
sedimentary
Limonite (Iron Ore)
Hydrated Iron(III) Oxide-Hydroxide (FeO(OH)·nH2O)
Hardness: 4 to 5.5 on Mohs scale; Color: Yellowish-brown to dark brown; Luster: Dull to earthy; Crystal Structure: Amorphous (does not form distinct crystals); Specific Gravity: 2.7 to 4.3.
- Hardness
- 4 to 5
- Color
- Yellowish-brown to dark brown
- Luster
- Dull to earthy
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Physical properties
Hardness: 4 to 5.5 on Mohs scale; Color: Yellowish-brown to dark brown; Luster: Dull to earthy; Crystal Structure: Amorphous (does not form distinct crystals); Specific Gravity: 2.7 to 4.3.
Formation & geological history
Formed from the secondary alteration of other iron minerals through weathering and oxidation in oxidizing environments. It is often found as a precipitate in swamps (bog iron) or as a capping over iron-bearing hydrothermal deposits.
Uses & applications
Historically used as a major source of iron ore; currently used as a pigment (yellow ochre) in dyes and paints and as an additive in cement manufacturing.
Geological facts
Limonite is not a true mineral, but a mixture of related hydrated iron oxide minerals, primarily goethite. It was one of the earliest pigments used by humans, found in prehistoric cave paintings.
Field identification & locations
Identify in the field by its characteristic yellowish-brown streak and earthy appearance. It often appears as a rusty coating on other rocks. Commonly found in gossans (iron hats) and bog deposits globally.
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