
sedimentary
Chert (Flint)
Silicon Dioxide (SiO2)
Hardness: 7 (Mohs scale); Color: White, tan, or grey (often weathered); Luster: Waxy to dull; Crystal Structure: Microcrystalline/cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
- Hardness
- 7 (Mohs scale)
- Color
- White, tan, or grey (often weathered)
- Luster
- Waxy to dull
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Physical properties
Hardness: 7 (Mohs scale); Color: White, tan, or grey (often weathered); Luster: Waxy to dull; Crystal Structure: Microcrystalline/cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
Formation & geological history
Formed from the accumulation of siliceous remains of organisms like diatoms or radiolarians, or via chemical precipitation within limestone or chalk beds. Most specimens date from the Phanerozoic eon.
Uses & applications
Historically used for stone tools and starting fires (striking steel). Modernly used in construction aggregate, road surfacing, and as a low-cost gemstone or garden stone.
Geological facts
Chert is so hard it can scratch glass and steel. It was the primary material for spearheads and arrowheads for thousands of years due to its predictable conchoidal fracture which creates razor-sharp edges.
Field identification & locations
Identify by its extreme hardness, smooth waxy texture when broken, and curved (conchoidal) fracture lines. Commonly found as nodules or layers in limestone or chalk deposits globally.
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