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Moolooite is a rare blue-green mineral with the formula Cu++(C2O4)·n(H2O) (n<1) (making it a hydrated copper oxalate). It was discovered by RM Clarke and IR Williams in Bunbury Well, Mooloo Downs station, Murchison, Western Australia in 1986. It has an orthorhombic crystalline structure, and is formed by the interaction of bat guano with weathering copper sulfides.


Boyd-Graber, Jordan. A Field Guide to Australian Minerals. (2004)

This article is licensed under the GNU Free Documentation License. It uses material from the Wikipedia article "Moolooite". A list of authors is available in Wikipedia.
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