Rock Identifier
Flint (SiO2 (Microcrystalline Quartz)) — sedimentary
sedimentary

Flint

SiO2 (Microcrystalline Quartz)

AI-generated identification · may be incorrect

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

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Physical properties

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

Formation & geological history

Formed through the chemical replacement of calcium carbonate in limestone or chalk by silica-rich groundwaters during the Cretaceous period.

Uses & applications

Historically used for making stone tools and fire-starting, and currently used in decorative aggregates and specialized industrial grinding.

Geological facts

Flint played a crucial role in human technological development during the Stone Age due to its ability to be knapped into extremely sharp edges.

Field identification & locations

Easily identified by its distinctive conchoidal fracture, waxy luster, and ability to produce sparks when struck with steel; commonly found inside chalk formations.