
mineral
Amethyst geode or polished amethyst slice
Quartz, SiO₂; purple coloration from iron-related defects and irradiation
AI-generated identification · may be incorrectHardness 7 Mohs; purple, translucent to transparent, with vitreous luster and hexagonal quartz crystals lining or comprising the specimen. Quartz has no cleavage, conchoidal fracture, and specific gravity about 2.65; the dark parallel bands may indicate agate or iron-oxide zoning.
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Physical properties
Hardness 7 Mohs; purple, translucent to transparent, with vitreous luster and hexagonal quartz crystals lining or comprising the specimen. Quartz has no cleavage, conchoidal fracture, and specific gravity about 2.65; the dark parallel bands may indicate agate or iron-oxide zoning.
Formation & geological history
Formed when silica-rich groundwater deposited quartz in volcanic vesicles, commonly during the Mesozoic to Cenozoic; later cutting and polishing produced the flat display face. Exact age and locality cannot be determined from the photograph.
Uses & applications
Used as a decorative stone, lapidary material, jewelry, and mineral-collection specimen; value depends strongly on color saturation, crystal quality, size, and provenance.
Geological facts
Amethyst is the purple variety of quartz and is often associated with gray, white, or reddish chalcedony and druzy quartz. Strong sunlight or heating can fade or alter its color.
Field identification & locations
Identify it by purple quartz, glassy luster, hardness, and lack of cleavage; common sources include Brazil, Uruguay, Zambia, and Namibia. A scratch test should be avoided on polished pieces; inspect for natural crystal texture rather than glass bubbles.
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