
mineral
Amethyst on Agate/Basalt Matrix
Silicon Dioxide (SiO2) with iron impurities
Hardness: 7 (Mohs); Color: Pale purple to lilac; Luster: Vitreous (glassy); Crystal structure: Hexagonal/Trigonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65
- Hardness
- 7 (Mohs)
- Color
- Pale purple to lilac
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 (Mohs); Color: Pale purple to lilac; Luster: Vitreous (glassy); Crystal structure: Hexagonal/Trigonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65
Formation & geological history
Formed in hydrothermal veins or cavities (vugs) within volcanic rocks. As mineral-rich water seeps into cavities in basalt, silica precipitates over millions of years, often starting as a layer of agate followed by crystalline quartz.
Uses & applications
Primary use is in jewelry, lapidary arts, and as collectible interior decor. Historically used as an amulet against intoxication and for spiritual/metaphysical practices.
Geological facts
Amethyst is the birthstone for February. Its purple color is caused by gamma irradiation of trivalent iron (Fe3+) in the crystal lattice. Most high-quality amethyst geodes come from Brazil and Uruguay.
Field identification & locations
Identify by its characteristic six-sided crystals with pyramidal terminations and purple hue. It is often found attached to a gray or green host rock (basalt) often with a thin layer of chalcedony or agate in between.
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