Rock Identifier
Milky quartz (Quartz (SiO₂)) — mineral
mineral

Milky quartz

Quartz (SiO₂)

AI-generated identification · may be incorrect

Likely a rough, translucent white quartz mass with a vitreous-to-greasy luster and irregular fracture. Mohs hardness 7; trigonal crystal structure, no cleavage; specific gravity about 2.65.

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Physical properties

Likely a rough, translucent white quartz mass with a vitreous-to-greasy luster and irregular fracture. Mohs hardness 7; trigonal crystal structure, no cleavage; specific gravity about 2.65.

Formation & geological history

Forms when silica-rich fluids crystallize in veins and cavities, or during cooling of silica-rich igneous rocks. Quartz occurs in rocks of many geological ages.

Uses & applications

Commonly used for ornaments, carvings, and decorative stone; quartz is also an important industrial source of silica, though this specimen appears to be a small rough piece.

Geological facts

Milky appearance comes from microscopic fluid or gas inclusions that scatter light.

Field identification & locations

Identify by its glassy sheen, hardness (it can scratch glass), and lack of cleavage. Common worldwide in quartz veins and pegmatites; the photo alone cannot establish the exact identification.