
sedimentary
Quartz Geode
Crystalline Silicon Dioxide (SiO2) within a nodule
AI-generated identification · may be incorrectHardness: 7 (Mohs scale); Color: Off-white/tan exterior, typically clear or white crystals inside; Luster: Dull/earthy exterior, vitreous (glassy) interior; Crystal Structure: Hexagonal; Cleavage: None; Specific Gravity: 2.65
- Hardness
- 7 (Mohs scale)
- Luster
- Dull/earthy exterior, vitreous (glassy) interior
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Physical properties
Hardness: 7 (Mohs scale); Color: Off-white/tan exterior, typically clear or white crystals inside; Luster: Dull/earthy exterior, vitreous (glassy) interior; Crystal Structure: Hexagonal; Cleavage: None; Specific Gravity: 2.65
Formation & geological history
Formed in cavities within sedimentary rocks (like limestone) or volcanic rocks. Mineral-rich groundwater seeps into hollow spaces, depositing layers of minerals over millions of years. Common in Mississippian-age strata.
Uses & applications
Primarily used for geological education, home decor, lapidary art, and mineral collecting. Large, high-quality geodes are popular display pieces.
Geological facts
Geodes are often nicknamed 'thunder eggs' in some regions. They are distinguished from nodules because they contain a hollow cavity or crystal linings. The word 'geode' comes from the Greek word 'Geoides' meaning earth-like.
Field identification & locations
Identify by the rounded, cauliflower-like exterior texture and lighter-than-expected weight if hollow. Commonly found in desert regions, stream beds, or limestone outcrops. Use a rock hammer to carefully crack or a saw to cut open.
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