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The interior plains were primarily formed through a combination of geological processes, including sedimentation, erosion, and glacial activity. Over millions of years, ancient seas deposited sediments that compacted into sedimentary rock, while later erosion shaped the landscape. Glacial activity during the last Ice Age also played a significant role by flattening the terrain and creating the characteristic features of the plains. As a result, the interior plains are characterized by broad, flat expanses with fertile soil, ideal for agriculture.

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3mo ago

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