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

Milky quartz crystal

Quartz, silicon dioxide (SiO₂)

AI-generated identification · may be incorrect

Hardness 7 Mohs; white to translucent, vitreous-to-waxy luster, hexagonal crystal structure, and no cleavage with conchoidal fracture. The specimen shows blocky/prismatic crystal faces and cloudy inclusions.

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Physical properties

Hardness 7 Mohs; white to translucent, vitreous-to-waxy luster, hexagonal crystal structure, and no cleavage with conchoidal fracture. The specimen shows blocky/prismatic crystal faces and cloudy inclusions.

Formation & geological history

Forms when silica-rich hydrothermal fluids or pegmatitic melts crystallize in cavities and veins. Quartz is widespread from Precambrian to modern geological settings.

Uses & applications

Used in glass, ceramics, electronics, abrasives, and ornamental objects; attractive crystals are collected but this cloudy specimen has modest gem value.

Geological facts

Its milky appearance results from microscopic fluid inclusions, fractures, or mineral impurities scattering light. Quartz is one of Earth’s most abundant and chemically resistant minerals.

Field identification & locations

Identify by its glassy luster, lack of cleavage, conchoidal fracture, and ability to scratch ordinary glass; it is commonly found in veins, geodes, pegmatites, and placer gravels worldwide.