Rock Identifier
Flint (Sedimentary cryptocrystalline quartz (SiO2)) — sedimentary
sedimentary

Flint

Sedimentary cryptocrystalline quartz (SiO2)

Hardness: 7 on the Mohs scale. Color: Typically dark grey, black, brown, or dark green. Luster: Vitreous to waxy. Crystal structure: Microcrystalline/cryptocrystalline quartz (chalcedony). Cleavage: None, exhibits conchoidal fracture. Specific gravity: 2.60 to 2.65.

Hardness
7 on the Mohs scale
Color
Typically dark grey, black, brown, or dark green
Luster
Vitreous to waxy
Identified More sedimentary
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Physical properties

Hardness: 7 on the Mohs scale. Color: Typically dark grey, black, brown, or dark green. Luster: Vitreous to waxy. Crystal structure: Microcrystalline/cryptocrystalline quartz (chalcedony). Cleavage: None, exhibits conchoidal fracture. Specific gravity: 2.60 to 2.65.

Formation & geological history

Formed by the chemical replacement of calcium carbonate in limestone or chalk by silica-rich solutions during the diagenesis of sedimentary rock. Can date from millions of years old, commonly associated with Cretaceous chalk deposits.

Uses & applications

Historically used for making stone tools, arrowheads, and firearm ignition mechanisms (flintlocks). Today primarily used for decorative purposes, lapidary work, and sometimes as abrasive grit.

Geological facts

Flint is virtually identical to chert chemically, though 'flint' is traditionally used specifically for the dark varieties found in chalk formations. It produces sparks when struck against steel, which made it crucial for early fire-starting.

Field identification & locations

Can be identified in the field by its conchoidal fracture (smooth, curved breakage patterns), high hardness that scratches glass, and waxy luster. Found worldwide in chalk and limestone strata, frequently in riverbeds or coastal gravels where nodules have weathered out.