
sedimentary
Chert / Flint
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 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
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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.
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