Ministry of Energy, Mines & Petroleum Resources Mining

AUTHOR(S): SIGNATURE(S):

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

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

PROPERTY NAME:

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

COMMODITIES SOUGHT:

MINERAL INVENTORY MINFILE NUMBER(S), IF KNOWN:

NTS/BCGS:MINING DIVISION:

LATITUDE: o ' " LONGITUDE: o ' "

OWNER(S):1) 2)

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

MAILING ADDRESS:

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

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

REFERENCES TO PREVIOUS ASSESSMENT WORK AND ASSESSMENT REPORT NUMBERS:

Ministry of Energy, Mines & Petroleum ResourcesMining & Minerals DivisionBC Geological Survey

Assessment ReportTitle Page and Summary

(at centre of work)

MAILING ADDRESS:

Next Page

A. Walcott, P. Walcott

5603602

Nov. 21st - Dec 7th, 2015

Getty

218508,218509,218510,208511,221561-221582,

221585 543766,758882,759482,759522,766082,1011732

Copper, Molybdenum

092INW040

092I055Kamloops

50 33 121 02

Getty Copper Inc.

Getty Copper Inc.

Geophysical, Induced Polarization 96,999.80

Highland Valley, Copper, Guichon Batholith, Triassic

28084,28072,24692,32370,24476

1000 Austin Avenue

Coquitlam, B.C.

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

Other

DRILLING(total metres; number of holes, size)

Core

Non-core

RELATED TECHNICAL

Sampling/assaying

Petrographic

Mineralographic

Metallurgic

PROSPECTING (scale, area)

PREPARATORY / PHYSICAL

Line/grid (kilometres)

(scale, area)

Legal surveys (scale, area)

Road, local access (kilometres)/trail

Topographic/Photogrammetric

Trench (metres)

Underground dev. (metres)

Other

TYPE OF WORK INTHIS REPORT

EXTENT OF WORK(IN METRIC UNITS)

ON WHICH CLAIMS PROJECT COSTSAPPORTIONED

(incl. support)

TOTAL COST:

(scale, area)

Line/grid (kilometres)

PROSPECTING (scale, area)

Metallurgic

Mineralographic

Petrographic

Sampling/assaying

Non-core

Core

Other

Rock

Silt

Soil

Airborne

Other

Seismic

Radiometric

Induced Polarization

Electromagnetic

Magnetic

Photo interpretation

Ground, mapping

96,999.80

96,999.80543766,759482,218510,221565-6616000 m

EVENT #5603602

AN ASSESSMENT REPORT

ON

INDUCED POLARIZATION SURVEYING

GETTY PROPERTY LOGAN LAKE AREA, BRITISH COLUMBIA

KAMLOOPS M.D. 50 33’N, 121 02’W

NTS 92I/ 10 & 11

Claims: 218508,218509,218510,208511,221561-221582,221585 543766,758882,759482,759522,766082,1011732

Work Dates: November 20th, - December 8th , 2015

FOR

GETTY COPPER INC. COQUITLAM, BRITISH COLUMBIA

BY

ALEXANDER WALCOTT, B.Sc PETER E. WALCOTT, P.Eng.

PETER E. WALCOTT & ASSOCIATES LIMITED

Coquitlam, British Columbia

AUGUST 2016

tfuller

Text Box

BC Geological Survey Assessment Report 36243

Peter E. Walcott & Associates Limited 2015 Induced Polarization Survey Geophysical Services Ge tty Property, B.C.

2

TABLE OF CONTENTS , Page INTRODUCTION…………………………………………………………….. 3 PROPERTY, LOCATION AND ACCESS…………………………………... 4 PREVIOUS WORK………………………………………………………….. 7 REGIONAL AND PROPERTY GEOLOGY………………………………... 8 PURPOSE…………………………………………………………………….. 10 SURVEY SPECIFICATIONS……………………………………………….. 11 DISCUSSION OF RESULTS………………………………………………… 13 SUMMARY, CONCLUSIONS & RECOMMENDATIONS………………… 17 APPENDIX I Cost of Project Personnel Employed on Project Certification Claim List References ACCOMPANYING MAPS Claim and Location Map Scale1:100,000 Detail Claim and Line Location Map Scale 1:10,000 Contours of Total Field Intensity with 2015 IP Lines Scale 1:10,000 2D Inverted Sections

3250N, 3500N, 4000N, 4500N, 5000N, 5500N Scale 1:10,000


3

INTRODUCTION. Between November 21st and December 7th, 2015, Peter E. Walcott & Associates Limited undertook induced polarization surveying over parts the Getty property, located in the Highland Valley of British Columbia, for Getty Copper Inc. The survey consisted of 6 east west orientated traverses, spaced between 250 m and 500 meters apart, for a total of some 16 line kilometers of deep penetrating induced polarization (IP) surveying. Additional traverses planned had to be abandoned due to access issues due to heavy snow fall. The survey was designed to augment the historic Titan 24 survey carried out over the Getty North and South deposits in 2010, in addition to attempting to define a target at depth proximal to the historic drill GL96-08, which intercepted elevated copper and molybdenum mineralization at depth.


4

PROPERTY LOCATION AND ACCESS The Getty property is located some 20 kilometres northwest of the community of Logan Lake, British Columbia. Access to the core of the property is obtained from Logan Lake, via highway 97C, and then by utilizing a network of logging roads.

Property Location Map


5

PROPERTY LOCATION AND ACCESS con’t

Line and Property Claim Location Map


6


Line and Claim Location Map


7

PREVIOUS WORK. The Getty Property and surrounding areas has been the subject of numerous exploration campaigns over the past 100 years. Well documented exploration programs conducted over the property have consisted of prospecting, geological mapping, geochemical samples, geophysics, and diamond drilling. The author would refer the reader to the BC Ministry of Energy and Mines – Assessment Report Indexing System (ARIS) http://www.empr.gov.bc.ca/mining/geoscience/aris for the historic public reports.


8

REGIONAL & PROPERTY GEOLOGY The Highland Valley is underlain by the Guchion Creek Batholith. This complex hosts a number of BC’s rich copper and molybdenum deposits, such as the Valley and Lornex. The Guichon Creek Batholith is composed of multiple intrusive phases, which can be distinguished by both composition and texture. These semi concentric phases are orientated in a north northwesterly orientation, stemming from a root some 8 kilometers down as interpreted form historic gravity data. The author would refer the reader to the numerous geological papers written about this prolific mining district for a detailed overview. The Getty property covers the northern extent of the late Triassic Guichon Creek Batholith. The intrusive rocks ranges in composition ranging from diorite to granodiorite, respective of the phase of emplacement. The property is also underlain by Tertiary sediments and Kamloops Group volcanics dominantly in the north eastern portion of the property.


9

REGIONAL & PROPERTY GEOLOGY con’t

General Geology


10

PURPOSE. The survey was designed to augment and expand on a previously conducted Titan 24 IP survey, proximal to the Getty West zone. The survey was also designed to test the thickness of volcanic cover to the north over Forge Mountain.


11

SURVEY SPECIFICATIONS. The Induced Polarization Survey. The induced polarization (IP) survey was conducted using a pulse type system, the principal components of which were manufactured by Instrumentation GDD of Quebec, Canada. The system consists basically of three units, a receiver (GDD), transmitter (GDD) and a motor generator (Honda). On this survey two transmitters used in series providing a maximum of 8.6 kw d.c. to the ground, obtains their power from two 7.5 kw 60 c.p.s. alternators driven by Honda 14 h.p. gasoline engines. The cycling rate of the transmitter is 2 seconds “current-on” and 2 seconds “current-off” with the pulses reversing continuously in polarity. The data recorded in the field consists of careful measurements of the current (I) in amperes flowing through the current electrodes C1 and C2, the primary voltages (V) appearing between any two potential electrodes, P1 through P5, during the “current-on” part of the cycle, and the apparent chargeability, (Ma) presented as a direct readout in millivolts per volt using a 200 millisecond delay and a 1000 millisecond sample window by the receiver, a digital receiver controlled by a micro-processor – the sample window is actually the total of twenty individual windows of 50 millisecond widths – at any time. The apparent resistivity (a) in ohm metres is proportional to the ratio of the primary voltage and the measured current, the proportionality factor depending on the geometry of the array used. The chargeability and resistivity are called apparent as they are values which that portion of the earth sampled would have if it were homogeneous. As the earth sampled is usually inhomogeneous the calculated apparent chargeability and resistivity are functions of the actual chargeability and resistivity of the rocks. The surveying was carried out using the “pole-dipole” / “dipole-pole” method of survey. With the pre-laid receiver array remaining stationary, the current C1 is moved along the survey lines at a spacing of “a” (the dipole) apart, while the second current electrode, C2, is kept constant at “infinity”. As the current (C1) is injected between the respective potential electrodes, and the receiving array is stationary, both pole-dipole and dipole-pole geometries can be measured with the maximum “n” separation, a function of the length of the receiver array which on this survey was “n” = 19.5, depending on the injection placement.


12

SURVEY SPECIFICATIONS cont. The distance, “na” between C1 and the nearest potential electrode generally controls the depth to be explored by the particular separation, “n”, traverse. On this survey a 100 metre dipole separation was utilized. On this survey a total of some 16 kilometres of survey traverses were completed. Horizontal control. The horizontal positions of the stations were recorded using a Garmin GPSmap 60CSx. Data Presentation. The data are presented as individual pseudo section plots of apparent resistivity and apparent chargeability at a scale of 1:10,000 generated using Geosoft Oasis Montaj. 2D inversions of both resistivity and chargeability modelled, using Res2DInv, are also presented at a scale of 1:10,000.


13

DISCUSSION OF RESULTS. The 2015 Induced Polarization survey carried on over parts of the Getty Copper property yielded a number of targets of potential interest, solely on the three southern lines, while the three northern lines exhibited no IP response. The lines were positioned to augment the existing deep IP coverage from the earlier Titan 24 survey. Line 3250 was re-read to allow for leveling between the two respective data datasets for future modelling.

Line Location Map with Airborne Magnetics


14

DISCUSSION OF RESULTS con’t. Anomaly cA is centered at 40400E on line 3250. This anomaly continues north through to Line 4000N at 40300E where it narrows and appears to truncate, potentially associated with a merging of two weak magnetic trends as seen above. This chargeability is dominantly associated with a higher resistivity unit overlying a flat lying resistivity low. The anomaly is situated within a magnetic low and appears to track the western flank of a weak magnetic feature.

Section 5603250N – Modelled Chargeability

This anomaly has been partially drill tested some 400 meters to the south. Hole 96GL-07 intercepted a broad zone of Tertiary volcanics in the bottom of the hole on the eastern flank of the anomaly within a resistivity low.


15

DISCUSSION OF RESULTS con’t.

Section 5603250N – Modelled Resistivity

Anomaly cB is centered at 40700E at a depth of some 250 m meters. This chargeability anomaly is associated with a sub-vertical resistivity high. The anomaly is also situated on a magnetic contact. This anomaly is of significant interest as drill hole 96GL-08 intercepted 42 metres grading 0.26% Cu and 0.02% Mo, immediately above the anomaly. Hole 200405A drilled some 100 meters to the north also intersected anomalous copper grades.


16

DISCUSSION OF RESULTS con’t. While anomaly cB does not appear to track through line 3500N, a weak feature does appear on Line 4000N on strike and is potentially the same anomaly. The lack of the chargeability response on Line 3500N could be due to an EW magnetic feature observed in the 2015 airborne magnetic survey.


17

SUMMARY, CONCLUSIONS & RECOMMENDATIONS. Between November 21st and December 7th, 2015, Peter E. Walcott & Associates Limited undertook induced polarization surveying over parts Getty property, located in the Logan Lake area of British Columbia, for Getty Copper Inc. The survey consisted of 6 east west orientated traverses, spaced between 250 m and 500 meters apart for a total of some 16 line kilometers of deep penetrating induced polarization surveying. The survey was hampered with access issues due to heavy snows, this limiting the program. The survey was designed to augment existing Titan 24 IP coverage conducted in 2010 over the Getty North and Getty South deposits, and to attempt to define targets in the Getty West zone. The survey identified and confirmed two chargeability targets proximal to the Getty West; Anomaly cA a broad anomaly, which has been partially drill tested south to the south with no significant results; Anomaly cB a deep chargeability anomaly where two historic drill holes yielded elevated copper grades proximal to the anomaly. This anomaly is of significant interest. A detailed review of all drill logs, and potential re-logging of holes within the Getty West zone should be undertaken by a geologist experienced in the Highland Valley exploration. Physical property measurement should also be undertaken, in order to understand better understand the geophysical response of the respective units. A full 3D inversion merging both the Titan and Walcott deep penetrating IP should be undertaken, and the results of the above exercises merged into a 3D compilation, prior to drill testing. Respectfully submitted, PETER E. WALCOTT & ASSOCIATES LTD. Alexander Walcott, B.Sc. Peter E. Walcott, P.Eng. Geophysicist Geophysicist Coquitlam, B.C. August 2016


18

APPENDIX I


19

COST OF PROJECT. Peter E. Walcott & Associates Limited undertook the survey on a daily basis providing a six man crew, IP equipment, GPS, altimeters and a 4x4 truck for a total of $66,750.00. Accommodation and fuel were billed at $ 11,068.64, while mobilization costs of $3,500.00 were incurred, so that the total cost of services provided was $ 88,818.64. A further 10% management and administration fee was accrued by Getty Copper, thus a total cost of $96,999.804 was incurred on this project.


20

PERSONNEL EMPLOYED ON PROJECT. Name Occupation Address Dates Peter E. Walcott Geophysicist Unit 111- 17,

Fawcett Rd. Coquitlam, B.C. V3K 6V2

Alexander Walcott

"

"

Marek Welz “

Nov. 20th – Dec 8th, 2015

Patrick Young “ “ Tom Kocan

Geophysical

Operator

“ Matt Magee “ “ Chris Roe

“

“


21

CERTIFICATION. I, Peter E. Walcott, of 605 Rutland Court, Coquitlam, British Columbia, hereby certify that:

1. I am a graduate of the University of Toronto in 1962 with a B.A.Sc. in Engineering Physics, Geophysics Option.

2. I have been practicing my profession for the last fifty four years.

3. I am a member of the Association of Professional Engineers of British

Columbia and Ontario.

4. I hold no interest, direct or indirect, in the property, nor do I expect to receive any.

Peter E. Walcott, P.Eng. Coquitlam, B.C. August 2016


22

CERTIFICATION. I, Alexander Walcott, of 38-181 Ravine Dr., Port Moody, British Columbia, hereby certify that:

1. I am a graduate of the University of Alberta with a B.Sc. Earth Sciences Major, with a Physics Minor.

2. I have been active in mineral exploration for the past 20 years. 3. I hold no interest, direct or indirect, in the property, nor do I expect to

receive any.

Alexander Walcott Coquitlam, B.C. August 2016


23

CLAIM LIST

Title

Number

Claim

Name

Owner Issue Date

Good To

Date

Status

Area

(ha)

218508 GETTY #80 133231 100% 1989/jun/10 2020/may/12 GOOD 25.00


218510

GETTY #82

FR. 133231 100% 1989/jun/10 2020/may/12 GOOD 25.00

218511

GETTY #83 FR.

133231 100% 1989/jun/10 2020/may/12 GOOD 25.00

221561 GETTY #1 133231 100% 1974/aug/06 2020/may/12 GOOD 25.00








221569 GETTY #9 133231 100% 1974/jul/16 2020/may/12 GOOD 25.00

















24

221585

GETTY A

FR 133231 100% 1974/aug/16 2020/may/12 GOOD 25.00

332395 BRAM 2 133231 100% 1994/nov/08 2017/may/15 GOOD 500.00


352941

GETTY

#113 133231 100% 1996/dec/04 2017/may/15 GOOD 25.00

412799

GETTY 2405

133231 100% 2004/jul/17 2017/may/15 GOOD 25.00

412800

GETTY

2406 133231 100% 2004/jul/17 2017/may/15 GOOD 25.00

519232

GETTY

SOUTH1 133231 100% 2005/aug/22 2017/may/15 GOOD 123.22

519235

GETTY

SOUTH 2 133231 100% 2005/aug/22 2018/may/31 GOOD 82.13

519237

GETTY


526953 GSOUTH 1 133231 100% 2006/feb/02 2018/may/31 GOOD 143.75

543766

GETTY

WEST 133231 100% 2006/oct/22 2017/may/15 GOOD 307.92

614103 133231 100% 2009/aug/01 2017/may/15 GOOD 164.14

614104 133231 100% 2009/aug/01 2017/may/15 GOOD 102.55

614123 133231 100% 2009/aug/01 2017/may/15 GOOD 204.89

616307 GWEN 133231 100% 2009/aug/08 2017/may/15 GOOD 20.49

621143

THE

BRIED'SG&G 133231 100% 2009/aug/18 2017/may/15 GOOD 348.44

640843 133231 100% 2009/sep/25 2017/may/15 GOOD 41.06

757822 133231 100% 2010/apr/26 2017/may/15 GOOD 1538.95

757882 133231 100% 2010/apr/26 2017/may/15 GOOD 1660.28

757902 133231 100% 2010/apr/26 2017/may/15 GOOD 1229.67

757962 133231 100% 2010/apr/26 2017/may/15 GOOD 1579.46

758022 133231 100% 2010/apr/26 2017/may/15 GOOD 1107.68

758222 133231 100% 2010/apr/26 2017/may/15 GOOD 1517.28

758422 133231 100% 2010/apr/26 2017/may/15 GOOD 1313.52

758483 133231 100% 2010/apr/26 2017/may/15 GOOD 20.51

758842 133231 100% 2010/apr/27 2017/may/15 GOOD 512.31

758882 133231 100% 2010/apr/27 2017/may/15 GOOD 1663.04

758902 133231 100% 2010/apr/27 2017/may/15 GOOD 553.68

758963 133231 100% 2010/apr/27 2017/may/15 GOOD 840.83

759302 133231 100% 2010/apr/27 2017/may/15 GOOD 1003.86

759342 133231 100% 2010/apr/27 2017/may/15 GOOD 574.41

759362 133231 100% 2010/apr/27 2017/may/15 GOOD 839.82


25

759402 133231 100% 2010/apr/27 2017/may/15 GOOD 942.97

759422 133231 100% 2010/apr/27 2017/may/15 GOOD 553.56

759482 133231 100% 2010/apr/27 2017/may/15 GOOD 615.55

759522 133231 100% 2010/apr/27 2017/may/15 GOOD 902.90

759562 133231 100% 2010/apr/27 2017/may/15 GOOD 1108.66

759702 133231 100% 2010/apr/28 2017/may/15 GOOD 164.38

759802 133231 100% 2010/apr/28 2017/may/15 GOOD 20.54

766082 133231 100% 2010/may/03 2020/may/12 GOOD 41.04

768142 BLU 133231 100% 2010/may/05 2017/may/15 GOOD 40.95

768162 133231 100% 2010/may/05 2017/may/15 GOOD 512.45

844516 133231 100% 2011/jan/26 2017/may/15 GOOD 20.51

917949 133231 100% 2011/oct/18 2017/may/15 GOOD 246.09

920784 133231 100% 2011/oct/21 2017/may/15 GOOD 246.23

937922 133231 100% 2011/dec/19 2017/may/15 GOOD 266.70

1011732 133231 100% 2012/aug/02 2017/may/15 GOOD 266.71

1011733 133231 100% 2012/aug/02 2017/may/15 GOOD 205.10

1011734 133231 100% 2012/aug/02 2017/may/15 GOOD 41.03

1027750 GETTY BT1 133231 100% 2014/apr/22 2017/may/15 GOOD 840.43



1033130 133231 100% 2015/jan/05 2017/may/15 GOOD 82.00


26

REFERENCES. Ager, C.A, McMillan, W.J., Ulrych, T.J, Bulletin 62: Gravity, Magnetics and Geology of the Guichon Creek Batholith, 1972 British Columbia Department of Mines and Petroleum Resources Bond, L., Graden, R. – Diamond Drilling Report on the Highland Valley Copper Getty Copper Option, 2005, BC Assessment Report 28084 Evans, G. Hewson, C. – 2005 Assessment Report, Geological Mapping, Line Cutting and Induced Polarization Geophysics on the Getty Copper Option, 2005, BC Assessment Report 28072 Geoscience BC, - Quest South Airborne Gravity Dataset, 2010 Northcote, K.E., Bulletin 56: Geology and Geochronology of the Guichon Creek Batholith, 1969 British Columbia Department of Mines and Petroleum Resources Perry, Bruce J, - Report on Diamond Drilling At The Getty North (Krain), Getty South( Trojan (South Seas), and Getty West (Transvaal) Areas, Highland Valley, 1996, BC Assessment Report 24692 Tournerie, B., Verweerd, A. , Metcalfe, J. – Titan 24 DC/IP/MT Survey Geophysical Report, Getty Project, 2011, BC Assessment Report 32370 Walcott, Peter E., - A Geophysical Report on Induced Polarization Surveying, Getty Property, 1996, BC. Assessment Report 24476

EVENT #5603602

AN ASSESSMENT REPORT

ON

INDUCED POLARIZATION SURVEYING

GETTY PROPERTY LOGAN LAKE AREA, BRITISH COLUMBIA

KAMLOOPS M.D. 50 33’N, 121 02’W

NTS 92I/ 10 & 11

Claims: 218508,218509,218510,208511,221561-221582,221585 543766,758882,759482,759522,766082,1011732

Work Dates: November 20th, - December 8th , 2015

FOR

GETTY COPPER INC. COQUITLAM, BRITISH COLUMBIA

BY

ALEXANDER WALCOTT, B.Sc PETER E. WALCOTT, P.Eng.


Coquitlam, British Columbia

AUGUST 2016


2

TABLE OF CONTENTS , Page INTRODUCTION…………………………………………………………….. 3 PROPERTY, LOCATION AND ACCESS…………………………………... 4 PREVIOUS WORK………………………………………………………….. 7 REGIONAL AND PROPERTY GEOLOGY………………………………... 8 PURPOSE…………………………………………………………………….. 10 SURVEY SPECIFICATIONS……………………………………………….. 11 DISCUSSION OF RESULTS………………………………………………… 13 SUMMARY, CONCLUSIONS & RECOMMENDATIONS………………… 17 APPENDIX I Cost of Project Personnel Employed on Project Certification Claim List References ACCOMPANYING MAPS Claim and Location Map Scale1:100,000 Detail Claim and Line Location Map Scale 1:10,000 Contours of Total Field Intensity with 2015 IP Lines Scale 1:10,000 2D Inverted Sections

3250N, 3500N, 4000N, 4500N, 5000N, 5500N Scale 1:10,000


3

INTRODUCTION. Between November 21st and December 7th, 2015, Peter E. Walcott & Associates Limited undertook induced polarization surveying over parts the Getty property, located in the Highland Valley of British Columbia, for Getty Copper Inc. The survey consisted of 6 east west orientated traverses, spaced between 250 m and 500 meters apart, for a total of some 16 line kilometers of deep penetrating induced polarization (IP) surveying. Additional traverses planned had to be abandoned due to access issues due to heavy snow fall. The survey was designed to augment the historic Titan 24 survey carried out over the Getty North and South deposits in 2010, in addition to attempting to define a target at depth proximal to the historic drill GL96-08, which intercepted elevated copper and molybdenum mineralization at depth.


4

PROPERTY LOCATION AND ACCESS The Getty property is located some 20 kilometres northwest of the community of Logan Lake, British Columbia. Access to the core of the property is obtained from Logan Lake, via highway 97C, and then by utilizing a network of logging roads.

Property Location Map


5


Line and Property Claim Location Map


6


Line and Claim Location Map


7

PREVIOUS WORK. The Getty Property and surrounding areas has been the subject of numerous exploration campaigns over the past 100 years. Well documented exploration programs conducted over the property have consisted of prospecting, geological mapping, geochemical samples, geophysics, and diamond drilling. The author would refer the reader to the BC Ministry of Energy and Mines – Assessment Report Indexing System (ARIS) http://www.empr.gov.bc.ca/mining/geoscience/aris for the historic public reports.


8

REGIONAL & PROPERTY GEOLOGY The Highland Valley is underlain by the Guchion Creek Batholith. This complex hosts a number of BC’s rich copper and molybdenum deposits, such as the Valley and Lornex. The Guichon Creek Batholith is composed of multiple intrusive phases, which can be distinguished by both composition and texture. These semi concentric phases are orientated in a north northwesterly orientation, stemming from a root some 8 kilometers down as interpreted form historic gravity data. The author would refer the reader to the numerous geological papers written about this prolific mining district for a detailed overview. The Getty property covers the northern extent of the late Triassic Guichon Creek Batholith. The intrusive rocks ranges in composition ranging from diorite to granodiorite, respective of the phase of emplacement. The property is also underlain by Tertiary sediments and Kamloops Group volcanics dominantly in the north eastern portion of the property.


9

REGIONAL & PROPERTY GEOLOGY con’t

General Geology


10

PURPOSE. The survey was designed to augment and expand on a previously conducted Titan 24 IP survey, proximal to the Getty West zone. The survey was also designed to test the thickness of volcanic cover to the north over Forge Mountain.


11

SURVEY SPECIFICATIONS. The Induced Polarization Survey. The induced polarization (IP) survey was conducted using a pulse type system, the principal components of which were manufactured by Instrumentation GDD of Quebec, Canada. The system consists basically of three units, a receiver (GDD), transmitter (GDD) and a motor generator (Honda). On this survey two transmitters used in series providing a maximum of 8.6 kw d.c. to the ground, obtains their power from two 7.5 kw 60 c.p.s. alternators driven by Honda 14 h.p. gasoline engines. The cycling rate of the transmitter is 2 seconds “current-on” and 2 seconds “current-off” with the pulses reversing continuously in polarity. The data recorded in the field consists of careful measurements of the current (I) in amperes flowing through the current electrodes C1 and C2, the primary voltages (V) appearing between any two potential electrodes, P1 through P5, during the “current-on” part of the cycle, and the apparent chargeability, (Ma) presented as a direct readout in millivolts per volt using a 200 millisecond delay and a 1000 millisecond sample window by the receiver, a digital receiver controlled by a micro-processor – the sample window is actually the total of twenty individual windows of 50 millisecond widths – at any time. The apparent resistivity (a) in ohm metres is proportional to the ratio of the primary voltage and the measured current, the proportionality factor depending on the geometry of the array used. The chargeability and resistivity are called apparent as they are values which that portion of the earth sampled would have if it were homogeneous. As the earth sampled is usually inhomogeneous the calculated apparent chargeability and resistivity are functions of the actual chargeability and resistivity of the rocks. The surveying was carried out using the “pole-dipole” / “dipole-pole” method of survey. With the pre-laid receiver array remaining stationary, the current C1 is moved along the survey lines at a spacing of “a” (the dipole) apart, while the second current electrode, C2, is kept constant at “infinity”. As the current (C1) is injected between the respective potential electrodes, and the receiving array is stationary, both pole-dipole and dipole-pole geometries can be measured with the maximum “n” separation, a function of the length of the receiver array which on this survey was “n” = 19.5, depending on the injection placement.


12

SURVEY SPECIFICATIONS cont. The distance, “na” between C1 and the nearest potential electrode generally controls the depth to be explored by the particular separation, “n”, traverse. On this survey a 100 metre dipole separation was utilized. On this survey a total of some 16 kilometres of survey traverses were completed. Horizontal control. The horizontal positions of the stations were recorded using a Garmin GPSmap 60CSx. Data Presentation. The data are presented as individual pseudo section plots of apparent resistivity and apparent chargeability at a scale of 1:10,000 generated using Geosoft Oasis Montaj. 2D inversions of both resistivity and chargeability modelled, using Res2DInv, are also presented at a scale of 1:10,000.


13

DISCUSSION OF RESULTS. The 2015 Induced Polarization survey carried on over parts of the Getty Copper property yielded a number of targets of potential interest, solely on the three southern lines, while the three northern lines exhibited no IP response. The lines were positioned to augment the existing deep IP coverage from the earlier Titan 24 survey. Line 3250 was re-read to allow for leveling between the two respective data datasets for future modelling.

Line Location Map with Airborne Magnetics


14

DISCUSSION OF RESULTS con’t. Anomaly cA is centered at 40400E on line 3250. This anomaly continues north through to Line 4000N at 40300E where it narrows and appears to truncate, potentially associated with a merging of two weak magnetic trends as seen above. This chargeability is dominantly associated with a higher resistivity unit overlying a flat lying resistivity low. The anomaly is situated within a magnetic low and appears to track the western flank of a weak magnetic feature.

Section 5603250N – Modelled Chargeability

This anomaly has been partially drill tested some 400 meters to the south. Hole 96GL-07 intercepted a broad zone of Tertiary volcanics in the bottom of the hole on the eastern flank of the anomaly within a resistivity low.


15

DISCUSSION OF RESULTS con’t.

Section 5603250N – Modelled Resistivity

Anomaly cB is centered at 40700E at a depth of some 250 m meters. This chargeability anomaly is associated with a sub-vertical resistivity high. The anomaly is also situated on a magnetic contact. This anomaly is of significant interest as drill hole 96GL-08 intercepted 42 metres grading 0.26% Cu and 0.02% Mo, immediately above the anomaly. Hole 200405A drilled some 100 meters to the north also intersected anomalous copper grades.


16

DISCUSSION OF RESULTS con’t. While anomaly cB does not appear to track through line 3500N, a weak feature does appear on Line 4000N on strike and is potentially the same anomaly. The lack of the chargeability response on Line 3500N could be due to an EW magnetic feature observed in the 2015 airborne magnetic survey.


17

SUMMARY, CONCLUSIONS & RECOMMENDATIONS. Between November 21st and December 7th, 2015, Peter E. Walcott & Associates Limited undertook induced polarization surveying over parts Getty property, located in the Logan Lake area of British Columbia, for Getty Copper Inc. The survey consisted of 6 east west orientated traverses, spaced between 250 m and 500 meters apart for a total of some 16 line kilometers of deep penetrating induced polarization surveying. The survey was hampered with access issues due to heavy snows, this limiting the program. The survey was designed to augment existing Titan 24 IP coverage conducted in 2010 over the Getty North and Getty South deposits, and to attempt to define targets in the Getty West zone. The survey identified and confirmed two chargeability targets proximal to the Getty West; Anomaly cA a broad anomaly, which has been partially drill tested south to the south with no significant results; Anomaly cB a deep chargeability anomaly where two historic drill holes yielded elevated copper grades proximal to the anomaly. This anomaly is of significant interest. A detailed review of all drill logs, and potential re-logging of holes within the Getty West zone should be undertaken by a geologist experienced in the Highland Valley exploration. Physical property measurement should also be undertaken, in order to understand better understand the geophysical response of the respective units. A full 3D inversion merging both the Titan and Walcott deep penetrating IP should be undertaken, and the results of the above exercises merged into a 3D compilation, prior to drill testing. Respectfully submitted, PETER E. WALCOTT & ASSOCIATES LTD. Alexander Walcott, B.Sc. Peter E. Walcott, P.Eng. Geophysicist Geophysicist Coquitlam, B.C. August 2016


18

APPENDIX I


19

COST OF PROJECT. Peter E. Walcott & Associates Limited undertook the survey on a daily basis providing a six man crew, IP equipment, GPS, altimeters and a 4x4 truck for a total of $66,750.00. Accommodation and fuel were billed at $ 11,068.64, while mobilization costs of $3,500.00 were incurred, so that the total cost of services provided was $ 88,818.64. A further 10% management and administration fee was accrued by Getty Copper, thus a total cost of $96,999.804 was incurred on this project.


20

PERSONNEL EMPLOYED ON PROJECT. Name Occupation Address Dates Peter E. Walcott Geophysicist Unit 111- 17,

Fawcett Rd. Coquitlam, B.C. V3K 6V2

Alexander Walcott

"

"

Marek Welz “

Nov. 20th – Dec 8th, 2015

Patrick Young “ “ Tom Kocan

Geophysical

Operator

“ Matt Magee “ “ Chris Roe

“

“


21

CERTIFICATION. I, Peter E. Walcott, of 605 Rutland Court, Coquitlam, British Columbia, hereby certify that:

1. I am a graduate of the University of Toronto in 1962 with a B.A.Sc. in Engineering Physics, Geophysics Option.

2. I have been practicing my profession for the last fifty four years.

3. I am a member of the Association of Professional Engineers of British

Columbia and Ontario.

4. I hold no interest, direct or indirect, in the property, nor do I expect to receive any.

Peter E. Walcott, P.Eng. Coquitlam, B.C. August 2016


22

CERTIFICATION. I, Alexander Walcott, of 38-181 Ravine Dr., Port Moody, British Columbia, hereby certify that:

1. I am a graduate of the University of Alberta with a B.Sc. Earth Sciences Major, with a Physics Minor.

2. I have been active in mineral exploration for the past 20 years. 3. I hold no interest, direct or indirect, in the property, nor do I expect to

receive any.

Alexander Walcott Coquitlam, B.C. August 2016


23

CLAIM LIST

Title

Number

Claim

Name

Owner Issue Date

Good To

Date

Status

Area

(ha)



218510

GETTY #82

FR. 133231 100% 1989/jun/10 2020/may/12 GOOD 25.00

218511

GETTY #83 FR.

133231 100% 1989/jun/10 2020/may/12 GOOD 25.00









221569 GETTY #9 133231 100% 1974/jul/16 2020/may/12 GOOD 25.00

















24

221585

GETTY A

FR 133231 100% 1974/aug/16 2020/may/12 GOOD 25.00

332395 BRAM 2 133231 100% 1994/nov/08 2017/may/15 GOOD 500.00


352941

GETTY

#113 133231 100% 1996/dec/04 2017/may/15 GOOD 25.00

412799

GETTY 2405

133231 100% 2004/jul/17 2017/may/15 GOOD 25.00

412800

GETTY

2406 133231 100% 2004/jul/17 2017/may/15 GOOD 25.00

519232

GETTY

SOUTH1 133231 100% 2005/aug/22 2017/may/15 GOOD 123.22

519235

GETTY


519237

GETTY


526953 GSOUTH 1 133231 100% 2006/feb/02 2018/may/31 GOOD 143.75

543766

GETTY

WEST 133231 100% 2006/oct/22 2017/may/15 GOOD 307.92

614103 133231 100% 2009/aug/01 2017/may/15 GOOD 164.14

614104 133231 100% 2009/aug/01 2017/may/15 GOOD 102.55

614123 133231 100% 2009/aug/01 2017/may/15 GOOD 204.89

616307 GWEN 133231 100% 2009/aug/08 2017/may/15 GOOD 20.49

621143

THE

BRIED'SG&G 133231 100% 2009/aug/18 2017/may/15 GOOD 348.44

640843 133231 100% 2009/sep/25 2017/may/15 GOOD 41.06

757822 133231 100% 2010/apr/26 2017/may/15 GOOD 1538.95

757882 133231 100% 2010/apr/26 2017/may/15 GOOD 1660.28

757902 133231 100% 2010/apr/26 2017/may/15 GOOD 1229.67

757962 133231 100% 2010/apr/26 2017/may/15 GOOD 1579.46

758022 133231 100% 2010/apr/26 2017/may/15 GOOD 1107.68

758222 133231 100% 2010/apr/26 2017/may/15 GOOD 1517.28

758422 133231 100% 2010/apr/26 2017/may/15 GOOD 1313.52

758483 133231 100% 2010/apr/26 2017/may/15 GOOD 20.51

758842 133231 100% 2010/apr/27 2017/may/15 GOOD 512.31

758882 133231 100% 2010/apr/27 2017/may/15 GOOD 1663.04

758902 133231 100% 2010/apr/27 2017/may/15 GOOD 553.68

758963 133231 100% 2010/apr/27 2017/may/15 GOOD 840.83

759302 133231 100% 2010/apr/27 2017/may/15 GOOD 1003.86

759342 133231 100% 2010/apr/27 2017/may/15 GOOD 574.41

759362 133231 100% 2010/apr/27 2017/may/15 GOOD 839.82


25

759402 133231 100% 2010/apr/27 2017/may/15 GOOD 942.97

759422 133231 100% 2010/apr/27 2017/may/15 GOOD 553.56

759482 133231 100% 2010/apr/27 2017/may/15 GOOD 615.55

759522 133231 100% 2010/apr/27 2017/may/15 GOOD 902.90

759562 133231 100% 2010/apr/27 2017/may/15 GOOD 1108.66

759702 133231 100% 2010/apr/28 2017/may/15 GOOD 164.38

759802 133231 100% 2010/apr/28 2017/may/15 GOOD 20.54

766082 133231 100% 2010/may/03 2020/may/12 GOOD 41.04

768142 BLU 133231 100% 2010/may/05 2017/may/15 GOOD 40.95

768162 133231 100% 2010/may/05 2017/may/15 GOOD 512.45

844516 133231 100% 2011/jan/26 2017/may/15 GOOD 20.51

917949 133231 100% 2011/oct/18 2017/may/15 GOOD 246.09

920784 133231 100% 2011/oct/21 2017/may/15 GOOD 246.23

937922 133231 100% 2011/dec/19 2017/may/15 GOOD 266.70

1011732 133231 100% 2012/aug/02 2017/may/15 GOOD 266.71

1011733 133231 100% 2012/aug/02 2017/may/15 GOOD 205.10

1011734 133231 100% 2012/aug/02 2017/may/15 GOOD 41.03




1033130 133231 100% 2015/jan/05 2017/may/15 GOOD 82.00


26

REFERENCES. Ager, C.A, McMillan, W.J., Ulrych, T.J, Bulletin 62: Gravity, Magnetics and Geology of the Guichon Creek Batholith, 1972 British Columbia Department of Mines and Petroleum Resources Bond, L., Graden, R. – Diamond Drilling Report on the Highland Valley Copper Getty Copper Option, 2005, BC Assessment Report 28084 Evans, G. Hewson, C. – 2005 Assessment Report, Geological Mapping, Line Cutting and Induced Polarization Geophysics on the Getty Copper Option, 2005, BC Assessment Report 28072 Geoscience BC, - Quest South Airborne Gravity Dataset, 2010 Northcote, K.E., Bulletin 56: Geology and Geochronology of the Guichon Creek Batholith, 1969 British Columbia Department of Mines and Petroleum Resources Perry, Bruce J, - Report on Diamond Drilling At The Getty North (Krain), Getty South( Trojan (South Seas), and Getty West (Transvaal) Areas, Highland Valley, 1996, BC Assessment Report 24692 Tournerie, B., Verweerd, A. , Metcalfe, J. – Titan 24 DC/IP/MT Survey Geophysical Report, Getty Project, 2011, BC Assessment Report 32370 Walcott, Peter E., - A Geophysical Report on Induced Polarization Surveying, Getty Property, 1996, BC. Assessment Report 24476

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GETTY COPPER INC.INDUCED POLARIZATION SURVEY

LINE LOCATION

GETTY PROPERTYLOGAN LAKE AREA, B.C.

DECEMBER 2015


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NAD83(CSRS) / UTM zone 10N

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GETTY COPPER INC.

INDUCED POLARIZATION SURVEYCLAIM AND LINE LOCATION MAP


DECEMBER 2015


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Scale 1:10000

GETTY COPPER INC.

INDUCED POLARIZATION SURVEYLINE LOCATION on TMI (nT)


DECEMBER 2015


54881.2

55026.5

55105.4

55161.3

55209.0

55250.9

55287.1

55319.8

55348.3

55374.9

55399.9

55424.5

55447.2

55470.5

55493.8

55516.2

55538.1

55559.7

55582.2

55604.0

55625.0

55646.7

55669.0

55691.5

55715.2

55740.6

55766.5

55794.9

55826.5

55860.0

55896.4

55938.1

55987.0

56044.4

56116.6

56206.4

56332.2

56576.8

nT

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GETTY COPPER

INDUCED POLARIZATION SURVEYGETTY PROJECT

Date: DECEMBER 2015RES2DINV

Inversion By:PETER E. WALCOTT & ASSOCIATES LIMITED

200 0 200 400 600

(meters)

Scale 1:10000

Line 3250

Pole-Dipole Array

VI

a na a

plot point

1.79

2.42

2.80

3.10

3.34

3.54

3.73

3.90

4.05

4.20

4.34

4.47

4.60

4.72

4.84

4.96

5.07

5.19

5.30

5.42

5.53

5.65

5.76

5.88

6.00

6.13

6.25

6.38

6.52

6.67

6.82

6.99

7.18

7.39

7.63

7.92

8.30

8.93

Modelled Chargeability

mV/V

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44.86

52.39

59.43

66.44

72.71

80.10

87.91

96.86

106.78

117.71

129.08

140.31

155.04

173.03

195.01

220.54

242.75

268.42

293.83

318.44

346.56

392.82

502.16

Modelled Resistivity

ohm-m

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1763.17

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Pole-Dipole Array

VI

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2.68

2.82

2.96

3.10

3.24

3.38

3.52

3.66

3.80

3.94

4.08

4.22

4.36

4.50

4.64

4.78

4.92

5.06

5.20

5.34

5.48

5.62

5.76

5.90

6.04

6.18

6.32

6.46

6.60

6.74

6.88

7.02

7.16

7.30

7.44

7.58

7.72

7.86


mV/V

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44.86

52.39

59.43

66.44

72.71

80.10

87.91

96.86

106.78

117.71

129.08

140.31

155.04

173.03

195.01

220.54

242.75

268.42

293.83

318.44

346.56

392.82

502.16


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1795

800

900

1000

1100

1200

1300

1400

1500

1600

1700

741.22

1795


Ele

vation (

metr

es)

1 0 0

10

0

100

00

1

39

00

0

39

10

0

39

20

0

39

30

0

39

40

0

39

50

0

39

60

0

39

70

0

39

80

0

39

90

0

40

00

0

40

10

0

40

20

0

40

30

0

40

40

0

40

50

0

40

60

0

40

70

0

40

80

0

40

90

0

41

00

0

411

00

41

20

0

41

30

0

41

40

0

41

50

0

41

60

0

GETTY COPPER




100 0 100 200 300 400 500 600 700

(meters)

Scale 1:10000

Line 4000

Pole-Dipole Array

VI

a na a

plot point

2.68

2.82

2.96

3.10

3.24

3.38

3.52

3.66

3.80

3.94

4.08

4.22

4.36

4.50

4.64

4.78

4.92

5.06

5.20

5.34

5.48

5.62

5.76

5.90

6.04

6.18

6.32

6.46

6.60

6.74

6.88

7.02

7.16

7.30

7.44

7.58

7.72

7.86


mV/V

33.98

44.86

52.39

59.43

66.44

72.71

80.10

87.91

96.86

106.78

117.71

129.08

140.31

155.04

173.03

195.01

220.54

242.75

268.42

293.83

318.44

346.56

392.82

502.16


ohm-m

900

1000

1100

1200

1300

1400

1500

1600

1700

1800

1900

804.28

1941.19

900

1000

1100

1200

1300

1400

1500

1600

1700

1800

1900

804.28

1941.19


Ele

vation (

metr

es)

39

10

0

39

20

0

39

30

0

39

40

0

39

50

0

39

60

0

39

70

0

39

80

0

39

90

0

40

00

0

40

10

0

40

20

0

40

30

0

40

40

0

40

50

0

40

60

0

40

70

0

40

80

0

40

90

0

41

00

0

411

00

41

20

0

41

30

0

41

40

0

41

50

0

41

60

0

cA

cB

900

1000

1100

1200

1300

1400

1500

1600

1700

1800

1900

804.28

1941.19

900

1000

1100

1200

1300

1400

1500

1600

1700

1800

1900

804.28

1941.19


Ele

vation (

metr

es)

10

0

0 0 1

100

39

10

0

39

20

0

39

30

0

39

40

0

39

50

0

39

60

0

39

70

0

39

80

0

39

90

0

40

00

0

40

10

0

40

20

0

40

30

0

40

40

0

40

50

0

40

60

0

40

70

0

40

80

0

40

90

0

41

00

0

411

00

41

20

0

41

30

0

41

40

0

41

50

0

41

60

0

GETTY COPPER




200 0 200 400 600

(meters)

Scale 1:10000

Line 4500

Pole-Dipole Array

VI

a na a

plot point

2.68

2.82

2.96

3.10

3.24

3.38

3.52

3.66

3.80

3.94

4.08

4.22

4.36

4.50

4.64

4.78

4.92

5.06

5.20

5.34

5.48

5.62

5.76

5.90

6.04

6.18

6.32

6.46

6.60

6.74

6.88

7.02

7.16

7.30

7.44

7.58

7.72

7.86


mV/V

33.98

44.86

52.39

59.43

66.44

72.71

80.10

87.91

96.86

106.78

117.71

129.08

140.31

155.04

173.03

195.01

220.54

242.75

268.42

293.83

318.44

346.56

392.82

502.16


ohm-m

900

1000

1100

1200

1300

1400

1500

1600

1700

1800

1900

818.28

1941.55

900

1000

1100

1200

1300

1400

1500

1600

1700

1800

1900

818.28

1941.55


Ele

vation (

metr

es)

39

00

0

39

10

0

39

20

0

39

30

0

39

40

0

39

50

0

39

60

0

39

70

0

39

80

0

39

90

0

40

00

0

40

10

0

40

20

0

40

30

0

40

40

0

40

50

0

40

60

0

40

70

0

40

80

0

40

90

0

41

00

0

411

00

41

20

0

41

30

0

41

40

0

41

50

0

41

60

0

900

1000

1100

1200

1300

1400

1500

1600

1700

1800

1900

818.28

1941.55

900

1000

1100

1200

1300

1400

1500

1600

1700

1800

1900

818.28

1941.55


Ele

vation (

metr

es)

00

1

100

10

0

10

0

00

1

39

00

0

39

10

0

39

20

0

39

30

0

39

40

0

39

50

0

39

60

0

39

70

0

39

80

0

39

90

0

40

00

0

40

10

0

40

20

0

40

30

0

40

40

0

40

50

0

40

60

0

40

70

0

40

80

0

40

90

0

41

00

0

411

00

41

20

0

41

30

0

41

40

0

41

50

0

41

60

0

GETTY COPPER




200 0 200 400 600

(meters)

Scale 1:10000

Line 5000

Pole-Dipole Array

VI

a na a

plot point

2.68

2.82

2.96

3.10

3.24

3.38

3.52

3.66

3.80

3.94

4.08

4.22

4.36

4.50

4.64

4.78

4.92

5.06

5.20

5.34

5.48

5.62

5.76

5.90

6.04

6.18

6.32

6.46

6.60

6.74

6.88

7.02

7.16

7.30

7.44

7.58

7.72

7.86


mV/V

33.98

44.86

52.39

59.43

66.44

72.71

80.10

87.91

96.86

106.78

117.71

129.08

140.31

155.04

173.03

195.01

220.54

242.75

268.42

293.83

318.44

346.56

392.82

502.16


ohm-m

500

600

700

800

900

1000

1100

1200

1300

1400

1500

1600

1700

1800

481.2

1888.9

500

600

700

800

900

1000

1100

1200

1300

1400

1500

1600

1700

1800

481.2

1888.9


Ele

vation (

metr

es)

39

00

0

39

10

0

39

20

0

39

30

0

39

40

0

39

50

0

39

60

0

39

70

0

39

80

0

39

90

0

40

00

0

40

10

0

40

20

0

40

30

0

40

40

0

40

50

0

40

60

0

40

70

0

40

80

0

40

90

0

41

00

0

411

00

41

20

0

41

30

0

41

40

0

41

50

0

41

60

0

41

70

0

41

80

0

41

90

0

42

00

0

42

10

0

500

600

700

800

900

1000

1100

1200

1300

1400

1500

1600

1700

1800

481.2

1888.9

500

600

700

800

900

1000

1100

1200

1300

1400

1500

1600

1700

1800

481.2

1888.9


Ele

vation (

metr

es)0

1

10

0

10

0

00

1

0 01

0 0 1

00

01

00

01

39

00

0

39

10

0

39

20

0

39

30

0

39

40

0

39

50

0

39

60

0

39

70

0

39

80

0

39

90

0

40

00

0

40

10

0

40

20

0

40

30

0

40

40

0

40

50

0

40

60

0

40

70

0

40

80

0

40

90

0

41

00

0

411

00

41

20

0

41

30

0

41

40

0

41

50

0

41

60

0

41

70

0

41

80

0

41

90

0

42

00

0

42

10

0

GETTY COPPER




200 0 200 400 600

(meters)

Scale 1:10000

Line 5500

Pole-Dipole Array

VI

a na a

plot point

2.68

2.82

2.96

3.10

3.24

3.38

3.52

3.66

3.80

3.94

4.08

4.22

4.36

4.50

4.64

4.78

4.92

5.06

5.20

5.34

5.48

5.62

5.76

5.90

6.04

6.18

6.32

6.46

6.60

6.74

6.88

7.02

7.16

7.30

7.44

7.58

7.72

7.86


mV/V

33.98

44.86

52.39

59.43

66.44

72.71

80.10

87.91

96.86

106.78

117.71

129.08

140.31

155.04

173.03

195.01

220.54

242.75

268.42

293.83

318.44

346.56

392.82

502.16


ohm-m

500

600

700

800

900

1000

1100

1200

1300

1400

1500

1600

1700

1800

451.03

1838.96

500

600

700

800

900

1000

1100

1200

1300

1400

1500

1600

1700

1800

451.03

1838.96


Ele

vation (

metr

es)

38

90

0

39

00

0

39

10

0

39

20

0

39

30

0

39

40

0

39

50

0

39

60

0

39

70

0

39

80

0

39

90

0

40

00

0

40

10

0

40

20

0

40

30

0

40

40

0

40

50

0

40

60

0

40

70

0

40

80

0

40

90

0

41

00

0

411

00

41

20

0

41

30

0

41

40

0

41

50

0

41

60

0

41

70

0

41

80

0

41

90

0

42

00

0

42

10

0

500

600

700

800

900

1000

1100

1200

1300

1400

1500

1600

1700

1800

451.03

1838.96

500

600

700

800

900

1000

1100

1200

1300

1400

1500

1600

1700

1800

451.03

1838.96


Ele

vation (

metr

es)

0 0 1

001

00

1

100

00

1

00

1

100

38

90

0

39

00

0

39

10

0

39

20

0

39

30

0

39

40

0

39

50

0

39

60

0

39

70

0

39

80

0

39

90

0

40

00

0

40

10

0

40

20

0

40

30

0

40

40

0

40

50

0

40

60

0

40

70

0

40

80

0

40

90

0

41

00

0

411

00

41

20

0

41

30

0

41

40

0

41

50

0

41

60

0

41

70

0

41

80

0

41

90

0

42

00

0

42

10

0

55

96

00

05

60

00

00

56

04

00

05

60

80

00

56

12

00

05

61

60

00

55

96

00

05

60

00

00

56

04

00

05

60

80

00

56

12

00

05

61

60

00

618000 620000 622000 624000 626000 628000 630000 632000 634000 636000 638000 640000 642000 644000 646000 648000 650000 652000 654000

618000 620000 622000 624000 626000 628000 630000 632000 634000 636000 638000 640000 642000 644000 646000 648000 650000 652000 654000

2000 0 2000 4000 6000

(meters)

Scale 1:100000

GETTY COPPER INC.INDUCED POLARIZATION SURVEY

LINE LOCATION


DECEMBER 2015


200 0 200 400 600

(meters)


Scale 1:10000

GETTY COPPER INC.

INDUCED POLARIZATION SURVEYCLAIM AND LINE LOCATION MAP


DECEMBER 2015


L3250 N L3250 N

L4000 N L4000 N

L3500 N L3500 N

L5000 N L5000 N

L5500 N L5500 N

L4500 N L4500 N

56

03

50

05

60

40

00

56

04

50

05

60

50

00

56

05

50

0

56

03

50

05

60

40

00

56

04

50

05

60

50

00

56

05

50

0

639000 639500 640000 640500 641000 641500 642000

639000 639500 640000 640500 641000 641500 642000

38950

39050

39150

39250

39300

39350

39400

39450

39500

39550

39600

39650

39700

39750

39800

39850

39900

39950

40000

40050

40100

40150

40200

40250

40300

40350

40400

40450

40500

40550

40600

40650

40700

40750

40800

40850

40900

40950

41000

41050

41100

41150

41200

41250

41300

41350

41450

41550

41650

38950

39050

39150

39250

39300

39350

39400

39450

39500

39550

39600

39650

39700

39750

39800

39850

39900

39950

40000

40050

40100

40150

40200

40250

40300

40350

40400

40450

40500

40550

40600

40650

40700

40750

40800

40850

40900

40950

41000

41050

41100

41150

41200

41250

41300

38950

39050

39150

39250

39300

39350

39400

39450

39500

39550

39600

39650

39700

39750

39900

39950

40000

40050

40100

40150

40200

40250

40300

40350

40450

40650

40700

40750

40800

40850

40900

40950

41000

41050

41100

41150

41200

41250

41300

39300

39350

39400

39450

39500

39550

39600

39650

39700

39750

39800

39850

39900

39950

40000

40050

40100

40150

40200

40250

40300

40350

40400

40450

40500

40550

40600

40650

40700

40750

40800

40850

40900

40950

41000

41050

41100

41150

41200

41250

41300

41300

41350

41400

41450

41500

41550

41600

41650

41700

41750

41800

41850

41900

41950

42000

42050

42150

38850

38950

39050

39150

39250

39300

39350

39400

39450

39500

39550

39600

39650

39700

39750

39800

39850

39900

39950

40000

40050

40100

40150

40200

40250

40300

40350

40400

40450

40500

40550

40600

40650

40700

40750

40800

40850

40900

40950

41000

41050

41100

41150

41200

41250

41300

41350

41400

41450

41500

41550

41600

41650

41700

41750

41800

41850

41900

41950

42000

42050

42150

38950

39050

39150

39250

39300

39350

39400

39450

39500

39550

39600

39650

39700

39750

39800

39850

39900

39950

40000

40050

40100

40150

40200

40250

40300

40350

40400

40450

40500

40550

40600

40650

40700

40750

40800

40850

40900

40950

41000

41050

41100

41150

41200

41250

41300

41350

41450

41550

41625

200 0 200 400 600

(meters)


Scale 1:10000

GETTY COPPER INC.

INDUCED POLARIZATION SURVEYLINE LOCATION on TMI (nT)


DECEMBER 2015


54881.2

55026.5

55105.4

55161.3

55209.0

55250.9

55287.1

55319.8

55348.3

55374.9

55399.9

55424.5

55447.2

55470.5

55493.8

55516.2

55538.1

55559.7

55582.2

55604.0

55625.0

55646.7

55669.0

55691.5

55715.2

55740.6

55766.5

55794.9

55826.5

55860.0

55896.4

55938.1

55987.0

56044.4

56116.6

56206.4

56332.2

56576.8

nT

L3250 N L3250 N

L4000 N L4000 N

L3500 N L3500 N

L5000 N L5000 N

L5500 N L5500 N

L4500 N L4500 N

56

03

50

05

60

40

00

56

04

50

05

60

50

00

56

05

50

0

56

03

50

05

60

40

00

56

04

50

05

60

50

00

56

05

50

0

639000 639500 640000 640500 641000 641500 642000

639000 639500 640000 640500 641000 641500 642000

38950

39050

39150

39250

39300

39350

39400

39450

39500

39550

39600

39650

39700

39750

39800

39850

39900

39950

40000

40050

40100

40150

40200

40250

40300

40350

40400

40450

40500

40550

40600

40650

40700

40750

40800

40850

40900

40950

41000

41050

41100

41150

41200

41250

41300

41350

41450

41550

41650

38950

39050

39150

39250

39300

39350

39400

39450

39500

39550

39600

39650

39700

39750

39800

39850

39900

39950

40000

40050

40100

40150

40200

40250

40300

40350

40400

40450

40500

40550

40600

40650

40700

40750

40800

40850

40900

40950

41000

41050

41100

41150

41200

41250

41300

38950

39050

39150

39250

39300

39350

39400

39450

39500

39550

39600

39650

39700

39750

39900

39950

40000

40050

40100

40150

40200

40250

40300

40350

40450

40650

40700

40750

40800

40850

40900

40950

41000

41050

41100

41150

41200

41250

41300

39300

39350

39400

39450

39500

39550

39600

39650

39700

39750

39800

39850

39900

39950

40000

40050

40100

40150

40200

40250

40300

40350

40400

40450

40500

40550

40600

40650

40700

40750

40800

40850

40900

40950

41000

41050

41100

41150

41200

41250

41300

41300

41350

41400

41450

41500

41550

41600

41650

41700

41750

41800

41850

41900

41950

42000

42050

42150

38850

38950

39050

39150

39250

39300

39350

39400

39450

39500

39550

39600

39650

39700

39750

39800

39850

39900

39950

40000

40050

40100

40150

40200

40250

40300

40350

40400

40450

40500

40550

40600

40650

40700

40750

40800

40850

40900

40950

41000

41050

41100

41150

41200

41250

41300

41350

41400

41450

41500

41550

41600

41650

41700

41750

41800

41850

41900

41950

42000

42050

42150

38950

39050

39150

39250

39300

39350

39400

39450

39500

39550

39600

39650

39700

39750

39800

39850

39900

39950

40000

40050

40100

40150

40200

40250

40300

40350

40400

40450

40500

40550

40600

40650

40700

40750

40800

40850

40900

40950

41000

41050

41100

41150

41200

41250

41300

41350

41450

41550

41625

GETTY COPPER




200 0 200 400 600

(meters)

Scale 1:10000

Line 3250

Pole-Dipole Array

VI

a na a

plot point

1.79

2.42

2.80

3.10

3.34

3.54

3.73

3.90

4.05

4.20

4.34

4.47

4.60

4.72

4.84

4.96

5.07

5.19

5.30

5.42

5.53

5.65

5.76

5.88

6.00

6.13

6.25

6.38

6.52

6.67

6.82

6.99

7.18

7.39

7.63

7.92

8.30

8.93


mV/V

33.98

44.86

52.39

59.43

66.44

72.71

80.10

87.91

96.86

106.78

117.71

129.08

140.31

155.04

173.03

195.01

220.54

242.75

268.42

293.83

318.44

346.56

392.82

502.16


ohm-m

800

900

1000

1100

1200

1300

1400

1500

1600

1700

735.5

1763.17

800

900

1000

1100

1200

1300

1400

1500

1600

1700

735.5

1763.17


Ele

vation (

metr

es)

39

00

0

39

10

0

39

20

0

39

30

0

39

40

0

39

50

0

39

60

0

39

70

0

39

80

0

39

90

0

40

00

0

40

10

0

40

20

0

40

30

0

40

40

0

40

50

0

40

60

0

40

70

0

40

80

0

40

90

0

41

00

0

411

00

41

20

0

41

30

0

41

40

0

41

50

0

41

60

0

cA

cB

800

900

1000

1100

1200

1300

1400

1500

1600

1700

735.5

1763.17

800

900

1000

1100

1200

1300

1400

1500

1600

1700

735.5

1763.17


Ele

vation (

metr

es)

1 0 0

10

0

00

1

100

100

39

00

0

39

10

0

39

20

0

39

30

0

39

40

0

39

50

0

39

60

0

39

70

0

39

80

0

39

90

0

40

00

0

40

10

0

40

20

0

40

30

0

40

40

0

40

50

0

40

60

0

40

70

0

40

80

0

40

90

0

41

00

0

411

00

41

20

0

41

30

0

41

40

0

41

50

0

41

60

0

GETTY COPPER




200 0 200 400 600

(meters)

Scale 1:10000

Line 3500

Pole-Dipole Array

VI

a na a

plot point

2.68

2.82

2.96

3.10

3.24

3.38

3.52

3.66

3.80

3.94

4.08

4.22

4.36

4.50

4.64

4.78

4.92

5.06

5.20

5.34

5.48

5.62

5.76

5.90

6.04

6.18

6.32

6.46

6.60

6.74

6.88

7.02

7.16

7.30

7.44

7.58

7.72

7.86


mV/V

33.98

44.86

52.39

59.43

66.44

72.71

80.10

87.91

96.86

106.78

117.71

129.08

140.31

155.04

173.03

195.01

220.54

242.75

268.42

293.83

318.44

346.56

392.82

502.16


ohm-m

800

900

1000

1100

1200

1300

1400

1500

1600

1700

741.22

1795

800

900

1000

1100

1200

1300

1400

1500

1600

1700

741.22

1795


Ele

vation (

metr

es)

39

00

0

39

10

0

39

20

0

39

30

0

39

40

0

39

50

0

39

60

0

39

70

0

39

80

0

39

90

0

40

00

0

40

10

0

40

20

0

40

30

0

40

40

0

40

50

0

40

60

0

40

70

0

40

80

0

40

90

0

41

00

0

411

00

41

20

0

41

30

0

41

40

0

41

50

0

41

60

0

cA

800

900

1000

1100

1200

1300

1400

1500

1600

1700

741.22

1795

800

900

1000

1100

1200

1300

1400

1500

1600

1700

741.22

1795


Ele

vation (

metr

es)

1 0 0

10

0

100

00

1

39

00

0

39

10

0

39

20

0

39

30

0

39

40

0

39

50

0

39

60

0

39

70

0

39

80

0

39

90

0

40

00

0

40

10

0

40

20

0

40

30

0

40

40

0

40

50

0

40

60

0

40

70

0

40

80

0

40

90

0

41

00

0

411

00

41

20

0

41

30

0

41

40

0

41

50

0

41

60

0

GETTY COPPER




100 0 100 200 300 400 500 600 700

(meters)

Scale 1:10000

Line 4000

Pole-Dipole Array

VI

a na a

plot point

2.68

2.82

2.96

3.10

3.24

3.38

3.52

3.66

3.80

3.94

4.08

4.22

4.36

4.50

4.64

4.78

4.92

5.06

5.20

5.34

5.48

5.62

5.76

5.90

6.04

6.18

6.32

6.46

6.60

6.74

6.88

7.02

7.16

7.30

7.44

7.58

7.72

7.86


mV/V

33.98

44.86

52.39

59.43

66.44

72.71

80.10

87.91

96.86

106.78

117.71

129.08

140.31

155.04

173.03

195.01

220.54

242.75

268.42

293.83

318.44

346.56

392.82

502.16


ohm-m

900

1000

1100

1200

1300

1400

1500

1600

1700

1800

1900

804.28

1941.19

900

1000

1100

1200

1300

1400

1500

1600

1700

1800

1900

804.28

1941.19


Ele

vation (

metr

es)

39

10

0

39

20

0

39

30

0

39

40

0

39

50

0

39

60

0

39

70

0

39

80

0

39

90

0

40

00

0

40

10

0

40

20

0

40

30

0

40

40

0

40

50

0

40

60

0

40

70

0

40

80

0

40

90

0

41

00

0

411

00

41

20

0

41

30

0

41

40

0

41

50

0

41

60

0

cA

cB

900

1000

1100

1200

1300

1400

1500

1600

1700

1800

1900

804.28

1941.19

900

1000

1100

1200

1300

1400

1500

1600

1700

1800

1900

804.28

1941.19


Ele

vation (

metr

es)

10

0

0 0 1

100

39

10

0

39

20

0

39

30

0

39

40

0

39

50

0

39

60

0

39

70

0

39

80

0

39

90

0

40

00

0

40

10

0

40

20

0

40

30

0

40

40

0

40

50

0

40

60

0

40

70

0

40

80

0

40

90

0

41

00

0

411

00

41

20

0

41

30

0

41

40

0

41

50

0

41

60

0

GETTY COPPER




200 0 200 400 600

(meters)

Scale 1:10000

Line 4500

Pole-Dipole Array

VI

a na a

plot point

2.68

2.82

2.96

3.10

3.24

3.38

3.52

3.66

3.80

3.94

4.08

4.22

4.36

4.50

4.64

4.78

4.92

5.06

5.20

5.34

5.48

5.62

5.76

5.90

6.04

6.18

6.32

6.46

6.60

6.74

6.88

7.02

7.16

7.30

7.44

7.58

7.72

7.86


mV/V

33.98

44.86

52.39

59.43

66.44

72.71

80.10

87.91

96.86

106.78

117.71

129.08

140.31

155.04

173.03

195.01

220.54

242.75

268.42

293.83

318.44

346.56

392.82

502.16


ohm-m

900

1000

1100

1200

1300

1400

1500

1600

1700

1800

1900

818.28

1941.55

900

1000

1100

1200

1300

1400

1500

1600

1700

1800

1900

818.28

1941.55


Ele

vation (

metr

es)

39

00

0

39

10

0

39

20

0

39

30

0

39

40

0

39

50

0

39

60

0

39

70

0

39

80

0

39

90

0

40

00

0

40

10

0

40

20

0

40

30

0

40

40

0

40

50

0

40

60

0

40

70

0

40

80

0

40

90

0

41

00

0

411

00

41

20

0

41

30

0

41

40

0

41

50

0

41

60

0

900

1000

1100

1200

1300

1400

1500

1600

1700

1800

1900

818.28

1941.55

900

1000

1100

1200

1300

1400

1500

1600

1700

1800

1900

818.28

1941.55


Ele

vation (

metr

es)

00

1

100

10

0

10

0

00

1

39

00

0

39

10

0

39

20

0

39

30

0

39

40

0

39

50

0

39

60

0

39

70

0

39

80

0

39

90

0

40

00

0

40

10

0

40

20

0

40

30

0

40

40

0

40

50

0

40

60

0

40

70

0

40

80

0

40

90

0

41

00

0

411

00

41

20

0

41

30

0

41

40

0

41

50

0

41

60

0

GETTY COPPER




200 0 200 400 600

(meters)

Scale 1:10000

Line 5000

Pole-Dipole Array

VI

a na a

plot point

2.68

2.82

2.96

3.10

3.24

3.38

3.52

3.66

3.80

3.94

4.08

4.22

4.36

4.50

4.64

4.78

4.92

5.06

5.20

5.34

5.48

5.62

5.76

5.90

6.04

6.18

6.32

6.46

6.60

6.74

6.88

7.02

7.16

7.30

7.44

7.58

7.72

7.86


mV/V

33.98

44.86

52.39

59.43

66.44

72.71

80.10

87.91

96.86

106.78

117.71

129.08

140.31

155.04

173.03

195.01

220.54

242.75

268.42

293.83

318.44

346.56

392.82

502.16


ohm-m

500

600

700

800

900

1000

1100

1200

1300

1400

1500

1600

1700

1800

481.2

1888.9

500

600

700

800

900

1000

1100

1200

1300

1400

1500

1600

1700

1800

481.2

1888.9


Ele

vation (

metr

es)

39

00

0

39

10

0

39

20

0

39

30

0

39

40

0

39

50

0

39

60

0

39

70

0

39

80

0

39

90

0

40

00

0

40

10

0

40

20

0

40

30

0

40

40

0

40

50

0

40

60

0

40

70

0

40

80

0

40

90

0

41

00

0

411

00

41

20

0

41

30

0

41

40

0

41

50

0

41

60

0

41

70

0

41

80

0

41

90

0

42

00

0

42

10

0

500

600

700

800

900

1000

1100

1200

1300

1400

1500

1600

1700

1800

481.2

1888.9

500

600

700

800

900

1000

1100

1200

1300

1400

1500

1600

1700

1800

481.2

1888.9


Ele

vation (

metr

es)0

1

10

0

10

0

00

1

0 01

0 0 1

00

01

00

01

39

00

0

39

10

0

39

20

0

39

30

0

39

40

0

39

50

0

39

60

0

39

70

0

39

80

0

39

90

0

40

00

0

40

10

0

40

20

0

40

30

0

40

40

0

40

50

0

40

60

0

40

70

0

40

80

0

40

90

0

41

00

0

411

00

41

20

0

41

30

0

41

40

0

41

50

0

41

60

0

41

70

0

41

80

0

41

90

0

42

00

0

42

10

0

GETTY COPPER




200 0 200 400 600

(meters)

Scale 1:10000

Line 5500

Pole-Dipole Array

VI

a na a

plot point

2.68

2.82

2.96

3.10

3.24

3.38

3.52

3.66

3.80

3.94

4.08

4.22

4.36

4.50

4.64

4.78

4.92

5.06

5.20

5.34

5.48

5.62

5.76

5.90

6.04

6.18

6.32

6.46

6.60

6.74

6.88

7.02

7.16

7.30

7.44

7.58

7.72

7.86


mV/V

33.98

44.86

52.39

59.43

66.44

72.71

80.10

87.91

96.86

106.78

117.71

129.08

140.31

155.04

173.03

195.01

220.54

242.75

268.42

293.83

318.44

346.56

392.82

502.16


ohm-m

500

600

700

800

900

1000

1100

1200

1300

1400

1500

1600

1700

1800

451.03

1838.96

500

600

700

800

900

1000

1100

1200

1300

1400

1500

1600

1700

1800

451.03

1838.96


Ele

vation (

metr

es)

38

90

0

39

00

0

39

10

0

39

20

0

39

30

0

39

40

0

39

50

0

39

60

0

39

70

0

39

80

0

39

90

0

40

00

0

40

10

0

40

20

0

40

30

0

40

40

0

40

50

0

40

60

0

40

70

0

40

80

0

40

90

0

41

00

0

411

00

41

20

0

41

30

0

41

40

0

41

50

0

41

60

0

41

70

0

41

80

0

41

90

0

42

00

0

42

10

0

500

600

700

800

900

1000

1100

1200

1300

1400

1500

1600

1700

1800

451.03

1838.96

500

600

700

800

900

1000

1100

1200

1300

1400

1500

1600

1700

1800

451.03

1838.96


Ele

vation (

metr

es)

0 0 1

001

00

1

100

00

1

00

1

100

38

90

0

39

00

0

39

10

0

39

20

0

39

30

0

39

40

0

39

50

0

39

60

0

39

70

0

39

80

0

39

90

0

40

00

0

40

10

0

40

20

0

40

30

0

40

40

0

40

50

0

40

60

0

40

70

0

40

80

0

40

90

0

41

00

0

411

00

41

20

0

41

30

0

41

40

0

41

50

0

41

60

0

41

70

0

41

80

0

41

90

0

42

00

0

42

10

0

Documents

Ministry of Energy, Mines & Petroleum Resources Mining