Rock Identifier
Fire Opal (in matrix) (Hydrated Silica (SiO2·nH2O)) — Mineraloid
Mineraloid

Fire Opal (in matrix)

Hydrated Silica (SiO2·nH2O)

Hardness: 5.5-6.5 Mohs. Color: Vivid orange core (play-of-color) within a dark grey or basaltic matrix. Luster: Vitreous to sub-vitreous. Crystal structure: Amorphous. Specific gravity: 1.9-2.3.

Hardness
5
Luster
Vitreous to sub-vitreous
Identified More mineraloid

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Physical properties

Hardness: 5.5-6.5 Mohs. Color: Vivid orange core (play-of-color) within a dark grey or basaltic matrix. Luster: Vitreous to sub-vitreous. Crystal structure: Amorphous. Specific gravity: 1.9-2.3.

Formation & geological history

Formed from silica-rich water seeping into cavities in volcanic rock (usually rhyolite or basalt) millions of years ago, often during the Tertiary period. The microscopic silica spheres diffract light to create the internal 'fire'.

Uses & applications

Primary use is in jewelry as gemstones (cabochons or rough settings) and as a lapidary material for mineral collectors.

Geological facts

Unlike 'Precious Opal', Mexican Fire Opal is valued specifically for its intense background body color (orange/red). It is the national gemstone of Mexico and was revered by the Aztecs who called it 'quetzalitzlipyollitli'.

Field identification & locations

Identify in the field by looking for glassy, translucent orange nodules embedded in weathered volcanic rock. Common locations include Queretaro and Jalisco in Mexico, as well as parts of Ethiopia and Australia.