
sedimentary
Flint Nodule
Cryptocrystalline Quartz (SiO2)
AI-generated identification · may be incorrectHardness 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.
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