
mineral
Quartz Geode
Silicon Dioxide (SiO2)
Hardness: 7 (Mohs scale); Color: Colorless to milky white crystals on a tan/yellowish matrix; Luster: Vitreous (glassy); Crystal Structure: Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 (Mohs scale)
- Color
- Colorless to milky white crystals on a tan/yellowish matrix
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 (Mohs scale); Color: Colorless to milky white crystals on a tan/yellowish matrix; Luster: Vitreous (glassy); Crystal Structure: Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed as secondary mineral precipitates in hollow cavities (vugs) within sedimentary or volcanic rocks. Mineral-rich groundwater seeps through the porous host rock, depositing crystals over thousands of years.
Uses & applications
Commonly used for geological study, home decor, metaphysical collection, and as a source of high-purity silica for industrial applications.
Geological facts
Geodes are known as 'nature's surprise' because their unremarkable exterior hides a sparkling crystalline interior. Many quartz geodes from Morocco, like this one, date back to the Cretaceous period.
Field identification & locations
Identified by its hollow interior lined with inward-pointing crystals and a harder outer shell. They are frequently found in limestone deserts or volcanic ash beds. Look for round, lumpy rocks that feel lighter than they look.
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Arenite (SiO2 based)
sedimentary
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Schist
Metamorphic
Epidote
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metamorphic
Gypsum (variety Selenite or Alabaster)
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Mineral
Nephrite Jade
Nephrite
Mineral/Rock
Granite
Granite (Phaneritic intrusive igneous rock)
igneous