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Goethite is an iron oxyhydroxide mineral, α-FeO(OH), crystallizing in the orthorhombic system. Limonite is not a true mineral but a field term for a mixture of hydrous iron oxides, primarily goethite, often amorphous or cryptocrystalline, with variable water content (FeO(OH)·nH2O). It typically forms as a weathering product and is characterized by its earthy, often porous, and concretionary habits. The distinction between goethite and limonite is primarily based on crystallinity and water content, with goethite being crystalline and limonite being a more general term for amorphous or poorly crystalline hydrous iron oxides.
How to Identify
- Color
- Yellowish-brown to dark brown, blackish-brown, or reddish-brown. Limonite is typically more yellowish-brown.
- Luster
- Goethite can be adamantine, submetallic, silky (fibrous varieties), or dull/earthy. Limonite is typically dull and earthy.
- Texture
- Goethite can be fibrous, botryoidal, stalactitic, reniform, or massive. Limonite is typically earthy, porous, concretionary, mammillary, or stalactitic.
- Crystal Form
- Goethite forms prismatic, acicular, or tabular crystals, often radiating or fibrous. Limonite is typically amorphous or cryptocrystalline, lacking distinct crystal forms.
- Cleavage
- Goethite exhibits perfect cleavage on {010} and good cleavage on {100}. Limonite, being an aggregate, does not exhibit true cleavage.
- Geological Environment
- Found in the oxidized zones of iron ore deposits, gossans, bogs, swamps, and as a weathering product of iron-rich rocks and minerals. Common in sedimentary environments where iron-rich waters precipitate.
Key Facts
- Hardness: Goethite: 5-5.5 (Mohs); Limonite: 1-5.5 (variable, often softer and earthy)
- Specific Gravity: Goethite: 3.3-4.3; Limonite: 2.7-4.3 (variable)
- Crystal System: Goethite: Orthorhombic; Limonite: Amorphous to cryptocrystalline (no defined crystal system)
- Color: Yellowish-brown, brown, blackish-brown, reddish-brown
- Luster: Adamantine, submetallic, silky (fibrous), dull, earthy
- Transparency: Opaque
- Fracture: Goethite: Uneven to subconchoidal; Limonite: Earthy, conchoidal
- Cleavage: Goethite: Perfect on {010}, good on {100}; Limonite: None (aggregate)
- Composition: Goethite: Iron oxyhydroxide (FeO(OH)); Limonite: Hydrous iron oxides, predominantly goethite, with variable water content (FeO(OH)·nH2O)
Quick Check
- Color: Yellowish-brown to dark brown, blackish-brown
- Luster: Dull, earthy, submetallic, silky
- Streak: Yellowish-brown
Physical Characteristics
- Crystal Habit: Goethite: Prismatic, acicular, tabular, fibrous, radiating, botryoidal, stalactitic, reniform, massive. Limonite: Earthy, porous, concretionary, mammillary, stalactitic, massive.
- Cleavage Type: Goethite: Perfect {010}, good {100}; Limonite: None
- Fracture Type: Goethite: Uneven to subconchoidal; Limonite: Earthy, conchoidal
- Tenacity: Goethite: Brittle; Limonite: Friable to brittle
- Luster Type: Adamantine, submetallic, silky, dull, earthy
Formation
Goethite and limonite are secondary iron oxyhydroxide minerals that form through the weathering and oxidation of primary iron-bearing minerals (e.g., pyrite, siderite, magnetite, hematite) in the presence of water and oxygen. They are common products of hydrothermal alteration, supergene enrichment, and bog iron formation. Limonite is specifically a mixture of hydrous iron oxides, predominantly goethite, but also lepidocrocite and ferrihydrite, often amorphous or cryptocrystalline.
Usage
Historically, limonite was a significant iron ore, particularly for early iron smelting. Today, it is still used as a pigment (ochre) in paints, ceramics, and cosmetics. Goethite is also a minor iron ore and a source of pigment. Both are important in soil science and environmental studies due to their role in heavy metal adsorption and water purification.
Age Distribution
Forms continuously in surficial environments; therefore, its age varies widely from geologically recent to ancient, depending on the specific deposit.
Where to Find
Lake Superior Region, USA
Significant iron ore deposits, including goethite and limonite, are found in the Mesabi Range and other areas.
Germany
The Siegerland district is a classic locality for well-crystallized goethite specimens.
Cornwall, England
Known for various iron minerals, including goethite, often associated with tin and copper deposits.
Brazil
Large iron ore deposits, particularly in Minas Gerais, contain abundant goethite.
Australia
Extensive iron ore deposits in Western Australia are rich in goethite and other iron oxides.
Finding Tips
Look for Iron-Rich Environments
Search in areas with evidence of iron oxidation, such as rust-colored soils, gossans (weathered ore caps), and boggy areas.
Check Weathered Zones
Goethite and limonite are common in the oxidized zones of sulfide ore deposits and as alteration products of mafic and ultramafic rocks.
Examine Concretions and Nodules
Limonite often forms as concretions, nodules, or stalactitic growths in sedimentary rocks and soils.
Observe Color and Streak
The characteristic yellowish-brown to brown color and yellowish-brown streak are key identifiers. Hematite has a reddish-brown streak.
Test for Hardness
Goethite is relatively soft (5-5.5 on Mohs scale), while limonite can be even softer and earthy.
Similar Rocks
Hematite
Fe2O3
Also known as: Specularite, Kidney Ore, Red Iron Ore
Magnetite
Fe3O4
Also known as: Lodestone
Pyrite
FeS2
Also known as: Fool's Gold
Siderite
FeCO3
Also known as: Iron Carbonate
Scientific Classification
- Mineral Class
- Oxides and Hydroxides
- Group
- Goethite Group (for Goethite)
- Crystal System
- Goethite: Orthorhombic; Limonite: Amorphous/Cryptocrystalline
- Chemical Formula
- Goethite: FeO(OH); Limonite: FeO(OH)·nH2O (general formula)
- Composition
- Hydrous iron oxides
Explore Goethite with Limonite
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