
sedimentary
Chert Concretion
Silicon dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 Mohs; Color: Tan, brown, or gray; Luster: Waxy to dull; Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.5-2.8
- Hardness
- 6
- Color
- Tan, brown, or gray
- Luster
- Waxy to dull
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Physical properties
Hardness: 6.5-7 Mohs; Color: Tan, brown, or gray; Luster: Waxy to dull; Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.5-2.8
Formation & geological history
Formed through the precipitation of silica within porous sedimentary layers, typically limestone or chalk. These often grow around a nucleus like a fossil or a cavity during diagenesis millions of years ago.
Uses & applications
Historically used for making stone tools; today used in construction decorative stones and for geological education.
Geological facts
Chert is so hard it can scratch glass. It was one of the primary materials used by prehistoric humans to create arrowheads and scrapers due to its sharp edges when broken.
Field identification & locations
Identify in the field by its unusual, often bulbous or lumpy shape and high hardness compared to surrounding limestone. Frequently found in riverbeds or eroded limestone cliffs.
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Other sedimentary specimens
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
fossil
Fossiliferous Sedimentary Rock
Sedimentary limestone with invertebrate fossil imprint
fossil
Sandstone or Siltstone
Arenite (if sandstone)
Sedimentary
Sandstone
Arenite
sedimentary
Shale
Shale (clastic sedimentary rock)
sedimentary
Shale (or Mudstone/Siltstone)
Sedimentary Mudrock (SiO2, Al2O3 base with clay minerals)
sedimentary