British Columbia

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! -..

1 :y) GEOR MINE AND OIL LTD . (N. P. L. 1 . ASSESSMENT REPORT

AERIAL AND GROUND GEOPHYSICAL - GEOCHEMICAL - GEOLOGICAL

j', 'I .* < I L SURVEYS OF THE

VICTORIA LAKE 23 - 50 MINERAL CLAIMS

VICTORIA LAKE - PORT ALICE

NANAIMO MINING DIVISION

y e BRITISH COLUMBIA

Latitude: 50° 20' North: Longitude: 127O 22' West Aerial Geophysical Surveys By: Waterton Airex Ltd. Ground Geophysical Surveys By: Wm. Chang M. Sc., Geophysics Geochemical Surveys By: Weymark Engineering Ltd. Geological Surveys By: William J. Weymark P. Eng. I -Geophysical Geochemical Interpretation By: , I-

*f L 'i .I Wm. Chang M. Sc., McGill William J. Weymark P. Eng. L

'Up

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_. . .. .- ...... I- ...... _-... - ..... -.- -- ...... -. ... -I-. .- - ...... - ......

GEOR MINE AND o2 L LTD. (N.P.L.) .(v ASSESSMENT REPORT AERIAL AND GROUND GEOPHYSICAL - GEOCHEMICAL - GEOLOGICAL SURVEYS OF THE VICTORIA LAKE 23 - 50 MINERAL CLAIMS VICTORIA LAKE - PORT ALICE NANAIMO MINING DIVISION BRITISH COLUMBIA

I- CONTENTS

1.0 Property ...... 2.0 Location ...... 3.0 Geology ...... 4.0 Geophysical Surveys ...... i Aerial Surveys ...... ajb Ground Geophysical Surveys ... 5.0 Geochemical ...... 6.0 Summary Conclusions ...... 7.0 Recommendations ......

-* APPENDICES Annex - A Descriptive Details, Waterton Airex Procedures Annex - B Descriptive Details, McPhar Magnetometer Annex - C Descriptive Details, Scintrex Scopas Annex - D Core Laboratories, Analyses 1288-30-7031; 1280-30- 7031; 1274-30-7031 Annex - E Cost Distribution ILLUSTRATIONS c; -. Figure: 1 Frontispiece, General Location -4 Figure: 2 Claims Location I, +;Figure: 3 Access and Topography -L. ' -* -Figure: 4 Geology, Claims Area a. t -i Figure: 5 Geology, Vancouver Island , *.'- - Figure: 6A Aeromagnetic Survey - '- Figure: 6 Aerial Geophysical Survey, Flight Lines - Pattern +- Figure: 7 Aerial Geophysical Survey, Test Readings --- Figure: 8 Aerial Geophysical Survey, Anomalous Zones - ' Figure: 9 Ground Geophysical Survey, Magnetic Contour Map Figure:lO Ground Geophysical Survey, E.M. Azimuth Contour Map Figure:ll Ground Geophysical Survey, E.M. Vertical Field 'V'W Figure:l2 Ground Geophysical Survey, E.M. Dip Angle Profiles -d Figure:13 Ground Geochemical Survey - Sampling . i Figure:14:, Geochemical Frequency Graph -Figure:15 Geophysical - Geochemical Anomalies

WEYMARK ENGINEERING LTD.. CONSULTINO ENDINEERS ;I ._...... w0.I...... : E:$;.?' ...... 4H , ...... ,...... ' "..." j WEYMARK ENGINEERING LTD, Conucbmg €nyinuxr 3310 WESTMOUNT ROAD WEST VANCOUVER.B.C. CANADA

Geor Mine and Oil Ltd. (N.P.L.) 3856 Winlake Crescent Burnaby 2, British Columbia

Gentlemen: Re: Victoria Lake Claims Geophysical-Geochemical-Geological Surveys - Port Alice Area Nanaimo Mining Division Vancouver Island, British Columbia I am pleased to submit for your information, this Assess- ment Report of the results of the Aerial and Ground Geophysical Surveys, the Geochemical and Geological Surveys conducted on the Victoria Lake Mineral Claims, Port Alice Area, Vancouver Island, Nanaimo Mining Division, British Columbia. The Aerial Geophysical Surveys were carried out by Waterton Airex Ltd. of Sydney B. C. The Ground Surveys were conducted by Weymark Engineering Ltd. and the Tnterpretation was by William Chang M/Sc Geophysics, McGill University and W. J. Weymark P. Eng. c- Background technical reference relating to the Victoria Lake Claims include Report on the Victoria Lake Mineral Claims by E. D. Cru~,P. Eng. and Glen E. White Geophysical Consulting and Services Ltd, Report of the Victoria Lake Mineral Claims by E. D. Cruz, P. Eng. dated 26 November 1973 and various annual reports of the E. C. Department of Mines. 1.0 Property: The area covered by the Geo-Surveys involved the Victoria Lake Nos 23 - 50 inclusive Mineral Claims. Designation details are given in the following tabulation. Claim No. Record No. Staking Date Record Date Victoria Lake 23-42 36485 - 504 11 Feb/73 19 Feb/73 Victoria Lake 43-50 36770 - 777 16 Apr/73 19 AP473 The reference Mineral Claim Map of the British Columbia Department of Mines is 30. Check surveys have not been made of the claim boundaries, tags, posts atc relative to con- formity with the requirements of the Mineral Act of the Province of British Columbia. The surveys as conducted are within the boundaries of the claims as posted,

2.0 Location: The Victoria Lake Claims group is located about 12 miles south east of Port Alice distributed along the western shoreline and slopes of Victoria Lake. See Figure 2. The geo- (cp graphic reference is YO0 20' North and l27O 22' West, The Land District is Alberni with Registry Office in Port Alberni and the Mining Division is Nanaimo with Recording Office In Nanaimo B.C. 2 Oeor Mine and Oil Ltd. NPL: Assessment Report, Victoria Lake Claims

Access to the claims group is ready by automobile from Port Alice over log hadl roads of Rayonier Canada. These roads are open year round except during heavy snowfall and fire peril periods. Elevations of the claims range from 350' of Victoria Lake to over 2800' above sea level. Except for logged areas, the ground is forested with evergreen species and Alpine cover in sections above 2500 in altitude. During the survey, this area was snow covered and impassable. For the most part the terrain is steep, rugged and precipitous. On the ledges and knolls, rock outcrops are exposed. The flatter sections are overburdened cover with sand gravel and glacial till. There are many small creeks and streams flwoing down the hillside into Victoria Lake, Reference is to Figure 3 for topographic features. The Reference map is Alice Lake, 92 ~/6West Half. 3.0 Geology: The main reference to the geological characteristics of the area is Geology and Mineral Deposits of Quatsino - Nimpkish Area, Vancouver Island, Geological Survey Canada, Summary Report 1929, Part A pp 94 - 107. Subsequent regional presentations include, Memoir 272 Geological Survey of Canada, Gaology and Mineral Deposits of the Zeballos - Nimpkish Area, Vancouver Island, British Columbia By J. W. Hoadley , 1953; (ii) Preliminary Geological Map, Alice Lake - Benson Lake Area, Geology By W. G. Jeffery 1960-61 (iii) Volcanism, Plutonism and Mineralization: Vancouver Island By K. E. Northcote and J. E. Muller, CIMM Bulletin , October 1972 - see Fig: 4 and (iv) references in the E, C. Minister of Mines Reports, especially the 1968 - 71 reports in which presentations are made relating to the Geology , of various section of Northern Vancouver Island. Principal formations of the area include (i) Intrusive Rocks with varied composition from Diorite to Granite, including porphyritic phases as well as bas;ic varieties of Augite and Lamprophyre (ii) Lower Cretasceous Sedimentary Rocks,- conglomerate, siltsbDn9, shale, sandstone; (iii) Bonanza Subgroup, a lower sedimentary unit of limestone-shale- sandst0ne.r greywacke and an Upper Volcanic Uait, largely pyroclastic, tuff, lapilli Tuff, Tuff Breccia of Andesite and Basalt and Phyodacite flows, (iv) Quatsino Formation, Limestone with medium to thick beds, and (v) Karmutsen Formation with Basaltic amygdaloidal and massive flows with thin bedded limestone near the top of the formation. Economic mineralization has been located in sections, including Island Copper, The Benson (Old Sport - Coast Copper); Alice Lake Mines and several notable prospects. According to presented opinioas mineralization has been mainly associated with volcanic or plutonic processess. However, most of the importank deposits have . resulted from plutonic processes; some have been related to assessed volcanic exhalative processes and some of the porphyry copper type, Island Copper, are considered to be formed under subvolcanic conditions. Economic minerals located include, Copper, Molybdenum, Zinc, Lead, Iron, Gold, Silver etc. Local Geology: The rocks as revealed during the survey are classified -' as belonging to the Bonanza subgroup and range in variety from Hematitic Basalts - andesites, amygdailoidal and epidotized, Tuffs and Tuff breccia, Rhyolite - Dacit and porphyritic phases. The distribution e, is shown on Figure: 4. The strike is west - northwesterly and the dips as indicated are to the northeast. The rocks have been intensely fractured and there are several major block faults trending Westerly- North. The volcanics appear to phase into and out of each other. No

__-.I_------.,8harp contacts were noted. Copper mineralization__ -is distributed- ~ ---_ - - in-. - -_I -*-

WEYMARK ENGINEERING LTD.. CONSULTINO ENOINLERS

I 3 Gear Mine and Oil Ltd. (NPL): Assessment Report, Victoria Lake Claims .. I.- .. - - the basaltic phases in the form of chalcopyrite and bornite with some secondary copper mineralization as stain or in fracture filling. Blebs of Hematite occur in places. In the Andesitic phases, mineralization 3 appears to be closely related to the epidotized sections and amygdaloids. Higher values are recorded in the hematitized basaltic phases, * Rock Sample A - Basaltic --- 2400 PPM Cu Rock Sample B - ' ' IT- 2700 PPM CU I Rock Sample C - Andesitic e-- 230 PPM cu Rock Sample D - Andesitic --- 360 PPM Cu * See Annex D 4.0 Geophysical Surveys: Forming the base of the geophysical surveys was the Aeromagnetic Survey by the Department of Mines and Petroleum Resources of British Columbia and the Department of Mines and Technical Surveys, Geological Survey of Canada, Map 1737 G; Alice Lake Sheet 92 ~/6, 1962, see Figure: 6A. As indicated thereon , two ltLowsttare present : - i. One occurring in the Lake near the central part of the 'claims and the other ;- ii along the shoreline of the lake near the northeastern part of the claims. The direction of the linears is to the northwest. The gradients are steep, similar to those recorded over the Benson and Alice Lake Mines,

a) Aerial Surveys: A combined aeromagnetic, electromagnetic and Radioactivity was undertaken as part of this assessment programme. This was conducted under contract with Waterton Airex Ltd. of Sydney, British Columbia. Flight readings were taken, see Figure: 7 and consisted of combined aeromagnetic, electromagnetic and radioactivity testing. Annex - A contains the details relating to the. aircraft and the instrumentation used. >i The survey covered the claims area and involved 25 runs each 25,000 + feet in length. These runs were 500 feet apart and were flowbto a true bearing of 3360 North or 1540 Southerly in the reverse direction. The plane was captained by Claude Waterton VRS - 536, Senior Commercial,- the co-pilot was arnold Parlee, both of Sidney, British Columbia. The flight plan was filed with the D.O.T. Port Hardy B.C. Figure: 6 shows the flight plan pattern. Referring to Figure: 7, it will be noted that: - the variation in Radioactivity readings ranged from 0 to I/IOO MR/Hr. - the variation in Electromagnetic readings ranged from 0 to 17 (x.l)microamps - the3 variation in magnetometer readings varied from 0 to 16 (x100) gammas. Background average was set at IO (1000)gammas

3 - for the radioactivity and electro-magnetic tests background was dialed out. !! :j Results: Referring to Fig: 8, it will be noted that there is a strong northerly trend with a cross easterly-westerly exprossions. An interesting pattern is exhibited an Claims Nos 23, 24, and 26 where a succession of a High Magnetometer is adjacent to a similarly north trending Low which in turn neighbors an EM High. Radio- activity is strong in this section indicating alteration.

WEYMARK ENGINEERING LTD., CONSULTING ENGINEERS 4 Geor Mine and Oil Ltd. NPL: Assessment Report, Victoria Lake Claims - Another interesting combination, although smaller in extent occurs on Claims 26, 28 and 30 with a smaller magnetic Low bounded on the West and South by EM Highs. The Highs - EM in the w central parts of the Claims Group may not be in themselves significant, but they most prob- ably reflect formation - structural disharmon- ies. The Magnetic High anomaly offshore on I Claims 36 and 40 is of interest although isolated. Referring to Figure 6A, the Governmental Aero- magnetic Survey in which lows are recorded offshore in Victoria Lake, it will be noted that these features were not recorded in the Waterton Airex Survey. It may well be that the Lows of Claims 24, 26, 28 and 30 may be these features, - the epatial difference may be the due to differences in survey location. Conclusions: The areas depicting anomalous zones of interest are those located within Claims 24, 26, 28 and 30 with the Lows bounded by the EM and.Magnetometer Highs. The Magnet- ometer High of Claims 38 and 40 is of interest when recog- nition is given to the Mineralogical Characteristics of the Bonanza formation vis-a-vis Alice Lake and Benson Lake mining properties. The east-west and north-zone directional patterns of the anomalous zones undoubtedly reflect formation trends. b) Ground Geophysical Surveys: Ground EM and Magnetometer tests were made of the accsssible claims =reas. For the EM-Geophysical, a Scintrex Scopas Instrument Serial Number 10123, SE 80 Model 70722 was used with the reference transmitting station - Jim Creek, Washington, U.S.A. 48N12; 121W55; 18.6 KHZ; 250 KW. Deails of the instrument are given in Annex - C. The readings for the EM Survey are given on Figs: 10, 11 and 12 together with contoured interpretations, vis;- Fig: 10 - E.M. Azimuth Contour Map Fig: 11 - E.M. Vertical Field (VLF) Contour Map Fig: 12 - E.M. Dip Angle Profile Map For the Magnetometer tests, a McPhar M700 Flux Gate, Mag- netometer, Ser. No. - 7126 was used. Reference station O+OON and O+ OOEast which was set at 500 gammas. The readings are given on Fig: 9 as well as contoured interpretation. Wm. Chang M. Sc. Geophysics, McGill University Montreal conducted the EM and Magnetometer Surveys as well*as analyse of the data and interpretation in coordination with W. J. Weymark P. Eng. A composite plot the anomalous zones as interpreted for the EM and Magnetometer Surveys as well as for the Geochemical is given on Fig: 15. To ne noted thereon, the ground surveys reveal magnetic Highs to the southern section of the Claims group, with Magnetic Lows from 40+ N. This conforms with the general Geological pattern of Basaltic and alternatively the Andesitic phases of the Volcanic formations. The EM zones as interpreted are not as dominant 0) as revealed by tho Aerial Surveys. The most apparent section of interest is the succession of Magnetic Highs, EM-Highs sequenced by the Magnetic Lows. The differences in response by the various phases may be due to the magnetite content and conductivity capabilities. =-- *---2:-.: . -- -~ -- -__ - - -_------_--- ._ __--. - -- - -

WEYMARK ENOINEERINQ LTD.. C~NSULTIN~~ENOINLLRS 5 -- - _- - Geor Mine and Oil Ltd. NPL: Assessment Report, Victoria Lake Claims 5.0 Geochemical: Also, as part of the ground phase of the field invest- igation of the assessment of the metalliferous potentialities of the Victnria Lake Claims, a geochemical testing of the soils for copper was carried out by Weymark Engineering Ltd. Soil samples were taken at 500-foot intervals along the axis and cross- axis lines. The record of the samples and Assay results are given in Annex 1 D. Chemical Analyses were made by Core Laboratories of Vancouver. Samples were taken below the top humus layer or in the I31 Zone. Plots of the results are given on Fig: 13. Results: A Cumulative Frequency Plot of the results for copper was prepared on probability paper. Support mathematical cal- culations yielded the following;- See Fig: 14 Item Copper PPM Ari thmet i.cal Ave. 62.3 50s of Curve 37.5 !' Threshold 95% 145* Standard Deviation 76.8 I * Breaking Point Reviewing the plots on Fig: 13, it will be noted that the test area, using a control of 75 PPM Copper south of 60+N is not significant whereas from 60+~North continuity is portrayed. The extreme high at 97+ could represent accumul- ations from the phase contact between the Andesitic and c Basaltic members of the Volcanics. It is surprising that consistent low values were obtained in the southern sections (Y of the claims which are mostly underlain by Basaltic members that recorded higher copper values. Perhaps these are more I impermeable. Tests were not made for other minerals to i copper, The spectrographic analysis, AMex - D confirms that I copper is the most dominant insofar as commercial interest I I relates. Referring to a paper by Sutherland Brown, Deputy Chief, metallurgical Branch, British Columbia Department of Mines and Petroleum Resources, entitled Aspects of Metal Abundances and Mineral Deposits in the Canadian Cordillera, CIM Bulletin January 1974, the background level for Copper in the Insular belt is in the 40 - 50 range for soils. 6.0 Summary Conclusions: The results of the Geological-Geophysical- Geochemical Surveys as presently interpreted are: i. There does not appear to be coincidence between the aerial and ground geophysical testing. This could be attributed to many differences of controls. There does, however, appear to be a relationship between geological and geophysical patterns with trend and formation-structural Characteristics conforming. 8 ii. The relationship between the geological formations and geochemical behavior of the soils is not harmonious. An inconsistency exists between the soil sampling and the rock sampling,- basaltic vs andesitic members. iii. Further testing in detail is required in order to apprise the relationship between the geological-geophysical and geochemical characteristics of the claims area. 6 - . - _.. Geor Mine and Oil Ltd. NPL.: Assessment Report, Victoria Lake Claims _- -

7.0 Recommendations: On the bases of the results obtained from the relating Geochemical-Geophysical and Geological Surveys referred to in this report, it is considered that further field investigations are warranted. The presence of copper mineralization in the Bonanza geo- ogical formations underlying the claims area and the known economic metalliferous significance QS deposits close by with similar settings are primary considerations for carrying out further studies. Future programmes should be directed to test the indicated anomatous sones at closer intervals with special attent- ion given to determining the inconsistencies between the different geophysical surveys and between the mineralogical characteristics of the volcanic members and the geochemistry of the overlying soils.

Respectfully subrnitteQ 25 February 1974 eYill m J. Wey rk P. Eng.

!1 !i

! ANNEX - I3

Rugged, reliable instrument for hand-held field operation *

Self Levelling sensing head Five scale ranges: 1,000 to 100,000 gammas

Low temperature drift Latitude adjustment up to ~3Oo.000gammas everse .measurement potarity by - turn of switch Long battery life

.M700 Flux Gate Magnetometer is a For measuring the vertical component Measurement Ranges Sensitivity simple and efficient instrument for mea- of the earth's magnetic field, the ins- 1,000 gammas 20 gammaddiv. suring changes in the earth's magnetic trument is set to zero at a chosen base field. The two operating controls are station. 3,000gammas 50 gammaddiv. . mounted on the face of the instrument At each station on the survey the M700 10,000 gammas . 200 ga.mmas/div. is held roughly level, and a measure- with the latitude adjustment and ac- 30,000 gammas 500 gammas/div. cessory socket concealed behind a ment of the increase or decrease in the panel on the side. magneiic field is read off the meter 100,000 gammas 2,000 gammas/div. directly in gammas. Operating temperatures -35OC.to 55OC. Weight Temperature drift less than 50 gammas 6%pounds (3 kg.). less batteries and .' over entire operating range carrying case 8 pounds (3.8 kg.) with batteries Dimensions4x7xlO'hin. (10x18~ Batteries 27 cm.) Two internally mounted 9V batteries provide up to two months operation under normal conditions. 4 Head

External Battery Packw I. .

Side accessory socket Accessory socket is located in the side Chart Recorder For long term base allows use of: panel of the M700 along with the station monitoring an external heavy latitude adjustment control and acces- duty battery pack and chart recorder external battery pack soryswitch. It allows the use of various can be attached to the M700. Any pieces of equipment that extend the current type recorder with a sensitivity - chart recorder range of this instrument. of one milliampere for full scale deflection or any potential type recorder external sensing head External Battery Pack For below with a sensitivity of one volt for full freezing operation the internal batteries scale deflection can be used with the horizontalsensing head are removed and the external battery magnetometer. pack used. It is carried under the operator's clothing to prevent battery External Sensing Head An external freezing. An alternate external battery sensing head can be used on the M700 pack is available consisting of 12 "C" without modification to the instrument. size flashlight batteries. ' The sensing head plugs into the accessory socket.

McPhar Geophysics Instrument Sales Offices Canada Australis United Stater McPhar Geophysics Ltd. McPhar Geophysics Ply. Ltd. McPhar Geophysics Inc. 139 Bcod Street. Don Mills. Ontario 50 Mary Street. Unley 506. S. Australia 818 W. Miracle Mile. Tucson. Arizona 85705 Tel.: (416) 449-5551 Tel.: 72-2133 Tel.: (602) 624-2588 w 81 1 - 837 W. Hastings Street, Vancouver, B.C. 28 Nicholson Road, Subiaco. Y1.A. 6008 Tel.: (604) 685-3613 Tel.: 841-4955 Philipplner Singapore 63 Alexander Street. Manly 2095. NSW. McPhar Gcoservices (Philippines) Inc. McPhar (Asia) Pte. Ltd. Tcl.: 977-4192 P.O. BOA3279, Manila 51 Kallang Place, Singapore 12 Tel.: 50-53-06 lei.:53031 1 . . y C ..ANNEX d. '5

.. -. (Y The SCOPAS' VLF System employs V.L.F. tude relations and the elliptical polzriza- Radio Stations in the 15 to 25 kHz Range tion in the horizontal and vertical planes as primary field sources. The undist- can be determined as well. Thus, the urbed field from these remote sources is operator can select the parameters most essentially horizontal and of relatively useful for his search problem. constant strength. When conductors are present, the geometry and amplitude of - the field are locaily distorted and polarization of the field may occur. < - ._ -.--.With the versatile SCOPAS' unit, all .. amplitudes and geometric parameters as well as the characteristics of the C.-."-.;:-. . . -..-a . .- polarization ellipse can be measured. 'For fast reconnaissance surveys dip- clsp angle an? fie!d directions can be rapidly

,- ... '.. deierrnined. For detailed surveys, ampli- 5 '.Can. ?at. 670765 SPECIFICATIONS OF SCOPAS *----c---LI-C-----.---P 'u, LxVLF ELECTROMAGNETIC ------> ir' .' e'- UNIT MODEL SE-80 !:i t, ,.!I' 1: - !i . ' !I I; Id ii . :: Primary Field: From any selected VLF transmitting station in frequency !* .I :i range between 15.4 kHr to 25 kHr. I/ir 1..:-. 1 i 'I . ' :.i

82, il . .. By means of an eight step switch and variable control !! ij Station Selection: ! covering full range. ;I ;. .j ri :i 'I I] .!.!i.. Measured V-I ues: a) The azimuth of horizontal field. t.! b) The dip of the axis of the coil a? the minimum field, !.; . .. measured from the vertical. !i is . c) The amplitude of the horizontal field strength in any !I ' ?ti'. *li direction. 1' i ;.e if I 11 d) The amplitude of the vertical field strength. 1.; . The phase angle between the maximum horizontal and ver- fl :j tical field can be calculated from measured values. 1; 1. ,I . I! fi !;. Normal Rcading. Accuracy: Amplitude -e 21;. 'i. * Atlmst!: Qr) . li... -. . - t2'. . ._ - ii Dlp &lo.- Dependent on signal strength. . 'i!I .c1 . ii . Batteries: Two 9 volt dry cells...... - .. .. ii Dimensions: ' 9.66"~3.68"~ 5.80" . ij-. t.i 24.5 cm x 9.4 cm x 14.7 cm .. 11!. , qt 'i : !.I Weight: 3 Ibs. (135 kg) . iI) .t 1'; :I li ..:I Accessories: Carrying strap. !I."t.

I' :I li :!1. .. 11 ------CERTIFICATE

I, William James Weymark, P. Eng., Consulting Engineer President of Weyrmrk Engineering Ltd.. of the District of West Vancouver, of the Province of British Columbia hereby certify that :- 7. I am a graduate of Mining Engineering of QUeen'8 University, Kingston, Ontario B. Sc., 7940 and have been practising my profession for twenty-five years. 2. I am a practising Consulting Engineer and resid8 at 3310 Westmount Road, West Vancouver, Province of British Columbia. 3. I am a member of the As8ociation of Professional Engineers of the Province of British Columbia and also of the Consulting Engineers' Division of the Association of Professional Engineers of British Columbia. 4. I am a member of the Canadian Institute of Mining and Metallurgy, of the American Institute of Mining, Metallurgical and Petroleum Engineer8 and of the American Geophysical Union. 5. I have no direct or indirect interest whatsoever in the Victoria Lake Mineral Claims Group or in Geor Mine and Oil Ltd. (NPL) or any affiliate or security relating thereto. 6. The findings of the accompanying report are baaed on my personal examinations and study of the field setting of the mineral claims and the relating geophysical-geological and geochemical data. The geophysical readings were obtained by Aerial Geophysical Surveys by Waterton Airex Ltd., and the ground data was obtained by Wm Chang M. Sc. McGill Un-rsity. Interpretatlcn was made by Wm. Chang M. Sc. and myself. DATED at West Vancouver, 7 974

ymark P. Eng.

I I

WEYMARK ENOINEERINO LTD.. CONSULTlNCi TNOINLCRS '!

JPPENDICES

Q) .I

! 3

A patented Combined Method I Total Rad!oacUvlty IElectromapnetic unit .3 Microamp Scleetlve Radloactlve Thmhold Electromagnetic + Magnetometer Radioactivitv unit ,002 MR/HR Computer Processing Controlled Senrltlvlty ,Magnetometer unit 510 Gammas

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VICTORIA INTLRNATIONAL AIRPORT BOX 2002. SIDNEY.8.C.. CANADA PMONC636-2194 Proven in Western and Northern Capada for the highest degree of accuracy at the lowest cost. $10, per lineal mile including base and positioning expenses on average surveys. Oil aasessment in the North at $12. per lineal mile^ A 400 squaxe mile area at 1,000 foot spacing would cost $20,000.and could be cqleted in three .weaks. This should put your wound party a year or more (Y ahead in their exploration prograrp~ By the use of this combination method 8% of the unproductive anomalies can be calculated out of the survey which results In keeping the ground follow up costs to s minimum. Electromagneticst Waterton quadrature system. Trans. on 1,000 CPS, Rb'cefve In units of .lmicroampere& Magnetometers Flux-gate Sharpe PMF-3 'or McPhar WOO, or Proton, GeoMetrics 6.806, ( Modified to our system, ) Receive in units of 10 to 100 Gammasr Radioac tlvityt Detectron - DR299 24 tubes. Receive in units of .OOl MFt/HR. (Total count.)

*r Threshold8 Three inch crystal. # Positions 1.3 - 1,63 - 2,5 Mev, Grid supplied in scales of 1,000 to 2,000 feet per inch, with clear overlaye

* showing the anomalous WBLLSo Ground checks over mountain areas have found the accuracy to be within-500 feet on a 500 foot grid. Over 15,000 lineal miles of reconnaiseance and assessment assistance completed.- t-. t-. (v, in 40 different areas by the end of 1970. i ,.? .. Operation- range up to 400 miles from base. Aircraft type: ~iking-300 - . Twin Comanche. Computor processing available. ASSA YERS CHEMISTS GEOCHEMISTS

CORE LABORATORIES - CANADA LTD. 325 Howe Street Vancouver 1, B.C. Phone 688-3504

SAMPLE61 FROM MEXMARK ENGINEERING

C - _-_ - B ____- -- D- - - -. - __- - . Aluminum 8. 8. 8. 8. Antimony ND ND ND ND Arsenic ND ND ND ND Barium ND 0.01 0.03 0.01 -- Beryllium ND ND ND ND Bismuth ND ND ND ND Boron 9-01 0.001 ND 0.001 Cadmium ND ND ND m Calcium Major Major 5. 5. Chromium 0.01 0.005 0.005 0.003 Cobalt ND ND ND ND Copper 0.2 002 0.05 0.1 Gallium ND ND ND ND __ . . __ . Gold - __ Trace -Trace - Trace Trace -

Iron 5= 5. ~ 5. 7- Lead 0.1 0.01 0.01 0.01 Magnesium 2. 3. 3. 4. Manganese 0.1 0.2 0.2 0.1 - Molybdenum - 0.001 ND - ND ND Niobium ND ND ND ND Nhkel ND ND ND 0.001 Potassium 2. 2. 2. 2. Silicon Matrix Matrix Matrix Matrix _- Silver - - Trace Trace Trace Trace - - - - Sodium 2. 2. 5. 4. Strontium 0.1 0.1 0.01 - 0.03 Ta ntalum ND ND ND ND Thorium ND ND ND ND Tin -ND -- ND ND ND Titanium 0.5 0.5 0.5 0-5 Tungsten ND ND ND ND Uranium ND ND ND ND Vanadium 0.01 0.01 0.007 0.01 Zinc -- Trace Trace ND ND - -_. --@-- A

DATE 21 SIGNED February 197h c

PULP AND REJECTS DISCARDED AFTER 3 MONTHS ASSA Y ERS CHEMISTS GEOCHEMISTS

CORE LABORATORIES * CANADA LTD. 325 Howe Street Vancouver 1, B.C. Phone 688-3504

- PULP AND REJECTS DISCARDED AFTER 3 MONTHS ASSAYERS

! CHE~IISTS GEOCHEMISTS

CORE LABORATORIES - CANADA LTD. 325 Howe Street Vancouver 1, B.C. Phone 688-3504

SAMPLEW FROM WEyMARK ENGINEJZRING

6000N- 5Oar 7000N - 5W 8000N - 40Ui ASSA YERS CH€MISTS GEOCHEMISTS -0 CORE LABORATORIES - CANADA LTD. 325 Howe Street Vancouver 1, B.C. Phone 688-3504

...... - ...... ASSAYERS ' CHEMISTS GEOCHEMISTS

CORE LABORATORIES - CANADA LTD. 325 Howe Street Vancouver 1, B.C. Phone 688-3504

SLEW

_---- IVm: The Copper in Geochem soil or rock. Sample is attacked - by 1:l HNO in boiling water bath for 2 hours. Concentration is read bgatomic a3sorption spectrography.

DATE U, February 1974 SIGNED vi

PULP AND REJECTS DISCARDED AFTER 3 MONTHS ...... -I ...... - ....___ ._ .-- ...... - ...... _.- .

ANNEX - E

COST DISTRIBUTION

I, Waterton Airex Ltd., Aerial Surveys ...... $1350.00 2, Core Laboratories Ltd , Analyses \:'e.# 297.55 3. In8truaent Rentals ..(Geophysical) ...... 250.00 4. Weymark Engineering Ltd. Field Surveys - geological - geochemical geophysical data procurement Office collation - compilation - aseembly plotting, fairdrawing and interpretation uf dafa and preparation of Report.

...... $ra-.OO. 00

Total s ,o 7.55 Y: 1 v

_l______l___-^ I---..--.^---I__.^__l__l. ____-__..-._.--^-I jl--____*_._-__,____-.__I_____ ...... _._--...... --z .-7-.. -'

WEYMARK ENGlNEERlNO LTD.. CONSULTINO CNOINELRB !

.. b.. ..A. ... *: , - .','.I

NO.

--.. --...... NOTE: LOCATION OF CLAIMS IS APPXOX. REF. MAP: B. C. Minister of Mines No. 3D .. I

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...... -___ W EYPJARX ENG I N EE CONSULTING ENGIN WEST VANCOUVER, BRITISH

NO......

lOTE:I_ LOCATION OF CLAIMS IS APPROXI' 3EF. MAP: E. C. Ministor of Mincs SUBMITTED WJW No. 3D L

~otwoon- 0 - 800 I)

~ Bolow -800 13ammas ~ifforonooerofsrrod to station o+OO E & o+OOn Sot at 500 garaaurs Gatst~natnunontr nagnotomotorMoPhar M7oO-IISor NO. 7126, nophar ~oophymicrLtd. Toronto, Ont - SO. Ann0x-B

gpmmaS - diroct Latitud.

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!~A: .I -,-! .. .I E.H. AZIMUTH CONMUR MAP '4 LEGEND Apparon t Cornpram zizi Azimuth 15501650 - :;;o/ 1650 4 Azimuth & Asimuth 1750 - 1850 D Asimu t h 50 - Aaimuth 150 - 250 - Inatrumont: Soonttox Scopas Rocoivor - Sor 80, Model 707 011, Sor No. 10101 Transmittor: VU: Stn NLK; Jim Crook Waah.. 48N12r -I piold122W55 Roadinge - 250 KW : Via Chans MSO, Intorprotation: Wm Chang MSo Roforonoo: - AMOX- C Seal.: - I inch - 500'

Apparont Compasa + VLF Vortioal Fiold Contour Intorval - 5%. Vortical Fd Roa inga takon in of t Horizontal Fiold.

\ 4 CroaaOvor - Ron1 or0 oovor at chango poin from ponitivo to no6 atiV8 Sign - Toward oast on Wost-Eaat Soah: 1 Inch = 5001 Roforonoo: So. Annox - Cdr Fig, 10 lo ~ortioal~d. % 170 8 Dip Anglo0

E. Fobruary 19

I ., .. , . . , ...... ~ . . . . . -, ...... -... , . . . E. M. DIP ANOLE PROFILE '1 V.L.F. LEGEND - VLFProfile Dip Angle

-\3 Croasovor - Ron1 - Crossover at ChangO- point from pooitivo- to negativo 8ign - -. tho Fd Rmadings _. loss offoctiv. compononts of slop.-. - of topography - Toward Weat on wO8t---. Eaa t Linm _.

-8 1 Inch E 500' - So. Annex - c & Fig8 10 LEGEND .

E 750 - 500 ppm Cu.

soil Sample6 taken by L. MiSCOvic. - ffeologist References - Annexes - D :: Scale. 1 Inch = 500'

OEOCHEMICAL in read by atomic absorptio

---- ......

WEYWJWRK ENGlNEERlNG LTD. con5Lst~,z~€tyineez5 TELEPHONE 922-1536 3310 WESTMOUNT ROAD WEST VANCOUVER. B.C. CANADA

8 April 1974

Mr. E. J. Bowles Chief Gold Cornmissioner Departnient of Mines and Petroleum Resources Victoria, B.C.

Dear Mr. Bowles: Re: 766 Nanaimo Victoria Lake Claims Geochemical-Geophysical Report # 4907

Referring to your letter of the 25 March 1974 to Geor Mine and Oil Ltd. (NPL), I submit the following:

1. Outcrop map of geological formations of the claims 2. The strike in the text reports True North which was regretfully not noted. The grid was plotted as well as the formations on a magnetic basis.

3. The location of Rock Samples A,B, and C is designated now on the geological map.

Thanking you for your review of this submission.

... .,...... , -...... ;.I.. ..~...... ~ f\i 0...... , :. ,.. I ._. _.. 2. wo ...... , P 4 ~......

...... - ...... - ...... , ...... ,,,. :......

...... ! William J. Weymark P. Eng.,-President of Weymark Engineering Ltd., of 3,3370 Westmount Road, West Vancouver, British Columbia

in the Province or' Biiush Columbia, do solemnly declzre that aerial and ground geophysical - Geochemical and Geological Surveys have been conducted on the Victoria Lake Nos 23 - 50 , Record Nos 36485 - 504 and 36770 - 777, Victoria Lake - Port Alice Area, Nanaimo Mining Division, Vancouver Island, British Columbia with Report issued 25 February 1974.

The follwwing expenses were incurred:

1. Waterton Airex Ltd;,- Flying, positioning and reading Airborne Magnetometer, Electromagnetic and w Radioactivity tests on the aforesaid claims Approx: 700 miles 0 $13.50 per mile $7 350.00

2. Sample Analysis Core Laboratories 8297.55 3. Instrument Rentals 0 (Geophysical) 250 .00 4. Weymark Engineering Ltd . Field Surveys - Geophysical - Geochemical - Geological, data procurement, field supervision, sample collection analys'es of results, calculation, plotting and fairdrawing data and preparation of Report

...... $4200.00

Total $6097 55

Navigational aids were furnished by Geor Mine and Oil Ltd. (NPL) and Weymark Engineering Ltd to assist flight navigation.

And I nzkz this solemn declaration conscientious1:i believing it to be true, r?nd knowin$ that it is of

the same foxc a:id effect 3s if made undzr oath 2nd by virtue of the '' Canada Evidence Act."

Weymark P. Eng. I 'keymark Engineering Ltd , A.D. f ,-. .. .

ci,