Rock Identifier
Milky Quartz (Silicon Dioxide (SiO2)) — mineral
mineral

Milky Quartz

Silicon Dioxide (SiO2)

White to cloudy translucent color, vitreous luster, Mohs hardness of 7, trigonal crystal system, conchoidal fracture (no cleavage), specific gravity of 2.65.

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Physical properties

White to cloudy translucent color, vitreous luster, Mohs hardness of 7, trigonal crystal system, conchoidal fracture (no cleavage), specific gravity of 2.65.

Formation & geological history

Formed from hydrothermal solutions or igneous cooling primarily in veins and pegmatites. It is one of the most common minerals in the Earth's crust across all geological eras.

Uses & applications

Used in glassmaking, abrasives, jewelry (tumbled stones), and as a structural gemstone. Also important in the production of silicon for electronics.

Geological facts

The milky appearance is caused by microscopic inclusions of gas or liquid trapped during the crystal's formation. It is often found in large, vein-filling masses.

Field identification & locations

Identify by its hardness (will scratch glass but not be scratched by a steel file), white color, and waxy to vitreous luster. Found globally, especially in mountain ranges and stream beds.