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

Milky Quartz

Silicon Dioxide (SiO2)

Hardness of 7 on the Mohs scale, milky white or cloudy color due to microscopic fluid inclusions, vitreous to greasy luster, trigonal crystal system, conchoidal fracture, and no true cleavage. Specific gravity is approximately 2.65.

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Physical properties

Hardness of 7 on the Mohs scale, milky white or cloudy color due to microscopic fluid inclusions, vitreous to greasy luster, trigonal crystal system, conchoidal fracture, and no true cleavage. Specific gravity is approximately 2.65.

Formation & geological history

Forms in igneous, metamorphic, and sedimentary environments. It commonly precipitates from hydrothermal solutions at various temperatures and pressures over millions of years.

Uses & applications

Used in glassmaking, abrasives, electronics (though typically clear quartz is preferred for piezoelectric uses), decorative items, and lapidary work.

Geological facts

Milky quartz is the most common variety of the quartz family found on Earth. Its cloudy appearance is caused by tiny liquid or gas-filled inclusions trapped inside the crystals during their growth.

Field identification & locations

Easily identified in the field by its high hardness (scratches glass), white milky color, and conchoidal fracture. Found worldwide in almost all geological settings, particularly in pegmatites and hydrothermal veins.