KOKANEE EXPLORATIONS LTD. REPORT ON DIAMOND DRILL …

KOKANEE EXPLORATIONS LTD.

REPORT ON DIAMOND DRILL HOLES E90-4 AND 5

ENG PROPERTY

ENG 2 CLAIM

FORT STEELE MINING DIVISION

YAHK AREA

N.T.S. 82F/lE *'i, G E O L O G I C A L B R A N C H

m: 4 9 C 0 4 ' ~ A S S E S S M E N T R E P O R T LONG: 116%5'w


Suite 104, 135 - 10th Avenue South Cranbrook, B.C.

V1C 2N1

Work Performed from August 26, 1990 to September 5, 1990

Report: L. Stephenson Submitted: December, 1990

TABLE OF CONTENTS

PAGE

1.00

2.00

3.00

4.00

5.00

6.00

7.00

8 .00

In t roduc t i on . . . . . . . Claims . . . . . . . . . . Access and Location. . . . Regional Geology . . . . . Property Geology . . . . . 1 9 9 0 Work Program . . . . Diamond Drilling . . . . . Conclusion . . . . . . . . Exhibit "A" - Statement of

Affidavit . . . . . . . . Author's Qualifications. . Location Map . . . . . . . Section D-D1 - Hole E 9 0 - 5 .

Section C-C1 - Hole E90-4.

Drill Logs . . . . . . . .

. . . . . . . . . . . . 1

. . . . . . . . . . . . J.

1 . . . . . . . . . . . . . . . . . . . . . . . . 1

. . . . . . . . . . . . 1

. . . . . . . . . . . . 2

. . . . . . . . . . . . 2

. . . . . . . . . . . . 3

4 Expenditures. . . . . . 5 . . . . . . . . . . . . 6 . . . . . . . . . . . .

. . . . . . . . . . . . 7

8 . . . . . . . . . . . . . . . . . . . . . . . . 9

. . . . . . . . . .Attached


REPORT ON DIAMOND DRILL HOLE E90-4 and 5

ENG PROPERTY

L. Stephenson December, 1990

1.00 Int roduc t i on

This report has been written to outline the exploration drilling work and results on the Eng claim group, at Yahk, British Columbia, 50 kilometres south of Cranbrook.

2.00 Claims

The property consists of three 4-post claims (Eng 1 = 15 units, Eng 2 = 16 units and Eng 205 = 20 units) and 206 2-post claims (Eng 3 to 2 0 4 and Eng 205 to 209) held directly by Kokanee Explorations Ltd. and eight 2-post claims (Yahk 1 to 8), under option.

3.00 Access and Location

These claims are located astride British Columbia Highway 3/95 around the town of Yahk, in southeastern British Columbia (see Location Map). Kokanee has built access roads into the main areas of the claim groups.

4.00 Resional Geoloqy

The claims lie within the central portion of the Purcell Anticlinorium, which consists of sedimentary argillites, quartzites and related intruded gabbro sills and dykes of the Aldridge Formation. This formation hosts both the Sullivan deposit and the St. Eugene deposit approximately 72 kilometres north and 25 kilometres north, respectively.

5.00 Property Geoloqy

The property is located within the Middle Aldridge rocks with the southern portion closely associated with the Lower Aldridge/Middle Aldridge contact (stratigraphic time horizon of the Sullivan Mine).

- 2 -

Limited exploration mapping of the property by Cominco Ltd. and Kenneco Inc. have shown the presence of Moyie gabbro intrusive within the Aldridge quartzites. The reports also indicate a presence of quartz veins with sulphides and some disseminated pyrrhotite and sphalerite in samples taken on the northern part of the property.

6.00 1990 Work Prosram

Kokanee commenced exploration work on this project in early July of 1990. The exploration work consisted of base linecutting, soil geochem, geophysical surveying, geological mapping and diamond drilling of five drill holes.

7.00 Diamond Drillinq

Five diamond drill holes were spotted to test the coincident geochem and geophysics anomalies on both the north and south grids and to drill test the Yahk vein at depth. A total of 1550 metres of core was drilled. Geologically, the rocks were typically Middle Aldridge quartzites and argillites.

7.10 Drill Hole E90-4 and 5

E90-4 -45' 070' Line 6100W, 2875N

E90-5 - 450 070' Line 6100W, 3050N

These two holes were drilled to test the south grid's coincident geochem and geophysical anomalies. Again, the mineralization was spotty with traces of lead and zinc, however, one small zone was intersected in E90-4 that had native silver and copper. The mineralization occurred in a 15cm zone that was easily ground up and had very poor core recovery within a quartzitic argillite horizon with some disseminated pyrite and pyrrhotite mineralization. (Assay of one fragment 0.008 oz/ton gold, 997.0 oz/ton silver, 10.3% copper).

Geologically, the hole encountered markers and stratigraphy just above the Lower/Middle Aldridge contact. The contact area itself was as indicated previous indistinct.

- 3 -

8.00 Conclusion

The work completed to date on the Eng Property has not delineated any substantial zones of mineralization. However, it has outlined two areas for further exploration and of the regional geological factors with re North Star) and stratiform (Sullivan, Star the area.

ENSON, B.Sc., M . B . 3 . P. Eng.

EXH I B I T "A"

STATEMENT OF EXPENDITURES

DIAMOND DRILLING PROGRAM (E90 - 4 t 5 )

ON ENG 2 CLAIM FT. STEELE M.D.

Covering the period of August 26th to September 5th, 1990

INDIRECT

SALARIES: R. Edmunds - Geologist - Supervision/core P. Daignault - Geologist - Core logging

logging, sampling - 6.5 days @ $200/day $ 1,300.00

2 days @ $250/day 500.00

DOM I C I LE : 6 days @ $65/day (Edmunds) 390.00

TRANSPORTATION: 1 - 4x4 truck; 6 days @ $50/day 300.00

DIRECT

Conn 2007 Kaml

or's Drilling Ltd.

oops, B.C. West Trans Canada Highway,

68,360.05

$70,850.05

or's Drilling Ltd.

oops, B.C. 68,360.05 West Trans Canada Highway,

TOTAL INDIR $70,850.05

IN THE MATTER OF THE

B.C. MINERAL ACT

AND

IN THE MATTER OF A DIAMOND DRILLING PROGRAM

CARRIED OUT ON THE ENG PROPERTY

YAHK AREA

in the Ft. Steele Mining Division of of the Province of British Columbia

More Particularily N.T.S. 82G/llW

A F F I D A V I T

I, L. Stephenson, of the City of Cranbrook, in the Province of British Columbia, make oath and say:

1. That I am employed as a Geologist by Kokanee Explorations Ltd. and as such have a personal knowledge of the facts to which I hereinafter depose:

2 . That annexed hereto and marked as Exhibit "A" to this my Affidavit is a true copy of expenditures incurred on a diamond drilling program, on the Eng mineral claims;

3. That the sa of August, purpose of

id expenditures 1990 and the 5 mineral explo

26th day for the

AUTHOR'S QUALIFICATIONS

I, Laurence Stephenson, of Cranbrook, B.C., in the Province of British Columbia, do hereby certify that:

1. I graduated from Carleton University in 1975 with a Bachelor of Science degree in Geology then, in 1985, graduated from York University with a Masters of Business Administration;

2.

3.

I Pr st

I mi

am registered as ovince of Ontario ( anding;

have had over 23 ning exploration.

a Professional Engineer for the

vgT'/.B.A. , P.Eng.

- 7 -

s I

I I

€bla zoq

N.T.S. 8 2 W l E I KOKANEE EXPLORATION

I

ENG PROPERTY LOCATION MAP

DRILL HOLES E90-4 + 5

I ;50 000 I Date:Dec/90 Sca lo :

- 8 -

KOKANEE EXPLORATIONS LTD. ENG PROPERTY

SECTION D-DI

Scale : , : 2ooo 1 Date: DEC. 1990

1000 m

KOKANEE EXPLORATIONS LT[ ENG PROPERTY

SECTION C-CI

DEC. 1990 Date : I :2000 Scale:

KOKANEE EXPLORATIONS LTD-

DRILL HOLE RECORD

Name of Property: ENG Corr. Dip: -450

Hole No: E90-4 Length :

Location: ENG 2 Claim Start Date: August

Elevation: Azimuth: 070’

Core Size: NQ Tests at:

M E T E R A G E D E S C R I P T I O N From To

0.00 - 2.13 Casing.

2.13 - 7.30 Middle Aldridae: thin bedded sequence of 15cm - 25cm quartzites interbedded with lcm - lOcm argillites. Argillites display moderate t o strong metamorphic effects; recrystallized biotite, feldspar clasts to 0 . 5 m and a pervasive fabric cleavage. Occasional patches of concretionarymaterial containing coarse pink garnet and biotite aggregates t o 0.7cm, feldspars and trace pyrrhotite in quartzites. Little fracturing, but most faces are rusty, coated with chalky clay mineral and contain dendritic manganese oxides. Local incipient crenulation cleavage overprinting slatey fabric. Quartzites contain muscovite and, locally, garnets.

7.30 - 24.00 Li tho1 oay: as above. Principal 1 y quartzite in beds up to Sm thick.

26, 1990

Page No. 1

Remarks :

Finish Date:

Collar Dip:

Logged by: FRE Date: Aug.27/90

S a m p l e No. From To Au Ag Pb Zn cu

~ J J b PPm % % PP m

KOKANEE E X P L O R A T I O N S LTD. DRILL H O L E RECORD

Property: ENG Hole No.: E90-4

Page 2

Location: Eng 2 Claim


Argillites < 5 % , generally display soft- sediment disaggregation of fine laminae, load casting and current effects. Where quartzites are garnetiferous, they react to HC1. 9.58: 8cm concretionary band specked with pyrrhotite and very rare chalcopyrite. Also contains carbonate.

24.00 - 117.50 Litholoqy: as above. Quartzites about 60% in beds between 20cm and 80cm thick. Fracture faces are largely unmineralized - no longer rusty. Soft sediment effects throughout. 39.90: 3cm set of bedded seams and patches of coarse (to 2mm) rusty aggregates. Biotitic - but probably after sulphides. 42.00 - 48.50: the fracture faces contain pyrite coatings. 46.00 - 47.50: predominantly dark, quartz-argillites with occasional bands of biotite- feldspar-garnet. 1% - 2% pyrite o r pyrrhotite as fine disseminations and bedded aggregates, locally constituting bedded laminae and up to 4% iron sulphide. Short sections of purple, calcareous argillite. 47.50 - 47.78: disturbed laminae amounting to a bedded, soft-rock fragmental. 51.62: fracture set encrusted with pyrite crossing lOcn of argillite containing bedded laminae and seams of pyrite aggregates.


ppb ppm % % w m

KOKANEE EXPLORATIONS L T D - DRILL HOLE RECORD


66.56 - 70.4F: zone of faintly laminated, calcareous, slightly purple argi 11 i tes and 30% thin bedded quartzites with low dissemination of pyrrhotite and pyrite throughout. Fractures are faced with pyrite. Quartzites locally contain dendritic Mn oxide forms, muscovite, and regions of pale green alteration. 66.89: 15cm of fine, short (0.5cm) cracks @ "20' to bedding (45' to core axis) containing very fine pyrite. 86.60 - 87.20: frequent rusty fractures within quartzites @ 25 - 40' to core axis. 87.20 - 117.50: occasional fractures faced with pyrite and pyromorphite encrustations predominantly @ -45' to core axis ("60' to bedding). Occasional dark, pyrite bearing cracks -irregular and parallel to core axis. 102.08 - 103.34: strongly sericitized, partially slump disturbed argillite and patches of quartzite. Variable dissemination of pyrite in bleached quartzite around pyritic cracks, seams, and bedded aggregates. A t 103.10, 20cm of sericitic sediments containing bedded and cross-cutting concentration of rusty and pyritic veinlets and seams and speck of chalcopyrite. 104.06: VUggY veinlet, "3m @ "55' to core axis of

Page 3

S a m p l e No. From To A U Ag /?b Zn cu

p p b PP m % % PP m

,025 - D / 20 lO/b lC2@ /w < -

Property: ENG Hole No.: E90-4 Location: Eng 2 Claim

KOKANEE EXPLORATIONS L T D , DRILL HOLE RECORD

From To

inward growing quartz crystals encrusted with pyrite, pyrite aggregates and pyromorphite. 106.34: rusty seaming over 6cm as described at 103.10.

Page 4

No. From To Au Ag fb Zn cu pp b ppm % % PP m

129.37 - 162.25 As 24.00 - 117.50: occasional rusty and pyritic fractures @ 10 - 20’ t o core axis; more numerous, irregular fractures coated with pyrite pyromorphite. 139.00 - 143.00: zone of moderately intense fracturing @ “25 ’ to core axis - open, rusty, locally coated with pyrite. 144.76 - 145.00: minor fracture zone and slip in plane of bedding associated with smeared pyrite, pyromorphite, fine pyrite veinlets and bedded seams. 145.86 - 146.70: blocky fracture zone with faces coated with pyromorphite and

/oly /bO<’ /6/. I < - . O G f . o/ 4

KOKANEE EXPLORATIONS LTD- DRILL HOLE RECORD

168.25 - 324.90 Medium (+25cm) sequences o f 25% coarse laminated argillites, 60% quartzitic argillites, more or less disturbed by soft rock disaggregation, and 15% narrow quartzites and argillite quartzites. Moderate to strong metamorphic development of biotite and feldspar phenocrysts in argillites and garnets in

Page 5

l o / @ / 0 / 9

1 0 2 1 lO22

/0!2f

Location: Eng 2 Claim Property: ENG Hole No.: E90-4

M E T E R A G E D E S C R I P T I O N S a m p l e From To I No. From To AU Ag Pb Zn cu

pp b PPm % % PP m pyrite. Minor slickensiding. 155.30 - 160.30: frequent dark irregular cracks and veinlets, singly and in short (locm) zones containing fine pyrite. The longer, single veins are approximately parallel to core axis. The shorter (2 - 5cm) cracks in zones are 255' to core axis (525' to bedding). May amount to 3% pyrite over short sections.

162.25 - 168.25 Fine to Medium Grained Ouartzite and Arqillite: thick (+1.5m) units about 60% fine to medium grained quartzite and 40% argillite. Argillites are medium coarse (5mm - 2cm) banded and largely undisturbed by slump effects. 167.49: centre of frozen, 3cm quartz vein @ 13' to core axis. Vein contains coarse aggregates of bronze biotite and pale pyrite. Within zone of pale green alteration.

i


Property : ENG Hole No.: E90-4

Page 6

Location: Eng 2


quartzites. Fracturing is very minor: faces generally contain pyrite platings when oblique to bedding. Occasional minor bedding parallel slip. There is down hole increase in quartzite thickness and content, as noted below. 168.80 - 170.05: strong and irregular development of pyrite bearing cracks as 155.30 - 160.30. 190.00: quartzites amount to +40%, mostly fine to medium grained, with occasional patches of hard, pale green alteration and garnet and biotite concretionary material. Sequence is running in cycles, 5 - 10m thick, that terminate as described above and start (at base) in thicker quartzites (+lm) amounting to >80%. 203.40: quartz vein as at 167.49 from lm to lcm wide @ 12' to core axis within zone of pale green alteration of fine grained quartzite. 205.46 - 206.20: zone of welded disturbance. At top, 12cm of soft rock fragmental with aggregates of pyrite in matrix and surrounding one 3cm fragment. This followed by welded crush zones in approximately plane of bedding, 1 to 3cm wide, of siliceous fragments and pyrite and pyrrhotite aggregates associated with dark pyrite filled cross fractures and purplish and

KOKANEE EXPLORATIONS L T D - DRILL H OL E RECORD


greenish mottling. 206.20 - 207.65: argillaceous quartzite, vaguely and coarsely mottled with purple and greenish alteration. Trace disseminated pyrite and slightly calcareous throughout. 210.60 - 211.00: as above. HC1 reaction stronger, due to fine calcite as dissemination and local bedded bands of fine specks. 212.65 -

215.80; 218.70 - 219.00: cal cite quartzite, as above. 224.70 - 226.50: zone of irregular longitudinal fracturing and planes @ 20' and 115' to core axis coated with cream powdery mineral and pale green mineral (pyromorphite?). 230.00: below this point, quartzites frequently contain 20cm - 50cm sections and occasional faint broad laminae of fine disseminated carbonate. 250.25 - 255.58: single unit. Composite quartz-turbidite below 251.75. 261.30 - 261.45: band of concretionary material contains 5mm hornblende crystals. 265.88: genuine white chert pebble within turbidite - 2cm x 3mm. 266.60 - 266.80: minor chloritic slip zone @ 40' to bedding, 45' to core axis. Occasional pyrite plating of associated faces. 266.60 - 269.00: blocky, moderately fractured with

212.85; 213.92 - 214.50; 215.20 -

Page 7


% ppm ppm % ppb

Property: ENG Hole No.: E 9 0 - 4 Location: Eng 2 Claim



Page 8


M E T E R A G E D E S C R I P T I O N

occasional pyritic-chloritic slips. This is a compressive zone.

268.53: quartzitic argillite containing fine pyrite and pyrrhotite as dissemination, within dark, hairline cracks, and smearing on minor bedding plane slip faces. 268.53: ground core, abraded fragments and mud for 15cm. Fragments heavily clouded with fine pyrite or pyrrhotite. Two fragments appear to contain bedded seams (~0.5mm) of native copper, specks of gold and lacing of a silver mineral (native Ag?) within a purple-brown siliceous bed. 268.70 : medium grained quartzite containing longitudinal veinlets or cracks to lOcm long of fine pyrite. Pyrite disseminated throughout. 275.90: medium dark, slightly bluish grey, very thin to thin bedded siltstone. Occasional short ( 3 - 6cm) siliceous interval with biotite and small (1 - 2mm) pink garnet porphyroblasts. Small (12 x 24mm) elliptical, very pale grey, siliceous clast @ 270.70. Bedding tc core axis (B.C.A.): 80' @ 272.60. 275.90 - 282.40: siltstone medium grey to medium brownish grey, mainly thin bedded to local short (<1 - 2cm) sections, very thin beddedllaminated.

267.64 -


% m ~p ppm % PP b

KOKANEE EXPLORATIONS LTD. DRILL H O L E RECORD


Between 278.30 - 280.90 occasional very fine (<0.5mm) fracture, mainly sub- parallel to the core axis coated with very fine grained pyrite. B.C.A.: 77' @ 281.60. 282.40 - 496.20: quartzite (85 - 90%) medium grey, medium to thick bedded with short, general 1 y <2dm, intervals of very thin bedded/laminated pale grey to silty greenish-grey siltstone. Locally the quartzite is weakly chloritized with very small disseminated garnet porphyroblasts. 296.20 - 299.50: primarily very thin bedded to finely laminated medium grey siltstone with occasional narrow (<ldm) biotite and garnetiferous quartzite? zone. Some of the siltstone is medium brownish grey with occasional very fine grained pyrite disseminations or very fine grained pyrite as thin ("0.lmm) coating parallel to bedding. B.C.A.: "80' @ 299.00. Very fine grained pyrite

Page 9


Epb PPm % % PPm

i

KOKANEE EXPLORATIONS L T D . DRILL HOLE RECORD

Property : ENG Hole No.: E90-4

Page 10



299.50 - 324.90: siltstone and quartzite interbedded. Quartzites are generally pale to medium slight11 greenish-grey thick to very thick beddec fine grained and massive in appearance. The siltstones are generally medium tc medium dark grey to slightly bluisk grey, particularly where the siltstone is sandy and thin to medium bedded; these sandy siltstones occasional11 contain small sub-rounded pale grey tc white elliptically shaped clasts. Some of the very thin bedded siltstoner exhibit cross bedding, from -314.20, scoured contact and minor slum1 structure giving a somewhat "ropey' appearance; short finely parallel laminated sections within the "ropey' siltstone tend to have a slight11 brownish cast. The occasional short (2dm) quartzitic "concretionary" zone2 contain coarse grained biotite anc anhedral small ((2mm) pink garnet porphyroblasts. B.C.A.: 78' @ 311.30, 79' @ 322.60.

S a m p l e No. From To Au As3 Pb Zn CU

% ppm ppm % ppb

KOKANEE EXPLORATIONS L T D . DRILL H O L E RECORD


Page 11



324.90 - 378.30 Lower Aldridge: NOTE: the Lower/Middle Contact is not well defined and it iz not certain that the "Lower Aldridge' rocks are actually Lower Aldridge.

END OF HOLE @ 327.30m.

S a m p l e cu Pb Zn No. From To A u Ag

pp b ppm % % pp m


DRILL HOLE RECORD Page No. 1

Name of Property: ENG

Hole No: E90-5 Length:

Location: Eng 2 Claim Start Date: September 2 , 1990 Finish Date:

Corr. Dip: Remarks :

Elevation: 1178m Azimuth: 070'

Core Size: NQ Tests at:


0.00 - 3.30 Casing: in overburden.

3.30 - 16.50 Quartzites and Siltstones: typical Middle Aldridge sedimentation mainly medium to medium dark grey to slightly bluish grey. Quartzites and sandy siltstones, thin to thick bedded, with occasional short (<2dm) interval of mainly parallel laminated siltstone. Occasional, minor slump structure and cross bedding and rare small elliptical pebbles. Weak to moderate iron oxide on fractures. Bedding to core axis: 70' @ 14.00.

16.50 - 25.60 Siltstone: mainly very thin bedded to finely parallel laminated dark bluish grey siltstone with minor (<15%) thin to medium bedded medium dark grey quartzite and sandy siltstones over short (<2dm) intervals. B.C.A.: 68' @ 21.00.

Collar Dip: -45'

Logged by: PMD Date:

S a m p l e No. From To AU Ag Pb Zn cu

pp b ppm % % pp m


25.60 - 103.70 Quartzite ("2/3) and Siltstone ("1/3): typical Middle Aldridge sedimentations basically as described for the interval 103.70 - 146.70. B.C.A.: 73' @ 31.20, 70' @ 37.80, 71' @ 51.10, 72' @ 58.70, 70' @ 69.90, 68' @ 81.00, 73' @ 87.70, 72' @ 100.00.

103.70 - 146.70 Quartzite ("60%) and Siltstone ("40%): quartzites are generally medium to thick bedded separated by short (generally <lm) intervals of siltstone and sandy siltstone. Siltstones are medium to dark grey, locally slightly brownish grey, g e n e r a l l y very thin bedded/laminated with occasional soft sediment deformation structures. The siltstones are notable by the ubiquitous development of very fine grained sericite(?) which imparts a phyllitic appearance to the bedding plane surfaces. The quartzites are locally

i


pp b PPm % % PP m

KOKANEE EXPLORATIONS L T D . DRILL HOLE RECORD

Property: Eng Hole No.: E90-5

Page 3

Locat-ion: Eng 2

146.70

152.30


-

-

coarse (<5cm) patches of fine grained black biotite with occasional associated fine to medium grained clots of pyrite. Very finely parallel laminated siltstone between 112.60 - 112.90 with B.C.A.: 71'. Rubbly rock between approximately 112.90 - 113.10. Occasional small elliptical clast scattered randomly throughout the section. Very fine grained pyrite occurs as irregular wispy clots on fractures and rarely on bedding planes, between 112.90 and 124.40. Sample: 122.70 - 123.70. At 127.30, -5cm of pale grey, sericite rich bedding para1 lel fine gouge. B.C.A. : 74c @ 124.50; 68' @ 140.80.

152.30 Siltstone: ("80%) mainly parallel very thin bedded/laminated siltstone with occasional slumped bedding, sole mark and flame structure. B.C.A. = 74 ' @ 151.30.

182.60 Quartzite and Interbedded Siltstone: (approximately 1:1) generally similar lithology to that in the interval 103.70 - 146.70. Weakly chloritic on some


% m pp ppm % pp b

KOKANEE EXPLORATIONS LTD. DRILL H O L E RECORD


Page 4

Location: Eng 2


fracture surfaces. At 1 6 5 . 1 0 , 4 - 5cm of coarsely granular gouge. At 1 6 7 . 9 0 - 1 6 8 . 2 0 , possibly very finely parallel laminated. 1 7 8 . 9 0 - 1 7 9 . 2 0 : very finely parallel laminated siltstone. From 1 7 7 . 9 0 - 182.50: extremely fine grained pyrite(?) occurs as dark dendritic patches and along very fine irregular discontinuous healed fractures @ low angle t o bedding planes. The quartzite between 1 7 6 . 7 0 - 1 7 7 . 2 0 is spotted with innumerable fine (<lmm) anhedral white calcite grains. B . C . A . : 7 4 ' @ 1 6 0 . 9 0 ; 73' @ 1 6 8 . 0 0 ; 74' @ 1 7 9 . 1 0 .

1 8 2 . 6 0 - 1 9 6 . 9 0 Quartzite: predominantly pale to medium grey, mainly medium bedded quartzite with minor (10 - 1 5 % ) interbeds of mainly parallel very thin beddedllaminated finely sericitic siltstone.

1 9 6 . 9 0 - 207 .50 guartzite and Siltstone: as previously described. B.C.A.: 76' @ 1 9 9 . 0 0 .

END OF HOLE @ 207.50m

S a m p l e No. From To Au Ag Pb Zn c u

% P Pm pPm % ppb

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KOKANEE EXPLORATIONS LTD. REPORT ON DIAMOND DRILL …