Rock Identifier
Iron-rich laterite (possibly ferruginous soilstone) (Laterite; chiefly iron oxides/oxyhydroxides such as goethite (FeO(OH)) and hematite (Fe₂O₃), with clay minerals and quartz) — sedimentary
sedimentary

Iron-rich laterite (possibly ferruginous soilstone)

Laterite; chiefly iron oxides/oxyhydroxides such as goethite (FeO(OH)) and hematite (Fe₂O₃), with clay minerals and quartz

AI-generated identification · may be incorrect

Reddish-brown, earthy and rough, with no obvious crystals or cleavage; hardness and density vary with cementation. The image alone does not establish a precise mineral composition.

Identified More sedimentary →
Explore Iron-rich laterite (possibly ferruginous soilstone) in the encyclopedia →

Identify your own rocks.

Get a report just like this from any photo, free.

Physical properties

Reddish-brown, earthy and rough, with no obvious crystals or cleavage; hardness and density vary with cementation. The image alone does not establish a precise mineral composition.

Formation & geological history

Forms through intense chemical weathering and leaching in warm, wet climates, concentrating iron and aluminum. It may develop over long periods; the specimen’s age and exact setting cannot be determined from the photograph.

Uses & applications

Laterite is used locally as building stone and, in some deposits, as iron or aluminum ore; this small rough piece is mainly a geological or teaching specimen.

Geological facts

Its rusty color commonly comes from iron oxides. Lateritic material can harden when exposed to air as it dries.

Field identification & locations

Look for red-to-brown color, earthy texture, and iron-rich staining; compare with local laterite or ferruginous soilstone, since similar-looking ironstone has several origins. Common in tropical and subtropical weathering profiles.