Search results
Results From The WOW.Com Content Network
The Catskills became a major resort destination for Jewish New Yorkers in the mid-20th century. Borscht Belt is an informal term for the summer resorts of the Catskill Mountains in Sullivan and Ulster counties in upstate New York which were frequented by Ashkenazic Jews. At its peak of popularity, about 500 resorts operated in the region. [2]
The Catskill Mountains, also known as the Catskills, are a physiographic province and subrange of the larger Appalachian Mountains, located in southeastern New York.As a cultural and geographic region, the Catskills are generally defined as those areas close to or within the borders of the Catskill Park, a 700,000-acre (2,800 km 2) forest preserve protected from many forms of development under ...
The Borscht Belt, or Yiddish Alps, was a region noted for its summer resorts that catered to Jewish vacationers, especially residents of New York City. [1] The resorts, now mostly defunct, were located in the Catskill Mountains in parts of Sullivan and Ulster counties in the U.S. state of New York, in Upstate New York and the northern edges of the New York metropolitan area.
Catskill Mountain House. The Catskill Mountain House, which opened in 1824, was a famous hotel near Palenville, New York, and in the Catskill Mountains overlooking the Hudson River Valley. In its prime, from the 1850s to the turn of the century, it was visited by three U.S. presidents (U.S. Grant, Chester A. Arthur, and Theodore Roosevelt) and ...
Catskill Escarpment. The Catskill Escarpment, often referred to locally as just the Escarpment or the Great Wall of Manitou, [1] and known as the Catskill Front to geologists, is the range forming the northeastern corner of the Catskill Mountains in Greene and Ulster counties in the U.S. state of New York. It rises very abruptly from the Hudson ...
Michael Kudish is an author, railroad historian, forest historian, botanist, and retired emeritus professor. He received his Ph.D. in botany in 1971 from the State University of New York College of Environmental Science and Forestry at Syracuse. His dissertation, on the history of Catskill forests, was the beginning of a lifelong study.
The Catskill High Peaks are all of the mountains in New York 's Catskill Mountains above 3,500 ft (1,067 m) in elevation whose summits are separated either by one-half mile (0.8 km) or a vertical drop of at least 250 ft (76.2 m) between it and the next nearest separate summit. By usual standards, these mountains are rather low and rounded, and ...
Catskill Mountains, New York. The Devonian Catskill Group or the Catskill Clastic wedge is a unit of mostly terrestrial sedimentary rock found in Pennsylvania and New York. Minor marine layers exist in this thick rock unit (up to 10,000 feet (3,000 m)). It is equivalent to the Hampshire Formation of Maryland, West Virginia, and Virginia.