Image:Iron bearing water in a spring.jpg

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Picture of typical iron-bearing ground water emerging as a spring. The iron is oxidized to ferric hydroxide upon encountering the oxic environment of the surface. A large number of these springs and seeps on the flood plain provide the iron for bog iron deposits.

Obtained from http://pubs.usgs.gov/of/2003/of03-346/f5.htm Last modified: 14:38:53 Thu 02 Oct 2003

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current02:33, 24 June 2006395×300 (31 KB)Rifleman 82 (Talk | contribs) (Picture of typical iron-bearing ground water emerging as a spring. The iron is oxidized to ferric hydroxide upon encountering the oxic environment of the surface. A large number of these springs and seeps on the flood plain provide the iron for bog iron d)

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