Lake Stowe was a glacial lake that formed in Central Vermont approximately 15,000 years ago in the late Pleistocene epoch.
After the Laurentide Ice Sheet retreated, glacial ice melt accumulated at the terminal moraine.
[1][2] The lake existed until the glacier had completely melted.
Then it flowed out through the Lamoille River valley.
This article about a location in Vermont is a stub.