
sedimentary
Chert (Flint)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 Mohs. Color: usually brownish-black, grey, or dark tan. Luster: Vitreous to waxy. Structure: Microcrystalline/Cryptocrystalline. Features: Conchoidal fracture with sharp edges.
- Hardness
- 6
- Color
- usually brownish-black, grey, or dark tan
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5-7 Mohs. Color: usually brownish-black, grey, or dark tan. Luster: Vitreous to waxy. Structure: Microcrystalline/Cryptocrystalline. Features: Conchoidal fracture with sharp edges.
Formation & geological history
Formed as nodules or beds in sedimentary rocks (like limestone) through the chemical precipitation of silica, often from the remains of microscopic organisms like diatoms or radiolarians.
Uses & applications
Historically used for stone tools and weapons (arrowheads, scrapers) and to strike fire. Today used as a road aggregate, in jewelry as jasper/agate variants, and as a decorative stone.
Geological facts
Flint was a vital survival resource for prehistoric humans due to its ability to be knapped into extremely sharp tools and its sparking properties when struck against steel or iron pyrites.
Field identification & locations
Identify in the field by its smooth, waxy texture and curved, glass-like 'conchoidal' fractures. Found globally in chalk and limestone deposits. Highly prized by flint-knapping hobbyists.
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