
gemstone
Chevron amethyst point
Quartz, SiO₂, with purple amethyst and white quartz zoning
AI-generated identification · may be incorrectHardness 7 Mohs; purple to lilac and white bands, vitreous luster, hexagonal quartz structure, and no prominent cleavage. The polished, carved point appears to contain cloudy inclusions and possible druzy quartz.
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Physical properties
Hardness 7 Mohs; purple to lilac and white bands, vitreous luster, hexagonal quartz structure, and no prominent cleavage. The polished, carved point appears to contain cloudy inclusions and possible druzy quartz.
Formation & geological history
Forms when iron-bearing silica-rich fluids deposit quartz in cavities, with irradiation and trace iron producing amethyst; chevron banding commonly reflects alternating quartz and amethyst growth. Most commercial material comes from Brazil, Uruguay, Zambia, and India, generally formed in volcanic rocks over millions of years.
Uses & applications
Used for ornamental points, jewelry, carvings, mineral collections, and metaphysical objects; it has little structural or industrial use beyond quartz-based applications.
Geological facts
Chevron amethyst is a trade name for alternating V-shaped or zigzag amethyst and white quartz bands, not a separate mineral species. Color can fade with prolonged intense sunlight or heat.
Field identification & locations
Identify it by purple quartz zones, white zigzag banding, glassy luster, and hardness sufficient to scratch ordinary glass; a steel knife should not scratch it. Common sources include Brazil, Uruguay, Zambia, and India.
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