
mineral
Amethyst
Silicon Dioxide (SiO2) with iron impurities
AI-generated identification · may be incorrectHardness: 7 (Mohs scale); Color: Purple, violet, or lavender; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 (Mohs scale)
- Color
- Purple, violet, or lavender
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 (Mohs scale); Color: Purple, violet, or lavender; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed in hydrothermal veins or as linings in geodes. The purple color is caused by natural irradiation of trace iron impurities within the quartz crystal lattice. Found in volcanic rocks and metamorphic environments.
Uses & applications
Primarily used in jewelry (faceting and cabochons), decorative home decor, and as a popular specimen for mineral collectors.
Geological facts
Amethyst was once considered one of the 'Cardinal Gems' alongside diamond, ruby, sapphire, and emerald until large deposits were found in Brazil. Its 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 characteristic purple color, hexagonal crystal habit (if points are present), and inability to be scratched by a steel knife. Common locations include Brazil, Uruguay, Africa (Zambia), and Arizona, USA.
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Sandstone (with potential mineral staining/concretions)
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Epidote
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Granite
Granite (Phaneritic intrusive igneous rock)
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