
mineral
Iron-rich weathered rock (probable limonite/goethite)
Limonite, a mixture dominated by goethite (FeO(OH)) and related hydrated iron oxides
AI-generated identification · may be incorrectEarthy brown to rusty orange, dull to submetallic luster, irregular massive texture, and no obvious cleavage; approximate Mohs hardness 4–5.5, with typically high specific gravity around 3.3–4.3. The image alone cannot confirm mineral identity or distinguish it from ironstone.
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Physical properties
Earthy brown to rusty orange, dull to submetallic luster, irregular massive texture, and no obvious cleavage; approximate Mohs hardness 4–5.5, with typically high specific gravity around 3.3–4.3. The image alone cannot confirm mineral identity or distinguish it from ironstone.
Formation & geological history
Forms through intense weathering and oxidation of iron-bearing rocks or sulfide deposits, commonly accumulating in soils, cavities, and gossans; generally a modern-to-geologically ancient weathering product rather than a single-age rock.
Uses & applications
Used historically as an iron ore and earth pigment; attractive botryoidal or sharply textured pieces are collected, but this rough specimen has limited commercial value.
Geological facts
Limonite is not a single definitive mineral species but a field term for poorly crystalline hydrated iron oxides. Goethite-rich material may develop yellow-brown streaks and can occur with hematite and quartz.
Field identification & locations
Common in oxidized ore zones worldwide, including Australia, Brazil, the United States, and Europe. A yellow-brown to reddish-brown streak, strong heft, and possible attraction to a magnet help identification; acid and laboratory tests are more diagnostic.
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