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chrysocolla
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Chrysocolla from Miami, Ariz. A sample of chrysocolla after azurite, which is an example of a pseudomorph composed of orthorhombic copper hydroxyl silicate, from Ray Mine, Pinal county, Arizona, U.S.
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Basalt sample returned by Apollo 15, from near a long sinous lunar valley called Hadley Rille. Measured at 3.3 years old.
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Chrysocolla from Miami, Ariz.
Chrysocolla from Miami, Ariz.

chrysocolla

mineral
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History

chrysocolla, a silicate mineral, hydrated copper silicate, CuSiO3·2H2O, formed as a decomposition product of copper minerals in most copper mines, especially in arid regions. It occurs as crusts or masses in the upper parts of copper ore veins where the copper minerals have been altered by water containing dissolved silica. Specimens with a fine green or bluish green colour may be used as ornamental stones. For detailed physical properties, see silicate mineral (table).

A sample of chrysocolla after azurite, which is an example of a pseudomorph composed of orthorhombic copper hydroxyl silicate, from Ray Mine, Pinal county, Arizona, U.S.
A sample of chrysocolla after azurite, which is an example of a pseudomorph composed of orthorhombic copper hydroxyl silicate, from Ray Mine, Pinal county, Arizona, U.S.

The term chrysocolla was applied by Theophrastus and other ancient writers to various materials used in soldering gold.

This article was most recently revised and updated by John P. Rafferty.