Rock Identifier
Quartz pebble (Silicon dioxide (SiO2)) — sedimentary
sedimentary

Quartz pebble

Silicon dioxide (SiO2)

Hardness of 7 on the Mohs scale, typically white, gray, or clear, vitreous luster, hexagonal crystal structure when unweathered, conchoidal fracture, specific gravity of 2.65

Identified More sedimentary
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Physical properties

Hardness of 7 on the Mohs scale, typically white, gray, or clear, vitreous luster, hexagonal crystal structure when unweathered, conchoidal fracture, specific gravity of 2.65

Formation & geological history

Formed through the weathering and erosion of parent rocks, followed by transport via water and deposition in sedimentary environments such as rivers or beaches over geological timescales

Uses & applications

Used in landscaping, decorative gravel, aggregate in construction, and as raw material for glassmaking

Geological facts

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

Field identification & locations

Found worldwide in riverbeds, beaches, and conglomerate rock formations; identified by its high hardness (scratches glass) and conchoidal fracture