
mineral
Chalcedony (Common Opal variant or Agate)
Silicon Dioxide (SiO2)
Hardness: 6.5–7 (Mohs scale); Color: waxy white, translucent grey, or bluish; Luster: Waxy to vitreous; Crystal Structure: Microcrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.6–2.7.
- Hardness
- 6
- Color
- waxy white, translucent grey, or bluish
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5–7 (Mohs scale); Color: waxy white, translucent grey, or bluish; Luster: Waxy to vitreous; Crystal Structure: Microcrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.6–2.7.
Formation & geological history
Formed from the precipitation of silica-rich groundwater in the cavities of volcanic or sedimentary rocks. It often occurs in hydrothermal veins or as nodules in limestone.
Uses & applications
Used widely in semi-precious jewelry (beads, cabochons), ornamental carvings, and historical stone tools (due to its sharp conchoidal fracture).
Geological facts
Chalcedony is a cryptocrystalline form of silica. If it shows banding, it is called Agate; if it is opaque and reddish, it is Jasper. Archaeologists have found chalcedony seals dating back to the Bronze Age on Crete.
Field identification & locations
Identify in the field by its waxy appearance, smooth conchoidal (shell-like) fracture edges, and its ability to scratch glass. It is commonly found in desert regions or near volcanic ash deposits.
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