
sedimentary
Weathered iron-rich sandstone or ferruginous siltstone
Clastic sedimentary rock, likely quartz-rich sandstone cemented by iron oxides (Fe₂O₃/Fe₃O₄)
AI-generated identification · may be incorrectHardness about 5–7; brown to reddish-brown, dull earthy luster, very fine to medium clastic texture, and no visible cleavage. The elongated, rounded shape appears naturally weathered or water-worn; exact identification requires a fresh surface and grain inspection.
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Physical properties
Hardness about 5–7; brown to reddish-brown, dull earthy luster, very fine to medium clastic texture, and no visible cleavage. The elongated, rounded shape appears naturally weathered or water-worn; exact identification requires a fresh surface and grain inspection.
Formation & geological history
Formed from compacted and cemented sand or silt, with iron-bearing groundwater producing the rusty coloration; age cannot be determined from the image. Such rocks form in terrestrial, river, floodplain, or shallow-marine sedimentary environments.
Uses & applications
Common ferruginous sandstone is used as building stone, paving, aggregate, and landscaping material; this individual piece has mainly decorative or educational value.
Geological facts
Iron oxides can strongly stain sandstone red, orange, or brown. Its smooth, flattened form may reflect prolonged stream abrasion or weathering along natural bedding planes.
Field identification & locations
Look for visible quartz grains, gritty texture, sedimentary layering, and a reddish streak or iron staining; a steel nail may scratch softer varieties. Common worldwide, especially in iron-rich sedimentary basins.
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