
sedimentary
Chert (Flint variety)
Microcrystalline or cryptocrystalline Quartz (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Grey, tan, or white with a waxy or dull luster; Structure: Cryptocrystalline with conchoidal (shell-like) fracture; Cleavage: None.
- Hardness
- 7 on Mohs scale
- Color
- Grey, tan, or white with a waxy or dull luster
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Physical properties
Hardness: 7 on Mohs scale; Color: Grey, tan, or white with a waxy or dull luster; Structure: Cryptocrystalline with conchoidal (shell-like) fracture; Cleavage: None.
Formation & geological history
Formed from the accumulation of silica-rich organic remains or through precipitation from silica-saturated fluids within limestone or chalk beds. Commonly found in sedimentary basins worldwide.
Uses & applications
Historically used for making stone tools (arrowheads, scrapers) and as a spark-starter for firearms; currently used in construction aggregate and as a collector's specimen.
Geological facts
Chert is so hard it can scratch steel or glass. Primitive humans favored it for its ability to produce sharp, durable edges when struck.
Field identification & locations
Identify in the field by its waxy appearance and shell-like curved fracture surfaces when broken. It is extremely common in areas with limestone bedrock.
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