
sedimentary
Chert (Grey-Green Flint)
Microcrystalline silicon dioxide (SiO2)
Hardness: 6.5-7 on the Mohs scale. Color: Opaque grey or dull green. Luster: Waxy to dull. Crystal structure: Cryptocrystalline. Cleavage: None (exhibits conchoidal fracture). Specific gravity: 2.65.
- Hardness
- 6
- Color
- Opaque grey or dull green
- Luster
- Waxy to dull
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Physical properties
Hardness: 6.5-7 on the Mohs scale. Color: Opaque grey or dull green. Luster: Waxy to dull. Crystal structure: Cryptocrystalline. Cleavage: None (exhibits conchoidal fracture). Specific gravity: 2.65.
Formation & geological history
Formed from the chemical precipitation of silica-rich fluids or the accumulation of microscopic skeletal remains of silica-secreting organisms (like diatoms or radiolarians) in marine environments. It is often found as nodules in limestone or chalk beds. Geological age ranges from Precambrian to Cenozoic.
Uses & applications
Historically used for making stone tools (arrowheads, scrapers) due to its sharp edges when fractured. Modern uses include road surfacing, jewelry (when polished), and as a raw material for silicon production.
Geological facts
Chert has a unique property where it produces sparks when struck against steel, which made it essential for early firearms (flintlocks) and fire-starting. It is incredibly durable and chemically stable, often surviving billions of years of weathering.
Field identification & locations
Identify in the field by its characteristic shell-like (conchoidal) fracture pattern and its ability to scratch glass. It often feels smooth or waxy. Common in riverbeds, glacial deposits, and embedded in sedimentary rock layers.
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