sedimentary
Chert
Microcrystalline Quartz (SiO2)
AI-generated identification · may be incorrectHardness: 7 (Mohs scale), Color: Variegated brown, tan, and reddish, Luster: Waxy to dull, Structure: Cryptocrystalline, Cleavage: None (conchoidal fracture), Specific Gravity: 2.6-2.7
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Physical properties
Hardness: 7 (Mohs scale), Color: Variegated brown, tan, and reddish, Luster: Waxy to dull, Structure: Cryptocrystalline, Cleavage: None (conchoidal fracture), Specific Gravity: 2.6-2.7
Formation & geological history
Formed from the accumulation of siliceous remains of microscopic organisms (like diatoms or radiolarians) or through chemical precipitation in marine environments. Often found as nodules within limestone or chalk beds.
Uses & applications
Historically used for stone tools and arrowheads. Currently used as road aggregate, in glass manufacturing, and as decorative landscaping stones.
Geological facts
Because it fractures with extremely sharp edges, chert was one of the most important materials for early human technology (Stone Age tools). Variations include flint, jasper, and chalcedony.
Field identification & locations
Identify in the field by its hardness (scratches glass), waxy feel, and characteristic shell-like (conchoidal) fractures. Common in sedimentary basins worldwide.
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