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

Quartz

Silicon Dioxide (SiO2)

Hardness of 7 on the Mohs scale; white to clear or translucent color; vitreous (glassy) luster; trigonal crystal system; conchoidal fracture with no true cleavage; specific gravity of 2.65.

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Physical properties

Hardness of 7 on the Mohs scale; white to clear or translucent color; vitreous (glassy) luster; trigonal crystal system; conchoidal fracture with no true cleavage; specific gravity of 2.65.

Formation & geological history

Forms in a wide variety of geological environments including igneous, metamorphic, and sedimentary rocks. Often crystallizes from silica-rich hydrothermal veins and pegmatites.

Uses & applications

Used in glassmaking, electronics, oscillators, abrasives, gemstones, and ornamental objects.

Geological facts

Quartz is one of the most abundant minerals in Earth's continental crust and exhibits piezoelectric properties, meaning it can generate an electrical charge when mechanical stress is applied.

Field identification & locations

Easily identified by its hardness (scratches glass), lack of cleavage, and conchoidal fracture. Found worldwide in nearly every geological setting.