Rock Identifier
Quartz Vein in Granite (Silicon Dioxide (SiO2) within intrusive igneous host) — igneous
igneous

Quartz Vein in Granite

Silicon Dioxide (SiO2) within intrusive igneous host

AI-generated identification · may be incorrect

Mohs hardness of 7, white to translucent color, vitreous luster, hexagonal crystal system, and lack of cleavage.

Identified More igneous →
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Physical properties

Mohs hardness of 7, white to translucent color, vitreous luster, hexagonal crystal system, and lack of cleavage.

Formation & geological history

Formed through hydrothermal fluid precipitation filling fractures in cooling plutonic rocks during ancient geological periods.

Uses & applications

Used in aggregate, dimension stone, silica extraction for electronics, and as a popular specimen for mineral collectors.

Geological facts

Quartz veins are the primary geological structures responsible for hosting high-grade lode gold deposits worldwide.

Field identification & locations

Easily identified in the field by high relief, white color, and inability to scratch with a steel blade; found globally in mountainous and shield regions.