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

Banded Chert

Chert (Microcrystalline Quartz, SiO2)

Hardness: 7 on Mohs scale; Color: Tan, beige, grey, and brown; Luster: Waxy to dull; Structure: Cryptocrystalline; Fracture: Conchoidal; Cleavage: None

Hardness
7 on Mohs scale
Color
Tan, beige, grey, and brown
Luster
Waxy to dull
Identified More sedimentary
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Physical properties

Hardness: 7 on Mohs scale; Color: Tan, beige, grey, and brown; Luster: Waxy to dull; Structure: Cryptocrystalline; Fracture: Conchoidal; Cleavage: None

Formation & geological history

Formed by the accumulation and lithification of silica-rich organic remains (like diatoms or radiolarians) or chemical precipitation from hydrothermal fluids in marine environments. Often found as nodules or layers within limestone.

Uses & applications

Historically used for making stone tools (arrowheads, scrapers) due to conchoidal fracture. Currently used as road surfacing material, in construction, and as decorative landscape stones.

Geological facts

Chert is so hard it can scratch steel and was used for centuries as a 'flint' to start fires. The banding represents changes in sediment deposition or mineral impurities over time.

Field identification & locations

Identify in the field by its waxy texture and sharp, shell-like (conchoidal) fracture patterns when broken. Common in limestone belts and riverbeds in the Midwestern USA and Europe.