Return to Main Red River Basin Page |
Red River of the North Basin Glacial Lake Agassiz and the Red River Valley
Where drainage occurred was dependent upon the level of the lake and ice coverage. About 11,500-11,000 yeas ago, drainage occurred through the Minnesota River valley, until the level dropped to a point where drainage was blocked by a moraine between the Red River and Minnesota River valleys. As glacial ice retreated further north, an outlet opened to the Great Lakes. Ice again advanced southward and about 9,900 years ago, drainage again occurred through the Minnesota River valley until about 9,200 years ago when water levels dropped to a point where drainage to the south was blocked. The Great Lakes outlet closed about 8,500 years ago, and drainage since has occurred in a similar pattern to current drainage. The Red River Valley exists in what was the southwestern portion of Glacial Lake Agassiz, and what is now the center of the Red River Basin. The Red River Valley extends over 315 miles from Lake Traverse in the south to Lake Winnipeg in the north. It is 60 miles wide at its widest point. The elevation of the Red River falls 233 feet from the headwaters of the Red River to its mouth 545 river miles away, for an average slope of only about one-half foot per mile. The slope is greater near the headwaters and flattens toward the mouth. The elevation of the Valley in the south is 943 feet mean sea level (msl), while at the northern end, the elevation is 714 msl -- a change in elevation of 229 feet over its 315 mile length. (Information Sources: "A River Runs North" by Gene Krenz and Jay Leitch, Red River Water Resources Council (1993), and "Aquatic Communities and Contaminants in Fish from Streams of the Red River of the North Basin, Minnesota and North Dakota" by Robert Goldstein, U.S. Geological Survey (1995). Map Source: "A River Runs North," Figure 1-2.) More Information For questions about the Red River Basin information available on this Web site, contact Molly MacGregor at 218-846-0494. |