
sedimentary
Chert (specifically Flint or Nodular Chert)
Silicon dioxide (SiO2)
Hardness: 7 on Mohs scale; Color: Tan, beige, or cream; Luster: Dull to waxy; Structure: Microcrystalline; Fracture: Conchoidal (shell-like curves)
- Hardness
- 7 on Mohs scale
- Color
- Tan, beige, or cream
- Luster
- Dull to waxy
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Physical properties
Hardness: 7 on Mohs scale; Color: Tan, beige, or cream; Luster: Dull to waxy; Structure: Microcrystalline; Fracture: Conchoidal (shell-like curves)
Formation & geological history
Formed through the accumulation of silica-rich organic remains or chemical precipitation in marine environments, often as nodules within limestone or chalk beds.
Uses & applications
Historically used for stone tools (knapping) and fire-starting; currently used for decorative stone, landscaping, and as a raw material for ceramics and glass.
Geological facts
Chert breaks with a very sharp edge, which made it the primary material for arrowheads and spears for thousands of years. It is essentially a non-crystalline form of quartz.
Field identification & locations
Identify by its 'flinty' waxy surface and conchoidal fracture patterns. These specimens appear to be weathered nodules collected from a gravel pit or limestone deposit.
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