
sedimentary
Chert (Jasper/Flint variety)
Microcrystalline quartz (SiO2)
Hardness: 6.5-7 Mohs; Color: Mustard yellow to brown (ochre); Luster: Dull to waxy; Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.6-2.7
- Hardness
- 6
- Color
- Mustard yellow to brown (ochre)
- Luster
- Dull to waxy
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Physical properties
Hardness: 6.5-7 Mohs; Color: Mustard yellow to brown (ochre); Luster: Dull to waxy; Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.6-2.7
Formation & geological history
Formed through the accumulation of siliceous remains of organisms or chemical precipitation from silica-rich fluids in sedimentary basins. Primarily Paleozoic to Cenozoic eras.
Uses & applications
Historically used for stone tools (knapping). Currently used as landscaping stone, road aggregate, and sometimes as a minor gemstone (Jasper) in jewelry.
Geological facts
Chert is so hard it can scratch steel and was once the primary material for making arrowheads and spear points due to its sharp conchoidal fracture edges.
Field identification & locations
Identify by its 'shell-like' curved (conchoidal) fractures and its ability to scratch glass. Commonly found in riverbeds, glacial till, or as nodules within limestone/chalk layers.
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