Rock Identifier
Limonite (Iron Ore) (Hydrated ferric oxide mixture (FeO(OH)·nH2O)) — sedimentary
sedimentary

Limonite (Iron Ore)

Hydrated ferric oxide mixture (FeO(OH)·nH2O)

Hardness: 4.0-5.5 | Color: Brown, yellowish-brown, ochre | Luster: Dull, earthy | Crystal Structure: Amorphous/Microcrystalline | Cleavage: None | Specific Gravity: 2.7-4.3

Hardness
4
Identified More sedimentary

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Physical properties

Hardness: 4.0-5.5 | Color: Brown, yellowish-brown, ochre | Luster: Dull, earthy | Crystal Structure: Amorphous/Microcrystalline | Cleavage: None | Specific Gravity: 2.7-4.3

Formation & geological history

Formed as a secondary mineral through the oxidation and hydration of other iron-bearing minerals (like pyrite or magnetite) in weathered zones of ore deposits or as sedimentary bog iron.

Uses & applications

Historically used as a major ore of iron; currently used predominantly as a natural pigment (yellow ochre) in paints, dyes, and cosmetics.

Geological facts

Limonite is not a true mineral in the strictest sense but a mixture of minerals, primarily goethite. It was the source of iron for many early industrial ironworks.

Field identification & locations

Identify by its yellowish-brown streak on a porcelain plate and lack of magnetism compared to magnetite. Found globally in weathered capping of iron-rich mineral veins (gossans).