Ministry of Energy and Mines Assessment Report BC Geological Survey Title Page and Summary

TYPE OF REPORT [type of survey(s)]: Geological TOTAL COST:

AUTHOR(S): Rachel Morneau SIGNATURE(S): R. Morneau

NOTICE OF WORK PERMIT NUMBER(S)/DATE(S): YEAR OF WORK: 2016

STATEMENT OF WORK - CASH PAYMENTS EVENT NUMBER(S)/DATE(S): 5612622

PROPERTY NAME: Chew Tung Hydraulic

CLAIM NAME(S) (on which the work was done): Chew Tung Hydraulic

COMMODITIES SOUGHT: Gold

MINERAL INVENTORY MINFILE NUMBER(S), IF KNOWN:

MINING DIVISION: NTS/BCGS: 093 H04 53 o 03 '38.67 " 121 o 33 '53.44 " LATITUDE: LONGITUDE: (at centre of work)

OWNER(S): 1) Anthony Charls Derrien 2)

MAILING ADDRESS: 6202 190th St. Surrey, BC, V3S 8H7

OPERATOR(S) [who paid for the work]: 1) same 2)

MAILING ADDRESS:

PROPERTY GEOLOGY KEYWORDS (lithology, age, stratigraphy, structure, alteration, mineralization, size and attitude): Terrane, gold, Proterozoic, Paleozoic, greenschist, clastic sedimentary, carbonates, volcanic, Cariboo Group, argillite, phyllite

REFERENCES TO PREVIOUS ASSESSMENT WORK AND ASSESSMENT REPORT NUMBERS:

Next Page TYPE OF WORK IN EXTENT OF WORK ON WHICH CLAIMS PROJECT COSTS THIS REPORT (IN METRIC UNITS) APPORTIONED (incl. support)

GEOLOGICAL (scale, area)

Ground, mapping 2.5 km 1042691

Photo interpretation

GEOPHYSICAL (line-kilometres) Ground

Magnetic

Electromagnetic

Induced Polarization

Radiometric

Seismic

Other

Airborne

GEOCHEMICAL (number of samples analysed for...)

Soil

Silt

Rock

Other

DRILLING (total metres; number of holes, size)

Core

Non-core

RELATED TECHNICAL

Sampling/assaying

Petrographic

Mineralographic

Metallurgic

PROSPECTING (scale, area)

PREPARATORY / PHYSICAL

Line/grid (kilometres)

Topographic/Photogrammetric (scale, area)

Legal surveys (scale, area)

Road, local access (kilometres)/trail

Trench (metres)

Underground dev. (metres)

Other

TOTAL COST:

2016 Reconnaissance Geological Mapping

On Chew Tung Hydraulic Claim

Cariboo Mining Division

NTS Map Sheet 093 H04

53° 3'38.67"N latitude 121°33'58.44"W longitude

UTM 596083m E 5879988m N

Tenure 1042691

Prepared for Anthony Charls Derrien Owner 6202 190th Street Surry, V3S 8H7

By Rachel Morneau, BA, PGDip Cariboo Assessments & Geoservices 2325 Bowman Cresent Wells, British Columbia V0K 2R0

July 2016

TABLE OF CONTENTS

TABLE OF CONTENTS ...... 1 LIST OF FIGURES ...... 1 LIST OF TABLES ...... 1 APPENDICES ...... 1 INTRODUCTION ...... 4 PROPERTY DESCRIPTION AND LOCATION ...... 4 GEOLOGICAL SETTING ...... 4 HISTORY ...... 7 2016 MAPPING AND RECONNAISANCE ...... 12 DISSCUSSION AND RECOMMENDATIONS ...... 14 STATEMENT OF COSTS ...... 15 STATEMENT OF QUALIFICATIONS ...... 16 REFERENCES ...... 17

LIST OF FIGURES Fig 1 Location Map………………………………………………………….…………....2 Fig 2 Claim Map…………………………………………………………….…….….…..3 Fig 3 Bonanza Ledge Photo…………………………………...……………………….…8 Fig 4 Bowman’s Map of Williams Creek………..…………………………………...…..9 Fig 5 Snapshot of Bowman’s Map of Williams Creek………………………….……..…10 Fig 6 Nugget Photo from Lowhee Gulch…………………………………………………11 Fig 7 Google Earth Image Illustrating Historic Placer Operations………………...……..12 Fig 8 Outcrop photo………………………………………………………………………13 Fig 9 Outcrop photo…………………………………………………………………...…13

LIST OF TABLES Table 1 Local Creeks and Gold Yields…………………………………………………...9

APPENDICES Appendix A: Bedrock Maps

Highway Project Location Map Chew Tung Hydraulic Project Tenure Outline British Columbia, Canada Figure 1

INTRODUCTION

Cariboo Assessments & Geoservices was contracted by Anthony Charls Derrien, 100% owner of the Chew Tung Hydraulic claim (tenure number 1042691) to map outcrops, high channels, gravel deposits that have possibly been exposed by the expansion of new logging roads on Cow Mountain and prepare a technical report on the Chew Tung Hydraulic claim. Work scheduled to commence June 24th and be completed by July 8th but was extended slightly to try to complete the project. The claim is in good standing until January 26th 2017.

PROPERTY DESCRIPTION AND LOCATION

The Chew Tung Hydraulic claim is approximately 3km south of Wells on Cow and Richfield Mountains and is just over 1302 hectares. It is easily accessible by 4x4 vehicles or ATV, during the dry season, by the Jack of Clubs Creek Service Road located approximately 4km west of Wells off Highway 26.

The current project area lies south of Jack of Clubs Lake, situated within the Quesnel Highlands on the eastern edge of the Interior Plateau. The topography is moderate, rising from about 1200m at Wells to just over 1700m on Cow Mountain. The climate consists of cool summers and cold winters due to the moderately high altitude of the Wells area and is wet throughout the year, with a mean annual precipitation of 100 cm that includes a significant amount of snow, especially at the higher elevations. The area does experience Chinook conditions during the winter months and the climate becomes very mild for brief periods of time. Snowfall in the area is moderate to heavy. In the summer the area experiences fairly consistent rain in early and late summer with extended dry hot spells in between.

Summits in the immediate area are generally rounded, having been glaciated by continental ice sheets during the Pleistocene Epoch (Holland, 1976, Hart, 2001). Ice direction is generally to the northwest near Wells and glacial till is the most widespread surficial deposit in the area. The Wells area is generally well forested. Hillside slopes are dominated by spruce and sub-alpine fir, accompanied by alders and other deciduous foliage on lower wetter slopes flanking river valleys.

GEOLOGICAL SETTING

The geology of the Cariboo district has been presented in reports and maps by Bowman (1889, 1895), Johnston and Uglow (1926), Hanson (1935), Sutherland Brown (1957), Struik (1988) and Levson and Giles (1993). The Chew Tung Hydraulic Project lies within the Kootenay (Barkerville) Terrane, part of the Omineca Belt of the Canadian Cordillera (cf. Struik; 1986; 1988) The Barkerville Terrane consists of a Late Proterozoic and Paleozoic sequence of continental shelf and slope deposits developed adjacent to the craton of Ancestral North America and includes clastic sedimentary rocks along with lesser amounts of volcanic rocks and carbonates. It is structurally the lowest exposed stratigraphic sequence in the area and is more deformed and metamorphosed than adjacent terrains.

Rocks of the Snowshoe Group in the Wells area have been metamorphosed to lower greenschist facies, generally of lower metamorphic grade than other sequences in the Barkerville Terrane. Rocks of the Barkerville Terrane were subjected to an early period of ductile deformation that resulted in westward directed, asymmetrical folds plunging shallowly to the northwest. Post metamorphic open folds with upright cleavage are superimposed on earlier structures. During Late Cretaceous to Early Tertiary time, the terrane was disrupted by northwest trending dextral strike-slip faults such as the Willow Fault, a major strike slip fault of unknown displacement that has been mapped through Mount Tom, Island Mountain, Cow Mountain and Richfield Mountain in the Wells area (Struik, 1988)

A wide spread mantle of glacial drift overgrown with trees and vegetation, limits the, outcrop of bedrock largely to the tops of ridges, divides and individual mountains and along steep slopes of the more prominent rivers and streams. Outcrops of bedrock are not extensive even along the ridges and mountain tops. Local bedrock outcrops are found in the bottom of some of the incised streams and along the steep north side of Cow and Richfield Mountains. The remainder of the area contains a fairly thick mantle of glacial drift.

Stratigraphy

The Cariboo group, which underlies the area of the claim, is composed of clastic rocks with lesser amounts of carbonate rocks. The rocks have been subjected to a low-grade regional metamorphism and intense deformation. The deformation has impressed a marked secondary foliation on most all the clastic rocks and some carbonate rocks. Despite the effects of deformation and regional metamorphism, the rocks still commonly show original bedding and other sedimentary features. Many of the rocks are difficult to name accurately because of their original sedimentary and subsequent metamorphic character. Many clastic rocks of the Cariboo group are composed of poorly sorted sediments of grains much larger than average. It is very difficult to assign a name to this type of rock even if not metamorphosed. Most of the clastic rocks and even some of the limestones are schistose, however, in any one unit the degree of schistosity may vary, depending on structural position. For example, an argillaceous rock may range from an argillite through phyllite to a true schist or graphitic schist as it is traced from an open fold to a tight fold or its proximity to fault structures. In many places along the northerly trending fault zones, as mapped by different geologists, argillites are changed to a very soft and possibly pure graphitic schist.

The thickness of the formations in the Cariboo group cannot be measured directly and estimates are subject to considerable error due to poorness of exposures and the intricacy of structure. In many exposures of bedrock, the bedding cannot be distinguished from schistosity with any degree of certainty. The folding is known in general but the details are very rarely recognizable and measurements are liable to include duplications. According to A. Sutherland Brown in Bulletin No. 38, the thickness in this area is deemed to be less than 1200 metres. The age of the Cariboo group is now known to be Early Cambrian and younger. Earlier publications by Bowman, Johnston and Uglow, and George Hanson placed the age of the Cariboo group or series as Pre-Cambrian in age. No fossils have been found in the group in this general area and the age has been assigned on the basis of archaeocyathids and trilobites collected at Turks Nose Mt., Kimball Creek, and other localities within a thick limestone which has been traced into this general area and identified with the Cunningham limestone, which is the basal member of the Cariboo group.

Hydrothermal alteration has had a more severe effect on the various formations of the Cariboo group than the regional metamorphism. The alteration has obliterated all sedimentary structures and also cleavage that is common in the unaltered limestone. The distribution of the alteration is patchy and in some instances, seems to bear an areal relation to major faults primarily the more persistent northerly trending faults in the area. The rocks in the immediate area of the claims are argillites, quartzose phillite, grey to brown micaceous quartzite, slate, and thin lenses of grey limestones of the Snowshoe and Midas Formations of the Cariboo group.

Structure

The rocks of the Cariboo group within the claim block lie on the northeastern limb of a large northwesterly trending anticline or possible anticlinorium. The antiformal axis, as mapped by most observers, is situated immediately southwest of the claim block near the top of Mt. Burns, Mt. Amador and Mt. Nelson, with a N 50°-60° west bearing. The rocks strike northwest and dip to the northeast. In the main, the folding within the area of the claim seems simple, but in some places minor folds can be observed where the dip changes to 45° and some local evidence of overturning to the southwest. Many of the folds in the area have their original stratigraphic order disrupted by shearing, rupture and flowage. Some of the folds are so compressed that the actual texture cannot be recognized. The rocks of the Cariboo group have been folded at least twice. The more intense folding took place before the younger Slide Mountain group was laid down. It is rarely possible to identify the second generation folds in the Cariboo group, due partially to the less intense folding in the youngest folds.

Schistosity and cleavage are well developed in the Cariboo group in the area of the claims. The difference in the development of the two features is due primarily to the intensity of folding and mineral composition. The characteristic rocks of the Cariboo group are phyllite and micaceous quartzite.

Faults are very common in the area. Several fairly large and continuous northerly trending faults have been mapped in the area. Several major northerly trending faults are mapped by A. Sutherland Brown in this general area and are described in Bulletin No. 38. The Lowhee, Rainbow and No. 1 faults were all mapped and studied in some detail in the underground workings of the Cariboo Gold Quartz Mine. Near these faults there is also a preponderance of quartz veins of the transverse and diagonal types. Most of these veins contain sulphides and free gold. In the entire Barkerville Gold Belt, extending from the Island Mountain Mine in the northwest to the Round Mountain area in the southeast, there is a total of 13 northerly trending faults which have been identified and mapped. The northerly trending faults strike between north and north 20 degrees east and dip steeply to the east. Most are normal faults which have some strike-slip. Other faults with similar orientation or surface expression have been subject to large strike-slip and much less dip-slip. Johnston and Uglow, in Memoir 149, 1926, describe a northeast trending fault near the top of Island Mountain, immediately northwest of the lode mines in the Wells area, as having a horizontal displacement to the southwest of 4 miles. They further say that this has displaced the Barkerville Gold Belt to the southwest some 4 miles to near the Willow River. Stuart S. Holland, in Bulletin #26, recommends prospecting for gold mineralization along the three northerly trending fault zones he mapped in the Stanley area southwest of the claims.

HISTORY

The Chew Tung Hydraulic claim is situated within the Cariboo Gold Belt, a world-class producer of gold that has had a history of mining dating from the Cariboo in the 1860's. The region is estimated to have produced 2.6 million ounces of placer gold.

The majority of the placer gold was produced during the gold rush which started around 1861 and tapered off substantially near 1898 when the gold rush started in the Yukon. There was a slight resurgence of placer gold production in this area during the depression of the thirties. Lode gold production started in 1933 from the Cariboo Gold Quartz Mine at Wells, B.C. The Cariboo Gold Quartz Mine took over the Island Mountain Mines on the other side of the Jack of Clubs Lake, and during the period January 10, 1933 through April 15th, 1967, when the mine was closed down, some 2,929,246 tons of ore grading an average of 0.4 02. per ton produced a total of 1,253,683 ounces of gold. The foregoing figures are from the Canadian Mines Handbook 1982-83, page 337. The original Mosquito Creek Mine produced gold from replacement type ore bodies in contrast to the gold produced from quartz veins with pyrite and gold in the original Cariboo Gold Quartz Mine.

The project area is adjacent to the past producing Cariboo Gold Quartz Mine, situated south of Jack of Clubs Lake, which produced 1.68 million tons grading 0.37 oz/ton Au from 1933 to 1959, primarily from quartz veins. The Island Mountain/Aurum Mines (1934-1967) and the Mosquito Creek Gold Mine (1980- 1983) produced 603,800 ounces (18.8 tonnes) of gold from approximately 1.35 million tons (1.22 million tonnes) of ore (Hall, 1999) from quartz-type ore with an average grade of 0.35 ounces per ton (12.0 g/t) gold and pyrite-type ("replacement") ore with average grade of 0.67 ounces per ton (23.0 g/t) gold. The Bonanza Ledge Zone was discovered by International Wayside Gold Mines Ltd. In March of 2000 which is located about 3.5 km southeast of Wells on the southwestern flank of Barkerville Mountain directly . The Bonanza Ledge Zone contains significant gold grades associated with pyrite mineralization developed in a strongly dolomite-sericite-silica-pyrite altered turbidite sequence in the footwall of the B.C. Vein, a strike vein from which several pyritic ore shoots were historically mined from the Cariboo Gold Quartz workings. Production from the Cariboo Gold Quartz workings on Cow Mountain, 2 km northwest of the Bonanza Ledge Zone, was obtained from several zones including the No. 1, Tailings, Rainbow, Sanders and Pinkerton Zones.

Figure 3: Bonanza Ledge Mine taken from a claim boundary (photo by Rachel Morneau)

Placer mining in the Cariboo began after the decline of the . By 1860 the first miners reached the Cariboo in the areas of Likely and Keithley Creek. In 1861 William ‘Dutch Bill’ Dietz discovered gold on the creek that was named after him in his honor, Williams Creek. Ironically, he staked one of the poorest claims on what would be one of the richest gold bearing creeks. Many more gold discoveries all occurred during this year proving the extent of the Cariboo Goldfields.

Placer mining evolved in BC in a series of phases. By 1865 the shallow diggings in the Cariboo were becoming depleted and the time of individual miners and ability to strike it rich by hand were coming to an end. The next phase incorporated dredges, huge pumps and expensive machinery and even though hydraulic mining methods and dredging have been disallowed, placer mining methods have changed very little in the last 100 years other than increased technological advancements in the machinery.

Several famous past placer operations operated in the areas adjacent to the claim, such as at Williams Creek, Lowhee Gulch, Stouts Gulch, Emory Gulch, Walker Gulch, and Mink Gulch to name a few, produced tens of thousands of ounces of gold.

Table 1. Local creeks and gold yields

Creek Name Recorded placer gold ounces recovered (in troy ounces) Between 1854-1960 Williams Creek 86,000 Lowhee Creek 75,000 Stouts Gulch 16,000 Jack of Clubs Creek and tributaries (Victoria, Approx. 7,100 Stoney ect) Black Jack Gulch 900 Walker Gulch 500 Mink Gulch 350 Emory Gulch 100 Adapted from information in Cariboo Gold Strike, K.K. MacGowan

Figure 4: Bowman’s map taken from surveys done in 1878, 1885-86 of the Williams Creek area illustrating historical past placer operations several of which the origins can be traced from either Cow or Richfield Mtns

Figure 5: snapshot of the above Bowman map Williams Creek, as mentioned above, was discovered by William “Dutch Bill” Dietz in 1861. By 1862, 3,071 claims had been staked along Williams Creek. It was also in this year William “Billy” Barker made his famous claim at 52 feet below the surface along Williams Creek. The richest diggings in the Cariboo were on Williams Creek giving rise to the towns of Richfield, Barkerville and Camerontown. Several claims on Williams Creek were exceedingly rich. The Prairie Flower claim yielded 170 ounces in one day. The Diller claim’s highest yield for one day was 102 pounds of gold.

Lowhee Creek, discovered by Richard Willowby in 1860, was one of the richest areas in the Barkerville region. The gold bearing gravel was between 20 and 30 feet thick with the richest pay found in the uppermost 15 feet and some of the largest nuggets found in the Cariboo region were found here.

Figure 6. 18.75 oz nugget from the Lowhee Mine (Stuart Holland photo)

Stouts Gulch produced thirty million dollars between 1861 and 1898. In 1861 the Mucho Oro claim was yielding up to 30 pounds of gold a day and reported $2,600,000 worth of gold.

Fig 7: Google Earth Snapshot illustrating Historic Past Producing Placer Operations.

2016 MAPPING AND RECONNAISANCE

The geological field mapping consisted primarily of bedrock outcrops along newly cut logging roads and logged areas. Approximately 2.5 kilometers along of outcrop was mapped within the claim boundary. All of this was exposed during road and/or ditch construction and unfortunately the bedrock was highly fractured and broken up as a result making it difficult for the author to obtain reliable structural measurements. Traverses using the road as the baseline were proposed starting at the end of the road up and down slope in NW/SE directions every approximately 200m. As the area had very recently been logged the terrain was difficult and predominantly heavily covered with logging slash. Typically each line was only traversable for a couple of hundred meters in the SE direction before encountering muskeg and a few hundred in the downslope direction. A few short access roads were found but had been either decommissioned or degraded due to the extreme thunderstorm activity that had been occurring previous to and during the project time frame and was only traversable on foot. Unseasonably severe thunderstorm activity in the project area greatly hindered progress and the project was not completed as planned. Many roads became too water laden and soft to safely accommodate a pickup truck and some areas were only accessible on foot. By July 7th the traverses were abandoned and all efforts were focused on mapping the bedrock that was accessible along the main road. Generally, the bedrock consisted of thinly interbedded to massive in appearance weakly oxidized, silver coloured, fine to medium grained phyllite and quartzite with sparse cubic small pyrite cubes in localized exposures. Locally, a dark grey, strongly foliated phyllite was conformably overlying the first unit but only in very brief exposures. Geological units and observed structure concurs with historical geological mapping efforts in the Cow Mountain area. Where measurements were attainable with the bedrock unit typically with a NW strike and dipping moderately to steeply to the NE as was expected. No significant faults or quartz veins were exposed in the mapping area. Very little overburden was observed overlying the bedrock.

Figure 8 (above) and Figure 9 (below) Bedrock outcrop (photo by Rachel Morneau)

DISCUSSION AND RECOMMENDATIONS

Although more bedrock has been exposed from logging activity and road building there is still insufficient exposure to draw conclusions with regards to pin pointing a residual placer type deposit. Mineralization of the bedrock was weak and no significant quartz veins or faults were exposed. Overburden in the mapping area is shallow with insufficient amounts to warrant any other testing of any type for placer deposits in the immediate vicinity. Access to upslope adjacent areas for further mapping work may be a problem due to the muskeg areas on Cow Mountain though as mentioned access was hindered due to unusually heavy thunderstorm activity during the project time frame. Greater success is likely achievable when conditions are drier. As there is sufficient water additional exploration work on Chew Tung Hydraulic is strongly recommended using either traditional placer testing methods i.e. test pits and/or seismic survey. A second mapping attempt is also recommended but only if and when weather conditions allow for greater access to the areas not completed.

Figure 10: Phyllite, the predominate lithology in the mapping area (photo by Rachel Morneau

STATEMENT OF COSTS

Exploration Work Type Comment/Personnel Days Totals Personnel (Name)* / Field Days (list actual Days/Hrs Rate Subtotal Position Field Days days) R. Morneau/Geologist June 26, 27 July 6, 8, 9, 10 7 $500.00 $3500.00

Blair Harris/ Field assistant June 24, 25, 26, 27, July 6, 8 7 $350.00 $2450.00

Sub Total $5950.00 $5950.00 OffS ice Studies AAsAssistant Report preparation incl GIS R. Morneau 30 $50.00 $1500.00

Sub Total $1500.00 $1500.00

Transportation No. Rate Subtotal

Truck-km rate 4x2 Round trip from Nanaimo to 1700 $0.60 $1020.00 Wells

Truck-km rate 4x4 To and from Wells to claim 180 $0.68 $122.40

Sub Total $2869.30 $2869.30

Accommodations & Food Per day for 1 person 9 $100.00 $900.00

Sub Total $900.00 $900.00

Miscellaneous

SPOT X2 7 $10.00 $140.00

Chainsaw X2 7 $30.00 $420.00

Sub Total $560.00 $560.00

TOTAL Expenditures $10,52.40

!

Statement of Qualif icati**s

!k^ S^tl^' I D--l-^! lla-i-1-.I ^r rr,-!r. D-:&i-L !Ll^--+;'" !;ii rii' rurrv!'t}b'';*- i, iiui-i'ri ;y,J, !,uvu v, ,;Ciil, ,,ii';J;t -viu'!'u'd'^1""*L:- suppof( I am cwner of Cariboo Assessments & $eoservices; a Csribso based mineral exploration

seruices c0mpanY since 2016. in 2009. I graduated with a BA iEarth Sciences and Ge*graphy] frorn tJniv*rsitY lslanri I graduated with a past Graduaie Dlpleima ;* 6{v;nr:ed Sls Appliratinns fr*m Vancoltver Uriiversiiy iri 2;]i0.

i have compietei iiC:T's Arjvanceci Prospecting Lourse (:uuci'

i have been empioyed in the minerai exploration and mining fieid since l00b'

I have been employed in the Cariboo ftegion for a total of 4 years'

I have been an avid Drospector fcr cver 10 Vears' prooertY This report is comoiled from data that i obtainerj on visits to the and historical reports. Sigrffil/L re':i,

Rachel ivlorneau

REFERENCES

Bowman, A. (1889): Report on the geology of the mining district of Cariboo, British Columbia; Geological Survey of Canada, Annual Report for 1887- 1888, V. 3, pt. 1, pp. 1-49c.

Bowman, A. (1895): Maps of the principal auriferous creeks in the Cariboo mining district, British Columbia; Geological Survey of Canada, Maps 364- 372.

Eyles, N. and Kocsis, S.P. 1989: Sedimentological controls on gold distribution in Pleistocene placer deposits of the Cariboo mining district, British Columbia; British Columbia Ministry of Energy, Mines and Petroleum Resources, Geological Fieldwork 1988, Paper 1989-1, Pp. 377-385.

Hanson, G. 1935: Barkerville Gold Belt, Cariboo District, British Columbia. Geological Survey of Canada, Memoir 181,42 p.

Hart, S. 2001:Quesnel Highlands recreational and tourism overview. Report prepared by J.S. Hart and Associates Ltd., Tatla Lake, B.C. for the District of Wells, Wells, B.C. 32 p.

Holland, S.S. 1976: Landforms of British Columbia: A Physiographic Outline. Bulletin 48. British Columbia Department of Mines and Petroleum Resources. 138 p.

Hong, W.M. 1978: …And So…That’s How It Happened Recollections of Stanley-Barkerville 1900-1975, W.M. Hong

Johnston, W.A. and Uglow, W.L. 1926: Placer and vein gold deposits of Barkerville, Cariboo District, British Columbia; Geological Survey of Canada, Memoir 149.

Kelly, J.A. 1983: Summary report on the 1983 surface exploration programs, Mosquito Creek, Wharf and Bralorne properties. Unpublished report for Mosquito Creek Gold Mining Company Limited

Knight, J. and McTaggart, K.C. 1989: Lode and placer gold of the Coquihalla and Wells areas, British Columbia (92H,93H); British Columbia Geological Survey Branch, Exploration in British Columbia 1989, pp. 105-1 18.

Levson, V.M., and Giles, T.R. 1993: Geology of Tertiary and Quaternary Gold-Bearing Placers in the Cariboo Region, British Columbia (93A, B, G, H); British Columbia Geological Survey Branch, Bulletin 89.

MacGowen, K.K. Cariboo Gold Strike Detailed Maps and Information (Placer/Lode Typle, Gold Occurrences of the Quesnel, BC Easterly to Barkerville, BC Area

Pautler. J. 2004: Report on the 2003 Diamond Drill and Trenching Program on the Cariboo Gold Project - Wells, British Columbia; Report prepared for lnternational Wayside Gold Mines Ltd.

Pickett, J.W. 2002: Technical report on the 2002 exploration program of lnternational Wayside Gold Mines Ltd. on the Myrtle Claim Group, Wells area, British Columbia. Report for lnternational Wayside Gold Mines Ltd.

Ray, G., Webster, I., Ross. K. and Hall, R. 2001: Geochemistry of Auriferous Pyrite Mineralization at the Bonanza Ledge, Mosquito Creek Mine and Other Properties in the Wells-Barkerville Area, British Columbia. British Columbia Ministry of Energy and

Rhys, D. 2001: Lode gold in the Cariboo: the Bonanza Ledge discovery of lnternational Wayside Gold Mines. 2001 Cordilleran Roundup Abstracts p. 20-21.

Rhys, D.A. and Ross, K.V. 2001: Evaluation of the geology and exploration potential of the Bonanza Ledge Zone and adjacent areas between Wells and Barkerville, east central British Columbia. Unpublished report by Panterra Geoservices Inc. for lnternational Wayside Gold Mines Ltd.

2000: Report on Petrography, check sampling and geological interpretation of drill core at the Bonanza Ledge Zone, Cariboo Gold Quartz Property, British Columbia. Unpublished report by Panterra Geoservices Inc. for lnternational Wayside Gold Mines Ltd.

Skerl, A.C. 1948: Geology of the Cariboo Gold Quartz Mine, Wells, B.C. Economic Geology, v. 43, p. 571-597

Struik, L.C. 1986: Imbricated terranes of the Cariboo Gold belt with correlations and implications for tectonics in southeastern British Columbia; Canadian Journal of Earth Sciences, v. 23, pp.1047-1061.

Struik, L.C. 1988: Structural geology of the Cariboo Gold Mining District, East-Central British Columbia. Geological Survey of Canada, Memoir 421, 100 p.

Sutherland Brown, A. 1957: Geology of the Antler Creek area, Cariboo District, British Columbia. British Columbia Department of Mines, Bulletin No. 38, 105 p.

Appendix

Bedrock Outcrop Maps

5 5 5 5 5 5 9 9 9 9 9 9 6 6 6 7 7 7 , , , , , , 2 5 7 0 2 5 5 0 5 0 5 0 0 0 0 0 0 0

5,880,000 5,880,000

64

84

5,879,750 5,879,750

0 0.2

kilometres

5,879,500 5 Scale: 1:5,000 5 5 5 5,879,500 9 9 9 9 6 6 7 7 , , , , 5 7 0 2 0 5 0 5 0 0 0 0

Chew Tung Hydraulic Mapping Project 2016 Southern Section Extent of mapping project

Bedding Claim Boundary

Lake Interbedded phyllite and quartzite Creek Lowhee Fm Quartzite and Phyllite

Baker Fm Quartzite, Phyllite and Limestone

Simplified Geology adapted from Struik (1988) 5 5 5 5 5 9 9 9 9 9 5 6 6 6 6 , , , , , 7 0 2 5 7 5 0 5 0 5 0 0 0 0 0

60

5,881,000 5,881,000

64

5,880,750 5,880,750 52

0 0.2

kilometres 5 5 5 5 5 9 9 9 9 9

5 Scale: 1:5,000 6 6 6 6 , , , , , 7 0 2 5 7 5 0 5 0 5 0 0 0 0 0

Chew Tung Hydraulic Mapping Project 2016 Northern Section Extent of mapping project

Bedding Claim Boundary

Lake Interbedded phyllite and quartzite

Lowhee Fm Quartzite and Phyllite Creek

Baker Fm Quartzite, Phyllite and Limestone

Simplified Geology adapted from Struik (1988) 5 5 5 5 5 9 9 9 9 9 6 6 6 7 7 , , , , , 2 5 7 0 2 5 0 5 0 5 0 0 0 0 0

5,880,500 54 5,880,500 62 34

5,880,250 64 5,880,250 32

0 0.2

kilometres 5 5 5 5 5

9 9 Scale: 1:5,000 9 9 9 6 6 6 7 7

5,880,000 , , , , , 5,880,000 2 5 7 0 2 5 0 5 0 5 0 0 0 0 0

Chew Tung Hydraulic Mapping Project 2016 Central Section Extent of mapping project

Bedding Claim Boundary

Dark grey stronly foliated phyllite Lake

Interbedded phyllite and quartzite Creek Lowhee Fm Quartzite and Phyllite

Baker Fm Quartzite, Phyllite and Limestone Simplified Geology Adapted from Struik (1988)