Rock Identifier
Limonite Nodule (Hydrated Iron Oxide-Hydroxide (FeO(OH)·n(H2O))) — mineral
mineral

Limonite Nodule

Hydrated Iron Oxide-Hydroxide (FeO(OH)·n(H2O))

AI-generated identification · may be incorrect

Hardness 4-5.5 on Mohs scale, yellowish-brown to dark brown color, submetallic to earthy luster, amorphous or cryptocrystalline structure, specific gravity 2.7-4.3.

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Physical properties

Hardness 4-5.5 on Mohs scale, yellowish-brown to dark brown color, submetallic to earthy luster, amorphous or cryptocrystalline structure, specific gravity 2.7-4.3.

Formation & geological history

Formed through the alteration and oxidation of other iron-bearing minerals in weathering environments and sedimentary deposits.

Uses & applications

Used historically as a source of iron ore, as a yellow pigment (ochre), and collected by enthusiasts.

Geological facts

Limonite is not a single distinct mineral, but rather a mixture of related iron oxides and hydroxides. It often forms pseudomorphs after other minerals like pyrite.

Field identification & locations

Identify by its characteristic yellowish-brown streak and earthy appearance; commonly found in oxidized iron ore deposits worldwide.