Rock Identifier
Likely weathered iron-rich rock or laterite (Uncertain; possible limonite/goethite-rich laterite (FeO(OH)·nH₂O)) — igneous
igneous

Likely weathered iron-rich rock or laterite

Uncertain; possible limonite/goethite-rich laterite (FeO(OH)·nH₂O)

AI-generated identification · may be incorrect

Orange-brown, dull to earthy luster, porous and rounded; likely low-to-moderate hardness (about 3–5 Mohs) with no visible cleavage. The image is blurred, so mineral identification and crystal structure cannot be confirmed.

Identified More igneous
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Physical properties

Orange-brown, dull to earthy luster, porous and rounded; likely low-to-moderate hardness (about 3–5 Mohs) with no visible cleavage. The image is blurred, so mineral identification and crystal structure cannot be confirmed.

Formation & geological history

Likely formed by intense chemical weathering, concentrating iron oxides and hydroxides in tropical or subtropical soils; commonly younger than the parent bedrock and generally of Cenozoic surface-weathering age.

Uses & applications

Used locally as iron ore, pigment, or decorative stone when sufficiently rich; ordinary pieces have little commercial value.

Geological facts

Iron-rich specimens commonly develop red, orange, yellow, and brown colors from hematite, goethite, and limonite. A yellow-brown streak and attraction to a strong magnet may help distinguish iron-rich material.

Field identification & locations

Common in tropical lateritic terrains, including India, Brazil, Africa, Southeast Asia, and Australia. Confirm with a fresh surface, streak test, hardness test, and ideally magnetic or chemical analysis.