Rock Identifier
Limonite Concretion (Goethite/Limonite concretion (FeO(OH)·nH2O)) — sedimentary
sedimentary

Limonite Concretion

Goethite/Limonite concretion (FeO(OH)·nH2O)

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

Hardness
4-5
Identified More sedimentary
Explore Limonite Concretion in the encyclopedia →

Identify your own rocks.

Get a report just like this from any photo, free.

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.