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

Quartz Vein in Host Rock

Silicon Dioxide (SiO2) in matrix

AI-generated identification · may be incorrect

Hardness of 7 on the Mohs scale with a vitreous luster. Features prominent white quartz veins intersecting darker host rock with no visible cleavage.

Identified More metamorphic →
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 with a vitreous luster. Features prominent white quartz veins intersecting darker host rock with no visible cleavage.

Formation & geological history

Formed when mineral-rich hydrothermal fluids precipitate silica into fractures within existing rock under high pressure and temperature.

Uses & applications

Used primarily as decorative landscape stones, in lapidary work, and as geological educational specimens.

Geological facts

Quartz veins are the primary geological structures that host major gold and sulfide mineral deposits worldwide.

Field identification & locations

Identify by the stark color contrast between translucent white quartz and the darker host rock, combined with extreme scratch resistance.