Proglacial lakes of Minnesota

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Present-day Minnesota, with proglacial lakes added in dark blue.

The proglacial lakes of Minnesota were lakes created in what is now the U.S. state of Minnesota in central North America in the waning years of the last glacial period. As the Laurentide ice sheet decayed at the end of the Wisconsin glaciation, lakes were created in depressions or behind moraines left by the glaciers. Evidence for these lakes is provided by low relief topography and glaciolacustrine sedimentary deposits.[1] Not all contemporaneous, these glacial lakes drained after the retreat of the lobes of the ice sheets that blocked their outlets, or whose meltwaters fed them. There were a number of large lakes, one of which, Glacial Lake Agassiz, was the largest body of freshwater known to have existed on the North American continent; there were also dozens of smaller and more transitory lakes filled from glacial meltwater, which shrank or dried as the ice sheet retreated north.

Glacial Lake Agassiz[edit]

Main article: Glacial Lake Agassiz

Glacial Lake Agassiz was an enormous lake, larger in area than all the Great Lakes combined, and the largest body of fresh water ever to have existed in North America.[2] It extended from its outlet near Browns Valley, Minnesota west into South Dakota and North Dakota and north into Saskatchewan, Manitoba, and Ontario.[2] In Minnesota the lake occupied the Red River Valley in northwestern Minnesota and the western part of the watershed of the Rainy River in the northern part of the state.[3] Its southern outlet was through the Traverse Gap, a spillway channel cut through the Big Stone Moraine by Glacial River Warren,[4] an enormous stream which carved the valley of the Minnesota River as well as that of the Upper Mississippi River below the confluence of those successor streams.[5] Lake Agassiz' present-day remnants include Lake of the Woods and Upper and Lower Red Lake.[6]

Glacial Lake Upham[edit]

Glacial Lake Upham was formed in the wake of the retreat of the St. Louis Sublobe of the Des Moines Lobe.[7] It drained through a series of successively lower outlets to Glacial Lake Duluth, culminating in the Saint Louis River.[8] Its former lake bed is now a broad boggy area comprising much of the watershed of the latter stream.

Glacial Lake Aitkin[edit]

Glacial Lake Aitkin was also a product of the recession of the St. Louis Sublobe, and for significant portions of its history was contiguous with Glacial Lake Upham.[7] It occupied a broad lowland along the valley of the present-day Mississippi River between Grand Rapids and Aitkin in north central Minnesota. The lake bed is now a sandy and clayey plain.[9]

Glacial Lake Duluth[edit]

Main article: Glacial Lake Duluth

Glacial Lake Duluth is the name given to the largest of a series of named lakes or lake stages occupying parts of the Lake Superior basin. As its current outlet to the east was blocked by the Superior Lobe of the ice sheet, Lake Duluth drained through two outlets which crossed the present Laurentian Divide to the valley of the Saint Croix River and the Mississippi. One outlet was a route from the western part of the lake through the Nemadji River basin and down the present Moose and Kettle Rivers; the other was via the modern Bois Brule River to the Saint Croix.[10] At its peak, Lake Duluth was 148 meters higher than Superior's present level.[11] When the glacier retreated the lake was able to drain to the east.

Glacial Lake Grantsburg[edit]

Lake Grantsburg, formed when the Grantsburg Sublobe of the Des Moines Lobe blocked southward drainage of the ice-free land to its north. It extended from St. Cloud east-northeast to Grantsburg, Wisconsin, whence its outflow ran south along the east front of the ice sheet down the valley of the Saint Croix River.[12]

Glacial Lake Minnesota[edit]

Lake Minnesota was a complex of lakes formed by or on the Des Moines Lobe generally south of Mankato, Minnesota. Evidence for it is found in lacustrine sediments in that region.[13] The lakes may have consisted of bodies of water trapped on the surface of the decaying ice sheet,[14] lakes created as the lobe retreated,[7] or depressions filled from the overflow of Glacial River Warren.[15]

See also[edit]

References[edit]

Notes[edit]

  1. ^ Hudak et al., Landscape Suitability Models for Geologically Buried Precontact Cultural Resources, Glossary.
  2. ^ a b Waters, Streams and Rivers of Minnesota, p. 106.
  3. ^ Waters, Streams and Rivers of Minnesota, p. 107.
  4. ^ Sansome, Minnesota Underfoot, pp. 177-79.
  5. ^ Ojakangas and Matsch, Minnesota's Geology, pp. 109-110.
  6. ^ Ojakangas and Matsch, Minnesota's Geology, pp. 109.
  7. ^ a b c Ojakangas and Matsch, Minnesota's Geology, p. 109.
  8. ^ Waters, Streams and Rivers of Minnesota, pp. 26, 28-29.
  9. ^ Sansome, Minnesota Underfoot, p. 155; Waters, Streams and Rivers of Minnesota, pp. 26, 211, 225.
  10. ^ Waters, Streams and Rivers of Minnesota, pp. 28, 147.
  11. ^ Huber, Glacial and Postglacial Geologic History of Isle Royale National Park lists the peak elevation of Lake Duluth at 1085 feet (331 m), which is approximately 485 feet (148 m) higher than Superior's 2007 elevation of 600 feet (183 m). Ojakangas and Matsch list the peak elevation even higher, at 335 m. Minnesota's Geology, p. 110.
  12. ^ Ojakangas and Matsch, Minnesota's Geology, pp. 106-07, 212.
  13. ^ Cooper, Soil Forming Factors.
  14. ^ Ojakangas and Matsch, Minnesota's Geology, p. 226.
  15. ^ Hudak and Hajic, Landscape Suitability Models for Geologically Buried Precontact Cultural Resources, section 12.3.4.1 (Landscapes: Paleo-Valley Landscape).

Sources[edit]