BRITISH COLUMBIA Tlie Betf Place on Earth

Ministry of Energy, Mines & Petroleum Resources Mining & Minerals Division Assessment Report BC Geological Survey Title Page and Summary

TYPE OF REPORT [type of survey(s)]: Rock Geochemistry TOTAL COST: $2878.26

AUTHOR(S): Bruce Doyle SIGNATURE(S): /£y^J^/

NOTICE OF WORK PERMIT NUMBER(S)/DATE(S): YEAR OF WORK: 2018

STATEMENT OF WORK - CASH PAYMENTS EVENT NUMBER(S)/DATE(S): 5725341

PROPERTY NAME: FISHER

CLAIM NAME(S) (on which the work was done): FISHER 6 998808

COMMODITIES SOUGHT: Cg Flake Graphite

MINERAL INVENTORY MINFILE NUMBER(S), IF KNOWN: 082LSE081 082LSE076

MINING DIVISION: Slocan NTS/BCGS: 082L01E 082I020

LATITUDE: 50 ° 11 52.67 LONGITUDE: 118 02 '12.98 (at centre of work)

OWNER(S): 1) BRUCE DOYLE 2)

MAILING ADDRESS: 1424 Crease Ave Nelson, B.C. V1L 1A2

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

MAILING ADDRESS: 1424 Crease Ave Nelson, B.C. V1L 1A2

PROPERTY GEOLOGY KEYWORDS (lithology. age, stratigraphy, structure, alteration, mineralization, size and attitude):

Devonian to Silver Creek Formation Sedimentary rocks are metamorphosed to quartzite and quartz-biotite schist containing layered and disseminated crystaline flake graphite.

REFERENCES TO PREVIOUS ASSESSMENT WORK AND ASSESSMENT REPORT NUMBERS: 09447,33479,34974,35894

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

Photo interpretation

GEOPHYSICAL (line-kilometres) Ground Magnetic

Electromagnetic

Induced Polarization

Radiometric

Seismic

Other

Airborne

GEOCHEMICAL (number of samples analysed for...) Soil Silt

Rock 5 $2625.00

Other

DRILLING (total metres; number of holes, size) Core Non-core

RELATED TECHNICAL Sampling/assaying $253.26

Petrographic

Mlneralographlc

Metallurgic

PROSPECTING (scale, area)

PREPARATORY / PHYSICAL Line/grid (kilometres)

Topographic/Photogrammetric (scale, area)

Legal surveys (scale, area)

Road, local access (kilometresVtrai l

Trench (metres)

Underground dev. (metres)

Other

TOTAL COST: $2878.26 Assessment Report

2018 Rock Geochemistry

On the

FISHER PROPERTY

Nakusp, B.C.

Slocan Mining Division, British Columbia

NTS Map Sheets 82L01 82K04

UTM 426238E 5558686N

By:

Bruce Doyle, Prospector

1424 Crease Ave, Nelson, B.C

V1L 1A2 December, 28 2018 British Cancel COLUMBIA

Mineral Titles Online

Mineral Claim Exploration and Development Work/Expiry Date Confirmation Change Recorder: DOYLE, BRUCE ANTHONY (107050) Submitter: DOYLE, BRUCE ANTHONY (107050) Recorded: 2019/JAN/04 Effective: 2019/JAN/04 D/E Date: 2019/JAN/04

Confirmation

If you have not yet submitted your report for this work program, your technical work report is due in 90 days. The Exploration and Development Work/Expiry Date Change event number is required with your report submission. Please attach a copy of this confirmation page to your report. Contact Mineral Titles Branch for more information.

Event Number: 5725341

Work Type: Technical Work Technical Items: Geochemical, PAC Withdrawal (up to 30% of technical work required)

Work Start Date: 2018/OCT/18 Work Stop Date: 2018/OCT/22 Total Value of Work: $ 2878.26 Mine Permit No:

Summary of the work value:

New # of Good Area Applied Sub• Claim Issue Good Days Title Number To in Work mission Name/Property Date To For• Date Ha Value Fee Date ward 998808 FISHER 6 2012/JUN/19 2019/JAN/07 2019/sep/07 243 331.11 $ 3665.50 $ 0.00

Financial Summary:

Total applied work value:$ 3665.50

PAC name: bruce doyle Debited PAC amount: $ 787.24 Credited PAC amount: $ 0

Total Submission Fees: $ 0.0

Total Paid: $ 0.0 Table of Contents page 1.0 Summary- — — 1 2.0 Introduction- 2 2.1 Fisher Property: Location, Access, and Description — 2 3.0 Climate, Local Resources, Infrastructures and Physiography-— 2 4.0 History-—- -- — 5 4.1 2018 Exploration Program— — 5 5.0 Regional Geology 5 6.0 Property Geology — ——- 6 7.0 Sampling Method and Approach — 14 8.0 Sampling Preparation, Analysis and Security 14 9.0 Interpretation and Conclusions—-— —————_ 14 10.0 Recommendations— — 14

List of Figures

1. Location Map —~ — 3 2. Claim Map—— — 4 3. Property Geology— ———-— —- 7 3a. Lithology Legend ~— —-— 8 4. Regional Geology— — ——— —— 9 4a. Regional Geology Legend- —— ~ —- 10 5.2012 Time Domain Electromagnetic Survey — 11 6. Sample Location Map with % Cg Values-—— ——-—— 12 List of Tables

1. Claim Information- — 2 2. Fisher Property-2018 Rock Samples — 13 List of Appendices 1. Analytical Procedures 2. Statement of Qualifications 3. Cost Statement 4. Analytical Results 1.0 Summary

The Fisher Property is centered 36 km west of Nakusp in South British Columbia. It consists of one property totaling 331 hectares. The property covers metasedimentary rocks of the to Carboninferous Chase and Silver Creek formations within the Monashee metamorphic complex. These rocks have a complex structural history with at least 3 phases of folding and have intruded by - granodirorites and pegmatites. A thick 300-800 pelitic sequence has been metamorphosed forming crystalline flake graphite within organic rich horizons.

This report summarizes the results of a small rock sampling program carried out on the Fisher Property during 2018, to locate higher grade flake graphite mineralization. The first discovery of flakegraphit e in this area was made by Grant Doyle of Nakusp, B.C. and together with his brother staked over 12,000 hectares and optioned the property to Noram Ventures.

In 2012, Noram Ventures conducted an airborne TEM and Magnetic Survey over the entire property. This survey outline a 500-2000 m wide folded conductor that correlated with a graphite horizon.

2013- Noram Venture completed 1294.29 of diamond drilling in areas outside the strongest EM Conductors. One of the holes intersected 1.50% graphite over 124.36m and 2.819% graphite across 29.07 both being true width.

2014- A rock sampling program returned 48m chip across and outcrop on Branch #1 that returned 3.32% graphite.

2015- A sampling program targeted the conductive TEM Horizon with 84 samples. The highest grade sample of subcrop along a ditch on Branch #67 returned 16.6% graphite.

It would appear from previous sampling that the highest grade graphite is recessive on the property. In 2017, Noram Ventures dropped the Jumbo Property after paying Grant and Bruce Doyle out and owning it 100%. Subject only to the Royalty on the property. The Doyles were able to get a key claim back into their name again which is the Fisher Claim. The Doyles felt this claim had the highest potential for high grade graphite. It is on this claim where the TEM Survey completed by Noram Ventures shows the horizon being folded or faulted causing a thickening which should increase the overall grade for graphite.

See Figure 5. The 2018 rock sampling program consisted of collecting 5 rock samples from outcrops and the highest grade returned was 7.1 % graphite. It is believed higher grades will be discovered further to the north fromthes e locations. The areas to the north have strong conductors but less outcrop. Drilling and trenching may be the only way to test these areas that are recessive with strong conductors.

2.0 Introduction This report summarizes a small rock sampling program completed on the Fisher Property during the fall on October 18,2018 and October 22, 2018 by Grant and Bruce Doyle.

2.1 Fisher Property: Location, Access and Description The Fisher Property is located 36km west of Nakusp as shown on Figure 1. The property consists of 1 claim totaling 331 hectares, located on NTS Map Sheet 82L01. From Nakusp, access to the property is south on Highway B-6 for 22 km to the Arrowpark Ferry. Take the lower Mosquito road and head up the Stevens Ritchie Park road at 13.5 km. Turn onto the Fisher Road. Follow this road to the property.

Tenure Claim Name Owner Issue Date Good to Area (ha) Number Date 998808 Fisher 6 107050 06/19/2012 09/07/2019 331.11

3.0 Climate, Local Resources, Infrastructure and Physiography The terrain on the Fisher Property has moderate slopes but most of the property is quite level. A significant portion of the property was logged in the late 1960's and 1970's. The current roads on the property are in very good shape but filled with alder. The forest consists of spruce, hemlock, and cedar. The average temperature during May to October ranges from 12 degrees to a high of 35 degrees in July. Winter temperatures range from 1 degree to minus 10. The average precipitation is about 570mm with snow fall averaging 200cm. The property is snow free from May to late October. -2- dSESSL Figure 1-Location Map

082L030

Legend Crown Land Layers (Tantalis) Land Act Survey Parcels - Tantalis - Legal Descriptions Label Text Land Act Survey Parcels - Tantalis - IT? Outlined • ISHER PROPE ttV t AdministrativFederal Transfeer BoundarieLands - Outlines d • Federal Transfer Lands - Colour Filled

Q82L020 • National Parks - 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 I Protected Areas Provincial Parks - Tantalis - Colour Filled I Provincial Parks Recreation Areas - Tantalis - Colour Filled Recreation Areas First Nations Layers First Nations Treaty Lands - Outlined Huu-ay-aht First Nations 9 082L010 J Ka:Vu:'kW/Che:k1les7etTr First Nations • Nisga'a Nation • Tla'amin Nation • Toquaht Nation |_2kmJ • Tsawwassen First Nation "1 I IrhnrHooahtTrlho This map is a user generated static output from an Internet Printed using the Mineral Titles Online (MTO) application. Center: 50°8'34",-118

\ \ • •'. i......

/ i Legend Mineral Titles (MTO) MTO Grid

Title (current) 1061248 • LEASE • CLAIM Reserves n No Registration • Conditional

\Z\ Heritage/Historic Site FISHER P&OPEflLTY Crown Land Layers (Tantalis) Land Act Survey Parcels - Tantalis - Legal ~9

On October 18,2018 and October 22,2018, Grant and Bruce Doyle carried out a small rock sampling program on the Fisher Property. Five samples were taken over the two day period. The highest graphite grade obtained assayed 7.13% Cg while another assayed 4.77%Cg. The samples were taken along the SkyTEM survey previously done by Noram Ventures. 5.0 Regional Geology The Fisher Property is underlain by the Monashee metamorphic complex and is in contact to the east with the Columbia River fault, a gently east-dipping Eocene age fault. Approximately 40 km to the north of the Fisher Property is the Thor-Odin dome. Regional geology is shown in Figure 4 as well as the lithological geology on Figure 4a. -5- 6.0 Property Geology The rock units on the Fisher Property have gone through a complex structural history with at least three phases of folding and several stages of faulting. These metasedimentary rocks were probably deposited in a continental margin environment. The rocks on this property have undergone upper amphibolite fades, medium to high grade metamorphism, with the development of biotite, garnet, and sillmaite (+ Staurolite; Thompson et al., 2004). The main rock units on the property appears to be quartz rich metasandstones. The graphite mineralization is concentrated in a dirty or less pure calcareous sections. During metamorphism, the organic material formed crystalline graphite flakes. The graphitic rocks are usually rusty coloured from having trace amounts of pyrite and traces chalcopyrite. Thin marble beds occur that carry flake graphite but have no pyrite and are absent of the rust colour. The graphite units also contain trace amounts of biotite. The most obvious structural deformations of stratigraphy are folds with east-southeast trending fold axes as shown in red in Figure 5 (Allen, 2015). The metasedimentary rocks have been intruded by leucoratic dykes and fine grained pegmatite granitic intrusions. More mapping is needed to fully understand the geology on this property.

7.0 Sampling Method and Approach All rock samples taken were from bedrock and were located in the field using a non- differential model Garmin 60CSX global positioning system instrument and were placed in plastic rock sampling bags. Each bag was given a sample number with a magic marker and marked in the field with orange or pink flagging.

8.0 Sample Preparation, Analysis, and Security All rock samples were collected, sealed, boxed, and shipped via courier to ALS Labs in Norm Vancouver. Samples were analyzed for carbon by Leco furnace with infrared detection. Results were given % carbon. (Appendix 4).

9.0 Interpretation and Conclusions The best area to continue prospecting and sampling is along the SkyTEM survey completed by Noram Ventures in 2012. On the Fisher claim, the airborne anomaly crosses through the Fisher claim and appears to be faulted or tightly folded. Both scenarios are thought to increase the graphite grade of the horizon. The higher grade graphite appears to be recessive and may require trenching or drilling to test the grades.

-6- 420000 425000 430000 L

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420000 425000 430000

Property Geology (GSC)

G. Allen. November, 2012 See Fi9ure 3* for Hthologic legend Figure 3 i CRETACEOUS Whaishan Lake Batholith (~77-79 Ma): Leucocraiic, potassium feldspar, megacrystic, hornblende-bearing quartz monzonite; includes Caribou Creek stock on east side of Arrow Late,

Interlayered KWLgd and Dqfb.

DEVONIAN TO Sitkum amphibole schist Hornbiende-biotite-piagioclase schist, maybe ^ DPas calcareous. Can occur as discontinuous markers v/ithin and overlying Dqfb.

DEVONIAN (and CARBONIFEROUS?) SILVER CREEK FORMATION (Jones, 1959) Stiver Creek schist Quartz-feldspar-muscovfte-biotite schist v/ith or without Dqfb garnet, staurolite and siHimanite; black carbonaceous schist dark-grey to tan micaceous quartzite: minor white-to-grey marble; amphibolitic schist minor amphibolMe (map units PsM and Psb6 of Read, 7 979a).

r Silver Creek marble: Medium to coarse crystalline, white to dark grey Dm marbie (map unit Psc5 of Read, 1979a).

Stiver Creek staurolite schist Grey- and brown- weathering Dqffas muscavite-bfotiie schist having a profusion of targe staurolite porphyroblasts up to 2 cm in length (map unit Psu5 of Read, 7979a).

MIDDLE? DEVONIAN CHASE FORMATION (CALCAREOUS QUARTZITE MARKER UNIT) White to light grey, cftff-form'mg, calcareous quarbdie having a coarse. pitted texure on weathered surfaces; diopside rich calcsiUcate bands (map unit F3 of Reesor and Moore, 1971).

Chase marble: White, coarse crystalline marble interlayered with Dqmu biotrte-muscovite schist and discontinuous layers of Chase Formation quartzite f Dcqm; map unit PscS of Read, 1979a).

Paieo- and/or Mesoproterozoic Tsuius schist Btotite-quartz-feidspar schist (with or without silfimanite, Pqfh garnet); feldspar-quartz-homblende schist (with or without biotite); amphibolite; calc-silicate gneiss; micaceous quartzite (map units M and F of Reesor and Moore, 1971).

Lithology Legend (GSC Open File 4370)

G. Allen, November. 2012 To accompany Figure 3 Figure 3q) 400000 450000

^:*:i:i::Li:500,ooo::::::

Geological Data Source:,www.mapptece.ca?,Read etal*-1981 :*:+:*:*;*^/ .Xf^*: ; Coord System?NAD83>Zohe*TIN*

400000 450000

Regional Geology G. Allen, November, 2014 See Figure 4o.for Hthoiogic legend Figure 41 Post Accretionary Intrusions Chilcorjn Group; young volcanics. to

Sheppard, Tuzo Creek, Shingle Creek Intrusions Kamloops Group; Eocene -Eocene (65-35.4 Ma)

jijijj Okanagan Batholith - Ladybird and Valhalla intrusions; P*T**3 Cretaceous (145.6-65 Ma) 5 Whatshan Batholith; Cretaceous (145.6-65 Ma)

Battle Range Batholith; Cretaceous (145.6-65 Ma) Quesnel Terrane

k><*v3 Nicola Group; Upper Triassic Slocan Group; Early to Lower Triassic i | Kaslo Group; Carboniferous to Permian

| Rossland Group :•:•:«! Kuskanax Batholith; Mid (180-170 Ma) J Rossland Group - Elise Formation; Lower Jurassic I Harper Ranch Group ;»;»;« Unnamed; various ages Harper Ranch and(?) Nicola Groups; Lower Jurassic

Kootenay Terrane j^yg^ Mitford Formation; to Permian to Devonian Lardeau Group - Broadview Formation Ancestral North America j Lardeau Group - Index Formation j Lardeau Group - Jowett Formation Badshot Formation; Lower Cambrian limestone j Lardeau Group - Lade Peak Formation Mohican Formation; Lower Cambrian phyllite J Lardeau Group - Triune Formation

j Eagle Bay Assemblage Monashee Metamorphic Complex; to Early Paleozoic

I i ; I| calcsilicate metamorphic rocks Shuswap Assemblage; { metamorphic rocks, undivided Proterozoic to Paleozoic paragneiss metamorphic rocks ffv)]^i quartzite, quartz arenite sedimentary rocks

Monashee Terrane; gneiss domes and nappes I*;*;*;] Core (Basement) orthogneiss intrusions; Early Proterozoic Core (Basement) paragneiss; Archean to Early Proterozoic

Geological Data Source: www.mapplace.ca

, Regional Geology Legend G. Allen, November, 2014 To accompany Figure q Figure Ifa 420000 425000 430000 435000 1

420000 425000 430000 435000 Noram Ventures Inc. Jumbo Property Time Domain Electromagnetic High Moment (HM) Z Coil Data, Gate 16 [0] G.Aiien, November, 2012 Colour Shaded Equal Area (EA) Plot Figure 5 BRITISH MTO Sample Location Map % Cg COLUMBIA

Graphite Horizon

3029565 FISHER PROPERTY 7.13%Cg Legend Mineral Titles (MTO) MTO Grid r - 3029566 Title (current) 3.66%Cg • LEASE • CLAIM \ 3029562 Reserves \ 2.96%C • Mo Registration • Conditional 998808 0 Heritage/Historic Site Crown Land Layers (Tantalis) Land Act Survey Parcels - Tantalis - Legal Descriptions 10612 Label Text Land Act Survey Parcels - Tantalis - Outlined • 3029563 AdministrativFederal Transfeer LandBoundaries - Outlines d • 3.66%Cg Federal Transfer Lands - Colour Filled • National Parks - Outlined 3029564 • National Park 3.71%Cg National Parks - Colour Filled Conservancy Areas - Tantalis - Colour Filled • Conservancy Areas Ecological Reserves - Tantalis - Colour Filled Ecological Reserves Protected Areas - Tantalis - Colour Filled I Protected Areas Provincial Parks - Tantalis - Colour Filled 100 m [ Provincial Parks Recreation Areas - Tantalis - Colour Filled This map is a user generated static output from an Internet Printed using the Mineral Titles Online (MTO) application. Center: 50°10'16",-118°1'25 mapping site and is for general reference only. Data layers that Figure 6 Scale: 1 :8464 N appear on this map may or may not be accurate, current, or SRS: EPSG:3857 otherwise reliable. THIS MAP IS NOT TO BE USED FOR NAVIGATION. UTMZone: 11 Fisher Property- 2018 Rock Samples -table 2.

Sample UTM Easting UTM Northing Date Description Cg% 3029562 0427027 5558114 18-Oct-18 Grab of quartz schist with flake 2.96 graphite 3029563 0427026 5558107 18-Oct-18 Grab of metamorphosed carbonate 3.66 rock with flake graphite 3029564 0427025 5558108 18-Oct-18 Grab of subcrop quartz schist rust 3.71 colored with flake graphite 3029565 0426797 5558395 22-Oct-18 Grab of semi massive flake graphite 7.13 blebs in a metamorphosed carbonate rock 3029566 0426782 5558383 22-Oct-18 Grab of dark black schist with flake 4.77 graphite 10.0 Recommendations On the Fisher claim, the recessive graphite horizon could be drilled without trenching. In addition, if a better control on the conductive horizon is warranted, a ground based EM Survey could be carried out to locate the best drill targets.

-14- 11.0 References Allen, G.S., 2012. Technical Report, Jumbo Property Report 33479 Allen, G.S., 2014. Technical Report, Jumbo Property for Noram Ventures, Report Number 34974 Allen, G.S., 2015. Technical Report, Jumbo Property for Noram Ventures Rock Sampling Survey, Report Number 35894 Doyle, G. 2012 Verbal Information Minfile Records Department of Energy, Mines, and Petroleum Resources. Minfile Search. Reesor, J.E., and Moor, Jr, J.M. Bulletin #195 Petrology and Structure of Thor-Odin Gneiss Dome, Shuswap Metamorphic Complex.

-15- Febuary 2014 REVISION 2.0 ALS) DeochemistrL| Specialty Assay Procedure

C-IR18 - Graphitic Carbon bv LECO

Sample Decomposition: LECO Furnace

Analytical Method: Infrared Spectroscopy

A 0.1 g sample is leached with dilute hydrochloric acid to remove Inorganic carbon. After filtering, washing, and drying, the remaining sample residue is roasted at 425°C to remove organic carbon. The roasted residue is analysed for Carbon - High temperature LECO furnace with infrared detection.

List of Reportable Analytes:

Default Overlimit Analyte Symbol Units Lower Limit Upper Limit Method Carbon E1H 0.02 50 N/A

Page 1 of 1

RIGHT SOLUTIONS | PAR TN R R STATEMENT OF QUALIFICATIONS

I, Bruce Doyle of Nelson, B.C. hereby certify that:

I am a professional prospector and have been involved with mineral exploration since 1982.

I have successfully completed the Advanced Prospecting Course at Mecashi Lake on Vancouver Island 1990.

I have been employed by junior and senior mining companies in British Columbia.

I have been self-employed as a professional prospector since 1990.

I have had over 30 option deals with senior and junior mining companies.

Respectfully Submitted

Bruce Doyle

Nelson B.C.

March,7 2019 COST STATEMENT

Labour:

Bruce Doyle Prospecting rock sampling Oct, 18,22 @375 day $ 750.00

Grant Doyle Prospecting rock sampling Oct, 18,22 @375 day $ 750.00

Analytical Costs:

ALS Labs, Vancouver, B.C.

5 rock samples- Cg Assay $ 253.26

Other Expenses:

Vehicle Rental

Bruce Doyle 2 days @ $150 including fuel $ 300.00

Grant Doyle 1 day @ $150 including fuel $ 150.00

Grant Doyle 1 day Four Trax rental @ $75.00 $ 75.00

Shipping samples $ 27.00

Field supplies $ 20.00

Report preparation $ 550.00

TOTAL COSTS $ 2,875.26 ALS Canada Ltd. To: DOYLE, BRUCE Page: 1 2103 Dollarton Hwy 1424 CREASE AVE Total # Pages: 2 (A) North Vancouver BC V7H 0A7 NELSON BC VIL 1A2 Plus Appendix Pages Phone: +1 (604) 984 0221 Fax: +1 (604) 984 0218 Finalized Date: 14-DEC-2018 www.alsglobal.com/geochemistry This copy reported on 18-DEC-2018 Account: SKJ

QC CERTIFICATE VA18307857 SAMPLE PREPARATION ALS CODE DESCRIPTION

Project: FISHER WEI-21 Received Sample Weight PUL-QC Pulverizing QC Test L0C-21 Sample logging - ClientBarCode This report is for 10 Rock samples submitted to our lab in Vancouver, BC, Canada on CRU-31 Fine crushing - 70% <2mm 3-DEC-2018. SPL-21 Split sample - riffle splitter The following have access to data associated with this certificate: PUL-31 Pulverize split to 8596 <75 urn BRUCE DOYLE | I DISP-01 Disposal of all sample fractions CRU-QC Crushing QC Test

ANALYTICAL PROCEDURES ALS CODE DESCRIPTION INSTRUMENT

C-IR18 Graphitic carbon by LECO LECO

This is the Final Report and supersedes any preliminary report with this certificate number. Results apply to samples as submitted. All pages of this report have been checked and approved for release. Signature: ***** See Appendix Page for comments regarding this certificate ***** Colin Ramshaw, Vancouver Laboratory Manager ALS Canada Ltd. To: DOYLE, BRUCE Page: 2 - A 2103 Dollarton Hwy 1424 CREASE AVE Total # Pages: 2 (A) North Vancouver BC V7H 0A7 NELSON BC VIL 1A2 Plus Appendix Pages Phone: +1 (604) 984 0221 Fax: +1 (604) 984 0218 Finalized Date: 14-DEC-2018 www.alsglobal.com/geochemistry Account: SKJ

Project: FISHER QC CERTIFICATE OF ANALYSIS VA18307857

Method C-IR18 Analyte C Craphl % Sample Description ^OD 0.02

STANDARDS CCC-08 0.42 Target Range • Lower Bound 0.34 Upper Bound 0.44 NCSDC60121 >50 Target Rang* - Lower Bound 71.1 Upper Sound 50.0

BLANKS BLANK <0.02 Target Range - Lower Bound <0.02 Upper Bound 0.04

DUPLICATES 3029567 3.72 DUP 3.73 Target Range - Lower Bound 3.52 Upper Bound 3.93

See Appendix Page for comments regarding this certificate *** ALS Canada Ltd. To: DOYLE, BRUCE Page: Appendix 1 2103 Dollarton Hwy 1424 CREASE AVE Total # Appendix Pages: 1 North Vancouver BC V7H 0A7 NELSON BC VIL 1A2 Finalized Date: 14-DEC-2018 Phone: +1 (604) 984 0221 Fax: +1 (604) 984 0218 Account: SKJ www.alsglobal.com/geochemistry

Project: FISHER QC CERTIFICATE OF ANALYSIS VA18307857

CERTIFICATE COMMENTS

LABORATORY ADDRESSES Processed at ALS Vancouver located at 2103 Dollarton Hwy, North Vancouver, BC, Canada. Applies to Method: C-IR18 CRU-31 CRU-QC DISP-01 LOG-21 PUL-31 PUL-QC SPL-21 WEI-21 VA18307857-Finalized CLIENT: "S Bruce" # of SAMPLES: 10 DATE RECEIVED : 2018-12-03 DATE FINALIZED : 2018-12-14 PROJECT: "FISHER" CERTIFICATE COMMENTS: PO NUMBER : " " C-IR18 SAMPLE C Graphitic DESCRiPTIC%

3029562 2.96 3029563 3.66 3029564 3.71 3029565 7.13 3029566 4.77