Rock Identifier
Flint / Chert (Silicon dioxide (Microcrystalline quartz, SiO2)) — sedimentary
sedimentary

Flint / Chert

Silicon dioxide (Microcrystalline quartz, SiO2)

Hardness of 7 on the Mohs scale, colors range from gray, brown, to dark green/black, vitreous to waxy luster, cryptocrystalline structure, no cleavage (exhibits characteristic conchoidal fracture)

Identified More sedimentary
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Physical properties

Hardness of 7 on the Mohs scale, colors range from gray, brown, to dark green/black, vitreous to waxy luster, cryptocrystalline structure, no cleavage (exhibits characteristic conchoidal fracture)

Formation & geological history

Formed through the replacement of calcium carbonate by silica-rich solutions in sedimentary environments such as chalk or limestone formations, typically over millions of years.

Uses & applications

Historically used for making stone tools, arrowheads, and striking fire; currently used in abrasives, landscaping, and decorative knapping.

Geological facts

Flint was one of the earliest materials manipulated by early humans for weaponry and fire-making due to its predictable conchoidal fracture.

Field identification & locations

Easily identified in the field by its smooth, weathered outer cortex, sharp conchoidal edges when broken, and ability to scratch glass.