Rock Identifier
Quartz Vein in Rhyolite (Silicified extrusive igneous rock with hydrothermal quartz veinlets) — igneous
igneous

Quartz Vein in Rhyolite

Silicified extrusive igneous rock with hydrothermal quartz veinlets

AI-generated identification · may be incorrect

Hardness 7 on Mohs scale for quartz; tan-brown groundmass with white crystalline veins; vitreous luster; cryptocrystalline to microcrystalline structure.

Identified More igneous →
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Physical properties

Hardness 7 on Mohs scale for quartz; tan-brown groundmass with white crystalline veins; vitreous luster; cryptocrystalline to microcrystalline structure.

Formation & geological history

Formed when silica-rich hydrothermal fluids filled fractures in cooling volcanic rock, solidifying over millions of years.

Uses & applications

Commonly collected as a lapidary specimen or used in landscape decoration and crushed stone aggregates.

Geological facts

These contrasting vein patterns form when tectonic forces crack cooling lavas, allowing mineral-rich groundwater to precipitate quartz.

Field identification & locations

Easily identified by hard white quartz veins cutting sharply through a fine-grained, brownish volcanic host rock.