Rock Identifier
Amethyst (Quartz, purple variety — silicon dioxide (SiO₂), colored mainly by iron-related defects) — mineral
mineral

Amethyst

Quartz, purple variety — silicon dioxide (SiO₂), colored mainly by iron-related defects

AI-generated identification · may be incorrect

Typically purple, vitreous/glassy luster, translucent to transparent, conchoidal fracture, and no cleavage; Mohs hardness 7, trigonal crystal structure, specific gravity about 2.65. The specimen appears to be a rough, fractured amethyst piece, possibly cut or broken from a larger crystal.

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Physical properties

Typically purple, vitreous/glassy luster, translucent to transparent, conchoidal fracture, and no cleavage; Mohs hardness 7, trigonal crystal structure, specific gravity about 2.65. The specimen appears to be a rough, fractured amethyst piece, possibly cut or broken from a larger crystal.

Formation & geological history

Forms when iron-bearing silica-rich fluids fill cavities in volcanic rocks, especially basaltic geodes, where quartz crystals grow slowly. Most deposits are Cenozoic to Mesozoic in age, commonly associated with volcanic provinces.

Uses & applications

Used as a gemstone, ornamental carving material, mineral specimen, and abrasive-grade quartz source. Commercial jewelry value depends strongly on color, clarity, cut, and size.

Geological facts

Deep, evenly distributed violet (“Siberian” or “Deep Russian” color) is generally more desirable than pale purple. Heating amethyst can produce yellow citrine or green prasiolite, sometimes intentionally treated.

Field identification & locations

Identify it by its purple color, glassy luster, hardness, and lack of cleavage; it should scratch ordinary glass but not be scratched by a steel knife. Common sources include Brazil, Uruguay, Zambia, Bolivia, Mexico, and the United States.