Rock Identifier
Flint (Sedimentary cryptocrystalline quartz (SiO2)) — sedimentary
sedimentary

Flint

Sedimentary cryptocrystalline quartz (SiO2)

Hardness of 7 on the Mohs scale, dark gray to black color, waxy to vitreous luster, conchoidal fracture, and amorphous/microcrystalline crystal structure.

Identified More sedimentary
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Physical properties

Hardness of 7 on the Mohs scale, dark gray to black color, waxy to vitreous luster, conchoidal fracture, and amorphous/microcrystalline crystal structure.

Formation & geological history

Formed by the replacement of calcium carbonate by silica in chalk or limestone beds during the Cretaceous period through diagenesis.

Uses & applications

Historically used for making stone tools, arrowheads, and striking fire; currently used in specialized grinding and abrasives.

Geological facts

Flint is extremely durable and produces sharp edges when fractured, making it one of the earliest materials utilized by human ancestors for primitive technology.

Field identification & locations

Easily identified by its conchoidal fracture, sharp edges, and hardness capable of scratching glass. Commonly found within chalk formations across northern Europe.