
sedimentary
Chert (Flint)
Chert (Cryptocrystalline variety of Quartz, SiO2)
Hardness: 7 (Mohs scale); Color: Tan, brown, gray, and cream with waxy luster; Crystal Structure: Microcrystalline/Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
- Hardness
- 7 (Mohs scale)
- Color
- Tan, brown, gray, and cream with waxy luster
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Physical properties
Hardness: 7 (Mohs scale); Color: Tan, brown, gray, and cream with waxy luster; Crystal Structure: Microcrystalline/Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
Formation & geological history
Formed through the accumulation of silica-rich organic remains (like diatoms or radiolarians) or chemical precipitation from silica-rich fluids. Generally found in marine limestone or dolomite beds as nodules or layers. Can range from Precambrian to Recent geological periods.
Uses & applications
Historically used for stone tools and weapons (arrowheads). Modernly used in road construction, as a source for silica in glassmaking, and by survivalists for fire-starting.
Geological facts
Because of its conchoidal fracture, it can be knapped to create edges sharper than a steel scalpel. Native Americans and many ancient cultures traded high-quality chert over thousands of miles.
Field identification & locations
Identify in the field by its very hard, smooth surface that cannot be scratched by steel and its sharp, shell-like (conchoidal) breaks. Often found as hard nodules protruding from softer limestone cliffs.
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