
sedimentary
Chert (Flint)
Chert (Silicon Dioxide, SiO2)
Hardness: 6.5-7 Mohs; Color: Tan, brown, white with iron staining; Luster: Waxy to dull; Crystal structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.6
- Hardness
- 6
- Color
- Tan, brown, white with iron staining
- Luster
- Waxy to dull
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Physical properties
Hardness: 6.5-7 Mohs; Color: Tan, brown, white with iron staining; Luster: Waxy to dull; Crystal structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.6
Formation & geological history
Formed primarily from the accumulation of silica-rich organic remains such as radiolaria or diatoms in marine environments, or via chemical precipitation within limestone/chalk beds during the Phanerozoic eon.
Uses & applications
Historically used for stone tools (arrowheads, knives) due to sharp edges; currently used for road ballast, industrial abrasives, and as a decorative stone in collecting.
Geological facts
Chert has been crucial to human evolution; it was one of the first materials used to create specialized tools and to spark fires. It is so tough it can often scratch steel.
Field identification & locations
Identify by its waxy luster, extreme hardness, and distinctive shell-like (conchoidal) fracture pattern. Commonly found in riverbeds or weathered out of limestone formations.
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