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File Created: 08-Mar-1989 by Wim S. Vanderpoll (WV)
Last Edit:  28-Jan-2014 by Karl A. Flower (KAF)

Summary Help Help

NMI
Name KAOUK PYTT Mining Division Alberni
BCGS Map 092L006
Status Showing NTS Map 092L02W
Latitude 050º 05' 44'' UTM 09 (NAD 83)
Longitude 126º 59' 13'' Northing 5551196
Easting 643978
Commodities Iron Deposit Types
Tectonic Belt Insular Terrane Wrangell, Plutonic Rocks
Capsule Geology

The Kaouk Pytt occurrence is located on a south east facing slope between the Kaouk and Artlish rivers, approximately 8.75 kilometres northeast of the Kaouk River mouth.

The area between Kaouk and Artlish Rivers is underlain by Jurassic granodiorite of the Island Plutonic Suite. Lower Jurassic Bonanza Group volcanics and sediments lie to the west and north (Geological Survey of Canada Map 4-1974).

A property examination (Property File - H. Veerman) indicates a northwest trending belt of Quatsino (?) limestone extending between the two rivers, possibly as a roof pendant within the intrusive rocks. The examination indicates unspecified pyrrhotite mineralization in the location given.

Bibliography
EMPR BULL 20-V; 27
EMPR PF (Veerman, H.,: Report, see Kaouk - 092L 304)
GSC MAP 4-1974
GSC MEM 204; 272
GSC OF 9; 170; 463
GSC P 74-8
Sangster, D.F., (1964): The Contact Metasomatic Magnetite Deposits of Southwestern British Columbia, Ph.D. Thesis, University of British Columbia
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
Sangster, D.F. (1964): The Contact Metasomatic Magnetite Deposits of Southwestern British Columbia, Ph.D. Thesis, University of British Columbia

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