
sedimentary
Chert (Jasper variety)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 Mohs; Color: Brown, dark grey, reddish-brown; Luster: Dull to waxy; Structure: Microcrystalline (Cryptocrystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.6-2.7
- Hardness
- 6
- Color
- Brown, dark grey, reddish-brown
- Luster
- Dull to waxy
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Physical properties
Hardness: 6.5-7 Mohs; Color: Brown, dark grey, reddish-brown; Luster: Dull to waxy; Structure: Microcrystalline (Cryptocrystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.6-2.7
Formation & geological history
Formed through the accumulation of silica-rich microfossils (like radiolaria or diatoms) or by chemical precipitation in saltwater environments. Typically found in marine sedimentary layers from various geological ages.
Uses & applications
Historically used for making stone tools due to conchoidal fracture. Modernly used in landscaping, as road aggregate, and for lapidary work (jewelry/polished stones).
Geological facts
Chert is so hard it can scratch steel. It was one of the most important minerals for early humans to create arrowheads and scrapers.
Field identification & locations
Identify by its waxy luster, smoothness when wet, and sharp edges where broken. Commonly found in riverbeds, glacial deposits, and as nodules in 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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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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