
sedimentary
Weathered iron-rich river pebble
Ferruginous chert or iron-stained jasper (cryptocrystalline SiO₂ with iron oxides)
AI-generated identification · may be incorrectTypically hardness 6.5–7, opaque rusty orange-brown with black to gray veins, and dull to waxy luster; lacks visible crystals and has no obvious cleavage. The rounded shape and smooth surface indicate water abrasion or tumbling.
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Physical properties
Typically hardness 6.5–7, opaque rusty orange-brown with black to gray veins, and dull to waxy luster; lacks visible crystals and has no obvious cleavage. The rounded shape and smooth surface indicate water abrasion or tumbling.
Formation & geological history
Likely formed from silica-rich chert/jasper later stained or cemented by hematite and goethite during weathering, then transported in a stream or glacial deposit. Exact age and locality cannot be determined from the image.
Uses & applications
Used mainly as a lapidary, landscaping, or collectible stone; attractive pieces may be polished for cabochons or decorative objects, but this specimen appears modestly ornamental.
Geological facts
Iron oxides produce the orange-red coloration, while dark zones may be manganese oxides, magnetite, or inclusions. A polished surface and strong conchoidal fracture would support a chert/jasper identification.
Field identification & locations
Common in iron-rich gravels and weathered volcanic or sedimentary terrains worldwide. Test for glassy/conchoidal fracture and hardness sufficient to scratch ordinary glass; a streak test may show a reddish-brown powder.
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