REPORT ON DIAMOND DRILLING GOLDSTREAM MINE

LO6 NO 6 ACTION: I

REPORT ON DIAMOND DRILLING GOLDSTREAM MINE

Revelstoke Mining Division 51"38' N Latitude - 118"26' W Longitude

NTS 82M/9W/10E

G E O L O G I C A L B R A N C H A S S E S S M E N T R E P O R T

W. Raven, P.Geol. December 22, 1994

OREOUEST CONSULTANTS LTD.. 306-595 Howe Street, Vancouver, E.C.. Canada V6C 2T5 Telephone: (604) 686-6768 Fax: (604) 688-9727

SUMMARY

A surface' diamond drilling program was completed on the

Goldstream Mine orebody to upgrade and define ore reserves below the

300 metre elevation panel. The subject property is located

approximately 70 Ian north of Revelstoke, B.C. in the Selkirk Mountains

of southern British Columbia. The Goldstream Mine is a stratabound

massive sulphide copper - zinc deposit. The property is jointly held by Bethlehem Resources Corp. and Goldnev Resources Inc. with Bethlehem

being the operator.

This report describes the the diamond drilling program completed

on the property from July 17, 1994 to November 26, 1994. Eleven drill

holes totalling 5226.53 metres (17,143 ft.) were completed on the

orebody, all are on the north side of the Goldstream River.

Economic results were obtained from most of the holes with the

program considerably expanding the drill proven ore reserves and

adding significantly to the life of the mine. An in-house ore reserve

calculation has been completed by Bethlehem but is not part of this

report. The deep holes on the deposit represent a complete

stratigraphic section through lower portions of Hamill Group rocks,

all of the Badshot (and Mohican) Formations and all of the Lower Index

Formation to just below the Goldstream orebody and may prove quite

useful for regional stratigraphic correlations.

TABLE OF CONTENTS

Summary Introduction Location and Access Physiography and Vegetation Claim Status History and Previous Work Regional Geology Property Geology Mine Stratigraphy and Mineralization Exploration Program Diamond Drilling

6-94-1 6-94-2 6-94-3 G-94-4 6-94-5 G-94-6 G-94-7 G-94-8 G-94-9 G-9 4- 10 G-9 4-1 1

Conclusions Statement of Costs Certificate of Qualifications

Wesley Raven, P.Geo1 Bibliography

1 1 2 3 3 4 5 6 11 13 16 16 17 17 18 18 19 19 20 20 21 22 23

LIST OF FIGURES

Figure 1 Location Map Following Page 1 Figure 2 Claim Map Following Page 3 Figure 3 Tectonic Map Following Page 5 Figure 4 Plan View 1994 Drilling In Pocket Figure 5 Diamond Drilling West Side Intersections In Pocket Figure 6 Diamond Drilling East Side Intersections In Pocket Figure 7 Diamond Drilling Central Intersections In Pocket

LIST OF TABLES

Table 1 Drillhole Location Information Table 2 Drillhole Assay Information

LIST OF APPENDICES

Appendix 1 Claim Information Appendix 2 Analytical Results Appendix 3 Drillogs

Page 14 Page 15

INTRODUCTION

This report describes the details of the recently completed ore

reserve definition drilling program conducted on the Goldstream Mine

orebody. The purpose of the program was to delineate the orebody

boundaries below 350 metres elevation thus upgrading the

classification of reserves from Geologically Inferred to Drill

Indicated.

The program began on July 17 , 1994 and was completed on September 17, 1994 and consisted of 6 diamond drill holes totalling 2638.42

metres (8654 ft.). Favorable results from this initial work led to an

additional program beginning October 2, 1994 and finishing on November

26, 1994 consisting of 5 holes totalling 2588.11 metres. In summary

11 diamond drill holes totalling 5226.53 metres (17,143 ft.) were

completed on the orebody on the north side of the Goldstream River.

LOCATION AND ACCESS

The property is located along the Goldstream River Valley about

70 kilometres north of Revelstoke, British Columbia, and stretches for

13 km east of Highway #23 at 51°38'N Latitude, 118"26'W Longitude, on

riTS 62 M/9W, 1OE (Figures 1 and 2). Access is approximately 90 km by

paved Highway #23 which links Revelstoke with Mica Dam, and by 13 km

of good gravel road from the junction to the Goldstream Mine.

Relief in the project area varies from 650 m ASL in the

Goldstream Valley to 1700 m on ridge crests. Treeline is at 1770 m.

P A C I F I C

O C E A N BETHLEHEM RES CORP. & GOLDNEV RES INC

GOLDSTREAM PROPERTY

LOCATION MAP Revelstoke Mining Division

British Columbia NTS 82M/9W & 10E

December 1994 xY3

- 0 100 200 kilomeires - 0 100 miles

- 2 -

. . Mature stands of cedar, hemlock, balsam and spruce cover parts of the

property.

PHYSIOGRAPHY AND VEGETATION

Climate is that of the Interior Rain Belt with temperatures

ranging between -15C and +30C. Annual precipitation averages 1.15 m,

of which more than half falls as snow. Elevation varies from 660 m

above sea level at the Goldstream River to over 1100 m up the valley

slopes.

The Goldstream Valley is "U" shaped with the central portion

covered by thick glacial boulder, till and sand. Overburden decreases

with increased elevation up the valley slopes, where locally derived

material prevails.

Vegetation consists of mixed stands of mature cedar, hemlock and

balsam and spruce with logged areas covered by dense undergrowth of

alder and devil's club. Large portions of the property have now been

logged and are covered by second growth conifers and alder.

- 3 -

CLAIM STATUS

The Goldstream property consists of 92 claims totalling 328 units

covering 7909 hectares situated in the Revelstoke Mining Division.

(Figure 2). All claims are the subject of a joint venture between

Bethlehem Resources Corp and Goldnev Resources Inc.

A detailed list of relavent claim information can be found in

Appendix 1. The expiry dates listed do not include any assesment

credit that can be applied from the work described in this report.

HISTORY AND PREVIOUS WORK

The Goldstream area has had a long history of mineral exploration

dating back to the 1860's. Two of the better known copper-zinc-silver

deposits, the Montgomery and the Standard were both discovered in the

late 1890's and have been worked on intermittently since then.

The Goldstream Mine was discovered in 1972 when mineralized

copper bearing float was discovered during construction of a logging

road. The deposit was staked in 1973 by local prospectors Frank King

and Gordon Bried and in 1974 hand pitting and x-ray drilling had

outlined a near surface sulphide zone. Noranda Exploration Co. Ltd.

optioned the property in late 1974 and by late 1975 50 drill holes had

outlined a deposit of 3.175 million tons grading 4.49% copper and

L

/ I - -

I I \

0

BETHLEHEM RESOURCES CORP. GOLDNEV RESOURCES INC.

GOLDSTREAM PROJECT

CLAIM MAP Revelstoke Mining Division

British Columbia NTS 82M/9 dt 10

IATE: SEPT. 1994 fXE: COLDCLMS.DWC

- 4 -

3.14% zinc. The mine was officially opened in 1983 and operated for

approximately 7 months before closing due to prevailing low metal

prices.

*.

a .

In 1989 Bethlehem Resources Corp. and Goldnev Resources Inc.

acquired the property from MacLaren Forest Products a wholly owned

subsidiary of Noranda Inc. as a 50:50 joint venture with Bethlehem

being the operator of the project. The partners flew an airborne

geophysical survey over the property in 1990 and in 1991 conducted

extensive ground surveys over most of the property culminating in a

diamond drilling program consisting of 42 drill holes totalling

8,012.8 m (26,282 ft.)

Since then minor drill programs have been completed in 1992 and

1993 to better define the ore reserves in developing parts of the

mine from both underground and surface programs.

REGIONAL GEOLOGY

The regional geology of the Goldstream area has been described

in detail by several authors: Gunning (1928), Wheeler (1965), Gibson

(1978-86), Hoy et a1 (1977, 1984) and Read and Brown (1981-89). The

regional geology consists of metasedimentary and lessor metavolcanic

rocks of Late Proterozoic to early Paleozoic age that are part of the

Selkirk Allochthon. These rocks have been subsequently complexly

- 5 -

deformed and intruded by many plutonic bodies of probable Cretaceous

age. (Figure 3 ) .

The Selkirk Allochthon is a composite terrain comprised of at

least four major fault bounded slices, one of which is the Goldstream

slice. It was emplaced from west to east over the core and mantling

gneisses of the Monashee Complex along the Monashee decollement and

east dipping Columbia River normal fault during Mesozoic to Eocene

time. The Monashee decollement separates the gneisses fromthe Shuswap

Metamorphic Complex to the west while the Columbia River Fault

separates the Selkirk Allochthon fromthe underlying Monashee Complex.

Rocks within the Selkirk Allochthon have undergone at least three

phases of deformation. Phase 1 is believed to have inverted much of

the Goldstream slice possibly as the underlimb of a major recumbent

nappe. Large tight isoclinal to recumbent folds with strong axial

planer foliation and northwest trending fold axes define Phase 2

folding. A third phase of deformation is evidenced by kink folds,

crenulation cleavages and broad, upright, open folds.

PROPERTY GEOLOGY

The project area is underlain by complexly deformed

metasedimentary and metavolcanic rocks of probable early to middle

Paleozoic age. These rocks belong to the metavolcanic phyllite

-52"

-51"

--O- Selkirk Fan Axis

0 Zn-Pb Occurrence

A Cu-Zn Occurrence

0 20 40

kilometres

BETHLEHEM RES CORP. & GOLDNEV RES INC.

Figure 3

GOLDSTREAM PROPERTY REGIONAL

TECTONIC MAP Revelstoke Mining Division

British Columbia NTS 82M/9W & 1 OE

December 1994 xY3

- 6 -

division (Lardeau Group) of the Omenican Crystalline Belt (Hoy, 1984)

and are tentatively correlated with lesser deformed stratigraphy of

the Kootenay Arc to the south. These rocks are interpreted to be

miogeosynclinal rocks deposited in a transitional zone between

platformal quartzites, and deeper water thin bedded impure carbonates,

dark carbonaceous and calcareous phyllites, with interbedded

metavolcanics. Increased carbonaceous material probably indicates

restricted basinal conditions with metavolcanic intervals indicative

of a rifting environment.

The Goldstream property is underlain by a 700 metre thick

succession of metasedimentary rocks with a minor metavolcanic

component, herein called the Goldstream mine stratigraphy. These

rocks have an apparent west-northwest strike, along the Goldstream

Valley, dip 30"-35O to the north and plunge to the northeast.

Regional correlations indicate the entire sequence to be overturned.

These rocks belong to the Index Formation of the Lower Paleozoic aged

Lardeau Group.

MINE STRATIGRAPHY AND MINERALIZATION

The oldest rocks structurally underlying the Goldstream Mine area

are correlated with the Lower Cambrian Hamill Group and consist mostly

of metasedimentary siliceous chlorite - sericite phyllite and

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rhythmatically bedded quartzite. Graded bedding in this sequence

suggests that it is overturned.

The next unit is a carbonate rich package of rocks correlated

with the Lower Cambrian Badshot Formation. It is comprised largely of

light grey thin bedded argillaceous limestone and thicker bedded grey

marble with minor interbedded chlorite - biotite - sericite phyllite. There is a possible siliceous core within the Badshot Formation

observed in some of the 1994 drill holes though this feature was not

recognized in all of the recent holes. Local sections of impure,

coarsely crystalline to fine grained, dense porcelainous dolomite was

noted in a few of the drill holes particularly along the western ore

boundary.

The next sequence of rocks belong to the Lower Index Formation

of the Lower Paleozoic aged Lardeau Group. This is the typical

stratigraphic sequence observed at the Goldstream Mine as the Hamill

Group and Badshot Formation are only observed in the deeper holes

drilled on the deposit, generally north of the Goldstream River.

It appears to be conformable with the Badshot Formation and has

been subdivided into several sub units, one of which hosts the

Goldstream Mine. A general description of the sub units is as follows.

- 8 -

The structurally highest unit consists of chlorite - sericite - biotite phyllite that has variable degrees of silicification. The

unit is well foliated and locally quite broken and fractured along

foliation planes when sericite content is high. The unit is much more

comNtent when strongly silicified.

This unit is underlain by a thick succession of dark brown to

black well banded variably calcareous and carbonaceous biotite - chlorite phyllite referred to as the Dark Banded Phyllite. A notable

feature in this unit is the presence of a tan or bronze coloured

biotite more prevalent in areas of Phase 3 deformation and in

irregular zones within portions of the unit. In the northern most

holes completed on the deposit this Dark Banded Phyllite appears to

have some facies changes as calcareous rocks very similar in

appearance to the Badshot Formation were seen in the upper portion of

the "Dark Banded Phyllite Sequence" structurally below the Chlorite - Sericite - Biotite Phyllite.

The next sequence of rocks can be considered to be the ore

sequence that encloses the Goldstream Mine. It begins with the Garnet

Zone, a complex interval consisting of Dark Banded Phyllite and

Chlorite - Sericite Phyllite, with the Dark Banded Phyllite being the most prevalent unit. The zone is commonly contorted, sheared, broken,

and quartz veined. It contains variable concentrations of rounded

pinkish brown garnets from 1 - 35% and banded chert in concentrations

- 9 -

of 1-20%. The contact with the overlying Dark Banded Phyllite is

usually broken and faulted with graphitic gouge and abundant quartz - carbonate tension gash infillings. It includes some dark grey to

greasy black chlorite rich graphitic and calcareous quartzite layers.

Sulphide mineralization is comprised largely of pyrrhotite as fine

disseminations and foliation parallel streaks averaging 2 - 5 % but is

locally semi-massive to 35-40%. Very minor chalcopyrite is intergrown

with the pyrrhotite, usually < 1%.

Below the Garnet Zone is a variable sequence of rock units

comprised largely of siliceous Grey - Green Phyllite with lessor limestone and minor Dark Banded Phyllite. These units have a variable

thickness and degree of alteration which is usually silica. In the

drillogs for this report a division called the Hanging Wall Sulphide

Zone has been created to mark the beginning of significant sulphide

concentrations generated by the mineralizing event that produced the

Goldstream Mine orebody. Mineralization in this unit is usually fine

disseminations of pyrrhotite and chalcopyrite with occasional minor

sphalerite and rare galena grading to stringers and local small

sections of semi-massive sulphide with sulphide content increasing

when approaching the massive sulphide layer.

The Ore Zone can be divided into three sub units (Mitchell 1989)

those being fragmental ore, banded massive sulphide and disseminated

ore, and contorted disseminated ore. The fragmental ore consists of

- 10 -

a matrix of massive sulphide material supporting clasts of grey to

white quartz, banded massive sulphide material, and wall rock

fragments. The matrix commonly shows flow or shear banding as a result

of remobilization during deformation. Banded massive sulphide and

disseminated ore consists of alternating lamellae .or bands of massive

sulphide and quartz carbonate material commonly folded and disrupted.

The contorted disseminated ore consists of highly contorted and

brecciated banded ore along with stringers and lenses of remobilized

sulphides and can be equated to the Hanging and Footwall Sulphide

Zones.

The massive sulphide layer is generally 1 to 3 m thick but can

be up to 5.5 m thick and is the highest grade component of the ore.

It is typically comprised of 20 to 40% pyrrhotite, 15 to 25%

chalcopyrite, 10 to 15% sphalerite and rare galena. Gangue comprises

10-25% and is mostly silica.

Underlying the Ore Zone is the Footwall Disseminated Zone which

has weak disseminated and occasional disseminated stringer

mineralization corresponding to the contorted disseminated ore. This

unit is quite variable in thickness and is not always present or was

not recognized as such.

Underlying this Ore Zone section is either the footwall limestone

that is similar to that within the Badshot Formation or variable

- 11 -

Chlorite - Sericite Phyllite or Micaceous Quartzite that grades into the footwall marble or limestone. . EXPLOFCATION ZROGRAM

The 1994 exploration program completed at the Goldstream Mine,

operated by Bethlehem Resources Corp of Vancouver, B.C., consisted of

a two phase diamond drilling program. The purpose of the initial

program was to upgrade the ore reserve classification below 350 metres

elevation from Geologically Inferred to Drill Indicated. Prior to the

commencement of this work there were no holes beyond the western ore

boundary below the 400 metre panel, no intersections in the 300 metre

panel, 1 in the 250 metre panel, 1 in the 200 metre panel and 2 in the

150 metre panel.

The initial drilling program commenced on July 17, 1994 and was

completed on September 17, 1994, it consisted of 6 diamond drill holes

totalling 2638.42 metres (8654 feet). Favorable results from this

first program led to a second drill program to further delineate the

ore reserves between 0 - 250 metres elevation to the Drill Indicated Category. The second program began on October 2, 1994 and was

completed on November 26, 1994, it consisted of 5 holes totalling

2588.11 metres (8489 ft). In summary 11 holes totally 5226.53 metres

(17,143 ft.) were completed on the orebody.

- 12 -

The drilling contracts were awarded to Olympic Drilling and

Consulting Ltd. of New Westminster, B.C. The first phase of drilling

was conducted with a Longyear 38 skid mounted drill, the second phase

began with the same drill rig for the first hole then a Longyear 56

skid mounted drill was used to complete the final four holes. Core

size was NQ2 for all holes except G-94-4 and G-94-5 which were a

combination of NQ2 and BQ. It was necessary to reduce to the small

core size in hole 4 because of severe ground conditions resulting in

the NQ rods getting stuck in a fault zone. Hole 5 was drilled to a

depth beyond the capabilities of the Longyear 38 to complete the hole

with the larger NQ2 core size, hence bringing in the larger drill for

the second phase of the program.

Virtually all of the holes were collared as vertical holes with

consistent flattening and deviation to the south. This pattern was

observed in the 1991 drilling program with the 1994 program attempting

to plan the amount of deviation in a hole and thus determine the

collar location for a given hole. All holes were surveyed for

deviations in azimuth and inclination utilizing a single shot Sperry-

Sun. The mineralized intercepts were split and sent to Acme Analytical

Laboratories in Vancouver, B.C. for analysis of gold, silver, copper,

lead and zinc.

- 13 -

DIAMOND DRILLING

All of the holes completed during both phases of the program

encountered the typical stratigraphic succession described previously

in the section on stratigraphy and mineralization. The only exception

is the southernmost holes which collared in the Badshot formation

below the Hamill Group rocks. The following discussion on individual

holes will be limited to the mineralized intercepts, details of the

various lithologies can be obtained from the drillogs. Geology on the

drill sections has been simplified for purposes of clarity.

A complete list of hole collar co-ordinates is presented in Table

1, a list of significant intersections is presented in Table 2 -Assay

Intersections. All depth of intersections are at the hanging wall - massive sulphide contact and are in metres above sea level. A detailed

list of assay intersections and the individual sample results can be

found in Appendix 2 - Analytical Results.

In Table 2 the true thickness of the mineralized intercepts was

calculated using an angle of 2 0 degrees.

- 14 -

G-94-1

TABLE 1

DRILL HOLE INFORMATION

3099.26 15856.02 665.52 371.04

I ~~

Hole No. I Northing I Easting I Elevation (m) Length (m)

6-94-2

G-94-3

3119.33 15926.48 664.59 392.07

3089.95 15952.30 665.35 382.62

G-94-4

G-94-5

G-94-6

3220.20 15979.11 666.89 451.83

3512.64 16246.72 709.73 672.87

3077.96 15986.87 666.11 367.99

G-94-7

6-94-8

6-94-9

6-94-10

3304.00 16024.00 675.00 498.48

3279.00 16089 .OO 675.00 503.05

3522.00 16187.00 710.00 639.02

3585 .OO 16032.00 690.00 561.28

6-94-11 3123.00 15878.00 665.00 386.28

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TABLE 2 DRILL HOLE ASSAY INFORMATION

Interval (rn) Length True Thickness

0-94-11 364.44 368.81 4.37 4.11

C-94-11 368.81 370.47 1.66 1.56

- 16 -

6-94-1

This hole was collared on the west side of the orebody to intersect the

300 m panel with the actual intersection at 310m ASL. A thick and well

mineralized hanging wall sulphide zone was present from 351.83 to 358.49 m

with assays ranging from 0.457% - 2.551% copper over various lengths. The entire zone averaged 1.322% copper and 0.84% zinc over 6.66 m. The 2.87 m

massive sulphide zone, to 361.36 m, contained significant sulphides but

unfortunately these were mostly pyrrhotite, the zone averaged 2.017% copper

and 2.89% zinc over a core thickness of 2.87 m (2.70 m true) including

3.785% Cu and 2.35% Zn over 1.05 m (0.99 m true). No footwall mineralization

was observed with the hole bottoming in limestone at a depth of 371.04 m.

6-94-2

This hole was collared on the west side also intended to test the 300

m panel and intersected the west-central portion of the orebody at an

elevation of 285 m ASL. It was among the best intersections obtained from

this program. A moderate hanging wall was present over 3.40 m with the

lowermost sample assaying 1.704% Cu over 1.47 m (1.38 m true). A thick

section of massive sulphide was encountered from 381.65 to 387.28 m which

averaged 5.450% Cu and 4.05% Zn over 5.63 m (5.29 m true) with a combined

intersection of 4.675% Cu and 3.28% Zn over 7.10 m (6.67 m true). Within

this interval is a small section of limestone from 386.28-386.95 m

separating a small section of massive sulphide from the main bulk of the

zone. No footwall mineralization was observed with the hole bottoming in

limestone at a depth of 392.07 m.

- 17 -

G-94-3

This hole was planned to intersect the 300 m panel and intersected the

central portion of the orebody at 292 m ASL. A weakly to moderately

mineralized hanging wall sulphide zone was intersected over 5.78 m with the

lower portion averaging 0.764% Cu and 0.58% Zn over 2.00 m (1.88 m true).

Two small lenses of massive sulphide separated by 0.52m of altered phyllite

comprised the ore zone averaging 5.027% Cu and 2.29% Zn over 1.32 m (1.24 m

true). A 0.75 m (0.70 m true) footwall intersection assayed 1.884 % Cu and

0.10% Zn. The entire combined interval averaged 2.353% CU and 1.05% Zn over

4.07 m (3.82 m true).

G-94-4

This hole was also drilled on the west side of the ore body to test the

250 m panel with the actual intersection at 233.5 m ASL. Drilling

difficulties required reducing the core size from NQ2 to BQ resulting in

greater flattening of the hole than was estimated.

The hole contained a fairly well developed hanging wall over 5.05 m

with the lower 2.20 m (2.07 m true) averaging 1.418% Cu and 0.19% Zn. The

ore zone intersection consisted of intercalated massive and stringer

sulphides averaging 5.046% Cu and 0.91% Zn over 3.38 m (3.18 m true). The

combined intersection is 3.615% Cu and 0.62% Zn over 5.58 m (5.24 m true).

- 18 -

G-94-5

This hole is the deepest hole completed on the property to - date ,.. and

represents a significant stepout down plunge. The hole deviated more than

was estimated as it was hoped to intersect the centre of the orebody in the

50 m panel. The actual intercept was along the eastern ore boundary at an

elevation of 83 m ASL.

. - ..

Weak hanging wall mineralization was encountered over 2.38 m (2.24 m

true) averaging 0.646% Cu and 0.49% Zn. Strong disseminated and massive

sulphides comprise the ore zone which assayed 3.970% Cu and 3.35% Zn over

1.80 m (1.69 mtrue). Aweaklymineralized footwall zone did not contain any

significant assays. The hole ended in limestone at a depth of 672.87 m.

G-94-6

This hole was collared on the east side of the deposit to intersect the

300 m panel. The actual intercept was along the eastern ore boundary at an

elevation of 309 m ASL. The hole was similar to

G-94-3 with a fairly strong disseminated sulphide zone over 4.14 m (3.89 m

true) with the best intersection assaying 2.107% Cu and 0.82% Zn over 3.14

m (2.95 m true). A narrow massive sulphide/quartz vein over 0.40 m (0.38 m

true) represents the true massive sulphide interval which assayed 4.284% Cu

and 3.86% Zn. A weak footwall zone was present over 2.04 m (1.92 m true).

The combined zones assay 2.038% Cu and 0.91% Zn over 4.73 m (4.44 m true)

including 3.512% Cu and 2.10% Zn over 1.03 m (0.97 m true).

- 19 -

6-94-7

Hole 94-7 was the first hole completed in the second phase of the

program collared on the west side of the deposit north of G-94-4 to test the

200 m.pane1. The actual intercept was at 203 m ASL on the west side of the

orebody. A weak hanging wall zone was intersected over 3.50 m with no

significant assays except at the last sample above the main ore zone which

assayed 1.153% Cu and 0.24% Zn over 0.57 m (0.54 m true).

4. .. .,

The ore zone is comprised of intercalated massive, semi-massive,

disseminated and stringer sulphides. There is a possible fold repeat in the

central portion of the ore zone with strong mineralization above and below

this area of weak sulphides. The hole returned an excellent intersection

assaying 6.594% Cu and 1.67% Zn over 4.19 m (3.94 m true). Weak footwall

mineralization is present over 0.66 m (0.62 m true) with no significant

assays. The hole bottomed in limestone at a depth of 498.48m

6-94-8

This hole was collared in the central portion of the orebody to test

the 200 m panel, intersecting at 189 m ASL. There was a very weak hanging

wall zone in silicified limestone with no significant assays. The ore zone

is similar to 6-94-7 in that there is a core of weak sulphides with massive,

disseminated, and stringer sulphides above and below this core. The ore zone

assayed 4.345% Cu and 1.65% Zn over 5.15 m (4.84 m true). There is a well

developed footwall zone over 3.76 m (3.53 m true) with assays ranging from

0.180% - 1.472% CU.

- 20 -

G-94-9

Hole 94-9 represents the other deep hole intended to test the 0 to 50

m panel actually intersecting at 129 m ASL as the hole deviated more than

was anticipated. It was collared on the edge of the presumed western ore

boundary, actually intersecting the centre of the deposit. It appears that

holes drilled through a thick section of the siliceous Hamill Group rocks

deviate strongly in the upper portion of the hole compounding the deviation

at depth when the hole was expected to flatten out.

There was virtually no recognizable hanging wall zone in this hole

except for minor silicification near the ore zone. The ore zone is comprised

of disseminated to massive sulphides assaying 2.915% Cu and 2.08% Zn over

1.15 m (1.08 m true). A strongly silicified, weakly mineralized footwall

zone is present with assays ranging from 0.019% -0.531% Cu.

G- 9 4 - 10 Hole 94-10 was planned as a significant step-out on the west side of

the ore zone to define some limits on the mineralization intersected in

holes 94-4 and 94-1. As both these hole intersected above average ore

grades, information was needed to determine how far these results could be

projected to the west. The hole was planned to test the 150 m panel

intersecting at 146.5 m ASL. An attempt to minimize the deviation of holes

penetrating a thicker section of Hamill Group rocks was tried on this hole

by orientating the hole 5 degrees to the north (-85 degrees) instead of

drilling a vertical hole. This seems to have worked quite well as the hole

- 21 -

did begin to flatten out in the Hamill Group rocks but was essentially

vertical when it reached the Badshot Formation, from there the deviation was

more typical of what was expected.

The hole did not intersect any economic sulphide zones with

disseminated and stringer sulphides encountered over 4.02 m (3.78 m true)

which assayed 0.139% Cu and 0.34% Zn. A narrow (0.55mtrue) graphitic shear

lies directly below this zone followed by a 0.75 m (true) footwall zone

neither of which returned any significant assays.

G-9 4-1 1

The last hole of the program was drilled in the area of G-94-1 to see

if the low copper values returned from that hole were an isolated

occurrence. Hole 94-1 had a reasonably thick massive sulphide interval but

the grade was disappointing and the current mining plan indicated that the

boundary was west of that indicated by hole 94-1.

Hole 94-11was successful in expanding the western ore boundary further

than was initially indicated by hole 94-1. The hole intersected a thick

hanging wall zone similar to G-94-1 which assayed 1.602% Cu and 1.38% Zn

over 4.37 m (4.11 m true). The massive sulphide ore zone assayed 6.438% Cu

and 4.29% Zn over 1.66 m (1.56 m true). Aweak footwall zone did not return

any significant assays.

- 22 -

CONCLUSIONS 4 .< r. . ,.. . . ,.

; , . , . . (

;Ls

An ore reserve definition drilling. program was completed at the .

Goldstream Mine, Revelstoke, B.C. to upgrade Geologically Inferred Resertes

to Drill Indicated Reserves and to refine the eastern and western ore

boundaries. Previous drilling in 1991 had indicated that the ore body

continued underneath the Goldstream River to the north but these holes were

widely spaced and did not define the eastern and western ore limits.

The area of interest in this program was from the 300 m panel down to

the 0 m panel. The information from this work will be used to aid in

determining future development planning and calculating a new ore reserve

for the mine.

The program was successful in meeting all of its objectives with 11

holes totalling 5226.53 m (17,143 ft.) completed from July 17, 1994 to

November 26 , 1994. In house ore reserve calculations have been completed but are not part of this report.

- 23 -

STATEMENT OF COSTS

Diamond Drilling (5,226.52 metres, 17,143 ft.) Includes mob/demob, materials, etc.

Wages W. Raven 111 days @ $350/dav L. Lewis 3 days @ $275/day

Equipment Rental Truck Computer Sperry Sun

Room and Board 600 days @ $30.69/day

Assaying

Surveying

Fuel Diesel 22,178.9 litres @ $0.3l/litre Gas 504.98 litres @ $0.42/litre

Travel and Miscellaneous Expenses

Report and Drafting

TOTAL :

$332,362.60

38,850.00 825.00

3,900.00 925.00

8,909.59

18,416.00

2,723.85

825.26

6,815.46 212.09

3,840.27

2,115.99

.$ 421,441.11

The above total does not include GST.

CERTIFICATE OF OUALIFICATIONS

I, Wesley D.T. Raven, of #lo8 - 1720 West 12th Avenue, Vancouver, British Columbia, hereby certify:

1.

2.

3 .

4.

5.

6.

7.

8 .

I am a graduate of the University of British Columbia (1983) and hold

I am presently retaiied as a consulting geologist lkfth OreQuest Consultants Ltd. of #306 - 595 Howe Street,, Vancouver, British Columbia.

I have been employed as an exploration geologist on a full time basis since 1983.

I am a Fellow of the Geological Association of Canada.

I am a Professional Geologist registered with the Association of Professional Engineers and Geoscientists of British Columbia.

The information contained in this report is based on information listed in the Bibliography, and from managing and performing the 1994 exploration program.

Neither OreQuest Consultants Ltd. nor myself have or expect to receive direct or indirect interest in the Goldstream Project nor in the securities of Bethlehem Resources Corp. or Goldnev Resources Inc.

I consent to and authoritze the use of the attached report and my name in the Company's Prospectus, Statement of Material Facts or other public document, providng the report is used in its entirety or any summary thereof is approved by the author.

a B.Sc. degree in geology. . . . -

, .

Wesley D.T. Raven, P.Geo1.

DATED at Vancouver, British Columbia, this 22nd day of December, 1994.

BIBLIOGRAPHY

BROWN, R.L., LANE, L.S., PSUTKA, J.F., AND READ, P.B. 1983: Stratigraphy and Structure of the Western Margin of-the Northern

Selkirk Mountain: Downie Creek Map Area, British Columbia; in Current Research, Part A; Geol. Surv. Can., Paper 83-lA.

BROWN, R.L., TOPPETT, C.R., AND LANE, L.S. 1977: Stratigraphy, Facies Changes, and Correlations in the .Northern

Selkirk Mountain, Southern Canadian Cordillera; Can. Jour:Earth Sci., Vol. 15, pp. 1129-1140.

CAMPBELL, I. 1991: Report of Exploration on Murder Creek Project, Rain Property,

Revelstoke Mining division, for Bethlehem Resources Corp., October 25, 1991.

1991: Report on Surface Exploration, Goldstream Project, Revelstoke Area, B.C., Internal Report, Goldnev Resources Inc.

1992: Personal Communication.

CANADIAN MINES HAND BOOK, 1992-93

CAVEY, G., RAVEN, W. 1992 : Report of Diamond Drilling on Murder Creek Project, Rain Property,

Revelstoke Mining Division, October 22, 1992.

CHENI GOLD MINES 1991: July 30, 1991 Press Release.

DEVLIN, W.J. 1988: Stratigraphy and Sedimentology of the Hamill Group in the Northern

Selkirk Mountains, B.C.: Evidence for latest Proterozoic-Early Cambrian Extensional Tectonism; Can. Jour. Earth Sci., Vol 26, pp. 515-533 (1989).

FOX, J.S. 1984: Besshi-Type Volcanogenic Sulphide Deposits - A review, CIMM V77

#864, p. 57-68.

GEORGE CROSS NEWSLETTER 1992: No. 202 (1992), October 22, 1992.

GIBSON, G.

1994: Geological, Geochemical, and Drilling Report on the Natal 1,2, Kate, Rick 1,2,3, Brew 8,9,12,15, and 16 Mineral C l a i m s , Revelstoke Mining Division, July 4, 1994

GIBSON, G., HUGHES, B.B., AND BRADISH, L.B. 1977: Geological, Gebchemical and Geophysical Survey, Mars 1 to 4, Key

3 to 5, 9, 16.;- 17, 20, 21, Standard 1 to 4, and Kelly 1; B.C. Min. En. Min. Pet. Res., Assessment Report 6187.

H0Y, T. 1989 : Geology of the Goldstream Area; B.C. Min. en. Min. Pet. Res.,

Bulletin 71.

H0Y, T., GIBSON, G., AND BERG, N.W. 1984: Copper-Zinc Deposits Associated with Basic Volcanism, Goldstream

Area, Southeastern British Columbia; Econ. Geol. , Vol 79, pp. 789- 814.

LANE, L.S. 1977: Structure and Stratigraphy, Goldstream River-Downie Creek Area,

Selkirk Mountains, B.C.; Unpublished M.Sc. Thesis, Carleton University, Ottawa, Ontario.

LEBEL, J. L. 1992: Report on Bore Hole Electromagnetic Survey, Murder Creek Project,

Rain Property, Revelstoke Mining Division, December 7, 1992.

McARTHUR, G., RAVEN, W., LEWIS, L. 1991: Diamond Drilling on the Goldstream and Jenkins Project Area,

Revelstoke Mining District, B.C.

MATHIESON, G.A., AND LEWIS, T. 1980: Geological, Geophysical and Geochemical Report on the SOC 1 and 2

Mineral Claims, Revelstoke Mining Division; B.C. Min. En. Min. Pet. Res., Assessment Report.

MITCHELL, M.A. 1989: Geological Report on the Goldstream Copper - Zinc Deposit,

Revelstoke Mining District, B.C., August 8, 1989

Columbia River Fault Zone: Southeastern Margin of the Shuswap and Monashee Complexes, Southern B.C.; Can. Jour. Earth Sci., Vol 18,

READ, P.B., AND BROWN, R.L., 1981:

pp. 1127-1145.

VANCOWER STOCKWATCH, WESTERN EDITION 1992: Bethlehem Resources Corp., September 23, 1992.

Bethlehem Resources Corp., October 21, 1992. Goldnev Resources Inc., October 16, 1992

WHEELER, J.O. 1965: Big Bend Map Area, B.C.; Geol. Surv. Can., Paper 64-32.

WILD, C.J. 1990: Geological and Geochemical Report on the Rain 1-17 Mineral Claims.

Assessment Report.

WILD, C.J. AND ADAMSON, R.S. 1990: Drilling Report on the Keystone Property, Revelstoke Mining

Division; B.C. Min. En. Min. Pet. Res., Assessment Report.

WILD, C.J. AND ZERB, W.M. 1992: Drilling report on the Goldstream Mine, Revelstoke Mining

Division, November 30, 1992

APPENDIX 1 CLAIM INFORMATION

LAND FACTS P a g e A o f 3

GOLDSTREAM I DATE REVISED: SEP 16 ,1994

UNITS: 328 CLAIMS: 92 AREA(ha): 7909

RECORD DATE 1 CLAIM TENURE AREA(ha

20.9 20 .9 20 .9 2 0 . 9 2 0 . 9

EXPIRY DATE

247851 248511 248552 248512 248513

1 1 1 1 1

OCT 2 6 / 8 1 -

OCT 26/99 SEP 06/99 L MAY 23 /99 SEP 06/99 L SEP 06/99 L

GS #1 FI PAT 1 PAT 1 FI PAT 2

SEP 0 6 j 7 7 MAY 23 /74 SEP 0 6 / 7 3

/PAT 3 SEP 06173

248514 248516 248517 248518 248519

SEP 06 /73 OCT 1 1 / 7 3 OCT 1 1 / 7 3 OCT 1 1 / 7 3 OCT 1 1 / 7 3

SEP 0 6 / 9 9 T. PAT 4 PAT 5 PAT 6 PAT 7 PAT 8

20 .9 2 0 . 9 2 0 . 9 20 .9 20.9

2 0 . 9 20.9 20 .9 2 0 . 9 2 0 . 9

- OCT i i j 9 3 L OCT 1 1 / 9 9 L OCT 1 1 / 0 0 OCT 1l)OO

PAT 1 0 PAT 11 PAT 1 2 r PAT 1 3

OCT 1 1 / 7 3 OCT 1 1 / 7 3 OCT 1 1 / 7 3 OCT 1 1 / 7 3 OCT 1 1 / 7 3

248520 248521 248522 2.48523 248524

248525 248526 248527

248529 248528

OCT 1 1 / 0 0 OCT 1 1 / 0 0 OCT 11 /00 OCT 1 1 / 0 0 OCT 1 1 / 0 0

OCT 1 1 / 7 3 OCT 1 1 / 7 3 OCT 1 1 / 7 3 OCT 1 1 / 7 3 OCT 1 1 / 7 3

PAT 1 4 PAT 1 6 PAT 1 7 PAT 1 8 PAT 1 9

OCT 1 1 / 0 0 20 .9 20 .9 2 0 . 9 2 0 . 9 20 .9

20 .9 2 0 . 9 20 .9 20.9 20.9

OCT i i j 9 9 L OCT 1 1 / 9 9 L OCT 1 1 / 9 9 L OCT l l j 9 9 L

248530

248532 248533 248534

248531 OCT 1 1 / 7 3 OCT 1 1 / 7 3 OCT 1 1 / 7 3 OCT 1 1 / 7 3 OCT 1 1 / 7 3

PAT 2 0 PAT 2 1 PAT 22 PAT 23 PAT 24

OCT 1 1 / 9 9 L OCT 1 1 / 9 9 L OCT 11 /99 L OCT 1 1 / 9 9 L OCT 11 /99 L

1 1 1 1 1

2 0 . 9 20.9 20.9 2 0 . 9 20 .9

MAY 23/00 MAY 23 /99 MAY 23/99 MAY 23/00 MAY 23 /00

PAT 2 5 PAT 26 PAT 27

PAT 29 PAT 28

248545 248546 2.18547 248548 248549

248550 248551 248553 248554 248555

MAY 23 /74 ~GLY 23/74

23/74 MAY 23/74 MAY 23 /74

MAY 23/74 MAY 23 /74 SEP 03 174 SEP 03 /74 SEP 03/74

1 1 1 1 1

1 1 1 1 1

-

- - M I N I 1

PAT 3 0 PAT 31 PAT 32 PAT 33 PAT 34

20 .9 2 0 . 9 20 .9 20.9 2 0 . 9

20 .9 20.9 2 0 . 9 20 .9 20 .9

MAY 23 /00 MAY 23/00 SEP 03/99 SEP 03/99 SEP 03/99

SEP 0 3 / 9 9 SEP 03 174 SEP 03 /74 SEP 03/74 SEP 03 /74 OCT 2 3 / 7 4

PAT 35 PAT 3 6 PAT 37 PAT 38 PAT 39

248556

248558 248559 248568

D WITH11

248557 SEP 03199 SEP 0 3 / 0 0 SEP 03joo OCT 23 / 00

LEASE 4 5 1 ; NO ASSESS NT REQUIRED

LAND FACTS P a g e L o f L

GOLDSTREAM: I DATE REVISED: SEP 16 ,1994

I CLAIMS: 92 UNITS: 328 AREA(ha): 7909

I CLAIM TENURE INIT' AREA ( h a RECORD DATE EXPIRY DATE

20 .9 20.9 20 .9 20.9 20.9

OCT 23/74 OCT 23/74 OCT 23/74 OCT 23/74 OCT 23/74

OCT 23/00 OCT 23/00 OCT 23/00 OCT 23 /00 OCT 23/00

PAT 4 0 PAT 4 1 PAT 42 PAT 43 PAT 44

20 .9 20 .9 20.9 20.9 2 0 . 9

OCT 23 /74 OCT 2 3 / 0 0 PAT 4 5 PAT 46 PAT 47

PAT 49 PAT 4 a

OCT 2 3 j 7 4 OCT 2 3 / 7 4

OCT 2 3 j 9 9 OCT 23/99 OCT 23 /99 OCT 2 3 j 7 4

OCT 23/74 OCT 23199

20 .9 20.9 20.9 2 0 . 9 20 .9

OCT 23/74 OCT 23/74 JAN 1 3 / 7 5 J A N 13/75 J A N 1 3 / 7 5

OCT 23/00 OCT 23/00 JAN 13 /99 JAN 13 /99 J A N 1 3 / 9 9

PAT 50 PAT 51 PAT 52 PAT 53 PAT 5 4

20.9 20.9 20 .9 20 .9 20 .9

JAN 1 3 / 7 5 J A N 13 /99 J A N 1 3 / 9 9 JAN 13 /99 JAN 13 /99 J A N 13 /99

PAT 55 PAT 56 PAT 57

PAT 59 PAT 5a

'JAN i 3 j 7 5 ' J A N 1 3 / 7 5 JAN 1 3 / 7 5 J A N 1 3 / 7 5

20.9 20 .9 2 0 . 9 2 0 . 9 20.9

JAN 1 3 / 7 5 JAN 1 3 / 7 5 JAN 1 3 / 7 5 J A N 1 3 / 7 5 J A N 1 3 / 7 5

J A N 1 3 / 9 9 L JAN 13 /99 L J A N 13 /99 JAN 13 /99 JAN 13 /99

PAT 60 PAT 6 1 PAT 62 PAT 63 PAT 64

I P A T 65 1 1 1 20 9

20 20

-

a a 20

20.9 20.9 20.9

500.0 225.0

. J A N 1 3 / 7 5 JAN 1 3 / 7 5

J A N 1 3 / 9 9 J A N 1 3 / 9 9

248595 248596 24a597 247687 247689

247690 247691 247692 247693 247694

JAN i 3 j 7 5 JUL 04 /75 AUG 26 /75

PAT 1 0 0 I PAT 200 JUL 0 4 j o o AUG 26/99

500 .0 500.0 200.0 200.0 500.0

AUG 2 6 / 7 5 AUG 26/99 AUG 26 /97 AUG 26/97 AUG 26/99 AUG 2 6 / 9 5

PAT 300 PAT 400 PAT 500 PAT 600 PAT 700

AUG 26j75 AUG 2 6 / 7 5 AUG 2 6 / 7 5 AUG 26175

247696 247697

247699 247700

247698

1 1 1 1 2 1 0

25.0 25 .0 25 .0 $00.0 250.0

SEP 18/75 SEP 18 /75 SEP 18/75 OCT 16/75 OCT 1 6 / 7 5

SEP i a m PAT aoo PAT 900 PAT 1 0 0 0 PAT 1100

SEP i a j 9 9 SEP 1 8 / 9 9 OCT i 6 j 9 9 OCT 1 6 / 9 9 JPAT i z o o

L - INCLUDED WITHIN M I N I N G LEASE 4 5 1 ; NO ASSESSMENT REQUIRED .# - SUBJECT TO EMPR APPROVAL

LAND PACTS P a g e l o f 3

TAP 51 RICK 1 RICK 2 RICK 3

GOLDSTREAM

248186 1 248408 20 248409 18 248407 6

I DATE REVISED: SEP 16,1994

FAR 2 GR 3 GR 4 KATE

I CLAIMS: 92 I UNITS: 328

248544 1 247886 10 247887 10 248449 16

I CLAIM I TENURE IUNITS

L E A S E ~ ~ I NATAL 1

BILL NATAL 2

306287 1 323447 20

326594 12 323448 15

IHUMP 1 I 248375 I 12

UtEA(ha)

20.9 500 450 150 300

400 500 4 00 300 20.9

20.9 250 250 4 00

356 500 375 300

AREA(ha): 7909

RECORD DATE

JUN o9/89* JUN 16/90 JUN 19/90 JUN 19/90 MAY igiso

MAY 13/90 MAY 13/90 MAY 13/90 MAY 13/90 OCT 14/71*9

MAR 22/74*3

NOV 08/82*3 NOV 08/90

NOV 08/82*3

APR 23/91 FEB 04/94 FEB 03/94 JUN 23/94

EXPIRY DATE

JUN 09/99 JUN 16/95 #

MAY 13/93 E MAY 13/93 E MAY 13/93 E MAY 13/93 E OCT 14/97

MAR 22/96 NOV 08/95 NOV 08j95 NOV 08/95 #

APR 2312021 FEB 04/97 # FEB 03/97 # JUN 23/95

* LOCATION DATE # SUBJECT TO EMPR APPROVAL ** CLAIMS HELD UNDER OPTION E EXPIRED CLAIMS

. .i -. - . . 5 . . ,.

APPENDIX 2 ANALYTICAL RESULTS

BETHLEHEM RESOURCES CORPORATION GOLDSTREAM MINE

1994 DRILLING RESULTS

TRUE HOLE SAMPLE INTERVAL (m) THICK THICK % C' 91 Zn DESCRIPTION

G-94-1 402 351.83 353.00 1.17 1.10 1,457 0.48 HW Diss Zone 403 353.00 354.00 1.00 0.94 0.874 0.82 HW Diss Zone 404 354.00 355.00 1.00 0.94 1.090 0.56 HW Diss Zone 405 355.00 356.00 1.00 0.94 0.457 0.82 HW Diss Zone 406 @6.00 357.00 1.00 0.94 2.552 1.15 HW Diss Zone . 407 .+ 357.00 358.00 1.00 0.94 1.598 0.85 HW Diss Zone 408 358.00 358.49 0.49 0.46 1.087 1.76 HW Diss Zone

~

r ~ ~ ~ 3 5 1 1 e 3 358.49 6.66 6.26 1.322 0.84 HW Diss Zone I

406 35G.00 357.00 1.00 0.94 2.552 1.15 HW Diss Zone 407 357.00 358.00 1.00 0.94 1.598 0.85 HW Diss Zone 408 358.00 358.49 0.49 0.46 1.087 1.76 HW Diss Zone

[~ ~ - 3 5 6 . 0 0 ~ ~-358.49 2.49 2.34 - 1.880 1.15 HW Diss Zone I

409 350.49 359.42 0.93 0.87 0.666 4.91 Massive Sulphide 410 359.42 360.31 0.89 0.84 1.344 1.42 Massive Sulphide 411 360.31 361.36 1.05 0.99 3.785 2.35 Massive Sulphide

cI358xG 361.36 2.87 2.70 2.017 LE Massive Sulphide I

351.83 358.49 6.66 6.26 1.322 0.84 HW Diss Zone 350.49 361.36 2.87 2.70 2.017 2.89 Massive Sulphide

~ ~ ~~~ _~ 1~~ ~I 351.831- ~ 36!?--?2?>96~-- 1.532 1.46 Combined I


~ ~ ~~~

[ ~ ~ ~ ~ ' 3 5 6 . 0 0 ~ . . 361.36 5.36 5.04 1.954 2.08 Combined I ~~~ ~ . ... . ~

411 r_-360:3L.. 361.36 1.05 0.99 3.785 2.35 O&aje MS I

416 417 418 419 I 2 0 421 422

301.65 382.65 1.00 0.94 382.65 383.65 1.00 0.94 303.65 384.65 1.00 0.94 384.65 385.65 1.00 0.94 315.G5 38F.28 0.63 0 59

386.95 387.45 0.50 0.47 386.28 386.95 0.67 0.63

4.627 1.49 Massive Sulphide 5.81 1 4.10 Massive Sulphide 6.401 6.31 Massive Sulphide 4.662 2.46 Massive Sulphide 5.491 '1.20 Massive Sulpliide 0.504 2.90 Massive Sulphide

10.662 7.70 Massive Sulphide

5 450 4 . 0 s Massive Sulphide I


, 3 8 0 - l - 8 ~ - ~ ~ ~

381:28~--~ 7.10- 6 . 6 7 L 3.28 Combined I

TRUE HOLE SAMPLE INTERVAL (m) THICK THICK % c, % Zn DESCRIPTION

G-94-3 424 372.19 373.19 1.00 0.94 0.894 0.21 HW Diss Zone HW Diss Zone 425 373.19 374.19 1.00 0.94 0.634 0.95

[ 377 19 -374 19 200 1 8 8 0764 0 58 HW Diss Zone I

426 374.19 374.79 0.60 0.56 8.890 3.19 Massive Sulphide 427 374.79 375.31 0.52 0.49 0.349 0.04 Phyllile 428 375.31 375.51 0.20 0.19 5.600 5.44 Massive Sulphide cI.~_ ..

374.19 375.51 1.32 1.24 5.027 2.29 Ore Zone I

FW Diss Zone 429[--' 37515r~ 376.26 0.75 0.70 1.884 0.10 I

372.19 374.19 2.00 1.88 0.764 0.58 HW Diss Zone 374.19 375.51 1.32 1.24 5.027 2.29 Ore Zone 375.51 376.26 0.75 0.70 1.884 0.10 FW Diss Zone

__ - ~ 1 ~ ~ - ~372.19 ~ 376.26 . . . 4.07 . . 3.82 .. .. . 2.353 1.05 Combined I

TRUE HOLE SAMPLE INTERVAL (rn) THICK THICK % c u % Zn DESCRIPTION

G-94-4 438 436.28 437.38 1.10 1.03 1.769 0.21 HW Diss Zone 439 437.38 438.48 1.10 1.03 1.066 0.17 HW Diss Zone

[63628 ~- 438.48 2.20 2.07 1.418 0.19 HW Diss Zone I - .....

440 438.48 439.50 1.02 0.96 8.438 1.18 Massive Sulphide 441 439.50 440.28 0.78 0.73 1.027 0.56 442 440.28 440.85 0.57 0.54 6.178 1.29 Massive Sulphide 443 440.85 441.65 0.80 0.75 4.004 0.63 Semi-massive Sulphide

Massive Sulphide 444 441.65 441.86 0.21 0.20 4.391 0.90

Diss Sulphide

,.-la~3s,4.~~ . 441.86 3.38 3.18 0.91 Ore Zone I 5.046 _~ ______..

436.28 438.48 2.20 2.07 1.41 8 0.19 HW Diss Zone 438.48 441.86 3.38 3.18 5.046 0.91 Ore Zone

~~ ~ I 436.26 ~~ ~ 441.86 5.58 5.24 3.615 0.62 Combined I

G-94-5 453 660.20 661.00 0.80 0.75 3.135 0.74 Diss Sulphide 454 661.00 662.00 1.00 0.94 4.638 5.43 Massive Sulphide

451 65835 65993 158 148 0 937 0 64 HW Diss Zone ~~~ ~~ ~~

452 659.93 660.20 0.27 0.25 0.139 0.20 HW Oiss Zone 453 660.20 661.00 0.80 0.75 3.135 0.74 Diss Sulphide 454 661.00 662.00 1.00 0.94 4.638 5.43 Massive Sulphide 455 662.00 662.75 0.75 0.70 0.237 0.03 FW Diss Zone

L 6 5 R . 3 5 562.75 4.40 4.13 2.009 1.62 Combined 1

TRUE HOLE SAMPLE INTERVAL (m) THICK THICK 96 C8 96 Zn DESCRIPTION

G-94-6

G-94-7

G-94-8

c~-94-9

G-94-10

461 353.97 355.22 1.25 1.17 1.737 1.17 HW Diss Zone 462 355.22 356.48 1.26 1.18 2.026 0.40 HW Diss Zone 463 356.48 357.11 0.63 0.59 3.002 0.96 HW Diss Zone c~~

~353,97- 357.11 3.14 2.95 2.107 0.82 HW Diss Zone 1

353.97 357.1 1 3.14 2.95 2.107 0.82 HW Diss Zone 464 357.11 357.51 0.40 0.38 4.284 3.86 Massive Sulphide 465 357.51 358.70 1.19 1.12 1.089 0.15 FW Diss Zone

463 356.48 357.11 0.63 0.59 3.002 0.96 HW Diss Zone 464 357.11 357.51 0.40 0.38 4.284 3.86 Massive Sulphide

~ ~ ~ 3 5 6 ~ ~ ~ ~ ~ 357.51 1.03 0.97 3.512 2.1:- Ore Zone 1

471 472 473 474 475 476 477

i I

481.15 481.91 482.35 483.28 483.89 484.69 485.06

481.15 ~~ ~-

~~

481.91 0.76 0.71 4.050 0.29 Semi-Massive Sulphide 482.35 0.44 0.41 9.532 0.95 Massive Sulphide 483.28 0.93 0.87 1.556 0.41 Disseminated Sulphide 483.89 0.61 0.57 8.494 3.42 Semi- Massive Sulphide 484.69 0.80 0.75 12.127 2.65 Massive Sulphide 485.06 0.37 0.35 4.800 1.32 Disseminated Sulphide 485.34 0.28 0.26 8.039 4.60 Massive Sulphide

485.34 4.19 3.94 6.594 1.67 Ore Zone 1

-_ . ~~ ~- 478 1 ~ 4~85.34 486.00 0.66 0.62 0.662 0.09 FW Diss Zone 1

481 488.07 488.57 0.50 0.47 4.588 0.39 Disseminaled Sulphide 482 488.57 489.54 0.97 0.91 9.364 483 489.54 489.94 0.40 0.38 1.810 0.59 Disseminated Sulphide 484 489.94 490.98 1.04 0.98 0.202 0.40 Phyllile 485 490.98 492.02 1.04 0.98 2.751 1.10 Disseminated Sulphide 486 492.02 493.22 1.20 1.13 6.005 4.52 Massive Sulphide

1.14 Massive Sulphide

. . ..... -~ 488.07 493.22 5.15 4.84 4.345 1.65- Ore Zone 1: ~ " ' ~ ' ' ~ . ~ _ _ _ ~ ~ I

- _ ~ __ 487 r~~ ~ 493.22~~~-~49402~~~p.B0 0_75_. 1.465 0.27 FW Diss Zone I

494 G X 48 G27.43 0.95 089 2 162 0 89 Diss Sulphide 495 627.43 627.63 0.20 0.19 6.494 7.74 Massive Sulphicle

~~

[-:-.1626.48 627.63 1.15 1.08 2.915 2.08 Ore Zone I

1853 550.60 551.42 0.82 0.77 0.261 0.80 HW Diss Zone 1854 551.42 552.60 1.18 1 . 1 1 0.096 0.12 HW Diss Zone 1855 552.60 553.60 1.00 0.94 0.156 0.41 HW Diss Zone 1856 553.60 554.62 1.02 0.96 0.073 0.17 HW Diss Zone

~~ ~ ~. ~ ~ i 550.60~ 554%- ~ 4.02 ~ ~~~3.778~~~~~-0,13?____. 0.34 Combined I

406 2.551, 0.01, 1.15,.23,.001 2.577 . 0 2 1.16 .21 - 0 0 2 2.526 <.01 1.14 .26 . 0 0 2 RE 4 0 6 1.087 .32 1.15 . 27 .001 407

. 0 0 2 408 ..- 1.598 .09 .a5 - 2 5 . oo i 409 I - 6 6 6 -30 4 . Y I

410 1 . 3 4 4 .23 1.42 .22<.001 411 3.785 .31 2.35 .57 .001 412 . 0 0 6 .01 .01 .05<.001 STANDARD R-l/AG-I/AU-I .841 1.29 2 . 3 4 . 9 8 -099

1 Gn S W L E LEACHED I N 75 HL AWA - RECIA, DILUTE TO 250 ML, AMALYEIS BY I C P . AG** B AU** 6Y FIRE ASSAY PROH 1 A.T. SWPLE. - SAMPLE TYPE: CORE # S i t e s /irminq ‘RE’ are dud)? 5

DATE RECEIVED: JUL 28 1994 >ATE =PORT MAILED: 4 4L,b SIGHED BY. . .. . ... .D.fOYE, C.LE(WIG, J.UANG; CERTIFIED E.C. ASSAYERS

r

. , . .. . . __ . .. . ._ . .___ . . . . . -.- _.__-----_I__

413

G-44-2 4 14 415 RE 4 1 5 416 4 17 4 18 4 19 4 2 0 421 422 4 2 3

Cu Pb Zn Ag** Au** b % % oz/t o z / t

.080 ,039

,1.705 1 . 7 0 4 4 .627

. 0 4

.01

.Ol 01 .06

.Ol

.06

.31

.31 1 . 4 9

. 0 3 < . 001 < .01<. 0 0 1

.14 ,002

. 1 4 . 0 0 2

. 4 6 , 008

5 . 8 1 1 . 3 6 4 . 1 0 .70 .005 6 . 4 0 1 . 7 9 6 . 3 1 1 .01 .006 4.662 .17 2 . 4 6 .50 .006 5 . 4 9 1 .27 4 . 2 0 .58 .003

~ ,584 . 2 4 2 . 9 0 .22<.001 10.662 1.11 7 . 7 0 1 . 8 2 .005

.013 .01 .01 <.01<,001

1 GM MPLE LEACHED IW 7s HL wn - REGIA, DILUTE TO no HL, mirsIs BY ICP. AG** I IuT* BY f lRE ASSAY FROM 1 A.1. SMPLE, - SAMPLE IYPE: CORE

DATE RECEIVED1 AUG 3 19p4 DATE REPORT MAXLED4

in DJ 4

.D.IOYE, C.LE(mG, J.UAIIG; CERlIFlED B.C. ASSAYERS

. . ,'.

.. .

G - 9 4 - 3

4 2 4 RE 4 2 4 4 2 5 4 2 6 427

428 4 2 9 4 3 0

% % % oZ/t o z j t .887 <,01 .21 ,07 .0011 0 . B q i .901 <.01 .21 .07 .001

8 .890 .48 3.19 .92 ,010 ,634 c . 0 1 -95 .oa<.ooi- . 3 4 9 .O1 . 0 4 .02<*001

5.600 .73 5 . 4 4 a 9 9 ,005

- 0 8 4 < a 0 1 002 <.01<.001 1.884 .02 .lo .09 .001

I Ow SAnPLE LEACHEO I N 75; 111 AQUA - REGIA, DILUTE TO 250 M l , A W A l Y S l S BY ICP. AG** & MP* BY FIRE ASSAY FROM 1 A.T. W L E . ' SAMPLE IYPE: CORE

DATE RJSCEXVEDi AUG 16 1994 DATE REPORT WILED: .IOYE, C.CEONG, J.UAHG; CERlIFlED B.C. ASSAYERS

.

431 432

434 G-44-3 4 3 3 435

436 437 4 3 8 ' 439 4 4 0

G-44- 4 4 4 1 4 4 2

444 RE 4 4 4

CowlplcSe 44 3

4 4 5 4 4 6 STANDARD R-l/AG-I/AU-l

% % o z / t oz/t ,030 c.01 -02 .05<.001 .081 <.01 .03 ,04 .001 .277 -03 . 6 8 .04<.001 .I90 <.01 .23 <.01<.001 .121 K.01 .ll .05<.001

,121 <.01 . 05 .01<.001 . 5 0 6 .01 .06 .07 .001

1.769 <.01 .21 .16 .002 1.066 <.01 .17 .08 .001 8 . 4 3 8 .02 1.18 .75 .005

1.027 . 0 6 . 5 6 .14 .001 6.178 .02 1 . 2 9 .60 ,006 4.004 C.01 . 6 3 . 4 4 .003 4.367 . 0 7 . 8 9 . 4 3 .003 4.415 .08 .90 .48 ,003

. l o 5 <.01 .02 .04<.001 ,133 .01 $02 .04<.001 . 8 4 8 1.29 2.36 . 98 ,101 -

1 GM SAMPLE LEACHED 1W 75 NL AWA - R E G I A , DILUTE TO 250 WL, ANALYSIS BY I C P . AC*' 6 W* BY FIRE ASSAY FROM 1 A.T. S M P l E . - SAMPLE TYPE: CORE Smote6 beslnnins 'RE' ere duol icate s w i c s .

DATe RECEIVED: AUG 26 1994 DATE REPOW MAILBD: D.TOYE, C.LEONG, J-UANG; CERTIrlED B . C . ASSAYERS

* * n h h

LL c a Q

- a t- C I-

* *

,

431 4 3 2

434 4 3 5

G-94-3 433

436 437 4 3 8 ' 439 44 0

445 446 STANDARD R-l/AC-l/AU-l

,121 <.01 . 0 5 .01<.001 .506 .01 .06 .07 .001

1.769 C.01 .21 .16 ,002 1.066 C.01 .17 .08 .001 8 . 4 3 8 . 0 2 1 . 1 8 . 7 5 . 0 0 5

1 .027 . 0 6 . 5 6 .14 . 0 0 1 6 .178 .02 1.29 .60 ,006 4.004 <.01 .63 . 4 4 .003 4 .367 .07 .89 . 4 3 00 4.415 .08 .90 .48]7& Oeq5

. l o 5 <.01 .02 .04<.001

.133 .01 .02 .04<.001

. a 4 8 1 . 2 9 2 . 3 6 .98 ,101

1 GM SAMPLE LEACHED IH 75 NL AQUA - REGIA, DILUTE TO 250 HL, ANAlYSlS BY I C P . AC*' 6 ACT* BY F IRE ASSAY f R O n 1 A.T. SMPlE. * SAHPlE TYPE: CORE

DATE RECEIVED: AUC 26 1994 DATg REPORl MRILBDr D-IOIE, C-LEOHG, J-UANG; CERTIFIED B.C. ASSRYERS

* * N m m W VJ

R

-I U I- 0 I-

* *

a

I

447 448

G- 94-5 449 450 451

452 453 454 455 456

457 RE 457 458 459 STANDARD R-l/AG-l/AU-l

- % % % oZ/ t o z / t

.056 <.01 .06 .01 .002

.005 .01 .03 <.01<.001

.114 .07 .03 .10 .001

.038 .02 .21 <.01<.001

.937 .01 .64 .07 .002

1 GM SAMPLE LEACHED I N 75 ML AQUA - REGIA, DILUTE TO 2 5 0 HL, ANALYSIS BY ICP. AG** & AU** BY F I R E ASSAY FROM 1 A.T. SAMPLE. - SAMPLE TYPE: CORE

DATE RECEIVED: SEP 12 1994 DATE REPORT MAILED: C.LEONG, J.WANG; CERTIFIED B.C. ASSAYERS

SAMPLE#

460 461 462 463 464

465 RE 465 466 467

DATE RECEIVED

% % % oZ/t o z / t

.260 1.737 2.026 3.002 4.284

.01

.12

.12

.14

.54

.16 1.17 .40 .96

3.86

.02

.14

.17

.24

.51

.001

.003

.003

.003

.003

1.090 .02 .15 .07 .001 1.088 .02 .14 .07<.001 ,517 .01 .02 <.01<.001 .082 .04 .08 <.01<.001

1 GM SAMPLE LEACHED IN 75 ML A W A - REGIA, DILUTE TO 250 ML, ANALYSIS BY ICP. AG** & A V * BY FIRE ASSAY FROn 1 A.T. SAMPLE. - SAMPLE TYPE: CORE

SEP 19 1994 DATE REPORT MAILeD: C.LEONG, J.UANG; CERTIFIED B.C. ASSAYERS

4 68 469 470 4ii 472

473 474 475 476 47 7 RE 477 4 7 8 479

DATB REcElxvaD

,043 <.01 .03 <.01<.001 ,116 <.01 . 0 3 <.01<.001

1.153 <,Ol .24 .I0 ,002 4 , 0 5 0 .01 .29 . 3 4 ,003 9.532 .01 .95 .85 ,014

1,556 <.01 .41 .13 .001 8.494 <.01 3.42 .85 ,009 4.800 .ll 1.32 .48 .006 8 * 0 4 3 4'61 lg4' * O o 7 7 g . o 3 q , 1-02. 4.@, ),45, 0008

12.127 no1 2.65 1.19 -013

8.035 1.01 4.59 1.41 ,009) ~

,662 .01 .09 .05<.001 ,009 c . 0 1 .01 <.01<.001

1 Gw W l E LEACHED IN 15 HL M U A - RECIA, OlLUlE TO 230 M l , A H A l Y S l S BY ICP. AC** & @* BY FIRE ASSA - W P L E tYPE: CORE

OCT 17 IOPQ DATB REPORT WAfLBDt .D.TOYE, C.LEOIIG, J,MNG; C E R l l f I E D B.C. ASSIY€RS

SAMPLE#

480 4 8 1 482 RE 482 483 4 8 4 485 486 487 488

489 490

,028 .01 .06 .02<.001 4.508 < . 0 1 .39 .25 .005 9.451 . 0 1 1.15 .67 .009 3 9 . 3 6 3 , ~01, 1,141 0.65, o.oO@ 9 . 2 7 6 <.01 1.13 .64 .008

.12 - 0 0 2 1.810 .03 .59

,202 .01 . 4 0 2.751 .10 1.10 6.005 .78 4.52 1.465 .04 .27 .325 .01 <.01

1.472 .01 . 2 9 .180 .01 c.01

.02<. 001 -27 .004 . 8 5 .007 .08 .001 . OlC. 001 .04 .001 .01 .002

1 GM SAMPLE LEACHED IN 75 HL AQUA - RECIA, DILUTE 10 250 HL, ANALYSIS BY I C P . AG- & A W BY F I R E ASSAY FRON 1 A.T. N P t E . - SAMPLE TYPE: CORE

DATE RECeIVED: oC1 26 1W4 DATE: REPORT MAILED:

2 C> C

W

CD n -

c

4

m ul

T1 ;(7

D

3

..

n n r- D m cn

cn m n ru cn w c

4

m -I 0

c

c

a3 w 4 P m m cn

73

0 ru \ (z, N

, I

1851 1852 1853 1854 RE 1854 1855 1856 1857 1858 1859

STANDARD R-l/AG-l/AU-l

Cu Pb Zn Ag** Au** % % % o z / t o z / t

.042 .01 .11 .02<.001

.067 <.01 .10 .07 .002

.261 .08 .80 .19 .001

.096 .03 .13 .05<.001

.096 .03 .ll .09 .001

.156

.073

.153

.006

.004

.Ol

.05 <.01 <.01 <.01

.41

.17

.03

.01

.Ol

.02 .002

.13<. 001

.05<. 001 <. 01<. 001 .06 .001

.846 1.28 2.36 .97 .098

1 GM SAMPLE LEACHED I N 75 ML AQUA - REGIA, DILUTE TO 250 ML, ANALYSIS BY I C P . AG** 8 AU** BY F I R E ASSAY FROM 1 A.T. SAMPLE. - SAMPLE TYPE: CORE Samles beginning 'RE' are duplicate ss/idples.

I P

SAMPLE# -

1860 1861 1862 1863 1864

1865 1866 RE 1866 1867 1868

1869 STANDARD R-l/AG-l/AU-l

Cu Pb 2n Ag** Au** % % .8; o z l t o z l t

. 0 4 6 .01 .69 .12<.001 1.277 . 0 1 .43 .20 .001 1.522 . 0 3 2.05 .17 .001 2.478 .16 2.20 . 3 4 .001 1.553 .20 1.32 .29<.001

1.123 - 0 9 . 5 5 .12<.001 6.833 .85 5 . 7 0 1.14 .004

6 .030 .23 2.87 .70 .003 6.860 . 8 3 5.74 1.16 '.003 .543 .03 -17 .06<eO01

.023 .01 .01 .02<.001

. a 4 3 1.28 2 . 3 4 .97 ,098

I Cn SAMPLE LEACHED I N 75 NL AQUA - RECIA, DILUTE TO 250 NL, ANALYSIS BY ICP. RGn & Av"* BY FIRE ASSAY FROM 1 A . 1 . SAMPLE. - SAMPLE TYPE: WRE Sam,\es besinnine ' R E ' are dupli? 5

DATE RECEIVEiDr NOV 28 1994 DATE REPORT MAILED, 7 / q y SIGHED BY.. .*. . , . . . . . O . l O Y E , C.LEONC, J.UANG; CERTIFlEO 8.C. ASSAYERS

APPENDIX 3 DRILLOGS

OREQUEST CONSULTANTS LTD - DIAMOND DRILL HOLE RECORD C l i e n t BETHLEHEM Page il 1 o f 1

Hole No. G-94-1 N o r t h i n g 309A. 26 Core Size NQ I 1 Depth Dip Azimuth Depth D ip Azimuth S t a r t e d JULY 19, 1994 Target M I N E OREBODY Proper ly GOLDSTREAM East i n g 15856.02 Casing 5 ' LEFT 64.6 - 88 130 125.6 - 86 160 Completed JULY 25, 1994 Comwnts HOLE CEMENTED Locat ion REVELSTOKE E l e v a t i o n 665.62 Length 311.04 185.6 - 84 110 247.6 - 80 la5 Drill Co. OLYMPIC NIS 82M/9W L a t i t u d e 51 38' 00" N D i p - C o l l a r -90 305.5 - 78 188 369.5 - 7a 190 Logged By W . RAVEN Claim No Longi tude 118 24 ' 40" W Bear ing N/A U n i t s METERS

FROM TO ROCK ALT FOL DESCRIPTION 2 SAMFLE No, FROM T O LENGTH Au Ag Cu Pb i n TYFE C / A SULPHIDE ops t ops t p c t p c t pc t

55.49 OVERBURDEN

55.49 90.28 CARBONATE PACKACE (BADSHOT AND MOHICAN FORMATIONS)

55.49 76.70 ARGILLACEOUS L IRESTONE

51,90 59.00 59.20 60.50 63.00 72.00

68.00 72.00

12.70 13.10

73.70 73.68 75.50 76.10

76.70 83.09

83.09 90.28

Carbonate package c o n s i s t i n g o f we l l f o l i a t e d and banded c h l o r i t e and b i o t i t e +/- s e r u , t e (40'6) i n a carbonate m a t r i x . Local s e c t i o n s o f c l e a n 1 inestone (marble). N i n o r secondary carbonate v e i n i n g 1-32 p a r a l l e l t o and c:oss c u t t i n g t h e f o l i a t i o n . Local b r e c c i a t i o n w i t h carbonate tens ion gash i n f i l l i n g s . Minor disseminated PO and py ( t race-12) as small cubes and b lebs . F o l i a t i o n as 40-50 t o SCA. Good recovery a t 95-1009,. Minor quar tz augens (<15). F a i r l y competent core. Lower contac t sharp a t 30 t o SCA.

-c ross c u t t i n g r d r b - q t z ve ins 1-3mn wide a t 30 t o SCA -broken and f rac tu red , minor gouge -broken with ninor gouge t o 64.50 then competent b u t with b r e c c i a t e d carb-q tz ve ins and tens ion gash i n f i l l i n g s

-2-4% carb-q tz tzr is ion gash i n f ill ings and 1-2 q t z augens, competent t o 71.60 then broken w i t h n i n o r gouge, a i n o r carb-q tz v e i n s a t 85 SCA

- g r a p h i t i c 53 c;.ei iu lat ion c leavage a t 65 t o SCA w i t h some minor f o l d s d1SO a t 65 t o '9

- m i l k y q t z vein, i l C 1 4 0 , LC 1 7 0 , t race-12 b lebs o f PO -broken, most ci'rr 5cn l o n q

LIMESTONE / MARBLE

Grey-white c lean marble with l o c a l d i r t i e r banded s e c t i o n s . R e c r y s t a l l i z e d 1 inestone t h a t i s medium grained. Conta ins about 1% g r a p h i t i c s t y l o 1 11s. Trace PO and py. 1-22 q tz -carb ve ins . Where banded f o l i a t i o i l P 45. Very n i n o r c h e r t y sec t ions approx. 5cm long. Genera l l y q u i t e competent core. UC sharp a t 30, LC nore g r a d a t i o n a l .

INTERCALATED MARBLE / CHLORllE - SERlCllE PHYLLllE

OREQUEST CONSULTANTS LTD, HOLE II : 6-94-1 PAGE I 2 of 7

FROM TO POCK A L I FOL TYPE C i A

DESCRIPTION 2 SAMPLE No. FROM TO LENGTH A u A9 Cu Pb Zn SULPHlDE GpSt OpSt pCt pCt pCt

90.28 371.04

90.28 132.20

90.55 90.65 91.03 92.18 92.1s 92.50 96.98 97.05 97.05 97.55 97.55 97.73

97.80 97.88 91.70

101.78 101.82 104.34 104.46 106.72 106.98

107.25 107.50

111.60 111.75 112.45 112.70 113.85 113.95 114,40 114.95 114.95 115.12 115.56 115.70 116.00 119.00

121.75 129.10 129.53

I n t e r v a l contd n c sec t ions of marble as above (703) w i t h i n t e r c a l a t e d r h l o r i t e - s e r i L I!+ p h y l l i t e (30%). Some banded sec t ions bu t mostly 10-20cm length: o f CSP w i t h i n the marble. Trace- l t d issa. b lebs o f PO and py. UC somewhat a r b i t r a r y wh i le LC sharp a t 40. Fol ia t ion ibands a t 40-50. The CSP i s non calcareous. Both u n i t s a re competent, recovery i s 98%. Minor ( 2 4 % ) t a n b i o t i t e i n the CSP along with 1-2% carb ve ins .

LOWER INDEX FOR3AIION

CHLORlTE - SER!C!TE PHYLLllE

Pa le greenish-grey coloured rock. Greyer sec t ions are s e r i c i t e > c h l o r i t e , green :ections are c h l o r i t e > s e r i c i t e . U n i t i s we l l f o l i a t e d a t 40-50. Comprised o f c h l o r i t e (30-401), s e r i c i t e (20-40%), and q tz - fe ldspdr groundmass (lO-ZOt), carb veins (<l t ) and p tygnat ic o r augens o f q ' . (2-41). U n i t i s f i n e l y laminated. Minor t a n b i o t i t e (1-2%). Variat8:t s i l i c i f i c a t i o n w i t h about h a l f the u n i t s t r o n g l y s i l i c i f i e d . Spli ts e a s i l y along S2, p o s s i b l e t a l c along p a r t i n g s . UC sharp a t 40, L C i n gouge and rubb le zone.

- s t r o n g l y sheared, Minor gouge -s t rong c l a y weak carbonate gouge, 30% recovery -s t rong s i l i c i f i c a t i o n , d is rup ted f o l i a t i o n a t 10-20 -broken q t z vein with minor carb -contor ted f o l i a t i o n a t 70 -mi lky q t z v e i n a t 60 w i t h minor i n t e r c a l a t e d CSP and 1% PO blebs and

3% tan b i o t i t e -5% Massive PO b lebs, t race cpy, t r a c e sph? -3-4cn wide q t i ve in a t 50, bar ren -wavy ntinor f o l d s = S3 a t 70 -broken q t z ve in with 21 PO b lebs - q t z f looded (20.30%) as ptygmat ic ve ins and boudins, t race-1% PO

blebs, S3 i n te r fe rence -mi lky q t z ve in a t approx 5 5 , has 2% PO as Massive b lebs w i t h t race

-broken and f r a c t u r e d -broken and f r a c t u r e d -broken and f r a c t u r e d -sp lo tchy carb tsns ion gash i n f i l l ings -broken and f rdc !u red w i t h minor q t z ve ins - q t z vein, s e r i c i t e - t a l c ? gouge a t UC a t 60, t race PO and py - s t r o n g l y s i l i c i f i e d -51 Massive PO, 12 py i n p t y g n a t i c q t z v e i n -s t rong ly broken and f r a c t u r e d w i t h vuggy carb veins

PY and CPY

HOLE U: 6-94-1

OREQUEST CONSULTANTS LTD- HOLE B : G-94-1 PAGE il 3 of 7

FROh T O ROCK At1 FOL TYPE C I A

DESCRIPTION 1 SAMPLE No. FROM T O LENGTH Au A9 Cu Pb Zn SULPH IDE opst opst pct pc t pc t

130.60 131.12 -broken and frar:ured w i t h gouge

132.20 1 3 9 , l l

132.85 133.80 134.33

131.50 134.80

134.80 134.95 135.33 135.48 137.90 139.11

139.11 145.84

145.84 332.50

146.38 147.38

DARK BANDED PPYLLITE (CALCAREOUS C ; i ! 3 R I T E - BIOTITE - GRAPHITE PHYLLITE)

UC i n a gouge -,id rubble zone from 132.00-132.30 so no contact neasurewent PO:. i b l e . Well banded and laminated dark brown t o black coloured u n i t w ' !h white carbonate bands. Local minor cher t p a r a l l e l t o f o l i a t i o n nhich i s p lanar w i t h minor wavy undli lat ions but general ly a t 35-45. Comprised of carbonate (25-409) wi th c h l o r i t e - b i o t i t e - g raph i te (35-45:), qtz augens and boudins (2-521, and cross c u t t i n g carbonate vein: (1-2%). P y r i t e and p y r r h o t i t e are ubiquous (1-31 combined). Ver, l i t t l e tan b i o t i t e i n the uppermost menber ( t r -2%) . Minor S3 inter'?:ence as c renu la t ion cleavage and small f o l d s . Var iab le seric',+.? general ly (52.

-contains 5% c , h i n e d py and PO i n equal proport ions -S3 f o l d , ax is a! 85-90 -GARNET ZONE - r i a l 1 weakly s i l i c i f i e d i n t e r v a l con ta in ing 10-15t rounded l i g h t p ink garnets ranging from 1-7an averaging 2-3mn, S2 i s d is rup ted aroiind the garnets and they appear s1 i g h t l y ro ta ted

-cher t w i t h 20: a rg i l laceous mater ia l

-CHLORITE -SERli:IE - PHYLLITE - small in te rca la ted bed, greenish-grey -GARNET ZONE - 2' 134.50-134.80

co lour , sharp :per and lower contacts a t 30, f a i r l y broken

DARK BANDED PHYLL I I E (CALCAREOUS - T A N BIOTITE - CHLORITE PHYLLITE)

S i m i l a r t o above u n i t but less arg i l laceous (b io -ch l -g raph i te mix) Mater ia l and n m with 10-152 tan b i o t i t e and l o c a l l y up t o 45-50% carbonate and 10: green c h l o r i t e

DARK BANDED PHV!I ITE (IAN BIOTITE - EiOTITE - CHLORITE - GRAPHITE CALCAREOUS PHYLLITE)

Banded u n i t wit5 tan b i o t i t e [S-20%), b lack arg i l laceous Material (b io -ch l -g raph i te n i x ) (40-502), carbonate (20-302 l o c a l l y higher), quartz augens ( 5 2 ) and qtz-carb veins (1-58), ub iqu i tous py and PO (1-32) as f i n e disseminations. U n i t i s well fo l ia ted , genera l l y planer bu t s o w contoi:?d and wavy sections, f o l i a t i o n a t 30. Local sections o f s t r o n g S3 deformation ind ica ted by graphite. Local s e r i c i t e t o 5%.

-s t rong 53 a t 40-50 w i th g r a p h i t i c c renu la t ion cleavage and ptygmatic f o l d 5

HOLE #: 6-94-1

PAGE B 4 of 7 . OREQUEST CONSULTANTS LTD, HOLE I : 6-94-1

%OM TO ROCK At1 FOL TYPE CIA

DESCRIPTION % SAMPLE No. FROM T O LENGTH Au Ag Cu Pb !n SULPHIDE opst opst p c t pc t pc t

147.67 148,68 150,OO 150.35

151.00 151.40 152.10 153.29 156.20 156.40 157.96 161.78

162.25 162.50 16!,20 164.10

164 I 20 168.47

169.30 169.45 173.20 173.44 189.08 189.25 189.57 189.74

. 192.67 192.j4 196.15 196.32

196 I 86 196.99

204.86 205 I 00 205.38 205.78

206.25 207 I 59 208 I 72 210.20 210.25 217.08 217.60 240.97 241.07 242.95 243.20 254.75 255.18

264.75 270.65

268.90 271.76

213.48 274.14

-broken core, minor gouge -h igh angle (80 t o S C A l cross c u t t i n g qtz-carb veins and S3 de forna t ion w i t h 3cn q tz ve in a t end o f i n t e r v a l w i th 4-6,. combined PY and PO

-40% tan b i o t i ' e , 102 green c h l o r i t e 5 3 c renu la t io r i cleavage and f o l d s w g g y carb v e i n lcn wide a t 80 -Deformation Zone - strong carb-qtz ve in ing tha t i s b recc ia ted w i t h angular f ragner ts o f DBP, veins are 1-4ca wide, l o c a l l y q u i t e vuggy w i t h q t z c rys t31 growth i n open space, in te rva l i s well n i n e r a l i z e d w i t h 5-71 combined py and PO, veins a t 70-85

-as above w i th carb-qtz veins -broken w i t h m:i,or gouge and sporadic carb-qtz veins as above -below t h i s p o i n t the tan b i o t i t e i s a b i t l o r e p reva len t avg. 15% -Minor g r a p h i t i c gouge on l c a qtz-carb ve in -vuggy carb-qtz ve in a t 70 -as above -broken and f r x t u r e d -broken and f t x : u r e d - q t z v e i n a t 25, 21 po blebs -brecciated qt:-carb ve in a t 70 -1cn q t z f lood ing w i th 10% PO and 1t sph? -1cR qtz-po VF:; , at 25 wi th 401 PO, t race sph? (reddish brown co lour ,

small b lebs) -qtz-carb f l o c i , 19 and g r a p h i t i c gouge a t 60 - S 3 minor f o l d s a t 60 drags out f o l i a t i o n a t 70 -S3 minor fold: a t 70 - f o l a t 70 from S3 minor fo lds -b recc ia ted ca ib ve in w i th g r a p h i t i c gouge a t end -q tz vein, UC sharp a t 40, LC sharp at 70, ve in i s bar ren -q tz f looded (LO:) -broken and f r i i ' u r e d -broken and f r ', , t i red

Deformation Zone

Strong S3 witi- g i a p h i t i c c renu la t ion cleavage and fo lds . Fo ld axes a t 60, zone a v e r q e r 4'6 dissen blebby PO and 12 py. F r o m 265.54-266,OO i s broken and contains carb-qtz ve in ing a t 20 and 70. The 70 v e i n i s 3cm wide and i s b recc ia ted w i th angular wa l l rock fragments w i t h n i n o r c l a y gouge, sulphides = 6-8'6

-Minor carb v e i n m g and 32 carb tension gash i n f i l l i n g s , ve ins cause

- q u i t e f rac tu red along S2 with sfla11 (5cm) broken sections, f o l i a t i o n ininor o f f s e t of S2 by 1-311

f l a t t e n i n g t o 20 HOLE # : 6-94-1

O R E Q U E S T C O N S U L T A N T S LTD, HOLE # : G-94-1 PAGE $ 5 o f 7 ~

FROM TO ROCK k t 1 FOI. DESCRIFTION % SAMPLE NO. FROM T O LENGTH Au Ag Cu Pb Zn TYPE CIA SULPHIDE opst opst pc t p c t pc t

274.65 275.41 291.94 292 I 08 -broken core 295.99 296.11

301.21 301.2P 305.76 305.81 - g r a p h i t i c shear w i th gouge a t 25 310.19 310.92 -broken and f - 3 . tured 313.90 314.05 -broken and f'::tured

314.60 314.65 -broken core

322.10 322.35 -broken and f rac tu red 323.81 323.88 - g r a p h i t i c gouge 323.88 324.10 -broken w i t h g r a p h i t i c gouge 324 I 50 324 I 65 -broken core 328.35 328.40 -broken core 328.40 32e.u -q tz -carb ten. gash i n f ill ings

332.50 337.21 GARNET ZONE (UE;#K)

-6 q t r veins 1.5-30 wide a t 25 w i t h la PO blebs

-qt2 ve in w i t h minor c h l o r i t e and wa l l rock fragments and 1% PO a t

-q t2 vein, disrl.ipted, one g r a p h i t i c suture, has trace-1% f i n e dissm py 25-30 t o SCk

314.20

319.42

-elongated qt- ,:in, 2ca s t re tched ou t by S3 minor fold a t 40

-vuggy carb-q!; ve in a t 60 t o SCA, (1% massive PO blebs

U n i t looks l i i p dark banded p h y l l i t e but not as calcareous though there i s apprc) 515% carb laminat ions and 1-2% cross c u t t i n g veins. S t rong ly s i l k i ' i e d throughout r i t h 5% cherty bands. Only 3-51 small p ink garnets v i w h d is rup t S2 f o l i a t i o n a t 10. 2-3% qtz-carb tens ion gash i n f i l l i n q c . Sulphides are l a r g e l y small blebs o f PO, average 2%. Graph i t i c t h r w j 7 o u t espec ia l l y on f r a c t u r e planes. UC i n gouge zone.

332.50 333.32

33S.37 336.58 536.58 337.21

?37.21 345.18

340.60 340.81

-broken and f i i c t u r e d , Minor gouge, rock i s contorted and brecciated w i t h 10% q t z - i z r b tension gash i n f i l l i n g s

-broken w i t h '.'>1.9e and rubble -contor ted and brecciated w i th 5% qtz-carb tens ion gash i n f i l l ings, S3 f o l d i n g and ':renulation cleavage a t 20

GARNET ZONE (SIR ' ING)

Same as above m i t on ly garnets are v i s u a l l y much more obvious (5-151) and are general!^ l a r g e r up t o 1Omn but average 4-5am. Also s t rong ly s i l i c i f i e d w i th aavy S3 deforna t ion throughout nost o f the u n i t . Gradational upper contact, lower contact sharp a t 10. 3 4 % qtz-carb tens ion gash i ~ f i l l i n g s . Sulphides = po a t 2-32 but l o c a l l y higher. Local s e r i c i t i i .ec t ions which are not s i l i c i f i e d . S3 var ies from 10-40 t o SCA. G r j p h i t i c f r a c t u r e s throughout.

-d is rup ted q tz vein w i th s t rong graph i te around ve in wa l ls where f rac tu red

HOLE #: 6-94-3

OREQUEST CONSULTANTS LTD, HOLE I : 6-94-1 PAGE W 6 of 7

F R O M TO ROCK At1 FOL TYPE CIA

O E S C R I P I I O N 2 SAMFLE No. FROH TO LENGTH Au A9 Cu Pb Zn SULPHIOE ops t ops t pct pc t pct

341.05 341.20

342.12 342.17 342.40 342.99

343.70 344.25 344.25 345.04 345 I 04 345.18

345.18 351.83

345.18 348.36 348.36 349.05 349.05 349.94 349.94 350.03 350.26 350.78 350178 351 00 351.00 351:8? CSP c h l . s i l 10

351 I 83 358.49

351.83 353.00 HWSSZ c h l , s e r 10

353.00 354.00 HWSSZ ch1,ser 10 354.00 355,OO HWSSZ c h l , s e r 10 355.00 356.00 HUSSZ c h l , s e r 10

356.00 357.00 HWSSZ ch1,ser 10

357.00 358.00 HWSSZ c h l , s e r 10 358.00 358.49 HWSSZ ch1,ser 10

358.49 361.36

-10: PO a s wisp! blebs and f o l i a t i o n p a r a l l e l s t r i n g e r vein masses

-d is rupted qtz e i n i n g with 1520% Massive PO and t r a c e cpy -PO enr iched sec t ion a s highly contorted wavy s t r i n g e r s , a re rage 25% PO, t r a c e cpy , ends i n 5cn rubble and gouge -20% coarse g a r r e t porphyroblasts t o lcrn - l i l y bed, no gdrne ts -30% massive pa, t r a w l % cpy

a t 20 t o SCA

CHLORITE - SEP! I E P H Y L L I I E

Pale greenish - grey colour. As 90.28-132.20. F o l i a t i o n a t 10. Minor su lphides = trace-1% PO. UC sharp a t 10, L C in 8cn gouge and rubble

-as general d e i c r i p t i o n -banded 1 imy urii t grading t o 1 inestone -20-25t t a n b i o t i t e , Minor nar ipos i te? (green i i c a j -q tz ve in , barren -gouge and rubbl t , 501 recovery -very s o f t = c l q a l t e r e d , speckled appearance -as above

HANGING WALL Sl ' !PLIIDE STRINGER ZONE

Host rock i s Cl I L , i t e - S e r i c i t e P h y l l i t e with loca l carbonate a l t e r a t i o n . Variable sulphide conten t , weakly t o non s i l i c i f i e d . Sulphides a r e as wispy to Massive b lebs which a r e contor ted with conten t averagio.; 5-15? conbined PO, cpy and sph. Also conta ins 15-202 q t z b l e b i and augens.

-from 351.83-35?.48 = 8-102 PO, 5% cpy and t race sph, 352.48-352.96 =

-8-10% PO, 3-59 tpy , trace-12 sph -8-101 PO, 3-51 ( p y , trace-12 sph

t r a c e cpy, 355.85-355.90 i s gouge -356.00-356.25 3% reddish - brown s p h a l e r i t e , 356.25-357.00 i s 5% PO, 5% cpy, and 2-32 sph

3-5% PO, 1-22 -;!, 352.96-353.00 10% PO, 5% CPY

-355.00-355.18 = 10% PO, 52 C P Y , 355.18-356.00 = 2-39, sph, 1% PO,

-357.00-357.88 8-101 PO, 59 C P Y , 3-4'. sph - f e n su lphides !O 358.25 then 15-201 PO, 3-42 sph, 1-2% cpy

MASSIVE SUlPHlOE ZONE

F a i r l y sharp u p p e - contact along a 2cm wide q tz -cher t vein a t 50. The lower contai! a l s o sharp a t 30 t o SCA. Conprised of massive su lphides up t o 70-802 though genera l ly a b i t lower. Zone i s

t r 401 351 .OO 351.83 .83 < ,001 .21 ,031 .Ol .05

10 402 351.83 353.00 1.17 .DO2 . 3 5 1.457 .03 .48

13 403 353.00 354.00 1.00 ,001 -13 ,874 .02 -82 12 404 354.00 355.00 1.00 ,001 -20 1.090 .02 .56

4 405 355.00 356.00 1.00 ,001 -08 ,457 (.Ol .82

8 406 356.00 357.00 1.00 ,002 .23 2.551 .01 .23

15 407 357.00 358.00 1.00 ,001 -25 1.598 .09 -85 12 408 358.00 358.49 .49 ,001 .27 1.087 -32 1.76

HOLE # : 6-94-1 ' ,

OREQUEST CONSULTANTS LTD, HOLE il : G-94-1 PAGE I 7 o f 7

DESCRIPTION % SAMFLE No. FROH TO LENGTH Au Ag Cu Fb ln SULPHIDE opst opst pc t pct pc t

358.49 359.42 MZ s i l 359.42 360.31 MZ s i l 360.31 361.36 MZ s i l

361.36 371.04

361.36 362.00 LST carb 10 366.87 369.82

371.04

s i l i c i f i e d w i t h p i rvas ive f i n e grained s i l i c a and 5-152 c l e a r i s h q t z augens and .: inded blebs.

-60% massive PO, 2% cpy, 2% sph 64 409 358.49 359.42 .93 ,002 .37 .666 .30 4.91 -20% PO, 3t C P ~ , 3% sph 25 410 359.42 360.31 .89 <.001 .22 1.344 .23 1.42 -60% nassive pn I02 dissen cpy, 5t dissen sph, and trace galena 15 411 360.31 361.35 1.05 ,001 .57 3.785 .31 2.35

LlMESTONE / HRR5.F.

Abrupt contact wi th Massive sulphide zone, no f o o t n a l l a l t e r a t i o n . The u n i t i s well bar j i td / laminated a t 10. The bands are c h l o r i t i c and p lanar though :OSK sec t ions of wavy f o l i a t i o n .

-as general d e s c r i p t i o n 412 361.36 362.00 ,64 c.001 .05 ,006 .01 .01 3 - 8 2 qtz-carb I ,::ision gash i n f i l ings and d is rup ted h igh angle

carb ve in ing

END Of HOLE

0 RE Q U E S T C 0 N S U L T A N T S L T D - DIAMONG GRILL HOLE RECORG C1 i e n t GEIHLEHEM Page fl 1 o f 6

Hole No. G-94-? Nor th ing 3119.33 Core S i i e NQ I 1 Depth D i p Azimuth Depth D ip Azimuth S t a r t e d JULY 26, 1994 Target MINE OREBODY F r o p e r t i GOLOSIREAM East ing 15926.48 Casing 10 ' PVC PIPE 70.9 - 90 146,6 - 88 184 Completed JULY 31, 1994 Comments HOLE CEHEEIED Locat ion REVELSTOKE E l e v a t i o n 664.59 l e n g t h 392.07 192.4 - 85 200 268.6 - 83 205 Drill Co. OLYNPIC RIS 82M/9W l a t i t u d e 51 38' 00" R ! . ip -Co l la r -90 314.3 - 80 206 390.5 - 18 208 logged By W . RAVEN Claim No Longi tude 118 24' 40" W ~ e a r i n g N/A U n i t s METERS

FROM T O ROCK At1 FOL TYPE C I A

GESCRIPTION 2 SAMPLE No. FROM T O LENGTH Au Ag Cu Pb Zn SULPHIDE ops t ops t p c t p c t p c t

59 I 15

59.15 116.35

55.15 87.10

60.84 61.48 63.04 63.82 66.43 67.13

74-92 75.30 7G.24 77.97 80.40 81.35

84.45 87.10

87.10 103.06

92.20 32.50 q4.40 103.06

OVERBURDEN

CARBONATE FACKPX (BADSHOI AND MOHICAN FORMATIONS)

ARGILLACEOUS L lPiSIONE

Carbonate package c o n s i s t i n g o f we l l f o l iated/banded c h l o r i t e - b i o t i t e + / - s e r i c i t e (?,MI%) i n a carbonate m a t r i x = a r g i l l a c e o u s l imestone, Loca l c lean inai.b:e/l imestone sec t ions . i f i n o r secondary c ross c u t t i n g carb v e i n i n g (1~::) a t 70-90 t o SCA. L o c a l l y f r a c t u r e d and broken. Minor d issen ina ted py and PO ( t race-1%) . f o l i a t i o n a t 40. Q t z augens i t r a c e - 2 2 ) ) . Good recovery a t 98-100%. Loca l S3 d e f o r n a t i o n and l o c a l t a n b i o t i t e . L w t r con tac t i s a g radat iona l change.

-53 f o l d i n g a t 'C

- S 3 f o l d i n g a t 75 -broken q t z ve in , UC broken, LC a lso broken bu t approx 80, v e i n has

massive c l o t s o f pa t o 101 with l b py, average su lph ides = 42 -broken and f r a c t u r e d with rubb le -52 carb-q tz tens ion gash i n f i l l ings, s t ronger f roR 79.00-79.77 -broken and f r a c t i r r e d bar ren q t 2 v e i n save f o r one c l o t o f PO,

u n c e r t a i n contac ts -broken and f r a c t l i r e d throughout

GREY MARBLE

Grey-nh i te c lean marble w i t h l o c a l a rg i l laceous sec t ions . I t i s a r e c r y s t a l l i z e d 1 imestone - mediua grained. Contains (1% g r a p h i t i c s t y l o l i t e s . Trare It d issen ina ted py and PO. Upper and lower contac ts a re g radat iona l rhanges. Where banded f o l i a t i o n a t 45. Good recovery throughout u n i t at 95-1001

-carb v e i n i n g at '0 - l o c a l s e c t i o n s o f i n t e r c a l a t e d C h l o r i t e - S e r i c i t e F h y l l i t e genera l l y <lOcm l o n g and '5% o f u n i t

OREQUEST CONSULTANTS L T D , HOLE 1 : 6-94-2 PAGE B 2 o f 6

FROM T O ROCK At1 FOL IYFC CiA

OESCR IF1 ION f SAMFLE NO. FROM TO LENGTH Au A9 Cu Fb Zn SULFH IDE opst opst pc t pc t pc t

103.06 116.35

~~ ~~~ ~~

INTERCALATED MARBLf / CHLORITE - S E R I C I T E PHYLLITE

I O E . ~ ~ 107.14

116.35 39?.07

116.35 141.40

116.35 117.99 117.99 121.04 121.04 123.80 123.80 127.15

127.15 133.23

133.23 134.15 134.15 136.28

136.28 137.00 137.00 137.91 137.91 139.85 1 3 ~ 5 142.68 142.68 147.40

147.40 350.33

U n i t i s l a r g e l y c lean marble as above w i th 20% i n te rca la ted CSP. Some banded section: and laminated i n t e r v a l s with f o l i a t i o n a t 45. Trace-1% disseminated py and PO. Upper contact q u i t e a r b i t r a r y wh i le lower contact sharp a t 40. Minor tan b i o t i t e t o 5% i n the CSP.

-Ch lor i te -Ser ic i t -e P h y l l i t e , UC and I C sharp at 40

LOWER ItJDCX FORMAT I O N

CHLORITE - SERlCIlE PHYLLITE

Pale greenish-grey t o green cololrred rock, greyish sections are s e r i c i t e r i c h , green sec t ions are c h l o r i t e r i ch . Variable s i l i c i f i c a t i o n w i t h approx 502 moderately t o s t rong ly s i l i c i f i e d . Comprised o f c h l o r i t e (20-40\), s e r i c i t e (20-40%), and f ine quartz- feldspar? mat r ix (20-30%), b i o t i t e (%), qtz augens (1-3t), and t race- 12 disseminated py and PO. Well f o l i a t e d a t 40. Upper contact sharp a t 40, lower contac t i n lOcr gouge zone. Broken and f rac tu red over l a r g e sec t ions w i t h Fau l t gouge and rubble w i t h ioderate recovery averaging 60-70t over e n t i r e u n i t . Uppermost p a r t i s competent.

-competent core, good recovery a t 981 -broken and f rac to red , 60% recovery -semi competent w i t h 90% recovery -h igh ly f r a c t u r e d and broken w i t h l o c a l strong gouge, rubble and rock

ch ips throughout most o f i n t e r v a l w i t h 50-602 recovery - f a i r l y competent bu t s t rong ly f rac tu red and s t rong ly s i l i c i f i e d w i t h

8 0 4 5 % recovery -broken w i t h gouge, 50% recovery - f a i r l y competent, weakly s i l i c i f i e d , w i th broken q tz ve in from

-gouge, rubble and rock chips -competent bu t ~ t r o n g l y f rac tu red -s t rong ly broken and f rac tu red m i a p e t e n t bu t s t rong ly f rac tu red -s t rong ly f rac tu red , minor sol i d core

DARK BANDED PHYLLIlE (CALCAREOUS TAN B I O T I T E - BIOTITE - CHLORITE PHVLLITE)

134.70-134.80

Brown-black co lour w i t h white calcareous bands. D i s t i n c t l y banded and re11 f o l i a t e d . Comprised of carbonate (25-40%), c h l o r i t e - b i o t i t e t i - graph i te mix = a rg i l laceous i a t e r i a l (30-40%), tan to bronze b i o t i t e (5-2021, p a l e grey quartz (10%). Quartz as layers p a r a l l e l t o S 2 and

HOLE # : 6-94-2

OREQUEST CONSULTANTS L T D - HOLE I : 6-94.? FAGE I 3 of 6

F R O M TO ROCK A L T FOL TYPE C I A

RESCRIPT 10N % SRMFLE NO. F R O M TO L E N G T H Au A9 Cu Fb l n SULPH ID! opst opst p c t p c t pc t

147.40 151.25

151.25 153.40 176.40 176.50 183.48 184.77 196.82 197,06 200.50 206.52

207.52 208.30

208 .S4 208..86 221.56

222.00 222.45 222.45 222.55 224.12 224.22 227.79 228.84 235.70 235.78 241.69 243.45

245.83 251.40 252.13

262.80 274.51 274.76 276.15 276.25

276.25

300.60 301.37 307 I 60 307.66 308.96 309.05 317.31 319.62 319.62 320.13 328.29 328.50 339.05 339.17

341.23

as augens//boL:'is, cross r u t t i n g carbonate veins (1-32) and ub iqu i tous PO ' t i n y b lebs and l a y e r p a r a l l e l s t reaks averaging 1-32 but l o c a l l y up to 5-7%. Rela t ive percentage o f c o n s t i t u e n t s v a r i e s n o n - s y s t e f l a t i r a l l y downhole. F o l i a t i o n a t 40 gradua l ly f l a t t e n i n g dornhole as a: k l e f l a t t e n s w i t h depth, genera l l y p lanar w i t h wavyi undulose s e c t k . Recovery i s exce l len t a t 100%. Upper contact in lOcm gouge zone. tower contact conformable a t 10 t o SCA. General ly 1001,: r l u i t e homogeneous, minor broken sec t ions .

-2-4% qtz -carb ! rns ion gash i n f i l l i n g s w i t h lOcn gouge a t

- C h l o r i t e - S e . i r i t e P h y l l i t e , conformable a t 40 t o SCA -q tz vein, t ra,< PO

-1 i g h t e r co lour , 30% tan b i o t i t e -s t rong gouge and rubble with 31 py -wavy f o l i a t i o n and S3 crenu la t ion cleavage a t 6 0 , increase i n

pa and s i l i c i f i e d -h igh angle q tz -carb ve ins a t 85, 2ma wide except one v e i n i s 1.5cn

o f most ly q tz , b i g ve in i s broken with broken core t o 208.50 -S3 c r e n u l a t i o n cleavage a t 50-60 -5mm PO ve in w i t h t r a c e cpy a t 30 which i s p a r a l l e l t o f o l i a t i o n -S3 f o l d , a x i s a t 55 t o SCA -S3 minor f o l d : ,t 40-70 w i t h c renu la t ion cleavage - q t 2 vein, 1% dksem PO -S3 f o l d a t 50 t o SCA -conforaable q tz ve in , 1% PO, f o l i a t i o n now a t 30 t o SCA -conformable q t z vein, 1% PO, -con tor ted f o l i a t i o n w i t h c renu la t ion cleavage and minor f o l d s a t

50-70 and bar ren qtz ve in a t 242.32-242.42 -minor f o l d a x i s a t 60 t o SCA -re-ground core, must have f a l l e n out o f tube, 852 recovery -8mn qtz-carb v e i n with 10% aassive PO c l o t s o f f s e t s S2 by l c m -S3 c r e n u l a t i o n cleavage a t 60 t o SCA -broken core, minor gouge -beconing more s i l i c i f i e d downhole, l o c a l 1 ilny sect ions, f o l i a t i o n f l a t t e n i n g t o 20

-S3 deformat ion a t 50-60 as c renu la t ion cleavage and minor f o l d s -conformable qti ye in with 4% PO b lebs m n f o r a a b l e q l z :ein w i t h 1% PO b lebs -2% qtz-carb t f . . ' ion gash i n f i l l ings above zone o f broken core -broken and fr.,lL i red core 3 weak shear or f a u l t zone -q tz f looded (10-10%) as conformable veins w i t h (1% PO

-q tz vein, conforniable a t 15, (1% pa 4 3 f o l d a x i s a t 40

150.75-150.85

HOLE #: 6-94-2

PAGE 1 1 o f 6 OREQUEST CONSULTANTS LTD. HOLE I : 6-94-2

FROM T O ROCK ALT FOL DESCRIPTION 2 SANPLE NO. FROM TO LENGTH Au Ag Cu Fb Zn TYPE C I A SULPH IDE opst opst p c t p c t p c t

350.33 355.79 GARNET ZONE (DARK BANDED FHYI. I T E , QUARTZ - CARBONATE SUTURED GOUGE ZONE)

Zone i s neak ly r j r a p h i t i c w i t h v a r i a b l e garnet con ten t (1-38). A very d i s t i n c t f a u l t ;otie i n dark banded p h y l l i t e . U n i t was broken then subsequent ly he;.iEd with q tz -carb v e i n i n g with 209, tens ion gash i n f i l l ings. Upper contac t l o o k s c o n f o r i a b l e a t 10 t o SCA, l o w e r contac t a l s o appeGrs confornab le bu t i s broken. L o c a l l y q u i t e vuggy with q t z c rys ta l : in open space f i l l i n g s . Ueak su lph ides as It dissea PO. L o c a l l y s i l i c i f i e d , s t r o n g l y b r e c c i a t e d appearance.

355.79 359.49

359.41 360,43

360.43 362.33

362.33 367.11

362.33 364.40 364.50 366.17 366.17 366.75 366.95 367.11

GARNET ZONE (DARK BANDED PHYLLITE)

More t y p i c a l l o o h i n g garnet zone in DBP. U n i t i s s t r o n g l y s i l i c i f i e d with 5-10t p i n k garnets 1-lOme averaging 311. 1-2t qtz -carb t e n s i o n gash i n f i l l i ngs . Graphi te p a r t i n g s a long S2 a t 10. Again 1 i t t l e su lph ides as 1% i:.ssen PO. l l i n o r S3 c r e n u l a t i o n f o l d i n g , axes a t 60. Lower c o n t a c t reasonably sharp a t 55 t o SCA.

GARNET ZONE (SILICIFIED CHLORITE - SERICITE PHYLLITE)

M o t t l e d green - giry c o l o u r with 10-15% p i n k garnets 1-lOmn. 1% dissem PO. U n i t i s s t r o n g l y s i l i c i f i e d . Lower 8cn i s healed fa lu l t b r e c c i a a t gradual /arbi ! i -ary lower contac t .

GARNET ZONE (BRECCIATED SILICIFIED CHLORITE - SERICITE PHYLLITE)

Abundant garnet:, a i e r a g i n g 30%. U n i t has brecc ia ted appearance with 5% qtz -carb ten:ioti gash i n f i l l ings. Local p i t t e d core sur faces due to weathered o u t czrbonate.

GARNET ZONE (SILICIFIED CHLXI!E - SERICITE PHYLLITE)

Greenish-grey t o bldck-brown co lour . Seems t o be par1 CSP and DBP with l o c a l l imestone. V a r i a b l e garnet con ten t of 5-25,. w i t h no garnet in the l i m y s e c t i o n s . Sulphides are 1% dissem PO. No graph i te .

-semi b r e c c i a t e d appearance w i t h c h e r t y sec t ions -more t y p i c a l l o o k i n g CSP - l i n y bed, no garnets - s t r o n g garnets dnd 2U% n ispy PO

HOLE #: 6-94-2

OREQUEST CONSULTANTS L T D . HOLE I : G-94-2 FAGE I 5 o f 6

fXOH T O ROCK ALT FOL TYPE CIA

DESCRIFTION % SAMPLE No, FROM T O LENGTH A i l A9 Cu Fb Zn SULPHIDE opst opst p c t p c t pc t

367.11 369.20

369.20 370.44

370.44 374.11

~~ ~~

CHLORITE - SER:"TE PHYLLITE

As p r e v i o u s l y l ? c c r i b e d , 116.35-147.40. F a i r l y t y p i c a l l o o k i n g CSP. Very minor gar1 1'5 (<1%), upper contac t sharp a t 10 t o SCA, l o n e r c o n t a c t i n gou,-

GARNET ZONE (DARK BANDED FL"L ITE)

Abundat garne ts (30%) i n smal l i n t e r v a l t h a t has been f o l d e d s t r e t c h i n g the f o l i a t i o n o u t t o 70-85 t o SCA. l o c a l q t z v e i n i n g w i t h massive b l e b s o i PO and f i n e d issen PO throughout averaging 5-81, Fron 370.19-370 4 4 i s 15% banded PO.

ARG I Ll ACEOUS L IMESTONE

D i r t y l o o k i n g 1 iinestone with CSP. Sharp upper contac t a t 10, lower contac t g r a d a t i m l with 5% garnets over lower 40cn. Hoderate S3 de format ion thral ighout as c r e n u l a t i o n cleavage a t 55 t o SCA. Has 2.5% q tz -carb t e n s i o n gash i n f i l l ings.

374.11 375.55 dASSIVE SULPHIPE !ONE

S i l i c e o u s m a s s i e su lph ide zone i n DBP. Small zone above main zone. Comprised o f 408 po as wispy l a y e r p a r a l l e l b lebs with t r a c e cpy. U n i t i s s t r o n g i , s i l i c i f i e d . Upper and l o n e r contac ts a re f a i r l y sharp bu t brokcr i .

374.11 375.55 MSZ s i l 10 -as general de 'c l i p t i o n 40 113 374.11 375.55 1.44 (.DO1 .03 ,080 .04 ,01

375.55 378.25 ARG ILLACEOUS L ! tiF ;TONE

As p r e v i o u s l y d p c r i b e d , 370.44-374.11. Upper and lower contac ts are broken. re covet^ i s good a t 98%

378.25 381.65 HANGING WALL GI:' CMINATED/STRINGERS SULPHIDE ZONE

U n i t 15 l i k e l y r c p t h a t i s q u i t e broken throughout. Most ly gouge and r u b b l e over upyy-nost 1 . 5 ~ . # i n e r a ) i z a t i o n cons is ts o f PO (5-1021, cpy (1-S%), ano i p h (1%) as f i n e pervasive disseminat ions and wispy t o massive b lebq (massive l o c a l over 5cn). Only lower 1.h i s s i l i c i f i e d .

378.25 380.18 HUSSZ ch l ,ser 10 -50% gouge and - m b l e , r e s t s t r o n g l y f r a c t u r e d and broken, recovery 1 i s 702, 5% b r o h q t z v e i n i n g

414 378.25 380.18 1.93 (.001 <.01 ,039 .01 .06

HOLE 1: 6-94-2

OREQUEST CONSULTANTS L T D . HOLE I : 6-94-2 PAGE I 6 o f 6

FROM T O ROCK TYPE

ALT FOL C I A

380.18 381.65 HWSSZ

181 I 65 386.28

381.65 382.65 MSZ 382.65 383,65 MSZ

383.65 384.65 MSZ 384.65 385.65 MSZ 385.65 336.25 MSZ

386 I 28 386 I 95

386.28 386.95 LST

386 I 95 381.45

386.95 381.45 MSZ

381,45 392.01

387.45 388,34 LS1

392.07

s i l 10

s i l s i l

s i l s il s i l

s i l

s i l

carb 25

DESCRIPTION % SAMPLE NO. FROM 10 LENGTH Au Ag CIA Pb Zn SULPH IDE opst opst pc t p c t pct

-broken and f r z r - ired w i th stronger sulphides, f r o # 380.18-381.13 8 415 380.18 381.65 1,4? .002 .14 1.704 .01 .31 i s 5-72 PO, 1.;' cpy and t race sph, from 381.13-381.65 i s 2% PO

5-62 cpy and 15 ' t rong ly s i l i c i f i e d

MASSIVE SULPHIF 'ONE

S i l iceous m a s s k sulphide zone. Conprised of 'up to 20% grey rounded quartz blebs and 5 1 0 % i a t r i x quartz w i th 501 PO and 10-201 cpy and 1-52 sph. Sulphide: are as massive concentrat ions w i th some areas o f wispy blebs. Also approx 5% f i n e grained carb i n Matrix, as m a l l blebs and very niinor veins. The PO i s moderately magnetic.

-30-352 PO, 15-20; cpy, broken from 382.13-382.25 50 416 381.65 382.65 1.00 ,008 -46 4.627 -06 1.49 -broken and f r a c h r e d t o 383.23 with manganese on f rac tu res , 75 417 382.65 383.65 1.00 .005 .?O 5.811 -36 4.10 502 PO, 20% cpy, 5% sph

-502 PO, 159. cr,, 3-42 sph 68 418 383.65 384.65 1.00 ,006 1.01 6.401 .79 6.31 -40% PO, 202 cp,, 5% sph t o 385.17 then 20% PO, 5% cpy, 1-21 sph 55 419 384.65 385.65 1.00 .006 .50 4.662 .17 2.46 -40% PO, 209, CP,, 39, sph 63 420 385.65 386.28 .63 ,003 .58 5.'491 - 2 1 4.20

LIMESTONE

Sharp upper contact a t 10 t o SCA along 2cn carb vein, upper lOcn we l l mineral izrd. 10% qtz-carb tension gash i n f i l l i n g s

-as general d e s i tp t ion 2 421 386.28 386.95 .61 c.001 . 22 ,584 .24 2.90

MASSIVE SULPHICL ZONE

As described 381.65-386.28. Uppper and lower contacts broken.

- r i c h sec t ion with 552 PO, 30% cpy 85 422 386.95 387.45 -50 ,005 1.82 10.662 1.11 7.70

LIMESTONE

Banded w i t h 10; ; i rgi l laceous material I Minor g raph i t i c s t y l o l i t e s . Local q tz -carb 1 . i c c i a veins 1-2cn wide. f o l i a t i o n at 25-35 t o SCA

-as general der r p t i o n t r 423 381.45 388.34 -89 <.001 (.01 ,013 - 0 1 .01

END OF HOLE

0 REQUEST C 0 N S U L T A N T S L T D - DIAMOND DRILL HOLE RECORD C1 i e n t BETHLEHEM Page II 1 o f 7

Hole No. 6-94-3 N o r t h i n g 3089.95 :ore Size NO I1 Depth D i p Azimuth Depth D ip Azimuth S t a r t e d JULY 31, 1994 Target MINE OREBODY Proper ty GOLDSTREAM f a s t i n g 15952.30 r a s i n g 1O'FVC PIPE 72.6 - 89 020 152.4 - 88 145 Completed AUG. 13, 1994 Comments HOLE CEMENTED L o c a t i o n REVELSTOKE E l e v a t i o n 665.35 .ength 38?,62 228,6 - 87 176 304.9 - 85 200 Drill Co. OLYMPIC !IS 82M/9W L a t i t u d e 51 38' 00" N : { p - C o l l a r -90 381.1 - 83 202 Logged By id. RAVEN Claim No Long i tude 118 24' 40" W i e a r i r i g N/A U n i t s METERS

.-

FROM TO ROCK At1 FOL OESCRIFT ION !2 SAMFLE No. FROM TO LENGTH Au A9 Cu Fb Zn TYPE C/A SULPHIDE opst opst p c t p c t p c t

52.44 OVERBURDEN

52.44 96.72 CARBONATE PACKAGE (BADSHOT AND MOHICAN FORIATIONS)

52.44 70.50 ARGILLACEOUS L IHESTONE

64.55 65.70 66.16

70.50 80.15

70.83 73.35

7a.20 78.50

80.15 96.72

Carbonate package c o n s i s t i n g o f w e l l f o l iated/banded c h l o r i t e - b i o t i t e 4/- s e r i c i t e p h y l l i t e (30-402) i n a calcareous m a t r i x = a r g i l l a c e o u s 1 imestone. Contains 1-39 cross c u t t i n g q tz -carb ve ins a t 60-85 t o SCA and 1-2% qt2 augens and boudins. Trace - 1% disseminated p y and PO. Local S3 deformat ion, f o l i a t i o n a t 40 t o SCA. Loner contac t g radat iona l I L ? c j i s t rong green c h l o r i t e and t a n b i o t i t e .

-S3 c r e n u l a t i o r cleavage a t 60 -carb v e i n 5 - ~ P V i i d e a t 80 crea tes f r a c t u r e d core

GREY MARBLE

Grey ish-wh i te to:oured medium gra ined r e c r y s t a l l i z e d 1 imestone with (5% a r g i l l a c e o u s l i a t e r i a l as f o l i a t i o n p a r a l l e l bands a t 40. Contains 1% g r a p h i t i c s t ; i ~ l i t e s . Upper and l o n e r contac ts are g r a d a t i o n a l . M i n e r a l i z a t i o n -Lsrlsists o f t race-1% dissen. py and PO. Local broken sec t ions . Good i i i o v e r y a t 95-100%.

-broken and frz-1 i red with lOcn gouge a t s t a r t o f sec t ion , l o c a l l y s o l i d core, t:. i n t e r v a l has weathered out g raph i te -carbonate s t y l o l i t e s

-broken and fr?:: ired, p a r t i a l CSP

INTERCALATED G R E Y MARBLE / CHLORITE - SERlCITE PHYLLITE

L a r g e l y c lean marble as above with 101 i n t e r c a l a t e d CSP. Most sec t ions o f CSP are (lOtm long. F o l i a t i o n a t 30-35 t o SCA. Minor g r a p h i t i c s t v l o l i t e s i n the marble.

HOLE 1 : 6-94-3 PAGE il 2 o f 7 OREQUEST CONSULTANTS L T D ,

FROM T O ROCK ALT FOL IYPE C I A

. _ DESCRIPTION S, SAMPLE No. FROM T O LENGTH Au Ag Cu Pb Zn SULPH 1DE opst opst p c t p c t pc t

83.54 83.67 86.43 87.37 90.35 90.40 11.17 93.50

96.72 382.62

96.72 143.30

-broken and f r a c t u r e d - C h l o r i t e - Sep:ci te P h y l l i t e -broken and f r a c t u r e d -broken and f r a c t u r e d w i t h h i g h angle carb veins

LOWER INDEX F O P M A T I O N

CHLORITE - SERlCiTE PHYLLIIE

97.10 97.44 102.74

103.05 106.00 106.06 106.12 110.13 115.06

115.06 117.38 118.20 118.35 119,OO 119.15 119.45 119.55 121.10 125.88

129.15 129.90 130.18 135.46

135.46 139.33

139.33 143.30

143.30 346.89

Pale green t o 1,r enish-grey coloured rock. Local sec t ions are darker co loured due t o b i o t i t e a t the expense o f c h l o r i t e and l o c a l l y s t r o n g l y broker1 and f rac tu red . Conprised of c h l o r i t e (30-40%), s e r i c i t e (30-40%!, quar tz (5%) as p t y g ~ a t i c veins and boudins, b i o t i t e (1-5%), carbonate in mat r ix ( t race-1%) and 1% f i n e grained dissen py and PO. Upper contact i s sharp a t 35 t o SCA, lower contac t i s g radat iona l w i t h some i n t e r c a l a t e d DBP. U n i t i s wel l f o l i a t e d a t 35-40 t o SCA. L o c a l l y s i l i c i f i e d .

-broken and f r a c t u r e d w i t h gouge -1cn o f gouge - l o c a l s e c t i n s o f c r e n u l a t i o n cleavage and minor f o l d s a t 60 -barren q t z v e i n -BIOTITE - S E R l C l T E PHYLLIIE, reddish-grey-brown co lour with b i o t i t e

ins tead o f c h l o r i t e with broken sec t ions a t 110.84-111.03 and 113.68-113.82

- s t r o n g l y broken and f r a c t u r e d with 90% recovery - s t r o n g l y broken and f r a c t u r e d - s t r o n g l y broken and f r a c t u r e d - s t r o n g l y broken and f r a c t u r e d - s i l i c i f i e d with f i n e grained q t z , s t r o n g l y broken and f r a c t u r e d a t 122.60-123.39 and from 125.68-125.88

- i n t e n s e l y f r a c t u r e d n i th 30% recovery -more t a n b i o t i t e , l e s s c h l o r i t e , weakly t o aoderately s i l i c i f i e d ,

i n t e n s e l y f r a c t u r e d a t 132.10-132.65 with 60-70: recovery - s i l i c i f i e d and s t r o n g l y f r a c t u r e d and broken CSP w i t h 5-102 quar tz -

carbonate tens ion gash i n f i l l i n g s , p i t t e d core surfaces due t o weathered ou t carbonate

-DBP t o 138.80 then greenish-grey CSP t h a t i s s t rong ly broken t o 140.60 then N C ~ . r a t e l y broken t o 143.30, lower lOc# i s gouge

DARK BANDED PHYLL I I E (CALCAREOUS CHLOR!TE - BIOTIIE - GRAPHITE + I - S E R I C I T E PHYLLIIE)

Well banded and to1 i a t e d u n i t a l t e r n a t i n g whi te carbonate and b lack c h l - b i o - g r a p h i t e hands. Conprised o f carbonate i30-501), with c h l - b i o - g raph i te -ser (3') 155), q t z augens and p tyqnat ic veins (2%) and cross

HOLE #: G-94-3

OREQUEST CONSULTANTS L T D - HOLE B : 6-94-3 PAGE R 3 o f 7


OESCR IPT ION 1 SAMFLE No. FROM TO LENGTH Au Ag Cu Pb i n SULPHIDE OpSt OpSt pCt pCt pCt

153.33 153.50 156.87 157.06

161.66 163.06 163.72 161.66 169.87

169.90 170.00 114.65 174.14 185.50 185.60 185.91 186.12 186.50 186.65 192.82 192.90

203.92 209 I 25 209.30 210.14 210.22 211.43 211.56

212.23 233.35 233.65

233.65 241.49 241.82 253.25 254.74 263.80 264.22

210.00 274.08 274.20

280.00 284.21 284.57 289 I 82 290.62

291.04 291.31

291.36 291.72 294.28 294.48 101.74 301.83

c u t t i n g carb v e i n s ( 1 ~ 2 % ) - P y r i t e and p y r r h o t i t e are ub iqu i tous a t (1-31 combined", l o c a l l y h igher concentrat ions as f i n e gra ined b lebs u s u a l l y p a r a l l i 1 t o f o l i a t i o n . R e l a t i v e percentage o f c o n s t i t u e n t s v a r i e s non sys temat ica l l y downhole. f o l i a t i o n a t 30 g radua l ly f l a t t e n i n g dowiNhcle. Upper contact i n 10-15cm wide gouge zone, lower contac t i s gouge bu t appears conformable a t 10 t o SCA. Local S3 d e f o r m t i o n as c r e n u l a t i o n cleavage and minor f o l d s . Approx 10% s e r i c i t e ill I -n i t , more pronounced i n areas o f S 3 deformat ion.

-broken and f rac t l r red -2-4ca wide q t i ve in w i t h 1-22 PO, v e i n a t 10 4 3 f o l d a t 55 -broad S3 f o l d produces f o l i a t i o n a t 70 t o SCA -area o f S3 d e f a m a t i o n as broad open f o l d s over SOcm and t i g h t

c r e n u l a t i o n f c l d s and cleavage a t 60 t o SCA -broken and f r a i t i i r e d -q tz ve in a t 35, barren -broken and f ra ' - tv red -broken and f r a i t i red -broken and fract.lired -gouge zone, a p r e i r s c o n f o r i a b l e a t 30 t o SCA -3-4mm wide PO , f ' n a t 30 t o SCA -conforMable q i i .e in , 1% PO -conformable q t r : e m , 1% PO -broken and fra 1 , red - n i n o r f o l d a t ;O t o SCA -PO enr iched sec t ion up t o 5-68 - f o l i a t i o n f l a t t e n i n g t o 25 t o SCA -S3 f o l d a x i s acd c r e n u l a t i o n cleavage a t 55 t o SCA -broken i n h a l f a long 1-2nm wide carb v e i n a t 85-90 t o SCA -S3 c r e n u l a t i o n cleavage a t 50 t o SCA - u n i t now moderate:y s i l i c i f i e d t o end o f DBP -broken and frac:u:ed - f o l i a t i o n s t i l l d! 25 t o SCA -broken and f r a i t i i r e d -broken and f r a t t h r e d w i t h S3 f o l d axes a t 40-50 t o SCA, i n t e r v a l

con ta ins broke:, , q g y q tz -carb ve in ing a t 80 t o SCA with small q t z c r y s t a l s irl o;sen space f i l l i n g

- q t z vein, q u i t c t d r r e n with rare specks o f PO, upper and lower contac ts appro} !!! t o SCA, 5cm o f broken core below the ve in t o 291.36

-S3 f o l d s and c i ! r i8 ,1a t ion cleavage a t 60 t o SCA, 20% s e r i c i t e - q t z ve in UC a t 10, LC a t 50, 1% PO b lebs -qt2 vein, confctmdble a t 20-25 t o SCA which i s a lso f o l i a t i o n angle

v e i n has 2% PO 4: f i n e t o coarse ( 4 x 5 ~ ~ ) blebs

HOLE W I 6-94-3

.

304.68 305.26 315.10 315.15 317.21 311,35 325.30 325.70 326.62 326.16 330.30 330.56 33R.01 338.12 334.00 346.89 340.14 340.22 341 .ll 341.88 342.46 342.66 342.91 343.05

346.89 351.44

OREQUEST CONSULTANTS LTB fi HOLE II : 6-94-3 PAGE 1 4 o f 1

Pb :n FFOM T O ROCK ALT FOL DESCRIPTION 2 SAMFLE NO. fROM T O LENGTH Au A9 Cu TYFE CIA SULPHIDE opst opst pct p c t pc t

- t i g h t n i n o r i s o c l i n a l f o l d s a t 10-20 t o SCA -broken core, g r a p h i t i c -broken core, minor g r a p h i t i c gouge - @ i n o r S3 d e f o r r a t i o n -confornable qtz Yein, trace dissen po -broken core, 2% qtz-carb tension gash i n f i l l i n g s -broken core - s i l i c i f i e d -conformable q t z vein, trace PO blebs -S3 c renu la t ion fo lds and cleavage a t 60 t o SCA -as above -q tz vein, trace PO

j49.40 349.52

352.90 353.45 356.08 356.37 356.65 351.44 GZ si1,gar

357.44 358.49

357.44 358.49 MSZ s i 1

358.49 366.21

GARNET ZONE (SUTURED FAULT 2OuE IN DARK BANDED PHVLLITE)

Host u n i t i s lwjt l y DBP w i th n i n o r l o c a l sections resembling CSP. H igh ly deformed tbroughout, appears t o be a f a u l t zone as u n i t has been broken and i w t o r t e d and subsequently healed w i t h f i n e s i l i c a as u n i t i s pervas i .e lg s i l i c i f i e d . Also contains 5-101 qtz-carb tension gash i n f i l l i n g s . Graphite read i l y v i s i b l e on S2 par t ings . Local cherty bands. Contains 1 y h t p ink garnet porphyroblasts averaging 5% but l o c a l l y h igher , : 4 m m (rounded) up t o l O m m , Local s e r i c i t e t o 10%. M i n e r a l i z a t i o n 5 , f i n e grained dissea PO, 1-3t. Upper contact i s gouge but appears c o n f . : m b l e at 10 t o SCA. tower contact broken but approx 20-30 to SCA, Q t i veins comprise 5-109 o f u n i t w i t h 206 qt2 blebs. Variable breccia, ion throughout u n i t .

-qtz vein, UC arid :C a t 25-30 t o SCA, 5 4 % contorted graphite veins and 2-31 py and 1 . 2 % PO as dissem blebs

-30-35% qtz ve in f 'ood ing -enriched PO avf .ajing 15% -broken and frai.!,ired, i n t e n s i t y increasing downhole, 15-20? garnets, 5% PO most obv ,w;: on f rac tu re planes

MASSIVE SULPHIDL 7'INE

S i l i c e o u s massive ,.ulphide zone i n DBP. A s n a l l zone above the main zone. Comprised r!f 40-602 PO as massive and wispy l a y e r p a r a l l e l blebs, t race cpy intergrown w i t h the PO.

-as general dest r i p t i o n

SlLlClFlED CHLORIIl - SERlClTE PHYLLlTE

Mot t led grey-brown co lour w i th l o c a l wh i te r sections due t o strong

5 431 356.65 351.44 .19 <.001 .05 .030 <.01 . 0 2

,001 .04 ,081 c . 0 1 -03 50 432 351.44 358.49 1.05

HOLE d i G-94-3

OREQUEST C O N S U L T ~ N P S LTfB- HOLE II : 6-94-3 PAGE 1 5 of 7

F R O M 10 ROCK A11 FOL TYPE C I A

DESCRIPI ION 1 SAMPLE No. FROM T O LENGTH Au A9 Cu Pb :n SULPHIDE opst opst pc t p c t pct

359.90 361.45 361.82 361.89 363.15 363.57

s e r i c i t e . General ly s i l i c i f i e d except i n areas o f s t rong s e r i c i t e . F o l i a t i o n approx 20 t o SCA bu t navy due t o S3 i n te r fe rence. Local tan b i o t i t e t o 20%. Weak a i n e r a l i z a t i o n = 1% dissen PO blebs. Upper and l o n e r contac ts are gradational I Pervasive weak S3 c renu la t ion cleavage a t 50 t o SCA

-grey-white coloured sec t ion n i t h 202 f i n e grained Mat r ix carbonate -q t2 v e i n trace-1; PO -q tz f looded w i t h 3 veins a t 25 to SCA w i t h 502 s i l i c a i n i n t e r v a l

366.21 368.41

368.41 372.19

368.41 369.33 HVDSZ E i l

369.33 370.76 HWDSZ s i l

370.76 372.19 HWDSZ s i l

372.19 374.19

372.19 373.19 HUDSZ s i l

373.19 374.19 HVDSZ s i l

374.19 374.79

ARGILLACEOUS LIMESTONE

Gradational upper and l o n e r contacts. Par t clean marble w i t h up t o 402 arg i l laceous m i t e r i a l g i v i n g f o l i a t i o n a t 30 t o SCA. Contains 1-22 qtz -carb t e - i o n gash i n f i l l i n g s .

HANGING WALL DlSSEMlNAlED SULPHIDE ZONE (WEAK MINERALIZAI !1N)

Host u n i t i s si'i I( i f i e d CSP t h a t i s l o c a l l y alnost pure s i l i c a . Local s t rong tan b i o t blebs of po 1-4' m d cpy 1-42 but genera l l y i n the 1-2 range f o r both. Gradation ! upper and l o n e r contacts.

-mostly pure q t r from 368.65-369.33 averaging 3% PO and 32 cpy as f i n e dissen b l tb:

- laott led grey-brown s i l i c i f i e d CSP, l o c a l l y s t rong ly s i l i c i f i e d , average 21 PO, !: cpy

-371.17-371.57 and 371.94-372.19 i s strong tan b i o t i t e up t o 30-35%, 12 PO, 1% cpy

t o 301 over lOcn sections. H i n e r a l i z a t i o n i s dissen

HANGING WALL Dlt,SfMINATED SULPHIDE ZONE (MODERATE I INEPF, . IZATION)

Same as 368.41-:;'.19 on ly minera l i za t ion i s more prevalent, espec ia l l y over L!'? lower Petre. Host rock i s s t i l l s i l i c i f i e d CSP. Upper and lower :i:itacts are setai gradational.

-as general des, i pt ion , from 372.19-372.46 i s good sulphides n i t h -10% pa, 5% cpy, trace sph and galena then strong tan b i o t i t e t o

373.19 w i t h 2-2: PO, trace-19, cpy -more s i l i c i f e d !han above w i t h s t ronger sulphides averaging 10-151 PO, 3-5; c p y and t race spha ler i te

MASSIVE SULPHIDE ZONE

' . . I

433 368.41 369.33 .92 (.001 .04 ,277 ,03 .68

434 369.33 370.76 1 .43 <.001 <.Ol ..190 (.01 .23

435 370.76 372.19 1 . 4 3 <.OD1 .05 ., ,121 <.Ol .11 b

5 424 372.19 373.19 1.00 .001 .07 .894 < .01 .21

1 5 425 373.19 374.19 1.00 <.001 .08 ,634 <.01 .95

HOLE #: 6-94-3

OREQUEST CONSULTANTS L T D - HOLE I : 6-94-3 PAGE II 6 o f 1

FROM TO ROCK ALT FOL DESCR 1PT ION 2 SAMFLE No. FROM T O LENGTH Ai l Ag Cu Pb Zn TYPE CIA SULPHIDE opst ops t p c t p c t p c t

374.19 374.79 MSZ s i l

374.79 375.31

374.79 375.31 CSP ch1,s i l

375.31 375.51

375.31 315.51 MSZ

375.51 376.26

315.51 376.26 FWDSSZ

376.26 380.33

376.26 317.00 CSF

380.33 382.62

s i l

s i l

s i l

S i l i c e o u s mas: i v s su lph ide zone. Contains about 201 grey rounded qtz b l e b s and 51 w:iite q t z . Rest o f i n t e r v a l c o i p r i s e d o f 20-30% cpy and 502 PO which il r e r y weak t o weakly magnetic. Hanganese ? s t a i n i n g on f r a c t u r e s .

-as general de i p t i o n , 502 PO, 25'. cpy

CHLORITE - SERIClIE PHYLLITE / LIMY DARK BANDED PHYLLITE

As p r e v i o u s l y derc r ibed, broken and f r a c t u r e d near end. Contains 2-32 PO, t r a c e c r j with s t rong i i n e r a l i z a t i o n t o 374.89. Gradat iona l upper c o n t a c t , , " i l e r con tac t f a u l t e d .

-as general d e s c r i p t i o n

MASSIVE SULPHICE LONE

Small f a u l t boiinded s e c t i o n o f massive sulphides as descr ibed 374.19-374.79 ~ + more py than PO

-as general d e s c r i p t i o n , 50% py and pa, 30% cpy

FOOTWALL SULPHIDE ZONE / LIMY DARK BANDED PHYLLITE

Not sure i f hoct rock i s CSF or DBP but u n i t i s l i m y with l o c a l s i l i c i f i c a t i o n . 'on ta ins 32 qtz -carb tens ion gash i n f i l l i n g s and i s moderately a i n t i , l i z e d with 10% PO and 3-5% cpy as d isseminat ions and s t r i n g e r s .

-as general de, 8.1 i p t ion

SILICIFIED CHLO'!'E - SERICITE PHYLLITE

As p r e v i o u s l y des t r ibed. Local s t rong s i l i c i f i c a t i o n and l o c a l l i m y beds. 5 1 cross c t i t t i n g q tz -carb veins and 52 tens ion gash i n f i l l i n g s . Upper c o n t a c t ' . ~ i w h a t broken, lower contac t sharp a t 60 t o SCA. Contains 12 d i , . I PO b lebs .

- s t r o n g l y broken and f r a c t u r e d

ARGILLACEOUS L IKSIONE

As p r e v i o u s l y w x r i b e d . Strong S3 c r e n u l a t i o n cleavage throughout a t 50-60 t o S C A , 3 d issen PO blebs

75 426 314.19 314.79 .60 ,010 -92 8.890 -48 3.19

3 427 374.19 375.31 -52 C.001 -02 ,349 .01 .04

80 428 315.31 315.51 .20 .005 -99 5,600 -13 5.44

13 429 375.51 376.26 .15 ,001 .09 1.884 .02 .lo

1 430 376.26 377.00 .74 < .001 <.Ol ,084 <.Ol ,132

HOLE #: G-94-3

OREQUEST CONSULTANTS L T D - HOLE # : G-94-3 PAGE R 1 o f ?

FROM TO ROCK ALT FOL TYPE CIA

DESCRIPTION % SAMPLE No. FROM TO LENGTH Au Ag CIJ Fb i n SULPHIGE o p s t o p s t pct p c t p c t

382.62 END OF HOLE

OREQUEST CONSULTANTS LTD - DIAMOND DRILL HOLE RECORD Cl ient BETHLEHEH Page I 1 o f 7

Hole No. G-94-4 Northing 3220.20 Core Size NQ I 1 I BQ Depth Dip Az i iu th Depth Dip Azinuth Started AUG. 14, 1994 Target HINE OREBODY Property GOLDSTREAN East ing 15979.11 Casing STUCK, BLASTED 72.6 - 88 215 213.4 - a3 188 Conpleted AUG. 23, 1994 Coinents HOLE CEMENTED Locat ion REVELSTOKE Elevation 666.89 Length 451.83 289.6 - 78 220 365,8 - 75 218 Drill Co. OLYMPIC - NTS 8211911 Lati tude 51 38' 00" N Dip-Collar -90 451.2 - 72 231 Logged By W . RAVEN C l a i i No Longitude 118 24' 40" W Bearing NIA Units HETERS

FROH TO ROCK ALT FOL TYPE C I A

DESCRIPTION 2 SAHPLE No. FROM TO LENGTH Au Ag Cu Pb Zn SULPHIDE opst opst pct pct pct

79.27

19.27 183.51

79-27 85.10

85.10 91,13

95.70 120.70

OVERBURDEN

CARBONATE PACKAQ (BADSHOT AND MOHICAN FORHATIONS)

LIMY CHLORITE - SERICITE PHYLLITE I ARGILLACEOUS LINESTONE

Unit i s comprised o f banded chl-ser-bio that i s grey-brown colour (30-401) and white carbonate (30-50t ) , qtz as augens and ptygaatic veins (511, minor tan b i o t i t e (1-52) and 12 f i n e d isse i PO. Fo l i a t i on at 45-50 t o SCA, Uinor loca l broken sections, LC reasonably sharp at 10 t o SCA wi th 53 crenulat ion cleavage a t 70 t o SCA

CHLORITE - SERICITE PHYLLITE

Looks p re t t y s i a i l a r t o the nine phase CSP. S i a i l a r t o un i t above but iuch less carbonate which i s p a r t i a l l y replaced by s i l i ca . Comprised of chl-ser-bio a i x (709,), i a t r i x qtz (10-15t u n i t i s p a r t i a l l y s i l i c i f i e d ) , p t yg ia t i c qtz (5-881, tan b i o t i t e ( 6 8 ) and f i n e dissea and f o l i a t i o n pa ra l l e l PO (trace-2\), UC reasonably sharp a t 10, LC also reasonably sharp a t 50 t o SCA. Carbonate = 5-101 i n i a t r i x .

-broken and fractured

LIMY CHLORITE - S E R I C l I E PHYLLITE

As described 79,27-85.10~. UC a t 50, LC at 40 t o SCA

GREY MARBLE

Grey-white colour, aediui grained f a i r l y clean recrysta l l ized iarb le , Hinor argi l laceous nater ia l gives fo l i a ted appearance a t 30-35 to SCA. Contains 2-42 ptyg iat ic qtz. Local nore argi l laceous sect ions and trace graphi t ic s t y lo l i t es . Minor d isse i py and PO usually associated with s i l i c a enrichnent

OREQUEST CONSULTANTS L T D , HOLE B : G-84-4 PAGE II 2 o f 7


DFSCRlPl ION % SAMPLE No, FROM T O LENGTH Au A9 . Cu Pb Zn SULPHIOE opst opst p c t p c t p c t

99.16 100.26 101.10 102.30 102.89

120.89 103.12 112.70 113.10 115.26 115.70

115.60 120.70

120.70 135.26

120.70 121:04 121.04 124.08 124.08 127.13 127.13 130.18 130.18 133.23 133.23 134.76 134.76 135.26

135.26 160.41

135.26 142.38 135.45 135.86 141.75 142.02 142.48 144.60 150.04 151.10

151.20

153.50 155.78 155.78 156.00

-1-2mn PO v e i n a! 30 t o SCA -1 imy CSP -q tz v e i n poor ly de f ined UC and LC, patchy blebs o f PO up t o 5%

b u t averaging 1’ -broken and f ra r !u red with gouge over l a s t 4-5cn - s t r o n g l y brok?n and f r a c t u r e d -broken and f r d c t u r e d

- I n t e r c a l a t e d i !’ and Arg i l laceous Linestone w i th CSP t o 117.37 then 1s t t o 1. 70

FAULT ZONE ( IN APGILLRCEOUS LIMESTONE)

Host rock i s a rg i l laceous 1 s t w i t h l o c a l c lean sec t ions . Zone i s i n t e n s e l y f r a c h r e d t o shat te red and broken w i t h gouge, rubble, and rounded rock chips with l o c a l pure c l a y gouge and f i n e sand. l o c a l l y the f o l i a t i o n , \ a t 90 t o SCR though genera l l y c l o s e r t o 70 t o SCA. Var iab le recovery throughout f a u l t zone

- c l a y gouge with s e r i c i t e -509. recovery -50% recovery -409. recovery -708 recovery, i a s t 40c i i s f i n e sand -809 recovery k i t h f a i r l y s o l i d core t o 134.45 -90% recovery r , t h rock chips over l a s t 15cm

ARGILLACEOUS L I bLSlONE

U n i t con ta ins ! -ded green c h l o r i t e (20%) and brown b i o t i t e (5-101) i n a grey-white c: .onate mat r ix . Also conta ins up t o 5 t p t y g r a t i c q t z v e i n s and 1-2% cross c u t t i n g qtz-carb veins. Local tens ion gash i n f i l l i n g s . F o l i a t i o n steep a t top o f u n i t a t 60-65 t o SCA g radua l ly f l a t t e n i n g downhole t o 45. LC i s g radat iona l . S e r i c i t e 5-15%.

-2-3% qtz -carb tens ion gash i n f ill ings -q tz -carb ve in 9C a t 10, LC a t 50, minor PO and py -broken and f r a c t i i r e d -S3 c r e n u l a t i o q cleavage a t 70-80 t o SCA -broad S3 f o l d oioduces f o l i a t i o n a t 90 t o SCA

Reduce core 5 1 : ~ from NQ I I t o 60

-2-3% qtz -carb t r r ts ion gash i n f i l l ings - c a l c i t e ve in !+ ‘ h 1-21 py and ch l and g r a p h i t i c s t y l o l i t e s

HOLE # : 6-94-4

OREQUEST CONSULTANTS LTD. HOLE il : G-94-4 PAGE il 3 o f 7

FROX T O ROCK At1 FOL TYPE C I A

DESCRIPTION 2 SAMPLE No. FROM T O LENGTH Au A9 cu Pb Zn SULPH I D E opst opst pc t p c t p c t

160.41 175.10 GREY MARBLE

166.92 166.98 167.80 168.00 168.74 168.96 171,24 171.58

175.10 183.51 175.10 183.51

175.40 175.60

183.51 151.83

183.51 228.94

184.97 185.33 187.66 187.71 189.38 189.44 190.03 192.38

193.20 200.43

191.21 194.49 194.49 194.54 195.26 195.58 195.58 196.06

m a 0 193.20

197.81 198.07

Clean look ing ' I ' as described 95.70-120.78n. Minor in te rca la ted CSP. UC f a i r l y shar: t! 50 , LC i s gradational change. F o l i a t i o n a t 30-35 t o SCA. Local ;:.,phitic s t y l o l i t e s .

-broken core -CSP -ESP, UC and L C conformable t o f o l i a t i o n a t 30 -two small layers o f CSP

BADSHOT FORMAT ION INTERCALATED GPEV MARBLE / CHLORITE - SERICITE PHYLLITE

Limestone as above (60-652) w i t h in te rca la ted greenish CSP (30-402). Local sec t ions of broken core. Minor qtz-carb tension gash i n f i l l i n g s .

-broken core w i t h gouge

LOWER INDEX FORMAT ION

CHLORITE - S E R l C l I E PHYLLITE

Green t o g reen i ih -grey co lour depending upon r e l a t i v e percentages o f ch l and ser. Corncrised o f c h l o r i t e (20-4011, s e r i c i t e (20-40%), b i o t i t e (52), m i : r i x q t2 (5-15%), and p tygnat ic q tz veins and augens (1-48). U n i t i: . a r i a b l y s i l i c i f i e d and broken and fractured. Mineral i z a t i o n , dissen and f o l i a t i o n p a r a l l e l blebs o f py and PO (1-22). Some S G . : , ~ t a l c on f r a c t u r e surfaces. F o l i a t i o n a t 30 gradua l ly f l a t t ~ 8 , i n g t o 25 a t bottom o f u n i t . UC f a i r l y sharp at 30, LC somewhat gra! t i o n a l t o under ly ing DBP

-broken and f r a r t l i r e d -broken and f r i , ' i r e d -broken and frC8:.ired -broken and f rdc t , i red "poker c h i p core" -broken and fract1:red - s i l i c i f i e d s e t ' '.#n as f i n e grained pervasive s i l i c a and sone l a r g e r

q t z veins -broken and f r a t hired -q tz ve in a t 3C ! , I SCA -broken and f r a i t i l r e d -1cm wide q t z v e i l a t 85 t o SCA has 1 -2 pa blebs, sec t ion i s weakly fractur;,

-2-3cm wide q t ? . ? i n a t 75 t o SCA w i t h 1-22 PO blebs

HOLE #: 6-94-4

OREQUEST CONSULTANTS L T D , HOLE I : 6-99-4 PAGE II 4 of 1

FRUh TO ROCK A l l FOL DESCRIFTION % SAMPLE No. FROM T O LENGTH Au A9 , Cu Pb Zn TYPE C I A SULPHlDE opst opst p c t pc t pct

.~

200.83 201.22 -moderately f r i i t i i r e d 202.32 202.43 -vuggy qtz-carb ve in 204.10 217.05 -paler coloured i i l i c i f i e d sec t ion 204.33 204.58 -50-60% qtz f l t ,=d, trace PO

208.50 209.90 -moderately frat :,ired 213.12 213.90 215.52 215.51 -broken w i t h q t - fragments 215.66 215.87 -qtz vein, UC dpprox 60, LC approx 70, ve in has 3-5% massive 6

218.36 218.81 218.81 219.15 -broken and f r a r t i i r e d 219.75 219.85 -qtz vein, l b pa 221.05 128.94

-q tz vein, UC a t 7 0 , LC broken but approx 10-20, lninor traces o f PO

PO blebs and 1-21 galena blebs - f rac tu red q tz vein, UC a t 85, L C a t 45, 1-23 pa blebs

- s i l i c i f i e d sec! :on rith minor vuggy o r p i t t e d core surfaces due t o weathered w! carbonate

228.94 416.33 DARK BANDED PHYLL ITE

228.94 231.86

237.68 237.88 243.11 243.40 246.60 247.21 251.00 251.81

253.50 265.10 211.42 271.90

274.26 289.69 290.14

291.91 298.73

299.53 299.74 299.74 302.64

307.05 307.63 310.37 310.70 317.73 318.04

Banded u n i t , da layers . U n i t i s comprised of greenish b i o - c h l (30-40%), tan b i o t i t e (5-20%), carbonate (30-502) s e r i c i t e (5-10%), graphite (1-3 t ) , ptygnat ic q tz veins (1-52) and dissem and f o l i a t i o n p a r a l l e l blebs o f PO (1-5tI. Upper contact a b i t broken, lower contact sharp but a lso broken. Proport ion o f cons t i tuents var ies non-systematical ly downhole. 1-2% cross c u t t i n g qtz-carb veins. F o l i a t i o n a t 25 t o SCA.

-broken and frac:'ired w i th 5% qtz -carb tens ion gash i n f i l l ings, minor graphite, there i s CSP from 230.79-231.20

-broken and f r a i I t i red -qtz vein, UC almprox 10, LC approx 30 t o SCA, ve in has trace-1% pa -broken and f r a r h r e d w i t h g raph i te -Minor broken cnrr w i t h vuggy h i g h angle carb veins a t 70 t o SCA w i t h trace-2% r r

- l i g h t l y f rac t i i re i l along f o l i a t i o n planes a t 30 t o SCA - s i l i c i f i e d w i th qtz veins, 3-42 PO

-2-3cm o f black 9:aphitic gouge -S3 crenu la t ion cleavage and f o l d s a t 50 t o SCA enclose a q tz ve in

-broken w i t h miriur gouge and 5% qtz - [a rb tension gash i n f i l l i n g s ,

-qt2 vein, trace p o blebs, UC and LC approx 30 t o SCA -S3 crenu la t ion cleavage and fo lds , weakly contorted and wavy o f f s e t s 52 a t 50-55 t o SCA

-S3 deformation at 55 t o SCA -53 deformation d t 55 t o SCA -broken and f rac t tired

brown t o black co lour w i t h f i n e grey-white carbonate

f r o n 289.94-29G.31 w i t h 1-22 PO

g raph i te i n tti< jouge

; . HOLE #: 6-94-4

PAGE II 5 o f 7 OREQUEST CONSULTANTS LTD, HOLE 1 : 6-94-4

FROH TO ROCK At1 FOL TYPE C I A

DESCRIPTION % SAMPLE No. FROM TO LENGTH Au A9 CIA Pb Zn SULPHIDE opst opst pct p c t pct

324.66 324.71 328 .OO

344.54 344.99

345.39 345.78 356.88 357.14 357.76 358.31 359.83 361.54 361.54 361.70 363.11 365.29 367.02 370.85 376.77 376.86 377.00 378.16 378.23 378.40

383.57 383.87 397.93 398.08

404.48 404.69 404.74 408.41 411.34 41633

416.33 418.14

382.87 3a2.89

418.14 426.53

419.63 420.80 421.51 4?1.65

-broken arid f l j l lured wi th graphite on f ractures - f o l i a t i o n gradually f l a t t e n i n g a t 25-30 t o SCA -qtz vein, UC a t 30 , LC a t 50 t o SCA, 3-41 dissen PO and t r a w l 8

-qt2 vein, UC at 40, LC at 35 SCA, trace-12 disses PO minor c h l o r i t e -broken and fractured, 50% recovery -S3 f o l d axes at 50 drags f o l i a t i o n out t o 60 t o SCA -S3 f o l d i n g and crenulat ion cleavage as above -qtz ve in UC at 10, LC at 30, 1-22 dissem PO blebs - t i g h t S2 fo lds at 10 t o SCA - f o l i a t i o n drags out a t 60 t o SCA long f o l d l i n b ? -15% massive PO i l o t s around d isrupted looking qtz-carb veining -strong S3 f o l d i n g and crenulat ion cleavage a t 50-60 t o SCA -qtz vein, UC a t 30, LC at approx 30, 2-3% PO blebs and minor graphite -9raphi t ic gouge wi th carb - in tensely broken and f ractured w i t h graphi t ic gouge -broken qtz vein wi th 2-42 PO, 3-51 reddish brown sphaleri te?,

UC sharp at 30, LC broken - l imy bed wi th minor fo lds a t 10-15 t o SCA -S3 crenulat ion cleavage at 20-40 t o SCA -53 crenulat ion cleavage a t 20-40 t o SCA

GARNET ZONE (SUTURED FAULl GOUGE I N DARK BANDED PHYLLIIE)

Zone i s s i l i c i f i e d and i s brecciated and strongly f ractured and subsequently s i l i c a healed. Contains 10-259 qtz-carb tension gash i n f i l l i n g s , 2.5% pink garnets (3-5nd. Strong graphite on S2 (5-108) and l o c a l carb bands i n the DBP. l o c a l narrow cherty bands (<5%), qtz (10-209,) as ptygmatic veins and augens. Minera l izat ion i s 2-51 wispy PO. Upper contact sharp but broken, lower contact sharp at - 15 t o SCA

GARNET ZONE (DARK BANDED PHYLLITE)

Basica l ly same as above u n i t but not broken and faulted. Garnets vary up t o lcm but bost are 4 - 5 ~ n and percentage varies froM 5-35%. Uni t i s s i l i c i f i e d . Weakly t o moderately f ractured and averages 58 qtz-carb tension gash in f ill ings. Contains 51 cherty bands. Minera l izat ion averages 2-52 wispy and blebby PO, l o c a l l y higher. F o l i a t i o n at 10 t o SCA, l o c a l l y wa;) and contorted a t 30 t o SCA, UC - 15 t o SCA, L C i s gradational. G n p h i t e 5-10%.

reddish brown sphaler i te

-wavy f o l i a t i o n , 108 qtz-carb tension gash i n f ill ings -broken and f ra i ' l t red

HOLE #: 6-94-4

OREQUEST CONSULTANTS L T D - IIOLI 1 : 6-94-4 PAGE I 6 o f 7

FROM T O ROCK ALT FOL DESCRIPTION 1 SAMPLE No. FROM TO LENGTH Au A9 cu Pb Zn TYPE C I A SULPHIPE ops t o p s t p c t p c t p c t

422.80 422.81

423.14 424.00 421.00 424.95 424.95 425.30 425.30 426.36 126.36 426.53

426.53 431.59

422.81 423.14

428.41 428.46 430.68 430.92

431.59 433.43

433.43 436.28

133.43 434.85 HWDS2

434.85 436.28 HWPS2

l X . 2 6 438.48

436.28 437.38 HWDSZ

137.38 438.48 HWDSZ

-broken and ir:,. t u r e d -broken n i t h ' r , q t z - c a r b t e n s i o n gash i n f i l l n g s and 30'6 s i l i c a - c o n t o r t e d ses ~ on with 30% garne ts and f r o i 423.76-423.88 i s 10% PO - l i m y s e c t i o i H th 50% carb, t race -1% garne ts -coarse ga rne ts t o l c n , average 20-25% -1 imy s e c t i o r 40-502 carb, t race -1% garne ts -30'6 wispy PO

CHLORITE - SEK;CIIE PHYLLITE

As p r e v i o u s l y descr ibed. f i o t t l e d grey-green c o l o u r with 30-351 c h l and 30% s e r i c i t e . h i a l l y s i l i c i f i e d b u t n o t s t rong , 5% q t r v e i n i n g . Weak su lph ides = 1.''; PO, 10-15% b i o t i t e and 5% t a n b i o t i t e . UC g r a d a t i o n a l IC sharp a t 311 t o SCA which i s approx f o l i a t i o n angle. Rare ga rne ts .

- q t z v e i n a t C C ; t r a c e PO

- q t z vein, n a i j l ipper and l o w e r con tac ts , t race -1% blebby PO

ARGILLACEOUS t IMESTONE

Wavy f o l i a t i o r J: 50 t o SCA. UC sharp a t 30, LC g r a d a t i o n a l .

HAMGIPG WALL DISSEMINATED SULPHIDE ZONE (WEAK MINERAL I!A!ION)

U n i t i s mder:i:;ly broken and f r a c t u r e d . S t rong ly s i l i c e o u s - l o c a l l y 5 0 4 0 % s i l i c a * ; t h c h l o r i t e and s e r i c i t e , probably a l t e r e d CSP as s e r i c i t e t o 2 0 . . F o l i a t i o n i s navy a t 30 t o SCA. F i n e g r a i n e d dissem PO 1-3%, tra8.e 1% cpy.

- s t r o n g t a n b i s r i t e t o 433.14, broken and f r a c t u r e d from 434.00-434.35 q u i t e s i l i ceo ' c

gouge from 42' , 13-436.28 w i t h 50% recovery, 1% PO, t r a c e cpy

HANGING WALL C iS5EMINATED SULPHIDE ZONE (MODERATE MI#rYa' iZATlON)

Same as above mt o n l y s t r o n g l y s i l i c i f i e d throughout and s u l p h i d e n i n e r a l i z a t i o n 1' inuch s t ronger .

s i l 3

s i l -more s e r i c i t i than s i l i c e o u s , s t r o n g l y broken and f r a c h r e d with 1

s i l - s t r o n g mineral ) ; a t i on 1% PO, 10% cpy and 1'6 sph t o 436.49 t hen

s i l - s l i g h t l y weak6 w l p h i d e s than above i n t e r v a l ave rag ing 5-82 pa, 9

15 weaker averagi'i,, 5% PO, 1% cpy t o 437.04, then 10% PO, 102 cpy and 1% sph from 4i7.04-437.38

3-51 cpy and " sy

136 433.43 434.85 1.42 <.001 .01 .121 <.Ol -05

431 434.85 436.28 1.43 ,001 .07 .506 .01 -06

438 436.28 437.38 1.10 ,002 .06 1.769 (.01 2 1

431 431.30 438.48 1.10 .001 .08 1.066 <,Ol .11

HOLE # : 6-94 - 4

HOLE 1 : G-94-4 PAGE B 7 o f 7 OREQUEST CONSULTANTS LTD.

FPOM TO ROCK At1 POL DESCRIPTION 1 SAMPLE No. FROM TO LENGTH Au A9 Cu Pb Zn TYPE CIA SULPHIDE opst opst p c t p c t p c t

43S.48 441.86

438.48 439.50 SHMSZ s i l

439.50 440.28 SMMS2 s i l 440.28 440.85 SMMS! s i l

440.85 441.65 SMMSZ s i l

441.65 441.86 SMMSZ s i l

411.86 451.83

141.86 443.00 L S I carb

447.18 447.98 012 VN s i l

451.83

SEMI MASSIVE 1P PASSIVE SULPHIDE ZONE

Zone o f s i l i c e w i massive su lph ides with v a r i a b l e su lph ide conten t . Local massive : rLbions with 60-75% su lph ides then weak zones n i t h o n l y 5Z s u l p h i d i i and s e c t i o n s o f d isseminated and s t r i n g e r su lph ides averaging 30%. i ! r i a b l e s i l i c a conten t as wh i te q t2 eyes from 10-301 and f i n e g r a i n d i i a t r i x quar tz .

-semi massive t L , 438.73 with 15% cpy, 10% pa and 1% sph then rsassive with 30% cpy, X% PO and 31 sph t o 439.25, broken from 438.79-439.02 with 40% recovc iy and broken frors 439.25-439.29 then s t r o n g s t r i n g e r s with 20-252 cpy, 20% PO, 2-42 sph from 439.29-439.50

-much weaker su loh ides as s t r i n g e r s with 510% PO, 2-32 cpy, 1% sph -massive sulphii.:. zone with 30-40t PO, 30% cpy, and 5% sph, broken

from 440.57-440.80 with 30% recovery - s t r o n g s t r i n g e r siulphides with 20% PO, 15% cpy and 3-52 sph as s t r i n g e r s a t 25 t o SCA

-massive su lph ide zone, sharp UC and LC a t 30 t o SCA, 40% pa, 30% cpy and 51 Lph

ARGILLACEOUS L I W S T O N E

Banded 1 ines tonr with 30% a r g i l l a c e o u s m a t e r i a l g ives f o l i a t i o n a t 35-40 t o SCA. t o c ~ l l y broken with 2-3% py.

-as general des, , i p t i o n , q t r v e i n n i t h 5% PO, 1% cpy from 441.97-442.07

- q t 2 v e i n with c, i i tor ted upper and lower contacts, v e i n has 5% PO, 1% cpy and t r a r ? galena as massive c l o t s , 5% ep ido te

END OF HOLE

60 440 438.48 439.50 1.02 .DO5 .75 8.438 .02 1.18

441 439.50 440.28 .78 ,001 .14 1.027 .06 .56 10 442 440.28 440.85 .51 ,006 .60 6.178 -02 1.29 70

35 443 440.85 441.65 .80 ,003 -44 4.004 <,Ol .63

75 444 441.65 441.86 .21 ,003 .45 4.391 .07 ,89

445 441.86 443.00 1.14 <.001 .04 ,105 <.Ol -02

446 447.18 447.98 .80 <.DO1 .04 ,133 .01 .02

0 f? E u E S T C 0 N S U L T A N T S L T D . GIAWOND DRILL HOLE RECORD C1 ien t BETHLEHEM Page I 1 o f 14

Hole No, 6-94-5 Northing 3512.64 Core Size NQ I 1 1 8 0 Depth Dip A z i i u t h Depth D ip Azimuth Star ted AU6. 26, 1994 Target HINE OREBOGV Property GOLOSTREAH East ing 16246,72 Casing 10' PVC PIPE 91.5 - 86 190 170,7 - 85 195 Coapleted SEPT. 8, 1994 Coiaents HOLE CEMENTED l o c a t i o n REVELSTOKE Elevation 709.73 Length 672.87 250.0 - 78 199 329.3 - 73 204 Drill Co. OLYMPIC NTS 8211911 La t i tude 51 38' 00" N D ip-Co l la r -90 408.5 - 69 208 487.8 - 66 211 Logged By W . RAVEN C l a i i No Longitude 118 24' 40" W Bearing NIA 581.4 - 61 214 672.9 - 60 214 U n i t s HETERS

FROM TO ROCK ALT FOL TYPE C I A

GESCRIPTION t SAHPLE No, FROH TO LEN6TH Au Ag Cu Pb Zn SULPHIDE opst opst pc t p c t pct

39.63 OVERBURDEN

39,63 346.71 HAMIlL GROUP

39.63 42,66 QUARTZITE

41.02 41.77

42,66 46,41

45,41 45.54

46.41 62.70

48.95 50.45 50.45 50,70 50,91 51.80

t r e y to greyish-white coloured u n i t , very s i l i ceous . Loca l l y greenish coloured = i n t e r c a l a t e d andes i t i c mater ia l I Corprised o f f i n e gra in rd qtz (70-801), b i o t i t e (101) c h l o r i t e ( 5 t ) , and s e r i c i t e (<5%). Local whiter patches have carbonate i n u a t r i x but o v e r a l l <52, Trace d i s s r i p y r i t e . Weak f o l i a t i o n a t 40 t o SCA. Local broken sec t ions w i t h u i n o r Fe-ox s t a i n . Lower contac t sharp a t 40 t o SCA,

-broken and f rac tu red , 65-70! recovery

TUFFACEOUS 10 PORPHYR IT 1C ANDESITE

Pale t o Medium green t o l o u r w i t h darker green p o r p h y r i t i c pyroxene c r y s t a l s (augite?) up t o 6 u u x 6 ~ , Comprised o f f i n e grey t o c l e a r qtz (45-5581, p a l e green t h l - s e r mix (30-3511, augite? c r y s t a l s ( 5 2 ) , f i n e a a t r i x carb (5-10t) and t r a c e d i s s e i p y r i t e . Sptckled appearance w i th weak l o c a l f o l i a t i o n a t 40 t o SCA. Quartz veins p a r a l l e l t o f o l i a t i o n = 1-2t . Lower contact broken.

-s t rong ly f r a c t u r e d

QUARTZITE (WITH LESSOR INTERCALATED ANDESITE)

As described 39,63-42.66. Contains 2-3% py as h a r i d e veins p a r a l l e l t o f o l i a t i o n . Local greenish sec t ions = ch l enriched. Minor muscovite on f r a c t u r e s (1-32),

-tuffaceous green andesite -broken and f rac tu rpd , 158 recovery - in tense ly broken and f rac tu red , a l l rock chips

OREQUEST CONSULTANTS LTD, HOLE I : 6-94-5 PAGE I 2 of 14

FROH T O ROCK ALT FOL TYPE C I A

DESCRIPT ION 'I SAMPLE No. FROW TO LENGTH Au Ag Cu Pb Zn SULPHIDE opst opst pct pct pct

54.06 55.03 57.01 61.85

62,70 69.18

-1uffaceous Andesitp UC and LC at 40 to SCA -veiy strongly brokm and fractured, local competent sections

( loc i ) , 25X rock rh ips with broken qtz veins at 51.02-51.13 and 60.53-60.57 and 60, -61.14, the l a t t e r vein at 10 t o SCA with 3-5% py, 12 PO as d i s s e i blebs

SILICIFIED TUFFACEOUS ANDESITE

63,62 63.12 65.20 65.30 66,90 67.02 61.02 67.80

69.18 12.77

71.20 11.11 72.18 72.41

72.77 97,30

17,lO 17,50 79.93 80,26 80,26 81.49 82,38 86.88

88.26 89.67 88.48 88.58

90.55 119.80

Basical ly sane as 42.66-46.41 but not porphyri t ic. Variably s i l i c i f i e d from none to strong, also loca l s i a l l quartzite sections, Weak t o moderate f o l i a t i o n at 40 t o SCA, Upper contact i s a gradational change lower contact also semi-gradational. Trace-l l dissem py, trace carb.

-strongly fractured -strongly fractured -qtz vein, UC d i s t o r t d , LC sharp at 40, barren -qtz flooded with 30 409, qtz veins

QUART2 ITE

As described, 46.41-62.70

-1uffaceous Andes i t e -qtz vein, UC sharp at 35, LC w e d i f fuse but approx 10 t o SCA, has 2 - 3 massive PO blebs with 301 PO, 11 cpy frou 72.43-72,47

TUFFACEOUS 10 PORPHYRll IC ANDESITE

As described 62.10-69.18 except that un i t i s not s i l i c i f i e d except l oca l l y . Also contains approx 5t carb as 1-311 veinlets and sole f i ne ua t r i x carb which gives a speckled appearance, Trace-lt dissm py and PO. Upper contact gradational as i s loner contact.

-broken and fractured, 702 recovery -broken and f ractured -porphyrit ic, so f t with 308 se r i c i t e - intensely broken and fractured t o shattered, mostly broken rock chips with i i n o r conpetent sections, carb and clay on fractures

-Porphyrit ic Andesit e - fractured wi th c lay yuuge

FRACTURE ZONE

The rock i s very strongly fractured throughout with local sections o f rock chips, rubble and c lay gouge. Local uore competent sections but these are scarse. The andesi t i r un i t grades in to what looks 1 ike the

' 8

HOLE #: 6-94-5

HOLE il : 6-94-5 PAGE I 3 of 14 OREQUEST CONSULTANTS LTD,

FROH TO ROCK ALT FOL DESCRIPTION 1 SAMPLE NO. FRO\ T O LEN6TH AU Ag Cu Pb Zn opst opst pct pct pct TYPE CIA SULPHIDE

Lower Index Chlor i tP-$er ic i te Phy l l i t e . Hard to rea l ly d is t inguish between the two uni ts as the CSP could be a i o re altered version of the andesite that i s variably s i l i c i f i e d .

91.90 92.05 95.74 97,30

- s e r i c i t i c gouge -101 qtz-carb tension gash i n f i l l i n g s , below t h i s i s a rb i t ra ry CSP

97,30 152.93 CHLORITE - SERICITE PHYLLITE

97.30 119.80 96.64 99,70 102.90 103.23

103.23 135.70 120.75 135.70 .

133,55 133,70 135,65 135.70 138.85 139.02 136.28 139.02

144.35 144.68 145.77 146.10 148.24 148,47 149,80 150,17 152.26 156.93

152 I 93 158 I 03

158.03 189.05

S i i i l a r t o andesite u n i t above but a l i t t l e bet ter f o l i a ted and stronger se r i c i t e . Comprised o f f i ne qtz (30-4021, s e r i c i t e (30X), ch lo r i t e (20-301), and p tyg ia t i c qt2 veins (3-52). Hineral izat ion i s 1% dissen pya Fo l i a t i on at 35 t o SCA, Locally s i l i c i f i e d , UC i s gradational, LC i s seBi-confonabk at 35 t o SEA,

-part o f saw fracture zone described 90.55-119.80 -601 recovery -qtz vein, d is tor ted UC and LC, has 1-3% dissea py and PO, trace cpy trace cpy

- ioderately t o strongly s i l i c i f i e d -5-101 qt2 veins 1-5cn wide with i i n o r tension gashes throughout but

- intensely fractured with 2-3% py - intensely fractured with s e r i c i t i c gouge -broken and fractured with ser ic i te-c lay gouge -60% recovery, doesn't look that broken but nust have los t some core around a couple o f small gouge and rubble zones - intensely fractured -broken and fractured -broken and fractured -1uf faceous Andes i t e -strongly s i l i c i f i e d

ARGILLACEOUS LIHESTONL

rock i s qu i te coipetent and well s i l i c i f i e d

Greyish coloured l inestone with dark brown to black argi l laceous bands (10-15%) = f o l i a t i o n a t 35 t o SCA, l o c a l l y brerciated looking with qtz-carb tension gash i n f i l l i n g s , UC seii-confornable at 35 t o SCA, LC broken.

O U A A I Z I T E ?

6rey-green coloured f i i ie grained rock. Conprised of 802 qt2, 5-15? b i o t i t e and <51 s e r i r i t e which i s l o r e evident on f racture planes, Local coarser qtz eye$ Local s i a l l sections of intercalated green andesite which i s tuffareous, and very narrow sections wi th speckled

HOLE 1: 6-94-5

OREQUEST CONSULTANTS LTD, HOLE I : 6-94-5 PAGE f 4 of 14


DESCRIPTION 2 SAHPLE No, FROH TO LENGTH A u Ag Cu Pb Zn SULPHIDE opst opst pct pct pct

162,03 162,14 163.33 163.50 164.04 165.62 166.77 167,lO 168.31 168.86 169,82 170,74 172.46 172,68 174.90 175,91 175.71 176 I 10 176.10 176.86

178.03 180,65 180,65 181.45 185.06 188,61 186.02 186.68 188,ll 188.61

189,05 194.38 .

193.68 194,21

194,38 196.50

196.50 201.76

201 I 76 203.88

203.88 209.00

r h i t e carbonate, usi iai ly < 1 0 t h i n length, Weak f o l i a t i o n at 35 t o SCA Local qtz veins, UC broken, LC sharp at 25 t o SCA

-qt2 vein, trace py -broken and fractured -Tuffaceous AndesitP -1uffaceous Andesi t P -Tuf faceous Andesi t P -Tuf faceous Andesi t? -broken and fractured wi th c lay gouge -re-ground core, dropped out o f tube, 60% recovery -101 dissei py on f ractures -qtz vein, UC a t 50, L C broken and las t 15cr of vein i s fract i i red and broken, 12 PO as f ine d i sse i and rare i o r e massive c lo t s

-Argillaceous Linestone, f o l i a t i o n a t 30 t o STA -TSP that i s broken and fractured -roderately t o strongly fractured -CSP, UC at 30 , L I broken -very strong s e r i c i t e a l t e ra t i on

CHLDRITE - SERICITE PHYLLITE

As previously descrihpd, Hediui t o dark green coloured un i t that i s s i l i c i f i e d over upper 50ca, UC sharp at 25 t o SCA, L C broken and gradational I Fol i a t i ~ ~ t at 25-30 t o SCA.

-qtz vein and in terca lated quar tz i te

OUARTZ ITE

Highly si l iceous, very f i n e grained, strongly fractured throughout,


As previously described. Hediuu t o paler green colour, Contains 1-32 qtz-[arb tension ga5h mf ill ings, l oca l s i l i c i f i c a t i o n and white specks o f carbonate. Fo l i a t i on at 25-30 to SCA which i s same as the upper and lower contacts.

AR6ILLACEOUS L IHESTONE

As previously described. Fo l i a t i on UC and LC at 25-30 to SCA, i i n o r intercalatpd g iaph i t i c Dark Banded Phy l l i t e

OUARTZITE

HOLE I: 6-94-5

OREQUEST CONSULTANTS LTD, HOLE I : 6-94-5 PAGE f 5 of 14

FROM T O ROCK ALT FOL DESCRIPTJON 2 SAIPLE No. FROM T O LENGTH AIJ A9 Tu Pb Zn TYPE C I A SULPHIDE opst opst pct pct pct

As previously described. Pale greenish-white colour, 1-22 d is tor ted qtz veins, Port ions o f t h i s u n i t are sof ter and bear closer reseiblence t o CSP but s i l i c i f i e d , Changes are subtle and d i f f i c u l t t o dist inguish,

209.00 331,17 QUARTZITE AND SILICIFIFD THLORITE - SERICITE PHYLLITE

Unit i s f o l i a ted a t 30 to SCA, Contains 1-2 t cross cu t t i ng qtz veins. Some sections look 1 )he good quartzite, others resemble CSP. Pervasive s i l i r i f i c a t i o n i n the CSP makes i t look l i k e quartzite and there i s approx 5t s e r i c i t e i n the quar tz i te so very hard to d is t inguish between the two uni ts , gradational contacts.

210.60 211.35 218.81 219,35 228,66 230,93 233.65 233,lO 239.95 240,Ol 240-20 240.25 245 I 01 152.13

253.03 253,15 253.15 254.66 255.18 256.20 257.75 258,08 259,23 259.35 259,41 259,44 259,59 259.63 261.37 261.90 265,14 265.22 265.50 255,28 268.88 273.27 278.40 278,67 279,OO 279,22 280.93 280,98 282.47 282.67 286.20 186.35 291.50 291,57 292.15 291,25

293.80 295,62 101 I 88 302,21 103,lO 304.63

292.25 292.83

-strongly fractured "poker chip" core -CSP, weak s i l i c i f i r a t ion -Porphyrit ic Andesit ji -qtz vein, UC and LC approx 10 t o SCA, 1% po blebs -qtz f looding as veiii5 (lo?,) with trace py, cpy, PO -strongly fractured -strongly broken and f m t u r e d , lipper ha l f f a i r l y s e r i c i t i c , lower ha l f l o r e s i l i c i f i w , s e r i c i t i c gouge f ron 246,04-246.25, loca l l o re competent sect ion$

- s e r i r i t i c gouge -Tuff aceous Andes i t e -strongly fractured -strongly fractured -strongly fractured -strongly fractured -strongly fractured -1uffaceous Andesite -strongly fractured -moderately t o strongly fractured -as above, intensely broken and fractured from 212.80-273,27 -strongly fractured - intensely fractured -highly fractured q t i vpins -qtz flooded (502) a5 veins a t 10-20 t o SCA -moderately fractured -qtz vein, UC at 30, I r at 20 t o SCA, trace py -strongly fractured -vuggy carb veins, 1 3 a ~ wide at 70 t o SCA -moderately t o strongly fractured -moderately fractured -much so f te r due to strong ch l and ser and speckled with 52 white carb, conformable contacts

HOLE #: 6-94-5

OREQUEST CONSULTANTS LTD, HOLE I : 6-94-5 PAGE I 6 of 14 -

FROH TO ROCK At1 FOL TYPE C I A

DESCRIPTION % SANPLE No, FROH TO LEN6lH Au Ag Cu Pb 2n SULPHIDE opst opst pct pct pct

304,94 307,74 310,42 312-59 315.66 315,78 318.73 318.83

327.02 327.15 328.12 331.17

-moderately fractured, lower 20cn i s strongly fractured with gouge -sof ter section 1 ike 103,lO-304.63 with gouge zone f roa 311J6-311.52 - s i l i c i f i e d section ai th 30% PO, 1-21 cpy, 3-51 galena - s i l i c i f i e d section r i t h 52 PO, 1% cpy, 32 galena and 30-40% brown b io t i t e , 5% qtz tension gash i n f i l l i n g s

-broken and fracturpd -stronger s i l i c i f i c a t i o n and more b i o t i t e than ch lo r i t e as un i t approaches a small gouge zone

331.17 333,50 GREY - WHITE QUARTZITE

333.50 335.46

335.46 346.71

346.71 414.04

346.71 362.04

Very f i ne grained d m e , massive looking greyish-white coloured quar tz i te - very hard (init, Upper contact i s along strong chl-ser a l tered gouge zone a t 60 t o SCA from 331.17-331.50, lower contact i n gouge at 65 t o SCA, minor py r i t e (2%) and graphit ic s t y l o l i t e s around lower contact, Unit 15 strongly fractured t o 332,33 then competent, From 332.85-333.50 ha5 brown argi l laceous bands. Trace dissen py, Lower contact confoindble with gouge zone a t 20-25 t o SCA.

GOUGE ZONE

Semi-competent r h l - v r a r b gouge zone, haz green-white colour, P i t t ed surface due t o weathPii.d out carb, Contains approx 3% qtz-carb veins at 20 t o SCA, looks 1 ike a l tered CSP, UC at 20-25 to SCA, From 335.23- 335,46 i s CSP with ?ha rp LC at 10-15 t o SCA

QUARTZITE (WITH BANDFD ARGILLACEOUS HATERIAL)

Mott led brownish-greenish-white coloured un i t . S i l i c i f i e d b i o t i t e and ch lo r i t e phy l l i tps. Loral dense massive greyish-white sections. Fo l i a t i on at 20 t o SrA Contains 5% qtz (milky white) as veins and augens, Upper contart at b i t broken but sharp at 10-15 t o SCA, lower contact sharp at 20 to SCA. Minor dissem py ( t r - l t ) , l oca l l y s e r i c i t i c Competent un i t , 1002 rrcovery,

CARBONATE PACKALE (BADSHOT AND MOHICAN FORMATIONS)

HIGHLY CALCAREOUS DARK BANDED PHYLLITE OR ARSILLACEOUS 1 IHESTONE

Unit looks very s i i i l r i r t o DBP but i s very l imy and l a y be be t te r described as highly argi l laceous limestone. Hell f o l i a ted a t 20 t o SCA Coiprised of carb (40 601 and up to 702) and argi l lareous material = b io- rh l -ser (10-40t) p tyg ia t i c qtz veins (1-281, cross-cutt ing qtz- carb veins (12) and d i v e a py (1%). Local sections of clean marble, UC sharp at 20 t o SCA, LC Nore gradational at 20 t o SCA.

HOLE P : t-94-5

OREQUEST CONSULTANTS LTD, HOLE II : 6-94-5 PAGE I 7 of 14

FROM TO ROCK ALT FOL TYPE C/A

DESCRIPTION 8 SAHPLE NO, FROH TO LENGTH AIJ A9 Cu Pb 2n SUL PH IDE opst opst pct pct pct

349 I 60 355 I 00

362.04 380,63

362.04 366,76 366.76 380.63

:69.88

373,29 374.21 314,26 378,56 380,62

380,63 403,30

382 I 73 384,07 358.63 386.28 395.57 398,42 396,02 396,27

399.54 399 I 98

403,30 414.04

409,66 410,22 410.89 411,79 411.79 412.28 412.28 412.39 412.39 414.04

-11 qtz-carb tension gash i n f i l l in95

ARGILLACEOUS L IHESTONF

Basical ly saie as above un i t only less banded a rg i l l aceou~ material (10-159) and rore carb Looks nore 1 ike 1 i iestone than DBP. B i t of a gradational change fo i both UC and LC which are conformable at 20 t o SCA, uore of a facie.. change

- f a i r l y clean ia rb le - lore argi l laceous M d t e t i a l avg. 20-30%, loca l very l i l y section<

<30cu that are f a i r l y r lean l iuestone -1cu qtz vein at 20 t o SCA with 10% PO as discontinuous vein with rare speck5 of rpy

-ca lc i te vein, lcn wide at 70-75 to SCA -qt2 vein, 1-22 PO -cleaner looking 1 ineqtone, 10% argi l laceous material

CALCAREOUS DARK BANDFD PHYLLITE / ARGILLACEOUS L MESTONE

As desrribed 346,71-162 04, Again un i t looks qui te s i n i l a i t o the DBP and i s very weakly s i l i c i f i e d but also has very l i r y beds. Local S3 defor ia t ion as crenulat ion cleavage at 50-60 t o SCA. Mineral izat ion consists o f f i ne d i s w PO (1-41j . Gradational UC and LC. Cross cut t ing qtz-rarb vcitic at 40-60 t o SCA = 3%.

4 3 r r t nu la t i on clca~;lge at 60 t o SCA -both 1 iuy and s i l ic i f led, paler colour 4 3 crenulat ion cleavage at 55 t o SCA, f o l i a t i o n steepen$ to 65-70 -qt2 vein, UC at 60, l r at 10, contains 2-38 PO c lo t s with 101 Massive

PO at UC, rare Speck\ o f cpy - f a i r l y clean ia rb lp / l irnestone bed

GREY HARRLE

As described 362,04-380.63, Maxiuum 101 argi l laceous romponent I Fo l ia t i on at 10 t o STA UC gradational, LC sharp a t 30 t o SEA. Local rore argi l laceous sect ion<, Strong graphi t ic s t y l o l i t e s with minor gouge near botton of i i i i i t ,

-5040% argi l laceous material -12 graphit ic s t y l o l i t w , 3-4% qtz-carb tension gash i n f i l l i n g s -looks 1 ike 1 i r y CSP, 59, qtz-carb tension gash i n f i l l ings -graphite-chl-ser 90uf,t at approx 30-40 t o SCA -as general descript iiii, Minor greenish-brown chl-bio bands

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HOLE #; 6-94-5

QREQUEST CONSULTANTS LTD. HOLE I : 6-94-5 PALE I 8 of 14


DESCRIPTION 8 SAMPLE No. FROM TO LENGTH Au Aq Cu Pb Zn SULPHlDE opst opst pct pct pct

414,04 672.87

414.04 431.90

416,65 416.97 417,16 422.07

423,88 424.51 426,15 426,26 430.98 431.90

431.90 643.49

431.90 449106

431.90 437.44

436,68 436,86 443,37 444.64 447.99 449,06

449,06 459,92

451,22 452,17 452.11 452,40

LOWER INDEX FORHAT ION

CHLORITE - SERICITE PHYLCITE

k d i u i green colout hard but not rea l ly s i l i c i f i e d . HUierOuS in terca lat ions of t l m grey-white i a rb le generally as w a l l beds < l o c i though local larger sections. Comprised of chl (409) qtz (20-30%) se r i c i t e (lot), catb beds (52) cross cut t ing qtz-carb veins (1-31, ua t r i x carb (11) and d i ssc i po (12). Overall f a i r l y coipetent un i t with i i n o r broken v r t i o n s . UC sharp a t 20, LC sharp at 60 t o SCA,

-broken and fractiitt-d -Argillaceous Linestone - th ick bed of intercalated 1st i n CSP, UC sharp a t 20, L C sharp a t 10, contains 20-402 argillaceous i a t e r i a l

-clean grey i a rb le -broken and fractured -Moderately fracturFd

"DARK BANDED PHYLL IT! SEOUENCE"

ARGILLACEOUS LIHESTONE 1 GARK BANDED PHYLLITE (LIMY UNIT THAT IS START OF DARK BANDED P H Y L L l l E SEQUENCE)

As previously described 346.71-362.04. Looks a b i t l i k e the DBP but i s strongly calcareous rontains 40-702 carb, 10-302 argi l laceo~rs material (ch l -b in +i tpr) tan b i o t i t e (<52), Local sections o f clean grey i a rb le . UC sharp a t 60, LC gradational but at 20 t o SCA, Fo l i a t i on at 20 t o YA Contains 18 f i ne grained po and py,

- f a in t pale green colour, looks l i k e calcareous CSP, contains approx 3-49 qtz-carb tenziorr gash i i i f i l l ingc

-broken rock, s m i gouge -r lean grey narble r l t h graphi t ic s t y l o l i t e s near bo t to i of un i t - f a i r l y clean grey marble, UC and LC at 20 t o SCA

DARK BANDED PHYLLITE

Similar t o 1 i iestone above but argi l laceous uaterial exceeds carbonate content. Contains b i o t i t e (20-25t) ch lo r i t e (201) sp r i c i t e (101) carbonate (10-302) qr, augens (1-32) cross ru t t i ng qtz-carb veins (1-22) and dissem po (1-381, UC and L C are gradational, Fo l i a t i on at 15-20 t o SCA

-clean grey marble -S3 crenulat ion cleavige at 50 t o SCA

HOLE #: 6-94-5


FROM TO ROCK At1 FOL DESCRIPTION 1 SAMPLE No, FROM T O LENGTH AIJ Ag Cu Pb 2n TYPF CIA SULPHIDF opst opst pct pct pct

452.36 452t45 452.89 454,40

454.53 455.17 4 5 a a 457.74

459,92 419,90

459.92 460,90

460,90 470,80

468,04 468.19 474.21 474.30 475,OO 415,26

479 I 90 492 I 99

480.90 481.04 481.30 481,45 485.34 486,04

488,11 492,09 492.99

492,99 508.16

496.85 497,34 497.58 491,80 505.76 506.11

508.16 550,91

-qtz vein, d i s t o r t d UC, LC approx 50 t o SCA -3-5% qtz-carb tension gash i n f i l l i n g s with broken tore and gouge f ron

- f a i r l y clean grey narble -pale greenish colour, s i l i c i f i e d

AKJLLACEOUS LIMESTONE I DARK BANDED PHYLLITE

More calcareous than above un i t but has a high content of a r q i l l a c m s i a t e r i a l . Fo l i a t i on at 10-15 t o STA. Trace-1% disseR po and py. Upper and lower contacts are gradational,

-moderately fract i j red and broken with i i n o r gouge and 52 qtz-carb tension gash i n f i l l ings

-1-3% cross cu t t i ng qtz-carb veins at 70 to SCA and 1-32 qtz-carb tension gash i n f i l l ings

-50% qtz flooded as conformable veins -qtz ve in l f looding with 1-21 PO blebs, trace cpy -clean grey marble

AR6 ILLACEOUS L IHESTONE

Simi lar t o above uni t , as described 431.90-449,06 n i t h 25-351 arg i l lareouz Material, UC i s broken core but gradational, LC i z gradational and i n zert ions of broken core,

-broken and fractured n i t h 3t py on fractures -broken and fractured with gouge -52 qtz-carb tension gash i n f i l l i n g s -REDUCE CORE S I Z E FRO# NQ I I t o 60 -broken and fractured

GREY MARBLE

Fa i r l y clean greyish-Mhite re-crystal1 i z t d 1 inestone, Local ly argi l lacpous and also has 5 t narrow interbeds o f green rhl-ser+/-bio phy l l i t e . Fo l ia t ion, when prezent, at 10 to SCb, Trace-12 dissem PO

-weakly fractured with 3% navy graphit ic s t y l o l i t e s that are p a r t i a l l y weathered out

-Chlori te P h y l l i t e ronfornable at 10 t o SCA -vuggy sections, 5t weathered s t y lo l i t es , minor brokm core -Chlori te P h y l l i t e

DARK BANDED PHYLLITE (CHLORITF - S E R I C I T E +/ TAN B I O T I T E PHYLLITE)

454.08-454.22

HOLE #: G-94-5

OREQUEST CONSULTANTS LTD. HOLE I : 6-94-5 PA6E I 10 of 14

FROM T O ROCK A l l FOL DESCRIPTION X SAHPLE NO. FROH TO LENGTH AII A9 Cu Pb Zn TYPF C h SULPHIDE opst opst pct pct pct

Greenish grey ro lour td rock comprised of ch lo r i t e (30-501) se r i c i t e (10-30t) tan b i o t i t e i3-1Ot) quartz (10%) quartz augens (2-41) and f i ne d i sse i PO (13%) Like ly represents a facies change from the typ ica l dark brown to black DBP with l o r e ch l and ser a t the rxpense nf b i o t i t e and graphite. UC sharp 20, LC gradational, Local paler coloured s i l i c i f i e d in terva ls ,

5 0 ~ ~ 1 6 soa.19

soa.44 5 0 ~ ~ 4 9 511.13 511.17 515,91 516,04 521 I 49 525 I 42 522 I 28 522.31

534.04 534,22 534,62 534.14 535.14 540.22

543.22 544.55 545.28 545*38 541,16 541q92

m i 1 541.48

~48.96 ~49.03

550,91 643.49

moo s51,ia

559.23 559,a6 555.89 556,Ol

559.86 561 .SO 515.16 575,42 575.42 516.25 516.35 576,50 576,75 576,90 sai.53 ~ 8 4 ~ 3 3

-308 strongly magnetic PO and 1-31 iagneti te, trace cpy at contact with 1 inestone abovr

-conformable qtz vein d t 20 with 1-22 dissem PO blebs -as above but trace po -qt2 vein as above -paler grey colour, c.fron9 s i l i c i f i c a t i o n -qtz vein at approx 20 t o SCA, vein has 5% massive c lo t s o f PO n i t h trace tpy and g a l ~ n a , ainor (5%) p h y l l i t e i n vein

-qtz vein a t 60 t o S C A ; 3-4t massive PO c l o t s with tr cpy and galena -qtz vein with trace pn - s i l i c i f i e d section with 601 grey-nhite q t r f r o 1 538.72-539.90 - lore typ ica l looking graphi t ic DBP -moderately to strongly fractured -broken and fractured -qtz vein, trace dissrn PO


DARK RANDEO PHYLL ITE

gradational change in to the i n re typ ica l looking dark brown t o black graphi t ic p h y l l i t e , Conprised o f bio-chl (30-402) se r i c i t e (10-201) tan b i o t i t e (102) carbonate (5-201) qtz (10-201) p tyg ia t i c qt2 veins 12-51) graphite (5-102) and dissem t o f o l i a t i o n pa ra l l e l PO (1-581, Fo l i a t i on at 10 t o 3 ! , IIC gradational, LC gradational I Minor loca l S3 fo lds, Weakly s i l i r i f i e d throughout except f o r l oca l b i o t i t e - se r i c i t e r i c h section<

-S3 f o l d axes a t 50 t . ) SCA and contorted qtz vein with 5% PO, t r cpy -53 f o l d axes at 60 t n SCA -strongly brnken aloi1g 52 -7-49 qtz-carb tension gash i n f i l l ings -9orrge breccia subseqilmtly healed n i t h s i l i c a - local S3 crenulat ion cleavage at 30 t o SCA -qtz vein UC at 10, LC at 30, 1 - 2 PO trace rpy -S? f o l d axes at 10 t o SCR - 3 - 3 qtz-carb tension gash in f ill ings and 10% qtz-carb veining, weakly fractured with strong f ractur ing and gouge f ron 582,82-583,24, l oca l l y brerciated with near ver t ica l f o l i a t i on , small S7 f o ld a t

HOLE 1: 6-94-5

OREQUEST CONSULTANTS LTD, HOLE I : 6-94-5 PAGE D 11 o f 14

FROM TO ROCK ALT FOL DESCRIPTION 1 SAHPLE NO, FROU TO LFNGTH AIJ Ag b Pb Zn TYPE CJA SULPHIDE opst opst pct: pct pct

584.09 axis at 10 t i i SCA

-2-41 qtz-carb tension gash in f ill ings, brerciated looking f r o r 593,16-593.22

-5ca section o f b re r r i a ted looking qtz-carb veining at 60 t o SCA -vuggy qtz-carb vein 2 - 4 ~ wide at 85 t o SCA, ends i n gouge zone

-5% qtz-carb tension gash i n f i l l ings, ioderately fractured with 53 crrn l r la t ion cleavage and i i n o r fo lds f ron 599-31-599.61 at 50-60 t o SCA and one section o f ve r t i ca l f o l i a t i o n

-moderately t o strongly fractured and broken rith 5-81 qtz-carb tension gash i n f i l l i n g s and 5% qtz-carb veining, loca l gouge 5% py

-1cm o f pure grey mud -PO t o 5% as f i n e f o l i a t i o n para l le l wisps and pa r t i a l veins at 10 SCA

-q!2 vein UC di f fuse q t ? flooding, LC sharp a t 20, has 5 4 % PO i n the upper qt2 f looding t o 625,77 then the vein i t s e l f i s barren - t r po

587.96 588.30 -52 qtz-carb tpnsion qash i n f i l l ings 591.70 593,46

595 I 10 597.89 598,49 598.49 598.55 -graphit ic c lay gouge r i t h 51 py 598.55 599.61

600 I 34 603,55

605~40 605.79 -strongly fractured 610,63

610.64 616,46 622.02 615.11 -51 qtz-carb tension gash i n f i l l i n g s and disrupted veins 625.74 625,98

626.76 626,92 -strongly f ractured ,ind broken 6 2 6 ~ 9 6 2 7 , ~ -qtz vein with 5% po 631.70 633.74 . -aarked increase i n q t ~ a r b veining and tension gash i n f i l l i n g s and

ptygnatic q tz veins with qtz-carb content o f 10-308, veins vary f r o i 20-60 t o SCA, l oca l htoken g raph i t i r sections, brecciated and sutured gotrge from 642.86-641.98 and strong qtr-carb (301) to 643,ll

.

643,49 649,99 GARNET ZONE

643,49 644.26 644.26 645.57

645.57 646,06 646.06 646,45

646,45 646.88

Greyish-white intensiy F i l i r i f i e d / cherty phy l l i t e rith 3-52 dis tor ted l i g h t pink gdrnets t o 644,26. Then f ron 644.26-645,57 i s ziitirred s i l icpous and stz-carb flooded bretciated DBP with 1-21 garnet From 645,57-649.99 i 5 various s i l iceous dark phy l l i t es (DBP?) rith variablp garnet rontpnt f ron 1-29 to over 30% local ly , Garnets are 1-211 t o up t o lcn pniphyroblasts, Highly variable sulphide content f ro# trace-20 dissen PO and cpy with one section of 20-251 po trace rpy as f o l i a t i o n par& ~1 s t r ingers and disserrinations, Upper and l o w ron ta r t s are 91 i l a t i ona l based upon f i r s t and las t visual appearance of garnet<

- rher ty /s i l icpous grey phy l l i te , f o l i a t i o n at 10 t o SCA -302 qtz-carb veining and tension gash i n f i l l ings = s i l ica zrrtured fault zone, brecciatpd and graphi t ic on fractures, 2-31 PO, 2% py

-cherty grey colourpd handpd p h y l l i t e with 8t garnets -Tan B i o t i t e - Chlor i te - Ser ic i te - Carbonate P h y l l i t r with no garnets, well f o l i a ted at I0 t o SCA

-s i l iceous and 1 iny FBP with 20-308 very coarse garnets up to l c u (rounded and rotated) f o l i a t i o n wraps around the garnets, minor py

HOLE #: G-94-5

OREQUEST CONSULTANTS LTD. HOLE I : 6-94-5 PAGF I 12 of 14 .'

FROH TO ROCK ALT FOL DESCRIPTION % SANPLE No, FROM TO LENGTH du Ag Cu Pb 7n TYPE r/A SUlPHIDE opzt opst p r t pct pct *

I

veins at end, 1-2aia wide at 45 to SCA

(1-32) and 20-301 handed PO emplaced along f o l i a t i o n at 10-20 t o SCA with t r a w l % rpy, rocal large garnets that are s l i g h t l y f la t tened lip to 1a5x1,0ci, thi. po i s very weakly magnetic

646.88 648.47 62 s i l 15 -SPmi-Hassive Sulphide Zone i n s i l i c i f i e d DBP, contains i i n o r garnets 15 447 646.88 648.41 1,59 .002 .01 ,056 ( . D l -06

648,47 649,lO FZ s i l - s i l i r i f ied, s p e r k l d grey phy l l i te , 2-38 garnets, n inor dissem PO 1 448 648,47 649.10 .63 <.001 <.01 ,005 .01 .03 649.10 649.62 $2 q i l -Spa i-Kass ive-Sul ph &-Zone, as 646,88-648 I 41 except PO i s mode rat e l y 35 449 649.10 649,62 ,52 ,001 ,10 ,114 -07 ,03

nagnetir and i s 81 I , massive, less individual str ingers, UT LC @ 10

649.99 655.29

650.73 651,58

655.29 651.82

657.87 660-20

BIOTITE - rHLORlTE - SERICITE PHYLLITE 6rry brorn colour, well foiated at 5-20 t o SCA, Comprised o f b i o t i t e (10-151) ch lo r i t e (10-15%) se r i c i t e (206) quartz (30%) muscovite (10%) p tygmt i c qtz veins (51) and f i ne dissem and layer pa ra l l e l PO and py (1-2t), UC gradational, LC sharp at 25, weak local s i l i c i f i c a t i o n ,

-ztrongly f rar turpd

ARFILCACEOUS 1 IHESTONE

Well banded un i t with bands/fol iat ion at 20-30 t o SCA* Local S3 defoaation a t 60-70 t n SCA. Strong tan b i o t i t e from 657.00-657.82 wi th gradual s i l i t i f i r a t i o n near end o f un i t .

HANGING HALL OISSEi4lNAlED SULPHIDE ZONE W A K TO HODFRATF Ml)rlRALI2ATION)

Looks l i k e !he S a w lriiit az abovt but has been strongly s i l i c i f i e d , llr a t 20, LC also at 20 t o SCA but based on sirlphide cnntent, # i w a l i z a t i o n i s large ly f i ne l y d isvn inated pa and rpy,

657.82 658.75 HWDSZ q i l -weaker s i l i c i f i t a t Ion and weak dizzem PO (3%) and trace cpy 1 450 657.82 658,35 .53 (,001 c,D1 ,038 .02 .21 658,35 659,93 HWOSZ s i l 20 -stronger s i l i c i f i r a t i o n and moderate t o l o r a l l y strong sulphides, 15 451 65R,35 659,93 1,58 ,002 ,07 ,937 ,01 -64

ainera l izat ion i s a? dissem blebs and z t r i n g e n a t 20 t o SCA and local d i s to r ted c l n t q , loca l r i c h qt r inger section? spperated by rpaker d i w n i n a t e d , po = 5-81 cpy = 5-81 qph = 1-12 py = 10 and galma = trace, b r o k m from 658.55-658A7

659.91 6h0,20 HUDSZ s i l -wak d i ~ i sulphides, 2% PO trace cpy 3 457 659.93 660.10 J 7 <.001 <*Ol ,139 <.01 ,?O

660,20 661,OO HANGING WALL DISSEdINATFD SULPHIDE ZONE (STRONG HINERALIZATION)

As above bi i t much Ttronger sulphides nostly as heavy diszeninations but l oca l areas o f good s t r inger n inera l izat ion a t 10-15 t o SrA. Reasonably sharp LC with massive sulphide zone below a t 10 to SCA. Hineral i r a t ion i z po (5-108) cpy (10-15t) sphaleri te (1-3) and galpna (trace), The PO i s reakly magnetic. Sulphides i n a s i l iceous matrix,

HOLE #: 6-94-5

QREQUEST CONSULTANTS LTD, HOLE I : 6-94-5 PAGE I ,13 of 14

FRDK T O ROCK ALT F0L TYPE C I A

DESCRIPTION % SAMPLE NO, FROH T O LENGTH A u Ag Cu Pb 7n SULPHIOE opst opst pct pct pct

660.20 661.00 HVDSZ s i l

661-00 662,OO

667.00 662.75 .DRP s i l 662.75 663.50 DbP s i l

663.50 665,P?

663.50 664-71 FUDSZN s i l 664.71 665,92 FWDSZN s i l

6692 667,34

665.92 67-34 DRP s i l 20

667 I 34 668,36

668.36 670,OO

670.00 ~72~87

671.56 671.95

-as general desrr ip t ion 70 451 660,?0 661.00 ,RO ,003 ,29 3,135 ,11 .74

MASSIVE SULPHlOE ZONE

Sil iceous seai-nassivc to naszive sulphide 20ne. l l ineral izat ion i s Massive disseminations and str ingers set i n 4 white m d grey quartz i a t r i x with 52 white carb blebs, Cross-cutting white qtz-(arb vein< are 1-5111 wide and comprise 5% o f the zone, Mineral izat ion i s po i30-40%) cpy (10-202) <phaleri te (3-52) and t r a w l 1 galena and 21 py, t o r a l l y p i t t e d and virggy around weathered out carb. Broken LC.

-as general desrr ip t ion

SlLlCIFIED DARK BANDED PHYLLTTE

55 454 661,OO 662,OO 1.00 ,004 ,94 4,638 1,32 -94

Contorted f o l i a t i o n wi th 109 qtz-carb veins and tenzion gazh i n f i l l i n g Broken UC, LC sharp at I0 t o STA, Rroken over upper ha l f of un i t , lore competent and c i l i c i f i e d over lower h a l f ,

-nore rompetent, w e l l f o l iated at 15-20 t o SCA, 3-42 Po, trace rpy 3 456 662,75 663.50 ,75 (.001 (,01 ,017 (.01 .01 -Moderately to strongly fractured, d i s s i py (1-2U cpy (1-4t) 5 455 662,no m t 7 5 -75 (.ooi (.oi ,237 .oi .03

FOOlUAtL DISSFWINATED SULPHIDE ZONE

Strongly s i l i c i f i e d gtey un i t with 801. grry qt2, H i n m l i z a t i o n i s f ine diszzen PO (52 * i t h trace cpy, UC and LC both zharp at 10 t o SCA

-as general descripi ion -as general descript itjn

DARK BANDED PHYLL JTF

Strongly s i l i c i f i e d rhroughout. Fo l i a t i on at 20 t o SCA, N inera l izat ion = 2-41 f i ne dissen r' LC sharp at 20 to SCA

-as general desrr ip t , in

AR6ILLACEOOS L IHESTlIhl


ARGILLACEOUS 1 IWESTONf

-broken and fractured along tarb vein at 85 t o SCA

5 457 663,50 664.71 1.21 (.001 .02 ,036 ,OI ,04 5 458 664.71 665.92 1.21 (.001 .02 ,004 c.01 (.01

3 159 665.92 667,34 1,42 (.001 <.01 ,004 <.Ol (-01

HOLE I : 6-94-5

OREQUEST CONSULTANTS LTD, HOIE I : 6-94-5 PR6E 1 19 of 14

FROi4 TO ROrK ALT FOL TVPF CIA

DESCRIPTION 2 SAMPLE NO, FROH TO LENGTH A u Ag Cir Ph 2n SULPHIDE opst opst pct pct pct


END OF MOLE

OREQUEST CONSULTANTS LTD - DIAMOND DRILL HOLE RECORD C l i e n t BETHLEHEM Fage I 1 of 6

t io le No. 6-'?4-6 Nor th ing 3077.96 Core S ize No 11 I BQ Oepth D i p Azimuth Depth D ip Azimuth S t a r t e d SEPT, 9, 1994 Target HlNE OREBODY Property LOLDSTREAM East ing 15986.87 Casing 10' PVC PIPE 61.0 - 89 210 137.2 - 88 208 Completed SEPI. 15 1991 Comments HOLE CEIIEPTED @

Lorat ion REVELSTOKE E levat ion 666.11 Length 367.99 213.4 - 86 219 298.6 - 83 217 D r i l l Co. OLYMPIC NTS 82Mi9W L a t i t u d e 5 1 38' 00" N Dip-Co l la r -90 365.9 - 80 220 Logged By W . R A W Claim No Longi tude 118 24' 40" W Bearing N/A U n i t s METERS


DESCRIPTION 2 SAMPLE No. FRON TO LENGTH Au Ag Cu Pb Zn SULPHlDl o p t opst p c t p c t p c t

51.83

51.83 79.03

51,83 61.17

51.83 54.10 55.11 55.43 57.94 60.65

61.17 68.40

62.37 62.70 62.13 63.04 65.83 65.94 66.79 66.87 67.22 67.24 67.32 68.40

68.40 79.03

OVERBURDEN

CARBONATE PACKAGE (BADSHOT AND MOHICAN FORRATIONS)


B lack t a green a r g i l l a c e o u s bands colnprised o f b i o t i t e and c h l o r i t e w i t h l e s s o r s e r i c i t e and tan b i o t i t e (10-409) in a grey wh i te carb m a t r i x (50-80%) ptyglaat ic q t z veins (1-3%) and c r o s s - c u t t i n g qtz-carb ve ins (1-32, lower down in u n i t ) . L o c a l l y broken and f rac tu red . Well f o l i a t e d a t 30-35 t o SCA. Trace-1% dissem py. LC sharp a t 70 t o SCA.

-h igh a r g i l l a c e o u s content (409) - C h l o r i t e Phy l l i t e , very weakly s i l i c i f i e d -51 q tz -carb tens ion gash i n f i l l ings in s t rong ly a r g i l l a c e o u s

1 imestone, from 60.18-61.65 i s c leaner look ing marble, i n t e r v a l i s weakly f r a c t u r e d with l o c a l broken sect ions.

GREY MARBLE

Weakly banded ( a r g i l l a c e o u s m a t e r i a l ) / f o l i a t e d a t 30-35 t o SCA. Much c\eaner l o o k i n g than u n i t above. Minor i n t e r c a l a t e d c h l - b i o p h y l l i t e <5% of u n i t . UC sharp a t 70 along g r a p h i t i c s l i p with s t r o n g qtz-carb ve in ing . LC more gradat iona l . 1-42 g r a p h i t i c s t y l o l i t e s w i t h 5-8% over the (upper 50cm o f u n i t a t contact . T race- l t f i n e dissem p y a

-Calcareous B i o t i t e - S e r i c i t e P h y l l i t e , conformable -Calcareous B i o t i t e - S e r i c i t e P h y l l i t e , conformable -Calcareous B i o t i t e - S e r i c i t e P h y l l i t e , conformable -Calcareous B i o t i t e - S e r i c i t e P h y l l i t e , conformable -pale apple green rnar iposi te ? - s t r o n g l y broken and f r a c t u r e d

1NTERCALATED GREY MARBLE / CHLORITE - SERlClTE PHYLLITE

Limestone as above with 20% conformable in te rca la ted qreen C h l o r i t e -

68.40 68.46 69.00 69.33 70.00 70.14 70.49 71.01 71.30 71.76 74.14 74.39 75.46 ?5.86 76.23 76.40 76.46 76.56 17.63 77.15 77.38 71.03

PAGE 2 of 6 OREQUEST CONSULTANTS LTD, HOLE 1 I 6-94-6

FROM T O ROCK A t 1 FOL D E S C R I F T I O N I SAMPLE No. FROM TO LENGTH AII Ag , $u Fb l n o p s t ops t , P i t ' p c t >, p c t TYPE C I A SULPHIDE

S e r i c i t e P h y l l i t e . S e r i c i t e conten t i s auch weaker than in the u n d e r l y i n g CSP. UC a r b i t r a r y a t broken core area, L C sharp a t 35 t o SCA. Minor g r a p h i t i c s t y l o l i t e s , c r o s s - c u t t i n g q tz -carb vein:. (2-41) a t h i g h angles o f 70-85 t o SCA.

- s t r o n g l y broken and f r d c t u r e d -CSP with lcn c a l c i t e v e i n a t 85 t o SCA -CSP -CSP -moderately f r a c t u r e d and broken -CSP -CSP with q tz -carb ve ins a t 85 t o SCA o f f s e t S? ve ins by l c m -CSF -CSP -CSP -1-5cm wide brown b i o t i t e p h y l l i t e

7?.03 357.99

73.03 133.53

73.79 101.00

80.96 81.11

81.40 84.45 84.45 84.90

93.60 96.65

96.65 99.70 99.70 101.00

101 .oo

103.27 103.35

82.13 82.44

87.50 94.06

LOWER INDEX FORMATION

CHLORITE - S E R I C I T E P H Y L L I T E

Pa le greenish-grey co loured rock comprised o f M a t r i x q t z (40-601) c h l o r i t e (10-20%) s e r i c i t e (10-252) brown b i o t i t e (5%) t a n b i o t i t e (59,) p t y g a a t i c q t 2 ve ins (1-3 t ) and f i n e dissem PO (l%), Minor soapy t a l c on S2 f r a c t u r e s . H e l l f o l i a t e d a t 30 t o SCA. UC and L C b o t h sharp a t 35 t o SCA. V a r i a b l y s i l i c i f i e d and broken and f rac tu red .

FRACTURE ZONE

Zone o f moderately t o s t r o n g l y f r a c t u r e d rock, l a r g e s e c t i o n s o f broken rock ch ips with c l a y gouge..Local competent s e c t i o n s t o t a l l i n g 10-15% o f zone.

-q tz v e i n a t 30-40 t o SCA, one c l o t o f PO w i t h cpy -vuggy q tz -carb ve ins a t 40-60 t o SCA, 2 - 4 m m wide -40% recovery bu t n o t t h a t broken so can ' t see where core was l o s t v e r y s t r o n g l y broken with c l a y - s e r i c i t e gouge -weak t o moderate s i l i c i f i c a t i o n with a fen l o c a l s o f t e r s e c t i o n s -35-402 recovery, i n t e n s e l y broken with much gouge from 14.06-96.65, some s e c t i o n s o f gouge have rounded q t2 "pebbles"

-70-75% recovery, s t r o n g l y f r a c t u r e d and broken -65% recovery, s t r o n g l y f r a c t u r e d and broken -below t h i s depth u n i t i s much more competent w i t h o n l y l o c a l broken s e c t i o n s and i s g e n e r a l l y weakly s i l i c i f i e d

-bar ren q t 2 v e i n with f o l i a t i o n Harped around minor S3 f o l d

..

HOLE # : 6-94-6

OREQUEST CONSULTANTS LTD. HOLE II : 6-94-6 PAGE II 3 o f 6

FROM TO ROCK ALT FOL DFSCRIPTION '6 SAMPLE No. FROM TO LENGTH Au Ag Cu Pb Zn TYPE C I A SULPHIDE opst opst p c t pc t pc t

108.55 112.16 -nore c h l o r i t i c and s o f t e r 112.16 112.94 115.52 115.58 122.24 122.37 -inoderatel y f r a c t u r e d 122.37 133.53 -1-2% qtz-carb tens ion gash i n f ill ings 123.38 124.06 -s t rong ly f rac tu red w i t h 60% recovery 125.03 115.10 125.85 127.13

128.30 129.85 -moderately f r a c t u r e d

-s t rong ly f rac tu red w i t h ser-clay gouge and barren broken up q t z veins -qtz ve in w i t h 1-2% PO blebs, UC a t 35, LC a t 60-65 t o SCA

-qt2 ve in a t 50 t o SCA with 2-31 PO blebs, trace cpy -qtz ve in or intense qtz f lood ing , minor sections o f CSF wi th in , trace-2% PO, t race cpy

133.53 337.71 DARK BANDED PHYLLIIE

Typical dark brown t o b lack coloured u n i t . Conprised o f q tz (30-401) b i o t i t e - c h l o r i t e (20-30%), g raph i te (S- lOt) , s e r i c i t e (5%)), carbonate (10-301) and 1-52 dissem and l a y e r p a r a l l e l PO. Well f o l i a t e d a t 25-30 t o SEA. UC sharp a t 35, LC i n f a u l t zone. Ptygeatic qt2 veins (5%) and var iab le tan b i o t i t e from (5-20%.

133.53 135.27

136.43 136.88 137.54 140.15 140.68 146.22

146.02 146.15 148.58 149.40 154.53 155.53 159.26 159.56 166.01 166.32 166.96 167.04

172.16 175.96 181.15

186 I 36 186.44 193.62 193.76 195.00 197.24 204.70 204.75 206.01 206 I 08

207.43 213 I 27 213.58 227.77 228.15

-2-4% qtz-carb tens ion gash i n f i l l i n g s , s t rong ly broken f r o i 135,OO-

- interbedded CSP -Ch lor i te - S e r i c i t e P h y l l i t e with l o c a l DBP and 3-4% banded PO -moderate S3 deformation steepens f o l i a t i o n t o 65-70 t o SCA and small

c renu la t ion f o l d i n g with axes a t safle angle, f r o @ 143.18-143.31 i s qt2 ve in a t 50 t o SCA with 2-3% PO, f r o n 143.31-144.20 i s moderately f rac tu red with 33% conbined py and PO

-qt2 ve in UC at 60, LC a t 40 t o SCA, trace py and PO -strong chl and reddish-brown b i o t i t e a1 t e r a t i o n -wavy f o l i a t i o n from weak S3 in te r fe rence -moderately f r a c t u r e d s t a r t i n g with 4mn o f g raph i t i c gouge a t 25 SCA -s t rong ly f r a c t u r e d -70% q t 2 f looded with 3-4% PO

-5% PO blebs with t race s p h a l e r i t e -1cn wide q tz ve in with 5% PO, 2% sph, 1% cpy at 25 to SCA -5nn gouge ve in a t 20 t o SCA with carb and graph i te -broken and f r a c t u r e d -broken and f r a c t u r e d -navy f o l i a t i o i i from $3 i n te r fe rence -broken and f r a c t u r e d -broken and f r a c t u r e d -warped f o l i a t i o n a t 50 t o SCA -navy f o l i a t io r i , 3-4% PO

-strong S3 c r e n u l a t i o n cleavage and f o l d i n g a t 50 t o SCA, f o l i a t i o n

135.10 with l o c a l S3 c renu la t ion cleavage at 50 t o SCA.

l o c a l l y a t 90 t o SCA around f o l d c losure

.

8

HOLE # : G-94-6

OREQUEST CONSULTANTS L T D , flOLE R : 6-94-6 FAGE 1 4 of 6 -

[ROM 70

229.49 232.29 238.75 238.80 243.63 243.69 744.11 244.32 246.04 246.16 247.74 247.84 290.33 249.46

252.60

256.09 257.04 ni.ii 258.52

263.60 263.80 267.12 267.38 268.YO 269.34 271.58 211.64 275.61 216.16 276.16 276.83

283.10 283.16 290.04 290.98 294.56 296.20 299.10 299.30 307.58 307.78 308.43 308.78 309.40 309.50 310.06 310.28 317.49 317.65

318.34 318.42 319.18 319.83 325.73 326.15 332.80 333.55 333.55 333.68 334.45 335.85

337.71 346.85

ROCK ALT FOL DESCRIPTION % SAMPLE No. FROM TO LENGTH Au Ag C U Pb Zn TYPE C I A SULFlllDE opct opst pc t pc t pc t

-S3 c renu la t ion cleavage a t 50 t o SCA -q tz vein, seni-conformable a t 20 t o SCA wi th 3% pa -q t2 ve in UC at 15, LC a t 50, 1% PO blebs -q tz veins and q t z f lood ing w i t h 3-4% pa -qt2 f l o o d i n g w i t h 2-3s. PO

-q tz f l o o d i n g with 2 - 3 pa -broken and f rac tu red -q tz vein, ~ C R wide a t 75 t o SCA w i t h 3% PO and 1% cpy as dissen blebs the cpy i s n i t h i n w i t h PO

4 3 crenu la t ion cleavage a t 50 t o SCA, l o c a l f o l d i n g -white qt2 veins, UC sharp a t 60, LC sharp a t 45 t o SCA, sulphides =

PO as coarse c l o t s (12) w i t h t race cpy and galena -s t rong ly broken and f rac tu red -5-61 PO along f o l i a t i o n -10-122 p tygaat ic q t z ve ins and augens -coarse p tygnat ic q t z ve in w i t h 3% po and 1k sph as dissem blebs -moderately f rac tu red and broken -a t2 ve in UC and LC a t 45 t o SCA, q u i t e barren except a t contacts, espec ia l l y UC which has approx 5% dissen and blebby PO

-q tz ve in a t 30 t o SCA, 19. PO w i t h epidote and c h l o r i t e -p tygnat ic qt2 ve in w i t h 2% dissen PO - 4 q t z veins, 5-1Ocm wide with 2-3% dissem PO, trace cpy -moderately broken and f r a c t u r e d -broken and f rac tu red with l o c a l g raph i te - carbonate gouge -moderately f rac tu red -s t rong ly f rac tu red w i t h g r a p h i t i c gouge -Moderately f rac tu red -moderately fract lured w i t h g r a p h i t i c gouge along narrow qtz-carb ve in a t 60 t o SCA

-as above bu t a t 30 t o SCA -q t2 ve in w i t h 1% dissea PO Mostly a t contacts -contorted f o l i a t i o n from S3 c renu la t ion cleavage and fo lds a t 50 SCA -q t2 vein, 1-2mn wide a t 85 t o SCA w i t h 3-4% py ha5 s p l i t core i n h a l f -broken and f rac tu red w i t h g r a p h i t i c gouge - loca l closed S2 f o l d s

GARNET ZONE iSUlURED DARK BANDED PHYLLITE FAULT ZONE)

Brecciated u n i t w i t h 10-15% qtz-carb tension gash i n f i l l i n g s . Strongly s i l i c i f i e d and has 5 1 0 % contor ted cher ty bands. Strong graphite on f rac tu res . Variable garnet content froa 2-3% up to 20% over small sections. Sulphides dre as disseminations and contorted wispy blebs w i t h py (1-31) and PO (14%) with l o c a l higher concentrat ions. UC i n f a u l t gouge, LC gradational but seni-conformable look ing a t 20 t o SCA.

r HOLE #: 6-94-6

OREQUEST CONSULTANTS L T D . HOLE II : 6-94-6 F A R II 5 o f 6

FROM TO ROCK At1 FOI TYPE CIA

GESCRIPTION % SAMPLE No. FROM T O LENGTH Au Ag Cu -' Fb Zll

SULFH IDE ops t ops t p c t p c t p c t

337.71 337.81 337.81 341.00

341.00 346.85

345.27 346.51

346.85 352.97

347.04 347:08 349.00 349.86 349.86 350.00 351.51 351.74 351.79 351.91

352.97 357.11

352.97 353.97 HWGSSZ s i l 353.97 355.22 HWGSSZ c i l

355.22 356.48 HWDSSi s i l

356.48 357.11 HWGSSi s i l

357.11 357.51

-b lack g r a p h i t i c gouge with 5% py - s t r o n g q t z - c a r b t e n s i o n gash i n f i l l i n g s averaging 15%, f o l i a t i o n i s q u i t e c o n t o r t e d and i s a t 65 t o SCA f r o # 340.55-310.88, garnet conten t i s f a i r l y low throughout a t 6%.

- inc rease i n c h e r t y bands t o approx 30% and a l s o in garnets t o 10-20"6, the c h e r t y bands are i n v a r i a b l e concent ra t ions , q tz -carb tens ion gash i n f i l l i n g s drop t o 1-3%, froln 343.80-343.95 i s s t r o n g l y f r a c t u r e d , 343.95-344.00 i s 30% PO and from 344.31-344.66 i s 40% magnetic PO

- s t r o n g l y f r a c t u r e d and broken

SILICIFIED LIMESTONE

Calcareous u n i t t h a t was probab ly a r g i l l a c e o u s 1 h e s t o n e t h a t i s now s i l i c a f looded. U n i t f i z z e s with HCl b u t i s q u i t e hard - can b a r e l y be scra tched w i t h k n i f e . Has q u i t e v a r i a b l e c h l o r i t e and b i o t i t e content with l o c a l sect 3ns o f f a i r l y c lean Marble w i t h minor g r a p h i t i c s t y l o l i t e s . U( i 5 gradat iona l , LC sharp a t 20 t o SCA. Sulphides are f i n e disseminated PO 1-3%.

- r u b b l e and rock c h i p s - c l e a n l imestone, UC a t 55 a long q t 2 vein, LC i n broken c a l c i t e v e i n - h i g h l y broken c a l c i t e - q t z v e i n - in tense s i l i c i f i c a t i o n - d i r t y brown s i l i c i f i e d l imestone o r b r o r n b i o t i t e p h y l l i t e

HANGING WALL DlSSEMlNAlED / STRINGERS SULFHIDE ZONE (WEAK TO STRONG MINERALIZATION)

Sharp UC a t 20, LC a l s o semi-sharp a t 40 t o SCA. Very s t rong t o in tense s i l i c i f i c a t i o n . M i n e r a l i z a t i o n i s weak t o s t rong disseminated t o weak s t r i n g e r ve ins . The PO i s non t o very weakly aagnet ic.

-weak disselo su lph ides , PO = 2-4%, cpy = t race-1% -s t ronger dissem su lph ides averaging 5-72 PO and 3-51 cpy and t r a c e

3 9

18

15

s p h a l e r i t e with 30% su lph ides from 354.53-354.73 -g rey t o b lack c h e r t y bands and s t ronger su lph ides w i t h 10-15% PO, 5-81 cpy and 1% s p h a l e r i t e

- s t r o n g d i s w sulphides, PO = 10-201, cpy = lo%, s p h a l e r i t e = 1-29

MASSIVE SULFHIDE ZONE / QUARTZ VEIN

St rong s i l i c e o u s massive su lph ide zone t o 357.42 i i t h 402 PO, 20% cpy, 5% s p h a l e r i t e then a su lph ide enr iched q t z v e i n w i t h 25% PO, 5 4 % cpy, and 2-38 s p h a l e r i t e . The q t z v e i n contac t i s a b i t d i f f u s e though t h e I C i s f a i r l y sharp a t 20 t o SCA

460 352.97 353.97 1.00 461 353.97 355.22 1.25

462 355.22 356.48 1 .26

463 356.48 357.11 .63

,001 .02 ,260 .01 .16 .003 .14 1.737 -12 1.17

,003 -17 2.026 . l 2 .40

,003 .24 3.002 .14 ,96

HOLE #: 6-94-6

OREQUEST CONSULTANTS L T D , HOLE II : 6-94-6 PAGE II 6 o f 6

FROIl T O ROCK ALT fOL TYPE C i A

DESCR IFT ION 2 SAMPLE No. ftOM TO LENGTH Au Ag Cu Pb Zn SULFHIDE ops t ops t p c t p c t p c t

357.11 357.51 MSZiUV s i l

357.51 359.55

357.51 358,?0 fWDSZ s i l 358.70 359.55 FWDSZ s i l

359.55 361.94

359.55 360.35 DBF s i l

361.94 363.07

363.07 364.46

361.46 367.99

-as general d e s c r i p t i o n

FOOIWALL DISSEMINATED T O SEMI-MASSIVE SULPHIDE ZONE

60 464 357.11 357.51 -40 ,003 ,51 4.284 -54 3.86

H i g h l y t o moderately s i l i c e o u s with v a r i a b l e s u l p h i d e c o n t e n t . UC sharp a t 20, LC is f a i r l y sharp based on su lph ide con ten t .

-8-10'6 d i s s e n PO, 5% d i s s e n cpy, 1-2% s p h a l e r i t e 15 465 357.51 358.70 1 .19 .DO1 .07 1.089 .02 .14 -semi-massive s u l p h i d e s w i t h pa = 30%, cpy = 1.2% and s p h a l e r i t e = t r 32 466 358.70 359.55 .85 <,001 c.01 ,517 .Ol .02


-gradual decrease in su lph ides with PO = 5b and cpy = t race-1% 5 467 359.55 360.35 -80 c.001 c.01 .082 .04 -08

GREEN CHLORITE PHYLLITE

S I t I C I f I E D BIOTITE - SERICITE FHYLLITE

ARGILLACEOUS L IMESTOPE

367.99

F o l i a t i o n a t 30 t o SCA

END OF HOLE

Page I 1 of 10 0 RE Q UE S T C 0 N S U L T A N T S L T D - DIAHOND DRILL HOLE RECORD C1 ient BETHLEHEH

Hole No. 6-94-7 Northing 3304 Core Size NQ I1 Depth Dip Azimuth Depth Dip Azimuth Started OCT. 4, 1994 Target NINE OREBODY Property GOLDSTREAH East ing 16024 Casing 10 FT PVC PIPE 91.5 - 88 190 176.8 - 84 203 Coupleted OCT, 13, 1994 Coaaents HOLE CEHENTED Location REVELSTOKE Elevation 675 Length 498.48 253.1 - 79 203 314.0 - 77 210 Drill Co. OLYHPIC NTS 82111911 Lati tude 5 1 38' 00" N Dip-Collar -90 359,8 - 75 210 405.5 - 72 210 Logged By W . RAVEN Claia No Longitude 118 24' 40" W Bearing N/A 451.2 - 72 211 497,O - 71 215 Units HETERS


DESCRIPTION 1 SANPLE No. FROH T O LEN6TH Au Ag Cu Pb Zn SULPHIDE OpSt OpSt pCt pCt pCt

85.37

85.37 131.25

85,37 123.67

85.37 88.58 88,58 94.67 94.67 97.54

105.52 105.67 111.18 113.25

113.25 116.22

117.13 117.45 118.34 118.82 121.76 122,37

123.67 131,25

OVERBURDEN

HAHILL GROUP

SILICEOUS CHLORITE - SERICITE PHYLLITE / QUARTZITE

Hediui green coloured f i n e grained equigranular un i t , Local sections of grey-white dense iassive quartzite, Comprised of f i ne quartz (50-70%), ch lo r i t e (10-30%), s e r i c i t e (5-102), p t yg ia t i c quartz veins (1-3%), cross-cutt ing quartz veins (trace - 111, 6enerally weakly t o moderately s i l i c i f i e d though c h l o r i t e +/- se r i c i t e r i ch sections are softer. The grey-white true quar tz i te sections are s l i g h t l y vuggy. Unit i s f o l i a ted o r rhythuat ica l ly bedded a t 35 to SCA. Some minor carbonate on fracture planes (11), Hinor disseminated py (1). Lower contact sharp and confonable a t 35 t o SCA.

-greenish - grey - white quar tz i te -greener s i l iceous CSP with loca l tuffaceous sections -quartzite? stronger s i l c i f i c a t i o n with qtz f loodinglvein f ro# 96.42-96.90 1 1 - 2 2 PO, trace cpy & sph f ro4 96.47-96,51, lower par t of the vein looks broken and subsequently healed with graphite rims around quartz fragrrents.

-broken and fractured -2-31 qtz-carb tension gash i n f ill ings above gouge zone

-60U6E ZONE - strong se r i c i t e - ch lo r i t e - carbonate i n green & white speckled gouge, F a i r l y coapetent i n core, not iush, but eas i ly crushed; seii-brecc iated appearance,

-strongly fractured and broken -strongly fractured and broken -strongly fractured and broken

QUARTZITE

Grey - white to s l i g h t l y greenish coloured, f i n e grained, dense,

.*

OREQUEST CONSULTANTS L T D - HOLE II : 6-94-7 PAGE 1 2 of 10


DESCRIPTION % SAMFLE No. FROM TO LENGTH Au A9 Cu Fb l n SUL PH IDE opst opst pc t pc t pc t

123.80 124.08 124.08 127.13

127.94 128.97 128.97 129.14 130.18 131.06

131.25 246.22

131.25 157.52

131.25 147.40

147.40 151.42

151.52 154.90

154.90 156.30 156.30 157.52

157.52 167.17

massive quar tz i te . Local s e r i c i t e and c h l o r i t e , espec ia l l y where u n i t i s broken. Loca l l y vuggy where carb s t r i n g e r veins have weathered out. Contains 3-51 p tygnat ic quartz veins i n sec t ions t h a t resemble s i l i c e o u s CSP. UC I LC sharp @ 35 t o SCA. Ninor dissen py.

-rock ch ips and rubble, strong ser, 35% recovery -on ly 10-15% recovery, looks l i k e nost core was l o s t from 124.08 - 126.68 as core a t the lower 127.13 b lock i s competent.

-moderately f rac tu red w i th warped f o l i a t i o n -s t rong ly broken and f rac tu red -Moderately t o s t rong ly f rac tu red and broken

CARBONATE PACKAGE (BADSHOT AND MOHICAN FORMATIONS)

ARGILLACEOUS L IMESTONE

S t rong ly a rg i l laceous w i t h grey-white carb (45-65%), f i n e rounded q t z blebs (lmn set i n the carb n a t r i x (5%) and black b i o t i t e - s e r i c i t e - graph i te n i x (30-40%). F o l i a t i o n i s q u i t e wavy 8 disr1,ipted and the u n i t looks f a u l t e d as i t contains 10% qtz-carb tension gash i n f i l l i n g s . Strong S3 i n te r fe rence. UC f a i r l y sharp @ 35-45 t o SCA along a 5ca wide q tz ve in r i t h 22 PO. LC a t 40 t o SCA. Healed f a u l t zone froar 131.25 - 156.30.

-brecciated appearance w i th 10% qtz-carb tens ion gash i n f ill ings, s t rong 53 crenu la t ion cleavage t 30-60 t o SCA, weakly t o moderately f rac tu red , core i s reasonably competent, f o l i a t i o n i s var iab le due t o d is rup ted nature of i n t e r v a l ranging f r o n 30-60 t o SCA, l o c a l s t rong ly broken 8 f rac tu red sections ranging from 10-3Ocm i n length, l o c a l cleaner marble sections w i t h 1-39. g r a p h i t i c s t y l o l i t e s .

-as above bu t 10-202 qtz-carb tens ion gash i n f i l l i n g s , f o l i a t i o n l o c a l l y @ 90 t o SCA, s t rong ly b recc ia ted look ing

-GOUGE ZONE, very s t rong ly b recc ia ted w i t h c l a y gouge conta in ing subangular t o rwnded Rarble pebbles, rubble 8 rock chips,

-s t rong ly broken 8 f rac tu red bu t no gouge -cleaner look ing grey ra rb le , UC sharp along g r a p h i t i c f r a c t u r e 1 6 0 t o SCA; LC a lso sharp t 40 t o SCA; the f a u l t zone ends a t the s t a r t o f t h i s u n i t .

SILICIFIED bRGILLACEOUS LIMESTONE

U n i t looks more l i k e the DBP w i t h p tygnat ic q tz veins t o 59. 8 has more ch l -b io -ser 8 f i n e grained q tz i n the r i a t r i x . S i l i ceous core i n the Carbonate Package. Local s t rong 1 iny sec t ions s t i l l present as in te rca la t ions . Contains 1-32 f i n e dissen PO. Well f o l i a t e d @ 35-40 t o SCA. UC cosformable @ 40 t o SCA. LC i s i r r e g u l a r .

HOLE I : 6-94-7

O R E Q U E S T C O N S U L T A N T S L T D , HOLE 1 : 6-94-7 PAGE II 3 o f 10

FROM TO ROCK At1 FOL DESCRIFTION % SAMPLE No. FROM TO LENGTH Au. Ag Cu Pb Zn opst ops t p c t . p c t p c t TYPE C I A SULPHIGE

167.17 170.01 GREY MARBLE

Hediun gra ined r e - c r y s t a l 1 i zed 1 imestone w i t h minor a r g i l l a c e o u s m a t e r i a l and p h y l l i t e . U n i t has 1-29. g r a p h i t i c s t y l o l i t e s . UC i r r e g u l a r , LC sharp @ 20 t o SCA.

170.01 175.35 SILICIFIED ARGILLACEOUS LIMESTONE

170.88 171.49

171.49 172.02 112.02 175.35 173.46 173.90

175.35 177.63

177.63 183.16

178.09 178.14 177.63 178.64 178.64 179.66 179.66 180.50

180.50 181.88

181.88 183.16

183.16 186.74

As descr ibed 157.52-167.17n. A b i t More v a r i a t i o n f rom DBP t o more c h l 8 s e r - r i c h sec t ions t o more o f the t y p i c a l l o o k i n g a r g i l l a c e o u s 1 imestone ( n o n - s i l iceous). M i n e r a l i z a t i o n i s 1-28 d i s s e i py 8 PO. UC sharp t7 20 t o SCA. LC sharp t7 25 t o SCA.

-broken q t z v e i n @ upper contac t , lower contact i s sharp P 45 t o SCA, conta ins 1-2% dissem py 8 PO.

- p a l e r g reen ish c o l o u r due t o c h l 8 s e r - v a r i a b l y s i l i c i f i e d - i n t e n s e l y broken 8 f r a c t u r e d

GREY MARBLE AND ARGILLACEOUS L MESTONE

S i m i l a r t o t h a t descr ibed 167.17 - 170.01 but more banded a r g i l l a c e o u s m a t e r i a l a t 30 t o SCA.

HEDIUM TO COARSE CRYSTALLINE GOLOMITE / MARBLE

White t o g r e y i s h wh i te co lour , f a i r l y pure l o o k i n g except f o r Midd le p o r t i o n which has 5-101 a r g i l l a c e o u s m a t e r i a l . F izzes f a i r l y e a s i l y i n HCL so must be inpure dolomite, j u s t looks q u i t e pure. F a i r l y competent except f o r one zone o f broken 8 f rac tu red rock. Loca l f i n e gra ined s e c t i o n s o f more pure do lomi te . UC sharp t7 28 t o SCA. LC sharp P 50 t o SCA. Minor d issen py ( t r - 1 % ) .

-smal l band o f conformable CSP. -medium t o coarse ly c r y s t a l l ine - f i n e r g ra ined, more porcelaineous do lomi te -more f r a c t u r e d with 101 grey ish-b lack arg i l laceous n a t e r i a l z b i o t i t e ? and graph i te? , w i t h n i n o r s e r i c i t e

- s t r o n g l y f r a c t u r e d and broken throughout, contains the c r y s t a l 1 ine and porce la ineous do lomi te with minor competent core 8 l o c a l py to 2%

- f a i r l y c l e a n coarse c r y s t a l l i n e dolorni te

FINE GRAINED PORCELAINEOUS DOLOMITE

Fure wh i te c o l o r except f o r minor f r a c t u r e s w i t h p a l e g rey nicaceous HOLE # : G-94-7

. . . , 1.

O R E Q U E S T C O N S U L T A N T S LTD, HOLE R : 6-94-7 PAGE II 4 o f 10

F R O M T O ROCK ALT FOL TYPE C I A

DESCRIPTION % SAMPLE No. FROM T O LENGTH Au Ag Cu Pb SULPHIDE ops t ops t p c t p c t p

186.74 195.51

189.61 190.26 192.17 192.36 133,33 194.88

195.51 204.29

204.29 212.99

212.99 220.23

214.41 214.81 217.10 217.81 217.98 218.25

m a t e r i a l . U n i t b a r e l y e f fe rvesces i n 102 HCL when powdered. Rare s t y l o l i t e s , UC sharp I 50, LC sharp ! 30 t o SCA. S t y l o l i t e s are g r a p h i t i c t o nicaceous. V i r t u a l l y no su lph ides in u n i t .

CHLORITE-BIOT HE-SERICITE SILICIFIED PHYLLITE

Grey-green co loured u n i t t h a t i s v a r i a b l y s i l i c i f i e d . Upper p o r t i o n t o 191.37 i s s o f t e r with moderate s i l i c i f i c a t i o n from 191.37 - 195.51. Minor soapy t a l c on f r a c t u r e s on t h e upper p o r t i o n . UC 8 LC sharp ! 30 t o SCA. Po as dissem t o 1%.

- r o d e r a t e l y f r a c t u r e d - q t z vein, i r r e g u l a r UC 8 LC, 8% w a l l r o c k f rags , 1% PO

-2% q t 2 carb tens ion gash i n f i l l i n g s

INTERCALATED ARGILLACEOUS LIMESTONE / GREY MARBLE 8 CHLORITE PHYLLITE

Contains 65% a r g i l l a c e o u s t o moderately c r y s t a l 1 ine marble with 30% i n t e r c a l a t e d green c h l o r i t e p h y l l i t e . The a r g i l l a c e o u s p o r t i o n o f the marble ends a t -199.00, then it i s the c l e a n grey Marble. LSTiCP c o n t a c t s a re conformable a long f o l i a t i o n a t 25-30 t o SCA. Local b r o r n b i o t i t e (la), ptygmatic q t z v e i n s (1-2%) and c r o s s - c u t t i n g q tz -carb ve ins (1-28). UC sharp 1 2 5 t o SCA. LC sharp 1 30. C h l o r i t e - P h y l l i t e interbeds vary f r o i 1-40cn.

CHLORITE - SERICIIE - BIOTITE PHYLLIIE

Greenish c o l o u r w i t h f i n e l y laminated c h l - s e r +/- b i o t i t e , v a r i a b l e s i l i c i f i c a t i o n . Contains q t z (30-5011, c h l o r i t e (30-40%), s e r i c i t e (10-1591, ptygmatic q t 2 ve ins (1-52) & c r o s s - c u t t i n g q tz -carb ve ins (1-22). M i n e r a l i z a t i o n i s t r a c e - 2% d issen PO. UC sharp 1 3 0 , LC sharp ! 25 t o SCA. Upper metre i s most ly C h l o r i t e P h y l l i t e .

SlLlClFIED DOLOMITE

Pure wh i te t o greenish-grey c o l o u r . S i m i l a r t o 183.16-186.74 but has pervas ive secondary s i l i c i f i c a t i o n - hard, cannot s c r a t c h w i t h k n i f e . F a i n t banding I 2 5 t o SCA. Minor interbedded t a n b i o t i t e - c h l o r i t e p h y l l i t e . UC sharp ! 30, LC sharp I 35 t o SCA. L o c a l l y broken, t race d isseu pa. Minor s e r i c i t e on some f r a c t u r e s .

-moderately f r a c t u r e d and broken -moderately f r a c t u r e d and broken - t a n b i o t i t e - c h l o r i t e p h y l l i t e

HOLE 1: 6-94-7

O R E Q U E S T C O N S U L T A N T S LTD, HOLE B : G-94-7 PAGE II 5 o f 10

FROM TO ROCK CLT FOL TYPE C I A

DESCRIPTION 2 SAMPLE No. FROM T O LENGTH Au A9 Cu Fb Zn SULPH IDE opst opst pc t p g ., pct

a 220.23 227.81 CHLORITE-SERICITE-BIOTITE PHYLLITE

227.81 246.2?

234.40 234.70 236.14 236.22 245.00 246.22

246.22 498.98

246.22 292.08

246.22 249.20 255.59 264.23 256.02 256.28

256.28 256 I 50 260.68 260.94 261.17 261.26 261.31 261.43 264.23 268.35 266.17 266.27 267.38 268.10

268.35 279.72

As descr ibed 204.29-212.99, but has about 10-15% carbonate, though u n i t i s s t i l l weakly s i l i c i f i e d b u t v a r i a b l y , Local q tz r i c h sec t ions UC sharp 1 35, LC sharp 1 30 t o SCA. Trace - 2% dissen PO.

ARGILLACEOUS LIMESTONE 1 MINOR CSP

As descr ibed 131.25 - 157.52 with n i n o r i n t e r c a l a t e d CSP as descr ibed 186.74 - 195.51. Local c leaner narb le with 1-22 g r a p h i t i c s t y l o l i t e s . F o l i a t i o n i s wavy to weakly contor ted due t o pervasive $3 i n te r fe rence. P tygnat ic q t z veins (1-33). UC sharp e 30, LC sharp @ 60 along g r a p h i t i c gouge. Contains 51 qtz-carb ve ins which are d i s r u p t e d "net" t e x t u r e and minor tens ion gash i n f i l l ings. CSP more preva len t near bottom o f u n i t . S3 c r e n u l a t i o n f o l d s and cleavage ij 50-60 t o SCA.

-3% PO as dissem and p a r t i a l veins -c lay gouge -c leaner marble with 5% g r a p h i t i c s t y l o l i t e s

LOWER INDEX FORMATION

CHLORITE - S E R I C l T E PHYLLITE (VARIABLY SILICIFIED)

Green - greenish-grey t o reddish co loured u n i t . General ly weakly t o moderately f rac tu red with s o w shat te red sec t ions . > s e r i c i t e = more broken, > s i l i c a more competent. Comprised o f c h l o r i t e , s e r i c i t e , + / - muscovite and b i o t i t e i n s i l i c e o u s mat r ix , f i n e l y laminated and f o l i a t e d a t 20-25 t o SCA. P tygaat ic q t z ve ins (1-511, t r a c e - 2% d issen PO. UC sharp e 60 along graph i tc gouge, LC sharp a t 30 t o SCA.

- s t r o n g l y f rac tu red t o shattered, "poker chip" core -purp l i sh- redd ish co lour , s t rong s i l i c i f i c a t i o n -minor f o l d s t r u c t u r a l upper 1 inb 1 85 t o SCA, lower 1 imb @ 70 t o

SCA, a x i s 1 5 0 t o SCA. -moderately f r a c t u r e d -broken q t z ve in with 1-2: PO, 11 galena, t race s p h a l e r i t e -q t2 vein, conformable 1 25 t o SCA, bar ren -as above - s t r o n g ch l 8 ser, l e s s s i l i c a as u n i t i s no t s i l i c i f i e d - rubb le and rock chips, s t rong s e r i c i t e -moderately t o s t rong ly f r a c t u r e d w i t h broken q t z v e i n from 267.71

268.05 with 2% py, 1% sph. -moderately s i l i c i f i e d , greenish-grey t o f a i n t p u r p l i s h co lour ,

minor broken sec t ions and l o c a l s o f t e r i n t e r v a l s , t race - 2% quar tz -

'L

.

I

HOLE #: 6-94-7

OREQUEST CONSULTANTS LTD, HOLE I : 6-94-7 PALE I 6 o f 10

FXOM T O ROCK At1 FOL TYPE C I A

DESCRIFTION % SAMPLE No. FRO1 T O LENGTH Au A9 Cu Pb Zn SUL PH IDE opst opst pc t p c t pc t

273.25 273.48 273.48 273.64

278.23 278.70 279.16 279.27 279.72 281.52 281.52 281.73 281.73 292.08 284.68 284.78

289.02 289.13 286.37 286.85

292.08 466.62

292.08 294.70

294.70 300.68

300.68 300.91 302.00

310.14 310.56 317.38

318.01 318.21 319.05 319.13 320.06 320.22 320.22 320.53 324.00 324.08 333.93 334.05 334.14 334.21 336.91 337.28

carb tens ion gashes. -s t rong ly f r a c t u r e d -qt2 ve in w i t h 10-15% ch l -ser rock fragments and trace - 1% dissen

PO blebs. -s t rong ly f r a c t u r e d t o broken -broken and f r a c t u r e d w i t h 2 c i confornable gouge - s o f t e r sec t ion w i t h more s e r i c i t e and c h l o r i t e -qt2 b recc ia ve in w i t h 8 cm of s e r i c i t i c gouge @ 50 t o SCA - s i l i c i f i e d w i t h l o c a l s o f t e r sec t ions & l o c a l l y f rac tu red 8 broken -s t rong ly f r a c t u r e d and broken -s t rong ly f rac tu red and broken -ptygmatic q t2 ve in w i t h 1-22 PO, t race cpy

DARK BANDED PHYLL I T E

Typical DBP comprised o f tan b i o t i t e (15-25%), dark b i o t i t e - c h l o r i t e (10-20%), s e r i c i t e (5%), g raph i te (3-10'6), quartz (102) 6 carbonate (20-40%), ptygmatic quart2 veins ( l - S t ) , Po i s ub iqu i tous as small b lebs 8 l a y e r p a r a l l e l streaks (1-221, l o c a l l y up t o 5-7%. U n i t i s d i s t i n c t l y banded and we l l f o l i a t e d . Local S3 deformation o f f s e t t i n g S2 f o l i a t i o n . UC sharp 1 30 t o SCA along g r a p h i t i c gouge = semi- c o n f o r i a b l e contact. LC i s sheared / fau l ted .

-FAULT ZONE - s t rong g r a p h i t i c gouge a t UC, then brecciated w i t h q t2 - carb tens ion gash i n f i l l i n g s and l o c a l g r a p h i t i c gouge, 2-42 py 8 PO i n the gouge i n t e r v a l s .

-DISRUPTED ZONE - d is rup ted i n t e r v a l below f a u l t zone, up t o 5'6 qt2 +/- carb tens ion gash i n f i l l i n g s , h i g h angle qt2 veining o f f s e t t i n g S 2 and the f o l i a t i o n angle var ies f r o n about 30-60 t o SCA, minor q tz -brx w i n s . UC gradational, LC sharp 1 60 t o SCA. F o l i a t i o n changes n o t i c a b l e below t h i s i n t e r v a l t o 20 t o SCA, so hole must f l a t t e n through t h i s f a u l t i n g .

-below t h i s p o i n t i s more t y p i c a l DBP - l o c a l l y d is rup ted by S3, contains 2 X lOcln qtz veins, broken w i th

minor gouge over lower 20 CA

-53 c r e n u l a t i o n f o l d s and cleavage @ 40-45 t o SCA - b i t change w i t h 8 CR o f cave below t h i s p o i n t -S3 f o l d i n g 1 55 t o SCA -q t2 vein, i r r e g u l a r UC 8 LC, 5% PO c l o t s , trace cpy -stockwork q t2 b recc ia veining, UC along 5 -q tz vein, UC @ 65, LC @ 35, minor PO c l o t s - q t z ve in @ 40 t o SCA, 1t PO, t race sph -1 cm qtz-carb ve in 1 5 5 t o SCA w i t h g raph i te 8 3% PO - g r a p h i t i c gouge -q tz ve in w i t h n i n o r carb, 3-4 mm wide @ 85 t o SCA, vein ha: 5-86 PO

as disseminations.

gouge

HOLE #: 6-94-7

HOLE 1 : 6-94-7 PAGE tl 1 o f . 10 O R E Q U E S T C O N S U L T A N T S L T D ,

F R O M T O ROCK ALT FOL DESCRIPTION % SAMPLE No. FRON T O LENGTH Au A9 Cu F6, Zn TYPE C I A SUL FH IDE OpSt OpSt pCt pCt pCt

331.40 331.70 -as above bu t v e i n has 10-152 PO 344.90 344.97 341.74 347.84 360.03 360.29 373.02 373.28

314.27 318.70

384.12 387.86 -carb-enr iched i n t e r v a l t o 45%

-p tygnat ic ve in on h a l f o f core with 32 d issen PO - q t z v e i n 50 t o SCA, 12 PO, t r a c e sph e contac ts - q t z f looded (353) as i r r e g u l a r v e i n s with 2% PO -q tz f l o o d i n g (35-402)) with 2-32 PO 9, t r a c e sph, sub-para l le l t o

- i n t e r v a l o f enr iched PO as d isseminat ions and smal l f o l i a t i o n f o l i a t i o n @ 30.

p a r a l l e l s t reaks averaging 4-62, t r a c e cpy, sph

-1.5 cm q tz -carb v e i n with b r e c c i a t e d w a l l r o c k fragments, v e i n has 5% PO b lebs @ 50 t o SCA

-wavy f o l i a t i o n @ 60-65 to SCA n i t h 6-8% dissem 6 l a y e r p a r a l l e l PO

396.86

403.00 410.37 -aoderately s i l i c i f i e d 404.68 405.65 410.52 415.45 -FRACTURE ZONE

I n t e r v a l i s moderately t o l o c a l l y s t r o n g l y f r a c t u r e d w i t h n i n o r 1-4 ma gouge ve ins and 14% qtz-carb t e n s i o n gash i n f i l l i n g s .

-wavy f o l i a t i o n with S3 c r e n u l a t i o n c leavage a t 45-50 t o SCA

-qtz-carb-aragoni te? v e i n @ 75 to SCA, has c l e a r needle-1 i k e c r y s t a l s up t o 5 mH l ong

415.94 418.00 418.93 418.53 - s t r o n g l y broken and f r a c t u r e d 418.71 418.17

419.35 419:43 -broken and f r a c t u r e d 419.82 420.17 -broken q tz -carb v e i n i n g a t 60 t o SCA 431.55 431.70 -broken and f r a c t u r e d 437.41 437.41 438.64 439.13

-broken and f r a c t u r e d with 1 cm g r a p h i t i c gouge v e i n P 15 t o SEA -con tor ted f o l i a t i o n w i t h l o c a l f o l d axes @ 45-85 t o SCA, i n t e r v a l con ta ins -15% PO (moderately Magnet ic) as f i n e gra ined d issen p a r a l l e l t o f o l i a t i o n and as coarse b l e b s up t o 1 cm X 1 t m and massive c l o t s a long d i s r u p t e d q t z - c a r b ve ins .

-4-62 f i n e gra ined PO as f i n e f o l i a t i o n p a r a l l e l d isseminat ions - v a r i a b l e S3 d e f o r a a t i o n as weak t o moderately n e l l developed

c r e n u l a t i o n c leavage and l o c a l c r e n u l a t i o n f o l d s @ 40-50 t o SCA, a lso have c losed S2 f o l d s p a r a l l e l t o f o l i a t i o n @ 70-80 t o SCA.

-narrow q tz -carb ve ins @ 70-80 t o SCA

439.13 444.15 451.62 466.62

465.18 466 I 62

466.62 473.38 GARNET ZONE ( I N CONTORTED, SILICIFIED GARK BANDED PHYLLITE)

E n t i r e zone i s q u i t e d i s r u p t e d and c o n t o r t e d due t o l o c a l l i z e d f o l d i n g and f a u l t i n g . The UC i s sheared l fau l ted , LC i s sharp a t 30 t o SCA w i t h under ly ing grey-green p h y l l i t e . The zone is g r a p h i t i c i n the s t r o n g l y sheared areas and i s s i l i c i f i e d throughout w i t h l o c a l l i z e d c h e r t bands up t o 15%. Also has b r e c c i a t e d and s w i r l e d cher t bands and white q t z b lebs . Garnet concent ra t ions are v a r i a b l e frora 5% l i g h t p i n k rounded porphyrob las ts t o 30% d u l l p i n k t o d u l l greenish-brown co lo red garnets. Var iab le s u l p h i d e conten t dominated by PO from 1-28 up t o 30-40'6 w i t h minor t races o f cpy.

HOLE #: 6-94-7

O R E Q U E S T C O N S U L T A N T S L T D , HOLE I : 6-94-7 PAGE II 8 o f 10

FROM TO ROCK At1 FOL TYPE C I A

DESCRIPTION % SAMPLE No. FROM TO LENGTH Au A9 cu Pb 211 SULPHIDE opst ops t p c t p c t p c t

466.62 461.26

167.26 467.50

467.50 467.58 467.58 469.12

469.12 469.51 169.51 470.08

470.08 470.56 470.56 471.15

471.95 472.82

472.82 473.38

473.38 476.94

474.13 414.16 474.86 415.01

476.94 477.65

477.65 181.15

-upper 3 cn i s f r a c t u r e d with gouge; b r e c c i a t e d appearance w i t h 10-

-15-201 contor ted wispy PO, minor f o l d s e 85 t o SCA, s t r o n g g r a p h i t e

- s t r o n g l y f r a c t u r e d and broken w i t h g r a p h i t e -10-209 c h e r t bands, f rom 468.01-468.57 the f o l i a t i o n i s a t 60 t o SCA, and the cher t bands are l o c a l l y o f f s e t by 1-2mm a long h a i r l i n e f r a c t u r e s , from 468.57-169.12 i s b r e c c i a t e d l o o k i n g

- s i m i l a r t o above i n t e r v a l b u t with 10% PO - s t r o n g l y cher ty i n t e r v a l with 5-83 p i n k garnets, 3 4 % q t z t e n s i o n gash i n f ill ings.

-broken and f rac tu red , 60% recovery, one s e c t i o n w i t h 20% PO

- m i - b r e c c i a t e d appearance, 30% garnets, the f o l i a t i o n 30 t o SCA,

-Arg i l laceous Linestone, warped f o l i a t i o n f rom 25-70 t o SCA, 15% q t 2

-DBP garnet zone w i t h 30-402 garnets over lower 10cn, l o c a l PO t o 15'6.

15% whi te q tz , 30% d u l l greenish-grey garnets, 2-33 d issea PO

on f r a c t u r e s

471.26-471,30 broken with gouge

t e n s i o n gash i n f i l l i n g s , no garnets in t h i s i n t e r v a l

GREY-GREEN PHYLLIIE (VARIABLY SILICEOUS CHLORITE-SERICITE PHYLLIIE)

U n i t i s weakly t o moderately c o n t o r t e d with v a r i a b l e s i l i c i f i c a t i o n . Comprised o f quar tz (30-10%), c h l o r i t e (10-153), s e r i c i t e / m u s c o v i t e (30-40%), p t y g n a t i c q t z (51) , b i o t i t e ? 8 graph i te? ( l o % ) , cross- c u t t i n g carb ve ins (1%). M i n e r a l i i a t i o n i s f i n e d issen PO ( t race-2%) , t r a c e cpy. UC sharp k! 30, LC sharp e 40 t o SCA which i s a l s o general f o l i a t i o n angle.

-q t2 v e i n e 45 t o SCA, dissem PO = 12, t r a c e cpy -q t2 vein, UC 1

PO 2 3-41, t race cpy


Good f o l i a t i o n k? 30 t o SCA.

40, LC -60 t o SCA, b o t h are a b i t i r r e g u l a r , d i s w

HANGING WALL DISSEMINATED SULPHIDE ZONE (WEAK H INERAL I Z A T ION)

Comprised o f s i l i c i f i e d l imestone t o 478.84, then h i g h l y c o n t o r t e d and a l t e r e d grey-green p h y l l i t e t o 461.15, F o l i a t i o n in the upper s i l i c i f i e d 1 s t P 30-40 t o SCA, 1 i t t l e f o l i a t i o n present i n lower u n i t . M i n e r a l i z a t i o n i s sparce, very f i n e gra ined PO, t race - 2-31. UC i s sharp 1 40. LC e I 40-50 t o SCA based on su lph ide conten t .

HOLE # : G-94-7

OREQUEST CONSULTANTS LTD. HOLE B : 6-94-7 FAGE I 9 o f 10

FROM T O 40CK ALT F O l TYPE C I A

DESCRIPTION 9, SAMFLE No. FROM TO LENGTH Au Ag cu Pb Zn SULPH IDE opst opst pc t p c t pc t

477.65 478.84 HUDSZ s i l

478.84 480.58 HWDSZ s i l ser

480.58 481.15 HWDSZ s i l ser

481.15 485.34

-as described above ( s i l i c 1 s t ) w i th 2% f i n e grained dissem PO and trace cpy

-contorted grey-green p h y l l i t e , looks seai-brecciated, broken q tz ve in ing around warped f r a c t u r e I! 85 t o SCA t o 479.15; s t rong ly f rac tu red and broken w i t h minor gouge from 479.91-480.53, then a 5 CR

q tz ve in @ 30-40 t o SCA. - f r a c t u r e d and broken, looks l i k e the s i l i c i f i e d 1st t o 480.84 w i t h f o l d axes ! 85, good cpy (1%) and 102 PO f o r 1 cm a t q tz ve in contac t and from 480.87-480.96 w i th 10% cpy, 152 PO.

SEMI MASSIVE T O MASSIVE SULPHIDE ZONE

481.15 481.91 SMDSZ s i l

481.91 482:35 MSZ s i l

48?.35 483.28 DID s i l

483.28 483.89 SMPSZ s i l

483.89 484.69 MSZ s i l

484.69 485.06 SMDSZ s i l

485.06 485.34 MSZ s i l

485.34 498.48

485.34 486.00 DBP/LS gra,car

486.00 487.00 LSI carb

S i l i ceous sulphide zone w i th Minera l i za t ion found as disseainations, s t r i n g e r s and massive ore. Often see massive disseminations forming a "net-1 ike" tex tu re . Contains 10-251 rounded grey q tz eyes and 10-201 secondary white quartz. UC sharp ! 40-50, LC i s a t small gouge zone.

-SEN[-MASSIVE DISSEMINATIONS AND STRINGERS - s t r ingers @ 15 t o SCA, PO = 10-202, cpy a l s o 10-20%, var ies w i t h i n i n t e r v a l , there i s 1-21 f i n e reddish brown s p h a l e r i t e around pa g r a i n nargins.

-MASSIVE SULPHIDE ZONE - aassive d isse i ina t ions o f PO = 30%, cpy = 20-302, i 51 s p h a l e r i t e in t imate ly intergrown r i t h the PO.

-"WEAK ZOCE" - i n t e r v a l o f weak sulphide content, s t a r t s a t 17 C R

q t z vein, then the f o l i a t i o n gradua l ly steepens t o 80 t o SCA, then f l a t t e n s back t o 50 t o SCA, looks l i k e a small f o l d n i t h a poss ib le repeat o f the above ore sequence below the fo ld , dissem PO 2 52, cpy = 52, sph = 1%

-SEMI-MASSIVE DISSEMINATIONS AND STRINGERS - good strong cpy t o 25% as coarse c l o t s up t o 2-3 cm, PO averages 10% w i t h 1-41 sph.

-MASSIVE SULPHIDE ZONE - "net-1 ike"" tex tu re of dissem and s t r i n g e r s with 30-352 cpy, 15-201 PO and 3-51 spha ler i te .

-DISSEMINATED AND STRINGERS - weaker sulphides and s t ronger s i l i c a w i t h 8-102 cpy, 10% PO, 3-52 sph.

-MASSIVE SULPHIDE ZONE - strong PO = 402, cpy = 30-35%, 3-5% sph.

ARGILLACEOUS L IHESIONE

Upper contact w i t h su lph ide zone a t area o f g raph i t i c gouge and broken core. Well f o l i a t e d a t 40 t o SCA. Loca l l y broken, c russ-cu t t ing q tz veins = 1-2% @ t o t o SCA.

-s t rong ly g r a p h i t i c PEP t o a rg i l laceous 1s t t o 486.00, most sulphides are i n the DBP : 2% PO, t race cpy

-broken t o 486.33, t race PO

485.84 w i t h 20t recovery, then

2

3

6

30

60 11

35

55

18

75

2

t r

468 477.65 478.84 1.19

469 478.84 480.58 1,74

470 480.58 481.15 .57

471 481.15 481.91 -76

472 481,91 482.35 .44

473 482.35 483.20 .93

474 183.28 483.89 .61

475 483.89 484.69 .80

476 484.69 485.06 .80

477 485.06 485.34 .28

478 485.34 486.00 .66

479 486.00 487.00 1.00

(.001

(.OD1

,002

. 003

,014

.DO1

,009

,013

,006

,008

< . 001

<.DO1

C.01 ,043 ( . O l .03

( . O l ,116 <.01 .03

.10 1.153 (.01 .24

. 34 4.050 .01 .29

.88 9.532 .Oi ,95

.13 1.556 <.Ol .11

.85 8.494 ( - 0 1 3.42

1.19 12.127 .01 2.65

.48 4,800 .ll 1.32

1.45 8.039 1.02 4.60

-08 ,662 .01 .09

c.01 ,009 ( . O l ,O:

' HOLE # : 6-94-7

OREQUEST CONSULTANTS L T D - HOLE I : 6--11-7 FAGE II 10 o f 10

FROM T O ROCK At1 FOL l Y P E C I A

D E S C R I P T I O N k SAMPLE No. FROM T O LENGTH Au A9 Cu Fb i n SULFHIDE opst opst pct pct pct

481.06 489.26

490.46 410.76

-qtz vein, irregular contacts, -60 to SCA, has 102 "net-like" PO

-qtz f looded (50%) with 2-38 dissen py. n i t h 1% cpy

498.48 END OF HOLE

OREQUEST CONSULTANTS LTD - CIAMOND GRILL HOLE RECORD C l i e n t EETHLEHEM Page 1 1 o f 9

I Hole No. 6-94-8 Nor th ing 3279 Core S ize NQ I1 Depth D i p Azimuth Depth D i p Azimuth S t a r t e d OCT. 14, 1994 Target MINE OREBODV Proper ty GOLDSIREAk F a s t i n g lb089 Casing 10 FT.PVC PIPE 89.9 - 88 040 166.2 - 88 355 Co ip le ted O C I . 24, 1994 Comments HOLE CEMENTED Locat ion REVELSIOKE E l e v a t i o n 675 Length 503.05 242.4 - 88 192 303.4 - 86 191 Drill Co. OLYMPIC NTS 821/9W L a t i t u d e 51 38' 00" N D i p - C o l l a r -90 364.3 - 82 202 410.1 - 80 204 Logged By W . RAVEN Claim No Longi tude 118 24' 40" W Bear ing N/A 455.8 - 78 205 501.5 - 76 205 U n i t s NETERS

FROM T O ROCK ALT FOL TYPE CIA

DESCRIPI ION 1 SAMPLE No. FROM T O LENGTH Au A9 Cu Pb ln SULPHIDE ops t ops t p c t p c t p c t

86.89

86.89 151.06

86.89 151.06

91.78 93.15 94.11 94.57 96.87 97,16 98.98 100.00

104.75 104.90 105.79 106.57 106.57 107.13

107.13 108.00 109.66 110.13 112.54 114.10

115.06 115.98

116.00 118.47 122.68 124.16 124.16 124.72 125.23 125.33 125.78 126.05 130.44 130.53 131.06 132.73

OVERBURDEN - CASING

HAMILL GROUP

QUARTZITE / CHLORITE - SERICITE PHYLLIIE

F a l e g reen ish co lour , r h y t h m i c a l l y banded H i g h l y s i l i c e o u s (as it should be) with l o c a l s o f t e r sec t ions due t o s t r o n g e r s e r i c i t e and c h l o r i t e . Contains 2-31 ptygrnat ic q t z ve ins and 1% c r o s s - c u t t i n g q t 2 ve ins . L o c a l l y f r a c t u r e d and broken, l o c a l wh i te q t z ve ins . Only minor t r a c e s o f py present. UC i s a t casing, LC i s broken with gouge and rubble.

f o l i a t i o n a t 40 t o SCA.

-moderately f r a c t u r e d , s l i g h t l y vuggy, 1 x lOcn q t z v e i n - s o f t e r s e c t i o n w i t h 152 s e r i c i t e - p o r p h y r i t i c s e c t i o n with coarse c h l c l o t s drawn o u t a long f o l i a t i o n -moderately f r a c t u r e d and broken -moderately f r a c t u r e d and broken -moderately f r a c t u r e d and broken - q t z vein, b a r r e n b u t w i t h 10-153 wa l l rock fragments, UC broken, LC i r r e g u l a r

- s o f t e r s e r i c i t i c s e c t i o n -q t2 f looded as v e i n s a t 40-50 t o SCA w i t h a few b lebs o f py and PO -PORPHYRITIC / TUFFACEOUS ANDESIIE ? s t ronger s e r i c i t e and c h l o r i t e over upper h a l f o f u n i t w i t h coarser wh i te q t d f e l d s p a r g r a i n s g i v i n g a speckled appearance and pervas ive carb in n a t r i x

-1-1.h wide q t 2 v e i n a t 80 t o SCA w i t h 3-52 PO and brownish f i n e g r a i n e d minera l = b i o t i t e ?

- s o f t e r :ect ion with s t r o n g c h l and 5er - t u f f a c e o u s l o o k i n g as 112.54-114.10 -speck led wh i te carb in p u r p l i s h co loured unit - s t r o n g l y f r a c t u r e d -moderately f r a c t u r e d - s t r o n g l y f r a c t u r e d - s l i g h t l y s o f t e r with more c h l and ser

.. .,

8 . . ,

!..

OREQUEST CONSULTANTS LTD, HOLE I : 6-94-8 FAG€ I 2 o f 9


DESCRIFTION 1 SAMPLE No. FROM TO LENGTH Au A9 Cu Pb Zn SULFHlDE opst opst pc t p c t p c t

133.66 134.47 136.00 143.17 140.00 140.15 141.67 142.82

143.17 146.80

146.80 148.94 148.94 151.06

151.06 278.00

151.06 189.74

151.67 152.56 159.55 159.74

160.67 162.78

162 I 96 164 I 33 161.82 171.78

171.78 178.00

177.36 179.70 179.70 182.24 182.24 187.75

187.75 189.74

189.74 200.56

-as above -genera l l y s o f t e r with l o r e ch l and s e r w i t h l o c a l s i l i c i f i c a t i o n -s t rong ly f r a c t u r e d and broken - s t r o n g l y f r a c t u r e d and broken

FAULT ZONE - moderately t o s t r o n g l y f r a c t u r e d and broken with l o c a l gouge, s t r o n g l y s e r i c i t i c . From 145.20-146.40 i s 1 - 1 . 5 ~ ~ wide gouge- carb-py v e i n a t 85 t o SCA with up t o 15% py i n vein, l o c a l carb

-conpetent pa le g rey ish-wh i te Massive q u a r t z i t e - s t r o n g l y broken and f r a c t u r e d throughout with c l a y gouge and brecc ia

a t con tac t w i t h the under ly ing Badshot Formation

CARBONATE PACKAGE (BADSHOT AND MOHICAN FORMAT IONS)


Typical grey banded 1 inestone with 3 0 4 0 % b lack arg i l laceous mater ia l (ch l -b io -ser -g raph i te ) . Contains t r a w l % dissen py, 1-2% ptygmat i c q t z veins. Local qtz-carb tens ion gash i n f i l l i n g s . Ne l l f o l i a t e d a t 40 t o SCA, l o c a l l y warped and contorted, l o c a l s t rong S3 c r e n u l a t i o n cleavage. UC i s in gouge and rubble, LC i s g radat iona l b u t conformable a t 35 t o SCA.

- g r a p h i t i c S3 c r e n u l a t i o n cleavage a t 60 t o SCA -q tz vein, UC a t - 50, LC a t 25 t o SCA, ve in has 1-2% dissen b lebs o f

PO, t race cpy and galena -2-42 qtz-carb tens ion gash i n f i l l i n g s with 10% gashes from 161.92- 162.30, S3 c r e n u l a t i o n cleavage o f f s e t s S2 by 5-Earn

-s t rong ly 1 irny s e c t i o n -minor broken core above then f o l i a t i o n changes t o 50 then gradua l ly

steepens t o 70 then ends i n f o l d c losure and back t o 40 t o SCA -proainent S3 c r e n u l a t i o n cleavage a t 65-70 t o SCA with c r e n u l a t i o n

f o l d axes a t same angle, most o f t h i s i n t e r v a l i s q u i t e l i n y with l e s s arg i l laceous mater ia l

-usual aaount o f a rg i l laceous bands b u t w i t h 3-42 f i n e d i s s e i PO

-"Clean Grey Marble", 10% a r g i l l a c e o u s n a t e r i a l -"DBP" - more s i l i c e o u s and more arg i l laceous n a t e r i a l , l e s s carb, resembles the DBP and has 5% p t y g ~ a t i c q t z ve ins

-QUARTZITE - s i l i c i f i e d grey ish-wh i te u n i t t h a t i s e i t h e r q u a r t z i t e o r c lean grey marble t h a t has been replaced w i t h s i l i c a as cannot sc ra tch w i t h k n i f e , confornable contac ts a t 40 t o SCA

DARK BANDED PHYLLITE I ARGILLACEOUS LIMESTONE

U n i t looks a l o t more l i k e DBP than the arg i l laceous l ines tone, weakly HOLE #: 6-94-8

OREQUEST CONSULTANTS LTD. HOLE 1 : 6-94-8 PAGE 1 3 o f 9

rROM TO ROCK At1 F O I TYFE C I A

DESCRiFT ION % SAMPLE No. FROM T O LENGTH Au A9 Cu Pb 7n SULPHIDE ops t opst p c t p c t ,pct

197.26 191.65 198.22 198.32 198.49 199.15 200.10 200.20

200.56 202.33

202.33 201.05

207.05 211.56

211.56 242.53

212.94 213.90 213.90 214.56 211.93 220.01 221.14 227.99 228.24 228.41 230.13 232.06

232.06 235.79 235.79 236.89

s il iceilus. Compr i sed o f c h l o r i te-se r i c i t e (SO%), b i o t i t e (5-10%), carbonate 110-202). m a t r i x quar tz (20-30%), p t y g a a t i c quar tz ve ins ( 3 4 % ) and dissem PO (trace-15.). Well f o l i a t e d a t 35-40 t o SCA. Conformable bu t g radat iona l lupper and l o n e r contac ts a t 35 t o SCA.

-moderately f r a c t u r e d - s t r o n g l y f r a c t u r e d and broken - s t r o n g l y f r a c t u r e d and broken, 10% recovery - s t r o n g l y f r a c t u r e d and broken,

CHLORllE - SERlClTE PHYLLllE

Pa le greenish-grey co loured u n i t w i t h s t rong s e r i c i t e throughout. Looks 1 i ke the Lower Index Format ion CSP t h a t l i e s s t r u c t u r a l l y below t h e Carbonate Package. Fron 201.98-202.12 i s q t z f looded and carb r i c h w i t h broken q t r v e i n i n g g i v i n g brecc ia ted appearance.

ASSORTED FHYLL ITES

l n t e r n i x e d DBP, CSP and l imestone as t r a n s i t i o n a l change t o t y p i c a l Arg i l laceous Limestone belon. S3 c r e n u l a t i o n cleavage a t 50 t o SCA.


As descr ibed 151.06-182.24. Has 3 4 % py on h i g h angle f r a c t u r e s . Local very 1 imy sec t ions .

GREY MARBLE

Mediun gra ined c r y s t a l l i n e g a r b l e with lot b lack a r g i l l a a t e o u s bands Bands = f o l i a t i o n a t 35-40 t o SCA. Minor g r a p h i t i c s t y l o l i t e s . UC broken bu t approx 20 t o SCA, LC sharp a t 30 t o SCA. Minor i n t e r c a l a t e d a r g i l l a c e o u s 1 inestone, minor g r a p h i t i c s t y l o l i t e s i n the c lean grey marble. H i n o r d issen py and PO ( t r a w l % ) . Also has c lean wh i te marble bands up t o 1Ocm.

-moderately f r a c t u r e d a t 70-85 t o SCA - s t r o n g l y f r a c t u r e d and broken with minor muddy gouge, 80% recovery - S e r i c i t i c DBP, UC and LC a t 40 t o SCA - C h l o r i t e P h y l l i t e - C h l o r i t e F h y l l i t e -SIL ICEOUS CHLORlIE - SERlClIE PHYLLITE - s a a l l beds i n t e r c a l a t e d

w i t h marble, conformable UC and LC a t 35-40 t o SCA -ARG Ill ACEOUS LIMESTONE -SILICEOUS CSP t h a t i s s t r o n g l y f r a c t u r e d throughout, UC conformable a t 30 t o SCA b u t i s p a r t i a l l y o f f s e t by ICB a long f r a c t u r e a t 85 t o

HOLE #: 6-94-8

OREQUEST CONSULTANTS L T D - HOLE R : 6-94-8 PAGE B 4 o f 9

FROM 10 ROCK At1 F O L TYPE C I A

DESCRlFl ION % SAMPLE No. FROM TO LENGTH Au Ag Cu Fb Zn SULPH IDE opst ops t p c t p c t p c t

236.89 239.51 139.51 242.53

242.53 251.13

242.53 244.20 249.05 243.31 252,OO 256.71

257.73 261.28

261.28 273.74

261.28 264.00

261.28 164 .33 264.00 173.14

264.33 267.38 267.38 270.43 270.43 273.48 273.18 273.74

SCA, LC i s broken -CLEAN GREY MARBLE with minor p a l e green t a l c i n h i g h angle ve ins -ARGILLACEOUS LIHESTONE, Moderately t o s t r o n g l y f r a c t u r e d and broken

t o 240.60 then moderately f r a c t i i r e d along qtz-carb ve ins a t 70-85 SCA

S I L I C I F I E O CHLORITE - SERICIIE PHYLLITE

Pa le greenish-grey co lour , v a r i a b l e s i l i c i f i c a t i o n from none t o neak. Comprised o f m a t r i x quar tz (30-552), c h l o r i t e (5-20%), s e r i c i t e (10-2%), b i o t i t e ( < % I , ptygmatic q t z veins (2-51) and d i s s m PO ( t race-2%) . Local s t rong s i l i c i f i c a t i o n , l o c a l l y s t r o n g l y broken. UC sharp a t 60 t o SCA b u t no t conformable w i t h the f o l i a t i o n , LC sharp a t 30 t o SCA

-moderately t o s t r o n g l y broken and f r a c t u r e d -weakly t o moderately f r a c t u r e d -moderately t o s t r o n g l y f r a c t u r e d and broken throughout except for 255.30-256.16 which i s conpetent, i n t e r c a l a t e d Arg i l laceous Limestone from 254.41-256.27, UC a t approx 40 t o SCA, LC broken

ARGILLACEOUS LIMESTONE TO GREY MARBLE

U n i t s as p r e v i o u s l y descr ibed. Minor 1 - 5 ca. bands o f CSP. Well f o l i a t e d a t 30 t o SCA

FAULT ZONE (IN ARGILLACEOUS LIMESTONE)

H i g h l y f r a c t u r e d and broken t o shat te red rock, var ious 1 i t h o l o g i e s b u t most ly a r g i l l a c e o u s 1 iiaestone. Abundant q tz -carb t e n s i o n gash i n f ill ings (5 - 159,) throughout the zone. Var iab le recover ies from 20 - 85%. Sparse m i n e r a l i z a t i o n as dissemiaated py and PO

-Quar t2 Breccia, broken rock subsequently healed w i t h q t z rith coarse angu lar q t z fragments up t o 2 CM x 2cm in a p a l e r co loured quar tz mat r ix , minor carb present - may have o r i g i n a l l y been a do lomi te? Upper 40 CI i 5 c l a y gouge, lower contac t t 80 t o SCA, sandy with pebbles

-70% recovery - a l l a r g i l l a c e o u s l imestone, broken and f r a c t u r e d as general d e s c r i p t i o n , l o c a l c l a y gouge most ly i n t e r n i x e d with s e c t i o n s of rubb le

-85% recovery, l o n e r metre i s f a i r l y competent -251 recovery, l o o k s 1 i k e most core nas l o s t belon 267.35 m -852 recovery, s t r o n g l y f r a c t u r e d and broken -85% recovery, s t r o n g l y f r a c t u r e d and broken

HOLE # : G-94-8

O R E Q U E S T C O N S U L T A N T S L T D , HOLE II : 6-94-9 PAFE 11 5 o f 9

FROM TO ROCK ALT FOL TYPE C/A

DESCR IPT ION 2 SAMPLE No. FROM TO LENGTH Au A9 Cu Fb i n SULPHIDE ops t ops t p c t p c t p c t

273.74 278.00 ARGILLACEOUS LIMESTONE (SEMI FAULTED)

As p rev ious ly descr ibed. \ i n o r c lean grey marble w i t h g r a p h i t i c s t y l o l i t e s . B tz -carb tens ion gash i n f i l l i n g s = 5 - 101. F o l i a t i o n a t 50 - 70 t a SCA

273.74 216.52 276.52 278.00

278.00 501.05

278.00 251.77

278.00 279.57

219.57 280.38 280.38 282,62 282.62 285.67 285.67 288.72

288.72 291.77

291.77 323.43

291.77 294.49 294-49 303.83

295.90 296 I 23 296.23

298.85 299.00 300.70 300.91 302.31 302.97 303.10 303.83

303.83 310.29

-95% re rovery -95% recovery

LOUER INDEX FORMAT ION

F AULT ZONE (IN CHLORITE -SER 1C HE-6101 1lE PHYLL 1lE )

H igh ly f r a c t u r e d and broken t o shat te red rock, upper contac t w i t h 1 ilaestone i s c l a y - s e r i c i t e gouge, lower contac t i s gradat iona l change t o l e s s broken rock, no t an abrupt change.

-greenish-grey c l a y gouge, 40% recovery, UC sharp a t 10 t o SCA, LC sharp a t 70 t o SCA

- g r a p h i t i c , b r e c c i a t e d 1 ooking -102 recovery, most ly rock ch ips and gouge -358 recovery, f r a c t u r e d rock ch ips , 21 py -65% recovery, f r a c t u r e d rock ch ips , broken q t2 a t 287.19 w i t h 5%

d issen ina ted py -80% recovery, s t r o n g l y f r a c t u r e d and broken

S I L I C I F I E D SERICITE - CHLORIIE P H V L L I I E

As descr ibed 242.53 - 257.73 1. Moderately f r a c t u r e d b u t no t broken l i k e f a u l t iones. Hore s e r i c i t e than c h l o r i t e r e s u l t i n g i n p a l e r grey co lour as opposed t o t h e greener c h l r i c h e r u n i t . UC i s g radat iona l as rock s t i l l q u i t e f rac tu red , 1C sharp a t 30 t o SCA

-pale grey co lour , f o l i a t i o n a t SO t o SCA -genera l l y s t r o n g l y s i l i c i f i e d with v a r i a b l e greenish-grey t o purp l ish-brown c o l o u r , l o c a l s o f t e r sec t ions over s h o r t i n t e r v a l s

-moderately t o s t r o n g l y f r a c t u r e d -be lo r t h i s p o i n t i s approx. 20 cm of rounded q t2 pebbles 2 cave? - s t r o n g l y f r a c t u r e d and broken -s t rong ly f r a c t u r e d and broken - s t r o n g l y f r a c t u r e d and broken -40 - 501 wh i te q t z f l o o d i n g genera l l y p a r a l l e l t o f o l i a t i o n a t

- s i l i c e o u s bu t can be scratched, v a r i a b l e ser and c h l , genera l l y 45 - 50 t o SCA

f o l i a t e d a t 50 t o SCA, minor PO and cpy around a t 2 v e i n a t 308.80 - 308.87

HOLE # : 6-94-8

OREQUEST CONSULTANTS LTD- HOLE II : 6-94-8 PAGE II 6 o f 9

:POK 10 ROCK At1 FOL TYPE C I A

RESCRIPT ION % SAMPLE No. FROM TO LENFTH Au A9 Cu Pb i n SULPHIGE opst ops t p c t p c t p c t

310.21 319.00

316.16 316.50

3!8.17 31S.33 318.93 319.00 319.00 323.43 320.14 320.31

320.40 320.55 321 .ll 322.11

323.43 473.62

323.43 323.46

323.48 324.15 314.15 327 -41

330.14 330.53 331.77 332.10 335.81 335.85 336.11 337.34 ?38.@0 331.46 335.00 340.00 340.83 351.14

328.35 3 2 8 . ~ 9

343.60 343.70 348.17 348.64

351.24 356. E l 357 .b2 357.74 359.38 364.64 365.62

368.40 373.10 378.42 381 -38

- s i l i c i f i e d t o c l o s e t o contac t w i t h DBP below, weakly t o Moderately f r a c t u r e d throughout, l o c a l l y laminated a t 40 to SCA

-q t2 ve in , UC broken, LC a t 55 t o SCA, v e i n has 1% py, 12 PO and 1% g r a p h i t i c s t y l o l i t e s

-q t2 v e i n w i t h 5% c l o t t y po and 1 - 2'6 cpy and py intergrown - q t 2 re in as above - s i l i c e o u s b u t can be scra tched - q t z ve in o r p t y g i a t i c c l o t as doesn' t penet ra te completely through core, 3 - 4 % PO most ly around margins

-as above though more o f a t r u e v e i n - s i l i c e o u s with c o n t o r t e d f o l i a t i o n f r o i 40-85 t o SCA = s f l a l l S2 f o l d

DARK BANGED PHVLL I T E

Var iab le g raph i te , c h l o r i t e , b i o t i t e , quar tz and carbonate conten t , e s p e c i a l l y i n upper p o r t i o n . UC sharp a t 30 t o SCA, LC i s broken b u t approx 50 t o SCA. Ub iqu i tous pa ( t r - 58) as f i n e d i s s e s i n a t i o n s and l a y e r p a r a l l e l b lebs

-competent core r i g h t a t con tac t then broken and f r a c t u r e d below l i k e weak f a u l t o r shear zone

- s t r o n g l y g r a p h i t i c and broken and f r a c t u r e d w i t h l o c a l gouge -moderately f r a c t u r e d with 5 - 81 q t z +/- carb tens ion gash i n f i l l i n g s -vuggy q tz -carb v e i n 7 a 1 r i d e a t 80 t o SCA -moderately broken and f r a c t u r e d -broken with g r a p h i t i c gouge a t 70 t o SCA w g g y q t z - c a r b v e i n a t 50 t o SCR - f o l d ? f o l i a t i o n changes f r o i 40 - 85 t o SCA -as above with S3 a t 65 t o SCA -weakly dis i -upted l o o k i n g w i t h 1 - 4% qtz-carb tens ion gash i n f i l l i n g s - d i s r u p t e d i n t e r v a l with 3 - 8% qtz -carb tens ion gash i n f i l l i n g s ,

l o c a l l y q u i t e broken w i t h s t r o n g g r a p h i t e and l o c a l g r a p h i t i c gouge, l o c a l S? f o l d s and S3 c r e n u l a t i o n cleavage d i s r u p t f o l i a t i o n a t v a r i o u s a t t i t u d e s , 2 - 4 % d issen ina ted PO

- g r a p h i t i c gouge and rock c h i p s - b r e c c i a t e d q t z v e i n with 10 - 12% coarse PO c l o t s , moderately magnetic

-below the d i s r u p t e d zones f o l i a t i o n a t 25 - 30 t o SCA -minor S? f o l d s t r e t c h e s f o l i a t i o n , n i n o r S3 a t 50 -minor S2 f o l d s t r e t c h e s f o l i a t i o n , minor S3 a t 50 -2 b r e c c i a t e d l o o k i n g q t 2 +I- carb ve ins 1 - 1.5 CI wide a t 80 t o SCA

w i t h t r a c e PO -3 - 5% q t z - c a r b t e n s i o n gash i n f i l l i n g s , very a i n o r gouge - s t r o n g S3 c r e n u l a t i o n c leavage and f o l d i n g a t 60 - 70 t o SCA with l o c a l i z e d PO enrichment t o 5t, S3 weaken: a t end o f i n t e r v a l

HOLE #: 6-94-8

OREQUEST CONSULTANTS L T D - HOLE 1 : 6-94-8 PAGE II 7 o f 9

F R O n TO ROCK At1 FOL D E S C X I F I I D N % SAMFLE No. FROM TO LENGTH Au A9 Cu Pb Zn TYPE C I A SULPHIDE ops t opst p c t p c t p c t

381.38 382.16

382.16 383.72 384.34 388.44

400.35 401.60 401.78 410.67 410.67 445.00 419.07 419.32 119.32 419.70 420.65 420.74 424.81 425.60

433.00 134.81 135.14

435.14 135.46 438.49 439.12 441.94 442.10

444.79 145.00 446.48

446.48 456.66 456.86

470.28 471.13

- q t z v e i n m i l k y wh i te co lour , bar ren look ing , UC approx 60 b u t broken, LC a t 20 t o SCA, t r a c e o f PO and py i n h a i r l i n e s t r i n g e r s

-5 - 8% qtz -carb t e n s i o n gash i n f i l l ings -3 - 5% q tz -carb t e n s i o n gash i n f i l l i n g s , a t 386.28 - 386.35 i s q t z ve in , and from 368.20 t o 388.44 i s g r a p h i t i c gouge and q tz -carb r e i n , the gouge i s a t approx 65 t o SCA

-9 f o l d i n c e n t r e o f i n t e r v a l , S3 a t 65 - 70 t o SCA - s i l i c i f i e d and we l l f o l i a t e d a t 20 t o SCA -weak s i l i c i f i c a t i o n , can b a r e l y scratch, more carb - s t r o n g l y broken w i t h g r a p h i t i c gouge a t 50 t o SCA -moderately f r a c t u r e d - q t z v e i n i n g with a f e n coarse c l o t s o f PO -wavy f o l i a t i o n , S3 a t 45, S2 a t 65 - f o l i a t i o n a t 15 - 20 t o SCA - q t z vein, UC a t 65, LC i s i r r e g u l a r , v e i n has 2 - 3% f i n e

disseminated and blebby pa around Margins -50% q t z f l o o d i n g -moderately f r a c t u r e d -moderately f r a c t u r e d -below t h i s p o i n t i s 30 cm o f cave - s i l i c i f i e d , f o l i a t i o n a l i t t l e steeper a t 25 t o SCA, very b lack with

5 - 62 disseminated PO -below t h i s p o i n t as 410.67 - 445.00 - g r a p h i t i c gouge with q tz -carb tens ion gash i n f i l l ings, on ly l o c a l gouge

-moderately t o s t r o n g l y f r a c t u r e d with l o c a l g r a p h i t i c gouge

473.62 480.51 GARNET ZONE (GRAPHITIC AND SILICIFIED DARK BANDED PHYLLITC)

472.62 474.20 474.20 474.57 474.57 477.93

477.93 479.53

479.53 480.59

Garnet zone i n g r a p h i t i c DBP t h a t i s v a r i a b l y s i l i c i f i e d , broken and f r a c t u r e d . Garnets range from 2 - 3% t o l o c a l “beds” up t o 6 mm wide t h a t are 50 - 60% garnet. Size i s from 1 - 2 RM t o allnost 1 cm x 1 cm. Zone looks contor ted throughout and i s l o c a l l y s t r o n g l y f r a c t u r e d and broken with 3 - 15Z qt2 +/- carb tens ion gash i n f i l l i n g s UC i s broken b u t approx 50 t o SCR, I C a t 40 t o SCR, low su lph ide conten t w i t h t r a c e - 2% disseminated PO

- s t r o n g l y broken and f r a c t u r e d w i t h l o c a l gouge -contor ted w i t h 10 - 152 qtz -carb tens ion gash i n f i l l i n g s - g e n e r a l l y f a i r l y competent, w e l l f o l i a t e d a t 20 - 30% t o SCA,

l o c a l garnet beds a t 40 t o SCA - s t r o n g l y broken and f r a c t u r e d , b recc ia ted l o o k i n g with 159. qtz -carb

tens ion gash i n f i l l i n g s , looks l i k e p a r t i a l l y healed f a u l t gouge - f a i r l y competent rock b u t raoderately t o s t r o n g l y f ract iured

HOLE #: 6-94-8

PAGE 1 8 o f . 9 OREQUEST CONSULTANTS L T D - HOLE I : 6-94-8

FROM T O ROCK At1 FOL DESCRIPTION % SAMPLE No. FROM TO LENGTH Au A9 Cu Pb l n TYPC C I A SULPHIDE opst ops t p c t p c t p c t

480.59 483,12

480.74 481.05 482.06

482.86 483.00

483.17 483.54

483.54 488,07

483.54 484.76 484.76 185.16

485.16 486.20 486.20 487.00 487.00 488.07 HUDSZ s i l

488.07 493.21

488.07 488.57 DSSZ s i l 50

488.57 489.54 SllIHS2 s i l

GARNET ZONE (SILICIFIED GREY PHYLLITE)

S t rong ly g a r n e t i f e r o u s averaging 15%, ranging up t o 40'6 p i n k garnets. Ub iqu i tous PO as disseminated t o b lebs from 2 - 10b t h a t i s weakly t o very l o c a l l y moderately magnetic. Cherty bands 5 - 15%. Wispy ye l low ish-green minera l , no t s i r e what i t is . UC a t 40, LC a t 35 t o SCA

- rubb le and rock ch ips -minor f o l d , a x i s a t approx 40 t o SCA, upper l i m b appears t runcated but a t approx 30, lower l i n b a t 60

-broken and f r a c t u r e d

GREY-GREEN SlLiLClFlED PHYLLITE (MINOR GARNETS)

ARGILLACEOUS LIMESTONE i HANGING WALL DISSEMINATED SULPHIDE ZONE

Grey-white c o l o u r i n upper p o r t i o n w i t h minor grey-green p h y l l i t e and garnet zone then grad ing t o a w h i t e and reddish brown s i l i c i f i e d l imestone. L i k e l y represents s i l i c i f i c a t i o n o f lower p o r t i o n o f 1 imestone from the u n d e r l y i n g semi-massive t o massive su lph ide zone. Th is would be equ iva len t t o t h e Hanging Wall Disseninated Zone with sparse suphides, UC broken, 1.C i s g radat iona l i n t o s t r o n g e r su lph ide zone.

- t y p i c a l a r g i l l a c e o u s l imestone, minor f o l d a x i s a t 65 t o SCA -9arnet i fe rous DBP, UC a t 35, LC a t 45 with 35% s t r o n g l y nagnet ic

banded PO from 484.94 - 485.16 -calcareous grey-green p h y l l i t e - s i l i c i f i e d 1 iiaestone, tr - 12 f i n e disseminated pa -as above, 1 - 2% PO, t race cpy

SEMI-MASSIVE T O MASSIVE SULPHIDE ZONE

A c t u a l l y 2 zones o f massive su lph ides separated by a su lph ide poor i n t e r v a l represent ing the core o f a f o l d w i t h the su lph ide r i c h i n t e r v a l s represent ing the 1 imbs. Zone i s s i l i c e o u s w i t h 10 - 25% grey m a t r i x quartz and 5 - 10% w h i t e quar tz

-DISSEMINATED AND SULPHIDE STRINGERS - sharp upper contac t a t 50 which i s o r i e n t a t i o n o f s t r i n g e r s o f cpy and PO, zone averages 6 - 8% PO, 8 - 12% cpy and 1 - 3% sph

-SEMI -MASSIVE T O MASSIVE SULPHIDE ZONE, semi-Passive d issen ina t ions , c l o t s and s t r i n g e r s , the lower 23 cm i s t r u l y massive averaging 65 - 701 su lph ides , i n t e r v a l averages 20 - 25% cpy and 5% sph locked up d5 "reddish" PO

I

2 480 487.00 488.07 1,07 <.001 .02 ,028 -01 .06

20 481 188.07 488.57 .50 ,005 .25 4.588 <.Ol .39

55 482 488.57 489.54 -97 ,008 -65 9.363 -01 .65

HOLE #: 6-94-8

OREQUEST CONSULTANTS LTD.

- . HOLE 1 : 6-94-8 PAGE ? 9 of 9

FROM 10 ROCK A t 1 FOL TYPE CIA

D E S C R I P I ION % SAMPLE NO. FROM TO LENGTH A i l Ag Cu Fb z n SULPH I D E opst opst . pct pct pct

489.54 489.94 BSSZ s i 1 , s e r - S I R I N L E R S AND DISSEMINATED (FOLD CORE), s t a r t of weaker sulphide

489.94 490.98 BC s e r -BARREN CORE - s i l i c e o u s but only t r a c e - 21 conbined PO and cpy,

490.98 192.02 B C i D S Z s i 1 , s e r

f o l d core , averages 5% PO, 5% cpy, t r a c e sph

15% b i o t i t e , Moderate s e r i c i t e -STRINGERS AND DISSEMINATED - FOLD CORE, lower por t ion of fo ld core

10 483 489.54 489.94 .40

1 484 489.94 490.98 1.04

8 485 490.98 492.02 1.04

492.02 493.22 MSZ

4’33.24 497.00

493.22 494.02 FWDSSZ 494.02 494.45 FWDSSZ 494.45 4’35.00 FWOSSZ

495.00 496.04 FWDSSZ

496.50 496.68

497 I 00 503.05

with s t r o n g e r su lphides appearing, 809, recovery but c a n ’ t see where core was l o s t , averages 5 - 6% PO, 3-52 cpy, t race sph, s t rong sa lphides over 6 cm near q tz vein

-MASSIVE SULPHIDE ZONE - upper 42 CI averages 40% sulphide , lower 78 cm a s t r u l y massive with 70 - 75% sulphides , UC and L C a r e sharp , averages 35% PO, 20 - 25% cpy and 10% sph, very s t rong :ph in in te rva l

s i l

FOOTWALL D ISSEMINATED AND STRINGERS SULPHIDE ZONE

L o o k s 1 ike s i l iceou: dark banded phyll i t e with ninor cherty bands and v a r i a b l e su lphide conten t . UC s e i i sharp a t 10 - 15 t o SCA based on su lphide conten t , L C sharp a t 20 t o SCA

-moderate PO t o 25%, 3% cpy, 1% sph -weaker su lphides , 4‘6 PO, 1% cpy -10 - 15% PO, 3 - 5% cpy with one massive PO c l o t approx 10 cm x 2 C M t h a t wraps around c o r e , 2 cm o f gouge

-5% PO, 1% cpy, 60% recovery a s c o r e dropped out o f tube, had t o pul l rods t o recover

-moderately broken and f r a c t u r e d

ARGILLACEOUS L IMESIOIJE

s i l s i l sil

s i l

.

29 481 493.22 494.02 .80 5 488 494.02 494.45 .43

16 489 494.45 495.00 .55

5 490 495.00 496.04 1.04

,002

<.001

,004

,007

,001 <.001

,001

,002

.12 1.810

.02 ,202

.27 . 2.751

-85 6.005

.08 1.465 -01 ,325 .04 1.472

c .01 .180

.03

.01

-10

-78

I 04 -01 * 01

.01

* 59

I 40

1.10

4.52

.27 <,ill

-29

<.Ol

503.05

Well f o l i a t e d a t 15 t o 20 to SCA, l o c a l l y broken and f rac tured

END OF HOLE

OREQUEST CONSULTANTS LTD . DIAIOND DRILL HOLE RECORD Client BETHLEHEH Page I 1 o f 10

Hole No 6-94-9 Northing 1522 ro rp Size NQ J I Depth Dip Az i iu th Depth Dip Azimuth Started OCT. 24, 1994 Target MINE OREBODY Property 601 USTREAM Easting 16187 razing 10’ PVC PIPE 43.0 - 88 340 73.5 - 88 149 Completed NOV, 4 , 1994 Coinents HOLE CEMENTED Locat ion REVELSTOKE Elevation 710 Length 639.02 134.4 - $2 191 195,4 - 72 190 Drill Co, OLYHPIC N7S 8 7 W U Lati tude 51 78’ 00” N Dip-Collar -81 256.4 - 67 206 317.4 - 65 710 Logged By W. RRVFN

Units HETERS Claia No longitude 118 24’ 40” W Bearing 020 370.4 - 64 208 4?9.3 - 62 214 500.3 - 61 226 546.0 - 60 218 591,8 - 59 227 637.5 - 58 223

FROM i 0 ROCK ALT FOL iYPE C I A

DESCRIPTION t SAHPLE No, FROH TO LENSTH Au Ag Crr Pb Zn SULPHIDE opst opst pct pct pct

36.58 OVERBURDEN

36.58 333,OO HAHILL GROUP

36.58 333,OO INTERCALATED QUARTZITE / CHLORITE - SFRICITF PHYLLITE

36-58 43,73

43.73 48,09 48,09 49,60 49,60 50,91 50.91 66.20

51.40 53.00 54.57 56.58 61.69 61.89 63,11 64-65 64,% 65.13 65.13 65.59 66.20 78.14

67,02 67.20 68.70 68.80

Gradational changes from so f te r chl-spr r i c h rock t o hard rhythaat ica l ly bedded quar tz i te , Both are green, contacts are hard t o d is t inguish though ocrasional ly the quar tz i te i s greyish-white. Local coarspr porphyr i t ic sect ions = tuffaceous andesite ? l oca l l y broken and fractured and fau l ted rith gouge, generally uoderately fractured, Fo l i a t i on / bedding at 40 t o STA. Hinor t rams o f py, LC a b i t broken but confonable at 20 t o STA

-black sperkled u n i t = CSP/TUFFACEOUS ANDESITE rith s l i g h t l y porphyr i t ic hornblende crystals, grpy quar tz i te fron 41,80-42,18, porphyr i t ic r h i t e feldspar ? crysta ls f r o r 42,34-43,21

-pale greyish-green QUARTZITE -CSP, loca l white feldspar crysta ls -pale greenish-grey QUARTZITE -largely CSP with local QUARTZITE that i z hard to dist inguish f ron the CSP, there i s conziderable fau l t i ng throughout the w t i o n with areas of gouge, rubblp and rock chips

-mostly gouge, rubble and angiilar rock chips -mostly gouge, rubblp and angular rock th ipz -aostly gouge, rubble and angular rock chips -mostly gouge, rubble and angular rock rh ips -qtz vein -gouge zone a t 40 to STA -TSP with local q i ra r t z i t i c vc t i onz , not as strongly broken or

-strongly broken wi th gouge -qt2 vein, UC at 10, LT broken

fractured as 50.91-66,20 but l oca l l y fractured

OREQUEST CONSULTANTS LTD, HOLE I : t-94-9 PAGE II 2 of 10

FROR T O ROCK ALT FOL TYPE C I A

DESCRIPTION I SAMPLE No, FROd TO LENGTH AIJ Ag CIA Pb Zn SULPHIDE opst opst pct pct pct

76.00 77.31 77.31 78.14 78,14 S1,40 81.40 87.76 87.76 90.17 90.17 9?,24 92.24 92.99 92.99 96.50 95.60 97,70 97.70 98,65 98,65 100,46

100-46 103,22

103,22 104,73 104,73 106,65 108.65 110.04 110,04 114.00

114,OO 118,35 118,35 122.23 122.23 123.07 113.07 127.13 127.13 118.77

128.77 130.32 130.32 138.34 138.34 142,21 142,21 149.73 149.73 153.41

151.41 159.68

159 I 68 16?,82

163.87 183,55

163,82 164.75 170.34 172.87 180.10 181.77 183.55 185.33

185.33 1R8,47

-QUARTZITE -TUFFACEOUS ANDESITF -SCP, ioderate se r i c i t e -QUARTZITE, pale green colour, l o c a l l y broken -LIMY section wi th in quartzite, UC and LC at 40 to SCA -QUARTZIT€ -ARSILLACEOUS LIHESTONE -CSP -QUARTZ I l E -CSP -LIMY sect ion -SERICITE - CHLORITE PHYLLITE (SCPj, folded section (S2) with 2 folds sole very strong s e r i c i t e i n t h i s interval gives a d is t i nc t sheen t o the core, contains 2 qtz veins f r o i 100,71-100.95 and 101,94-102.31 both with trace-2t disseu PO

-QUARTZITE -CSP -QUARTZITE -CSP, strongly broken and fractured frow 110.31-112,lO with qt7 vein

-QUARTZITE -CSP -QUARTZITE -CSP, ioderately fract i i red frow 124.83-125.57 -QUARTZITE, n i t h qtz vein from 127.29-127.35 with 1OI py r i t e and 41 pyrrhot i t e around vein margins

-CSP, strongly broken and fractured fro, 129,68-130,32 -0UARTZITE

fro, 111-62-112,lO

-CSP and SCP, strongly broken and fractured f ro1 138,34-139,33 -QUARTZITE -PORPHYRITIC ANDESITE, contains porphyr i t ic white carbonate blebs and Minor banded carb, UT at 30, LC a t approx 10 t o SCA

-QUARTZITE and CSP, nozt ly q u a r t i i t e but l oca l section< resenble TSP, 10% py on fracture fro4 154.32-154,42

-ARFILLACEOUS LIHESTONE - local interbed o f l i l es tone wi th in the s i l iceous package, UT sharp a t 30 t o STA, LT sharp at 35 t o STA, f i ne graphite f i l l e d f ractures

-QUARTZITE, p re t t y good quar tz i te to 173,30 then a l i t t l e sof ter = pa r t i a l CSP

-noderatcly fractured and broken -noderateiy fractured and broken -CSP wi th in the quar tz i te -AR6ILLACEOUS LIMESTONE, a2 159,68-16?.8?, UC sharp at 20, L I sharp at 35 t o SCA with graphite a t contact and z l i g h t l y broken a t contact

-QUARTZITE, strongly fracturpd and broken t o 183.80 then ioderately fractured and broken t o 184,73 trrffaceous andesite f ro# lR4,87-187,68

HOLE #: G-94-9

OREQUEST CONSULTANTS LTD. HOLE f C-94-9 PAGE I 3 of 10

FROll i o ROCK ALT FOL DESCRIPTION t SAllPLF No, FROH i0 LENGTH AIJ Ag CU Ph Zn TYPF CIA SULPHIDE Op5t Opzt pCt pCt pCt

188.47 191 I 31 -CSP and TIIFFATEOUS ANDESITE 191 -31 191 .% -QUARTZITE, greyish-white, f i ne grained, dense 191.98 195,73 -CSP, roderatply fractured and broken froa 194.00-195,73 195.73 196,99

197.99 198,71 -CSP, strongly broken f ron 198,40-148,93 including approxiaately

198.17 201.13 -QUARTZITE 201.13 204.26 - intercalated CSP and QUARTZITF and TUFFArEOUS ANDESITE, l oca l l y

204.26 212,97 -QUARTZITE, l o c a l l y f ractured 212.97 215.91 215.97 223.17 -QUARTZITE, ioderately t o l oca l l y ztrongly fractured from 215,97-

223,17 125.22 -CSP

-ARGILLACEOUS 1 IIIESTONE, UT and LC a t 20 t o STA 196.99 197,98 -QUART? I T E

20ci o f broken qtz vein t o 198.60

broken, sof ter and s e r i t i t i c f r o i 203.62-204,13

-PORPHYRITIC / TUFFACEOUS MOESITE, UC sharp a t 20, LC approx 70 STA

220,45, rontainq 8-10? py along fracturez t o 216,68

225.22 234.80

234.80 136.13

236.13 237,82 237.82 239,80 239.80 275,OI

242,61 243.65 245.48 246.42 250.48 251.15 161.28 262,OO 262.63 262.73 ?6?.49 265.88 770.43 270 .~1

275.01 278.51 278.52 283.81 283.81 285,86 285.86 795.90

309,34 309.52 318.90 319.15

-QUARTZITE, l oca l l y broken a t 225,43-225.76, 230,00-230.10, and

-CSP / TUFFACEOUS ANDESITF, UC a b i t broken at approx 30 to SCA, LC broken over lower 20ca

-QUARTZITE, qtrongly broken and fractured to end o f interval

-QUARTZITE, with ainor sections o f CSP/TUFFACEOUS ANOFSITE < 1n i n length, l oca l l y fractured and broken

-fracture I qtz-carb vein wi th 2-42 pa, 511 wide at 85 to SCA -TUFFACEOUS ANDESITE, so f te r and s l i g h t l y broken -noderately fractured -5D-60% qtz flooded as veins at 10-15 t o SCA, minor traces o f PO -rubble and rock chips -moderately fractured and broken -strongly fractured and broken, i o s t l y just rock chips with se r i c i t e on fractures

-CSP, gradational contacts, ainor gouge at 275,30 -QUARTZITE, strongly fractured and broken from 282.62-283.14 -CSP -QUARTZITE, r i n o r i n t m a l a t e d CSP with one d i s t i nc t bed 4 t 290.97- 291,64, qtz vein / f looding with 3-41 PO blebs, trace cpy f r o r 295,50-295.70

-6SP with FAULT SOUSE f ro4 295.90-296,82, UT a b i t i r regular LC sharp at 30 t o SCA

-QUART7ITE, 1-31 cross cu t t i ng qtz-[arb veins, l oca l l y fractured and broken over 3-1Oca intervals, minor qtz veins < 5 c i with 1-44 PO, internixed purp l ish colour over lower ha l f and f i ne l y l a ~ i n a t e d a t 20 t o SCA

.-qtz vein, UC and 1.C approx 20 to SCA, minor po -strongly fracturpd and broken, mostly a broken q t z vein with 1-31 po and py

233,10-233,14

-TUFFACEOUS ANDESITE

. . .- . HOLE #: * Gr94-9

OREQUEST CONSULTANTS L T D - HOLE B : 6-94-9 PAGE 1 4 of 10

FROK i o ROCK ALT FOL TVPF CIA

DESCRIPTION % SAMPLE No, FROW TO LENGTH A u A9 C u Pb Zn SULPH IDE opst opst pct pct pct

320.57 321.35 121,35 3??,68 3?2,68 324.11 374,Il 333.00

333.00 346,65 ?34,45 334.16

319.51 339 I 14

339,14 339,82 339.82 340,02

342.35 342,88

345,22 345.55 348.61 349.69

>54.64 159.63

159.63 366,59

-6SP with barren qt2 vein f rou 320.81-321,OO -QUARTZITF -CSP / TUFFACEOUS ANOESITE -QUARTZITE, minor vuggy sections from weathered out carb veins, moderatpl y fractured from 328 I 61-32!?, 03, t rate-32 qtz-rarb tension gash i n f i l l ings

CARBONATE PACKAGE (BAIISHOT AND HOHICAN FORMATIONS)

ARKILLACEOUS LIMESTONE

Typical grey t o black and white banded liaestone. Coiprised o f carb (40-651) with argi l laceous bands o f chl-bio-ser-graphite i30-451), ptygnatic qtz veins (trace-31) and f i ne dissem py and PO (trace-28) most evident on fractures, Well f o l i a ted at 20 to SCA, UC i s a b i t broken over 2cm but appears conforiable at 20 to SCA, LC sharp a t 20.

-weak qtz-carb tension gash i n f i l l in95 -S3 rrenrr lat ion cleavage at approx 45 t o SCA and local S2 fo lds with axes a t 20 t o SCA

-qt2 w i n , i r regular UC, broken LC, 3-5% coarse blebs o f PO, vein i s general ly conforuable

-broken and fractured with qt2 chips -qt2 vein at approx 60 t o SCA with 81 cnarse PO blebs and trace rpy, w i n s p l i t i n two and o f f se t by 6cu along fracture at 85 t o SCA

-qt2 vein, UC a t 55, L C a t 10-15 t o SCA - i r reg i i lar along a graphi t ic suture, minor traces o f PO

-strongly broken and fractured with ninor gouge at approx 50 to SCA -Moderately fractured and broken

DARK BANDFD PHVLLITF

Si l i reous in terva l wi th in the carbonate package that has nor? argi l laceous material and s i l ica at the expense of rarbonate, Looks l i k e DBP rather than Argi l laceous Li iestone, UC sharp at 20, LC sharp at 10 t o SCA along a Rni wide qtz vein with 3-41 PO blebs

AR6ILLACEOUS L IHFSTONE

As previously dev r ibed> 333,OO-354,64, I1C at 10 along qt2 vein. L C i r r ~ g u l a r at approx 20 t o SCA. Qt2-rarb tension gash i n f i l l i n g s (2-42) throughout u n i t .

-moderately fractured, minor gouge -as above

HOLE #: 6-94-9

OREQUEST CONSULTANTS LTD, HOLE II : 6-94-9 PAGE II 5 of 10

FRO14 T O ROCK All FOL TYPF riA

DFSCRIPTION % SAllPlE No. FRO8 T O LENGTH A u Ag Cu Pb 7n SUI PHlDF opst opst pct pct pc t

365.16 265.27 366, no 3 ~ ~ 3 6

366 I 59 766,50

368,50 171.00

371.00 375.46

275.46 176.95

376.95 381.70

351.20 385.07

785.07 390,58

390 I 58 394 I 92

404,65 406.74

-qt2 vein, 1% d i w n and blebby po - lodera tp ly f r a c t u r p d w i t h goiige

UEAN GREY WARBLE

Has < 102 arg i l laceouz Pater ia l , 3% g r a p h i t i c s t y l o l i t t s , bedded a t 20 t o SCA. UC i r r e g u l a r a t approx 20, LC sharp a t 20 t o SCA,

SILICIFIED CHLORITE - CERICITE PHYLLITE

Conformable contac ts f i n e l y lan ina ted a t 20 t o STA.

AR6ILLACEOUS 1 IWESTONE

SILICIFIED CHLORITE - SERICITE PHYI.LITE

TLFAN GREY MARBlE (pi i r i n h i t e sec t ions below 380,OO)

SILICIFIED THLORITF - SERICITE PHYLLITE

One qt? ve in a t 383,94 184.07 with 1% PO blebs

ARGl l LACFOUS 1 IWESTONE / GREY HARRLE

Several w a l l f o l d s over 20-4Orm core l m g t h s = f o l d ravp l rng th and S? crenrrlat ion r leavage at approx 60 t o SCA,

INIERCALATED HARM E AND rHlORITF PHYLLlTE

Comprispd o f grey narb ie (80%) and local bands o f green p h y l l i t e (202) confor iab le w i t h f o i irft Ion a t 20 t o SEA,

LOWER INDFX FORNATION

SII KIFIEO CHLORITE V R I C I T E PHYLLITE

Strongly s i l i c i f i e d m t , Comprised o f f i n e mat r ix q tz (45-55t) , r h l o r i t e (2011, w i r i t e (10-15?), p t y g i a t i r q tz veins i l-4tj, c r o w c u t t i n g qt2 +/- r a r h ve ins (lt) , b i o t i t e (5%) and disseminated PO

(trare-??). F o l i a t e d a t 15-?O t o SCA.

SILICIFIED DMOWITE

Dul l greyish-white r o l o i r r , Extremely hard - cannot s r r a t r h w i th f i k , looks l i k e q t z but has f a i n t laminat ion< = bedded mater ia l ;It 10-15 t o SCA. H inor vlrgqy core s u r f a c t z ,

HOLE # : 6-94-9

OREQUEST CONSULTANTS LTD.

b

HOLE I : t -94-9 PAR I 6 of 10

F R M TO ROCK At1 FOL DESCR IPT ION R SAMPLE NO. FRO1 T O LFNGTH All A9 Crr Pb 7n CIA SULPHIBF opst opst pc t pc t p r t TYPE

406,79 4!5,31 SILICIFIED TAN BIOTITE - SFRICITE +I- CHLORIiF PHYLLITE

B a s i c a l l y s i i i l a r t o 394,92-404.65 but has l e s s s i l ica, 52 c h l o r i t e , 15% tan b i o t i t e and 5% carbonate bands, S t i l l r i l i t i f i e d , Well f o l i a t e d a t 15-20 t o SCA . .

420.99 422,07

424.69 426.07

426,07 476.00 .

426.07 434,98

428.55 429,09 430.88 431.21

436.00 471+85

437.85 4 x 1 5 452.21 452.63 457.44 457,78

462,89 464.71 465.55 468.60

471.00 471,?4 468.60 469,6n

"DARK BANDED PHYLLITE SEOUENCE"

ARSILLACEOUS LIHESTONE

Variable r o i p o s i t i o n cons is t ing o f rarbonatp 160-75t), a rg i l la teor rz i a t e r i a l (chl-ser-bio-graphite - 35-1013, p t y g i a t i t qt2 veins ( t r - % ) , Me11 banded / f o l ia ted a t I0 to SCA.

-2-48 q tz - ra rb tens ion gash i n f i l l ings, i i n o r grey i a r h l e sec t ions with 31 g r a p h i t i c s t y l o l i t e s

-grey i a r b l e


Typical dark banded p h y l l i t e r o i p r i s p d o f biotite-rhl-ser-qraphite bands (40-6011, a l t e r n a t i n g with white carb (20-35t3, i a t r i x q tz (10-201), p t y g i a t i t qtz veins (52) and f i n e d i s ~ e 8 PO (1-59), F o l i a t e d a t 15 t o SCA,

-p ro i inent S3 f o l d i n g and t r e n u l a t i o n r leavage well developed at 50-60 t o SCA

-grey marble -qtz vein, 1-22 PO c l o t s Mostly a t ripper t o n t a r t

CALCARFOUS DARK BAN[iED PHYLLITE / AR6ILLACEOUS LlHESiONE

S i i i l a r t o above u n i t (426.07-436.00) but carbonate ron ten t i s n o t i c a b l y h igher (40-602), otherwise w e n t i a l l y the m e iunit ,

-s t rong ly broken and f rac tu red - f rac tu red qt7 vein, c l n t t y PO at contac ts -qt2 ve in a t 70 t o SCA, approx 6 c i wide, b l o w o u t a b i t a t K, has 52 coarse PO c l o t s

-15-20% green r h l o r i t c bands -strong l i i y sec t ion with 702 carb - t a l c i t e healed h r e r t i a -s t rong ly broken and f rac tu red

*

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OREQUEST CONSULTANTS LTD, HOLE i : 6-94-9 PAGE II 7 of 10

mu In ROCK A L T FOL OFSTRIPTION % SAHPLE NO, FROH TO LFNFTH Air A9 Cu Pb 711 TYPF CIA SUI PHIOE opst opst pct pct p r t

471.85 494,91 GREY HARBLE (UITH INTERCAILATED THI ORITE PHYLLITE)

4 7 8 , ~ 47a,49 480.79 483.84 486.15 486.41

486,40 488,47 488.83 490.01 490.55 490.91 491.06 491.35 49?,10 493.14 493,64

494,91 504,24 .

500,67 500,96

504.24 514,33

511.77 511.84 5 1 4 ~ 0 514.33

514.33 516,08

516.08 537,34

Mediiim t o coarsely c rys ta l l i ne grey uarble with < 51 black argi l laceolrz material and 5-101 interbedded grern Chlori te Phyil i t e which i s pa ra l l e l t o f o l i a t i o n at 10-15 to SCA. UC and IT are sharp at 10 t o STA, V i r t l r a l l y no wlphides. Host interbedded Chlor i te Phy l l i t e w t i o n s are < 1Oca except near bottom of t ini t where they are longer and there i s also tan b i o t i t e present,

-Mottled pink and green rn lour , looks semi-granit ic -801 recovery, can't s ~ e why any (ore wiz lost - f o l i a t i o n zteepens to 25 t o STA -3cu vein o f tan b i o t i t e with S3 rrenulat ion clravage a t 50 t o SCA -THLORITE PHYLL I T E

CHLORITE PHYLL ITE -40% tan b i o t i t e -THI ORITE PHYLL I T F - fractured at 85 to SCA

CHLORITE - SERICITF - BIOTITE PHYLL I T E

Strongly rezembles r i th upper TSP un i t that marks the s ta r t of the Lower Index Formation, Conprised o f qtz (308), ch lo r i t e ( 3 0 X ) , s e r i c i t r (10-20%), b i o t i t e (5-1021, and ptygaatic qt7 veins (2-413, Local ly more graphi t ic and look< l i k e DBP. [lissetr PO = 1-42. UC zharp at 10 t o SCA, LC i s broken n i t h minor gouge.

-broken rip qtz w i n at approx 75 t o SCA with 1-71 PO and 101 pale greenish chl-ser 7 mix

SILICIFIED CHLORIlE - SFRICITE - BIOTITE PHYILITF

Bazical ly same as un i t above but \ trongly z i l i c i f i e d . Haz a mottled pale greenish-grey t o greyish pink rololtr , Has 2-42 d i z w PO. UC and L C are at snal l broken in terva ls ,

strongly fractured and broken -5trnngly fractured and broken

rHLORITF - SERICITE - BIOTITE PHYLLLITE

As described 494,91-504.24, IJC sharp a t broken core area. L T a h i t gradational but conformble a t 10 t o STA

SILICIFIFD rHLDRITF - S E R I T I T E - BIOIITE PHYLLITE

' HOLE # : C-94-9

OREQUEST CONSULTANTS LTD. HOLE II : 6-94-9 PAGE I a of 10

FROti T O ROCK A L T FOL DESCRIPTION 2. SAMPLE NO. FROM T O LENGTH Au Ag Tu Pb Z n TYPE CIA SULPH IDE opst opst pct pct pct

As described 504.74-514,22, Generally i t i s strongly s i l i c i f i e d though local sections are sof ter . Minor qtz-carb tension gash i n f i l l i n g s .

517,38 517.48 519.24 520.11 522.30 522.70 525.23 525,37 577.00 528.00

531.91 532 I 12

537.34 603,23

537.34 538.72

553,96 554 I 09 555.01 555.18 556,90 557,21 558,46 558.79 560.95 561 -24 567.02 562.23 566 I 00 567 I 36

574.78 575.19 578.54 578.92 579,80 580.02 580.02 581.75 583,OS 583.14 583.14 586.68

600.61 602-74

603,23 61R,18

-strongly fractured and broken -S3 f o l d wi th l O c i wavelength at 65 t o STA -4inor fo ld , f o l i a t i o n at 45 t o SCA on each l i u b -gouge, rubble and rock chips -aoderately fractured and l o c a l l y qu i te broken o r i s cave, can't t e l l for sure, qtz src t ions near end f o r 30rm

- q t i vein, 2-31 PO, UC sharp at 10, L C i r regular

DARK BANDED PHYLLLITE

Typical black and white banded graphi t ic DRP, As described 426.07- 436.00. Ubiquitous d isse i pa (2-5%). UC sharp at 10 to SCA along area of graphi t ic faul t breccia. LC sharp a t 10 to STh. Local section< of tan b i o t i t e instead of b r o w to black dark coloured b i o t i t e , Fo l ia t ion at 10 t o SCA. Hoderately to strongly s i l i c i f i e d ,

-broken and fractured with graphi t ic goluge and loca l l y brecciated - esper ia l ly a t upper contact with 5% qtz-carb tension gash i n f i l l i n g s

-brecciated qtz-(arb vein at 60 t o SCA, 2cn wide -noderately fractured and broken -qt7 vein / fracture, qnn wide a t 75 t o STA -qtz vein / fracture, 4ni wide a t 75 t o SCA -broken and fractured -broken and fractured -2-71 qtz-carb tension gash i n f i l l i n g s with 2Ocm o f h ig l y broken and fractured rock a t end

-152 qtz flooded with 41 d i w n PO -broken and fractured along qtz-carb vein at 70 t o STA -broken and fractured along qtz-rarb vein at 70 t o SCA 5 3 folds and cleavage at 65-85 t o STA -graphit ic gouge -Moderately fractured, weakly broken except f ro# 586.15-586.68 which i s strongly broken and fractured, 5% qtz-carb veins and gashes -S? r rpn i r la t ion cleavage at 15 t o SCA

FARNET ZONE (IN DARK BANDED P H Y l l I T E )

S i l i reous and g raph i t i r garnet 7one i n DBP, Contain.. 5t garnets on average, l o r a l l y up t o 30%. Moderately fractured throughout, l o r a l l y quite broken. Fol ia ted at 10-15 t o STA, Contains up t o 15-20! chert bands and i s l o r a l l y qu i te graphi t ic ezpecial ly when broken. Has 2-51 qtz-rarb tension gazh i n f i l l i n g s . Averages 3-51 f i ne d i s w PO with

HOLE # : 6-94-9

OREQUEST CONSULTANTS LTD. HOLF II : 6-94-9 PAGE il 9 of 10

FROM TO ROCK ALT fOL TYPE C I A

DESCRIPTION 8 SAKPLE No. FROM TO LFNGTH AIJ A9 CU Pb Zn SUI PH IOF opst opst pct pct pct

618.18 620,94

622,48 624.13

624,13 626,48

loca l sectionz o f 30-351 PO. l lC sharp but i s broken r i t h gouge. 1C i s i r regular warped around S 3 minor fo ld ,

-healed fau l t gouge, strongly broken over l o r e r lOra -10% qtz-carb tension 9azh i n f i l l ings -202 chert bands, uinor S1. fo lds a t 10 t o SfR -10% qt7-carb tension gash i n f i l l i n g z , gougr, rubble and rork chips from 610,32-610.84

-256 garnets -strongly fracturpd and broken -5trongly fractured and broken r i t h r a l r i t e veining

pyrrhot i te and trace rpy s i l -Semi Haszive Sulphide Zone consist ing of 35-401 strongly iagnet i r 35 491 617.31 618 18 .87 ,001 d 1 -054 ,O? ,01

ARK11 LACEOUS LIMESTONE

625.74 626,48 HWDSZ 5 i l

626.48 627,63

626,48 627,43 DSZ sil

Ueakly s i l ireotrz grey and black banded 1 iiestone, Fol iated a t 10 t o SfA, loca l l y rontorted. UC i s i r regular arolrng SB fold, LC zharp at 10 t o STA, Only trarP po, minor garnets near LC,

SEHI-RASSIVE Sll lPHlDE Z O l E (PYRRHOTITF)

q i l -banded PO, ztrongly magnetic, iup to 35-402 but averages 202 PO, 10 491 620.94 61?,48 1.54 ,on1 ,oi ,073 .03 ,n2 It py and trace rpy

DARK BANDED PHYLL IIE

Very l i t t l e carbonate, l o r e z i l r a and dark brown to black argillaceoirz aater ia l I Hinor green ch lo r i t e . Iracp-2% dissei Po,

ARGILLATEMIS LINESTONF

Typiral argillaceous 1 irrestone, l o c a l l y intercalated with DRP, minor s i l i r i f i r a t i o n and chert near rontact with srrlphide zone belor,

-rhert bands to 626,17 then w r y strong b i o t i t e to 626.48, trace-28 1 493 625.74 6 7 ~ 4 8 ,74 <.ooi <.ni ,197 ,oi -11

DISSEMINATED i n WASSIVF SUI PHIDE ZONE

f i n e d i s w PO

S i l ireoris ztrlphide ione . UT sharp at 10 t o SCA based on wlphide rontent, zaae f o r LT,

-DISSEWINAIED SIILPHIDE ZONf - variable sulphide d is t r ih i r t ion a< 11 494 6?6.48 6 u . 4 1 .q5 ,002 - 2 7 2.162 , i8 ,89 f ine diszeainat ions and l o r e roncentratpd 1 ike vr inz at 10 to SCA, av~rages 101. PO (non-reakly magnetic) 5% cpy and trace sphaleri te

HOLE I f : 6-94-9

HO1.F I : 6-94-5 PAGE I 10 o f 10 OREQUEST CONSULTANTS LTD.

rROM T O ROCK ALT FOL TYPE CIA

DESCRIPTION 8 SAMPLE NO. FROM TO lFN6TH Air Ag Cu Ph Zn StllPHIDE opst opst pct pct pct

627,43 627,63 HSZ SIL - IASSIVF SUIPHIbE 7ONF - averages 352 po and 25-30? cpy, variable 65 495 611.43 627,63 .20 ,no9 1.3s 6.494 1.79 7,73 qphalpri te and 3-59. galena near upper rontact only

627.63 631.28 FOOTUALL DISSFMINATED SULPHIDF /ONE

Strongly s i l i c i f i e d , cherty banded DBP. Sharp UC and L C at 10 t o SCA Strongest sulphides jwt below BSZ then weaker d i w i i n a t p d averaging 2-# PO, 18 cpy and t ra re sphaleri te,

627.63 618.26 FWOSZ s i l -9 PO, 12 cpy, t ra re sph, t i gh t S2 fo ld ing at 10 to SCA over 5cn 6 496 627.63 678J6 .63 <,001 <.Ol ,531 .O? ,135 628.26 628.98 FWDSZ s i l -25-30% cherty banding, strongly z i l i c i f i ed , 2% PO, trace-1% rpy 2 497 618.16 628.98 ,77 <,001 <,01 ,019 ,01 .03

628.98 629,45 FWbSZ s i l -strongly broken and f r a c t w d with gouge 1 498 628.98 619.45 .47 mi ,n i ,012 .o? .n3 619.45 630,18 -11 ireoils DBP 630.18 631,18 -cherty banded, highly s i l iceoiis

631.28 639.02 ARGILLACEOUS LIHESIONF

and trace sphaleri te

631.28 632.04

Typical grey 1 iwstone with black a r g i l l a r o m band\, Well f o l iatpd a t 15-70 t o STA. UC zharp at 10 t o SCA.

-brerr ia tpd looking n i t h 201 qt7-rarb veining enclozinc) angular 1 inestone fragments

0 RE Q U E S T C 0 N S U L T A N T S L T D - DIAMOND DRILL HOLE RECORD C1 ient BETHLEHEM Page I 1 of 10

Hole No. 6-94-10 Northing 3385 Core Size NQ I 1 Depth Dip Azimuth Depth Dip Az i iu th Started NOV. 5, 1994 i a r i e t ~ I N E OREBODY Property GOLDSTREAM East ing 16032 Casing 10 FT.PVCPIPE 85.6 - 86 011 146.3 - 90 Completed NOV. 17, 1994 Conments HOLE CEHENTED Location REVELSTOKE Elevation 690 Length 561.28 222.6 - 87 186 300.6 - 85 216 Drill Co. OLYNPIC NTS 8211/9H Lati tude 5 1 38' 00" N Dip-Collar -85 361.6 - 83 217 422.6 - 78 218 Logged By W . RAVEN C l a i m No Longitude 118 24' 40" H Bearing 020 468.3 - 75 216 514.0 - 74 216 Units METERS

559,8 - 72 217

FROM T O ROCK ALT FOL TYPE C/A

DESCRIPTION % SAMPLE No. FRON TO LEN6TH Au Ag Cu Pb Zn SULPHIDE opst opst pct pct pct

71.74

71.74 193.89

77.74 164.55

77.74 96.15

71.74 81.12 81.12 81.82 81.82 86.35 86.35 94.20 94.20 107.07

107,07 112.24

112,24 115.37 115.37 120.06

120.06 121.13 121.13 121,76 121,76 122.32 122.32 128.48 128.48 139.24

139.24 142.38 142.38 145.43

OVERBURDEN

HAHILL GROUP

INTERCALATED QUARTZITE AND CHLORITE - SERICITE PHYLLITE

Both un i t s are i e d i u i green colour though on occasion the quar tz i te i s greyish and glassy. Quartzite i s rhythmatical ly laminated a t 45 t o SCA while CSP i s f o l i a ted a t sane angle. Minor intercalated Tuffaceous Andesite. Ptyg iat ic qtz veins (1-211, trace d i sse i py and PO, cross- cu t t i ng qtz-carb veins (1-2%). LC i s a t 70 t o SCA a t gouge zone,

-moderately t o strongly fractured, l oca l l y qu i te broken, minor sections of competent core but most pieces < loci long

-QUARTZITE -GREY MARBLE, UC a t 35 to SCA, LC at 45 to SCA, both are sharp -QUARTZITE -CSP -QUARTZITE, generally more competent except moderately fractured f r o i 100.00-101.55

-PORPHYRITIC TO COARSE TUFFACEOUS ANDESITE, one qtz vein 3cn wide with 2 1 PO and trace cpy a t 45 t o SCA a t 108.53

-CSP, very p i t t e d core surface with strong carb f r o i 115.37-116.77 then carb decreases

-QUARTZITE, vuggy fo r l as t lOcm -CSP -QUARTZITE -CSP, well f o l i a ted a t 40 t o SCA -QUARTZITE, laminated a t 40 t o SCA, l o c a l l y a pale greenish-grey colour, weak local f ractur ing

-CSP, s e r i c i t i c gouge from 140.31-140.50 -QUARTZITE, strongly broken and fractured t o 144.10 and moderately fractured f roa 144.90-145.43

-QUARIZITE



DESCRIPTION 1 SAMPLE No. FROH T O LENGTH Au A9 Cu Pb Zn SULPHIDE opst opst pct pct pct

145.43 150,56 150.56 153.47 153.47 157.62

157.62 164.55

157,62 160.87

-CSP -QUARTZITE -INTERCALATED QUARTZITE 8 CSP, strongly broken and fractured from 156.52-156.89

-QUARTZITE, strongly broken and fractured from 161,70-162.15 and 163.00-163.72 with 7011 recovery, laminated a t 40-45 t o SCA

-FAULT ZONE, strongly broken and fractured wi th rubble and rock chips

164.55 168,88 FAULT ZONE

168.88 193.89

Strong clay gouge throughout most of interval and brecciated looking with angular qtz fragments i n gouge. UC and LC are both at 70 t o SCA. Local strong se r i c i t e and carbonate,

QUARTZITE

Pale greenish-grey colour, not as dark as sane u n i t above f a u l t zone. Still laminated a t 35-40 t o SCA. Hinor intercalated CSP but in terva l i s doi inated by quartzite. Minor f i n e grained d isse i py and PO ( t race- l t ) , UC i s sharp a t 70, LC broken at l o c i gouge zone.

168.88 175.66

175.91 188.30 FAULT / FRACTURE ZONE

-1-21 qtz-carb tension gash i n f i l l ings, l oca l l y fractured and broken

188.30 193.89

193.89 341.32

193.89 207.31

193.89 202.82

Hoderately to strongly fractured and broken with local gouge. Local conpetent sections with core pieces < loci long. Hostly quar tz i te but some CSP and B i o t i t e Phy l l i t e . F ro i 185.95-188,30 i s the most broken interval and i s v i r t u a l l y a l l rock chips, rubble and gouge. Hinor sections o f Tuffaceous Andesite.

-QUARTZITE t o CSP, loca l q tz veining, moderately fractured over l a s t metre, qtz vein from 188.53-188,71 wi th trace-12 PO, contacts a t 40 to SCA

CARBONATE PACKAGE (BADSHOT AND NOHICAN FORMATIONS)

AR6 ILLACEOUS LIHESTONE

Typical grey limestone wi th black bands of f i ne argi l laceous material (chl-bio-ser-graphite mix). Hell f o l i a ted a t 30-40 to SCA. Local S3 defoiat ion. UC a t loci gouge, LC sharp at 35 t o SCA. Occasional traces of py and PO usually i n fractured zones.

-noderately to strongly fractured throughout with 2-8t qtz-carb tension gash i n f i l l ings, l o c a l l y brecciated with gouge and graphite

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FROM T O ROCK ALT FOL DESCRIPTION 2 SAMPLE NO. FROH TO LENGTH Au Ag Cu Pb Zn TYPE CIA SULPHIDE opst opst p c t p c t p c t

202.82 207.31 - t y p i c a l Argi l laceoous Linestone

207.31 212.96 GREY HARBLE

Fine c r y s t a l l i n e marble with genera l l y < 101 arg i l laceous bands. UC and LC both sharp a t 35 to SCA, Minor t races o f p y r i t e .

207.89 209.33 209.33 212.96

-banded Arg i l laceous L inestone -3-5% qtz-carb tens ion gash i n f i l l i n g s and 2-3% g r a p h i t i c s t y l o l i t e s

212.96 225.60 ARGILLACEOUS LIMESTONE

212.96 217.12 220.93 223.44

225.60 249.11

233.26 240,49

245-10 245.30 247.95 248,26 248.26 249.11

249.11 250,50

250.9 259.50

255.68 255.91

As described 193,89-207.31. Well f o l i a t e d a t 30-35 to SCA. UC sharp a t 35 t o SCA, LC a l s o sharp a t 35 to SCA. H inor t races o f p y r i t e .

-wavy f o l i a t i o n o f f s e t by 1-311 due t o c renu la t ion cleavage a t 45 SCA -6rey Marble


S i l i ceous core t o the carbonate package, The carbonate i s replaced by nore arg i l laceous i a t e r i a l and s i l i c a . Carbonate i s s t i l l present as a minor conponent (10-152, down f r o n 601). Trace-11 f i n e dissea py and PO. Contains 2-59 p t y g a a t i c q t z veins.

-noderate t o s t rong S3 c r e n u l a t i o n cleavage a t 60 to SCA, f o l i a t i o n a l i t t l e steeper a t 45-50 t o SCA, f r o a 240.00-240.22 i s a f o l d t h a t s t re tches f o l i a t i o n t o 90 t o SCA

-n inor f o l d - b e y Marble -green C h l o r i t e P h y l l i t e


As prev ious ly described, 193.89-207.31

GREY MARBLE

As prev ious ly described 207.31-212.96. Has < 52 arg i l laceous l a y e r s a t 30-35 t o SCA. Contains 1-32 g r a p h i t i c s t y l o l i t e s . UC sharp a t 35 t o SCA, LC approx 20 t o SCA. Trace-1% f i n e grained d i s s e i py l o c a l l y up t o 52 along narrow f r a c t u r e faces.

-q tz vein, UC a t 30, LC a t 50 t o SCA w i th g r a p h i t i c s t y l o l i t e s a t bo th contacts, contains 2-3% coarse c l o t s of po wi th t r a c e - l t py and cpy and t race s p h a l e r i t e

HOLE I : 6-94-10

OREQUEST CONSULTANTS L T D - HOLE I : 6-94-10 PAGE I 4 o f 10

FROH T O ROCK ALT FOL TYPE CIA

DESCRIPTION '1 SAMPLE No. FROM TO LENGTH Au Ag Cu Pb Zn SULPHIDE opst opst pct pct pct

256,lO 256.52

259.50 262.78

262.78 270.43

270.43 272.17

272,I l 293.33

272,Il 276.52

276.52 293,33 280.12 280.20 287.98 293.33

293.33 294.82

-Moderately fractured

INTERCALATED ARSILLACEOUS LIMESTONE AND SERICITE - CHLORITE PHYLLITE

Typical argi l laceous 1 i iestone wi th s i l iceous ser ic i te-ch lor i te phy l l i t e , Hoderately fractured throughout, stronger near b o t t o i of un i t where f o l i a t i o n i s steeper a t 50 t o SCA, Rubble and rock chips from 263.42-263.78 with 251 recovery.

ARCILLACEOUS LIMESTONE

As described 193.89-207.31, Moderately fractured throughout becoiing stronger over the l a s t 2 ie t res. Fo l i a t i on i s steeper throughout u n i t at 60 t o SCA, Minor l oca l ser ic i te-c lay gouge. Contains 1-3% qtz-carb veins. Trace d i sse i py wi th 2-4% py on fractures.

DMOMlTE (PORCELAINEOUS)

Pure white colour wi th minor grey streaks = grey marble. Minor pale green ta l c o r s e r i c i t e ? f a i r l y hard f o r ta lc . No r e l i c bedding v i s ib le i n the dolomite which i s f a i r l y hard but efferveses i n HC1, No v i s ib le sulphides, UC i s poorly defined, LC a t gouge a t 40 t o SCA.

SILICIFIED CHLORITE - B I O T I T E - S E R I C I T E PHYLLITE

Variably s i l i c i f i e d f rou weak t o uoderate. Uell f o l i a ted at 35 t o SCA. Has a pale greenish-grey colour with variable ch lor i te , se r i c i t e and b i o t i t e content, Has f i n e ua t r i x qtz as well as 1-32 p tyg ia t i c q tz veins. Trace-1% f i n e grained disseu py and PO. UC sharp at 40 t o SCA along clay gouge, LT sharp a t 25 t o SCA at q tz vein.

-FAULT ZONE - uost ly rock chips and rubble wi th clay gouge. loca l coipetent sections general ly < loc i , of ten brecciated looking bound together by gouge. F r o i 275,91-276.35 i s coarse green sand, probably cave f r o i upper H a i i l l Group rocks. F r o i 276.35-276.52 i s sub-rounded rock chips that also look l i k e cave.

-coipetent rock except f o r Minor broken sections -rock chips -10-151 white carbonate bands and 5% tan b i o t i t e and a b i t greener due t o more ch lo r i t e

QUARTZ VEIN

UC sharp at 25 t o SCA, LC sharp at 65 t o SCA. Minor PO and py but otherwise barren looking vein. Fron 293.66-294.15 i s 65'1 qtz, 352 chl-ser-bio p h y l l i t e , Has 60cn o f green sandy cave with rock chips

HOLE # I G-94-10

I .

.i

HOLE I : G-94-10 PAGE I 5 of 10 OREQUEST CONSULTANTS LTD,

FROH T O ROCK ALT FOL TYPE C I A

DESCRIPTION 2 SAWPLE No. FROH T O LENGTH Au Ag Cu Pb Zn SULPHIDE opst opst pct pct pct

306.82 319.23 .

310.59 310.91 312.62 314.51 314.51 317.56 317,56 319.23

319,23 332.56

319.23 319.83 331.60 332,OO

332.56 341.32

near bottom of vein f ron b i t change

ARGILLACEOUS L IHESTONE I CALCAREOUS DARK BANDED PHYLLITE

Quite s i a i l a r t o argi l laceous 1 imestone as described 193.89-207.31. More l i k e calcareous DBP to 297.07 as it has a f a i r b i t more argillaceous material, Below 297.07 more 1 ike the argi l laceous limestone with local grey marble. UC sharp a t b o t t o i o f qtz vein a t 65 t o SCA. LC a b i t gradational but confonable at 40 t o SCA. l l inor trace dissem py. Fo l i a t i on a t 40-45 t o SCA which i s steeper.

+nor fo ld stretches f o l i a t i o n t o 70 to SCA -moderately fractured and broken

GREY MARBLE

As described 207.31-212.96 but with fewer s t y lo l i t es , Contains two fa in t folds l i k e 294.82-295-27, UC sharp but gradational at 40 t o SCA, LC sharp a t 40 t o SCA,

CALCAREOUS DARK BANDED PHYLLITE

Consists of f i ne matrix q tz (10-1521, dark brown t o black argi l laceous i a t e r i a l (chl-bio-ser+/-graphite i i x , 40-501), white bands o f carb (25-35%), p t yg ia t i c qtz veins (2-51) and trace-1% f i ne grained dissen PO. UC sharp a t 40 t o SCA, LC sharp at 60 t o SCA.

-node rate1 y fractured and broken -3-41 qtz-carb tension gash i n f i l l ings -1-28 qtz-carb tension gash i n f ill ings -10% qtz-carb tension gash i n f i l l ings

GREY MARBLE

As previovsly described 207.31-212.96. Hediur t o coarsely crysta l1 ine, coarsely bedded at 40 t o SCA. Has < 5t confonably interbedded green Chlor i te Phy l l i t e . Local bands o f pure white i a rb le generally < Scm, Trace very f i ne grained d i sse i py, UC sharp at 60 to SCA, LC i s gradational at 40 t o SCA.

-10% qtz-carb tension gash i n f i l l ings -sei i-brecciated looking with white f i ne grained dolonite (608) with i a rb le and 5 4 % b i o t i t e

INTERCALATED GREY HARBLE 8 CHLORITE PHYLLITE

HOLE 1: 6-94-10

OREQUEST CONSULTANTS LTD. HOLE f : 5-94-10 PAGE I 6 o f 10

FROM T O ROCK ALT FOL TYPE C I A

DESCRIPTION % SAHPLE No. FROM T O LENGTH Au A9 Cu Pb Zn SULPHIDE opst opst pct pct pct

332.56 332,85 ?34,62 335.23 338.10 338.93

341,32 561,28

341.32 356.76

345.66 346.23 349-48 350.20 352,49 352.74 356.08 356,28

356,49 356.76

356.76 365.05

357.00 357.20 357,20 360.73 361 I 18 361 I 38

365.05 368,79

368.79 373.26

Marble as described above (319.23-332.56) with 20% intercalated green Chlor i te Phyl l i te . The p h y l l i t e in terva ls are conforiable at 40 t o SCA and range f ron a few cm to 60ca i n core length. UC gradational a t 40 to SCA, LC sharp at 45 to SCA. Trace disscm pya Larger intervals of Chlor i te Phyl l i t e are 1 is ted below.

-Chlori te Phy l l i t e -Chlori te Phyl l i t e -Chlori te Phy l l i t e with 158 marble

LOWER INDEX FORNATION


Coiprised o f ch lo r i t e -se r i c i t e and quartz with lessor muscovite and b i o t i t e . Has 5% p tyg ia t i c qtz veins and 11 cross-cutting qtz-carb veins. Trace-12 f i ne d i sse i PO. UC sharp a t 45 t o SCA. LC sharp but i r regular along qtz vein contact. Unit i s moderately fractured throughout with very fen pieces > l o c i long, fractured but not broken, Minor areas o f tan b i o t i t e enrichment. Fo l i a t i on at 35 to SCA.

-broken and fractured, 701 recovery -moderately fractured and broken -noderately fractured and broken -qt2 vein, UC a t approx 40 t o SCA along lcm o f gouge, LC broken with minor gouge, trace dissem PO

-qtz vein, UC i r regular but approx 10-20 t o SCA, LC i r regular and dif fuse, has 1-22 dissem PO and trace py aostly at contacts

SILICIFIED CHLORITE - SERICITE PHVLLITE

Basical ly sane as above u n i t only i t i s s i l i c i f i e d due t o increase i n f ine matrix qt2. Pale greyish-green colour. UC irregular along qtz vein. LC i s a gradational change, Fo l i a t i on a t 30 to SCA.

-strongly broken and fractured -1-22 qtz-carb tension gash i n f i l l ings -strongly fractured and broken


As described 341.32-356.76. Fo l i a t i on i s a l i t t l e steeper at 50 to SCA. Fro# 366.92-368.07 i s DRP that i s l oca l l y broken and fractured.

SILICIFIED CHLORITE - SERICITE PHVLLITE

.

HOLE / I E-94-10



DESCRIPTION 1 SAWPLE No, FROM T O LENGTH Au Ag Cu Pb l n SULPHIDE opst opst pct pct pct

313.26 380.95

380.95 382,80

382.80 383,66

383.66 393 J 4 385 I 59 3R5.95

393.74 402,60 402.99 404.02 404.22 414,62 415.86

418,37 418.52 422,17 422.38 423.92 421,18

444.00 445.95 458.55

451.15 458.39 465,12 465.65 411,22 419.35

478.87 480.29 480.35

484.85 485,lO

As described 356,76-365,05

VARIABLY SILICIFIED CHLORITF - SERICITE PHYLLITE

Intercalated s i l i c i f i e d and non-s i l i c i f i ed CSP. Fa i r l y competent r i t h loca l areas that are broken and fractured.


Typical DBP corprised o f biotite-graphite-sericite (50-601) r i t h r h i t e carb bands (10-202), f i ne na t r i x qtz (10-15%), p tyg ia t i c qt2 veins (3-8t), cross-cutt ing qtz-carb veins (1-211, and f i n e d isse i PO and py ( t r a ~ e - 5 1 ) ~ UC i s along graphi t ic gouge a t approx 70 to SCA but soiewhat irregular. Weakly fractured throughout except at UC rhere there i s strong f ractur ing and broken rock. LC a b i t broken but approx 15-20 t o SCA. Fo l i a t i on at 30-35 to SCA.

-graphit ic clay gouge r i t h 5% f i ne py, also rock chips and rubble, only 401 recovery from 381,33-382.80

-strongly fractured but bound together wi th graphi t ic gouge, 10% qtz-carb tension gash i n f i l l ings

- fo l i a t i on i s steeper than average at 45-50 to SCA -1-2cm gouge veins at 50 t o SCA with 10-151 qtz-carb tension gashes - fo l i a t i on f l a t tens t o 30 t o SCA -5% pale green bands = chl-ser n i x ? with up t o 5% coarser blebby PO

-minor gouge, broken -QUARTZ VEIN - UC i s i r regular along zone of reak shearing, LC sharp at 55 to SCA, has 1-2% coarse PO c lo t s with trace py and cpy, otherwise f a i r l y barren looking b u l l quartz

-qtz vein, UC approx 40 t o SCA, LC at 65 t o SCA, minor traces of PO -2 small isoc l ina l fo lds -1-21 qtz-carb tension gash i n f i l l ings - fo l i a t i on at 30-35 t o SCA - ioderately s i l i c i f i e d and p tyg ia t i c q tz veining increases t o 5-8%, sulphides as PO increase t o 4-6% as d isse i inat ions and layer para l le l blebs and streaks, loca l qtz veins 2 - 8 c i r ide, f o l i a t i o n at 30 to SCA

-contorted and navy f o l i a t i o n -strongly fractured, weakly broken -S3 crenulat ion cleavage at 65 t o SCA l o c a l l y o f f se ts f o l i a t i o n and produces navy f o l i a t i o n

-belor t h i s point the DBP i s ioderately t o strongly s i l i c i f i e d -brecciated carb-qtz vein wi th 5-101 angular fragients o f DBP at 10 t o

SCA, vein i s 1-1Scm r i d e but blows out a t UC, 2% dissea py -qtz vein at 70 t o SCA, vein has true r i d t h o f 5cm, has 1t dissem PO nostly at nargins

HOLE 1: 6-94-10

OREQUEST CONSULTANTS LTD. HOLE I : 6-94-10 PACE I 8 o f 10

FROM TO ROCK ALT FOL DESCRIPTION t SAHPI.E NO. FROM TO LENGTH AU ~9 r u Pb Zn TYPE C I A SULPHIDE opst opst p t t pct pct

487,20 488.20 4 3 f o l d produces f o l i a t i o n at 65-70 t o SCA 488,20 488.45

495.84 496.04

496,04 500,OO

-qtz vein, UC f a i r l y sharp at 20 to SCA, LC irregular, tontains 38 D8P and 38 f i n e t o coarse blebs o f PO with trace cpy

-brecciated carb-qtz vein with 10-158 angular fragments of DBP, vein at 70 t o SCA wi th graphi t ic part ings

-Moderately t o strongly broken and fractured with 1-22 qtz-carb tension gash i n f i l l i n g s and 5-83 qtz-carb veining with up to 58 py that i s los t obvious on fractures

-a b i t More fractured with 1-22 qtz-carb tension gash i n f i l l i n g s and 5-71 ptygnatic qtz veins

-S3 fo ld , f o l i a t i o n at 55-60 t o SCA, interval has 5 4 % tan b i o t i t e

500.00 ' - f o l i a t i o n s ta r t i ng to f l a t t e n a t 20 t o SCA 500.00 517.69

502-50 504,04 -s l ight increase i n dissen PO t o 4-6t 513,15 513-87 527.10 527.86 -weak S3 defor ia t ion produces wavy f o l i a t i o n

*

529,31 542,02 GARNET ZONE

529.31 535,15

535.15 537.59

531.59 539.42

539.42 539,86

539.86 542.02

542,02 546.50

Strong garnet zone i n DBP. Variable garnet content f r o i 1-32 t o 30-351 with garnets ranging f r o i 1-211 t o 10~1 , they are rounded and the f o l i a t i o n wraps around the garnets. Chert bands range from 5-252. Ptygnatic qtz veins f r o i 5-101, Variable sulphide content f ro# 1-2\ d isse i PO t o 35% wispy banded PO. UC a b i t broken but approx 15-20 t o SCA, LC a b i t i r regular at approx 10-15 to SCA. Variable f o l i a t i o n throughout un i t , most disrupted i n the upper port ion. Strong graphite present, Most v i s ib le on fractures,

-cherty banded DBP with 5-15t chert bands and 1-3% garnets, strong qtz-carb tension gash i n f i l l i n g s throughout (5-10b) up to 151 f r o i 534.20-535.15, ninor fau l t i ng and brecciat ion at upper and lower contacts, f o l i a t i o n i s f a i r l y steep a t 55-60 t o SCA, 52 f ine grained disseminated PO

-garnet zone i n DBP as above but not brecciated and semi-faulted looking, f o l i a t i o n at l i t t l e f l a t t e r at 40 to SCA but s t i l l steeper than average d ip of broad l i t ho log ies

-Mottled pale greenish toloured garnet zone with 10-301 garnets and up t o 30% cherty banding, pale greenish - yellow i i ne ra l = ?, core i s heavier than average but doesn't look l i k e i t i s caused by sulphides as has 3-52 d isse i PO

-Seii-Massive PO as wispy net-1 ike texture, averages 352 PO,

trace cpy and trace sphaleri te -strong garnets (20-352) and cherty bands (301) and 6-10? banded and dissei inated po

CREY - GREEN PHYLLITE

Variably s i l i c i f i e d but generally qu i te weak. Conprised of qtz, chl, HOLE R: 6-94-10 i.

. - . . * *



DESCRIPTION 2 SAMPLE No. FROM T O LENGTH A u Ag Cu Pb Zn SULPHIDE opst opst pct pct pct ,

546.50 547.50 LST si1,car 549.60 550.60 LST s i l ,car

550,60 554.62

550.60 551.42 DSSZ s i l

551,42 552,60 DSSZ s i l

552,60 553.60 OSSZ s i l

553,60 554,62 OSSZ s i l

554.62 555.20

554.62 555.20 FAULT grap

555.20 556.00

ser and b io and 2-32 ptygnatic q tz veins, 1-2% dissei PO and trace cpy, UC a b i t i r regular at approx 10-15 t o SCA, LC also i r regular at approx 60 t o SCA, Poorly defined f o l i a t i o n a t approx 15 t o SCA

AR6 ILL ACEOUS L IMESTONE

Generally grey-white l i i es tone wi th black bands of argillaceous Material. Local sections are chl-ser r ich, Weakly fractured, l oca l l y broken and fractured, Has 1-2% qtz-carb tension gash i n f i l l i n g s l oca l l y up t o 10% i n brecciated p a r t i a l vein structures. UC i s i r regular a t approx 60 t o SCA, LC f a i r l y sharp at 50 t o SCA larked by strong s i l i c a f looding and sulphide n inera l izat ion, Generally f o l i a ted at 10 t o SCA, l o c a l l y contorted over several CI. Hinor d isse i f i ne grained PO and a few coarser blebs of PO.

-3-5% cherty bands and blebs, 3% d isse i and blebby PO with trace cpy 3 1851 546.50 547.50 1.00 m i ,oz ,042 ,oi .ii -19 f i np grained d isse i PO, trace cpy 1 1852 549,60 550.60 1.00 ,002 ,07 ,067 a 1 .lo

DISSEHINATED AND STRINFER SULPHIDE ZONE

Strong s i l i c i f i c a t i o n as f i ne grained na t r i x qt2 and 20-31 grey chert bands. H o s t rock i s greyish-white 1 inestone. Has 1-3t qtz-carb tension gash i n f i l l i n g s , 5% ptygmatic qt2 veins. UC approx 50 to SCA and i s i r regular , LC approx 15 t o SCA a t graphi t ic gouge zone. n inera l izat ion consists o f PO, cpy and sphaleri te as w e l l as trace galena as f i ne layer pa ra l l e l disseninations and f i ne s t r ingers o r bands o f sulphide.

-15-20% cnarse bands (lcn) o f PO a t approx 20 t o SCA with 1% cpy and 10 1853 550.60 551.42 .82 ,001 .19 ,261 .08 .80 trace-11 sphaleri te and trace galena f r o i 550,60-550.82 and f r o i 551.11-551,33 i s 5% PO, 5% sph and 2% cpy and trace galena, the PO i s non t o very weakly aagnetic

-weak dissen sulphides, 2% PO, 2% py, 12 cpy with one 2cn band of 5 1854 551.42 552.60 1.18 ,001 .07 ,096 .03 .12 202 t o ta l sulphide

- f a i r l y cherty with 1-21 t o ta l d i sse i PO, py, and cpy to 553.37 then 5 1855 552.60 553.60 1.00 ,002 .02 ,156 -01 ,41 8% PO, 1% cpy, 1% sphaleri te to 553.60

-strong s i l i c i f i c a t i o n , most o f un i t looks l i k e s i l i c i f i e d grey-green 8 1856 553.60 554.62 1.02 <.001 -13 ,073 .05 .17 p h y l l i t e wi th banded and layer pa ra l l e l PO (5t), py (521, cpy (1%) and sphaleri te (lt), very weakly nagnetic PO

GRAPHITIC FAULT / SHEAR ZONE

-strongly broken with nuch gouge, rock chips and rubble, ztrong 5 1857 554.62 555.20 .58 <,001 -05 ,153 <.01 ,03 graphite, 52 dissen f i ne grained py and PO, contacts are approx 10-15

FOOTWALL DISSEMINATED SllLPHlDE ZONF

HOLE I: G-94-10

OREQUEST CONSULTANTS LTD. HOLE II : 6-94-10 PAGE I 10 o f 10


DESCR 1PT ION 1 SANPLE No. FROM TO LENGTH Au A9 Cu Pb 2n SULPH IDE opst opst pc t pct pct

555,ZO 556.00 FWDSZ s i l - internixed grey-green phy l l i t e and argi l laceous 1 inestone, weakly 3 1858 555.20 556.00 .80 <.ooi <.o i ,006 < . o i . o i si l icpous, 2-32 f i n e grained d i sse i PO, trace cpy, UC approx 10-15 t o SCA, LC sharp at 20 t o SCA


556.00 557.01 LST car 20 557.66 557.96

558.17 558.30

Well f o l i a ted at 20 t o SCA. 1-2% cross-cutt ing qtz-carb veins, 1-25 qtz-carb tension gash i n f i l l i n g s . Has 1% f i n e d isse i PO

-as general descript ion -bul l qtz vein at 20 t o SCA, 1-2% PO and trace py and cpy around vein iarg ins

-qtz vein, UC approx 35 t o SCA, LC approx 30 t o SCA, trace-11 PO around vein i a rg ins

END OF HOLE

1 la59 556.00 557,oi 1.01 ,001 .06 ,004 <.01 -01

561, za .

0 RE Q U E S T C 0 N S U L TAN T S L T D - DIAMOND DRILL HOLE RECORD C1 ient BETHLEHEH Page I 1 of 6

Hole No. 6-94-11 Northing 3123 Core Size NQ I1 Depth Dip Azinuth Depth Dip Az i iu th Started NOV. 18, 1994 Target MINE OREBODV Property GDLDSTREAM East ing 15878 Casing 10' PVC PIPE 61.6 - 90 107,3 - 88 158 Completed NOV. 24, 1994 Connents HOLE CEMENTED Location REVELSTOKE Elevation 665 Length 386.28 168.3 - 83 180 229,3 - 81 188 Drill Coo OLYNPIC NTS 82111911 Lati tude 51 38' 00" N Dip-Collar -90 290.2 - 79 193 356.0 - 76 200 Logged By W . RAVEN Clain No Longitude 118 24 ' 40" W Bearing N/A 381.7 - 75 202 Units NETERS


DESCRIPTION 2 SAMPLE No. FROM TO LENGTH A u Ag Cu Pb l n SULPHIDE opst opst pct pct pct

58 I 54

58.54 112,23

58.54 105,79

58.54 60,61

60.61 61,86 72.16 72,26 78.12 78A9

82,80 83.47

86,67 87,OO 89.95 91,64

93,13 93,57 93.41 93.60 95,95 101.28

101.33 102,18

102.63 102.78 103.28 103,46 105.65 105~79

105.79 112.23

OVERBURDEN

CARBONATE PACKAGE (BADSHOT AND MOHICAN FORMAT IONS)


6reyish-white 1 i iestone wi th black argi l laceous bands. Coiprised o f carbonate (50-85%), b i o t i t e (5-151), ch lo r i t e (S-lSt), se r i c i t e (5rl), tan b i o t i t e (511, ptygmatic qtz veins (1-31) and trace-12 f i ne dissen py, Minor graphite i n the argi l laceous nater ia l . Local cross-cutt ing qtz-carb veins (1%). Well f o l i a ted at 35-40 to XA. LC sharp at 35 SCA

-wavy f o l i a t i o n f ro# S3 interference, weak crenulat ion cleavage a t approx 70 to SCA, poorly defined

-qtz +I- carb vein 3-411 wide at 85 t o SCA -strongly broken and fractured -qtz vein, UC and LC at approx 70 t o SCA, 1% dissei PO around Margins, i i n o r fo ld ing a t UC o f vein with f o l d axes at 70 t o SCA

-qtz s t r inger vein 5un wide at 80 t o SCA with 5-81 henati te and 3-5t galena

-greenish coloured Chlor i te - Tan B i o t i t e - Phy l l i t e -3t qtz-carb tension gash i n f i l l i n g s , a b i t more fractured throughout t h i s interval

-Chlori te Phyl l i te , conforiable at 35 to SCA -broken and fractured ca l c i t e - qtz vein -GREY IlARBLE - generally has < 10% argi l laceous nater ia l and i s confonable at 35 t o SCA

-has 40-50; conformble qtz veining with 1-29 PO blebs i n the veins which are 3-10 cu r i de

-S3 crenulat ion cleavage at 50-60 to SCA -interbedded Chlor i te Phyl l i t e -interbedded Chlor i te Phyl l ite

GREY MARBLE

Fa i r l y clean f i ne - iedium grained grey narble with < 10% argi l laceous

HOLE I : 6-94-11 PAGE I 2 of 6 OREQUEST CONSULTANTS LTD, ~~~

FROM T O ROCK ALT FOL DESCRIPTION % SAHPLE No. FROH TO LEN6TH AU Ag Cu Pb Zn TYPE C I A SULPHIDE opst opst pct pct pct

bands which define f o l i a t i o n at 35 t o SCA. UC sharp at 35 t o SCA, LC at gouge and rubble that i s cemented together with the contact at approx i ia te ly 50 t o SCA,

108.17 108.90

110,22 112.23

-brecciated section with 8% qtz-carb tension gash i n f i l l i n g s , some o f the brecc iat ion i s i n a pa r t i a l vein structure at 70-80 to SCA with 52 graphite

-brecciated marble, 5t graphi t ic s t y l o l i tes, angular f ragwnts o f i a r b l e subsequently healed, c lay gouge f r o i 112,08-112.21

112.23 386.28 LOUER INDEX FORMATION

112-23 125,31 CHLORITE - B I O T I T E - SERICITE PHYLLITE

112.23 113,73

113,73 120,31

125,31 144.79

124,OO 124.08

125.66 125,76 126.75 126.85 127,OO 128,ZO 129,OO 129.30 130.30 130,62

131,39 131.66 133.76 133.89 135.00 135,77

Greyish-green colour, variable s i l i c i f i c a t i o n from none t o weak, Comprised of ch lo r i t e (20-40%), b io t i te (10-25t), ser ic i te / iuscov i te (10-15%), tan b i o t i t e (5-1021, f i n e i a t r i x qtz (15-208) and p tyg ia t i c qtz veins (1-3%). Strongly fractured over upper por t ion then f a i r l y coipetent, Fine d i sse i PO and py (trace-2%), UC i n fau l t zone but f a i r l y sharp a t 50 t o SCA. LC gradational change through broken core,

-strongly fractured and broken with gouge, rubble and rock chips, sole breccia f rag ients i n the gouge

-strongly fractured, weakly t o moderately broken, very few pieces o f core > loci long, l oca l l y strongly broken, up t o 52 py i n c a l c i t e veins

CHLORITE - BIOTITE - TAN BIOTITE - SERICITE PHYLLITE

Simi lar t o un i t above (112.23-125,31) only reakly t o ioderately s i l i c i f i e d and wi th nore obvious tan b i o t i t e (20-301). UC gradational change through broken core, LC f a i r l y sharp at 30 t o SCA, Fine dissen PO (trace-2%), well f o l i a ted t o laninated at 30 t o SCA.

-graphi t ic gouge and rubble, looks l i k e DEP, UC appprox 55 to SCA, LC i s broken

-strongly broken and fractured -strongly broken and fractured - ioderately broken and fractured -strongly broken and fractured with clay -small f o l d stretches f o l i a t i o n to 70 to SCA and interval has 49 f i n e grained d isse i PO

-S3 f o l d axes at 60 to SCA, numerous s i a l l crenulat ion fo lds -two "2"-folds, axes a t 55 to SCA -38 qtz-carb tension gash i n f i l l ings, broken over loner lOtn

a

HOLE # I G-94-11

PAGE I 3 of 6 HOLE I : 6-94-11 OREQUEST CONSULTANTS LTD,


DESCRIPTION '1 SAMPLE No. FROM TO LENGTH Au Ag Cu Pb 2n SULPHIDE opst opst pct pct pct

136.36 136,71 137.37 137.60 138.70

144.79 343.79

145,43 146.45

146.41 148.48 149.10 150.30

150.30 158.21

168-55 175.20

178.42 178.71 180.96 181.08 184,86 185.06 187.60 187,68 189,75 189.91 193 I 82 194,Ol 195 I 95 203 I 35

200.34 200.68

208 I 20 208 I 38 218.60 221.65

221,74 231.40 233.96

233.12 233.35

-53 fold, axis a t 55 t o SCA 4 3 folds, axes at 55 t o SEA -20-25% qtz flooded, one vein has 51 medium t o coarse po blebs

DARK BANDED PHYLL I T E

Dark-brown t o black argi l laceous band with white carb bands. Comprised of b i o t i t e (30%), ch lo r i t e (lot), se r i c i t e and muscovite (lot), tan b i o t i t e (5-102 l o c a l l y higher), carb (10-25%), ptygrat ic qtz veins and augens (5t, l o c a l l y up t o 811, cross-cutting qtz +/- carb s t r inger veins (trace-1%) and f i n e disspn and layer pa ra l l e l po ( 2 - 5 t ) . Well f o l i a ted at 30 t o SCA gradually f la t ten ing downhole. Weakly s i l i c i f i e d throughout, l o c a l l y stronger especial ly near bottonm of un i t , UC sharp at 30 t o SCA, LC broken at l o c i o f graphi t ic gouge,

-semi-brecciated looking wi th 3-5%, and up t o 1st qtz-carb tension gash i n f i l l i n g s , from 146,OO-146.20 has 5% py and f r o i 146.20-146,41 i s Mini GARNET ZONE

-5-61 combined py and po -CHLORITE - SERICITE PHYLLITE - moderately fractured, loca l 1 y qu i te broken

-strongly calcareous in terva l t o 154.77 then f a i r l y strong tan b i o t i t e (10-200 before grading in to the rore typ ica l looking DBP

-moderately to strongly fractured, l oca l l y qu i te broken, 2-3t cross- cu t t i ng qtz-carb veins, f r o i 170.94-171,40 i s qtz vein with 39 coarse PO blebs, lower 20 cm i s shattered and from 175.05-175.20 i s broken high angle qtz vein with r i n o r PO

- i r regular q tz vein, 1-2% po -gouge and small rock chips m d e r a t e l y fractured and broken -broken with gouge -5-6'1 py i n wallrock around ca l c i t e vein 4 cm wide at 50 t o SCA -broken and fractured with local p y r i t i c gouge -graphit ic crenulat ion cleavage at 60-65 t o SCA, from 198,55-200.00

(approx) i s f o l d wi th f o l i a t i o n a t 70-85 t o SCA -qtz vein with minor carb, UC a t 60, LC a t approx 60 t o SCA but not r l e a r l y defined, vein has about 5t py, 1-2% po and trace rpy t o 200.44 then 2'1 PO, 1% py

-graphit ic crenulat ion cleavage at 60 t o SCA -2% qtz-carb tension gash i n f i l l i n g s and S3 crenulat ion cleavage and fo ld ing at approx 60 t o SCA, l oca l l y moderately fractured

- f o l i a t i o n at 20 t o SCA -S3 crenulat ion cleavage and fo lds at 60 t o SCA l oca l l y o f fsets fo l i a t ion by 1-3nm

-qtz vein, UC a t 60, LC a t approx 20 t o SCA, vein has 2 coarse c lo t s of PO wi th trace cpy

HOLE #: G-94-11

OREQUEST CONSULTANTS LTD, HOLE f : 6-94-11 PAGE II 4 of 6

FRO# TO ROCK ALT FOL TYPF C i A

DESCRIPTION 0 SAMPLE No. FRO# TO LENGTH Au Ag Cu Pb Zn SULPHIDE opst opst pct pct pct

237,66 231-95 238,37 240.76

248 I 00 251.00 251 I 55

252,46 252.87 254 I 13 254 I 49 266,45 261 I 30 215 I 81 216-09 292.33 293.21

295.35 297,39

297,613 299.19 308.64 309.42 313.94 315,82 334.91 336,87 338,30 343.19

m d e r a t e l y fractured and broken -strong S3 crenulat ion cleavage and fo ld ing at 55-65 to SCA, wavy f o l i a t i o n

- fo l i a t i on at 20-25 t o SCA - w e s i l iceous with 5-64 po including a 3-411 wide qtz-po vein at 80 t o SCA with 301 PO, t h i s vein of fsets f o l i a t i o n by l c n

-6% dissen PO -q!2 vein, 2 c i wide at 75 t o SCA with 2-3?, d isse i blebs o f PO

-strong S3 crenulat ion cleavage and fo lds at 60 to SCA - isoc l ina l fo lds and weak S3 d isrupt ion o f f o l i a t i o n -strong S3 interference as crenulat ion fo lds and cleavage at approx 55 t o SCA, qtz vein f ro# 293,04-293.27 at 75 t o SCA, vein i s 4 cn wide with 1-2% d isse i PO

-S3 crenulat ion fo lds and cleavage at approx 60 t o SCA, in terva l has 1-2% qtz-carb tension gash i n f i l l i n g s

-node rate1 y fractured - ioderately fractured -noderately fractured, broken over l as t 30 cn -noderately fractured, l oca l l y ioderately t o strongly broken -2-5% qtz-carb tension gash i n f i l l i n g s , ioderately fractured, l oca l l y broken, f ron 339,40-339,64 i s q tz-ca lc i te breccia veining a t 50 t o SCA. f o l i a t i o n a t 20 t o SCA

343,79 348.61

348,61 350140

350,40 357,31

GARNET ZONE (FAULT SUTURED DARK BANDED PHVLLITE)

Seii-brecciated looking DBP that averages lo?, qtz-carb tension gash i n f i l l i n g s , Also has 5-101 snal l chert fragaents - probably o r i g ina l l y banded chert but now broken up. Garnets are small and rare but the 10 CI o f gouge at the top i s indicative o f the contact with the upper DBP, Fo l ia t ion i s qu i te contorted ranging f ron 20-50 t o SCA, As mentioned UC i s a t graphi t ic gouge zone, LC sharp at 15-20 t o SCA. Unit has strong graphite on fractures (51) and contains 1-38 f i ne grained dissei inated PO,

GARNET ZONE ( I N DARK BANDED PHYLLITE)

S in i l a r to above un i t only not sei i-brecciated and garnets are much nore obvious averaging 5% and range f ron 2-311 up t o 8nn, The garnets are rounded and f o l i a t i o n wraps around thea, UC sharp at 15-20 t o SCA, LC i s f a i r l y sharp at 10-15 t o SCA. S i l i c i f i e d but not cherty banded. Sulphides consist o f 2% f i ne dissen PO.

GARNET ZONE

Contorted garnet zone i n probable 6rey - Green Phy l l i t e . Strong chert bands (20-309) and abundant garnets (20-40t) that are generally sNall

HOLE P: G-94-11

OREQUEST CONSULTANTS LTD, HOLE I : 6-94-11 PACE I 5 of ' 6

FROM T O ROCK A l l FOL TYPE C I A

DESCRIPTION 8 SAMPLE No, FROH TO LEN6TH A u Ag Cu Pb . Zn SULPHIDE opst opst pct pct pct '[ J

r. 1 i ..

..-& 2 ' . ?

' 4 (1-311) but l o c a l l y up t o 6m, 6enerally has a l o r sulphide content with trace-21 f i n e disseu PO. UC f a i r l y sharp at 10-15 t o SCA, LC about the saw.

350,19 351.05

352.62 352,14

-paler coloured host rock with 501 garnets, from 350,94-351.14 i s a p a r t i a l qtz vein wi th 15% coarse c lo t s o f PO that i s reakly aagnetic with 12 cpy wi th in the PO, one PO vein 3un wide at 40 to SCA

-nostly rock chips and rubble, strongly broken

353 I 31 355 I 34 ORNET ZONE

Garnet zone i n p a r t i a l Grey-been P h y l l i t e and Argillaceous Limestone, Contains 3-101 rounded garnets and 2-48 disseu PO with minor loca l sections o f 108 PO which i s strongly wagnetic. Strongly broken and f ractrrred f rom 354.01-355.34.

355 I 34 364 44 PHYLLITIC MARBLE

Mottled un i t that i s l i k e l y a l t e r t d marble. Froa 355.34-358.43 has 20-359 b i o t i t e , 10-152 se r i c i t e and 10-15% ch lo r i t e i n a calcareous and s i l iceous nat r ix , Has 2-38 f i ne grained PO and 18 coarser blebs of PO, trace cpy, Fron 358-43-359.13 i s grey-white marble. Fron 359.13-360,93 i s same as 355.34-358,43, From 360.93-364.44 i s less tan b i o t i t e (5%) with l o r e s i l i c a and s e r i c i t e i n a pale greyish coloured rock, UC i s broken, LC i s sharp a t 40 t o SCA.

363,44 364.44 LST si1,rar -mottled l iuy-s i l iceous and s e r i c i t i c rock wi th 11 f ine dissew po 1 1860 363.44 364.44 1.00 <,DO1 ,12 ,046 .01 ,139

364,44 368.81 HANGING WALL SULPHIDE ZONE

Host rock was probably o r i g ina l l y limestone that i s now s i l i c i f i e d and sulphide enriched, Sulphides are variable i n nature ranging from local massive sections over 5-15cu t o disseminated and str ingers. Zone has 5 4 % white qtz-carb blcbs and cross-cutt ing veins. Local sections arp sulphide poor, < 5% to ta l siilphides. UC sharp a t 40 t o SCA along 3cn wide q t i vein, LC i s sharp at 15 t o SCA as defined by uaqs ive sir1 ph ides I

364,44 365.36 HYSZ z i l 60 -seai-uassive sulphides t o 364,16 with 201 PO, 5-88 cpy and 1-31 i a 1861 364,44 365.36 ,92 .001 ,20 1,271 -01 .43 sphaleri te, the PO i s strongly wagnetic, from 364,76465-36 i s more disseninated wi th 8% PO, 5-69 cpy and I t sphaleri te, wavy f o l i a t i o n at 60-65 t o STA

365-36 366,55 H#SZ s i l 40 -strong semi-nassive sulphide to 365.61 with 302 pa (strongly 14 1862 365-36 366.55 1,19 ,001 .11 1,522 .03 , 2.05 magnetic), 5% cpy and 5% sphaleri te, frM 365.61-366,55 i s more ' b

. .. disseainated and s t r ingers a t 40 t o SCA wi th 101 PO, 52 cpy and 5% sphaleri te

. .

HOLE I: 6-94-11

OREQUEST CONSULTANTS LTD, HOLE il : 6-94-11 PAGE f 6 o f 6

FROM T O ROCK ALT fOL TYPE C I A

DESCRIPTION 1 SAMPLE No. FROH TO LEN6TH AIJ Ag Cu Pb Zn SULPHIDE opst opst pct , pct pct

166.55 367.45 HWSZ s i l

367.45 368.05 HMSZ s i l

368.05 368.81 HUSZ s i l

368,81 370.47

368.81 369,64 152 s i l 369,64 370.47 6 2 s i l

170.47 371,47

370.47 371,47 FDSZ si1,car

371,47 W . 5 4

371,47 372.50 LST car 15

380.18 381.54

381,54 386.28

-strong disseminated t o l o c a l l y massive wi th 10-121 PO, 8-10t cpy 23 1863 366,55 367.45 .90 ,001 ,34 2,478 -16 2.20 and 3-52 sphaleri te, i i n o r broken sections and 5-101 white qtz-carb veins and blebs

-highly s i l iceous section r i t h 123 PO, 3-71 cpy and 1 - 3 sphaleri te 15 1864 367.45 368.05 .60 <.001 .29 1.553 .20 1.32 nostly as d isse i inat ions o r s t r inger masses at 20 t o SCA

-disserrinated t o mi-massive wi th 15-20% PO, 51 cpy and 1-38 20 1865 368,05 368,81 ,76 ~ 3 0 1 .12 1.123 ,09 .55 sphaleri te, broken near end, 901 recovery

HASSIVE SULPHIDE ZONE

Si l iceous massive sulphide zone r i t h 5t white qtz-carb blebs and 10% grey qtz, The PO throughout the zone i s strongly iagnetic, Averages 502 PO, 20-25t cpy and 58 sphaleri te that i s intergrown rith the PO, Hinor broken sections. UC sharp at 15, LC sharp a t 10 to SCA.

-as general descript ion -as general descript ion

FOOTWALL DISSEHINATED SULPHIDE ZONE

75 1866 368.81 369,64 .83 ,003 1,15 6.846 .84 5.72 75 1867 369.64 370-47 .83 ,003 .lo 6.030 ,23 2.87

-host un i t i s s i l i c i f i e d l i i t s tone , Moderate sdphide t o 370.67 with 2 1868 370,47 371.47 1.00 <,001 ,06 ,543 -03 -17 101 PO, 51 cpy and 21 sphaleri te then 1-22 dissei PO, moderately fractured r i t h 70% recovery t o 371.04

ARGILLACEOUS 1 IHESTONE

6enerally well f o l i a ted a t 15 t o SCA, Has 5-81 qtz-carb tension gazh i n f i l l i n g s to 377.82 then l o r e o f a cleaner banded marble to 381-54, LC is s ~ n i gradational I

-as general descript ion

-Moderately broken and fractured r i t h interbedded quartzite

QUARTZITE

Pale greenizh-grey rhy th ia t i ca l l y l a i i na ted quartzite, Laminations at 15 t o SCA, Has approx 20% pale chl-ser n i x r i t h i n highly s i l iceous matrix, 1-22 qtz-carb tension gash i n f i l l ings, V i r tua l l y no sulphides. Strongly broken and fractured from 383.20-383,42,

END OF HOLE

tr 1869 371,47 372.50 1,03 <.001 -02 ,023 -01 .01

386,28

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