sedimentary

Ironstone (Limonitic Shale)

Ferruginous Siltstone / Goethite-rich Sedimentary Rock

AI-generated identification · may be incorrect

Hardness: 4.0-5.5 (Mohs scale); Color: Reddish-brown, ochre, rusty orange; Luster: Dull to earthy; Crystal Structure: Amorphous/massive; Cleavage: None (conchoidal or irregular fracture); Specific Gravity: 3.3-4.3

Hardness: 4
Color: Reddish-brown, ochre, rusty orange
Luster: Dull to earthy

Identified May 13, 2026More sedimentary →

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Physical properties

Formation & geological history

Formed by the precipitation of iron oxides (hematite, goethite, limonite) within sedimentary layers, often in marine or swampy environments where iron-rich waters react with oxygen. Typically from the Paleozoic or Mesozoic eras.

Uses & applications

Historically used as a low-grade iron ore; currently used as construction aggregate, road base, and occasionally in landscape design or as a source of natural pigments (ochre).

Geological facts

Ironstone was a primary source of iron for the early industrial revolution in parts of Europe and the United Kingdom. Oxidation gives it its characteristic 'rusty' appearance.

Field identification & locations

Identify by its heavy weight (high specific gravity) compared to other rocks, its distinct rusty streak when rubbed on porcelain, and its common association with shale or sandstone beds. Found worldwide in iron-rich geological basins.