
sedimentary
Chert (Jasper/Flint variety)
Microcrystalline quartz (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 on Mohs scale. Color: Tan, brown, and yellowish-orange. Luster: Dull to waxy. Crystal structure: Trigonal (microcrystalline/cryptocrystalline). Cleavage: None, exhibits conchoidal (shell-like) fracture. Specific gravity: 2.65.
- Hardness
- 6
- Color
- Tan, brown, and yellowish-orange
- Luster
- Dull to waxy
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Physical properties
Hardness: 6.5-7 on Mohs scale. Color: Tan, brown, and yellowish-orange. Luster: Dull to waxy. Crystal structure: Trigonal (microcrystalline/cryptocrystalline). Cleavage: None, exhibits conchoidal (shell-like) fracture. Specific gravity: 2.65.
Formation & geological history
Formed through the accumulation of silica-rich organic remains (like diatoms or radiolarians) or the chemical precipitation of silica in groundwater. Can be found in various geological ages, often replacing limestone or dolostone through chemical substitution.
Uses & applications
Historically used for stone tools (knapping) due to its sharp edges when broken. Today used in construction aggregate, road surfacing, jewelry (as Jasper varieties), and as a collector's item.
Geological facts
Chert is so hard that it will spark when struck against steel, which is why the 'Flint' variety was critical for early firearms and fire-starting tools. It is also highly resistant to chemical weathering.
Field identification & locations
Identify in the field by its smooth, waxy feel, extreme hardness (it will scratch glass), and the way it breaks into curved, sharp fragments. Common in riverbeds and limestone outcrops.
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