
sedimentary
Quartz Geode
Crystalline Silicon Dioxide (SiO2) in Geode form
Hardness: 7 on Mohs scale; Color: Clear to milky white crystals with gray/brown outer shell; Luster: Vitreous; Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Clear to milky white crystals with gray/brown outer shell
- Luster
- Vitreous
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Physical properties
Hardness: 7 on Mohs scale; Color: Clear to milky white crystals with gray/brown outer shell; Luster: Vitreous; Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed via chemical precipitation of mineral-rich groundwater within hollow cavities in sedimentary or volcanic rock. Over millions of years, silica layers deposit to form an outer chalcedony shell with internal crystal growth.
Uses & applications
Primarily used for geological education, home decor, and crystal collection. High-purity quartz is used in electronics and glass manufacturing.
Geological facts
Geodes are often called 'thunder eggs' and can remain hidden for millions of years looking like ordinary round rocks until they are cracked open to reveal their hidden hollow interior.
Field identification & locations
Identify in the field by looking for unusually light, round, or lumpy nodules in limestone or volcanic ash beds. A hollow sound when tapped is a key indicator. Commonly found in deserts like those in Morocco, Mexico, and the Western United States.
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