geological geochemical report
TRANSCRIPT
J
GEOLOGICAL AND GEOCHEMICAL REPORT
THREE BEARS MINERAL CLAIMS
SXEENA MINING DIVISION
MORESBY ISLAND QUEEN CIlARLOTTE ISLANDS B C
NTS 103B J l2W
LATIXUDE 52 41 N LONGITlJDE 131 52 W
CLAIMS THREE BEARS MAMA BEAR PAPA BEAR
BABY BEAR HOT PORRIDGE
OWNER Gordon G Richards
OPERAOOR Ventures West Minerals Ltd
CONnlACTOR JMT Services Corp
DATES OF WORlC April 20 May 4 1982
MINERAL RESOURCEP lNCH
ASSESSMiNT REPORT
June 1982 1001j
it
ii
rTABLE OF CONTENTS
LIST OF ILLUSTRATIONS ill
INTRODUCTION
1 Location and Access
2 Claims
3 Work Summary
1
GEOLOGY I
GEOCHEMISTRY 4
CONCLUSIONS AND RECOMMENDATIONS 4
STATEMENT OF COSTS 5
STATEMENT OF QUALIFICATIONSGordon G Richards 6
Colin Earivel 7
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Figure
1
2
3
4
5
8
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LIST OF ILLUSTRATIONS
Property Location Map
Claims Map
Geology
Gold GeoChemistry
Arsenic Geochemistry
Hi
Page
2
3
In Pocket
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l
1
J INTRODUCTION
1 Location and Access
The claims are located in the Lockeport area of Central Moresby
Island some 58 kin south of Sandspit The claims extend from tidewater
around Anna Inlet north and west to elevations as high as 3400 feet Access
can be made by boat or float equipped fixed wing aircraft using Trans Provin
cial Airlines Otters or Beaver to Anna Inlet or more easily by helicopter
from Sandspit using either Queen Charlotte Helicopters or Vancouver Island
Helicopters
o
2 Claims
The property was staked in
are presently in good standing
Name Record No
THREE BEARS 2986 5
MAMA BEAR 2987 5
PAPA BEAR 2988 5
BABY BEAR 2989 5
HOT PORRIDGE 3088 6
1981 by Gordon G Richards and the claims
units Record Date
20 May 4 198L
20 May 4 1981
20 May 4 1981
20 May 4 1981
4 June 9 1981
3 Work Summary
In 1982 280 samples were collected of which 17 were rock chips
60 were silt samples and 203 were soil samples The purpose of this work
was to provide broad scale samling to discover areas anomalous for Au and
As worthy of more detailed mapping and sampling
GIDLOGY
I
The oldest rocks on the property are armutsen Formation greenstones
that underlie most of the property In the north half of the THREE BEARS
mineral claim the larmutsen greenstones are overlain as elsewhere on the
Charlottes by Kunga formation limestones limy argillites and argillites
Felsite dykes cut the Kunga sediments in this area The south eastern limit
of a fine grained quartz diorite intrusion was mapped and is shown along
the eastern end of Anna Lake
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PROf cRT
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J M T SERVICES CORP
THREE BEARSPROPERTY LOCATION MAP
Fi ute 1tCALE
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THREE BEARS
CLAIM MAP
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4
iAn old trail leadsfrom the western end of Anna Inlet SOUthwesF to
Anna Lake where old trails are visible along both north and south shoreI
lines An old adit is supposed to lie about 30 metres uphill from the LCP
for BJlBY BEAR mineral claim but was not located during the present survey
The Karmutsen float on the hillside in this area contains small quartz
veinlets with very low sulphide content Another area of intense quartz
veining occurs east of the outlet of Anna Lake see Figure 3 This zone
may extend several hundred meters or more east onto flat bottom land
immediately southwest of the head of Anna Inlet There is a second quartz
showing in this flat land at B194
GEOCHEMISTRY
Samples were collected in standard kraft sample bags and shipped
to Chemex Labs Ltd 212 Brooksbank North Vancouver B C
Soil samples were taken from the B horizon at a depth of from 5 to
20 em Rock chip samples were made up of 3 to 10 chips and weighed 200 400
gm Stream sediments were taken from the active part of creek beds
Samples were analyzed using the following standard procedures
Gold
Perchloric Nitric Atomic Absorption Analysis
Fire preconcentration Neutron Activation Analysis
Arsenic
Arsenic results have outlined a large zone of 30 ppm As northwest
of the outlet of Anna Inlet over terrain underlain by Karmutsen greenstones
and Kunga sediments
A second zone of anomalous arsenic occurs at and around the area
of intense quartz veining east of Anna Lake
Other anomalous arsenic results occur in stream sediments collected
at the base of the northwest facing slope that faces Anna Inlet and Anna
Lake
Too few samples have been analyzed for gold to provide a proper
evaluation of the gold mineralization potential
CONCLUSIONS AND RECOMMENDATIONS
oarmUtsen greenstones overlain by Kunga sediments are exposed on
the property An area of intense quartz veining east of Anna Lake is the
5
J most interesting mineralization seen to date and corresponds with an area
of anomalous arsenic results Another zone of anomalous arsenic oc s
northwest of the outlet of Anna Inlet
All samples should be analyzed for gold Following the gold
analyses more prospecting and some detailed evaluation should be undertaken
The quartz veined area between Anna Lake and Anna Inlet should be mapped
and sampled in detail The northwest facing slopes above Anna Lake and
Anna Inlet should be prospected further
STATEMENT OF COSTS
Time
G Richards April 28 May I 3C Harivel April 28 May 1 3W Howell April 23 May 1 3M Hagamoen May 1 3
Truck Rental May I 3
3 days @ 250 750 003 days @ 250 750 00
3 days @ 250 750 002 days @ 150 300 00
100 00
Q C Helicopters 348 00 924 80Richmond ReproductionVancal ReproductionP W A freightAirfare one man Vcr SandspitFood and AccommodationB C Tel
Supplies flagging string flares bags etc
DraughtingTypingVancal sepias black lines and photocopyingOlemex Labs
Report
1 272 80
343 55
122 94
88 00
132 85
534 31
37 25
300 00
400 00
50 00150 00
1 881 50
500 00
8 463 20
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STAlEMENT OF QUALIFICATIONS
I Gordon G Richards of Vancouver British Columbia do hereby
certify that
I I am a Professional Engineer of the Province of British Columbia
residing at 6195 Lynas Lane Richmond B C V7C 3K8
2 I am a graduate of the University of British Columbia B A Sc
196B M A Sc m 1974
3 I have practised my profession as a mining exploration geologist
continuously since 1968
4 This report is based on my personal knowledge of the district
and mapping of the geology at the property
L idJGordon G Richards P Eng
rII
certify that
1
2
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3
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SrATEMENT OF QtmLIFICATIONS
II
I C01in Harive1 of VAncouver British 1umbia do herebyi
II
I am a geologist iresiding at 3996 WestI
Vancouver British Columbia
II
lOth Avenue
II
I am a graduate of the University of British Columbial
B Sc Honours Geology 1972i
I have practised my profession as a mining exploration
geologist continuously since 1972
I am a FellOW of the Geologica1 Association of Canada
Harive1 B Sc
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THREE BEARS PROSPECT
SKEENA MINING DIVISION NTS 103 B 12W
GEOLOGY AND
SAMPLE LO CATIO N
Survey by I 50 000 Map Enla rge men Hip Chain Compos s a Barometer
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Ku nga Formation black flaggy limestone
K un go Formation massive grey limestone
Kormutsen Formation massive basaltic flows and pillowlalias volcanoclastlcs greenstone
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THREE BEARS
D IV ISION
CORP
PROSPECT
NTS 103 B 12WSKEENA MINING
ARSENIC
i urvey by
I
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150000 Mop Enlargement Hip Chain Barometer
FIG 4o
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ARSENIC
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SOl L S
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EXPLANATION
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Creek
Outcrop
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Rock chip sample
Sample location numberArsenic As Gold Au
ppm ppb
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J M T S E RV ICE S COR p
T HREE BEARS PROSPECT
SKEENA MINING DIVISION
GO LD
S rvey by
NTS 103 B 12W
GEOCHEMISTRY
I 50 000 Map Enla rge men Hip Chain Compass 80 Bara meter
FIG 5oI
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L EGENDI
GOLD
0 I L S
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15 ppb Au
15 25 ppb Au
26 50 ppb Au
50 ppb Au
X PL AN ATION
SCALE I 5000200 300 400
I I I
METERS
trike and dip of bedding or contact
and dip of fault or shear zone
ute rop
Sloil sampleS lt
ock chip sample
Sample location numberArsenic A s Gold Au
ppm ppb
RAVEN I
Cove
rI
I
I
G
3j
18
514
4 5I
I 8818G74 0 88513
tLst
511
4c
Iz 045 2I j
509
1 2M
f JlllI
II
311Y
I
0 0Zl42
3
C928 0
8504
I2
4 3
d0
O IA484 v
7 1615 YI
d8481
66
C i I 8490 101I
0 4T 848 6 48 in 6400 41 46I 0
73837
t0214 1
G
112 36
6l I CUISOG2 i2
0G
4 0G 32
3211
oo0
ZI96221
Zl97
141oII90
41o
lIesoZ 187
551
500I
MINERAL RESOURCES BRANCH
ASSESSMENT REPORT
QROCKS
t 15 50 ppb Au
50 ppb Au4
I
I
CJ
J
I
iIIII