
gemstone
Polished amethyst quartz
Quartz, SiO₂; purple coloration from trace iron and irradiation
AI-generated identification · may be incorrectMohs hardness 7; translucent white to lavender-purple, with a vitreous luster and typically no visible cleavage. Hexagonal crystal structure; specific gravity about 2.65, though this specimen is cut and polished.
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Physical properties
Mohs hardness 7; translucent white to lavender-purple, with a vitreous luster and typically no visible cleavage. Hexagonal crystal structure; specific gravity about 2.65, though this specimen is cut and polished.
Formation & geological history
Forms when silica-rich hydrothermal fluids fill cavities in volcanic rocks, commonly basalt, where quartz crystals grow over millions of years. The pictured piece is human-cut from amethyst-bearing quartz.
Uses & applications
Used as a decorative gemstone, cabochon, carving material, and collector specimen; also sold for ornamental and metaphysical purposes. It is less commonly used industrially than ordinary quartz.
Geological facts
Amethyst is the purple variety of quartz; heating can turn it yellow-orange, producing citrine. Color commonly occurs in bands or zones, and pale material may be marketed as “chevron” or “lavender” amethyst when combined with milky quartz.
Field identification & locations
Identify it by purple zoning, glassy luster, hardness sufficient to scratch glass, and lack of cleavage; fluorite and glass are softer. Common sources include Brazil, Uruguay, Zambia, Bolivia, and Mexico.
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