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

Flint

Microcrystalline quartz (SiO2)

Hardness of 7 on the Mohs scale, color ranges from grey, white, to brown and black, vitreous to dull luster, cryptocrystalline structure, conchoidal fracture with no cleavage, specific gravity of 2.60 to 2.65.

Identified More sedimentary
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Physical properties

Hardness of 7 on the Mohs scale, color ranges from grey, white, to brown and black, vitreous to dull luster, cryptocrystalline structure, conchoidal fracture with no cleavage, specific gravity of 2.60 to 2.65.

Formation & geological history

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

Uses & applications

Historically used for making stone tools, arrowheads, and striking fire. Modern uses include decorative landscaping, aggregates, and historically in flintlock firearms.

Geological facts

Flint is extremely durable and has been utilized by humans for hundreds of thousands of years due to its sharp conchoidal fracture when struck.

Field identification & locations

Commonly found embedded in chalk cliffs or along beaches where chalk erodes. Easily identified by its weathered white outer cortex and dark interior with sharp edges.