Rock Identifier
Chrysocolla (Hydrated copper phyllosilicate (Cu,Al)2H2Si2O5(OH)4·nH2O) — mineral
mineral

Chrysocolla

Hydrated copper phyllosilicate (Cu,Al)2H2Si2O5(OH)4·nH2O

Hardness: 2.5-3.5 (can be higher if silicified); Color: Cyan, blue-green, or green; Luster: Vitreous, dull, or earthy; Crystal Structure: Amorphous (usually massive or botryoidal); Specific Gravity: 2.0-2.4.

Hardness
2
Color
Cyan, blue-green, or green
Luster
Vitreous, dull, or earthy
Identified More mineral
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Physical properties

Hardness: 2.5-3.5 (can be higher if silicified); Color: Cyan, blue-green, or green; Luster: Vitreous, dull, or earthy; Crystal Structure: Amorphous (usually massive or botryoidal); Specific Gravity: 2.0-2.4.

Formation & geological history

Formed in the oxidation zones of copper ore bodies as a secondary mineral. It precipitates from silica-rich groundwater reacting with copper minerals like malachite or azurite.

Uses & applications

Predominantly used as a minor ore of copper, as a gemstone for jewelry (cabochons), and as a popular specimen for mineral collectors.

Geological facts

Chrysocolla was used as a soldering agent for gold by ancient Greeks, which is where its name originates (chrysos - gold, kolla - glue). It is often found intergrown with quartz, chalcedony, or malachite.

Field identification & locations

Identify in the field by its distinct cyan color, low hardness, and its tendency to stick to the tongue due to its high water content and porosity. Commonly found in Arizona (USA), Chile, and the DRC.