Rock Identifier
Flint (SiO2) — sedimentary
sedimentary

Flint

SiO2

AI-generated identification · may be incorrect

Mohs hardness of 7, vitreous to dull luster, cryptocrystalline quartz structure, conchoidal fracture, and typically dark gray to brown with a white chalky cortex.

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Physical properties

Mohs hardness of 7, vitreous to dull luster, cryptocrystalline quartz structure, conchoidal fracture, and typically dark gray to brown with a white chalky cortex.

Formation & geological history

Formed through the chemical replacement of calcium carbonate by silica-rich groundwater within chalk or limestone formations during the Cretaceous period.

Uses & applications

Historically used for making stone tools and striking fire; currently utilized in abrasives and decorative landscaping.

Geological facts

Flint was one of the earliest materials mastered by early humans for weaponry and fire-starting due to its predictable sharp conchoidal fracture.

Field identification & locations

Identified easily by its waxy luster, conchoidal edges, and the chalky white outer rind; commonly found embedded in chalk cliffs worldwide.