sedimentary

Ironstone (with Limonite/Goethite)

Ferruginous Sedimentary Rock (contains Limonite FeO(OH)·nH2O and Hematite Fe2O3)

Hardness: 4-5.5 on Mohs scale. Color: Dark brown, reddish-brown to rusty yellowish. Luster: Dull, earthy to sub-metallic. Crystal structure: Amorphous or microcrystalline. Cleavage: None. Specific gravity: High (heavy for its size).

Hardness: 4-5
Color: Dark brown, reddish-brown to rusty yellowish
Luster: Dull, earthy to sub-metallic

Identified April 26, 2026More sedimentary →

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Physical properties

Formation & geological history

Formed by the chemical precipitation of iron minerals from water or the weathering of iron-rich mineral deposits. Common in bog environments, marine shelf settings, or as late-stage oxidation of sulfide ores.

Uses & applications

Historically used as an ore of iron. Currently used as road aggregate, in cement manufacturing, and occasionally as structural stone or garden landscaping.

Geological facts

Ironstone nodules often contain fossils or unique internal structures called septarian cracks. It is heavily associated with 'iron age' industrial history in regions like the UK and Great Britain.

Field identification & locations

Identify by its distinctive heavy weight (density), rusty outward appearance, and reddish-brown streak when rubbed against unglazed porcelain. Commonly located in sedimentary basins and near mining tailings.

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