
mineral
Chalcedony (Agate/Seashell replacement)
Silicon Dioxide (SiO2) - Cryptocrystalline Quartz
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs), Color: Translucent white to tan, Luster: Waxy to vitreous, Crystal Structure: Trigonal (microscopic), Cleavage: None/Conchoidal fracture
- Hardness
- 6
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Physical properties
Hardness: 6.5-7 (Mohs), Color: Translucent white to tan, Luster: Waxy to vitreous, Crystal Structure: Trigonal (microscopic), Cleavage: None/Conchoidal fracture
Formation & geological history
Formed by the precipitation of silica from groundwater within cavities, often replacing biological matter like shells in sedimentary environments near volcanic activity.
Uses & applications
Used in gemstone carving, jewelry, as decorative collector specimens, and historically for tools due to conchoidal fracturing.
Geological facts
This specimen appears to be a 'chalcedony coral' or a silica-replaced shell fragment, where quartz has slowly replaced the original calcium carbonate structure atom by atom.
Field identification & locations
Identify by its waxy luster, translucency when held to light, and its inability to be scratched by a steel knife. Commonly found in riverbeds and coastal regions with ancient limestone or volcanic deposits.
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