Rock Identifier
Chrysocolla in Quartz (Hydrated copper phyllosilicate with silicon dioxide (Cu2-xAlx(H2-xSi2O5)(OH)4·nH2O + SiO2)) — mineral
mineral

Chrysocolla in Quartz

Hydrated copper phyllosilicate with silicon dioxide (Cu2-xAlx(H2-xSi2O5)(OH)4·nH2O + SiO2)

Hardness: 2-4 for chrysocolla, 7 for quartz; Color: Bright cyan, turquoise blue, green, mixed with white quartz; Luster: Vitreous to earthy; Crystal structure: Amorphous/Cryptocrystalline; Specific gravity: 2.0-2.4

Hardness
2-4 for chrysocolla, 7 for quartz
Color
Bright cyan, turquoise blue, green, mixed with white quartz
Luster
Vitreous to earthy
Identified More mineral
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Physical properties

Hardness: 2-4 for chrysocolla, 7 for quartz; Color: Bright cyan, turquoise blue, green, mixed with white quartz; Luster: Vitreous to earthy; Crystal structure: Amorphous/Cryptocrystalline; Specific gravity: 2.0-2.4

Formation & geological history

Formed in the oxidation zones of copper ore bodies, typically secondary mineral deposits formed through hydrothermal activity or weathering.

Uses & applications

Used primarily as a decorative stone, in cabochons for jewelry, and as a collector's specimen.

Geological facts

Chrysocolla gets its vivid blue-green color from the presence of copper. The ancient Greeks used it as a soldering material for gold.

Field identification & locations

Found worldwide in copper-rich regions such as the southwestern United States, Chile, Peru, and Russia. Identified by its striking turquoise-blue coloration matrix.