
sedimentary
Chert (likely a small flake)
Microcrystalline quartz (SiO₂); the flake-like shape alone does not establish whether it is naturally fractured or worked
AI-generated identification · may be incorrectOpaque tan-brown with a dull to slightly waxy surface and irregular, sharp edges. Chert is typically Mohs 6.5–7, with a fine-grained, non-cleavable structure and conchoidal fracture; hardness and luster cannot be confirmed from the image.
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Physical properties
Opaque tan-brown with a dull to slightly waxy surface and irregular, sharp edges. Chert is typically Mohs 6.5–7, with a fine-grained, non-cleavable structure and conchoidal fracture; hardness and luster cannot be confirmed from the image.
Formation & geological history
Forms when silica accumulates and hardens in sedimentary settings, often as nodules in limestone or chalk. Its age and exact formation environment cannot be determined from the photograph.
Uses & applications
Chert has been used for tools and construction aggregate; suitable material may be collected or cut for decorative pieces.
Geological facts
Its conchoidal fracture can produce very sharp edges, making chert important in prehistoric toolmaking.
Field identification & locations
Look for a uniformly fine texture, no visible grains, and curved fracture surfaces; a fresh edge may be sharper and more diagnostic. Chert occurs worldwide in sedimentary rocks, but this small specimen’s locality is unknown.
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