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Neversink River
The Neversink River (also called Neversink Creek in its upper course) is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map accessed April 1, 2011 tributary of the Delaware River in southeastern New York (state), New York in the United States. The name of the river comes from the corruption of an Algonquin language, Algonquian language phrase meaning "mad river." The Neversink River is considered by many to be the birthplace of American dry fly fishing.Askins, Justin. ''The Legendary Neversink: A Treasury of the Best Writing About One of America's Great Trout Rivers'', Skyhorse Publishing, 2007, page xv Course The Neversink's main flow begins just south of the border between present-day Ulster County, New York, Ulster and Sullivan County, New York, Sullivan County (United States), counties, where the east and west branches of the river join near the hamlet (place), hamlet of Claryville, New York, Claryville. Both branches begin o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
United States
The United States of America (U.S.A. or USA), commonly known as the United States (U.S. or US) or America, is a country primarily located in North America. It consists of 50 states, a federal district, five major unincorporated territories, nine Minor Outlying Islands, and 326 Indian reservations. The United States is also in free association with three Pacific Island sovereign states: the Federated States of Micronesia, the Marshall Islands, and the Republic of Palau. It is the world's third-largest country by both land and total area. It shares land borders with Canada to its north and with Mexico to its south and has maritime borders with the Bahamas, Cuba, Russia, and other nations. With a population of over 333 million, it is the most populous country in the Americas and the third most populous in the world. The national capital of the United States is Washington, D.C. and its most populous city and principal financial center is New York City. Paleo-Americ ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dry Fly Fishing
Dry fly fishing is an angling technique in which the lure is an artificial fly which floats on the surface of the water and does not sink below it. Developed originally for trout fly fishing. The fish and the dry fly Fly fishing for trout can be done using various methods and types of flies. Trout mostly feed near the bed of the stream, where wet flies and especially nymphs are used. They typically only come to the surface to feed when there is a large bug hatch during which thousands of aquatic insects grow wings and leave the water to mate and lay eggs. Particularly during the summer months and on smaller mountain streams, trout also often feed on terrestrial insects such as ants, beetles and grasshoppers when they fall onto the water surface. It is on these surface-feeding occasions that the dry fly can be an effective lure. At certain times, salmon will also rise to a fly on the surface and dry flies may also be used to fish for them. The aim of dry-fly fishing is to mimic ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
South Fallsburg, New York
South Fallsburg is a hamlet and census-designated place in Sullivan County, New York, United States. South Fallsburg is located within the Town of Fallsburg at (41.716489, -74.630279). History South Fallsburg is located in the one-time resort area of the Catskill Mountains known as the Borscht Belt. The Raleigh Hotel on Heiden Road is a 320-room Glatt Kosher Cholov Yisrael hotel for Hasidic Jews sitting on ; it also serves as a convention center for religious and nonreligious groups. The Rivoli Theatre and South Fallsburg Hebrew Association Synagogue are listed on the National Register of Historic Places. The town is home to a center of Siddha Yoga, the Shree Muktananda Ashram of the SYDA Foundation. Demographics As of the 2010 United States Census, there were 2,870 people, 909 households, and 606 families residing in South Fallsburg. There were 1,385 housing units. The racial makeup of the CDP included 63.7% White and 14.2% African American. Hispanic or Latino of any race w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fallsburg (CDP), New York
Fallsburg is a hamlet and census-designated place (CDP) in the town of Fallsburg in Sullivan County, New York, United States. It was first listed as a CDP prior to the 2020 census. The community is in eastern Sullivan County, in the center of the town of Fallsburg. It is bordered to the south by South Fallsburg and to the north by Woodbourne. The Neversink River, a tributary of the Delaware River, flows from north to south through the community. New York State Route 42 passes through the community, following the west side of the Neversink. The highway leads north to Woodbourne and to Grahamsville, while to the southwest it leads to Monticello Monticello ( ) was the primary plantation of Founding Father Thomas Jefferson, the third president of the United States, who began designing Monticello after inheriting land from his father at age 26. Located just outside Charlottesville, V .... Demographics References Census-designated places in Sullivan County, Ne ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Woodbourne, New York
Woodbourne is a hamlet (and census-designated place) in the town of Fallsburg in Sullivan County, New York, United States. Woodbourne is bordered by the town of Neversink, the hamlet of Grahamsville, the hamlet of Loch Sheldrake, the hamlet of Old Falls and the hamlet of Hasbrouck. The major thoroughfares of Woodbourne are New York State Routes 42 and 52. The center of the hamlet is where the two highways briefly overlap and cross the Neversink River. Woodbourne is in the Catskills Borscht Belt and in its heyday was home to many summer hotels, bungalow colonies and boarding houses, which are mainly uninhabited throughout most of the calendar year. To this day, the population of Woodbourne and nearby areas increases dramatically each summer with an influx of Orthodox Jewish residents from New York City, New Jersey and other surrounding Jewish population centers. With this, the local economy expands in the warmer months as locally owned small businesses thrive until approximatel ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fallsburg, New York
Fallsburg is a town in Sullivan County, New York, United States. The town is in the eastern part of the county. The population was 14,192 at the 2020 census. (It is not to be confused with the hamlet of Fallsburg which bears a similar name and is within the town of Fallsburg.) History On March 9, 1826, the New York State Legislature passed an act establishing the town of Fallsburg. The town was created from parts of the towns of Thompson and Neversink. Fallsburg takes its name from a waterfall on the Neversink River and was established in 1826. One month later, on April 4, the first town meeting was held in the schoolhouse where the hamlet of Fallsburg is today. The Neversink River runs from north to south through the town and played an important role in its early development. In the late 1780s, the valley above the falls on the Neversink was known as having fertile and cheap land. This brought an influx of settlers from Ulster County. By 1800, the upper areas along the rive ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Delaware Aqueduct
The Delaware Aqueduct is an aqueduct in the New York City water supply system. It takes water from the Rondout, Cannonsville, Neversink, and Pepacton reservoirs on the west bank of the Hudson River through the Chelsea Pump Station, then into the West Branch, Kensico, and Hillview reservoirs on the east bank, ending at Hillview in Yonkers, New York. The aqueduct was constructed between 1939 and 1945, and carries approximately half of New York City's water supply of per day. At wide and long, the Delaware Aqueduct is the world's longest tunnel. Reservoirs and watersheds The Delaware Aqueduct carries water from the , watershed using the Rondout, Cannonsville, Neversink and Pepacton reservoirs with the Delaware and Neversink tunnels. (The latter three reservoirs are within the Delaware River watershed. Rondout is considered by the New York City Department of Environmental Protection (NYCDEP) to be part of the Delaware system despite being firmly within the Hudson River w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rondout Reservoir
Rondout Reservoir is part of New York City's water supply network. It is located 75 miles (120 km) northwest of the city in the Catskill Mountains, near the southern end of Catskill Park, split between the towns of Wawarsing in Ulster County and Neversink in Sullivan County. It is the central collection point for the city's Delaware System, which provides half its daily consumption. History The reservoir was made possible by the construction of Merriman Dam along Rondout Creek. Construction began in 1937 and ended in 1954, three years after the reservoir began delivering water. It would be the first of four built by the city to satisfy its growing demand in the years after World War II. Three villages – Lackawack, Montela and Eureka – were condemned and flooded in the process. The small settlement of Grahamsville remains in existence just west of the reservoir. In 1998, the city's Department of Environmental Protection (DEP) issued an advisoryNew York City De ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Water Tunnel (physical Infrastructure)
Water tunnels are tunnels (below-ground channels) used to transport water to areas with large populations or agriculture. They are frequently part of aqueducts. Some aqueducts, such as the Delaware Aqueduct are single long tunnels. In other cases, such as the San Jacinto tunnel on the Colorado River Aqueduct, water tunnels form parts of far longer aqueducts. In cases where the outflow of a water tunnel is into an existing stream or river flowing to the point of water use, the term aqueduct is less likely to be used, as with the Harold D. Roberts Tunnel from Dillon Reservoir to the North Fork South Platte River. Notable water tunnels, or systems including water tunnels * Alva B. Adams Tunnel from the western slope of the Colorado River drainage to the eastern Front Range of Colorado, *Angeles Tunnel 7.2 mile (11.6 km) *Bagur Navile Tunnel 6 miles (9.7 km) * Bosporus Water Tunnel *Chicago Tunnel and Reservoir Plan 109.4 miles (176.1 km) *Denver Water **Moffat Tunnel 6.2 mi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Neversink Reservoir
Neversink Reservoir is a reservoir in the New York City water supply system. It is located in the Catskill Mountain town of Neversink in Sullivan County, New York, 75 miles (120.6 km) northwest of the City. It is fed by the Neversink River, the longest tributary of the Delaware River. Water collected in the reservoir in turn goes through the Neversink Tunnel a short distance east to Rondout Reservoir to be pooled with that from Pepacton and Cannonsville reservoirs which form the west-of-the-Hudson River components of the Delaware Aqueduct. Together, they provide nearly half of the city's daily consumption. History Construction began in 1941, as the city realized that after World War II, it would need to increase its supply aggressively to meet explosive growth. Neversink was ultimately chosen after opposition from the region's trout fishermen and the geologic unfeasibility of the site scotched plans for smaller reservoirs along Willowemoc Creek. Two local hamlets wi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Frost Valley YMCA
Frost Valley YMCA is a camping, environmental education, and conferencing center located in Claryville, New York, part of the Catskill Mountains. Founded in 1901 as Camp Wawayanda, the camp moved to its present location in 1958. During the summer, Frost Valley runs a camp for 6–15 year-olds, most of whom are from New York, New Jersey, and Connecticut. Throughout the rest of the year, Frost Valley hosts school groups and other organizations for environmental education and conferencing activities. Summer Camp The summer camp program at Frost Valley runs for eight weeks (four sessions, 12 days each). Each session starts on a Sunday and ends on a Friday, and nearly 500 campers attend each session. About 250 summer-time staff arrive the week before the first session, many of whom were campers when they were younger. Campers are broken up into villages by age and live together in cabin groups. Each village has a corresponding brother or sister village for the oppo ... [...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] |
