Rock Identifier
Flint (chert) (Microcrystalline quartz (SiO₂), a variety of chert) — sedimentary
sedimentary

Flint (chert)

Microcrystalline quartz (SiO₂), a variety of chert

AI-generated identification · may be incorrect

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.

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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.