Glacial Lake McKenzie explained

Lake McKenzie
Location:McLean, Mercer, and Dunn, Counties, North Dakota
Coords:47.5286°N -101.4062°W
Lake Type:Glacial lake (former)
Inflow:Laurentide Ice Sheet
Outflow:Over the divide to the Yellowstone River or along the face of the Ice sheet.
Pushpin Map:North Dakota
Basin Countries:United States
Length:about 140miles
Width:40miles
Area:varied
Elevation:1940m (6,370feet)
Reference:[1]

Before the Pleistocene Ice Age, circa two million years before present (YBP), the rivers in North, South Dakota and eastern Montana drained northeast into Canada and then into Hudson Bay.[2] The Keewatin Lobe of the continental ice sheet, block the flow of water northward and impounded it along the ice front. Lakes formed, until the waters could find a new way to drain. Initially, the north flowing rivers followed the front of the glacier eastward and into a valley that passed between Garrison and Riverdale, to the Turtle Lake area, and on into Sheridan County. This is known as the preglacial McClean River.[2] This valley became blocked by the glacier and the glacial lake identified as Lake McKenzie formed. Eventually, water level rose to crest the south ridge a point near Riverdale — at the site of the modern Garrison Dam and a diversion trench was cut. The modern Missouri River follows this pathway.[2]

See also

Bibliography

Notes and References

  1. Physiography and Glacial Geology of Eastern Montana and Adjacent Areas; William C. Alden; United States Government Printing Office: Washington, D.C.; 1932
  2. The Missouri River; John P. Bluemle; North Dakota Geological Survey; Bismarck, North Dakota; 02-Jan-2008