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

White Quartz

Silicon Dioxide (SiO2)

Hardness of 7 on the Mohs scale, white to milky color, vitreous to greasy 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 milky color, vitreous to greasy 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, most commonly in hydrothermal veins, pegmatites, and as a primary component of igneous, metamorphic, and sedimentary rocks.

Uses & applications

Used in electronics, manufacturing of glass and ceramics, gemstone carvings, and as a specimen for mineral collectors.

Geological facts

Quartz is the second most abundant mineral in Earth's continental crust, surpassed only by feldspar. Milky quartz owes its color to microscopic fluid inclusions trapped during crystal growth.

Field identification & locations

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