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

Chert

Chert (SiO2)

Hardness: 7 Mohs scale; Color: typically gray, brown, or tan; Luster: dull to waxy; Structure: microcrystalline or cryptocrystalline; Cleavage: none, conchoidal fracture.

Hardness
7 Mohs scale
Color
typically gray, brown, or tan
Luster
dull to waxy
Identified More sedimentary
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Physical properties

Hardness: 7 Mohs scale; Color: typically gray, brown, or tan; Luster: dull to waxy; Structure: microcrystalline or cryptocrystalline; Cleavage: none, conchoidal fracture.

Formation & geological history

Formed in marine environments through the accumulation of siliceous remains of organisms like diatoms and radiolarians, or via chemical precipitation from silica-rich fluids.

Uses & applications

Historically used for making stone tools (flint knapping); currently used as road base, construction aggregate, and occasionally for lapidary work.

Geological facts

Chert is so hard it can scratch glass. It is often found as nodules within limestone or dolomite beds. Flint is a specific dark variety of chert.

Field identification & locations

Identified by its extreme hardness, smooth conchoidal (shell-like) fracture surfaces, and waxy texture. Extremely common in sedimentary basins worldwide.