
mineral
Limonite (Iron Ore)
Hydrated iron(III) oxide-hydroxide (FeO(OH)·nH2O)
Hardness: 4.0-5.5 on Mohs scale; Color: Yellowish-brown to dark brown; Luster: Dull to earthy; Crystal Structure: Amorphous (no definite crystal form); Streak: Yellow-brown; Specific Gravity: 2.7-4.3.
- Hardness
- 4
- Color
- Yellowish-brown to dark brown
- Luster
- Dull to earthy
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Physical properties
Hardness: 4.0-5.5 on Mohs scale; Color: Yellowish-brown to dark brown; Luster: Dull to earthy; Crystal Structure: Amorphous (no definite crystal form); Streak: Yellow-brown; Specific Gravity: 2.7-4.3.
Formation & geological history
Formed usually by the oxidation and hydration of iron-rich sulfide minerals (like pyrite) or the weathering of other iron-rich rocks. It often occurs as a secondary mineral in the oxidation zones of ore deposits.
Uses & applications
Historically used as an Important iron ore. Today, it is primarily used as a pigment (ocher) for paints, dyes, and concrete, and as a soil conditioner.
Geological facts
Limonite is not a true mineral in the modern sense but a mixture of related hydrated iron oxide minerals, mostly goethite. It has been used by humans as a pigment since prehistoric times, found in cave paintings worldwide.
Field identification & locations
Identify by its characteristic yellowish-brown streak on a porcelain plate and its rusty, earthy appearance. It often forms 'gossans' or iron caps over mineral veins. Commonly found in bog deposits or weathered outcrops.
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