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

Quartz in Host Rock

Silicon Dioxide (SiO2)

Hardness of 7 on the Mohs scale, vitreous luster, colorless to translucent, conchoidal fracture, hexagonal crystal system.

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Physical properties

Hardness of 7 on the Mohs scale, vitreous luster, colorless to translucent, conchoidal fracture, hexagonal crystal system.

Formation & geological history

Formed in hydrothermal veins and pegmatites through the cooling of silica-rich solutions over millions of years.

Uses & applications

Used in electronics, watchmaking, glass manufacturing, and as a popular mineral specimen for collectors.

Geological facts

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

Field identification & locations

Easily identified by its high hardness (scratches glass) and hexagonal crystal habit. Found worldwide in nearly all geological environments.