Rock Identifier
Rounded quartz pebble (Quartz (SiO₂), possibly milky or smoky quartz) — mineral
mineral

Rounded quartz pebble

Quartz (SiO₂), possibly milky or smoky quartz

AI-generated identification · may be incorrect

Small tumbled/abraded pebble with pale gray-beige color, translucent edges, and dull to weakly glassy luster. Quartz has Mohs hardness 7, no cleavage, conchoidal fracture, hexagonal crystal structure, and specific gravity about 2.65.

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Physical properties

Small tumbled/abraded pebble with pale gray-beige color, translucent edges, and dull to weakly glassy luster. Quartz has Mohs hardness 7, no cleavage, conchoidal fracture, hexagonal crystal structure, and specific gravity about 2.65.

Formation & geological history

Likely weathered from quartz-rich igneous or metamorphic rock and rounded by stream or beach transport; its precise geological age and source cannot be determined from the image.

Uses & applications

Common quartz pebbles are used in landscaping, crafts, collections, and occasionally jewelry; this specimen has minimal commercial value unless unusually clear or from a documented locality.

Geological facts

Quartz is one of Earth’s most abundant minerals and is highly resistant to chemical and physical weathering, allowing it to survive as rounded sediment.

Field identification & locations

Check for hardness by testing glass (quartz should scratch it), lack of cleavage, and translucent gray-white appearance; common worldwide in river gravels, beaches, veins, and quartz-rich rocks.