Rock Identifier
Likely ironstone or ferruginous sandstone fragment (Iron-oxide-cemented sandstone; commonly quartz grains cemented by hematite/goethite (composition cannot be confirmed from the image)) — sedimentary
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 incorrect

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.

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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.