Rock Identifier
Limonite Boxwork / Iron Ore Concretion (FeO(OH)qnH2O (Hydrated iron oxide)) — sedimentary
sedimentary

Limonite Boxwork / Iron Ore Concretion

FeO(OH)qnH2O (Hydrated iron oxide)

Hardness: 4.0 - 5.5; Color: Dark brown to yellow-brown; Luster: Dull or earthy; Structure: Amorphous or microcrystalline; Highly porous and irregular shape.

Hardness
4
Color
Dark brown to yellow-brown
Luster
Dull or earthy
Identified More sedimentary
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Physical properties

Hardness: 4.0 - 5.5; Color: Dark brown to yellow-brown; Luster: Dull or earthy; Structure: Amorphous or microcrystalline; Highly porous and irregular shape.

Formation & geological history

Formed through the oxidation and hydration of iron-rich minerals. Often found as a secondary mineral in the oxidation zones of ore deposits or as bog iron in swamps.

Uses & applications

Primary source of iron ore in historical times; currently used as a pigment (ochre) and for mineral collecting.

Geological facts

Limonite is not a single mineral but a mixture of hydrated iron oxide minerals, most commonly goethite. It was historically used to produce brown and yellow paints.

Field identification & locations

Identify by its yellowish-brown streak, lack of magnetism compared to magnetite, and irregular, often hollow or 'bubbly' (botryoidal) texture. Found worldwide in weathered bedrock.