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

Quartz

Silicon Dioxide (SiO2)

AI-generated identification · may be incorrect

Mohs hardness of 7; white, clear, or translucent; vitreous luster; trigonal crystal system; conchoidal fracture with no cleavage; specific gravity of 2.65.

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Physical properties

Mohs hardness of 7; white, clear, or translucent; vitreous luster; trigonal crystal system; conchoidal fracture with no cleavage; specific gravity of 2.65.

Formation & geological history

Formed through crystallization from silicate melts in igneous environments, hydrothermal veins, and precipitation in sedimentary rocks over wide geological timescales.

Uses & applications

Used extensively in glassmaking, electronics, abrasives, gemstones, and construction aggregate.

Geological facts

Quartz is the second most abundant mineral in Earth's continental crust and exhibits piezoelectric properties, making it vital for electronic oscillators.

Field identification & locations

Identified easily by its high hardness (scratches glass), lack of cleavage, and conchoidal fracture; found worldwide in almost all geological settings.