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The Great Lakes, also called the Great Lakes of North America, are a series of large interconnected freshwater lakes spanning the Canada–United States border. The five lakes are Superior, Michigan, Huron, Erie, and Ontario. (Hydrologically, Michigan and Huron are a single body of water, as they are joined by Straits of Mackinac.)
During the Late Pleistocene, the Laurentide ice sheet reached from the Rocky Mountains eastward through the Great Lakes, into New England, covering nearly all of Canada east of the Rocky Mountains. [8] Three major ice centers formed in North America: the Labrador, Keewatin, and Cordilleran. The Cordilleran covered the region from the Pacific ...
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. At its peak, the lake's area was larger than all of the modern Great Lakes combined. [2]
Toggle North America subsection. ... This a partial list of glacial moraines. ... Moraines of the Great Lakes Region. Lake Ontario Basin
Lake Algonquin is an example of a proglacial lake that existed in east-central North America at the time of the last ice age. Parts of the former lake are now Lake Huron, Georgian Bay, Lake Superior, Lake Michigan and inland portions of northern Michigan. [1] Examples in Great Britain include Lake Lapworth, Lake Harrison and Lake Pickering.
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
The Seven Rila Lakes in Rila mountain, Bulgaria, are of glacial origin. The Great Lakes as seen from space. The Great Lakes are the largest glacial lakes in the world. The prehistoric glacial Lake Agassiz once held more water than contained by all lakes in the world today. A glacial lake is a body of water with origins from glacier activity ...
Lake Maumee was a proglacial lake and an ancestor of present-day Lake Erie.It formed about 17,500 calendar years, or 14,000 Radiocarbon Years Before Present (RCYBP) as the Huron-Erie Lobe of the Laurentide Ice Sheet retreated at the end of the Wisconsin glaciation.