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, white to clear color, vitreous luster, hexagonal crystal system, conchoidal fracture.

Identified More mineral →
Explore Quartz Vein in Host Rock in the encyclopedia →

Identify your own rocks.

Get a report just like this from any photo, free.

Physical properties

Hardness of 7 on the Mohs scale, white to clear color, vitreous luster, hexagonal crystal system, conchoidal fracture.

Formation & geological history

Formed by hydrothermal fluids precipitating silica into fractures within surrounding host rock under high pressure and temperature.

Uses & applications

Used in electronics, glassware, gemstone carving, and mineral specimen collecting.

Geological facts

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

Field identification & locations

Identify by its high hardness (scratches glass) and lack of cleavage; commonly found in hydrothermal veins worldwide.