
mineral
Amethyst (likely rough or cleaved crystal)
Quartz, silicon dioxide (SiO₂), purple variety colored mainly by iron impurities and irradiation
AI-generated identification · may be incorrectTypically Mohs hardness 7, vitreous luster, conchoidal fracture, and hexagonal crystal structure; this specimen appears dark purple and opaque-to-translucent, though the blurred image limits certainty. No obvious cleavage is expected.
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Physical properties
Typically Mohs hardness 7, vitreous luster, conchoidal fracture, and hexagonal crystal structure; this specimen appears dark purple and opaque-to-translucent, though the blurred image limits certainty. No obvious cleavage is expected.
Formation & geological history
Forms when iron-bearing quartz crystallizes in gas cavities and fractures of volcanic rocks, especially basalt, from silica-rich hydrothermal fluids; commonly Cenozoic to older, depending on deposit.
Uses & applications
Used as a gemstone, ornamental stone, crystal specimen, and in polished geodes or décor. It is also popular in mineral collecting and metaphysical markets.
Geological facts
Purple color intensity varies with iron content and heat exposure; heating can produce yellow citrine or green prasiolite-like material. Amethyst is February’s birthstone.
Field identification & locations
Common localities include Brazil, Uruguay, Zambia, Namibia, and Mexico. Confirm with a glass-scratching test only cautiously, inspect for quartz-like fracture, and avoid relying on color alone because dyed glass or slag can resemble it.
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