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

Quartz Vein in Host Rock

Silicon Dioxide (SiO2)

AI-generated identification · may be incorrect

Hardness of 7 on the Mohs scale, vitreous luster, white to clear color, and conchoidal fracture without distinct cleavage.

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Physical properties

Hardness of 7 on the Mohs scale, vitreous luster, white to clear color, and conchoidal fracture without distinct cleavage.

Formation & geological history

Formed through hydrothermal precipitation, where silica-rich fluids crystallized within fractures of surrounding host rock.

Uses & applications

Used in electronics, glassmaking, industrial abrasives, and as a popular specimen for mineral collectors.

Geological facts

Quartz is one of the most abundant minerals in the Earth's continental crust and exhibits strong piezoelectric properties.

Field identification & locations

Identify by its high hardness, inability to be scratched by steel, and crystalline habit filling fractures.