
mineral
Rough Precious Opal
Hydrated Silica (SiO2·nH2O)
Hardness: 5.5-6.5 (Mohs); Color: Multi-colored flashes (play-of-color) on a brownish-yellow base; Luster: Sub-vitreous to waxy; Crystal structure: Amorphous (non-crystalline); Cleavage: None (conchoidal fracture); Specific gravity: 1.9-2.3
- Hardness
- 5
- Luster
- Sub-vitreous to waxy
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Physical properties
Hardness: 5.5-6.5 (Mohs); Color: Multi-colored flashes (play-of-color) on a brownish-yellow base; Luster: Sub-vitreous to waxy; Crystal structure: Amorphous (non-crystalline); Cleavage: None (conchoidal fracture); Specific gravity: 1.9-2.3
Formation & geological history
Formed from the precipitation of silica-rich water in cavities and cracks of igneous or sedimentary rocks. This specimen appears to be an Ethiopian or Australian 'chocolate' or 'matrix' opal, often dating from the Cretaceous to Miocene periods.
Uses & applications
Primary use is in the gemstone and jewelry industry. High-quality pieces are cut into cabochons. Lesser specimens are kept as rough mineral samples for collectors.
Geological facts
Opals are unique because they contain up to 20% water trapped within their silica structure. The 'fire' is caused by the diffraction of light through tiny, regularly spaced silica spheres.
Field identification & locations
Identify by looking for 'play-of-color' (iridescent flashes of green, red, or yellow) when rotated under light. Commonly found in Australia (Coober Pedy/Lightning Ridge) and the Wollo Province of Ethiopia. Field identification involves checking for a waxy texture and spectral colors.
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