
sedimentary
Limonite Geode / Ironstone Concretion
Hydrated Iron Oxide (FeO(OH)·nH2O)
Hardness 4-5.5 on Mohs scale, earthy to submetallic luster, rusty orange-brown to dark brown exterior and interior, amorphous/microcrystalline structure, dense and heavy, earthy fracture.
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Physical properties
Hardness 4-5.5 on Mohs scale, earthy to submetallic luster, rusty orange-brown to dark brown exterior and interior, amorphous/microcrystalline structure, dense and heavy, earthy fracture.
Formation & geological history
Formed by the precipitation of iron oxide minerals from aqueous solutions around a nucleus or within cavities in sedimentary rocks, creating a hollow or secondary mineral-filled concretion over millions of years.
Uses & applications
Primarily collected as geological curiosities and mineral specimens; historically used as a minor iron ore source and mineral pigment (ochre).
Geological facts
Ironstone geodes are often colloquially referred to as 'rattle stones' or 'etites' when a small loose piece inside creates a rattling sound when shaken. Historically, they were believed to have magical or medicinal properties.
Field identification & locations
Identified by its distinctive spherical or nodular form, thick rusty crust, reddish-brown streak, and hollow interior filled with iron-rich earthy masses or small crystals. Commonly found in sedimentary deposits in the US Midwest, Europe, and Australia.
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