
sedimentary
Flint (chert)
Microcrystalline quartz (SiO₂), a variety of chert
AI-generated identification · may be incorrectDense, fine-grained stone with a dull-to-waxy luster, gray-brown coloration, and conchoidal fracture with sharp edges; hardness about 7 Mohs. The image shows a broken flake surface and weathered brown cortex.
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Physical properties
Dense, fine-grained stone with a dull-to-waxy luster, gray-brown coloration, and conchoidal fracture with sharp edges; hardness about 7 Mohs. The image shows a broken flake surface and weathered brown cortex.
Formation & geological history
Forms as silica-rich nodules or layers in sedimentary rocks, commonly limestone or chalk, through diagenetic replacement. Its age depends on the host formation; flint deposits range from Paleozoic to Cenozoic.
Uses & applications
Historically used for tools and fire-starting; today collected and sometimes used in decorative stonework.
Geological facts
Flint fractures into sharp flakes, making it an important material for prehistoric blades and scrapers.
Field identification & locations
Look for a smooth, curved fracture face, sharp edges, and a contrasting weathered outer rind. Common in chalk and limestone regions, including parts of Europe and North America.
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