
sedimentary
Chert / Flint
Chert (Cryptocrystalline Quartz, SiO2)
Hardness: 7 (Mohs scale); Color: Brown, tan, cream; Luster: Waxy to dull; Structure: Cryptocrystalline (microscopic crystals); Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
- Hardness
- 7 (Mohs scale)
- Color
- Brown, tan, cream
- Luster
- Waxy to dull
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Physical properties
Hardness: 7 (Mohs scale); Color: Brown, tan, cream; Luster: Waxy to dull; Structure: Cryptocrystalline (microscopic crystals); Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
Formation & geological history
Formed through the accumulation of silica-rich organic remains (like diatoms or radiolarians) or chemical precipitation from groundwater within limestone or chalk beds. It can date from the Precambrian to the Cenozoic era.
Uses & applications
Historically used for stone tools (arrowheads, scrapers) due to its sharp edges; used in construction as road metal and aggregate; also used in fire-starting kits (flint).
Geological facts
Chert was one of the first materials used by early humans for tools because of its conchoidal fracture, which creates razor-sharp edges. It is incredibly durable and chemically resistant.
Field identification & locations
Identify by its extreme hardness (cannot be scratched by steel), waxy texture, and conchoidal (shell-like) fracture patterns. Frequently found in stream beds or within limestone outcrops.
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