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Where is Iron-rich concretion found?

Goethite/Limonite concretion

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Iron-rich concretion occurs in specific geological environments. Knowing where to look, and in what kind of rock, is the difference between going home empty-handed and finding a great specimen.

Where to find Iron-rich concretion

Midwestern United States

Abundant in Cretaceous sandstones (e.g., Dakota Formation) and glacial tills, often weathering out as 'ironstone concretions' or 'Indian paint pots'.

Utah, USA

Famous for 'Moqui Marbles' (Navajo Sandstone concretions), which are iron-rich concretions with a hematite-rich outer shell and sandstone core.

England

Common in Jurassic and Cretaceous sedimentary rocks, such as the Dogger Formation and various clay formations.

Australia

Widespread in lateritic soils and weathered profiles, forming 'ironstone gravels' or 'ferricretes'.

Worldwide

Found globally in diverse sedimentary basins and soil profiles where conditions for iron precipitation exist.

Collecting tips

  1. Look in weathered sedimentary outcrops. Concretions are often more resistant to weathering than the surrounding host rock, causing them to stand out or erode free.
  2. Check stream beds and gravel pits. Eroded concretions can accumulate in these areas, especially if the source rock is nearby.
  3. Examine soil profiles. In some regions, iron-rich concretions (e.g., bog iron, lateritic nodules) form directly within soils.
  4. Note the host rock type. Concretions are common in sandstones, shales, and limestones. Understanding the local geology can guide your search.

Quick Check

Color:
Brown, yellow, reddish-brown
Luster:
Dull, earthy, sub-metallic
Streak:
Yellowish-brown to brownish-yellow (for goethite/limonite)

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