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

Quartz

Silicon Dioxide (SiO2)

Hardness of 7 on the Mohs scale, vitreous luster, conchoidal fracture, lacks distinct cleavage, hexagonal crystal system, specific gravity of 2.65, often translucent to transparent, varying in color from clear to milky white.

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Physical properties

Hardness of 7 on the Mohs scale, vitreous luster, conchoidal fracture, lacks distinct cleavage, hexagonal crystal system, specific gravity of 2.65, often translucent to transparent, varying in color from clear to milky white.

Formation & geological history

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

Uses & applications

Used extensively in electronics, glassmaking, precision instruments, abrasive materials, and as a gemstone or ornamental mineral.

Geological facts

Quartz is one of the most abundant and widely distributed minerals found on Earth's continental crust. Its piezoelectric properties make it essential for keeping time in quartz watches.

Field identification & locations

Easily identifiable in the field by its high hardness (scratches glass), conchoidal fracture, and lack of cleavage. Found globally in almost all geological settings.