Lake Agassiz

Lake Agassiz (/ˈæɡəsi/ AG-ə-see) was a large proglacial lake that existed in central North America during the late Pleistocene, fed by meltwater from the retreating Laurentide Ice Sheet at the end of the last glacial period. At its peak, the lake's area was larger than all of the modern Great Lakes combined.

Lake Agassiz
Map of the extent of Lake Agassiz in central North America, by 19th century geologist Warren Upham. The regions covered by the lake were significantly larger than shown here.
Lake Agassiz
Location in North America
LocationManitoba, Ontario, and Saskatchewan in Canada; Minnesota and North Dakota in the U.S.
Coordinates51°N 97°W
Lake typeproglacial lake
EtymologyLouis Agassiz
Primary inflowsLaurentide Ice Sheet
Primary outflowsGlacial River Warren, the Vermilion River, the Wanapitei River, and the Montreal River valley
Basin countriesCanada, United States
First flooded12,875 years before present
Max. length475 mi (764 km)
Max. width296 mi (476 km)
Surface area260,000 km2 (100,000 sq mi)
Surface elevation
  • 335 metres (1,099 ft)
  • 258 metres (846 ft)
  • 325 metres (1,066 ft)
  • 310 metres (1,020 ft)

First postulated in 1823 by William H. Keating, it was named by Warren Upham in 1879 after Louis Agassiz, the then-recently deceased (1873) founder of glaciology, when Upham recognized that the lake was formed by glacial action.

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