Lake Minong

Glacial Lake Minong

Lake Minong was a proglacial lake that formed in the Lake Superior basin during the Wisconsin glaciation around 10,000 B.P. (Before Present). This was the last glacial advance that entered Michigan and covered only part of the upper peninsula. Lake Minong occurred in the eastern corner of the Lake Superior basin while Lake Duluth was in the western end. The lakes became separated when the glacier reached the upper peninsula. Lake Minong expanded to the north as the ice retreated after 9,800 B.P. When the ice retreated from the Keweenaw Peninsula, Lake Duluth merged into Lake Minong.[1]

Chronology

See also

Glacial Lakes in the Lake Superior basin

References

  1. "Post-Valders Lake Stages in the Lake Superior Basin", in Glacial and Postglacial Geologic History of Isle Royale National Park, Michigan by N. King Huber, USGS Geological Survey Professional Paper 754-A
  2. 1 2 3 4 A late Lake Minong transgression in the Lake Superior basin as documented by sediments from Fenton Lake, Ontario; Andy Breckenridge, Thomas V. Lowell, Timothy G. Fisher, & Shiyong Yu; Springer Science+Business Media B.V. 2010

External links


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