Airphoto/Photogrammetric Interpretation Project, Tulameen Ultra-Mafic Complex, South-Central British Columbia, Canada

(INTERIM) SUMMARY REPORT:

Airphoto/Photogrammetric Interpretation Project, Tulameen Ultra-mafic Complex, South-Central British Columbia, Canada

Hidden Dragon Mineral Property

NTS 92H/046, 056 Lat. 49 29 51 N; Long. 120 53 27W 653,000 East; North 5,484,000 UTM zone 10 (NAD 83) Mineral Tenures 1010603-606, 1010858, 1010859, 1010849, 1011880, 1010871, 1011376, 1011369, 1013863, 1012421, 1012750, 1015805, 1915836, 1017786, 1017334, 1017342, 1021890, 1021892

and

Crouching Tiger Mineral Property NTS 92H/047 Lat. 49 26 23 N, Long. 120 48 7 W 653,000 East; North 5,484,000 UTM zone 10 (NAD 83) Mineral Tenures 1015953, 1015954

Similkameen Mining Division British Columbia, Canada

Authors: Bruce J. Perry, Ph.D., P. Geo. (ret.), FGAC (ret.), Box 294, Savona, B.C., V0K 2J0 Devin Tetz, Prospector, 1209 MacCleave Ave., Penticton, B. C. V2A 3E1

In support of Statement of Work Event #'s 5455980, 5457634, 5457635, 5457636, 5459787, 5483991, and 5484958

Date of Report: January 16, 2014

Table of Contents page

1.0 Scope of Work and Summary 1-2

2.0 Property Mineral Tenure 2

3.0 Location and access 4

4.0 Physiography and Climate 4

5.0 Regional Geology, Property Geology and Mineralization 6-8

6.0 Previous Explorations of the Property 8

7.0 2013 Reconnaissance Technical Program and Results 9-10

8.0 Conclusions and Recommendations 12

9.0 Bibliography 13

Statement of Costs 14 Statements of Qualifications 15

Figures:

Figure 1. Map: Property Location cover

Figure 2. Map: Mineral Tenures Location 3

Figure 3. Map: Regional Geology 5

Figure 4. Map: Property Geology 7

Appended

1. Photographs and descriptions of some examples of (raw) rock samples collected and being studied, primarily for structural geologic information. 17-19

2. Photographs and descriptions of some cut/polished sections of rock samples being studied, primarily for structural geologic information 20-21

Table 1. Subject Mineral Tenures 11 1.0 Scope and Summary

This report is an interim report, only, of some of the progress made to date within an on-going program of geological structural studies being made over a large area (approximately 120 sq. km.) and does not contain the final conclusions and recommendations to be derived from the results of the ultimate program, which are expected in mid-2014. This report describes results, mainly, of the fieldwork component of the program to date, and some of the considerations having resulted from the on-going airphoto/photogrammetric study, research, compilations and consultations. We are sharing the data with our associates of North American Mining Ltd. (NAM), Richmond, B.C. Hence, their mineral claims within the study areas are shown on the pertinent maps that comprise the figures included within this report.

The general area of the subject mineral tenures has been explored intermittently by various traditional and modern methods, historically during the past 150 years, more or less.

However, most of the earlier historic work is poorly documented and/or was conducted within areas that were during more recent times subjected to clear-cut logging which has virtually wiped out various survey grids, exploratory prospecting pits and trenches, workings of small- time historic mines/adits and previously existing landmarks and access trails/roads. Altogether these above-mentioned issues render most of the historic exploration results much less useful than they might otherwise have been to modern day mineral exploration within in this particular area.

More modern methods, such as airborne magnetic and vlf-EM surveys were applied in a generalized sense, especially the work of Bright Star Ventures (Yeomans, 2002, 2003, ARIS #'s 26,914; 27,040; and, 27,189), during the past decade or so, but in only a few instances were follow-up field explorations, such as grid based geophysical ground magnetic, vlf-EM and IP surveys, geochemical 'soil' sampling, property scale geological mapping and diamond drilling applied to specific, very much smaller targeted areas of specialized exploration interests.

An important component of technologically sophisticated, modern mineral exploration programs is the application of remote sensing and photogrammetric studies intended to elucidate geological features that may be favorable hosts for economic mineralization, but may not be apparent by means of conventional surface prospecting and surface geologic mapping because of being buried beneath overburden. Previous to this project, these important components of modern exploration have not yet been applied to the local area containing the subject mineral properties. The program as conducted during the Fall of 2013 consisted of compilation, research, property prospecting/reconnaissance expeditions, and consultations with various geologists and others who have prior familiarity with the property and/or the general area and/or the styles of mineralization known to occur within the mineral property and/or for which the property is thought to be favourably prospective, both before and after the expeditions and in conjunction with the on-going airphoto/photogrammetric studies.

The subject mineral property is favourably situated within the central zone of the Tulameen Ultra-mafic Complex, an area which hosts several important, known mineral deposits of magmatic genesis, e.g., Lodestone magnetite + PGE+Ti/V deposit ( 93 million tonnes, drill proven ) and the Magnetite Ridge area magnetite + PGE+Au+Ti/V deposits ( estimated at several hundred million tonnes, but not yet drill proven ) and some genetically later, structurally controlled mineralization events thought to be of hydro-thermal genesis, some of which host relatively large concentrations of Cu and/or Ag, Pb, Zn and/or Au, but are either small tonnage deposits or unproven 'showings', merely, at this point in time.

In conjunction with concomitant airphoto analyses and photogrammetric considerations, prospecting reconnaissance traverses were made in order to attempt to correlate and verify in the field the features detected by these technologically sophisticated means. Mere 'desktop' airphoto and/or photogrammetic studies are of very limited value to exploration planning unless they are investigated 'on the ground'. As a result of the initial and on-going research, airphoto and photogrammetric studies and companion field reconnaissance program, several areas were identified as being prospective or permissive in regard to structurally controlled mineralization, and/or lithological contact hosted mineralization, which are the types of mineralization that airphoto and photogrammetric analyses can be helpful in regards to explorations aimed at finding these types of mineralization. Large areas of the properties and of the general project area remain yet unexplored due to severe topography, access difficulties due to lack of roads, the 'decommissioning' and clear-cutting destruction of previously existing old roads and trails, and/or extensive overburden through which no bedrock is exposed at the surface. Continued exploration of this property is thought to be warranted by these authors and by all the geological professionals consulted regarding the mineral potential of this area.

2.0 Property Mineral Tenure

The current project is investigating the areas contained within the Hidden Dragon claim group, the Crouching Tiger claim group, and the Magnetite Ridge claim group, altogether encompassing approximately 1900 hectares (19 sq km). However, this cannot be done in isolation from the areas contained within neighbouring claims and the local unclaimed ground. Thus, the coverage of this project greatly exceeds the area of the claims listed in Table 1, and is on the order of 120 sq km. Most of the mineral tenures are adjacent or near to the Magnetite Ridge deposits.

3.0 Location, and Access

The project mineral property tenures are situated in the Cascade Mountain Range of South- Central British Columbia, mostly on or nearby Olivine Mountain ( Hidden Dragon claim group and NAM claim group) within the historic Tulameen mining camp located approximately 45 km northeast of Hope, B.C. and 25 km west of Princeton B.C. (Fig. 1 and Fig. 2). The Crouching Tiger claim group is situated in an area of favourable geology located approximately 10km SE of the other two claim groups and is not near Olivine Mtn. The nearest settlement is the small town of Tulameen, B. C., while Princeton, B. C., the closest significant municipality, offers access to most supplies and services, and is mining orientated.

The western portions of the property are most conveniently accessed from the Coquihalla Lakes Rd. exit #228 of the Coquihalla Highway and by travelling on the Tulameen Forest Service Road (FSR) 22.5 km to the Tulameen-Olivine FSR and thence 6 to 9 km further depending on which tenures are to be accessed by gravelled logging roads and/or trails to various portions of the project area. The southeastern portion of the project is accessed by a maze of older logging roads no longer maintained on a regular basis, if not officially de-commissioned, and as such present much difficulty to, or even preclude access by 4x4 pick-up truck travel. Portions of the project area contain extensive recent or historic clear-cuts and areas of 'blow down' which impede or preclude travel by ATV, and/or traverses by foot.

4.0 Physiography and Climate

The elevation of the project area ranges between 1100m and 1800m. Thus, the property area experiences a severe climate which can impede exploration during the period November through April. The local climate can result in winter temperatures of -40 C or less, and summer temperatures in excess of + 30 C, with an average of 100 mm of precipitation yearly, both as rain and snow.

Within the project area the maximum variation of topographical relief, locally, is approximately 400m - 500m, which occurs mostly within the western portion of the property as between Champion Creek and Olivine Mtn. Most of the surface area of the property, though, is of moderate relief, containing swampy areas, some small ponds and one small lake. Drainage is by small streams which flow to the Tulameen River, and thence to the Similkameen River and on into the USA in a southerly direction.

Although bedrock outcrops can be found within areas of high relief, generally outcrop within the project area is otherwise infrequent. Some small areas along newer logging roads, and especially along the refurbished Coalmont Energy coal mine haul road (formerly Champion Creek FSR and Tulameen FSR), contain bedrock road cut exposures. Much of the area has sustained clear cut logging, both historically and recently, and contains areas of blow down and/or thick bushy re-growth, both of which impede foot traverse and visual detection of outcrop.

5.0 Regional Geology, Property Geology and Mineralization

Regional Geology

The project area is located within the Tulameen Ultra-mafic Complex (TUC), an Alaskan-type ultramafic complex situated within southwestern Intermontane Tectonic Belt, regionally, at the intersection of the Quesnellia tectonographic terrane and the Mt. Lytton complex (Fig. 3).

Nixon and Rublee (1988), among others, have recommended that Alaskan-type ultramafic complexes, and especially the TUC, should be considered as potential hosts of economic deposits of Platinum Group Metals (PGM's). The project area is located on and around the Olivine Mt. area, mostly, which is a central section of the larger mafic to ultra-mafic complex which extends NNW for 20km from Arrastrada Creek to Grasshopper Mt. The outlying Crouching Tiger area is situated near the southern terminus of the complex.

The TUC is orientated, largely, parallel to its contact to the west with the Upper Triassic Nicola Group of intermediate to felsic volcanic and metasedimentary greenschist - amphibolite facies metamorphic rocks, except along its NW margin where it is bounded by later granitic rocks of the Eagle Plutonic Group. East of the TUC are Nicola volcanics and later Princeton Group metamorphosed volcanic and sedimentary rocks and Miocene basalt flows, which were occur unconformably there over the TUC and the Nicola volcanics.

Local Geology

The TUC is comprised of 'bands/zones' of ultra-mafic to mafic rocks arranged in a roughly concentric fashion ( Fig. 3b ) having the ultra-mafics as its the core as exposed by surface geological mapping ( Findlay, 1969). Locally, the subject project area is underlain by a vry wide range of rock types including the Nicola volcanics, dunite, hornblende clinopyroxenite, olivine pyroxenite, syeno-diorite, gabbro and the occasional narrow mafic dyke, sporadically. The most up to date and detailed description of local geology is contained within R. Whiteaker's report for Magnetite Ridge Metal and Minerals Ltd., 2009 (see references). In addition, the reader is referred to the report of W. (Bill) Yeomans, P.Geo., 2003, for Bright Star Ventures Ltd., who, along with Ron Wells, P. Geo., conducted the most comprehensive exploration of the area to date. The present program focuses mostly on structural geological studies as derived from airphoto interpretation and other photogrammetric interpretive techniques.

Local Structural Geology

The local and property structural geology is influenced to a great degree by large-scale regional tectonic events and by the later emplacements of the TUC and neighboring, later local plutons and stocks. The regional scale tectonic events produced NNW trending major faults having westward dipping foliation. Largely, these bound various lithologies and sub-lithologies and some are known to host metallic mineralization, none of which showings/prospects have yet to be proved to be potentially economic deposits. Of special interest to the present program are potential 'splays' emanating from these major structures, most particularly the situation wherein a major fault or splay traverses different lithologies of significantly different chemical composition, e.g., from felsic to ultra-mafic. This scenario provides the opportunity for hydrothermal fluids that may have collected metals from one lithology to later deposit them in a different lithology because of the negative influence the change in conduit wallrock chemistry may have on the solubility of metals that may be contained/dissolved within metal-bearing hydrothermal fluids.

Known splays and cross-structures tend to occur normal and sub-normal to large-scale structures, and can contain one type of mineralization the present program is targeting. An example of a recent, albeit unexpected discovery of splay-hosted, potentially significant epi- thermal style gold mineralization that has signature geochemistry conforming to hydro-thermal fluids originating in felsic lithologies was made during Magnetite Ridge Metals and Mineral Ltd. 2008 drilling approximately ½ km within the ultramafic ( Whiteaker, 2009).

6.0 Previous Explorations of the Properties

Historically, exploration in the general area was sporadic, and had not achieved any significant commercial production. Some significant discoveries of magnetite deposits have been made during 2001-2003, and are seemingly headed toward large-scale open-pit production of steel smelter feed and coal cleaning medium. Recently, Huldra Silver, situated not far outside of the project area, has brought it's structurally controlled high-grade silver deposit into commercial production, and Coalmont Energy has developed its coal deposit and has begun trucking its product to Port of Vancouver for sale abroad. Available records indicate that several hardrock mineral prospects occur within the subject project mineral property tenures ( Minfile #'s: 092H/SE 120 and 142; O92H/NE 097 and 209). However, by and large, and excepting Bright Star's explorations during 2001-2003 (see each reference to reports of Yeomans) and Magnetite Ridge Metals and Minerals Ltd. (Whiteaker, 2009), the records of previous work are either poorly documented and/or the data are of limited usefulness.

7.0 2013 Reconnaissance Prospecting Program and Results

The subject exploration program began during late June, 2013. The phase prior to the first field trip ( June 26, 2013 ) consisted of compilation of historic reports and data, compilation of air photos of the project area and various consultations with professionals and others who have geologic or other valuable knowledge regarding the project area.

Otherwise, and beginning at the date of the first field excursion, the program then, and throughout until the date of this report, has consisted of ongoing database/publications research and compilation, on-going consultations with geologists and workers associated with previous explorations of the property, on-going consultations with other geologists having specialized knowledge of the project area and/or the styles of mineralization known or anticipated within the subject mineral claims or known to exist within nearby mineral properties within the project area, on-going airphoto interpretation work including review of available information regarding overburden as presented on various government maps of such, field trips (see Statement of Costs for dates/personnel) to claims held by Perry/Tetz and/or to claims held by project participant NAM during which field excursions structural geologic reconnaissance observations were made and rock samples were collected, primarily for the purpose of structural geologic examination, not chemical analyses, although as at the date of this report some have been sent for chemical analyses regarding in particular Pt, Pd, Cu and Au, and report writing with respect to this "interim" report.

During the above-listed field trips as many of the various roads traversing the property were traveled as were practicable to access by pick-up trucks, and during one trip by ATV's (2), also. Special attention was given to the area through which the new Coalmont Energy mine haul road traverses (63 km), the construction of which up-graded road has provided many new exposures of bedrock at roadside, the data from which may contribute significantly to the program's consideration of local structural geology, and later, in relation to overall project exploration planning including trenching and drilling, also.

Large portions of the Coalmont Energy mine haul road were at those times still under construction and contained within the road bed much very sharp, large, fresh blast rock, which resulted in considerable damage to the 6-ply Cooper brand steel belted radial tires of our pick- up truck and the ATV's employed, including a complete blow-out of one tire on the Coquihalla Hwy not long after leaving this road during the second field trip.

Roadside outcrop was observed wherever it occurred along any road being traversed. Some sites of (historic) previous works located within the project area were visited. Often, excursions were made short distances into the bush both in order to scout for outcrop and to confirm

reports of structures (faults, shear zones, splays, etc.) noted on geologic maps produced by others, including government and non- government parties. Outcrop is non-frequent within many large areas of the project area. Rock samples for the purposes of later structural study, and in some cases chemical analyses, also, were collected (see appended photographs of rock sample examples).

The potentially most important result was the likely discovery of the surface expression of a gold-bearing shear zone known previously only as a drill intersection at a depth of 123m within the Magnetite Ridge deposit. At surface this shear may be represented by a swarm of quartz veins outcropping sporadically north of the subject MRMM drillhole collar and trending in a NNE direction (see photograph of sample 2013-01-R, appended). Chemical analyses have been sought in order to compare the geochemistry of this sample to the geochemistry of the gold- bearing intersection reported by Whiteaker, 2009,within his report for Magnetite Ridge Metals and Minerals Ltd.

Tenure Good to date Area (ha)

Hidden Dragon claim group 100% Perry/Tetz 1195 ha Total

1010849 20140702 20.97 1010858 20140702 20.95 1010871 20140702 20.97 1011369 20140702 62.94 1011376 20140702 83.92 1011880 20140702 20.97 1012421 20140702 83.91 1012750 20140702 20.97 1013863 20140702 20.97 1015805 20141231 20.97 1015836 20141231 104.88 1021890 20140827 20.97 1021892 20140827 20.98 1010603 20140701 20.99 1010604 20140701 41.99 1010605 20140701 62.98 1010606 20140701 20.99 1010859 20140701 20.98 1017334 20140301 104.92 1017342 20140301 209.91 1017785 20140314 20.98 1020625 20140629 125.90 1017786 20140314 41.98

Crouching Tiger Claim group 100% Perry/Tetz 189 ha Total 1015953 20151231 84.02 1015954 20151231 105.02

North American Mining claim group 100% NAM 545 ha Total 591162 20140837 419.76 842489 20140831 20.98 845885 20140831 104.91

Total area of mineral properties is approximately 1929 ha; total project area ~ approx. 20 sq km

Conclusions and Recommendations

This report described some of the aspects and some of the completed work regarding an on- going program that was launched during late June 2013, and which is focussed on obtaining clues as to the existence of geologic structures, some of which may host metal mineralization of interest to us, that are not apparent via conventional on the ground geologic mapping exercises and traditional prospecting techniques. Since this is all "in-house" work not intended as consultative type work for a client, no conclusions or recommendations as such are offered. The work and the results of it so far, except that which are presented herein, are tentative and proprietary.

Instead, the authors state that the results, so far, are certainly encouraging enough to have prompted us to commit to continue various 'desk top' components of the program during the rest of the winter and spring so that as soon as the field is again accessible a plan will be in place that designates specific, smaller target areas to be examined closely and quickly in the field and sampled/prioritized by soil geo-chemical methods, all preparatory to submitting as early as possible in the field season a Notice of Work regarding site-specific overburden trenching over several of the most select structural targets determined by this work, in order to uncover bedrock that may host potential overburden covered faults, fault splays and shear zones so that rock samples of the rocks of those potential faults, fault splays, and shear zones may be obtained and subjected to chemical analyses for the economic metals of interest to us and our project participant North American Mining Ltd. Pending encouragement via those results, additional trenching or even follow-up diamond drilling may be conducted before winter of 2014.

Bibliography

Camsell, Charles, 1913. Geology and Mineral Deposits of the Tulameen District, Geological Survey, Department of Mines, Ottawa, Memoir No. 26.

Findlay,D.C., 1969. Origin of the Tulameen Ultramafic Complex, Southern British Columbia. Canadian Journal of Earth Sciences, p. 399-425.

Nixon, G.T., 1987. Geology and Precious Metal Potential of Mafic-Ultramafic Rocks in British Columbia; Current Progress. B.C. Ministry of Energy Mines and Petroleum Resources, Geological Fieldwork 1989, Paper 1990-1, p.281-294.

Nixon, G.T. and Rublee, V.J., 1988. Alaskan Type Ultramafic Rocks in British Columbia: New Concepts of the Structure of the Tulameen Complex. B.C. Ministry of Energy Mines and Petroleum Resources, Geological Fieldwork, 1987, Paper 1988-1, p.281-294.

Nixon, G.T., 1988. Geology of the Tulameen Complex. B.C. Ministry of Energy Mines and Petroleum Resources, Open File 1988-25, 94 pp.

Rublee, V.J., 1994. Chemical Petrology, Mineralogy and Structure of the Tulameen Complex, Princeton Area, British Columbia; M.Sc. thesis, University of Ottawa, Ottawa, Ontario. 183 pp.

Yeomans, W., 2002. Summary of Results and Proposed PGE Exploration Program for the Tulameen Ultramafic Complex, Similkameen, District, South-Central British Columbia. ARIS #26,914

Yeomans, W., 2002. Summary of Results and Proposed PGE Exploration Program for the Tulameen Ultramafic Complex, Similkameen, District, South-Central British Columbia. ARIS #27,040

Yeomans, W., 2003. Technical Summary Report on the Results of the 2002 Exploration Program on the Tulameen Ultramafic Complex, Similkameen District, South Central British Columbia. ARIS# 27,189

Whiteaker, R.J., 2009. Assessment Report for 2008 Diamond Drilling and Bulk Sampling on the MRM 1 Claim - Magnetite Ridge Project, Olivine Mountain South-Central British Columbia, Canada. ARIS #31,256

Statement of Costs

Field work (person-days, all 2013) Bruce Perry, Ph. D., Geologist, Savona, B. C., July 3, 4, 5; and July26, 27; and Oct 4 6 days @ 700/day 4200 Devin Tetz, Prospector, Penticton, B.C. July 4; and July 26 2 days @ 250/day 500 Christopher Green, Fieldhand, Savona, B.C. Oct 04 1 day@ 200/day 200 Marley Greavley, Fieldhand, Penticton July 04 and July 26 2 days @ 200/day 400

Research, Compilation, Consultations and Report writing, including drafting B. Perry, Ph. D., Geologist, 2013: July 6, 28 and Oct 5 3 days@600/day 1800 2014: January 2 - 16 6.5 days@600/day 3900 D. Tetz, map compilations, drafting, report tables, 2013 various days 2.0 days @ 250/day 500 2014 Jan 2,3,4 and 14,15,16 4.5 days @ 250/day 1125 M. Jones, drafting, photography, tenure management 2014 Jan 07 - 16 4.5 days @250/day 1125

Expenses and supplies B. Perry, Ph.D., Geologist: 3 trips Savona-Tulameen area and return: July 3-5 [email protected]/km pick-up truck 247 July 26-27 [email protected]/km pick-up truck 260 Oct 4 [email protected]/km 244 4 trips Savona -Ashcroft and return 2014: Jan 7, 10, 13, 16 84kmx3= [email protected] 105 D. Tetz, Prospector: 2 trips Penticton-Tulameen area and return: July 4 [email protected]/km 130 July 26 [email protected]/km 130

TOTAL $14,866

Author's Qualifications - Perry

I, Bruce J. Perry, Ph.D., P. Geo (ret.), FGAC (ret.), residing at 6452 Ashcroft Rd., Savona, B. C., Canada, do hereby certify that:

1. I obtained B. Sc., M. Sc. and Ph. D. degrees in the Department of Geology, University of Toronto, in 1987, 1990, and 1994, respectively, specializing in Geology and Analytical Geochemistry.

2. I had been registered as a P. Geo. (#23613) in The Association of Professional Engineers and Geoscientists of BC, but am presently retired.

3. I was an elected Fellow of the Geological Association of Canada (Fellow #6569), but am presently retired.

4. I was certified as a BC Supervisor of Open-pit Mines and Surface Exploration (certificate 96- 2368) and as a BC Supervisor of Underground Mines (certificate 96-2367), but I have let these expire as am presently retired.

5. I have been engaged in commercial mineral exploration/mining activity since 1978, initially as a prospector and field assistant, and later I actively practiced my profession continuously during the period 1987 - 2004, having retired then to part-time activity, only.

6. I have prospecting and professional experience with regard to bedrock mineralization exploration for Platinum and Palladium, Gold, Copper, and Iron within geological settings similar to those as are described within this Assessment Report.

7. I have personal knowledge of the work described within this report, having done some of it myself, and having directly involved in the remainder.

8. I am an owner, along with Mr. Devin Tetz, of the tenures which are the subject of this report.

Dated at Savona, B.C., this 10th day of January, 2014

______Dr. Bruce J. Perry, Ph.D., P. Geo. (ret.), FGAC (ret.)

Author's Qualifications - Tetz

I, Devin Tetz, residing at 1209 MacCleave Ave., Penticton, B. C., Canada, do hereby certify that:

1) I am a licenced Prospector (B.C. Free Miner's Certificate #226021) having more than 5 years years continuous activity in this industry.

2) I have direct knowledge of this work as reported, having participated in all the phases of it.

3) I am an owner, along with Dr. Bruce J. Perry, of the tenures which are the subject of this report.

Dated at Penticton, B.C., this 10th day of January, 2014

______Devin Tetz, Prospector, FMC #226021

Appendix 1: Photographs and descriptions of some examples of (raw) rock samples collected and being studied during the present program, primarily for structural geologic information. The sample ID sequence is for the purposes of this report, only, and is not representative of the actual number of samples collected and/or being studied within this program.

2013-01-R Qtz vein material containing carbonate and metal sulphides, predominately pyrite, potentially representing the surface expression of a gold mineralized shear-zone previously discovered at depth of 123 m during 2008 diamond drilling program of Magnetite Ridge Metals and Minerals Ltd. (see Whiteaker, 2009, ARIS #31,256).

2013-02-R Hornblende pyroxenite, represents least deformed mafic sub-lithology as situated east of Champion Creek fault, which separates the Nicola volcanics from TUC Hornblende pyroxenite band that hosts the gold bearing shear above-mentioned (sample 2013-01; sample location is proximal and westerly of Magnetite Ridge deposit; weakly, but distinctly foliated.

2013-03-R Greenschist facies felsic to mafic intermediate metavolcanic having 'waffley' schistosity, representative of Nicola volcanic felsic rocks nearly immediately peripheral to fault contact separating western margin of TUC from the eastern margin of the Nicola volcanic litho- assembalage; abundant sericitization, cabonatization and minor sulphides, predominantly pyrite.

2013-04-R Slightly deformed felsic metavolcanic Nicola volcanic having sparsely developed schistosity and sparse structurally controlled development of mica; represents felsic portion of Nicola metavolcanic volcanics immediately peripheral to fault contact separating western margin of TUC and eastern margin of Nicola volcanic litho-assembalage, and which have responded to the deformation event(s) seemingly much less intensively than the intermingled intermediate volcanics, e.g. 2013-03, above.

2013-05-R Intensely sheared greenschist to amphibolite facies intermediate Nicola metavolcanic having intensely developed sericitization, representative of some portions of the Nicola metavolcanic volcanics that are situated immediately peripheral to fault contact separating western margin of TUC and eastern margin of Nicola volcanic lithologic assemblages.

Appendix 2: Photographs and descriptions of some cut/polished sections of rock samples being studied, primarily for structural geologic information. The sample ID sequence is for the purposes of this report, only, and is not representative of the actual number of samples collected and/or being studied within this program.

2013-01-CP Magnetite rich (> 35%) hornblende-clinopryoxene having minor ( micro ) structures bearing carbonate, and sparse but discreet carbonate veinlets; representative of largely unaltered non-deformed areas containing Magnetite Ridge magmatic magnetite deposit and sister/companion deposit situated < 1 km to the north.

2013-02-CP Coarse-grained hornblende-pyroxenite bearing significant (exploration context) concentrations of Pt ( > 200ppb), Pd (> 400ppb), Au ( > 55ppb) and Cu (~ 1%), and a distinct fracture pattern. Location representation not disclosed in this report.

2013-03-CP Ultramafic to syeno-gabbroic lithology bearing chalcopyrite (>2%), minor pyrite and chlorite all within micro quartz/carb structurally controlled veinlets; potentially representative of eastern margin of TUC in gradational 'contact' with less mafic phases of the TUC.