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Limonite is not a true mineral but a general term for a mixture of hydrated iron oxide minerals, predominantly goethite (α-FeOOH) and lepidocrocite (γ-FeOOH), often with adsorbed water and impurities. It typically forms as a result of the weathering of other iron-bearing minerals. Goethite is a distinct mineral, an iron oxyhydroxide, and is the most common component of what is broadly termed limonite. These minerals are characterized by their earthy, often porous, and sometimes botryoidal or stalactitic habits, and their distinctive yellowish-brown to dark brown color and yellowish-brown streak. They are significant iron ores, particularly in tropical and subtropical regions where intense weathering occurs.
How to Identify
- Color
- Yellowish-brown, reddish-brown, dark brown, blackish-brown. Often has a rusty appearance.
- Luster
- Earthy, dull, submetallic, silky (in fibrous varieties).
- Texture
- Earthy, porous, often botryoidal, stalactitic, mammillary, or concretionary. Can be massive or oolitic.
- Crystal Form
- Goethite forms acicular, prismatic, or tabular crystals, often radiating or fibrous. Limonite is typically amorphous or cryptocrystalline, forming botryoidal, stalactitic, or massive aggregates.
- Cleavage
- Goethite has perfect cleavage on {010} and good cleavage on {100}, but it is rarely observed due to its fine-grained or massive habit. Limonite exhibits no cleavage.
- Geological Environment
- Found in gossans (weathered caps of sulfide deposits), lateritic soils, bog iron deposits, sedimentary iron formations, and as an alteration product in various rock types. It is common in oxidized zones of ore deposits and as a cementing agent in sandstones.
Key Facts
- Hardness: Goethite: 5-5.5 (Mohs); Limonite: 4-5.5 (Mohs, variable due to mixture and porosity)
- Specific Gravity: Goethite: 3.3-4.3; Limonite: 2.7-4.3 (variable, often lower due to porosity)
- Crystal System: Goethite: Orthorhombic; Limonite: Amorphous to cryptocrystalline (no defined crystal system)
- Color: Yellowish-brown, reddish-brown, dark brown, blackish-brown
- Luster: Earthy, dull, submetallic, silky
- Transparency: Opaque
- Fracture: Uneven, conchoidal (Goethite), earthy (Limonite)
- Cleavage: Goethite: Perfect on {010}, good on {100} (rarely observed); Limonite: None
- Composition: Goethite: Hydrous iron oxide (α-FeOOH); Limonite: A mixture of hydrated iron oxides, primarily goethite and lepidocrocite, with variable water content and impurities.
Quick Check
- Color: Yellowish-brown to dark brown
- Luster: Earthy, dull
- Streak: Yellowish-brown
Physical Characteristics
- Crystal Habit: Goethite: Acicular, prismatic, tabular, radiating, fibrous, botryoidal, stalactitic, massive. Limonite: Massive, earthy, botryoidal, mammillary, concretionary, oolitic.
- Cleavage Type: Goethite: Perfect {010}, good {100}; Limonite: None
- Fracture Type: Goethite: Uneven to subconchoidal; Limonite: Earthy, uneven
- Tenacity: Brittle
- Luster Type: Earthy, dull, submetallic, silky
Formation
Limonite and Goethite are secondary minerals, forming through the weathering and oxidation of primary iron-bearing minerals (e.g., pyrite, siderite, magnetite, hematite) in the presence of water and oxygen. They commonly precipitate from iron-rich solutions in bogs, swamps, and shallow marine environments (bog iron ore), or as residual accumulations in lateritic soils and gossans (weathered caps of sulfide ore deposits). Goethite is the more stable and common crystalline form, while limonite is often used as a field term for amorphous or cryptocrystalline mixtures of hydrated iron oxides.
Usage
The primary use of limonite/goethite-rich iron ore is as a source of iron for steel production. Historically, bog iron was a significant source of iron. It is also used as a pigment (ochre) and, less commonly, as a heavy aggregate.
Age Distribution
Can form throughout geological time, but significant deposits are often associated with specific paleoenvironments, such as the Cenozoic for bog iron ores, or as weathering products of older iron-rich rocks.
Where to Find
Mesabi Range, Minnesota, USA
Historically a major source of iron ore, including goethite-rich taconite and weathered iron formations.
Pilbara region, Western Australia
World-class iron ore deposits, including significant goethite and hematite ores, often formed from enriched banded iron formations.
Minas Gerais, Brazil
Extensive iron ore deposits, including high-grade hematite and goethite ores, often associated with banded iron formations.
Krivoy Rog, Ukraine
Large iron ore basin with significant goethite and hematite deposits.
Various bog and swamp environments worldwide
Bog iron ore (limonite) forms in modern and ancient wetlands where iron-rich groundwater precipitates hydrated iron oxides.
Finding Tips
Look for rusty stains
Limonite/goethite often manifests as rusty-brown stains on rocks, soil, and in water bodies, indicating the presence of iron oxidation.
Check weathered zones
Explore the weathered caps (gossans) of sulfide ore deposits, where limonite/goethite often forms as a residual product.
Investigate wetlands and bogs
Bog iron ore can be found in marshy areas, often as concretions or layers near the surface.
Observe streak color
The characteristic yellowish-brown streak is a key diagnostic feature, differentiating it from hematite (red streak) and magnetite (black streak).
Test for magnetism (weak)
While not strongly magnetic like magnetite, some limonite/goethite can exhibit weak magnetism due to inclusions of other iron oxides or heating during formation.
Similar Rocks
Hematite
Fe2O3
Also known as: Red Iron Ore, Specularite
Magnetite
Fe3O4
Also known as: Magnetic Iron Ore
Siderite
FeCO3
Also known as: Iron Carbonate
Pyrite
FeS2
Also known as: Fool's Gold
Scientific Classification
- Mineral Class
- Oxides and Hydroxides
- Group
- Goethite-Diaspore Group (for Goethite)
- Crystal System
- Orthorhombic (for Goethite); Amorphous (for Limonite)
- Chemical Formula
- Goethite: FeO(OH); Limonite: FeO(OH)·nH2O (general representation for the mixture)
- Composition
- Hydrated iron oxide, typically containing 50-65% iron, 10-15% water, and various impurities (e.g., silica, alumina, manganese).
Explore Iron Ore (Limonite/Goethite)
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