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The Mississippi River can be divided into three sections: the Upper Mississippi, the river from its headwaters to the confluence with the Missouri River; the Middle Mississippi, which is downriver from the Missouri to the Ohio River; and the Lower Mississippi, which flows from the Ohio to the Gulf of Mexico.
Itasca State Park (/ aɪ ˈ t æ s k ə /) is a state park of Minnesota, United States, and contains the headwaters of the Mississippi River.The park spans 32,690 acres (132.3 km 2) of northern Minnesota, and is located about 21 miles (34 km) north of Park Rapids, Minnesota and 25 miles (40 km) from Bagley, Minnesota.
Lake Itasca (/ aɪ ˈ t æ s k ə / eye-TASS-kə) [1] is a small glacial lake, approximately 4.7 square kilometres (470 hectares; 1,200 acres) in area.It is located in Itasca State Park, in south-eastern Clearwater County, in the Headwaters area of north-central Minnesota, and is notable for being the headwater of the Mississippi River.
The Mississippi River System, also referred to as the Western Rivers, is a mostly riverine network of the United States which includes the Mississippi River and connecting waterways. The Mississippi River is the largest drainage basin in the United States. [3] In the United States, the Mississippi drains about 41% of the country's rivers. [4]
HAER No. MN-21, "Upper Mississippi River 9-Foot Channel Project, Lock & Dam No. 3, Red Wing, Goodhue County, MN", 98 photos, 11 data pages, 7 photo caption pages HAER No. MN-22, " Upper Mississippi River 9-Foot Channel Project, Lock & Dam No. 5, Minneiska, Winona County, MN ", 92 photos, 11 data pages, 6 photo caption pages
The headwaters of the Mississippi River begin at Lake Itasca (see Mississippi River Basin map); where it flows through Winnibigoshish, the Mississippi is at its widest - more than 11 miles. [3] The former Winnibigoshish Township (now unorganized), located on the north shore of Lake Winnibigoshish, in Itasca County, Minnesota, was named after ...
Map of Mississippi River Basin This page was last edited on 9 January 2025, at 20:29 (UTC). Text is available under the Creative Commons Attribution-ShareAlike ...
Bayou Teche was the Mississippi River's main course when it developed a delta about 2,800 to 4,500 years ago. Through a natural process known as deltaic switching , the river's deposits of silt and sediment cause the Mississippi to change its course every thousand years or so.