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File Created: 27-Oct-1988 by Wim S. Vanderpoll (WV)
Last Edit:  14-Dec-2013 by Karl A. Flower (KAF)

Summary Help Help

NMI
Name STEWARDSON INLET Mining Division Alberni
BCGS Map 092E049
Status Showing NTS Map 092E08W
Latitude 049º 25' 24'' UTM 09 (NAD 83)
Longitude 126º 18' 05'' Northing 5478019
Easting 695694
Commodities Magnetite, Iron Deposit Types
Tectonic Belt Insular Terrane Wrangell, Plutonic Rocks
Capsule Geology

The Stewardson Inlet magnetite occurrence is located near shore on the southern end of Stewardson Inlet.

The area is underlain by granodioritic rocks of the Jurassic Island Plutonic Suite (Geological Survey of Canada Map 1537A).

Locally, a thin band of amphibolite striking south west is in contact with the intrusive rocks. The unit is approximately 200 metres wide and is part of the Paleozoic to Mesozoic West Coast Complex. The banded amphibolite is dark green to black in colour and consists of amphibole, plagioclase and magnetite. A selected sample assayed 14.63 per cent iron (Assessment Report 462).

In 1962, Paco Resources completed a program of geological mapping on the area.

Bibliography
EMPR AR 1962-131
EMPR ASS RPT *462
GSC MAP 1537A
GSC OF 463
GSC P 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 Univrsity, Ottawa
Sangster, D.F. (1964): The Contact Metasomatic Magnetite Deposits of
Southwestern British Columbia, Ph.D. Thesis, University of British
Columbia

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