Rock Identifier
Quartz Geode (Silicon Dioxide (SiO2)) — sedimentary
sedimentary

Quartz Geode

Silicon Dioxide (SiO2)

AI-generated identification · may be incorrect

Hardness of 7 on the Mohs scale, vitreous luster, conchoidal fracture, and hexagonal crystal system. Color ranges from clear to white with brownish iron oxide staining.

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Physical properties

Hardness of 7 on the Mohs scale, vitreous luster, conchoidal fracture, and hexagonal crystal system. Color ranges from clear to white with brownish iron oxide staining.

Formation & geological history

Formed when mineral-rich groundwater deposits silica inside gas cavities or nodules within sedimentary or volcanic rocks over millions of years.

Uses & applications

Used widely in decorative displays, crystal specimen collecting, and lapidary arts.

Geological facts

Geodes start as hollow nodules where crystals grow inward toward the center, creating a hollow cavity lined with sparkling quartz points.

Field identification & locations

Easily identified by its rounded exterior and sparkling crystalline interior cavity; commonly found in limestone formations and desert regions worldwide.