
mineral
Opal
Hydrated Silica (SiO2·nH2O)
AI-generated identification · may be incorrectHardness: 5.5-6.5 (Mohs), Color: Multicolored (play-of-color on white), Luster: Vitreous to waxy, Crystal Structure: Amorphous (non-crystalline), Cleavage: None, Specific Gravity: 1.9-2.3
- Hardness
- 5
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Physical properties
Hardness: 5.5-6.5 (Mohs), Color: Multicolored (play-of-color on white), Luster: Vitreous to waxy, Crystal Structure: Amorphous (non-crystalline), Cleavage: None, Specific Gravity: 1.9-2.3
Formation & geological history
Formed from silica-rich water seeping into cracks and cavities in sedimentary or volcanic rock layers. Most commercial deposits are from the Cretaceous period (approx. 100 million years ago).
Uses & applications
Primary use in fine jewelry as gemstones. It is also a high-value collector's item and the birthstone for October.
Geological facts
Opals contain between 3% and 21% water. Famous specimens include the 'Olympic Australis' and the 'Aurora Australis.' Australia produces approximately 95% of the world's precious opal.
Field identification & locations
Identify by 'play-of-color' (iridescence) and a characteristic internal glow. Commonly found in Coober Pedy (Australia), Ethiopia, and Mexico. Collectors should look for vibrancy of fire and body tone.
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Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
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Granite, a coarse-grained felsic intrusive igneous rock
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Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
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Granite
Granite (Phaneritic intrusive igneous rock)
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