
mineral
Limonite (Oxidized Iron Ore)
FeO(OH)·nH2O (Hydrous ferric oxide)
Hardness: 4-5.5 (Mohs), Color: Rusty brown, yellow, earthy orange, Luster: Dull or earthy, Crystal structure: Amorphous (often pseudomorphic after other minerals), Cleavage: None, Specific gravity: 2.7–4.3.
- Hardness
- 4-5
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Physical properties
Hardness: 4-5.5 (Mohs), Color: Rusty brown, yellow, earthy orange, Luster: Dull or earthy, Crystal structure: Amorphous (often pseudomorphic after other minerals), Cleavage: None, Specific gravity: 2.7–4.3.
Formation & geological history
Formed by the oxidation and hydration of iron-rich sulfide minerals (like pyrite) in the weathering zone near the Earth's surface. Can be found in gossans ("iron caps") covering ore deposits.
Uses & applications
Historically used as a low-grade iron ore and as a pigment for ochre paints. Today it's primarily of interest to collectors or used as a rough material in landscaping.
Geological facts
Limonite is not a single mineral but a mixture of hydrated iron oxide minerals, mostly goethite. It was one of the earliest pigments used by humans for cave paintings and Neolithic burials.
Field identification & locations
Identify by its distinctive rusty-yellow to brown streak on a porcelain plate and its earthy smell when damp. Commonly found in boggy areas and weathered outcrops. Collectors should look for 'pseudomorphs' where limonite has replaced the shape of pyrite cubes.
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