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Glaciated till plains, also known as glacial till plains, are typically found in regions that were historically covered by ice sheets, such as parts of North America, Europe, and Asia. In the United States, notable examples include areas in the Midwest, particularly in states like Wisconsin, Minnesota, and Michigan. These plains are characterized by a mix of clay, silt, sand, and gravel deposited by melting glaciers, forming a flat or gently rolling landscape.

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