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Lake Agassiz (/ ˈ æ ɡ ə s i / 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.
List of lakes of the Sawtooth Mountains (Idaho) List of lakes of the White Cloud Mountains; Little Redfish Lake (White Cloud Mountains) Long Pond (Hancock County, Maine) Loon Lake (Lake County, Illinois) Lost Man Lake
Most glacial lakes present today can be found in Asia, Europe, and North America. The area which will see the greatest increase in lake formation is the Southern Tibetan Plateau region from debris covered glaciers. [3] This increase in glacial lake formation also indicates an increase in occurrence of glacial lake outburst flood events caused ...
The early Erie fed waters to Glacial Lake Iroquois. The ancient lake was similar in size to the current lake during glacial retreat, but for some period the eastern half of the lake was covered with ice. Early-period Lake Erie was made up of smaller lakes (Lakes Warren, Wayne, Maumee and Lundy) with lower depths.
Glacial alpine lakes differ from other glacier-formed lakes in that they occur at higher altitudes and mountainous terrain usually at or above timberline. For example, the Great Lakes of the U.S. and Canada are formed by the retreat of the Laurentide Ice Sheet during the last Ice Age which scoured the flat rock surface but are not in the alpine ...
Meanwhile, the Huron-Saginaw lobe had melted back to the north and east along a line in Michigan extending from Holland eastward through Kalamazoo to Jackson. Beginning 14,000 years ago, the glacial lobes had cleared the valley of the Kankakee River of ice. At this point, the forward movement of ice coming from the north equaled the rate of ...
Lake Lacawac is a glacial lake that was formed more than 13,000 years ago (at the end of the last ice age). More specifically, it is known as a scour lake because when the Wisconsin glacier passed through the area, it formed a crater in the sandstone. [6]
The lake varied in size, but it was at its biggest during the post-glacial period and gradually shrank to the current Lake Huron and Georgian Bay. About 7,000 years ago, the lake was replaced by Lake Chippewa and Lake Stanley as the glaciers retreated and 3,000 years later by the current Lakes Michigan, Huron, and Superior.