
sedimentary
Chert (and Flint)
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale; Color: dirty white to light tan; Luster: waxy to dull; Crystal structure: cryptocrystalline; Cleavage: none, breaks with conchoidal (shell-like) fracture.
- Hardness
- 7 on Mohs scale
- Color
- dirty white to light tan
- Luster
- waxy to dull
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Physical properties
Hardness: 7 on Mohs scale; Color: dirty white to light tan; Luster: waxy to dull; Crystal structure: cryptocrystalline; Cleavage: none, breaks with conchoidal (shell-like) fracture.
Formation & geological history
Formed from the chemical precipitate of silica or the accumulation of silica-rich microfossils like diatoms and radiolarians on the ocean floor. Commonly found in nodular or layered form within limestone or chalk beds.
Uses & applications
Historically used for making stone tools (arrowheads, scrapers) and starting fires. Modernly used in construction aggregate and as a semi-precious gemstone when colorful (Jasper).
Geological facts
Chert is so hard it can scratch steel. It was one of the most vital resources for prehistoric humans due to its ability to produce razor-sharp edges when struck.
Field identification & locations
Identify by its extreme hardness, waxy texture, and sharp, curved edges where it has broken. Look for it in limestone outcrops or as rounded pebbles in riverbeds.
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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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