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

Milky Quartz

Silicon Dioxide (SiO2)

Hardness: 7 Mohs; Color: Cloudy white to opaque; Luster: Vitreous to greasy; Crystal Structure: Trigonal; Cleavage: None/Conchoidal fracture; Specific Gravity: 2.65

Hardness
7 Mohs
Color
Cloudy white to opaque
Luster
Vitreous to greasy
Identified More mineral

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Physical properties

Hardness: 7 Mohs; Color: Cloudy white to opaque; Luster: Vitreous to greasy; Crystal Structure: Trigonal; Cleavage: None/Conchoidal fracture; Specific Gravity: 2.65

Formation & geological history

Formed from hydrothermal solutions or the cooling of silica-rich magma; commonly found in veins or as a major constituent of igneous rocks like granite.

Uses & applications

Used in glassmaking, electronics, silicon chips, and as an ornamental gemstone or healing crystal in the metaphysical community.

Geological facts

The milky appearance is caused by tiny inclusions of gas or liquid trapped during the crystal's growth. It is one of the most common minerals found on Earth's crust.

Field identification & locations

Identify in the field by its hardness (scratches glass), lack of cleavage, and white waxy appearance. Commonly found in gravel beds, mountain ranges, and near volcanic sites.