Catskill Escarpment

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 / 42.26750; -74.10444
Geography
Catskill Escarpment
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.