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File Created: 24-Jul-1985 by BC Geological Survey (BCGS)
Last Edit:  17-Jan-1991 by George Owsiacki (GO)

Summary Help Help

NMI
Name KLANAWA AND CANYON Mining Division Alberni
BCGS Map 092C087
Status Showing NTS Map 092C15E
Latitude 048º 51' 05'' UTM 10 (NAD 83)
Longitude 124º 43' 35'' Northing 5412373
Easting 373355
Commodities Copper Deposit Types
Tectonic Belt Insular Terrane Wrangell
Capsule Geology

The Klanawa and Canyon occurrence area is near major lineaments separating Lower Jurassic Bonanza Group volcanics from Early to Middle Jurassic quartz diorite of the Island Plutonic Suite. In 1931, some "good chalcopyrite ore" was brought in from the showing and was reported to occur across a width of 9 metres. The mineralization is inferred to be hosted in a shear zone in Bonanza Group volcanics.

Bibliography
EMPR AR *1931-A165
EMPR FIELDWORK 1977, p. 23; 1989, pp. 503-510
EMPR PF (In 092C General File - Aeromagnetic Contour Map, Nitinat Lake Area, Noranda Mines Ltd., date unknown)
EMPR OF 1988-24; RGS 24, 1990
GSC MAP 1386A
GSC MEM 13
GSC OF 463; 821; 1272
GSC P 72-44; 76-1A; 79-30
Carson, D.J.T. (1968): Metallogenic study of Vancouver Island with emphasis on the relationships of mineral deposits to plutonic rocks, Ph.D. Thesis, Carleton University

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