
sedimentary
Chert (Red/Pink variety)
Microcrystalline quartz (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs scale), Color: Reddish-brown to pink due to iron oxide impurities, Luster: Waxy to dull, Crystal structure: Microcrystalline/Cryptocrystalline, Cleavage: None (conchoidal fracture), Specific gravity: 2.6-2.7
- Hardness
- 6
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Physical properties
Hardness: 6.5-7 (Mohs scale), Color: Reddish-brown to pink due to iron oxide impurities, Luster: Waxy to dull, Crystal structure: Microcrystalline/Cryptocrystalline, Cleavage: None (conchoidal fracture), Specific gravity: 2.6-2.7
Formation & geological history
Formed through the accumulation of silica-rich organic remains (like radiolarians) or inorganic precipitation from groundwater in sedimentary environments. Can date from various geological periods, often Precambrian to Cenozoic.
Uses & applications
Historically used for stone tools and arrowheads because it fractures like glass. Modernly used in landscaping, as an abrasive, and sometimes in jewelry (as Jasper) when highly polished.
Geological facts
Chert is so hard it can spark when struck against steel. Prehistoric humans traded high-quality chert over hundreds of miles to create specialized tools.
Field identification & locations
Identify in the field by its very smooth, shell-like (conchoidal) fracture surfaces and its ability to scratch glass easily. Commonly found as nodules in limestone or as distinct bedded layers.
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