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

Milky quartz

Quartz (silicon dioxide, SiO₂)

AI-generated identification · may be incorrect

Mohs hardness 7; white to translucent with a vitreous-to-waxy luster and irregular conchoidal fracture. Trigonal crystal structure; no cleavage. The pictured rough fragment appears quartz-like, though identification from the image alone is uncertain.

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Physical properties

Mohs hardness 7; white to translucent with a vitreous-to-waxy luster and irregular conchoidal fracture. Trigonal crystal structure; no cleavage. The pictured rough fragment appears quartz-like, though identification from the image alone is uncertain.

Formation & geological history

Forms when silica-rich fluids crystallize in veins and cavities, or as grains in many rock types. Quartz occurs in rocks of many ages, from ancient crust to recent deposits.

Uses & applications

Used in glassmaking, electronics, abrasives, and as a common decorative and collecting mineral.

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 glassy translucence, hardness sufficient to scratch glass, and lack of cleavage. Common worldwide in veins, pegmatites, and stream gravels; this small, unverified fragment has little diagnostic context.