
mineral
Chrysocolla
Hydrated copper silicate (Cu,Al)2H2Si2O5(OH)4·nH2O
Hardness: 2.5-3.5 (variable); Color: Cyan (blue-green) to green; Luster: Vitreous to earthy; Crystal structure: Monoclinic (usually cryptocrystalline); Cleavage: None; Specific Gravity: 2.0-2.4
- Hardness
- 2
- Color
- Cyan (blue-green) to green
- Luster
- Vitreous to earthy
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Physical properties
Hardness: 2.5-3.5 (variable); Color: Cyan (blue-green) to green; Luster: Vitreous to earthy; Crystal structure: Monoclinic (usually cryptocrystalline); Cleavage: None; Specific Gravity: 2.0-2.4
Formation & geological history
Secondary mineral formed in the oxidation zones of copper ore bodies where copper-bearing solutions react with silica-rich water. It is typically found in arid climates.
Uses & applications
Primarily used as a minor ore of copper, a gemstone for jewelry (cabochons and beads), and as a popular specimen for collectors due to its striking color.
Geological facts
Chrysocolla has been used since antiquity; its name comes from the Greek words 'chrysos' (gold) and 'kolla' (glue), referring to its ancient use as a material for soldering gold. It is often found intergrown with quartz (Chrysocolla Chalcedony) or malachite.
Field identification & locations
Identified in the field by its distinct cyan color and its tendency to stick to the tongue due to its porous nature. Commonly found in Arizona (USA), Chile, Peru, and Congo. Collectors look for high silicate content which increases durability.
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mineral