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Hunter Mountain (New York)
Hunter Mountain is in the towns of Hunter and Lexington, just south of the village of Hunter, in Greene County, New York, United States. At approximately in elevation, it is the highest peak in the county and the second-highest peak in the Catskill Mountains. While the mountain is closely associated with the eponymous ski area built around the Colonel's Chair ridge at the mountain's northwest corner, that takes up only a small portion of the mountain. The actual summit, some distance from the ski area, is graced with a fire lookout tower, the highest in the state and second-highest in the Northeast. The former road to it is open to hikers, horses (and possibly mountain bikers in the future). It is the most popular route to the mountain's summit. Geography Hunter takes the shape of a medium-length ridge, rising steeply from Stony Clove Notch in the east, then gently to the summit in the center, and gently back down to the west where the land makes a much less steep drop in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Black Dome (New York)
:''See Black Dome for other mountains of this name.'' Black Dome is a mountain located in Greene County, New York. The mountain is the highest peak of the Blackhead Mountains range of the Catskills. Black Dome is flanked to the east by Blackhead, and to the west by Thomas Cole Mountain. Black Dome stands within the watershed of Schoharie Creek, which drains into the Mohawk River, the Hudson River, and into New York Bay. The south side of Black Dome drains into East Kill, and thence into Schoharie Creek. The north side of Black Dome drains into Batavia Kill, and thence into Schoharie Creek. Black Dome is within New York's Catskill Park. See also * List of mountains in New York * Catskill High Peaks * Catskill Mountain 3500 Club The Catskill Mountain 3500 Club, incorporated as the Catskill 3500 Club and often just referred to as the 3500 Club, is a peakbagging organization for hikers in the Catskill Mountains of New York. Those wishing to become members must climb a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ridge
A ridge or a mountain ridge is a geographical feature consisting of a chain of mountains or hills that form a continuous elevated crest for an extended distance. The sides of the ridge slope away from the narrow top on either side. The lines along the crest formed by the highest points, with the terrain dropping down on either side, are called the ridgelines. Ridges are usually termed hills or mountains as well, depending on size. Smaller ridges, especially those leaving a larger ridge, are often referred to as spurs. Types There are several main types of ridges: ;Dendritic ridge: In typical dissected plateau terrain, the stream drainage valleys will leave intervening ridges. These are by far the most common ridges. These ridges usually represent slightly more erosion resistant rock, but not always – they often remain because there were more joints where the valleys formed or other chance occurrences. This type of ridge is generally somewhat random in orientation, often ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
West Kill
The West Kill, an tributary of Schoharie Creek, flows through the town of Lexington, New York, United States, from its source on Hunter Mountain, the second-highest peak of the Catskill Mountains. Ultimately its waters reach the Hudson River via the Mohawk. Since it drains into the Schoharie upstream of Schoharie Reservoir, it is part of the New York City water supply system. It lends its name to both a mountain to its south and a small town midway along its length. The West Kill's watershed accounts for 10 percent of the reservoir's basin. It has the highest elevations and steepest slopes of any of the Schoharie's subwatersheds, with runoff from seven of the 35 Catskill High Peaks draining into the stream. Due to limited development and extensive land protection in the stream's watershed, its water is relatively clean, supporting a habitat for both wild and stocked trout; historically it has drawn fly fishers and other anglers. However, the West Kill has contributed to t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Esopus Creek
Esopus Creek is a 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 above the reservoir by the Shandaken Tunnel, which carries water from the city's Schoharie Reservoir into the creek. The creek, originally known by the Native Americans in the area as ''Atkarkaton'' or ''Atkankarten'' and by Dutch settlers as the "Esopus Kill", takes its name from the Esopus tribe of the Lenape, who were living around the lower Esopus when the Dutch first explored ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stony Clove Creek
Stony Clove Creek is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map accessed October 3, 2011 creek in the Catskill Mountains in New York. It is a tributary of Esopus Creek, which in turn is a tributary of the Hudson River. It joins the Esopus in the village of Phoenicia, and has two smaller tributaries up north of Phoenicia. Description The Stony Clove starts near the Stony Clove Notch in Edgewood in Greene County. It originates at Notch Lake, near the Devil's Tombstone Campsite, and flows through the small villages of Edgewood and Lanesville, entering Ulster County at Chichester. History Early maps and deeds indicate that the Stony Clove flowed into the Warner Bushkill, or alternatively named, the Barber Bushkill, before flowing into the Esopus. Later cartographers have changed the nomenclature of the streams so that the Barber Bushkill or Warner Bushkill flows into the Stony Clove. It was formed about 10,000 years ago, d ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mohawk River
The Mohawk River is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map accessed October 3, 2011 river in the U.S. state of New York. It is the largest tributary of the Hudson River. The Mohawk flows into the Hudson in Cohoes, New York, a few miles north of the city of Albany.Mohawk River , The Columbia Gazetteer of North America The river is named for the of the Iroquois Confederacy. It is a major waterway in north-central New York. The largest tributary, the Schoharie Creek, accounts fo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Schoharie Creek
Schoharie Creek is a river in New York that flows north from the foot of Indian Head Mountain in the Catskills through the Schoharie Valley to the Mohawk River. It is twice impounded north of Prattsville to create New York City's Schoharie Reservoir and the Blenheim-Gilboa Power Project. During the American Revolutionary War, Iroquois Indian attacks against the cluster of farms in the valley of the Cobleskill Creek tributary was the site of the Cobleskill Massacre (May 1778), virtually depopulating settlements in the southern Mohawk valley. News of this and two other mixed Tory-Indian guerrilla attacks led to an appropriation of funds for the Sullivan Expedition dispatched by General Washington in 1779 to break the threat of Indian raids. The Erie Canal crossed over the creek by an aqueduct at Schoharie Crossing State Historic Site. Two notable bridge collapses have occurred on Schoharie Creek. In 1987, two spans of the New York State Thruway collapsed. On August 28, 20 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Drainage Basin
A drainage basin is an area of land where all flowing surface water converges to a single point, such as a river mouth, or flows into another body of water, such as a lake or ocean. A basin is separated from adjacent basins by a perimeter, the '' drainage divide'', made up of a succession of elevated features, such as ridges and hills. A basin may consist of smaller basins that merge at river confluences, forming a hierarchical pattern. Other terms for a drainage basin are catchment area, catchment basin, drainage area, river basin, water basin, and impluvium. In North America, they are commonly called a watershed, though in other English-speaking places, "watershed" is used only in its original sense, that of a drainage divide. In a closed drainage basin, or endorheic basin, the water converges to a single point inside the basin, known as a sink, which may be a permanent lake, a dry lake, or a point where surface water is lost underground. Drainage basins are similar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hudson River
The Hudson River is a river that flows from north to south primarily through eastern New York. It originates in the Adirondack Mountains of Upstate New York and flows southward through the Hudson Valley to the New York Harbor between New York City and Jersey City, eventually draining into the Atlantic Ocean at Lower New York Bay. The river serves as a political boundary between the states of New Jersey and New York at its southern end. Farther north, it marks local boundaries between several New York counties. The lower half of the river is a tidal estuary, deeper than the body of water into which it flows, occupying the Hudson Fjord, an inlet which formed during the most recent period of North American glaciation, estimated at 26,000 to 13,300 years ago. Even as far north as the city of Troy, the flow of the river changes direction with the tides. The Hudson River runs through the Munsee, Lenape, Mohican, Mohawk, and Haudenosaunee homelands. Prior to European ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cirque (landform)
A (; from the Latin word ') is an amphitheatre-like valley formed by glacial erosion. Alternative names for this landform are corrie (from Scottish Gaelic , meaning a pot or cauldron) and (; ). A cirque may also be a similarly shaped landform arising from fluvial erosion. The concave shape of a glacial cirque is open on the downhill side, while the cupped section is generally steep. Cliff-like slopes, down which ice and glaciated debris combine and converge, form the three or more higher sides. The floor of the cirque ends up bowl-shaped, as it is the complex convergence zone of combining ice flows from multiple directions and their accompanying rock burdens. Hence, it experiences somewhat greater erosion forces and is most often overdeepened below the level of the cirque's low-side outlet (stage) and its down-slope (backstage) valley. If the cirque is subject to seasonal melting, the floor of the cirque most often forms a tarn (small lake) behind a dam, which marks the down ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Southwest Hunter Mountain
Southwest Hunter Mountain (Leavitt Peak) is a subpeak of Hunter Mountain, located in Greene County, New York. It is considered one of the Catskills' High Peaks in its own right, because of its separation from the main summit, and its topographic prominence. Hunter Mountain is named after John Hunter, who also gave his name to the town of Hunter. Southwest Hunter is part of the Devil's Path range of the Catskill Mountains. SW Hunter is flanked to the northeast by the main summit of Hunter, and to the west faces West Kill Mountain across Diamond Notch. It is considered a bushwhack, as there are no official trails leading to its summit, in the midst of a dense montane boreal forest of red spruce and balsam fir. Attempts to climb from Diamond Notch, the closest approach of a maintained trail, have led to the creation of a maze of herd paths on the level area west of the mountain's summit, none of which leads to it and many of which dead-end. Hikers have instead been following t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Plateau Mountain (New York)
Plateau Mountain is located in the town of Hunter in Greene County, New York, United States. It is part of the Devil's Path range of the Catskill Mountains. Plateau has a two-mile-long () summit ridge above . The highest point, at least , is at the southeast end, facing Sugarloaf Mountain to the east across Mink Hollow Notch. It is the 12th-highest peak in the range Devils Tombstone is located west of Plateau Mountain. The northwest end faces Hunter Mountain to the west across Stony Clove Notch. Plateau Mountain stands within the watershed of the Hudson River, which drains into New York Bay. It feeds the Hudson by way of Esopus Creek through Stony Clove Creek from its western slopes, and through Beaver Kill from its southeast end. Its southwest slopes drain into Warner Creek, thence into Stony Clove Creek. The northeastern slopes of Plateau drain into Schoharie Creek, thence into the Mohawk River, and the Hudson River. Plateau Mountain is within New York's Catskill S ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
