Rock Identifier
Ironstone concretion (likely limonite/goethite-rich) (Iron-oxide/oxyhydroxide-rich concretion, chiefly goethite (FeO(OH)) and limonite; identification from the photo is provisional) — sedimentary
sedimentary

Ironstone concretion (likely limonite/goethite-rich)

Iron-oxide/oxyhydroxide-rich concretion, chiefly goethite (FeO(OH)) and limonite; identification from the photo is provisional

AI-generated identification · may be incorrect

Ochre-brown, earthy to dull luster, irregular knobbly surface; commonly about 4–6 Mohs hardness, with no obvious cleavage. The image does not show enough detail to determine crystal structure or confirm composition.

Identified More sedimentary →
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Physical properties

Ochre-brown, earthy to dull luster, irregular knobbly surface; commonly about 4–6 Mohs hardness, with no obvious cleavage. The image does not show enough detail to determine crystal structure or confirm composition.

Formation & geological history

Iron oxides precipitate and cement sediment around a nucleus, forming a concretion during or after burial; such deposits occur across many geological ages and sedimentary settings.

Uses & applications

Commonly collected as a geological specimen; iron-rich material has historically served as iron ore and earthy pigment, though this piece’s grade is unknown.

Geological facts

Goethite and related iron oxides produce yellow, brown, and reddish colors in soils and rocks.

Field identification & locations

Look for a heavy-feeling, rusty-brown specimen that may leave an ochre streak; confirm with a streak test and mineralogical analysis. Ironstone occurs widely in sedimentary basins worldwide.