Rock Identifier
Amethyst on Agate/Host Rock (Silicon Dioxide (SiO2) with iron impurities) — mineral
mineral

Amethyst on Agate/Host Rock

Silicon Dioxide (SiO2) with iron impurities

Hardness: 7 (Mohs scale), Color: Purple to pale lavender, Luster: Vitreous (glassy), Crystal system: Hexagonal, Cleavage: None (conchoidal fracture), Specific Gravity: 2.65

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Physical properties

Hardness: 7 (Mohs scale), Color: Purple to pale lavender, Luster: Vitreous (glassy), Crystal system: Hexagonal, Cleavage: None (conchoidal fracture), Specific Gravity: 2.65

Formation & geological history

Formed in hydrothermal veins or volcanic geodes where silica-rich fluids crystallized over millions of years. The purple color comes from irradiation of iron impurities within the quartz structure. Typically Cretaceous or Tertiary in age.

Uses & applications

Primarily used in jewelry, as ornamental display specimens, and in metaphysical practices. Also a popular collector gemstone.

Geological facts

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

Field identification & locations

Identify in the field by its purple crystalline quartz structure often sitting atop a banded chalcedony (agate) or basalt base. Commonly found in Brazil, Uruguay, Zambia, and Arizona. Look for hexagonal terminations and color zoning.