sedimentary

Ironstone Concretion (Limonite/Goethite)

Goethite-rich Concretion (FeO(OH))

Hardness: 5-5.5 (Mohs scale); Color: Dark brown to rusty orange-brown; Luster: Dull to sub-metallic; Crystal Structure: Orthorhombic (microcrystalline); Cleavage: None; Specific Gravity: Approx. 3.3 - 4.3.

Hardness: 5-5
Color: Dark brown to rusty orange-brown
Luster: Dull to sub-metallic

Identified April 19, 2026More sedimentary →

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Physical properties

Formation & geological history

Formed by the precipitation of iron oxide minerals within the pore spaces of sedimentary rock (usually sandstone or shale). These often form as chemical precipitates from groundwater. Geological age varies widely from Paleozoic to Recent.

Uses & applications

Primarily collected as geological curiosities; historically used as a low-grade iron ore. In some regions, they are sold as 'Prophecy Stones' or 'Moqui Marbles' in metaphysical shops.

Geological facts

These are often mistaken for meteorites due to their dark, heavy appearance and 'bubbled' or botryoidal surface texture. They are actually internal structural features of sedimentary rocks that are harder than the surrounding stone.

Field identification & locations

Identify by its high density relative to other rocks, rusty streak (yellow-brown), and botryoidal (grape-like) or nodular surface. Often found in eroded desert landscapes or exposed sandstone cliffs.

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Sandstone or Siltstone

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Shale or Slaty Mudstone

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Sandstone

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