Rock Identifier
Flint Nodule (Cryptocrystalline Quartz (SiO2)) — sedimentary
sedimentary

Flint Nodule

Cryptocrystalline Quartz (SiO2)

AI-generated identification · may be incorrect

Hardness of 7 on Mohs scale, earthy or waxy luster, concoidal fracture, colors range from gray, brown, to yellowish-white with a chalky cortex.

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Physical properties

Hardness of 7 on Mohs scale, earthy or waxy luster, concoidal fracture, colors range from gray, brown, to yellowish-white with a chalky cortex.

Formation & geological history

Formed diagenetically through the replacement of calcium carbonate in chalk or limestone by silica-rich solutions during the Cretaceous period.

Uses & applications

Historically used for prehistoric stone tools and fire-starting; currently valued by collectors and knappers.

Geological facts

Flint is extremely durable and breaks with razor-sharp edges, making it the primary material for ancient weaponry and tools.

Field identification & locations

Found embedded within chalk or limestone formations; identified by its distinctive conchoidal fracture and soft outer chalky rind.