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File Created: 23-Jan-2014 by Karl A. Flower (KAF)
Last Edit:  09-Jun-2022 by Karl A. Flower (KAF)

Summary Help Help

NMI
Name FRIENDLY 4 Mining Division Alberni, Nanaimo
BCGS Map 092L027
Status Showing NTS Map 092L07E
Latitude 050º 16' 19'' UTM 09 (NAD 83)
Longitude 126º 41' 49'' Northing 5571405
Easting 664112
Commodities Copper, Silver, Iron Deposit Types K : SKARN
Tectonic Belt Insular Terrane Wrangell
Capsule Geology

The Friendly 4 occurrence is located on the west side of Friendly Creek, at an elevation of 810 metres.

The area is underlain by andesites and basalts, with minor inter-bedded limestone of the Upper Triassic Karmutsen Formation (Vancouver Group). Granodiorite of the Upper Jurassic Nimpkish batholith, which is part of the Jurassic Island Plutonic Suite, intrudes the Karmutsen Formation volcanics. Locally, the granodiorite is epidote altered.

Locally, a coarse layered, intensely epidotized, volcanic hosts lenses of chalcopyrite and magnetite. The zone is exposed over 3 metres vertically and strikes 280 degrees with an 80-degree dip to the north.

In 2007, a lone rock sample assayed 1.5 per cent copper and 7.4 grams per tonne silver (Rock Sample 4; Assessment Report 30120).

Work History

During 2007 through 2013, Homegold Resources completed programs of rock and soil sampling air photo geological interpretation and a ground magnetometer survey on the area as the Bonanza River property. In 2017, Homegold Resources Ltd. completed a minor program of prospecting and rock sampling on the area as the White Fang property.

Bibliography
EMPR ASS RPT *30120, 30446, 31944, 33097, 33343, 34325, 37313
EMPR EXPL 1980-271
EMPR GEM 1969-209; *1970-274-278
GSC ANN RPT 1886
GSC BULL 242
GSC MAP 4-1974; 255A; 1029A; 1552A
GSC MEM 272
GSC OF 9; 170; 463
GSC P 38-2; 38-3; 72-44; *74-8
GSC SUM RPT 1929 Part A; 1931 Part A
CJES 18, p. 1; 20, p. 2, 1983
Carson, D.J.T. (1968): Metallogenic Study of Vancouver Island with Emphasis on the Relationship of Plutonic Rocks to Mineral Deposits, Ph.D. Thesis, Carleton University

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