Covellite |
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Crystal system: Hexagonal Covellite is a secondary mineral formed by the alteration of other sulphides containing copper. It is a minor copper ore usually found in association with other sulphides such as bornite (Cu5FeS4), Chalcocite (Cu2S), and chalcopyrite (CuFeS2). As can be seen, copper can, to a limited extent, be replaced by iron. Fine mineral specimens can be found at Butte, Montana, USA. The specimen shown comes from Butte, Montana. |