Rock Identifier
Amethyst (Silicon Dioxide with Iron Impurities (SiO2)) — mineral
mineral

Amethyst

Silicon Dioxide with Iron Impurities (SiO2)

Hardness: 7 (Mohs scale); Color: Purple, violet, or lavender; Luster: Vitreous (glassy); Crystal Structure: Hexagonal/Trigonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65

Hardness
7 (Mohs scale)
Color
Purple, violet, or lavender
Luster
Vitreous (glassy)
Identified More mineral
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Physical properties

Hardness: 7 (Mohs scale); Color: Purple, violet, or lavender; Luster: Vitreous (glassy); Crystal Structure: Hexagonal/Trigonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65

Formation & geological history

Formed in igneous or metamorphic environments, typically inside volcanic geodes. The purple color is caused by irradiation of trivalent iron (Fe3+) in the quartz structure. Most specimens are from the Mesozoic or Cenozoic eras.

Uses & applications

Primarily used as a gemstone in jewelry, for decorative carvings, and by crystal collectors for aesthetic and metaphysical purposes.

Geological facts

Amethyst was considered a precious stone comparable to diamond until large deposits were found in Brazil in the 1700s. Its name comes from the Ancient Greek word 'amethystos', meaning 'not intoxicated', as it was believed to prevent drunkenness.

Field identification & locations

Identify by its characteristic purple color and quartz-like hardness. Often found in geode formations in Brazil, Uruguay, Zambia, and South Korea. Look for hexagonal crystal faces and transparency transitions from dark to light.