
sedimentary
Chert (Flint)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 (Mohs scale); Color: dark gray, black, or bluish-gray; Luster: waxy to dull; Crystal structure: Cryptocrystalline (microscopic quartz); Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
- Hardness
- 7 (Mohs scale)
- Color
- dark gray, black, or bluish-gray
- Luster
- waxy to dull
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Physical properties
Hardness: 7 (Mohs scale); Color: dark gray, black, or bluish-gray; Luster: waxy to dull; Crystal structure: Cryptocrystalline (microscopic quartz); Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
Formation & geological history
Formed through the accumulation of silica-rich organic remains (like radiolarians or diatoms) or by chemical precipitation from silica-rich fluids within limestone or chalk beds.
Uses & applications
Historically used for stone tools (arrowheads, scrapers) due to its sharp edges; modern uses include construction aggregate, gemstones, and fire-starting kits.
Geological facts
Flint was one of the first materials used by early humans to create fire and sharp tools. It is extremely durable and weather-resistant, often surviving long after the surrounding limestone has eroded.
Field identification & locations
Identify in the field by its smooth, shell-like (conchoidal) fracture surfaces and its ability to scratch glass. It is common in limestone regions like the central US, UK, and France.
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