
sedimentary
Tumbled brown stone, likely chert or jasper
Microcrystalline quartz (SiO₂), likely ferruginous chert/jasper
AI-generated identification · may be incorrectTypically Mohs hardness 6.5–7, opaque brown to reddish-brown, with dull to waxy luster and no visible cleavage; compact microcrystalline quartz structure. The smoothly rounded surface indicates natural water wear or tumbling.
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Physical properties
Typically Mohs hardness 6.5–7, opaque brown to reddish-brown, with dull to waxy luster and no visible cleavage; compact microcrystalline quartz structure. The smoothly rounded surface indicates natural water wear or tumbling.
Formation & geological history
Forms when silica-rich fluids replace or cement sediment, with iron oxides producing the brown-red color; exact age and locality cannot be determined from the image. Common in gravel deposits and weathered sedimentary terrains.
Uses & applications
Used as a durable lapidary material for cabochons, carvings, beads, and decorative stones; less commonly used as aggregate. Its value is mainly ornamental.
Geological facts
Chert and jasper are varieties of microcrystalline quartz; jasper is generally opaque and impurity-rich, while chert may be gray, brown, or multicolored. The specimen could also be another iron-stained quartz-rich pebble.
Field identification & locations
Identify by its glassy-to-waxy appearance, exceptional resistance to scratching, and inability to scratch with a steel nail easily; a streak, hardness, and specific-gravity test would help distinguish it from ordinary sandstone or slag. Found worldwide, especially in river gravels.
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