
mineral
Limonite (Iron Ore)
Limonite (Hydrous ferric oxides), generic formula FeO(OH)·nH2O
Hardness: 4-5.5 (Mohs scale); Color: Yellowish-brown to dark brown; Luster: Dull, earthy, or submetallic; Crystal structure: Amorphous (no visible crystal habit); Cleavage: None; Specific gravity: 2.7–4.3.
- Hardness
- 4-5
- Color
- Yellowish-brown to dark brown
- Luster
- Dull, earthy, or submetallic
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Physical properties
Hardness: 4-5.5 (Mohs scale); Color: Yellowish-brown to dark brown; Luster: Dull, earthy, or submetallic; Crystal structure: Amorphous (no visible crystal habit); Cleavage: None; Specific gravity: 2.7–4.3.
Formation & geological history
Formed through the secondary alteration of iron-rich minerals (like pyrite, magnetite, or hematite) via weathering and oxidation. Found in oxidized zones of iron ore deposits and as bog iron in sedimentary environments.
Uses & applications
Historically used as a major iron ore and as a pigment (yellow ochre). Today, it is used in the production of brown and yellow paints and as a low-grade iron source in industry.
Geological facts
Limonite isn't a true mineral but a 'mineraloid' as it is a mixture of several hydrous iron oxide minerals. It has been used by humans as a pigment since prehistoric times (cave paintings).
Field identification & locations
Identify in the field by its distinct yellowish-brown streak on a porcelain plate and its earthy, rusty appearance. Often found in swampy areas or as 'gossan' capping metallic ore veins. Common globally.
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