Rock Identifier
Chert (Microcrystalline quartz (SiO2)) — sedimentary
sedimentary

Chert

Microcrystalline quartz (SiO2)

Hardness of 7 on the Mohs scale, typically green, grey, brown, or black in color, waxy to dull luster, cryptocrystalline structure, conchoidal fracture with no true cleavage, specific gravity around 2.60 to 2.65.

Identified More sedimentary
Explore Chert 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, typically green, grey, brown, or black in color, waxy to dull luster, cryptocrystalline 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, or the replacement of limestone by silica-rich fluids during diagenesis. Can range in geological age from Precambrian to recent.

Uses & applications

Historically used by ancient humans for making stone tools, arrowheads, and blades due to its conchoidal fracture. Occasionally used for decorative landscaping or lapidary purposes.

Geological facts

Chert is extremely durable and weather-resistant, which is why ancient stone tools made from it survive well in the archaeological record. Varieties of chert include flint and jasper.

Field identification & locations

Can be identified in the field by its hard, dense nature, waxy luster, and distinctive conchoidal fracture surfaces that resemble broken glass. Found worldwide in sedimentary rock sequences, particularly alongside limestone and chalk formations.