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Catskill Mountains


 

The Catskill Mountains, a natural area in New York State northwest of New York City and southwest of Albany, are not, despite their popular name, true geological mountains, but rather a mature dissected plateau, an uplifted region that was subsequently eroded into sharp relief. They are an eastward continuation, and the highest representation, of the Allegheny Plateau. They are sometimes considered an extension of the Appalachian Mountains into Upstate New York, although they are not geologically related. The Catskills are west of the Hudson River and lie within the bounds of six counties (Otsego, Delaware, Sullivan, Schoharie, Greene, and Ulster).

Related Topics:
New York State - New York City - Albany - Dissected plateau - Allegheny Plateau - Appalachian Mountains - Upstate New York - Hudson River - Otsego - Delaware - Sullivan - Schoharie - Greene - Ulster

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At the eastern end of the range, the "mountains" begin quite dramatically with the Catskill Escarpment rising up suddenly from the Hudson Valley. The western boundary is far less certain, as the mountains gradually decline in height and grade into the rest of the Allegheny Plateau. Nor is there a consensus on where the Catskills end to the north or south, with it being certain only that by the time one reaches either I-88, the Delaware River or the Shawangunk Ridge that one is no longer in the Catskills.

Related Topics:
Hudson Valley - Allegheny Plateau - I-88 - Delaware River - Shawangunk Ridge

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Whether you are in the Catskills or not in these peripheral regions seems to be as much a matter of personal preference as anything else, as an old saying in the region ? "When you have two rocks for every dirt, you are in the Catskills" ? seems to suggest.

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Many visitors, including owners of weekend or vacation homes in the region, seem to consider almost anything sufficiently rural west of the Hudson yet within a short drive of New York City to be in the Catskills.

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The Poconos, to the immediate southwest, are technically a continuation of the Catskills under a different name.

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The Catskills contain more than thirty peaks above 3,500 feet and parts of six important rivers. The highest mountain, Slide Mountain in Ulster County, has an altitude of 4,180 feet (1,274 m).

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Within the range is the Catskill Park and corresponding Catskill Forest Preserve. Not all the land is publicly owned; about 60% remains in private hands, but new sections are added frequently. Most of the park and the preserve are within Ulster County; however Greene County accounts for a significant portion as well and there are areas in Sullivan and Delaware counties too.

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This is a traditional vacation land with many summer resorts and camp grounds. During the first part of the 20th century, many ethnic groups (Germans, Czechs, Jews, etc) established summer resorts in the Catskills that catered to their needs. The "Borscht Belt" was a collection of Jewish resorts (Brown's, Grossinger's, etc) in this region, where many comics got a start in show business. This ethnic tradition has mostly disappeared, although some special groups maintain private resorts. Many of these resorts now attempt to remain open all year and cater to winter activities such as skiing.

Related Topics:
20th century - Ethnic groups - Borscht Belt

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The Catskills figure in Washington Irving's story, Rip van Winkle.

Related Topics:
Washington Irving - Rip van Winkle

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