sedimentary

Limonite with Iron Inclusions

Limonite (Hydrated Iron Oxide, FeO(OH)·nH2O)

AI-generated identification · may be incorrect

Hardness: 4.0-5.5 (Mohs scale); Color: Yellowish-brown to earthy brown; Luster: Dull, earthy, or submetallic; Crystal Structure: Amorphous/Microcrystalline; Cleavage: None; Specific Gravity: 2.7-4.3.

Hardness: 4
Color: Yellowish-brown to earthy brown
Luster: Dull, earthy, or submetallic

Identified April 27, 2026More sedimentary →

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Physical properties

Hardness: 4.0-5.5 (Mohs scale); Color: Yellowish-brown to earthy brown; Luster: Dull, earthy, or submetallic; Crystal Structure: Amorphous/Microcrystalline; Cleavage: None; Specific Gravity: 2.7-4.3.

Formation & geological history

Formed by the oxidation and hydration of iron-rich mineral deposits (like pyrite or magnetite) in secondary enrichment zones. Often found as bog iron or in weathered sedimentary ironstones.

Uses & applications

Historically used as a major iron ore. Today, it is primarily used as a pigment (yellow ochre) in paints, for manufacturing cement, and as a soil conditioner in agriculture.

Geological facts

Limonite is not a singular mineral but a mixture of hydrated iron oxide minerals, mainly goethite. It was used by many ancient cultures as the first source of iron and for cave paintings due to its bright earthy pigments.

Field identification & locations

Identify in the field by its distinct yellow-brown streak (even on black versions) and earthy odor when damp. Commonly found in riverbeds, marshy areas, and near oxidized ore veins. Collectors value it for 'pseudomorphs' where it replaces the shape of other minerals.