Rock Identifier
Likely iron-rich laterite or limonite/goethite nodule (Hydrated iron oxides, chiefly limonite (FeO(OH)·nH₂O) and/or goethite (FeO(OH))) — mineral
mineral

Likely iron-rich laterite or limonite/goethite nodule

Hydrated iron oxides, chiefly limonite (FeO(OH)·nH₂O) and/or goethite (FeO(OH))

AI-generated identification · may be incorrect

Dark brown, earthy to submetallic, irregular rounded nodules with a rough surface. Typical hardness is about 4–5.5 Mohs, streak yellow-brown to reddish-brown, and specific gravity roughly 3.3–4.3. The wet photo limits certainty; crystal structure cannot be confirmed visually.

Identified More mineral
Explore Likely iron-rich laterite or limonite/goethite nodule in the encyclopedia →

Identify your own rocks.

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

Physical properties

Dark brown, earthy to submetallic, irregular rounded nodules with a rough surface. Typical hardness is about 4–5.5 Mohs, streak yellow-brown to reddish-brown, and specific gravity roughly 3.3–4.3. The wet photo limits certainty; crystal structure cannot be confirmed visually.

Formation & geological history

Forms by intense tropical weathering and concentration of iron in lateritic soils, commonly over weathered basalt or other iron-bearing rocks. The reported Andhra Pradesh location is geologically plausible for lateritic iron nodules.

Uses & applications

Used historically as iron ore or natural pigment; small pieces have little industrial value and are mainly educational or collector specimens.

Geological facts

Magnetism varies: goethite/limonite is usually weakly magnetic, while associated magnetite can be strongly magnetic. A yellow-brown streak and reddish-brown powder are useful clues.

Field identification & locations

Likely common rather than a valuable gemstone. Test an inconspicuous edge for streak on unglazed porcelain and check magnetism; avoid relying on appearance alone because polished slag and iron-rich industrial waste can look similar.