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

Chert / Flint

Microcrystalline Quartz (SiO2)

Hardness: 7 on Mohs scale; Color: Grayish-brown to dark brown; Luster: Waxy to sub-vitreous; Fracture: Conchoidal; Specific Gravity: 2.65.

Hardness
7 on Mohs scale
Color
Grayish-brown to dark brown
Luster
Waxy to sub-vitreous
Identified More sedimentary
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Physical properties

Hardness: 7 on Mohs scale; Color: Grayish-brown to dark brown; Luster: Waxy to sub-vitreous; Fracture: Conchoidal; Specific Gravity: 2.65.

Formation & geological history

Formed through the accumulation of siliceous remains of microscopic organisms (diatoms, radiolarians) or chemical precipitation of silica in marine sedimentary environments.

Uses & applications

Historically used for stone tools, flintknapping, arrowheads, and spark generation. Modern uses include gravel, road aggregate, and lapidary art.

Geological facts

Flint is a variety of chert that produces sparks when struck against steel, making it vital for early human survival and early firearm mechanisms.

Field identification & locations

Identified by its smooth, waxy surface, extreme hardness, and sharp conchoidal edges when fractured. Commonly found in limestone, chalk beds, and river beds globally.