
sedimentary
Chert (likely flint)
Microcrystalline quartz (SiO₂), chiefly chalcedony and quartz
AI-generated identification · may be incorrectTypically Mohs hardness 6.5–7, brown to gray, dense and opaque, with a dull to waxy luster and conchoidal fracture; no visible cleavage. The smooth, fine-grained texture and sharp fractured edge fit chert.
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Physical properties
Typically Mohs hardness 6.5–7, brown to gray, dense and opaque, with a dull to waxy luster and conchoidal fracture; no visible cleavage. The smooth, fine-grained texture and sharp fractured edge fit chert.
Formation & geological history
Forms mainly by silica replacement of limestone or accumulation of microscopic siliceous remains, commonly during the Paleozoic–Cenozoic. Weathering can release durable nodules or cobbles from carbonate strata.
Uses & applications
Historically used for sharp tools, arrowheads, and fire-starting; today it is mainly a decorative, lapidary, aggregate, and teaching material.
Geological facts
Fresh fractures can produce exceptionally sharp edges because of conchoidal breakage. Brown coloration commonly reflects iron oxides or organic impurities.
Field identification & locations
Identify it by testing for glass-scratching hardness, very fine texture, lack of fizz in dilute acid, and curved fracture surfaces. Common in limestone regions worldwide, including river gravels and glacial deposits.
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