sedimentary
Chert (Jasper/Flint variety)
Microcrystalline or Cryptocrystalline Quartz (SiO2)
Hardness: 7 on Mohs scale; Color: typically grey, brown, or tan; Luster: waxy to dull; Crystal structure: hexagonal (microscopic); Cleavage: none (conchoidal fracture); Specific Gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- typically grey, brown, or tan
- Luster
- waxy to dull
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Physical properties
Hardness: 7 on Mohs scale; Color: typically grey, brown, or tan; Luster: waxy to dull; Crystal structure: hexagonal (microscopic); Cleavage: none (conchoidal fracture); Specific Gravity: 2.65.
Formation & geological history
Formed through the accumulation of silica-rich organic remains (like radiolarians or sponges) on the ocean floor, which later undergoes diagenesis and replaces host rock material, commonly found in limestone or dolomite beds.
Uses & applications
Historically used for stone tools and weapons due to its sharp edges when broken. Currently used as road aggregate, in landscaping, and some colorful varieties (Jasper) are used for jewelry and lapidary art.
Geological facts
Chert was used by prehistoric humans to create 'knapped' points. When struck against steel, it can create sparks, making it a primary component in flintlock firearms and primitive fire-starting kits.
Field identification & locations
Identify by its waxy texture and characteristic shell-like (conchoidal) fracture pattern. It feels very smooth to the touch and cannot be scratched by a steel knife. Commonly found in riverbeds and limestone outcrops.
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