
mineral
Iron-rich weathered stone, possibly hematite-rich ironstone
Hematite/goethite-bearing ironstone; predominantly Fe₂O₃ and FeO(OH)
AI-generated identification · may be incorrectDark reddish-brown, earthy to submetallic luster, smoothly water-worn surface with irregular pits and ridges; likely hardness about 5–6.5 Mohs and high specific gravity. Exact mineral identification requires a streak test and magnetism test.
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Physical properties
Dark reddish-brown, earthy to submetallic luster, smoothly water-worn surface with irregular pits and ridges; likely hardness about 5–6.5 Mohs and high specific gravity. Exact mineral identification requires a streak test and magnetism test.
Formation & geological history
Likely a naturally weathered and rounded iron-rich concretion or ironstone formed by oxidation and precipitation of iron minerals in soil, sediment, or hydrothermal environments; age cannot be determined from the photograph.
Uses & applications
Common ironstone is used as iron ore, pigment, and occasionally as a lapidary or display stone; this specimen has mainly decorative or collecting value.
Geological facts
Hematite produces a distinctive red-to-reddish-brown streak even when the exterior appears nearly black. Goethite-rich material may show yellow-brown streaks and stronger earthy texture.
Field identification & locations
Test an inconspicuous area: hematite streak is red-brown, goethite is yellow-brown, and magnetite gives a black streak and is strongly magnetic. Common sources include Australia, Brazil, India, and iron-rich sedimentary terrains worldwide.
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