
mineral
Chrysocolla
Hydrated copper silicates (Cu, Al)2H2Si2O5(OH)4·nH2O
Hardness: 2.5-3.5 on Mohs scale; Color: Cyan, turquoise-blue to blue-green; Luster: Vitreous to dull/earthy; Crystal Structure: Orthorhombic (usually amorphous); Specific Gravity: 2.0-2.4
- Hardness
- 2
- Color
- Cyan, turquoise-blue to blue-green
- Luster
- Vitreous to dull/earthy
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Physical properties
Hardness: 2.5-3.5 on Mohs scale; Color: Cyan, turquoise-blue to blue-green; Luster: Vitreous to dull/earthy; Crystal Structure: Orthorhombic (usually amorphous); Specific Gravity: 2.0-2.4
Formation & geological history
Formed in the oxidation zones of copper ore deposits where copper-bearing solutions react with silica; often found alongside malachite, azurite, and quartz.
Uses & applications
Used primarily as a minor ore of copper, as a gemstone for jewelry (cabochons and beads), and as a highly sought-after mineral specimen for collectors.
Geological facts
Chrysocolla often forms pseudomorphs after other minerals like malachite or azurite. It has been used since ancient times, and its name is derived from the Greek words 'chrysos' (gold) and 'kolla' (glue), referring to its use as a soldering material for gold.
Field identification & locations
Identify in the field by its striking blue-green color and its tendency to stick to the tongue due to its porous nature. Commonly found in arid copper-mining regions like Arizona (USA), Chile, and the DRC.
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