
mineral
Limonite (Ironstone)
Limonite (Hydrated iron(III) oxide-hydroxide, FeO(OH)·nH2O)
Hardness: 4-5.5 on Mohs scale. Color: Yellowish-brown to dark brown or black. Luster: Dull, earthy to submetallic. Crystal structure: Amorphous to microcrystalline. Cleavage: None. Streak: Yellowish-brown.
- Hardness
- 4-5
- Color
- Yellowish-brown to dark brown or black
- Luster
- Dull, earthy to submetallic
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Physical properties
Hardness: 4-5.5 on Mohs scale. Color: Yellowish-brown to dark brown or black. Luster: Dull, earthy to submetallic. Crystal structure: Amorphous to microcrystalline. Cleavage: None. Streak: Yellowish-brown.
Formation & geological history
Formed as a secondary mineral through the oxidation and hydration of iron-rich minerals such as pyrite, magnetite, or biotite. It is common in the oxidation zones of ore deposits and as bog iron in swampy environments.
Uses & applications
Historically used as a major ore of iron. Today, it is primarily used as a pigment (ochre or sienna) for paints and dyes. It is also of interest for geological specimen collecting.
Geological facts
Limonite is not a single mineral but a mixture of hydrated iron oxide minerals, primarily goethite. It has been used as a pigment since prehistoric times, notably in cave paintings like those at Lascaux.
Field identification & locations
Identify in the field by its characteristic 'rust' color and yellowish-brown streak. It is often found as a coating or mass in sedimentary environments. Look for heavy, earthy nodules in iron-rich soil or near mine tailings.
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