Limonite (Iron Ore)
Hydrated Iron(III) Oxide-Hydroxide (FeO(OH)·nH2O)
Rock Type: mineral

Physical Properties
Hardness: 4.0-5.5 (Mohs); Color: Yellowish-brown to dark brown; Luster: Dull, earthy; Crystal Structure: Amorphous; Cleavage: None; Specific Gravity: 2.7-4.3
Formation & Geological History
Formed as a secondary mineral through the weathering and oxidation of iron-rich minerals such as pyrite, magnetite, and siderite in the presence of water.
Uses & Applications
Historically used as a major source of iron ore (though largely superseded by hematite and magnetite) and used as a source of yellow ochre pigment since ancient times.
Geological Facts
Limonite is not a true mineral but a mineraloid mixture of various hydrated iron oxides; it is the material that gives many soils their yellow or rusty-brown color.
Field Identification & Locations
Identify by its yellowish-brown streak on a porcelain plate and its rusty appearance. Often found in marshes (bog iron) or as gossans (caps) over metallic ore deposits.
Identified on: 4/27/2026
Mode: Standard