Lake Minong

Coordinates: 47°42′N 87°30′W / 47.7°N 87.5°W / 47.7; -87.5
Source: Wikipedia, the free encyclopedia.
Lake Minong
Primary inflows
From Lake Agassiz through the Nipigon River
Primary outflowsGrand River valley in Michigan
Basin countriesCanada
United States
First flooded10,000 years before present
Residence time1,500 years in existence
Surface elevation450 ft (137 m)
ReferencesGlacial and Postglacial Geologic History of Isle Royale National Park, Michigan; N. King Huber; The Geology of Isle Royale National Park, Michigan; Geological Survey Professional Paper 754-A; United States Government Printing Office, Washington, D.C.; 1973.

Lake Minong was a proglacial lake that formed in the

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. ^ a b c d 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