
mineral
Ethiopian Fire Opal
Hydrated Silica (SiO2·nH2O)
AI-generated identification · may be incorrectHardness: 5.5 to 6.5 on Mohs scale; Color: Yellow-orange body tone with vivid red and green play-of-color; Luster: Vitreous to waxy; Crystal structure: Amorphous (non-crystalline); Specific gravity: 1.9 to 2.2.
- Hardness
- 5
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 5.5 to 6.5 on Mohs scale; Color: Yellow-orange body tone with vivid red and green play-of-color; Luster: Vitreous to waxy; Crystal structure: Amorphous (non-crystalline); Specific gravity: 1.9 to 2.2.
Formation & geological history
Formed from silica-rich water seeping into volcanic rock cavities (rhyolite or ash layers). Most major deposits in Ethiopia date to the Cenozoic era, specifically from the Welo district.
Uses & applications
Primarily used as a gemstone for fine jewelry (rings, pendants, earrings) and as high-value specimens for mineral collectors.
Geological facts
Ethiopian opals are often 'hydrophane,' meaning they can absorb water and change transparency or appearance temporarily when soaked. Significant mining in Ethiopia only began in the early 1990s and 2008.
Field identification & locations
Identify in the field by its conchoidal fracture, lightweight feel, and distinctive 'play-of-color' (iridescence) when rotated under light. Major locations include the Wollo (Welo) and Shewa provinces of Ethiopia.
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