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

Flint

SiO2 (Microcrystalline Quartz)

AI-generated identification · may be incorrect

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

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Physical properties

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

Formation & geological history

Formed through the chemical replacement of limestone or chalk by silica-rich groundwaters in marine environments during the Cretaceous period.

Uses & applications

Historically used for making stone tools and fire-starting; currently used for landscaping, road aggregate, and novelty items.

Geological facts

Flint was crucial for early human survival due to its ability to fracture into extremely sharp edges, known as conchoidal fracture.

Field identification & locations

Easily identified in the field by its distinct conchoidal fracture, sharp edges, and white weathered outer cortex; commonly found in chalk deposits worldwide.