
mineral
Amethyst
Silicon Dioxide (SiO2) with iron impurities
Hardness: 7 (Mohs scale); Color: Pale violet to deep purple; Luster: Vitreous; Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 (Mohs scale)
- Color
- Pale violet to deep purple
- Luster
- Vitreous
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Physical properties
Hardness: 7 (Mohs scale); Color: Pale violet to deep purple; Luster: Vitreous; Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed in hydrothermal veins or geodes within igneous rocks. Purple coloration is caused by irradiation of iron impurities in the quartz lattice.
Uses & applications
Primary use in jewelry, decorative items, and as a popular collector specimen. Historically believed to prevent intoxication.
Geological facts
Amethyst was once considered one of the 'cardinal gems' along with diamond, ruby, and emerald until large deposits were found in Brazil.
Field identification & locations
Look for purple crystalline quartz clusters. Common in Brazil, Uruguay, and South Korea. Collectors should look for deep uniform color and lack of visible inclusions.
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