Rock Identifier
Milky quartz (Quartz (silicon dioxide, SiO₂)) — mineral
mineral

Milky quartz

Quartz (silicon dioxide, SiO₂)

AI-generated identification · may be incorrect

White to translucent, with a vitreous-to-dull luster and irregular fracture; Mohs hardness 7, trigonal crystal structure, no cleavage, and specific gravity about 2.65. The image shows a small, rough, pale specimen; exact identification is uncertain from appearance alone.

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Physical properties

White to translucent, with a vitreous-to-dull luster and irregular fracture; Mohs hardness 7, trigonal crystal structure, no cleavage, and specific gravity about 2.65. The image shows a small, rough, pale specimen; exact identification is uncertain from appearance alone.

Formation & geological history

Forms when silica-rich fluids crystallize in veins and cavities, or as a common component of igneous and metamorphic rocks. Quartz occurs in rocks of many geological ages.

Uses & applications

Used in glassmaking, electronics, abrasives, and construction; attractive pieces are collected or used decoratively.

Geological facts

Quartz is one of Earth’s most abundant minerals and is piezoelectric, producing an electrical charge under pressure.

Field identification & locations

Look for hardness—quartz can scratch glass—and its lack of cleavage; common worldwide, especially in quartz veins and granitic terrains.