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Notch Lake
Notch Lake is an artificial lake in Edgewood, New York, in the Town of Hunter in the Catskill Mountains. It is located near the Stony Clove Notch, and is located near the edge of the Devil's Tombstone Campsite, bordering New York State Route 214. There is also a parking lot near the shore. It is the beginning of the Stony Clove Creek. One thing unusual about it is that it is one of the few places in the Catskills where there is a patch of Boreal Forest Taiga (; rus, тайга́, p=tɐjˈɡa; relates to Mongolic and Turkic languages), generally referred to in North America as a boreal forest or snow forest, is a biome characterized by coniferous forests consisting mostly of pines, spruc ... growing below 3,000 feet above sea level. A fire occurred near the northern shore in the 1990s. Camping is not allowed at the day-use area next to the parking lot and Pond, however, camping is allowed a short walk South along Route 214 at the Devil's Tombstone Campground. Refer ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Edgewood, New York
Hunter is a town located in Greene County, New York, United States. The population was 2,732 at the time of the 2010 census. The town contains three villages, one named Hunter on the west , another is Lanesville on the southern side of Hunter, and the third called Tannersville the largest and center of the town. The town is on the southern border of Greene County with Lanesville Village adjacent to Ulster County. The Hamlet of Haines Falls is on the east of the town. History The town was formed on January 27, 1813 from the town of Windham, but was then called "Edwardsville". The name of "Hunter" was assumed in 1814, named after John Hunter. Afterwards, the town lost some territory to the town of Saugerties in 1814 and to Jewett in 1849. The area became a popular tourism destination in the late 19th and early 20th centuries. It was served by the Ulster and Delaware Railroad, which brought tourists to resort towns throughout the Catskill Mountains. Geography Accordin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Artificial Lake
A reservoir (; from French ''réservoir'' ) is an enlarged lake behind a dam. Such a dam may be either artificial, built to store fresh water or it may be a natural formation. Reservoirs can be created in a number of ways, including controlling a watercourse that drains an existing body of water, interrupting a watercourse to form an embayment within it, through excavation, or building any number of retaining walls or levees. In other contexts, "reservoirs" may refer to storage spaces for various fluids; they may hold liquids or gasses, including hydrocarbons. ''Tank reservoirs'' store these in ground-level, elevated, or buried tanks. Tank reservoirs for water are also called cisterns. Most underground reservoirs are used to store liquids, principally either water or petroleum. Types Dammed valleys Dammed reservoirs are artificial lakes created and controlled by a dam constructed across a valley, and rely on the natural topography to provide most of the basin of the r ... [...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] |
Hunter (town), New York
Hunter is a town located in Greene County, New York, United States. The population was 2,732 at the time of the 2010 census. The town contains three villages, one named Hunter on the west , another is Lanesville on the southern side of Hunter, and the third called Tannersville the largest and center of the town. The town is on the southern border of Greene County with Lanesville Village adjacent to Ulster County. The Hamlet of Haines Falls is on the east of the town. History The town was formed on January 27, 1813 from the town of Windham, but was then called "Edwardsville". The name of "Hunter" was assumed in 1814, named after John Hunter. Afterwards, the town lost some territory to the town of Saugerties in 1814 and to Jewett in 1849. The area became a popular tourism destination in the late 19th and early 20th centuries. It was served by the Ulster and Delaware Railroad, which brought tourists to resort towns throughout the Catskill Mountains. Geography Accordin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Catskill Mountains
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 comedian ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stony Clove Notch
Stony Clove Notch is a narrow pass, roughly 2,220 feet (677 m) in elevation located in the Town of Hunter in Greene County, New York, deep in the Catskill Mountains. It is traversed by New York State Route 214, although in the past the Ulster and Delaware Railroad went through it as well. The notch divides Hunter and Plateau mountains. There is just enough room for the road, and the steep, soaring slopes of both mountains are some of the Catskills' most striking scenery, with landslides and rocky cliffs visible. It sits at one end of the range of mountains known as the Devil's Path, and early visitors found it a terrifying place to visit. Today it is a popular destination not only for tourists in the region but for outdoor recreationists as well. One of the Catskills' major hiking trails crosses the road near the notch, and ice climbers and snowboarders have lately been attracted to the cliffs and slopes in winter. History Natural origins Stony Clove Notch was created ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
New York State Route 214
New York State Route 214 (NY 214) is a long state highway through the Catskill Park sections of Ulster and Greene counties. The route begins at an intersection with NY 28 in the town of Shandaken, just southwest of the hamlet of Phoenicia. The route runs through the narrow mountain pass called Stony Clove Notch before reaching the town of Hunter, where it ends at NY 23A. NY 214 was part of a tannery road constructed by Colonel William Edwards of Hunter in the late 1840s, opening by 1849. The road was upgraded in 1873 to the Stoney Clove Turnpike, which serviced hotels and resorts in the Catskills. In 1930, the route was designated as NY 214, but the part in Greene County was not state-maintained, instead by the county. From 1946 to 1956, the residents of the hamlet of Lanesville spent time fighting for NY 214 to be reconstructed due to being an unsafe dirt road for their children to attend school using their bus. After two sections were com ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Boreal Forest
Taiga (; rus, тайга́, p=tɐjˈɡa; relates to Mongolic and Turkic languages), generally referred to in North America as a boreal forest or snow forest, is a biome characterized by coniferous forests consisting mostly of pines, spruces, and larches. The taiga or boreal forest has been called the world's largest land biome. In North America, it covers most of inland Canada, Alaska, and parts of the northern contiguous United States. In Eurasia, it covers most of Sweden, Finland, much of Russia from Karelia in the west to the Pacific Ocean (including much of Siberia), much of Norway and Estonia, some of the Scottish Highlands, some lowland/coastal areas of Iceland, and areas of northern Kazakhstan, northern Mongolia, and northern Japan (on the island of Hokkaidō). The main tree species, depending on the length of the growing season and summer temperatures, vary across the world. The taiga of North America is mostly spruce, Scandinavian and Finnish taiga consists of a m ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Reservoirs In New York (state)
A reservoir (; from French ''réservoir'' ) is an enlarged lake behind a dam. Such a dam may be either artificial, built to store fresh water or it may be a natural formation. Reservoirs can be created in a number of ways, including controlling a watercourse that drains an existing body of water, interrupting a watercourse to form an embayment within it, through excavation, or building any number of retaining walls or levees. In other contexts, "reservoirs" may refer to storage spaces for various fluids; they may hold liquids or gasses, including hydrocarbons. ''Tank reservoirs'' store these in ground-level, elevated, or buried tanks. Tank reservoirs for water are also called cisterns. Most underground reservoirs are used to store liquids, principally either water or petroleum. Types Dammed valleys Dammed reservoirs are artificial lakes created and controlled by a dam constructed across a valley, and rely on the natural topography to provide most of the basin of the re ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Reservoirs In Greene County, New York
A reservoir (; from French ''réservoir'' ) is an enlarged lake behind a dam. Such a dam may be either artificial, built to store fresh water or it may be a natural formation. Reservoirs can be created in a number of ways, including controlling a watercourse that drains an existing body of water, interrupting a watercourse to form an embayment within it, through excavation, or building any number of retaining walls or levees. In other contexts, "reservoirs" may refer to storage spaces for various fluids; they may hold liquids or gasses, including hydrocarbons. ''Tank reservoirs'' store these in ground-level, elevated, or buried tanks. Tank reservoirs for water are also called cisterns. Most underground reservoirs are used to store liquids, principally either water or petroleum. Types Dammed valleys Dammed reservoirs are artificial lakes created and controlled by a dam constructed across a valley, and rely on the natural topography to provide most of the basin of the res ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
