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GEOLOG I CAL SUMMARY
B~~_~IB~_~~ebgBeIIg~_eBg~~~I_=_§eb~g~_~~~~
LAT: 49 01'N.1 LONG: 117 23'W., MAPSHEET 82 F 3W.
(Nelson Mining Division)
for:
GOLDEN EYE MINERALS LTD.
411 - 850 W. HASTINGS ST.
VANCOUVER, B.C.
669-2449
by:
Barry Price, M.Sc., F.G.A.C.
Consulting Geologist
Rapitan Resources Inc.
3447 W.7th Ave., Vancouver, B.C.
V6R lW2
733-6902'
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81 0 640
Feb 20, 1987
~~.
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Summary
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Introduction
3
Location & Access
3
Property Definition
4
History of the Red Bird Property
5
Regional Geology
6
Geology of the Red Bird Property
7
1985-86 Exploration Program
9
1986-87 Exploration Program
11
Exploration Potential
14
Mineralized Zones
14
Prospect Zone
15
Caviar Property
15
Mining Conditions
15
Conclusions and Recommendations
16
Suggested Exploration Budget
17
Bibliography
18
Appendix I
Core Logs
Appendix II
Assay Sheets
Appendix III
Germanium Facts
Appendix IV
Adjacent Mineral Deposits
Reeves MacDonald Mine
Jersey Mine
J
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HB Mine
Salmo Area Mine Production
Metalline Area Production
~!§I_QE_E!§UB~§~
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Figure
1
Location Map
Figure
2
Claim Locations
Figure
3
Regional Geology
Figure
4
Red Bird Area Geology
Figure
5
Composite Geological Plan
Figure
6
Drill Hole Section
Figure
7
Drill Hole Section 4,5
Figure
8
Drill Hole Section 6
Figure
9
Drill Hole Section 7
1~1A,2,3
Figure 10
Drill Hole Plan
2650 Level
Figure 11
Drill Hole Plan
800 Level
Figure 12
Drill Hole 86-5 Mineralized Section
Figure 13
Longitudinal Section
Figure 14
Kootenay Arc.
Figure 15
Reeves MacDonald Geology
Geology
~
Deposits
[
3 - ]
GEOLOGICAL REPORT
B~~~lB~_EBQ~~~I
SALMO MINING CAMP - NELSON M.D.
!~IBQ~Y~IIQ~~
A significant stratiform Zinc-Lead-Silver-Cadmium-Germanium
discovery has been made by Golden Eye Minerals Ltd.
The prospect is
adjacent to the abandoned Reeves Macdonald Mine, from which 7.2
million tons of ore containing approximately 540 million pounds of
Zinc, 140 million pounds of Lead, 1.5 million ounces of Silver, and
3.0 million pounds of Cadmium were produced from 1949 to 1975.
Geological data indicate that ore zones mined at the Reeves
MacDonald Mine project onto the ground now held by Golden Eye Minerals
Ltd.
This includes the high grade deposits of the Red Bird and Annex
zones.
This report summarizes the geological data and mining potential;
recommendations for continued exploration of this significant
discovery are included.
The report relies heavily on work done by Gerald
Klein~
P.Eng.,
who was employed as mine geologist at the Reeves Macdonald Mine from .
1970 until
1973~
Information gathered from Hecla Mining Company,
Reeves Macdonald Mines Ltd., Cominco Ltd., Diem Mines Ltd., and
government publications has been used in this report.
bQ~aI!Q~_a~~_a~~~§§
The properties are situated 30 kilometres south-southwest of Salmo
B.C. and 35 kilometers southeast of Trail, B.C.
The claims cover an
area roughly 4 km by 8 km, west and east of the Nelway border crossing
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GOLDEN EYE MIN ERALS LT
REO B\RC> PRoPER-r{
DIEM-NOR CLAIMS
LOCATION MAP
SCALE
o 32
b=d
64
98
b=-d
128 160 Miles
b==d
MAY
1985
FIG. I
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[ 4 ]
to the U.S.A., and are bounded ,to the south by the International
Border.
The western portion of the property can be reached by crossing
B.C. Hydro's Seven Mile Dam at Church Creek, and then by good. logging
road. The northern part of the property is accessible by a.bridge
crossing the Pend d'Oreille River on the Reeves Macdonald property.
All supplies and services are available in Salmo or Trail; daily
air service from Calgary and Vancouver is available at the Castlegar
Airport, 45 km from the property.
Power lines cross the Reeves
Macdonald property nearby; water is available for drilling purposes
from a number of creeks or the Pend D'Oreille River.
A significant
pool of experienced underground miners is available in Salmo, which
has been a mining center for a long time.
A partially filled tailings
pond is situated on the Reeves Macdonald property.
Idle mills are
situated at the H.B. Mine site 12 miles to the north and at the Pend
D'Oreille mine site at Metaline Falls in the U.S.A., 15 miles to the
south.
EBQE~BIY_~~EI~IIIQ~~
The property comprises several groups of claims acquired by
staking, option to purchase and lease-purchase agreements.
The Red Bird, Caviar and Grouse groups of Crown-granted mineral
claims were acquired by Golden Eye Minerals Ltd from Diem Mines Ltd.,
of Nelson, B.C., a Canadian subsidiary wholly owned by Hecla Mining
Company of Wallace, Idaho. Golden Eye Minerals can, through a series
of cash payments and work committments, earn 100% interest in the
property subject to a 20% Net Profits Interest payable to Diem Mines
Ltd.
-
--
- -
......
- - -
-
-
GOLDEN EYE MINERALS LTD.
RED 81 RD PROJ ECT
CLAIM LOCATION
MAY 1985
FIG. 2
-
-
[ 5 ]
The Nor 2 and 3 claims were acquired from Gerald Klein under an
option agreement in 1985.
These claims, which adjoin the Redbird
property on the west, were partially evaluated by the 1985-86 drilling
program and have now been returned to the vendor.
The Blue and Tic claims were staked by Golden Eye Minerals and
are owned outright.
Claim data are listed in Appendix, I.
The spatial
arrangement of claims is displayed in Figure 3.
tll§IQ8Y_QE_I~~_B~~_~IB~_~BQ~~BIY~
The Redbird property was originally owned by S.Coulter and
A.J.Campbell of Ymir.
In 1925 an option was acquired by Conrad Wolfe
and associates of Spokane and in 1926 the property was held by the Red
Bird Mining Company of Spokane.
By 1927, 1000 feet of tunneling had
been done on the property, which included 17 claims.
In 1928, the
adit was advanced to 1,200 feet and some diamond drilling was done.
In 1929, the property was acquired by Boundary Basin Mines Ltd., who
did further drilling (Walker, 1934).
Little work was done on the property between 1929 and 1944,
although a sampling plan exists dated 1942.
In 1944, the property was
purchased by Hecla Mining Company of Wallace,
Idaho.
mapping and surface work was done by Hecla in 1947.
Geological
In 1955, Fyles
and Hewlett mapped the area (see accompanying figure), but the adits
were caved at this time.
In 1961, the property was leased to Consolidated Mining and
Smelting Co., who advanced the Redbird heading in the oxide zone about
800 feet, and completed 4,126 feet of diamond drilling.
The drilling
showed "strong and apparently continuous oxidized zinc-lead
mineralization of ore grade", but no sulfides were encountered and the
lease was relinquished.
r
[ 6
III
]
In 1973, under an agreement with Hecla, Reeves MacDonald Mines
advanced the hsading of their 800 level in the Annex mine an
..
additional 700 feet into the Red Bird property.
From this heading, 15
diamond drill holes totalling 6200 feet were completed.
From the
face, 4 diamond drill holes encountered four separate bands of
zinc-lead mineralization each 20 feet wide, averaging 4.18 X Zinc,
0.12 X Lead, 0.56 oz/ton silver and 0.04 X Cadmium, similar grade to
..
ore being mined by Reeves MacDonald.
The Reeves MacDonald Mine closed
in 1975, and nothing further was accomplished on the Redbird property.
The 16 crown-granted mineral claims comprising the Red Bird
property are now owned by Diem Mines Ltd., of Nelson, B.C., a
subsidiary of Hecla Mining Company, of Coeur dlAlene, Idaho.
The Nor claims were staked in 1981 by Gerry Klein, P.Eng., who had
....
...
been mine geologist at Remac, and who recognized the potential for
sulphide ore at depth on the Red Bird property •
In 1985, Golden Eye Minerals secured a lease on the Red Bird,
...
Grouse and Caviar properties property from Diem Mines Ltd., and an
option on the Nor Claims from Klein.
...
The Red Bird property is situated near the south end of the
"Kootenay Arc", described by Fyles and Hewlett (1959) as a curving
....
belt of limy sedimentary rocks of early Paleozoic (mainly Cambrian)
age folded around the Cretaceous Nelson and Kuskanax Batholiths.
The
Kootenay arc is characterized by significant Zinc-lead-silver deposits
-
in Cambrian "Reeves" or IIBadshot" carbonates extending from the Lead
Point area, near Northport, Washington to the numerous deposits north
..
..
MAJOR STRUCTURAL UNITS
OF THE
SALMO LEAD-ZINC AREA
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, NTERNATIONAL
BOUNDARY
LEGEND
...
Mesoloic volcanic rocks
Cambrian sedi men tary rocks, (Quartz Ite Ranoe
and Reno formations, Laib group)
Ordovician (?) black argillite (Active(?) formation)
Cambrian sedimentary rocks, (Quartzite Range,
Reno and Nelway formations, and Laib <;lroup)
Granitic rocks
-
Major thrust faults
Transverse faults
Lead- Zinc orebodies
GOLDEN EYE MINERALS LTD.
SA.L(\/\O
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REGIONAL GEOLOGY
-
-Aug 1985
FIG.3
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Sheep Creek Anticline. South Side of
South Salmo River
Formation Member
APproxi-1
mate
Thickness
(Feet)
Top not
exposed.
Nelway.
500 (1)
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Reeves MacDonald Mine Area, Composite Section
APproXi-1
mate
Thickness
(Feet)
Lithology
Lithology
Grey dolomite containing distinctive
black masses with small white spots.
I Dark
limestone
Grey calcareous phyllite, grey brown and
green phyllite; thin calcareous lenses.
Top not
exposed.
IR~~~
450
Brown-weathering grey siliceous argillite.
Grey, poorlv banded limestone.
200-300
350
Trum--;;-
350
Green phyllite.
Emerald.
I
Truman Hill-.Emerald Mine Area, Composite Section
3,000
Upper
Laib.
,
APprOXi-1
mate
Thickness
(Feet)
Lithology
blue-grey fine-grained
with thin argillaceous beds.
Gradational contact.
Laib.
f
100
I
Grey anb· brown micaceous quartzite; Top not
minor green phyllite, black argillite, and exposed.
limestone.
Black calcareous argillite.
I
500
Interbanded white grey and black crys- I
130
tall.ne limestone.
Green and grey phyllite, grey and
brown m;caceous quartz.te. minor limestone lenses.
Black, crenulated calcareous phyllite.
Banded grey and white limestone.
Brown skarny calcareous argillite.
Green and brown phyllite, white limestone.
60
Brown micaceous arg;llite.
Grey-green and brown phyllite. with calcareous lenses most common near the
base.
Brown argillite with thin calcareous beds.
10-20 feet of white crystalline argillaceous
I
Reno.
limestone.
Conformable contact
it
\
.
I
Blocky grey quartzite, of which the
upper 30 feet contains coarse calcareous
quartzite; cross-bedded.
40-50
Up"",
Reno.
60
Blocky grey quartzite with lenses of calcareous quartzite, micaceous quartzite,
and minor limestone.
S-tO
Blocky grey quartzite.
Lower
Reno.
560
Grey micaceous quartzite and dark-greY
to black phyllite.
500
Grey-brown to grey micaceous quartzite
with grey blocky beds near t:le ba~e
230
Dark-grey micaceous quartzite Interbedded with dark-grey to black phyllite.
Upper
Navada.
250
White quartzite beds as much as 2 feet
thick.
135
White quartzite, beds less than 1 foot
thick.
Lower
Navada.
400
Thin-bedded I!reyish-wh:te quartzite and
dark grey-brown micaceous quartiite,
some greenish-grey phyllite.
100
Brown micaceous quartzite with greyishwhite beds.
I
Conformable contact
Quartzite
Range.
35
100
Thin-bedded white quartzite.
White grey and brown quart7ite inter-
bedded with grey and green phyll:te.
._----_. --------------------------
65
Greenish
quartzite.
phyllite
and
grey-brown
------_. -------------------------20
Interbedded grey and white limestone
and greyish-brown phyllite.
-._---_. -------------------------100
NURget.
":.L.'-jLU.. l:.
Base not
exposed.
Massive white quartzite.
Base not
exposed.
Nugget (1) massive white quartzite.
Base not
exposed.
Greyish-brown phyllite and quartzite.
Massive white quartzite.
Coltmnar sections of Canbrian rocks, Salno area (from Pyles and Hewlett, 1959).
r--
LAtS FORMATION
GEOLOGICAL MAP
OF
§§I UPPER
THE
SALMO LEAD-ZINC AREA
WEST KOOTENAY DISTRICT
BRITISH
Scole
1000
0
1000
Contour
LAIS UN DIVIDED: ph),ll i te. sc hisi. micaceous quartzite.
and minor
3000
Interval
200 feet
~EM£RAlD MEMBER: block phyllite and crgillite
a!:J REEVES
MEMBER: grey limestone. minor dolomite
:~ TRUMAN MEMBER: phyllite and argillite ..... ith lenses
COLUMBIA
ZOOO
limestone
400{'l
5000
of limestone
Feet
~
RENO FORMATION; grey blocky and grey micaceous quartzite
OUARTZITE RANGE FORMATION
Geology by J.T.Fyles and e.G. Hewlett 1952-1955
~;:s_~
~NAVADA
-IP~® NUGGET
MEMBER; white quartzih and brown micaceous
MEMBER: white quartzite
=
GOLDEN EYE MI NERALS LTD.
RED
=f.-~_~
MAY 1985
BIRD PROJECT
,
FIG. 4
..
[
of Revelstoke.
7 J
Metamorphic grade in the zone varies from chlorite
assemblages to sillimanite zones •
Deposits occur at several
stratigraphic levels within the belt and vary from replacement
III
deposits to metamorphosed sedimentary exhalative deposits; these are
well described by Muraro,
..
(1966) and the major deposits are shown on
the accompanying Figures.
§~QbQ§Y_QE_I~~_8~Q_~18Q_EBQE~BIY~
The Red Bird deposit occurs at the southwest end of liThe Mine
Belt
..
ll
,
a broad zone of Proterozoic to Ordovician rocks bearing
stratiform zinc-lead-silver deposits that have been folded and
cut by transverse, normal and thrust faults.
Stratigraphy in the Red Bird area, as shown in the accompanying
..
..
stratigraphic column, includes the lower Cambrian Quartzite Range
Formation, and the Reno and Laib Formations, in ascending order. To
the south and west, the Ordovician Acti.ve Argillite is thrust over
the Cambrian rocks.
The Laib Formation is subdivided into the Emerald schist, Truman
-
Argillite, Prospect Dolomite, Reeves Limestone, and Upper Laib Member.
Dolomitized portions of one band of the Reeves Limestone are the
m~in
hosts for the zinc-lead mineralization, although less important
deposits are also known in the Prospect Dolomite and Nelway
Formations.
Deposits in the area, mined from this band of the Reeves
Member include the Emerald and Jersey mines, (Placer Development Ltd.),
the H.B. Mine (Cominco), the Reeves Macdonald Mine and the Red Bird
Deposit, as shown on the accompanying generalized geological map.
The mineralized zones in the Reeves Member are stratabound massive
..
..
..
-
[ 8
sulphides surrounded by dolomite. Origin of the sulphide zones is
uncertain; some sections have characteristics of sedimentary
exhalatives, but textures and alteration patterns indicative of
replacement may also be present. The Reeves Ore Zone had a total mined
and explored length of 6500 feet, with further plunge extensions
likely.
Other mineralized zones thought to have the same plunge are
the Annex, Annex West, and Redbird Zones, all of which are thought to
correlate with oxidized mineralized horizons present on the Reeves
MacDonald claims (see Long Section).
The mineralized zones occur in one particular band of the Reeves
Member on the south limb of a regional anticline, the Salmo River
anticline, mapped by Fyles and Hewlett.
At least three other
carbonate bands are correlated with the Reeves member, but only the
Prospect Dolomite has significant mineralization.
-
]
The bands are
thought to represent repetitions by folding and faulting.
Dominant structural features east of the Red Bird property are
transverse normal faults, which have the effect of displacing the
-
orebodies to a higher elevation, providing better conditions for
mining than
~f
the orebodies had continued unbroken. A transverse
fault originally postulated to occur within the Redbird property has
been disproven by Drillholes 86-2 and 3, and there is now a strong
probability that all four mineralized zones, the Reeves, Annex, Annex
West and Red Bird zones continue unbroken along the plunge extending
throughout the property.
At least two additional zones, the Beer
Bottle zone and an un-named zone to the west, are thought to be
faulted sections of the Red Bird zone.
The relationship of these
zones is shown in plan and section in the accompanying figures.
...
[ 9 ]
The entire Cambrian sequence is capped by the thick graphitic
phyllite unit known as the Active argillite (Ordovician), separated
.
.
...
from the older units by a low-angle thrust fault •
In 1985, Golden Eye Minerals extended a logging road from Church
Creek valley toward the Redbird property, and this road was extended
to the Red Bird showing late in 1985 and early in 1986 by Teck
Explorations Ltd. prior to their drilling program.
Funds expended on
road building and reclamation in 1985 and 1986 were $ 43,985.26.
Core drilling at the property began Jan 6, 1986 and finished March
18, 1986.
Six holes were drilled, but only three of these were
completed to depth,
..
(three were abandoned because of drilling
problems).
Drilling Data are as follows:
DRILLHOLE
ELEVATION
LOCATION
AZIMUTH
INCL.
DEPTH
===============================================================
GE 86-1
3343.31
971.52N/
983.25E
340
-60
384 FT
GE 86-1A
3368.59
991.11N
1017.15E
340
-73.5
569 FT
GE 86-2
3570.02
1361.84N
1057.14E
332
-80
2464 FT
-
GE 86-3
3570+/-
1361.8N
1057.1E
..... ·oJL
~'"":!",..,
-67.5
2203 FT
-
GE 86-4
3520.27
1647.98N
2711.92
340
-80
755 FT.
GE 86-5
3494.65
1909.12N
2572.96E
340
-81
2454 FT
-
-
==================================================================
6 HOLES
TOTAL
8829 FT
-
[ 10 ]
Q~i!!bQ!g§_!_~ng_!a~
on Nor 3 claim near West Russian Creek were
drilled to intersect the down-dip projection of the Redbird oxide
zone; both holes encountered bad ground and excessive water and had to
be abandoned prematurely.
(Betmanis, 1986).
Q~i!!bQ!g§_~~ng_~ were
drilled from the same location above the
iIIII
..
..
-
..
-
-
-
previous two holes.
Prospect dolomite.
Weak zinc mineralization was intersected in the
Three separate bands of mineralization from 3.5 to
5 feet thick assayed from 1.24 to 4.20X zinc. in DDH BE 86-3.
core logs in appendix).
(see
No mineralization was encountered in the
Reeves member, but a strong strike-slip fault is postulated to have
displaced the Red Bird zone easterly.
QLi!lnQl~_~,
about 500 meters to the east was drilled to test the
revised interpretation but was
.abandoned when drilling problems were
encountered in the Argillite Fault.
QLillnQl~_~,
collared about 100
me~ers
north (see drill Section),
at a steeper angle, sucessfully passed the fault, and encountered a
thick section of Reeves member, near the base of which an oxidized
zone of mineralization from 2264 to 2312.8 feet
(54.8 feet) assayed up
to 7.20 X Lead and 8.95 % zinc, with up to 0.83 oz/ton silver,
indicating oxidized massive
~ulphides.
The 5 assay samples of
oxidized mud with dolomite and sulphide fragments average about 10 %
combined lead-zinc, but can not be considered representative,
considering poor core recovery.
The 5 foot section of dolomite with
sulphides directly below the oxidized material assayed 5.64 X zinc,
0.38 X lead, 0.31 oz./ton silver and 0.06 X cadmium.
The material is considered to be the oxidized Red Bird zone,
perhaps faulted as well, representing a technical drilling success.
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RED. BIRD PROJECT
DRILL HOLE LOCATIONS
PEND D'OREILLE RIVER
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FIGURE 6
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....
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[ 11 ]
Overall cost of the initial drill program was in the order of
$400,000 (funded by Teck Explorations Ltd.>, of which $343,919.65 was
filed for assessment purposes in 1986.
12§~=12§Z_~XebQBeI!Q~_eBQ§Be~~
With funding provided by Knights Mineral Partnership Ltd. and a
Provincial Government IIFAME" grant, a drill program of two holes
commenced November 15, 1986 and was completed February 12, 1987.
-
Drillhole 86-6 was spotted at 3300 feet elevation, 260 feet west
of the southeast corner of the Royal Fraction Claim (Lot 14155>.
The
hole was started at azimuth 330 degrees and inclination -80 degreees;
at total depth 3313, Sperry Sun instrument readings indicate azimuth
337 degrees and inclination -57 degrees.
The drillhole cored the expected sequence; Active Argillite to 899
feet, an unnamed Limestone unit 899 feet to 921 feet, a major fault
from 921-929 feet, Emerald schist from 929-951 feet, Truman Limestone
and schist from 951-1186, Prospect Dolomite from 1186 to 1684 feet,
Faults and argillite from 1684 to 1765, The IIArgillite Fault",
Emerald Schist from 1765 to 2667, argillite from 2667-2677, Truman
Limestone from 2677-2687, Reeves Member (Limestone and Dolomite) from
-
2687-3204, and Truman Limestone and Schist from 3204 to the end of the
hole at 3313.
Drillhole
86-6~
intended to test the Redbird mineralized zone
below the oxidized intercept in DDH 86-5 evidently was steeper than
anticipated, and passed below the plunge of the mineralization by a
distance estimated by Klein to be 400 to 600 feet.
Scattered
mineralization was present in the Prospect Dolomite, and a narrow
section of up to 20% pyrite with minor sphalerite and galena from 3187
-
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FIGURE 8
Dian-w()"J Dri H ,",ole
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FIGURE 9
...
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....
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....
-
[ 12 ]
to 3191.7 returned sub-economic values.
This narrow zone may
represent the Redbird mineralization beyond the ore-shoot •
Q~i!!nQ!g_§Z=l~
was collared Jan 15, 1987 and completed Feb 4, 1987
at a total depth of 3250 feet.
This hole, roughly 1600 feet east of
hole 86-6 was selected to intercept the IlAnnex
mineralized zone about
ll
500 feet down plunge from known mineralization in the most westerly
heading of the Reeves Macdonald IlAnnex
ll
mine.
was 330 degrees and inclination -73 degrees.
Azimuth at the collar
At depth 3030 feet the
final Sperry-Sun test indicated azimuth 338 degrees and inclination.
The section cored was comparable in stratigraphy with the previous
hole; with the following sequence:
0-1077
1077-1153
1153-1205
1205-1731.5
1731.5-2205
2205-2278
2278-2843
2843-3250
Active Argillite;
Limestone, dolomite, schist
Emerald schist
Truman Limestone and schist
Prospect Dolomite
Argillite
Emerald phyllite
Reeves Member
The hole encountered significant zinc mineralization in the
Prospect Dolomite, with the following mineralized intervals:
Intercept
Pb %
Zn
'X.
Ag (oz / t )
Cd %
Ge ppm
-----------------------------------------------------------------1733.3-1766.8
0.03
2.26
0.02
N.A.
15.5
(33.5 ft)
0.03
1767-1789
0.03
1.73
N.A.
19.0
(22 ft)
0.05
1.95
1827.5-1828.5
0.07
N.A.
10
11.21
0.07
1852-5-1857.5
0.11
N.A.
15
3.60
0.06
1862.4-1863.6
0.08
N.A.
4
1893.4-1901
0.02
2.07
0.02
8.3
N.A.
1915-1916.5
0.02
1.88
0.06
7
N.A.
2098-2102.2
4.26
0.09
2
0.15
N.A.
2125.5-2128.9
0.04
2.06
0.01
N.A.
1
2
2154-2157.5
0.09
1.58
0.03
N.A.
0.06
0.01
N.A.
1
2169-2171
2.12
1
2173-2176.6
0.69
0.01
N.A.
0.02
================================================================
[ 13 ]
-
-
2205 feet
(Total thickness 473.5 feet).
The unit consists of light to
dark grey dolomite with a thick cherty layer in the middle.
Minor
solution cavities are present and a "Tweedy' texture is common.
Bands
of massive sphalerite and pyrite are present and a total of 86.2 feet
of the Formation is mineralized in many separate bands.
The wide section at the top of the unit, from 1733.3 to 1789 feet
-
-
-
(54.5 feet thick) averages 2.06 percent zinc, with very minor lead,
silver and germanium values.
The best section, a 5 foot zone from
1852.5 to 1857.5 feet averages 11.21 % zinc.
This is the only section
that appears to be of ore-grade, but persistence of the mineralization
suggests proximity to an important economic zone which must be further
tested, perhaps by wedging from existing drillholes.
of the hole at 3250 feet ()393 feet thick) has an upper section (21.5
feet) of limestone, and the balance is massive to blocky dolomite with
IITweedy" texture., host to an important, thick mineralized zone.
The
zone, from 3080.9 feet to 3134.7 feet (53.8 feet) assays as follows:
Ag (oz/t)
Cd %
Be ppm
Intercept
Pb %
Zn 'Y.
==================================================================
0.87
7.97
1.64
22.7
3080.9-3134.7
0.085
(53.8 ft)
including:
29.25
1.64
10.0
2.21
.10
3099-3125
(26 ft)
===================================================================
r
1-_
h
'ACTIVE ARGILLITE
7_ -
3000FT
SCALE
o
1--=:1
1000
led
2000
3000
FEET
1
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/IQ9~~ Zn /11.5'
'"
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•
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.
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REDBIRD 6.5%Pb,IB.5%Zn
600'x 20'
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REEvES
REDBIRD
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ANNEX
:::1::
:r a:
EXISTING DRILL HOLES
PROPOSED DRILL HOLES
Red
LONGITUDiNAL
B~rd
ProjecT
SECTION, Lookln'} NorTh
HGUHE lS
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FIGURE 12
[ 14 ]
EXPLORATION POTENTIAL:
Combination of previous exploration data and information from
..
..
..
recent diamond drilling by Golden Eye Minerals Ltd. enables projection
of at least four potentially productive mineralized zones on to the
Red Bird claims.
Arbitrarily a 2000 foot plunge dimension (rake>
is chosen for calculating potential. Tonnage potential and Gross
Metal Value for each of the four zones is shown on the following
table, with the following metal prices assumed: Lead-$0.345 lIb; Zinc
-
- $0.505/lb/; Cadmium - $1.25/lb.; Silver - $7.35/0z. Germanium -
..
======================================================================
..
$1060 U.S./kg •
MINERA~IZED
ZONES - RED BIRD/NOR CLAIMS
RED BIRD
ANNEX
: ANNEX WEST :
K-ZONE
======================================================================
...
GRADE LEAD
6.5
1.0
3.5
1.5
GRADE ZINC
18.5
8.0
3.5
4.5
...
GRADE CADMIUM
.10?
0.09
0.02
0.02
GRADE SILVER
2.0?
2.5
1.0
0.30
GRADE GERMANIUM
50
22
?
WIDTH
20
45
-
20
?
20
TONS/VERT.FT
1,200
2,700?
TOTAL TONS
2.4 M
2.7 M
1.4 M
1.8 M
G.M.V $/TON
$235
$109
$67
$68
GROSS VALUE
$560 M
$94 M
$122 M
$294M
700
900
======================================================================
TOTAL GROSS METAL VALUES ALL ZONES: 1,070,000,OOO.in 8.3 Million Tons.
[
....
15 ]
EBQ§E~~I_IQ~~!.
Some potential for mineable ore exists in the Prospect Dolomite,
..
since the discovery in DDH GE 87-1 of wide sections of near ore grade
-
~e~leB_EBgE~BIY!.
-
material.
The 16 crown-granted claims comprising the Caviar prospect are
owned by Diem Mines Ltd., wholly-owned <since 1981) Canadian
subsidiary of Hecla Mining Company., and are included in the lease to
Golden Eye Minerals Ltd.
..
-
Surface zinc mineralization is exposed for a length of 150 feet
and widths up to 20 feet.
Four holes were drilled, the best
intersection being 20 feet assaying 6.5% zinc.
This zone is open to
the west and down plunge.
Little is known of this zone, or its relationship to the other
-
mineralization in the area.
Exploration is warranted.
~I~I~§_~Q~~IIIQ~§:
The orebodies at the Reeves Macdonald mine lent themselves,
because of their steep dip, good width, and favorable ground
conditions, to low cost sub-level benching and blast-hole mining
methods.
Direct operating costs, inclusive of mining, milling,
development etc. in June 1973, were $10.62 per ton on a throughput of
approximately 18,000 tons.
The orebodies were capable of being mined
at the rate of one vertical foot per day and milling averaged 1200
tons per day.
Present mining costs have not been calculated, but modern bulk
mining methods could be used.
adjacent property.
A tailings pond area is present on the
( 16 ]
~Q~~bY§!Q~§_a~~_B~~Q~~~~QaI!Q~§~
The writer concludes that the Redbird property presents an
exceptional opportunity to develop economically mineable reserves in
an area where logistics are favorable and mining conditions are
..
excellent •
The property may contain the nearest zinc-rich reserves to
the zinc smelter at Trail.
It is recommended that at least six more deep drillholes be
..
..
..
completed to test plunge extensions of all four mineralized zones.
these drillholes are
successful~
If
calculation of probable reserves and
a mini-feasibility study could indicate that underground development
and exploration and environmental studies should
begin~
with a view to
economic production of zinc-Iead-silver-cadmium-germanium from an
underground mine.
The possibility that near surface oxide material
may be treated should not be completely ruled out, as large reserves
...
of oxide material are certainly present •
It is likely that an early start on environmental work would be
worthwhile.
Additional geological mapping should be done during the
next summer season, and initial
metta~urigical
testing of mineralized
material would be useful.
It is recommended that orthophoto basemaps be prepared and
additional surveys be done to tie in roads, drillholes and claim posts
with as much accuracy as possible and to aid in surface geological
mapping and preparation of reserve estimates.
...
...
...
[ 17 ]
The preferred targets for exploration are the massive sulphide
zones of the Red Bird and Annex areas.
Proposed exploration is by
surface diamond drilling, construction of an exploration/haulage
heading, and underground diamond drilling.
...
Initially, at least 5
surface diamond drill-holes are necessary to determine continuity of
all of the mineralized zones.
Estimated costs of the next two stages
of exploration are as follows.
...
-
STAGE I
Road Building
Geological work
Diamond Drilling 18,000 ft @ $35
Assaying, Met~a~urgical
Misc. Costs
Consulting and Supervision
$ 30,000
15,000
630,000
10,000
25,000
~~~QQQ
Contingency 207..
TOTAL
.755,000
145,000
$900,000
STAGE II:
Combined exploration/haulage drift
(6000 feet @ $300/ft.)
$1,800,000
Diamond drilling 25,000 ft @$20
500,000
Associated costs Hydro, overhead, Camp
and equipment.
1,000,000
TOTAL $3,300,000
STAGE I I I :
Feasibility Study
Permits, Bonds, Environmntal etc.
STAGE IV:
Mill Construction etc.
1,000,000
Costs not estimated
Respectfully submitted:
~I~I~~~~
__ - - - - - - - -
~~Price M.Sc ••
FGAC.
Consul ti ng Geolo . )~e( tti ;.. , ,
Feb 25 1987.
L~~'O~,'
-
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',",
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.
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F[LLO'~~ .
..
..
[ 18 ]
Betmanis, A.I., P.Eng., (1986);
Report on Diamond Drilling, Redbird
Group, Nelson Mining Division., Pend D'Oreille River.
Assessment
Report for Teck Exploration Ltd. dated May 27, 1986 •
Canadian Mines Handbooks, Misc.
Issues to 1985.
Dings, McClelland G., and Whitebread,Donald H.,(1965);
Geology and
Ore Deposits of the Metalline Zinc-Lead District, Pend Oreille County,
Washington. U.S.G.S. Prof. Paper 489.
Elson, M.,
1986.
..
..
(1986);
Redbird Project, Private Memorandum, Sept 17,
Fyles, James T., and Hewlett, C.G., (1959);
Stratigraphy and
Structure of the Salmo Lead-Zinc Area.
B.C.Department of ~ines
Bulletin No. 41 •
Green, L.H., (1953), Wall-rock alteration at certain Lead-Zinc
Replacement Deposits in Limestone, Salmo Map-Area, B.C., G.S.C.Bull
29,
Guinet, V., (1986);
Golden Eye Minerals Ltd., Company Review.,
(Private), September 18, 1986.
Hecla Mining Co.
..
...
...
Unpublished Company Documents, 1956-1977
Hecla Mining Co., (1977); Report on the Redbird Zinc Lead Property,
Remac, Nelson Mining District. B.C.
Internal Private Report.
Klein, G.H., P.Eng., (1986);
Redbird Project - Exploration Proposal
and Summary of Geology. Private Report to Golden Eye Minerals Ltd •
May 24, 1985.
Klein, G.H., P.Eng., (1986);
Redbird Project - Summary of 1985-86
Winter Program and Recommendations for Further Work.
Private Report,
April 1986.
Klein, G.H., P.Eng.,
Sections.
(1987);
Redbird Project - Core Logs and Drill
Little, H.W. (1960)
Nelson Map Area, West Half, British Columbia,
Geol. Surv. Canada Memoir 308, 205 pp.
...
Monger, J.W.H and Preto, V.A. (1972);
Geology of the Southern
Cordillera, Excursions A03 - C03, XXIV International Geological
Congress, pp.36-38.
Muraro, T.W., (1966); Metamorphism of Zinc-Lead deposits in
Southeastern British Columbia.
CIM Special Volume #8, pp 239-247.
Walker, J.F.,(1934); Geology and Mineral Deposits of Salmo Map Area
GSC Memoir 172
..
ACME ANALYTICAL LABORATORIES LTD.
_852 E.HASTINGS ST.VANCOUVER B.C. V6A 1R6
PHONE 253-3158
DATA LINE: 251-1011
ASSAV
-
DATE RECEIVED:
FEB 11 1987
DATE REPORT MAILEDf'...:M
7/0
!7jd.l ..
CERTIFICATE
SAMPLE TYPE: CORES
ASSAYER:
.A~.D~AN
TOYE. CERTIFIED B.C. ASSAYER.
GOLDEN EYE MINERALS
SAMF'LE#
FILE # 87-0306
Pb
Zn
Ag
Cd
'l..
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aZ/T
I.
.04
.09
.06
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2.06
1.58
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.02
.01
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.09
1.09
.54
.44
.45
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.04
.01
.01
.030
.010
.010
.010
.010
· 110
110
GE
GE
GE
GE
GE
1025
1026
1027
1028
1029
GE
GE
GE
GE
GE
1030
1031
1032
1033
1034
GE
GE
GE
GE
GE
1036
1037
1038
103
1040
.09 10.03
9.67
.31
1.06
4.87
9.01
1.80 11.35
1.35
.77
.09
2.00
2.50
GE
GE
GE
GE
GE
1041
1042
1043
1044
1045
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20
PAGE
1
ACME ANALYTICAL LABORATORIES LTD.
852 E.HASTINGS ST.VANCOUVER B.C. V6A lR6
PHONE 253-3158
DATA LINE: 251-1011
lilt
.
.
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ASSAV
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ASSAYER:
• •1..-.
•
TYPE: CORES
DATE REPORT MAILED:
AUI 10 GRAM REGULAR ASSAY
TOYE. CERTIFIED B.C. ASSAYER.
GOLDEN EYE MINERALS
FILE # 87-0190
Pb
Zn
Ag
'I.
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Ge
PPM
.03
.03
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13
7
15
16
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1.44
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15
17
20
24
16
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15
17
10
15
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GE
GE
GE
GE
1005
1006
1007
1008
1009
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GE
GE
GE
GE
1010
1011
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1013
1014
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2.26
GE
GE
GE
GE
GE
1015
1016
1017
1018
1019
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1.56
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.03 2.87
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GE
GE
GE
GE
GE
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1021
1022
1023
1024
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. 15
.06
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.06
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~
JAN 29 1987
CERTIFICATE
.q. DEAN
SAMPLE#
DATE RECE I VED:
. .:..-",-::-
2.78
2.84
~
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3.60
1.06
6.31
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1-.
----..
~
LEGEND
em Lompropnyre
REEVES MACDONALD MINE
dyke
w
o
o
o
PART OF THE 1900 ANO 2650 LEVELS
~
~ Sulphide minrrolizotioo
LAIB FORMATION
zoo
0
Scole
~ EMERALD MEMBER: block phyllih
200
400
FHt
~ REEVES MEMBER; 'imntonr
~
dolomih
w
o
o
o
~ TRUMAN MEMBER: gfeltn and brown phyllite and limntora
•
w
RENO fORMATION
o
o
~ Grey micocro\J!t quarhite
o
~
'...,
QUARTZITE RANGE fORMATION
~ NAVADA MEMBER: white. grey. and bro.... n micoctou!t quartzite.
gfeen phyllite. minor limestone
I
",aOON
I
3000N
'T,.
.j','I'.',',',
°"1'1""'1'
j',',1I
",,',',
~'NUGGET MEMBER: mouin .... hite quorhih
1,1,111,1 , ,1
- - Bedding fault
_'VW
Tron$vcnr fault
-
Diamond-drill holt. Horiz.ontol unless (lngle of inclination indicated
w
o
o
o
•
Rttvu
w
o
o
o
Orcbod)'
•
I
~lGURE
15
~Ofl[8QO\"
~"rr.V{$ll"'(ST~(ANO
~"'("'OlR
lflU"''''H
....
[ ] II(NO fORMATION
I4:1 DUA~lll'[
~A"IG[
\900 Lev
:f.ilUil.i.IUUUU .... ' .... ·
\
(
I
\1
I
ZOOON
-, /
,/
Isometric sketch of the Reeves orebody end its foulteE
segment~
F\G 3A
~
7
KooTENP\y'
ARC
Geo\o~'1 C\'t\& D.eP0C;l~.
Section A
;!'~~~v.~
Revelstoke
5 miles
Legend
PROPERTIES
I Lead Point Area
2 Ree"es-MacDonald mine
3 Jersey mine
4 H.B. mine
5 Duncan
6 Wigwam
7 R udd ock Cr.
o
c=J
Granite
~
Post- Reeves
[Z]
Reeves-Badshot
~
Pre-Reeves
20
,
I
Miles
R~D 8\R.t:>
Canada
U.S.A.
Figure 15-1
Map of the Kootenay Arc showing approximate distribution of the Lower Cambrian Badshot-Reeves limestone, pre-Reeves and post-Reeves metasediments and principal granitic masses.
Inset reveals style of folding near Duncan Lake. ~umbers locate deposits treated in text. Modified after Fyles, 1964.
~urt:U"o
19 b~.
FIGURE 14
1/-.'
---
[ 19 ]
aEE~~Q!X_!!!
GERMANIUM
§Q~8~~§£_8~~Q~~BY_~~I~QQ§_a~Q_~§~§
U.s STATISTICS
=======================================================
1984 (E)
1983
1982
=======================================================
REFINERY PRODUCTION
IMPORTS
26,000 KG
20,000 KG 20,000 KG
6,000
6,500
6,000
REPORTED CONSUMPTION
42,000
35,000
35,000
PRICE; U.S $ PER KG
$1,060
$1,060
$1,060
------------------------------------------------------Source: Mining Annual Review, 1985.
Germanium is considerably rarer than gallium, and makes up only
0.0004% of the earths crust. Up until the present, it has been
produced only as a by-product of smelting of copper and zinc.
From
zinc ore, germanium is volatilized during the refining process, and is
collected electrostatically.
In copper smelting it is collected
magnetically in flue dust.
These are leached with Hydrochloric acid
to form germanium tetrachloride which is hydrolyzed and reduced to
metal with hydrogen.
The metal is produced in the U.S. by Eagle-Picher and a subsidiary
of Union Miniere; elsewhere in the world it is produced by Union
Miniere, and such well-known metals producers as Pennarroya, and
Preussag, and others.
About 5% of production 'is used in electroni~s,
most is used in infra-red optics (important in military and civil).
New uses are in gamma radiation detectors, germanium-silicon
thermoelectric devices, and in fibre optics.
It is also used as a
catalyst in petroleum and polyester fibre industries and a high growth
usage is in polyethylene terephthalate, the plastic used in soft-drink
bottles.
Recent data acquired by Golden Eye Minerals Ltd. suggests that the
usage of germanium for semi-conductor technology may increase relative
to gallium in the near future, and consequently, forecasts for
germanium prices are optimistic.
[ 20 ]
APPENDIX IV
e~Je~~~I_~I~~Beb_~~EQ6II6_1~_I~~_~I~~_~~bI
B~~~~§_~e~~Q~ab~_~I~~6_bI~~
The presence of zinc-lead gossan zones on the Reeves-Macdonald and
Red Bird properties led to surface and underground exploration on
both properties in the 1920's; the mining of near-surface sulphide
mineralization in the Reeves resulted in the production of 7,252,000
tons of ore yielding 110,000 tons of lead concentrate, 499,000 tons of
zinc concentrate, 500,000 ounces of silver and 3,000,000 pounds of
cadmium prior to its closure in 1975.
In today's values, this
represents over $340,000,000 in production.
Four distinct zones were mined by Reeves Macdonald Mines Ltd.
Orebodies averaged 600 feet in length, were 20 to 30 feet in width,
had a steep plunge to the south-west, were mineralogically
distinguishable from each other and had distinctive metal ratios.
None of these zones were traced to mineralogical termination at depth.
The most westerly portion of the Reeves mine, known as the Annex
Zone contained more than double the grade of ore previously mined,
having a grade of 1% lead, 8.0% zinc, 2.5 ounces per ton silver, and
0.09% cadmium.
Plans and sections accompany this brief summary.
[ 21 ]
I~5_~5B§5Y_~!~5:
The Jersey Mine, situated 50 kilometers northeast of the Red Bird
prospect, comprises 56 crown granted claims and is owned by Placer
Development Ltd.
Between 1949 and 1970, the mine operated
suceessfully, starting at 300 tons per day production and increasing
to 2500 tons per day in 1969.
It was the first major mine in Canada
to adopt trackless mining methods.
During 1969 and 1970 production
increased from pillar recovery as the orebody was depleted.
Production ceased in 1970, and milling machinery was moved to the
adjacent Invincible tungsten orebody, which had been discovered in
1968, and production in 1970 amounting to 430 tons per day came from
the rehabilitated Dodger orebody, as the production shaft had not yet
reached the Invincible ore.
The concentrator was located on the highway south of Salmo but the
mine offices, plant buildings, 60 company residences, and a school
were located at the 4000 ft elevation on Iron Mountain.
The zinc-Iead-silver-cadmium ore occurs at the base of the Reeves
Limestone member of the Laib Formation, concentrated in the western
limbs of two fold structures, which are overturned to the west.
The
"A" zone (the more westerly), has an axis striking about due north,
and consists of several ore bands up to several feet thick, with an
overall thickness of 80 feet.
Trough
II ,
complex.
The eastern structue, the "Dodger
has an axis striking North 15 degrees east, and is more
The ore occurs as a variety of band lenses and mantos which
dip from flat to 30 degrees easterly.
[ 22 ]
Mining was by open stope methods.
to the Bunker Hill Smelter at
Kellog~
Lead concentrates were shipped
Idaho, and zinc concentrates
were shipped to the Anaconda Smelter at Black Eagle, Montana.
In 1967
there were 225 men employed, 94 of whom worked underground.
I~~_~~~~_~I~~
The H.B.Mine, operated from 1955 to 1978 by Cominco (originally
Consolidated Mining and Smelting Company Ltd.), is situated on the
west side of Aspen Creek, on the north side of Sheep
Creek~·
7 miles by
road from Sal mo.
The ore occurs as a sphalerite-galena -pyrite replacement of
dolomite in the Reeves member of the Laib Formation.
Several types of
are zones are present; the No 1 zone - the main productive zone was a
steeply dipping lens with a long axis plunging gently to the south.
Several flat-lying tabular zones
occur~
and the Garnet zone outcrops
at surface, where it was mined by open pit; the same zone was mined
undergound by long hole methods. Ore production began in 1955 at a
level of 1000 tons per day.
Although ore reserves were not exhausted,
the mine was closed down November
prices.
1~
1966, because of low metal
Production resumed in 1973 and continued to August 17, 1978,
when the mine was permanently closed.
From 100 to 130 people were employed, about 28 of whom were on
Staff payroll.
Concentrates were shipped to the Trail Smelter.
amounts of gold were recovered in 1975 and 1976.
Small
[ 23 ]
SAl"O AREA "INE PRODUCTION
===================================================================================================
TONS
MINE
YEARS
PRODUCTION
ZINC LB.
LEAD LB.
SILVER OZ
SRADE
GRADE I
GRADE OllT
~
CADMIUM LB. BROSS VALUE
$
GRADE X
===================================================================================================
REEVES HAC
7,232,000 541,850,405
142,625,454
1,572,173
$322,872,863.
3,000,000
1
(TO 1975)
H.B.
3.74'1.
7,282,997 648,186,804
(TO 1978)
JERSEY
(TO
135,463,744
4.45'1.
0.93'1.
0.21 OZIT
1~954,868 1
0.12
0.013'1.
f
231,000,000
600,000
7.19'1.
1.85'1.
0.09'1.
1,702
?
?
0.02%
875,376 1
6,256,000 490,000,000
1966)
RED BIRD (1974)
O.9BX
$367,456,960.
1
3,730,000
$312,845,000.
0.030%
?
?
===================================================================================================
SOURCE: ANN REPTS MINMINES, CAN MINES HANDBOOK
[ 24 ]
KETAlINE AREA "INE PRODUCTION
--------------------------------------------------------------------------------------------------'tINE
YEARS
TONS
PRODUCTION
ZINC
LEAD
SILVER
6RADE X
GRADE 1
GRADE OllT
t
COPPER
f
BROSS VALUE
$
GRADE Z
===================================================================================================
PEND D,OREILLE 5,451,328. 281,290,369
145,362,573
257,226
2.58%
1.331
0.047
0.002%
2,347,974 139,344,708
64,394,015
76,261
152,983
2.96k
1.37%
0.032
0.003
36,944,947
10,346,736
9,710
202
4.28%
1.20%
0.022
0.00005
(1924-1956)
GRANDVIEW
~ETALlNE
431,480
201,648
$179,056,176.
$86,449,903.
$21,132,123.
===================================================================================================
SOURCE: US6S PAPER 489
NOTE: METAL PRICES
ASSU~ED;
ZINC - $O.SO/LB, LEAD-$O.25/LB, SILVER $7.50/0Z, CADMIUM -$1.50/LB
CALCULATED IN CANADIAN DOLLARS
GEOLOGICAL SUMMARY
B~Q_~IBQ_~!EbgBaIIg~_EBgJ~~I
SALMO MINING CAMP - NELSON M.D.
SUMMARY
This report details exploration results from the IIRed Bird
ll
stratabound sulphide zinc exploration project on claims adjacent to
the Reeves Macdonald Mine, a long term producer of zinc, lead and
silver located 25 miles east of the Cominco Trail Smelter in the
prolific mine-making southern portion of the Kootenay Arc.
Golden Eye Minerals Ltd. can earn an
80~
interest in Hecla Mining
Company's Red Bird property which contains the high grade Red Bird
Deposit and adjacent Beerbottle, Annex, Prospect, and suspected Annex
West and Reeves zones that are plunge continuation of zones mined at
the Reeves McDonald Mines.
Additional ground has been staked by the
company adjacent to these prospects.
The mineralized zones are massive to disseminated base-metal
sulphides in stratiform tabular bodies striking southwest, dipping.
steeply southeast and plunging southwesterly within dolomitized IIReeves
Member
ll
limestone of the Cambrian Laib Formation.
From November 22, 1985 to March 23, 1986, a total of 6 diamond
drill holes totalling 8924 feet were completed under an exploration
agreement with Teck Corporation, at a total cost of approximately
$400,000.00
From November 1986 to February 10, 1987, an additional two deep
drill-holes were completed by Golden Eye Minerals Ltd., with financing
provided by Knights Mineral Partnership, and a FAME grant from the
Provincial Government ($80,000). A ninth hole, funded by a private
placement, is currently drilling.
The project has been successful in locating zones which may
provide substantial tonnages of excellent grade zinc with associated
lead, silver, cadmium and germanium values.
Recommendations are made for at least 6 additional deep drill
holes to be followed, if results warrant, by underground development
and exploration.
~~~-----------Barry J.Price, M.Sc.
Consulting Geologist.
Feb