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	<title>Dissected Till Plains - Revision history</title>
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	<updated>2026-04-22T08:17:52Z</updated>
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	<entry>
		<id>https://wikimd.com/index.php?title=Dissected_Till_Plains&amp;diff=5887507&amp;oldid=prev</id>
		<title>Prab: CSV import</title>
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		<updated>2024-06-05T21:11:43Z</updated>

		<summary type="html">&lt;p&gt;CSV import&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;[[File:US_physiographic_regions_map.jpg|thumb|US_physiographic_regions_map]] &amp;#039;&amp;#039;&amp;#039;Dissected Till Plains&amp;#039;&amp;#039;&amp;#039; are a geographical region characterized by rolling hills and valleys formed by the erosion of glacial till. This region is primarily found in the central United States, particularly in states such as [[Iowa]], [[Nebraska]], [[Missouri]], and [[Kansas]]. The landscape is a result of the last glacial period, where the retreating glaciers left behind a thick layer of till, which was subsequently eroded by water and wind.&lt;br /&gt;
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==Geography==&lt;br /&gt;
The Dissected Till Plains are part of the larger [[Interior Plains]] of North America. The region is bounded by the [[Central Lowlands]] to the east and the [[Great Plains]] to the west. The topography is characterized by gently rolling hills, deep river valleys, and fertile soils, making it an important area for agriculture.&lt;br /&gt;
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==Formation==&lt;br /&gt;
The formation of the Dissected Till Plains began during the [[Pleistocene Epoch]] when glaciers advanced and retreated over the region. As the glaciers melted, they deposited a mixture of clay, silt, sand, gravel, and boulders known as till. Over time, streams and rivers cut through the till, creating the dissected landscape seen today.&lt;br /&gt;
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==Climate==&lt;br /&gt;
The climate of the Dissected Till Plains is typically [[humid continental]], with hot summers and cold winters. Precipitation is relatively evenly distributed throughout the year, supporting a variety of vegetation and agricultural activities.&lt;br /&gt;
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==Flora and Fauna==&lt;br /&gt;
The region supports a diverse range of plant and animal life. Native vegetation includes tallgrass prairies, oak-hickory forests, and riparian woodlands. Common wildlife includes [[white-tailed deer]], [[wild turkey]], and various species of songbirds and small mammals.&lt;br /&gt;
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==Agriculture==&lt;br /&gt;
The fertile soils of the Dissected Till Plains make it one of the most productive agricultural regions in the United States. Major crops include [[corn]], [[soybeans]], and [[wheat]]. Livestock farming, particularly cattle and hogs, is also prevalent.&lt;br /&gt;
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==Human Settlement==&lt;br /&gt;
The Dissected Till Plains have been inhabited by humans for thousands of years. Native American tribes such as the [[Omaha]], [[Iowa]], and [[Missouri]] lived in the region before European settlement. Today, the area is home to numerous towns and cities, with [[Omaha, Nebraska]] and [[Des Moines, Iowa]] being among the largest urban centers.&lt;br /&gt;
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==Related Pages==&lt;br /&gt;
* [[Interior Plains]]&lt;br /&gt;
* [[Central Lowlands]]&lt;br /&gt;
* [[Great Plains]]&lt;br /&gt;
* [[Pleistocene Epoch]]&lt;br /&gt;
* [[Humid continental climate]]&lt;br /&gt;
* [[Tallgrass prairie]]&lt;br /&gt;
* [[Agriculture in the United States]]&lt;br /&gt;
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==Categories==&lt;br /&gt;
[[Category:Geography of the United States]]&lt;br /&gt;
[[Category:Plains of North America]]&lt;br /&gt;
[[Category:Glacial landforms]]&lt;br /&gt;
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{{Geography-stub}}&lt;/div&gt;</summary>
		<author><name>Prab</name></author>
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