Rock Identifier
Iron-rich concretion or weathered ironstone (Goethite–hematite-bearing ironstone; identification is uncertain from appearance alone) — sedimentary
sedimentary

Iron-rich concretion or weathered ironstone

Goethite–hematite-bearing ironstone; identification is uncertain from appearance alone

AI-generated identification · may be incorrect

Rusty red-brown, earthy to dull luster, irregular porous texture, and rounded water-worn shape; likely hardness about 4–6 Mohs, with variable density and weak or absent cleavage. Dark patches may be manganese oxides or concentrated iron minerals.

Identified More sedimentary
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Physical properties

Rusty red-brown, earthy to dull luster, irregular porous texture, and rounded water-worn shape; likely hardness about 4–6 Mohs, with variable density and weak or absent cleavage. Dark patches may be manganese oxides or concentrated iron minerals.

Formation & geological history

Formed by precipitation and cementation of iron oxides/hydroxides in sediment, soil, or weathering zones; commonly Cenozoic to recent, though ironstone can occur at many geological ages.

Uses & applications

Used as iron ore when sufficiently concentrated and historically as a red-brown pigment; otherwise mainly a teaching or collecting specimen, typically with little commercial value.

Geological facts

The red color generally reflects hematite or iron-rich clay, while yellow-brown components may be goethite or limonite. A streak test is more diagnostic than surface color.

Field identification & locations

Common in lateritic soils, river gravels, deserts, and sedimentary ironstone beds worldwide. Test an inconspicuous area: hematite gives a red to reddish-brown streak; goethite gives yellow-brown, and a magnet may detect associated magnetite.