sedimentary

Ironstone Concretion

Siderite or Limonite Concretion

AI-generated identification · may be incorrect

Hardness: 4-5.5 on Mohs scale; Color: Brown, yellowish-brown, to rusty black; Luster: Dull to earthy; Crystal Structure: Amorphous or microcrystalline; Cleavage: None; Specific Gravity: 3.0-3.9.

Hardness: 4-5
Color: Brown, yellowish-brown, to rusty black
Luster: Dull to earthy

Identified April 13, 2026More sedimentary →

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Physical properties

Hardness: 4-5.5 on Mohs scale; Color: Brown, yellowish-brown, to rusty black; Luster: Dull to earthy; Crystal Structure: Amorphous or microcrystalline; Cleavage: None; Specific Gravity: 3.0-3.9.

Formation & geological history

Formed by the precipitation of iron-rich minerals (like siderite, hematite, or limonite) around a nucleus in sedimentary rock layers. This often occurs shortly after sediment deposition in marsh, river, or coastal environments.

Uses & applications

Historical source of low-grade iron ore; used as decorative garden stones; often collected by hobbyists for their odd, 'alien-egg' shapes.

Geological facts

Concretions are often mistaken for meteorites or dinosaur eggs due to their heavy weight and rounded shapes. They sometimes hold well-preserved fossils at their center.

Field identification & locations

Identify by its rounded, nodular shape, high density (it feels heavy for its size), and rusty appearance. Commonly found in eroded creek beds or sandstone/shale formations.