Rock Identifier
Flint (Cryptocrystalline quartz (SiO2)) — sedimentary
sedimentary

Flint

Cryptocrystalline quartz (SiO2)

Hardness of 7 on the Mohs scale, typically dark gray, black, or dark brown with a waxy to vitreous luster, conchoidal fracture, and no true cleavage.

Identified More sedimentary
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Physical properties

Hardness of 7 on the Mohs scale, typically dark gray, black, or dark brown with a waxy to vitreous luster, conchoidal fracture, and no true cleavage.

Formation & geological history

Formed as nodules or masses in sedimentary rocks such as chalk and limestone through the replacement of calcium carbonate by silica-rich solutions over millions of years.

Uses & applications

Historically used for making stone tools, weapons, and fire-starting flint-and-steel sets; currently used in decorative landscaping and occasionally in specialized industrial applications.

Geological facts

Flint has been utilized by humans since the Stone Age due to its ability to fracture sharply, creating extremely keen edges known as conchoidal fractures.

Field identification & locations

Easily identified by its dark, often weathered exterior, smooth waxy interior fracture surfaces, conchoidal chipping, and ability to scratch glass.