
mineral
Quartz Geode
Crystalline Silicon Dioxide (SiO2) in Geode
Hardness: 7 on Mohs scale; Color: Clear to white crystals within a gray/tan host rock; Luster: Vitreous (glassy) crystals with a dull/earthy exterior; Crystal Structure: Hexagonal; Cleavage: None (conchoidal fracture).
- Hardness
- 7 on Mohs scale
- Color
- Clear to white crystals within a gray/tan host rock
- Luster
- Vitreous (glassy) crystals with a dull/earthy exterior
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Physical properties
Hardness: 7 on Mohs scale; Color: Clear to white crystals within a gray/tan host rock; Luster: Vitreous (glassy) crystals with a dull/earthy exterior; Crystal Structure: Hexagonal; Cleavage: None (conchoidal fracture).
Formation & geological history
Formed via the precipitation of mineral-rich groundwater within hollow cavities in volcanic ash or sedimentary limestone over millions of years.
Uses & applications
Primarily used for decorative purposes, crystal healing, educational displays, and as a popular entry-level mineral for collectors.
Geological facts
Geodes are often called 'thunder eggs' when they are solid or have specific shapes. The word 'geode' comes from the Greek word 'geoides' meaning 'earth-like'.
Field identification & locations
Identify in the field by looking for rounded, bumpy, potato-like nodules that feel lighter than they look (indicating a hollow center). Common in desert regions of the SW United States, Brazil, and Morocco.
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