
mineral
Quartz Geode (Druzy Quartz)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale. Color: Translucent white to faint pinkish/orange tint on the exterior shell. Luster: Vitreous (glassy) to crystalline sparkle. Crystal Structure: Trigonal / Hexagonal prismatic micro-crystals forming a druzy cavity. Cleavage: None (conchoidal fracture). Specific Gravity: ~2.65.
- Hardness
- 7 on Mohs scale
- Luster
- Vitreous (glassy) to crystalline sparkle
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Physical properties
Hardness: 7 on Mohs scale. Color: Translucent white to faint pinkish/orange tint on the exterior shell. Luster: Vitreous (glassy) to crystalline sparkle. Crystal Structure: Trigonal / Hexagonal prismatic micro-crystals forming a druzy cavity. Cleavage: None (conchoidal fracture). Specific Gravity: ~2.65.
Formation & geological history
Formed when mineral-rich hydrothermal fluids precipitate quartz crystals inside cavities (gas bubbles in volcanic rock or hollows in sedimentary beds) over long periods.
Uses & applications
Popular as decorative collector specimens, crystal healing items, lapidary art, and jewelry accents (druzy stone pendants).
Geological facts
Geodes often appear as plain, unspectacular round rocks from the outside, but cracking them open reveals brilliant hollow cavities lined with glistening quartz crystals.
Field identification & locations
Identified by the distinct hollow cup-like shape lined with tiny, sparkling quartz crystal terminations over a chalcedony or chert matrix. Commonly found in sedimentary deposits in Indiana, Iowa, and Missouri (Keokuk geodes), as well as volcanic regions in Brazil, Uruguay, and Morocco.
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Epidote
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Granite
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