17 · 2020. 11. 6. · LONG. 119 17' 36" W GEOCHEMICAL, QEMSCAN REPORT ON MINERAL TENURES 1067360 106736,1 WORK DONE ON MINERAL TENURE 1067360,106736S 1 VALEMOUNT MICA PROJECT VALEMOUNT,

B R I T I S H / ; " C O " \ C O L U M B I A : % 7

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

T Y P E O F R E P O R T [type of survey(s)]: Geochemical T O T A L C O S T : $ 2,557.05

AUTHOR(S ) : Andris Kikauka S I G N A T U R E ^ ) : A .

NOTICE O F W O R K P E R M I T NUMBER(S )/DATE (S ) : Y E A R O F W O R K : 2019

S T A T E M E N T O F W O R K - C A S H P A Y M E N T S E V E N T NUMBER(S )/DATE (S ) : 5?64?£&- 3?6&0%2.

P R O P E R T Y N A M E : Valemount Mica

C L A I M N A M E { S ) (on which the work was done): 1067360, 1067361

C O M M O D I T I E S S O U G H T : Mica (muscovite, phlogopite, biotite)

M I N E R A L I N V E N T O R Y MINFILE N U M B E R ( S ) , IF K N O W N : 083D 012

MINING DIVISION: Cariboo

52 LAT ITUDE :

O W N E R ( S ) :

D Andris Kikauka

45 59 L O N G I T U D E : 119

N T S / B C G S : 083D 14/W , 083D.074

'36 17 {at centre of work)

M A I L I N G A D D R E S S :

4199 Highway 101, Powell R, B C V 8 A 0C7

O P E R A T O R ( S ) [who paid for the work]: 1) same 2)

M A I L I N G A D D R E S S :

same

2'

P R O P E R T Y G E O L O G Y K E Y W O R D S (lithology, age, stratigraphy, structure, alteration, mineralization, size and attitude):

The high mica content is associated with folded (minor crenulation and chevron folds) Hadrynian l o w e r K a z a Group with

muscovite-phlogopite-biotite-quartz-feldspar pelitic schist minor kyanite-staurolite-garnet, psammite, amphibolite, marble,

calc-si l icate, conglomerate, coarse grained grit and diamictite. The foliation of mica trends 060, dipping 10 degrees north

accessory chlorite, Ti -bearing minerals, Fe oxides, pyrite, apatite, and trace amphibole, andalusite/kyanite/sillimanite, zircon

R E F E R E N C E S TO P R E V I O U S A S S E S S M E N T W O R K A N D A S S E S S M E N T R E P O R T N U M B E R S : 7687

Next Page

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TYPE OF WORK IN THIS REPORT

EXTENT OF WORK (IN METRIC UNITS)

ON WHICH CLAIMS PROJECT COSTS APPORTIONED

(incl. support)

GEOLOGICAL (scale, area)

Ground, mapping

Photo interpretation

GEOPHYSICAL (line-kilometres)

Ground

Magnetic

Electromagnetic

Induced Polarization i

Radiometric

Seismic

Other

Airborne

GEOCHEMICAL

(number of samples analysed for...)

Soil

Silt

Rock 2 samples whole rock ME-XRF26, assay S 1067360, 1067361 $1,331.55

Other

DRILLING

((total metres; number of holes, size)

Coro Non-core

RELATED TECHNICAL

Sampling/assaying

Petrographic

Mineralographic QEMSCAN Mineralogical Report 1067361 1,225.50

Metallurgy

PROSPECTING (scale, area)

PREPARATORY / PHYSICAL

Line/grid (kilometres)

Topographic/Photogrammetric

(scale, area)

Legal surveys (scale, area)

Road, local access (kilometres)/)

Trench (metres)

rail Road, local access (kilometres)/)

Trench (metres)

Underground dev. (metres)

) Other

TOTAL COST: $ 2,557.05

O LAT. 52 45' 59" N NTS 083D 14/W, TRIM 083D.074

LAT. 52 45' 59" N LONG. 119 17' 36" W

GEOCHEMICAL, QEMSCAN REPORT ON MINERAL TENURES 1067360, 1067361

WORK DONE ON MINERAL TENURES 1067360,1067361 VALEMOUNT MICA PROJECT

VALEMOUNT, B.C.

Cariboo Mining Division

O by Andris Kikauka, P.Geo.

4199 Highway 101, Powell River, BC V8A 0C7

December 8, 2019

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TABLE OF CONTENTS AND LIST OF FIGURES

1.0 SUjMJVtARY

2.0 Introduction

3.0 Location;, Access, Physiography, Infrastructure, Claim Data

4.0 Property History

5.0 General Geology

6.0 Property Geology

7.0 2019 Geochemical <fc Geological Fieldwork 2019

7.1 IVIethods and. Procedures

page# 1

3

3

5

5

6

6

7.2 2019 Valemount QEMSCAN Mineralogy 7

7.3 2019 Mica Head Assay (sulphur), Whole Rock Major Oxide Analysis 7

8.0 Conclusion & Reconrxnendations 8

9.0 References

Certificate and Date

9

Itemized Cost Statement

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q LIST OF FIGURES

Fig 1 Valemount Mica Property General Location

Fig 2 Valemount Mica MTO Tenure Location

Fig 2 B Valemount Mica MTO Tenure Location (Detail)

Fig 3 Valemount Mica General Geology

Fig 4 Valemount Mica Mineral Claims 2019 Rock Chip Samples

Fig 5 Valemount Mica Mineral Claims 2019 Rock Chip Samples (Detail)

Fig 6 Valemount Mica Mineral Claims 2019 Rock Chip Samples (Google Earth)

APPENDLX A ALS Geochemical QEMSCAN, Whole Rock Analysis, S Assay Certificate

APPENDIX B ALS Geochemical Methods

APPENDIX C Rock Chip Sample Descriptions & Geochemical Analysis

APPENDIX D Minfile Description

Q ) APPENDIX E Koppers International Canada Ltd 1979 drill hole locations

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1.0 SUMMARY

This report describes results of a geochemical rock chip sampling conducted on the south-central portion of the VALEMOUNT MICA mineral claims in April, 2019. The VALEMOUNT MICA (Canoe Mica North) property is located approximately 12 km south-southwest of Valemount, British Columbia. The property is situated on the north side of the Canoe River about 5 kilometres southwest of Cedarside, and consist of 2 mineral claims (total area 39.14 hectares) within the Cariboo Mining Division.

Mica-bearing schist occurs in the central and south (lower elevation) portions of the mineral claims. High mica content schist is associated with folded (rninor crenulation and chevron folds) Hadrynian Lower Kaza Group muscovite-phlogopite-biotite-quartz-feldspar pelitic schist with minor kyanite-staurolite-garnet. Other lithologies of the lower Kaza Group include psammite, amphibolite, marble, calc-silicate, metamorphosed conglomerate, coarse grained grit and diamictite.

The VALEMOUNT MICA property has a history of previous work. In 1960, Georgian Mineral Industries Ltd developed a small quarry along the lower road. The mica schist located in the quarry consists predominantly of muscovite and quartz with lesser garnet, biotite and feldspar. Georgian's quarry is about 61 metres in diameter and 3.0 to 4.5 metres deep. The schist was processed at a plant at nearby Cedarside, and the final processing was done by Magcobar Mining Company Limited at a plant in Rosalind, Alberta. In 1961, Magcobar attempted to prove up larger reserves with a program of bulldozer trenching and 18 short holes. Results indicated approximately 200,000 tonnes of reserves grading 85 to 90 per eent mica to depth of 3.65 metres (Northern Miner March 15,1962). Some holes were drilled to a depth of 12 metres without reaching the lower limit of the mica-rich layer. The mica occurs in a mica-quartz-garnet schist. A program of short-hole drilling in 1961 had shown that a thickness of at least 25 feet (7 62 meters) of mica schist occurs. A processing plant was built in Cedarside in 1960 and 100 tonnes of mica nroduct was nroduced for market bv Georgia Mineral Industries Ltd (Tvlinister of Mines Annual Report 1960) During 1961 a further 125 tonnes of mica were produced (Minister of Mines Annual Report 1961) In 1962 remodelling of the plant was completed and testing begun Several shipments of mica were made to dry-wall faint cement consumers (Minister of Mines^nual Report 1962).

A magnetometer survey was done in the summer of 1978, and several small pits were dug. The Property was optioned by Koppers International Canada Limited (drilled a 91.5 metre hole on the Canoe 1 claim in 1978). In 1979, a further 16 holes were drilled totalling 641.3 metres. Forty five samples were submitted for froth flotation for mica recovery. Results ranged from 51.6 to 68.5 per cent muscovite (Assessment Report 7687). Koppers authorized a 14 hole drilling program totalling 670 metres to attempt to outline enough tonnage of schist to support a mining operation. The core size was NQ (4.7 cm in diameter), in order to give a large sample and to maximize recovery in the schist which in some sections is very soft and friable. The first 13 holes were drilled as planned, and showed that the dip is shallower than expected from the surface mapping and that Band A had been removed by erosion in the NE part of the drilling area. A total of 641.3 metres were drilled in 1979. The schist is difficult to core in some sections that are very soft. It was found that there was no systematic relationship between loss of core and grade of mica in the samples. Band B, which lies approximately 30 metres below Band A, was

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^ intersected in Holes 79-1,2 and 11, but was not traced to the SE to determine its area of subdrift O outcrop because the available diamond drill footage was used for the primary objective of

outliriing that part of Band A which is near the surface and amenable to mining by means of an open pit (Richardson, 1979). Mica aecurs in mica-quartz-garnet schist interlayered with beds of quartzite. One bed of schist, Band A, sub-outcrops under shallow overburden, and dips gently into a low hill. The proportion of quartzite within the schist bed varies from place. The schist bed has been truncated to the NE by a drainage channel which was immediately post glacial as indicated bv the verv fresh disarticulated schist and quartzite fragments which, with rounded boulders fill the channel. Considerable fracturing and faulting occur in Holes 79,9,10,11,12 and 13, and within zone of weakness (relatively easy to excavate this fractured and fissile zone).

Outland Resources Corp. outlined 2,290,000 tonnes of reserves after acquiring the property in 1980. The grade was 60.5 per cent muscovite. Another 1,000,000 tonnes of reserves was fairly assured (Canadian Mining Journal, May 1982). Property work in 1986 and 1987 included a pre-feasibility study.

A total of 2 rock chip samples were analyzed in 2019 (QEMSCAN, whole rock analysis, & sulphur assay). The upper and lower road high-mica pelitic schist zone contains muscovite-phlogopite-biotite-quartz-feldspar mineral assemblages, that include accessory chlorite, Ti-bearing minerals (ilmenite), Fe oxides (hematite-magnetite), pyrite, apatite, and trace amphibole, andalusite-kyanite-sillimanite, zircon). Foliation is relatively flat-lying, striking 240 degrees and dipping 10 degrees northwest.

O The objective of the fieldwork was to identify mineralogy and geochemistry of high mica content quartz-muscovite-phlogopite-biotite schist. A total of 5 rock samples were taken (Fig 4-6). A total of 2 rock chip samples were analyzed. One rock sample was taken from the upper road area where previous drilling in 1979 took place at 900 meters elevation, and the other sample was a composite of 4 rock samples from exposures along a distance of 300 meters along the lower road at 850 meters elevation (Fig 4-6). The upper and lower road zones are hosted in muscovite-phlogopite-biotite-quartz-feldspar pelitic schist.(including accessory chlorite, Ti-bearing minerals, Fe oxides, pyrite, apatite, and trace amphibole, andalusite-kyanite-sillimanite, zircon. The lower road (sample # 19VM-1 to 4) muscovite schist has 4.7% higher A1203 content, 12.1% higher muscovite content, and 1.9% higher phlogopite-biotite content, & 7.8% less Si02thanthe upper road (sample # 19VM-5) zone suggesting the mica content of lower road zone is higher than the upper road zone where the previous drilling took place.

Rock chip sample descriptions from 2019 fieldwork (on MTO claim 106) as listed as follows:

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Easting NAD Northing Elev Sample ID Zone name MTO claim 83 NAD 83 (m) Elev (ft) Lithology 19VM-1 lower road 1067361 345316 5847572 853 2798 mica schist 19VM-2 lower road 1067361 345360 5847570 853 2798 mica schist 19VM-3 lower road 1067361 345185 5847551 859 2818 mica schist 19VM-4 lower road 1067361 345460 5847618 857 2985 mica schist 19VM-5 upper road 1067360 345307 5847775 922 3024 mica schist

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o Sample foliation ID Sample type Comments Strike foliation Dip

19VM-1 Float lower rd 19VM-1 to 4 analyzed as composite

19VM-2 Outcrop lower rd 19VM-1 to 4 analyzed as composite 85 18 N

19VM-3 Float lower rd 19VM-1 to 4 analyzed as composite

19VM-4 Float lower rd 19VM-1 to 4 analyzed as composite

19VM-5 Outcrop upper rd 19VM-5 analyzed separately 72 20 N % % %

Sample ID %Si02 %AI203 %Fe203 %MgO CaO Na20 K20 %P205 Ti02 MnO

19VWI-1* 60.8 20 6.81 2.12 0.46 1.05 4.62 0.09 0.8 0.06

19VM-2

19VM-3

19VM-4

19VM-5 68.6 15.3 5.88 1.56 0.36 0.92 3.75 0.07 0.58 0.05

19VM1 to 19VM4 composite = 19VM-1*

Width (cm)

85

75

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2.0 INTRODUCTION

This report describes geochemical sampling and geological mapping performed during April 30, 2019 on the VALEMOUNT MICA claim (MTO ID number 1068181). The writer has prepared this report to comply with standards for the purpose of assessment reports. The intent of geochemical whole rock analysis and QEMSCAN was to discern mineralogical variations of the upper road (900 meters elevation) and lower road (850 meters elevation) exposures of mica schist.

.3.0 LOCATION, ACCESS, PHYSIOGRAPHY, INFRASTRUCTURE, CLAIM DATA

Work carried out on property is centered at 52 45' 59" north latitude and 119 17' 36" west longitude on NTS map sheet 83D 14/W. Access to the property is obtained from Valemount, via well-maintained logging access roads. The property elevations range from 820-960 meters above sea level. In general, topography has gentle to moderate slopes. Outcrop is rare but is exposed along portions of roadcuts, and deeper incised creek gullies.

The VALEMOUNT MICA property is located along the metamorphic (schist, quartzite) belt west of the Rocky Mountain Trench in northeast-central British Columbia. The area has been extensively glaciated resulting in low lying areas having deep overburden. The mineral property covers low lying hills. Portions of the property have been logged. Tree species consist of white spruce, fir and lodgepole pine with relatively little brush. The climate is typical of the northern interior of British Columbia with long cold winters and warm summers. The snow begins to accumulate in November and melts in April during a typical fall to spring cycle. Mining infrastructure can be supported by local communities and Kamloops located 250 kilometers south of the VALEMOUNT MICA mineral claims. The Main Line of the Canadian National Railway is 2 km east of the mica showings on the mineral claims. The Avola Valemount Transmission Line crosses the valley approximately 300 meters east of the rnineral claims, and the Canoe River is at the south boundary of the Property

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o Mineral Claim data from MTO website is listed as follows:

Title Number Claim Name Owner

VALEMOUNT 114051 1067360 MUSCOVITE (100%)

VALEMOUNT 114051 1067361 MUSCOVITE 2 (100%)

Title Type

Map Nutaber Issue Date

Area Good To Date (ha)

Mineral 083D 2019/MAR/21 2027/NOV/20 19.57

Mineral 083D 2019/MAR/21 2027/NOV/20 19.57

Andris Kikauka (ID # 114051) is registered owner of Valemount Muscovite, & Valemount Muscovite 2 mineral claim.

4.0 PROPERTY HISTORY

In I960, Georgian Mineral Industries Ltd developed a small quarry along the lower road. The mica schist located in the quarry consists predominantly of muscovite and quartz with lesser garnet, biotite and feldspar, in layers striking 240 degrees and dipping 10 degrees to the northwest. A sample from the main quarry was sent to the Department of Mines, Ottawa where garnet, ruffle and ilmenite were identified by x-ray diffraction. The main quarry is about 61 metres in diameter and 3.0 to 4.5 metres deep.

The mica on the present claim has been investigated several times in the past. Many years ago, a large amount of sluicing was done near the stream to investigate the area around a large mica schist outcrop. In 1961, Georgian Mineral Industries Ltd. produced small amounts of mica schist from a pit near the logging road. The schist was processed at a plant at nearby Cedarside, and the final processing was done by Magcobar Mining Company Limited at a plant in Rosalind, Alberta. In 1961, Magcobar attempted to prove up larger reserves with a program of bulldozer trenching and 18 short holes. In 1961, a drill program, consisting of 18 short holes covering an area of 152 square metres, indicated approximately 200,000 tonnes of reserves grading 85 to 90 per cent mica to depth of 3.65 metres (Northern Miner March 15, 1962). Some holes were drilled to a depth of 12 metres without reaching the lower limit of the mica-rich layer. The mica occurs in a mica-quartz-gamet schist. A program of short-hole drilling in 1961 had shown that a thickness of at least 25 feet (7.62 meters) of mica schist occurs. A processing plant was built in Cedarside in 1960 and 100 tonnes of mica product was produced for market by Georgia Mineral Industries Ltd. (Minister of Mines Annual Report 1960). During 1961, a further 125 tonnes of mica were produced (Minister of Mines Annual Report 1961). In 1962 remodelling of the plant was completed and testing begun. Several shipments of mica were made to dry-wall joint cement consumers (Minister of Mines Annual Report 1962).

A magnetometer survey was done in the summer of 1978, and several small pits were dug. The Property was optioned by Koppers International Canada Limited in July, 1978. Mits Development Company Ltd. drilled a 91.5 metre hole on the Canoe 1 claim in 1978. In 1979, a further 16 holes were drilled totalling 641.3 metres. Forty five samples were submitted for froth flotation for mica recovery. Results ranged from 51.6 to 68.5 per cent muscovite (Assessment Report 7687). Koppers authorized a 14 hole drilling program totalling 670 metres to attempt to outline enough tonnage of schist to support a mining operation. The core size was NQ (4.7 cm in diameter), in order to give a large sample and to maximize recovery in the schist which in some

4

^ sections is very soft and friable. The first 13 holes were drilled as planned, and showed that the CJ dip is shallower than expected from the surface mapping and that Band A had been removed by

erosien in the NE part of the drilling area. The total metres drilled in 1979 was 641.3. The schist is difficult to core in some sections that are very soft. It was found that there was no systematic relationship between loss of core and grade of mica in the samples. Band B, which lies approximately 30 metres below Band A, was intersected in Holes 79-1,2 and 11, but was not traced to the SE to determine its area of subdrift outcrop because the available diamond drill footage was used for the primary objective of outlining that part of Band A which is near the surface and amenable to mining by means of an open pit. Mica occurs in mica-quartz-garnet schist interlayered with beds of quartzite. One bed of schist, Band A, sub-outcrops under shallow overburden, and dips gently into a low hill. The proportion of quartzite within the schist bed varies from place. The schist bed has been truncated to the NE by a drainage channel which was immediately post glacial as indicated by the very fresh, disarticulated schist and quartzite fragments which, with rounded boulders, fill the channel. Considerable fracturing and faulting occur in Holes 79-9,10,11,12 and 13, and the position of the channel was probably governed by this zone of weakness.

Outland Resources Corp. outlined 2,290,000 tonnes of reserves after acquiring the property in 1980. The grade was 60.5 per cent muscovite. Another 1,000,000 tonnes of reserves was fairly assured (Canadian Mining Journal, May 1982). Property work in 1986 and 1987 included apre-feasibility study. Conclusions of the study were that present markets were inadequate to justify production at that time.

O 5.0 GENERAL GEOLOGY

The Property is adjaeent on the west to the Rocky Mountain Trench, and is underlain by the Proterozoic Kaza Group of Windermere ago (Campbell, 1967). The rocks mapped on the Property consist of a thick series of interbedded quartzite and mica-quartz-garnet schist beds which strike northeasterly and dip shallowly to the northwest. Individual quartzite and schist members vary in thickness from a fraction of a metre to several metres. Outcrops are sparse, and occur mainly along the stream which crosses the drilling area at 900 meters elevation, the Property. GSC Map 15-1967 indicates that the Property is adjacent to a staurolite-kyanite grade metamorphic zone, and trace amounts of these minerals have been identified (Appendix A: QEMSCAN).

6.0 PROPERTY GEOLOGY

Mica-bearing schist occurs in the central and south (lower elevation) portions of the mineral claims. High mica content schist is associated with folded (minor crenulation and chevron folds) Hadrynian Lower Kaza Group muscovite-phlogopite-biotite-quartz-feldspar pelitic schist with minor kyanite-staurolite-garnet.

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7.0 GEOCHEMICAL, GEOLOGICAL FIELDWORK 2019

7.1 METHODS & PROCEDURES

A total of 5 rock samples taken in the south-central portion of the VALEMOUNT MICA claims, one of the two samples is a composite taken from 4 separate locations. Location survey was performed using Garmin 60Cx GPS receiver with 3 meter accuracy (elevations are approximately 30 meter accuracy). Using rock hammer, 3.4-4.6 kilograms of acorn sized rock chips were placed in a plastic poly ore sample bag along with a numbered sample tag. The rock sample was taken across an outcrop of75-85 cm sample length intervals (3 out of 5 rock chip samples were angular float). Sample bags were labelled with black felt markers, and flagged. Samples were securely shipped to ALS Metallurgical Ltd, Kamloops for QEMSCAN mineralogy, head assay (S sulphur, S-IR08 S Total 0.01%-50% Total sulfur by Leco furnace, O.lg sample), and whole rock analysis, sample preparation ALS Prep-31, and ICP-AES finish ME-XRF06 (analysis details, methods & procedures are described in Appendix A: QEMSCAN, Head Assay, Whole Rock Analysis, Mineralogy, antl Appendix E: ALS Methods and Procedures).

7.2 QEMSCAN Mineralogy

The objective of the QEMSCAN was to identify mineralogy and geochemistry of high mica content schist. The schist is characterized by abundanee of fine to medirarn-grained bronze-coloured phlogopite-muscovite. A total of 5 rock samples were taken (Fig 4-6). QEMSCAN and whole rock analysis of 2 samples were performed. One rock sample from the upper road area where previous drilling in 1979 took place at 900 meters elevation, the other sample was a composite of 4 rock samples from the lower road at 850 meters elevation (Fig 4-6).

Results suggest the upper and lower road zones are hosted in muscovite-phlogopite-biotite-quartz-feldspar pelitic schist.(including accessory chlorite, Ti-bearing minerals, Fe oxides, pyrite, apatite, and trace amphibole, andalusite-kyam^e-sillimanite, zircon). The lower road (sample # 19VM-1 to 4) muscovite schist has 4.7% higher A1203 content, 12.1% higher muscovite content, 1.9% higher phlogopite-biotite content, & 7.8% less Si02 than the upper road (sample # 19VM-5) suggesting the overall mica content of lower road zone is several percent higher than the upper road zone where the previous drilling took place.

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o 7.3 2019 ROCK CHIP SAMPLE HEAD ASSAY & WHOLE ROCK GEOCHEMICAL ANALYSIS

Fieldwork in 2019 includes geochemical analysis of 5 rock chip samples covering approximately 5 hectares located in the south-central portion of the mineral claims (Fig 4-6). Five rock chip sample descriptions from 2019 fieldwork (on MTO claim 1067360,1067361) are listed as follows:

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Sample ID Zone name

MTO Easting NAD claim 83 Northing NAD 83

Elev (m)

Elev (ft) Lithology

19VM-1 lower road 1067361 345316 5847572 853 2798 mica schist

19VM-2 lower road 1067361 345360 5847570 853 2798 mica schist

19VM-3 lower road 1067361 345185 5847551 859 2818 mica schist

19VM-4 lower road 1067361 345460 5847618 857 2985 mica schist

19VM-5 Sample ID

upper road Sample type

1067360

Comments

345307 5847775

foliation Strike

922 3024 foliation Dip

mica schist Width (cm)

19VM-1 float 19VM-1 to 4 analyzed as composite

19VM-2 outcrop 19VM-1 to 4 analyzed as composite 85 18 N 85

19VM-3 float 19VM-1 to 4 analyzed as composite

19VM-4 float 19VM-1 to 4 analyzed as composite

19VM-5 Sample ID

outcrop 19VM-5 analyzed separately % % % % % Si02 AI203 Fe203 MgO CaO NaZO

72

K20 %P205

20 N % Ti02

% MnO

75

%S

19VM-1 ^60.8 20 6.81 2.12 0.46 1.05 4.62 0.09 0.8 0.06 0.06

19VM-2 ,

19VM-3 /

19VM-4/ COMPOSITE S A M P L E

19VM-5 68.6 15.3 5.88 1.56 0.36 0.9Z 3.75 0.07 0.58 0.05 0.04

Iron values of 5.88 & 6.81 % Fe from the whole rock geochemical analysis of the mica samples suggest high iron is from biotite.

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8.0 CONCLUSIONS AND RECOMMENDATIONS

The Valemount Mica mineral claims compares favourably to other mica deposits, in Quebec (Suzerite Twp rnining property) contains similar grades of mica. The Valemount Mica has historic estimates of200,000 tonnes of high-mica schist that is available for open pit mining, and estimated potential for over 2,000,000 tonnes high-mica schist. Valemodnt Mica occurs in an area of moderate topography, and the upper band of muscovite-phlogopite-biotite bearing schist is extensive (estimated to contain and flat-lying. A study of mining costs should be made and milling tests (froth flotation, recovery, dissociation, end product suitability for drywall compound), should be conducted to determine the type of products that can be produced and the cost of producing them. A market study should be made to determine the size of the market for mica products.

Detailed geological mapping, trenching and bulk sampling are recommended. Follow-up exploration should include the area immediately southwest of the area of 1979 drill holes. Development work should include bulk sample processing (mica separated from other minerals by flotation), and tested in drywall compounds and for additional industrial mineral applications, e.g. The plastic industry used ground mica as an extender and filler and also as a reinforcing agent. The rubber industry uses ground mica as an inert filler and as a mold lubricant in the manufacture of molded rubber products, including tires. Sheet mica is used principally in the electronic and electrical industries

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9.0 REFERENCES

Campbell, R.B. (1967) "Geology of Canoe River, British Columbia", G.S.C. Map 15-1967.

Carter, J.S. (1961) "Preliminary Report on Drill ing Program Conducted by Magcobar Mining Company, Limited for Georgian Mineral Industries Ltd. for Mica at Cedarside, B.C." Private report to Magcobar.

Minister of Mines Annual Report 1960,1961, & 1962

Richardson, T, 1979, Report on Koppers-Valemount Mica Project, Assessment Report # 7,687

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o CERTIFICATE AND DATE

I, Andris Kikauka, of 4199 Highway, Powell River, BC am a self-employed professional geoscientist. I hereby certify that:

1. I am a graduate of Brock University, St. Catharines, Ont, with an Honours Bachelor of Science Degree in Geological Sciences, 1980. 2. I am a Fellow in good standing with the Geological Association of Canada. 3. I am registered in the Province of British Columbia as a Professional Geoscientist. 4. I have practiced my profession for thirty five years in precious and base metal exploration in the Cordillera of Western Canada, U.S.A., Mexico, Central America, and South America, as well as for three years in uranium exploration in the Canadian Shield. 5. The information, opinions, and recommendations in this report are based on fieldwork carried out in my presence on the subject property during which time a technical evaluation consisting of geochemical sampling, and surveying carried during April 30,2019 6. I have a direct interest in the Valemount Mica Property, the recommendations in this report are intended to serve as a guideline, and cannot be used for the purpose of public financing. 7. I am not aware of any material fact or material change with respect to the subject matter of this Technical Report that is not reflected in the Technical Report, the omission to disclose which makes the Technical Report misleading. 8. This technical work report supports requirements of BCEMPR for Exploration and Development Work/Expiry Date Change.

O Andris Kikauka, P. Geo.,

December 8,2019

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o ITEMIZED COST STATEMENT-MINERAL TENURES 1067360,1067361 FIELDWORK PERFORMED APRIL 30,2019 (VALEMOUNT MICA), WORK CONSISTED OF GEOCHEMICAL SURVEYS ON MINERAL TENURE 1067360 & 1067361 CARIBOO MINING DIVISION, NTS 83D 14 W (TRIM 083D 074)

FIELD CREW:

A. Kikauka (Geologist) 1 day (surveying, mapping, sampling) $

FIELD COSTS:

577.50

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Equipment & supplies Mob/demob (vehicle & fuel cost) Shipping samples Meals and accommodations ALS Metallurgical QEMSCAN mineral identification geochemical analysis geochemistry 2 rock samples (sample 1 is a composite of 4 samples)

Report

8.30 192.50 36.25

140.00

1,102.50

Total=$ 2,557.05

O

O A X Append A - . Q E M S C A N C A L S ) 1 H e n A A c c , , T+250 828 6157 F+250 828 61 59

ALS Metallurgy Kamloops 2957 Bowers Place

Kamloops, BC VIS 1W5

Hea<* Assay Whole Rode k^U'm

November5, 2019

Mr. Andris Kikauka Project Geologist and Director American Manganese Inc. 4199 Highway 101 Powell River, BC V8A OC7

O Dear Mr. Kikauka;

Re: Mineraloqical Study on Two Samples from the Canoe Property - KM6053

We are pleased to report that we have now completed mineralogical analyses on

2 samples from the Canoe North Mica property located near Valemont, British

Columbia. The samples, identified as 19VM-1 and 19VM-5 and weighing 4.6 and

3.4 kilograms, respectively, were received as bulk rock in a single shipment on

October 24, 2019.

The objective of the assessment was to investigate the mineralogical

characteristics of the samples using QEMSCAN. In addition to the mineralogical

analysis, samples were also submitted for whole rock and sulphur analyses.

Detailed assay results are located in Appendix I - Sample Origin.

O Right Solutions • Right Partner www.alsglobal.com

o The primary minerals identified in the samples by QEMSCAN Particle Mineral

Analysis (PMA) protocols were identified as quartz, muscovite, biotite/phlogopite,

feldspars, and chlorite. Titanium minerals, iron oxides, pyrite, and apatite were

also identified, along with trace amounts of amphibole,

andalusite/kyanite/sillimanite, and zircon. Detailed results are located in

Appendix II - Mineralogical Data.

Thank you for the opportunity to participate in your mineralogical studies. If you

have any questions regarding this report, or the results generated by this

program, please contact us directly.

Regards,

Robert Sloan, P. Eng. VP ALS Metallurgy Americas

Pierce Liu, Jr. Metallurgist ALS Metallurgy

O £ R. R SLOAN ^ 5 40376 l//y/5.20l1

November 5, 201 9 KM6053

Electronic Distribution: Andris Kikauka, Powell River, BC o

1

o 1.0 Sample Origin

Mineralogical analyses were completed on two samples reported to have been

sourced from the Canoe North Mica property near Valemont, British Columbia.

The samples were received as bulk rock in a single shipment on October 24,

2019. A detailed list of the samples received is located in Table 1-1. Assay data,

including whole rock analysis, is located in Table 1-2 and 1-3, respectively.

TABLE 1-1 SAMPLES RECEIVED

Sample ID Weight (kg)

19VM-1 19VM-5

4.6 3.4

o TABLE 1-2 HEAD ASSAY DATA

Product Elements for Assay - percent Product S

19VM-1 19VM-5

0.06 0.04

TABLE 1-3 WHOLE ROCK ANALYSIS DATA

J Product Elements for Assay - percent |

J Product Al 2 0 3 BaO CaO Cr 20 3 Fe 20 3 K20 MgO MnO Na20 P205 Si02 Ti0 2 |

19VM-1 20.0 0.10 0.46 0.04 6.81 4.62 2.12 0.06 1.05 0.09 60.8 0.80 I J 19VM-5 15.3 0.08 0.36 0.04 5.88 3.75 1.56 0.05 0.92 0.07 68.6 0.58 |

o

1

o TABLE1A MINERAL COMPOSITION OF CANOE PROJECT SAMPLES

KM6053

Minerals 19VM-1 19VM-5

Sulphide Minerals <0.1 0.1

Iron Oxides 0.2 0.2

Quartz 39.5 54.9

Muscovite 37.8 25.7

Biotite/Phlogopite 9.1 7.2

Feldspars 5.0 7.3

Chlorite 5.7 3.6

Titanium Minerals 0.4 0.2

Apatite 0.1 0.1

Others 2.1 0.9

Total 100 100

o Notes: 1) Sulphide Minerals includes Pyrite.

2) Iron Oxides includes Magnetite, Hematite and Goethite/Limonite. 3) Feldspars includes K-Feldspar, Feldspar Albite (Na Feldspar) and Calcium Plagioclase. 4) Titanium Minerals includes Rutile/Anatase, llmenite and Sphene (Titanite). 5) Others includes trace amounts of Amphibole, Andalusite/Kyanite/Sillimanite, Zircon

and unresolved mineral species. 6) Particle Mineral Analysis was used for this data. 7) All values are expressed as a percent. 8) Measurement was scanned on the QEMSCAN ®.

o

2

TABLE 1B % ALUMINUM BEARING MINERAL OF TOTAL ALUMINUM

KM6053

Mineral 19VM-1 19VM-5

Muscovite 73.6 71.1

Biotite/Phlogopite 9.4 10.5

Feldspars 6.5 11.6

Chlorite 5.6 4.9 Other Aluminum Bearing Minerals 4.9 1.8

Total 100 100 Note 1) Other Aluminum Bearing Minerals includes Andalusite/Kyanite/Sillimanite.

TABLE1C % SILICON BEARING MINERAL OF TOTAL SILICON

o Mineral 19VM-1 19VM-5

Quartz 61.1 73.7

Muscovite 26.4 15.6

Biotite/Phlogopite 4.4 3.0

Feldspars 4.2 5.8

Chlorite 2.7 1.5 Other Silicon Bearing Minerals 1.2 0.5 Total 100 100 Note 1) Other Silicon Bearing Minerals includes Zircon, Amphibole

and Andalusite/Kyanite/Sillimanite.

o

3

TABLE1D CHEMICAL COMPOSITION OF CANOE PROJECT SAMPLES

KM6053

o

Element Assay Methods 19VM-1 19VM-5

Al QEMSCAN 10.4 7.32 Al Chemical 10.6 8.10

Ca QEMSCAN 0.40 0.29 Ca Chemical 0.33 0.26

Fe QEMSCAN 3.62 2.65 Fe Chemical 4.76 4.11

K QEMSCAN 4.61 3.45 K Chemical 3.84 3.11

Mg QEMSCAN 0.76 0.57 Mg Chemical 1.28 0.94

S QEMSCAN 0.01 0.03 S Chemical 0.06 0.04

Si QEMSCAN 30.2 34.8 Si Chemical 28.4 32.0

o

A p p e a l * & " A L S Me+Ws t froc&l*res S a r n p k

PREP-31 Standard Sample Preparation: Dry, Crush, Split and Pulverize

Sample preparation is the most critical step in the entire laboratory operation. The purpose of preparation is to produce a homogeneous analytical sub-sample that is fully representative of the material submitted to the laboratory. The sample is logged in the tracking system, weighed, dried and finely crushed to better than 70 % passing a 2 mm (Tyler 9 mesh, US Std. No.l 0) screen. A split of up to 2 50 g is taken and pulverized to better than 85 % passing a 75 micron (Tyler 200 mesh, US Std. No. 200) screen. This method is appropriate for rock chip or drill samples.

Method Code Descript ion

LOC-22 Sample is logged in tracking system and a bar code label is attached.

CRU-31 Fine crushing of rock chip and drill samples to better than 70 % of the sample passing 2 mm.

SPL-21 Split sample using riffle splitter.

PUL-31 A sample split of up to 2 50 g is pulverized to better than 85 % of the sample passing 75 microns.

R I G H T

Sample Preparation Package F low C h a r t

S a m p l e P r e p a r a t i o n P a c k a g e - PREP-31

S t a n d a r d S a m p l e P r e p a r a t i o n : Dry , C r u s h , Sp l i t a n d P u l v e r i z e

Receive Sample

L0G-22 Affix Bar Code and Log Sample in LIMS

WE Record receive*

-21 j sample weight

CRU-31 Fine crushing of rock chip and drill samples

to belter than 70 % < 2 mm

Keep Reject Reject

PUL-31 Up to 250 g sample split is pulverized to

belter than 85 % < 75 microns

Retain pulp for analysis

If samples air-dry overnight, no charge to

client. If samples are excessively wet. the

sample should be dried to a maximum of 120X. (DRY-21)

~QC testing of crushing efficiency is conducted

on random samples (CRU-QC)

"The sample reject is saved or dumped

pending client instructions. Prolonged storage (> 45 days} of rejects will be charged

to the client.

QC testing of pulverizing efficiency is conducted on random samples (PUL-QC).

Lab splits are required when analyses must

be performed at a location different than

where samples received.

R I G H T

WHOLE ROCK GEOCHEMISTRY

M E - X R F 0 6 SAMPLE DECOMPOSITION 5 0 % - 50% Li, B4 0 7 - l iBO, (WE I GRA06)

ANALYTICAL METHOD X - R a y F l u o r e s c e n c e S p e c t r o s c o p y (XjJI)

A calcined or ignited sample (0.9 g) is added to 9.0g of Lithium Borate Flux (50 % 50 $ Li B, 0 • LiBO ). mixed well and fused in an auto fluxet between 1050 - 1100°C. ft flat molten glass disc is prepared Irom the resulting melt This disc is then analysed by X-ray fluorescence spectrometry.

ELEMENT SYMBOL UNITS LOWER LIMIT UPPER LIMIT

Aluminum Oxide Al 0 0.01 100

Barium Oxide BaO % 0.01 100

Calcium Oxide CdO % 0.01 100

Chromium Oxide Cr 0, 0 0.01 100

Feme Oxide Fe,0, • 0.01 100

Potassium Oxide K 0 i 0.01 100

Magnesium Oxide MgO 0.01 100

Manganese Oxide MgO • 0.01 100

Sodium Oxide Na 0 0.01 100

Phosphorus Oxide P.O., 0.01 100

Silicon Oxide SiO. • 0.01 100

Strontium Oxide SrO 0.01 100

Titanium Oxide TiO • 0.01 100

Loss On ignition LOI • 0.01 100

Total % 0.01 101

NOTE: Since samples that are high in sulphides or base metals can damage Platinum crucibles, a ME- KP06 finish method can be selected as an alternative method

REVISION 0 4 . 0 0 SEP 14, 2006 WWW.ALSCiLOBAL.COM

O MTO Easting NAD Northing NAD Elev Elev Sample ID Zone name claim 83 83 (m) (ft) Lithology 19VM-1 lower road 1067361 345316 5847572 853 2798 mica schist 19VM-2 lower road 1067361 345360 5847570 853 2798 mica schist 19VM-3 lower road 1067361 345185 5847551 859 2818 mica schist 19VM-4 lower road 1067361 345460 5847618 857 2985 mica schist 19VM-5 upper road 1067361 345307 5847775 922 3024 mica schist

Sample Sample foliation foliation Width ID type Comments Strike Dip (cm) 19VM-1 float 19VM-1 to 4 analyzed as composite 19VM-2 outcrop 19VM-1 to 4 analyzed as composite 85 18 N 85 19VM-3 float 19VM-1 to 4 analyzed as composite 19VM-4 float 19VM-1 to 4 analyzed as composite 19VM-5 outcrop 19VM-5 analyzed separately 72 20 N 75

o Sample ID 1 9 V M ~ 19VM-2 19VM-3 19VM-4 19VM-5

Na20 1.05

K20 4.62

%P205 0.09

% Ti02

0.8

% MnO

0.06

WVM-1 C O M P O S I T E

S A M P L E

68.6 15.3

f O.0(,

5.88 1.56 0.36 0.92 3.75 0.07 0.58 0.05 0.0 4.

o

B R I T I S H C O L U M B I A

Ministry of Energy, Mines and Petroleum Resources

News I The Premier Online I Ministr ies & Organizat ions I J o b Opportunit ies I Main Indole

Help ^

MTMFILE Home page ARIS Home page MINFILE Search page Properly File Search

MINFILE Record Summary MINFILE No 083D012 XML Extract / Production Report / Inventory Report

Print Preview PDF S E L E C T R E P O R T -

File Cremed. 24-Jul-19S5 by B C Geological Survey (BCGS) Last Etlil.

SUMMARY Summary Help

31-AUQ-20O? by Sarah Meredith-Jones (SMJ]

N a m e

Status L a t i t u d e L o n g i t u d e

C o m m o d i t i e s Tec ton ic Beit

C A N O E NORTH MfCA C A N O E . C A N O E V V T S GRID. VALEMOUNT, C A N O E RIVER. VALEMONT. JOHN 1-11, CEDARSIDE

Past Producer 052° 45' 35" 119° 17'40"

Mica Omineca

N M I M i n i n g D i v i s i o n

BCGS M a p NTS H a p UTM N o r t h i n g E a s t i n g Depos i t T y p e s T e r r a n e

083D14/Q83D11 M i d Cariboo

083D074 083D14W 11 (NAD 83] 5848011 345177 P02 : Kyanite-sillimanile schists Kootenay. Ancestral North America

C a p s u l e G e o l o g y The Canoe North Mica property is situated on the north side of the Canoe River about 5 kilometres southwest ol Cedarside.

The showing is underlain by folded Hadrynian Lower Kaza Group Kyanite-staurolile-garnel-biotite and/or muscovite-quartz-feldspar pelitic schist. Other lithotogies of the lower Kaza Group include psammite, amphibolite. marble, calc-silicate. conglomerate, coarse grained grit and diamictite. The foliation of layers within the showing strike 240 degrees and dip 10 degrees northwest. A more delated description of the regional structure and metamorphism is given in the Canoe South Mica (083D 017) and Albreda (083D018) occurrences.

In the quarry, schist consists predominantly of muscovite and quartz with lesser garnet, biotile and feldspar, in layers striking 240 degrees and dipping 10 degrees to Ihe northwest. A sample from the mam quarry was sent to the Department of Mines. Ottawa where garnet, mtlte and ilmenite were identified by x-ray diffraction. The main quarry is about 61 metres in diameter and 3.0 to 4.5 metres deep,

In 1961. a drill program, consisting of 18 short holes covering an area of 152 square metres, indicated approximately 200.000 tonnes of reserves grading 85 to 90 per cent mica to depth of 3.65 metres (Northern Miner March 15, 1962). Some holes were drilled to a depth of 12 metres without reaching Ihe lower limit of the mica-rtch layer. A processing plant was built in Cedarside in 1960 and 100 tonnes of mica product was produced (or market by Georgia Mineral industries Ltd. (Minister of Mines Annual Report 1960). During 1961. a further 125 tonnes of mica were produced (Minister of Mines Annual Report 1961). In 1962 remodelling ot Ihe plant was completed and testing begun. Several shipments of mica were made to dry-wall joint cement consumers (Minister o l Mines Annual Report 1962).

Mils Development Company Ltd. drilled a 91.5 metre hole on the Canoe 1 claim in 1978. In 1979. a further 16 holes were drilled totalling 641.3 metres. Forty live samples were submitted for froth flotation for mica recovery. Results ranged from 51.6 to 68.5 percent muscovite (Assessment Report 7687),

Outland Resources Corp. outlined 2.290.000 tonnes of reserves after acquiring the property in 1980, The grade was 60.S per cent muscovite. Another 1,000,000 tonnes of reserves was fairly assured (Canadian Mining Journal. May 1982).

Property work in 1986 and 1987 included a pre-feasibility study. Conclusions of.the study were that present markets were inadequate to justify production at thai lime.

B i b l i o g r a p h y E M P R AR 1902-1083-1084; "1960-146: -1961 -151: -1962-158

E M P R A S S RPT '7687

E M P R B C METAL (Induslnal mineral production fiche for Georgian

Mineral Industries Ltd.)

E M P R E X P L 1978-E289; 1979-333; 1986-A79

EMR MIN BULL MR 223 (1989) B.C. 86

G S C EC G E O L No. 19, pp. 83.84

G S C M 15-1967, 1339A

G S C OF 2324

G S C P '89 -1E , pp. 101-107, "90-1E. pp. 71-80

C M J 'May 1982. p. 13

GCNL No. 62. 155. 1981; No. 45. 1982; No. 107, 112, 1987

N MINER "March 15. 1962; March 11. 1982: Sept 1. 1983

C O P Y R I G H T | D I S C L A I M E R | P R I V A C Y } A C C E S S I B I L I T Y

(I r • ,

I o

1

Outline of Mineral Claim.

Area of 1979 short drill holes

I \

r M T O 1067360 Valemount Muscovite

M T O 1067361 Valemount Muscovite 2

APPENDIX E: 1979 Short Drill Holes, After: Koppers Project, Richardson Geo Consulting Ltd Assessment Report 7,687

Fig 1 Valemount Mica Mineral Claims General Location

Valemount

VALEMONT

V

+ Cedarside

outline of mineral claims -*r—I ' CAI

U CANOE NORTH MICA

c *

2 K w

SCALE 1 : 75,000

1

M I L E S

Kinbasket Lake

V

golumma F '9 2 M T 0 Valemount Mica

Legend

1000 m

Mineral Titles (MTO) MTO Grid

Title (current) • LEASE • CLAIM Reserves

• No Registration

| Conditional

Heritage/Historic Site Crown Land Layers (Tantalls) Land Acl Survey Parcels • Tantalis - Legal Descriptions

Label Text Land Act Survey Parcels - Tantalis -Outlined

Administrative Boundaries Federal Transfer Lands - Outlined

Federal Transfer Lands - Colour Filled

National Partes - Outlined • National Park National Parks-Colour Filled

Conservancy Areas - Tantalis - Colour Filled • Conservancy Areas Ecological Reserves - Tantalis - Colour Filled

Ecological Reserves Protected Areas - Tantalis - Colour Filled P Protected Areas Provincial Parks - Tantalis - Colour Filled

Provincial Parks Recreation Areas - Tantalis - Colour Filled

This map is a user generated static output from an Internet mapping site and is for general reference only. Data layers that appear on this map may or may not be accurate, current, or otherwise reliable. THIS MAP IS NOT TO BE USED FOR NAVIGATION.

Printed using the Mineral Titles Online (MTO) application. 083D 14/W, 083D.074. Cariboo M.D. Center: 52°47'2".-119°17'12" Scale: 1 :135420 SRS: EPSG:3857 UTM Zone: 11

N

BRITISH C O L U M B I A

Fig 2B MTO Valemount Mica

Legend Mineral Titles (MTO) MTO Grid

Title (current) • LEASE

• CLAIM Reserves

• No Registration

Conditional

Heritage/Historic Site

Crown Land Layers (Tantalis) Land Act Survey Parcels - Tantalis - Legal Descriptions

Label Text Land Act Survey Parcels - Tantalis -Outlined

Administrative Boundaries Federal Transfer Lands - Outlined

Federal Transfer Lands - Colour Filled

National Parks - Outlined • National Park National Parks - Colour Filled • Conservancy Areas - Tantalis - Colour Filled • Conservancy Aieas Ecological Reserves - Tantalis - Colour Filled

Ecological Reserves Protected Areas - Tantalis - Colour Filled

Ptotecled Areas Provincial Parks - Tantalis - Colour Filled

Provincial Parks Recreation Areas - Tantalis - Colour Filled

This map is a user generated static output from an Internet mapping site and is for general reference only. Data layers that appear on this map may or may not be accurate, current, or otherwise reliable. THIS MAP IS NOT TO BE USED FOR NAVIGATION.

Printed using the Mineral Titles Online (MTO) application. 083D 14/W. 083D.074, Cariboo M.D. Center: 52°45'34", -119° 17'23" Scale: 1 : 33855 SRS: EPSG:3857 UTMZone: 11

N

Fig 3 Valemount Mica General Geology NTS 083D 14/W, BCGS 083D.074, Cariboo Mining Division

EPrG 1

^ m C m d o

uPrKLsf X uPrKLsf

Lithology Legend mCmdo Middle Cambrian

marble, recrystallized dolomitic carbonate

uPrlCLsf Upper Proterozoic Kaza Grp, Lower Division pelitic schist, phyllite, psammite, amphibolite, metamorphosed clastic sedimentary rocks

EPrG Early Proterozoic Gold Ck gneiss, orthogneiss

EPrM Early Proterozoic Malton gneiss complex, orthogneiss

. Normal Fault A A Thrust Fault

m C m d o

T X-C A N O E N O R T H M I C A

/ * A A * A A K K K \ * A A A A A A A A A

Outline of Mineral Claim

/

E P r M

SCALE 1 : 80,000

i M I L E S V

Fig 4 Valemount Mica Mineral Claims Rock Sample Locations NTS 083D 14AV, BCGS 083D.074, Cariboo Mining Division

Fig 5 Valemount Mica Claims Rock Sample Locations (Detail) NTS 083D 14/W, BCGS 083D.074, Cariboo Mining Division

MTO kjsling NAD Northing NAD Elev Elev

Sample ID Zone name claim S3 S3 (IT. (It) Lithology

19VM-1 lower road 1067361 345316 5847572 853 2798 mica schist

19VM-2 lower rood 1067361 345360 SS47S70 853 2798 mica schist

19VM-3 lower road 1067361 3451B5 S847S5I 8S9 2818 mica schist

19VM-4 lower road 1067361 345460 5S47618 857 2985 mica schist

19VM-5 upper road 1067361 345307 5847775 922 3024 mica schist

[outline of mineral claims

id

I D

m

5,848,000 M

i (

1067360 \

M T O 1067361

Area of 1979 short drill holes

IT

D19VM-5 —

Sample type

float

outcrop

float

float

outcrop

% % % SK32 AI203 Fe203 MgO CaO Na20 K20 %P20S Ti02 MnO

60S 20 6.81 2.12 0.46 1.05 4.62

19VM-1 to 4 combined to = composite sample 19VM-1

68 6 15.3 5 88 1.56 0.36 0.92 3.75 0.07 0.58 0.05

Comments

19VM-1 to 4 analyzed as composite

19VM-1 to 4 analyzed as composite

19VM-1 to 4 analyzed as composite

19VM1 to 4 analyzed as composite

19VM-5 analyzed separately

* %~ t A n n f a r t

foliation

Strike

foliation

Dip

85 18 N

Width Icm)

S5

0.8 0.06

- A •

,j,19VM-4|

19VM-3 ^ JT „ --19VM-1

o 19VM-2

Zoom SCALE 1 : 5,000 a Rock C h i p Sample

5 0 0 5 0 0

F E E T

1 , 0 0 0 1.500 V

Fig 6 Valemount Mica Rock Sample Locations NTS 083D 14/W, B C G S 083D.074, Cariboo Mining Division, Upper & Lower Raod Zones

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