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 | |
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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 | |
Location | Manitoba, Ontario, and Saskatchewan in Canada; Minnesota and North Dakota in the U.S. |
Coordinates | 51°N 97°W |
Lake type | proglacial lake |
Etymology | Louis Agassiz |
Primary inflows | Laurentide Ice Sheet |
Primary outflows | Glacial River Warren, the Vermilion River, the Wanapitei River, and the Montreal River valley |
Basin countries | Canada, United States |
First flooded | 12,875 years before present |
Max. length | 475 mi (764 km) |
Max. width | 296 mi (476 km) |
Surface area | 260,000 km2 (100,000 sq mi) |
Surface elevation |
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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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