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

Chert

Microcrystalline Quartz (SiO2)

Hardness: 7 on Mohs scale; Color: Brownish-tan; Luster: Dull to waxy; Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture)

Hardness
7 on Mohs scale
Color
Brownish-tan
Luster
Dull to waxy
Identified More sedimentary

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Physical properties

Hardness: 7 on Mohs scale; Color: Brownish-tan; Luster: Dull to waxy; Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture)

Formation & geological history

Formed through the accumulation of silica-rich organic remains or chemical precipitation in marine environments; age varies from Precambrian to Cenozoic.

Uses & applications

Historically used for making stone tools; currently used as road aggregate and for lapidary work in some forms like jasper or flint.

Geological facts

Chert is so hard it can create sparks when struck against steel. It was one of the most important raw materials for early humans to create arrowheads and knives.

Field identification & locations

Identify by its extreme hardness (cannot be scratched by a steel knife) and its wavy or shell-like fracture pattern. Often found as nodules in limestone or as thin beds.