File:Iron bearing water in a spring.jpg
Iron_bearing_water_in_a_spring.jpg (395 × 300 pixels, file size: 31 KB, MIME type: image/jpeg)
Summary
[edit]| Description |
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. | ||
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| Source |
Obtained from http://pubs.usgs.gov/of/2003/of03-346/f5.htm | ||
| Date |
Last modified: 14:38:53 Thu 02 Oct 2003 | ||
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Licensing
[edit] | This image is a work of a United States Geological Survey employee, taken or made as part of that person's official duties. As a work of the United States Government, the image is in the public domain in the US. For more information, see the USGS copyright policy. See Wikipedia:Public domain and Wikipedia:Copyrights for more details. |  |
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File history
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
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| current | 02:33, 24 June 2006 | | 395 × 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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