
mineral
Amethyst (purple quartz)
Quartz, silicon dioxide (SiO₂), purple variety colored mainly by iron impurities and irradiation
AI-generated identification · may be incorrectHardness 7 Mohs; translucent lavender-purple color, vitreous luster, conchoidal fracture, trigonal crystal structure, and no cleavage. The piece appears cut or broken, with visible crystalline translucency.
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Physical properties
Hardness 7 Mohs; translucent lavender-purple color, vitreous luster, conchoidal fracture, trigonal crystal structure, and no cleavage. The piece appears cut or broken, with visible crystalline translucency.
Formation & geological history
Forms in silica-rich hydrothermal fluids filling cavities in volcanic rocks, especially basaltic geodes; many amethysts formed during the Mesozoic and Cenozoic. The image alone cannot establish its precise age or locality.
Uses & applications
Used as a gemstone, ornamental stone, and collector specimen; lower-grade material is used for carvings, beads, and polished objects. It has no major structural or industrial use compared with ordinary quartz.
Geological facts
Purple color ranges from pale lilac to deep violet and can fade with prolonged heat or sunlight. Amethyst is February’s birthstone and a variety of quartz, not a separate mineral species.
Field identification & locations
Identify it by its purple color, glassy luster, hardness, and lack of cleavage; glass may imitate it but is generally softer and often contains bubbles. Common sources include Brazil, Uruguay, Zambia, and Bolivia.
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