Dissected Till Plains
The Dissected Till Plains are physiographic sections of the Central Lowlands province, which in turn is part of the Interior Plains physiographic division of the United States, located in southern and western Iowa, northeastern Kansas, the southwestern corner of Minnesota, northern Missouri, eastern Nebraska, and southeastern South Dakota. The Dissected Till Plains were formed by pre-Wisconsin glaciations during the Pre-Illinoian Stage. Glacial scouring and deposition by the Laurentide Ice Sheet and the later accumulation of loess during the Wisconsin Stage left behind the rolling hills and rich, fertile soils found today in the region. The  region is also the western edge of the Corn Belt. Geology. As a part of the Central Lowland geomorphic province. It is a glacier till plain from flat to rolling plain that slopes towards either the Missouri or Mississippi rivers. It is moderately dissected. Local relief is . The region is pocketed by small human landform, i.e., strip-mines among a hummocky or ridge-swale topography. Streams drain and erode the area, moving soils and depositing them downstream. Elevation ranges from . Loess (unconsolidated aeolian silt), as much as thick thins toward the east, covers most uplands. Pleistocene (pre-Illinoisan) till lies  beneath the loess, covering the bedrock up to deep. Along the edges, it thins to less than . The Mississippi and Missouri floodplains have up to of unconsolidated Tertiary and Quaternary alluvium (gravel, sand, silt, and clay) over the bedrock, thinner in the river valleys. Bedrock appears along the margins. Cretaceous shale and sandstone occur in the northwestern corner, the Nebraska, Minnesota and Iowa boundary section. Permian sandstone is along the western margin or the Missouri Valley. Pennsylvanian shale, limestone, and coal is beneath nearly the entire geologic unit. Mississippian, Devonian and Ordovician shale and carbonate are the bedrock along the  eastern and southern areas. Bedrock is visible along the deeper drainage's and in eroded "windows" of the unconsolidated surface soils. Geography. The Dissected Till Plains is a sub-unit of the Central Lowlands in the Interior Plains of North America. It is centered on the Iowa-Missouri state line. The eastern border is the Mississippi River and bounded on the south by the Missouri River Valley across central Missouri. Its western boundary is about west of the Missouri Rivers border along the Kansas/Missouri – Nebraska/Iowa state line. Its northern border is a line dipping from the Sioux River  valley of South Dakota and Minnesota, south into Iowa along a line demarking the Missouri valley from the interior lowlands of Iowa, then curving northward again on a line demarking the interior lowlands of Iowa, from the Mississippi River valley on the east.