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The southern A part of the Central Lowland is kind of different, coated largely with loess (wind-deposited silt) that further subdued the currently lower relief surface. Somewhere else, especially close to key rivers, postglacial streams carved the loess into rounded hills, and visitors have aptly in comparison their billowing designs https://berita-viral89899.wikipowell.com/4255424/usa_info_secrets


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