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

Flint / Chert

Silicon dioxide (SiO2) - Microcrystalline Quartz

Hardness: 7 on the Mohs scale, Color: Grey, black, brown, or white, Luster: Waxy to vitreous, Crystal structure: Microcrystalline/Cryptocrystalline, Cleavage: None (exhibits conchoidal fracture), Specific gravity: 2.60 to 2.65

Identified More sedimentary
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Physical properties

Hardness: 7 on the Mohs scale, Color: Grey, black, brown, or white, Luster: Waxy to vitreous, Crystal structure: Microcrystalline/Cryptocrystalline, Cleavage: None (exhibits conchoidal fracture), Specific gravity: 2.60 to 2.65

Formation & geological history

Formed by the replacement of calcium carbonate by silica-rich solutions in marine environments (such as chalk or limestone formations) during the Cretaceous period or other sedimentary deposition eras.

Uses & applications

Historically used for making stone tools, arrowheads, and spark generation with steel; occasionally used in ornamental objects or abrasive media.

Geological facts

Flint was crucial for human survival during the Stone Age due to its ability to be chipped into extremely sharp edges through knapping and its capacity to strike sparks for fire.

Field identification & locations

Can be identified in the field by its distinct conchoidal fracture with razor-sharp edges, waxy luster, and high hardness capable of scratching glass.