
mineral
Chrysocolla
Chrysocolla (Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O)
Hardness: 2.5-3.5 on Mohs scale; Color: Cyan, blue-green, or sky blue, often with brown/black matrix; Luster: Vitreous to dull; Crystal structure: Orthorhombic (usually massive); Cleavage: None; Specific gravity: 2.0-2.4.
- Hardness
- 2
- Color
- Cyan, blue-green, or sky blue, often with brown/black matrix
- Luster
- Vitreous to dull
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Physical properties
Hardness: 2.5-3.5 on Mohs scale; Color: Cyan, blue-green, or sky blue, often with brown/black matrix; Luster: Vitreous to dull; Crystal structure: Orthorhombic (usually massive); Cleavage: None; Specific gravity: 2.0-2.4.
Formation & geological history
Formed in the oxidation zones of copper ore bodies. It is a secondary mineral that precipitates from silica-rich waters reacting with copper minerals like malachite or azurite.
Uses & applications
Used primarily as a minor ore of copper, as a gemstone for jewelry (cabochons), and as highly sought-after mineral specimens for collectors.
Geological facts
The name comes from the Greek words 'chrysos' (gold) and 'kolla' (glue), referring to its ancient use as a flux for soldering gold. It is often confused with turquoise but is generally softer and has a higher water content.
Field identification & locations
Identify by its characteristic blue-green color and lack of crystal faces (usually amorphous/massive). It often adheres slightly to the tongue due to its porous nature. Commonly found in Arizona (USA), Chile, and the DRC.
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Mineral/Rock
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mineral