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

Quartz Pebble

Silicon Dioxide (SiO2)

Hardness: 7 (Mohs), Color: Off-white/cloudy with tan inclusions, Luster: Vitreous to greasy (when weathered), Crystal System: Hexagonal (trigonal), Cleavage: None/Conchoidal fracture.

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Physical properties

Hardness: 7 (Mohs), Color: Off-white/cloudy with tan inclusions, Luster: Vitreous to greasy (when weathered), Crystal System: Hexagonal (trigonal), Cleavage: None/Conchoidal fracture.

Formation & geological history

Formed via hydrothermal activity or crystallization from cooling magma. This specific specimen is a water-worn or weathered pebble likely eroded from a larger quartz vein and transported by fluvial processes.

Uses & applications

Industrial use in glassmaking, electronics (piezoelectric properties), abrasives, and as a common decorative landscape stone.

Geological facts

Quartz is the second most abundant mineral in Earth's continental crust. Pure quartz is clear, but tiny inclusions of air or fluid create the 'milky' appearance seen in this pebble.

Field identification & locations

Identify by its inability to be scratched by a steel knife (hardness) and the lack of cleavage. Commonly found in riverbeds, glacial deposits, and mountain ranges globally.