
sedimentary
Tumbled red-brown chert or jasper
Microcrystalline quartz (SiO₂), likely iron-stained chert/jasper
AI-generated identification · may be incorrectHardness about 6.5–7 Mohs; reddish-brown, opaque, with a smooth tumbled surface and dull to waxy luster. It has cryptocrystalline quartz structure, no obvious cleavage, and typically specific gravity near 2.6.
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Physical properties
Hardness about 6.5–7 Mohs; reddish-brown, opaque, with a smooth tumbled surface and dull to waxy luster. It has cryptocrystalline quartz structure, no obvious cleavage, and typically specific gravity near 2.6.
Formation & geological history
Forms when silica-rich fluids replace or cement sediment, often with iron oxides producing the red color; commonly Paleozoic or younger, depending on locality. The rounded form is human-tumbled or naturally water-worn.
Uses & applications
Used as ornamental stone, cabochons, beads, carvings, lapidary material, and occasionally as a durable aggregate. It has modest collector value unless unusually patterned or locality-specific.
Geological facts
Jasper is technically an opaque, impure variety of microcrystalline quartz, while chert is commonly more uniform and gray or brown; the boundary between them is gradual.
Field identification & locations
Identify it by its opaque red-brown body, very fine texture, waxy luster, and inability to scratch with a steel knife easily; it should scratch glass. Common in gravel beds and silica-rich sedimentary formations worldwide.
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