Lake Albany | |
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![]() Proglacial and prehistoric lakes of New England during the end of the Wisconsin Glacial Epoch of the Pleistocene Era | |
Location | between Poughkeepsie, New York at its northern-most tip to near Glenn Falls, New York at its southern-most end |
Coordinates | 42°43′06″N73°51′52″W / 42.7183°N 73.8644°W |
Type | Proglacial lake |
Primary inflows | Lake Vermont |
Primary outflows | Hudson River |
Basin countries | United States |
Max. length | 160 miles (260 km) |
References | Coordinates approximated using details in International Oaks [1] |
Location | |
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Glacial Lake Albany was a prehistoric North American proglacial lake that formed during the end of the Wisconsinan glaciation. [2] [3] It existed between 15,000 and 12,600 years ago and was created when meltwater from a retreating glacier, along with water from rivers such as the Iromohawk, became ice dammed in the Hudson Valley. [2] [4] [5]
Organic materials in Lake Albany deposits have been carbon dated to approximately 11,700 years ago. [6] The lake spanned approximately 160 miles (260 km) from present-day Poughkeepsie to Glens Falls. [2] [4] [7]
Lake Albany drained about 10,500 years ago through the Hudson River due to post-glacial rebound. [2] [7] [8] When the lake drained it exposed the sandy and gravelly glaciolacustrine deposits left by the glacier, along a broad plain just west of Schenectady, where the Mohawk emptied into the lake. [9] Dune and deltaic sands, containing lenses of silty sand, silt and clay, [10] compose the topsoil which now underlies the Albany Pine Bush. [11] Beneath the surficial deposits are lake-bottom silt and clay, which overlie till and shale bedrock. [10] A small rill caused by the lake's drainage created Patroon Creek, Sand Creek, Lisha Kill, Shaker Creek, Delphus Kill and the Salt Kill in the town of Colonie, New York. [12]