new york’s finger lakes were formed by the same process as the great lakes. what was this process
Finger Lakes These glacial finger lakes originated as a series of northward-flowing streams. Around two million years ago, the first of many continental glaciers of the Laurentide Ice Sheet moved southward from the Hudson Bay area, initiating the Pleistocene glaciation. These scouring glaciers widened, deepened, and accentuated the existing river valleys. Glacial debris, possibly terminal moraine left behind by the receding ice, acted as dams, allowing lakes to form. Despite the deep erosion of the valleys, the surrounding uplands show little evidence of glaciation, suggesting that the ice was thin, or at least unable to cause much erosion at these higher altitudes. The deep cutting by the ice left some tributaries hanging high above the lakesâ€”both Seneca and Cayuga have tributaries hanging as much as 120 m above the valley floors.[1]
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New York (state) New York has a diverse geography. The state is bordered by New Jersey and Pennsylvania to the south and Connecticut, Massachusetts, and Vermont to the east. The state has a maritime border with Rhode Island, east of Long Island, as well as an international border with the Canadian provinces of Quebec to the north and Ontario to the northwest. The southern part of the state is in the Atlantic Coastal Plain and includes Long Island and several smaller associated islands, as well as New York City and the lower Hudson River Valley. The large Upstate New York region comprises several ranges of the wider Appalachian Mountains, and the Adirondack Mountains in the Northeastern lobe of the state. Two major river valleys – the north-south Hudson River Valley and the east-west Mohawk River Valley – bisect these more mountainous regions. Western New York is considered part of the Great Lakes Region and borders Lake Ontario, Lake Erie, and Niagara Falls. The central part of the state is dominated by the Finger Lakes, a popular vacation and tourist destination.
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