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MAP NO:
ASSESSMENT REPORT
PROSPECTUS
CONFIDENTIAL X
OPEN FILE
1OSD/02
REPORT FILED UNDER:
DATE PERFORMED:
LOCATION:
DOCUMENT NO:
093215
MINING DISTRICT:
WHITEHORSE
TYPE OF WORK:
GEOCHEMISTRY
FEATHER GOLD RESOURCES CORPORATION
DATE FILED:
AUG/93
LAT.:
LONG.:
60°05’
134040!
APRIL 29,
AREA:
1994
MONTANA MOUNTAIN
VALUE $:
N/A
CLAIM NAME & NO.: BARB 1—34 (YA86607—40), RAT 1—12 (Y312725—36), RAT 13—29 (YB131O1—17), MON 1—16
(YA$2825—40), TB 1—6 (YA82967—72), NYAK 1—4 (YA82997—3000), NYAK 5—48 (YA85201—44), JEAN (L202)
19237, KODAK (L2O3) 18304, HAZEL H (L205) 19285
WORK DONE BY:
T,L. SADLIER-BROWN
WORK DONE FOR:
FEATHER GOLD RESOURCES CORPORATION
DATE TO GOOD STANDING:
REMARKS:
GEOCHEMICAL SAMPLING & PROSPECTING TO DEFINE A DRILLING
PROGRAM PERFORMED IN SEPTEMBER 1993.
ASSESMENT FOR THIS PROPERTY IS
BASED UPON THIS DRILLING (SEE REPORT 093216)
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SUMMARY
Feather Gold Resources Ltd. holds 136 mineral claims and
Crown Grants at Montana Mountain near Carcross, Yukon.
They
include the Barb, TB, Rat, Man, Nyak, Jean, Hazel M and Kodak
claims which cover a nunther of gold and silver prospects.
Areas covered in part by the Barb, TB, Rat and Jean claims
were evaluated during June and August of 1993 at which times
a total of 48 samples were taken and analyzed by fire assay
(for Au and Ag) and ICP methods (for Ag, As, Bi, Cd, Cu, Hg,
Mo, Pb, Sb and Zn).
The property lies between elevations of about 1400-2200 in
above
sea
level
and
is
entirely
above
timberline in
moderately to steeply-sloping
terrain,
mostly within the
drainage basin of Big Thing Creek, which flows easterly to
Windy Arm on Tagish Lake.
The region was first explored for gold and silver during the
late 19th century and by about 1906, numerous gold and silver
occurrences had been discovered and staked.
Betv~een 1909 and
1921,
limited production was obtained from several early
discoveries including the Big Thing Mine which adjoins the
Feather Gold property.
In the late 1960s and early 1970s the
Big Thing deposit was redeveloped as the Arctic Mine and saw
a brief period of production.
The Jean Claim was staked to cover a high nc~g~g1dquartz
vein in 1936 and during the late 1950s and early 1960’s, a
20Th adit was driven in an unsuccessful attempt to intersect
the vein,
Subsequent exploration
included underground
drilling by Arctic Gold and Silver Mines in 1967 and a
comprehensive program of bulldozer trenching, prospecting,
mapping,
road construction,
soil and stream sampling and
additional diamond drilling by Anoorag Resources in 1984 and
1985.
The project area lies within the rocks of the Coast Plutonic
Complex where they are intrusive into the dominantly Hë~ö7i51c
bI~a~jicrocks of the Nisling Terrane.
The eastern limit of
the claim area is traversed by the Nahuin Fault, an easterly
dipping thrust fault which superimposes Paleozoic volcanic
and sedimentary rocks of the Cache Creek Group over the
Mesozoic Nisling rocks.
The mineral occurrences are all
hosted by the mid-Cretaceous granitic rocks of the Montana
Mountain Pluton which are in both intrusive and fault contact
with the intermediate volcanic rocks of the Montana Mountain
Volcanics.
All of the observed mineralization is in quartz veins and
stringers usually associated with zones of hydrothermal
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136,000 tons and the potential for the immediate mine area
could be 1,000,000 tons.
As it appears likely that the mineral occurrences in the
Ridge Zone represent a westward extension of the vein system
at the Arctic/Big Thing Mine continued exploration work is
strongly reccommended.
The objective of this work should be
to identify and de1ineat~ one or more intermediate tonnage
vein type gold-silver deposits.
Initial work should include:
1)
a preliminary diamond drilling program totalling
about 300 m oE drilling in 3 to 5 holes;
2) continued excavator and bulldozer trenching;
3) geological mapping, sampling and survey work.
An estimate of the cost of carrying out this work during the
fail of 1993 is on the order of $80,000.
The Rat Claim Area contains a number of good Au Ag prospects
which returned assay values grading up to O~645 ct/ton and
further exploration work in this area is justified.
This
should include additional trenching, prospecting, rock and
soil sampling and geological mapping and warrants provision
of a budget on the order of $5,000.
Sample taken from the Jean Vein and Lower Trench Areas gave
were
found to have very high precious metal values.
Material obtained from rubble in a trench on the Jean Vein
contained respectively 12.018 & 7~542 oz/ton Au and 2L1 &
7.6 az/ton Ag and loose mineralized material from the Lower
Trench Area contained respectively O~99O & 1.470 az/ton Au
and 4~B & 1.7 oz/ton Ag.
The mineral occurrences in the Jean Claim area all lie within
an elongate multi-element geochemical anomaly extending from
the Jean Vein exposure about 450 in northwest to below the
Lower Trench.
The mineralization, however, appears to occur
in narrow and discontinuous veins and, accordingly, the area
is not presently considered a high priority site for further
work. Any follow-up work should include detailed geological
mapping in order to develop an interpretation of the geology
as an aid in identifying targets for any additional testing.
Provision for a preliminary survey expenditure of $4,500 is
recommended.
The total reccommended expenditure for the next phase of
explortation work on the property is $ 89,500. The immediate
emphasis should be on the Ridge Zone as it appears to hola
most promise for a significan discovery.
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1.0
INTRODUCTION
1.1
Terms of Reference and Scope of Report
Nevin
Sadlier—Brown
Goodbrand
(NSBG) was
by the
management
of
Feather
Gold Ltd.
Resources
Ltd. retained
to
prepare
a
preliminary
geological
and
economic
evaluation
of
the
Company’s
holdings
in
the
Montana
Mountain
area near
Carcross, Yukon Territory.
The objective of the evaluation
was to characterize the mineral occurrences on the claims and
to
prepare
a
set
of
recommendations
for
such further
exploration,
development
and engineering work
as may be
required to establish reserves and, if advisable, advance the
property to the pre—feasibility stage.
The information contained in this report is based upon a
field examinations of the property carried out between June
10th and 14th and between August 1st and 6th 1993.
The field
data was supplemented by a review of previous reports on the
various mineral occurrences contained within claims now held
by Feather Gold and by additional useful information provided
by Mr. Larry Barrett who is a director of Feather Gold and
the supervisor/manager of the field work being conducted on
the property at the time of the visits.
The work carried out during the course of the examination
consisted of assessing and sampling’ a number of mineral
showings situated within the Barb, TB, Rat, Mon. Jean and
Kodak claims.
These occurrences had been identified by
exploration work, particularly bulldozer, excavator and hand
trenching, carried out on behalf of Feather Gold, Anooraq
Resources
Corp.
and their predecessors.
The principal
occurrences in the Jean Claim area have also been tested by
diamond drilling carried out on behalf of Anooraq.
A total of 48 samples were analyzed by fire assay (for Au and
Ag) and IC? methods (for Ag, As, Bi, Cd, Cu, Hg, Mo, Pb, Sb
and Zn).
Analytical results and geological observations were
compared with those in earlier reports, in particular MacKean
(1987 & 1988) and Carlyle (1990), and used with the earlier
data to characterize and evaluate each of the occurrences.
1.2
Description of Mineral
Tenures
The property under discussion consists of a total of 133
mineral claims and 3 Crown grants for a total of 136 mineral
tenures controlled by Feather Gold Resources Ltd.
The Mon,
TB,
Nyak,
Jean,
Kodak,
and Hazel N properties
are held
directly by Feather Gold under the terms of an agreement with
I
2
Anoorag
Resources Ltd.
The Barb and Rat Claims are held by
Feather Gold under agreement with Larry and Bill Barrett.
Claim names,
record
numbers,
expiry dates
and ownership
details are provided in Table 1.
The claims all lie within
the Whitehorse Mining District and are recorded with the
Whitehorse Mining Recorder’s office at
300 Main Street,
Whitehorse, Yukon,
Table 1
Schedule of Claims
Claim Name
Record No.
~pj~y
Barb 1-34
YA86607-40
May 3 1996
Larry Barrett
Rat 1—12
YB12725—36
Dec 15 1993
Bill Barrett
Rat 13—29
YB131OI—17
Mar 15 1994
Feather Gold
Mon 1-16
YA82825—40
Aug 27 1993
Feather Gold
TB 1-6
YA82967-72
Sept 4 1993
Feather Gold
Nyak 1-4
YA82997—3000
Dec 4 1993
Feather Gold
Nyak 5-48
YA85201-44
Dec 4 1993
Feather Gold
Jean (L202)
19237
Kodak
18304
(L203)
Hazel N (L205)
1.3
Date
Owner of Record
19285
Location and Access
The Feather Gold property comprises an area of approximately
3,000 ha on Montana Mountain, which is 12 km due south of the
village of Carcross, Yukon.
Carcross is a small community on
Bennett Lake, 74 km by road south of Whitehorse.
It may be
reached from both Whitehorse and Skagway, Alaska via Highway
2 or from the Alaska Highway at Jake’s Corner via Highway B.
The areas of interest within the claim group are accessible
from a gravel road which intersects Highway 2 just south of
the Nares River bridge at Carcross.
The road was the
principal access to the old Big Thing and Arctic Mines and
leads southerly up the northern slope of Montana Mountain and
the valley of Upper Tin Cup Creek.
The northern boundary of
the Barb Claims is about 11 km from the highway it is about
13 km to the vicinity of the Ridge Trench Area which is the
site of the bulk of the recent Feather Gold exploration work.
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West Trenches
Three trenches were excavated in the vicinity of the Barb and
TB Claim boundary about 300 to 400 m west of the trenches
described above.
They were intended to test areas of altered
near—bedrock float possibly derived from westerly extensions
of Ridge Zone structures
Trench L lies immediately north of the access road and about
20 m west of the Barb 1 and 2 Initial Posts.
It strikes
north-south in faulted granitic rocks hosting two discrete
mineralized structures:
1)
an east west striking zone of
intense hydrothermal alteration and veining and 2) a northsouth striking mineralized quartz vein.
The altered zone(l) strikes at 85° and dips northerly at 62°.
It is 7 to S m thick with a core of consisting of a 1.5 m
thick band of yellow clay bounded to the north and south by
intensly weathered and leached quartz-sulphide veins and
bands of scorodite up to 30 cm thick.
Samples obtained from
this zone are as follows:
F—13
Loose fragments of massive sulphide consisting of
galena, arsenopyrite, tetrahedrite-tennantite and
minor pyrite encountered in rust colured
clay
overburden during trenching.
FG-15
Rusted and altered
limit of zone.
FG-16
Impure
yellow
clay
and
argillically
granite appoximately 2 m wide.
Ft-li
Blue-green glassy granular scorodite
approximately 30 cm thick associated
broken quartz vein material
granite
2
m wide
from north
altered
from a seam
with rusted
FG-lS Band of yellowish-green clay about 1.5 m thick.
FG-19 Quartz scorodite vein 5 to 6 cm thick.
FG—20 Altered rusted granite extending
end of the trench.
5 m south to the
The mineralized quartz vein is exposed in the east wall of
the trench about 5 m from the south end.
It strikes at 010°,
dips east at 45° and is 30 to 40 cm thick.
It consists of
massive white quartz containing patches of coarse euhedral
galena, pyrite, arsenopyrite and possibly minor sphalerite
and tetrahedrite-tennantite.
Samples FG-21 and FG-22 are
representative of this material.
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Carlyle Vein
The Carlyle Vein is located 40-50 m northeast of a small
ultrabasic body which outcrops on the north face of Montana
Mountain east of the Rat Trench.
It consists of a quartz
vein bearing 010° and dipping easterly at 85-90° mineralized
with arsenopyrite.
Sample F-16 is a representative grab
sample of mineralized vein material.
Assay results are as
follows:
Au
oz/ton
&I
oz/ton
As
Cu
Pb
PPM
PPM
PPM
PPM
Wheelbarrow Vein
The Wheelbarrow Vein lies just west of the entrance to a
small cirque at the base of the Montana Mountain edifice and
due south of the Arctic Mine workings.
The vein has been
excavated by a large trench which was filled with snow at the
time of the writers visit.
The main vein system strikes at
about 090° and consists of massive quartz with disseminated
galena, tetrahedrite-tennantite and arsenopyrite.
The main
vein
is crosscut by
one or more narrow apparently
discontinuous vertical quartz sulphide veins which strike at
170°.
These are mineralized with pyrite, arsenopyrite and
minor tetrahedrite-tennantite.
Sample F-18 is a grab sample of sulphide rich loose material
which may be representative of the main zone. It is made up
of massive quartz with strongly disseminated arsenopyrite,
galena and tetrahedrite-tennantite.
Sample F-17
is a grab sample of mineralized vein material
from a crosscutting vein striking at 170° at the extreme
western end of the Wheelbarrow vein trench.
The sample
consists of quartz with disseminated arsenopyrite and pyrite.
It does not appear to be completely discrete from the quartz
monzonite host rock but rather a zone of silicification and
mineralization within the intrusive and of undetermined but
narrow width.
Assay results are are as follows:
Au
oz/ton
As
oz/ton
As
PPM
Cu
-
PPM
Pb
-
PPM
Zn
-
PPM
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ASSAY RESULTS
Au
oz/ton
LEGEND
Trench
Waste Pile
Quartz Sulphide Vein.
Alteration Zone
Strike & Dip of Vein.
Fault
Sample Number
Road
B c.2-.~
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0.776
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1.290
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0.031
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0.004
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0.418
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0.775
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0.388
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0.015
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0.338
oz/ton
10 .20
0 .28
0 .56
12 .06
0 .85
14 .92
0 .12
2 .75
5 .74
4
63
12 .54
16 .06
0 .33
1 .25
As
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Cu
PPM
Pb
PPM
>10000
2160
924
651
1152
>10000
1076
4780
761
9490
>10000
4510
>10000
<1000 0
80 60
97
41
792
92
3150
64
75
227
32
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62
1 18
1470
151
349
5810
1220
1777
96
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>10000
944
5050
7700
202
762
zn
PPM
274
85
82
1310
132
134
117
1081
>10000
69
49
116
68
4880
FEATHER GOLD RESOURCES LTD.
PLAN of the RIDGE ZONE; BARE & TB CLAIM AREA
Montana Mountain Project Area
Whitehorse M.D., Yukon
Nevin Sadlier-Brown Goodbrand Ltd.; Aug.1993
NTS 105D2
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Chemex Labs Ltd5
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NEVIN SADLIER-BROWN G0000RAND LTD.,
V7J 2C1
Project:
Comments:
PRZP
CODE
F-01
208
208
208
208
208
F—02
1—03
F—04
1—05
274
AurA
oz/T
<
274
274
274
274
<
0.003
0.056
0.134
0.086
0.003
1—06
1-07
1-00
F-14
1—15
208
208
208
208
208
274
274
274
274
274
0.034
0,022
0.020
0,744
0,642
F—iS
F-il
F—lB
.11-10
208
208
208
208
208
274
274
274
274
274
0.036
0.008
0.003
0.990
0.003
.11—11
JF-12
.11-13
208 274
208 274
208 274
.11—19
.11-20
208 274
208 274
JF—21
ARCTIC BIG THING
208 274
208 274
.11—09
—
—
—
—
C
C
AgFA
oz/T
<
0.1
0.5
2.3
0_a
0.1
Ag
ppm
Si
As
ppm
0.6
1L2
86.6
8.8
1.6
Cd
ppm
ppm
AUN: TIM SADLIER-BROWN
42
2760
3560
>10000
116
2
8
56
18
6
.c
c
Cu
ppm
0.5
2.5
2.5
0.5
1.0
1.0
1.0
0.7
1.2
0.9
312
33,0
17.8
42,0
54,6
>10000
5870
6310
>10000
7340
60
8
32
46
10
0.5
1.0
< 0.5
2.0
>100,0
0.2
0.1
0.1
4,9
0.2
2,6
0.2
1.2
168,0
1.8
>10000
>10000
>10000
>10000
3340
8
8
2
16
4
0.5
0.5
< 0.5
>100.0
6.0
12.018
0.344
21.1
0.9
>200
15,0
>10000
170
90
18
0.716
7.542
0.003
10.2
7.6
0,3
>200
>200
4,8
>10000
>10000
2560
0.042
0.546
0.8
120.1
210
>200
>10000
>10000
______
<
______
——-----
—
—---
Hg
ppm
4
68
97
25
26
33
46
94
15
17
Mo
ppm
<
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<
<
1
86
< 1
<
C
<
1
1
1
1
1
>100.0
6.0
136
68
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1
564
18
8
7.0
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3.0
8060
78
112
14
96
6.0
>100.0
319
5370
——------
—--—-----
____—
C
c 1
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2
68
244
58
568
1090
4990
32
30
8
6
12
36
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20
8
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7
4
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66
8
58
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410
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6
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6
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4
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132
1
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1800
1470
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112
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4
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52
6
>10000
220
274
>10000
280
26
22
396
9410
42
>10000
244
4590
1
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3
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126
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168
c 1
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4
66
20
14
4
12
2
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1
1
______
5963
Zn
ppm
ppm
2
1
1
1
1
-<
A931
Sb
Pb
ppm
—
a
Page Number :
Total Pages
:
Certificate Date: 29-JUN-93
Invoice No.
:19315963
P.O. Number
Account
: GT
fl~ERTIFICATE OF ANALYSIS
SM4PLE
a
VANCOUVER, BC
V6B 1B6
Brooksbank Ave., North Vancouver
British Columbia, Canada
PHONE: 604-984-0221
a
500 -342 WATER ST
Anatytical Chemists Geochernists Registered Assayers
212
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MINFILE:
PAGE NO:
UPDATED:
p/
105D 008
I of 2
07/29/94
YUKON MINFILE
STANDARD REPORT
EXPLORATION AND GEOLOGICAL SERVICES DIVISION, DIANI)
WI{ITEHORSE
NAME(S): Jean
MJNFILE #: 105D 008
MAJOR COMMODITIES: Au,Ag
MINOR COMMODITIES: Pb,Zn
TECTONIC ELEMENT: Northern Stikine Terrane
NTS MAP SHEET: 105 D 2
LATITUDE: 60°03’49”N
LONGITUDE: 134°42’49”W
DEPOSIT TYPE: Vein
STATUS: Drilled prospect
CLAIMS (PREVIOUS AND CURRENT)
JEAN, ELEANOR, KODAK, HAZEL M, ATHES, MON. TB, AFI
WORK HISTORY
Staked as Jean and Eleanor ci (19237) in Sep/36 by MR. Watson, who added Kodak & Hazel M ci
(19274) in Jun/39 and explored with hand trenching prior to taking the claims to lease in 1958. The property
was optioned in 1960 by New Imperial ML, which did further trenching and drove a 69 m x-cut below the
showing in 1961 and 1962. During 1967, Arctic Gold and Silver ML drilled four holes from the face of the
x-cut.
DuPont tied on Athes ci (YA60875) in Jun/81 on the west side and performed limited mapping and
sampling later in the year. Anooraq Res Corp optioned the leased claims, tied on Mon and TB ci (YA82825) in
Aug/84 and performed bulldozer and hand trenching, prospecting and road construction later in the year.
Univex Mg Corp L acquired a large interest in Anooraq’s position and performed a preliminary evaluation in
1985 and explored with soil sampling and 9 holes (215 m) in 1986,
Omni Res L tied on AFI cl (YB7855) to the northwest in Sep/87 and conducted mapping and geochem
sampling later in the year and trenched in 1989. Anooraq performed soil sampling on the Mon and TB claims
in 1988.
The Jean, Kodak. Hazel M, Mon and TB claims were transferred to Feather Gold Res L in Mar/92.
Feather Gold Resources performed a program of lithogeochemical sampling and diamond drilling (10 holes
totalling 791 metres) in Aug and Sept/93.
GEOLOGY
Two subparailel quartz veins that may be faulted extensions of a single structure occur along the
contact between andesitic flows and Cretaceous quartz monzonite. The veins strike 1500 and dip
north.
The upper (Jean) zone is up to 61 cm wide and contains 20% galena, sphalerite and pyrite plus minor
arsenopyrite. The lower (Kodiak) zone consists of a swarm of veinlets 2,5 to 3 m wide containing stibnite,
arsenopyrite, pyrite and galena. The best sample taken from the upper zone assayed 940.1 g/t Au, 1080 g/t Ag,
10.6% Pb and 6.5% Zn over 30.5cm while the lower zone returned up to 65.8 g/t Au, 175.5 g/t Ag and 2.1%
Pb over 15,2 cm. Drilling intersected only minor amounts of vein quartz, suggesting the vein rapidly pinches at
depth.
On Omni’s claims three 1989 trenches exposed vuggy, banded quartz-suiphide veins up to 50 cm thick,
cutting altered granodiorite. The veins are marked by surface gossans and successive envelopes of sericitic,
argillic and propylitic alteration. Vein minerals include arsenopyrite, galena and pyrite. Assays returned values
up to 532.1 g/t Ag and 9,63 g/t Au.
550
MINFILE:
PAGE NO:
UPDATED:
IOSD 008
2 of 2
07/29/94
REFERENCES
ANOORAQ RESOURCES CORP., Mar/86. Assessment Report by G. MacDonald, P.Eng..
FEATHER GOLD RESOURCES CORP., Jun194. Assessment Report #093215 by T.L. Sadlier-Brown.
FEATHER GOLD RESOURCES CORP., Jun/94. Assessment Report #093216 by T.L. Sadlier-Brown.
GEORGE CROSS NEWSLETTER, 8 Jun/93.
GEOLOGICAL SURVEY OF CANADA Memoir 234, p. 26.
GEOLOGICAL SURVEY OF CANADA Paper 64-36, p. 39-40.
GEOLOGICAL SURVEY OF CANADA Paper 68-68, p. 61.
NEW IMPERIAL MINES LTD, Nov/60. Prospectus.
OMNI RESOURCES INC., Dec/89. Assessment Report #092777 by H.F. MacKinnon.
YUKON GEOLOGY AND EXPLORATION 1979-80, p. 117, 120, 167.
YUKON EXPLORATION 1985-86, p. 153, 172; 1989, p. 28.