
mineral
River Chalcedony / Agate
Chalcedony (Silicon Dioxide, SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 on the Mohs scale. Color: Translucent grey to brown with waxy luster. Crystal structure: Cryptocrystalline. Cleavage: None (conchoidal fracture). Specific Gravity: 2.6-2.64.
- Hardness
- 6
- Color
- Translucent grey to brown with waxy luster
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Physical properties
Hardness: 6.5-7 on the Mohs scale. Color: Translucent grey to brown with waxy luster. Crystal structure: Cryptocrystalline. Cleavage: None (conchoidal fracture). Specific Gravity: 2.6-2.64.
Formation & geological history
Formed as a chemical precipitate from silica-rich groundwater within volcanic cavities (vesicles) or sedimentary fissures. Often millions of years old, it is weathered out of its host rock and polished naturally by river motion.
Uses & applications
Used primarily in lapidary work for making cabochons, beads, and jewelry. Also used for decorative 'river rocks' in landscaping and as a popular specimen for rock tumbling.
Geological facts
Chalcedony is a broad term for microcrystalline quartz. When it exhibits banding, it is called Agate. Because it is highly resistant to weathering, it often survives long trips downstream, becoming rounded and smooth over centuries.
Field identification & locations
Identify in the field by its translucency (light can pass through it when held to a torch), smooth waxy feel when wet, and lack of visible grains. Common in pebble beaches and gravel bars of ancient riverbeds.
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