
sedimentary
Chert (Jasper variety)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 on Mohs scale; Color: Tan, brown, or yellowish; Luster: Waxy to dull; Crystal structure: Microcrystalline/Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.6-2.7.
- Hardness
- 6
- Color
- Tan, brown, or yellowish
- Luster
- Waxy to dull
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: Tan, brown, or yellowish; Luster: Waxy to dull; Crystal structure: Microcrystalline/Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.6-2.7.
Formation & geological history
Formed from the accumulation of silica-rich organic remains (like diatoms or radiolarians) or through the replacement of limestone. It typically forms in marine sedimentary environments during various geological eras from Precambrian to Cenozoic.
Uses & applications
Historically used for stone tools (arrowheads). Modernly used in landscaping, as a gemstone (Jasper), and as a component in construction aggregate.
Geological facts
Chert is so hard it can scratch steel and produce sparks when struck against iron; it was one of the primary materials used by prehistoric humans for tool making due to its predictable fracturing pattern.
Field identification & locations
Identify by its 'flint-like' waxy appearance and smooth, shell-like (conchoidal) breaks. This specimen appears as water-worn gravel, commonly found in riverbeds and glacial deposits. For collectors, look for uniform color or interesting patterns.
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