Rock Identifier
Quartz (River Pebble) (Silicon Dioxide (SiO2)) — mineral
mineral

Quartz (River Pebble)

Silicon Dioxide (SiO2)

Hardness: 7 Mohs; Color: Grayish-white, translucent; Luster: Vitreous/Waxy; Crystal Structure: Trigonal; Cleavage: None/Conchoidal fracture; Specific Gravity: 2.65

Hardness
7 Mohs
Color
Grayish-white, translucent
Luster
Vitreous/Waxy
Identified More mineral
Explore Quartz (River Pebble) in the encyclopedia →

Identify your own rocks.

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

Physical properties

Hardness: 7 Mohs; Color: Grayish-white, translucent; Luster: Vitreous/Waxy; Crystal Structure: Trigonal; Cleavage: None/Conchoidal fracture; Specific Gravity: 2.65

Formation & geological history

Formed from silica-rich hydrothermal fluids or crystallization from magma. This specific specimen has been rounded and smoothed by water erosion in a fluvial (river) environment.

Uses & applications

Common quartz is used in construction as aggregate, in glassmaking, and as an abrasive. Polished pebbles are used in landscaping and aquariums.

Geological facts

Quartz is the second most abundant mineral in Earth's continental crust. It is chemically very stable, which is why quartz pebbles often remain long after other minerals have weathered away.

Field identification & locations

Identified by its hardness (can scratch glass), lack of cleavage, and rounded 'river stone' shape. Found globally in riverbeds, beaches, and glacial deposits.