
sedimentary
Ironstone concretion (probable hematite–goethite-rich ironstone)
Iron oxide/hydroxide concretion; chiefly hematite (Fe₂O₃) and goethite (FeO(OH)), with possible magnetite and quartz
AI-generated identification · may be incorrectHardness about 5–6.5 Mohs; dark brown to rusty red, earthy to submetallic luster, dense and fine-grained, with rounded weathering pits and little or no cleavage. Its heavy feel and possible weak magnetism support an iron-rich composition.
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Physical properties
Hardness about 5–6.5 Mohs; dark brown to rusty red, earthy to submetallic luster, dense and fine-grained, with rounded weathering pits and little or no cleavage. Its heavy feel and possible weak magnetism support an iron-rich composition.
Formation & geological history
Formed when iron-bearing minerals precipitated and cemented sediment around nuclei, commonly in ancient river, lake, or shallow marine deposits; later weathering concentrated the iron. Exact geological age cannot be determined from the image.
Uses & applications
Used historically as iron ore when sufficiently rich; otherwise it is mainly a common field specimen, landscaping stone, or lapidary material. It has limited jewelry value unless polished and attractively patterned.
Geological facts
The porous, knobby surface is typical of ironstone concretions or weathered iron-rich nodules, not necessarily a meteorite. A reddish-brown streak and high density are characteristic of hematite/goethite.
Field identification & locations
Common in sedimentary terrains and gravel bars worldwide, including Australia, North America, India, and Africa. Test with an unglazed porcelain streak plate, magnet, and specific-gravity comparison; identification remains approximate without testing.
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