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

White Quartz

Silicon Dioxide (SiO2)

Hardness: 7 on Mohs scale. Color: White to milky white. Luster: Vitreous to greasy. Crystal structure: Trigonal. Cleavage: None, exhibits conchoidal fracture. Specific gravity: 2.65.

Hardness
7 on Mohs scale
Color
White to milky white
Luster
Vitreous to greasy
Identified More mineral
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Physical properties

Hardness: 7 on Mohs scale. Color: White to milky white. Luster: Vitreous to greasy. Crystal structure: Trigonal. Cleavage: None, exhibits conchoidal fracture. Specific gravity: 2.65.

Formation & geological history

Forms in a wide variety of geological environments, most commonly in igneous, metamorphic, and sedimentary rocks. It is a major constituent of pegmatites and hydrothermal veins.

Uses & applications

Used in glassmaking, electronics, oscillators, abrasives, and as a semi-precious gemstone or crystal specimen in jewelry and decor.

Geological facts

Milky quartz gets its white color from microscopic fluid inclusions of gas or liquid trapped during crystal growth. It is one of the most abundant minerals on Earth's continental crust.

Field identification & locations

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