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

Chert (Flint nodule)

Microcrystalline Quartz (SiO2)

AI-generated identification · may be incorrect

Hardness of 7 on Mohs scale; waxy to dull luster, conchoidal fracture, and a brownish-gray interior surrounded by a pale weathering rind (cortex).

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Physical properties

Hardness of 7 on Mohs scale; waxy to dull luster, conchoidal fracture, and a brownish-gray interior surrounded by a pale weathering rind (cortex).

Formation & geological history

Formed biochemically or diagenetically by precipitation of silica from siliceous organism remains (like radiolarians or sponge spicules) within chalk or limestone beds.

Uses & applications

Historically used for making knapped stone tools and fire-starting; currently used in gravel, road construction, and decorative landscaping.

Geological facts

When struck with steel or another hard stone, flint sparks easily, making it one of the earliest technological materials used by early humans for fire and weaponry.

Field identification & locations

Identifiable by its smooth, shell-like conchoidal fracture, high hardness (scratches glass), and chalky exterior crust; widely found in Cretaceous chalk and marine limestone formations worldwide.