
sedimentary
Likely ironstone or ferruginous sandstone fragment
Iron-oxide-cemented sandstone; commonly quartz grains cemented by hematite/goethite (composition cannot be confirmed from the image)
AI-generated identification · may be incorrectReddish-brown, dull to slightly earthy surface with irregular fracture; likely Mohs 5–7 depending on cement and grain content. Crystal structure and specific gravity cannot be determined visually; it appears non-crystalline at this scale.
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Physical properties
Reddish-brown, dull to slightly earthy surface with irregular fracture; likely Mohs 5–7 depending on cement and grain content. Crystal structure and specific gravity cannot be determined visually; it appears non-crystalline at this scale.
Formation & geological history
Probably formed when iron oxides cemented sand or accumulated as an iron-rich sediment, then lithified. Its age and precise formation setting cannot be determined from the photograph.
Uses & applications
Commonly used as building or landscaping stone when present in larger deposits; this small fragment has mainly educational or modest display value.
Geological facts
Iron oxides produce the characteristic rusty red-brown color and may stain nearby surfaces.
Field identification & locations
Look for gritty sand grains, rusty coloration, and a hard, irregular break; a fresh surface or simple hardness and streak tests would help confirm it. Ferruginous sandstones occur worldwide.
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