Moolooite is a rare blue-green
mineral with the formula Cu
++(C
2O
4)·n(H
2O) (n<1) (making it a hydrated
copper oxalate). It was discovered by
Richard M Clarke and
Ian R 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.
A second occurrence is reported from the Sainte-Marie-aux-Mines silver mining district of Vosges Mountains, France.
References
Boyd-Graber, Jordan.
A Field Guide to Australian Minerals. (2004)