
mineral
Chalcedony (Botryoidal or Agate nodule)
Silicon Dioxide (SiO2)
Hardness: 6.5-7.0 (Mohs scale); Color: Translucent tan, honey-yellow, or greyish; Luster: Waxy to vitreous; Crystal structure: Trigonal/Microcrystalline; Cleavage: None; Specific gravity: 2.58–2.64.
- Hardness
- 6
- Color
- Translucent tan, honey-yellow, or greyish
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7.0 (Mohs scale); Color: Translucent tan, honey-yellow, or greyish; Luster: Waxy to vitreous; Crystal structure: Trigonal/Microcrystalline; Cleavage: None; Specific gravity: 2.58–2.64.
Formation & geological history
Formed through the deposition of silica-rich water in cavities (vugs) within volcanic ash or basaltic rock. It precipitates at relatively low temperatures, often resulting in smooth, rounded, or 'bumpy' (botryoidal) surfaces. These specimens can range in age from the Cenozoic to much older depending on the host formation.
Uses & applications
Commonly used in lapidary work for cabochons, beads, and carvings. High-quality specimens are popular for rock collecting. Historically used for making tools and seals due to its toughness and lack of cleavage.
Geological facts
Chalcedony is a cryptocrystalline form of silica, meaning its crystals are too small to be seen without high magnification. It often forms the base material for named varieties like agate, carnelian, and onyx.
Field identification & locations
Identify in the field by its waxy luster, translucency, and conchoidal (shell-like) fracture when broken. It cannot be scratched by a steel knife. Frequently found in desert regions, gravel beds, or weathering out of volcanic rock. Common locations include the Western USA, Brazil, and India.
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