
sedimentary
Chert (Flint)
Silicon Dioxide (SiO2)
Hardness: 7; Color: White, cream, tan, grey; Luster: Waxy to dull; Crystal structure: Microcrystalline (Cryptocrystalline); Cleavage: None (Conchoidal fracture); Specific gravity: 2.65
- Hardness
- 7
- Color
- White, cream, tan, grey
- Luster
- Waxy to dull
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Physical properties
Hardness: 7; Color: White, cream, tan, grey; Luster: Waxy to dull; Crystal structure: Microcrystalline (Cryptocrystalline); Cleavage: None (Conchoidal fracture); Specific gravity: 2.65
Formation & geological history
Formed as nodules or layered deposits in sedimentary rocks like limestone or chalk. It originates from the accumulation of siliceous remains of marine organisms (radiolarians/diatoms) that dissolve and reprecipitate as silica.
Uses & applications
Used historically for stone tools and weapons (arrowheads). Modern uses include road surfacing, jewelry (as jasper/agate), and as a component in certain ceramics.
Geological facts
Because it breaks with a conchoidal fracture, it creates sharp edges that were vital for early human survival in making cutting tools and spear tips.
Field identification & locations
Identify by its extreme hardness (scratches glass), waxy luster, and curved, shell-like (conchoidal) fracture surfaces. Commonly found in riverbeds or eroding out of limestone cliffs.
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Sandstone or Siltstone
Arenite (if sandstone)
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Cone-in-cone structure (Limestone)
Cone-in-cone structure (Secondary Sedimentary Structure)
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Chert Breccia
Brecciated Chert (Microcrystalline Silica)
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Sandstone Grain
Clastic Sedimentary Rock Grain (SiO2 dominated)
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Shale or Slaty Mudstone
Argillaceous sedimentary rock
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Sandstone
Arenite (primarily SiO2)
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