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

Quartz Geode

Silicon Dioxide (SiO2) in Host Rock

Hardness: 7 (Mohs scale), Color: White to colorless crystals with tan/pink host rock, Luster: Vitreous (glassy) to dull, Crystal Structure: Hexagonal, Cleavage: None (conchoidal fracture), Specific Gravity: 2.65

Identified More sedimentary

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Physical properties

Hardness: 7 (Mohs scale), Color: White to colorless crystals with tan/pink host rock, Luster: Vitreous (glassy) to dull, Crystal Structure: Hexagonal, Cleavage: None (conchoidal fracture), Specific Gravity: 2.65

Formation & geological history

Formed in sedimentary or volcanic rock cavities. Mineral-rich water seeps into hollow pockets, precipitating crystals over millions of years. This host material appears to be a rhyolitic or sedimentary matrix.

Uses & applications

Commonly used for geological education, home decor, lapidary projects, and as a popular item for novice collectors.

Geological facts

Geodes are often referred to as 'thunder eggs' when they are solid or have specific patterns. The word 'geode' comes from the Greek word 'geodes' meaning earth-like.

Field identification & locations

Identify in the field by looking for rounded, lumpy nodules that feel lighter than solid rocks of similar size. Common in areas like the American Southwest, Mexico, and Brazil.