Rock Identifier
Chert / Flint Nodule (Microcrystalline Quartz (SiO2)) — sedimentary
sedimentary

Chert / Flint Nodule

Microcrystalline Quartz (SiO2)

Hardness of 7 on the Mohs scale, dull to waxy luster, crypto-crystalline structure, conchoidal fracture, colors range from grey, brown, white to black.

Identified More sedimentary
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Physical properties

Hardness of 7 on the Mohs scale, dull to waxy luster, crypto-crystalline structure, conchoidal fracture, colors range from grey, brown, white to black.

Formation & geological history

Formed through the chemical precipitation of silica from aqueous solutions or the replacement of limestone/chalk by silica-rich fluids over geological time.

Uses & applications

Historically used for making stone tools and weapons due to its sharp edges when fractured; currently collected as a geological specimen.

Geological facts

Ancient humans heavily utilized chert and flint for knapping arrowheads and blades because of its predictable conchoidal fracture.

Field identification & locations

Found worldwide in sedimentary sequences, particularly within chalk and limestone formations. Identify by its smooth, weathered exterior rind and typical conchoidal fracture.