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

Milky quartz

Quartz (silicon dioxide, SiO₂)

AI-generated identification · may be incorrect

White to cream, opaque and massive with a glassy-to-dull luster; Mohs hardness 7, trigonal crystal structure, no cleavage, and conchoidal fracture. The specimen’s rough, granular appearance is consistent with quartz, though a photo cannot confirm it definitively.

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Physical properties

White to cream, opaque and massive with a glassy-to-dull luster; Mohs hardness 7, trigonal crystal structure, no cleavage, and conchoidal fracture. The specimen’s rough, granular appearance is consistent with quartz, though a photo cannot confirm it definitively.

Formation & geological history

Forms when silica-rich fluids crystallize in veins and fractures, or as quartz-rich material in igneous and metamorphic rocks. Quartz occurs in rocks of many geological ages.

Uses & applications

Used as a silica source in glassmaking, ceramics, and some industrial applications; attractive pieces may be polished or collected.

Geological facts

Quartz is among Earth’s most abundant minerals and can persist through extensive weathering because of its hardness and chemical durability.

Field identification & locations

Look for hardness sufficient to scratch glass, no cleavage, and irregular fracture; common in quartz veins and many rock types worldwide.