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File Created: 09-Jan-2014 by Karl A. Flower (KAF)
Last Edit:  15-Jan-2014 by Karl A. Flower (KAF)

Summary Help Help

NMI
Name WOSS, WOSS A, B, C Mining Division Nanaimo
BCGS Map 092L007
Status Showing NTS Map 092L02E
Latitude 050º 01' 44'' UTM 09 (NAD 83)
Longitude 126º 38' 13'' Northing 5544518
Easting 669243
Commodities Gold Deposit Types I : VEIN, BRECCIA AND STOCKWORK
Tectonic Belt Insular Terrane Wrangell
Capsule Geology

The Woss occurrence is located on an unnamed creek flowing north into Woss Lake, north of the divide with the Tahsis River.

The area is underlain by basic volcanic rocks of the Upper Triassic Karmutsen Formation (Vancouver Group). A north trending regional fault extends from the Tahsis River valley north through Woss Lake.

Locally, small (3 centimetre wide) quartz veins and stringers host pyrite, chalcopyrite and arsenopyrite. Two samples of quartz stringers yielded 7.62 and 9.84 grams per tonne gold, respectively (Assessment Report 19782).

In 1989, Teck Corporation completed a program prospecting and soil sampling on the area as the Woss A, B and C claims.

Bibliography
EMPR ASS RPT *19782
EMPR EXPL 1981-324
GSC MAP 1027A; 1537A
GSC MEM 272, p. 56
GSC OF 463
GSC P 72-44; 80-16
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, Ottawa

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