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

Quartz (Milky Quartz)

Silicon Dioxide (SiO2)

Hardness of 7 on the Mohs scale, milky white to pale cream color, vitreous to greasy luster, trigonal crystal system, conchoidal fracture, specific gravity of 2.65.

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Physical properties

Hardness of 7 on the Mohs scale, milky white to pale cream color, vitreous to greasy luster, trigonal crystal system, conchoidal fracture, specific gravity of 2.65.

Formation & geological history

Forms in igneous pegmatites, hydrothermal veins, and metamorphic rocks. The milky appearance is caused by tiny fluid inclusions trapped during crystal growth.

Uses & applications

Used in glassmaking, ceramics, electronics (piezoelectric applications), abrasives, and as decorative gravel or mineral specimens.

Geological facts

Quartz is the second most abundant mineral in Earth's continental crust. Pure quartz is clear, but microscopic fluid gas/liquid bubbles turn it milky white.

Field identification & locations

Identified by its ability to easily scratch glass and steel, lack of cleavage, milky translucency, and hexagonal/crystalline texture. Found abundantly worldwide.