
sedimentary
Polished banded chert
Chert (microcrystalline quartz, SiO₂), likely banded jasper/chert
AI-generated identification · may be incorrectHardness about 6.5–7 Mohs; dark gray to black with thin pale and rusty-brown bands, waxy to dull luster, very fine-grained cryptocrystalline structure, and conchoidal fracture. The rounded shape is polished or tumbled.
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Physical properties
Hardness about 6.5–7 Mohs; dark gray to black with thin pale and rusty-brown bands, waxy to dull luster, very fine-grained cryptocrystalline structure, and conchoidal fracture. The rounded shape is polished or tumbled.
Formation & geological history
Forms when silica-rich fluids replace or precipitate within sediment, commonly from microscopic marine organisms; individual layers may be Precambrian to much younger. Brown bands likely contain iron oxides or other impurities.
Uses & applications
Used for ornamental stones, cabochons, carvings, and decorative objects; historically, chert was an important material for tools and projectile points.
Geological facts
Chert can resemble flint, but “flint” commonly refers to dark chert associated with chalk. Its hardness allows it to scratch ordinary glass.
Field identification & locations
Identify by its glassy/waxy appearance, fine texture, lack of visible crystals, and conchoidal fracture; acid produces no fizz. Common in sedimentary formations worldwide, including the Great Lakes, Texas, England, and Australia.
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