
sedimentary
Chert (Flint)
Microcrystalline Quartz (SiO2)
Hardness: 7 on Mohs scale; Color: typically tan, brown, or gray; Luster: waxy to dull; Crystal structure: cryptocrystalline; Cleavage: none, exhibits conchoidal fracture; Specific gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- typically tan, brown, or gray
- Luster
- waxy to dull
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Physical properties
Hardness: 7 on Mohs scale; Color: typically tan, brown, or gray; Luster: waxy to dull; Crystal structure: cryptocrystalline; Cleavage: none, exhibits conchoidal fracture; Specific gravity: 2.65.
Formation & geological history
Formed through the accumulation of silica-rich organic remains or chemical precipitation in sedimentary environments such as limestone or chalk beds. Often Cretaceous or Jurassic in age.
Uses & applications
Historically used for stone tools and weapons due to its ability to hold a sharp edge. Modernly used in construction aggregate and as a fire-starter (flint).
Geological facts
Flint was one of the most important resources for prehistoric humans to create arrowheads and knives. It produces sparks when struck against steel, which revolutionized fire-making.
Field identification & locations
Identify by its glassy, waxy texture and sharp, shell-like (conchoidal) breaks. Often found as nodules within limestone or along riverbeds and beaches.
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