Gypsum in British Columbia

Of four main gypsum areas in the province, commercial production has only come from Falkland and the Kootenay and Columbia River valleys of southeast British Columbia. The Windermere deposit in southeast B.C. has been the major producer since /948. Gypsum and anhydrite from the Falkland deposit is used principally in cement-making at Kam/oops. GYPSUM deposits in British Columbia are known from four different areas: the southeast part of the province in the proximity of the Kootenay and Columbia River valleys; Forgetmenot Creek astride the British Columbia - Alberta boundary near Intersection Mountain; Falkland; and O'Connor River north of Haines . To date, commercial production has only come from Falkland and the southeast part of the province. Gypsum deposits of southeast British Columbia occur in the Burnais Formation of Devonian age. Outcrops of gypsum and numerous sinkholes indicating its presence are scattered over large areas of the Stanford Range. Several properties have been examined by industry in both the recent and more distant past. Significant production is reported from only two deposits. The Mayook deposit, active from 1926 to 1929 and from 1947 to 1954, produced approximately 95,000 tonnes of gypsum. The Windermere deposit, which has been active since 1948, is operated by Westrock Industries and has produced more than 6.8 million tonnes of gypsum. The Burnais Formation is composed principally of well bedded, finely 'laminated gypsum but also contains thin lenses of black fetid limestone and dolomite. Part of the Formation consists of breccia with angular carbonate clasts in massive, coarse grained gypsum. In several exposures, the Formation appears 10 be from 200 10 400 m thick, of which more than 75 Industrial Minerals in Canada per cent is gypsum . In the Stanford Range reserves mineable by quarry methods are estimated to be approximately 450 million tonnes.