
mineral
Quartz Geode
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: typically white, clear, or cloudy internally with a tan or gray outer rind; Luster: vitreous (glassy) inside, dull outside; Crystal structure: Trigonal/Hexagonal; Cleavage: none.
- Hardness
- 7 on Mohs scale
- Luster
- vitreous (glassy) inside, dull outside
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Physical properties
Hardness: 7 on Mohs scale; Color: typically white, clear, or cloudy internally with a tan or gray outer rind; Luster: vitreous (glassy) inside, dull outside; Crystal structure: Trigonal/Hexagonal; Cleavage: none.
Formation & geological history
Formed when mineral-rich groundwater seeps into hollow cavities in volcanic or sedimentary rocks. Over thousands to millions of years, silica precipitates out of the water to form crystals pointing inward.
Uses & applications
Highly popular for mineral collecting, education, decorative displays, jewelry, and as 'metaphysical' stones. Crushed quartz is used in commercial glassmaking and electronics.
Geological facts
The word 'geode' comes from the Greek word 'Geoides' meaning 'earth-like.' While they look like ordinary rocks on the exterior, they contain hidden crystal cathedrals inside.
Field identification & locations
Identify by looking for round or egg-shaped nodules that feel significantly lighter than solid rocks of the same size. Commonly found in desert regions of the US (Utah, Arizona), Mexico, and Brazil.
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Other mineral specimens
Gneiss or Schist
Gneiss or Mica Schist with Garnet
Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Tumbled granite
Granite, a coarse-grained felsic intrusive igneous rock
igneous
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
igneous
Granite
Granite (Phaneritic intrusive igneous rock)
igneous