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There are three major mountain ranges in New York: the Adirondack Mountains, the Catskill Mountains, and part of the Appalachian Mountains.
The Adirondack Mountains are sometimes considered part of the Appalachians but, geologically speaking, are a southern extension of the Laurentian Mountains of Canada. The Adirondacks do not form a connected range, but are an eroded dome consisting of over one hundred summits, ranging from under 1,200 feet (366 m) to over 5,000 feet (1,524 m) in altitude.
The highest of the Adirondack mountains are listed in the Adirondack High Peaks. Other mountains in the Adirondacks include:
The Catskills, which lie northwest of New York City and southwest of Albany, are a mature dissected plateau, an uplift region that was subsequently eroded into sharp relief. They are an eastward continuation of the Allegheny Plateau. They are sometimes considered an extension of the Appalachian Mountains, but are not geologically related.
The highest of the Catskills are listed in the Catskill High Peaks. Other high peaks in the Catskills include:
The mountains of southern New York State are part of the Appalachian Mountains. Ranges include:
Myles, William J., Harriman Trails, A Guide and History, The New York-New Jersey Trail Conference, New York, N.Y., 1999.
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.
The Catskill Park is in the Catskill Mountains in New York in the United States. It consists of 700,000 acres of land inside a Blue Line in four counties: Delaware, Greene, Sullivan, and Ulster. As of 2005, 287,500 acres (116,300 ha) or 41 percent of the land within, is owned by the state as part of the Forest Preserve; it is managed by the Department of Environmental Conservation (DEC). Another 5% is owned by New York City to protect four of the city's reservoirs in the region that lie partially within the park and their respective watersheds.
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 mostly covered by vegetation.
The Beaver Kill, sometimes written as the Beaverkill or Beaverkill River, is a tributary of the East Branch Delaware River, a main tributary of the Delaware River, approximately 44 miles (71 km) long, in the U.S. state of New York. The kill drains a 300-square-mile (780 km2) area of the Catskill Mountains and has long been celebrated as one of the most famous trout streams in the United States. Its preservation helped establish many of the basic conservation principles of rivers in the United States.
The East Branch Delaware River is one of two branches that form the Delaware River. It is approximately 75 mi (121 km) long, and flows through the U.S. state of New York. It winds through a mountainous area on the southwestern edge of Catskill Park in the Catskill Mountains for most of its course, before joining the West Branch along the northeast border of Pennsylvania with New York. Much of it is paralleled by State Route 30.
The Long Path is a 357-mile (575 km) long-distance hiking trail beginning in New York City, at the West 175th Street subway station near the George Washington Bridge and ending at Altamont, New York, in the Albany area. While not yet a continuous trail, relying on road walks in some areas, it nevertheless takes in many of the popular hiking attractions west of the Hudson River, such as the New Jersey Palisades, Harriman State Park, the Shawangunk Ridge and the Catskill Mountains. It offers hikers a diversity of environments to pass through, from suburbia and sea-level salt marshes along the Hudson to wilderness and boreal forest on Catskill summits 4,000 feet (1,220 m) in elevation.
Esopus Creek is a 65.4-mile-long (105.3 km) tributary of the Hudson River that drains the east-central Catskill Mountains in the U.S. state of New York. From its source at Winnisook Lake on the slopes of Slide Mountain, the Catskills' highest peak, it flows across Ulster County to the Hudson at Saugerties. Many tributaries extend its watershed into neighboring Greene County and a small portion of Delaware County. Midway along its length, it is impounded at Olive Bridge to create Ashokan Reservoir, the first of several built in the Catskills as part of New York City's water supply system. Its own flow is supplemented 13 miles (21 km) above the reservoir by the Shandaken Tunnel, which carries water from the city's Schoharie Reservoir into the creek.
Sugarloaf Mountain or Mount Sugarloaf, is a butte-like mountain located in South Deerfield, Massachusetts, United States, with two summits, North Sugarloaf Mountain 791 ft (241 m) and its more popular knee, South Sugarloaf Mountain 652 ft (199 m). Its cliffs, made of arkose sandstone, are a very prominent landscape feature visible for miles. Despite low elevations relative to the Berkshire Mountains to the west, dramatic cliff faces and a rise of 500 feet (150 m) to 600 feet (180 m) from the nearby Connecticut River make the mountain a popular tourist and hiking destination. Sugarloaf Mountain is the southern terminus of the Pocumtuck Range.
The Pocumtuck Range, also referred to as the Pocumtuck Ridge, is the northernmost subrange of the Metacomet Ridge mountain range of southern New England, itself a subrange of the Appalachian Mountains. Located in Franklin County, Massachusetts, between the Connecticut River and the Deerfield River valleys, the Pocumtuck Range is a popular hiking destination known for its continuous high cliffs, scenic vistas, and microclimate ecosystems.
Bearpen Mountain is a mountain located in the Catskill Mountains of New York. The mountain's highest peak is in Greene County, but its northwest subpeak at 42°16.42′N74°29.05′W is the highest point in Delaware County at 3,520 ft. Bearpen Mountain is flanked to the north by Roundtop, and to the southeast by Vly Mountain.
Vly Mountain is a mountain located in the town of Halcott, New York, United States in Greene County. The mountain is part of the Catskill Mountains. Vly Mountain is flanked to the northwest by Bearpen Mountain, to the east by Vinegar Hill, to the northeast by Kipp Hill, and to the southeast by Beech Ridge.
Halcott Mountain is one of the Catskill Mountains of the U.S. state of New York. It is mostly located in Greene County, with some of its lower slopes in Delaware and Ulster counties. Its exact summit elevation has not been officially determined, but the highest contour line on the mountain is 3,520 feet (1,070 m). It is one of the peaks on the divide between the Delaware and Hudson watersheds.
Sugarloaf Mountain is a mountain located in Greene County, New York. The mountain is part of the Devil's Path range of the Catskill Mountains. To the northwest, Sugarloaf is separated from Plateau Mountain by Mink Hollow Notch; to the southeast, Sugarloaf is separated from Twin Mountain by Pecoy Notch.
Balsam Mountain is one of the High Peaks of the Catskill Mountains in the U.S. state of New York. Its exact height has not been determined, so the highest contour line, 3,600 feet (1,100 m), is usually given as its elevation. It is located in western Ulster County, on the divide between the Hudson and Delaware watersheds. The summit and western slopes of the peak are within the Town of Hardenburgh and its eastern slopes are in Shandaken. The small community of Oliverea is near its base on that side. Most of the mountain is publicly owned, managed by the New York State Department of Environmental Conservation as part of the state Forest Preserve, part of the Big Indian-Beaverkill Range Wilderness Area in the Catskill Park. The summit is on a small corner of private land.
Balsam Lake Mountain is one of the Catskill Mountains, located in the Town of Hardenburgh, New York, United States. It is the westernmost of the range's 35 High Peaks. Its exact height has not been determined, but the highest contour line on topographic maps, 3,720 feet (1,130 m), is usually given as its elevation.
Graham Mountain is the seventh highest of the Catskill High Peaks and the highest privately owned mountain in the range. It is located in the town of Hardenburgh, New York, United States.
The Catskill Escarpment, often referred to locally as just the Escarpment or the Great Wall of Manitou, 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 Balsam Lake Mountain Fire Observation Station is located at the summit of the mountain of that name in the Town of Hardenburgh, New York, United States. It comprises a steel frame fire lookout tower, the observer's cabin and privy and the jeep road to the complex.
Deep Notch, sometimes West Kill Notch, or Echo Notch, is a mountain pass in Lexington, New York, United States. It divides two Catskill peaks, both subpeaks of high peaks of the range. The narrow groove between the steep, high slopes on either side is traversed by state highway NY 42 and the Shandaken Tunnel, part of the New York City water supply system. It has been called "striking" and "a marvel of grandeur and beauty".
