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

Quartz Pebbles

Silicon Dioxide (SiO2)

AI-generated identification · may be incorrect

Hardness of 7 on the Mohs scale, vitreous luster, conchoidal fracture, and lack of cleavage. Colors range from translucent yellow-orange to white and pink due to iron oxide impurities.

Identified More sedimentary →
Explore Quartz Pebbles in the encyclopedia →

Identify your own rocks.

Get a report just like this from any photo, free.

Physical properties

Hardness of 7 on the Mohs scale, vitreous luster, conchoidal fracture, and lack of cleavage. Colors range from translucent yellow-orange to white and pink due to iron oxide impurities.

Formation & geological history

Formed through the weathering and water-transport of quartz-rich parent rocks, becoming rounded pebbles over long periods in fluvial or marine environments.

Uses & applications

Used in landscaping, decorative stone, aquarium gravel, and as abrasive media.

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

Easily identified in the field by its high hardness (scratches glass) and smooth, water-worn tumbled shape found in riverbeds and beaches.