
sedimentary
Chert (and associated Sedimentary rocks)
Microcrystalline Silica (SiO2)
Hardness: 7 on Mohs scale; Color: Gray, tan, brown, or black; Luster: Waxy to dull; Crystal structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Gray, tan, brown, or black
- Luster
- Waxy to dull
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Physical properties
Hardness: 7 on Mohs scale; Color: Gray, tan, brown, or black; Luster: Waxy to dull; Crystal structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
Formation & geological history
Formed through the accumulation of siliceous remains of marine organisms (like diatoms or radiolarians) or by the chemical replacement of limestone/dolomite by silica-rich fluids. Usually found in Phanerozoic age strata.
Uses & applications
Historically used for stone tools (arrowheads, scrapers) due to sharp edges; currently used for road base, decorative landscaping, and as a raw material for silicon-based products.
Geological facts
Chert is so hard it can scratch glass and steel. Flint is a high-quality variety of chert. It has been used by humans for millions of years to start fires and create weaponry.
Field identification & locations
Identify in the field by its very hard surface, waxy texture, and distinctive 'shell-like' shell-like (conchoidal) fractures. Often found in nodules within limestone layers or as river pebbles.
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