
mineral
Chrysocolla and Azurite in Matrix
Hydrated copper phyllosilicate (Chrysocolla - Cu2H2Si2O5(OH)4) and Copper carbonate (Azurite - Cu3(CO3)2(OH)2)
Hardness: 2-4 (Chrysocolla) to 3.5-4 (Azurite); Color: Cyan, teal, and deep azure blue in a tan/grey host rock; Luster: Vitreous to dull; Crystal Structure: Amorphous/Monoclinic; Specific Gravity: 2.0-2.4.
- Hardness
- 2-4 (Chrysocolla) to 3
- Color
- Cyan, teal, and deep azure blue in a tan/grey host rock
- Luster
- Vitreous to dull
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Physical properties
Hardness: 2-4 (Chrysocolla) to 3.5-4 (Azurite); Color: Cyan, teal, and deep azure blue in a tan/grey host rock; Luster: Vitreous to dull; Crystal Structure: Amorphous/Monoclinic; Specific Gravity: 2.0-2.4.
Formation & geological history
Secondary mineral formed in the oxidation zones of copper-bearing ore bodies. It occurs as a result of the weathering of primary copper minerals by silica-rich and carbonate-rich waters.
Uses & applications
Used primarily as an ore of copper, as a gemstone for lapidary work (cabochons), and highly prized as decorative display specimens for collectors.
Geological facts
Chrysocolla is often confused with turquoise, but can be distinguished by its higher hydration and lower hardness. Azurite is famous for its deep blue 'bluebird' color and often alters into green malachite over geological time.
Field identification & locations
Identify in the field by the vibrant blue/green staining on host rock (often quartz or limestone) near copper mines. Common locations include Arizona (USA), Congo, Chile, and Australia.
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