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

Chert / Flint

Microcrystalline Quartz (SiO2)

Hardness of 7 on the Mohs scale, earthy to waxy luster, concoidal fracture, colors range from white, grey, brown to black, specific gravity around 2.60.

Identified More sedimentary
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Physical properties

Hardness of 7 on the Mohs scale, earthy to waxy luster, concoidal fracture, colors range from white, grey, brown to black, specific gravity around 2.60.

Formation & geological history

Formed via the replacement of calcium carbonate by silica in marine environments or the accumulation of siliceous oozes from microscopic organisms, generally dating from the Mesozoic and Cenozoic eras.

Uses & applications

Historically used for making stone tools, arrowheads, and striking fire; currently used in aggregate, abrasive industries, and decorative landscaping.

Geological facts

Chert and flint are chemically identical; flint is traditionally the darker variety found in chalk, while chert is found in limestone. It was one of the most critical materials for early human technological development due to its sharp edges when fractured.

Field identification & locations

Can be identified in the field by its distinct conchoidal fracture and high hardness (scratches glass). Commonly found globally in limestone and chalk formations.