
mineral
Amethyst
Silicon Dioxide (SiO2)
Hardness: 7 on the Mohs scale. Color: Purple to violet, occasionally dark violet or brownish. Luster: Vitreous (glassy). Crystal Structure: Trigonal, commonly forming prismatic crystals with pyramidal terminations, often doubly terminated as seen in Herkimer-style or growth-matrix specimens.…
- Hardness
- 7 on the Mohs scale
- Color
- Purple to violet, occasionally dark violet or brownish
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 on the Mohs scale. Color: Purple to violet, occasionally dark violet or brownish. Luster: Vitreous (glassy). Crystal Structure: Trigonal, commonly forming prismatic crystals with pyramidal terminations, often doubly terminated as seen in Herkimer-style or growth-matrix specimens. Cleavage: None (conchoidal fracture). Specific Gravity: 2.65.
Formation & geological history
Formed in hydrothermal veins and cavities (vugs or geodes) within basaltic and other volcanic rocks, where silica-rich fluids cool and crystallize over millions of years under the influence of natural irradiation of trace iron impurities.
Uses & applications
Widely used in jewelry, lapidary arts, decorative items, and as highly prized specimens for mineral collectors.
Geological facts
Amethyst was historically considered one of the 'cardinal' precious gems, equal in value to diamond, ruby, and sapphire, until extensive deposits were discovered in Brazil in the 19th century.
Field identification & locations
Easily identified by its characteristic purple coloration, high hardness (scratches glass), and vitreous luster. Commonly sourced from Brazil, Uruguay, Zambia, and parts of the United States.
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