
mineral
Quartz Geode
Crystalline Silicon Dioxide (SiO2) in a Geode
Hardness: 7 on Mohs scale; Color: Clear to white interior crystals with a brown or tan outer rind; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture).
- Hardness
- 7 on Mohs scale
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 on Mohs scale; Color: Clear to white interior crystals with a brown or tan outer rind; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture).
Formation & geological history
Geodes form in cavities within volcanic or sedimentary rocks. Over millions of years, mineral-rich groundwater seeps into these hollows, precipitating crystals onto the inner walls. Most common in regions with ancient volcanic activity.
Uses & applications
Primarily used for decorative display, educational purposes in geology, metaphysical spiritual practices, and as a collector's specimen. Sliced pieces may be used in jewelry.
Geological facts
Geodes are like nature's 'jack-in-the-box'; they look like ordinary rocks on the outside but contain beautiful crystal hidden inside. The word 'geode' comes from the Greek word 'Geoides' meaning earth-like.
Field identification & locations
Identify in the field by looking for rounded, nodular rocks that feel unusually light for their size. Commonly found in desert regions of the SW United States, Brazil, and Mexico. Use a rock hammer to carefully crack them open.
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