
sedimentary
Chert (Jasper/Jasperoid)
Chert (chemically precipitated microcrystalline Quartz, SiO2)
AI-generated identification · may be incorrectHardness: 6.5–7 (Mohs); Color: Dark brown to black with tan/yellowish streaks; Luster: Waxy to dull (on weathered surfaces); Crystal structure: Cryptocrystalline; Cleavage: None (Conchoidal fracture); Specific gravity: 2.6–2.7
- Hardness
- 6
- Color
- Dark brown to black with tan/yellowish streaks
- Luster
- Waxy to dull (on weathered surfaces)
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Physical properties
Hardness: 6.5–7 (Mohs); Color: Dark brown to black with tan/yellowish streaks; Luster: Waxy to dull (on weathered surfaces); Crystal structure: Cryptocrystalline; Cleavage: None (Conchoidal fracture); Specific gravity: 2.6–2.7
Formation & geological history
Formed through the accumulation of silica-rich organic remains (like radiolaria) or chemical precipitation from hydrothermal fluids in sedimentary environments. Its age can range from Precambrian to Cenozoic.
Uses & applications
Historically used for stone tools (flintknapping); currently used in landscaping, as a gemstone (when colorful labels like Jasper are applied), and in concrete aggregate.
Geological facts
Chert is so hard it can scratch glass and steel. It was one of the most important commodities in human prehistory because it breaks into razor-sharp edges used for arrows and knives.
Field identification & locations
Identify by its waxy luster, extreme hardness, and 'smooth' curved fractures. Common in riverbeds as rounded pebbles or as nodules within limestone or shale layers.
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