
mineral
Chrysocolla on Matrix
Hydrated copper phyllosilicate (Cu,Al)2H2Si2O5(OH)4·nH2O
Hardness: 2.5-3.5 (often harder if mixed with quartz); Color: Cyan-blue, turquoise, green; Luster: Vitreous to dull; Crystal structure: Orthorhombic (usually cryptocrystalline); Specific Gravity: 2.0-2.4.
- Hardness
- 2
- Color
- Cyan-blue, turquoise, green
- Luster
- Vitreous to dull
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Physical properties
Hardness: 2.5-3.5 (often harder if mixed with quartz); Color: Cyan-blue, turquoise, green; Luster: Vitreous to dull; Crystal structure: Orthorhombic (usually cryptocrystalline); Specific Gravity: 2.0-2.4.
Formation & geological history
Secondary mineral formed in the oxidation zones of copper ore bodies. Frequently occurs as crusts, vein fillings, or botryoidal masses alongside other copper minerals like malachite and azurite.
Uses & applications
Primarily used as a minor ore of copper, as a gemstone for jewelry (cabochons), and as a popular specimen for mineral collectors.
Geological facts
Chrysocolla is often confused with turquoise due to its color, but it is softer. The name comes from the Greek 'chrysos' (gold) and 'kolla' (glue), referring to its ancient use as a soldering material for gold.
Field identification & locations
Identify in the field by its distinct blue-green color and its tendency to stick to the tongue if licked (due to its porous, hydrated nature). Commonly found in arid regions like Arizona (USA), Chile, and the DRC.
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