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, with a vitreous-to-dull luster and irregular fracture; hardness 7 on the Mohs scale, trigonal crystal structure, and no cleavage. The specimen’s rough, blocky shape and surface wear make visual identification probable but not definitive.

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Physical properties

White to cream, opaque, with a vitreous-to-dull luster and irregular fracture; hardness 7 on the Mohs scale, trigonal crystal structure, and no cleavage. The specimen’s rough, blocky shape and surface wear make visual identification probable but not definitive.

Formation & geological history

Forms when silica-rich fluids crystallize in veins and cavities, or during igneous and metamorphic processes. Quartz occurs in rocks of many ages, from ancient crust to modern veins.

Uses & applications

Commonly used as a decorative and collectible mineral; quartz is also used in glass, electronics, and engineered stone.

Geological facts

Quartz is among Earth’s most abundant minerals; its hardness lets it scratch ordinary glass.

Field identification & locations

Look for glassy luster, lack of cleavage, and hardness near 7; common in veins and many rock types worldwide. The image alone cannot confirm the identification.