Opal
Hydrated Silica (SiO2·nH2O)
Rock Type: mineral

Physical Properties
Hardness: 5.5-6.5; Color: Milky white with iridescent play-of-color; Luster: Vitreous to waxy; Structure: Amorphous (non-crystalline); Conchoidal fracture.
Formation & Geological History
Formed from silica-rich water seeping into cracks and cavities in sedimentary or volcanic rock over millions of years, often in arid regions.
Uses & Applications
Primarily used as a gemstone in jewelry (rings, pendants) and highly valued by mineral collectors for its unique optical properties.
Geological Facts
The 'play-of-color' is caused by the diffraction of light through microscopic silica spheres. Unlike most minerals, opal is a mineraloid because it lacks a crystalline structure.
Field Identification & Locations
Identify in the field by its waxy luster, iridescent flashes (if precious), and presence in volcanic or sedimentary layers. Australia and Ethiopia are major sources.
Identified on: 5/19/2026
Mode: Standard