
sedimentary
Limonite Concretion
Goethite/Limonite concretion (FeO(OH)·nH2O)
AI-generated identification · may be incorrectHardness: 4-5.5 on the Mohs scale, Color: yellowish-brown, dark brown, or reddish-brown, Luster: earthy to submetallic, Crystal structure: amorphous or microcrystalline (pseudomorphic after pyrite or marcasite), Cleavage: none, Specific gravity: 2.7-4.3
- Hardness
- 4-5
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Physical properties
Hardness: 4-5.5 on the Mohs scale, Color: yellowish-brown, dark brown, or reddish-brown, Luster: earthy to submetallic, Crystal structure: amorphous or microcrystalline (pseudomorphic after pyrite or marcasite), Cleavage: none, Specific gravity: 2.7-4.3
Formation & geological history
Formed through the low-temperature chemical precipitation of iron oxides and hydroxides in sedimentary environments, often replacing precursor minerals like pyrite or accumulating in sandstone pores through groundwater movement.
Uses & applications
Used historically as a pigment (ochre), as an iron ore, and commonly collected as geological specimens or curiosity stones.
Geological facts
Limonite is not a true distinct mineral species, but rather a field term for a mixture of hydrated iron oxide minerals, predominantly goethite.
Field identification & locations
Easily identified by its characteristic yellowish-brown streak, concentric banding or boxwork structure, and rust-like appearance. Commonly found worldwide in weathering zones of iron-bearing rocks.
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