Limonite (Iron Ore)
Limonite (Hydrous iron(III) oxide-hydroxide mixture, primarily FeO(OH)·nH2O)
Rock Type: mineral

Physical Properties
Hardness: 4-5.5; Color: Yellowish-brown to dark brown; Luster: Dull to earthy; Crystal structure: Amorphous; Cleavage: None; Specific gravity: 2.7-4.3
Formation & Geological History
Formed as a secondary material through the oxidation and weathering of primary iron-bearing minerals like pyrite, magnetite, and hematite in oxygen-rich environments.
Uses & Applications
Historically used as an iron ore; currently used as a natural earth pigment (yellow ochre) in paints and dyes, and for soil amendment.
Geological Facts
Limonite is not a true mineral but a mixture of related hydrated iron oxide minerals. It was the primary source of iron for ancient civilizations and is what gives many soils their yellow-brown color.
Field Identification & Locations
Identify by its characteristic yellowish-brown streak on a porcelain plate and dull, rusty appearance. Often found in bog deposits, gossans (weathered rock caps), and as a staining agent in sedimentary rocks.
Identified on: 4/17/2026
Mode: Standard