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

Chert / Flint

Microcrystalline Quartz (SiO2)

Hardness of 7 on the Mohs scale, waxy to vitreous luster, conchoidal fracture, colors range from white, grey, brown to yellow and black, cryptocrystalline structure, specific gravity around 2.60.

Identified More sedimentary
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Physical properties

Hardness of 7 on the Mohs scale, waxy to vitreous luster, conchoidal fracture, colors range from white, grey, brown to yellow and black, cryptocrystalline structure, specific gravity around 2.60.

Formation & geological history

Formed through the chemical or biochemical precipitation of silica from aqueous solutions, often replacing carbonate rocks (limestone or chalk) during diagenesis. Can form in marine environments over millions of years.

Uses & applications

Historically used for making stone tools, arrowheads, and striking fire due to its sharp conchoidal fracture. Today used in abrasives, road aggregates, and decorative landscaping.

Geological facts

Known as flint when dark-colored and found in chalk deposits. It was one of the most critical materials for early human survival and tool-making.

Field identification & locations

Easily identified by its extreme hardness, smooth waxy surface, and sharp conchoidal edges. Commonly found in limestone and chalk formations worldwide.