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Tug Hill, sometimes referred to as the Tug Hill Plateau, [4] is an upland region in northern New York state, notable for heavy winter snows. [5] [6] The Tug Hill region is east of Lake Ontario, north of Oneida Lake, and west of the Adirondack Mountains. The region is separated from the Adirondacks by the Black River Valley.
The Tug Hill Transition Eco-region encircles the Tug Hill Plateau in New York state, forming a distinctive doughnut-shaped area that serves as a bridge between the plateau and the surrounding lowlands. This region features sloping topography, a contrast to the adjacent areas it borders.
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Montague is on the northern end of the Tug Hill Plateau, which is well known for having some of the snowiest winters in New York. Hooker holds the state record for seasonal snowfall of 466.9 inches (11.86m) during the winter of 1976-1977. [ 6 ]
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English: New York State map showing greater Tug Hill region, and its forested "core" region. Core area based on The Nature Conservancy's delineation as displayed on page 56 of the Tug Hill Tomorrow Land Trust Strategic Land Conservation Plan (December 2006).
The Allegheny Plateau (/ ˌ æ l ɪ ˈ ɡ eɪ n i / AL-ig-AY-nee) is a large dissected plateau area of the Appalachian Mountains in western and central New York, northern and western Pennsylvania, northern and western West Virginia, and eastern Ohio. It is divided into the unglaciated Allegheny Plateau and the glaciated Allegheny Plateau.
The Deer Isle Bridge is a suspension bridge spanning Eggemoggin Reach in the state of Maine. The bridge is the only vehicular connection from the Maine mainland to Little Deer Isle, one of the segments that make up the island. The span was completed in March 1939 with a main span of 1,088 feet (332 m).