sedimentary

Ironstone (Limonitic Sandstone)

Ferruginous Sandstone (rich in Limonite: FeO(OH)·nH2O)

AI-generated identification · may be incorrect

Hardness: 4-5.5 on Mohs scale; Color: Rusty brown, orange, and dark grey; Luster: Dull/Earthy; Crystal Structure: Amorphous/Microcrystalline (as part of matrix); Specific Gravity: 2.7-4.3 (variable based on iron content)

Hardness: 4-5
Color: Rusty brown, orange, and dark grey
Luster: Dull/Earthy

Identified April 17, 2026More sedimentary →

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Physical properties

Formation & geological history

Formed through the deposition of iron-rich sediments or the chemical precipitation of iron oxides within porous sandstone. Often occurs as concretions or Bog Iron in swampy, oxygen-rich environments where groundwater interacts with iron minerals.

Uses & applications

Historically used as a low-grade iron ore. Today, used primarily in road construction (crushed stone), as landscaping rocks, and occasionally in the pigments industry (ochre).

Geological facts

Ironstone often forms 'concretions' that can look like fossils or extraterrestrial objects (meteor-wrongs). It was a vital resource for early iron smelting during the Industrial Revolution before higher-grade ores were discovered.

Field identification & locations

Identify by its characteristic rust-orange surface oxidation and high density compared to standard sandstone. It will usually leave a yellow-brown streak on a porcelain plate and is rarely magnetic unless it contains magnetite.