Rock Identifier
Chert (likely flint) (Microcrystalline quartz (SiO₂), chiefly chalcedony and quartz) — sedimentary
sedimentary

Chert (likely flint)

Microcrystalline quartz (SiO₂), chiefly chalcedony and quartz

AI-generated identification · may be incorrect

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.

Identified More sedimentary
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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.