Rock Identifier
Quartz Crystal Cluster / Quartzite (Silicon Dioxide (SiO2)) — mineral
mineral

Quartz Crystal Cluster / Quartzite

Silicon Dioxide (SiO2)

Hardness of 7 on the Mohs scale, transparent to translucent with a vitreous (glassy) luster, trigonal crystal system, conchoidal fracture with no true cleavage, and a specific gravity of 2.65.

Identified More mineral
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Physical properties

Hardness of 7 on the Mohs scale, transparent to translucent with a vitreous (glassy) luster, trigonal crystal system, conchoidal fracture with no true cleavage, and a specific gravity of 2.65.

Formation & geological history

Formed in hydrothermal veins, pegmatites, and as a primary component of many igneous, metamorphic, and sedimentary rocks over millions of years.

Uses & applications

Used in electronics, watchmaking, glass manufacturing, abrasives, gemstone carving, and mineral collections.

Geological facts

Quartz is one of the most abundant and widely distributed minerals on Earth's continental crust, known for its piezoelectric properties.

Field identification & locations

Identified by its high hardness (scratches glass), lack of cleavage, and characteristic glassy luster. Commonly found worldwide in almost all geological environments.