
sedimentary
Limonite Concretion (Ironstone)
Limonite / Goethite (FeO(OH)·nH2O)
Hardness: 4-5.5 (Mohs); Color: Dark brown to yellow-brown or reddish; Luster: Dull to earthy; Crystal Structure: Amorphous or cryptocrystalline; Cleavage: None; Specific Gravity: 2.7–4.3.
- Hardness
- 4-5
- Color
- Dark brown to yellow-brown or reddish
- Luster
- Dull to earthy
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Physical properties
Hardness: 4-5.5 (Mohs); Color: Dark brown to yellow-brown or reddish; Luster: Dull to earthy; Crystal Structure: Amorphous or cryptocrystalline; Cleavage: None; Specific Gravity: 2.7–4.3.
Formation & geological history
Formed by the precipitation of iron oxides/hydroxides from groundwater within sedimentary rock layers, often as nodules or concretions in sandstone or shale. They can form over thousands to millions of years.
Uses & applications
Historically used as a low-grade iron ore. Today, used primarily for educational specimens, aquascaping, and as earth-tone pigments (ochre).
Geological facts
Limonite is not a true mineral but a mixture of hydrated iron oxide minerals. These rounded nodules are sometimes called 'shaman stones' or 'Moqui marbles' in specific regions like the Southwestern USA.
Field identification & locations
Identify in the field by its high density (heavy for its size), rusty streak when scratched, and characteristic pitted or rounded 'nodular' surface. Commonly found in eroded sedimentary basins.
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