
mineral
Limonite (Iron Stone/Iron Ore)
FeO(OH)·nH2O (Hydrous ferric oxide)
AI-generated identification · may be incorrectHardness: 4.0-5.5 (Mohs scale); Color: Yellowish-brown to dark brown; Luster: Dull or earthy; Crystal structure: Amorphous; Cleavage: None; Specific gravity: 2.7-4.3
- Hardness
- 4
- Color
- Yellowish-brown to dark brown
- Luster
- Dull or earthy
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Physical properties
Hardness: 4.0-5.5 (Mohs scale); Color: Yellowish-brown to dark brown; Luster: Dull or earthy; Crystal structure: Amorphous; Cleavage: None; Specific gravity: 2.7-4.3
Formation & geological history
Formed as a secondary material through the oxidation and hydration of iron-rich mineral ores (like pyrite or magnetite) in weathering zones. It can occur in sedimentary layers or as gossans over metal deposits.
Uses & applications
Historically used as an iron ore; currently used as a natural pigment (yellow ochre) in paints, and occasionally as a low-cost building material or for minor geological teaching kits.
Geological facts
Limonite is not a true mineral species but a mixture of similar hydrated iron oxide minerals, predominantly goethite. It's the primary component of 'iron hat' or gossan, which prospectors use to find gold and copper deposits.
Field identification & locations
Identify in the field by its distinct mustard-yellow to rust-brown streak (test by scratching on unglazed porcelain) and its earthy, dull appearance. Common in wet soils and boggy environments.
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Epidote
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