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Geography in New York (state)


Geography in New York (state)

There is no concise way to describe the geography of New York, except maybe to say it is "diverse". The city of New York, a major Atlantic port, is of course at sea level. It serves as a small fulcrum connecting Long Island (to the east) and the rest of the state (to the north)—to reach one from the other, one must pass through New York City. North of the city lies the vast majority of the state, known as "Upstate New York". The land rises as one goes north, following the Hudson River upstream. The river cuts a gorge through these Appalachian highlands, forming a wide river valley. To the west of this valley, the Catskills rise—a "dissected plateau" to geologists, but just "mountains" to laymen. Beyond the Catskills, the terrain drops and levels, forming the rolling hills of the Southern Tier. North of the Catskills is the Mohawk River valley, which runs from west to east into the Hudson. Further west, you will find the Finger Lakes region, a series of long skinny lakes formed when river valleys were blocked by debris from retreating glaciers. North of the Finger Lakes, between them and Lake Ontario, lie large swaths of lowlands, areas which were once underneath the surface of a much larger, pre-glacial Lake Ontario. North of the Mohawk valley and east of Lake Ontario, you can find the vast mountain range of the Adirondacks, which gradually give way to the St. Lawrence River valley in the northernmost part of the state.

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New York (state) Travel Guide from Wikitravel. Many thanks to all Wikitravel contributors. Text is available under Creative Commons Attribution-ShareAlike 3.0, images are available under various licenses, see each image for details.

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