
sedimentary
Chert (variations include Flint)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 Mohs; Color: Gray, tan, or brown; Luster: Waxy to dull; Crystal structure: Microcrystalline (Cryptocrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
- Hardness
- 7 Mohs
- Color
- Gray, tan, or brown
- Luster
- Waxy to dull
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Physical properties
Hardness: 7 Mohs; Color: Gray, tan, or brown; Luster: Waxy to dull; Crystal structure: Microcrystalline (Cryptocrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
Formation & geological history
Formed by the precipitation of silica from water, often replacing organic material or filling cavities in limestone/dolomite. Common in marine sedimentary environments through various geological ages.
Uses & applications
Used historically for stone tools and reaching fire (flint). Currently used as a raw material for ceramics, construction aggregate, and occasionally for lapidary work.
Geological facts
Chert was one of the most vital resources for prehistoric humans due to its ability to be chipped into sharp edges. It is extremely resistant to chemical weathering.
Field identification & locations
Identify by its waxy appearance and the sharp, curved (conchoidal) edges when broken. It will easily scratch glass and steel. Found globally in nodules or bedded layers within limestone.
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Fossil-bearing concretion, possibly containing a fossil shell or other organic inclusion
Calcareous concretion; exact fossil and host-rock composition are not identifiable from the image
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Fossiliferous Sedimentary Rock
Sedimentary limestone with invertebrate fossil imprint
fossil
Sandstone or Siltstone
Arenite (if sandstone)
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Sandstone
Arenite
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Shale
Shale (clastic sedimentary rock)
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Shale (or Mudstone/Siltstone)
Sedimentary Mudrock (SiO2, Al2O3 base with clay minerals)
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