|
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 or tayga ( ; , ), also known as boreal forest or snow forest, is a biome characterized by pinophyta, coniferous forests consisting mostly of pines, spruces, and larches. The taiga, or boreal forest, is the world's largest land biome. I ... growing at an elevation below . 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. References ... [...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 3,035 at the time of the 2020 census.U.S. Census Bureau, 2020 census results. https://www.census.gov/search-results.html?searchType=web&cssp=SERP&q=Hunter%20town,%20Greene%20County,%20New%20York The town contains two villages, one named Hunter on the west, and the second called Tannersville, as well as a number of hamlets such as Haines Falls, Platte Clove, Lanesville and Edgewood. Additionally, there are three residential parks location within town limits: Onteora Park, Twilight Park and Elka Park. The town is on the southern border of Greene County and abuts the towns of Woodstock and Saugerties, located in Ulster County. 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 Saugerties in 1814 and to Jewett in 18 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Artificial Lake
A lake is often a naturally occurring, relatively large and fixed body of water on or near the Earth's surface. It is localized in a basin or interconnected basins surrounded by dry land. Lakes lie completely on land and are separate from the ocean, although they may be connected with the ocean by rivers. Lakes, as with other bodies of water, are part of the water cycle, the processes by which water moves around the Earth. Most lakes are fresh water and account for almost all the world's surface freshwater, but some are salt lakes with salinities even higher than that of seawater. Lakes vary significantly in surface area and volume of water. Lakes are typically larger and deeper than ponds, which are also water-filled basins on land, although there are no official definitions or scientific criteria distinguishing the two. Lakes are also distinct from lagoons, which are generally shallow tidal pools dammed by sandbars or other material at coastal regions of oceans or larg ... [...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 3,035 at the time of the 2020 census.U.S. Census Bureau, 2020 census results. https://www.census.gov/search-results.html?searchType=web&cssp=SERP&q=Hunter%20town,%20Greene%20County,%20New%20York The town contains two villages, one named Hunter on the west, and the second called Tannersville, as well as a number of hamlets such as Haines Falls, Platte Clove, Lanesville and Edgewood. Additionally, there are three residential parks location within town limits: Onteora Park, Twilight Park and Elka Park. The town is on the southern border of Greene County and abuts the towns of Woodstock and Saugerties, located in Ulster County. 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 Saugerties in 1814 and to Jewett in 18 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Catskill Mountains
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 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 ... [...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 du ... [...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 County, New York, Ulster and Greene County, New York, Greene counties. The route begins at an intersection with New York State Route 28, NY 28 in the town of Shandaken, New York, Shandaken, just southwest of the Hamlet (New York), hamlet of Phoenicia, New York, Phoenicia. The route runs through the narrow mountain pass called Stony Clove Notch before reaching the town of Hunter (town), New York, Hunter, where it ends at New York State Route 23A, 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Boreal Forest
Taiga or tayga ( ; , ), also known as boreal forest or snow forest, is a biome characterized by pinophyta, coniferous forests consisting mostly of pines, spruces, and larches. The taiga, or boreal forest, is 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 Hokkaido). The principal 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 Finland, Finnish taiga consists of a mix of Norway spruce, spruce, pines and Betula, birch; Russian taiga has spruces, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Reservoirs In New York (state)
A reservoir (; ) is an enlarged lake behind a dam, usually built to store fresh water, often doubling for hydroelectric power generation. Reservoirs are created by controlling a watercourse that drains an existing body of water, interrupting a watercourse to form an embayment within it, excavating, or building any number of retaining walls or levees to enclose any area to store water. 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 reservoir. These reservoirs can either be ''on-stream reservoirs'', which are located on the original streambed of the downstream river and are filled by creeks, rivers or rainwater that runs off the surrounding forested catchments, or '' off-stream reservoirs'', which receive diverted water from a nearby stream or aqueduct or pipeline water from other on-stream reservoirs. Dams are typicall ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Reservoirs In Greene County, New York
A reservoir (; ) is an enlarged lake behind a dam, usually built to store fresh water, often doubling for hydroelectric power generation. Reservoirs are created by controlling a watercourse that drains an existing body of water, interrupting a watercourse to form an embayment within it, excavating, or building any number of retaining walls or levees to enclose any area to store water. 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 reservoir. These reservoirs can either be ''on-stream reservoirs'', which are located on the original streambed of the downstream river and are filled by creeks, rivers or rainwater that runs off the surrounding forested catchments, or ''off-stream reservoirs'', which receive diverted water from a nearby stream or aqueduct or pipeline water from other on-stream reservoirs. Dams are typically loca ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
