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

Quartz (Raw Specimen)

Silicon Dioxide (SiO2)

Hardness of 7 on the Mohs scale; Color ranges from white to off-white, yellowish, or colorless; Vitreous to dull luster; Trigonal crystal system; Conchoidal fracture; Specific gravity of 2.65.

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Physical properties

Hardness of 7 on the Mohs scale; Color ranges from white to off-white, yellowish, or colorless; Vitreous to dull luster; Trigonal crystal system; Conchoidal fracture; Specific gravity of 2.65.

Formation & geological history

Forms in a wide variety of geological environments, commonly in hydrothermal veins, pegmatites, and as a primary constituent of igneous, metamorphic, and sedimentary rocks.

Uses & applications

Used in electronics, glassware, precision instruments, gemstones, and decorative items.

Geological facts

Quartz is one of the most abundant minerals found in the Earth's continental crust and exhibits piezoelectric properties, meaning it can generate an electrical charge under mechanical stress.

Field identification & locations

Easily identifiable by its high hardness (scratches glass) and conchoidal fracture. Found worldwide in nearly every type of geological terrain.