
mineral
Limonite (Ironstone Concretion)
Hydrous ferric oxides (FeO(OH)·nH2O)
Hardness: 4-5.5 on Mohs scale; Color: Dull brown, yellowish-brown, to black; Luster: Dull, earthy, or sub-metallic; Crystal Structure: Amorphous (no visible crystals); Streak: Yellowish-brown
- Hardness
- 4-5
- Color
- Dull brown, yellowish-brown, to black
- Luster
- Dull, earthy, or sub-metallic
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Physical properties
Hardness: 4-5.5 on Mohs scale; Color: Dull brown, yellowish-brown, to black; Luster: Dull, earthy, or sub-metallic; Crystal Structure: Amorphous (no visible crystals); Streak: Yellowish-brown
Formation & geological history
Formed by the oxidation and hydration of iron-rich sulfide minerals or by the precipitation in marine or marshy mineral-rich environments (bog iron).
Uses & applications
Historically used as a low-grade iron ore and as a pigment for ochre paints. Today, it is primarily a geological specimen.
Geological facts
Limonite is not a single mineral but a mixture of similar hydrated iron oxide minerals, mostly goethite. It is responsible for the yellowish-brown coloring in many sedimentary rocks and soils.
Field identification & locations
Identify by its yellowish-brown streak on a porcelain plate and lack of magnetism compared to magnetite. Commonly found in gossans (weathered tops of ore deposits) or as concretions in sandstone and shale.
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