
mineral
Limonite (Iron Ore)
Limonite (Hydrous iron(III) oxide-hydroxide mixture, primarily FeO(OH)·nH2O)
Hardness: 4-5.5; Color: Yellowish-brown to dark brown; Luster: Dull to earthy; Crystal structure: Amorphous; Cleavage: None; Specific gravity: 2.7-4.3
- Hardness
- 4-5
- Color
- Yellowish-brown to dark brown
- Luster
- Dull to earthy
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Physical properties
Hardness: 4-5.5; Color: Yellowish-brown to dark brown; Luster: Dull to earthy; Crystal structure: Amorphous; Cleavage: None; Specific gravity: 2.7-4.3
Formation & geological history
Formed as a secondary material through the oxidation and weathering of primary iron-bearing minerals like pyrite, magnetite, and hematite in oxygen-rich environments.
Uses & applications
Historically used as an iron ore; currently used as a natural earth pigment (yellow ochre) in paints and dyes, and for soil amendment.
Geological facts
Limonite is not a true mineral but a mixture of related hydrated iron oxide minerals. It was the primary source of iron for ancient civilizations and is what gives many soils their yellow-brown color.
Field identification & locations
Identify by its characteristic yellowish-brown streak on a porcelain plate and dull, rusty appearance. Often found in bog deposits, gossans (weathered rock caps), and as a staining agent in sedimentary rocks.
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