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File Created: 24-Jul-1985 by BC Geological Survey (BCGS)
Last Edit:  22-Apr-2018 by Karl A. Flower (KAF)

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NMI 092G11 Cu4
Name BULLIONDALE, LADY OF THE LAKE (L.4654), INDIAN RIVER, BULLIONDALE NO. 1-3(L.4649-51), BULLIONDALE NO. 5 (L.4653) Mining Division Vancouver
BCGS Map 092G066
Status Showing NTS Map 092G10W, 092G11E
Latitude 049º 37' 01'' UTM 10 (NAD 83)
Longitude 123º 00' 11'' Northing 5496042
Easting 499779
Commodities Copper Deposit Types
Tectonic Belt Coast Crystalline Terrane Gambier
Capsule Geology

The Bulliondale occurrence is located on the south west side of the Indian River near its headwaters, approximately 16 kilometres southeast of Squamish.

The area is underlain by a sequence of andesitic volcanics of the Lower Cretaceous Gambier Group, near the south end of the Indian River roof pendant. The pendant is enclosed in Late Jurassic quartz diorite and diorite of the Tertiary to Jurassic Coast Plutonic Complex.

Locally, pyrite and chalcopyrite occur along a silicified limestone contact and in a felsic porphyritic dike. Several similar north west- striking zones of mineralization, up to 9 metres wide, are exposed in a nearby adit.

A chip sample across 0.9 metres of a mineralized zone in the adit assayed trace gold, trace silver and 0.5 per cent copper (Minister of Mines Annual Report 1917, p. 278).

The area has been explored since the early 1900’s including the construction of a short adit. In 2015, NEK Canada Mining Group completed a program of rock sampling and geological mapping on the area.

Bibliography
EMPR AR 1913-301; *1917-277,278; 1918-311; 1921-231; 1931-175
EMPR ASS RPT 36023
EMPR FIELDWORK 1980, pp. 165-184
EMR MP RESFILE (MC-167-C3-2-68)
GSC MAP 199A; 1069A; 1151A; 1386A
GSC MEM *158, pp. 114,115; 335, pp. 47-54,58,61,62
GSC P 89-1E, pp. 177-187; 90-1E, pp. 183-195, 90-1F, pp. 95-107
GSC SUM RPT *1917, Part B, p. 24
Armstrong J.E. (1990): Vancouver Geology, Geological Association of
Canada (Cordilleran Section)
Ditson, G.M. (1978): Metallogeny of the Vancouver-Hope Area,
British Columbia, M.Sc. Thesis, University of British Columbia
EMPR PFD 7977

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