
mineral
Amethyst
Amethyst (Silicon Dioxide - SiO2 with iron impurities)
Hardness: 7 on Mohs scale; Color: Pale violet to deep purple (tumbled); Luster: Vitreous (glass-like); Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Pale violet to deep purple (tumbled)
- Luster
- Vitreous (glass-like)
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Physical properties
Hardness: 7 on Mohs scale; Color: Pale violet to deep purple (tumbled); Luster: Vitreous (glass-like); Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
Formation & geological history
Formed in hydrothermal veins or as linings inside volcanic geodes (amygdules). The purple color results from irradiation, iron impurities, and the presence of trace elements. Age varies by location, often associated with Cretaceous basalt flows in Brazil/Uruguay.
Uses & applications
Primarily used in jewelry, ornamental carvings, and as a popular specimen for gemstone collectors. Industrially, it has been used in glassmaking and abrasives due to its hardness.
Geological facts
Formerly considered one of the 'Cardinal Gems' along with diamond and ruby until large deposits were found in South America. The name comes from the Greek 'amethystos', meaning 'not intoxicated', as it was anciently believed to prevent drunkenness.
Field identification & locations
Identify in the field by its purple hue and inability to be scratched by steel. Commonly found in Brazil, Uruguay, Madagascar, and Ontario. Collectors should look for saturated color and clarity in tumbled stones.
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