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

Amethyst Quartz

Silicon Dioxide (SiO2) with iron impurities

Hardness: 7 on Mohs scale; Color: Pale purple to violet with clear zones; Luster: Vitreous (glassy); Crystal structure: Trigonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65

Hardness
7 on Mohs scale
Color
Pale purple to violet with clear zones
Luster
Vitreous (glassy)
Identified More mineral
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Physical properties

Hardness: 7 on Mohs scale; Color: Pale purple to violet with clear zones; Luster: Vitreous (glassy); Crystal structure: Trigonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65

Formation & geological history

Formed in hydrothermal veins or geodes when silica-rich water cools. The purple color is caused by natural irradiation or iron impurities within the quartz lattice. Found globally in igneous and metamorphic environments.

Uses & applications

Primarily used as a gemstone in jewelry, for decorative items, lapidary arts, and by mineral collectors. Large specimens are used in architectural decor.

Geological facts

Amethyst is the birthstone for February. Its name comes from the Greek word 'amethystos', meaning 'not intoxicated', as ancient Greeks believed it could prevent drunkenness.

Field identification & locations

Identify by its 7 hardness (scratches glass), purple color, and lack of cleavage. Common in Brazil, Uruguay, and Africa. Small tumbled stones are basic entry points for new collectors.