Rock Identifier
Chrysocolla (with Quartz and Malachite) (Cu2-xAlx(H2-xSi2O5)(OH)4·nH2O) — mineral
mineral

Chrysocolla (with Quartz and Malachite)

Cu2-xAlx(H2-xSi2O5)(OH)4·nH2O

Hardness: 2-4 on Mohs scale (higher when silicified with quartz); Color: pale green, turquoise blue, bluish-green; Luster: vitreous, waxy, to earthy; Cleavage: none; Crystal structure: orthorhombic/amorphous; Specific Gravity: 2.0-2.4

Hardness
2-4 on Mohs scale (higher when silicified with quartz)
Color
pale green, turquoise blue, bluish-green
Luster
vitreous, waxy, to earthy
Identified More mineral
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Physical properties

Hardness: 2-4 on Mohs scale (higher when silicified with quartz); Color: pale green, turquoise blue, bluish-green; Luster: vitreous, waxy, to earthy; Cleavage: none; Crystal structure: orthorhombic/amorphous; Specific Gravity: 2.0-2.4

Formation & geological history

Secondary mineral formed in the oxidation zones of copper ore bodies. It is created by copper-rich water percolating through silica-rich rocks and precipitating in fractures and cavities alongside malachite, azurite, and quartz.

Uses & applications

Used primarily as a copper ore in some regions, as a popular mineral specimen for collectors, and for lapidary work (cabochons, beads, and carvings) when silicified into chrysocolla chalcedony.

Geological facts

Chrysocolla was used by ancient Greek philosopher Theophrastus as a fluxing agent in soldering gold. The name stems from the Greek words 'chrysos' (gold) and 'kolla' (glue). It is often mistaken for turquoise or malachite due to its vibrant blue-green hues.

Field identification & locations

Identifiable by its distinct soft bluish-green oxidation crust on copper-bearing matrix rock. It typically feels lightweight and adheres slightly to the tongue when wet. Commonly found in copper-mining regions like Arizona (USA), Chile, Peru, the DRC, and Namibia.