BC Geological Survey Assessment Report 30812

Assessment Report for the

CHAMPION Property

Kamloops Mining Division N.T.S. 83D/11E

Latitude: 51° 46' 40", Longitude: 118° 58' 30"

Submitted by:

Rick Walker 2601 - 42nd Ave South Cranbrook, BC V1C 7H3

and

Hunter Corrigal

Cranbrook, BC

Date: January 12th , 2009 i

SUMMARY

The Champion property consists of a single Mineral Tenure Online (MTO) mineral tenure comprising 157.01 ha. The property is located along the east side of the Albreda River, south of the community of Valemount and north of Blue River along the Yellowhead.

The claims are located on the west side of the Malton Range in the Monashee Mountains. Topography of the region is very rugged, characterized by very steep slopes and cliff faces, particularly on east facing exposures. The property, however, is located along the valley bottom and, while steep faces and rugged topography are present, is characterized by low to, locally, moderate relief.

“Four main rock units are recognized in the area. The most prominent are quartzite and quartz gneiss. These are interbedded with more recessive units of schist and hornblende gneiss. The thick sequences of quartzitic rocks were probably derived from quartz sandstones and the mafic-rich units from shales. Although on a broad scale these units appear to be laterally continuous, in the field individual outcrops can seldom be traced for more than a few hundred meters and often are exposed for less than ten meters. Units thicken and thin laterally and, schistose rocks and hornblende gneisses in particular, wedge out entirely over short distances in some outcrops.

All of these rocks have been highly metamorphosed and no evidence of original sedimentary structures was observed. The presence of kyanite and staurolite suggests a relatively high grade of metamorphism. Campbell (1968) shows the area to be within the staurolite-kyanite metamorphic zone” (Roed 1988).

The purpose of the 2008 limited prospecting program was to check road access, locate and access the powerline (specifically power pole 65-1 (locus of previously described mineralization) and, if possible, confirm the location of previous drill sites. ii

TABLE OF CONTENTS

Page Summary ...... i Table of Contents ...... ii List of Figures ...... iii List of Appendices ...... iii Introduction ...... 1 Location and Access ...... 6 Physiography and Climate ...... 6 Claim Status ...... 6 History ...... 7 Local Geology ...... 8 Property Geology ...... 10 2008 Program ...... 13 Results ...... 13 Discussion ...... 16 Conclusions ...... 17 Recommendations ...... 18 References ...... 19 iii

LIST OF FIGURES

Figure 1 - Location Map ...... 2 Figure 2 - Regional Location Map ...... 3 Figure 3 - Property Location Map ...... 4 Figure 4 - Detailed Location Map ...... 5 Figure 5 - Geology Map (taken from the MapPlace) ...... 9 Figure 6 - Prospecting Map ...... In Back Pocket Figure 7 - Photo along BC Hydro Power Transmission line ...... 14 Figure 8 - Photo along axis of slumped trench excavated in 1988 ...... 14 Figure 9 - Photo of representative piece of float from trench ...... 15

LIST OF APPENDICES

Appendix A - Statement of Qualifications Appendix B - Statement of Expenditures Appendix C - Program Related Documents 1

INTRODUCTION

REGIONAL LOCATION MAP

Scale: Date: Mapsheet: Approx. 1 : 8, 000, 000 January 2009 N.T.S. 82D / 11E BCGS: 082D 065 FIGURE 1

Drawn By: Rick Walker

Property Location DYNAMIC EXPLORATION LTD

PROPERTY LOCATION MAP

Scale: Date: Mapsheet: Approx. 1 : 3, 000, 000 January, 2009 N.T.S. 82D / 11E BCGS: 082D065 Property FIGURE 2 Location Drawn By: Rick Walker Figure 3: Property Location Map

Legend

0 3.5 7 km. Scale: 1:200,883 Map center: 52°42' N, 119°13' W This map is a user generated static output from an Internet mapping site and is for general reference only. Data layers that appear on this map may or may not be accurate, current, or otherwise reliable. THIS MAP IS NOT TO BE USED FOR NAVIGATION. Figure 4: Detailed Location Map

Legend

0 750 1500 m. Scale: 1:41,366 Map center: 52° 37' 29" N, 119° 7' 43" W This map is a user generated static output from an Internet mapping site and is for general reference only. Data layers that appear on this map may or may not be accurate, current, or otherwise reliable. THIS MAP IS NOT TO BE USED FOR NAVIGATION. 6

LOCATION AND ACCESS

The property is located along the east side of the Albreda River, south of the community of Valemount and north of Blue River along the Yellowhead Highway. The property is on the west side of the Malton Range at the northern termination of the Monashee Mountains (Fig. 1 and 2). The claims lie on NTS mapsheet 083D/11E at approximately 119° 07' 33" Longitude, 52° 37' 18" Latitude. Universal Transverse Mercator (UTM) coordinates are 356000 E, 5832500 N on TRIM map 083D065. The property consists of a single Mineral; Tenure Online mineral tenure, totaling 157.01 ha.

A number of service roads provide good access to and through the property from the Yellowhead Highway, approximately 30 km south of Valemount and 65 km north of Blue River. The service roads provide access to BC Hydro power poles along the power line right-of-way and a Ministry of Highways gravel pit.

PHYSIOGRAPHY AND CLIMATE

The claims are located on the west side of the Malton Range in the Monashee Mountains. The topography of the region is very rugged, characterized by very steep slopes and cliff faces, particularly on east facing exposures. Elevations within the proeprty range from 870 m (2,854 feet) along the Albreda River to 1,420 m (4,660 feet) at the northeastern margin of the property. Rock scarps and talus slopes are common throughout the area.

Snowfall in the area is heavy during the winter months, easily exceeding several metres in most years at high elevation. However the property is at lower elevations adjacent to the river. As a result, the field season available for exploration extends from early May to late October. Vegetation in the area consists predominantly of coniferous (cedar, spruce and fir) trees. Undergrowth is generally very thick, consisting of slide alder and Devil’s Club.

CLAIM STATUS

The Champion property consist of a single Mineral Tenure Online (MTO) mineral tenure (Fig. 3 - 5),consisting of 157.01 ha. Tenure information is summarized below:

Tenure # Claim Name Area (ha) Expiry Date* 567177 Champion 157.01 Oct. 27, 2012

* Upon acceptance of 2008 Assessment credits. 7

HISTORY

Very little work has been undertaken in the area since the Cariboo Gold Rush in the 1800's.

Roed (1987) reports a regional stream sediment sampling program was completed by Hudson’s Bay Minerals of Canada in the early 1970's directed toward identification of copper mineralization. Work was also completed for uranium in 1977 on the Lempriere carbonatite.

“In 1978 the Ingrid 1 to 4 (formerly W-M 1 to 4 ) 2 post claims were staked by Mr. Vagn Trarup of Kamloops, B.C., as a result of his discovery of a zone of malachite mineralization found while blasting holes for a new power transmission line. The discovery hole now has the B.C. Hydro pole 65-1 placed therein. The showing is located 165 meters above the Yellowhead Highway. After further prospecting, trenching, limited drilling and promotion of his property, Mr . Trarup brought the property to the attention of Redbird Gold Corp. Redbird optioned the Ingrid claims and along with Pundata Gold Corporation staked the Dove 1 to 6 claims. Subsequently Trio Gold Corp. staked the Expo 1, 2 and Cariboo 1 and 2 claims. During the summer of 1986 the Bluebird Syndicate staked the Bluebird 1 to 8 mineral claims. Early in 1987 Redbird Gold purchased Pundata's interest in the Dove 1 to 4 and Dove 6 claim blocks” (Roed 1987).

“The Kamloops district geologist for the B C Department of Mines and Petroleum Resources visited the showing and noted the presence of bornite in fractures in a 20 cm quartz vein hosted by amphibolite carrying disseminated malachite ... A quartzite unit underlying 17 m of amphibolite and schist overlain by 20 m of quartzite was observed.

In 1980 a Geologist from Dekalb Mining Corporation investigated the vicinity of the showing and noted the following sequence of flat lying to gently dipping metamorphosed sediments (from top to bottom): 1) more than 30 ft (9 m) of quartzite, 2) 10 ft (3 m) of hornblende-quartz-epidote paragneiss, 3) 10 ft (3 m) of biotite-sericite- quartz paragneiss, 4) 10 ft (3 m) of hornblende quartzite, and 5) greater than 30 ft (9 m) of quartzite ... Disseminated copper sulphide mineralization )malachite, bornite and chalcopyrite) was observed in units 2 and 3. In addition a hornblendite boulder outcrop with scattered specks of visible sulphide was observed about 1500 ft (455 m) east of the power line and at least 500 ft (152 m) stratigraphically above the showing ...

In October of 1986 a soil geochemistry sampling program was carried out on a 500 m2 grid focusing on the known mineral showing. The results of this program are the subject of a separate report ...

Although (it was) ...suggested that the mineralized rock at the showing may have been transported, (it has been) ... demonstrated that the mineralization occurred in bedrock outcropping at the site ...” (Roed 1988).

In 1987, Redbird Gold carried out a small exploration program consisting of soil sampling, magnetometer survey and diamond drilling. The 1986 grid was extended by cutting an additional 60 km of line, spaced at 100 m. A total of 1,018 soil samples were collected at 25 m stations from the “B” horizon and submitted to Kamloops Research and Assay Laboratories Ltd. for determination of gold and copper. 8

A 57 line km proton recession digital recording magnetometer survey was completed on the grid with readings taken every 25 m. A total of 7 drill holes, totaling 58 metres, were completed using a pack sack drill. Finally, a D-6 Cat was used to expose mineralized zones and were subsequently cleaned using an air compressor.

A total of 12 BQ sized diamond drill holes were also completed, totaling 225 m. Five of the holes were lost, while core recovery from the remaining holes were poor. Geologic mapping and prospecting were also completed as part of this program.

On the basis of this work two mineralized zones were outlined (upper and lower).

LOCAL GEOLOGY (taken from MINFILE 083D 045)

“The area is underlain by Upper Proterozoic rocks of the Malton Gneiss Complex. These comprise quartz mica schist, amphibolite, hornblende and/or biotite quartz-feldspathic gneiss, quartzite, granitic orthogneiss and feldspar augen gneiss. The rocks on the property are predominantly quartz mica schist, amphibolite and hornblende gneiss. All rock types contain numerous massive white quartz veins and stringers. There have been several folding episodes resulting in a fold with a west- northwest axis. The North Thompson Valley fault runs from Valemount to Blue River. The strata generally dips south-southwest but is variable.

The Dove occurrence consists of 2 vertically adjacent mineralized zones, containing gold and copper, and 2 mineralized stratiform units. The subsurface stratiform units are indicated by diamond drilling. Mineralization consists of native gold, malachite, bornite, and some hematite and chalcopyrite. Mineralization occurs along fractures and foliation surfaces and in quartz veins associated with biotite schist and hornblende gneiss.

A 70 metre exposure of the lower zone, about 3 metres wide, consists mainly of quartz veins, hornblende-quartz gneiss, quartz-biotite- muscovite gneiss and biotite schist. Assay values from samples ranged from 0.10 to 8.64 grams per tonne gold, 0.2 to 51.9 grams per tonne silver and less than 0.01 to 1.82 per cent copper (Assessment Report 17427).

A 20 metre exposure of the upper zone, about 4 to 5 metres wide, consists mainly of quartz veins, hornblende-biotite-quartz gneiss, mica schist and quartz-mica gneiss. Assays values from samples ranged from 0.18 to 7.45 grams per tonne gold, 0.1 to 60.5 grams per tonne silver, and 0.01 to 1.77 per cent copper (Assessment Report 17427).

In general, drilling indicated low grades even in some sections which contain visible native gold. The most encouraging values occurred along trend of slickenside lineations which suggests that the deposit is, to some extent, structurally controlled. Mineralization, proven by drilling, occurs over an areaof approximately 200 square metres.

Figure 5: Geology Map of Champion property and immediate area (approximate scale - 1:36,000, taken from The MapPlace) 10

PROPERTY GEOLOGY

The following has been taken from Roed (1988):

“... Four main rock units are recognized in the area. The most prominent are quartzite and quartz gneiss. These are interbedded with more recessive units of schist and hornblende gneiss. The thick sequences of quartzitic rocks were probably derived from quartz sandstones and the mafic-rich units from shales. Although on a broad scale these units appear to be laterally continuous, in the field individual outcrops can seldom be traced for more than a few hundred meters and often are exposed for less than ten meters. Units thicken and thin laterally and, schistose rocks and hornblende gneisses in particular, wedge out entirely over short distances in some outcrops.

Foliation planes are well developed in most units. Strikes and dips of foliation in schistose units are generally less uniform than gneissocity in quartzitic rock types. Generally lithologic units in the area dip south-southwest although locally some units dip dominantly to the south, southwest or west and rarely even to the east. Rock units in the south and west part of the map area generally have relatively steep dips compared to other areas. Superimposed on the regional structure are many small scale variations ranging from irregular changes along foliation planes to more uniform, small folds.

Due to this variability in the dip direction over short distances, larger scale structural features, if present, are nearly impossible to recognize. In addition, the predominant south-southwest dip of lithologic units may be due in part to downslope creep as evidenced by more gentle dips on large outcrops not as susceptible to creep, some southeastward dipping units in excavations and large fracture systems in the upper five to ten meters of the bedrock. These fractures were encountered in drilling and were responsible for poor core recovery and frequent binding of the drill stem. Fractures were also observed in outcrops and have widths up to several meters although generally they are less than one meter wide. The fractures generally parallel the major joint system in the area which trends within 15° of north-south (17 measurements ranging from 015° to 165°). Secondary joint systems have more variable trends, with the main clustering of measurements around 140° (12 measurements ranging from 120° to 158°) and minor clusters at approximately 90° 70° and 50°.

Slickenside surfaces, observed at widely separated localities, invariably dip to the west at angles of about 25° to 65°. In the vicinity of the showings a second slickenside surface dipping east southeast (105° to 120°) occurs in conjunction with the westerly dipping surfaces. The slickenside surfaces vary from planar to highly undulatory but overall they exhibit relatively consistent dip directions.

The most prominent lithologic unit in the area is a very hard, finely crystalline, white quartzite which forms steep cliffs. The unit commonly contains muscovite, and its fine grained equivalent sericite, which develop weak foliation planes. This foliation often gives the quartzite a flaggy or bedded appearance. The quartzite is vertically gradational in most outcrops with quartz gneiss, the most abundant rock type in the area. The gneissocity is developed mainly as the result of frequent micaceous layers, generally less than one centimeter thick, of muscovite, biotite and/or chlorite occurring between quartz rich bands which are usually one to ten centimeters thick. Augen structures, averaging about one centimeter in thickness and 10 to 20 cm in length, are common in the gneiss and consist of relatively pure quartz and sometimes potassium feldspar. Joints are 11 invariably chloritized. The gneiss is locally feldspathic and occasionally is rich in epidote. Plagioclase is a major component mineral of some biotite rich, quartz gneiss.

Exposures of mafic rich units are relatively rare compared to quartzitic units due to their more recessive nature. Biotite-muscovite-quartz schist is the most common, being gradational with quartz-biotite gneiss. Some mafic rich gneiss units also occur. They are generally dark grey to black in color, very hard and fine grained making the component mineral identification difficult. In contrast, hornblende-quartz gneiss and hornblende amphibolite are greenish black, much softer and generally very coarse grained with individual hornblende crystals commonly up to three centimeters long. Epidote rich beds commonly occur in hornblende gneiss units. Biotite and chlorite are common component minerals and, locally, garnets are present. Gold and copper bearing minerals are associated mainly with mafic rich rocks in the area, particularly hornblende-quartz gneiss and biotite schist.

The least common lithologic unit mapped in the area is a recessive, soft, reddish colored, muscovite- garnet-quartz schist. Kyanite, staurolite and biotite are locally present. This rock type was observed in only a few localities.

Quartz veins are common in the area and may be associated with rocks of any lithology. Most veins lie parallel or nearly parallel to foliation planes but occasionally they cross-cut lithologic units at steep angles. Veins are generally no more than one meter thick and ten meters wide. Coarsely crystalline potassium feldspar and mica crystals are sometimes present in the veins and give them a pegmatitic appearance

Mineralization

Two vertically adjacent mineralized zones were exposed during the course of this work, referred to here as the upper and lower zones. The original showing at the base of pole 65-1 is within the lower zone. North-south cross sections were excavated through both mineralized zones ...

Thick quartzitic units overlie and underlie the mineralized zones ... Strata at the top of the upper zone dip about 20° to the southwest (striking at 129°). The dip and strike of the lithologic units throughout the upper zone is relatively consistent and a quartzite at the top of the lower zone dips 23° southwest and strikes 118°. Foliation surfaces within the lower zone have more variable orientations. Generally there is a shift to more southerly and even southeasterly dips with increasing depth. Foliation planes within the flaggy quartzite at the base of the lower mineralized zone generally strike between 45° and 75°.

The most distinctive lithologic unit associated with gold and copper mineralization in the area is hornblende gneiss. Four separate exposures of hornblende gneiss occur in the immediate vicinity of the mineralized zones ... The two middle units are each associated with one of the two mineralized zones. A third exposure ... occurs stratigraphically below the mineralized zones but its upper contact was not observed. A fourth hornblende gneiss lies stratigraphically above the mineralized zones and its upper and lower contacts are not exposed. Consequently, it is not known if the four hornblende gneiss units are entirely distinct or if they are contiguous in places.

Small exposures of hornblende gneiss were also observed along the projected outcrop of the mineralized zones for approximately 250 m north and south ... of pole 65-1. No copper or gold mineralization was observed in either of these outcrops but scattered cobbles of schist containing malachite were encountered between about 100 m and 200 m north of pole 65-1. An additional 12 outcrop of hornblende gneiss was discovered approximately 375 m northeast of pole 65-1 ... Although no copper sulphides or gold was observed in the outcrop, a hornblende unit described ... (as) occurring about 455 m (1500 ft) east of the powerline, contained scattered specks of visible sulphide. These data suggest that the mineralized zones may be much more laterally extensive than exposed in the vicinity of pole 65-1 and that at least one other hornblende gneiss unit with potential sulphide and gold mineralization may occur upslope of the main showing.

A 70 m long exposure of the lower mineralized zone averages about 3 m in thickness ... The dominant mineralized unit is a wedge-shaped, hornblende-quartz gneiss that thickens to the south from zero to four meters over a horizontal distance of 35 m. This unit contains abundant malachite, particularly on slickenside surfaces and in epidote rich layers. Slickensides are very common and invariably trend to the west (250° to 293°) and plunge at angles varying from 25° to 65°. To the north, the lateral equivalent of the hornblende gneiss is dark colored quartz-biotite gneiss and biotite schist. Secondary mineralization is locally present in both of these rock types. The metamorphic foliation of the hornblende and quartz gneiss units is cross-cut by slickensided, westward dipping shear zones which are hard, greenish black, up to one centimeter thick and composed of very fine grained mafic rich minerals. Quartz-biotite-muscovite gneiss is the stratigraphically highest unit in the lower mineralized zone. The unit is locally dominated by unidentified, fine-grained minerals and generally contains less secondary mineralization than the underlying gneissic units.

Coarsely crystalline quartz veins are an obvious component of the lower mineralized zone and generally carry malachite, bornite, chalcocite, covellite and/or visible gold. The veins vary in size and shape from small sand lenses several centimeters long to beds 10 to 30 cm thick and up to 15 m long and lenses up to five meters wide and one meter thick,

The upper mineralized zone was exposed over 20 horizontal meters and averages about 5.5 m in thickness ... The zone is dominated by about four meters of hornblende gneiss with biotite, quartz and, in some beds, epidote. Malachite is abundant especially in the upper few meters. Westward dipping slickensided surfaces and shear zones are common and some eastward dipping surfaces are also present. A thin biotite schist unit with abundant malachite separates the upper part of the hornblende gneiss from a barren unit of quartz-biotite-muscovite gneiss to the north. The hornblende gneiss is overlain by about 1.5 m of interbedded biotite and muscovite schist and quartz and hornblende gneiss all of which exhibit malachite mineralization. Quartz lenses in these upper units are relatively rich in visible gold and copper sulphides and contain large potassium feldspar crystals. The largest lens is approximately two meters wide and 10 to 15 cm thick and cross-cuts the metamorphic foliation at a slight angle.

A striking feature of the mineralized zones is the association of sheared and slickensided surfaces with areas of relatively abundant gold and copper sulphide mineralization. Additionally the mineralization is associated primarily with mafic rich units such as hornblende gneiss and biotite schist and does not appear to be carried in the overlying and underlying quartzitic units. Shear zones and slickensided surfaces are also most common in these mafic rich units which are less competent and appear to have taken most of the movement during deformation. This is supported by the lateral discontinuity of the mafic rich units which thicken, thin and pinch out over short distances. The gold and copper mineralization thus appears to be associated with the deformation and is lithologically controlled mainly because of differences in unit competence. Hydrothermal solutions, possibly responsible for the secondary mineralization, may have moved up a zone of deformation associated with movement along the major fault in the valley bottom or some other episode of deformation.

Quartz veins were probably emplaced after the main lithologic units since they in places cross cut 13 metamorphic foliation planes and are locally pegmatitic. Mineralization probably post dates, at least in part, emplacement of the veins since veins in the adjacent strata are not mineralized. Mineralization is most pronounced along fractures in the veins as well as along shear zones and other planes of weakness such as foliation planes, thus suggesting that it was a late stage development.

Assay results indicate that the concentration of mineralization is variable ranging from less than 0.001 oz/ton to 0.938 oz/ton for gold, up to 2.9 oz/ton silver and up to 1.77% copper. The highest assays for gold are from quartz veins but some mica schist and epidote rich hornblende gneiss units also have significant yields ...” (Roed 1988).

2008 PROGRAM

The following is the prospecting log submitted by Hunter Corrigal, a partner in the property:

“I left for the claims on Wednesday, October 22. Drove to that access point along the highway. 950.4km one way. .... Thursday, October 23, I walked the road network covering the claims and took a number of pictures and GPS coordinates working out reference points on the map (Fig. 6).

Points included: Switchbacks, Power poles, (what I think was the mineralized zone (quartz vein trench)). Brought back a small representative sample of the quartz vein. I covered approximately 16 km of roads and observed very distinct changes in the areas geology. The terrain covering the claims is a combination of steep hill sides with narrow plateaus. Vegetation is relatively dense; a mix of clear cuts as new as a couple of years, to semi mature cut blocks to dense old growth cedar/spruce forests. There is an abundance of little tributaries with flowing water. Wild life signs are prevalent.

Access to the claims is simple via hwy 5. It takes approximately 15 minutes further to drive north to Valemont which has all necessary amenities for programs of varying involvement. The property itself is covered by many logging roads of varying quality. Debris, alder, washout are hazards you will encounter. Nothing to serious that will inhibit access by 4x4 truck”.

RESULTS

In addition, in the course of prospecting, an old trench was located. A representative sample of mineralization was taken at the probable location of sample VT-7.

There are moderately abundant bedrock exposures along the BC Hydro power transmission line (Fig. 7), exposed during construction of the powerline. Old roads indicated on the 1998 map of Roed are overgrown by second growth vegetation and are generally difficult to identify and/or located. No evidence could be found of the old grid and/or drill sites. 14

Figure 7 - Photo along the BC Hydro Power Transmission Line (above) and Figure 8 - Photo along the axis of the slumped trench with relatively abundant mineralized float along the bottom. 15

A trench approximately 20 m in length, 6 - 8 m wide and 2-3 m deep (at its deepest point) was located. The trench sides have slumped in and no bedrock was visible. However, a sample of the relatively abundant mineralized float along the bottom of the trench was recovered (Fig. 9 - above). 16

DISCUSSION

The following was taken from Roed (1988):

“Visible gold was positively identified in VT-2, 3, 5, and 6 but in all cases except VT-3, assays did not reflect the amount of gold suspected based on visual evidence, despite repeated assaying and screening of the samples.

Although the mineralization is commonly associated with fractures and quartz veins and appears more concentrated in mica schists and strongly developed lineation and slickenside zones associated with thickened hornblende units, mineralization has a distinct stratiform component. A combination of these features suggest that higher grade zones could occur in easterly trending linear culmination zones, and in hornblende and mica rich strata up and down dip as well as along strike. ...”

The results of preliminary metallurgical tests on two grab samples of malachite rich biotite schist and vein quartz with malachite, bornite and visible gold are ... summarized here.

Testing of the quartz sample confirmed the presence of free gold which could be concentrated into a gravity concentrate. An overall gold recovery of 84.4% was achieved following two flotation sequences with regrinding in between. The sample produced a jig concentrate assaying 179.05 OPT Au and 29.5 OPT Ag. Free gold was readily observable in the jig concentrate which recovered 33.4% of the gold. The total flotation concentrate assayed 11.3 OPT Au, 34.8 OPT Ag and recovered 42% of the gold, leaving 24.6 in the tailings.

The schist sample was tested using a similar procedure as for the quartz sample but the results were influenced by a much lower gold content (0.172 OPT Au in the schist vs 0.938 OPT Au in the quartz). The jig concentrate assayed 25.5 OPT Au, 4.7 OPT Ag and contained 15.5% of the gold. The total flotation concentrate assayed 6.24 OPT Au, 9.7 OPT Ag and approximately 4.5% Cu and recovered 56.5% of the gold, leaving 28% in the tailings. The overall gold recovery was only 78.3% for the schist sample.

Calculated head assay for the quartz is 0.938 OPT Au and 2.891 OPT Ag, and 0.172 OPT Au and 0.659 OPT Ag for the mica schist” (Roed 1988).

The recessive schists (mica and hornblende) were reported to have visible gold in drilling, which was subsequently confirmed in the metallurgical testing. Malachite staining was noted during prospecting and is evident in the sample recovered at the contact between a thin quartz vein and the host mica schist.

The limited program reported herein was intended to make a preliminary evaluation of the property, primarily in terms of access and evidence of previous work. 17

CONCLUSIONS

The property has seen several phases of previous work, many of which have documented the presence of mineralization. The metallurgical testing completed in 1988 suggests further work is justified in order to evaluate the potential for gold in the recessive units present on the property.

Mica schist and/or hornblende - quartz gneiss appear to be the primary lithologies of interest. Dependent upon the degree of chlorite development, the hornblende - quartz gneiss may be both resistant and recessive, whereas the mica schist is expected to be recessive. Visible gold was reportedly identified in the drill core recovered during the 1988 program, however, analytical results did not appear to confirm and/or were not consistent with the report of visible gold. This may reflect a “Nugget Effect” associated with coarse grained gold. Critical review of analytical procedures in co-operation with the lab may return more consistent results in future programs.

The purpose of the 2008 limited prospecting program was to check road access, locate and access the powerline (specifically power pole 65-1 - locus of previously described mineralization) and, if possible, confirm the location of previous drill site. The intent was to make an initial inventory of the infrastructure available on the property to utilize and/or rehabilitate in future programs. 18

RECOMMENDATIONS

1. Undertake geological mapping to confirm previous mapping, establish the presence and condition of existing roads and the location of the previous grid,

2. Re-habilitate the trench in an attempt to expose bedrock,

3. Take a suite of samples from any exposed bedrock in the excavated trench,

4. Confirm nature and character of mineralization at BC Hydro Transmission Pole 65-1,

5. Re-establish and re-sample Roed’s (1988) “upper” and “lower” mineralized zones,

6 Prospect for exposures of mineralized outcrop and obtain representative samples, and

7. Pan silt sediment samples from tributaries and watercourses throughout the property in an attempt to confirm the presence of gold and its size characteristics. 19

REFERENCES

Roed, M.A. 1988. Untitled, Assessment Report 17,427, dated January 10, 1988.

------. 1987. Soil Geochemistry of the Dove Group of Mineral Claims, Assessment Report 15,984, dated February 16, 1987. Appendix A

Statement of Qualifications STATEMENT OF QUALIFICATIONS

I, Richard T. Walker, of 2601 - 42nd Avenue South, Cranbrook, BC, hereby certify that:

1) I am a graduate of the University of Calgary of Calgary, Alberta, having obtained a Bachelors of Science in 1986.

2) I obtained a Masters of Geology at the University of Calgary of Calgary, Alberta in 1989.

3) I am a member of good standing with the Association of Professional Engineers and Geoscientists of the Province of British Columbia.

4) I am a consulting geologist with offices at 2601 - 42nd Ave South, Cranbrook, British Columbia.

5) I am the author of this report which is based on prospecting work completed by Hunter Corrigal between October 20 and 24, 2009 as owner of the claims.

Dated at Cranbrook, British Columbia this 12th day of January, 2009.

______

Richard T. Walker, P.Geo. STATEMENT OF QUALIFICATIONS

I, Hunter Corrigal, of PO BOX 454, Cranbrook BC, hereby certify that:

1) I am a graduate of the BCIT Prospectors Course. Obtaining my certificate in April of 2007,

2) I am a contractor for junior mining companies involved in field exploration work, and

3) I am a contributor to this report written by Rick Walker; based on field work completed by Hunter Corrigal between September 17 and 18, 2008 as a partner in the claims.

Dated at Cranbrook, British Columbia this 12th day of January, 2009. Appendix B

Statement of Expenditures STATEMENT OF EXPENDITURES

The following expenses were incurred on the CHAMPION property for the purpose of prospecting between October 22 - 24, 2008.

PERSONNEL H. Corrigal, prospector, 2 days @ $350 / day $ 700.00

EQUIPMENT RENTAL Food / Accommodation - 1 man-days at $100 / day $ 100.00 Hand-held GPS - 1 day at $15 / day $ 15.00 Vehicle, 3 days at $50 / day $ 150.00 - mileage - 1,900 km @ $0.60 / km $ 1,140.00 $ 1,405.00

FIELD SUPPLIES (Flagging, KRAFT bags, claim tags, etc.) 1 man-days @ $25 / day $ 25.00

DISBURSEMENTS Groceries $ 20.10 Fuel $ 126.06 Sub-Total $ 146.16

REPORT/REPRODUCTION R. T. Walker, P.Geo.: 2.0 days @ $500/day $ 1,000.00 Photocopying / Binding $ 50.00 $ 1,050.00

Total $ 3,326.16 Appendix C

Program Related Documents MINFILE Detail Report BC Geological Survey Ministry of Energy, Mines & Petroleum Resources

Location/Identification

MINFILE Number: 083D 045 Name(s): DOVE INGRID 1-4, DOVE 4, DOVE 1-6

Status: Showing Mining Division: Cariboo, Kamloops Electoral District: Kamloops-North Thompson Regions: British Columbia Forest District: Headwaters Forest District BCGS Map: 083D065 NTS Map: 083D11E UTM Zone: 11 (NAD 83) Latitude: 52 37 26 N Northing: 5832567 Longitude: 119 07 56 W Easting: 355674 Elevation: 1065 metres Location Accuracy: Within 500M Comments: Mineralized zones, near the centre of the Ingrid 1-4 Claims (Assessment Report 17427).

Mineral Occurrence

Commodities: Gold, Copper, Silver

Minerals Significant: Gold, Chalcopyrite, Bornite Associated: Quartz Alteration: Malachite, Hematite, Epidote Alteration Type: Oxidation Mineralization Age: Unknown

Deposit Character: Stratiform, Vein Classification: Syngenetic Dimension: 3x0x0 metres Comments: Dimensions of the lower zone. Host Rock Dominant Host Rock: Metamorphic

Stratigraphic Age Group Formation Igneous/Metamorphic/Other Hadrynian Horsethief Creek Undefined Formation ------Upper Proterozoic ------Unnamed/Unknown Informal

Isotopic Age Dating Method Material Dated ------

Lithology: Hornblende Quartz Gneiss, Quartz Biotite Muscovite Schist, Hornblende Biotite Quartz Gneiss, Mica Schist, Biotite Schist, Quartz Mica Schist, Gneiss, Schist, Amphibolite, Quartzite Comments: Metamorphic rocks of the Upper Proterozoic Malton Gneiss Complex. Geological Setting Tectonic Belt: Omineca Physiographic Area: Cariboo Mountains Terrane: Kootenay

Metamorphic Type: Regional Grade: Amphibolite Inventory

Ore Zone: LOWER Year: 1990 Category: Assay/analysis Report On: N NI 43-101: N

Sample Type: Grab

Commodity Grade Silver 51.9000 grams per tonne Gold 8.6400 grams per tonne Copper 1.8200 per cent Comments: Highest assay values from the lower zone. Reference: Assessment Report 17427.

Capsule Geology

The Dove showing is located on the Dove 4 claim, 165 metres above the Yellowhead highway (now covered by B.C. Hydro pole 67-1), 24 kilometres southeast of Valemount.

The North Thompson and Albreda River valleys have undergone little exploration since the Cariboo Gold Rush of the 1800s. In the early 1970s, a stream sediment sampling program was done in the area by Hudson's Bay Minerals exploring for copper. The area received some interest in 1977 during exploration of the nearby Lempierre (083D 005) uranium deposit. In 1978, the Ingrid 1-4 claims (formerly WM 1-4 claims) were staked by V. Trarup to cover malachite mineralization discovered while putting in the hydro line. Redbird optioned the Ingrid claims and staked the Dove 1-6 claims in about 1985 and, in 1986, conducted a geochemical survey. Prospecting in 1987 consisted of blasting and trenching a native gold showing, soil sampling on the Dove 3-4 and Ingrid 1-4 claims, geochemistry, 7 diamond drill holes, 7 pack sack holes, cat excavation of mineralized zones, mapping and a magnetometer survey. This work outlined two mineralized zones (upper and lower).

The area is underlain by Upper Proterozoic rocks of the Malton Gneiss Complex. These comprise quartz mica schist, amphibolite, hornblende and/or biotite quartz-feldspathic gneiss, quartzite, granitic orthogneiss and feldspar augen gneiss. The rocks on the property are predominantly quartz mica schist, amphibolite and hornblende gneiss. All rock types contain numerous massive white quartz veins and stringers. There have been several folding episodes resulting in a fold with a west-northwest axis. The North Thompson Valley fault runs from Valemount to Blue River. The strata generally dips south-southwest but is variable.

A 70 metre exposure of the lower zone, about 3 metres wide, consists mainly of quartz veins, hornblende-quartz gneiss, quartz-biotite- muscovite gneiss and biotite schist. Assay values from samples ranged from 0.10 to 8.64 grams per tonne gold 0.2 to 51.9 grams per tonne silver and less than 0.01 to 1.82 per cent copper (Assessment Report 17427).

Mineralization occurred relatively late and was associated with zones of deformation that apparently were confined mainly to less competent mafic rich units. Quartz veins, some mica schists and epidote rich layers in hornblende gneiss exhibit the highest degree of gold mineralization. Bibliography EMPR ASS RPT 7597, 12010, *15984, *17427 EMPR FAME FILE (1987, E-119) GSC MAP 15-1967; 1339A GSC OF 2324 GSC P 89-1E; 90-1E

Tuesday, April 21, 2009 MINFILE Number: 083D 045 Page 2 of 3 Placer Dome File Date Coded: 1985/07/24 Coded By: BC Geological Survey (BCGS) Field Check: N Date Revised: 1993/07/02 Revised By: Dorthe E. Jakobsen(DEJ) Field Check: N

Tuesday, April 21, 2009 MINFILE Number: 083D 045 Page 3 of 3 Parked Vehicle

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