Rock Identifier
Quartz Geode Fragment (Silicon dioxide (SiO2)) — sedimentary
sedimentary

Quartz Geode Fragment

Silicon dioxide (SiO2)

AI-generated identification · may be incorrect

Hardness of 7 on the Mohs scale, vitreous luster, conchoidal fracture, and hexagonal crystal system. Displays a yellowish-amber color due to iron oxide inclusions.

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Physical properties

Hardness of 7 on the Mohs scale, vitreous luster, conchoidal fracture, and hexagonal crystal system. Displays a yellowish-amber color due to iron oxide inclusions.

Formation & geological history

Formed through the deposition of silica-rich groundwater inside cavities of sedimentary or volcanic rocks over millions of years.

Uses & applications

Used primarily in lapidary arts, wire-wrapped jewelry, mineral collecting, and decorative display specimens.

Geological facts

Geodes form when mineral-rich water enters a hollow cavity in a host rock, slowly precipitating crystals inward over geological epochs.

Field identification & locations

Easily identified by its outer weathered limestone rind and sparkling internal quartz crystals. Found worldwide in limestone formations.