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File Created: 24-Jul-1985 by BC Geological Survey (BCGS)
Last Edit:  29-Jan-1990 by Garry J. Payie (GJP)

Summary Help Help

NMI
Name FELBER Mining Division Alberni
BCGS Map 092F042
Status Showing NTS Map 092F05W
Latitude 049º 25' 21'' UTM 10 (NAD 83)
Longitude 125º 47' 38'' Northing 5478178
Easting 297394
Commodities Iron Deposit Types
Tectonic Belt Insular Terrane Wrangell
Capsule Geology

A persistent lead of magnetite was located on the divide between Bedwell River and the first important tributary of Moyeha River coming in from the east (Geological Survey of Canada Memoir 204). No other details of the deposit were reported.

The region is underlain by andesitic to basaltic volcanics of the Upper Triassic Karmutsen Formation, Vancouver Group. Intruding the stratigraphy and covering large areas are rocks of the Jurassic Island Plutonic Suite, which on Vancouver Island, vary in composition from gabbro to quartz monzonite but are mainly granodiorite and quartz diorite. A north trending band of limestone about 5 kilo- metres in length occurs, bounded on the west by Karmutsen rock and on the east by Island Plutonic Suite rock (Geological Survey of Canada Open File 463). This limestone has not been assigned to a group or formation.

Similar types of rocks found several kilometres to the southeast near Bedwell River are known to host skarn-type magnetite deposits.

Bibliography
EMPR BULL 3, 1917
EMPR OF 1988-28
GSC BULL 172
GSC EC GEOL #3, Vol.1
GSC MAP 17-1968; 1386A
GSC MEM *204, p. 25
GSC OF 463
GSC P 68-50; 71-36; 72-44; 79-30; 80-16
CANMET RPT #47
Carson, D.J.T. (1968): Metallogenic Study of Vancouver Island With Emphasis on the Relationships of Mineral Deposits to Plutonic Rocks, Unpublished Ph.D. Thesis, Carleton University

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