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 System: Trigonal; Cleavage: None (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 System: Trigonal; Cleavage: None (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 crystallizes from silica-rich hydrothermal solutions or cooling magma.

Uses & applications

Used in electronics, manufacturing of glass, gemstones, ornamental items, and spiritual or metaphysical practices.

Geological facts

Quartz is one of the most abundant minerals in Earth's continental crust. Milky quartz gets its white color from microscopic fluid inclusions trapped during crystal growth.

Field identification & locations

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