
mineral
Limonite/Goethite (Iron Ore)
Hydrous ferric oxides (FeO(OH)·nH2O)
Hardness: 4.0-5.5 on Mohs scale; Color: Yellowish-brown to dark brown; Luster: Dull to earthy; Crystal structure: Amorphous or microcrystalline; Cleavage: None; Specific Gravity: 2.7 to 4.3
- Hardness
- 4
- Color
- Yellowish-brown to dark brown
- Luster
- Dull to earthy
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Physical properties
Hardness: 4.0-5.5 on Mohs scale; Color: Yellowish-brown to dark brown; Luster: Dull to earthy; Crystal structure: Amorphous or microcrystalline; Cleavage: None; Specific Gravity: 2.7 to 4.3
Formation & geological history
Secondary mineral formed by the oxidation and weathering of primary iron-bearing minerals like pyrite, magnetite, and hematite in sedimentary or hydrothermal environments.
Uses & applications
Historically used as a major source of iron ore and as a natural pigment (brown ochre) for paints and cosmetics.
Geological facts
Limonite is not a true mineral but a mixture of hydrated iron oxide minerals. It was often the source of iron for early bog iron smelting operations.
Field identification & locations
Identify by its characteristic yellowish-brown streak (when rubbed on unglazed porcelain) and lack of magnetism compared to magnetite. Commonly found in gossans (iron-caps) above ore deposits.
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