Rock Identifier
Quartz Pebble (Silicon Dioxide (SiO2)) — sedimentary
sedimentary

Quartz Pebble

Silicon Dioxide (SiO2)

Hardness of 7 on the Mohs scale, white to greyish color with a vitreous to greasy luster, trigonal crystal system, conchoidal fracture, and a specific gravity of around 2.65.

Identified More sedimentary
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Physical properties

Hardness of 7 on the Mohs scale, white to greyish color with a vitreous to greasy luster, trigonal crystal system, conchoidal fracture, and a specific gravity of around 2.65.

Formation & geological history

Formed through the accumulation and weathering of durable quartz grains over millions of years, often rounded by water transport in rivers or beaches.

Uses & applications

Used in landscaping, decorative stone, manufacturing of glass, and abrasive materials.

Geological facts

Quartz is one of the most abundant and durable minerals in the Earth's continental crust, highly resistant to both chemical and mechanical weathering.

Field identification & locations

Easily identified by its high hardness (scratches glass) and conchoidal fracture. Commonly found in riverbeds, beaches, and conglomerate rocks worldwide.