Bill McKinney McKinney Property Event 5724829

Bill McKinney (Owner)

John Nick Bakus (Operator)

Geological & Prospecting Report (Event 5724829)

Work done on Tenures

1061485, 1061715, 1061735, 1064559

of the nine claim

McKinney Property

Greenwood Mining Division

BCGS Maps 082E.004/.041/.005/.015

Centre of Work

5,443,390N, 339,973E (Zone 11U NAD 83)

work done from November 17, 2018 to January 1, 2019

Author & Consultant

Laurence Sookochoff, PEng Sookochoff Consultants Inc.

Report Submitted June 4, 2019

Report Amended August 12, 2019

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TABLE OF CONTENTS page Summary ------4. Introduction ------5. Property Location and Description ------5. Accessibility, Climate, Local Resources, Infrastructure and Physiography ------6. Water and Power ------8. History: Camp McKinney Property Area ------10. 082ESW018 – FONTENOY ------10. 082ESW019 – WATERLOO ------10. 082ESW020 – CARIBOO-AMELIA ------11. 082ESW217 – WIARTON ------12. History: McKinney Property ------13. 082ESW043 – GOLD HILL ------13. 082ESW044 – EUREKA ------14. 082ESW045 – SAILOR ------14. 082ESW046 – MINNIE HA HA ------15. 082ESW128 – GOLD STANDARD ------15. 082ESW213 – ANARCHIST ------16. 082ESW214 – GRANITE ------16. 082ESW215 – KAMLOOPS ------16. 082ESW216 – BIG BUG ------17. 082ESW218 – PANDRE ------17. 082ESW220 – SLAMET ------17. 082ESW222 – ARGEN ------17. Geology: Camp McKinney Property Area ------18. 082ESW018 – FONTENOY ------18. 082ESW019 – WATERLOO ------18. 082ESW020 – CARIBOO-AMELIA ------20. 082ESW217 – WIARTON ------21. Geology: McKinney Property ------21. 082ESW043 – GOLD HILL ------21. 082ESW044 – EUREKA ------23. 082ESW045 – SAILOR ------23. 082ESW046 – MINNIE HA HA ------24. 082ESW128 – GOLD STANDARD ------24. 082ESW213 – ANARCHIST ------25. 082ESW214 – GRANITE ------25. 082ESW215 – KAMLOOPS ------25. 082ESW216 – BIG BUG ------26. 082ESW218 – PANDRE ------27. 082ESW220 – SLAMET ------27. 082ESW222 – ARGEN ------27. Mineralization: Camp McKinney Property Area ------29. 082ESW018 – FONTENOY ------29. 082ESW019 – WATERLOO ------29. 082ESW020 – CARIBOO-AMELIA ------29. Table of Contents (cont’d)

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Mineralization: McKinney Property ------30. 082ESW043 – GOLD HILL ------30. 082ESW044 – EUREKA ------30. 082ESW045 – SAILOR ------31. 082ESW046 – MINNIE HA HA ------31. 082ESW128 – GOLD STANDARD ------32. 082ESW213 – ANARCHIST ------32. 082ESW214 – GRANITE ------33. 082ESW215 – KAMLOOPS ------33. 082ESW216 – BIG BUG ------33. 082ESW218 – PANDRE ------33. 082ESW220 – SLAMET ------33. 082ESW222 – ARGEN ------33. 2018 Exploration Program: ------34. Interpretation, Conclusions, and Recommendations ------40. Selected References ------41. Statement of Costs ------42. Certificate ------43. Field Crew Qualifications ------44. TABLES Table 1. Tenures of the McKinney Property ------6. Table 2. Crown Grants of the McKinney Property ------6. Table 3. Assays of 10 Samples from the McKinney Property ------37. Table 4. Approximate Location of Cross-Structures ------38. ILLUSTRATIONS Figure 1. Location Map ------5. Figure 2. Location from Vancouver ------8. Figure 3. Location from Rock Creek ------9. Figure 4. Claim Map ------9. Figure 5. Claim Map showing Claims and Crown Grants ------10. Figure 6. Cariboo-Amelia workings ------12. Figure 7. Camp McKinney historic Crown Grants ------28. Figure 8. Property Geology ------28. Figure 9. Faulted end of the Cariboo vein ------30. Figure 10. The Minniehaha Mine at Camp McKinney ------32. Figure 11. Indicated cross-structures ------34. Figure 12. North Sample Locations ------35. Figure 13. Mid Sample Locations ------35. Figure 14. South Sample Locations ------36. Figure 15. East Sample Locations ------36. Figure 16. Indicated Lineaments ------38. Figure 17 Rose Diagram ------39. APPENDICES Appendix I Sample Assays Appendix II Sample Locations and Descriptions Appendix III Photos

Sookochoff Consultants Inc. August 12, 2019 Page 3 of 51 Bill McKinney McKinney Property Event 5724829 SUMMARY The nine claim McKinney Property (“Property”) is located within the historic Camp McKinney, 282 kilometres east of Vancouver, 22 kilometres east of Osoyoos, and nine kilometres north of Beaverdell, a settlement on the British Columbia No.3 Crowsnest Highway. The McKinney property is within the historic Camp McKinney Camp which centred on the Cariboo-Amelia mine to which occurrence has been the most significant mineral deposit and mineral producer from Camp McKinney. It was British Columbia's first dividend paying lode gold mine from which 2,538,101 grams of gold, 1,008,979 grams of silver, 51,393 kilograms of lead and 89,875 kilograms of zinc were recovered over its 68 year mine life from 1894 to 1962. The Cariboo-Amelia mineral deposit type is a gold-quartz vein, gold skarn, silica vein (Figure 9) hosted by a complex interlayered succession of metabasalt flows, tuffs and minor marble of the Anarchist Group which have been intruded by granite and granodiorite of the Middle Jurassic Nelson intrusions. The Cariboo/McKinney vein, mined over a strike length of 754 metres, and to a depth of 107 metres in the west section of the No. 4 level and 171 metres in the east sections of the Nos. 5 and 6 levels, has a total surface trace of 1,630 metres long on the Crown Grants and an additional 780 metres east and west. Widths vary from 0.25 up to 3.5 metres and is composed of white quartz and pyrite with lesser sphalerite, galena, chalcopyrite and rare tetrahedrite and pyrrhotite. Visible native gold is locally prominent. The Cariboo-Amelia, and two other past producers, are enclosed within the McKinney property (Figure 5) with the McKinney property covering two past producers. nine mineral prospects, and one mineral showing. The Gold Hill past producer on the McKinney property is a polymetallic vein Ag-Pb-Zn+/- Au type deposit with mineralization consisting of pyrite occurring in small bunches and along fractures in bluish quartz of similar character to the Cariboo-Amelia (Minfile). The shaft is sunk 15 to 18 metres deep on a 2.1-metre wide quartz vein striking 120 degrees and dipping 55 degrees southwest. On surface the vein is 1.8 metres wide and is traceable for over 305 metres. The McKinney property's potential for a mineral resource is not only indicated by the three inclusive former past productive properties, the Gold Hill, the Granite, and the Gold Standard, which are all Cariboo-Amelia type of a polymetallic vein and/or a gold quartz mineral deposit, but by the eight polymetallic and/or gold quartz mineral prospects, and one gold quartz mineral showing. However, the greater prospective resource potential of the McKinney property would be in a concealed porphyry, bulk tonnage mineral resource which is indicated by the polymetallic and the gold quartz veins which are commonly associated with a mineralized porphyry. Although there is no surficial indication of a porphyry on the Property, a surficial indication might be manifest at any one of the three delineated cross-structures which would be the location of the most facilitative feeder zone for the venting of hydrothermal fluids from depth and the creation of breccia pipes. The prospecting and sampling program was successful in the determination of three mineral indicative areas. The three areas include sample locations M-05, M-08, M-19, and M-25. Rock samples that were assayed from two of these locations showed anomalous copper and gold (M-8: 178.1 ppm Cu; 2.5 ppb Au), and anomalous molybdenum and copper (M-19: 17.5 Mo, 50.6 ppm Cu), would be the priority locations to explore.

Sookochoff Consultants Inc. August 12, 2019 Page 4 of 51 Bill McKinney McKinney Property Event 5724829 INTRODUCTION From November 17, 2018 to January 1, 2019, a structural analysis in addition to a prospecting and sampling program were completed on the McKinney Property ("Property"). The purpose of the structural analysis was to locate any cross-structures which may be surficial indicators of a potential concealed mineral resource. The purpose of the prospecting and sampling program was to prospect and take samples within any prospective mineralized zone in order to gather geological information for future exploration. Information for this report was obtained from sources as cited under Selected References and from information on the procedures and results on the prospecting and sampling program given the author. Figure 1. Location Map (Base Map from MapPlace)

PROPERTY LOCATION & DESCRIPTION Location The McKinney Property is located 282 kilometres east of Vancouver, 22 kilometres east of Osoyoos, and nine kilometres north of Bridesville within BCGS Maps 082.004/.014/.005/.015 of the Greenwood Mining Division. Description The McKinney Property is comprised of nine contiguous mineral claims covering an area of 1078.4834 hectares. Particulars are as follows:

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Table 1.Tenures of the McKinney Property

Tenure Number Type Claim Name Good Until Area (ha)

1061485 Mineral 20210801 42.2934

1061715 Mineral MCKINNEY CAMP BIG BUG 20210801 42.2968

1061730 Mineral GOLD HILL CARIBOO AMELIAS 20210801 253.8017

1061735 Mineral GOLD HILL CARIBOO AMELIA 20210801 359.4475

1062768 Mineral GOLD HILL STANDARD 20210801 63.446

1062770 Mineral GOLD HILL STANDARD 2 20210801 21.1465

1063271 Mineral GOLD HILL GRANITE BANNER 20210801 105.7444

1064558 Mineral CMCK 20210801 21.1488

1064559 Mineral EAST MCKINEY 20210801 169.1583

*Upon the approval of the assessment work filing Event Number 5724829.

ACCESSIBILITY, CLIMATE, LOCAL RESOURCES, INFRASTRUCTURE AND PHYSIOGRAPHY Access From Vancouver, Highway 1 is taken eastward to Hope, then Highway 3 to Osoyoos and to the Mt. Baldy road which is taken northward for nine kilometres to the Property. From Kamloops, Highway 97 is taken southward to West Highway 3 to the Mt. Baldy road which is taken northward for nine kilometres to the Property. Climate (from https://en.wikipedia.org/wiki/Beaverdell) has one of the highest diurnal temperature variations in Canada. In addition, this community has the highest diurnal temperature variation in Canada from June through September by means of the dry and sunny climate, valley bottom location, relatively high elevation, and the surrounding geography. Frost can occur even in the middle of Summer. The daily temperature swings during the winter are less varied thanks to the presence of valley cloud. Despite its proximity to Kelowna, Beaverdell receives about 25% more rain, due to orographic precipitation induced by its higher elevation within the Okanagan Highland. However, it receives less precipitation than Grand Forks, which is lower and has more desert like vegetation Local Resources There are many settlements, communities, towns, and/or cities in the area that can provide sufficient accommodation and supplies, for any preliminary exploration program. Nearest is the settlement of Bridesville located on the BC No. 3 / Crowsnest Highway, nine kilometres south of the Property.

Sookochoff Consultants Inc. August 12, 2019 Page 6 of 51 Bill McKinney McKinney Property Event 5724829 Accessibility, Climate, Local Resources, Infrastructure and Physiography (cont’d) Beaverdell (From Wikipedia, the free encyclopedia) Beaverdell is an unincorporated settlement in the Monashee Country of the Southern Interior of British Columbia, Canada, which lies to the east of the Okanagan Valley and north of the Boundary Country region. It is located midway along the West Kettle River between Kelowna and Rock Creek along British Columbia Highway 33. Beaverdell was originally named Beaverton, but when its post office was amalgamated with that of nearby Rendell, the names of the two locations were combined into Beaverdell. It is the namesake of the Beaverdell Range, which is on the settlement's east side and is the mountain spine lying between the West Kettle River and the Kettle River. The larger community of Rock Creek, located 15 kilometres east of Bridesville is described in Wikipedia as: Rock Creek From Wikipedia, the free encyclopedia

Rock Creek

The small community of Rock Creek & the bridge over its namesake creek in the middle of the image.

Rock Creek is an unincorporated settlement in the Boundary Country of the Southern Interior of British Columbia, Canada. Located at the confluence of the Kettle River with the eponymous Rock Creek, site of the Rock Creek Gold Rush of 1860, the community also lies at the junction of British Columbia Highway 33 (from Kelowna via Big White) and British Columbia Highway 3, otherwise known as the Crowsnest Highway, which runs across the south of the province. Rock Creek was one of the settlements along the Dewdney Trail in gold rush times and, though very small today, remains important as a regional service centre for the farming and mining communities of the Boundary Country and the Monashee Country, which lies northwards. It is the effective basetown for Mount Baldy Ski Area, which lies to its northwest and overlooks the Okanagan Valley town of Oliver.

Sookochoff Consultants Inc. August 12, 2019 Page 7 of 51 Bill McKinney McKinney Property Event 5724829 Accessibility, Climate, Local Resources, Infrastructure and Physiography (cont’d) Infrastructure Any mining operations that require housing for employees, communication, and transportation facilities are readily available within 30 kilometres of the Property. Cell phone communication is available from the Property. The Trail smelter, to which any hi-grade ore and/or concentrate can be shipped for processing, is located 165 kilometres east of Bridesville. Physiography The camp is at an elevation of 4,400 feet on the lower south-eastern slopes of Baldy Mountain that attains a summit relief, and rises only through the Edward VI1 claim in a long elevation of 7,558 feet. The local topography is one of low ridge to higher summits. Elsewhere low ridges and mounds, and long slopes are characteristic. The area mapped is rocky in part and slightly higher than ground to the south- west, south and east. Mounds and ridges of glacial drift are abundant in the district and some are present within the area; the region has been heavily glaciated and only the area immediately about Camp McKinney has escaped the prevailing general coverage by glacial debris (Hedley, 1940).

WATER AND POWER Rice Creek, a tributary of McKinney Creek, flows through the Property. A main transmission-line passes through the Property and could be the source of power required for any future mining operation. Figure 2. McKinney Property Location to Vancouver (Base Map from MapPlace & Google)

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Figure 3. McKinney Property Location from Rock Creek (Base Map from MapPlace & Google)

Figure 4. Claim Map (Base map from MapPlace)

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Figure 5. McKinney Property showing Claims and Crown Grants (Base map from MapPlace and Google Earth)

HISTORY: CAMP McKINNEY PROPERTY AREA Minfile reports on the history of past producers adjacent to the McKinney property area as follows. FONTENOY past producer (Au-quartz veins) Minfile 082ESW018 In CG enclosed by McKinney claims The approximate centre of the Fontenoy Crown Grant is located at 1265 metres elevation on the southern slopes of Baldy Mountain. The occurrence is part of the historic Camp McKinney, located 9 kilometres north-northwest of Bridesville, British Columbia. The Fontenoy group originally consisted of the following Crown and Reverted Crown-granted claims: Fontenoy (Lot 752), Vernon (Lot 759), Last Chance (Lot 751) and later included the Knight Rambler (Lot 3015) and Islander (Lot 1090). The Fontenoy occurrence was first discovered in 1893. At this time a 24.4-metre inclined shaft was developed which intersected the Fontenoy vein in 1895. The vein had a strike of 315 degrees and a dip of 45 to 55 degrees to the northeast, different from the Cariboo/McKinney vein and other veins in the McKinney camp. Surface trenching also uncovered the Fontenoy vein. By 1899, two shafts were developed; the No. 1, 36.6 metres deep with 54.9 metres of drifting and the No. 2, 19.8 metres deep with 5.5 metres of drifting. Free gold was reported associated with vein quartz (Minister of Mines Annual Report 1899, page 603). The vein was abandoned and then in 1929 dewatered but no further work was reported. In 1933, the property was amalgamated with the Cariboo-Amelia (082ESW020) by Cariboo-McKinney Gold Mines. No further work was reported until 1987. In 1987, Bravo Resources Inc. carried out an exploration program consisting of electromagnetic and magnetometer geophysical surveys and a soil geochemical survey. Numerous pits, trenches and shafts were encountered during their exploration program.

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History: Camp Mckinney Property Area (cont'd) WATERLOO past producer (Au-quartz veins) Minfile 082ESW019 In CG enclosed by McKinney claims The Waterloo occurrence is located at 1311 metres elevation on the southeastern slopes of Baldy Mountain, 750 metres east-southeast of the Cariboo-Amelia occurrence (082ESW020). The occurrence is part of the historic Camp McKinney, located 9 kilometres north-northwest of Bridesville, British Columbia. A five-stamp mill was erected at the Waterloo occurrence in 1899 by the Waterloo Consolidated Mining and Milling Company. The mill operated for only a month in that year and intermittently in the following year. There was renewed interest in the Waterloo occurrence in 1902 but failed to keep the mill operating. The Waterloo shaft was dewatered in 1929 by C.F. Law but no further work was done. A forest fire in 1929 destroyed all abandoned structures in the McKinney camp. The main shaft was 79 metres deep from which there was a substantial amount of drifting. Another shaft 104 metres west of the main shaft is on an offset continuation of the vein. During the early 1960s the occurrence was owned as part of a claim group by McKinney Gold Mines Ltd. but no work was reported. CARIBOO-AMELIA past producer (Au-quartz veins; Au-skarn; Silica veins) Minfile 082ESW020 In CG enclosed by McKinney claims The approximate centre of the Cariboo-Amelia underground workings is located at 1333 metres elevation on the southeastern slopes of Baldy Mountain. The occurrence is part of the historic Camp McKinney, located 9 kilometres north-northwest of Bridesville, British Columbia. The Cariboo-Amelia occurrence was first located on a group of eight Crown-granted claims: Emma (Lot 270), Alice (Lot 271), Cariboo (Lot 272), Amelia (Lot 273), Maple Leaf (Lot 613), Sawtooth (Lot 952), Okanagan (Lot 274) and Wiarton (Lot 856) (082ESW217). Underground mining began soon after the discovery of the Cariboo vein in 1887. The approximate centre of the Cariboo-Amelia underground workings is located at 1333 metres elevation on the southeastern slopes of Baldy Mountain. The occurrence is part of the historic Camp McKinney, located 9 kilometres north-northwest of Bridesville, British Columbia. The Cariboo-Amelia occurrence was first located on a group of eight Crown-granted claims: Emma (Lot 270), Alice (Lot 271), Cariboo (Lot 272), Amelia (Lot 273), Maple Leaf (Lot 613), Sawtooth (Lot 952), Okanagan (Lot 274) and Wiarton (Lot 856) (082ESW217). In 1957, the eastern extension of the Cariboo vein was discovered by surface G. McAuley and Associates formed the Cariboo-Mining and Milling Company and erected the first 10-stamp mill in 1894. By 1898, the Cariboo McKinney Mining and Milling Company Limited was formed to take over the operation and milling capacity was increased by 10 stamps. At the end of 1903, mining ceased as exploration failed to find the eastern extension, beyond a north-striking fault. The workings at this time consisted of 110-metre vertical shaft to the No. 4 level and a winze to the No. 6 level. The Consolidated Mining and Smelting Company optioned 29 claims of the McKinney camp and limited surface exploration was conducted. In 1934, the Bralco Development and Investment Company optioned the Cariboo-Amelia claim group. An effort was made to discover the western extension of the Cariboo vein with 5 diamond-drill holes. Pioneer Gold Mines of B.C. Ltd. optioned the property in 1939.

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History: Camp Mckinney Property Area (cont'd) Cariboo-Amelia past producer (cont'd) Underground drilling from the Nos. 4 and 5 levels and surface diamond drilling to the north explored the eastern extension. Results were poor and the option dropped. In the following year, G. Boag and Associated mined pillars and stoped remnants above the tunnel level. In 1941, Highland-Bell Ltd. explored the Wiarton claim, mined ore and developed 61 metres of drifts and crosscuts above the tunnel level. The lease reverted by the end of the year, however. From 1942 to 1946, E. Wanke and Associates dewatered the mine to the No. 2 level and resumed drilling. In 1998, Blackfoot Resources Ltd. optioned the property from Consolidated Gold City Mining Corp. and conducted drilling. Figure 6. Cariboo-Amelia workings (From Hedley, 1940)

WIARTON past producer (Au-quartz veins) Minfile 082ESW217 In CG enclosed by McKinney claims The Wiarton occurrence is located at 1295 metres elevation on the Wiarton (Lot 856) Crown grant in the historic Camp McKinney. The occurrence is 750 metres east of the Cariboo-Amelia occurrence (082ESW020). The camp lies 9 kilometres north-northwest of Bridesville, British Columbia Development on the Wiarton occurrence began in 1894 and continued to 1899 under ownership by the Camp McKinney Development Co. Ltd. By 1899, three shafts, 15.8, 16.1 and 18.3 metres respectively were developed along with 27 metres of drifting. The eastern continuation of the Cariboo/McKinney vein was intersected. The vein was 91 centimetres wide and of similar character to the Cariboo-Amelia and Waterloo (082ESW019) occurrences. In 1934, Pioneer Gold Mines of B.C. Limited conducted a limited surface diamond drilling program on the western edge of the Wiarton and on the Amelia claims to locate the eastern extension of the Cariboo-McKinney vein, without success. It was reported only one high grade quartz section was intersected (Bulletin 6, page 4). Later in that same year an unknown lessee sank a shaft down on one the earlier vertical drillholes of Pioneer. The results of this work is unknown.

Sookochoff Consultants Inc. August 12, 2019 Page 12 of 51 Bill McKinney McKinney Property Event 5724829 HISTORY: CAMP McKINNEY https://bcgoldadventures.com/camp-mckinney/ The discovery of Camp McKinney was made in 1884 by two placer miners, who uncovered free gold- bearing quartz. The camp, however, takes its name from Al McKinney, who located the first mineral claim, staking out the now famous Cariboo mine. Camp McKinney has been ever since a more or less active field for prospectors and miners. It is situated at an altitude of 4,600 feet, on round-topped hills, almost midway between Penticton and Greenwood. It is bounded on two sides by the forks of Rock Creek, while Rice Creek flows through the centre. Rock Creek, a short distance in the direction of Greenwood, was in the sixties a very active placer mining camp, and several million dollars are said to have been taken from there. In later years, the deposits have only been worked at intervals. https://en.wikipedia.org/wiki/Camp_McKinney,_British_Columbia Camp McKinney is a ghost town in the Boundary Country region of British Columbia, Canada. It is located southeast of Mount Baldy, northeast of Osoyoos. Several mines in the area led to the creation of Camp McKinney. The premier mine was called Cariboo- Amelia, usually referred to as the Cariboo. Al McKinney and Fred Rice staked a claim in 1888 which eventually became the Caribou Mine. Founded in 1896, Camp McKinney was situated on the south-eastern slopes of towering Mount Baldy. By 1901, the population of McKinney was 250. Hotels such as St. Louis, Sailor, Camp McKinney, McBoyle & West's, Cariboo and Miner's exchange competed for the miners' trade. The stagecoach of Hall line from Fairview and from the east came Meyerhoff's stage from Midway. The business section of town consisted of five saloons, three general stores, a drug store, a real estate office, butcher shop, a school and a church. In 1901, 16,862 tons of ore yielded 9,439 ounces of gold bullion, and 428 tons of concentrates. Up until October, 1900, dividends of $478,087 were paid, and in 1902, $496,837. However, gold mining declined in the area, the Cariboo Mine closed in December 1903 and Camp McKinney became a ghost town. Several unsuccessful attempts were made to revive the camp from 1907. Today, all that is left is a cemetery and a few abandoned workings.

Lost gold bars On August 18, 1896, George B. McAulay of Spokane, Washington, one of the major shareholders in the Cariboo mine, left Camp McKinney for Midway. McAulay had three gold bricks valued at more than $10,000. He was robbed half an hour later on his way to Midway. Cariboo Mining Company posted a $3,000 reward for information leading to recovery of the gold bars. The bars were never recovered. It is believed the bars were hidden or buried somewhere in the area, close by Camp McKinney still waiting to be discovered.

HISTORY: MCKINNEY PROPERTY The history on some of the mineral MINFILE reported showings, prospects, and past producers within the McKinney Property is reported as follows. The descriptions herein are copied from Minfile. GOLD HILL past producer (Polymetallic veins Ag-Pb-Zn+/-Au) Minfile 082ESW043 Within Tenure 1061735

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History: Camp Mckinney Property (cont'd) Gold Hill past producer (cont'd) Production records indicate that the Gold Hill occurrence produced 110 tonnes of ore in 1932 and 1935 with the recovery of 529 grams of silver, 435 grams of gold, 111 kilograms of lead and 96 kilograms of zinc. The work was done by Camp McKinney Gold Hill Mining Co. Ltd. and J. Carmichael. The Gold Hill occurrence is located at 1372 metres elevation on the southeastern slopes of Baldy Mountain. The occurrence is part of the historic Camp McKinney, located 9 kilometres north-northwest of Bridesville, British Columbia. In 1935, the Gold Hill property consisted of the Gold Hill Nos. 1 to 4, Little Billy, Paystreak Nos. 1 and 2, Allan, Mary, Douglas and Evelyn; the result of a partial restaking of the original eight claims which included the George Hurst (Geo Hurst) (Lot 1456), Dolphin, Bellevue Fr. (Lot 1268) and Bellringer No. 1 claims. During this time the property was developed by Camp McKinney Gold Hill Mining Co. Ltd. and J. Carmichael. Many of the above claims and Crown-granted claims have lapsed and have been restaked more recently as the Billie, Lou and Doreen claims. EUREKA prospect (Au-quartz veins; Polymetallic veins Ag-Pb-Zn+/-Au) Minfile 082ESW044 Within Tenure 1061735 The Eureka occurrence is located at approximately 1394 metres elevation on the southeast slopes of Baldy Mountain, 1.25 kilometres west-northwest of the Cariboo-Amelia occurrence (082ESW020). Bridesville, British Columbia lies 9.5 kilometres to the south-southeast. While physical evidence indicates the removal of a considerable amount of vein material from the Eureka occurrence, there are no known production records. It is uncertain whether this vein represents the western continuation of the Maple Leaf and Cariboo/McKinney veins. The Lou claim, located in 1982 by J. Craney, covers the Eureka and Eureka Fraction. In 1987, it was optioned to Wapiti Exploration Inc., who conducted magnetometer and VLF-EM surveys. Big Blackfoot Resources optioned the claim in the mid-1990s as part of a larger grouping. Apparently, no work was done on the Lou claim between 1987 and 2004. In 2004, one inclined NQ diamond-drill hole was completed, to a depth of 107.59 metres, to test the Eureka vein downdip, between the Eureka and the Little Eureka shafts. SAILOR prospect (Polymetallic veins Ag-Pb-Zn+/-Au; Polymetallic manto Ag-Pb-Zn) Minfile 082ESW045 Within Tenure 1061735 The Sailor occurrence is located at 1336 metres elevation on the southeastern slopes of Baldy Mountain, 600 metres southwest of the Cariboo-Amelia occurrence (082ESW020). The occurrence is part of the historic Camp McKinney, located 9 kilometres north-northwest of Bridesville, British Columbia. The Sailor occurrence is located on the Sailor (Lot 766) and Sailor Fraction (Lot 2523) of the former Sailor Claim Group held by Sailor Consolidated Mining and Milling Co. (circa 1901). At this time the claim group consisted of the Minnie-Ha-Ha (Lot 680), Cariboo Fraction, Golden Crown Fraction (Lot 924), Sailor (Lot 766), Rover Fraction (Lot 769), Alice Fraction, Bellevue (Lot 1268), Bellevue Fraction (Lot 1652), Snowshoe (Lot 1269), Diamond (Lot 1455) and Toledo (Lot 1270) claims, most of which were Crown granted.

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History: Camp Mckinney Property (cont'd) MINNIE HA HA prospect (Au-quartz veins) Minfile 082ESW046 Within Tenure 1061735 The Minnie-Ha-Ha occurrence is located at 1318 metres elevation on the southeastern slopes of Baldy Mountain, 600 metres southwest of the Cariboo-Amelia occurrence (082ESW020). The occurrence is part of the historic Camp McKinney, located 9 kilometres north-northwest of Bridesville, British Columbia. In 1901, the Sailor and Minnie-Ha-Ha claims were amalgamated under the ownership of Minnie-Ha-Ha Gold Mining Co. Little exploration has been done on the Minnie-Ha-Ha since this time. Jan Resources Ltd. conducted an exploration program on the Teaser (Lot 1625), Minnie-Ha-Ha, Pandre (Lot 1740), Alma (Lot 1741), Sneezer (Lot 2772) and Mitch (Lot 3589) Crown and Reverted Crown grants. The program consisted of soil geochemistry and prospecting. In 1980, the Minnie-Ha-Ha claim was acquired by Nexus Resource Corporation as part of the Sailor Group. An electromagnetic and magnetometer geophysical survey were conducted in that year. In 1981, geochemical soil and geological mapping were conducted. Then in 1988, another more detailed soil and rock geochemical program was conducted. A five stamp mill was erected and ran for three weeks during March 1900. No production records could be found. The property was abandoned later that same year. It is questionable whether pay ore was ever found (Minister of Mines Annual Report 1901, page 1151). GOLD STANDARD prospect (Au-quartz veins; Polymetallic veins Ag-Pb-Zn+/-Au) Minfile 082ESW128 Within Tenure 1061735 The Gold Standard occurrence is located at 1006 metres elevation adjacent to Rock Creek near its confluence with Jolly Creek, 600 metres west of the Victoria occurrence (082ESW021). Bridesville, British Columbia lies 8 kilometres to the south-southwest. Early development on the Gold Standard claim was a 122-metre adit near the quartz lens and a 27 metre shaft on the small quartz vein located 122 metres downstream. The adit exposes a number of stringers and masses of quartz which carry pyrite and coarsely crystalline galena. The large lens of quartz occurring near the portal is not reported in the workings. This early work was conducted by Lemon Gold Mining Co. from 1898 to 1901. A 5-stamp mill was reported shipped and operated to process ore from the 38-metre level of the adit, in 1901 No production records could be located however. Claims owned at this time included the Lemon (Lot 760), Gold Standard, Pennsylvania, Last Chance and Galena. By 1935, the property was referred to as the Gold Standard Group and included the Gold Standard, Ogofan and Ecuador (Lot 1452) claims. ANARCHIST prospect (Au-quartz veins; Polymetallic veins Ag-Pb-Zn+/-Au) Minfile 082ESW213 Within Tenure 1063217 The Anarchist occurrence is located at 1219 metres elevation on the banks of McKinney Creek, 6 kilometres south of Baldy Mountain. Bridesville, British Columbia is located 8.5 kilometres to the south-southeast. The Anarchist claim was one of the earliest explored claims in the vicinity of the former Camp McKinney.

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History: Camp Mckinney Property (cont'd) Anarchist prospect (cont'd) Exploration began in 1894 by R.G. Sidley with development of two short shafts and an opencut. Property development continued through to 1899 with the Dynamite Reverted Crown grant (Lot 767) added in 1897. By 1898, three parallel veins had been discovered on the Anarchist claim. The main vein was explored by the two shafts previously mentioned, now 18 and 15 metres deep. Little other work was conducted on the Anarchist or Dynamite claims until 1984. In 1981, Empire Resources Inc. completed a 143 metres diamond drill program in 4 holes. No production records could be found for the Anarchist occurrence and the Dynamite claim has received only exploration work. GRANITE past producer (Au-quartz veins) Minfile 082ESW214 Within Tenure 1063271 The Granite occurrence is located at 1204 metres elevation 6.5 kilometres east of McKinney Creek and south of Baldy Mountain. The Cariboo-Amelia occurrence (082ESW020) is located 4.5 kilometres to the northeast and Bridesville, British Columbia is located 8 kilometres to the south-southeast. Work was reported on the Banner and Granite claims as early as 1899. At this time they were owned and operated by Camp McKinney Mines. A substantial amount of work was reported and a 5-stamp mill was reported to have run for some time with very satisfactory results. No records could be found, however, concerning the length of time, the amount of ore that was processed, or the recovered grades. It is thought that most of the mill ore was supplied from the Banner claim. Recent work on the Granite and Banner claims has been conducted in 1981 by the Rock Creek Joint Venture Syndicate, 1985 by A. Dupras, 1986 by Gold Hill Syndicate and in 1987 under option to Wapiti Exploration Inc. KAMLOOPS showing (Au-quartz veins) Minfile 082ESW215 Within Tenure 106559 Development work began on the Kamloops occurrence pre-1897, as by this time it was reported that a 30-metre shaft, with 23 metres of drifting, was sunk on a quartz vein (Minister of Mines Annual Report 1901, page 1151). A second 12-metre shaft is located 24 metres southwest of the main shaft. The shaft was sunk in quartzite but little quartz vein or mineralization was observed. Two other prospecting shafts were also commenced and were 3.6 and 4.6 metres deep, respectively. At this time the Crown- granted claim was owned by J. Moran and development was carried out by the McKinney-Kamloops Company until 1900. In 1940, the property was owned by J.L. Grant. BIG BUG showing (Au-quartz veins) Minfile 082ESW216 Within Tenure 1061715 The Big Bug occurrence is located at 1234 metres elevation 8.5 kilometres southeast of Baldy Mountain, in the former historic Camp McKinney. The Big Bug (Lot 923) Reverted Crown grant lies below the Minnie-Ha-Ha (Lot 680) Reverted Crown grant of the McKinney camp. The camp lies 9 kilometres north-northwest of Bridesville, British Columbia. Development work began on the Big Bug occurrence in 1897 under the ownership of A. McGraw and W.H. Norris and continued until 1901. A 9.1-metre shaft was sunk on a small quartz vein striking 090 degrees. Apparently, no further work was done. The Big Bug property is now owned by W.G. Hallauer.

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History: Camp Mckinney Property (cont'd) PANDRE prospect (Au-quartz veins) Minfile 082ESW218 Within Tenure 1061735 The Pandre occurrence is located at 1432 metres elevation on the southern slopes of Baldy Mountain, 1.25 kilometres northwest of the Cariboo-Amelia occurrence (082ESW020) of the historic Camp McKinney. The occurrence consists of quartz veins on the Pandre (Lot 2661) and Alma (Lot 2660) Reverted Crown grants. The earliest recorded development on the Pandre occurrence was in 1898 when a 46-centimetre wide quartz vein was discovered on the Alma and a quartz vein carrying free gold was discovered on the Pandre (Minister of Mines Annual Report 1898, page 1117). At this time, development on the Alma consisted of two 3-metre shafts. On the Pandre, a 3.6-metre shaft was sunk. Surface stripping exposed the vein for 30 metres length. In the following year, two shafts on the Pandre were 9.1 and 10.7 metres deep, respectively. Several test pits were also dug. The vein was traced along these test pits for 640 metres length. The average width of the vein was 60 centimetres. Free gold, pyrite and galena comprised the vein mineralogy (Minister of Mines Annual Report 1899, page 774). Assay values were reported to have been very high (Minister of Mines Annual Report 1899, page 774). No further work was reported on either claim until 1981. However, the Alma claim was Crown granted to P.B.S. Stanhope in 1905 and the Pandre was Crown granted to Executors of the E. James estate in 1909. In 1981, a joint exploration program was conducted on the ground covering the Pandre occurrence by McQuillan Gold Ltd. and Jan Resources Ltd. The program was limited to prospecting and a soil geochemistry survey. A zinc soil anomaly was found which extended onto the Pandre and eastern edge of the Alma claims. In 1986, A. Dupras conducted limited prospecting and rock geochemistry sampling on ground surrounding the Pandre occurrence. No significant results were reported. SLAMET prospect (Au-quartz veins) Minfile 082ESW220 Within Tenure 1061735 The Slamet occurrence is located at 1417 metres elevation on the Slamet (Lot 2663) Reverted Crown grant, 6.75 kilometres southeast of Baldy Mountain. The Cariboo-Amelia occurrence (082ESW020) is located 1 kilometre to the east, both in the historic Camp McKinney. Development began in the early 1900s on the Slamet occurrence. In 1905, it was first Crown granted to L.W. Shatford, W. Edwards and others. Later in 1918, the property was Crown granted to E. Hallet. No records could be found of the early development work or vein geology. Little other work was done on the property again until the 1980s. In 1984, Mintek Resources Ltd. staked ground which included the Slamet occurrence but no work was recorded. In 1986, G. Allen prospected the occurrence. Limited rock geochemistry sampling was also done. ARGEN prospect (Intrusion related pyrrhotite veins; Au-quartz veins) Minfile 082ESW222 Within Tenure 1064559 The Argen occurrence is located on the west side of Rock Creek at 1250 metres elevation, 7.75 kilometres southeast of Baldy Mountain. The Cariboo-Amelia of the historic Camp McKinney lies 1.25 kilometres to the southwest and 9 kilometres north of Bridesville, British Columbia.

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History: Camp Mckinney Property (cont'd) Argen prospect (cont'd) No early records could be found concerning the development of the Argen occurrence on the Argen claim. The claim was Crown granted to J.A. Mara in 1896. In 1980, the Rock Creek Joint Venture optioned the ground covering the Argen occurrence from Dayton Creek Silver Mines Ltd. The following is their description of the Argen occurrence. The Argen shaft is 6.1 metres deep. Nine metres to the northwest is a small caved pit. Opencuts extend northwest from this pit 45 metres. Other old trenches and opencuts are scattered on the Argen claim.

GEOLOGY: CAMP McKINNEY PROPERTY AREA Minfile reports on the geology of past producers adjacent to the McKinney property area as follows. FONTENOY past producer (Au-quartz veins) Minfile 082ESW018 In CG enclosed by McKinney claims The Camp McKinney area is underlain by a complex interlayered succession of metamorphosed sediments and volcanics of the Carboniferous to Permian Anarchist Group. The group consists mainly of metabasalt and andesite flows and tuffs, greenstone (locally calcareous), minor marble, altered and argillaceous quartzite (locally micaceous), greywacke, limestone and locally micaceous quartzite and calcareous and biotite schist. Granite and granodiorite of the Middle Jurassic Nelson intrusions have intruded the Anarchist Group to the west and south as small stocks and plugs. Along the contacts of these intrusions the Anarchist rocks have been deformed and hydrothermally altered. Younger dikes of felsic and mafic composition intrude both stratified and granitic rocks and may have been associated with faults related to these granitic intrusions. Intense deformation and hydrothermal alteration comprising silicification and carbonatization is evident in the hostrocks. To the north are Cretaceous granites and granodiorites of the Okanagan batholith. Eocene Penticton Group volcanic and sedimentary rocks overlie locally sheared amphibolite and serpentinite bodies of the Anarchist Group to the east. Complexly folded and faulted metasediments and metavolcanics have a regional northwest strike with moderate to steep northeast dips. Surface mapping has outlined a northwest plunging recumbent synform. The limbs dip moderately to steeply to the northeast. The major regional structural feature in the vicinity of the Fontenoy occurrence is a northeast trending fault zone 5 kilometres to the east. The fault follows Conkle Creek, Conkle Lake and Jolly Creek. Faulting in the Cariboo-Amelia (082ESW020) mine area is postmineral and widespread. Major east dipping, low angle thrust faults in the central portion of the mine have displaced the hangingwall to the northwest by about 122 metres. An east- dipping fault has also moved the hangingwall south by about 91 metres. The complexly faulted and folded rocks are predominantly north. The primary hostrock of the Fontenoy vein is siliceous argillite of the Anarchist Group, striking northwest and dipping northeast. Several intercalated silicified greenstone beds are locally hosted in argillite. To the east of the occurrence, a major north-trending fault is expressed by a deep gully. WATERLOO past producer (Au-quartz veins) Minfile 082ESW019 In CG enclosed by McKinney claims The Camp McKinney area is underlain by a complex interbanded sequence of Carboniferous to Permian Anarchist Group metamorphosed sediments and volcanics.

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Geology: Camp Mckinney Property Area (cont'd) Waterloo past producer (cont'd) The group is mainly sedimentary and consists of greenstone, locally calcareous, altered quartzite and argillaceous quartzite, greywacke, limestone and locally micaceous quartzite and calcareous biotite schist. The minor volcanics are described as mainly altered andesitic and basaltic flows. Granite and granodiorite of the Middle Jurassic Nelson intrusions have intruded the Anarchist Group to the west and south as small stocks and plugs. Along the contacts of these intrusions the Anarchist rocks have been deformed and hydrothermally altered. Younger dikes of felsic and mafic composition intrude both stratified and granitic rocks and may have been associated with faults related to these granitic intrusions. To the north lie Cretaceous granitic and granodioritic rocks of the Okanagan batholith. Eocene Penticton Group volcanic and sedimentary rocks overlie locally sheared amphibolite and serpentinite bodies of the Anarchist Group to the east. The major regional structural feature in the vicinity of the Cariboo-Amelia occurrence is a northeast trending fault zone 5 kilometres to the east. The fault follows Conkle Creek, Conkle Lake and Jolly Creek. Faulting in the Cariboo-Amelia mine area is postmineral and widespread. Major east dipping, low angle thrust faults in the central portion of the mine have displaced the hangingwall to the northwest by about 122 metres. An east-dipping fault has also moved the hangingwall south by about 91 metres. The complexly faulted and folded rocks are predominantly northwest striking and steeply to moderately northeast dipping. Greenstones at the Waterloo occurrence are composed largely of shreddy secondary amphibole, possibly representing metamorphism of impure calcareous sediments. Calcite is absent. The major regional structural feature in the vicinity of the Cariboo-Amelia occurrence is a northeast trending fault zone 5 kilometres to the east. The fault follows Conkle Creek, Conkle Lake and Jolly Creek. Faulting in the Cariboo-Amelia mine area is postmineral and widespread. Major east dipping, low angle thrust faults in the central portion of the mine have displaced the hangingwall to the northwest by about 122 metres. An east-dipping fault has also moved the hangingwall south by about 91 metres. The complexly faulted and folded rocks are predominantly northwest striking and steeply to moderately northeast dipping. Greenstones at the Waterloo occurrence are composed largely of shreddy secondary amphibole, possibly representing metamorphism of impure calcareous sediments. Calcite is absent. The major regional structural feature in the vicinity of the Cariboo-Amelia occurrence is a northeast trending fault zone 5 kilometres to the east. The fault follows Conkle Creek, Conkle Lake and Jolly Creek. Faulting in the Cariboo-Amelia mine area is postmineral and widespread. Major east dipping, low angle thrust faults in the central portion of the mine have displaced the hangingwall to the northwest by about 122 metres. An east-dipping fault has also moved the hangingwall south by about 91 metres. The complexly faulted and folded rocks are predominantly northwest striking and steeply to moderately northeast dipping. Greenstones at the Waterloo occurrence are composed largely of shreddy secondary amphibole, possibly representing metamorphism of impure calcareous sediments. Calcite is absent.

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Geology: Camp Mckinney Property Area (cont'd) CARIBOO-AMELIA past producer (Au-quartz veins; Au-skarn; Silica veins) Minfile 082ESW020 In CG enclosed by McKinney claims The Camp McKinney area is underlain by interbanded and intergrading Carboniferous to Permian Anarchist Group metamorphosed sediments and volcanics. The group is mainly sedimentary and consists of greenstone, locally calcareous, altered quartzite and argillaceous quartzite, greywacke, limestone and locally micaceous quartzite and calcareous biotite schist. Granite and granodiorite of the Middle Jurassic Nelson intrusions have intruded the Anarchist Group to the west and south as small stocks and plugs. Along the contacts of these intrusions the Anarchist rocks have been deformed and hydrothermally altered. Younger dikes of felsic and mafic composition intrude both stratified and granitic rocks and may have been associated with faults related to these granitic intrusions. Faulting in the Cariboo-Amelia mine area is postmineral and widespread. Major east dipping, low angle thrust faults in the central portion of the mine have displaced the hanging wall to the northwest by about 122 metres. An east-dipping fault has also moved the hangingwall south by about 91 metres. The complexly faulted and folded rocks are predominantly northwest striking and steeply to moderately northeast dipping. At the Cariboo-Amelia mine, the main quartz vein, commonly referred to as the Cariboo or McKinney vein, is hosted by a complex interlayered succession of metabasalt flows, tuffs and minor marble of the Anarchist Group. The rocks appear to be metamorphosed to upper greenschist or amphibolite facies. Metabasalts are sheared and altered to sericite, carbonate and quartz along vein walls. Plagioclase, amphibole, biotite, chlorite, carbonate, quartz and pyrrhotite comprise metavolcanics. Marble forms a 9-metre thick band striking northwest through the Amelia claim. Other thin marble bands are found within metasediments. Metasedimentary rocks include successions of interbedded quartzite and argillite. Intense deformation and hydrothermal alteration comprising silicification and carbonatization is evident in the hostrocks. Complexly folded and faulted metasediments and metavolcanics have a regional northwest strike with moderate to steep northeast dips. Surface mapping has outlined a northwest plunging recumbent synform. The limbs dip moderately to steeply to the northeast. The Cariboo/McKinney vein crosscuts all rock types (except the mafic dikes), commonly at a high angle to bedding. The vein is more regular where it crosscuts competent metabasalts and irregular with offshoots where it crosscuts quartzite and other metasediments. The vein itself is offset by numerous faults having a variety of orientations which include low angle thrust faults with displacements of up to 120 metres. The Cariboo/McKinney vein strikes 090 degrees and dips vertically with local steep south dips. It has been mined over a strike length of 754 metres, and to a depth of 107 metres in the west section of the No. 4 level and 171 metres in the east sections of the Nos. 5 and 6 levels. The total surface trace of the vein is 1630 metres long on the Crown grants, and an additional 780 metres east and west. The vein width is quite variable over short distances along strike and dip. Widths vary from 0.25 up to 3.5 metres. The Cariboo/McKinney vein is composed of white quartz and pyrite with lesser sphalerite, galena, chalcopyrite and rare tetrahedrite and pyrrhotite.

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Geology: Camp Mckinney Property Area (cont'd) Cariboo-Amelia past producer (cont'd) Visible native gold is locally prominent. Higher gold grades occur where the vein hosts narrow massive sulphide bands(up to 3 to 5 per cent) or higher sphalerite and galena concentrations (Assessment Report 20668). Locally the quartz appears bluish and chalcedonic, and contains free gold (Bulletin 6). The vein has been classified as a mesothermal vein based on its: (1) strike length, (2) the character of the quartz and sulphides and (3) its similarity to Report 20668) with an average recovered grade of 24.68 grams per tonne gold (Gold City Mining Corp. (mesothermal veins of the nearby Fairview Camp (Assessment Report 20668). WIARTON past producer (Au-quartz veins) Minfile 082ESW217 In CG enclosed by McKinney claims Hostrocks of the Wiarton occurrence are dominantly argillaceous quartzites. Other lithologies include soft quartzose rocks and other silty to calcareous sediments metamorphosed to The Camp McKinney area is underlain by interbanded and intergrading Carboniferous to Permian Anarchist Group metamorphosed sediments and volcanics. The group is mainly sedimentary and consists of greenstone, locally calcareous, altered quartzite and argillaceous quartzite, greywacke, limestone and locally micaceous quartzite and calcareous biotite schist. The minor volcanics are described as mainly altered andesitic and basaltic flows. Granite and granodiorite of the Middle Jurassic Nelson intrusions have intruded the Anarchist Group to the west and south as small stocks and plugs. Along the contacts of these intrusions the Anarchist rocks have been deformed and hydrothermally altered. Younger dikes of felsic and mafic composition intrude both stratified and granitic rocks and may have been associated with faults related to these granitic intrusions. The major regional structural feature in the vicinity of the Cariboo-Amelia occurrence (082ESW020) is a northeast trending fault zone 5 kilometres to the east. The fault follows Conkle Creek, Conkle Lake and Jolly Creek. Faulting in the Cariboo-Amelia mine area is postmineral and widespread. Major east-dipping, low angle thrust faults in the central portion of the mine have displaced the hangingwall to the northwest by about 122 metres. An east-dipping fault has also moved the hangingwall south by about 91 metres. The complexly faulted and folded rocks are predominantly northwest striking and steeply to moderately northeast dipping. amphibolite. The amphibolite is composed primarily of fibrous amphibole. A north-trending gully on the Wiarton claim is indicative of a local fault.

GEOLOGY: MCKINNEY PROPERTY Descriptions of the geology on reported showings and past producers within the McKinney Property are reported as follows. The descriptions herein are copied from Minfile. GOLD HILL past producer (Polymetallic veins Ag-Pb-Zn+/-Au) Minfile 082ESW043 Within Tenure 1061735

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Geology: Camp Mckinney Property (cont'd) Gold Hill past producer (cont'd) The Camp McKinney area is underlain by interbanded and intergrading Carboniferous to Permian Anarchist Group metamorphosed sediments and volcanics. The group is mainly sedimentary and consists of greenstone, locally calcareous, altered quartzite and argillaceous quartzite, greywacke, limestone and locally micaceous quartzite and calcareous biotite schist. The minor volcanics are described as mainly altered andesitic and basaltic flows. Granite and granodiorite of the Middle Jurassic Nelson intrusions have intruded the Anarchist Group to the west and south as small stocks and plugs. Along the contacts of these intrusions the Anarchist rocks have been deformed and hydrothermally altered. Younger dikes of felsic and mafic composition intrude both stratified and granitic rocks and may have been associated with faults related to these granitic intrusions. Eocene Penticton Group volcanic and sedimentary rocks overlie locally sheared amphibolite and serpentinite bodies to the east. For a more detailed description of the geology of the area refer to the Cariboo-Amelia (082ESW020). Development on the Gold Hill No. 4 claim consisted of two adits. The first adit was an 18-metre shaft at 1463 metres elevation with 4.5 to 6.1 metres crosscutting from the bottom. The shaft is sunk 15 to 18 metres deep on a 2.1-metre wide quartz vein striking 120 degrees and dipping 55 degrees southwest. On surface the vein is 1.8 metres wide and is traceable for over 305 metres. A crosscut driven south from the bottom of the shaft intersected three quartz veins of a different structure from the main vein. Mineralization consists of pyrite occurring in small bunches and along fractures in bluish quartz of similar character to the Cariboo-Amelia (082ESW020). The vein is well jointed parallel to the strike and dip of the host sheared quartzites. Another adit was encountered to the north of the main Gold Hill adit. This adit was driven 40 metres with an average trend of 333 degrees. The adit was exploratory. No vein material or mineralization is reported. About 183 metres southeast along the strike of the Gold Hill vein and 45 metres lower in elevation the second 104-metre adit has been sunk on a quartz vein. At the adit entrance the vein is 1.5 metres wide, strikes 310 degrees and dips 60 to 85 degrees northeast. It consists of white to bluish chalcedonic quartz with scant mineralization. With depth the vein continually narrows, eventually pinching out at 18.0 metres. Pyrite, galena and sphalerite comprise mineralization; some short sections of quartz vein up to 25 centimetres wide with sheared host rock occur. The innermost 40 metres of the adit follows a slip that strikes 302 degrees and dips 70 degrees northeast. In the footwall of this slip there is a narrow and discontinuous quartz stringer. The Dolphin showing is claimed to consist of three veins: (1) a 46 to 240 centimetre wide quartz vein striking 060 degrees was intersected in the Dolphin adit, (2) to the west, a band of mineralized quartzite explored by an 18-metre tunnel in quartzose schists and (3) near the western boundary, a 91 to 150 centimetre wide quartz vein striking 290 degrees and traceable on surface for 304 metres. Pyrite and galena comprise mineralization One hundred and fifty-two metres east of the Dolphin adit and 53-metres southwest of the north neighbouring Edward VII claim, are a series of pits and opencuts which explore a 61 metre length of quartz vein striking 075 degrees and dipping 75 degrees south. The vein is as narrow as 22 centimetres and is hosted in the footwall of a 50 to 90 centimetre wide shear zone. In this vicinity mineralization consists of shattered pyrite masses veined with quartz.

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Geology: Camp Mckinney Property Area (cont'd) EUREKA prospect (Au-quartz veins; Polymetallic veins Ag-Pb-Zn+/-Au) Minfile 082ESW044 Within Tenure 1061735 The Eureka occurrence lies in a complex sequence of volcanic and metasedimentary rocks of the Carboniferous to Permian Anarchist Group. To the north are Cretaceous granitic and granodioritic rocks of the Okanagan batholith. Middle Jurassic granitic rocks of the Nelson intrusions occur to the southwest. Eocene Penticton Group volcanic and sedimentary rocks overlie locally sheared amphibolite and serpentinite bodies of the Anarchist Group to the east. For a more detailed description of the regional geology of the McKinney camp refer to the Cariboo-Amelia occurrence (082ESW020). Two shafts exist on what is known as the Eureka vein on the Eureka claim. The first main shaft was sunk in 1899, to a depth of 49 metres with a 34-metre drift at 26 metres depth. The second shaft is 30 metres east of the main shaft and is 5 metres deep. On the west side of the claim the quartz vein is up to 2.74 metres wide, striking 110 degrees and dipping 82 degrees south. Flat faults have displaced the lower sections of the vein to the south. Opencuts and a 6.1-metre deep shaft have traced the vein 76 metres along a strike of 112 degrees. In the northwest section of these workings the vein is 1.2 to 1.8 metres wide while in the southeast section, it is 30 to 91 centimetres wide. The vein is hosted predominantly in greenstone. Wallrocks consist of argillic quartzites and greenstone. Carbonate alteration occurs within a few centimetres of this vein. Development work on the Eureka Fraction consisted of several trenches and shafts. The deepest shaft is reported to be 4.6 metres deep. On the Eureka Fraction the vein is 1.2 to 1.8 metres wide and strikes 280 degrees. The vein can be traced for 46 metres on surface and consists of pyrite and chalcopyrite containing gold and silver in a quartz gangue. While physical evidence indicates the removal of a considerable amount of vein material from the Eureka occurrence, there are no known production records. It is uncertain whether this vein represents the western continuation of the Maple Leaf and Cariboo/McKinney veins. The Lou claim, located in 1982 by J. Craney, covers the Eureka and Eureka Fraction. In 1987, it was optioned to Wapiti Exploration Inc., who conducted magnetometer and VLF-EM surveys. Big Blackfoot Resources optioned the claim in the mid-1990s as part of a larger grouping. Apparently no work was done on the Loptu claim between 1987 and 2004. In 2004, one inclined NQ diamond-drill hole was completed, to a depth of 107.59 metres, to test the Eureka vein downdip, between the Eureka and the Little Eureka shafts. SAILOR prospect (Polymetallic veins Ag-Pb-Zn+/-Au; Polymetallic manto Ag-Pb-Zn) Minfile 082ESW045 Within Tenure 1061735 The Sailor occurrence lies in a complex sequence of volcanic and metasedimentary rocks of the Carboniferous to Permian Anarchist Group. To the north are Cretaceous granitic and granodioritic rocks of the Okanagan batholith. Middle Jurassic granitic rocks of the Nelson intrusions occur to the southwest. Eocene Penticton Group volcanic and sedimentary rocks overlie locally sheared amphibolite and serpentinite bodies of the Anarchist Group to the east. For a more detailed description of the regional geology of the McKinney camp refer to the Cariboo- Amelia occurrence (082ESW020).

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Geology: Camp Mckinney Property (cont'd) Sailor prospect (cont'd) Development of the Sailor was via a 53-metre shaft with levels at 23, 30, and 46 metres, respectively. The shaft, sunk in 1899, is located on flat ground and is now caved. On the Sailor Fraction, development is through a shaft about 4.5 metres deep. It is also inaccessible. A series of surface strippings, opencuts and trenches extend from the Sailor shaft for 61 metres along a strike of 112 degrees and then an additional 15 metres along a strike of 135 degrees. The vein is hosted in greenstone and varies from 1.2 to 1.8 metres wide along the northwestern section and 0.3 to 0.9 metres wide along the southeastern section. A series of surface strippings, opencuts and trenches extend from the Sailor shaft for 61 metres along a strike of 112 degrees and then an additional 15 metres along a strike of 135 degrees. The vein is hosted in greenstone and varies from 1.2 to 1.8 metres wide along the northwestern section and 0.3 to 0.9 metres wide along the southeastern section. A series of surface strippings, opencuts and trenches extend from the Sailor shaft for 61 metres along a strike of 112 degrees and then an additional 15 metres along a strike of 135 degrees. The vein is hosted in greenstone and varies from 1.2 to 1.8 metres wide along the northwestern section and 0.3 to 0.9 metres wide along the southeastern section. MINNIE HA HA prospect (Au-quartz veins) Minfile 082ESW046 Within Tenure 1061735 The Minnie Ha-Ha occurrence lies in greenstone metavolcanic and metasedimentary rocks of the Carboniferous to Permian Anarchist Group. To the north are 'Valhalla' Jurassic-Cretaceous granitic and granodioritic rocks. Middle Jurassic granitic rocks occur to the southwest. Eocene Penticton Group volcanic and sedimentary rocks overlie locally sheared amphibolite and serpentinite bodies of the Anarchist Group to the east. For a more detailed description of the regional geology of the McKinney camp refer to the Cariboo-Amelia occurrence (082ESW020). The Minnie-Ha-Ha occurrence is hosted by calcareous greenstone crosscut by quartz feldspar veinlets. Hostrocks are strongly bleached near the vein walls and altered to sericite, calcite and ankerite with minor secondary quartz and disseminated pyrite. Silicification of the hostrocks is also common. GOLD STANDARD prospect (Au-quartz veins; Polymetallic veins Ag-Pb-Zn+/-Au) Minfile 082ESW128 Within Tenure 1061735 The Gold Standard occurrence is situated in a sequence of metavolcanic and metasedimentary rocks of the Carboniferous to Permian Anarchist Group. The sequence, over 1000 metres thick, consists of greenstone and diorite grading upward into a sedimentary sequence which in turn grades upward into a tuffaceous sedimentary sequence. Calcareous greenstone is the dominant rock type surrounding the Gold Standard occurrence. The greenstone is locally sheared, schistose and talcose. Where less altered, a porphyritic texture is observed. Other greenstones are finely crystalline and tuffaceous grading to a medium grained hornblende porphyritic hornblende diorite. Elsewhere greenstones contain argillaceous and minor marble partings and bands. Orthogneiss is developed along faults to the northeast. To the north are Cretaceous granites and granodiorites of the Okanagan batholith. Middle Jurassic Nelson granites occur to the southwest. Eocene Penticton Group volcanic and sedimentary rocks overlie locally sheared amphibolite and serpentinite bodies to the east. Lithologies located east and northeast of the Gold Standard occurrence include quartz latite, trachyandesite and syenite. For a more detailed description of the geology refer to the Cariboo-Amelia (082ESW020).

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Geology: Camp Mckinney Property (cont'd) ANARCHIST prospect (Au-quartz veins; Polymetallic veins Ag-Pb-Zn+/-Au) Minfile 082ESW213 Within Tenure 1063217 Lithologies underlying the Anarchist occurrence consists of granitic rocks of the Middle Jurassic Nelson intrusions. The dominant composition is biotite granite. The dominant fractures strike 032 degrees. For a more detailed description of the surrounding geology refer to the Cariboo-Amelia occurrence (082ESW020). Three parallel veins were discovered on the Anarchist claim over 9 metres width. The veins were traceable for up to 183 metres along strike. Drilling in 1981 did not intersect two parallel veins. All three veins strike 020 degrees and dip vertically. The west wall (hangingwall) of the main vein is silicified and bleached over a few centimetres and has a gneissic fabric. The footwall is composed of granite. Underground, the main vein has an average width of 1.4 metres. The vein width and dip is consistent throughout its traceable length. The vein appears to follow an auxiliary fault structure of varying orientation. At the main shaft the fault strikes 032 degrees, dips vertical and is 150 centimetres wide. Thirty metres south, the fault strikes 360 degrees and dips vertical. The vein is visible at this point and is 60 centimetres wide. To the south 30 metres, the fault strikes 032 degrees and is 120 centimetres wide. Underground, the main vein has been displaced, a distance equivalent to the vein width, by near-horizontal faults. GRANITE past producer (Au-quartz veins) Minfile 082ESW214 Within Tenure 1063271 Lithologies underlying the Granite occurrence consists of biotite granodiorite of the Middle Jurassic Nelson intrusions. The dominant fractures strike 032 degrees. For a more detailed description of the surrounding geology refer to the Cariboo-Amelia occurrence. KAMLOOPS showing (Au-quartz veins) Minfile 082ESW215 Within Tenure 106559 The Camp McKinney area is underlain by interbanded and intergrading Carboniferous to Permian Anarchist Group metamorphosed sediments and volcanics. The group is mainly sedimentary and consists of greenstone, locally calcareous, altered quartzite and argillaceous quartzite, greywacke, limestone and locally micaceous quartzite and calcareous biotite schist. The minor volcanics are described as mainly altered andesitic and basaltic flows. Granite and granodiorite of the Middle Jurassic Nelson intrusions have intruded the Anarchist Group to the west and south as small stocks and plugs. Along the contacts of these intrusions the Anarchist rocks have been deformed and hydrothermally altered. Younger dikes of felsic and mafic composition intrude both stratified and granitic rocks and may have been associated with faults related to these granitic intrusions. The major regional structural feature in the vicinity of the Cariboo-Amelia occurrence (082ESW020) is a northeast trending fault zone 5 kilometres to the east. The fault follows Conkle Creek, Conkle Lake and Jolly Creek. Faulting in the Cariboo-Amelia mine area is post mineral and widespread.

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Geology: Camp Mckinney Property (cont'd) Kamloops showing (cont'd) Major east dipping, low angle thrust faults in the central portion of the mine have displaced the hangingwall to the northwest by about 122 metres. An east-dipping fault has also moved the hangingwall south by about 91 metres. The complexly faulted and folded rocks are predominantly northwest striking and steeply to moderately northeast dipping. The Kamloops occurrence is hosted in banded greenstone of the Anarchist Group dipping flatly northward. Considerable quartz was reported in a dump near the shaft. Development work began on the Kamloops occurrence pre-1897, as by this time it was reported that a 30-metre shaft, with 23 metres of drifting, was sunk on a quartz vein (Minister of Mines Annual Report 1901, page 1151). A second 12-metre shaft is located 24 metres southwest of the main shaft. The shaft was sunk in quartzite but little quartz vein or mineralization was observed. Two other prospecting shafts were also commenced and were 3.6 and 4.6 metres deep, respectively. At this time the Crown- granted claim was owned by J. Moran and development was carried out by the McKinney-Kamloops Company until 1900. In 1940, the property was owned by J.L. Grant. The vein intersected in the two shafts is considered to be the eastern extension of the Sailor vein (082ESW045) and the faulted western extension of the Minnie-Ha-Ha vein (082ESW046). Refer to these two occurrences for further details on the vein geology and mineralization BIG BUG showing (Au-quartz veins) Minfile 082ESW216 Within Tenure 1061715 The Camp McKinney area is underlain by interbanded and intergrading Carboniferous to Permian Anarchist Group metamorphosed sediments and volcanics. The group is mainly sedimentary and consists of greenstone, locally calcareous, altered quartzite and argillaceous quartzite, greywacke, limestone and locally micaceous quartzite and calcareous biotite schist. The minor volcanics are described as mainly altered andesitic and basaltic flows. Granite and granodiorite of the Middle Jurassic Nelson intrusions have intruded the Anarchist Group to the west and south as small stocks and plugs. Along the contacts of these intrusions the Anarchist rocks have been deformed and hydrothermally altered. Younger dikes of felsic and mafic composition intrude both stratified and granitic rocks and may have been associated with faults related to these granitic intrusions. The major regional structural feature in the vicinity of the Cariboo-Amelia occurrence (082ESW020) is a northeast trending fault zone 5 kilometres to the east. The fault follows Conkle Creek, Conkle Lake and Jolly Creek. Faulting in the Cariboo-Amelia mine area is postmineral and widespread. Major east-dipping, low angle thrust faults in the central portion of the mine have displaced the hangingwall to the northwest by about 122 metres. Outcrop is sparse on the Big Bug property. Calcareous greenstone is found in a few outcrops west of the old shaft. Alteration and shearing have given a weak schistose texture to the greenstone. The shaft was sunk on a 5 to 20 centimetre quartz vein striking 090 degrees and dipping 80 degrees south. The vein has been traced on surface, 10 metres west of the shaft. Pyrite occurs as fracture fillings and disseminations in the quartz vein.

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Geology: Camp Mckinney Property (cont'd) PANDRE prospect (Au-quartz veins) Minfile 082ESW218 Within Tenure 1061735 The Pandre occurrence lies in a complex sequence of volcanic and metasedimentary rocks of the Carboniferous to Permian Anarchist Group. To the north are Cretaceous granitic and granodioritic rocks of the Okanagan batholith. Middle Jurassic granitic rocks of the Nelson intrusions occur to the southwest. Eocene Penticton Group volcanic and sedimentary rocks overlie locally sheared amphibolite and serpentinite bodies of the Anarchist Group to the east. For a more detailed description of the regional geology of the McKinney camp refer to the Cariboo-Amelia occurrence (082ESW020). Quartzites of the Anarchist Group are reported to the dominant hostrock of the Pandre occurrence (Assessment Report 9840). SLAMET prospect (Au-quartz veins) Minfile 082ESW220 Within Tenure 1061735 The Slamet occurrence lies in a complex sequence of volcanic and metasedimentary rocks of the Carboniferous to Permian Anarchist Group. To the north are Cretaceous granitic and granodioritic rocks of the Okanagan batholith. Middle Jurassic granitic rocks of the Nelson intrusions occur to the southwest. Eocene Penticton Group volcanic and sedimentary rocks overlie locally sheared amphibolite and serpentinite bodies of the Anarchist Group to the east. For a more detailed description of the regional geology of the McKinney camp refer to the Cariboo-Amelia occurrence (082ESW020). Intense silicification of greenstone has occurred at the Slamet occurrence (Bulletin 6, page 9). The Slamet occurrence lies along a prominent ridge of thinly bedded granular white quartzite, trending 020 degrees. An old adit and trenches have uncovered several quartz veins that strikes 280 to 300 degrees and dips steeply southwest. The largest of these veins is 1 metre wide and is hosted in sheared and silicified greenstone. ARGEN prospect (Intrusion related pyrrhotite veins; Au-quartz veins) Minfile 082ESW222 Within Tenure 1064559 The Argen occurrence lies in a complex sequence of volcanic and metasedimentary rocks of the Carboniferous to Permian Anarchist Group. Granitic and granodioritic rocks of the Cretaceous to Tertiary Okanagan batholith and Middle Jurassic granitic rocks of the Nelson intrusions lie immediately to the north. Eocene Penticton Group volcanic and sedimentary rocks overlie locally sheared amphibolite and serpentinite bodies of the Anarchist Group to the east. For a more detailed description of the regional geology of the McKinney camp area refer to the Cariboo-Amelia occurrence (082ESW020). Locally, the Argen occurrence is hosted in siliceous schist and quartzite. These rocks strike north with steep dips and are highly fractured, banded and jointed.

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Figure 7. Camp McKinney Historic Crown Grants (From Hedley, 1940)

Figure 8. Property Geology (From Hedley, 1940)

Sookochoff Consultants Inc. August 12, 2019 Page 28 of 51 Bill McKinney McKinney Property Event 5724829 MINERALIZATION: CAMP McKINNEY PROPERTY AREA Minfile reports on the mineralization of past producers adjacent to the McKinney property area as follows. FONTENOY past producer (Au-quartz veins) Minfile 082ESW018 In CG enclosed by McKinney claims Mineralization is confined to a northwest striking quartz vein dipping 45 to 55 degrees northeast. The 1.5-metre vein is confined to a shear zone within the argillaceous quartzite and greenstone. Minerals within the vein include: sphalerite, galena, massive pyrite, and gold. Dump samples of the wallrock have been reported to contain graphitic slickensides, pyritization and some alteration. Past production from the Fontenoy occurrence is uncertain and production records could have been combined with production from the Cariboo-Amelia occurrence (082ESW020Fontenoy (Lot 752), Vernon (Lot 759), Last Chance (Lot 751) and later included the Knight Rambler (Lot 3015) and Islander (Lot 1090). WATERLOO past producer (Au-quartz veins) Minfile 082ESW019 In CG enclosed by McKinney claims Mineralization is confined to a vein zone striking east- southeast, dipping 85 degrees north and having a width of 1.22 metres. It consists of a number of bluish quartz stringers occurring in sheared greenstone. Free gold is reported from this zone. Stripping and open-cutting in greenstone near the shaft exposed 30.5 metres of vein striking east-southeast and dipping 85 degrees north. The vein is 50 to 76 centimetres wide and largely barren. Past production from the Waterloo occurrence is uncertain and production records could have been combined with production from the Cariboo-Amelia occurrence (082ESW020). CARIBOO-AMELIA past producer (Au-quartz veins; Au-skarn; Silica veins) Minfile 082ESW020 In CG enclosed by McKinney claims The Cariboo-Amelia occurrence has been the most significant mineral deposit and mineral producer from Camp McKinney. It was British Columbia's first dividend paying lode gold mine (Assessment 1996): Geological/Mineral Deposit Field Trip Report). Over its intermittent 68 year mine life, from 1894 to 1962, the Cariboo-Amelia produced 124,452 tonnes ore of which 112,254 tonnes is reported milled on-site. Recovery included 2,538,101 grams of gold, 1,008,979 grams of silver, 51,393 kilograms of lead and 89,875 kilograms of zinc, with lead and zinc recovered since 1940. The ore (about 10,243 tonnes) from 1960 to 1962, was also used as a siliceous flux in the Trail smelter.

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Figure 9. Faulted end of the Cariboo vein (From BC Archives )

MINERALIZATION: MCKINNEY PROPERTY The mineralization on the MINFILE reported past producers and showings within the McKinney Property area are reported as follows. The descriptions herein are copied from Minfile. GOLD HILL past producer (Polymetallic veins Ag-Pb-Zn+/-Au) Minfile 082ESW043 Within Tenure 1061735 Mineralization on the property is confined to four or more bluish quartz veins, varying in attitude and size. Minerals within the veins include galena, sphalerite, pyrite and pyrrhotite. Free gold is associated with galena. The veins are hosted mainly by argillaceous quartzite and lesser calcareous greenstone. Feldspar porphyry dikes are reported halfway between the two main workings on the claim. The relationship between the dikes and veins, however, is unknown. EUREKA prospect (Au-quartz veins; Polymetallic veins Ag-Pb-Zn+/-Au) Minfile 082ESW044 Within Tenure 1061735 Mineralization in the vein is reported to consist of pyrite, chalcopyrite, galena and mariposite. The dump from the main shaft consists of quartz with pyrite and minor chalcopyrite. The dump is estimated to contain 1814 tonnes of variably mineralized quartz. Nine samples from this dump were assayed in 1986 yielding values ranging from 0.03 to 12.31 grams per tonne gold and an average of 4.59 grams per tonne gold (Assessment Report 16168). The smaller shaft dump is reported to yield 9.0grams per tonne gold (Assessment Report 16168).

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Mineralization: Camp Mckinney Property(cont'd) SAILOR prospect (Polymetallic veins Ag-Pb-Zn+/-Au; Polymetallic manto Ag-Pb-Zn) Minfile 082ESW045 Within Tenure 1061735 Mineralization on the Sailor and Sailor fraction is hosted in quartz veins up to 1 metre wide with accessory calcite in veinlets and chloritic partings. Quartz-carbonate, sericite and chlorite alteration are closely associated with these veins. Galena, chalcopyrite, sphalerite and native gold comprise vein mineralogy and occur as fine grained disseminations comprising less than 1 per cent of the veins. Traces of arsenopyrite are reported associated with quartz-carbonate alteration surrounding the veins. Most quartz specimens with high grade gold and silver contain 1 to 2 per cent galena and sphalerite, and 2 to 5 per cent pyrite. Native gold occurs as fine specks in quartz (Assessment Report 17815). In the Sailor dump, there are considerable quantities of carbonate altered rock bearing mariposite and possibly annabergite. This contains anomalous quantities of nickel and chromium (Assessment Report 17815). At the Sailor shaft, mineralization is confined to a 1 to 2 metre wide quartz vein which strikes 045 degrees. On the lower level the vein is reportedly very broken up. Material taken from the dump indicates that minerals present consist of galena, sphalerite, pyrite some of which is shattered and veined with quartz, and rarely chalcopyrite. Grab sample 42974, taken during prospecting in 1987, of galena-bearing quartz from the Sailor dump assayed 15.10 grams per tonne gold and 34.0 grams per tonne silver (Assessment Report 15519). Sampling in 1988 yielded similar values. Sample CM8807 yielded 2.49 grams per tonne gold, 19.7 grams per tonne silver, 0.95 per cent lead and 0.16 per cent zinc (Assessment Report 17815). On the Sailor Fraction, just north of the Sailor corner post and west of the Sailor shaft, a quartz mass 2.1 by 1.5 metres trends east. Here, sparse pyrite and rare chalcopyrite are the only mineralization indicated in dump samples. Flat lying faults have displaced the lower segment of the vein to the south. West of this massive quartz vein on a small creek, another vein is reported. It is about 21 metres in length, strikes 110 degrees and dips near vertical. The vein is up to 1.5 metres wide and consists of white-coarsely crystalline to bluish quartz containing pyrite and sparse chalcopyrite, near its eastern end. A sample of this material from a dump yielded 2.05 grams per tonne gold and 13.7 grams per tonne silver (Bulletin 6, page 18). A dump sample, taken during an exploration program by the Gold Hill Syndicate in 1986, from the best mineralized quartz yielded 8.9 grams per tonne gold and 27.4 grams per tonne silver (Assessment Report 16168). MINNIE HA HA prospect (Au-quartz veins) Minfile 082ESW046 Within Tenure 1061735 Mineralization consists of minor pyrite and galena within a 15 centimetre to 1.37 metre wide quartz vein striking 280 degrees and dipping 80 degrees north. Trace chalcopyrite, sphalerite and free gold were found in dump samples in 1988. The vein is reported traceable for 15 metres on surface. Several samples taken from the Minnie-Ha-Ha dump in 1988 yielded anomalous results. The best sample, Sample CM8803, yielded 11.9 grams per tonne gold, 30.0 grams per tonne silver, 0.63 per cent lead, 0.16 per cent zinc and 0.04 per cent copper (Assessment Report 178155). Sample CM8806, a 30- centimetre chip sample taken from the Minnie-Ha-Ha shaft, yielded 4.7 grams per tonne gold, 3.3 grams per tonne silver, 0.07 per cent zinc, 0.03 per cent lead and 0.01 per cent copper (Assessment Report 178155). The vein width was 30-centimetres with a strike of 116 degrees and a dip of 81 degrees northwest. The footwall consisted of white bull quartz. The hangingwall contained chloritic partings with 5 per cent disseminated pyrite, 0.5 per cent sphalerite, trace galena and chalcopyrite.

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Figure 10. The Minniehaha Mine at Camp McKinney (From BC Archives )

GOLD STANDARD prospect (Au-quartz veins; Polymetallic veins Ag-Pb-Zn+/-Au) Minfile 082ESW128 Within Tenure 1061735 Mineralization on the Gold Standard claim of the Gold Standard Group is within small quartz lenses and stringers, and an irregular quartz lens. Stringers and lenses intersected in underground workings carried disseminated pyrite and minor coarsely crystalline galena. The lens is 1.8 to 2.4 metres wide and hosted by black schist. The lens is parallel to the foliation of the schist. Smaller veins of quartz occur in the wallrock. Approximately 122 metres downstream from the lens along Jolly (Rock) Creek is a small quartz vein reportedly containing free gold. Still further downstream, along Rock Creek, a 30 centimetre wide quartz vein containing pyrite and galena, striking east and dipping 45 degrees north, outcrops. ANARCHIST prospect (Au-quartz veins; Polymetallic veins Ag-Pb-Zn+/-Au) Minfile 082ESW213 Within Tenure 1063217 Mineralization consists predominantly of pockets and blebs of pyrite and fine to coarse-grained galena in blebs up to 5 centimetres across. Small amounts of native gold, sphalerite, chalcopyrite and tetrahedrite are also reported in a white or locally rose quartz gangue. In 1894, a 41-centimetre ore streak was reported discovered on the main vein. In 1981, gold values obtained from assay samples of drill core were low in both gold and silver overall (Assessment Report 9686). The best silver values was from the 3 metre interval from 22.2 to 25.2 metres in drillhole #2. The sample yielded 12.3 grams per tonne silver but only trace gold (Assessment Report 9686).

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Mineralization: Camp Mckinney Property Area(cont'd) GRANITE past producer (Au-quartz veins) Minfile 082ESW214 Within Tenure 1063271 On the Granite claim, it is reported that a quartz vein carried chalcopyrite, galena, pyrite and minor sphalerite. The vein is 140 centimetres wide and strikes 290 to 330 degrees in the main shaft. The vein has been traced 41 metres north to a second shallower shaft in granodiorite hostrock. In 1985, a sample was taken from 4.6 metres deep in the main shaft. This sample (582060) yielded 8.2 grams per tonne gold (Assessment Report 14609). On the Banner claim, another quartz vein is hosted in granodiorite. Three samples were taken by the Rock Creek Joint Venture Syndicate in 1981. The best sample, a 60-centimetre chip across the vein, yielded 0.24 gram per tonne gold and 2.81 grams per tonne silver (Assessment Report 12389). BIG BUG showing (Au-quartz veins) Minfile 082ESW216 Within Tenure 1061715 Four samples were taken from the Big Bug dump in 1991, however, assay results for gold and silver were not significant (Assessment Report 21464). Sample R2-91001WH yielded 0.07 gram per tonne gold. 4 grams per tonne silver and 0.03 per cent zinc (Assessment Report 21464). Four samples were taken from the Big Bug dump in 1991, however, assay results for gold and silver were not significant (Assessment Report 21464). Sample R2-91001WH yielded 0.07 gram per tonne gold. 4 grams per tonne silver and 0.03 per cent zinc (Assessment Report 21464). PANDRE prospect (Au-quartz veins) Minfile 082ESW218 Within Tenure 1061735 Free gold, pyrite and galena comprised the vein mineralogy (Minister of Mines Annual Report 1899, page 774). Assay values were reported to have been very high (Minister of Mines Annual Report 1899, page 774). SLAMET prospect (Au-quartz veins) Minfile 082ESW220 Within Tenure 1061735 Disseminated pyrite was the only mineralization observed (Assessment Report 15005). A grab sample taken from this vein in 1986 yielded 9.05 grams per tonne gold (Assessment Report 15005). ARGEN prospect (Intrusion related pyrrhotite veins; Au-quartz veins) Minfile 082ESW222 Within Tenure 1064559 This shaft intersected a shear zone striking 125 degrees and dipping 80 degrees to the southwest. The shear zone varies from 15 to 61 centimetres wide and is rusty. Quartz in the shear zone is mineralized with pyrite and galena (Assessment Report 8928). A 36-centimetre chip sample (23188) taken from freshly blasted vein material in 1980 yielded 2.4 grams per tonne gold, 48.0 grams per tonne silver and 1 per cent lead (Assessment Report 8928).

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Prospecting and Rock Sampling Purpose The purpose of the program was to locate any location of a geological prospect that may have the potential to be developed to an economic resource. Any indication of mineralization may indicate a potential concealed polymetallic or porphyry type deposit. Prospecting Prospecting of area; orange flagging and marking of sample sites. Multiple photos taken of samples and areas. GPS coordinates were taken, and all samples recorded and mapped. Prospecting notes, operating with equipment (Truck, GPS, Tools and sampling). Twenty--five samples were taken and 10 samples were assayed. Field notes on the samples are shown in Appendix II. Sampling Bakus, McKinney, Bradshaw took 25 samples from various locations throughout the property area. Points of interest (access) were also noted. Laurence Sookochoff BSc P Eng. performed the historic research data compilation, structural report, mapping and technical report preparation. 10 dump samples were assayed. Bag size samples were taken between one-half and four kilograms (rock float samples heavy mineral soil samples.) Results Prospecting descriptions, and sample location maps with selected assays, are within the report. Complete assays are shown in Appendix 1 as Bureau Veritas Certificate of Analysis VAN 19000909-1. The sample preparation code PRP70-250 and the analytical code AQ200 descriptions as reported on the first page of the Certificate and as contained within the Bureau Veritas Fee Schedule publication booklet is as follows: PRP70-250 Crush 1 kg to ≥70% passing 2mm ... Pulv 250 g ≥85% 75µm AQ200 Sample splits of 0.5 g are leached in hot modified Aqua Regia. Analysis by ICP ES/MS* *ICP ES/MS Inductively Coupled Plasma Emission Spectroscopy/Mass Spectrometry Table 2. Assays* of 10 samples taken from the McKinney property

Sample ppm Mo ppm Cu ppm Ag ppm As ppb Au M-2 0.2 0.4 <0.1 <0.5 0.6 M-4 0.5 5.9 <0.1 <0.5 <0.5 M-5 0.1 0.2 <0.1 <0.5 0.8 M-7 0.7 77 0.2 0.6 1.4 M-8 0.1 178.1 0.1 0.8 2.5 M-9 0.6 69.9 0.1 1.1 1 M-10 5.9 40 <0.1 1.7 2 M-19 17.5 50.9 0.1 6.5 <0.5 M-20 9.9 57.9 0.1 6.3 0.8 M-22 2.3 9.8 0.2 2.8 2.5

* See Appendix I for complete assays

Sookochoff Consultants Inc. August 12, 2019 Page 34 of 51 Bill McKinney McKinney Property Event 5724829 2019 Exploration Program (cont'd) Figure .11 Index Map showing indicated cross-structures, Minfiles, and sample locations on Tenure 1061040 (Base map: Google Earth)

Figure 12. Northwest sample locations* (Base map from MapPlace)

D * see Figure 11 for location on McKinney Property

Sookochoff Consultants Inc. August 12, 2019 Page 35 of 51 Bill McKinney McKinney Property Event 5724829 2019 Exploration Program (cont'd) Figure 13. Mid Sample* locations* (Base map from MapPlace)

**see Figure 11 for location on McKinney Property. See Appendix 1 for all assay values. * samples and assays shown were the only samples assayed, Figure 14. South sample** locations* (Base map from MapPlace)

Sookochoff Consultants Inc. August 12, 2019 Page 36 of 51 Bill McKinney McKinney Property Event 5724829 2019 Exploration Program (cont'd) Figure 15. East sample** locations* (Base map from MapPlace)

**see Figure 11 for location on McKinney Property. See Appendix 1 for all assay values. * samples and assays shown were the only samples assayed,

STRUCTURAL ANALYSIS a) Purpose The purpose of the structural analysis was to delineate any area of relative major fault intersections that could be the centre of maximum brecciation and be depth intensive to provide the most favourable feeder zone to any residual fluids from a potentially mineral laden reservoir source. b) Method A DEM image hillshade map downloaded from MapPlace was utilized as the base map for the structural analyses of Tenure 1061044. A total of 65 structurally indicated lineaments were marked, compiled into a 10 degree class interval, and plotted as a rose diagram. c) Results Three cross-structural locations, A, B, & C, were delineated from indicated major northerly, northwesterly, and northeasterly trending structures.

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Table 3. Approximate location of cross-structures (UTM-11NAD 83) Cross-structure UTM East UTM North Elevation (m) A 339,713 5,543,194 1,435 B 339,615 5,442,480 1,363 C 339,123 5,442,989 1,481

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STATISTICS

Axial (non-polar) data kappa = 0.57 No. of Data = 65 (von Mises concentration param. estimate) Sector angle = 10° Scale: tick interval = 2% [1.3 data] Resultant length = 17.87 Maximum = 15.4% [10 data] Mean Resultant length = 0.2749 Mean Resultant dir'n = 143-323 [Approx. 95% Confidence interval = ±31.8°] 'Mean' Moments: Cbar = 0.0794; Sbar = -0.2632 (valid only for unimodal data) 'Full' trig. sums: SumCos = 5.1639; Sbar = - ______17.1059 Mean Resultant dir'n = 143.4 - 323.4 Mean resultant of doubled angles = 0.2897 Circ.Median = 134.0 - 314.0 Mean direction of doubled angles = 178 Circ.Mean Dev.about median = 35.1° Circ. Variance = 0.28 (Usage references: Mardia & Jupp, Circular Std.Dev. = 46.04° 'Directional Statistics', 1999, Wiley; Circ. Dispersion = 4.70 Fisher, 'Statistical Analysis of Circular Data', Circ.Std Error = 0.2689 1993, Cambridge University Press) Circ.Skewness = 1.20 Note: The 95% confidence calculation uses Circ.Kurtosis = -6.65 Fisher's (1993) 'large-sample method'

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INTERPRETATION, CONCLUSIONS, and RECOMMENDATIONS The 2018 exploration program of sampling, and prospecting exploration program on the McKinney Property was successful in that samples were obtained from locations that may indicate the surficial geological expression of a Cariboo-Amelia type (Minfile 082ESW020) resource where recovery included 2,538,101 grams of gold, 1,008,979 grams of silver, 51,393 kilograms of lead and 89,875 kilograms of zinc over its intermittent 68 year mine life, from 1894 to 1962. Three formerly productive mines, including the Cariboo-Amelia, are enclosed within the McKinney property (Figure 5). The McKinney property's potential for a mineral resource is not only indicated by the three inclusive former past productive properties, the Gold Hill, the Granite, and the Gold Standard, which are all Cariboo-Amelia type of a polymetallic vein and/or a gold quartz mineral deposit, but by eight polymetallic and/or gold quartz mineral prospects, and by one gold quartz mineral showing. The greater prospective resource potential of the McKinney property would be in a concealed porphyry, bulk tonnage mineral resource which is indicated by the polymetallic and the gold quartz veins which are commonly associated with a mineralized porphyry (Figure 19). Although there is no surficial indication of a porphyry on the Property, a surficial indication might be manifest at a cross-structural location which would be the most facilitative feeder zone for the venting of hydrothermal fluids and the creation of breccia pipes. Three cross-structural locations have been delineated where the surficial indications of a potential concealed mineralized porphyry may be exposed. The geological indications that should be prospected for and noted are signs of hydrothermal breccias, alteration types, and mineralization. Samples of rocks indicating the potential would be subject to a multi-element analysis for indicatory or pathfinder minerals such as mercury and arsenic. Unfortunately, the prospecting and sampling program did not cover the cross-structural locations, However, was successful in locating areas of potential mineralization. The rock samples containing quartz veins with alteration may be locations that merit additional localized prospecting and/or soil sampling. These rock sample indicated areas include sample locations M-05, M-08, M-19, and M-25. Rock samples that were assayed from two of these locations showed anomalous copper and gold (M-8: 178.1 ppm Cu; 2.5 ppb Au), and anomalous molybdenum and copper (M-19: 17.5 Mo, 50.6 ppm Cu), would be the priority locations to explore Respectfully submitted Sookochoff Consultants Inc.

Laurence Sookochoff, PEng

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SELECTED REFERENCES Hedley, M.S. 1940 - Geology of Camp McKinney and the Cariboo-Amelia Mine, Similkameen District. Bulletin No. 6. British Columbia Department of Mines. MapPlace – Map downloads MtOnline - MINFILE downloads. 082ESW018 – FONTENOY 082ESW214 – GRANITE 082ESW019 – WATERLOO 082ESW215 – KAMLOOPS 082ESW020 – CARIBOO-AMELIA 082ESW216 – BIG BUG 082ESW043 – GOLD HILL 082ESW217 – WIARTON 082ESW044 – EUREKA 082ESW218 – PANDRE 082ESW045 – SAILOR 082ESW220 – SLAMET 082ESW046 – MINNIE HA HA 082ESW222 – ARGEN 082ESW128 – GOLD STANDARD 082ESW213 – ANARCHIST

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STATEMENT OF COSTS Field work was performed on the McKinney Property between November 17, 2018 and January 1, 2019 to the value as follows: Structural Analysis L. Sookochoff, PEng November 18 - 25, 2018 (cumulative time) 3 days @ $1,000.00 ------$ 3,000.00 Prospecting and Sampling Labour Bradshaw: November 17-18, 2018 2 days @ $300.00/day ------600.00 B. McKinney: November 16-19, 2018 4 days @ $450.00/day ------1,800.00 J. Bakus: November 18, 2018 1 day @ $300.00/day ------300.00 2,700.00 Travel/Transportation Vancouver to property return 920 km Kamloops to property return 590 km 1,510 kilometres @ $0.68 ------1,026.80 Exploration Equipment GPS, , clinometer, electronics radios, etc ----- 40.00 Spot Locator's safety equipment and supplies - 40.00 Bear spray, axes, mallets, pry bars, etc ------40.00 Chainsaw ------40.00 160.00 Food/Lodging 5 man days @ $ 125.00 ------625.00 Assays ------324.00 Report L. Sookochoff, PEng ------3,000.00 Maps ------500.00 $ 11,335.80 ======

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CERTIFICATE

I, Laurence Sookochoff, of the City of Vancouver, in the Province of British Columbia, do hereby certify: That I am a Consulting Geologist and principal of Sookochoff Consultants Inc. with an address at 120 125A-1030 Denman Street, Vancouver, BC V6G 2M6. I, Laurence Sookochoff, further certify that: 1) I am a graduate of the University of British Columbia (1966) and hold a B.Sc. degree in Geology. 2) I have been practicing my profession for the past fifty-three years. 3) I am registered and in good standing with the Professional Engineers and Geoscientists British Columbia. 4) The information for this report is based on information as itemized in the Selected Reference section of this report, from exploration work done in the Camp McKinney area. 5) I have no interest in the McKinney Property as described herein.

Laurence Sookochoff, P. Eng.

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FIELD CREW QUALIFICATIONS John Bakus: 10 years prospecting experience. Bill McKinney: 10 years prospecting experience. Lance Bradshaw: five years prospecting experience.

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Appendix I

Sample Assays

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Appendix II

Sample Locations and Descriptions

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Camp 2018 Sample IS In Situ, HM Heavy Mineral/Dump McKinney Types FB Float, POI Point of interest/Access

Sample Notes Assayed * Lat Lon M-01 49.11458 -119.1757 FB Igneous , speckled, mica non oxidized M-02* 49.11451 -119.17535 FB Calcite banded, soft green coloring M-03 49.11447 -119.17498 FB Greywacke oxidized fine grained porous M-04* 49.11466 -119.17505 FB Igneous course grained black specs M-05* 49.11465 -119.17526 FB Metamorphic multi quartz banding layered M-06 49.11463 -119.17551 FB Igneous large crystals no visible sulphides M-07* 49.10412 -119.17717 FB Igneous heavy iron staining dark green heavy M-08* 49.10452 -119.17659 FB Sheared amphibolite fine grained chalcopyrite throughout M-09* 49.10452 -119.17757 FB Igneous slight iron staining iron leaching M-10* 49.10514 -119.17725 FB Igneous small 1 mm stringers iron staining vuggy M-11-18 49.11108 -119.19054 HM Heavy Mineral 08 samples 1 KG Creek area M-19* 49.11669 -119.19672 FB Igneous quartz layering rusty no visible pyrite M-20* 49.11678 -119.19657 FB Metamorphic?? Iron cavities heavy no sulphides M-21 49.11683 -119.19665 FB Igneous quartz orange iron staining blue colorization folding M-22* 49.11664 -119.19666 FB Metamorphic Multi quartz blocking porous leaching M-23 49.11611 -119.19955 FB Granodiorite fine grained speckled porous M-24 49.11578 -119.19953 FB Ultramafic fine grained vuggy no oxidation M-25 49.11597 -119.19927 FB Igneous quartz some iron staining some black specs

MP -01 49.11042 -119.17767 POI Lower Mine Road West MP-02 49.11121 -119.20343 POI Road North to Main Road MP-03 49.11624 -119.19568 POI North Road to Gold Hill Blocked 200 M in

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Appendix III

Photos

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Access Road to Samples

Camp McKinney

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