
sedimentary
Chert (Flint)
Silicon Dioxide (SiO2)
Hardness: 6.5-7 Mohs. Color: Black to dark grey. Luster: Waxy to vitreous. Structure: Microcrystalline/Cryptocrystalline. Cleavage: None (conchoidal fracture). Specific Gravity: 2.58-2.91.
- Hardness
- 6
- Color
- Black to dark grey
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 Mohs. Color: Black to dark grey. Luster: Waxy to vitreous. Structure: Microcrystalline/Cryptocrystalline. Cleavage: None (conchoidal fracture). Specific Gravity: 2.58-2.91.
Formation & geological history
Formed by the precipitation of silica in sedimentary environments, often replacing organic material or filling cavities in limestone/chalk. Found in nodules or bedded deposits throughout the geologic record from the Precambrian to Cenozoic.
Uses & applications
Historically used for stone tools (knapping) and starting fires (flint and steel). Modern uses include gemstones (jasper/agate varieties), road surfacing, and industrial grinding media.
Geological facts
Flint was one of the most important resources for prehistoric humans due to its ability to break into sharp edges. It is chemically identical to quartz but has a different internal crystal structure.
Field identification & locations
Identify by its 'shell-like' conchoidal fracture, waxy feel, and ability to scratch glass. Often found in chalk cliffs or as nodules in limestone fields.
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