
mineral
Amethyst (Druze)
Silicon Dioxide (SiO2) with iron impurities
Hardness: 7 on Mohs scale; Color: Pale lilac to deep purple; Luster: Vitreous (glassy); Crystal Structure: Hexagonal/Trigonal (terminating in six-sided pyramids); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Pale lilac to deep purple
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 on Mohs scale; Color: Pale lilac to deep purple; Luster: Vitreous (glassy); Crystal Structure: Hexagonal/Trigonal (terminating in six-sided pyramids); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed in hydrothermal veins or cavities (geodes) when silica-rich water precipitates crystals at low to moderate temperatures. Common in volcanic basalt pockets. Many commercial specimens are from the Cretaceous period.
Uses & applications
Used extensively in jewelry (as a semi-precious gemstone), decorative carvings, and as a popular specimen for mineral collectors. Also used in spiritual or metaphysical practices.
Geological facts
Amethyst is the purple variety of quartz; its color comes from irradiation of trivalent iron impurities. The name comes from the Greek 'amethystos', meaning 'not intoxicated', as it was once believed to prevent drunkenness.
Field identification & locations
Identify by its purple hue, hexagonal crystal points, and ability to scratch glass. Found globally, with major deposits in Brazil (Rio Grande do Sul) and Uruguay. Look for it in volcanic rock outcrops or inside rounded 'thunder egg' nodules.
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