
sedimentary
Geode with Quartz Crystal Cavity
Silicon Dioxide (SiO2) in Calcareous/Siliceous Matrix
AI-generated identification · may be incorrectHardness: 7 (crystals) / 3-5 (matrix). Color: Tan/brown exterior with white/clear crystals. Luster: Vitreous (crystals) to dull (exterior). Crystal structure: Trigonal (hexagonal prisms). Cleavage: None/Conchoidal.
- Hardness
- 7 (crystals) / 3-5 (matrix)
- Color
- Tan/brown exterior with white/clear crystals
- Luster
- Vitreous (crystals) to dull (exterior)
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Physical properties
Hardness: 7 (crystals) / 3-5 (matrix). Color: Tan/brown exterior with white/clear crystals. Luster: Vitreous (crystals) to dull (exterior). Crystal structure: Trigonal (hexagonal prisms). Cleavage: None/Conchoidal.
Formation & geological history
Formed as hollow cavities in sedimentary rock layers, often by bubbles or dissolved organic material. Minerals precipitate from groundwater over millions of years (often Jurassic to Eocene ages) to line the cavity.
Uses & applications
Primarily used for geological education, tabletop decor, and as a popular item for amateur rock collectors and metaphysical stores.
Geological facts
Geodes appear to be ordinary rocks from the outside, but their hollow interiors can contain massive crystal formations. The name comes from the Greek word 'Geoides' meaning earth-like.
Field identification & locations
Identify by looking for rounded, lumpy, or 'cauliflower-like' textures on the exterior. Often lighter in weight than solid rocks of the same size. Commonly found in desert environments like Utah, Iowa, and Mexico.
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