Rock Identifier
Weathered iron-rich rock, possibly laterite or limonite-bearing sandstone (Laterite/limonite mixture; primarily hydrated iron oxides such as goethite (FeO(OH)) and iron-rich clay minerals) — sedimentary
sedimentary

Weathered iron-rich rock, possibly laterite or limonite-bearing sandstone

Laterite/limonite mixture; primarily hydrated iron oxides such as goethite (FeO(OH)) and iron-rich clay minerals

AI-generated identification · may be incorrect

Brown to ochre, earthy to dull luster, porous and strongly weathered, with no visible crystal faces; estimated Mohs hardness 3–6 depending on cementation, and typically moderate specific gravity (about 2.5–3.5).

Identified More sedimentary
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Physical properties

Brown to ochre, earthy to dull luster, porous and strongly weathered, with no visible crystal faces; estimated Mohs hardness 3–6 depending on cementation, and typically moderate specific gravity (about 2.5–3.5).

Formation & geological history

Likely formed by intense chemical weathering in a warm, humid terrestrial environment, concentrating iron oxides near the surface; age cannot be determined from the photograph and may range from relatively young soil crust to ancient weathered bedrock.

Uses & applications

Generally used as a geological specimen or pigment source; iron-rich laterite can be mined for nickel or iron, while limonite has historically been used as ochre and a minor iron ore.

Geological facts

The rusty coloration comes from oxidized iron, similar to natural rust. Some porous iron-rich specimens can weakly attract a magnet if they contain magnetite.

Field identification & locations

Common in tropical and subtropical regions, especially Australia, India, Brazil, Africa, and Southeast Asia; a reddish-brown streak, earthy texture, and possible yellow-brown powder support identification, but a streak and hardness test are needed.