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

Milky Quartz

Silicon Dioxide (SiO2)

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

Hardness
7 on the Mohs scale
Color
White, milky, translucent to opaque
Luster
Vitreous to greasy
Identified More mineral
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Physical properties

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

Formation & geological history

Forms in hydrothermal veins, pegmatites, and metamorphic environments as silica-rich fluids cool and crystallize under varying temperatures and pressures.

Uses & applications

Used in landscaping, decorative stone, glass manufacturing, and as a popular specimen for mineral collectors.

Geological facts

Milky quartz is the most common variety of crystalline quartz found on Earth. Its milky appearance is caused by microscopic fluid or gas inclusions trapped during crystal growth.

Field identification & locations

Easily identified by its hardness (scratches glass), white milky color, and lack of cleavage. Found worldwide in almost all geological environments.