mineral

Opal (Precious Opal)

Hydrated Silica (SiO2·nH2O)

AI-generated identification · may be incorrect

Hardness: 5.5-6.5 Mohs; Color: Multi-colored play-of-color on a white, gray, or clear body; Luster: Subvitreous to pearly; Crystal structure: Amorphous (mineraloid); Cleavage: None; Specific Gravity: 1.9-2.3.

Hardness: 5
Color: Multi-colored play-of-color on a white, gray, or clear body
Luster: Subvitreous to pearly

Identified March 25, 2026More mineral →

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Physical properties

Formation & geological history

Formed from silica-rich water seeping into cracks and cavities in sedimentary rocks (like sandstone) or volcanic rocks. Most precious opals formed between 65 and 145 million years ago (Cretaceous period).

Uses & applications

Primarily used in high-end jewelry as gemstones (cabochons or faceted) and highly sought after by mineral collectors.

Geological facts

The 'play-of-color' is caused by the diffraction of light through microscopic silica spheres arranged in a regular grid. Opals are the birthstone for October and over 90% of the world's supply comes from Australia.

Field identification & locations

Identify by its unique internal flashes of color that shift when the stone is moved. Commonly found in Coober Pedy (Australia), Ethiopia, and Mexico. Collectors look for 'fire' intensity and body tone.