
sedimentary
Chert (Flint)
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale; Color: White, grey, light blue-grey; Luster: Waxy to dull; Crystal structure: Microcrystalline/Cryptocrystalline (trigonal); Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- White, grey, light blue-grey
- Luster
- Waxy to dull
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Physical properties
Hardness: 7 on Mohs scale; Color: White, grey, light blue-grey; Luster: Waxy to dull; Crystal structure: Microcrystalline/Cryptocrystalline (trigonal); Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
Formation & geological history
Formed through the accumulation of silica-rich organic remains (like radiolaria or diatoms) or by chemical precipitation in marine environments. Often found as nodules within limestone or chalk beds.
Uses & applications
Historically used for stone tools and weapons due to sharp edges; currently used as road aggregate, in glass manufacturing, and occasionally in jewelry as a cabochon.
Geological facts
Chert has a conchoidal fracture, which means it breaks like glass, producing sharp, curved edges. This property made it the primary material for arrowheads and spear points for thousands of years.
Field identification & locations
Identify by its hardness (it can scratch glass), its waxy texture, and the distinctive curved 'shell-like' patterns where it has been chipped. Commonly found in stream beds or within sedimentary rock outcrops.
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Cone-in-cone structure (Secondary Sedimentary Structure)
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Chert Breccia
Brecciated Chert (Microcrystalline Silica)
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