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

Chert / Flint

Microcrystalline Quartz (SiO2)

Hardness of 7 on the Mohs scale, typically brown, tan, grey or black in color, waxy to vitreous luster, conchoidal fracture with sharp edges, specific gravity around 2.60.

Identified More sedimentary
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Physical properties

Hardness of 7 on the Mohs scale, typically brown, tan, grey or black in color, waxy to vitreous luster, conchoidal fracture with sharp edges, specific gravity around 2.60.

Formation & geological history

Formed via the chemical replacement of limestone or chalk by silica-rich solutions or through the accumulation of siliceous skeletal remains of marine organisms over millions of years.

Uses & applications

Historically used for making stone tools, arrowheads, and spark-striking fire starters; currently used in abrasives, road aggregate, and historically in flintlock firearms.

Geological facts

Chert is extremely durable and resistant to weathering, which is why ancient stone tools made of chert often survive intact in the archaeological record for thousands of years.

Field identification & locations

Can be identified in the field by its distinct conchoidal fracture (smooth, curved breakage patterns), high hardness that scratches glass, and waxy luster. Commonly found nodules within sedimentary limestone formations worldwide.