
mineral
Limonite (Iron Ore)
Limonite (unstructured hydrated iron(III) oxide-hydroxides, often FeO(OH)·nH2O)
Hardness: 4.0 - 5.5 (Mohs); Color: Yellowish-brown to dark brown; Luster: Dull, earthy; Crystal Structure: Amorphous (no internal structure); Streak: Yellowish-brown; Specific Gravity: 2.7 - 4.3.
- Hardness
- 4
- Color
- Yellowish-brown to dark brown
- Luster
- Dull, earthy
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Physical properties
Hardness: 4.0 - 5.5 (Mohs); Color: Yellowish-brown to dark brown; Luster: Dull, earthy; Crystal Structure: Amorphous (no internal structure); Streak: Yellowish-brown; Specific Gravity: 2.7 - 4.3.
Formation & geological history
Formed by the oxidation and hydration of iron-rich sulfide minerals (like pyrite) or the weathering of iron-rich silicates. It typically forms in the oxidation zones of ore deposits or as sedimentary deposits in bogs.
Uses & applications
A historic source of iron ore; currently used as a yellow-brown pigment (ochre) in paints, enamels, and concrete coloring.
Geological facts
Limonite is not a true mineral but a mixture of similar hydrated iron oxide minerals. It has been used by humans as a pigment since prehistoric times, appearing in cave paintings.
Field identification & locations
Identify in the field by its distinct mustard-yellow to brown streak on a porcelain plate and its frequently 'rusty' or earthy appearance. It often occurs as a coating or mass associated with other iron minerals.
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