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Iron ore, in the context of Limonite and Goethite with a primary iron mineral core, refers to an aggregate of iron oxyhydroxide minerals, predominantly Goethite (α-FeO(OH)) and Limonite (a field term for a mixture of hydrated iron oxides, often including Goethite, Lepidocrocite, and amorphous ferrihydrite), which have formed from the alteration of primary iron minerals. These ores are characterized by their typically earthy, yellowish-brown to dark brown colors and often exhibit botryoidal, stalactitic, or concretionary habits. They are significant sources of iron, particularly in younger, surficial deposits.
How to Identify
- Color
- Yellowish-brown, reddish-brown, dark brown, or black. The streak is typically yellowish-brown to brown.
- Luster
- Earthy, dull, submetallic, or silky (fibrous varieties).
- Texture
- Often earthy, porous, botryoidal, stalactitic, mammillary, or concretionary. Can be massive or fibrous.
- Crystal Form
- Goethite forms acicular, prismatic, or tabular crystals, often radiating. Limonite is typically amorphous or cryptocrystalline, forming botryoidal, stalactitic, or earthy masses. The primary iron mineral core (e.g., magnetite, hematite) would retain its characteristic crystal form if unweathered.
- Cleavage
- Goethite has perfect cleavage on {010} and good cleavage on {100}. Limonite, being a mixture, generally lacks distinct cleavage and exhibits irregular fracture.
- Geological Environment
- Found in gossans (oxidized caps of sulfide ore deposits), bog iron deposits, lateritic soils, and as weathering products in sedimentary and metamorphic iron formations. Often associated with zones of intense chemical weathering.
Key Facts
- Hardness: Goethite: 5-5.5 on Mohs scale. Limonite: Variable, typically 4-5.5 (due to its mixed nature and porosity).
- Specific Gravity: Goethite: 3.3-4.3. Limonite: Variable, typically 2.7-4.3 (lower if very porous).
- Crystal System: Goethite: Orthorhombic. Limonite: Amorphous to cryptocrystalline (no defined crystal system).
- Color: Yellowish-brown, reddish-brown, dark brown, black.
- Luster: Earthy, dull, submetallic, silky.
- Transparency: Opaque.
- Fracture: Goethite: Uneven to subconchoidal. Limonite: Earthy, irregular.
- Cleavage: Goethite: Perfect on {010}, good on {100}. Limonite: None.
- Composition: Goethite: Hydrous iron oxide, α-FeO(OH). Limonite: A mixture of hydrated iron oxides, primarily Goethite, Lepidocrocite (γ-FeO(OH)), and ferrihydrite (Fe5HO8·4H2O), often with adsorbed water and impurities. The 'core of a primary iron mineral' implies the presence of unweathered or partially weathered magnetite (Fe3O4), hematite (Fe2O3), or siderite (FeCO3).
Quick Check
- Color: Yellowish-brown to dark brown
- Luster: Earthy to dull
- Streak: Yellowish-brown to brown
Physical Characteristics
- Crystal Habit: Goethite: Acicular, prismatic, tabular, radiating, botryoidal, stalactitic, massive. Limonite: Earthy, massive, botryoidal, mammillary, concretionary.
- Cleavage Type: Goethite: Perfect {010}, good {100}. Limonite: Absent.
- Fracture Type: Goethite: Uneven to subconchoidal. Limonite: Earthy, irregular.
- Tenacity: Goethite: Brittle. Limonite: Brittle to friable.
- Luster Type: Earthy, dull, submetallic, silky.
Formation
Limonite and Goethite are secondary iron oxyhydroxide minerals formed through the weathering and oxidation of primary iron-bearing minerals (e.g., pyrite, siderite, magnetite, hematite) in various geological environments. This often occurs in the upper, oxidized zones of ore deposits (gossans), in bog environments, or as lateritic weathering products in tropical and subtropical regions. The 'core of a primary iron mineral' refers to the common occurrence where these secondary minerals form as alteration products around unweathered or partially weathered primary iron minerals.
Usage
The primary use of iron ore is in the production of iron and steel. It is also used as a pigment (ochre), in heavy media separation, and as a weighting agent in drilling fluids.
Age Distribution
Found in geological formations ranging from Precambrian to Cenozoic, with significant deposits in Precambrian Banded Iron Formations (BIFs) and younger lateritic and bog iron deposits.
Where to Find
Mesabi Range, Minnesota, USA
Historically a major source of Limonite and Goethite derived from the weathering of Precambrian Banded Iron Formations.
Krivoy Rog, Ukraine
Significant deposits of weathered iron ores, including Limonite and Goethite, derived from Precambrian iron formations.
Minas Gerais, Brazil
Extensive lateritic iron ore deposits, rich in Goethite and Hematite, formed by intense tropical weathering.
Pilbara region, Western Australia
World-class iron ore deposits, primarily Hematite, but with significant occurrences of Goethite and Limonite as weathering products.
Bog iron deposits worldwide
Found in wetlands, swamps, and bogs where iron-rich groundwater precipitates iron oxyhydroxides.
Finding Tips
Look for weathered outcrops
Iron ore (Limonite/Goethite) often forms in the oxidized zones of other iron-rich deposits. Look for reddish-brown or yellowish-brown staining on rocks and soil.
Check for heavy samples
Despite their often porous appearance, iron ores are relatively dense. A sample that feels heavier than expected for its size is a good indicator.
Perform a streak test
The characteristic yellowish-brown to brown streak is a key diagnostic feature for Limonite and Goethite, distinguishing them from other iron minerals like Hematite (red streak) or Magnetite (black streak).
Examine geological maps
Consult geological maps for areas known to have iron formations, gossans, or lateritic soils. These are prime locations for finding Limonite and Goethite.
Observe morphology
Look for botryoidal, stalactitic, or earthy masses, which are common habits for these minerals.
Similar Rocks
Hematite
Hematite (Fe2O3)
Also known as: Red Iron Ore, Specularite
Magnetite
Magnetite (Fe3O4)
Also known as: Magnetic Iron Ore
Siderite
Siderite (FeCO3)
Also known as: Iron Carbonate
Pyrite
Pyrite (FeS2)
Also known as: Fool's Gold
Scientific Classification
- Mineral Class
- Oxides and Hydroxides
- Group
- Goethite is a member of the Diaspore group. Limonite is a field term for a mixture of hydrated iron oxides.
- Crystal System
- Goethite: Orthorhombic. Limonite: Amorphous to cryptocrystalline.
- Chemical Formula
- Goethite: α-FeO(OH). Limonite: FeO(OH)·nH2O (generalized, as it's a mixture).
- Composition
- Goethite is hydrous iron oxide. Limonite is a variable mixture of hydrous iron oxides, often including Goethite, Lepidocrocite, and ferrihydrite, with varying amounts of adsorbed water and impurities. The 'core' refers to the presence of primary iron minerals like magnetite or hematite.
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