Rock Identifier
Amethyst cabochon (Quartz, silicon dioxide (SiO₂), purple variety colored mainly by iron impurities and irradiation) — gemstone
gemstone

Amethyst cabochon

Quartz, silicon dioxide (SiO₂), purple variety colored mainly by iron impurities and irradiation

AI-generated identification · may be incorrect

Hardness 7 Mohs; purple, translucent to transparent, vitreous luster, trigonal crystal structure, and poor cleavage. The rounded polished form is a cabochon, likely set in a decorative jewelry piece.

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Physical properties

Hardness 7 Mohs; purple, translucent to transparent, vitreous luster, trigonal crystal structure, and poor cleavage. The rounded polished form is a cabochon, likely set in a decorative jewelry piece.

Formation & geological history

Amethyst forms in silica-rich hydrothermal veins and volcanic cavities, commonly lining basalt geodes; associated deposits range from Precambrian to younger volcanic rocks. The image does not permit confirmation that the insert is natural rather than synthetic or glass.

Uses & applications

Used in jewelry, carvings, collections, and ornamental objects. Commercial cabochons are generally inexpensive.

Geological facts

Purple color varies with iron content and irradiation and may fade with prolonged heat or intense sunlight. Amethyst is February’s birthstone and a quartz variety rather than a separate mineral species.

Field identification & locations

Identify by hardness, glassy luster, conchoidal fracture, and purple zoning; it should scratch glass but not be scratched by a steel knife. Common sources include Brazil, Uruguay, Zambia, and Mexico; microscopic bubbles or very uniform color may indicate glass or synthetic material.