Rock Identifier
Flint (Microcrystalline quartz (SiO2)) — sedimentary
sedimentary

Flint

Microcrystalline quartz (SiO2)

AI-generated identification · may be incorrect

Hardness of 7 on the Mohs scale, typically brown, gray, or black with a waxy to vitreous luster and conchoidal fracture.

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Physical properties

Hardness of 7 on the Mohs scale, typically brown, gray, or black with a waxy to vitreous luster and conchoidal fracture.

Formation & geological history

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

Uses & applications

Historically used for making stone tools, arrowheads, and fire-starting flintlocks; modernly used in abrasives and decorative gravel.

Geological facts

Flint produces sparks when struck against steel due to its high hardness and brittle fracture creating micro-hotspots.

Field identification & locations

Easily identified by its sharp conchoidal edges, waxy luster, and occurrence as nodules within chalk or limestone deposits.