
mineral
Chrysocolla
Hydrated copper phyllosilicate, (Cu,Al)2H2Si2O5(OH)4·nH2O
AI-generated identification · may be incorrectHardness: 2 to 4 on the Mohs scale. Color: Green, blue-green, or cyan, often mottled with brown or black matrix. Luster: Vitreous to earthy. Crystal structure: Orthorhombic, though rarely found as distinct crystals; usually found as amorphous masses, crusts, or vein fillings. Cleavage: None.…
- Hardness
- 2 to 4 on the Mohs scale
- Luster
- Vitreous to earthy
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Physical properties
Hardness: 2 to 4 on the Mohs scale. Color: Green, blue-green, or cyan, often mottled with brown or black matrix. Luster: Vitreous to earthy. Crystal structure: Orthorhombic, though rarely found as distinct crystals; usually found as amorphous masses, crusts, or vein fillings. Cleavage: None. Specific gravity: 2.0 to 2.4.
Formation & geological history
Forms as a secondary mineral in the oxidized zones of copper ore bodies, typically in arid environments where copper-bearing solutions interact with silica-rich water.
Uses & applications
Frequently used as a gemstone, carved into ornamental objects, or made into cabochons for jewelry, though its softness requires protective settings.
Geological facts
Chrysocolla's name is derived from the Greek words "chrysos" (gold) and "kolla" (glue), referencing its historical use in soldering gold.
Field identification & locations
Easily identified by its vibrant blue-green color and relative softness. Commonly found in copper-rich mining regions such as the southwestern United States, Chile, Peru, and Russia.
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