Rock Identifier
Flint / Chert (Silicon Dioxide (SiO2)) — sedimentary
sedimentary

Flint / Chert

Silicon Dioxide (SiO2)

Hardness: 6.5-7 Mohs; Color: Grey, black, or brown; Luster: Waxy to dull; Crystal structure: Microcrystalline/Cryptocrystalline quartz; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.

Hardness
6
Color
Grey, black, or brown
Luster
Waxy to dull
Identified More sedimentary
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Physical properties

Hardness: 6.5-7 Mohs; Color: Grey, black, or brown; Luster: Waxy to dull; Crystal structure: Microcrystalline/Cryptocrystalline quartz; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.

Formation & geological history

Formed as nodules in sedimentary rocks like chalk and limestone through the replacement of calcium carbonate by silica-rich fluids. Often contains microscopic fossil remains.

Uses & applications

Historically used for stone tools and starting fires; currently used in grinding media, road construction, and as a decorative stone.

Geological facts

Flint was the primary material for the Stone Age technology due to its ability to break into sharp edges. It produces sparks when struck against steel.

Field identification & locations

Look for a glassy or waxy interior and sharp, shell-like (conchoidal) fractures when broken. Commonly found in coastal chalk cliffs or gravel deposits.