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

Quartz (River Pebble)

Silicon Dioxide (SiO2)

Hardness: 7 (Mohs scale), Color: Milky white to translucent pale yellow, Luster: Vitreous to waxy (when water-worn), Crystal Structure: Trigonal/Hexagonal, Cleavage: None (conchoidal fracture), Specific Gravity: 2.65

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 scale), Color: Milky white to translucent pale yellow, Luster: Vitreous to waxy (when water-worn), Crystal Structure: Trigonal/Hexagonal, Cleavage: None (conchoidal fracture), Specific Gravity: 2.65

Formation & geological history

Formed through the cooling of silica-rich magma or from hydrothermal veins. This specific specimen has been smoothed and rounded by the mechanical action of water in a river or stream environment over thousands of years.

Uses & applications

Raw quartz is used in glass making, electronics (due to piezoelectric properties), and as an abrasive. Smooth river pebbles are commonly used in landscaping, aquarium decor, and home ornamentation.

Geological facts

Quartz is the second most abundant mineral in Earth's continental crust. Its name comes from the German word 'quarz', which likely has Slavic origins meaning 'hard'.

Field identification & locations

Identify in the field by its hardness (it will scratch glass and steel) and lack of cleavage. It is found globally in riverbeds, beaches, and mountain soil. Collectors look for clarity or unique smooth shapes.