Rock Identifier
Flint / Chert (or fossiliferous nodule) (Microcrystalline quartz (SiO2)) — sedimentary
sedimentary

Flint / Chert (or fossiliferous nodule)

Microcrystalline quartz (SiO2)

Hardness: 7 on Mohs scale. Color: Varies from grey, white, brown to yellowish. Luster: Waxy to vitreous. Crystal structure: Cryptocrystalline or microcrystalline quartz (chalcedony). Cleavage: None, exhibits conchoidal fracture.

Hardness
7 on Mohs scale
Color
Varies from grey, white, brown to yellowish
Luster
Waxy to vitreous
Identified More sedimentary
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Physical properties

Hardness: 7 on Mohs scale. Color: Varies from grey, white, brown to yellowish. Luster: Waxy to vitreous. Crystal structure: Cryptocrystalline or microcrystalline quartz (chalcedony). Cleavage: None, exhibits conchoidal fracture.

Formation & geological history

Formed through the replacement of calcium carbonate by silica-rich solutions in sedimentary environments, often within chalk or limestone formations over millions of years during the Cretaceous period and other geological eras.

Uses & applications

Historically used for making stone tools, arrowheads, and striking fire. Today used for decorative landscaping, gravel, flint knapping hobbies, and historically in flintlock firearms.

Geological facts

Flint and chert are chemically identical, though archaeologists and geologists often use 'flint' to describe material found in chalk formations and 'chert' for varieties found in limestone.

Field identification & locations

Identified by its distinctive conchoidal fracture, sharp edges when broken, waxy luster, and high hardness capable of scratching glass. Commonly found in chalk deposits and river gravels.