
sedimentary
Chert (Flint)
Microcrystalline Quartz (SiO2)
Hardness: 7 on Mohs scale; Color: Cream, tan, gray; Luster: Waxy to dull; Crystal structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Cream, tan, gray
- Luster
- Waxy to dull
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Physical properties
Hardness: 7 on Mohs scale; Color: Cream, tan, gray; Luster: Waxy to dull; Crystal structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
Formation & geological history
Formed from the accumulation of siliceous remains of marine organisms or through chemical precipitation of silica-rich fluids in limestone or chalk beds. Commonly found in sedimentary basins worldwide.
Uses & applications
Historically used for stone tools and fire-starting. Currently used in road construction, as an abrasive, and for knapped decorative items.
Geological facts
Chert has a conchoidal fracture which creates razor-sharp edges, making it the primary material for prehistoric arrowheads and spear tips. It is also sparks when struck against steel.
Field identification & locations
Identify by its smooth, waxy feel and shell-like (conchoidal) breakage patterns. It is much harder than steel and cannot be scratched by a knife. Often found as nodules within limestone.
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