Brisco Barite Mine

Canadian Institute of Mining, Metallurgy and Petroleum
G. R. MANSON
Organization:
Canadian Institute of Mining, Metallurgy and Petroleum
Pages:
2
File Size:
1833 KB
Publication Date:
Jan 1, 1984

Abstract

The Brisco Barite Mine lies 70 km south-southeast of Golden, British Columbia. Barile mineralization occurs in a northstriking brecciation zone within Ordovician-Silurian Beaver/ oot dolomites and quartzites. Brecciation was caused by faulting related to the Mount Forster-Steamboat Fault. The main barite vein occupies a fault zone and is up to 12 m wide and over 250 m long. It is light grey to white, fine grained and compact; BaSO4 content is 9/. 70 per cent. Production started in 1945 and has continued to the present. Barile originally was removed from an open pit; later, an adit, begun in 1957, reached more than 240 m along the vein, 15 m below the pit floor. Today ore is hoisted from a decline resting some 37 m below the pit floor.
Citation

APA: G. R. MANSON  (1984)  Brisco Barite Mine

MLA: G. R. MANSON Brisco Barite Mine. Canadian Institute of Mining, Metallurgy and Petroleum, 1984.

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