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West Branch Of The Delaware River
The West Branch Delaware River is one of two branches that form the Delaware River. It is approximately 90 mi (144 km) long, and flows through the U.S. states of New York and Pennsylvania. It winds through a mountainous area of New York in the western Catskill Mountains for most of its course, before joining the East Branch along the northeast border of Pennsylvania with New York. Midway or so it is empounded by the Cannonsville Dam to form the Cannonsville Reservoir, both part of the New York City water supply system for delivering drinking water to the City. Course It rises in Schoharie County, New York and flows generally southwest, entering Delaware County and flowing past Stamford and Delhi. In southwestern Delaware County it flows in an increasingly winding course through the mountains, generally southwest. At Stilesville it is impounded to form the Cannonsville Reservoir. At Deposit, on the border between Broome and Delaware counties, it turns sharply to the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hamden Covered Bridge
Hamden Bridge is a wooden covered bridge over the West Branch of the Delaware River in the hamlet of Hamden, New York, Hamden in Delaware County, New York. It was built in 1859, and is a single span, timber and plan framed bridge. It measures 128 feet long and 18 feet wide. A supporting center pier was added in 1940. ''Note:'' This includes an''Accompanying photographs''/ref> It was listed on the National Register of Historic Places in 1999. See also *List of bridges on the National Register of Historic Places in New York *National Register of Historic Places listings in Delaware County, New York References External links Hamden Bridge, at New York State Covered Bridge Society {{NRHP bridges Covered bridges on the National Register of Historic Places in New York (state) National Register of Historic Places in Delaware County, New York Bridges completed in 1859 Wooden bridges in New York (state) Bridges in Delaware County, New York Tourist attractions in Delaware Count ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Little Delaware River
Little Delaware River is a river in Delaware County, New York. It begins along the western slope of Plattekill Mountain, northeast of the Hamlet of Bovina and flows generally westward before converging with the West Branch Delaware River by the Village of Delhi. Fishing In the Little Delaware River the wild brown trout and brook trout populations are supplemented with the stocking of about 700 brown trout yearlings each year. The fish are stocked in a zone at the mouth and a zone downstream of the hamlet of Bovina Center. Brown trout are the dominant wild trout in the stream, but there are also large amounts of brook trout upstream of Bovina Center. Watershed The Little Delaware River's watershed makes up for 7.84% of the West Branch Delaware River's drainage area. Hydrology The United States Geological Survey (USGS) maintains one stream gauge along the Little Delaware River. The station by the Village of Delhi Delhi, officially the National Capital Territory (N ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stream Gauge
A stream gauge, streamgage or stream gauging station is a location used by hydrologists or environmental scientists to monitor and test terrestrial bodies of water. Hydrometric measurements of water level surface elevation ("stage") and/or volumetric discharge (flow) are generally taken and observations of biota and water quality may also be made. The locations of gauging stations are often found on topographical maps. Some gauging stations are highly automated and may include telemetry capability transmitted to a central data logging facility. Measurement equipment Automated direct measurement of streamflow discharge is difficult at present. In place of the direct measurement of streamflow discharge, one or more surrogate measurements can be used to produce discharge values. In the majority of cases, a stage (the elevation of the water surface) measurement is used as the surrogate. Low gradient (or shallow-sloped) streams are highly influenced by variable downstream c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
United States Geological Survey
The United States Geological Survey (USGS), formerly simply known as the Geological Survey, is a scientific agency of the United States government. The scientists of the USGS study the landscape of the United States, its natural resources, and the natural hazards that threaten it. The organization's work spans the disciplines of biology, geography, geology, and hydrology. The USGS is a fact-finding research organization with no regulatory responsibility. The agency was founded on March 3, 1879. The USGS is a bureau of the United States Department of the Interior; it is that department's sole scientific agency. The USGS employs approximately 8,670 people and is headquartered in Reston, Virginia. The USGS also has major offices near Lakewood, Colorado, at the Denver Federal Center, and Menlo Park, California. The current motto of the USGS, in use since August 1997, is "science for a changing world". The agency's previous slogan, adopted on the occasion of its hundredt ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
New York–Pennsylvania Border
The New York–Pennsylvania border is the state line between the U.S. states of New York and Pennsylvania. It has three sections: * Along the center line of the Delaware River from the Tri-States Monument tripoint with New Jersey at the confluence of the Delaware with the Neversink River in Port Jervis, New York to the 42nd parallel north between Hancock, New York and Deposit, New York about 2.8 km downstream from Hale Eddy; above Hancock this is the West branch of the Delaware; * Across the 42nd parallel north to the corner of the Erie Triangle; * North along the east boundary of the Erie Triangle to Lake Erie. The survey of the 42nd parallel north was carried out in 1785–86 and accepted by the two states in 1787. The surveying technique that was used at the time was not especially accurate, and as such, this boundary wanders a bit on both sides of the true parallel. The 82nd mile stone was used as the starting point of the Preemption Line defined in the Treaty of Hart ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
New York State Route 17
New York State Route 17 (NY 17) is a major state highway that extends for through the Southern Tier and Downstate regions of New York in the United States. It begins at the Pennsylvania state line in Mina and follows the Southern Tier Expressway east through Corning to Binghamton and the Quickway from Binghamton east to Woodbury, where it turns south to follow the Orange Turnpike to the New Jersey state line near Suffern, where it connects to New Jersey Route 17. From the Pennsylvania border to the village of Waverly and from Binghamton to Windsor, NY 17 is concurrent with Interstate 86 (I-86). Eventually, the entire east–west portion of NY 17 from the Pennsylvania border to Woodbury will become I-86 as projects to upgrade the route to Interstate Highway standards are completed. At , NY 17 is the longest state route in New York, and is the second-longest highway of any kind in the state, beside the Thruway. It serves 11 counties (Chau ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Broome County, New York
Broome County is a county in the U.S. state of New York. As of the 2020 United States census, the county had a population of 198,683. Its county seat is Binghamton. The county was named for John Broome, the state's lieutenant governor when Broome County was created. The county is part of the Binghamton, NY Metropolitan Statistical Area. It is home to Binghamton University, one of four university centers in the State University of New York (SUNY) system. History When counties were established in the Province of New York in 1683, the present Broome County was part of the enormous Albany County, including the northern part of New York State as well as all of the present State of Vermont and, in theory, extending westward to the Pacific Ocean. This county was reduced in size on July 3, 1766, by the creation of Cumberland County, and further on March 16, 1770, by the creation of Gloucester County, both containing territory now in Vermont. On March 12, 1772, what was left of Alb ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stilesville, New York
Stilesville is a hamlet in Delaware County, New York. It is located northeast of Deposit at the intersection of NY Route 8 and NY Route 10. The West Branch Delaware River The West Branch Delaware River is one of two branches that form the Delaware River. It is approximately 90 mi (144 km) long, and flows through the U.S. states of New York and Pennsylvania. It winds through a mountainous area of New York ... flows west through the hamlet. References Geography of Delaware County, New York Hamlets in Delaware County, New York Hamlets in New York (state) {{DelawareCountyNY-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
New York City Water Supply System
A combination of aqueducts, reservoirs, and tunnels supplies fresh water to New York City. With three major water systems ( Croton, Catskill, and Delaware) stretching up to away from the city, its water supply system is one of the most extensive municipal water systems in the world. New York's water treatment process is simpler than most other American cities. This largely reflects how well protected its watersheds are. The city has sought to restrict development surrounding them. One of its largest watershed protection programs is the Land Acquisition Program, under which the New York City Department of Environmental Protection (DEP) has purchased or protected, through conservation easement, over since 1997. With all the care given, the city's water supply system is partially exempted from filtration requirements by both the federal and the state government, saving more than "$10 billion to build a massive filtration plant, and at least another $100 million annually on it ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cannonsville Reservoir
The Cannonsville Reservoir is a reservoir in the New York City water supply system in Delaware County, New York. It was formed by construction of the Cannonsville Dam on its west end, which impounded over half of the West Branch of the Delaware River. Lying on the western part of the Delaware Watershed, it is the westernmost of New York City's reservoirs. It was placed in service in 1964, and is the most recently constructed New York City-owned reservoir. The town of Cannonsvile was destroyed to make room for the reservoir, which lies within the towns of Tompkins and Deposit. Its drainage basin is the largest of all of the NYC reservoirs. Capacity is . Water from the reservoir flows through the West Delaware Tunnel into the Rondout Reservoir, before joining the Delaware Aqueduct, which provides New York City with about 50% of its drinking water. The Delaware Aqueduct then crosses beneath the Hudson River and continues on to the West Branch Reservoir in Putnam County, Ne ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cannonsville Dam
The Cannonsville Reservoir is a reservoir in the New York City water supply system in Delaware County, New York. It was formed by construction of the Cannonsville Dam on its west end, which impounded over half of the West Branch of the Delaware River. Lying on the western part of the Delaware Watershed, it is the westernmost of New York City's reservoirs. It was placed in service in 1964, and is the most recently constructed New York City-owned reservoir. The town of Cannonsvile was destroyed to make room for the reservoir, which lies within the towns of Tompkins and Deposit. Its drainage basin is the largest of all of the NYC reservoirs. Capacity is . Water from the reservoir flows through the West Delaware Tunnel into the Rondout Reservoir, before joining the Delaware Aqueduct, which provides New York City with about 50% of its drinking water. The Delaware Aqueduct then crosses beneath the Hudson River and continues on to the West Branch Reservoir in Putnam County, New ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
East Branch Delaware River
The East Branch Delaware River is one of two branches that form the Delaware River. It is approximately 75 mi (121 km) long, and flows through the U.S. state of New York. It winds through a mountainous area on the southwestern edge of Catskill Park in the Catskill Mountains for most of its course, before joining the West Branch along the northeast border of Pennsylvania with New York. For a long stretch it serves as the Blue Line, the park's boundary. Much of it is paralleled by State Route 30. The river was impounded just north of Downsville in the mid-20th century to create Pepacton Reservoir, part of the New York City water supply system supplying drinking water to the City. It is a popular destination for fly fishing for brown trout. In 1881 John Burroughs, a native of the area, published "A Summer Voyage", recounting a solo boat trip down the East Branch from Arkville to Hancock. There are many variant names for the river that include: Papaconck, Papakonk River ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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