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.
11,400 B.P. Lake Minong covered only Whitefish Bay with the Laurentian glacial mass lying across the central Lake Superior basin. Lake Duluth existed in the *lowlands of St. Louis Bay and Spirit Lake on the St. Louis River.
10,600 B.P. The glacial ice had receded northward, opening a link between the eastern and western basins of Lake Superior.
9,500 B.P. Lake Minong expands to cover the entire lake basin as the glacial front moves northward from the basin. At this time, Lake Minong is an intermediary basin with waters from Lake Agassiz flowing in through the Nipigon River valley and further east through the Aquasabong valley.
8,500 B.P. Lake Superior forms as the Lake Agassiz basin joins with the Lake Ojibway, shifting it’s drainage into the headwaters of the Ottawa River. The Lake Superior basin becomes the headwaters of the Great Lakes system.
^"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
^ abcdA 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