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

Quartz Pebble

Silicon Dioxide (SiO2)

Hardness of 7 on the Mohs scale, typically white, grey, or pinkish in color, vitreous luster, conchoidal fracture, and no true cleavage.

Identified More sedimentary
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Physical properties

Hardness of 7 on the Mohs scale, typically white, grey, or pinkish in color, vitreous luster, conchoidal fracture, and no true cleavage.

Formation & geological history

Formed through mechanical weathering and water transportation of larger quartz-bearing rocks, commonly found in riverbeds, beaches, and alluvial deposits over geological timescales.

Uses & applications

Used in landscaping, decorative purposes, and as raw material for aggregate in construction.

Geological facts

Quartz is one of the most abundant and durable minerals on Earth's continental crust, surviving weathering processes that destroy other minerals.

Field identification & locations

Easily identified by its high hardness (scratches glass) and smooth, rounded shape resulting from water erosion. Found worldwide.