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i GEOLOGICAL AND GEOCHEMICAL REPORT

!.

SYRUP 1 AND 2 M1NEF;LAL (LAIMS

NICOLA AND VERNON MIXING 3ISTRICTS

NTS 823/13

Lat.49" 57' N. Long. 119" 47' W

BY

W. A. Howell, B.Sc. consulting geologist 15294 96 A Avenue

Surrey B.C. V3R-8P5

and

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up4 26 Guinet Management Corp.

305 - 250 W. &stings St. Vancouver B . C .

V6C-lEl

on behalf of d b 4 z U M

536-999 Canada Place "E a, o w & d w

% VERDSTONE GOLD COW.

Vancouver, B . C . , 'r

November 25, 1339 O m w m C P f

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TABLE OF CONTENTS i

SUMMARY

INTRODucrIoN Location, Access, Topography Property definition TABLE 1 (List of claims) History Current work program

MINEWKSZATION AND m S T R Y Regional aspects S F U P property

mcLlus1oNs

R E C D ~ A T I O N S

BIBLJ(XSAF"Y

APPENDIX I Statement of Qualifications I1 Statement of Costs I11 Description of Rock Samples IV Certificates of AMlySeS

LIST OF FI(XIRES

FIGURE 1 Location Map FIGURE 2 Claim Map FIGURE 3 Compilation Map FI- 4 Geology and Geochemistry

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Province of British Columbia RECEIPT 470732 J

THE SUM OF I$ --- --- _ _ - I__I_ I___ ̂ _--- - ------I - - DOLLARS

ON ACCOUNT OF

ON ,,\ <.*.\ : 19

WHITE CdSTOMER PINK MINISTRY FILE CANARY RETAIN IN BOOK FOR AUDIT

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SUMMARY

The Syrup property is located 22km west of t h e city of Keloma, in the

Vernon mining district. The current work program consisted of prospecting, soil order to understand the distribution of rock types. Mapping and sampling control was provided by an extensive road network, servicing the logging industry, and maps available from the B.C. Forest Service. A total of 383 soil samples, 3 silt samples and 4 4 rock samples were collected and subjected to multi-element geochemical analysis. a total of 20,600 metres of sample line were flagged and sampled and 1400 metres of baseline flagged and stationed every 50 metres.

sampling and geological mapping in

Sampling is widely spaced and of J reconnaissance nature. Although precious metal values so far detected are generally low, some areas warrant further exploration.

The poperty is underlain by Pennsylvanian to Permian volcanics and sed-

iments of the Thompson assemblage (formerly Cache Creek Group) and/or the Upper Triassic Nicola Group and granitoid intrusive rocks believed to be of Upper Jurassic t o Cretaceous age. The Thompson/Nicola rocks strike generally northwest to southeast and dip moderately to the southwest. They have also been intruded by the Old Dave ultra basic intrusions which are pre-Late Triassic in age. Brenda Mine, a large, operating copper-molyWenum mine, is located about 20 km to the south in felsic intrusive rocks believed to be of Late Jurassic age.

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INTRODUCTION

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Location, Access, Topography

The property is located on the west s i d e of t h e Okanagan valley about 22 ( f igu re 1) and j u s t east of t h e height of km west of t h e c i ty of Kelowna B.C.

land between t h e Okanaqan Valley and t h e Nicola Valley t o t h e north west. Access is by paved road from Westbank or Vernon along the west side of

Okanagan Lake, then by t h e Bear Lake Main and t h e Horseshoe Lake Main, grave1 logging roads t o t h e property. Access w i t h i n t h e property is provided by a network of spur roads and haul roads over much of the claim area. The

property is centred on approximately latitude 49O 57" and longitude 119O 47'W on NTS map area 82 E/13. Several small l a k e s are located nearby, most of which

provide water t o local i r r i g a t i o n districts i n both the Nicola and t h e

Okanagan Valleys. They also provide r ec rea t iona l camping an6 f i sh ing areas f o r t he general publ ic . Topography on the claims is gentle t o moderate wi th

e leva t ions averaging approximately 1350 m (4500 f t ) . About 25% of the

property has and vegetat ion comprises l o c a l l y mature s tands of spruce, balsam and pine with immature second growth i n t h e previously logged areas.

k e n logged i n the past

Property Def in i t ion

The Syrup Property cons i s t s of two ( 2 ) metric grid s y s t e m minerai claims

of B r i t i s h Columbia. t o t a l l i n g 40 units located i n t h e Vernon Mining District (Table 1, Figure 2).

TzLBLEd

C l a i m Name Units Record No. Record Date

syrup 1 20 3053 November 20 1988 S F U P 2 20 3054 November 21 1988

me claims are c u r r e n t l y owned by Verdstone Gold Corp. sub jec t t o a 2% net smelter roya l ty payable t o t h e vendors. The author h a s examined t h e claims i n t h e f i e l d and is of t h e opinion t h a t they were staked i n accordance with regulat ions.

VERDST'ONE GOLD CORI?

SYRUP CLAIMS British Cdumbio Vernon Mining Division

LOCATION MAP Fig. 1

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SYRUP 2 3054

VERDSTONE GOLD CORP

SYRUP CLAIMS . Vernon Mining Division British Cdumbia

PROPERTY MAP ? 20~m Fig 2 1000

V A Howell 1 NTS 82Ell3[ Now 1989

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History The area west of Okanagan lake has received the attention of prospectors

since at least the turn of the century arid prokably pr ior Lo that time ?:so.

A.J.Schmidt, has swmrized the history of the area very we1.I. Huch of the following is taken from his 1989 report.

The Blue Hawk and White Elephant gold-silver prospects were located and tons /day), explored in the 1920's. The active Brenda Mine (producing 20,000

developed in 1965/68,

It is reputed to be the lowest grade porphyry copper-molybdenm mine in the world (present reserve grade 0.15% 0-1, 0.03% Mo). The entire district was vigorously explored f o r similar deposits during 1960-1975, during which time several prospects were located. The same area was again explored for its uranium potential during a shorter flurry of activity, about 1970-78.

has been in almost constant prduction since 1969.

The discovery, by Huntington Resources, on t he Brett p o p e r t y about 33 kin to the north-northeast of the SYRUP claims, of high grade gold mineralization in 1988, has Zed to the present exploration activity in t he

area.The recent activity has seen almost the entire west side of Okanagan Lake completely covered by mineral claims. Within the area, gold mineralization has k e n found in 1988 on the FLAP claims 7 kms to the north; in 1980 on the NCGAN (now Jubilation) claims 4 kms to the east; and on the ZUMAR claims in 1979 from which a 60 ton shipment, grading 0.139 opt Au and 1.23 opt Ag., was made in 1980 to the Trail Smelter.

The Location of the various mines and prospects is presented on Figure 3

which has been adapted from A.J . Schmidt's 1989 report to Verdstone Gold Corp.

Chevron Minerals completed a prospecting/geological & geochemical program on the FLIP claim during 1988, and reported the presence of c o p p r values t o 2000 ppm and the presence of gold -lues to The claim is situated 2%m to the north of the SYRUP claims.

200 ppb.

Kerr Addison Mines completed a geological and geochemical program during 1988 on the LAMB claims immediately to the east of the JACi 4 and the FLIP claims. They reported only erratic mineralization from small quartz veins and disappointing results from garnet diopside skarn development.

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Current Work Program

The field phase of the current work progrcun was undertaken on September 10, 1989 and completed on October 7, 1989. Not a l l the time during this period was spent on the SYRUP claims. Two prospectors, P. Newman and J. Boutwell prospected and conducted reconnaissance style mapping and sampling. Several lines across the claims were sampled and prospected. The network of logging roads afforded a good means of mapping and sampling control and often provide a source of outcropping bedrock otherwise not always common. W.A. Howell, geologist, reviewed the prospecting results and conducted preliminary mapping and rock &impling. During the field phase of the program, Victor Guinet was present and contributed to prospecting and geological napping for two days on the SYRUP claims. G. Medford, PhP. was a lso present an2 made a similar contribution f o r one day on the SYRUP claims.

Regional Aspects

The SYRUP property is located within a north westerly trending belt of lower grade Carboniferous t o Triassic metasedimentary an6 metavolcanic rocks of island arc and oceanic derivation. Metamorphism has proceeded to greenschist facies. Regionally, the rocks are intruded by grsnitoid plutonic: rocks of the middle Jurassic Nelson suite arid the JUrd-CrekaCeOUS Valhalla suite. Ultramafic rocks of undeterminable age or genesis OCCUL as small msses throiq!toi~t t h e Thompson-Okanagan-Shuswap area, Only the n:d Dave Intrusions (northwest of pre-Late Triassic in age and suspected to be of intrusive origin. Tertiary (Eocene) volcanic rocks unconformably overlay all the older formations, and are generally unmetamorphosed.

the syrup claims) are knowri to be

The Okanagan Valley is believed to mark the location of a major crustal separating the lower grade metamorphic assemblages on the west break o r fault

.from higher grade metamorphic rocks to the east.

U W r N i W Gp; redimontr Lornr JUR.

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Goology of1.r Church (1980), Morrlaon (1980) ond Tomeleman-Kluif [ 19891

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Fau1tir.g is ubiguitolis throughout the region. Drainage ,wtteuns m c ? air photo linear features commonly reflect underlying faults OK fault controlled structures. This is particularly evident in the area of, an2 surround.iiicJ, the

SYRUP claims.

syrup Property

Reconnaissance mapping has shown volcanic rocks and sediments of the Thompson assemblage (formerly Cache Creek Group) and possibly Nicola Group to underlay the northeast portion of the SYRU? No.1 claim (Figure 4 ) . The southwestern portion of the SYRUP No.1 and almost all of the SYRUP N0.2 are underlain by uniform, massively textured, hornblende / biotite quartz-diorite.

The sediments are observed in faulted contact with the intrusive rocks

along the Rear Main in the vicinity of Km 30. The road cut ex?oses siltstones

and shaley members of ? Nicola sediments with the quartz-diorite along a faulted surface trending 130°/80%.

Reconnaissance mapping has shown volcanic rock and sediments of the Thompson assemblage and/or Nicola Group to lay in a northwesterly t o

mutheasterly of the SYRUP claims. The southwestern portion of the claims is underlain by intrusive rocks of the Jura-Cretaceous Okanagan htholith (Figure 4 . ) In the vicinity of the SYRUP

claims, the intrusive rocks are very homogeneous, medium tu coarse-grained, biotite-hornblende quartz diorite. They weather very massive and blocky. The Intrusives are relatively unfractured and show little variation in alteration except for diagenetic effects. The volcanics and sediments are poorly exposed arid the sediments, particularly, weather recessively. me volcanics commonly are metamorphosed t o greenschist facies. They are well-fractured and biocky in nature, foliated in a NW to SE trend and are occasionally fractured with quartz veins. Sulphide mineralization is variably present, usually in quartz veins, or as an accessory or minor constituent. Within the quartz veins, ?site content is yenerally greater than pyrrhotite which is greater than chalcopyrite. Within the black shales, pyrrhotite is ubiquitous along bedding planes and parting planes, and is by far the dominant sulphide mineral. "he

trend across the northeastern portion

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pyrrhotite, in the black shale environment, is believed to be syngenetic in origin .

The intrusive rucks have !xen observed along t h e &dr ??din (logging road) in fault contact with the older volcanics a d sediments. The primary contact is along a faulted surface treiiding l?O"/aC%. This direction 5as been o f f s e t left laterally in a series of step-like patterns along 03Oo/9O0.

The black shales occasionally have limy and silty interbeds. These offer potential as marker horizons for future mapping. Tho shales outcropping some

near the eastern side of the property do not appear to have endured the same degree of metamorphism as sediments outcropping regionally farther north and west. The former may be members of the Upper Triassic - Lower Jurassic Nicola group, while the latter, members of the earlier Carboniferous assemblages.

Major faults are postulated in a northwesterly t rend and appear to be o f f s e t in a secondary northeasterly direction. This pzttern has been observe? in the intrusive - sediment contact mentioned above, along t h e Bear Main, and

is reflected in the regional drainage patterns, an example of which is t h e

"zig-zag" course of Powers Creek as it traverses the SYR!JP claim;. Numerous air photo linear features are undoubtedly fault related, several of them are continuous for several kilometres without visible offset, rlesgite the relative abundance of the northeasterly trending linear fedt:ires. Rejuvenation or

repeated episodes of faulting along pre-existing sI.ructurcs mxy allow t h e

presence of such unbroken lineations. In any case, t h e geclogy of both the property and the region will be complicated to some deyree by fault controlled structures.

MINERALIZATION AND GEOCHEMISTRY

Regional Aspects

Exploration f o r gold and other metals has occurred in cyclical fashion within the Okanagan area, as it has done throughout Britisll Columbia, since the arrival of the first prospectors and settlers prior to t he turn of the last century. In the 192O's, work vas done on the Blue Hawk and White Elephant gold-silver prospects. Some minor placer gold production frcjm Trepanier Creek

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and lode copper exploration at the head of that drainage through t o the i940'~ led porphyry copper explorationists to develop the operating Brenda Mine which went into production in 1969. In more recent years the discovery of gold on the Brett Property by Huntington Resources, ahoi.it 3; km northeast of the SYRUP claims has spurred renewed interest in the regiort.

Adjacent or nearby the SYRUP claims, gold exploration work has been carried out by several operators. Chevron Hinerals has rc-ported anomalous gold values to 200 ppb, and copper values to 2000 Spm on the FLIP claims during 1388. Kerr Addison also performed an exploration program on their LAMB Claims in 1988. They apparently had a gold skarn model in mind ant! cited numerou Eeatures to substantiate the idea. mey reported very low values for gold from skarns and sporadic values from small quartz veins. To the north, on the regional strike direction of foliation and bedding from the SYRW claims, gold was discovered on the FLAP claim durinq 1988. The gold occurs in narrow quartz veins along northwesterly trending 2yritic stringer zones (Schmidt, 19891. Schmidt also has drawn a comparison between t h e FLA? claim and the Jubilation gold prospect (NOGAN), where low concentrations of gold occur in pyrite bearing narrow quartz veinlets within brecciated and altered limy argillite.

Forty-four rock samples, three silt samples arid 3 i L e e hundred eighty- three soil samples weze collected from the SYRUP property.

Samples were analyzed by T.C.?. techniques for 10 ciements including: Mo; Cu; Pb; Zn; Ag; Ni; Co; As; Sb; and Ba. Gold was determined by acic! leach followed by atomic adsorption analysis using a 10 gram sample. All samples were analyzed by Acme Analytical Laboratories Ltd. 852 E. Hastings St. Vancouver B.C. V6A 1R6.

The data is presented in the appendix to this re2ort. Au, Ag, and As values are also illustrated on Figure 4 .

Molvbdenum - Molybdenite mineralization was not observed in any of the samples collected. Geochemical values ranged from a tackground of 1 to 5

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pprn to a high of 325 ppm (sample JS-5-R) from an area of very rusty argillaceous metasediments near the contact with intrusive rocks. the

same area gave a result of 30 ppm for an adjacent sain2,le (JS-5-R). A

sample from greenstone collected near the intrusive contact in t5e

southeast corner of Syrup 1 (89-BS-32R), produced a value of 6 3 ppm. Within soils, all values were below l0ppm.

Comer - Copper values in soils ranged from a low of 6 pprn to a high of 152 ppm. The high value and the adjacent sample, 109 ppm, are located in the southeastern part of syrup 1 within the area underlain by sediments (samples 44+50S , 16t00E and 16t50E). Copper values within rocks were more variable, ranging from a low of 7

ppm to a high of 535 pprn from an area of hornfelsec! sediments with minor clay-silica alteration on fractures (Sample JS-12-R).

- Lead - Lead values in soils ranged from 2 y?m to 75 ppm. Nine samples were 15 ppm or greater. Within rock samples, the range vas 3 pgm to 41 ppm. vith seven samples 15 ppm or greater.

- Zinc - Zinc values from soils were highly variable, as is common fo r that

metal, ranging from a low of 22 ppm to a high of 4 4 8 ppm. Values, withir. rocks, ranged from 4 ppm to 762 ppm. The higher values within rocks occur near the northern edge of the property froin an outcropping of limy rusty black shale alongside a road connecting the Horseshoe Main vith the Lambly Main along the eastern side of the property.

Silver - Silver values are all low, ranging from .I to 1.1 22x1 within soil and from .1 to 1.5 within rock samples. only marginally anomalous for soils generally aqd within normai background ranges for rock samples. Results f o r silver are presented on Figure 4 .

The upper end of the range is

Nickel - Nickel values from soil samples range from 6 =pm to 138 ppm. The high value was collected adjacent to samples which yielded anomalous values for copper. The coincidence of the values may be significant geologically in light of the anomalous copper associated with mafic and ultramafic rocks (gabbro and peridotite) reported from the FLIP c l a i m

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about 3km t o the north.

~ t i ~ ~ h 3 ~ ~ - Co1sl.t values in soils and rocks ranged from 4 psm t o 92 gpm and a r e

not considered s i g n i f i c a n t .

Arseriic - Arseriic values i n s o i l ranged Erom 2 ppm t o 25 ppm with 20 samples

over 10 ppm. The range is Considered r e s t r j c t e d , the cause may ?x simply due t o a l a c k of a rsen ic , o r other fac tors , ilnl.;novn a t t h i s time.

Arsenic values from' r o c k samples ranged froin 2 ppn t o 1139 pgm. S i x

samples were Srea te r than 20 ppm. Sample 83-RS-38 yielded a resul t of I149 ppm, t he sample was co l l ec t ed from an angular, rusty quartz r i c h

borilder apparent ly ripped lip during Lhe construct i im of a local sk id road. The boulder is i n the v i c i n i t y of t he intrusive-sediment contac t .

A value of 35 ppb Au was re turned from the sane sample. No other analyses a r e considered anomalous for t h i s sample. R e s u l t s for arsenic are presented on Figure 4 .

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Aritimonv -- Antimony values ranged from 2 ppn! t o 4 pprn. Antimony is c l e a r l y not

a s i g n j f icant component i n any of the samples collected.

Barium - Barium undergoes only a p r t i a l leach u s i n g tt-,t-. i?itjt.-;tior. Lcchniques

employed. The results i n f o r m other than sulphate (ie. 'Daritic f e ldspa r ) , to a grea te r 6ecjree thmn the more common r e z u l t s ranged from 3 ppm t o s o i l s responzci! with results ranging from 3 ppm t o 347 ppm. b r i m is indeterminate a t t h i s time.

tend t o r e f l e c t b r i m bouiid

barium sulphate (barite). Rock sample 342 ppm (sample 89-BS-42). The

The in t e rp re t a t ion of t he r e s u l t s for

Gold - Gold results derived from rock samples ranged from 1 ppb t o 1 6 1 ppb.

values der ived from so i l s ranged from 1 t o 213 ppb. Sixteen samples were i o ppb or g r e a t e r . Threshold anomalous values are ar5itrarily considered t o be between 10 ppb and 19 ppb. Seven samples yielded results 20 ppb 01

greater. The results for gold a r e preserited (XI F l y ~ r e 4 . A list of rock sample desc r ip t ions is appended t u t h i s report;.

CONCLUSIONS

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The Syrup property is underlain by sedimentary and volcanic rocks of t he T r i a s s i c t o upper Jurassic Nicola Group and/or Carboniferous Thompson

assemblage and by of the Jura-Cretaceous

Okanagan Bathol i th . The rocks f a u l t s i n a v a r i e t y

of a t t i t u d e s but dominated by a s t rong northwesterly t rending set and a north-

easterly t rending set . these f a u l t s may have been repeatedly activated throughout t h e geological h i s t o r y of t h e area. Anomalous geochemical values

for gold, copper, lead, z inc and a r s e n i c have been detected from an area extending from the north c e n t r a l boundary of t he p o p e r t y t o t h e southeast corner of t he SYRUP 1 claim. This area is underlain by p y r i t i c and rusty sediments and volcanics i n contac t with qua r t z -d io r i t c . The area is geologica l ly similar t o the zones of mineral izat ion d i s c w e r e d on t h e FLAP claims (Medford 1989, pers. comm.) The geochernical values i n so i l s (up t o 213ppb Au) compares very favourably with t h e geochemical e q r e s s i o n obkained from s o i l s surrounding the quar tz vein eiscovery and volcanic sxha la t ive

horizon on the FLAP property. Much covered by widespread, genera l ly th in , overburden. The Area from t h e north centra!

boundary t o the southeast corner of t h e SYRUP 1 claim requires fu r the r explorat ion and a more de t a i l ed examination using geological mapping, s o i l

sampling and geophysical techniques.

i n t rus ive rocks believed t o bc part are cut by hr3e and small

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RECOMMENDATIONS

Continued exploration of the SYRUP property is recommended t o test fo r

gold mineralization related to pyritic quartz veins and t o test for base m e t d l

horizons within the types may not ke mutually exclusive). The survey grid should be extended for continuing geochemical sampling and conducting geophysical studies. Line spciny should be 1GO n? apart with station spacing every 25 m. along the lines. The grid anc! survey area can be restricted t o include only that portion of the claim underlain by the volcanic am3 sedimentary units. Overburden depths are not expxted to be excessive and shoulZri't place undue interpretation diff:cu:ties on the mi: geochemical surveys. Initially, magnetometer and vL%-EM surveys should be done in conjunction with the geochemical surveys anC de tailed map pin^. Tie surveys can be expanded t o fill-in lines or additional surveys such as 1.P.surveys m y be performed as required. An excavator may readily be employed &cause of the excellent road access and minimal overburden cover, to evaluate any anomalous areas defined. Future diamond drilling programs will !x contingent on the preceeding results.

volcanic and sedimentary horizons (the two

November 25 1989 Surrey, B.C.

W.A. Howell, B.Sc. Consulting Geologist

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BIBLICXXWHY

To Accompany report dated Novem!xr 25, 1389 by W. A. Howell, 2. Sc., Geological and Geochemical report on the Jcyxa Claim.

1. Church, B.N. (1980): Geology of the Kelowna Tertiary Outlier, B. C. Ministry of Mines, Prelim. Yap 29, Scale 1:50,000

2. Church, B.N. (1980): Geology of the Terrace Htn. Tertiary Outlier, B.C. Ministry of MInes, Prelim. Yap 37, Scale 1:50,000

a. 7 Claim Map, B.C. Dept of Mines, NTS 82E/13W, Scale 1:50,000.

4. G o d , D.R. (1979): Geological, Geochemical, Geophysical Report on the Rich, Jack, et a1 claims; Ass. Rpt. 7214, for Pan Ocean Oil Ltd.

5. H i l l , J . R . (1978): Geochemical Assessment Report on the COMA Claims. Ass. Rpt. 7309, for Canadian Occidental Petroleum Ltd.

6. Jones A.G. (1959): Vernon Map Area, B.C. Geological Survey of Canada Memoir 296, Geological Map 1059A, Scale i:?53,ZZ?.

7. Little, H.W. (1961): Kettle River, West Half, R.C. (82E/W1/2) Geological Survey of Cana6a, Map 15-1961, Scale 1:?53,440

8. Morrison, M. (1986): Geological Assessment Report on ",he Jubilation Claims. Ass. Rpt. 15,157.

9. Myers, R.E., Taylor, W.A., "Metallogenic Studies of i d e Gold-Silver Occurrences in South-Central B.C. a Progress 2eSort" B.C. Ministry of Mines Paper 1989-1, pg. 355-363.

10. Yyers, R.E., Taylor, W.A. and Tempelman-Klui:, D. (1989): "Lode Go:?- Silver occurrences of the Okanagan Region, South-Central B.C." B.C. Ministry of Mines, Open File 1989-5.

11. Nicholson, R.J. (1980): Ceological and Geochemical ReBort on the Nocpn Claims; Ass. Rpt. 9186, for Cominco Ltd.

12. Okulitch, A.V. (1979) Thompson-Shuswap-Okanagan, Geological Survey of Canada, O p e n File Map 637, Scale 1:250,000.

13. Pautler, J. (1988): Geological and Geochemical Report on the Lamb Claims Ass.Rpt. 17,854, for Ken Mdison Kines Ltd.

14. Tempelman-Kluit, D. (1989): Penticton Yap Area, i3.C. (52E! Geological Survey of Canada, Open File 1969. Geological Map, Scale 1:250,000

15. Topographic Map. Peachland, B.C.NTS 82E/13, Scale 1:50,000

16.

17.

18.

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20.

21.

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Van Bosen, G. (1979): Geological ar?? Geophysical r e s o r t or! f5e SS.T an2 HO?E Mineral Claims, Ass. ap t . 7229.

Van Rosen, G. (1976): Geochemical Report of Heavy %?tal Concentration and Analysis on the C.V. Mineral Cla im. Ass.R?t. '5,233, f o r Laramie Mining Corp.

Wilmot, A.D. (1986): Geophysical and Geochemical Report on the Z m r Claims; Ass. Rpt. 15,400 f o r Skyworld nevelopment & Resources

Wilmot, A.D. (1987): Geochemical an6 Dr i l l i ng Report on the Zumar Cla ims : Ass. 2pt. 16,416 for Skyworld Pevelopment & liesources.

Ziebart, P. (1987): Prospecting Report on J u b i l a t i o n Claims; Ass. Rat. 16,504, f o r Chevron Canada Ltd.

Ziebart , P. (1988): Prospecting Report on FLIP claims; Ass. 9p t . :7,70(? fo r Chevron Canada Ltd.

Winister of Mines Annual Report: 1929 gages 247-249

1933 pages 196-197 1950 page 115

1930 pq5.s 207-208

S.C. A i r Photos: BC 88077; 016, 128, 129. BCC 362; 150, 151. BCC 370; 055, 056.

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Appendix I

Statement of Qualifications

I, William A. Howell, hereby certify that:

I am a Geologist and reside at 15294 - 96A Avenue, Surrey, B.C. V3R 8P5

I am a graduate Bachelor of Science in Geology (1971).

of the University of British Columbia with a degree of

I am a member of the Geological Association of Canada.

I have practised my profession as a geologist since 1971, having worked as an employee and/or consultant for several Internationa: Mining Corporations and Junior Resource Companies.

This report is based September 23rd to October 5, 1989.

upon field work undertaken on the property

I have no direct or indirect interest, nor do I expect to receive any interest directly or indirectly in the property or securities of Verdstone Gold Corp.

November 25, 1989. Surrey, B.C.

William A. Howell, i3.S~. Consulting Geologist

APPENDIX I1

APPENDIX I1 : COST STATEUENT

PERSONNEL:

J . Boutwell (Prospector) 19 days, Q $225.00/day P. Newnan (Prospector) 6 Days @ 225.00/day V . Guinet (Prospector) 2 Days 8 225.00/day W . Howell (Geologis t ) 7 Days Q 300.00/day G. Medford (Consul t a n t ) 1.5 Day Q 375.00/day

P1 us: Disbursements o f

DISBURSMENTS:

Assays S o i l s 386 x $10.85 Rocks 44 x 13.00 Shipping

Gas and o i l Drafting Material s and suppl i e s Air Travel Base Maps Mi sce l l aneous

ST

$ 4,188.10 572.00 54.55

336.55 306.00

96.35 471.57 231.66

75.34 6,332 12

6 4,275.00 1 ,350.00

450.00 2,100.00

562.50 89.51

6,332.12

RENTALS :

4 x 4 truck ren ta l 16 days Q $ 60.00/day $ 960.00 Room and Board 34 Man Days 8 50.00/day 1,700.00

REPORTING: B i ndi ng , copies , word processi ng

TOTAL

2,000.00 180.87

$ 20.000.00

J

APPENDIX 111

Sample

JS-IR

JS-2R

JS-3R

JS-4R

JS-5R

JS-6R

JS-7R

JS - 8R

JS-9R

JS-1OR

JS-llF!

JS-12R

JS-13R

JS -1 4R

JS-1SR

JS-16R

Desa ipt ion

Grab sample of siliceous pyritic amphibolite, mineralization appears to be associated with quartz veining.

Grab sample from quartz vein, 3 cm. wide pyrite.

with fine grained

Same location as above, quartz with 60% wall rock.

Grab sample from quartz vein containing wall rock plus some pyrite, same location as above.

Grab sample along logging road.

of silicified pyritic rock from gossanous zone

Grab sample from 2 cm. vide quartz vein, very pyritic, 10 m. from above sample.

Grab sample of pyritic, schistose, mafic volcanic from a 1.5 m. wide shear zone.

Pyritic crumbly schist from same location as JS-7R.

Same location as above two samples with hematite and more pyrite.

Grab sample from 6 an. wide quartz vein with minor pyrite.

Grab sample from 3 an. wide quartz vein, rusty and vuggy.

Same location as above sample, with 15% pyrite.

Quartz stringers in calc silicate rock.

Grab sample grained pyrite.

of sheared siliceous volcanic rock with fine

Grab sample of rusty banded calc silicates.

Grab sample of fine grained siliceous andesitic rock with fine grained sulphides.

Sample #

89-BS 5

89-BS 6

89-BS 7

89-BS 8

89-BS 9

89-EJ 10 89-BJ 11 89-BJ 12

89 BJ 13

89-BJ 14

89-BS 23

89-B 2 4

89-BS 27

Description

Qtz veins with pyrite. o b . in coarse roadside rubble but not in outcrop. local outcrop is limey interbeded fine sandy tuffsand crossbedding. Rx are locally rusty but not silicified. Located across the road from the "Horseshoe lake recreational site .'I

argillites with local thickening and

4an qtz vein in small re-entrant bi qtz diorite on west side of road at the south end of horseshoe lake.

Ian qtz vein in diorite contains pyrite and chalcopyrite. vein is uncommon, lies 090/lOS total sulphide is 15% with no moly. py/cpy = 3/1 or more. Sample is "high- graded. "

Rusty pyritic fractures in contact phase f.g. diorite. ?trace cpy present.

Flat E-W strike, 10s dip qtz vein/orthoclase,muscovite pegmatite. very little sulphide present. Old Cat stripping in this area looks like exploration dating to about 18 years ago. (c.1971)

chip samples across 2m each, of high sulphide, siliceous sintery black shale in "nose" of road along the south side of logging slash near the southeast boundary of the Jack claims.

Fine gr. grey heavy rock, o / c has 15% diss. f.g. sulphides in f.g.qtz/ser Matrix within the black shales.

Very hard siliceous & pyritic nubbin in the road bed. Difficult to sample properly. Rock is probably a siliceous tuff.

Sintery grey vertically bedded fine sandy seds. v.f.g. sulphides possibly po. old sampling here is "TLE 88-83" sample is on a N-S yellow flag line vith white tags and is located on the Bear Main adj. to km 28.

200m up spur road at 24km on the lambly creek road. The sample is off the property. the sample is of strongly quartz-carbonate altered sediments exposed in the road bed and the ditch over several tens of meters.

Hfls/pyritic greenstone fract. py and occasional

89-BS 28

89-BS 29

89-BS 30

89-BS 31

89-BS 32

89-Bs 33

89-Bs 34

89-BS 35

89-BS 36

89-BS 37

89-BS 38

89-BS 39

89-BS 40 89-BS 41

89-BS 42

clay/silica alteration. Old trenching in this area is probably 10-14 years old.

Greenstone breccia cemented with f.g. qtz/carb.

Qtz vein in rusty hornfelsed blocky greenstone.

Silt from well developed drainage. Sample is highly organically contaminated very fine silt.

Pyritic hornfelsed tuff or fine sediment.

Rusty, pyritic/pyrrhotitic hornfels and argillaceous tuffs. very minor qtz.

Rusty, hard, hornfelsed fine grained greenstone. contains py&po.

Sintery boxwork of fine silica stringers in a buff to khaki green v.f.g. volcanic matrix. The stringers are commonly composed of terminated quartz enclosing very smallvugs and open spaces.

Highly broken, leached, rusty, ?tuff? or greenstone. In bank of old skid trail.

Pyritic silica/sericitic alt'd greenstone in bank of old skid trail.

Intrusive, not typical, the quartz diorite comtains minor (2mm) qtz. vein with limonitic fractures and exhibits about 30% alteration to sericite. very minor possible MoS, in qtz.

Float boulder, about 200 lb. Silicified, Qtz veined volcanic breccia. Vuggy qtz veins up to 2 cm vide with abundant limomite & fine grained disseminated pyrite. boulder is in the road bed and is highly angular as if ripped out by a cat while building the road. There is no evidence of glacial rounding or smoothing.

no record

Quartz vein in hornfelsed greenstone with secondary Biotite. (both samples)

Hornfelsed greenstone contains l%py and possible cpy. veathers very rusty.

0 mi k Ili It E P‘ It.. t Is E” E m, e a,” @I* t t PHONE(604)253-3158 FAX(604)253-1716 852 E. BASTINGS ST. VANCOUVER B . C . V6A 1R6

GEOCHEMICAL ANALYSIS CERTIFICATE

a , ACME ANALYTICAL LABORATORIES LTD.

ICP - .SO0 GRAM SAMPLE IS DIGESTED WITH 3ML 3-1-2 HCL-”03-HZO AT 95 DEG. C FOR OWE HOUR AND IS DILUTED TO 10 ML WITH WATER. THIS LEACH IS PARTIAL FOR MN FE SR CA P LA CR MG EA T I E U AND LIMITED FW WA K AND AL. MI DETECTIOH LIMIT BY ICP IS 3 P W . - SAMPLE TYPE: SILT/ROCK A L T ANALYSIS BY ACID LEACH/M FROM 10 GM SAMPLE.

DATE RECEIVED: OCT 6 1989 DATE REPORT HAILED: cd l / l p s , SIGNED .TOYE, C.LEOHG, J.WANG; CERTIFIED E.C. ASSAYERS

Guinet Management PROhECT SYRUP File 4 # 89-4130

SAMPLE#

8 9 -BS-3 0 P-S-R-1 P-S-R-2 8 9 -BS-7R 8 9 -BS -8R

89-BS-9R 89-BS-23R 8 9 -BS-2 4R 89-BS-2 5R 8 9 -BS -2 7 R

89-BS-2 8 R 89-BS-29R 89-BS-31R 89-BS-32R 8 9 -BS-3 3R

89-BS-40R 89-BS-4 1 R 89-BS-42R STD C/AU-R

Mo PPM

3 11

2 4 1

4. 6 1 1 2

1 2 8

63 9

1 2 3 8 3

1 1 1

10

cu PPM

81 37 10

195 5 0

7 7

34 64 49

2 0 16 65 64 60

8 4 8 56 5

24

17 9 1 64 58

P b Zn Ni PPM PPM P% PPM

15 13

3 6 7

8 16 4 1

9 2 1

3 3

1 4 4 6

1 3 5 5 9 5

2 3 8

38

103 1 0

4 53 58

1 4 4

103 92 4 3

2 3 4

1 2 7 675

49

16 37 2 5 13 67

44 58

151 1 3 2

34 7 7 5 4

9 6 8

34 26

1 3 8

77 65 48

15 9

38 5

1 0 3

6 2 7 6 24 67

co PPM

9 4 1

92 7

3 1 3

29 1 0

5 5

13 9

16

6 5

13 5

18

15 18 2 1 3 0

A s PPM

4 2 2 2 2

2 27 8 5

2 5

2 2 2 5 3

5 2 2 5

1199

5 1 3

2 42

Sb Ba Au* PPM PPM PPB

2 2 2 2 2

2 2 2 3 2

2 2 2

‘ 2 2

2 2 2 2 2

2 2 2

15

3 4 1 2 3

3 7 3

4 3 1

1 2 3 7 3

56 3

161 2

95

1 4 2

4 9 5

Guinet Management FILE # 89-4037 : 114 PbY1’ SAMPLE# Mo C u Pb Zn A Ni Co A s Sb Ba Au*

PPM PPM PPM PPM PP8 PPM PPM PPM PPM PPM PPB

JS-1-R JS-2-R JS-3-R JS-4-R JS-5-R JS-6-R JS-7-R JS-8-R JS-9-R JS-10-R

JS-11-R JS-12-R JS-13-R JS-14-R JS-15-R

gs z1tj-R

1 84 4 107 2 227 2 175 30 61

10 5 5 2

I4

49 15 26 44 97

46 10 10 9 21

22 10

52 22 15 10 2

2 4 2 1 2 2 2 1 2 2

2 12 2 4 2 2 2 1 2 5 2 2 2 1 2 1 2 1 2 1 5 1

38 24 22 17 19 24 21 2

325 137 1 204 2 273 1‘. 288 9 13

10 6 5 6 2

36 226 375 9:

28 9

2 2 2 2 3

11 1 5

2 36 10 535 1 118 4 110 6 92

2 3

6 29

5 8

154 97 43

2 27 19 26 11

2 4 16 3 4

2 6 5

14 131 18

26 70 12 89 13 8 .

J . I c a 0; I t mi rn liI a 6 E I R a Ik D 0 Guinet Management FILE # 89-4037 P a g e 11

SAMPLE# Mo Cu Pb Zn Ni C o A s Sb Ba Au* PPM PPM PPM PPM PC8 PPM PPM PPM PPM PPM PPB

48s 48s 48s 48s

12+50E 13+00E 13+50E 14+00E

6 1 1 2 1

73 26 20 25 21

12 9

174 120

83 24

12 10

16 5 5 4 5

4 2 7 7

11 10

80 80 76

19 30 22

9 10 10

4 1

2 1

12 2 1

48s 14+50E 7 6 10 7

2 3 2 2 2

2 2 2 2 2

485 48s 48s 48s

15+00E 15+50E 16+00E 16+50E

4 3 3 1 2

38 35

11 9

167 165 117 122 133

40 55 34 36 42

13 12 12 13 15

35 38 24

13 15 14 8 48s 17+00E

9 11 8 3 4

3 1 5 4

48s 48s 48s 48s 48s

17+50E 18+00E 18+50E 19+00E 19+50E

1 2

34 26 30 27 31

12 8 12 12 10

111 167 176 109 106

34 39 33 36 28

13 14 14 13 11

2 2 1

107 55 130 131 74

39 27 55 33

11 5 12 14

7 4 7 7 2

2 2 2 2

48s 48s 48s 48s 48s 48s 48s 48s 48s 48s

20+00E 20+04E 20+50E 21+00E 21+50E

2 1 1 1 1

49 45 65 32 18

18 7 14 11 7

SILT

22 9 2

22+00E 22+50E 23+00E 23+50E 24+50E

2 2 3 1

21 29 73

10 8 9

109 106 107 157 173

23 25 41

10 11 9 11 12

. 8 6

2 2

1 2

6 5 9

' 2 3 2 4

24 29 69 62

11 8 14 40

2i 34

2 2 2

48s STD

25+00E C/AU-S

2 19

184 132

65 65

11 31

7 40

2 15

2 53

D E I I I 0

SAMPLE#

4 7 5 18+50S 4 7 s 19+oos 4 7 s 19+50S 4 7 s 20+00s 4 7 s 20+50S

4 7 s 21+00s 4 7 s 21+50S 4 7 s 22+00s 4 7 s 22+50S 4 7 s 23+00S

4 8 s O+OOE 4 8 s 0+50E 4 8 s 1+00E 4 8 s 1+50E 4 8 s 2+00E

4 8 s 2+50E 4 8 s 3+00E 4 8 s 3+50E 4 8 s 4+00E 4 8 s 4+50E

4 8 s 5+00E 4 8 s 5+50E 4 8 s 6+00E 4 8 s 6+50E 4 8 s 7+00E

4 8 5 7+50E 4 8 s 8+00E 4 8 s 8+05E SILT 4 8 s 8+50E 4 8 s 9+00E

4 8 s 9+50E 4 8 s 10+00E 4 8 s 10+50E 4 8 s 11+00E 4 8 s i i + 5 0 ~

4 8 s 12+00E STD C/AU-S

c E 0. I E 6 E a Guinet Management FILE # 89-4037

Mo C u Pb Zn A Ni Co A s Sb PPM PPM PPM PPM PP8 PPM PPM PPM PPM

1 1 1 ~

2 1

1 18 10 9 2 2 0 10 3 2 1 2 1 8 1 2 1 2 7 11 6 2

9 2 4 5 55 15 11 2 2

3 30 2 3 2 10 1 7 4 50 15 7 4 4 8 1 2 2 3 6 7 2 1 9 15 2

1 2 0 7 100 3 1 11 6 2 1 19 11 117 2 8 11 5 2 2 2 1 10 1 2 1 2 6 11 8 2 1 58 10 116 4 4 15 11 2 1 70 10 1 3 4 4 4 15 10 2

2 37 9 1 2 0 3 4 1 3 3 2 2 4 3 9 138 3 1 17 4 2 5 36 1 4 1 3 2 4 0 13 6 2 2 30 13 1 4 6 35 1 4 9 2

' 2 3 1 15 105 2 5 1 6 3 2

8 1 4 6 9 8 2 8 1 1 4 4 9 1 8 88

50 2 0 2 3 4 6 19

4 9 2 5 2 7 4 4 2 6

2 0 10 10 13 11

7 2 8 2 9 2 5 2 7 3

1 2 6 1 4 92 30 1 2 8 2 1 18 8 9 4 2 7 1 0 5 2 2 4 1 11 3 2 8 4 2 13 9 2 2 2 2 10 1 8 2 19 10 5 2 1 2 6 10 99 30 1 2 9 2

1 18 13 78 2 5 10 7 2 1 17 9 1 1 4 2 0 10 5 2 2 5 2 13 3 5 4 2 3 11 7 2 1 19 4 80 2 3 10 2 2 1 2 9 15 100 3 2 11 4 3

18 18 2 2 18 2 2

11 1 3

7 11 11

1 1 4 111

79 1 2 7

87

2 7 2 8 2 2

11 11 11 11 11

4 7 6 5 4

2 2 2 2 2

1 2 3 13 115 .5 18 11 9 3 18 6 0 4 5 133 7.2 67 31 4 0 1 6

a

Ba PPM

I

Au* PPB

2 4 3 1 2

2 1 3 3 4

1 6 1 3 1

1 2 3 2 ~

3

8 6 4 6 3

2 1 5

18 1

4 3

2 1 3 3

5 4 9

c e Page 10

E I; @ lir I h

SAMPLE# . .

4 6 s 26+50E 4 6 s 27+00E 4 6 s 27+50E 4 6 s 28+00E 4 7 s 1+00E

4 7 s 1+50E 4 7 s 2+00E 4 7 s 2+50E 4 7 s 3+00E 4 7 s 3+50E

4 7 s 4+00E 4 7 s 4+50E 4 7 s 5+00E 4 7 s 5+50E 4 7 s 6+00E

4 7 s 9+50E 4 7 s 10+50E 4 7 s 1 1 + 0 0 E 4 7 s 11+50E 4 7 s 12+00E

4 7 s 12+50E 4 7 s 13+00E 4 7 s 13+50E 4 7 s 14+00E 4 7 s 14+50E

4 7 s 15+00E 4 7 s 15+50E 4 7 s 16+50E 4 7 s 17+00E 4 7 s 17+50E

4 7 s 18+00E STD C/AU-S

It I Guinet

Mo PPM

1 1 2 1 1

1 1 1 1 2

3 6 1 2 2 2 2 1 1 1

1 1 2 1 1

1 1 1 1 1

1 1 2 1 1

1 18

cu PPM

44 34 44 23 1 5

4 1 4 1 4 6 32 35

5 1 32 33 3 1 34

3 1 28 29 22 18

30 17 5 1 28 22

2 1 17 1 6 17 32

18 24 25 22 19

17 59

& ~ % ir t. 0. 1. e E E t e' 1 Ir Management FILE # 89-4037 P a g e 9

Pb Zn A Ni Co As Sb Ba Au* PPM PPM PP8 PPM PPM PPM PPM PPM PPB

8 9

10 6 7

9 13

5 9 8

7 9

10 9 9

9 9 9

11 9

7 7

13 13

5

10 6 7 5

11

7 10 1 0 12

8

146 145 159 127

92

196 155 116 134 247

150 291 115 103

69

110 9 6

119 8 0

109

8 0 74

111 100 135

101 8 1 91

115 127

111 100 110 1 0 1 126

42 31 48 22 1 3

38 36 26 25 17

51 49 34 34 20

26 27 34 22 27

28 21 43 32 28

23 25 22 3 1 28

22 24 26 26 27

14 11 14 12 9

16 14 16 13 20

1 6 2 1 13 13

9

13 11 12 10 11

11 10 1 3 11 12

12 11 10 12 14

13 13 12 12 1 0

8 9 8 8 5

5 9 7

1 0 6

8 5 9 6 6

15 10 1 3

8 9

7 5

10 8 7

9 6 5 5 9

7 10

7 6 5

2 2 2 2 2

2 2 2 4 2

2 2 2 2 2

2 2 2 2 2

2 2 2 2 3

3 2 2 4 2

2 2 2 2 3

1 4 2 3 1

6 3 1 2 1

1 1 1 1 2

2 1 5 1 1

5 3 2 2 2

5 1 1 1 4

1 2

2 0 4 1

25 10 4 2 1 48

10 98 36 132 68 3 1 39 15

L. a- b ai%& &La, a E. c t It I ab", " m P a g e 8 Guinet Management FILE # 89-4037

SAMPLE# Mo Cu Pb Zn A Ni Co As Sb Ba Au* PPM PPM PPM PPM PP8 PPM PPM PPM PPM PPM PPB

25 17 20 25 15

123 110 106

35 31

11 10 10 10 10

8 3 1 9 1

46s 9+00E 46s 9+50E 46s 10+00E 46s 10+50E 46s 11+00E 46s 11+28E SILT 46s 11+50E 46s 12+00E 46s 12+50E 46s 13+00E 46s 13+50E 46s 14+00E 46s 14+50E 46s 15+00E

8 12 11

7

31 26 24

96 156

448 296 177 188 147

-

1 2 1 7 4

2 1 1 2

58 29 27 36 16

31 14

13 10 12 12 11

8 11 12 14 8

13 11 9

24 35 21 i 1

1 1 1 2

2 1 1 1

'. 1

27 25 19 23 15

8 3

119 86

33 24 22 31 14

12 12 10 13 11

13 9 7 14 6 10 10 5 7 3

. 4 7 10 7 5

8 4 9 6

91 105 82 1 46s 15+50E

46s 16+00E 46s 16+50E 46s 17+00E 46s 17+50E 46s 18+00E 46s 18+50E 46s 19+00E 46s 19+50E 46s 20+00E 46s 20+50E

2 2 2 2

1 1 1 1 1

1 1

28 27 18 17 18 17 29 19 31 23

111 115

23 24 17 22 24

15 14 11 13 10

8 11 75

8

1 1 1

124 14 5 103 2

7 9 9 11 11

97 141 84 160 161

94 60 89 68 13 1

21 27 19 33 25

11 13 12 14 13

2 2 '2

5 1

1 2 2 1 1

2 2 2 2 2 2 2 2 2 2 2 2 2 15

46s 21+00E 46s 21+50E 46s 22+00E 46s 22+50E

1 1 1 1 1

18 18 17 12 21

12 10 7

11 10

31 20 28

11 9 12

2 4 3

1 2 1

9 9

9 12 13 11 6 12 38

46s 23+00E

2 2 24 4

46s 23+50E 46s 24+00E 46s 24+50E 46s 25+00E 465 25+50E

1 1 1

125 135 167 92 85

22 11 6 10 5 6 6

32 58 36 28

13 15 13 11

42 22 21

1 1 6

28 65

13 31

6 40

2 51

46s 26+00E STD C/AU-S

1 18

22 60

117 132

e 0 9 li e &

SAMPLE#

45s 28+00E 45s 28+50E 45s 29+00E 45s 29+50E 45s 30+00E

45s 30+50E 455 31+00E 45s 31+50E 45s 32+00E 45s 32+50E

45s 33+00E 45s 33+50E 455 34+00E 45s 34+50E 45s 35+00E 45s 35+50E 455 36+00E 45s 36+50E 45s 37+00E 45s 37+50E

45s 38+00E 45s 38+50E 465 2+00E 46s 2+50E 46s 3+00E 46s 3+50E 46s 4+00E 46s 4+50E 46s 5+00E 46s 5+50E 46s 6+00E 46s 6+50E 465 7+00E 46s 7+50E 46s 8+00E 46s 8+50E STD C/AU-S

I- c Guinet

Mo PPM

2 1 1 4 1 1 1 2 1 2 1 1 r 2 1 2 1 1

2 1 2 1 2 1 3 1 1 2 1 3 2 1 1

1 18

cu PPM

36 41 37 62 27 30 20 29 23 22

33 28 32 24 27 34 35 43 30 31 73 73 39 45 43 28 35 28 21 30

25 32 45 25 24 37 63

- E - &. E e- t E li E P C " a Management FILE # 89-4037 P a g e 7

Pb PPM

13 8 8 17 11 14 10 14 9 10

15 7 12 9 10 13 9 9 10 10

9 11 12 10 7 11 6 10 9 7

10 12 11 4 6 9 35

Zn Ni Co As Sb Ba Au* PPM F'$# PPM PPM PPM PPM PPM PPB

171 121 227 2 14 141

129 152 137 119 92 131 121 234 131 132 139 92 172 139 130 123 155 146 134 111 140 139 107 119 85 126 86 79 103 86 103 132

47 31 61 65 23

31 25 28 23 22 46 32 51 30 27 38 29 66 27 31 46 53 32 38 37 33 52 32 28 38 22 32 45 35 28 40 66

17 17 15 14 13

15 12 13 12 14

14 12 16 12 11 14 14 20 13 13 18 20 15 13 15 12 14 12 10 11 12 12 12 13 12 12 31

3 4 4 6 4 4 3 4 2 3

2 6 3 2 5 6 3 15 4 5 10 . 6 5 5 2 2 6 2 4 3

4 6 15 7 6 5 38

2 2 : 2 1 2 2

2 2 2 2 2

2 2 2 2 2 2 3 2 2 2 2 2 2 2 2 2 2 2 2 2 2 2 2 2 2

2 15 . .

1 1 2 1 1

3 3 1 1 1 4 1 1 4 3 1 3 1 2 2 5 1 4 5 1 1 3 1 3 1

31 1 1 8 3

2 49

a I e.. It 1. B 1.- Q Y . I, e.* E 0 Ir I B a t a Guinet Management FILE # 89-4037 P a g e 6

SAMPLE11 Mo Cu Pb Zn A Ni Co As Sb Ba Au* PPM PPM PPM PPM PPZ PPM PPM PPM PPM PPM PPB

45s 9+00E 1 21 7 83 45s 9+50E 1 23 8 84 45s 10+00E 1 21 7 65 455 10+50E 2 20 11 72 45s 11+00E 1 32 8 133

45s 11+50E 1 16 8 94 45s 12+00E 1 16 7 103 45s 12+50E 1 20 5 89 45s 13+00E 1 26 7 313 45s 13+50E 1 23 6 127

45s 14+00E 1 42 7 123 45s 14+50E 1 24 11 113 45s 15+00E 1 21 7 164 45s 15+50E 2 15 8 75 45s 16+00E 1 24 12 91

45s 16+50E 2 27 12 91 45s 17+00E 1 13 6 58 45s 17+50E 3 24 9 77 45s 18+00E 3 15 7 83 45s 19+50E 1 24 7 215

45s 20+00E 1 20 11 168 45s 20+50E 2 44 13 101 45s 21+00E 1 38 8 116 45s 21+50E 1 28 6 112 45s 22+00E 1 28 15 88

23

9 11 10 7 11 9 11 9 14 11

13 13 8

4

4

3

4 5

10 7 12

4 7 9 6 5

2 2 2 3 2 1 2 1 2 1

2 1 3 1 2 2 2 1 2 13 2 1 2 2 2 2 2 1 2 2 2 1 2 1 2 2 2 1 2 1 2 1 2 2 2 2 2 1 2 2

45s 22+50E 1 40 8 115 21 16 4 2 2 45s 23+00E 1 26 9 86 23 12 5 2 2

1 19 10 106 19 13 5 2 2 1 45s 23+50E

45s 24+00E 1 45 11 120 24 16 3 2 45s 24+50E 1 22 7 101 11 11 6 2 1

45s 25+00E 1 26 11 108 25 13 4 2 5 455 25+50E 1 21 8 102 25 11 6 2 1

6 2 2 28 15 2 213

2 5 455 26+00E 1 20 9 120 45s 26+50E 1 45 5 81 45s 27+00E 1 30 12 115 22 13 6

29 4

45s 27+50E 1 21 9 99 24 12 4 3 2 STD C/AU-S 18 61 38 132 67 30 39 15 47

SAMPLE# Mo C u Pb Zn A Ni Co As Sb Ba Au* PPM PPM PPM PPM PPi PPM PPM PPM PPM PPM PPB

2 2 1 1 1

35 30 19 22 2 1

39 35 27 3 1 2 1

1 4 1 2 1 0 11 1 0

5 5 5 4

3 2

22 2 7 5

4 4 5 27+50E 4 4 s 28+00E 44+50S 14+00E 44+50S 14+50E 44+50S 15+00E

11 6 8 9

11

34 52 2 1 2 6 2 8

5 6 5 5

1 4 1 1 1

3 4 1 1 1

3 1 33 2 3 22 4 0 4 6

36 109 1 5 2

2 6 30

6 10

7

4 5 96

1 3 8 30

3 11 1 2

6 5

2 5 3

2 3 4 1

’ ‘1 8

10 1 4

1 2

50 1 3

9 9 8 9 9

9 7 8 9

11

44+50S 18+00E 44+50S 18+50E 44+50S 19+00E 44+50S 19+50E

1 1 1 2

18 15 1 2 38 16

6 2 6

‘ 6 6

30 16 17 4 1 2 8

2 1 1 44+50S 20+00E

44+50S 20+50E 44+50S 21+00E 44+50S 21+50E 4 5 s 2+50E 4 5 s 3+00E

1

1 2

18 49

9 6

20 34 20 15 37

3 2 2 1 1

1 1 2

2 0 19 34

2 7

11

42 3 1 22 22 2 8

13 13 9

1 0 1 0

1 1 2 3

1 34 30 2 3 2 5 28

3 10

8 7

1 1 1 1 1

5 1 1

11 2

4 5 s 6+00E 4 5 s 6+50E 4 5 s 7+00E 4 5 s 7+50E

2 1 1 1

32 2 5 29 24 5 2

11 11 1 0 1 0 18

5 4 7 4 9 455 8+00E 1 2

. . . . . . . . . . .

4 5 s 8+50E STD C/AU-S

1 2 1 6 97 22 9 2 2 1 18 63 38 132 67 30 . 40 1 4 5 2

1. 6 e 0 I Q 1 E * & . Q cy. I c I Q t I &> I Guinet Management FILE # 89-4037 P a g e 4

SAMPLE# Mo Cu Pb Zn A Ni Co A s Sb Ba Au* PPM PPM PPM PPM PPZ PPM PPM PPM PPM PPM PPB

44s 7+00E 44s 7+50E 44s 8+00E 44s 8+50E 44s 9+00E

5 26 4 58 3 14 5 84 1 24 9 75 1 15 10 75 2 26 13 64

3 48 8 51 1 18 10 69 1 16 6 91 1 12 13 93 1 18 10 82

20 16 28 23 39

6 8 10 9 10

1 4 4 1 1

8 7 10 8 9

4 13 2 5

44s 9+50E 44s 10+00E 44s 10+50E 445 11+00E 44s 11+50E

44s 12+00E 44s 12+50E 44s 13+00E 44s 13+50E 44s 14+00E

27 23 25 14 17 2

15 11 23 15 10

8 8 7

7 2 9 3 4

2 2 2 2

1 1 12 4

1 22 5 73 1 14 6 66 3 19 5 59 2 28 7 82 I 14 9 72

9 6

~

2 1

1 12 11 55 22 28

13 10 6 11 9

101 73 97 92 97

15 12 38 17 22

8 6 15 9

6 5 10 5

2 2 2 2

1 2 1

2 2 2

~

1 1 2 11 2

7 5 4 8 7 9 8 9 13 6

2

44s 17+00E 44s 17+50E 44s 18+50E 44s 18+00E

2 ' 2 2 2 3

9 7

121 87

22 16 19 37 42

10 9

2 2

1 3

5 7 6

S i 112 113

9 16 13

2 2 2

4 3 1 4 4 s 19+00E 18 5 1 1 2

445 19+50E 44s 20+00E 44s 20+50E 44s 21+00E 44s 21+50E

2 29 6 109 2 25 2 62 2 42 8 172 3 28 8 105 2 21 5 62 2 58 9 104 6 62 11 287 8 32 8 246 3 40 10 159 3 35 5 96

34 26 65 53 27

13 10 17 13 10 21 17 11 13

25 5 7

2 2 2 2 5

4 8 38

1 1 5 51

35 11 2

44s 24+50E STD C/AU-S

2 33 4 72 19 62 36 132

29 67

12 31

2 15

SAMPLE#

42s 5+50E 42s 6+00E 42s 6+50E 42s 7+00E 42s 7+50E 42s 8+00E 42s 8+50E 42s 9+00E 42s 9+50E 42s 10+00E 42s 10+50E 42s 11+00E 42s 11+50E 42s 12+00E 42s 12+50E 42s 13+00E 42s 13+50E 42s 14+00E 42s 14+50E 42s 15+00E

445 1+50E 445 2+00E 44s 2+50E 44s 3+00E 4 4 s 3+50E 44s 4+00E 44s 4+50E 44s 5+00E 44s 5+50E 44s 6+00E 44s 6+50E STD C/AU-S

e . s Guinet

Mo PPM

1 1 1 1 1

1 1 1 1 2 2 1 r. 1 1 1 1 1 1

' 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 18

cu PPM 13 14 13 25 19

14 11 9 21 30 30 11 28 14 7 14 14 10 16 11 8 17 21 17 16 17 19 18 23 20 29 28 14 16 15 21 61

. a *" . a,' a Management F I L E # Pb PPM

5 8 5 11 10 10 5 8 13 69 11 7 17 11 9

6 6 10 10 5 10 13 7 7 8 11 8 7 5 9 15 11 8 8 10 21 36

83 98 81 73 81

85 102 69 96 01 83 79 61 61 62 78 68 119 81 86 73 75 88 87 72 78 92 70 79 78 89 89 79 58 56 115 132

Ni PPM 15 17 20 37 25

21 12 12 31 12 14 17 50 17 6

15 14 12 15 10 7 13 29 31 23 21 24 21 26 25 37 59 27 23 20 18 67

* a- 89-4037 co PPM

7 8 7 7 9 7 6 5 9 3

3 8 9 8 6 8 7 6 8 6 5 7 10 9 8 9 9 8 10 9 11 11 9 9 7 8 30

As PPM

2 2 2 2 5 2 3 2 3 4 6 2 6 4

. 2 3 3 4 3 5 6 3 4 6 3 4 5 3 5 4 3 7 4 5 3

6 41

Sb Ba PPM PPM

2 2 2 2 2

2 2 2 2 2 2 2 2 2 2

2 2 2 2 2 2 2 2 2 2 2 2 . 2 2 3

2 2 2 2 2 2 15

Au* PPB

1 4 1 2 1

1 2 4 1 5

2 1 2 1 1 1 1 1 1 2 3 1 2 1 1 2 2 3 1 2

4 1 3 4 2 3

48

c (i 0 It a. I;

' SAMPLE#

4 0 5 13+00E 4 0 s 13+50E 4 0 s 14+00E 4 0 s 14+50E 4 0 5 15+00E

4 0 s 15+50E 4 0 s 16+00E 4 2 s 9+OOW 4 2 5 8+50W 42s 8+OOw

4 2 s 7+50W 4 2 s 7+00W 4 2 s 6+50W 4 2 s 6+00W 4 2 s 5+50W

4 2 s 5+00W 4 2 s 4+50W 4 2 s 4+00W 4 2 s 3+50W 4 2 s 3+00W

4 2 s O+OOE 4 2 s 0+50E 4 2 s 1+00E 4 2 s 1+50E 4 2 s 2+00E

4 2 s 2+50E 4 2 s 3+00E 4 2 5 3+50E 4 2 s 4+00E 4 2 s 4+50E

4 2 s 5+00E STD C/AU-S

Guinet Mo

PPM

1 1 1 3 1

1 1 1 1 1

1 1 1 2.. 1 1 1 1 1 1

2 1 1 2 2

1 2 1 1 1

1 2 1 1 1

1 18

cu PPM

1 4 10 10 38 11

15 11 16 20 2 6

19 19 15 2 3 18

2 1 2 3 48 48 15

62 22 18 28 16

33 17 18 19 18

1 2 30 19 22 16

2 1 62

Management FILE # 89-4037 P a g e 2

Pb PPM

1 4 10 10 13

6

16 8 8 7

13

1 4 10 11 13 8

10 1 2 7 7 9

15 10 11 10

4

7 1 2 10 11 13

11 17 11 9

16

11 4 1

Ni Co As Sb Ba Au* P% P% PPM PPM PPM PPM PPM PPB

89 8 2

108 8 2 69

119 66 8 2 79 79

6 0 6 3 56 72 8 2

9 2 1 0 2 68 6 0 6 6

5 3 69 65 6 7 5 4

55 56 5 7 79 77

62 66 71 68 52

8 4 1 3 2

2 1 13 1 4 27 1 6

15 15 37 4 1 34

4 5 43 33 43 34

42 52 54 46 29

98 43 30 49 23

34 30 31 28 27

1 3 39 24 29 24

23 67

a 7 8

11 7

7 7 8

10 1 0

9 9 9

11 10

10 10 8 7 9

10 11 8

11 7

11 8 9 9 8

7 1 2 8 9 8

9 30

2 3 7 8 3

2 4 2 5 5

2 7 4 5 5

6 3 5 3 3

6 5 8 6 2

4 5 5 2 4

6 4 7 2 5

4 43

2 2 3 2 2

2 2 2 2 2

2 2 2 2 2

2 2 3 2 2

5 2 3 2 2

2 2 2 2 2

2 3 2 2 2

2 15

1 1 3

7 4 1

2 2

10 5 3

1 2 7 1 2

5 1 1 1 1

10 1 1 1 2

1 1 1 1 1

2 1 1 1 1

2 47

e.. e c "..+ & .L a. 6-. a*- a, L, a# a, t u I k. a &&& ah* t. ,ACMB TdALYTICAL LRBORATORIES LTD. 852 E. HASTINGS ST. VANCOWER B.C. V6A 1R6 PBONE(604)253-3158 FAX(604)253-1716

GEOCHEMICAL ANALYSIS CERTIFICATE ICP - .5W GRAM SAMPLE IS DIGESTED UlTH U I L 3-1-2 HCL-HNO3-H20 AT 95 DEG. C FOR ONE HOUR AND IS DILUTED TO 10 HL UlTH WATER. T H I S LEACH IS PARTIAL FOR HN FE SR CA P LA CR HG BA TI B U AND LIMITED FOR MA K AND AL. AU DETECTIOW LIHIT BY ICP IS 3 P W . - SAMPLE TYPE: P1-P13 SOIL P I 4 ROCK AU* ANALYSIS BY ACID LEACH/M FROM 10 Gn S Y P L E

DATE RECEIVED: OCT 2 1989 DATE REPORT HAILED: 0 ~ 2 &/y? SIGNED BY.C. .'. L q D . T O Y E . C.LEONG, J.WANG; CERTIFIED B.C. ASSAYERS

SAMPLE#

4 0 s 5+00W 4 0 s 4+50W 4 0 s 4+00W 4 0 s 3+50W 4 0 s 3+00W

4 0 s 2+50W 4 0 s 2+00W 4 0 s 1+50W 405 1+OOW 4 0 s 0+50W

405 O+OOE 40A 0+50E 40A 1+00E 4 0 s 1+50E 4 0 s 2+00E

4 0 s 2+50E 4 0 s 3+00E 4 0 s 3+50E 4 0 s 4+00E 4 0 s 4+50E

4 0 s 5+00E 4 0 s 5+50E 4 0 s 6+00E 4 0 s 6+50E 4 0 s 7+00E

4 0 s 7+50E 4 0 s 8+00E 4 0 s 8+50E 4 0 s 9+00E 4 0 s 9+50E

4 0 s 10+00E 4 0 s 10+50E 4 0 s 11+00E 405 11+50E 4 0 s 12+00E

4 0 s 12+50E STD C/AU-S

Guinet Management Mo

PPM 1 1 1 1 1

I' 1 1 1 3

1 1 1

'1 1

1 1 1 1 1

1 1 1 1 2

1 1 1 1 1

1 1 1 2 1

1 19

cu PPM

59 48 32 18 19

18 11 27 33 2 3

2 1 26 2 5 20 2 3

2 1 1 3 18 15 17

15 1 3 1 3 11 18

22 17 11 26 13

15 16 33 22 1 4

18 62

Pb PPM

1 2 16 16 8 9

8 6 8

1 3 11

6 18

6 13 1 2

7 7 9 7

10

10 9 9

13 1'4

9 6 6 8

10

10 10 10

7 9

7 40

File #

39 68

113 68 8 2

49 70

105 51 44

46 9 3 63 62 40

64 58 55 58 67

109 42 62

1 2 6 62

88 85 88 57 63

48 85 75 88 6 1

8 0 132

89-4037

Ni PPM

6 4 94 54 33 46

34 1 3 47 35 38

29 31 31 26 27

28 15 24 22 27

27 24 2 1 15 2 5

24 18 22 31 1 7

2 5 1 9 3 2 29 22

20 69

co PPM

4 10 1 4 9 9

9 6

1 2 6

13

8 11

9 9 7

10 6 8 7 8

10 6 7 6 8

9 8 6 8 7 8 9 8

1 0 8

8 3 1

Age 1

A s PPM

3 7 6 5 4

2 2 8 3 7

2 5 5 4 4

2 2 5 2 4

5 2 2 2 5

6 8 2 5 3

7 2 7 8 4

2 4 5

Sb Ba PPM PPM

2 2 2 2 2

2 2 3 2 2

2 2 2 2 2

2 2 2 2 2

2 2 2 2 2

2 2 3 2 2

2 2 2 3 3

2 1 4

Au* PPB

4 5 6 2 3

1 1 4 1 3

1 1 1 1 1 2 1 1 1 1

1 1 1 1 2

3 1 1 1 1

1 1 1 1 1

1 49

l c ) . ld l . , .ALYI--IA a. . m a s 4 a E@ ST** ~ til'* ,ICOL& 6.a ~ V b * A U I * ( ~ A J L * A ~ u @ , A \ U ~ ,a&# t GEOCHEMICAL ANALYBIB CERTIFICATE

ICP - .SO0 GRAM SAMPLE IS DlGESTkO WITH 3ML 3-1-2 HCL-HNO)-H20 AT PS DEG. C FOR ONE HOUR AND IS DILUTED TO 10 ML WITH WATER. THIS LEACH IS PARTIAL Fa HM FE SR U P LA CR MG BA T I B W AND LIMITED FOR DETECTIOW LIMIT BY ICP IS 3 PPM. - SAMPLE TYPE: P1-P3 ROCK P4 SOIL A V ANALYSIS BY ACID LEACH/M FROM 10

Page 1 DATE RECEIVED! OCT 6 1989 DA!l!E REPORT WAILED: Ork / 3 / q .SIGNED .TOYE, C.LEONG, J.UANG; CERTIFIED B.C. ASSAYERS

Guinet Management PROJECT F i l e # 89-4131 SAMPLE# Mo Cu Pb Zn Ni Co As Sb Ba Au*

PPM PPM PPM PPM P% PPM PPM PPM PPM PPM PPB

8 2 2 8 3 2

374 11 187 17 18 211 16 83 103 20 15

2 2 2

70 107 20 762 89-BJ-10R 89-BJ-llR 45 88 22 304

34 110 21 596 89-BJ-12R 89-BJ-13R 3 63 13 86 89-BJ-14R 10 40 6 276 57 7 2 2 5