Rock Identifier
Chert (Flint) (Silicon dioxide (SiO2)) — sedimentary
sedimentary

Chert (Flint)

Silicon dioxide (SiO2)

Hardness of 7 on the Mohs scale, typically white, grey, brown, or black in color, waxy to vitreous luster, microcrystalline or cryptocrystalline structure, conchoidal fracture with no true cleavage, and a specific gravity of 2.60 to 2.65.

Identified More sedimentary
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Physical properties

Hardness of 7 on the Mohs scale, typically white, grey, brown, or black in color, waxy to vitreous luster, microcrystalline or cryptocrystalline structure, conchoidal fracture with no true cleavage, and a specific gravity of 2.60 to 2.65.

Formation & geological history

Formed through the chemical or biochemical precipitation of silica from aqueous solutions, often replacing carbonate rocks like limestone during diagenesis. Commonly found within chalk or limestone formations and dates across various geological eras.

Uses & applications

Historically used for making stone tools, arrowheads, and spark generation in firearms. Today used in abrasives, ceramics, and as a decorative or collection specimen.

Geological facts

Ancient humans prized chert and flint for its sharp conchoidal fracture, which allows it to be knapped into extremely sharp edges and points for hunting and survival tools.

Field identification & locations

Identified easily by its waxy luster, conchoidal fracture surfaces, and high hardness capable of scratching glass. Found globally in sedimentary strata, particularly marine limestone and chalk deposits.