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

Amethyst

Silicon Dioxide (SiO2) with iron impurities

Hardness: 7 (Mohs scale); Color: Purple, violet, or lavender; Luster: Vitreous/Glassy; Crystal structure: 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: Trigonal; Cleavage: None/Conchoidal fracture; Specific gravity: 2.65

Formation & geological history

Formed in hydrothermal veins and basaltic geodes. The purple color comes from irradiation of iron impurities within the quartz crystal lattice. Found in rocks ranging from millions to over a billion years old.

Uses & applications

Mostly used for jewelry (faceted or cabochon), decorative ornaments, crystal healing, and as a popular specimen for mineral collectors.

Geological facts

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

Field identification & locations

Identify by its characteristic purple color and hexagonal crystal faces (if not tumbled). It can be found globally with major deposits in Brazil and Uruguay. Collectors should look for deep color saturation and clarity.