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.[1]
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 accumualtion 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.
Cartography·Geographic Information Systems (GIS)·Geostatistics·Global Positioning System (GPS)·Remote sensing·Spatial analysis·Qualitative research
Societies
American Geographical Society·Association of American Geographers·European Geography Association·Geographical Association·Hong Kong Geographical Association·International Geographical Union·National Geographic Society·Royal Canadian Geographical Society·Royal Geographical Society·Royal Scottish Geographical Society·Russian Geographical Society·Saudi Geographical Society·Société de Géographie·Society of Woman Geographers
Geographers
Ptolemy·Gerardus Mercator·Carl Ritter·Alexander Von Humboldt·Alfred Russel Wallace·Richard Chorley
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