Catskill Escarpment | |
---|---|
Great Wall of Manitou | |
![]() The Escarpment as seen from Olana State Historic Site, across the Hudson River | |
Highest point | |
Peak | Blackhead Mountain, Windham/Jewett/Cairo |
Elevation | 3,940 ft (1,200 m) |
Coordinates | 42°16′03″N 74°06′16″W / 42.26750°N 74.10444°W |
Geography | |
Country | United States |
State | New York |
Regions | Catskill Mountains and Hudson Valley |
Counties | Ulster, Greene and Schoharie |
Falls and lakes | Kaaterskill Falls and North-South Lake |
Parent range | Catskill Mountains |
Biome | temperate hardwood forest, boreal forest |
Geology | |
Orogeny | Acadian |
Age of rock | Silurian and Devonian |
Type of rock | Shale and sandstone |
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 Valley to summits above 3,000 feet (910 m) in elevation, including three of the Catskill High Peaks, with almost no foothills. The plateau to the south and west averages 2,000 feet (610 m) above sea level.
The Escarpment was the first area of the Catskills to attract the interest of European settlers. Botanist John Bartram wrote a widely read account of an expedition there prior to independence, and a century later the North-South Lake area he had visited became home to a number of exclusive resorts, including the Catskill Mountain House. Views of it inspired Thomas Cole and other painters of the Hudson River School, the first art movement in the United States. Today much of it is New York State Forest Preserve within the Catskill Park, and a popular place for hiking, camping and other outdoor recreation.