Rock Identifier
Geode (Chert or Quartz Nodule) (Silicon Dioxide (SiO2)) — sedimentary
sedimentary

Geode (Chert or Quartz Nodule)

Silicon Dioxide (SiO2)

Hardness: 7 (Mohs scale); Color: Tan, beige, or white exterior; Luster: Dull/earthy exterior, vitreous (glassy) interior; Crystal structure: Hexagonal/Trigonal (cryptocrystalline); Cleavage: None (conchoidal fracture).

Hardness
7 (Mohs scale)
Color
Tan, beige, or white exterior
Luster
Dull/earthy exterior, vitreous (glassy) interior
Identified More sedimentary

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Physical properties

Hardness: 7 (Mohs scale); Color: Tan, beige, or white exterior; Luster: Dull/earthy exterior, vitreous (glassy) interior; Crystal structure: Hexagonal/Trigonal (cryptocrystalline); Cleavage: None (conchoidal fracture).

Formation & geological history

Formed as secondary fillings in cavities within sedimentary rocks like limestone or dolomite. Silica-rich groundwater percolates through the rock, depositing layers of minerals over millions of years.

Uses & applications

Commonly used for lapidary work, home decor, educational specimens, and crystal healing collections.

Geological facts

Geodes are often nicknamed 'thunder eggs' when they are solid or filled with agate. They are essentially time capsules that contain minerals crystallized thousands to millions of years ago.

Field identification & locations

Identify by its rounded, cauliflower-like exterior texture and surprising lightness (indicating a hollow center). Commonly found in the Midwest USA (Keokuk region) and desert environments.