
mineral
Amethyst quartz crystal
Quartz, silicon dioxide (SiO₂), purple variety amethyst
AI-generated identification · may be incorrectHardness 7 Mohs; purple to violet with translucent areas and a vitreous luster. It has a hexagonal crystal structure and indistinct cleavage, commonly breaking conchoidally; the pale tip may be quartz or weathered matrix.
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Physical properties
Hardness 7 Mohs; purple to violet with translucent areas and a vitreous luster. It has a hexagonal crystal structure and indistinct cleavage, commonly breaking conchoidally; the pale tip may be quartz or weathered matrix.
Formation & geological history
Forms when iron-bearing quartz is irradiated within volcanic cavities, especially basaltic geodes and veins. Crystals range from ancient to relatively young, depending on the host rock and deposit.
Uses & applications
Used as a gemstone, ornamental specimen, and metaphysical collectible; also sold as crystal points and geode material. This rough, hand-sized specimen has modest commercial value.
Geological facts
Purple color results mainly from irradiation-related defects involving iron impurities. Heating can turn amethyst yellow-orange, producing citrine.
Field identification & locations
Identify it by purple quartz color, glassy luster, hardness, and lack of prominent cleavage; it should scratch glass but not be scratched by a steel knife. Common sources include Brazil, Uruguay, Zambia, and Mexico.
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