
mineral
Amethyst cluster
Amethyst, purple quartz (SiO₂)
AI-generated identification · may be incorrectMohs hardness 7; purple, vitreous luster, typically hexagonal quartz crystals with indistinct cleavage and conchoidal fracture; specific gravity about 2.65. The specimen appears to be a natural crystal cluster or crystal-lined fragment, possibly with darker matrix attached.
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Physical properties
Mohs hardness 7; purple, vitreous luster, typically hexagonal quartz crystals with indistinct cleavage and conchoidal fracture; specific gravity about 2.65. The specimen appears to be a natural crystal cluster or crystal-lined fragment, possibly with darker matrix attached.
Formation & geological history
Forms when iron-bearing quartz in volcanic cavities is exposed to mildly radioactive or oxidizing fluids, commonly in basalt geodes. Many commercial specimens formed in Mesozoic–Cenozoic volcanic regions, especially Brazil and Uruguay.
Uses & applications
Used as a gemstone, ornamental display stone, carved object, and popular collecting specimen; fine transparent crystals are faceted, while clusters are decorative.
Geological facts
Purple color results mainly from irradiation-related defects involving iron impurities. Heating can turn amethyst yellow or orange, producing citrine-like material.
Field identification & locations
Identify by purple quartz crystals, glassy luster, hardness sufficient to scratch ordinary glass, and lack of obvious cubic cleavage. Common sources include Brazil, Uruguay, Zambia, Namibia, and Mexico.
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