
mineral
Amethyst geode slice
Quartz (SiO₂), purple variety amethyst; commonly a volcanic vesicle geode
AI-generated identification · may be incorrectHardness 7 Mohs; white-to-gray chalcedony/quartz rind with purple crystalline quartz interior, vitreous luster, hexagonal crystals, and no prominent cleavage. Purple color comes mainly from iron impurities and irradiation.
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Physical properties
Hardness 7 Mohs; white-to-gray chalcedony/quartz rind with purple crystalline quartz interior, vitreous luster, hexagonal crystals, and no prominent cleavage. Purple color comes mainly from iron impurities and irradiation.
Formation & geological history
Forms when silica-rich groundwater deposits quartz and amethyst crystals inside cavities in basaltic volcanic rocks. Most commercial examples formed in Mesozoic–Cenozoic volcanic provinces, especially Brazil and Uruguay.
Uses & applications
Used as a decorative specimen, jewelry, cabochons, and crystal-collecting material; small slices commonly sell as affordable ornaments.
Geological facts
The outer band is typically microcrystalline quartz or chalcedony, while the cavity contains larger drusy crystals. Deeper violet color generally increases desirability, though natural color zoning is common.
Field identification & locations
Identify it by the hard, glassy purple quartz crystals lining a hollow, contrasting with a pale chalcedony rind; it should scratch glass but not be scratched by a steel knife. Common sources include Brazil, Uruguay, Mexico, and Morocco.
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