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File Created: 18-Jul-1986 by Larry Jones (LDJ)
Last Edit:  07-Mar-1989 by Laura L. Duffett (LLD)

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NMI 103B6 Cu15
Name MAPLE LEAF, COLLISON BAY, BLACK PRINCE, MINE FR., KENORA, OFFICE FR., SHAMROCK, GORDON Mining Division Skeena
BCGS Map 103B025
Status Prospect NTS Map 103B06E
Latitude 052º 16' 04'' UTM 09 (NAD 83)
Longitude 131º 09' 31'' Northing 5793017
Easting 352705
Commodities Copper, Iron, Silver, Gold Deposit Types K01 : Cu skarn
Tectonic Belt Insular Terrane Wrangell
Capsule Geology

Discovered in 1906, the Maple Leaf group is located between sea level and 152 metres elevation at the mouth of Collison Bay.

In 1908 owners J.H. Gordon and associates bonded the property to the Bellingham Copper Company of Bellingham, Washington, and some work was done under the agreement. Collision Bay Mining Company, Limited, was incorporated in January 1909 to acquire the property, comprising 5 claims, the Black Prince, Mine Fraction, Kenora, Office Fraction, and a half interest in the Shamrock claim. The workings in 1909 included an upper adit (Gordon Tunnel), at the 152-metre elevation, which was 5 metres in length; the No. 1 adit, at an elevation of 107 metres, which comprised a 30-metre cross-cut from which a 30-metre drift and 24-metre winze were driven; and a lower adit, 15-metres in length, which did not reach the mineralization. The mine closed in November 1909.

In 1973 Barrel Resources Ltd. held 40 claims in the Itsa and CU groups, covering the southern and western shores of Collison Bay and including several old properties. Work done in the area included: linecutting and magnetometer survey, 7.4 kilometres; electromagnetic survey, 4.6 kilometres; geochemical soil survey, 97 samples taken on a 30 by 61-metre grid spacing.

Falconbridge Limited sampled on the property in 1985.

Basalts from the Vancouver Group, Upper Triassic Karmutsen Formation are conformably overlain by limestones of the Jurassic to Triassic Kunga Group. Diorites of the Collison Bay Stock, part of the Middle to Late Jurassic Burnaby Island Plutonic Suite, lie to the east.

A vein-like north trending zone, variably replaced by magnetite, pyrrhotite, pyrite and chalcopyrite, occurs within metasomatically altered Karmutsen greenstones. A 2-metre chip sample from the middle adit returned 1.4 per cent copper, 14.7 grams per tonne silver and 0.7 gram per tonne gold (Assessment Report 14189). The vein strikes intermittently for about 250 metres and is up to 4 metres wide.

Grab sampling from the upper adit returned values such as 10.6 grams per tonne of gold, 13.5 grams per tonne of silver and 1.84 per cent copper. Estimate of reserves of the dump material is 1600 tonnes with an average grade of 1.22 grams per tonne gold (Assessment Report 14189).

Bibliography
EMPR AR 1908-59; 1909-70-81; 1912-110; 1918-44,45; 1920-45
EMPR ASS RPT 4668, *14189, 14818
EMPR BULL *54, p. 213
EMPR EXPL 1985-C362; 1986-C418
EMPR GEM 1973-482
GSC MAP 278A; 1385A
GSC P 88-1E, pp. 213-216,221-227; 89-1H, pp. 95-112; 90-10, pp. 59-87; 91-1A, pp. 383-391
GSC SUM RPT *1909, pp. 74,75
MIN REV March/April 1988, pp. 19-24
EMPR PFD 840917

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