Newburgh is a town in Orange County, New York, United States. It forms part of the Poughkeepsie—Newburgh—Middletown metropolitan area, which is a part of the New York megacity, and is a suburban satellite of the urbanized city of Newburgh. The city of Newburgh was a part of the town prior to 1865. New York Stewart International Airport is partially located within the township, and much of the land into which it could have been expanded has been turned into Stewart State Forest.
Lake Havasu is a large reservoir formed by Parker Dam on the Colorado River, on the border between San Bernardino County, California and Mohave County, Arizona. Lake Havasu City sits on the Arizonan side of the lake with its Californian counterpart of Havasu Lake directly across the lake. The reservoir has an available capacity of 619,400 acre-feet (0.7640 km3). The concrete arch dam was built by the United States Bureau of Reclamation between 1934 and 1938. The lake's primary purpose is to store water for pumping into two aqueducts. Prior to the dam construction, the area was home to the Mojave people. The lake was named after the Mojave word for blue. In the early 19th century, it was frequented by beaver trappers. Spaniards also began to mine the areas along the river.
The Dale Hollow Reservoir is a reservoir situated on the Kentucky/Tennessee border. The lake is formed by the damming of the Obey River, 7.3 miles (11.7 km) above its juncture with the Cumberland River at river mile 380. Portions of the lake also cover the Wolf River. Dale Hollow is one of four major flood control reservoirs for the Cumberland; the others being Percy Priest Lake, Lake Cumberland, and Center Hill Lake. It is also the site of Dale Hollow Lake State Park on the north (Kentucky) side.
The Wachusett Reservoir is the second largest body of water in the state of Massachusetts. It is located in central Massachusetts, northeast of Worcester. It is part of the water supply system for metropolitan Boston maintained by the Massachusetts Water Resources Authority (MWRA). It has an aggregate capacity of 65 billion US gallons (250,000,000 m3) and an area of almost 7 square miles (18 km2). Water from the reservoir flows to the covered Norumbega Storage Facility via the Cosgrove Tunnel and the MetroWest Water Supply Tunnel. The reservoir has a maximum depth of 120 feet (37 m) and a mean depth of 48 feet (15 m).
New York State Route 300 (NY 300) is a state highway located west of the city of Newburgh in the Hudson Valley of New York in the United States. The southern terminus of the route is at a five-way intersection with NY 32 and NY 94 in the hamlet of Vails Gate. From there, it runs generally northwesterly through the towns of New Windsor, Newburgh, and Shawangunk, to a junction with NY 208 near the hamlet of Wallkill. NY 300's two major changes of direction are marked by slightly unorthodox intersections with other state highways.
Rondout Reservoir is part of New York City's water supply network. It is located 75 miles (121 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.
The Ashokan Reservoir is a reservoir in Ulster County, New York. It is at the eastern end of the Catskill Park, and is one of several in the region created to provide the City of New York with water. It is the city's deepest reservoir at 190 feet (58 m) near the dam at the former site of Bishop Falls.
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 (121 km) northwest of the City.
The Pepacton Reservoir, also known as the Downsville Reservoir, is a reservoir in Delaware County, New York on the East Branch of the Delaware River in the Catskill Mountains of New York. Part of the New York City water supply system, it was formed by the construction of Downsville Dam, and impounds over one-quarter of the East Branch's flow.
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 Kensico Reservoir is a reservoir spanning the towns of Armonk and Valhalla, New York, located 3 miles (5 km) north of White Plains. It was formed by the original earth and gravel Kensico Dam constructed in 1885, which impounded waters from the Bronx and Byram rivers. In 1917, a new masonry dam was completed, replacing the old dam and expanding the water supply by bringing water from the Catskill Mountains over a distance of more than 100 miles.
The Boyds Corner Reservoir is a small reservoir in Putnam County, New York. It is in the town of Kent, New York, and is about 50 miles north of New York City. It is the northernmost reservoir in the Croton River watershed, but is not part of the New York City water supply system's Croton Watershed. and was formed by impounding the middle of the West Branch of the Croton River, submerging the village of Boyds Corner.
Lake Washington is the primary reservoir for the city of Newburgh, New York, United States. It is located just southwest of the city, lying partially within it and the neighboring towns of Newburgh and New Windsor. It holds approximately 1.5 billion US gallons (5,700,000 m3), an amount equivalent to the city's annual consumption.
Browns Pond, in the Town of New Windsor in Orange County, New York, United States, is the smaller of two reservoirs for the nearby City of Newburgh. The 0.3 square mile pond is hook-shaped, with the circuitous Mount Airy Road running past both ends.
Quassaick Creek is an 18.4-mile-long (29.6 km) tributary of the Hudson River in Orange and Ulster counties in the U.S. state of New York. It rises in the glacial ridges west of the river, near the boundary between the towns of Plattekill and Marlborough. From there it flows south into the town of Newburgh and then the city, where it eventually forms part of the border between it and neighboring New Windsor before emptying into the Hudson.
Little Seneca Lake is a reservoir located near the Boyds community in Montgomery County, Maryland.
Lake Gleneida is a controlled lake in the hamlet of Carmel within the Town of Carmel in central Putnam County, New York. Originally a smaller natural water body, Shaw's Pond, it was dammed by New York City in 1870 and enlarged to 168 acres (68 ha) for inclusion in its water supply system. It is part of the New York City water system's Croton Watershed.
Lake Shenorock is a lake located in the hamlet of Shenorock in the town of Somers, New York. The lake is used for fishing and was used for recreational swimming until the Clean Water Act was passed and the lake became a source of drinking water. The Clean Water Act was passed in 1972, recreational swimming ended in 1977. The lake is part of the Croton Reservoir System and is a tributary to the Amawalk Reservoir, which is used as a source of water for New York City residents. There are no major tributaries to the class B lake.
[[File:Crotonrivermap.png|thumb|right|Map of the Croton River watershed. Note that this is not identical with the New York City water supply system's "Croton Watershed"{{efn|Numerous small natural lakes and ponds, as well as large Lake Mahopac, are part of the Croton River's watershed but not part of New York City’s supply system. A map of the actual Croton Watershed is found here. ]]
This page is about the Croton River watershed, a hydrological feature. For the component of the New York City water supply system with a similar name, see Croton Watershed
