Rock Identifier
Likely tumbled or polished dark purple mineral (Possibly amethyst (purple quartz, SiO₂), though the image is insufficient for confident identification) — mineral
mineral

Likely tumbled or polished dark purple mineral

Possibly amethyst (purple quartz, SiO₂), though the image is insufficient for confident identification

AI-generated identification · may be incorrect

Violet-gray, translucent to opaque, with a glassy luster and irregular fracture; quartz hardness is 7 Mohs, trigonal crystal structure, and no cleavage. The dark appearance may result from inclusions, coating, or low lighting.

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Physical properties

Violet-gray, translucent to opaque, with a glassy luster and irregular fracture; quartz hardness is 7 Mohs, trigonal crystal structure, and no cleavage. The dark appearance may result from inclusions, coating, or low lighting.

Formation & geological history

If amethyst, it formed when iron-bearing quartz crystallized in gas cavities of volcanic rocks, commonly during the Mesozoic to Cenozoic. Geological age cannot be determined from the photograph.

Uses & applications

Amethyst is used for jewelry, ornaments, and mineral collecting; lower-grade material is sold as polished stones. Value depends strongly on color, transparency, and treatment.

Geological facts

The specimen could also be purple fluorite, glass, or another coated mineral; a clear view of crystal faces and tests are needed.

Field identification & locations

Check for consistent purple color, quartz-like glassy fracture, and hardness: it should scratch ordinary glass but not be scratched by steel. Common amethyst sources include Brazil, Uruguay, Zambia, and Mexico.