benji ass 2015 - newfoundland and labrador · second year assessment report on prospecting, recee...

Government of Newfoundland and Labrador Department of Natural Resources

Mineral Lands Division

Geological Survey No:

Registry File Nos:

Confidential Until:

Mineral Rights:

Licence Extended Licence Impost Mining Lease Regional Other

Licence/Property

No. of Claims Assessment Year

Date Issued

NTS Map

Continued next page Yes No Number of Volumes: Digital Copy Only Enclosures (indicate number of each): CD: DVD: Flash drive: Paper Maps: Other: Received: Comments:

Signed: Date:

✔

✔

✔

2017.06.07 11:53:36 -02'30'

002E/1925

1

Second Year Assessment Report on prospecting, Recee geophysics and Petrography reports on the

Benji/Finecrack Property, licences 023048M,023045M and 021569M NTS 2E/01 and 2E/02, Newfoundland and

Labrador.

For Clyde Burt, Perry Warren and Garth Graves

Work completed from Oct 2014 to Oct, 2015

Total Eligible Expenditures $9015.36

Work Year 2

Total Claims 30

Oct 7/2015

Written By Clyde Burt

2

Contents Introduction................................................................................................................................................3 Location andAccess.................................................................................................................................4 Previous Work..........................................................................................................................................4 Geology and Mineralization/Current work............................................................................................5

Property Location……………………………………………………………………………………………………………………..6 Sample Report Sheet..........................................................................................................................7 Results .....................................................................................................................................................8 Em ‐16 Data………………………………………………………………………………………………………………………………………..9‐11 Statement of Expenses……………………………………………………………………………………………………………………..12‐13

3

Introduction The Benji/Finecrack Project includes claims in M license under Clyde Burt and Perry Warren in partnership with Garth Graves. The claims are located near Island Pond, approximately 17 km north of the community of Gander. The property was staked in 2013 for its copper potential which was exposed after new quarry operations on the property. Initial assays showed elevated vanadium and titanium and copper.

4

Location and Access The Benji property is located in NTS map areas 2E/02, just off a woods road off highway 330 North of Gander (Figure 1).

Previous Work The area was first worked by International Mogul Mines in 1975. An airbourne Mag/Em survey that identified a coincidental Mag/Em anomaly was referred to as system 21. A grid (21A) was cut in the general area of the quarry and surface geophysics was conducted (mag/Em) outlining an Em conductor with a large mag anomaly flanking the west side of the conductor. One drill hole 75-9 was drilled just to the north of the quarry with no sampling at the time. Recent sampling of the drill core(Pasadena) has returned anomalous vanadium and titanium. The area of the recent exposed quarry was deemed at the time to be a #2 priority but never drilled. In the early 90’s Gander River Minerals did a recce soil survey over the area and after reviewing the Geofiles anomalous Vanadium values (200 ppm range) were recorded in the analysis’ of the soil.

5 Geology and Mineralization

The Benji/Finecrack properties cover rocks belonging to the Gander River Ultrabasic Belt (GRUB), a

continuous 2 to 6 km wide belt of plutonic and volcanic units north of Gander Lake. Generally mafic to

ultramafic in composition, the GRUB represents a major structural boundary between the Gander

Dunnage Terranes. The GRUB is structurally above and in fault contact to the east with metasediments

of the Lower Ordovician or earlier Gander Group, and nonconformably overlain and bounded to the

west by sediments of the Middle Ordovician Davidsville Group. Small outliers (windows) of Davidville

Group sediments occur within the GRUB.

On the property, rocks belonging to the GRUB include ultramafics (pyroxenite), altered

(serpentinite,magnesite and talc‐tremolite schist), gabbro, mafic flows ,trondhjemite and porphyry. The

pyroxinite is generally massive, and occurs as elliptical pods, within gabbro. The altered ultramafic rocks

occur as linier and elliptical zones of dominantly magesite‐rich carbonate and serpentinite, with minor

talc and tremolite. Disseminate Chromite occurs as regular 1 to 2cm bands in magnesite. Schistope yalc‐

carbonate zones trend northeast, with moderate to steep dips. The gabbro is the dominate GRUB unit

on the property, with minor diorite and tonalite. The gabbro varies from massive to strongly foliated,

with local mylonite zones. The dark green mafic flows are pillowed or massive and commonly

amgdaloidal. A north‐northeast trending penetrative foliation is present in the mafic flows, with chlorite

schist developed locally. The trondhjemite occurs along the western portion of the GRUB and is

commonly brecciated. (copied from Geofile 002E/0577 written by Raymond L Kohlsmith, Falconbridge

Ltd)

2nd year work consisted of prospecting, drilling 1 meter deep core samples in Benji showing and recee

Mag and Vlf(EM‐16). Research found an updated airbourne survey that better outlines the system 21

Airbourne anomaly. Both the Finecrack and Benji showings lie with‐in this‐oval shaped mag anomaly.

7 SD 15070910

Sample# Location UTM North

Utm East Type Mineralization Comments

127459 Finecrack East 5442785 682400 O/C 2‐3 % sul Altered mafic on System 21

127460 Finecrack East 5442795 682410 O/C 2‐3% sul Airbourne Mag Anomaly

SD 14190605

Sample# Depth Location

North

East Type Cu ppm V205 % Ti02%

Ag ppm

Fe %

Cu %

127210 Van Pit 105N 35E Rubble 11500 0.748 8.27 2.03 30.8 1.15

127212 0.7M Van Pit 97N 30E CORE 129 0.176 2.77 0.05 16.4

127213 0.7M Van Pit 100N 38E CORE 596 0.268 4.47 0.09 23.4

127214 0.7M Van Pit 100N 45E CORE 416 0.196 3.84 0.10 25.4

127215 Van Pit 95N 45E rubble 4740 0.311 5.61 1.06 27.7 0.47

127216 Van Pit 95N 30E O/C 5500 0.305 4.14 1.10 21.7 0.55

127217 Van Pit 100N 46E O/C 1960 0.066 1.25 0.39 24.5 0.20

127218 Van Pit 109N 28E O/C 241 0.189 2.66 0.10 16.2

SD 15004041

Sample# Location UTM North

Utm East Type Mineralization Alteration Comments

127313 Benji/FC 5442925 682000 float angular subcrop

127314 Benji/FC 5443106 682359 O/C

127315 Benji/FC 5441515 681173 O/C

127316 Benji/FC 5442435 681720 O/C

127317 Benji/FC 5442967 681947 O/C 1‐3 % py/po Sil

127318 Benji/FC 5443616 681833 O/C 1‐3 % sulphides Ultra mafic

127319 Benji/FC 5443733 681879 O/C Gabbro

127320 Benji/FC 5443469 681746 O/C 2‐3 % sulphides Ultra mafic

127321 Benji/FC 5443305 681919 O/C Tr‐1% sulphide Sil Altered mafic

127322 Benji/FC 5442724 681849 O/C 2‐3 % sulphides Mafic/Ultra mafic

127323 Benji/FC 5442375 681668 O/C sheared Altered mafic

127324 Benji/FC 5440621 680942 O/C Sil

8 Results Results in prospecting improved the higher Cu grades on both the Benji (up to 1.15% Cu) and Finecrack

(12.0% Cu) showings. Petrography on the Benji helped confirming the geoglogy however was

unsuccessful in identifying the source of the vanadium. Recee mag and Vlf was very successful in

outlining the “system 21” airbourne anomaly.

9 VLF Em ‐16v Data

UTM in‐phase out‐of‐phase Fraser Filter Comments

680440E/5443916N ‐6 3

12.5E ‐6 2

‐16

25E ‐6 ‐1

‐26

37.5E 10 2

‐42

50E 14 ‐2

‐17

62.5E 24 1

4

75E 17 ‐8

0

87.5E 17 ‐9

‐5

100E 24 ‐8

16

112.5E 15 ‐6

21

125E 10 ‐5

‐1

137.5E 8 ‐3

‐1

150E 18 ‐4

4

162.5E 18 ‐3

24

175E 4 3

50

187.5E 8 4

56

200.0E ‐36 15

‐26

212.5E ‐8 12

10

‐64

225E 6 8 Benji Pit

‐25

237.5E 14 5

7

250E 9 3

31

237.5E 4 5

38

250E ‐12 5

18

262.5E ‐13 8

2

275E ‐14 20

‐8

287.5E ‐10 22

‐25

300E ‐9 24

‐24

312.5E 10 24

‐10

325E ‐5 18

14

337.5E ‐4 20

12

350E ‐5 18

‐23

362.5E ‐16 10

‐45

375E 30 ‐20 O/C Cu/V top of hill

‐4

387.5E ‐6 14

28

400E ‐4 18

‐4

412.5E 0 14

2

425E ‐6 10

‐9

11

437.5E 0 10

450E 3 14 681200E 5443385N

12

Statement of Expenses. Lic 023048M Prospecting, recee geophysics 24 days @ $100/day $2400.00 Clyde Burt 11.5 days Kristopher Burt 2 days Nicholas Burt 4 days Perry Warren 5 days Andrew Burt 0.5 day Dan Lee 1 day Report preparation 2 days @ $100 $200.00 Analytical Charges $1123.52 Shipping samples $126.87 Thin Sections VanPetro $694.05 Truck use 14 days @ $60 $840.00 Per Diem 24 @ $30 $720.00 Gas $ 815.00 Sub-Total $6919.44 15% overhead $1037.92 Total $7957.36

13

Statement of Expenses. Lic 023045M Prospecting, recee geophysics 2 days @ $100/day $200.00 Clyde Burt 1 day Kristopher Burt 1 day Truck use 1 days @ $60 $60.00 Per Diem 2 @ $30 $60.00 Gas $30.00 Sub-Total $350.00 Overhead 15% $52.50 TOTAL $402.50

Note This claim block is covers a large bog. Prospecting was not successful in finding outcrop.

14

Statement of Expenses. Lic 021569M Prospecting, recee geophysics 3 days @ $100/day $300.00 Clyde Burt 1.5 day Kristopher Burt 1 day Andrew Burt 0.5 day Truck use 2 days @ $60 $120.00 Per Diem 3 @ $30 $90.00 Gas $ 60.00 Sub-Total $570.00 Overhead 15% $85.50 TOTAL $655.50

Note This claim block lies just east of the mag anomaly. Prospecting was unsuccessful in finding significant mineralization. Recee mag is included in the Finecrack East survey map.

ALS CODE DESCRIPTION

SAMPLE PREPARATION

WEI-21 Received Sample WeightLOG-22 Sample login - Rcd w/o BarCodeCRU-31 Fine crushing - 70% <2mmSPL-21 Split sample - riffle splitterCRU-QC Crushing QC TestPUL-QC Pulverizing QC TestPUL-31 Pulverize split to 85% <75 umLOG-24 Pulp Login - Rcd w/o Barcode


ANALYTICAL PROCEDURES

ME-MS61 48 element four acid ICP-MSME-OG62 ICP-AESOre Grade Elements - Four AcidCu-OG62 VARIABLEOre Grade Cu - Four AcidPGM-ICP24 ICP-AESPt, Pd, Au 50g FA ICP

CERTIFICATE SD14190605

This report is for 8 Drill Core samples submitted to our lab in Sudbury, ON, Canada on 11-DEC-2014.

Project: BENJI

The following have access to data associated with this certificate:CLYDE BURT

CLYDE BURTATTN: CLYDE BURTGLENWOOD NL

To:

Page: 1Total # Pages: 2 (A - D)

Plus Appendix PagesFinalized Date: 24-DEC-2014

Account: CBP

CLYDE BURTGLENWOOD NL

To:ALS Canada Ltd.

2103 Dollarton HwyNorth Vancouver BC V7H 0A7 Phone: 604 984 0221 Fax: 604 984 0218 www.alsglobal.com

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:

Colin Ramshaw, Vancouver Laboratory Manager***** See Appendix Page for comments regarding this certificate *****

Page: 2 - ATotal # Pages: 2 (A - D)


Account: CBP

ALS Canada Ltd.



To:

Project: BENJI

CERTIFICATE OF ANALYSIS SD14190605

Sample Description

MethodAnalyteUnitsLOR

WEI-21 ME-MS61 ME-MS61 ME-MS61 ME-MS61 ME-MS61 ME-MS61 ME-MS61 ME-MS61 ME-MS61 ME-MS61 ME-MS61 ME-MS61 ME-MS61 ME-MS61Recvd Wt. Ag Al As Ba Be Bi Ca Cd Ce Co Cr Cs Cu Fe

kg ppm % ppm ppm ppm ppm % ppm ppm ppm ppm ppm ppm %0.02 0.01 0.01 0.2 10 0.05 0.01 0.01 0.02 0.01 0.1 1 0.05 0.2 0.01

127210 0.97 2.03 3.95 5.1 70 0.08 0.16 4.56 2.61 0.41 242 210 11.65 >10000 30.8127212 0.55 0.05 4.63 3.0 10 0.10 0.01 7.30 0.08 1.80 77.0 28 2.83 129.0 16.40127213 0.57 0.09 3.56 2.1 40 0.07 0.02 5.44 0.07 0.92 80.4 26 16.60 596 23.4127214 0.62 0.10 3.73 41.2 370 0.09 0.08 3.93 0.03 1.16 65.2 39 127.0 416 25.4127215 0.22 1.06 3.50 7.6 90 0.07 0.21 5.14 0.79 0.69 248 123 17.30 4740 27.7

127216 0.22 1.10 6.79 2.3 30 0.06 0.15 3.40 2.30 0.96 67.5 78 7.76 5500 21.7127217 0.16 0.39 3.28 9100 90 <0.05 0.27 6.35 0.46 0.89 89.4 53 179.5 1960 24.5127218 0.30 0.10 3.91 7.1 40 0.11 0.06 8.01 0.09 1.24 94.3 75 5.22 241 16.20

***** See Appendix Page for comments regarding this certificate *****

Page: 2 - BTotal # Pages: 2 (A - D)


Account: CBP

ALS Canada Ltd.



To:

Project: BENJI


Sample Description


ME-MS61 ME-MS61 ME-MS61 ME-MS61 ME-MS61 ME-MS61 ME-MS61 ME-MS61 ME-MS61 ME-MS61 ME-MS61 ME-MS61 ME-MS61 ME-MS61 ME-MS61Ga Ge Hf In K La Li Mg Mn Mo Na Nb Ni P Pb

ppm ppm ppm ppm % ppm ppm % ppm ppm % ppm ppm ppm ppm0.05 0.05 0.1 0.005 0.01 0.5 0.2 0.01 5 0.05 0.01 0.1 0.2 10 0.5

127210 22.0 0.15 0.1 0.112 0.04 <0.5 3.6 2.47 1020 0.52 0.17 0.1 126.5 10 15.0127212 17.70 0.09 0.4 0.127 0.02 <0.5 0.9 6.93 1690 0.23 0.92 0.2 36.2 60 2.2127213 26.0 0.12 0.2 0.107 0.05 <0.5 1.5 4.30 2040 0.25 0.35 0.1 31.5 100 5.0127214 25.0 0.20 0.2 0.097 0.34 <0.5 1.7 4.22 1700 0.16 0.25 0.2 27.7 40 5.7127215 16.00 0.18 0.2 0.083 0.06 <0.5 2.4 3.43 1140 0.19 0.47 0.1 131.0 20 13.1

127216 15.40 0.15 0.2 0.063 0.02 <0.5 22.0 5.45 1560 0.30 0.46 0.2 33.2 20 2.6127217 13.20 0.20 0.1 0.062 0.44 <0.5 6.1 2.23 1280 0.21 0.22 0.1 33.5 <10 5.2127218 13.00 0.07 0.3 0.087 0.03 <0.5 1.8 6.70 1550 0.17 0.87 0.1 49.9 40 5.2


Page: 2 - CTotal # Pages: 2 (A - D)


Account: CBP

ALS Canada Ltd.



To:

Project: BENJI


Sample Description


ME-MS61 ME-MS61 ME-MS61 ME-MS61 ME-MS61 ME-MS61 ME-MS61 ME-MS61 ME-MS61 ME-MS61 ME-MS61 ME-MS61 ME-MS61 ME-MS61 ME-MS61Rb Re S Sb Sc Se Sn Sr Ta Te Th Ti Tl U V

ppm ppm % ppm ppm ppm ppm ppm ppm ppm ppm % ppm ppm ppm0.1 0.002 0.01 0.05 0.1 1 0.2 0.2 0.05 0.05 0.2 0.005 0.02 0.1 1

127210 4.1 <0.002 8.61 1.20 30.4 35 0.4 12.6 <0.05 0.11 <0.2 4.96 0.11 <0.1 4190127212 1.1 <0.002 1.03 0.69 86.0 4 0.4 43.7 <0.05 <0.05 <0.2 1.660 0.03 <0.1 987127213 7.1 0.002 3.02 3.03 51.0 10 0.3 24.1 <0.05 <0.05 <0.2 2.68 0.16 <0.1 1500127214 52.1 <0.002 5.08 11.40 58.1 13 0.4 70.6 <0.05 0.09 <0.2 2.30 0.25 <0.1 1100127215 6.8 0.002 9.61 2.56 41.7 32 0.3 25.9 <0.05 0.13 <0.2 3.36 0.21 <0.1 2840

127216 2.9 <0.002 1.06 1.91 52.7 7 0.3 19.0 <0.05 0.62 <0.2 2.48 0.04 <0.1 1710127217 75.0 0.002 >10.0 18.05 44.4 32 0.2 239 <0.05 0.91 <0.2 0.750 0.28 <0.1 372127218 1.8 <0.002 3.52 2.14 91.2 14 0.6 32.5 <0.05 <0.05 <0.2 1.595 0.10 <0.1 1060


Page: 2 - DTotal # Pages: 2 (A - D)


Account: CBP

ALS Canada Ltd.



To:

Project: BENJI


Sample Description


ME-MS61 ME-MS61 ME-MS61 ME-MS61 Cu-OG62 PGM-ICP24 PGM-ICP24 PGM-ICP24W Y Zn Zr Cu Au Pt Pd

ppm ppm ppm ppm % ppm ppm ppm0.1 0.1 2 0.5 0.001 0.001 0.005 0.001

127210 1.3 4.7 127 3.4 1.150 0.009 <0.005 <0.001127212 0.4 21.9 70 7.7127213 0.5 10.4 116 4.3127214 2.8 16.5 105 4.7127215 0.9 8.2 78 4.1

127216 0.8 13.6 91 5.4127217 18.0 10.5 56 2.3 0.224 <0.005 <0.001127218 0.2 16.6 59 6.4


Page: Appendix 1 Total # Appendix Pages: 1

Finalized Date: 24-DEC-2014Account: CBP

ALS Canada Ltd.



To:

Project: BENJI


CERTIFICATE COMMENTS

ANALYTICAL COMMENTSREE's may not be totally soluble in this method.ME-MS61Applies to Method:

LABORATORY ADDRESSESProcessed at ALS Sudbury located at 1351-B Kelly Lake Road, Unit #1, Sudbury, ON, Canada.CRU-31Applies to Method: CRU-QC LOG-22 LOG-24PUL-31 PUL-QC SPL-21 WEI-21

Processed at ALS Vancouver located at 2103 Dollarton Hwy, North Vancouver, BC, Canada.Cu-OG62Applies to Method: ME-MS61 ME-OG62 PGM-ICP24


SAMPLE PREPARATION

WEI-21 Received Sample WeightLOG-22 Sample login - Rcd w/o BarCodeCRU-31 Fine crushing - 70% <2mmSPL-21 Split sample - riffle splitterCRU-QC Crushing QC TestPUL-QC Pulverizing QC TestPUL-31 Pulverize split to 85% <75 um



ME-MS61 48 element four acid ICP-MSPGM-ICP24 ICP-AESPt, Pd, Au 50g FA ICP


This report is for 12 Rock samples submitted to our lab in Sudbury, ON, Canada on 9-JAN-2015.

Project: GBR


PERRY WARRENATTN: CLYDE BURTGLENWOOD NL

To:


Plus Appendix PagesFinalized Date: 20-JAN-2015

Account: CBPPW

PERRY WARRENGLENWOOD NL

To:ALS Canada Ltd.






Account: CBPPW

ALS Canada Ltd.



To:

Project: GBR


Sample Description




127313 0.47 0.02 7.82 6.8 60 0.27 0.02 5.70 0.07 7.20 46.8 23 0.78 62.0 8.73127314 0.47 0.03 1.15 <0.2 10 <0.05 0.01 10.80 0.06 0.12 59.6 800 1.03 117.0 6.70127315 0.36 0.02 7.91 1.0 60 0.23 0.01 5.61 0.30 5.40 41.5 34 0.72 88.2 9.76127316 0.55 0.08 7.76 7.7 60 0.24 0.01 1.76 0.07 8.01 30.5 3 0.65 9.0 8.89127317 0.59 0.02 7.59 3.7 210 0.19 0.01 4.20 0.11 4.47 36.0 29 0.65 57.7 9.36

127318 0.85 <0.01 8.94 0.6 <10 0.06 0.01 5.85 0.03 0.34 82.4 7 0.57 13.1 16.25127319 0.66 0.01 4.74 <0.2 <10 <0.05 0.01 8.96 0.03 0.64 59.5 198 0.16 8.6 7.03127320 0.76 0.03 8.19 0.4 70 0.11 0.02 3.91 0.09 1.59 32.6 5 1.60 54.1 9.57127321 0.61 0.01 6.53 1.2 40 0.31 0.04 1.57 0.02 7.26 6.3 12 1.16 2.7 3.97127322 0.77 0.07 7.57 1.1 20 0.24 0.04 3.80 0.14 5.34 40.2 17 0.44 280 9.97

127323 0.49 0.01 7.27 0.5 30 0.29 0.01 5.74 0.06 6.41 41.3 2 0.58 46.3 10.35127324 0.61 0.02 5.84 2.2 40 0.29 0.02 0.15 <0.02 25.0 1.1 17 0.43 6.2 1.52




Account: CBPPW

ALS Canada Ltd.



To:

Project: GBR


Sample Description




127313 19.40 0.23 1.4 0.063 0.30 2.0 13.6 3.45 1670 1.01 2.05 0.6 15.2 360 1.9127314 2.23 0.05 <0.1 0.018 <0.01 <0.5 1.9 12.00 1500 0.08 0.05 <0.1 162.5 <10 <0.5127315 17.70 0.10 0.9 0.085 0.76 1.5 10.5 4.42 1540 0.13 2.54 0.6 21.3 390 1.1127316 20.4 0.13 1.8 0.066 0.40 2.4 15.7 2.12 1200 0.10 4.20 0.8 3.5 560 <0.5127317 16.45 0.12 1.0 0.069 0.68 1.2 13.0 3.64 1480 0.27 2.98 0.5 19.4 300 0.9

127318 22.9 0.07 0.1 0.054 <0.01 <0.5 22.3 3.99 2190 0.06 0.07 0.1 12.5 30 0.5127319 6.21 <0.05 0.1 0.028 0.03 <0.5 6.1 10.10 1130 0.06 0.80 <0.1 139.5 20 0.6127320 15.95 0.07 0.3 0.061 0.04 0.6 9.1 2.62 1830 1.03 4.03 0.2 9.0 280 6.6127321 11.55 0.17 1.0 0.089 0.25 2.8 7.0 0.54 655 0.57 3.31 0.5 1.4 280 2.0127322 17.85 0.08 1.0 0.074 0.13 1.6 8.0 3.60 1720 0.73 3.15 0.5 15.7 360 1.7

127323 19.20 0.08 1.4 0.076 0.36 2.0 18.7 3.78 1580 0.11 3.12 0.6 8.5 370 1.2127324 9.29 0.18 1.8 0.024 0.11 12.9 4.8 0.23 141 0.97 4.40 0.9 1.1 110 0.9




Account: CBPPW

ALS Canada Ltd.



To:

Project: GBR


Sample Description




127313 6.7 0.004 0.27 0.12 41.3 2 0.4 184.5 <0.05 <0.05 0.3 0.711 0.03 0.2 392127314 0.3 <0.002 <0.01 0.13 75.1 <1 <0.2 6.2 <0.05 <0.05 <0.2 0.045 <0.02 <0.1 205127315 4.6 <0.002 0.08 0.22 46.1 1 0.6 237 0.05 <0.05 0.2 0.781 0.02 0.1 361127316 3.5 0.002 1.75 2.64 35.1 6 0.3 72.8 0.07 <0.05 0.4 0.737 0.05 0.2 242127317 2.6 0.002 0.06 0.21 42.1 1 0.5 175.5 <0.05 <0.05 0.2 0.692 0.02 0.1 381

127318 0.1 <0.002 0.07 0.21 48.4 1 <0.2 138.5 <0.05 <0.05 <0.2 0.278 <0.02 <0.1 445127319 0.4 <0.002 <0.01 0.10 66.5 <1 <0.2 53.9 <0.05 <0.05 <0.2 0.089 <0.02 <0.1 197127320 0.1 0.003 0.18 0.26 48.0 1 0.2 62.0 <0.05 <0.05 <0.2 0.436 0.02 0.1 280127321 3.3 0.002 0.14 0.40 19.2 1 0.4 134.5 <0.05 <0.05 0.6 0.170 <0.02 0.3 32127322 0.6 0.014 0.47 0.14 41.2 2 0.7 130.0 <0.05 <0.05 0.2 0.720 <0.02 0.1 387

127323 2.9 <0.002 0.02 0.40 44.4 1 0.3 94.4 <0.05 <0.05 0.2 0.909 <0.02 0.1 565127324 1.8 0.002 0.10 0.22 10.6 1 0.3 59.3 0.06 <0.05 0.6 0.098 <0.02 0.2 6




Account: CBPPW

ALS Canada Ltd.



To:

Project: GBR


Sample Description


ME-MS61 ME-MS61 ME-MS61 ME-MS61 PGM-ICP24 PGM-ICP24 PGM-ICP24W Y Zn Zr Au Pt Pd

ppm ppm ppm ppm ppm ppm ppm0.1 0.1 2 0.5 0.001 0.005 0.001

127313 0.1 22.6 73 38.5 0.002 <0.005 <0.001127314 0.1 0.9 34 <0.5 0.098 0.026 0.105127315 <0.1 24.3 102 16.5 <0.001 <0.005 <0.001127316 0.1 33.7 64 53.5 0.003 <0.005 <0.001127317 0.1 19.7 95 23.6 <0.001 <0.005 <0.001

127318 0.2 4.4 107 2.2 <0.001 <0.005 <0.001127319 0.1 4.2 30 2.2 <0.001 <0.005 <0.001127320 0.1 8.1 96 6.6 <0.001 <0.005 <0.001127321 0.5 23.7 33 30.1 <0.001 <0.005 <0.001127322 0.1 22.6 93 21.3 <0.001 <0.005 <0.001

127323 0.2 24.4 66 37.8 <0.001 <0.005 <0.001127324 0.3 17.9 6 51.6 <0.001 <0.005 <0.001



Finalized Date: 20-JAN-2015Account: CBPPW

ALS Canada Ltd.



To:

Project: GBR




LABORATORY ADDRESSESProcessed at ALS Sudbury located at 1351-B Kelly Lake Road, Unit #1, Sudbury, ON, Canada.CRU-31Applies to Method: CRU-QC LOG-22 PUL-31PUL-QC SPL-21 WEI-21

Processed at ALS Vancouver located at 2103 Dollarton Hwy, North Vancouver, BC, Canada.ME-MS61Applies to Method: PGM-ICP24


SAMPLE PREPARATION

WEI-21 Received Sample WeightLOG-22 Sample login - Rcd w/o BarCodeCRU-31 Fine crushing - 70% <2mmSPL-21 Split sample - riffle splitterPUL-QC Pulverizing QC TestPUL-31 Pulverize split to 85% <75 um



ME-MS61 48 element four acid ICP-MSPGM-ICP23 ICP-AESPt, Pd, Au 30g FA ICP


This report is for 2 Rock samples submitted to our lab in Sudbury, ON, Canada on 15-MAY-2015.

Project: BENJI EAST


CLYDE BURTATTN: CLYDE BURTGLENWOOD NL

To:


Plus Appendix PagesFinalized Date: 27-MAY-2015

This copy reported on 28-MAY-2015Account: CBP


To:ALS Canada Ltd.

2103 Dollarton HwyNorth Vancouver BC V7H 0A7 Phone: +1 (604) 984 0221 Fax: +1 (604) 984 0218 www.alsglobal.com





Account: CBP

ALS Canada Ltd.



To:

Project: BENJI EAST


Sample Description




127459 0.47 0.03 1.03 <0.2 10 <0.05 0.02 10.80 0.06 0.14 52.7 681 1.09 10.7 5.49127460 0.39 0.03 1.27 0.3 20 <0.05 0.02 10.35 0.13 0.09 53.9 898 1.32 165.5 6.03




Account: CBP

ALS Canada Ltd.



To:

Project: BENJI EAST


Sample Description




127459 2.25 <0.05 <0.1 0.013 0.01 <0.5 5.3 11.90 1460 0.30 0.04 <0.1 126.0 <10 0.9127460 2.51 <0.05 <0.1 0.016 0.01 <0.5 7.1 12.00 1780 0.11 0.04 <0.1 159.5 10 1.2




Account: CBP

ALS Canada Ltd.



To:

Project: BENJI EAST


Sample Description




127459 0.7 <0.002 <0.01 0.52 74.0 <1 <0.2 6.1 <0.05 <0.05 <0.2 0.044 <0.02 <0.1 187127460 1.0 <0.002 <0.01 0.50 83.8 <1 <0.2 5.0 <0.05 <0.05 <0.2 0.051 <0.02 <0.1 227




Account: CBP

ALS Canada Ltd.



To:

Project: BENJI EAST


Sample Description


ME-MS61 ME-MS61 ME-MS61 ME-MS61 PGM-ICP23 PGM-ICP23 PGM-ICP23W Y Zn Zr Au Pt Pd

ppm ppm ppm ppm ppm ppm ppm0.1 0.1 2 0.5 0.001 0.005 0.001

127459 0.1 0.8 34 <0.5 <0.001 0.007 0.017127460 0.2 1.0 53 <0.5 0.016 0.039 0.106



Finalized Date: 27-MAY-2015Account: CBP

ALS Canada Ltd.



To:

Project: BENJI EAST




LABORATORY ADDRESSESProcessed at ALS Sudbury located at 1351-B Kelly Lake Road, Unit #1, Sudbury, ON, Canada.CRU-31Applies to Method: LOG-22 PUL-31 PUL-QCSPL-21 WEI-21

Processed at ALS Vancouver located at 2103 Dollarton Hwy, North Vancouver, BC, Canada.ME-MS61Applies to Method: PGM-ICP23

PETROGRAPHIC REPORT ON 2 SAMPLES OF MAFIC/ULTRAMAFIC ROCK WITH

SULFIDE MINERALIZATION

Report for: Clyde Burt Invoice 140971

24 Valley Road

P.O. Box 98, Glenwood,

Newfoundland A0G 2K0 (709) 679-2235 Jan. 13, 2015.

SUMMARY:

Capsule descriptions are as follows:

127210: ultramafic rock (originally amphibolite?) with minor, disseminated primary oxide (ilmenite)-

sulfide (pyrrhotite) mineralization, strongly affected by alteration to secondary biotite-chlorite-Mg

carbonate-minor fibrous secondary amphibole, associated with stronger pyrrhotite/local chalcopyrite

mineralization, partly remobilized into fracture veinlets. The source of the anomalous Ti and Cu is

obvious, but the locus for the V is not.

127211: mafic (originally gabbroic?) rock composed of amphibole and former plagioclase (?), minor

interstitial ilmenite and rare chalcopyrite, strongly altered to epidote-chlorite-minor sphene-trace

hematite. The source of anomalous V is uncertain.

Detailed petrographic descriptions and photomicrographs are appended (by email attachment). If you

have any questions regarding the petrography, please do not hesitate to contact me.

Craig H.B. Leitch, Ph.D., P. Eng. (250) 653-9158 [email protected]

492 Isabella Point Road, Salt Spring Island, B.C. Canada V8K 1V4

2

127210: ULTRAMAFIC ROCK (AMPHIBOLITE?) WITH MINOR, DISSEMINATED PRIMARY

OXIDE (ILMENITE)-SULFIDE (PYRRHOTITE) MINERALIZATION, STRONGLY AFFECTED

BY ALTERATION TO SECONDARY BIOTITE-CHLORITE-MG CARBONATE-MINOR

FIBROUS SECONDARY AMPHIBOLE, ASSOCIATED WITH STRONGER PYRRHOTITE AND

LOCAL CHALCOPYRITE MINERALIZATION, PARTLY REMOBILIZED INTO FRACTURES

Described as mafic/ultramafic rock with sulfide mineralization (possibly primary pyrrhotite,

secondary chalcopyrite/bornite/pyrite, local magnetite and ilmenite), containing anomalous V, Cu and

Ti; hand specimen shows very fine-grained, blackish-green, sulfide-rich rock with variably pyrrhotite

or chalcopyrite enriched, irregular disjointed veinlets. The rock is strongly magnetic, shows trace

very slow, minor reaction to cold dilute HCl (only where scratched), and no stain for K-feldspar in

the etched offcut. Modal mineralogy in polished thin section is approximately:

Amphibole (hornblende?), variably retrograded 50%

Pyrrhotite (variably remobilized, e.g. into veinlets) 15%

Biotite (secondary; partly chloritized) 15%

Chlorite (variable composition; largely after biotite) 5%

Carbonate (magnesite?) 5%

Chalcopyrite 3%

Ilmenite 1-2%

Sphene (?) <1%

This sample is roughly divisible into two halves, one more primary (amphibole, minor secondary

minerals, minor sulfides and oxides) and the other mainly secondary (composed mostly of sulfides

and biotite-chlorite-carbonate, after amphibole?), minor relict ilmenite. Sulfides, mainly pyrrhotite,

occur in the latter either as fine disseminations intimately associated with carbonate and micas,

suggestive of secondary origin, or along discontinuous veinlets, suggestive of remobilization.

In the less altered portion, amphibole forming relatively coarse, but commonly highly

fractured, disrupted subhedral crystals up to 8 mm long (with more or less random orientations) are

attacked and replaced along a network of fractures or around margins by the same set of secondary

minerals seen in the more altered portion (biotite, chlorite, minor carbonate, trace sphene), mostly

concentrated along the fractures. Yellow stain in the offcut, also mostly along the fractures, is likely

due to potassium in the biotite since no K-feldspar is noted in thin section. The amphibole shows

weak pleochroism from pale brownish to pale greenish, suggestive of primary or late-magmatic

hornblende, although extinction angle is rarely over 12º, suggestive of actinolitic hornblende. At

margins and along fractures, it is locally replaced by almost colourless to pale sea-green, fibrous finer

grained amphibole (secondary tremolite-actinolite?). Within the larger fracture veinlets, mostly <1

mm thick, alteration is to biotite and chlorite as described below. Ilmenite occurs as aggregates up to

~2mm across, composed of rounded subhedra <0.5 mm, typically associated with aggregates up to

1.5 mm across of fine-grained pyrrhotite or chalcopyrite (subhedra mainly <0.2 mm). These sulfide-

oxide aggregates are interstitial to the amphibole, strongly suggestive of primary oxide/sulfide

accumulations in an ultramafic rock (amphibolite). Where larger aggregates occur, they are typically

in the form of veinlets <3 mm thick, in which chalcopyrite predominates as subhedra <0.25 mm and

pyrrhotite is much less common, but of similar size.

In the strongly altered half, after a transition zone in which relict amphibole crystals are partly

replaced by fibrous amphibole partly interleaved by secondary biotite (subhedral flakes <0.4 mm

with dark brownish green pleochroism) and “spotted” by minute crystals of carbonate (euhedra <0.1

mm), amphibole all but disappears to be almost entirely replaced by biotite, chlorite, carbonate and

associated fine-grained sulfides. The biotite (and phlogopite?) typically forms sub/euhedral flakes

either up to 0.5 mm with dark greenish brown pleochroism or mostly <0.1 mm, with faint brownish

pleochroism, the latter mainly controlled along the fracture system, where it stains faintly yellow in

etched offcut, likely due to potassium content. Commonly, the latter is converted in places to chlorite

that is either pale green and length-slow (more iron-rich, with Fe:Fe+Mg, or F:M, ratio above 0.5,

3

possibly 0.6?) or almost colourless and length-fast (more magnesian, with F:M 0.3-0.4?) as sub- to

euhedral flakes up to0.3 mm. Carbonate occurs in intricate networks of minute fractures <0.2 mm

thick, where it forms sub-equant or slender needle-like euhedra <0.1 mm long with strong relief

change (and anisotropy in reflected light) on rotation, which together with lack of reaction to HCl in

hand specimen suggests magnesian (or Fe-Mg) rich composition, such as magnesite (or siderite?).

The carbonate is intimately intergrown with sulfides, mainly pyrrhotite as very fine-grained, tabular

subhedra rarely over 0.1 mm, suggestive of replacement of former silicates accompanying biotite-

chlorite alteration. However, the pyrrhotite commonly surrounds aggregates of ilmenite similar to

those described above, at least permissive of a primary (magmatic) origin for the oxides and part of

the sulfides. Chalcopyrite is almost entirely restricted to short, stubby segments of veinlets up to 2

mm thick by ~5 mm long, where it forms ragged subhedra mainly <0.25 mm and is accompanied by

pyrrhotite as rounded subhedra up to 0.5 mm, suggestive of remobilization (i.e., “secondary”) origin.

There may be minor sphene (?) associated with carbonate rimming/alteration of ilmenite.

In summary, this sample appears to represent ultramafic rock (originally amphibolite?) with

minor, disseminated primary oxide (ilmenite)-sulfide (pyrrhotite) mineralization, strongly affected by

alteration to secondary biotite-chlorite-Mg carbonate-minor fibrous secondary amphibole, associated

with stronger pyrrhotite and local chalcopyrite mineralization, partly remobilized into fractures. The

source of the anomalous Ti and Cu is obvious, but the locus for the V is not.

4

127211: MAFIC (ORIGINALLY GABBROIC?) ROCK COMPOSED OF AMPHIBOLE AND

FORMER PLAGIOCLASE?, MINOR INTERSTITIAL ILMENITE, RARE CHALCOPYRITE,

STRONGLY ALTERED TO EPIDOTE-CHLORITE-MINOR SPHENE-TRACE HEMATITE

Described as from the same deposit as 127210 (with elevated V, Ti and Cu, but with less

sulfide mineralization); hand specimen shows mottled, grey-green/white mafic rock with minor

disseminated oxides and local splashy chalcopyrite mineralization. The rock is locally slightly

magnetic, shows trace very slow, minor reaction to cold dilute HCl (only where scratched), and no

stain for K-feldspar in the etched offcut (local weak yellow stain likely indicates micas). Modal

mineralogy in polished thin section is approximately:

Amphibole (relict, hornblende?) partly altered to actinolite? 40%

Epidote-group (zoisite, clinozoisite?) 30%

Chlorite (after amphibole, possible secondary biotite) 25%

Ilmenite (relict primary?) 3%

Chalcopyrite (restricted to blebs/remobilized veinlets) 1%

Sphene (after ilmenite?) <1%

Hematite (after ilmenite) <<1%

This sample is similar to 127210 in apparently consisting largely of relict amphibole (after

pyroxene?) and possible former plagioclase (?) sites, with interstitial, likely primary, oxides

(ilmenite), strongly altered to epidote-group minerals and chlorite, minor sphene and trace hematite;

local blebs of chalcopyrite are of uncertain timing and origin.

Amphibole occurs as ragged, corroded-looking “cores” or kernels up to ~6 mm across

composed of randomly oriented, subhedral crystals mostly <3 mm in size, commonly altered at

margins and along myriads of fractures or cleavages to chlorite or rarely fibrous amphibole. The

(primary or late-magmatic?) amphibole displays faint brownish to medium olive-greenish

pleochroism and extinction possibly up to ~20º, suggestive of hornblende; the secondary fibrous

amphibole shows almost colourless to pale sea green pleochroism, suggestive of actinolite.

Chlorite typically replaces amphibole either along fractures, where it is very fine-grained

(<0.1 mm) or forms interstitial masses up to 1 cm long, where it is coarser-grained (euhedra to ~0.35

mm) (both with faint pale green pleochroism). Optical properties vary from weakly length-slow,

anomalous blue birefringence (F:M 0.5?) to weakly length-fast, greyish birefringence (F:M 0.4?).

Epidote-group mineral occurs as either fine-grained aggregates of subhedra <0.25 mm with

normal to locally anomalous bluish or yellowish birefringence but no pleochroism (clinozoisite?), or

radiating sprays of euhedral acicular crystals up to 2 mm long with anomalous blue or grey

birefringence (zoisite?). The latter is associated with fine-grained chlorite and blebs of chalcopyrite.

Epidote-group minerals likely mainly replace former plagioclase (?) interstitial to mafic minerals,

suggestive of a mafic rock such as gabbro (?), although some may also replace the margins of

adjacent amphibole sites. Minor yellow stained areas associated with the relict plagioclase (?) sites in

etched offcut do not appear to represent Kspar; instead, yellow stain appears to relate to micas

(chlorite) which may have replaced former secondary biotite (?) as in sample 127210.

Ilmenite occurs as irregular-shaped aggregates up to ~2 mm across composed of subhedral

crystals mostly <1.5 mm in diameter, interstitial to presumed primary silicates. The ilmenite is

locally partly altered around rims to fine-grained sphene (subhedra <50 µm) or rarely hematite

(subhedra <25 µm). Sulfides are very rare within these oxide aggregates, but local poddy

chalcopyrite occurs in lensy aggregates up to ~5 mm long that partly surround or are associated with

ilmenite, and so may represent partly remobilized primary sulfides. Pyrrhotite is not seen.

In summary, this appears to represent mafic (originally gabbroic?) rock composed of

amphibole and former plagioclase (?), minor interstitial ilmenite and rare chalcopyrite, strongly

altered to epidote-chlorite-minor sphene-trace hematite. The source of anomalous V is uncertain.

5

127210: relict amphibolite (?) composed of shattered pale greenish amphibole (AM) crystals with local interstitial, likely

primary, aggregates of oxides/sulfides (opaque, mainly ilmenite, il), altered along fracture network to secondary

biotite/chlorite/carbonate, partly associated with pyrrhotite (po). Transmitted plane light, field of view ~3 mm wide.

127210R: heavily altered ultramafic in which relict ilmenite (il) is preserved but amphibole is altered to fine-grained mix

of chlorite-biotite-carbonate (cb), the latter associated with pyrrhotite (po) that also occurs, with chalcopyrite (cp) re-

mobilized into short discontinuous veinlets. Reflected light, uncrossed polars, field of view ~3 mm wide.

6

127211: relict amphibole (am) partly altered to or with interstitial chlorite (ch) and local (relict primary?) ilmenite (il,

opaque), plus fine-grained epidote-group mineral (ep, likely clinozoisite?) partly mixed with chlorite, probably after

former plagioclase or in part amphibole. Transmitted plane light, field of view ~3 mm wide.

127211R: splashy lensy aggregate of chalcopyrite (cp) in part surrounding or associated with ilmenite (il, partly altered at

rims to sphene, sp), hosted by fine-grained chlorite (ch) associated with radiating sprays of relatively coarse-grained

zoisite (zo). Reflected light, uncrossed polars, field of view ~3 mm wide.

7

Overview of thin sections and offcuts (blue semi-circles mark photomicrograph locations).

CoordinatesCapitalCorporation Suite # 805, # 140 Water Street, St. John’s, NL, Canada, A1C 6H6

Main Office Telephone : 709.758.1700 Main Office Fax : 709.758.1708

11.03.2014.1222 – 11.04.2014.1237

Clyde Burt

C/O General Delivery

Glenwood

Newfoundland & Labrador

A0G 1K0

709.679.2235

[email protected]

Good Afternoon Clyde,

Despite the July and August 2014 having its challenges, all samples which you deployed to site were cut to provide multiple crossections

for microscopic review prior to forwarding 14 representative samples totaling 2525 g to Eastern Analytical Ltd. on 09.19.2014.

Designated by Coordinates Capital Corporation as Project # 1 Gander, by 09.23.2014, Eastern Analytical Ltd. confirmed that your samples

had arrived and all 14 sets of rock material were being prepared for Au Pt Pd Fire Assay as well as 34 Element I.C.P. – Inductively Coupled Plasma

Analyses by 09.23.2014.

Although I will forward all results directly to you following this correspondence, we requested that Au Ag Pt Pd Precious Elements as well as

Al Co Cr Cu In Mg Mo Ni Pb Sb Sn Ti V W Zn Base Metal Elements have an additional assay completed if the initial result presented in excess of

upper detection limit.

As indicated by the correlative highlights presented in the table below, complete laboratory analysis of the # 1 Gander Project was

available on 09.26.2014 and transmitted to myself at Coordinates Capital Corporation on 09.29.2014.1620.

Unfortunately, Vanadium, the commodity which we discussed earlier as possibly adding potential value to your property, was not

reassayed as initially requested and in reviewing both Cu Ti V data sets, we determined that in all likelihood, our V values would reconfirm and

likely correlate directly with your Vanadium levels so a second request to assay for Vanadium was not completed.

The most prospective results from your Gander River Complex Rock Samples, remain the Fine Crack Chalcopyrite mineralized Quartz

Boulder C.Burt Sample # 127457 – C.C.C. Sample # 75628 recording Cu 12% and Ag 9100 ppb as well as the C.Burt Fine Crack Outcrop Gabbro

with Pyrite - Chalcopyrite Stringers – C.C.C. Sample # 75629 recording Cu 2.33 %.

As mentioned in the 1st Year Geological, Geophysical and Geochemical Assessment report prepared for Gander River Inc 01.1991,

reconnaisance soil surveys have already been completed over the Fine Crack Showing yielding Cu 7.0% in outcrop while VLF and Magnetic Surveys

have already been completed on your claims, “.the EM data was relatively useless…” due to the your property’s proximity to Power Lines and Towers.

Therefore we recommend establishing a trenching program to expose bedrock between the Cu 12.0 % Boulder and the Cu 2.33 % Fine

Crack Outcrop which would provide strategic Geological and Structural Exploration details as to the Strike and Dip of the Gabbro Hosted Quartz

Viens yielding High Grade Base Metal Copper and Precious Element Silver values further unlocking the potential of your property.

In recent deposit delineations by Kodiak Exploration Ltd at their Hercules Gold Project and Marathon Gold Corporation at their Valentine

Lake Gold Project both utilized this method to expose mineralized veins on surface to assess Gold Deposition trends prior to drilling.

# Coburn C.Burt C.C.C. Au Ag Pd Pt Cu Co Cr Ni V

Samples Sample Location Sample Description Assay ppb ppb ppb ppm ppm ppm ppm ppm ppm

1 # 127457 Cu 10.75 % 75628 167 9100 8 < 3 120000 84 158 15 10

2 Fine Crack Outcrop 75629 48 1.7 < 3 < 3 23300 19 195 13 20

3 Tower Pit Cpy Stringers V? 75630 19 1.8 5 < 3 5329 29 23 15 160

4 Pit Sulfide Rubble 75631 < 3 1.8 < 3 < 3 5415 163 85 77 >550

5 # 127456 Tower 75632 < 3 0.3 < 3 < 3 162 16 230 17 111

6 # 127359 Tower Hand Sample 75633 < 3 0.2 < 3 < 3 37 8 300 9 11

7 # 127360 Tower Outcrop 75634 11 <0.2 < 3 < 3 17 11 170 12 13

8 # 127362 Tower Rubble 75635 117 0.3 < 3 < 3 38 94 180 21 10

9 # 127201 Vanadium 95 N 20 E 75636 < 3 0.7 < 3 < 3 729 110 146 60 >550

10 # 127202 Vanadium 95 N 30 E 75637 < 3 1.6 < 3 < 3 6064 40 62 19 >550

11 # 127203 Vanadium 100 N 37 E 75638 < 3 0.6 < 3 < 3 1526 82 60 36 >550

12 # 127204 Vanadium 100 N 46 E 75639 206 0.8 < 3 < 3 2144 59 27 22 473

13 Vanadium 108 N 75640 < 3 0.5 < 3 < 3 1045 73 59 33 >550

14 # 127205 Vanadium 109 N 28 E 75641 < 3 0.4 < 3 < 3 245 45 45 21 >550

mailto:[email protected]

-2-

In general, our initial objectives were to review the potential of your group of claims based on the following investment criteria:

Geological Potential

Anomalous Precious Elements – Grade and Tonnage Potential

Anomalous Base Metal Elements – Grade and Tonnage Potential

Geological, Geochemical, Geophysical, Metallurgical, Petrological Assessments and Recommendations

Economical Potential

2014 & Future Commodity Demand by Element

Advanced Projects For Anomalous Elements With Reserves, Resources and Market Timeline

Mining Projects With Grade and Tonnage of Anomalous Elements Presenting With Preliminary Economic Assessments

However, as 2014 continued to unfold with challenging commodity markets, Coordinates Capital Corporation continued to internally

review the merit our current projects and consequently, assess all current or future investments in prospective ventures.

Therefore, with the investment market for exploration stage projects continuing to be stagnant as global mining markets struggle

through the 4th year of a downward cycle, Coordinates Capital Corporation declines to invest in your Gander Project at this time.

Should market conditions change towards a positive and investment sustainable climate, Coordinates Capital Corporation encourages

you to keep us advised of your project’s progress as you continue to complete additional exploratory work on your claims.

As you requested, I have stored all the sample portions which were not forwarded to Eastern Analytical Ltd for Geochemical Analysis

and the entire rock set can be retrieved anytime at my home satellite office.

Additionally, I have included several internet coordinates pertaining to Vanadium Commodity Demand and Supply trends as well as Fe

Ti V Deposit Models which could provide you with additional insight into the marketability of a property with elevated Fe Ti V.

Again, with many advanced Vanadium Projects poised to enter the V markets and Titanium Deposits recoding grades ranging from

TiO2 50%-70% compared to your TiO2 8.18%, focusing future exploration proximal to The Fine Crack Cu 2.33% - Cu 7.0 % - Cu 12.0% could

possibly further uncover both the Silver and hopefully Gold Potential of your property which would warrant a further review of your data as well as

scheduling of a possible site visit should you determine to further engage Coordinates Capital Coorporation.

We wish the very best during the 2014 C.I.M. Convention and remain receptive to developments on your property as they unfold.

Yours in Mineral Exploration,

BJB

CoordinatesCapitalCorporation

Barry J.B. Verbiski

B.Sc. B.Ed.

Vice President of Strategic Operations

Coordinates Capital Corporation

Satellite Office:

# 32 Rostellan Place

St. John's, NL. Canada A1B 2T9

Telephone : # 709.754.7101

Personal Cellular : # 709.697.1231

Corporate Cellular : 709.727.7127

E-Mail Coordinates :

[email protected]


-3-

In general, Deposit Profiles, provided by the Government of British Columbia provide 1-12 page reports identifying:

Mineral Deposit Profiles

http://www.empr.gov.bc.ca/MINING/GEOSCIENCE/MINERALDEPOSITPROFILES/Pages/default.aspx

Mineral Deposit Profiles By Commodity

http://www.empr.gov.bc.ca/Mining/Geoscience/MineralDepositProfiles/Pages/ListingbyCommodity.aspx

Deposit Type

Commodities

Global Deposit Examples

Geological Characteristics

Capsule Description

Tectonic Settings

Depositional Environment – Geological Setting

Age of Mineralization

Host Rocks & Associated Rock Types

Deposit Form

Mineralization Texture & Structure

Ore Mineralogy

Gangue Mineralogy

Alteration Mineralogy

Weathering

Ore Controls

Genetic Model

Associated Deposit Types

Comments

Exploration Guides

Geochemical Signature

Geophysical Signature

Unique Exploration Criteria

Economic Factors

Grade & Tonnage

Economic Limitations

Element or Commodity Importance

Copper – Silver Quartz Vein Deposits

http://www.empr.gov.bc.ca/Mining/Geoscience/MineralDepositProfiles/ListbyDepositGroup/Pages/IVeinBrecciaStockwork.aspx#I06

Vanadium

Cu Cr Ti Fe V Deposits

http://www.empr.gov.bc.ca/Mining/Geoscience/MineralDepositProfiles/ListbyDepositGroup/Pages/MUltramaficMafic.aspx#M04

2013 Vanadium Potential in Newfoundland and Labrador – Review and Assessment – Current Research Geological Survey Report 13-1 P 137-165

http://www.nr.gov.nl.ca/nr/mines/geoscience/publications/currentresearch/2013/Kerr-Walsh_2013.pdf

06.17.2014 Fe Ti V Mineral Sands Project – Churchill River Labrador Canada

http://www.muskratminerals.ca/files/Independent%20Technical%20Report%20for%20the%20Churchill%20River%20Mineral%20Sands%20Project

,%20Labrador,%20Canada.%20%20June,%202014.pdf

08.2014 Vanadium Commodity – Mineral Industry Survey – United States Geological Survey

http://minerals.usgs.gov/minerals/pubs/commodity/vanadium/mis-201408-vanad.pdf

Vanadium Investing News

http://vanadiuminvestingnews.com/vanadium/world-class-vanadium-deposits

Largo Resources – Brazil Vanadium Flagship Maracas Menchen Mine

http://www.largoresources.com/English/projects/maracas/default.aspx

2014 Mineral Commodity Summaries U.S Department of The Interior & U.S. Geological Survey Au Ag Cu Co Cr Pt Ti V

http://minerals.usgs.gov/minerals/pubs/mcs/2014/mcs2014.pdf

http://www.empr.gov.bc.ca/MINING/GEOSCIENCE/MINERALDEPOSITPROFILES/Pages/default.aspx

http://www.empr.gov.bc.ca/Mining/Geoscience/MineralDepositProfiles/Pages/ListingbyCommodity.aspx

http://www.empr.gov.bc.ca/Mining/Geoscience/MineralDepositProfiles/ListbyDepositGroup/Pages/IVeinBrecciaStockwork.aspx#I06

http://www.empr.gov.bc.ca/Mining/Geoscience/MineralDepositProfiles/ListbyDepositGroup/Pages/MUltramaficMafic.aspx#M04

http://www.nr.gov.nl.ca/nr/mines/geoscience/publications/currentresearch/2013/Kerr-Walsh_2013.pdf

http://www.muskratminerals.ca/files/Independent%20Technical%20Report%20for%20the%20Churchill%20River%20Mineral%20Sands%20Project,%20Labrador,%20Canada.%20%20June,%202014.pdf

http://www.muskratminerals.ca/files/Independent%20Technical%20Report%20for%20the%20Churchill%20River%20Mineral%20Sands%20Project,%20Labrador,%20Canada.%20%20June,%202014.pdf

http://minerals.usgs.gov/minerals/pubs/commodity/vanadium/mis-201408-vanad.pdf

http://vanadiuminvestingnews.com/vanadium/world-class-vanadium-deposits

http://www.largoresources.com/English/projects/maracas/default.aspx

http://minerals.usgs.gov/minerals/pubs/mcs/2014/mcs2014.pdf

-4-

CoordinatesCapitalCorporation Suite # 1002, # 140 Water Street, St. John’s, NL, Canada, A1C 6H6

Main Office Telephone : 709.758.1700 Main Office Fax : 709.758.1708

GOLD & PGE FIRE ASSAY + I.C.P. 30 ELEMENT ANALYSIS REQUEST FOR EASTERN ANALYTICAL

Results To : Invoice To :


Barry J.B. Verbiski

B.Sc. B.Ed. Vice President of Strategic Operations

Coordinates Capital Corporation

Satellite Office: # 32 Rostellan Place

St. John's, NL. Canada A1B 2T9 Telephone : # 709.754.7101

Personal Cellular : # 709.697.1231 Corporate Cellular : 709.727.7127

E-Mail Coordinates : [email protected]


Tammy Welsh

Executive Assistant

Chris Daly Chief Financial Officer

Main Office

Suite # 805, T.D. Place # 140 Water Street,

St. John’s, NL, Canada, A1C 6H6 Main Office Telephone : 709.758.1700

Main Office Fax : 709.758.1708 E-Mail Coordinates :

[email protected]

Sample Details

Submitted By & Results Forwarded To Project # Date :

Barry J.B. Verbiski 1 09.19.2014

[email protected] Gander 17:40

# Samples

Sample #

Sample Type

Weight Of Sample

Au Fire Assay

Pt Pd Fire Assay

I.C.P. 34

Priority Service

1 75628 Rock 207 g X X X X

2 75629 Rock 206 g X X X X

3 75630 Rock 111 g X X X X

4 75631 Rock 65 g X X X X

5 75632 Rock 188 g X X X X

6 75633 Rock 177 g X X X X

7 75634 Rock 147 g X X X X

8 75635 Rock 168 g X X X X

9 75636 Rock 282 g X X X X

10 75637 Rock 171 g X X X X

11 75638 Rock 92 g X X X X

12 75639 Rock 92 g X X X X

13 75640 Rock 375 g X X X X

14 75641 Rock 244 g X X X X

1 - 14 75628 - 75641 14 2525 g 14 14 14 14

* Please Assay The Following Precious Metal & Base Metal Elements Recording Higher Than The Upper Detection Limit * Precious Elements Pt Pd Au Ag

Base Elements Al Co Cr Cu In Mg Mo Ni Pb Sb Sn Ti V W Zn

00

Additional Mineral Exploration Supplies Accounting Details

Item

Total Amount

Total Cost

Supplies To : Invoice To :

C.C.C

# 140 Water St.

Suite # 1002

St. John’s,

NL. A1C 6H6




-5-

[email protected] From: Eastern Analytical Ltd. [[email protected]] Sent: Wednesday, September 24, 2014 10:22 AM To: [email protected] Subject: samples received

CONFIRMATION OF SAMPLES RECEIVED & REQUESTED ANALYSIS Client: Coordinates Capital Corporation Project: # 1 Gander Priority Service Requested: Rush Delivery Information: Canada Post Sample Type: Rock No. of Samples: 14 Analysis Requested: Au / ICP34 / Pt, Pd Analysis to be completed at: EAL DskFile Assigned: 635-1407958 / 635- 1407959 Date Received: September 23, 2014 Expected Date Completed: RUSHED 2

Report To: As per Requisiton Invoice To: As per Requisiton Pulp Disposal:

Reject Disposal: ___________________________________________ CONFIDENTIALITY NOTE: This e-mail, including any attachments, may contain information that is confidential and privileged. Any unauthorized disclosure, copying, or use of this e-mail is prohibited. If you are not the intended recipient, please notify us by e-mail or telephone at the number below, and permanently delete this e-mail and any copies immediately. Thank you. Eastern Analytical Ltd. 403 Little Bay Road Springdale, NL A0J 1T0 Telephone: 709-673-3909 Fax: 709-673-3408 www.easternanalytical.ca

http://www.easternanalytical.ca/

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