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The Kankakee River Basin drains 2,989 square miles (7,740 km 2) in northwest Indiana, 2,169 square miles (5,620 km 2) in northeast Illinois, and about seven square miles (18 km 2) in southwest Lower Michigan. The Kankakee River heads near South Bend, then flows westward into Illinois, where it joins with the Des Plaines River to form the Illinois.
Kankakee River State Park is an Illinois state park on 4,000 acres (1,619 ha) primarily in Kankakee and Will Counties, Illinois, United States. Originally, 35 acres (14 ha) of land was donated by Ethel Sturges Dummer for the creation of the state park in 1938.
In the northwest part of the state, it includes the Grand Calumet River area in Lake and Porter counties, and includes the cities of Gary and Hammond. This watershed is defined by the Valparaiso Moraine. The second, and larger Lake Michigan watershed is the St. Joseph River watershed, which drains the north central and northeastern part of the ...
Kankakee River Plain; [6] - The largest unit of outwash is along the Kankakee River from South Bend to the Illinois border. It is 15 miles (24 km) to 20 miles (32 km) wide including the Kankakee Marsh and the surrounding sand and gravel plains. [4] Tippicanoe- Iroquois plain - The next largest unit is along the Tippecanoe River in Fulton County.
Because of this, the river has cut through the rock, forming a gorge, most of which is in the state park. A trail in the park follows the creek. A trail in the park follows the creek. The Rock Creek waterfall is approximately 1.5 miles (2.4 km) upstream from the main entrance of the state park and is on land owned by Camp Shaw-waw-nas-see, a ...
Devonian stratigraphic column. The basin is bordered on the northeast by the Kankakee Arch, on the southeast by the Cincinnati Arch, on the south by the Pascola Arch, on the southwest by the Ozark Dome, on the northwest by the Mississippi River Arch, and on the north by the Wisconsin Arch.
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Lake Kankakee formed 14,000 years before present (YBP) in the valley of the Kankakee River. It developed from the outwash of the Michigan Lobe, Saginaw Lobe, and the Huron-Erie Lobe of the Wisconsin glaciation .