Quartz
Silicon Dioxide (SiO2)
Rock Type: mineral

Physical Properties
Hardness: 7 on Mohs scale; Color: Colorless to white; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: Indistinct (conchoidal fracture); Specific Gravity: 2.65.
Formation & Geological History
Formed through the cooling of silica-rich magma or from hydrothermal veins. It is one of the most abundant minerals in Earth's crust and can be found in rocks of all geological ages.
Uses & Applications
Used in electronics (oscillators), glass manufacturing, abrasives, jewelry (as semi-precious gemstones), and construction as a component of sand.
Geological Facts
Quartz is piezoelectric, meaning it generates an electric charge when mechanical stress is applied. This property makes it essential for timekeeping in watches and clocks.
Field Identification & Locations
Identify in the field by its hardness (scratches glass), glassy luster, and lack of cleavage planes. Found globally in granites, metamorphic rocks, and sedimentary sands.
Identified on: 4/16/2026
Mode: Standard