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

Quartz Pebble

Silicon Dioxide (SiO2)

Hardness: 7 (Mohs scale), Color: tan to yellowish-brown (likely due to iron staining), Luster: vitreous to waxy, Crystal structure: Hexagonal (trigonal), Cleavage: None/Conchoidal fracture, Specific gravity: 2.65

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Physical properties

Hardness: 7 (Mohs scale), Color: tan to yellowish-brown (likely due to iron staining), Luster: vitreous to waxy, Crystal structure: Hexagonal (trigonal), Cleavage: None/Conchoidal fracture, Specific gravity: 2.65

Formation & geological history

Formed through the cooling of silica-rich magma or precipitation from hydrothermal veins. This specific specimen is a water-worn river pebble, shaped by mechanical erosion over time.

Uses & applications

Commonly used in construction (sand/gravel), glassmaking, electronics (piezoelectric properties), and as decorative landscaping stone.

Geological facts

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

Field identification & locations

Identify by its ability to scratch glass, its lack of cleavage, and its typical translucent appearance. It can be found globally in almost all geological environments.