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Limonite

Mineraloid (historically considered a mineral)

FeO(OH)·nH2O

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

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Description

Limonite is a generic term for a mixture of hydrated iron oxide minerals, predominantly goethite (FeO(OH)) and lepidocrocite (γ-FeO(OH)), often with amorphous components. It is not a true mineral in the strict sense because it lacks a definite crystal structure and chemical composition, but rather a mineraloid. It is characterized by its earthy, dull appearance and yellow-brown to dark brown color. It is a common product of the weathering of iron-rich rocks and minerals.

How to Identify

Color
Yellow-brown, reddish-brown, dark brown, or black. Often has a characteristic earthy yellow-brown color.
Luster
Earthy, dull, sometimes submetallic in botryoidal or stalactitic forms.
Texture
Earthy, porous, often botryoidal, mammillary, stalactitic, or concretionary. Can be massive or pisolitic.
Crystal Form
Amorphous or cryptocrystalline; does not form distinct crystals. Occurs as earthy masses, concretions, stalactites, or coatings.
Cleavage
None, due to its amorphous or cryptocrystalline nature.
Geological Environment
Common in oxidized zones of iron ore deposits, gossans, bog iron deposits, lateritic soils, and as a weathering product of iron-bearing minerals in sedimentary and metamorphic rocks. Forms in both terrestrial and aquatic environments where iron-rich solutions are exposed to oxygen.

Key Facts

  • Hardness: 4 to 5.5 on the Mohs scale (variable due to its composite nature)
  • Specific Gravity: 2.7 to 4.3 (variable, depending on composition and porosity)
  • Crystal System: Amorphous or cryptocrystalline (no defined crystal system)
  • Color: Yellow-brown, reddish-brown, dark brown, black
  • Luster: Earthy, dull, sometimes submetallic
  • Transparency: Opaque
  • Fracture: Conchoidal, uneven, earthy
  • Cleavage: None
  • Composition: Hydrated iron oxides, primarily goethite (FeO(OH)) and lepidocrocite (γ-FeO(OH)), with variable water content and impurities.

Quick Check

  • Color: Yellow-brown to dark brown
  • Luster: Earthy, dull
  • Streak: Yellowish-brown

Physical Characteristics

  • Crystal Habit: Massive, earthy, botryoidal, mammillary, stalactitic, concretionary, pisolitic, oolitic, reniform, coatings.
  • Cleavage Type: None
  • Fracture Type: Conchoidal, uneven, earthy
  • Tenacity: Brittle to friable
  • Luster Type: Earthy, dull, sometimes submetallic

Formation

Limonite forms as a secondary mineral through the weathering and oxidation of primary iron-bearing minerals (e.g., pyrite, siderite, magnetite, hematite) in the presence of water and oxygen. It is a common component of gossans (iron-rich caps over sulfide ore bodies), bog iron deposits, and lateritic soils.

Usage

Historically, limonite was a significant ore of iron. Today, its primary uses are as a pigment (ochre) in paints, ceramics, and cosmetics, and occasionally as a low-grade iron ore. It is also used in some water purification processes due to its adsorptive properties.

Age Distribution

Forms in various geological settings throughout Earth's history, often associated with weathering processes.

Where to Find

Mesabi Range, Minnesota, USA

Known for extensive iron ore deposits, including significant limonite occurrences in the oxidized zones.

Krivoy Rog, Ukraine

Major iron ore district with abundant limonite as a weathering product.

Lorraine, France

Historically significant iron ore region where limonite was a primary ore.

Various bog iron deposits worldwide

Found in swamps, bogs, and shallow lakes where iron-rich groundwater precipitates hydrated iron oxides.

Lateritic soils in tropical and subtropical regions

Common component of highly weathered soils, often forming iron-rich crusts.

Finding Tips

Look for Iron-Rich Environments

Search in areas with known iron ore deposits, gossans (weathered sulfide deposits), or where iron-bearing rocks are exposed to weathering.

Identify Bog Iron Deposits

Explore bogs, swamps, and shallow lake beds, particularly in temperate regions, where limonite can precipitate as concretions or layers.

Check for Yellow-Brown Staining

Limonite often forms as a stain or coating on other rocks and minerals, indicating the presence of iron oxidation.

Observe Earthy Texture

Its characteristic earthy, dull luster and often porous or concretionary forms are key identifiers.

Similar Rocks

Goethite

FeO(OH)

Also known as: Alpha-FeOOH

Lepidocrocite

γ-FeO(OH)

Also known as: Gamma-FeOOH

Hematite

Fe2O3

Also known as: Red Iron Ore

Jarosite

KFe3(SO4)2(OH)6

Also known as: Potassium Iron Sulfate Hydroxide

Scientific Classification

Mineral Class
Oxides and Hydroxides (specifically a mineraloid composed of hydrated iron oxides)
Group
Iron Hydroxides
Crystal System
Amorphous or cryptocrystalline
Chemical Formula
FeO(OH)·nH2O (generalized, representing a mixture)
Composition
Hydrated iron oxides, predominantly goethite and lepidocrocite, with variable water content and impurities such as silica, clay minerals, and manganese oxides.

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