Rock Identifier
Amethyst (Silicon dioxide with iron impurities (SiO2)) — mineral
mineral

Amethyst

Silicon dioxide with iron impurities (SiO2)

Hardness: 7 (Mohs scale); Color: Purple to violet; Luster: Vitreous (glassy); Crystal structure: Hexagonal/Trigonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65.

Hardness
7 (Mohs scale)
Color
Purple to violet
Luster
Vitreous (glassy)
Identified More mineral

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Physical properties

Hardness: 7 (Mohs scale); Color: Purple to violet; Luster: Vitreous (glassy); Crystal structure: Hexagonal/Trigonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65.

Formation & geological history

Formed in hydrothermal veins or as linings in geodes within igneous volcanic rocks. Its purple color is caused by irradiation of iron impurities within the silicon dioxide crystal lattice. It can be found in rocks from various geological ages, often associated with basaltic flows.

Uses & applications

Primarily used in jewelry (faceting, beads, and carvings like the bracelet shown), decorative ornamental objects, and as a popular mineral specimen for collectors.

Geological facts

Amethyst was considered a Cardinal Gem until the 18th century, ranked alongside diamonds and rubies in value until large deposits were found in Brazil. Its name comes from the Greek 'amethystos', meaning 'not intoxicated', as it was historically believed to prevent drunkenness.

Field identification & locations

Identify by its characteristic purple color and lack of cleavage (it breaks with curved, glass-like surfaces). In the field, look for purple crystals inside hollow spherical rocks (geodes). Major deposits are located in Brazil, Uruguay, Zambia, and Ontario, Canada.