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

Amethyst

Quartz (Silicon Dioxide with iron impurities), SiO2

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

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

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

Formation & geological history

Forms in hydrothermal veins and hollow rocks (geodes) when silica-rich water cools. The purple color is caused by natural irradiation of trace iron impurities within the quartz lattice. Geologic age varies based on locality.

Uses & applications

Extensively used in jewelry, as decorative display pieces, for lapidary work, and among mineral collectors.

Geological facts

Amethyst was considered a Cardinal Gem until the 18th century, ranking alongside diamonds and rubies in value until large deposits were found in Brazil. Its name comes from the Ancient Greek 'amethystos', meaning 'not intoxicated'.

Field identification & locations

Identified by its purple color and typical quartz crystal habit (6-sided prisms) or conchoidal fracture. Common locations include Brazil, Uruguay, Zambia, and South Korea. Look for hexagonal points and characteristic growth striations.