
mineral
Limonite with Hematite
Hydrated iron(III) oxide-hydroxide with variable composition (FeO(OH)·nH2O)
Hardness: 4-5.5 (Mohs); Color: Dark brown to yellowish-orange; Luster: Dull or earthy; Crystal structure: Amorphous; Cleavage: None; Specific gravity: 2.7-4.3
- Hardness
- 4-5
- Color
- Dark brown to yellowish-orange
- Luster
- Dull or earthy
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Physical properties
Hardness: 4-5.5 (Mohs); Color: Dark brown to yellowish-orange; Luster: Dull or earthy; Crystal structure: Amorphous; Cleavage: None; Specific gravity: 2.7-4.3
Formation & geological history
Formed through the chemical weathering of iron-rich minerals such as pyrite, magnetite, or biotite. It is typically found in oxidation zones of ore deposits or as a secondary mineral in sedimentary rock layers.
Uses & applications
Historically used as an iron ore; currently used primarily as a pigment/ocher for paints and dyes. In geological prospecting, it is used as a 'gossan' indicator to find deeper metal deposits.
Geological facts
Limonite is not a true mineral but a mixture of various hydrated iron oxides. It was a major source of iron for early civilizations and was used by prehistoric humans as a cave painting pigment.
Field identification & locations
Identify in the field by its distinct yellow-brown streak, earthy texture, and association with rust-colored staining on surrounding rocks. Found globally in weathered terrains and swampy 'bog iron' areas.
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