
mineral
Quartz Geode (Cracked Open)
Quartz (Silicon Dioxide - SiO2)
Hardness: 7 (Mohs scale); Color: White, clear, often stained with iron oxides (red/orange); Luster: Vitreous to waxy; Crystal structure: Hexagonal/Trigonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
- Hardness
- 7 (Mohs scale)
- Color
- White, clear, often stained with iron oxides (red/orange)
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 7 (Mohs scale); Color: White, clear, often stained with iron oxides (red/orange); Luster: Vitreous to waxy; Crystal structure: Hexagonal/Trigonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
Formation & geological history
Formed in cavities within volcanic or sedimentary rocks. Silica-rich hydrothermal fluids or groundwater seep into hollow shells (vesicles or nodules), slowly precipitating quartz crystals over thousands to millions of years.
Uses & applications
Used primarily for interior décor, crystal healing collections, and educational specimens. Quartz itself is used in electronics and glass manufacturing, but geode forms are for collecting.
Geological facts
Geodes are the state rock of Iowa. They are unique because they look like ordinary rocks on the outside but contain hidden crystal wonders inside.
Field identification & locations
Identify in the field by looking for spherical or potato-like nodules that feel lighter than other rocks of the same size. Commonly found in riverbeds or limestone deposits.
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