
mineral
Chalcedony on Matrix
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 on Mohs scale. Color: Translucent honey-yellow to amber with grey host rock. Luster: Waxy to vitreous. Crystal structure: Cryptocrystalline (hexagonal/trigonal). Cleavage: None, conchoidal fracture.
- Hardness
- 6
- Color
- Translucent honey-yellow to amber with grey host rock
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 on Mohs scale. Color: Translucent honey-yellow to amber with grey host rock. Luster: Waxy to vitreous. Crystal structure: Cryptocrystalline (hexagonal/trigonal). Cleavage: None, conchoidal fracture.
Formation & geological history
Formed from the deposition of microcrystalline silica in volcanic or sedimentary cavities at relatively low temperatures. Often found in hydrothermal veins or as a secondary mineral in basalt vesicles.
Uses & applications
Used primarily for lapidary work, semi-precious jewelry, and as decorative cabinet specimens for mineral collectors.
Geological facts
Chalcedony was one of the first materials used by early humans for tools because of its hardness and the sharp edges it creates when fractured. It is a fibrous variety of quartz.
Field identification & locations
Identify in the field by its waxy appearance, translucency, and inability to be scratched by a steel knife. Common in desert environments and areas with ancient volcanic activity.
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