
sedimentary
Chert (River Stone)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 Mohs. Color: Tan, grey, brown. Luster: Dull to waxy. Structure: Microcrystalline/Cryptocrystalline. Cleavage: None (conchoidal fracture). Specific Gravity: 2.5-2.8.
- Hardness
- 6
- Color
- Tan, grey, brown
- Luster
- Dull to waxy
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Physical properties
Hardness: 6.5-7 Mohs. Color: Tan, grey, brown. Luster: Dull to waxy. Structure: Microcrystalline/Cryptocrystalline. Cleavage: None (conchoidal fracture). Specific Gravity: 2.5-2.8.
Formation & geological history
Formed through the accumulation of silica-rich organic remains or chemical precipitation in sedimentary environments. Usually associated with marine limestone or as nodules in chalk. This specimen shows water-worn rounding, suggesting a fluvial (river) history.
Uses & applications
Historically used for stone tools and arrowheads due to its sharp edges. Modernly used in landscaping, road construction aggregate, and as a decorative river rock.
Geological facts
Chert is so durable that it often survives long after the surrounding rock has eroded. It was the preferred material for making fire-starting flints in early history.
Field identification & locations
Identify by its extreme hardness (cannot be scratched by steel) and smooth, shell-like (conchoidal) fracture surfaces. Commonly found in riverbeds and gravel pits.
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