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

Quartz Pebble

Silicon Dioxide (SiO2)

Hardness of 7 on the Mohs scale, typically white, clear, or light brown, vitreous luster, hexagonal crystal system when formed well, conchoidal fracture with no true cleavage, specific gravity of 2.65.

Identified More sedimentary
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Physical properties

Hardness of 7 on the Mohs scale, typically white, clear, or light brown, vitreous luster, hexagonal crystal system when formed well, conchoidal fracture with no true cleavage, specific gravity of 2.65.

Formation & geological history

Formed from parent igneous or metamorphic rocks through weathering and erosion, then transported and rounded by water in rivers or beaches over thousands to millions of years.

Uses & applications

Used in landscaping, decorative stone, construction aggregate, and occasionally in lapidary work.

Geological facts

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

Field identification & locations

Found worldwide in riverbeds, beaches, and sedimentary deposits. Identified by its high hardness (scratches glass) and lack of cleavage.