
mineral
Quartz Geode
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale; Color: Clear to white crystals within a tan brownish exterior; Luster: Vitreous (glassy) inside, earthy outside; Crystal Structure: Hexagonal/Trigonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Clear to white crystals within a tan brownish exterior
- Luster
- Vitreous (glassy) inside, earthy outside
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Physical properties
Hardness: 7 on Mohs scale; Color: Clear to white crystals within a tan brownish exterior; Luster: Vitreous (glassy) inside, earthy outside; Crystal Structure: Hexagonal/Trigonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed in hollow cavities of volcanic or sedimentary rocks. Over millions of years, mineral-rich groundwater seeps into the cavity, precipitating silica crystals onto the walls. Often found in formations dating back to the Mississippian or Jurassic periods.
Uses & applications
Primarily used for decorative display, crystal healing practices, educational specimens, and as a collectible for rockhounds.
Geological facts
Geodes are essentially 'rock bubbles'. While they look like ordinary round stones from the outside, they contain hollow centers lined with crystals. Brazil and Uruguay are world-renowned for giant amethyst and quartz geodes.
Field identification & locations
Identify in the field by looking for rounded, vuggy, lightweight nodules that may rattle when shaken. Common locations include Morocco, Mexico, and the Midwestern United States (Keokuk region).
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