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

Chert / Flint

Silicon Dioxide (SiO2)

AI-generated identification · may be incorrect

Hardness: 6.5-7 on Mohs scale. Color: Gray, purple-tinted, brown, to translucent white. Luster: Waxy to dull. Fracture: Conchoidal with sharp edges. Microcrystalline structure.

Hardness
6
Color
Gray, purple-tinted, brown, to translucent white
Luster
Waxy to dull
Identified More sedimentary
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Physical properties

Hardness: 6.5-7 on Mohs scale. Color: Gray, purple-tinted, brown, to translucent white. Luster: Waxy to dull. Fracture: Conchoidal with sharp edges. Microcrystalline structure.

Formation & geological history

Formed through biochemical and chemical precipitation of microcrystalline quartz, often in marine environments within limestone or chalk beds as nodules or layers.

Uses & applications

Historically used for making stone tools, arrowheads, and spark-striking flint. Today used in lapidary art, decorative stone, and gravel aggregate.

Geological facts

Chert fractures with a distinct conchoidal (shell-like) fracture, producing razor-sharp edges that were crucial for ancient stone tool production.

Field identification & locations

Look for smooth, waxy surfaces with curved, glass-like sharp fractures. Highly durable and non-porous compared to surrounding limestone or dolomite matrix.