
sedimentary
Chert (Flint)
Chert (Silicon Dioxide, SiO2)
AI-generated identification · may be incorrectHardness: 7 (Mohs), Color: Grey, tan, brown, white; Luster: Dull to waxy; Structure: Cryptocrystalline; Cleavage: None (Conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 (Mohs), Color: Grey, tan, brown, white
- Color
- Grey, tan, brown, white
- Luster
- Dull to waxy
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Physical properties
Hardness: 7 (Mohs), Color: Grey, tan, brown, white; Luster: Dull to waxy; Structure: Cryptocrystalline; Cleavage: None (Conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed as nodules or layers in carbonate rocks through the precipitation of silica-rich fluids (often from microfossils like diatoms or radiolaria) during diagenesis.
Uses & applications
Used historically for stone tools and fire-starting; currently used in road construction, as an abrasive, and sometimes for decorative landscape gravel.
Geological facts
Chert has a conchoidal fracture, allowing it to break with sharp edges, which made it the primary material for arrowheads and spear points in prehistoric times.
Field identification & locations
Look for a microcrystalline texture that doesn't show visible grains, a waxy luster on fresh surfaces, and edges that are sharp and glass-like when broken. Common in limestone deposits.
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