Rock Identifier
Chert (Flint) (Silicon Dioxide (SiO2)) — sedimentary
sedimentary

Chert (Flint)

Silicon Dioxide (SiO2)

Hardness: 7 on Mohs scale; Color: Black, grey, or brown often with a weathered white/tan cortex; Luster: Dull to waxy; Structure: Microcrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65

Hardness
7 on Mohs scale
Luster
Dull to waxy
Identified More sedimentary
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Physical properties

Hardness: 7 on Mohs scale; Color: Black, grey, or brown often with a weathered white/tan cortex; Luster: Dull to waxy; Structure: Microcrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65

Formation & geological history

Formed as nodules or layers in limestone or chalk through the accumulation of siliceous remains of marine organisms like diatoms and radiolarians. The silica precipitates and replaces calcite through diagenesis.

Uses & applications

Historically used for stone tools and weapons due to its sharp edges; modern uses include flintlocks for firearms, road surfacing, and as a raw material in ceramics.

Geological facts

Chert exhibits conchoidal fracture, allowing it to be chipped into extremely sharp blades. It was one of the most important minerals for prehistoric humans during the Stone Age.

Field identification & locations

Identify by its waxy luster on fresh surfaces and glass-like, sharp edges when broken. It will scratch glass but cannot be scratched by a steel knife. Common in limestone outcrops and riverbeds.