
mineral
Raw amethyst quartz
Amethyst, purple variety of quartz (SiO₂)
AI-generated identification · may be incorrectHardness 7 Mohs; translucent purple to lavender, with a vitreous luster and conchoidal fracture. Trigonal quartz crystals are present or partly obscured; the pale matrix may include milky quartz and minor host-rock material.
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Physical properties
Hardness 7 Mohs; translucent purple to lavender, with a vitreous luster and conchoidal fracture. Trigonal quartz crystals are present or partly obscured; the pale matrix may include milky quartz and minor host-rock material.
Formation & geological history
Forms when iron-bearing quartz is irradiated by natural radiation in volcanic cavities, hydrothermal veins, and geodes. Individual specimens commonly formed during relatively young volcanic episodes, though exact age depends on locality.
Uses & applications
Used for jewelry, carvings, polished specimens, and mineral collecting; gem-quality material has greater value than cloudy or fractured pieces.
Geological facts
Purple color results mainly from irradiation-induced defects involving iron impurities. Heating can produce yellow citrine or reddish-brown “burnt amethyst.”
Field identification & locations
Identify by purple zoning, glassy luster, hardness sufficient to scratch glass, and lack of obvious cleavage; quartz fractures rather than cleaves. Common sources include Brazil, Uruguay, Zambia, Bolivia, and Mexico.
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