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  2. Geography of Iowa - Wikipedia

    en.wikipedia.org/wiki/Geography_of_Iowa

    Barringer Slough, a remnant of the extensive prairie wetlands that once covered the Des Moines Lobe. Often called the Prairie Pothole Region, the Des Moines Lobe was glaciated up until 12,000 years ago during the Wisconsin glaciation. The area is marked by rolling terrain and ridges. [20]

  3. Glacial history of Minnesota - Wikipedia

    en.wikipedia.org/wiki/Glacial_history_of_Minnesota

    The subsequent glacier that moved into Minnesota was quite thin and unable to cause much erosion. The Des Moines lobe produced a northeast-moving projection known as the Grantsburg sublobe. Also protruding from the main Keewatin ice sheet was the St. Louis sublobe. The drift of these ice lobes is generally in late Wisconsin time.

  4. Western Corn Belt Plains - Wikipedia

    en.wikipedia.org/wiki/Western_Corn_Belt_Plains

    The Iowan Surface ecoregion is a geologically complex region located between the bedrock-dominated landforms of the Paleozic Plateau/Coulee Section (52b) and the relatively recent glacial drift landforms of the Des Moines Lobe (47b).

  5. Driftless Area - Wikipedia

    en.wikipedia.org/wiki/Driftless_Area

    43°30′N91°00′W43.5°N 91°W The Driftless Area, also known as Bluff Country and the Paleozoic Plateau, is a topographical and cultural region in the Midwestern United States [ 1 ] that comprises southwestern Wisconsin, southeastern Minnesota, northeastern Iowa, and the extreme northwestern corner of Illinois. The Driftless Area is a USDA ...

  6. Environment of Iowa - Wikipedia

    en.wikipedia.org/wiki/Environment_of_Iowa

    The Des Moines lobe, a remnant of the extensive prairie wetlands that once covered the Des Moines Lobe. Often called the Prairie Pothole Region, the Des Moines Lobe was glaciated up until 12,000 years ago during the Wisconsin glaciation. The area is marked by rolling terrain and ridges.

  7. Archaeology of Iowa - Wikipedia

    en.wikipedia.org/wiki/Archaeology_of_Iowa

    At the time the state was covered by tundra, conifer forests, and deciduous forests. Areas immediately north of Des Moines extending to Minnesota were covered by the receding Des Moines Lobe, a large glacier system. Highly mobile, their sites are scattered across Iowa and are noted for their large stone points.

  8. Coteau des Prairies - Wikipedia

    en.wikipedia.org/wiki/Coteau_des_Prairies

    Coteau des Prairies. Coordinates: 44.0000°N 96.3167°W. The Coteau des Prairies: blue arrows indicate paths of the two lobes of the glacier around either side of the formation. This excerpt from the Lewis and Clark map of 1814 shows the rivers of western Iowa and eastern South Dakota. The Coteau des Prairies is seen near the upper center of ...

  9. Iowa Great Lakes - Wikipedia

    en.wikipedia.org/wiki/Iowa_Great_Lakes

    The Iowa Great Lakes, often referred to as Okoboji, [1] is a group of natural lakes in northwestern Iowa in the United States. There are seven lakes in the region totaling 12,687 acres (5,134 ha) [2] with the three principal lakes of the group being Big Spirit Lake, [3] West Okoboji Lake, [4] and East Okoboji Lake. [5][6] They are the largest ...