
mineral
Precious Opal
Hydrated Silica (SiO2·nH2O)
AI-generated identification · may be incorrectHardness: 5.5-6.5 on Mohs scale; Color: Multi-colored play-of-color; Luster: Vitreous to pearly; Structure: Amorphous (mineraloid); Cleavage: None; Specific Gravity: 1.9-2.3.
- Hardness
- 5
- Color
- Multi-colored play-of-color
- Luster
- Vitreous to pearly
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Physical properties
Hardness: 5.5-6.5 on Mohs scale; Color: Multi-colored play-of-color; Luster: Vitreous to pearly; Structure: Amorphous (mineraloid); Cleavage: None; Specific Gravity: 1.9-2.3.
Formation & geological history
Formed from seasonal rains that leach silica from sandstone and carry it into deep cracks. As the water evaporates, it leaves behind solid silica deposits. Much of the world's opal formed in the Cretaceous period about 65-145 million years ago.
Uses & applications
Primarily used as a gemstone in fine jewelry (rings, pendants, earrings) and as unique collector specimens.
Geological facts
Opal is the only gemstone that can display all colors of the rainbow through a phenomenon called opalescence, caused by the diffraction of light through tiny silica spheres. Australia produces approximately 95% of the world's precious opal.
Field identification & locations
Identified by its distinctive 'play-of-color' when rotated in light. In the field, it is often found within sedimentary host rocks like sandstone or ironstone. Collectors look for high 'fire' and transparency.
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Other mineral specimens
Gneiss or Schist
Gneiss or Mica Schist with Garnet
Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
igneous
Granite
Granite (Phaneritic intrusive igneous rock)
igneous
Septarian Pebble
Septarian nodule / Concretion
sedimentary