
mineral
Amethyst
Silicon Dioxide (SiO2) with iron impurities
Hardness: 7 (Mohs scale); Color: Pale lilac to deep purple; Luster: Vitreous (glass-like); Crystal structure: Hexagonal/Trigonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65
- Hardness
- 7 (Mohs scale)
- Color
- Pale lilac to deep purple
- Luster
- Vitreous (glass-like)
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Physical properties
Hardness: 7 (Mohs scale); Color: Pale lilac to deep purple; Luster: Vitreous (glass-like); Crystal structure: Hexagonal/Trigonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65
Formation & geological history
Formed in hydrothermal veins and basaltic geodes. Secondary minerals crystallize from silica-rich solutions in cavities. The purple color is caused by gamma irradiation of trivalent iron (Fe3+) in the quartz structure.
Uses & applications
Primarily used for jewelry, lapidary arts, decorative items, and as a popular collector specimen. Historically used for amulets and carvings.
Geological facts
The name comes from the Ancient Greek word 'amethystos', meaning 'not intoxicated', as it was believed to prevent drunkenness. It is the birthstone for February.
Field identification & locations
Identify by purple hue and hexagonal crystal terminal faces. Commonly found in Brazil, Uruguay, Zambia, and South Korea. Collectors look for deep color saturation and clarity.
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Schist
Schist
Metamorphic
Potassium Feldspar (Orthoclase)
Orthoclase (KAlSi3O8)
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Gypsum (variety Selenite or Alabaster)
Calcium sulfate dihydrate (CaSO4·2H2O)
Mineral
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
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