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

Quartz Pebble

Silicon Dioxide (SiO2)

AI-generated identification · may be incorrect

Hardness of 7 on the Mohs scale, white to translucent color, vitreous luster, trigonal crystal system, and conchoidal fracture with no true cleavage.

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Physical properties

Hardness of 7 on the Mohs scale, white to translucent color, vitreous luster, trigonal crystal system, and conchoidal fracture with no true cleavage.

Formation & geological history

Formed via the accumulation of weathered quartz grains deposited in rivers or beaches, then smoothed by water abrasion over thousands to millions of years.

Uses & applications

Used in landscaping, decorative paths, abrasive manufacturing, and as a raw material for glass and electronics.

Geological facts

Quartz is one of the most abundant minerals on Earth's continental crust and is exceptionally resistant to chemical weathering.

Field identification & locations

Easily identified by its high hardness (scratches glass) and smooth, rounded water-worn shape. Found worldwide in stream beds, beaches, and gravel deposits.