
sedimentary
Chert (specifically Flint or Jasper variant)
Microcrystalline or Cryptocrystalline Silicon Dioxide (SiO2)
Hardness: 7 (Mohs scale); Color: Variegated brown, tan, and creamy white cortex; Luster: Waxy to dull; Crystal structure: Trigonal (microscopic); Cleavage: None (conchoidal fracture); Specific gravity: 2.6-2.7
- Hardness
- 7 (Mohs scale)
- Color
- Variegated brown, tan, and creamy white cortex
- Luster
- Waxy to dull
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Physical properties
Hardness: 7 (Mohs scale); Color: Variegated brown, tan, and creamy white cortex; Luster: Waxy to dull; Crystal structure: Trigonal (microscopic); Cleavage: None (conchoidal fracture); Specific gravity: 2.6-2.7
Formation & geological history
Formed through the accumulation of silica-rich organic remains (like radiolarians or diatoms) or chemical precipitation from hydrothermal fluids in sedimentary basins. Often found as nodules within limestone or chalk beds.
Uses & applications
Historically used for stone tools/weapons (knapping) and fire-starting. Industrially used in construction aggregates; aesthetically used for lapidary work, cabochons, and decorative landscaping.
Geological facts
Chert was one of the most vital materials for early humans due to its ability to fracture into razor-sharp edges. It is extremely resistant to chemical weathering, which is why it often remains as 'river rocks' long after the surrounding limestone has eroded.
Field identification & locations
Identify in the field by its smooth, shell-like (conchoidal) fracture surfaces and its ability to scratch glass. Commonly found in riverbeds, glacial tills, and chalk cliffs. Collectors look for unique color patterns and translucency.
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