Rock Identifier
Polished brown gemstone, likely smoky quartz (Smoky quartz (quartz, SiO₂), possibly brown chalcedony or tiger’s-eye based on the photograph) — gemstone
gemstone

Polished brown gemstone, likely smoky quartz

Smoky quartz (quartz, SiO₂), possibly brown chalcedony or tiger’s-eye based on the photograph

AI-generated identification · may be incorrect

Translucent brown to honey color with a vitreous polish and no visible crystals; quartz has Mohs hardness 7, conchoidal fracture, hexagonal crystal structure, and specific gravity about 2.65. The rounded shape indicates a tumbled or cabochon-cut specimen.

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Physical properties

Translucent brown to honey color with a vitreous polish and no visible crystals; quartz has Mohs hardness 7, conchoidal fracture, hexagonal crystal structure, and specific gravity about 2.65. The rounded shape indicates a tumbled or cabochon-cut specimen.

Formation & geological history

Smoky quartz forms when natural radiation colors quartz in granitic pegmatites, hydrothermal veins, and metamorphic rocks, generally from Precambrian to younger geologic settings. Exact identification and age require testing or provenance.

Uses & applications

Used for inexpensive jewelry, lapidary ornaments, carvings, and mineral collecting. Common polished pieces typically have modest commercial value.

Geological facts

Color intensity comes from radiation-induced defects associated with aluminum impurities; heating can remove the smoky color. Similar brown stones include glass, jasper, amber, and tiger’s-eye.

Field identification & locations

Check for quartz-like hardness, glassy luster, and conchoidal fracture; a steel file should not scratch it, while quartz should scratch ordinary glass. Common sources include Brazil, Madagascar, Switzerland, and the United States.