
sedimentary
Chert
Silicon Dioxide (Microcrystalline Quartz, $SiO_2$)
Hardness: 7 on the Mohs scale. Color: Varies widely from white, grey, and black to brown, red, or green. Luster: Vitreous to dull or waxy. Crystal structure: Microcrystalline or cryptocrystalline quartz (chalcedony/quartz aggregates). Cleavage: None, exhibits conchoidal fracture. Specific gravity: 2.60 to 2.65.
- Hardness
- 7 on the Mohs scale
- Luster
- Vitreous to dull or waxy
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Physical properties
Hardness: 7 on the Mohs scale. Color: Varies widely from white, grey, and black to brown, red, or green. Luster: Vitreous to dull or waxy. Crystal structure: Microcrystalline or cryptocrystalline quartz (chalcedony/quartz aggregates). Cleavage: None, exhibits conchoidal fracture. Specific gravity: 2.60 to 2.65.
Formation & geological history
Formed through chemical sedimentary processes, typically by the replacement of calcium carbonate in limestone by silica-rich solutions, or through the accumulation of microscopic siliceous skeletal remains (such as diatoms or radiolarians) in deep-marine environments over millions of years.
Uses & applications
Historically used extensively by early humans for making stone tools, arrowheads, and blades due to its sharp conchoidal fracture. Also used historically for striking fire with steel, and in modern aggregate or decorative landscaping.
Geological facts
Chert, flint, and jasper are all varieties of microcrystalline quartz. Flint is typically dark grey or black found in chalk, whereas chert is often lighter colored and found in limestone formations.
Field identification & locations
Can be identified in the field by its hard conchoidal fracture, sharp edges when broken, lack of reaction to hydrochloric acid, and hardness sufficient to scratch glass easily. Commonly found globally within limestone and chalk deposits.
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