sedimentary

Ironstone Concretion

Limonitic/Hematitic Concretion

AI-generated identification · may be incorrect

Hardness: 5.0 - 6.0; Color: Rusty brown, reddish-orange to dark grey; Luster: Dull/Earthy; Crystal Structure: Amorphous or Cryptocrystalline; Specific Gravity: 3.5 - 4.2

Hardness: 5
Color: Rusty brown, reddish-orange to dark grey
Luster: Dull/Earthy

Identified April 24, 2026More sedimentary →

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Physical properties

Hardness: 5.0 - 6.0; Color: Rusty brown, reddish-orange to dark grey; Luster: Dull/Earthy; Crystal Structure: Amorphous or Cryptocrystalline; Specific Gravity: 3.5 - 4.2

Formation & geological history

Formed by the precipitation of mineral cement (iron oxides) within the spaces between sediment grains, often around a nucleus like a shell or leaf. They typically form in sedimentary host rock layers like shale or sandstone over millions of years.

Uses & applications

Primarily collected as geological curiosities. In some contexts, ironstones have been used as a low-grade iron ore or used in rustic landscaping and construction.

Geological facts

Many concretions are mistaken for fossils, eggs, or meteorites due to their unusual symmetrical or nodular shapes. Historically, some cultures called them 'fairy stones' or 'shaman stones.'

Field identification & locations

Identify in the field by their rounded or odd shapes that differ from the surrounding bedding planes and their high density compared to adjacent rock. They often have concentric internal layers similar to an onion.