
sedimentary
Chert (Flint)
Chert (Silicon Dioxide, SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Gray, tan, white, or brown; Luster: Waxy to dull; Crystal structure: Microcrystalline/Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.6-2.7.
- Hardness
- 7 on Mohs scale
- Color
- Gray, tan, white, or brown
- Luster
- Waxy to dull
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Physical properties
Hardness: 7 on Mohs scale; Color: Gray, tan, white, or brown; Luster: Waxy to dull; Crystal structure: Microcrystalline/Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.6-2.7.
Formation & geological history
Formed through the accumulation of silica-rich organic remains or the chemical precipitation of silica in sedimentary basins, often occurring as nodules in limestone or chalk beds.
Uses & applications
Historically used for stone tools and fire-starting; currently used as road aggregate, in jewelry (as jasper or agate varieties), and for flintlock firearms.
Geological facts
Flint is a variety of chert that was the primary material for the Stone Age technology due to its ability to chip into sharp edges. It produces sparks when struck against steel.
Field identification & locations
Identify by its 'waxy' texture and sharp, curved (conchoidal) edges when broken. It is harder than steel and will scratch glass. Common in river beds and chalk cliffs.
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