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File Created: 06-Jun-1990 by Garry J. Payie (GJP)
Last Edit:  07-May-2014 by Karl A. Flower (KAF)

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NMI
Name HAWK 8 Mining Division Vancouver
BCGS Map 092G093
Status Showing NTS Map 092G14W
Latitude 049º 56' 21'' UTM 10 (NAD 83)
Longitude 123º 24' 00'' Northing 5531944
Easting 471297
Commodities Gold Deposit Types
Tectonic Belt Coast Crystalline Terrane Plutonic Rocks
Capsule Geology

The Hawk 8 occurrence is located on the south side of Ashlu Creek, approximately 1 kilometre west- north west of the mouth of Pokosha Creek.

The area is underlain by granodiorite of the Jurassic Cloudburst pluton of the Coast Plutonic Complex (Geological Survey of Canada Paper 90-1F). A major regional northwest trending shear zone of Cretaceous age, the Ashlu Creek shear zone, occurs to the immediate west.

The occurrence consists of a quartz vein that strikes 010 degrees and dips 15 degrees within granodiorite of the Jurassic Cloudburst pluton (Coast Plutonic Complex). A chip sample assayed 4.11 grams per tonne gold over 1 metre (Assessment Report 17889, Map 5).

The area has been explored in conjunction with the nearby Ashlu mine (MINFILE 092GNW013), a complete exploration history can be found there. During 2009 through 2012, Ashlu Mines completed a program of rock, soil and silt sampling on the area.

Bibliography
EMPR ASS RPT *17889, 31343, 32702, 33444
EMPR FIELDWORK 1980, pp. 165-178
GSC MAP 42-1963; 1386A
GSC MEM 158
GSC OF 611
GSC P 89-1E, pp. 177-187; 90-1E, pp. 183-195; 90-1F, pp. 95-107
Ditson, G.M. (1978): Metallogeny of the Vancouver-Hope Area,
British Columbia, M.Sc. Thesis, University of British Columbia

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