
sedimentary
Chert (Flint)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 (Mohs scale); Color: Dark brown to black with a tan weathering crust; Luster: Waxy to dull; Crystal structure: Microcrystalline/Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.65
- Hardness
- 7 (Mohs scale)
- Color
- Dark brown to black with a tan weathering crust
- Luster
- Waxy to dull
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Physical properties
Hardness: 7 (Mohs scale); Color: Dark brown to black with a tan weathering crust; Luster: Waxy to dull; Crystal structure: Microcrystalline/Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.65
Formation & geological history
Formed through the accumulation of silica-rich organic remains (like diatoms or radiolarians) or by chemical precipitation in marine environments; often found as nodules in limestone or chalk beds.
Uses & applications
Historically used for stone tools and weapons (arrowheads); currently used in construction aggregate, as a gemstone (variety of jasper/agate), and for fire-starting in survival kits.
Geological facts
Flint was one of the most important materials for early humans because of its ability to fracture into sharp edges and produce sparks when struck against steel or iron pyrites.
Field identification & locations
Identify by its characteristic conchoidal (shell-like) fracture, sharp edges when broken, and inability to be scratched by a steel knife. Commonly found in riverbeds or within limestone outcrops.
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