Catskill Mountains | |
---|---|
Highest point | |
Peak | Slide Mountain |
Elevation | 4,180 ft (1,270 m) |
Coordinates | 41°59′55″N 74°23′11″W / 41.99861°N 74.38639°W |
Dimensions | |
Length | 111 mi (179 km) N/S |
Width | 102 mi (164 km) E/W |
Area | 15,259 km2 (5,892 sq mi) |
Geography | |
Main regions of the northeast Appalachians, with the Catskills as "C" | |
Country | United States |
State | New York |
Region | Hudson Valley, Southern Tier, Mohawk Valley |
Counties | |
Rivers | |
Communities | |
Parent range | Appalachian (Allegheny Plateau) |
Borders on | |
Geology | |
Rock ages | |
Rock type | Sedimentary |
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 km2) forest preserve protected from many forms of development under New York state law.
Geologically, the Catskills are a mature dissected plateau, a flat region subsequently uplifted and eroded into sharp relief by watercourses. The Catskills form the northeastern end of the Allegheny Plateau (also known as the Appalachian Plateau).[1][2]
The Catskills were named by early Dutch settlers. They are well known in American society as the setting for films and works of art, including many 19th-century Hudson River School paintings, as well as for being a favored destination for vacationers from New York City in the mid-20th century. The region's many large resorts gave many young stand-up comedians an opportunity to hone their craft. Since the late 19th century, the Catskills have been a haven for artists, musicians and writers, especially in and around the towns of Woodstock and Phoenicia.