Rock Identifier
Quartz Vein in Green Schist (Silicon Dioxide (Quartz) and metamorphic silicate minerals) — metamorphic
metamorphic

Quartz Vein in Green Schist

Silicon Dioxide (Quartz) and metamorphic silicate minerals

AI-generated identification · may be incorrect

Hardness of 7 for the quartz top, variable lower hardness for the green schist; vitreous luster on the quartz portion with a green, foliated matrix below; uneven fracture.

Identified More metamorphic →
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Physical properties

Hardness of 7 for the quartz top, variable lower hardness for the green schist; vitreous luster on the quartz portion with a green, foliated matrix below; uneven fracture.

Formation & geological history

Formed via hydrothermal fluid deposition filling fractures in pre-existing rock, later subjected to regional metamorphism.

Uses & applications

Used primarily as a geological specimen, lapidary study, and educational tool.

Geological facts

Quartz veins often host valuable ore minerals like gold, though this specimen shows a barren vein cutting a greenstone or schist host.

Field identification & locations

Easily identified by the stark contrast between the translucent white quartz cap and the greenish micaceous or chloritic host rock beneath.