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

Chert / Flint

Microcrystalline Quartz (SiO2)

Hardness of 7 on the Mohs scale; colors range from dark gray, green, brown to black; waxy to vitreous luster; microcrystalline or cryptocrystalline crystal structure; conchoidal fracture with no true cleavage; specific gravity around 2.60 to 2.65.

Identified More sedimentary
Explore Chert / Flint in the encyclopedia →

Identify your own rocks.

Get a report just like this from any photo, free.

Physical properties

Hardness of 7 on the Mohs scale; colors range from dark gray, green, brown to black; waxy to vitreous luster; microcrystalline or cryptocrystalline crystal structure; conchoidal fracture with no true cleavage; specific gravity around 2.60 to 2.65.

Formation & geological history

Formed by the chemical precipitation of silica from aqueous solutions, often replacing carbonate rocks like limestone in marine environments over millions of years.

Uses & applications

Historically used by early humans for stone tools, arrowheads, and fire-starting (flint and steel); occasionally used in decorative landscaping, abrasive grinding, or knapping displays.

Geological facts

Chert is extremely durable and weathering-resistant, which is why ancient stone tools made of chert often survive intact in the archaeological record for tens of thousands of years.

Field identification & locations

Can be identified in the field by its distinct conchoidal fracture (smooth, curved breakage surfaces) and high hardness that readily scratches glass.