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

Quartz

Silicon Dioxide (SiO2)

AI-generated identification · may be incorrect

Hardness of 7 on the Mohs scale, white to translucent color, vitreous luster, trigonal crystal system, conchoidal fracture with no true cleavage, and specific gravity around 2.65.

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Physical properties

Hardness of 7 on the Mohs scale, white to translucent color, vitreous luster, trigonal crystal system, conchoidal fracture with no true cleavage, and specific gravity around 2.65.

Formation & geological history

Formed through crystallization from silica-rich hydrothermal solutions or cooling magmas, widely found in igneous, metamorphic, and sedimentary rocks across all geological eras.

Uses & applications

Used in electronics, glassmaking, abrasives, decorative items, and as a gemstone in jewelry.

Geological facts

Quartz is the second most abundant mineral in Earth's continental crust and exhibits strong piezoelectric properties.

Field identification & locations

Easily identified by its high hardness (scratches glass) and lack of cleavage, commonly found in river gravels, veins, and pegmatites worldwide.