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Goethite with Limonite

Mineral/Mineraloid Aggregate

FeO(OH) with FeO(OH)·nH2O

Also known as: Bog Iron, Iron Ochre, Brown Hematite

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Description

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

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