
sedimentary
Chert (Jasper/Flint variety)
Microcrystalline Quartz (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs). Color: Dark brown to blackish with olive/yellow undertones. Luster: Dull to waxy. Crystal Structure: Trigonal/Cryptocrystalline. Cleavage: None (conchoidal fracture). Specific Gravity: Approximately 2.65.
- Hardness
- 6
- Color
- Dark brown to blackish with olive/yellow undertones
- Luster
- Dull to waxy
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Physical properties
Hardness: 6.5-7 (Mohs). Color: Dark brown to blackish with olive/yellow undertones. Luster: Dull to waxy. Crystal Structure: Trigonal/Cryptocrystalline. Cleavage: None (conchoidal fracture). Specific Gravity: Approximately 2.65.
Formation & geological history
Formed through the accumulation of silica-rich microfossils (like radiolarians) or by the precipitation of silica from groundwater replacing organic matter. Often associated with limestone/chalk beds or river gravels; can range from Precambrian to Cenozoic in age.
Uses & applications
Historically used for stone tools (arrowheads/knapping) due to sharp edges; used today as a decorative landscape stone, abrasive, or in the manufacturing of glass and ceramics.
Geological facts
Chert is so hard it can strike sparks from steel, which led to the name 'flint' being used for lighting fires and early firearms. It is incredibly durable and can survive millions of years in riverbeds.
Field identification & locations
Identify in the field by its smooth, waxy feel and shell-like (conchoidal) fracture when broken. It cannot be scratched by a steel knife. Common in riverbanks and limestone outcroppings.
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