
sedimentary
Chert (Flint)
Microcrystalline or Cryptocrystalline Quartz (SiO2)
Hardness: 7 on Mohs scale; Color: Gray, brown, tan, or black; Luster: Waxy to dull; Crystal structure: Trigonal (microscopic); Cleavage: None (conchoidal fracture); Specific gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Gray, brown, tan, or black
- Luster
- Waxy to dull
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Physical properties
Hardness: 7 on Mohs scale; Color: Gray, brown, tan, or black; Luster: Waxy to dull; Crystal structure: Trigonal (microscopic); Cleavage: None (conchoidal fracture); Specific gravity: 2.65
Formation & geological history
Formed through the accumulation of siliceous remains of marine organisms (like diatoms or radiolaria) or via chemical precipitation from silica-rich fluids in limestone or chalk beds. Often found in nodules or bedded layers.
Uses & applications
Historically used for stone tools (arrowheads). Modernly used as road aggregate, in jewelry (when decorative like jasper), and as a spark-maker in survival fire-starting kits.
Geological facts
Chert has a conchoidal fracture, allowing it to break into razor-sharp edges. It was one of the most vital materials for early human technological development.
Field identification & locations
Identify in the field by its waxy texture and shell-like (conchoidal) curved breaks. It will easily scratch glass and produce sparks when struck against steel. Commonly found in limestone outcrops or riverbeds.
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