Rock Identifier
Flint / Chert (Microcrystalline quartz (SiO2)) — sedimentary
sedimentary

Flint / Chert

Microcrystalline quartz (SiO2)

Hardness of 7 on the Mohs scale, colors range from gray, dark brown, to black, vitreous to waxy luster, cryptocrystalline structure, conchoidal fracture with sharp edges, specific gravity of 2.60 to 2.65.

Identified More sedimentary
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Physical properties

Hardness of 7 on the Mohs scale, colors range from gray, dark brown, to black, vitreous to waxy luster, cryptocrystalline structure, conchoidal fracture with sharp edges, specific gravity of 2.60 to 2.65.

Formation & geological history

Forms by the replacement of calcium carbonate by silica in sedimentary environments such as chalk or limestone deposits, typically during the Cretaceous period or earlier.

Uses & applications

Historically used for making stone tools, weapons, and fire-starting (flint and steel). Currently used in decorative landscaping, abrasive grits, and as historical/archaeological collector specimens.

Geological facts

Flint played a crucial role in human evolution by providing durable cutting edges and a reliable method to create fire. It produces sparks when struck against steel due to tiny embedded iron pyrite crystals or friction-induced heat.

Field identification & locations

Easily identifiable in the field by its distinct conchoidal fracture, waxy luster, and ability to scratch glass. Commonly found nodular within chalk or limestone formations worldwide.