
mineral
Amethyst
Quartz (Silicon Dioxide with Iron impurities), SiO2
Hardness: 7 (Mohs scale); Color: Purple to violet due to irradiation and iron impurities; Luster: Vitreous; Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 (Mohs scale)
- Color
- Purple to violet due to irradiation and iron impurities
- Luster
- Vitreous
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Physical properties
Hardness: 7 (Mohs scale); Color: Purple to violet due to irradiation and iron impurities; Luster: Vitreous; Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed in hydrothermal veins or inside volcanic geodes (amygdules) when silica-rich water deposits crystals. The purple color is caused by the presence of trace amounts of trivalent iron (Fe3+) and natural gamma radiation within the host rock.
Uses & applications
Extensively used in jewelry (rings, necklaces), as decorative geodes, and in metaphysical/collecting communities. High-grade specimens are faceted into gemstones.
Geological facts
Amethyst is the birthstone for February. The name comes from the Ancient Greek 'amethystos', meaning 'not intoxicated', as it was believed to protect the wearer from drunkenness.
Field identification & locations
Identify by its distinct purple hue and 7 hardness (it will scratch glass). Often shows color zoning or white quartz bands (chevron amethyst). Commonly found in Brazil, Uruguay, and Zambia.
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