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File Created: 24-Jul-1985 by BC Geological Survey (BCGS)
Last Edit:  09-Jun-2020 by Karl A. Flower (KAF)

Summary Help Help

NMI
Name YREKA, SIRIUS, PF Mining Division Victoria
BCGS Map 092B082
Status Showing NTS Map 092B13E
Latitude 048º 50' 34'' UTM 10 (NAD 83)
Longitude 123º 39' 27'' Northing 5410187
Easting 451758
Commodities Copper, Gold, Silver Deposit Types
Tectonic Belt Insular Terrane Wrangell
Capsule Geology

The Yreka showing is located on the eastern flank of Mount Richards, approximately 2.3 kilometres south- south west of Crofton.

The area is underlain by volcanics of the Upper Devonian McLaughlin Ridge Formation, Sicker Group, reported to be altered to schists in the area. Intruding the country rocks is quartz feldspar porphyry of the Late Devonian Saltspring Intrusive Suite (formerly the Saltspring Intrusions). Gold and silver values are also reported.

Locally, a shear zone hosts copper mineralization.

Two shafts, one 64 metres deep and the other 43 metres, were sunk on the property in the early 1900's. In 1970, the area was explored as the Sirius claims by Canpac Minerals. In 1986 and 1987, the area was explored as the PF claims. Programs of geological mapping, prospecting, geochemical sampling and three diamond drill holes, totalling 1083.0 metres, were completed at this time.

Bibliography
EMPR AR *1901-1118; *1917-269
EMPR ASS RPT *2397, 16029, 16319
EMPR FIELDWORK 1982, p. 46; 1987, pp. 81-91
EMPR GEM 1969-224; 1970-292; 1971-224
EMPR MAP 40
EMPR OF 1988-8
EMPR PF ((Electromagnetic Profile, Canadian Pacific Minerals Ltd.,
1971; Apparent Chargeability Contour Plan, Canadian Pacific
Minerals Limited, 1971; *Mount Richards Geochemical Survey (shows
adit), Canadian Pacific Oil and Gas, 1969; Induced Polarization
and Electromagnetic Survey, Canadian Pacific Minerals, 1971) - see
Ironclad file - 092B 049; *Notes by J.Y. Wright, 1969)
GSC MAP 42A; 1386A; 1553A
GSC MEM 13; 36; 96
GSC OF 463
GSC P 72-44; 75-1A, p. 23; 79-30
Simmons, B. (2007-08-24): Report On The Cornucopia Project
Falconbridge File

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