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Kaaterskill High Peak
Kaaterskill High Peak (officially just High Peak) is one of the Catskill Mountains, located in the Town of Hunter in Greene County, New York, United States. It was once believed to be the highest peak in the entire range, but its summit, at 3,655 feet (1,114 m) in elevation, places it only 23rd among the Catskill High Peaks. It is, however, the fourth most prominent peak in the range. Due to its situation as the easternmost High Peak, its summit is just outside the watersheds of New York City's reservoirs in the region. Along with Round Top to the west, its distinctive ridgeline is a visual signature of the Catskills. Even today, it dominates the view of the range from the Hudson Valley. In the early 19th century, it was a frequent subject of works by Thomas Cole and other artists of the Hudson River School. Their works helped establish the Catskill Mountain House and other hotels around North-South Lake as the fashionable summer vacation spot for wealthy Americans of the era. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Catskill High Peaks
The Catskill High Peaks are all of the mountains in New York's Catskill Mountains above in elevation whose summits are separated either by ''or'' a vertical drop of at least between it and the next nearest separate summit. By usual standards, these mountains are rather low and rounded, and mostly covered by vegetation. Unlike the Adirondack High Peaks, those in the Catskills are more evenly distributed around the eastern half of the range instead of being confined to one small area. All except Bearpen and Vly lie within the Catskill Park Blue Line. The 3500s The elevation was chosen in the early 1950s when Dan Smiley, a descendant of the founders of Mohonk Mountain House and his fellow birders were trying to find the elusive Bicknell's thrush, which prefers to nest and breed in the boreal forests that predominate above that elevation in the Catskills. They drew up a list nearly identical to the one below and published it in a naturalists' journal. A decade later hikers ... [...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] |
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] |
Slide Mountain (New York)
Slide Mountain is the highest peak in the Catskill Mountains of the U.S. state of New York. It is located in the town of Shandaken in Ulster County. While the contour line on topographic maps is generally accepted as its height, the exact elevation of the summit has never been officially determined by the U.S. Coast and Geodetic Survey, and many informal surveys suggest the mountain may actually top 4,200 feet (1,280 m) above sea level. While it was not identified as the range's highest peak until the late 19th century, it has played a prominent role in Catskill history. Renowned naturalist John Burroughs wrote memorably of his climbs up Slide, and it helped get the Catskills added to New York's Forest Preserve. Bicknell's thrush was first identified on its summit. Geography Like most other Catskill peaks, Slide's summit is gentle and rounded, taking the form of a narrow ridge that rises to a wider bump on its eastern end. From there the mountain slopes down steeply to the c ... [...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] |
Plattekill Creek
Plattekill Creek is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map, accessed April 15, 2020 tributary of Esopus Creek in the Catskill Mountains in the U.S. state of New York. From its source on the southern slopes of Kaaterskill High Peak, it flows across Ulster and Greene counties to the Esopus at Mount Marion. The name is a Dutch word meaning "flat brook". Plattekill Creek passes through the Platte Clove Preserve, which is a 208-acre nature preserve, that includes Plattekill Falls along with other waterfalls and also trails. The preserve is located in Platte Clove in the town of Hunter. Recreation New York's Department of Environmental Conservation (DEC) regularly stocks fish in the creek to supplement the native population. In spring 2020, the DEC stocked 360 and 2060 long brown trout into the creek in April, then another 1140 brown trout in May. Hydrology New York's Department of Environmental Conservation ( ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kaaterskill Creek
Kaaterskill Creek is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map , accessed October 3, 2011 tributary of Catskill Creek in Greene and Ulster counties in New York. Via Catskill Creek, it is part of the Hudson River watershed. Kaaterskill Creek rises in the town of Hunter within the Catskill Forest Preserve, northwest of the village of Tannersville. It flows south to the hamlet of Haines Falls, where it turns east and drops precipitously into Kaaterskill Clove, paralleled by New York Route 23A and receiving Spruce Creek from the north, which drops over Kaaterskill Falls Kaaterskill Falls is a two-stage waterfall on Spruce Creek in the eastern Catskill Mountains of New York, between the hamlets of Haines Falls and Palenville in Greene County. The two cascades total 260 feet (79 m) in height, making Kaaterskil .... Kaaterskill Creek exits the mountains at the hamlet of Palenville and takes a zigzag course, crossing b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Drainage
Drainage is the natural or artificial removal of a surface's water and sub-surface water from an area with excess of water. The internal drainage of most agricultural soils is good enough to prevent severe waterlogging (anaerobic conditions that harm root growth), but many soils need artificial drainage to improve production or to manage water supplies. History Early history The Indus Valley civilization had sewerage and drainage systems. All houses in the major cities of Harappa and Mohenjo-daro had access to water and drainage facilities. Waste water was directed to covered gravity sewers, which lined the major streets. 18th and 19th century The invention of hollow-pipe drainage is credited to Sir Hugh Dalrymple, who died in 1753. Current practices Geotextiles New storm water drainage systems incorporate geotextile filters that retain and prevent fine grains of soil from passing into and clogging the drain. Geotextiles are synthetic textile fabrics specially ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kaaterskill Clove
Kaaterskill Clove is a deep gorge, or valley, in New York's eastern Catskill Mountains, lying just west of the village of Palenville and in Haines Falls. The clove was formed by Kaaterskill Creek, a tributary of Catskill Creek rising west of North Mountain, and is estimated by geologists to be as much as 1 million years old.Dunn, Russell: Catskill Region Waterfall Guide, Kaaterskill High Peak and Roundtop Mountain rise to the south of the gorge, while South Mountain is to its north. This makes the gorge as deep as 2,500 feet in places. History Little is known of Kaaterskill Clove's history prior to 1817, when Gilbert Palen built a tannery near the entrance to Kaaterskill Clove, giving the village of Palenville its name. After the War of 1812, with Americans free to pursue trade without fearing the interference of Great Britain, industry throughout the United States began to expand, with Palenville and Kaaterskill Clove becoming the site of many tanneries due to the large ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Platte Clove
Platte Clove, sometimes Plattekill Clove, is a narrow and steep valley in the Catskill Mountains of New York. The valley is situated between Kaaterskill High Peak and Roundtop Mountain to the north and Plattekill Mountain and Indian Head Mountain to the south. It is mostly in Greene County, although the lowest, eastern portions are in Ulster County. The stream that runs below is called Plattekill Creek. A few hiking trails go through the Clove including Devil's Path and Huckleberry Point Trail. The area hosts bicycle racing events. Geography Along with Kaaterskill Clove on the other side of Kaaterskill High Peak, Platte Clove is one of only two breaks in the Catskill Escarpment. A narrow, two-lane road that climbs along the clove's north wall is the only route through the valley. This road, called Platte Clove Road, runs from Blue Mountain Road / Harry Wells Road in West Saugerties in the southeast until Rt 23A in Tannersville in the northwest. The cliffs near ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Catskills Beyond Hudson
The Catskill Mountains, also known as the Catskills, are a physiographic province 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 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). 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
