GEOCHEMICAL REPORT ON THE LONG B CLAIMS TEXADA ISLAND

NANAIMO MINING DIVISION 92F/9W, 49' 37', 124" 17'

BY J.T. SHEARER, M.Sc.

for cj CARIB00 GOLD CORPORATION P.O. BOX 4237, QUESNEL, B.C. V2J 353

OWNERS: E.T. Johanson, R.E. Mickle, J.E. Newman Field work completed between April 15 and April 27, 1985

May 8, 1985 CONTENTS Page

LIST OF ILLUSTRATIONS AND TABLES i SUMMARY ii INTRODUCTION 1 CLAIM STATUS AND ACCESS 2 FIELD PROCEDURES 3 GEOLOGY 3 MINERALIZATION 5 GEOCHEMISTRY 6 cs CONCLUSIONS AND RECOMMENDATIONS 7 REFERENCES 10

APPENDIX I List of Personnel and Dates Worked 11 APPENDIX I1 Statement of Qualifications 12 APPENDIX I11 Statement of Costs 13 APPENDIX IV Analytical Procedures and Gold 15 Hi stogr am APPENDIX V Geochemical Assay Certificates 17 and Rock Description Sheets APPENDIX VI Department of Mines 30 G. Forms, Long B. Claims APPENDIX VI1 List of Suppliers, Texada Island 33 APPENDIX VI11 Estimate of Costs for Future Exploration 34 LIST OF ILLUSTRATIONS AND TABLES

Following Page

FIGURE 1 LOCATION MAP 1

2 ACCESS MAP 1 :125,000 2

3 CLAIM MAP 1 :50,000 2

4 TOPOGRAPHIC MAP 1 :50,000 2

5 REGIONAL GEOLOGY 1:250,000 3 o 6 DETAfL, SOUTHEAST 1 :2,500 (fold out) 4 AREA

7 DETAIL, UPPER CREEK 5 AREA 1:1,000 (fold out)

8 SOIL PROFILE 1 1 :10 (fold out) 6

9 SOIL PROFILE 2 1 :10 (fold out) 7

10 SOIL GRID, LONG 1 :2,500 (in B CLAIM pocket )

TABLES

TABLE 1 LIST OF CLAIMS 2 ii

SUMMARY 1. Soil sampling on the Long B Claims, Texada Island, was carried out between April 15 and April 27, 1985. The claims are owned by E. Johanson, R. Mickle and J.E. Newman. Some of the area has undergone juvenile forest spacing. 2. Previous work includes old trenches and pits on irregular chalcopyrite - bearing silicified zones and quartz veins. Recent surveys conducted by the present owners include SP, and limited soil sampling. Several small pits were blasted out for assessment purposes in 1985. 3. A total of 115 soil samples and 5 rock geochem samples were taken during the examination. Results indicate anomalous gold in soils in the Southeast Areas and along the Upper Creek showings. Soil profiles in the c; Southeast -Zone show highly anomalous conditions increasing with depth to definite cut-offs. The southern contact between the intrusive and volcanics is characterized by a high gold in soil content and was covered by detail fill-in soil samples in 1985. 4. Rock samples across short widths (less than 3Ocm) have previously assayed up to 0.59 oz/ton gold in copper-rich sections. Gold values attain 0.362 oz/ton in the present chip sampling over 30 to 60cm.

5. The claims are underlain by a granodiorite to quartz diorite stock in contact with altered Karmutsen Formation mafic-rich volcanics. Chlorite and epidote alteration is common near the intrusive contact. The area is within a weak porphyry copper system and some of the precious metal values could be related to peripherial zoning of this extensive mineralizing event. 6. Anomalous gold values in soil samples, SP, magnetics and VLF EM suggest a relatively narrow linear zone trending 288", marked by silicified and pyritized rocks in the Southeast Area. Discontinuous exposure of siliceous zones in the Upper Creek Area indicates a narrow mineralized trend nearly perpendicular to the cj Southeast linear. The higher gold-in-soils near the south intrusive-volcanic contact found in 1981 were checked by detail follow-up sampling in 1985. Highly anomalous areas should be exposed by hand trenching and may warrant backhoe trenching. INTRODUCTION Between April 15 and April 27, 1985, the Long Beach Claim Group, Texada Island, was examined. A total of 5 rock chips and 115 soil samples were collected and delivered to Acme Analytical Labs. The property is underlain by a composite quartz diorite to granodiorite stock in contact with altered Karmutsen Formation mafic volcanics. The area has been mapped by R.G. McConnell in 1908 and 1909 at 1:126,720. J. Muller has included Texada Island in his work on Island which is compiled as Geological Survey of Open File 463. Extensive prospecting was conducted throughout Texada Island beginning in the 1870’s and particularly between 1890 and 1910. The first recorded work in the Long Beach Area is in 1950 by D.W. Cochran who excavated the Upper Creek trenches (Minister of Mines 1950, pages 178 - 180). LI2 A large claim block was located by R. Samuelson and R. Mickle in late 1969 and optioned to Falconbridge Nickel Mines Ltd. (Wares 1971). Part of this old property encompasses the present Long B Claims and was referred to as the Airstrip Grid. Work by present owners included limited SP, magnet- ometer and soil sampling. Small hand pits have been blasted into areas of anomalous SP values.

Several small high grade copper-gold mines operated in . the early 1900’s near Vananda. The Marble Bay Mine produced about 314,000 tons of ore for a total of 50,000 oz. of gold. The main shaft reached a depth of 1,200 feet. Recently, Texada Iron Mines produced copper-iron con- centrate from a magnetite skarn deposit from between 1952 and 1976, yielding, approximately, from 20 million tons of ore averaging 33% iron, a total of 25,000 02. of gold. Currently there is a substantial output of limestone for cement and other uses by Lafarge, Ideal, Domtar and Imperial . In late 1984, spectacular specimens of coarse gold from a narrow quartz vein on the Holly Crown grant near Kirk Lake, were discovered in place. This claim was optioned to Northair Mines Ltd. in January 1985 and a diamond drill u program was completed in early May 1985. Results are to be released shortly. Many new claims have been located recently. 2

- *.- W*T COAST'''+

TRAiL ---.; CARIBOO GOLD +ORPOWTION W*~Y LONG B CLAIM GROU~ ises along the Pacific Coast are #: Royal Viking Lines; Sitmar LOCATION MAP aska Marine Transportation; I iisesiP & 0; Holland American dian Pacific Steamships; Pac- DATE: APRIL 6 1981 /MAY fOB5 8s; Black Sea Shipping CO.; Of YM nbia Ferry Corporation. MA TIC PAR NTS: 92 F/SW I I FfGURE I -2-

Considerable recent preliminary exploration effort has been concentrated on Texada Island by Aquarius-Longbar Minerals, Canada Cement Lafarge, Cambrian Explorations (near Long B), Kitimat Copper, Texada Lime, Ideal Basic Industries, Shima Resources and Arron Mining (near Long B), Bethex and numerous individuals. CLAIM STATUS AND ACCESS The Long B Claim Group is composed of the following modified grid claims as illustrated in Figure 3:

TABLE 1 LIST OF CLAIMS Name Units Record No. Date Recorded* Owner Long B21 20 1689 (4) April 9, 1984 E.T. Johanson

Long B24 4 1750 (5) May 1, 1984 J.E. Newman

Long B25 20 - 1751 (5) May 1, 1984 J.E. Newman ARL 4 2104 (4) April 9, 1985 R.E. Mickle * sufficient assessment has been filed with this report and previously to bring the expiry date to 1986.

The claims are situated around the Cheekye-Dunsmuir high voltage transmission line that is under Mineral Reserve o/c 574 79:03:01 subject to conditions. Access is by improved hydro road to the transmission line area and then by old logging roads into the property as shown in Figures 2 and 4. The main showings are 19 km southeast of the Gillies Bay Airstrip. The old roads are passable with difficulty by two wheel drive vehicle but a 4 x 4 is advisable. Parts of the claim group have undergone juvenile forest spacing and future line cutting will be time consuming. (1 Inch = 2 Miles approximately) ,165 1 0 2 4 HU 1 4 1 r pI HdU I 8.CARIBOO GOLD CORPORATION Magnetic Declination approximately 23‘12’ East at centre of map. 1976 Decreasing approximately 3’annually

1 Kilometre = 0 6214 Miles Universal Transverse Mercator Projection Fq.n In DETAIL LOCATION MAP

DRAWN BY JS DATE APRIL 6 1981 /MAY IS85

15’ M92F/9Wi

,

0 1- 2 Mikr

1 CARIB00 GOLD. 7CORPORATION UNLESS VERIFIED OR tuwEwo. TML w manow 01 A LONG 0 CLAIMsGROUP i3 LEGAL CORNER POST IS -0 ON THE LOCATOR’S SKETQC FOR FUR- TMER INfORNATIo(I, AWLV TO THE OFFIQ Of TIUi MINING #VISION k COWCERNER I CLAIM MAP

DATE OF MICROFILM: 85.04~-,ll DRAWN BI JS DATE APRIL t3 1-1 /MAYISB~

NTS 92F/9W FIGURE ~- 3 .ld cs

LONG 6 CLAIM GROUP TOPOGRAPHIC MAP

DRAWN BY JS DATE APRIL 6 1981 /MAY 1985 -3-

FIELD PROCEDURES The soil lines were run with a Silva compass and roughly measured for slope corrections by a Belt Chain calibrated in meters for which the manufacturer claims a 0.196 accuracy. A baseline was established in 1985 starting at the 1981 sample site of 150w + 270s. The baseline was cut out with a chainsaw and trends 250'. Lines are 50m apart trending 160"and are marked by many orange flags with stations in numbered blue flagging. Soil samples were taken at 10m intervals from the B horizon at depths ranging between 40 and 90cm by a grubhoe and shovel. Samples were put in waterproof Kraft bags and delivered to Acme Analytical Laboratories Ltd., 852 E. Hastings St., Vancouver. Standard soil data sheets were filled out in the field noting such items as sample number, location, depth, horizon, colour, particle size, 96 organics, pH, slope, vegetation and additional remarks. Analytical procedures are outlined in Appendix IV. Rock samples were taken as continuous chips over short intervals. Rock description are shown in Appendix V;. cj Results are plotted on Figure 10 (in pocket) using Hip Chain traverses between soil lines for control.Outcrop position was also plotted on airphoto BC 78032 No. 137.

GEOLOGY The regional geology of Texada Island is relatively simple as shown on Figure 5. Upper Paleozoic Sicker Formation volcanics, volcanoclastic sediments, and lime- stone are exposed on the extreme south tip. Most of the Island is underlain by Upper Triassic Karmutsen Formation amygdaloidal, pillowed to massive basalt, breccia and aquagene tuff. This is overlain by a massive Upper Triassic limestone (Quatsino Formation) which occurs mainly in a .belt extending across the north end of the Island. Five stocks of quartz diorite to diorite are exposed on the coastline. One of these stocks along Long Beach partially hosts the copper-gold showings on the Long B claims. Near Gillies Bay a fault block of Upper Cretaceous Group coarse clastics has been preserved. 3

\

._L

LEGEND

CAMBOO GOLD CORPORATION

LONG 8 CLAfM GROUP

-, \ REGIONAL GEOLOGY FROM MULLER I977 Own FiW 463

DRAWN BY JS DATE APRIL 6 1-1 /MAY 1985

NTS SZF/SW FIGURE 5 -4-

Wares (1971) describes the quartz diorite stock north of the Long B area as a "composite granodiorite intrusion". However, most of intrusive exposures mapped by Wares are identified as quartz diorite. The few granodiorite outcrops could possibly be the result of potassic feldspar alteration as observed on the Long B claims. Alteration appears to vary considerably over short distances. In one locality an intensely chloritized and K-spar rich rock is adjacent to relatively fresh biotite-hornblende diorite. Karmutsen Formation volcanics were seen in the Upper Creek area and near the 3E identification post for Long B25.These are dark green, very fine grained chloritized and epidotized greenstones. Occasionally 2 to 9mm feldspar phenocrysts were seen on weathered surfaces. Limited geological observations are plotted on Figure 10 (in pocket). A very pyritic, volcanic agglomerate- -breccia was noted 65 meters southwest of 150W + 00. Dark, polymictic, subangular, fine grained fragments averaging 1 to 2cm in diameter predominate. Occasionally clasts range up to 25cm in diameter. This rock contains about 596 pyrite dj but assayed 5ppb gold. The volcanic-intrusive contact is well exposed in the Main Creek striking 343" and dipping steeply to the west. This contact is sharp with some suggestion of a narrow, banded, chilled margin. A large quartz vein has been uncovered by trenching adjacent to the contact hosted by diorite. The vein structure passes westward into volcanics and becomes progressively less well defined. To the west and south a prominent topographic feature is a line of 30 to 40 meter high cliffs. These cliffs do not mark the volcanic-intrusive contact but rather start about lOOm within the volcanic terrain. All intrusive specimens are moderately to strongly magnetic whereas the volcanics are non-magnetic. Pyrite occurs in the Southeast Area in small lenses up to 15 - 20%, as 3 - 5mm stringers and thin fracture fillings. LEGEND

SOIL 16 Sol1 Sample Locatlon e 60111 bold'(ppb1; Lead (ppm) 3701 Rock Chlp Sample 19O/O.I Gold (ppb );Silver (ppm)

+ EM 16 Reading +82 In-Phase %Slope (- 7 1 Ouadrature Oh

+ Gold In roll - 1980 Sample 37Oppb

-7OOmv SP Readlng

0 Hand Trench

Pro!lle I Sdl Protlle

\\+I6 (+6 1 c I - Road

CLAIM POST SCALE 1:2400 INITIAL LONG B (c~c61L~D) +40 (-7 0 Kx) Po0 300 400 FEET

*34 (+I) 0 8b liO -METRES +b6f (+6)

SOUTHEAST SHWlNG,OETAlL WORK -35(- 33) P SELF POTENTIAL AND GEOCHEMISTRY wOJECT: LONG B CLAIM GROUP c ENG.: TRM .ENGINEERING LTD. Uork by: FIGURE 6 DATE : APRlL6,l98l REVISED MAY 1985 kom by: E.J., J.S.

. .. -5-

MINERALIZATION Several showings of various dimensions are known on the claims mainly within the intrusive but also in the Upper Creek zone passing into the volcanics, as shown on Figures 6, 7 and 10 (in pocket). King (1950) describes three showings that were sampled with the following results:

Quartz Vein Thi cknes s Gold Content Number 3 Vein width 12 inches 0.56 oz/ton gold

Southeast showing width 8 inches 0.39 oz/ton gold Main or Upper Creek width 14 inches 0.22 oz/ton gold Area Chip samples by D.A. Harron in 1980 show gold values over narrow widths up to 0.476 oz/ton gold in the chalcopyrite-rich Upper Creek showing. The old Southeast Vein mentioned by King (1950) has not been positively identified. However, the zone now referred to as the Southeast Area is somewhat farther along l'strikell from the apparent location of the 1950 work. The Upper Creek Zone is reported by King as follows: "The main vein, on which most of the work has been done, is in a creek near the centre of the group and has been traced nearly 210 feet by rock trenches and stripping. The vein is in a straight definite fracture that strikes north 22 degrees east and dips 66 degrees northwest between walls of andesite slightly mineralized with pyrite. The vein filling is of quartz mineralized with pyrite, chalcopyrite, and secondary bornite. Rock chips taken in this examination confirm the concept of gold values in two main, narrow, linear zones as shown by Samples 80976A to 80980A (Appendix V). This type of mineralization is to be expected on the periphery of a large porphyry copper-molybdenum system as outlined by Falconbridge (Wares 1971). The tonnage potential of the narrow linear zones outlined to date, appear to be limited. However, more significant would be the location of the \ \ \ L;EION \

LEGEND

80(~p7. Soil Sample Location 65/11 Gold (ppb1;Lead (ppm 1

3706 Rock Chip Sample +i.e/+41 Goid (ppb); Silver (ppm)

EM Reading (-+’* 71 * In-Phase O/O Slope Quadrature Oh

APPROXIMATE SCALE I :IO00

0 200 Feet

0 Ib eb i0 40 !5b 60 Metres THICK SECOND 6ROWTH CAMBOO GOLD CORPORATION

+ 74t-a) A UPPER CREEK SHOWING OLD WILLIAM CLAIM

PROJECT: LONG B CLAIM GROUP A+MHl ENG.: TRM ENGINEERING LTO. SOIL 81 Work by: J.S.,E.J. lS/O DATE : ,APRIL 6,1981 REVISED MAY 1985 i Drown by: J.S.,E.J. FIGURE 7 -6-

bedrock source for the high gold in soil values that have been found in the Southeast Area and at the south contact between the volcanics and intrusive. It is also possible that these high gold in soils are related to the porphyry copper system gold enrichment and inherent high mobility of metals in the presence of abundant pyrite decomposition.

GEOCHEMISTRY In February 1980 D.A. Harron collected soil samples near the high SP readings in the Southeast Area. Most of these samples show anomalous copper values with some high Mo and a few anomalous gold up to 570 ppb Au. A total of 129 soil samples were taken in 1981 examination as plotted on Figures 6, 7, and 10 (in pocket). Soil development is illustrated by two soil profiles, Figures 8 and 9, that were located around the small pits dug for previous assessment purposes on high SP results. In 63 profile 1 , Figure 8, gold content increases and then decreases with depth indicating a transported origin of the soil.. This is not surprising since the sampled area is within a wooded stable talus slope. Profile 2, Figure 9, shows a marked increase of gold with depth but a single sample in the lower forward part of the pit gives a much lower value. Other metals do not exhibit any trends through the profile, and cold extraction results are uniformly low. Presumably, hydromorphic dispersion is low in this area. Lead is the only exception with a high cold extractable content in the upper organic rich layer. The usual truncated population distribution for gold in soil is exhibited by the histogram in Appendix IV. A threshold value of 40 ppb Au is used considering the normal sample inhomogeneity of sieved samples and reproducibility of atomic absorption for gold. Soil samples near the Upper Creek showings were taken on two short lines as plotted on Figure 7. Gold values are near or below threshold. In contrast soils in the Southeast show, Figure 6, several sample sites with highly anomalous Au content. High gold values in soil along the Southeast Area SP zone have migrated some distance downslope as indicated by talus development and soil profiles. Soil lines established up slope from the Southeast Area give anomalous gold values on Lines 3OOE and 150E. A potentially significant area long the volcanic-intrusive , ISo SLOPE DEPTH SAMPLE Cm 0 - NUMBER moss AI C LE- I dark brown LB- I organic rich

organic rich irown,some grey 15 LB-2 A2 LE -2 xon ora&ylbrown E Horizon E 30 LE-3 LB-3

I k a W Lor* angular n 45 LE-4 talus blocks - LB-4 a W m I 3 z LE-5 LB -5 60 W J a grey brown I weathered 5' diorite v)

75 LE-6 * L -6 granulated rock

Cm 90 LE-7 reddish brown Le- 7 soil in toremrd section of Pit I METAL CONTENT I (PPb + PPm DATE : APRIL 6,1981 REVISED MAY 1985 LEGEND II I CARIB00 GOLD CORPORATION - X- Gold ppb total extraction -*-Mercury ppb total exctraction I SOIL PROFILE I SOUTHEAST AREA ...... A. , .. .. . Arsenic ppm total extraction I --e--Lead ppm total extraction Vertical Scale I: IO IPROJECT:LONG B CLAIM GROUP Refer to Assay Certificates for Sb ,Zn, Ag Total Extraction 0 IO 20 30 Cm ENG.: TRM ENGINEERING LTD. Plus Cold Extraction Ag , As , Pb, Zn and Sb Work by: R.S.,J.S. , FIGURE 8 I Drawn by : J.S. 1 I -7-

contact is indicated by five strongly anomalous samples on Line 150E between 330s and 450s and two anomalous sites 390s and 420s on Line 00. The samples on Line 00 mark the topographic change between the 30 meter high volcanic cliffs and the relatively uniform steep hill-side mainly underlain by intrusive. Samples taken in 1985 as plotted on Figure 10 (in pocket) show a number of highly anomalous areas between the three lines done in 1981. Of particular significance are the following zones: I Line 50E + 300s - high gold-in-soil up to 2300 PPb Au I1 Lines ZOOW, 150W and 1OOW from 360 to 370s I11 Line 200E + 320s to 350s To fully delineate soil anomaly 11, Lines ZOOW, 150W and 1OOW should be extended a further 100 meters and samples collected at 10 meter intervals. This is a strong multi-line anomaly. The anomaly centered on line 50E at 300s requires limited hand trenching to locate the probably nearby source. Once the zone of interest has been exposed a decision can be made to bring in a bulldozer for further stripping. The anomaly on line 2OOW is more diffused and ground conditions should be checked for a transported origin of the gold values.

CONCLUSIONS AND RECOMMENDATIONS Attention in the past, around the Long B Claim Group, has focused on the definition of narrow gold-bearing silicified zones and quartz veins. Several gold-bearing zones have been outlined in the Upper Creek and Southeast Areas. The western portion of the claims is characterized by an altered intrusive contact between a composite granitic pluton and Karmutsen Formation chloritic basalt. Local areas of intense chlorite, kaolin and potassic alteration are common with-in the intrusion. Silicification appears to be accompanied by abundant pyrite in lenses and heavy disseminations. SAMPLE 5O slope NUMBER spaced juvenile DEPTH forest I 0 (Cm) c .Cm) 0 moss AI LB- 8 dark brown LB -8 A organic rich \ \ reddish brown 15 LB-9 B LB- 9

fine pebbles

1 dark reddish I II I 30 LB -10 t- LB-10 brown o w angular 5cm n flatten pebblei - a W yellowish 45 LB II rn LB -11 510ppb Au brown I 3 z

W A 1800 ppb light brown a \+ 60 LE-12 I LB- 12 x Au sllghtly yellow U C m

ight yellow brow LB-I3 n foreword LB- 13 75 I rection of Pit 2.K I 151 I bedrock nol . I seen 20 PPb 40 60 80 100 120 h,Hg METAL CONTENT

( PPb + PPm 1

DATE : APRIL 6,1981 REVISED MAY 1985 LEGEND CAMS00 GOLD CORPORATION X- X- Gold in ppb total extraction -U- Mercury in ppb total extraction SOIL PROFILE 2 ...... ;11...... Arsenic in ppm total extraction SOUTHEAST AREA

Lead in ppm total extraction Vertical Scale I: 10 --*-- WOJECT: LONG B CLAIM GROUP c Refer to Assay Certificates for Sb, Zn, Ag Total Extraction 0 IO 20 30 ING.: TRM ENGINEERING LTD. Plus Cold Extraction Ag , As, Pb, Zn and Sb -0 Work by 1 R3,J.S. Irawn by: J.S. FIGURE 9 -8-

SP and VLF EM surveys indicate zones of anomalous response that correlate with sulphide-rich areas on surface. High gold-in-soil values are found in the Southeast Area, however, these results are thought to have migrated downslope and the bedrock source should be traced up hill. The area is covered by stable wooded talus sheets. Dr. R.B. Band in Wares (1971) comments that: "Steep slopes and generally sparse vegetation cover resulting from a recent (19673) forest fire favours mechanical down slope dispersion of the soil." The extent of downslope migration of gold values was evaluated by additional soil sampling in 1985. This area is not spatially associated with the narrow structure in the Southeast Area and should be considered as a separate zone. The 1985 work has indicated several subareas that warrant follow-up hand trenching. If hand trenching is successful in locating covered precious metal sources then mechanized trenching with a bulldozer will be required. Future work should concentrate on differentiating between scattered, small gold veins associated with normal porphyry copper deposit zoning and a potentially large, new gold zone associated with the volcanic-intrusive contact. An exploration program to further investigate the copper-gold showings and soil anomalies on the Long B Claims is recommended and summarized below. The estimated cost of such a program is tabulated in Appendix VIII.

Future exploration should consist of: (1) geological mapping and prospecting of the entire claim block, (a) reconnaissance fashion over all claims 1 :10,000

(b) more detailed mapping near showings 1:2500 These data will serve as a basis for a property inventory to assign priorities for mineralized areas. Information from previous Falconbridge work will be useful. Particular attention should be paid to faults and airphoto linears. -9-

(2) Hand trenching at specific locations (3) EM 16 (VLF) Survey to delineate faults and map structure (4) Contingent on the results of the above program bulldozer trenching may be required. A notice of work must be filed with the Department of Mines Inspector prior to work commencing.

Respectf ly Submitted,

v& M.Sc., F.G.A.C. May 8, 1985 - 10 -

REFERENCE B.C. Minister of Mines Annual Report 1950 R.B. King report- ing on Gordon and William Claims, Pages A178 - 180. Harron, D.A. February 1980 Chemex Lab certificates 684-9264 Dupont of Canada Exploration Johanson E. 1979, 1980 Sketch of SP readings, Geochemistry, Magnetometer, location map 1 inch = 500 feet McConnell, R.G. 1914 Texada Island, B.C. Geological Survey of Canada, Memoir 58, 112 p Mathews, W.H. 1947 Calcareous Deposits of the Georgia cj of Southwestern B.C. - B.C. Department of Mines, Bulletin 40 Muller, J. 1977 Vancouver Island Open File,.Geological Survey of Canada, 3 sheets 1 :250,000 Shearer, J.T. 1981 Geochemical Report on the Long B Claims Texada Island, Privatge Report for Carolin Mines Ltd. 18pp plus maps, May 18, 1981. Filed as assessment. Ware, R. April 1971 Mickle - Samuelson Option PN 158 Falconbridge Nickel Mine Ltd., Private Report 12 pp plus 5 appendices and maps (map 158-70-GP-1 missing). Stevenson, J.S. 1947 Lode Gold Deposits - Southwest British Columbia, B.C. Department of Mines, Bulletin 20 - Part IV 9 41 PP - APPENDIX I LIST OF PERSONNEL AND DATES WORKED

LONG B CLAIMS

FIELD WORK COMPLETED BETWEEN APRIL 15 AND APRIL 27, 1985 - 11 -

APPENDIX I

LIST OF PERSONNEL AND DATES WORKED

Dates Worked on Long B. Name 0 c cupat i on Address Claims, 1985

J.T. Shearer Geologist 3832 St. Thomas April 22, 1985 St., Port April 26, 1985 coqui t 1am, May 1, 1985 B.C., V3B 3 days total 221, 942-5377

R.E. Mickle “Prospector General Del. Powell River

D. Booth Soil General Del. April 23, 24, Sampler Vananda 25 VON 3KO 3 days total

Bob Weir Linecutter General Del. April 23, 24, Soil Vananda 25 , Sampler VON 3KO 3 days total APPENDIX I1

- STATEMENT OF QUALIFICATION

J.T. SHEARER, M.Sc., F.G.A.C.

LONG B CLAIMS

TEXADA ISLAND - 12 -

APPENDIX I1 I, J.T. Shearer of the City of Port Coquitlam in the Province of British Columbia, hereby certify that:

1) I am a graduate of the University of British Columbia (1973) B.Sc. in Honours Geology and University of London, Imperial College (1977) M.Sc., DIC. 2) I am a Fellow of the Geological Association of Canada. 3) I have worked continuously in Mineral Exploration since 1973 for McIntyre Mines Limited, J.C. Stephen Explorations Ltd., and Carolin Mines Ltd. I am presently employed by TRM Engineering Ltd. 4) I do not have any interest in the Long B Claims or the securities of Cariboo Gold Corporation and its affilliated companies, nor do I expect to receive any such interest in the future. 5) I personally worked on the Long B Claims between April 3 and May 3, 1981 and on April 22, 1985. This report is based on interpretation of data collected.

Dated at Vancouver British Columbia

- UT. SHEARER, M.Sc., F.G.A.C. May 8, 1985 APPENDIX I11

STATEMENT OF COSTS LONG B CLAIMS

1985 cj FIELD WORK COMPLETED BETWEEN APRIL 15 TO APRIL 27, - 13 -

APPENDIX I11

STATEMENT OF COSTS

LONG B CLAIMS

WAGES AND BENEFITS

J.T. Shearer Geologist 3 days @ $200 per day $ 600.00 R. Mickle Prospector 6 days @ 132 per day 792.00 D. Booth Sampler 3 days 8 110 per day 330.00 B. Weir Sampler 3 days @ 110 per day 330.00

Total Wages and Benefits = $2,052.00

TRANSPORTATION Burrard Air April 22/85 Vancouver - Texada $ 90.00 4 x 4 Rental $40 per day + $9 gas = $49 per day x 8 days = 392.00 ( 102km per day, 18 liters per day = $9 per day)

Total Transportation = $ 482.00

MEALS AND ACCOMMODATIONS 3 men for 11 man days at $24 per day accommod. $ 275.00 3 men for 11 man days at $15 per day meals 165.00

Total = $ 440.00

GEOCHEMISTRY ACME ANALYTICAL LABS LTD

115 soils for Au 8 4.60 $ 529.00 5 rocks for Au, Ag + Cu 8 17.00 85.00 26 rocks and soils Au, Ag 187.10 Total Analytical $ 801 .10

HAND TRENCHING

5 cubic meters x $60 per m3 in 2 trenches includes rental of drill and explosives $ 300.00 - 14 -

APPENDIX I11 STATEMENT OF COSTS LONG B CLAIMS

ROAD REPAIRS One day’s wages included above, ( SP Survey no claim, data not available) ---- DRAFTING AND REPRODUCTION

12 hours drafting at $1 5 per hour $ 180.00 Reproduction 35.00 Total $ 215.00 REPORT PREPARATION AND TYPING t, 9 Hours word processing @ $25 per hour $ 225.00

GRAND TOTAL: $4, 515.10

SUBDIVISON OF WORK PHYSICAL Trenching and road repairs:

Trenching 5 cubic meters @ $60 per m3 = $ 300.00 2 days labour trenching - 264.00 1 day labour, road repairs - 132.00 3 man days meals and accommodations =

$ 816.00

GEOCHEMICAL $3,699.10

GRAND TOTAL: $4,515.10 APPENDIX IV

ANALYTICAL PROCEDURE ACME ANALYTICAL LABORATORIES LTD. 852 E Hastings St. Vancouver, B.C. V6A 1R6 Dean Toye, Chief Geochemist - 15 -

r ACME ANALYTICAL LABORATORIES LTD. I Assaying 43 Trace Analysis 852 E. Hastings St.. Vancouver, B.C. V6A IA6 Telephone : 253 - 3158 GEOCHEMICAL LABORATORY METHODOLOGY - 1985 --+Sample Preparation oah 1. Soil samples are dried at 6OoC and sieved to -80 mesh. 8 2. Rock samples are pulverized to -100 mesh. Geochemical Analysis (AA and ICP) 0.5 gram samples are digested in hot dilute aqua regia in a boiling water bath t and diluted to 10 ml with demineralized water. Extracted metals are determined by : \I$ LJ A. Atomic Absorption (AA) Q Ag*, Bi*, Cd*, Co, Cu, Fey Ga, In, Mn, Mo, Ni, Pb, Sb*, T1, V, Zn b (* denotes with background correction. ) \ w6 B. Inductively Coupled Argon Plasma (ICP) Ag, Al, As, Au, B, Ba, Bi, Cay Cd, Co, Cu, Cry Fey K, La, Mg, Mn, Mo, Nay 1 Ni, P, Pb, Sb, Sr, Thy Ti, U, V, W, Zn. k Geochemical Analysis for Au* 10.0 gram samples that have been ignited overnite at 6OO0C are digested with 30 mls hot dilute aqua regia, and 75 mls of clear solution obtained is extracted 5 I with mls Methyl Isobutyl Ketone. Au is determined-in the MIBK extract by Atomic Absorption using background correction (Detection Limit = 1 ppb). '~~~~ph;{e4 41 " Geochemical.Ana1ysis for Au**, Pd, Pt, Rh 10.0 - 30.0 gram samples are subjected to Fire Assay preconcentration techniques to produce silver beads. The silver beads are dissolved and Au, Pd, Pt, and Rh are determined in the solution by graphite furnace Atomic Absorption. Detections - Au=l ppb; Pd, Pt, Rh=5 ppb Geochemical Analysis for As 0.5 gram samples are digested with hot dilute aqua regia and diluted to 10 ml. As is determined in the solution by Graphite Furnace Atomic Absorption (AA) or by Inductively Coupled Argon Plasma (ICP). Geochemical Analysis for Barium 0.25 gram samples are digested with hot NaOH and EDTA solution, and diluted to 20 ml. Ba is determined in the solution by ICP. Geochemical Analysis for Tungsten 0.25 gram samples are digested with hot NaOH and EDTA solution, and diluted to 20 ml. W in the solution determined by ICP with a detection of 1 ppm. Geochemical Analysis for Selenium I 0.5 gram samples are digested with hot dilute aqua regia and dilute to 10 ml with H20. Se is determined with NaBH3 with Flameless AA. Detection 0.1 ppm. c c

55 .I I o\ I \c) d I

5- APPENDIX V

GEOCHEMICAL ASSAY CERTIFICATE LONG B CLAIMS ds ACME ANALYTICAL LABORATORIES LTD. 852 E. Hastings St., Vancouver, B.C. V6A 1R6 Dean Toye, Chief Geochemist - 17 -

ACME ANALYTICAL LABORCITORIES LTD. IHS~RECEIVEDI llp~2s i9es 852 E-HCISTINGS ST-VANCOUVER B.C. V6A lR6 PHONE 253-3158 TELEX 04-53124 DATE REWRT WILED:

FISSAV CERTIFICCSTE

. SqtrPLE TYPE: ROCK CHIPS Aut! AND A681 BY FIRE ASSAY ASSCIYER:q/WEfiN TOYE OR TOM b;CWNDRY. CERTIFIED B.C. ASSAYER

CARIB00 GOLD CORPORATION FLIE # 85-0454 PAGE 1

SAMPLE# Cu AgSt AuSS % ot/t oz/t

80976A 2.515 2.08 -136 80977A 21.51 7.18 .362 809786 .02 .O1 .001 8097% .01 001 .001 80980A .01 .O1 .001

STD R-1 .89 - - - 18 - . GCME ANALYTICOL LOBORaTORIES LTD- DATE RECEIVED APR 29 1985 852 E. HASTINGS, VANCOUVER B.C. Pli: (604)253-3156 COlilPUTER LINE: 251-101 1 DATE REPORTS WILED

GEOCHEMICC1L 6ASSFIY CERTXFXCCITE lil 61f5 Pu SAWLE TYPE : SOIL - DRIED CIT 40 DE6 C. , -20 HEW. WLVERILO. rz I"ii .I6NITED, HOT AW E6IA LEACHED, HIM EXTRKTIW, M MYSIS.

If.\ \'/:.I:*' TOYE OR TOM SAUNDRY. CERTIFIED B.C. ASSAYEH , I\ CORIEOO GOLD FILE# 89-0463 PAGE# 1

SAMPLE AU* PFJb

1'9 11 7 7 21

10 65 14 12 19

175 60 40 0 46 17

15ow 4s 18 15C)W 5s 31 15OW 6s 35 15ow 7s 6 150W 8s 21

610 8S 1.L 2 17 39

1 oow 3s 30 1 c:)c:iW 4s 75 1oow 56 54 1 Oc3W 6s 25s lO0W 7s 60

30 39 34s 7s -.> 4

67 17 - 19 -

CARIB00 GOLD FILE# 85-0463 FAGE# 2

SR MFI- E Aut OPb

37 36 27 29 26 sow 9s 30 5ow 1C)S 21 0+200 os 4s (:)+2(:)0 1 s 32 0+200 2s 13

19 €3 170 55 4s

65 14 35 20 9

i:)+150 1sc\ 22 0+15o 2s 24 (:)+Is(:)3s 22 0+150 4s 34 (:).e 1s:) 5s 19

0+150 6s 17 (:)+150 7s 17 0+150 8s 24 150 9s 18 0+150 10s S3

50 42 3s 44 17

26 14 - 20 -

CARIEOO GOLD FILE# 85-0463 FAGE# 3

SAMPI-. E AU* QPb

1s 2300 550 20 37

15 18 2 (3 6S 16

23 14 22 13 65

70 32 6 13 10

BM-547 4 BM-548 S EM-549 7 BM -S5 (3 4 BM-551 13

BM-552 5 EM-555 7 BPI--554 9 EM-555 9 - 21 - ACME ANALYTICAL LABORATORIES LTD. D4TE RECEIVED AFf 15 i985 d'.? d'.? E. HASTINGS. VRNCOLJVER F.C. PH: (604)253-3158 COMPIJTER LINE:251-1011 DQTE REPORTS MAILED __+kJ ______ipj- GEOCHEMXCCAI ASSAY CERTIFICCITE

A .50 6H SAflPLE IS DI6ESTED WITH 3 HLS OF 3:1:3 HCltHNQ3:H20 AT 90 DE6. C. FOR 1 HOUR. THE SAWLE IS DILUTED TO 10 HLS WITH HATER. ELEHENTS ANALYSED BY AA : Aa kt SAflFCE TYPE : FI-SO[IS P?-SOILS-PULVERIZED P3-ROCKS Aut - 10 GH,lGNITED, HOT AWA RE6IA LEACHED, MlBK EXTRACTION, M ANALYSIS.

!-!'::I,, ., ,.:;vi. . 1 !!:>:' Tg!d/-FDEAN 'l-(]Yti; [If-i T(31'1 SfiUNDRY. CURT IF IED D. C. f?!;CiAYli:F? _. _.

R.E. MICKLE FILE# E35--C!TE36'2 FAGE# 1

EM-4E35 BM - 4 13 6 bM-487 Eri- 4138 ~~-48s

.I 17 .-3 65 7 . 4 10 Oh .-3 LL .4 14

FM-F 18 .7 18

I.,

, 11tr \ ',(I F:. E. MICKLE F I L.E # t3I5-031?2 ,J, ii 0 PAGE# 2 R.E. MICKLE PAGE# 3

nLI t cj opb 44a - 24 - ACME ANALYTICAL LABORATORIES LTD. Camlin Mines Ltd., Assaying & Trace Analysis J&xo20- 475 Howe Street, 852 E Hastings St., Vancouver, 0.C. V6A 1R6 Vancouver, R.C. phone:253 - 3158 81-P267 Attn.: Dr. P.W. Richardson File No. Soil IC Rock Gland. SPeof Smples - ______Disposition ______-

.1 17 14 36 4 .070 .065 .2 23 11 34 5 .I50 .065 .3 ' 22 12 53 3 .110 .925 .1 , 26 13 34 7 .065 .lo0 .1 11 25 52 1 .13q .915 .1 13 15 36 2 .085 .055 *l 14 12 35 1 1 .08@ .060 .1 13 13 25 1 .510 .win .4 14 13 28 1+1.800 .040 1 .075 .OS0 1 .150 .Oln 1 .230 .@I5 7 11 38 1 .e60 .om 7 12 42 1 .010 .loo 2 .025 .110 1 .030 .250 .2 16 : 17 ' 252- 1 .025 .140

1 .5 15 10 37 2 .030 .050 1 .on5 .@lo 1 -015 ,050 - __ 1 a150 4 .lo0

. __ 29 . __ I 1 .01" ,070 1 .005 .w5 1 .315 .075 -- -.

37801 __ . R .l _. 7 4 .190 .015 . --37802 - __ -R_ .8 -1 7 3 .300 .OlO .-37803 -R 4 9 1 .050 .010 -37804 R *27:0 9 10 .810 .010 -78 -035 37805 . R +16.0 18 g 5d.800 .O20 ,52 .c)3'J. 37806 R +4.0 '1 8+1.800 .010 i,is -076 40 April 7, 19811 All reports are the confidencial property of clients DATE SAMPLES RECEIVED______All results are in PPM. a I k;. , /('. April 14,1951 DATE REPORTS MAILED______DIG EST10 N:...... ".... DETERMINATION:......

DEAN TOYE, B.SC. CMIEV CMLMIST CERTWlED B.C. ASSAYER - 25 - ACME ANALYTICAL LABORATORIES LTD. To: Carolin Mines Ltd., Assaying 81 Trace Analysis 1020 - 475 Howe St., 852 E. Hastings St., Vancouver, B.C. V6A 1R6 Vancouver, B.C. phone:253 - 3158 V6C 2B3 8 1- 03 30 Attn.: Dr.P.W.Rlchardson & Mr,J.T.Shearer File NO. ______Sol 1s Speof Samples ______GEOCHEMICAL ASSAY CERTIFICATE . . Dispositmn - __ Project : LONG B Clalms (TEXADA) ______

1

0

~______~ ~~ All reports are the confidencial property of clients All results are in PPM. 0 DIGESTION:...... DETERMINATION:...... "-...-..-.."-..-"..-...-....

DEAN TOYE. B.SC. cniw cncwsi CERllClED E.C. ISSAVER - 26 - ACME ANALYTICAL LABORATORIES LTD. Assaying & Trace Analysis TO: Carolln Mlnes Ltd. 852 E. Hastings St., Vancouver. B.C. V6A lR6 phone:253 - 3158

File No. ______81-0330 Qpe of Samples ______soi 1 GEOCHEMICAL ASSAY CERTIFICATE Disposition ______-

2

i:

All reports are the confidencial property of clients All results are in PPM. (L DIGEST10 N:,...... ,.., ...... ,.-...... ,.,. DETERMINATION!.....,,..,.,,.,,......

DEAN TOYE. 8.6~. cntw cnmisT CERTIFIED B.C. A6SAVER - 27 - ACME ANALYTICAL LABORATORIES LTD. Assaying & Trace Analysis To : Carol In Mines Ltd. 852 E. Hastings St., Vancouver, B.C. V6A 1R6 phone:253 - 3158

J File No. ______81 -0330

Spe of Samples ______Soil & Rod GEOCHEMICAL ASSAY CERTIFICATE Disposition - ______-

SAMPLE No. 3 Ag As Au

c3

All reports are the confidencial property of clients All results are in PPM. 0 DIGESTION:...... OETERMINATION: ......

DEAN TOYE, 8.s~. cniEr CHEMIST CERTIFIED 0.C. ASSAVER xiii - 28 -

ACME ANALYTICAL LABORATORIES LTD. 253 E. HASTINGS ST. VANCOUVER BC V6A-lR6 (604) 253-3158 TELEX 04- 53 124

DI GESTI ON: 1 GRAM AQUA REGIA FINAL VOLUME: 100 ML DETERMI NATION: DI RECT READING I CP EM1 SSI ON SPECTROMETER RESULTS: IN PERCENT *W IS SUBJECT TO ZN INTERFERENCES

*HO/ 378 04 CAROLIN MINES FILE# 8 1-0267 PAGE : 1 EG C

BURN # 1 AY16 14: 05 20APR8 1 IS 136 1 MO cu PB ZN AG NI co MN FE AS *003,2 ~-1~-~0-).0001 00201 00025 00061 00100 00249 9.949 o001Q U IS TH IS CD SB BI v CA P -.a02 00008 -0000 -4516 00013 .0018 .0013 -0150 1.624 -0988 LA IN MG BA TI B AL IS IS W 00003 00018 1.094 .0049 .3335 -.a05 3.559 -.a03 .0007 .0007 *0/37805 EG C c c GEOCHEMlCAL DATA SHEET - ROCK GEOCHEM SAMPLING EXPLORAflUV DEPARTMENT JVTS 91 F./~w

SAMPLE ADDITIONAL LOCATION MINERAL f2 ATlON NUMBER n REMARKS & & & 7 4 3. I 1981 3 7802 360 7 3 50

-I

5 5 6 2!* % cu 136 ?.Ob 2.56

362 7. do 9 774 -IS 180 A/ two s 809 784 0.OOl 0.61

0.01 809794 -6. 61 - 0.01 0.61 t APPENDIX VI 0 BRITISH COLUMBIA DEPARTMENT OF MINES

G. FORMS

LONG B CLAIMS MAKE OATH AND SAY.- I COMMENCED LOCATING THE MINERAL CLAl

AND COMPLETED THE LOCATION

ON THE.aDAY OF r A

IDENTIFICATION POSTIS1 NOT PLACED WERE

CHECK ’V . APPLICABLE SQUARE ESS POST FOR THE LE

.C-cCI.LL. 01.‘ Kecora 01 Mineral Llaim FORM G 17Sl (5) - 31 - RECORD NO.

..' \r%G RECEIPT NO.ZbmE RECORDED .8C. THIS 1 DAYOF . 19- 84

DO NOT WRITE IN Ncnrpiia#, SHADED AREAS .,-",.',..c ICCO~OC~" "*C*C 01"1110* 'b- /

MAKE OATH AND SAY:- I COMMENCED LOCATING THE MINERAL CLAln "Od PILI ON THEADAY2 '4 OF P . 19B.T a7111 I*O*C.TC. I 0". .I 0 3 1 c/ ON THE-DAY OF Apt / J,&AT d*J0'pd ,1111 I*O#C.TE a u OI c 1 I

UMTLENGTHS' sod* AND 5- , UNlTLEkTHS ;r . AN0 .-r.c-.' .01.CCI)ONO I*U...CI.' Fa$ ! T'"=cv80N' i 5'. METAL TAGS NO 3-8.9-. 3 -3 . WHICH HAS BfEN SECilRELY FASTEkED TO THE POSTS As

ZL\TIFICATION POST#S#NOT PLACED WERE $-E is 3-E is

THE LEGAL CORNER POST ______1-- TZr( "v'" APPLICABLE %

0 __._. -. =r--,NG AND DISTANCE TO TRUE POSITION OF LEGAL CORNER POSl FROM THE L\ITNESS POST t 01 = r-- '"5 Ah0 DISTANCE FROM IDENTIFICATION POST TO WITNESS 20ST I --: -&.E COMPLIED WITH ALL THE TERMS OF THE MINERAL ACT AND REGULATIONS PERTllhlNG TO THE STAKING Z' '.' ',.fRAL CLAIMS AND HAVE ATTACHED A PLAhl. ACCEPTABLE TO THE hllNIPJG PECORCEH. OF THE LOCATION

.._.I...... :1 Record of Mineral Claim FORM G 1750 (5) - 32 - RECORD NO

'.TINING RECEIPT NO 2WLRECOA e c r~is.2~0~~o~--hhy .

DO NOT WRITE IN lQlndlw SHADED AREAS m+w*cz oivistom I ,,- "1I ervmaq AGENT FOR - *I Affidavit *.it Na-L for .OOIC.S ~OOmcS. Mineral Claim VALID SUBSISTING F.M.C. NO. 266 532 VALID SUBSISTING F.M.C. NO. _- MAKE OATH AND SAY:- I COMMENCED LOCATING THE MINERAL CLA 4

€TED THE LOCATION ..,mc ,mOIC.Tt .I 0. c m I ..._I ... : . .. .; .T,"C. I*OtC..C ." om c " *

IDENTIFICATION POSTISI NOT PLACED WERE

7.

CHECK "4" 4PPLICABLE SKARE

BEARING AND DISTAKE FROM IDENTIFICATION WST TO WITNESS POST

SWORN AND SUBSCRIBED TO AT

t9-BEFOFE M€ APPENDIX VI1

LIST OF SUPPLIERS

TEXADA ISLAND - 33 -

APPENDIX VI1 LIST OF SUPPLIERS TEXADA ISLAND

Burrard Air - Texada Island Service, 4480 Cowley Crescent, Richmond, B.C. $45 one way Sc3he.dule: Mon.-Fri. 6:00AM, lO:OOAM, 5:45PM cs Sat.-Sun. 3:OOPM (278-71 78) Joe Christenson (486-7533) Bob Duker Duker Road, Vananda Ed Johanson (486-7528) Bob Mickle Dave Murphy Rhyolite Resources Ltd., Jon Steward Camp at Millsite (486-741 1 ) Jon Stewart, home, Powell River (487-9055) Bob Weir at Millsite, 977 $90 per hour with blade and ripper APPENDIX VI11

ESTIMATE OF COSTS FOR FUTURE EXPLORATION

u .. -- - 34 -

APPENDIX VI11 Estimate of Costs For Future Exploration Work Long B Claims PHASE I Geological mapping and prospecting

Geologist 16 days 0$135 per day = $ 2,160 Helper-Prospector 16 days @$go per day = 1,440 $ 3,600

Rock Sampling 50 samples Q10.50 per sample 525

Soil Sampling 100 soil samples @ 7.25 6$ per sample 725 EM 16 VLF Survey 3 days surveying 675 MAP Preparation 1 :10,000 photo enlargement plus drafting 200 Field Supplies 200 Consulting Geologist 4 field days 800 (J. Shearer) 3 office days 600 Transportation 4 x 4 truck 16 field days 062.50 1,000 Per day Accommodation (meals and lodging)

39 field man days 0 $45 per day 1,755 Airfare (Vancouver - Texada) 360 Initially the intense soil anomaly on Line 50E could be opened by a small hand trench of 15 cubic meters 0$60 per cubicmeters - 900

Total Phase I = $1 1,640 - 35 -

PHASE I1 Approximate bulldozer trenching (accurate estimation of backhoe trenching requires actual walking of proposed sites with operator and forestry officers.) Using 9771; with side dumping bucket and ripper and equipped with CAT tracks C$90 per hour includes operator, fuels, etc.)

(a) trail building 2Km 6 days x 10 hours = 60 hours 8 $90 per hour - 5,400 (b) trenching 40 hours $90 per hour - 3,600 (c) Mobilization-demob (Lowbed from Powell River) - 1,000

Total Phase I1 $10,000 Contingency - 1096 2,164 c3 Grand Total $23,804 Approximately $24,000

lly submitted dC. Shearer, M.Sc., F.G.A.C.