
mineral
Yellow Ocher (Limonite)
Limonite (Hydrated Iron Oxide) - FeO(OH)·nH2O
Hardness: 4.0–5.5 on Mohs scale; Color: Yellowish-brown to deep yellow; Luster: Dull, earthy; Crystal Structure: Amorphous (often pseudomorphic after other iron minerals); Specific Gravity: 2.7–4.3
- Hardness
- 4
- Color
- Yellowish-brown to deep yellow
- Luster
- Dull, earthy
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Physical properties
Hardness: 4.0–5.5 on Mohs scale; Color: Yellowish-brown to deep yellow; Luster: Dull, earthy; Crystal Structure: Amorphous (often pseudomorphic after other iron minerals); 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, or siderite). It is often found in the oxidation zones of ore deposits or as a bog iron precipitate in swampy areas.
Uses & applications
Historically and currently used as a natural pigment (ocher) for paints, dyes, and cosmetics. It is also an accidental iron ore and used in geological education as a primary example of chemical weathering.
Geological facts
Limonite was one of the first pigments used by early humans in cave paintings (such as at Lascaux, France). Because it lacks a crystalline structure and contains variable amounts of water, it is technically a 'mineraloid' rather than a true mineral.
Field identification & locations
Identify in the field by its distinct mustard-yellow earthy streak when rubbed against a tile, its dusty texture, and its common occurrence near rusting iron-rich rocks. It is found globally in sedimentary and weathering environments.
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