
sedimentary
Chert (Flint)
Chert (SiO2)
Hardness: 7 (Mohs scale); Color: Gray, black, brown, or tan; Luster: Waxy to dull; Crystal structure: Cryptocrystalline (microscopic quartz); Cleavage: None (conchoidal fracture); Specific gravity: 2.65
- Hardness
- 7 (Mohs scale)
- Color
- Gray, black, brown, or tan
- Luster
- Waxy to dull
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Physical properties
Hardness: 7 (Mohs scale); Color: Gray, black, brown, or tan; 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 or chemical precipitation in marine or groundwater environments. Often found as nodules in limestone or chalk beds.
Uses & applications
Historically used for stone tools and weapons (arrowheads). Modern uses include road construction aggregate, fire-starting flint, and occasionally as semi-precious gemstones (jaspers).
Geological facts
Flint is a variety of chert that was essential to human survival in the Stone Age due to its ability to produce a sharp edge when fractured and create sparks when struck against steel.
Field identification & locations
Identified in the field by its smooth, waxy surface and distinctive shell-like (conchoidal) fracture patterns. Look for it in sedimentary outcrops or as rounded pebbles in stream beds.
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