
sedimentary
Gossan (Limonite/Ironstone)
Hydrated Iron Oxide (FeO(OH)·nH2O)
Hardness: 4-5.5 (Mohs scale); Color: Rusty brown, yellowish-orange to reddish-brown; Luster: Dull to earthy, greasy when wet; Crystal Structure: Amorphous or microcrystalline; Cleavage: None; Specific Gravity: 2.7–4.3
- Hardness
- 4-5
- Color
- Rusty brown, yellowish-orange to reddish-brown
- Luster
- Dull to earthy, greasy when wet
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Physical properties
Hardness: 4-5.5 (Mohs scale); Color: Rusty brown, yellowish-orange to reddish-brown; Luster: Dull to earthy, greasy when wet; Crystal Structure: Amorphous or microcrystalline; Cleavage: None; Specific Gravity: 2.7–4.3
Formation & geological history
Formed by the oxidation of sulfide minerals (like pyrite or chalcopyrite) in an ore deposit. As water and oxygen react with the minerals, sulfuric acid is produced, leaving behind these iron-rich oxides as a cap or 'hat' over the deposit.
Uses & applications
Historically used as an indicator for miners to find valuable underground metal deposits (gold, silver, copper). Sometimes used as a low-grade iron ore or mineral pigment (ochre).
Geological facts
Miners call these 'iron hats' because they sit on top of ore veins. They are often porous or 'vuggy' because the original minerals have been leached away.
Field identification & locations
Identify by its rusty color, heavy weight compared to non-metallic rocks, and staining. In the field, its presence suggests chemical weathering of minerals nearby. Commonly found in mining districts and arid environments.
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