{{cite news
, url = http://geo.msu.edu/extra/geogmich/glaciallake_nip.html
, title = THE NIPISSING GREAT LAKES
, work = Michigan State University
, archiveurl =
, archivedate =
, accessdate = 2019-11-23
, url-status = live
, quote = These lakes started forming as the North Bay outlet opened up, effectively draining Glacial Lake Algonquin down to the Chippewa-Stanley level. With time, from 10,000 BP to about 4500 BP, the outlet rose, due to isostatic rebound.
Former rivers