
sedimentary
Chert with Quartz Veining
Microcrystalline Quartz (SiO2)
Hardness: 7 (Mohs scale), Color: Dark grey to black with white quartz veins and some iron oxidation (orange/brown), Luster: Dull to waxy, Crystal structure: Cryptocrystalline, Fracture: Conchoidal to irregular
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Physical properties
Hardness: 7 (Mohs scale), Color: Dark grey to black with white quartz veins and some iron oxidation (orange/brown), Luster: Dull to waxy, Crystal structure: Cryptocrystalline, Fracture: Conchoidal to irregular
Formation & geological history
Formed by the accumulation of siliceous remains of marine organisms or via chemical precipitation from silica-rich fluids in sedimentary basins. The white veins are later-stage quartz filled fractures.
Uses & applications
Historically used for making stone tools due to its conchoidal fracture. Modern uses include abrasives and road surfacing material.
Geological facts
Chert is essentially a dense form of quartz. It was highly prized by indigenous cultures globally for crafting arrowheads, knives, and scrapers because it produces a very sharp edge.
Field identification & locations
Identify in the field by its high hardness (it will scratch glass) and smooth, shell-like fracture surfaces. Often found as nodules or lenses within limestone formations.
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