
sedimentary
Geode (Unopened)
Siliceous Geode (SiO2)
Hardness: 7 (Mohs scale for outer shell); Color: Tan, beige, or brownish outer rind; Luster: Dull/earthy exterior; Crystal structure: Trigonal (often containing internal quartz/chalcedony); Cleavage: None (conchoidal fracture when broken).
- Hardness
- 7 (Mohs scale for outer shell)
- Color
- Tan, beige, or brownish outer rind
- Luster
- Dull/earthy exterior
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Physical properties
Hardness: 7 (Mohs scale for outer shell); Color: Tan, beige, or brownish outer rind; Luster: Dull/earthy exterior; Crystal structure: Trigonal (often containing internal quartz/chalcedony); Cleavage: None (conchoidal fracture when broken).
Formation & geological history
Formed in voids created by bubbles in volcanic rock or hollows in sedimentary rock (limestone). Over time, mineral-rich groundwater seeps in, depositing microcrystalline quartz (chalcedony) and macrocrystalline quartz layers.
Uses & applications
Primary use as collector specimens, lapidary education, decorative display, and jewelry (once cut and polished to reveal the crystal core).
Geological facts
Geodes are often referred to as 'thunder eggs' in certain regions. The word geode comes from the Greek word 'Geoides' meaning 'earth-like'. They are Missouri's and Iowa's official state rocks.
Field identification & locations
Identify by their rounded, lumpy, or cauliflower-like exterior and unusually light weight for their size (suggesting a hollow center). Common locations include the Keokuk region of Iowa, Illinois, and Missouri.
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