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

Flint

Sedimentary cryptocrystalline quartz (SiO2)

Hardness of 7 on the Mohs scale, typically dark grey, blue, black, or deep brown with a waxy to vitreous luster, conchoidal fracture, and amorphous or microcrystalline crystal structure.

Identified More sedimentary
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Physical properties

Hardness of 7 on the Mohs scale, typically dark grey, blue, black, or deep brown with a waxy to vitreous luster, conchoidal fracture, and amorphous or microcrystalline crystal structure.

Formation & geological history

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

Uses & applications

Historically used for making stone tools, arrowheads, and fire-striking; currently used in grinding, decorative landscaping, and occasionally as a building material.

Geological facts

Flint was one of the earliest materials utilized by early humans to create sharp cutting edges and implements due to its predictable conchoidal fracture.

Field identification & locations

Easily identified by its dark color, smooth weathered cortex, conchoidal fracture, and extreme hardness. Commonly found embedded in chalk cliffs or as beach pebbles.