sedimentary
Chert (variations include Flint or Jasper)
Microcrystalline or Cryptocrystalline Quartz (SiO2)
Hardness: 6.5-7 on Mohs scale; Color: typically gray, brown, tan, or green; Luster: waxy to dull; Crystal structure: trigonal (microscopic); Cleavage: none, exhibits conchoidal fracture.
- Hardness
- 6
- Color
- typically gray, brown, tan, or green
- Luster
- waxy to dull
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: typically gray, brown, tan, or green; Luster: waxy to dull; Crystal structure: trigonal (microscopic); Cleavage: none, exhibits conchoidal fracture.
Formation & geological history
Formed through the precipitation of silica-rich fluids in marine environments or the accumulation of silica-based skeletal remains of organisms like diatoms and radiolarians. Common in ancient limestone and chalk beds.
Uses & applications
Historically used for stone tools (arrowheads, knives) due to its sharp edges; used today as road gravel, in concrete, and some colorful varieties (Jasper) are used in jewelry.
Geological facts
Chert was one of the most important minerals for early humans because its conchoidal fracture pattern allows it to be worked into extremely sharp blades.
Field identification & locations
Identify in the field by its very hard surface (scratches glass), waxy luster when freshly broken, and smooth, shell-like (conchoidal) fracture surfaces. Commonly found as nodules in limestone outcrops.
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