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

Chert / Flint

Microcrystalline quartz (SiO2)

Hardness of 7 on the Mohs scale, waxy luster, conchoidal fracture, colors range from gray, white, and brown to black, specific gravity of 2.60 to 2.65.

Identified More sedimentary
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Physical properties

Hardness of 7 on the Mohs scale, waxy luster, conchoidal fracture, colors range from gray, white, and brown to black, specific gravity of 2.60 to 2.65.

Formation & geological history

Formed via the chemical replacement of limestone or chalk by silica-rich solutions, or through the accumulation of siliceous skeletal remains of marine organisms such as diatoms and radiolarians over millions of years.

Uses & applications

Historically used for making stone tools, arrowheads, and striking fire. Occasionally used for decorative carvings, jewelry, and industrial grinding.

Geological facts

Known as flint when found as nodules in chalk, and chert when found in limestone formations. It was one of the most critical materials for prehistoric human survival due to its ability to fracture with extremely sharp edges.

Field identification & locations

Can be identified by its distinctive conchoidal (shell-like) fracture, hardness that easily scratches glass, and waxy luster. Common globally in sedimentary rock layers worldwide.