Rock Identifier
Weathered iron-rich concretion or limonite/goethite nodule (Limonite (largely hydrated iron oxides; commonly goethite, FeO(OH), and hematite, Fe₂O₃)) — mineral
mineral

Weathered iron-rich concretion or limonite/goethite nodule

Limonite (largely hydrated iron oxides; commonly goethite, FeO(OH), and hematite, Fe₂O₃)

AI-generated identification · may be incorrect

Hardness about 4–5.5 Mohs; rusty yellow-brown to dark brown, earthy to dull/submetallic luster, irregular botryoidal or porous texture, and no obvious cleavage. The specimen appears rounded, weathered, and iron-stained, possibly with a small cavity or fossil-like inclusion.

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Physical properties

Hardness about 4–5.5 Mohs; rusty yellow-brown to dark brown, earthy to dull/submetallic luster, irregular botryoidal or porous texture, and no obvious cleavage. The specimen appears rounded, weathered, and iron-stained, possibly with a small cavity or fossil-like inclusion.

Formation & geological history

Forms by oxidation and weathering of iron-bearing minerals, commonly as a soil or sedimentary concretion; age cannot be determined from the photograph and may range from recent to ancient.

Uses & applications

Used historically as an iron ore and yellow-brown pigment; attractive nodules are mainly collected as geological specimens.

Geological facts

Limonite is a field term rather than a single precisely defined mineral, because its hydrated iron-oxide mixture varies. Goethite-rich material may form botryoidal surfaces and stalactitic cavities.

Field identification & locations

Identify by its rusty color, heavy feel, earthy appearance, and potential reddish-yellow streak; a magnet may show weak attraction if magnetite is present. Common in weathered iron deposits, laterites, stream gravels, and sedimentary rocks.