
sedimentary
Weathered brown iron-rich pebble
Likely ferruginous sandstone or ironstone; exact identification requires testing
AI-generated identification · may be incorrectHardness roughly 5–7 Mohs; brown to reddish-brown, earthy to dull luster, fine-grained and massive, with pale gray weathering or cement-filled areas. No visible crystal faces or cleavage; density likely moderate to high from iron minerals.
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Physical properties
Hardness roughly 5–7 Mohs; brown to reddish-brown, earthy to dull luster, fine-grained and massive, with pale gray weathering or cement-filled areas. No visible crystal faces or cleavage; density likely moderate to high from iron minerals.
Formation & geological history
Probably formed from sand or clay cemented by iron oxides, then rounded and sculpted by stream or beach transport and weathering. Its precise geological age cannot be determined from the photograph.
Uses & applications
Primarily a natural specimen or curiosity; ferruginous sandstone may be used locally as building stone or aggregate, but this small rounded piece has little industrial value.
Geological facts
The dark brown color commonly reflects hematite, goethite, or limonite coatings and cement. The irregular lobes may be natural erosion, concretionary growth, or a fragment of an iron-rich rock.
Field identification & locations
Look for a rusty streak, moderate heft, granular texture, and possible attraction to a strong magnet if magnetite is present; a steel file, streak plate, and acid test would help distinguish ironstone from basalt or slag. Common in weathered sedimentary terrains, river gravels, and beaches.
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