast configuration in conformity with the Kootenay Arc trend.

6.2 Property Geology Stratigraphy The Property is underlain by an east-west trending, steeply north dipping homoclinal succession of carbonaceous mudstone and siltstone, and carbonaceous limestone intruded by thin (<20 cm) to relatively thick (>10m) homogeneous sill-like units of augite- or hornblende-porphyry, diabase, and hard, flinty pyrrhotite-bearing rock that may be fine sill material or, alternatively, altered (hornfels) country rock (Fig. 4).

Figure 4: Geological map of the Enigma Property showing a detailed distribution of lithofacies and location of measured stratigraphic sections.

16 Hence, Enigma is best mapped as two units: 1) uTr1, carbonaceous mudstone and associated lithologies lacking sills, and 2) uTr2, the economically important sill-rich succession, the focus of this report. The carbonaceous mudstones contain disseminated pyrite, interpreted to be authigenic, suggesting a restricted anoxic deposition setting (Fig. 5). Mudstone is interbedded with siltstone which occurs in thin to thick beds having sharp parallel boundaries and consistent along-strike thicknesses. Parallel laminations are evident on weathered surfaces; low-angle cross stratification may be present. The siltstone units are interpreted as distal laminates derived, perhaps, from sediment gravity flows.

Figure 5: Typical sooty, carbonaceous mudstone with euhedral pyrite crystals. The pyrite is interpreted as authigenic; pressure shadows filled with fibrous quartz adjacent to some cubes indicate crystal growth prior to deformation.

The sills consist of augite porphyry, lesser amounts of hornblende porphyry, and medium to dark grey diabase. Border phases may be aphanitic and flinty. These units are interpreted as sills rather than volcanic flows because volcanic textures were not observed. Contacts are sharp with no evidence of breccias, pillows, degassing structures,

Figure 6: Typical flaggy character of planar-bedded calcareous siltsone of the Upper Triassic Slocan Group on the Enigma Property.

Figure 7: Augite porphyry typical of sill textures encountered within the massive sulphide-bearing assemblage.

Figure 8: Hornblende-phyric sill present in the massive sulphide-bearing assemblage in stratigraphic section no. 2 (ref. Fig. 17a). or internal flow features. One feature they all have in common is pyrrhotite and pyrite with accessory chalcopyrite and sphalerite. Structure Large chevron folds account for the consistency of layer dips (long planar fold limbs, narrow tight hinges). A few mesoscopic scale examples were observed (Fig. 9); however fold amplitudes are regional scale. Some fold hinges can be inferred from dip reversals, these are interpreted as accessory to larger folds. Crumple zones, and low angle truncations were occasionally observed (Fig. 10) where space problems developed between incompetent and competent beds. Bedding dips cluster in the 60-80 degree range, consistent with the chevron model. It is noteworthy that folding occurred about an east-west axis which differs significantly from the north northwest structural trend that affects all rocks 10 km farther east where they define the curvilinear Kootenay Arc structural trend. The important regional implication of chevron folding is the potential for kilometer-scale repetition of economically important units.

Figure 9: Oblique view of asymmetric chevron anticline. Hammer is oriented along fold axial plane -- sense of vergence is to the right (south). This fold style is characterized by planar limbs and narrow hinges.

The massive sulphide-bearing map unit uTr2 which is vertical to steeply north-dipping, is overturned. This interpretation is based on two premises: 1) presumed younging of the stratigraphic succession southward towards the mouth of Wilson Creek where there is a significant thickness of younger Rossland volcanic rocks, and 2) overturned cross lamination truncations (Fig. 10). Neither premise is bullet proof but they are mutually supportive.

7.0 Deposit Type: Besshi

Pyrrhotite-pyrite-chalcopyrite-sphalerite massive sulphide lenses (Fig. 11) in mudstone breccia (Fig. 12) are known from at least two localities within a 70-300 m thick stratabound mineralized succession on the Property (ref geological map Fig. 4).

Disseminations, stringers and veinlets of pyrrhotite and pyrite with subordinate chalcopyrite and sphalerite are ubiquitous within the mineralized succession. Host

Figure 10: Inverted cross laminations illustrating the stoss side of a ripple truncated by overlying laminated sandstone. lithologies consist of mafic sills (augite porphyry; diabase), carbonaceous mudstone, mudstone breccia, siltstone and carbonaceous limestone (Figs. 13- ___).

Breccias consisting of aphanitic, flinty (sill) clasts in a mudstone matrix (Fig. 12) suggest intrusion of volatile-rich magma into semi-consolidated, saturated sediments proximal to the sea floor. The association: augite porphyry, breccia, and pyrrhotite- chalcopyrite-rich massive sulphide within a mineralized stratabound succession is consistent with Besshi- type massive sulphide deposits, a class of strata-bound deposit that occurs in thick sequences of clastic sedimentary rocks and intercalated mafic to intermediate volcanic rocks and (or) sills.

The Property Cu-Zn-Pb metal ratios mimic average compositions of Besshi-type massive sulphide deposits world wide: variable Cu/Zn with little or no Pb. Presence of Mn-rich spessartine garnet (coticule) is also characteristic of Besshi-type deposits as are sericite

Figure 11: part of massive sulphide lens, unknown width, within mudstone breccia host (ref. stratigraphic section no. 3 for location and details of setting)

Figure 12: Mudstone breccia consisting of flinty mudstone and sill clasts in a mudstone matrix.

Figure 13: Massive sulphide zone from stratigraphic cross section no. 2 illustrating its deeply weathered and fractured appearance. The zone is 8 m wide.

Figure 14: Massive sulphide layer 30 cm wide within zone illustrated in figure 13.

Figure 15: Deeply weathered and fractured massive sulphide zone with mineralized mudstone breccia showing fresh surfaces on samples of mineralized mudstone breccia extracted from shallow excavation. See figures 17a and 17b for details of stratigraphic position and relations. and (or) muscovite, epidote (after augite), mariposite (Ni-Cr mica), biotite, scorodite, and quartz-carbonate veining.

8.0 Mineralization Four mineralized zones are known on the Property, two of them have significant massive sulphide exposures. Each zone is represented by a measured stratigraphic section (ref. Fig. 4 for locations), illustrating the types and proportions of lithotypes in and near the zones of mineralization (Figs. 16 to 19). Three conclusions are apparent: 1) the presence of pyrrhotite presages the presence of sphalerite and chalcopyrite; 2) massive sulphide mineralization occurs within interlayered mudstone and sill, especially where the sill(s) are thickest and the proportion of sill to mudstone is greatest; and 3) mudstone breccia is an important host lithology.

Despite the significance of sills containing disseminations of pyrrhotite and pyrite, it’s the presence of mudstone breccia that appears most diagnostic of the massive sulphide

Figure 16: Stratigraphic cross section no. 1 measured along the lower west side of Wilson Creek (ref. Fig. 4 for location). Measured thicknesses from top are in meters and indicated on the right side of the representative column. The succession is interpreted to be overturned, in which case it decreases in age from north to south. Since the bedding is near vertical, the section is best viewed when laid on its side with the top on the left.

Figure 17a: Stratigraphic cross section no. 2 measured along the upper west side of Wilson Creek (ref. Fig. 4 for location). Measured thicknesses from top are in meters and indicated on the right side of the representative column. The massive sulphide zone is 8 m wide, from 470 m to 478 m.

Figure 17b: Detailed description of the 8 m wide massive sulphide zone depicted in figure 17a. Figures 13 to 15 are examples of lithologies occurring within this zone.

Figure 18: Stratigraphic cross section no. 3 measured along the upper east side of Wilson Creek (ref. Fig. 4 for location). Measured thicknesses from top are in meters and indicated on the right side of the representative column. Massive sulphide-bearing zone is 60 m thick from 343 m to 403 m; lenses of massive sulphide in mudstone breccia were collected from a 10 wide zone between 343m and 344m. The measured zone of mudstone breccia from 295m to 403 m is considered very prospective for massive sulphide lenses. Figures 11 and 12 illustrate massive sulphide and breccia textures.

Figure 19: Stratigraphic cross section no. 4 measured along the lower east side of Wilson Creek (ref. Fig. 4 for location). Measured thicknesses from top are in meters and indicated on the right side of the representative column.

lenses. The breccias consist of grey, flinty, angular to rounded fragments (grit to cobble size) of host mudstone and bleached sill set in a dark grey mudstone matrix. Occasionally, breccia fragments are replaced by sulphides. In section no. 2 (Figs. 17a and 17b), the 30 cm thick massive sulphide lens (Fig. 14) is contained within an 8 m thick zone of fractured, deeply oxidized and (or) bleached sill (Fig. 13) and mudstone breccia with replacement sulphide (Fig. 15). In section no. 3 (Fig. 18), at least 4 lenses of massive sulphide were observed within a 60 m thick succession of mudstone breccia (Figs. 11 and 12). Limited exposure precluded an accurate measurement of individual sulphide lenses; however, they appear significant. In sections no. 1 and no. 4 (Figs. 16 and 19), massive sulphide lenses were not observed; however, appropriate host lithologies were along with disseminated sulphides, as well as sulphide seams and stringers.

The dominant sulphide mineral species are: pyrite, pyrrhotite, sphalerite, chalcopyrite, and minor galena. The dominant alteration mineral species are: epidote, sericite, spessartine garnet, quartz-carbonate in veins, mariposite, and scorodite. Two samples with anomalous gold (Au) were sampled, one in section 3, the other in section 2.

The assemblage of prospective lithologies is 70 to 300 m thick and has a strike length of at least 4000 m – open at both ends (Fig. 4). Minimum depth of the mineralized zone is equal to the difference in elevation across the property, roughly 1000 m.

A subsurface phreatic explosion caused by hot sill material intruding wet, semi- consolidated sediment near the sea floor, might explain the association of sills with mudstone breccia containing clasts of sill material. The sills are viewed as a heat source capable of initiating and maintaining focused circulation of formational fluids and with them, the potential for deposition of Besshi-type massive sulphide lenses (Fig. 20).

Fig. 20: A schematic diagram illustrating a possible genetic relationship between sill intrusion, brecciation and mineralization. Mafic sills intrude semilithified (water saturated) mudstone near the seabed. The combination of heat and pore water creates phreatic-like reactions with water turning to vapor which escapes to the sea floor, and disrupting the mudstone on its way. Meanwhile, circulation of fluids created by the temperature differential between the heat source (sill complex) and the cool surrounding sediments, focuses fluid flow and with it the transport and deposition of sulphide minerals, either as replacements or as layers on the sea floor.

9.0 Exploration The property operator has conducted exploration on two fronts: 1) Prospecting supported by rock sample geochemistry, performed under contract by C. Kennedy, T. Kennedy, M. Kennedy and S. Kennedy (referred to herein as the Kennedy’s) all of Kimberly, B.C.; and 2) stratigraphic analysis and 3) geological mapping performed under contract by R. Thompson of RIT Minerals Corp.

Results from prospecting and rock geochemistry are provided in appendix 1 as tables of analytical results. Results of the stratigraphic analysis are provided as stratigraphic columns in figures 16 to 19; and results of geological mapping are presented in figure4.

The interpretations of these exploration initiatives have been presented in sections 1.0, 6.2, 7.0 and 8.0.

10.0 Sampling Method and Approach

All of the surface samples taken by the Kennedy’s from the Property are early-stage or reconnaissance geochemical exploration samples, intended to identify areas with anomalous precious and/or base metal grades and anomalous trace element geochemistry. Screened and panned concentrate samples were taken from sediments (alluvium) in tributary streams on either slope of Wilson Creek. Surface rock (grab) geochemical samples were collected from outcrops along road cuts that parallel both the west- and east-facing slopes of Wilson Creek. Each sample was provided a unique field number, UTM coordinates and a description of the sample material (Appendices 1 and 2).

All samples were securely handled. Sample material was placed in polyurethane bags, secured with tape and remained in the possession of the Kennedy’s prior to shipment to ACME Labs Ltd. in Vancouver, B.C together with a sample shipment form listing the sample numbers.

11.0 Sample Preparation, Analyses and Security

Rock samples, and panned concentrate samples from streams, were prepared at the Acme Analytical Laboratories Ltd (“Acme”) preparation lab in Vancouver, B.C. Rock samples were crushed to 70% passing a 2mm screen, and a 250 g split from the crushed sample was then pulverized to 85% passing a 75 micron screen. Panned concentrate samples received identical preparation. The samples were then fire assayed for gold (Group 3B, 30-gram sample), and analyzed by 35-element ICP-ES with four-acid digestion (Group 1E) at the ACME Vancouver analytical lab.

32 12.0 Data Verification

The surface samples from the Property are intended to identify areas with evidence of precious- and base-metal mineralization. Laboratory analytical certificates from Acme Labs were vetted by the author for unreasonable values caused by typographical errors, mistaken units, or corrupted data entries. Results were also checked against internal ACME standards for both accuracy and precision.

A phased geochemical exploration strategy for precious and base metals in southeastern British Columbia is used by Kootenay Gold Inc. to evaluate regions for possible mineralization. Once a target area has been defined using regional geoscience data bases available from provincial and government agencies, reconnaissance prospecting and rock (grab) sampling is undertaken to establish specific mineralized targets; once found, subsequent prospecting and rock sampling is done to better define the target supplemented by silt and (or) soil sample programs to help establish shape and size of the mineral target in areas where bedrock is not exposed. Hence, the target mineralized zones on the Property were sampled on two occasions, first on a reconnaissance basis and later on a more systematic basis. This sampling redundancy provides a check against spurious results.

The author was present at all sample sites during the 2008 sampling program and can vouch for the authenticity and credibility of the samples taken.

13.0 Mineral Processing and Metallurgical Testing To the best of the author’s knowledge, no metallurgical sampling or testing have been conducted on materials from the Property.

14.0 Mineral Resource and Mineral Reserve Estimates There are no Reserves or Resources on the Property either historically or as defined by NI 43-101 or conforming to CIMM standards.

33 15.0 Adjacent properties No evidence of third-party exploration was noted in the Wilson Creek area during the June 2008 property work, despite mineral tenures existing throughout the area; and there is no evidence of recent third-party exploration in the public record.

16.0 Other Relevant Data and Information There are no other relevant data or information of material significance to report.

17.0 Interpretation and Conclusions It is the author’s opinion this is a property of merit. Massive sulphide lenses outcropping at surface within a highly mineralized succession composed of lithologies typically associated with Besshi-type massive sulphide occurrences are strong reasons to redouble exploration efforts on the Property.

Breccias consisting of aphanitic, flinty (sill) clasts in a mudstone matrix suggest intrusion of magma into semi-consolidated, saturated sediments proximal to the sea floor were accompanied by phreatic-like subsurface eruptions. The association: augite porphyry, breccia, and pyrrhotite- chalcopyrite-rich massive sulphide within a mineralized stratabound succession is consistent with Besshi-type massive sulphide deposits, a class of strata-bound deposit that occurs in thick sequences of clastic sedimentary rocks and intercalated mafic to intermediate volcanic rocks and (or) sills.

Copper-Zn-Pb metal ratios mimic average compositions of Besshi-type massive sulphide deposits world wide (Slack, 1993): variable Cu/Zn with little or no Pb. Presence of Mn- rich spessartine garnet (coticule) is also characteristic of Besshi-type deposits. Sericite

34 and (or) muscovite, epidote (after augite), mariposite (Ni-Cr mica), biotite, scorodite, and quartz-carbonate veining are all consistent with this deposit class.

The combination of strike length, widths of mineralization, and massive sulphide exposed at surface, make Enigma a property of merit.

Access to Enigma is excellent via a network of forestry roads off Highway 6, 7km north of New Denver, BC. However, paucity of outcrop makes it difficult to assess the true potential of the property. To that end, systematic soil and vegetation geochemical sampling, geophysics, and in at least two cases, trenching across known massive sulphide-bearing outcrops seem appropriate follow-up strategies. The combination of near-by infrastructure, straight forward reliable access, and a structurally simple, steep- dipping planar target, make for excellent diamond drilling prospects.

18.0 Recommendations A two-phase follow-up exploration program is recommended, phase I to better define mineralized targets, and phase II to drill one or more showings to test for grade and tonnage.

Elements of phase I are the following: 1.0 Soil sampling on a grid of short, closely spaced lines oriented perpendicular to the zone of prospective lithologies outlined on figure 4. 2.0 Follow-up systematic prospecting of all exposures within the zone of interest.

35 3.0 Magnetic survey designed to outline any near surface (upper 500 m) pyrrhotite-rich massive sulphide bodies. 4.0 Trenching of the massive sulphide showings located on stratigraphic sections 2 and 3 (Figs. 17 and 18). Given that both showings are on good quality logging roads and that the host lithologies are steep dipping, this technique will provide a rapid, inexpensive and environmentally friendly approach to evaluating their shape and size.

If the results from the phase I program are encouraging, then a phase II drill program will be in order.

36 19.0 References

Danielson, V., 1991, Geddes more than doubles reserves at Windy Craggy: The Northern Miner, v. 77(39), Dec. 2, 1991, p. 1-2.

Downing, B.W., Webster, M.P. and Beckett, R.J., 1990, The Windy Craggy massive- sulphide deposit, northwestern British Columbia, Canada, in Abbott, J.G. and Turner, R.J.W., eds., Mineral Deposits of the Northern Canadian Cordillera, Yukon-Northeastern British Columbia: 8th IAGOD Symposium , Field Trip Guidebook 14, Geological Survey of Canada, Open File 2169, p. 25-30.

Gammon , J.B. and Chandler, T.E., 1986, Exploration of the Windy Craggy massive sulphide deposit, British Columbia, Canada, in Nesbitt, R.W. and Nichol, I. eds., Geology in the Real World – The Kingsley Dunham Volume: Institution of Mining and Metallurgy, p. 131-141.

Hoy, T. and Dunne, K.P.E., 1997, Early Jurassic Rossland Group, southern British Columbia: B.C. Ministry of Energy, Mines and Petroleum Resources, Bulletin 102, 124p.

Hyndman, D.W., 1968, Petrology and structure of Nakusp map area, British Columbia: Geological Survey of Canada Bulletin No. 161.

Mortimer, N., 1987, The Nicola Group: Late Triassic and Early Jurassic subduction- related volcanism in British Columbia: Canadian Journal of Earth Sciences, v. 24, p. 2521-2536.

Peter, J.M. and Scott, S.D., 1990, Mineralogy and Geochemistry of the Windy Craggy copper-cobalt-gold massive sulphide deposit, northwestern British Columbia, Canada in Abbott, J.G. and Turner, R.J.W., eds., Mineral Deposits of the Northern Canadian Cordillera, Yukon-Northeastern British Columbia: 8th IAGOD Symposium , Field Trip Guidebook 14, Geological Survey of Canada, Open File 2169, p. 31-67.

Read, P.B. and Wheeler, J.O., 1976, Geology of the Lardeau west half map-area, British Columbia: Geological Survey of Canada, Open File 432, 150,000.

Slack, J.F., 1993, Descriptive and grade-tonnage models for Besshi-type massive sulphide deposits, in Kirkham, R.V., and Sinclair, W.D., Thorpe, R.I. and Duke, J.M., eds., Mineral Deposit Modeling: Geological Association of Canada, Special paper 40, p. 343-371.

Thompson, R.I., Glombick, P., Erdmer, P., Heaman, L.M., Lemieux, Y. and Daughtry, K.L., 2006, Evolution of the ancestral Pacific margin, southern Canadian Cordillera: Insights from new geological maps, in Colpron, M. and Nelson, J.L., eds., Paleozoic Evolution and Metallongeny of Pericratonic Terranes at the Ancient Pacific Margin of North America, Canadian and Alaskan Cordillera: Geological Association of Canada, Special Paper 45, p. 433-482.

Thompson, R.I. (compiler), in press, Geology, Nakusp, British Columbia: Geological Survey of Canada, Open file 4389, 1:50,000.

Unterschutz, J.L.E., 2002, Geological and geochemical links between Quesnel “terrane” strata and ancestral North America, southern Canadian Cordillera: M.Sc. Thesis, University of Alberta, Edmonton, Alberta, 139 p.

20.0 Statement of Costs

Personnel: R. Thompson 7 days @ $800/d $ 5,600 S. Kennedy + truck 6 days @ $450/d $ 2,700 T. Kennedy 2 days @ $350/d $ 700 C. Kennedy 2 days @ $350/d $ 700

Field Expenses: Food and accommodation $ 1,350 Vehicle rental/expenses 7 days + km $ 3,000

Travel: $ 200

Analyses: $20 x 40 samples $ 800

Report preparation/filing $ 3,000

Drafting/GIS support/reproduction 16 hr @ $50/hr $ 800

$18,850

Management (15%) $ 2,738

TOTAL $21,678

39 21.0 Statement of Qualifications

I, Robert I. Thompson, do hereby certify that:

1) I attained the degree of Doctor of Philosophy (PhD) in geology from Queens University, Kingston, Ontario in 1972. 2) I have a Hon. B.Sc. in geology from Queens University, Kingston, Ontario (1968). 3) I am a registered member of the Association of Professional Engineers and Geoscientists of British Columbia (P.Eng. 1972). 4) I am a Fellow of the Geological Association of Canada. 5) I have worked as a geologist for a total of 36 years since my graduation from university, all of it in the Canadian Cordillera. 6) I have worked for the BC Geological Survey (1972-74) and the Geological Survey of Canada (1974- 2008). 7) I acted as a consultant to the Petroleum Department of the Bolivian Government (1990) under the auspices of PCIAC (Petro Canada International Aid Corp). 8) I have a thorough knowledge of the geology of southern British Columbia based on extensive field mapping. 9) I have authored numerous scholarly publications in peer-reviewed journals, and have published or am preparing to publish 32, 1:50,000 scale geological maps of Lardeau (NTS 82K) and Vernon (NTS: 82L) areas. 10) I was retained by Kootenay Gold Inc. to undertake geological mapping and evaluation of the Enigma Property. 11) I am the sole author of this report. 12) I am not aware of any material fact or material change with respect to the subject matter of this report, which is not reflected in this report. 13) I have no interest, direct or indirect, in the Enigma Property.

“signed and sealed” at North Saanich, B.C.

Robert I. Thompson, PhD, P.Eng RIT Minerals Corp 10915 Deep Cove Rd., North Saanich, B.C.

Dated at North Saanich, B.C. this 21st day of September, 2008 Reg. No. 115741 Association of Professional Engineers and Geoscientists of British Columbia

APPENDIX 1

LISTING OF ANALYTICAL RESULTS FOR SAMPLES TAKEN ON THE ENIGMA PROPERTY: SAMPLES ARE IDENTIFIED BY UNIQUE NUMBERS THAT ARE REFERENCED TO SPACTIAL COORDINATES PROVIDED AS UTMs in ZONE 11

41 DATA SOURCE SAMPLE_NUMBER YEAR METHOD ACME EASTING NORTHING PROPERTY DESCRIPTION Sample Type Au_PPB Mo_PPM Cu_PPM Pb_PPM KENNEDY DEN-001 2007 ICP-1D A704762 475798 5543000 Milky bull type quartz material with limonite, pyrite and galena with sericite - associated with aplitic granite DEN-1 Rock 46.6 14 18 1294 KENNEDY DEN-002 2007 ICP-1D A704762 475798 5543000 Quartz veins in quartzite unit with some limonite, pyrite and sericite alteration DEN-2 Rock <0.5 8 17 79 Milky bull type quartz material in quartzite interval with some limonite and pyrite with sericite alteration along margins -some feldspar in KENNEDY DEN-003 2007 ICP-1D A704762 475527 5542932 veins 70 degree orientation DEN-3 Rock 0.6 9 41 22 KENNEDY DEN-004 2007 ICP-1D A704762 475436 5542887 Limonite altered quartzite material with narrow milky quartz veinlets with pyrite, pyrrhotite and limonite (black and orange) DEN-4 Rock 0.8 23 8 154 KENNEDY EEH08-001 2008 ICP-1D VAN08006559 472407 5549124 Rossland Volcanic, Epidote, Pink/Purple garnet or Zns EEH08-01 Rock 4.8 2 149 4 KENNEDY EEH08-002 2008 ICP-1D VAN08006559 472426 5549122 Rossland Volcanic outcrop, Py, Po, Cu Py, Fracs/dissem, Calcite frac. EEH08-02 Rock 3.5 <1 1034 <3 KENNEDY EEH08-003 2008 ICP-1D VAN08006559 472443 5549148 qrtz breccia fracture zone 6", Py, Cu Py, Malachite. sericite EEH08-03 Rock 12 <1 740 <3 KENNEDY EEH08-004 2008 ICP-1D VAN08006559 472438 5549149 2 qrtz vein breccia possible, sulfide and rot EEH08-04 Rock 12.9 28 135 5 KENNEDY EEH08-005 2008 ICP-1D VAN08006559 472438 5549149 same as above with more argillic EEH08-05 Rock 19.2 27 205 13 KENNEDY EEH08-006 2008 ICP-1D VAN08006559 472434 5549156 qrtz float, carbonate vein, malachite, limonite, sulfide EEH08-06 Rock 9 4 4593 6 KENNEDY EEH08-007 2008 ICP-1D VAN08006559 472434 5549111 Rossland volcanic Znz, Py, Po EEH08-07 Rock 3.2 1 106 6 KENNEDY EEH08-008 2008 ICP-1D VAN08006559 472434 5549111 Rossland volcanic Znz, Py, Po EEH08-08 Rock 4.5 2 186 9 KENNEDY EN-001 2007 ICP-1D A705123 471620 5549873 Carbonate altered zone cutting dolomitic siltstone with pyrite and limonite in quartz carbonate veinlets EN-1 Rock 6.9 2 16 <3 KENNEDY EN-002 2007 ICP-1D A705123 471740 5549766 Pyrite and carbonate altered volcanic unit with some quartz calcite fractures with fine-grained pyrite EN-2 Rock 9.5 <1 114 5 KENNEDY EN-003 2007 ICP-1D A705123 470957 5550438 Quartz crystal vein breccia in dolomitic argillite unit with some limonite - 8 inches wide EN-3 Rock 18.6 1 36 8 KENNEDY EN-004 2007 ICP-1D A705123 471024 5550269 Creamy matrix carbonate pyrite stringer zone cutting volcanic unit EN-4 Rock 4.9 <1 75 <3 KENNEDY EN-005 2007 ICP-1D A705159 473654 5548817 Black argillite unit with pyrrhotite and pyrite rich zones with rare sphalerite -composite of interval EN-5 Rock 5.5 10 48 <3 KENNEDY EN-006 2007 ICP-1D A705159 473724 5548697 Crush zone in argillite volcanic sequence with pyrite stringers some creamy silicification EN-6 Rock 4.3 14 67 <3 Zone of sericitic greenish colloidal sediments within tuffaceous unit with fracture and disseminated sphalerite, and pyrite - composite of KENNEDY EN-007 2007 ICP-1D A705159 473739 5548651 material unit striking 100 degrees dip 55 degrees to N EN-7 Rock 1237.1 9 241 4 KENNEDY EN-008 2007 ICP-1D A705159 473836 5548540 1 foot wide calcite quartz crackle breccia zone with pyrite, chalcopyrite and sphalerite EN-8 Rock 4.1 19 81 <3 KENNEDY EN-009 2007 ICP-1D A705159 473836 5548540 N/S trending footwide quartz vein with some limonite and pyrite with clinozosite - dipping 80 degrees to E EN-9 Rock 4.3 <1 4 <3 KENNEDY EN-010 2007 ICP-1D A705159 473443 5547376 2-4 inch wide milky quartz vein with limonite, pyrite, carbonate within listwanite altered flow unit - 300 degree trend EN-10 Rock 1.7 <1 10 <3 KENNEDY EN-011 2007 ICP-1D A705468 1m wide composite of a pyrite rich argillite unit with tuffaceous inter-beds Rock 3.9 13 49 9 KENNEDY ENTK08-001 2008 ICP-1D VAN08006559 471750 5548500 Grasitic sheir, dolomite argalic 12" wide ENTK08-01 Rock 0.9 10 78 7 KENNEDY ESK08-001 2008 ICP-1D VAN08006559 472471 5549153 Hornfels bx between sills, Py/Po stringers, some Cpy, qtz veinlets ESK08-01 Rock 4.9 19 826 5 KENNEDY ESK08-002 2008 ICP-1D VAN08006559 Qtz vein cutting a sill, Cpy/Malachite along margin, sericite ESK08-02 Rock 13.7 <1 2253 4 KENNEDY ESK08-003 2008 ICP-1D VAN08006559 Micro-veined, carb rich sill bx with Cpy, sericite, Py, epidote ESK08-03 Rock 17.3 <1 1089 <3 KENNEDY ESK08-004 2008 ICP-1D VAN08006559 Fine grained sill/sed (hornfels) bx, epidote, Py/Po, Cpy ESK08-04 Rock 3.6 17 464 7 KENNEDY ESK08-005 2008 ICP-1D VAN08006559 Goethite rich slip, Mn, qtz, in a graphitic shear ESK08-05 Rock <0.5 9 661 18 KENNEDY ESK08-006 2008 ICP-1D VAN08006559 469920 5549330 Augite porphry sill, epidote, sericite, muscovite, Py, biotite, Po, carb, calcite ESK08-06 Rock 7.3 4 537 <3 KENNEDY ESK08-007 2008 ICP-1D VAN08006559 469939 5549377 Narro bx cutting alt sill, Po/Cpy, carb ESK08-07 Rock 13.1 15 512 12 KENNEDY ESK08-008 2008 ICP-1D VAN08006559 469939 5549377 Zone of semi-massive laminated sulphides, Py/Po/Cpy ESK08-08 Rock 3.3 3 931 <3 KENNEDY ESK08-009 2008 ICP-1D VAN08006559 469939 5549377 Py rich seams up to 1 cm wide, Cpy, in alt sill and hornfels material ESK08-09 Rock 24.7 5 173 3 KENNEDY ESK08-010 2008 ICP-1D VAN08006559 469939 5549377 30 cm wide bx, Cpy clasts, Py/Po, Pbs, carb, bedding parallel, polylithic ESK08-10 Rock 1488.9 1 454 436 KENNEDY ESK08-011 2008 ICP-1D VAN08006559 469939 5549377 Sulphide rich sill with bx material, fine Cpy, sulphide stringers ESK08-11 Rock 9.2 11 458 <3 KENNEDY ESK08-012 2008 ICP-1D VAN08006559 469945 5549387 Sulphide rich layers in sediments, between augite sills, minor carb spotting, ESK08-12 Rock 15.3 107 952 7 KENNEDY ESK08-013 2008 ICP-1D VAN08006559 473750 5548098 Over 2 meter wide zone of qtz veining/bx, in seds, Mn, goethite, py, carb ESK08-13 Rock <0.5 2 5 <3 KENNEDY ESK08-014 2008 ICP-1D VAN08006559 473781 5548583 Over 1 meter wide bx zone with barite?, rotted sulphides, poly lithic ESK08-14 Rock 2.4 23 110 7 KENNEDY ESK08-015 2008 ICP-1D VAN08006559 473775 5548586 Light grey hard unit at contact with augite sill, Po/ZnS,Cpy, Py/Po clots ESK08-15 Rock 1.3 12 112 6 KENNEDY ESK08-016 2008 ICP-1D VAN08006559 473753 5548623 Black muds with qtz veins and sulphide stringers, Py/Po/Cpy/ZnS ESK08-16 Rock 2.8 7 76 <3 KENNEDY ESK08-017 2008 ICP-1D VAN08006559 473724 5548746 Zone of mottled looking seds/hornfels along sill contact, py/AsPy ESK08-17 Rock 80 9 84 4 KENNEDY ESK08-018 2008 ICP-1D VAN08006559 473774 5548777 Alt seds with massive-laminations of Py ESK08-18 Rock 6.8 1 601 13 KENNEDY ESK08-019 2008 ICP-1D VAN08006559 473740 5548791 290 degree trending massive Po/Cpy lense 20 cm wide ESK08-19 Rock 7.4 18 1820 14 KENNEDY ESK08-020 2008 ICP-1D VAN08006559 473740 5548791 Semi-massive bedding parallel sulphides, Py/Cpy, sericite ESK08-20 Rock 1.7 2 1972 14 KENNEDY ESK08-021 2008 ICP-1D VAN08006559 473740 5548791 Semi-massive bedding parallel sulphides, Py/Cpy, sericite ESK08-21 Rock 4.1 4 1573 13 KENNEDY ESK08-022 2008 ICP-1D VAN08006559 473740 5548791 Semi-massive bedding parallel sulphides, Py/Cpy, sericite ESK08-22 Rock 1.3 <1 1127 13 KENNEDY ESK08-023 2008 ICP-1D VAN08006559 473740 5548791 Semi-massive bedding parallel sulphides, Py/Cpy, sericite ESK08-23 Rock 1.5 5 951 17 KENNEDY ESK08-024 2008 ICP-1D VAN08006559 473740 5548791 Same type of material as 19, parallel zone ESK08-24 Rock 7.1 3 2677 14 KENNEDY ESK08-025 2008 ICP-1D VAN08006559 473740 5548791 Semi-massive sulphide boulders, bx, qtz veins, Py/Cpy ESK08-25 Rock 6.1 1 1910 125 KENNEDY ESK08-026 2008 ICP-1D VAN08006559 473782 5548586 Qtz/carb veining perpendicular to bedding, Py/Cpy/Po ESK08-26 Rock 1.9 13 110 5 KENNEDY ESK08-027 2008 ICP-1D VAN08006559 472709 5549125 5 cm wide band with disseminated ZnS/Po ESK08-27 Rock 6.2 3 67 4 KENNEDY ESK08-028 2008 ICP-1D VAN08006559 472709 5549145 Colloidal white/blue fractures, with Cpy, Py, Po, malachite ESK08-28 Rock 4.9 36 269 <3 KENNEDY ESK08-029 2008 ICP-1D VAN08006559 472709 5549145 Same zone as last, massive py/Cpy fractures ESK08-29 Rock 0.8 8 574 4 KENNEDY ESK08-030 2008 ICP-1D VAN08006559 472709 5549145 Same zone as last, massive py/Cpy fractures ESK08-30 Rock 0.9 17 296 3 KENNEDY ESK08-031 2008 ICP-1D VAN08006559 472709 5549180 Same as above, less veining ESK08-31 Rock 51.3 <1 4166 <3 KENNEDY HIC-001 2007 ICP-1D A704737 475124 5548203 Weakly limonite altered dolo-siltstone with narrow milky bull type quartz veins with some limonite Rock <0.5 1 13 6 1 foot wide milky bull type quartz vein in quartzite interval with some limonite and pyrite - strike 325 degrees dip70 degrees to NE KENNEDY HIC-002 2007 ICP-1D A704737 474731 5548022 Rock 5.7 <1 9 <3 KENNEDY HIC-003 2007 ICP-1D A704737 474635 5547981 Quartz crystal breccia zone in argillic altered sediments with some limonite and pyrite in quartz - 90 degree strike dip to N Rock 72.4 1 5 3 KENNEDY HIC-004 2007 ICP-1D A704737 474507 5548478 6 inch wide milky bull type quartz vein with limonite and pyrite cutting volcanic unit - Rock 1.5 <1 3 <3 1m wide quartz carbonate breccia zone with an epithermal texture cutting dolomitic seds and volcanics some green chromium mica - KENNEDY HIC-005 2007 ICP-1D A704737 474428 5548874 Strike 90 degrees dip 50 degrees to S - sample is of quartz breccia material Rock 5.9 <1 19 <3 Same zone as Above -sample is of pyrite rich carbonate altered material with brilliant green chips and calcite quartz veinlets (epithermal KENNEDY HIC-006 2007 ICP-1D A704737 474428 5548874 looking) Rock 29.4 <1 91 4 Narrow quartz carbonate veinlets cutting volcanic flow unit with limonite and pyrite and brilliant green clasts/mica - strike 20 degrees dip KENNEDY HIC-007 2007 ICP-1D A704737 474553 5548976 60 degrees to E Rock 2 <1 16 4 6 inch wide quartz calcite breccia zone cutting volcanic and sedimentary package with some limonite and pyrite -110 degree strike dip 70 KENNEDY HIC-008 2007 ICP-1D A704737 474555 5548992 degrees to S Rock 18.6 <1 8 6 KENNEDY HIC-009 2007 ICP-1D A704737 474555 5548992 Parallel zone to above of similar material with rare limonite and pyrite Rock 18.6 1 6 <3 KENNEDY HIC-010 2007 ICP-1D A704737 474560 5549031 2 cm wide quartz calcite veinlets with fine-grained pyrite and sericite along margins Rock 3.6 <1 22 11 KENNEDY HIC-011 2007 ICP-1D A704737 474565 5549052 Narrow ribbon quartz shear with some carbonate and limonite/pyrite - 100 degree strike dip 75 degrees to N Rock 3.4 1 39 14 Series of narrow quartz carbonate veinlets with carbonate and pyrite in and along margins of veins - 0.5m wide zone 270 degree strike KENNEDY HIC-012 2007 ICP-1D A704737 474576 5549056 dip 70 degrees to S Rock 346.1 <1 28 5 KENNEDY HIC-013 2007 ICP-1D A704737 474587 5549077 Narrow quartz carbonate vein with limonite and pyrite in volcanic flow unit -strike 270 degrees dip 45 degrees to S Rock 1.5 1 40 <3 Composite of quartz carbonate veins cutting carbonate altered volcanic unit with some limonite and pyrite -320 degree strike dip 70 KENNEDY HIC-014 2007 ICP-1D A704737 474836 5549292 degrees to NE Rock 3.2 <1 3 3 KENNEDY HIC-015 2007 ICP-1D A704737 474836 5549292 6 inch wide vein parallel to above with rare limonite and pyrite in milky bull type quartz Rock <0.5 1 12 <3 KENNEDY MRT-001 2007 ICP-1D A704737 478268 5550722 Quartz stockwork zone in granite sill/dyke with sericite, limonite and pyrite in veinlets with rare galena and pyrrhotite Rock 8 <1 21 433 KENNEDY MRT-002 2007 ICP-1D A704737 478268 5550722 Same as above Rock 64.8 <1 7 65 KENNEDY MRT-003 2007 ICP-1D A704762 478268 5550722 Milky bull type quartz material in carbonate altered zone with rare pyrite and limonite - 300 degree trend Rock <0.5 <1 8 6 KENNEDY MRT-004 2007 ICP-1D A704762 479820 5548645 Ribbon textured quartz with some limonite and pyrite along black wispy ribbons and carbonate Rock <0.5 1 12 9 KENNEDY MRT-005 2007 ICP-1D A704762 479820 5548645 Quartz sub-crop of milky texture with limonite boxworks Rock 1 <1 44 11 KENNEDY MRT-006 2007 ICP-1D A704762 478133 5550275 Quartz stockwork zone in granitic body with disseminated limonite, sericite and pyrite Rock 6.4 <1 6 11 KENNEDY MRT-007 2007 ICP-1D A704762 477605 5551006 Extension of quartz stockwork zone in granitic sill (MRT-001,2) with limonite and pyrite sericite and carbonate Rock 9.2 <1 6 6 KENNEDY MRT-008 2007 ICP-1D A704762 478268 5550722 Same as above Rock 4.5 1 5 158 KENNEDY WIL-001 2006 ICP-1D A605992 449306 5564657 WILSON LK N/A Rock 1.8 <1 5 9 KENNEDY WIL-002 2006 ICP-1D A606328 450677 5564976 WILSON LK N/A Rock 37.5 <1 1 <3 KENNEDY WIL-003 2006 ICP-1D A606329 450677 5564976 WILSON LK N/A Rock 22.1 <1 2 <3 KENNEDY WIL-004 2006 ICP-1D A606330 450677 5564976 WILSON LK N/A Rock 3.1 <1 9 3 KENNEDY WIL-005 2006 ICP-1D A606331 450677 5564976 WILSON LK N/A Rock 57.7 <1 4 366 KENNEDY WIL-006 2006 ICP-1D A606332 450549 5565007 WILSON LK N/A Rock 28.4 <1 <1 23 KENNEDY WIL-007 2006 ICP-1D A606333 454459 5564302 WILSON LK N/A Rock 2.5 75 6 4 KENNEDY WIL-008 2006 ICP-1D A606334 454459 5564302 WILSON LK N/A Rock 0.6 21 <1 <3 KENNEDY WIL-009 2006 ICP-1D A606335 473302 5551365 WILSON LK N/A Rock <0.5 1 21 21 KENNEDY WIL-010 2006 ICP-1D A606336 472407 5554417 WILSON LK N/A WIL-10 Rock 0.8 1 2 16 KENNEDY WIL-011 2006 ICP-1D A607116 472407 5554417 WILSON LK N/A WIL-11 Rock 0.9 <1 2 26 KENNEDY WIL-012 2006 ICP-1D A607116 472157 5554659 WILSON LK N/A WIL-12 Rock <0.5 1 2 <3 KENNEDY WIL-013 2006 ICP1D A607116 472129 5554727 WILSON LK N/A WIL-13 Rock 1.2 1 2 2010 KENNEDY WIL-014 2006 ICP1D A607116 472129 5554727 WILSON LK N/A WIL-14 Rock 0.7 4 3 1972 KENNEDY WIL-015 2006 ICP1D A607116 472129 5554727 WILSON LK N/A WIL-15 Rock 1.9 33 4 1724 KENNEDY WIL-016 2006 ICP1D A607116 472129 5554727 WILSON LK N/A WIL-16 Rock 1.4 5 3 385 KENNEDY WIL-017 2006 ICP1D A607116 462672 5562678 WILSON LK N/A WIL-17 Rock <0.5 <1 3 15 KENNEDY WIL-025 2006 ICP1D A607116 452645 5565075 WILSON LK N/A WIL-25 Rock <0.5 1 2 20 KENNEDY WIL-026 2006 ICP1D A607116 452705 5565012 WILSON LK N/A WIL-26 Rock 6.9 <1 1 10 KENNEDY WIL-027 2006 ICP1D A607116 453960 5561791 WILSON LK N/A WIL-27 Rock <0.5 9 3 7 KENNEDY WIL-030 2007 ICP1D A607565 448695 WILSON LK N/A WIL-30 Rock 1.1 1 11 12 42

SAMPLE_NUMBER Zn_PPM Ag_PPM Ni_PPM Co_PPM Mn_PPM Fe_% As_PPM U_PPM Au_PPM Th_PPM Sr_PPM Cd_PPM Sb_PPM Bi_PPM V_PPM Ca_% P_% La_PPM Cr_PPM Mg_% Ba_PPM Ti_% B_PPM Al_% Na_% K_% W_PPM DEN-001 91 15.3 2 2 33 1.71 2 <8 <2 5 <0.5 <3 35 <1 0.02 0.002 <1 8 0.01 10 <0.01 <20 0.14 0.05 0.01 <2 DEN-002 43 0.9 10 4 369 1.79 2 <8 4 149 <0.5 <3 4 6 2.33 0.03 7 12 0.44 34 <0.01 <20 0.65 0.02 0.1 2 DEN-003 53 0.4 31 15 415 2.65 4 <8 5 132 0.5 <3 <3 5 1.89 0.04 4 9 0.52 47 <0.01 <20 0.49 0.01 0.16 <2 DEN-004 76 1.8 13 6 291 1.44 10 <8 3 89 0.6 <3 5 1 1.13 0.031 6 9 0.22 14 <0.01 <20 0.12 0.05 0.03 2 EEH08-001 983 0.5 52 27 804 5.43 6 <8 <2 <2 193 17.2 <3 <3 50 5.5 0.115 2 95 1.73 96 0.05 <10 1.62 0.01 0.19 <2 EEH08-002 104 1.4 34 25 752 5.53 8 <8 <2 <2 161 1.7 <3 3 211 3 0.145 4 68 2.83 32 0.07 <10 2.59 0.03 0.13 <2 EEH08-003 65 0.9 28 17 589 2.88 2 <8 <2 <2 652 1.3 <3 3 35 12.42 0.042 1 26 0.75 34 0.03 <10 0.93 <0.01 0.09 <2 EEH08-004 22 0.5 83 13 98 4.58 28 <8 <2 4 12 <0.5 <3 <3 401 0.22 0.077 5 102 1.25 40 0.05 <10 1.37 0.04 0.11 <2 EEH08-005 29 0.4 65 17 436 7.94 20 <8 <2 5 54 0.6 6 <3 407 0.3 0.303 15 94 1.28 164 0.11 <10 1.77 0.04 0.24 <2 EEH08-006 84 7.1 35 8 322 3.37 2 <8 <2 3 98 1.2 <3 <3 132 1.49 0.052 5 28 0.66 95 0.06 <10 0.97 0.03 0.19 2 EEH08-007 482 0.5 60 26 555 4.21 12 <8 <2 <2 151 6.1 <3 4 28 4.22 0.092 2 112 1.08 79 0.04 <10 0.97 <0.01 0.15 <2 EEH08-008 1253 1.3 96 40 810 7.01 35 <8 <2 <2 12 16 <3 3 134 0.43 0.13 4 306 3.87 76 0.08 <10 3.04 <0.01 0.15 <2 EN-001 34 0.3 31 6 1014 2.83 44 <8 <2 3 112 <0.5 <3 <3 17 4.11 0.201 11 19 0.2 271 <0.01 <20 0.42 0.01 0.19 <2 EN-002 38 0.5 30 21 1041 5.45 61 <8 <2 <2 392 <0.5 14 3 52 7.22 0.147 5 31 2.7 129 <0.01 <20 0.43 0.02 0.23 <2 EN-003 43 6 10 3 277 1.29 10 <8 <2 <2 10 <0.5 3 <3 6 0.05 0.014 1 9 0.11 97 <0.01 <20 0.31 <0.01 0.1 <2 EN-004 37 <0.3 33 18 1104 4.34 44 <8 <2 <2 521 <0.5 <3 <3 55 8.75 0.037 2 37 2.47 81 <0.01 <20 0.42 0.04 0.11 <2 EN-005 271 <0.3 31 14 111 2.57 2 <8 <2 3 28 3.9 <3 3 58 2.48 0.052 6 13 0.11 39 0.1 <20 1.87 0.06 0.07 <2 EN-006 412 0.5 44 12 129 2.68 <2 <8 <2 3 27 7.2 <3 4 148 1 0.078 9 27 0.29 114 0.15 <20 1.03 0.11 0.23 <2 EN-007 55 0.7 26 30 265 5.4 3 <8 <2 5 11 <0.5 <3 <3 94 0.22 0.072 9 31 0.95 111 0.1 <20 1.65 0.02 0.32 <2 EN-008 290 0.3 42 8 445 2.82 <2 <8 <2 3 128 5.1 <3 6 100 3.75 0.08 8 40 1.06 29 0.09 <20 1.44 0.12 0.05 <2 EN-009 9 0.3 2 <1 147 0.5 <2 <8 <2 <2 160 <0.5 <3 <3 11 1.99 0.003 <1 7 0.12 8 <0.01 47 0.31 <0.01 0.01 <2 EN-010 13 <0.3 18 5 623 2.24 35 <8 <2 <2 129 <0.5 <3 3 14 1.36 0.216 2 22 0.37 16 <0.01 <20 0.2 0.02 0.04 <2 EN-011 209 1 22 8 199 4.73 22 <8 2 43 2.7 6 <3 119 0.83 0.07 6 33 1.08 127 0.04 <20 1.44 0.03 0.16 <2 ENTK08-001 298 0.4 40 11 377 3.31 7 <8 <2 4 612 8.5 <3 <3 59 5.33 0.043 6 21 0.72 92 <0.01 <10 1.53 <0.01 0.15 <2 ESK08-001 88 1.8 57 19 479 5.95 8 <8 <2 5 9 1 <3 3 214 0.32 0.101 6 69 2.2 51 0.04 <10 2.32 0.02 0.15 2 ESK08-002 85 3 31 43 1374 4.97 11 <8 <2 <2 230 1.8 <3 5 104 3.04 0.132 6 48 1.75 37 0.06 <10 1.98 0.02 0.11 2 ESK08-003 94 1.7 31 22 680 5.52 <2 <8 <2 <2 79 1.6 <3 5 176 1.77 0.146 4 52 2.42 35 0.09 <10 2.36 0.03 0.11 <2 ESK08-004 83 0.7 62 20 113 3.1 2 <8 <2 3 16 1.1 <3 <3 78 0.59 0.089 5 16 0.29 101 0.1 <10 0.72 0.02 0.27 <2 ESK08-005 633 <0.3 19 <1 29 >40 15 <8 <2 2 1 7.6 <3 <3 727 <0.01 0.142 <1 103 <0.01 9 <0.01 <10 0.76 <0.01 <0.01 <2 ESK08-006 29 <0.3 40 30 391 4.73 <2 <8 <2 <2 84 0.6 <3 <3 74 3.05 0.119 3 145 1.66 16 0.06 <10 1.66 0.04 0.16 <2 ESK08-007 55 <0.3 71 56 914 13.89 2 <8 <2 <2 18 <0.5 <3 5 130 1.74 0.085 2 94 3.01 11 0.08 <10 3.13 0.01 0.02 <2 ESK08-008 52 <0.3 152 86 528 15.62 3 <8 <2 <2 17 0.6 <3 4 78 1.07 0.159 7 167 2.15 36 0.04 <10 2.59 <0.01 0.19 <2 ESK08-009 15 <0.3 23 17 190 7.31 7 <8 <2 4 15 <0.5 9 <3 45 0.25 0.08 5 24 0.72 38 0.1 <10 0.96 0.03 0.16 <2 ESK08-010 2295 3.1 43 28 1538 5.37 1840 <8 <2 <2 557 36.5 9 4 81 16.63 0.056 2 162 3.33 1 0.04 <10 2.43 <0.01 0.03 <2 ESK08-011 27 <0.3 95 65 339 6.86 <2 8 <2 <2 15 0.7 <3 <3 96 0.87 0.1 5 91 1.42 32 0.08 <10 1.76 0.05 0.12 <2 ESK08-012 47 0.5 322 63 225 6.29 13 <8 <2 <2 16 1.3 <3 <3 254 2.54 0.07 4 36 0.66 32 0.08 <10 2.23 <0.01 0.06 2 ESK08-013 8 <0.3 7 1 96 0.52 3 <8 <2 <2 5 <0.5 <3 <3 <1 0.04 0.014 2 12 <0.01 7 <0.01 <10 0.08 0.04 <0.01 <2 ESK08-014 250 1 40 10 272 3.3 3 <8 <2 3 14 9.5 <3 <3 115 0.34 0.07 5 44 1.14 95 0.17 <10 1.41 0.01 0.2 <2 ESK08-015 462 0.7 51 15 470 4.16 <2 <8 <2 <2 54 9.6 <3 <3 105 2.29 0.077 4 44 1.25 97 0.07 <10 1.53 0.02 0.21 <2 ESK08-016 225 0.4 26 12 157 3.02 2 <8 <2 2 13 3.6 <3 <3 83 0.47 0.061 5 24 0.46 41 0.08 <10 0.69 0.05 0.11 <2 ESK08-017 38 <0.3 31 78 170 2.04 4838 <8 <2 3 12 0.5 7 <3 84 0.68 0.056 5 35 0.46 63 0.05 <10 0.98 0.05 0.08 <2 ESK08-018 30 2.1 48 71 229 8.83 <2 <8 <2 <2 7 0.7 4 <3 76 0.53 0.08 3 14 1.2 16 0.1 <10 1.1 0.03 0.05 <2 ESK08-019 188 1.5 38 188 248 23.77 6 <8 <2 4 17 5.3 <3 5 45 1.16 0.061 2 14 0.39 31 0.06 <10 0.84 0.02 0.08 <2 ESK08-020 40 1.5 36 68 358 6.94 <2 <8 <2 4 17 1.6 <3 3 76 1.32 0.106 4 31 0.91 20 0.14 <10 1.6 0.03 0.05 3 ESK08-021 46 1.3 52 80 364 7.54 <2 <8 <2 4 23 1.1 <3 7 63 2.34 0.103 5 20 0.88 17 0.11 <10 2.38 0.05 0.05 2 ESK08-022 48 1.1 61 108 253 6.67 <2 <8 <2 4 16 1.4 <3 <3 66 1.28 0.118 35 22 0.45 20 0.08 <10 1.18 0.02 0.05 <2 ESK08-023 52 0.7 51 82 311 7.58 <2 <8 <2 2 18 1.6 <3 3 70 2.77 0.071 3 20 0.7 15 0.1 <10 2.27 0.03 0.04 <2 ESK08-024 268 2.1 102 133 363 10.38 <2 <8 <2 4 22 7 <3 4 72 1.41 0.071 3 17 0.82 20 0.11 <10 1.55 0.03 0.06 3 ESK08-025 48 5.4 20 87 320 6.55 13 <8 <2 3 11 1.8 <3 <3 103 0.72 0.065 3 32 1.37 21 0.08 <10 1.47 0.04 0.04 <2 ESK08-026 464 2.1 61 15 349 3.47 <2 <8 <2 4 24 9.2 <3 <3 140 0.89 0.086 5 62 1.11 79 0.13 <10 1.47 0.04 0.14 <2 ESK08-027 673 0.5 47 11 1371 3.35 <2 <8 <2 <2 302 12.5 <3 4 53 11.66 0.197 5 45 1.01 100 0.07 <10 1.14 0.02 0.15 <2 ESK08-028 68 1 114 13 509 3.57 13 <8 <2 5 164 1.5 <3 <3 193 4.06 0.104 13 51 1.89 54 0.1 <10 1.62 0.05 0.12 <2 ESK08-029 59 1.4 42 30 375 4.69 <2 <8 <2 5 46 1.4 <3 <3 119 1.92 0.409 13 36 1.13 148 0.07 <10 1.62 0.04 0.1 <2 ESK08-030 109 1.3 50 13 325 4.16 <2 12 <2 7 32 2.5 <3 <3 174 1.07 0.314 16 47 1.11 35 0.04 <10 1.26 0.03 0.15 <2 ESK08-031 348 9.6 19 11 766 3.43 <2 <8 <2 3 84 6.1 <3 <3 71 2.65 0.099 7 28 1.83 92 0.05 <10 1.55 0.02 0.09 <2 HIC-001 79 <0.3 10 5 195 3.11 <2 <8 3 22 <0.5 <3 <3 22 0.09 0.033 9 14 0.85 142 <0.01 <20 1.2 0.09 0.06 <2 HIC-002 3 <0.3 3 2 33 0.43 4 9 <2 3 <0.5 <3 <3 1 0.02 0.006 2 10 0.02 6 <0.01 <20 0.05 0.02 0.05 <2 HIC-003 19 <0.3 6 2 121 0.92 33 <8 <2 122 0.5 <3 <3 4 0.85 0.043 2 8 0.02 63 <0.01 <20 0.23 0.03 0.12 <2 HIC-004 30 <0.3 5 2 125 0.63 2 <8 <2 94 1.4 <3 <3 7 0.95 0.002 1 8 0.01 29 <0.01 <20 0.31 0.03 0.1 <2 HIC-005 21 0.3 18 7 339 1.64 36 <8 <2 234 <0.5 9 <3 10 2.76 0.031 1 26 0.59 45 <0.01 <20 0.19 0.02 0.11 <2 HIC-006 41 0.7 41 17 1199 4.99 122 <8 <2 830 1.2 28 4 47 11.31 0.081 3 115 4.03 139 <0.01 <20 0.5 0.04 0.29 <2 HIC-007 86 <0.3 38 19 699 4.56 105 <8 <2 1971 0.5 7 <3 43 7.27 0.712 46 17 1.84 108 <0.01 <20 1.14 0.02 0.27 <2 HIC-008 22 <0.3 10 6 414 1.5 298 <8 <2 54 <0.5 <3 <3 9 1.75 0.019 1 8 0.09 40 <0.01 <20 0.16 <0.01 0.09 <2 HIC-009 24 <0.3 9 6 292 1.51 107 <8 <2 17 <0.5 <3 <3 6 0.12 0.033 5 7 0.15 44 <0.01 <20 0.43 0.03 0.17 <2 HIC-010 31 <0.3 11 4 1588 3.56 41 <8 <2 1570 1.2 13 4 25 10.9 0.034 3 6 4.3 76 <0.01 <20 0.24 0.01 0.12 <2 HIC-011 60 <0.3 68 9 615 1.87 48 <8 2 161 0.7 8 <3 11 0.63 0.274 7 32 0.1 64 <0.01 <20 0.41 0.02 0.17 <2 HIC-012 52 <0.3 17 11 1443 4.63 2073 <8 <2 854 0.5 16 <3 40 8.98 0.107 3 10 2.46 78 <0.01 <20 0.48 0.03 0.24 <2 HIC-013 13 <0.3 15 5 877 3.32 16 12 <2 12 <0.5 12 <3 17 0.09 0.007 1 7 0.03 29 <0.01 <20 0.17 0.01 0.06 <2 HIC-014 32 <0.3 25 12 1409 3.49 48 <8 <2 280 <0.5 4 <3 26 4.59 0.096 5 24 1.09 31 <0.01 <20 0.45 0.11 0.1 <2 HIC-015 17 <0.3 19 11 1090 2.92 22 <8 <2 35 <0.5 4 <3 22 0.45 0.041 4 12 0.13 49 <0.01 <20 0.28 0.04 0.02 <2 MRT-001 65 1.1 5 4 107 1.36 27 <8 <2 2 9 <0.5 <3 5 1 0.03 0.006 10 11 0.01 41 <0.01 <20 0.13 0.05 0.07 <2 MRT-002 27 <0.3 1 2 69 1.81 49 <8 3 9 <0.5 <3 <3 1 0.01 0.007 17 7 <0.01 37 <0.01 <20 0.16 0.11 0.05 <2 MRT-003 6 <0.3 2 1 24 0.41 2 <8 <2 2 <0.5 <3 <3 1 0.01 0.001 <1 9 <0.01 6 <0.01 <20 0.03 0.01 0.01 <2 MRT-004 30 <0.3 13 3 529 1.82 3 <8 <2 56 0.6 <3 <3 9 1.04 0.005 <1 15 0.21 229 <0.01 <20 0.17 0.01 0.02 4 MRT-005 4 <0.3 4 2 43 1.11 10 <8 <2 1 <0.5 <3 <3 1 0.01 0.005 1 8 <0.01 6 <0.01 <20 0.06 0.01 0.01 <2 MRT-006 38 <0.3 1 1 129 0.78 8 <8 8 14 <0.5 <3 3 1 0.02 0.016 28 5 <0.01 12 <0.01 <20 0.15 0.1 0.02 <2 MRT-007 41 <0.3 1 1 292 1.09 21 <8 5 25 <0.5 <3 <3 1 0.16 0.015 24 3 0.01 25 <0.01 <20 0.14 0.09 0.03 <2 MRT-008 405 0.3 1 4 673 1.03 21 <8 5 7 0.8 <3 3 1 0.01 0.009 7 6 <0.01 63 <0.01 <20 0.16 0.07 0.07 2 WIL-001 11 0.3 <1 <1 95 0.34 <2 <8 <2 25 84 <0.5 <3 <3 9 0.34 0.004 15 4 0.01 41 0.03 <3 0.23 0.09 0.2 <2 WIL-002 6 0.3 <1 3 50 0.29 <2 <8 <2 2 >10000 <0.5 <3 4 6 0.07 0.002 4 11 0.02 1763 0.01 3 0.86 0.01 0.07 <2 WIL-003 9 <0.3 <1 1 86 0.4 <2 <8 <2 2 1792 <0.5 <3 <3 9 0.07 0.001 6 14 0.03 271 0.01 <3 0.31 <0.01 0.11 <2 WIL-004 1 <0.3 1 1 61 0.34 3 <8 <2 2 81 <0.5 <3 <3 5 0.04 0.002 4 15 0.02 43 0.01 <3 0.12 0.03 0.06 <2 WIL-005 31 0.4 <1 <1 48 0.66 6 <8 <2 2 29 <0.5 <3 <3 6 0.03 0.004 6 6 0.03 70 0.01 9 0.3 0.03 0.13 <2 WIL-006 37 0.3 <1 2 87 0.69 3 <8 <2 3 2213 <0.5 <3 4 14 1 0.004 9 5 0.03 1124 0.03 <3 0.99 0.2 0.54 <2 WIL-007 16 2.9 <1 1 201 0.78 3 <8 <2 <2 382 <0.5 <3 <3 22 9.44 0.006 6 4 0.06 614 0.04 93 2.44 1.36 1.03 <2 WIL-008 7 0.7 <1 <1 60 0.52 3 <8 <2 <2 64 <0.5 <3 <3 10 0.28 0.007 3 11 0.03 49 0.02 <3 0.27 0.06 0.09 <2 WIL-009 16 0.4 7 6 285 1.49 8 <8 <2 <2 143 <0.5 <3 <3 5 1.64 0.038 2 10 0.7 31 <0.01 3 0.18 0.03 0.07 <2 WIL-010 36 <0.3 5 2 249 0.77 <2 <8 <2 <2 195 <0.5 <3 <3 4 0.44 0.009 2 6 0.05 324 <0.01 <3 0.16 0.05 0.07 <2 WIL-011 23 0.3 4 2 239 0.75 <2 <8 <2 <2 104 <0.5 <3 <3 2 0.05 0.007 1 5 0.03 528 <0.01 <3 0.13 0.05 0.06 <2 WIL-012 25 <0.3 4 1 24 0.86 2 <8 <2 <2 34 <0.5 <3 <3 1 0.01 0.007 <1 4 <0.01 86 <0.01 <3 0.13 0.07 0.03 <2 WIL-013 48 0.7 2 1 17 0.88 4 <8 <2 <2 1769 <0.5 <3 5 1 0.01 0.005 <1 3 <0.01 1445 <0.01 3 0.08 0.05 0.03 <2 WIL-014 110 0.6 4 1 10 1.76 3 <8 <2 <2 4437 <0.5 <3 4 1 0.03 0.005 <1 5 <0.01 486 <0.01 3 0.09 0.05 0.02 <2 WIL-015 118 0.8 12 2 50 1.32 9 <8 <2 <2 151 <0.5 <3 3 2 0.03 0.009 1 6 0.01 485 <0.01 3 0.11 0.04 0.05 <2 WIL-016 49 0.6 4 1 17 0.72 5 <8 <2 <2 41 <0.5 <3 <3 1 0.01 0.002 <1 20 <0.01 147 <0.01 <3 0.03 0.02 0.01 <2 WIL-017 15 <0.3 1 <1 173 0.46 2 <8 <2 17 298 <0.5 <3 3 5 0.89 0.004 8 6 0.02 84 0.01 <3 0.11 0.03 0.05 <2 WIL-025 41 <0.3 2 <1 184 0.68 <2 <8 <2 4 34 <0.5 <3 4 11 0.05 0.006 3 6 0.07 49 0.02 <3 0.27 0.05 0.08 <2 WIL-026 39 0.3 1 1 138 0.79 3 <8 <2 2 65 <0.5 <3 <3 18 0.4 0.006 5 8 0.06 95 0.03 <3 0.24 0.03 0.11 <2 WIL-027 17 <0.3 8 2 194 0.47 3 <8 <2 <2 659 <0.5 <3 <3 20 31.33 0.161 3 15 0.54 61 0.02 <3 0.16 <0.01 0.04 2 WIL-030 76 0.3 4 1 88 1.1 3 <8 <2 13 29 0.5 <3 <3 7 0.05 0.013 25 6 0.12 187 0.03 <3 0.34 0.05 0.16 <2

48 49 50

APPENDIX 2 GEOLOGICAL MAP SHOWING SAMPLE LOCATIONS AND NUMBERS (See attached file: KTN_Enigma_Geology-Sample Map.pdf)

51 469000 470000 471000 472000 473000 474000 475000

Legend

Upper Triassic SLOCAN GROUP

Interbedded carbonaceous mudstone and calcareous mudstone, carbonaceous limestone; sharp, planar contacts; u=1 dark grey; parallel laminated to low angle cross laminated, shale to flaggy with bedding parallel cleavage; E45 disseminated pyrite; quartz-carbonate veins; occasional porphyritic (augite) and non porphyritic fine crystallline sills E44 <0.5m thick.

Porphyritic (augite) and non-porphyritic sills (>50%) interlayered with carbonaceous mudstone; pyrrhotite and pyrite u=2 ubiquitous as disseminations, blebs and fracture fillings; chalcopyrite and sphalerite as disseminations and in veinlets; sill margins often flinty exhibiting pseudo-flow textures; significant thicknesses of medium to dark grey, hard to break, aphanitic, sill-like material – may be altered mudstone. E71

86 Breccia containing massive sulphide lenses. Darg grey, angular to rounded flinty, pale green clasts (sill) E69 u=2a and mudstone clasts in fine carbonaceous mudstone matrix. Some clasts replaced by sulphide. Lenses E46 of pyrrhotite-pyrite-chalcopyrite±sphalerite >0.3m thick; stringers of massive sulphide in quartz-

5550000 E70 5550000 86 carbonate alteration zones.

85 78 k Augite porphyry and non porphyry sills interlayered with <30% carbonaceous mudstone; tan weathering, u= 1 E68 u=2b medium grey; pyrrhotite and pyrite ubiquitous as disseminations, blebs and vein/fracture fillings; sill E47 borders may be flinty; quartz-carbonate veining common. 75 e 68 Geological contact: defined, approximate, assumed ......

e E48 Syncline ......

r Cross section ...... 77E59 u=2b E80 Bedding: inclined, overturned ...... E14 E43 C 70 Axial Plane......

85 E67 78 E17 Hinge ...... ESK08-007 (512) E81 ESK08-008 (931) 76 E71 E18 E72 E13 ESK08-009 (173) E79 Section #4 Outcrop (with station ID) ...... u=2a ESK08-010 (454) 70 Section #1 ESK08-001 (826) 561730 ESK08-011 (458) Lower East Side 68 561983 Lower West Side 78 ESK08-012 (952) E82 65 E42 Rock geochemistry sample (Cu values provided in brackets adjacent to sample numbers...... u=2 Wilson Creek ESK08-006 (537) E01 E41 E12 E78 65 E03 E02 E11 E77 E74 63 E40 ESK08-004 (464) u= ESK08-003 (1089) ESK08-031 (4166) 2b E06 ESK08-001 (826) E39 E10 65 ESK08-028 (269) u=2a ESK08-002 (2253) ESK08-029 (574) Section #2 E08 ESK08-030 (296) 80 E37 38 Upper West Side ESK08-027 (67) Section #3 E75 ESK08-005 (661) Wilson Creek E36 Upper East Side E09 E35 80 E73 E49 E27 88

5549000 E33 ESK08-019 (1820) 5549000 E50 ESK08-020 (1972) ESK08-021 (1573) E76 65 ESK08-022 (1127) u=2b ESK08-023 (951) E26 50 E60 ESK08-024 (2677) ESK08-025 (1910) E25 76 u=2a u=2 ESK08-018 (601) E24 ESK08-017 (84) E66 E32 E23 u=1 ESK08-016 (76) E22 62 E21 ESK08-014 (110) ESK08-026 (574) E19 E51 E31 ESK08-015 (112) 40 48 E61 E65 46 E52 E64 88 64 86 E57 E53 n

E63 82 561984 E54 51 o 70 E62 45 ESK08-013 (5) s E30 E29 E55 25

E58 80 l E29 E29 45 35 66 i 5548000 5548000 68

SouthernENIGMA British Columbia, Canada Prepared by RIT Minerals Corp. for Kootenay Gold Inc. E34 September 2008 UTM Zone 11 NAD83

0 125 250 500 750 1,000 Meters

1:10000

469000 470000 471000 472000 473000 474000 475000