
mineral
Chrysocolla
Hydrated copper phyllosilicate (Cu,Al)2H2Si2O5(OH)4·nH2O
Hardness: 2.5-3.5 (can be higher if silicified); Color: Cyan, blue-green, or green; Luster: Vitreous, dull, or earthy; Crystal Structure: Amorphous (usually massive or botryoidal); Specific Gravity: 2.0-2.4.
- Hardness
- 2
- Color
- Cyan, blue-green, or green
- Luster
- Vitreous, dull, or earthy
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Physical properties
Hardness: 2.5-3.5 (can be higher if silicified); Color: Cyan, blue-green, or green; Luster: Vitreous, dull, or earthy; Crystal Structure: Amorphous (usually massive or botryoidal); Specific Gravity: 2.0-2.4.
Formation & geological history
Formed in the oxidation zones of copper ore bodies as a secondary mineral. It precipitates from silica-rich groundwater reacting with copper minerals like malachite or azurite.
Uses & applications
Predominantly used as a minor ore of copper, as a gemstone for jewelry (cabochons), and as a popular specimen for mineral collectors.
Geological facts
Chrysocolla was used as a soldering agent for gold by ancient Greeks, which is where its name originates (chrysos - gold, kolla - glue). It is often found intergrown with quartz, chalcedony, or malachite.
Field identification & locations
Identify in the field by its distinct cyan color, low hardness, and its tendency to stick to the tongue due to its high water content and porosity. Commonly found in Arizona (USA), Chile, and the DRC.
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Gypsum (variety Selenite or Alabaster)
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Mineral
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Mineral/Rock
Banded Gneiss (River Rock/Pebble)
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