
sedimentary
Chert (or Jasper)
Microcrystalline Quartz (SiO2)
AI-generated identification · may be incorrectHardness: 7 Mohs scale; Color: Cream, tan, and reddish-orange (iron-stained); Luster: Waxy to dull; Crystal structure: Trigonal/Microcrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 Mohs scale
- Color
- Cream, tan, and reddish-orange (iron-stained)
- Luster
- Waxy to dull
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Physical properties
Hardness: 7 Mohs scale; Color: Cream, tan, and reddish-orange (iron-stained); Luster: Waxy to dull; Crystal structure: Trigonal/Microcrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed by the precipitation of silica from groundwater or as a replaces of biological materials like limestone/chalk. Often found in nodules within sedimentary rock beds; age varies from Precambrian to Cenozoic.
Uses & applications
Historically used for stone tools (arrowheads). Modern uses include landscaping, as a construction aggregate, and occasionally as semi-precious gemstones in jewelry (when decorative like jasper).
Geological facts
Chert has been used by humans for millions of years to create sharp-edged tools because of its conchoidal fracture pattern, which produces edges sharper than a steel scalpel.
Field identification & locations
Identify by its smooth, waxy surface and the way it breaks into curved, shell-like flakes. It will easily scratch glass and cannot be scratched by a steel knife. Found globally in limestone areas.
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