
mineral
Limonite with Hematite
Hydrated Iron(III) Oxide-Hydroxide (FeO(OH)·nH2O)
Hardness: 4-5.5 (Mohs), Color: Yellowish-brown to black, Luster: Dull to sub-metallic, Crystal structure: Amorphous or microcrystalline, Specific Gravity: 2.7-4.3
- Hardness
- 4-5
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Physical properties
Hardness: 4-5.5 (Mohs), Color: Yellowish-brown to black, Luster: Dull to sub-metallic, Crystal structure: Amorphous or microcrystalline, Specific Gravity: 2.7-4.3
Formation & geological history
Formed through the oxidation and hydration of iron-rich mineral deposits (like pyrite or magnetite) in weathered environments. Most common in sedimentary bog iron or secondary enrichment zones.
Uses & applications
Historically used as an iron ore; commonly used as a natural pigment (yellow ochre) in paints, ceramics, and cosmetics. Primarily of interest to mineral collectors.
Geological facts
Limonite is not a true mineral but a mixture of various hydrated iron oxides. It has been used since prehistoric times as a cave painting pigment.
Field identification & locations
Identified by its signature yellow-brown streak, density, and lack of magnetism compared to magnetite. Found globally in weathering zones and hydrothermal vein outcrops.
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