
sedimentary
Ironstone concretion (possibly limonite/goethite-bearing)
Limonite, a mixture of hydrated iron oxides, commonly including goethite (α-FeO(OH))
AI-generated identification · may be incorrectSmall, irregular, dark brown to black specimen with rusty yellow-brown patches and a dull to locally shiny luster. Likely Mohs hardness about 4–5.5; exact composition and properties cannot be confirmed from the image.
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Physical properties
Small, irregular, dark brown to black specimen with rusty yellow-brown patches and a dull to locally shiny luster. Likely Mohs hardness about 4–5.5; exact composition and properties cannot be confirmed from the image.
Formation & geological history
Iron-rich minerals can precipitate or accumulate in sediments and weathering zones, forming ironstone concretions. Such deposits occur across many geological ages and environments.
Uses & applications
Ironstone is generally collected as a curiosity; iron-rich material has also been used as low-grade iron ore and pigment.
Geological facts
“Limonite” is a field term for a mixture of hydrated iron oxides rather than one mineral with a fixed formula.
Field identification & locations
Look for rusty brown or ochre staining, relatively high heft, and an earthy or botryoidal surface; these traits are not diagnostic, and a close examination or simple tests would help distinguish it from slag or other iron minerals. Ironstone is widespread in sedimentary rocks and weathered soils.
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