
sedimentary
Chert
Cryptocrystalline Quartz (SiO2)
Hardness: 7 on Mohs scale; Color: Gray, tan, and earthy brown; Luster: Dull to waxy; Texture: Fine-grained, microcrystalline; Fracture: conchoidal (shell-like)
- Hardness
- 7 on Mohs scale
- Color
- Gray, tan, and earthy brown
- Luster
- Dull to waxy
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Physical properties
Hardness: 7 on Mohs scale; Color: Gray, tan, and earthy brown; Luster: Dull to waxy; Texture: Fine-grained, microcrystalline; Fracture: conchoidal (shell-like)
Formation & geological history
Formed in marine environments through the accumulation of silica-rich organic remains (like diatoms or radiolarians) or chemical precipitation from groundwater within limestone or chalk beds.
Uses & applications
Historically used for making stone tools (arrowheads, scrapers) due to its sharp edges when broken. Today used in construction aggregate and as a collector's specimen.
Geological facts
Chert is so hard it can scratch glass. It is often found as nodules or 'flint' in chalk and limestone formations. It was one of the first materials used by early humans for tool development.
Field identification & locations
Identified in the field by its extreme hardness, smooth conchoidal fracture, and resistance to chemical weathering. Commonly found in riverbeds or eroding out of sedimentary rock layers.
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Sandstone or Siltstone
Arenite (if sandstone)
Sedimentary
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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