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

Quartz

Silicon Dioxide (SiO2)

Hardness: 7 (Mohs scale), Color: White/Colorless (Milky Quartz), Luster: Vitreous, Crystal Structure: Trigonal/Hexagonal, Cleavage: None (Conchoidal fracture), Specific Gravity: 2.65

Identified More mineral

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Physical properties

Hardness: 7 (Mohs scale), Color: White/Colorless (Milky Quartz), Luster: Vitreous, Crystal Structure: Trigonal/Hexagonal, Cleavage: None (Conchoidal fracture), Specific Gravity: 2.65

Formation & geological history

Formed from cooling magma or hydrothermal veins. It is one of the most abundant minerals in the Earth's crust and can be found in various environments ranging from igneous to metamorphic and sedimentary rocks.

Uses & applications

Extensively used in electronics (oscillators), glassmaking, abrasives, jewelry (gemstones), and as a structural component in construction (sand and gravel).

Geological facts

Quartz is piezoelectric, meaning it generates an electric charge in response to applied mechanical stress. This property led to its use in the first reliable clocks and watches.

Field identification & locations

Identify by its inability to be scratched by a steel knife (hardness 7) and its lack of cleavage. Found worldwide in nearly every geological setting.