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

Amethyst

Silicon Dioxide (SiO2) with iron impurities

Hardness: 7 (Mohs scale); Color: Pale violet to deep purple; Luster: Vitreous; Crystal Structure: Hexagonal (trigonal); Cleavage: None/Conchoidal fracture; Specific Gravity: 2.65

Hardness
7 (Mohs scale)
Color
Pale violet to deep purple
Luster
Vitreous
Identified More mineral
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Physical properties

Hardness: 7 (Mohs scale); Color: Pale violet to deep purple; Luster: Vitreous; Crystal Structure: Hexagonal (trigonal); Cleavage: None/Conchoidal fracture; Specific Gravity: 2.65

Formation & geological history

Formed in hydrothermal veins and volcanic geodes. The purple color results from irradiation of trivalent iron (Fe3+) in the quartz structure. These can range from hundreds of millions to a few million years old.

Uses & applications

Primarily used as a gemstone in jewelry, for decorative carvings, and value by collectors for its aesthetic and 'metaphysical' appeal.

Geological facts

Amethyst was once considered one of the 'Cardinal gems' (precious along with diamond, ruby, sapphire, and emerald) until large deposits were found in Brazil in the 19th century.

Field identification & locations

Identify by its purple hue and ability to scratch glass but not topaz. Commonly found in Brazil, Uruguay, Zambia, and Canada. Look for hexagonal crystal points in geodes.