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| | ch_4sast |
 | | Hydric soils in the basin occur as depressions (potholes) in young, late Wisconsinan-age glacial, closed drainage landscapes of the Dakotas, Minnesota, Iowa, and Illinois; in depressional areas on wide interfluve areas of southern Iowa and Illinois and northern Missouri; and in backland and backswamp areas on floodplains. |
 | | The highest concentration of hydric soils in the basin is in the floodplains of the Missouri and Mississippi Rivers and in the glacial pothole and depressional (closed drainage) areas of central Iowa, southern Minnesota, the northern half of Indiana, and central and northeastern Illinois. |
 | | Wetlands in the upland areas of the basin are discussed with respect to changes in wetlands from presettlement to the present, to their value for biodiversity and for water quality, and to their potential use for flood redirection in the basin. |
| edcwww.cr.usgs.gov /sast/www/ch_4sast.htm (5508 words) |
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