[[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. ]]
The Croton Watershed is the New York City water supply system's name for its southernmost watershed and its infrastructure, [lower-alpha 1] an organized entity rather than a mere hydrological feature. Spanning large swaths of Putnam and Westchester counties in far southeastern New York State, it represents the drainage, flow, and operating systems of some seven rivers, one dozen reservoirs, and three controlled lakes [1] [2] falling within the Croton River watershed. [lower-alpha 2]
Over 350 square miles (910 km2) in area, the Watershed holds some 100 billion US gallons (380,000,000 m3) of fresh water. [lower-alpha 3] The vast majority of this ends up at the Jerome Park Reservoir in the Bronx via the New Croton Aqueduct, from which it is distributed. Water in excess of New York City's needs spills over the New Croton Dam at the New Croton Reservoir and is carried by the Croton River into the Hudson River at Croton-on-Hudson, New York, about 30 miles north of the Metropolitan area.
The Croton Watershed is a term describing a part of the New York City water supply system. It is not synonymous with the biological feature Croton River watershed. Numerous small natural lakes and ponds, as well as large Lake Mahopac, are within the river's watershed but not part of the NYC water supply system (even though they too ultimately drain into it). A map of the actual Croton Watershed is found here.
The Croton River ( /ˈkroʊtən/ KROH-tən) is a river in southern New York with three principal tributaries: the West Branch, Middle Branch, and East Branch. Their waters, all part of the New York City water supply system, [3] join downstream from the Croton Falls Reservoir. [lower-alpha 4] Together, their waters and the reservoirs linked to them represent the northern half of the New York City water system's Croton Watershed.
Shortly after the confluence of the three Croton River branches the Croton River proper, along with its tributary, the Muscoot River, flows into the Muscoot Reservoir, after which it empties into the New Croton Reservoir, which feeds the New Croton Aqueduct supplying water to New York City via the Jerome Park Reservoir in the Bronx. Excess water leaves the spillway at the New Croton Dam and empties into the Hudson River at Croton-on-Hudson, New York at Croton Point, about 30 miles (50 km) north of New York City. [4] The river has a watershed area of 361 square miles (930 km2). [4]
Limited recreation is permitted within the Croton Watershed. Its guidelines and requirements are listed here.
A combination of aqueducts, reservoirs, and tunnels supplies fresh water to New York City. With three major water systems stretching up to 125 miles (201 km) away from the city, its water supply system is one of the most extensive municipal water systems in the world.
Titicus Reservoir is one of 12 in the New York City water supply system's Croton Watershed. It is located in the Town of North Salem in Westchester County, 30 miles (48 km) north of the city of New York.
East Branch Reservoir, is a reservoir in the town of Southeast, New York, near the village of Brewster. Part of the New York City water supply system, it was formed by impounding the East Branch of the Croton River. Forming part of the Croton Watershed, it was placed into service in 1891, and lies some 35 miles (56 km) north of the city, in the southeast corner of Putnam County.
The Kensico Reservoir is a reservoir spanning the towns of Armonk and Valhalla, New York, located 3 miles 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 West Branch Reservoir is a reservoir in the New York City water supply system. Formed by impounding the upper reaches of the West Branch of the Croton River, it is located in the Putnam County, New York, towns of Kent, and Carmel, about 50 miles (80 km) north of New York City.
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.
The Amawalk Reservoir is a small reservoir in the New York City water supply system located in central-northern Westchester County, New York. It is located at the intersection of U.S. Route 202 and New York State Route 35 in the town of Somers, and is over 32 miles north of New York City. Part of the system's Croton Watershed, it was formed by impounding the middle of the Muscoot River, one of the tributaries of the Croton River. This reservoir was put into service in 1897, and was named after the original community of Amawalk, New York, which was inundated by the reservoir and relocated near the dam.
The Bog Brook Reservoir is a 379-acre (153 ha) reservoir in the Croton Watershed in southern New York State, part of the New York City water supply system. It is located in the town of Southeast in Putnam County, approximately 38 miles (61 km) north of New York City. It was formed by the damming of Bog Brook, a small tributary of the East Branch of the Croton River. The reservoir was put into service in 1892, making it one of the older in the system.
The Cross River Reservoir is a reservoir in the New York City water supply system located directly east and north of the northern Westchester County, New York, Hamlet of Katonah. Part of the system's Croton Watershed, it lies within the towns of Bedford, Lewisboro, and Pound Ridge, about 1 mile (1.6 km) east of the village of Katonah, and over 25 mi (40 km) north of New York City. It was constructed around the start of the 20th century by impounding the Cross River, a tributary of the Croton River, which eventually flows into the Hudson River.
The Croton Falls Reservoir is a reservoir in the New York City water supply system in the Putnam County, New York townships of Carmel, and Southeast, roughly 50 miles (80 km) north of New York City. Part of the system's Croton Watershed, it was formed by impounding the West Branch and Middle Branch of the Croton River, tributaries of the Croton River, which flows into the Hudson River.
The Diverting Reservoir is a reservoir in the New York City water supply system in the town of Southeast, New York, in Putnam County immediately south of the village of Brewster, New York. Part of the system's Croton Watershed, it lies about 50 miles (80 km) north of New York City. Construction impounding the East Branch Croton River began early in the 20th century and was completed by 1911.
The Muscoot Reservoir is a reservoir in the New York City water supply system in northern Westchester County, New York, located directly north of the village of Katonah. Part of the system's Croton Watershed, it is 25 miles north of the City.
The New Croton Reservoir is a reservoir in Westchester County, New York, part of the New York City water supply system lying approximately 22 miles (35 km) north of New York City. It is the collecting point for water from all reservoirs in the Croton Watershed.
The Croton River is a river in southern New York with three principal tributaries: the West Branch, Middle Branch, and East Branch. Their waters, all part of the New York City water supply system, join downstream from the Croton Falls Reservoir. Together, their waters and the reservoirs linked to them represent the northern half of the New York City water system's Croton Watershed.
Lake Gilead is a 116-acre (0.47 km2) controlled lake located in Carmel Hamlet in Putnam County, New York. Originally known as Dean's Pond, it is 0.8 miles long, has a mean depth of 43 feet (13 m), and a maximum depth of approximately 120 feet (37 m). The lake is located within the lower Hudson River basin in the Croton River watershed.
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.
A controlled lake is both a general and specific term to describe a body of water. In its general sense it describes a lake or reservoir which has its water level controlled by some form of dam. In the specific, it refers to three small lakes within the New York City water supply system's Croton Watershed lying within central Putnam County in the state's far southwestern corner.
Kirk Lake is a controlled lake in the hamlet of Mahopac in the town of Carmel in Putnam County, New York. It lies due west and sharply below considerably larger Lake Mahopac. It is one of three controlled lakes in the New York City water supply system's Croton Watershed.
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
The Muscoot River is a short tributary of the Croton River in Putnam and Westchester counties in the state of New York. Approximately 6 mi (9.7 km) long and running north-to-south, it lies within the Croton River watershed and is part of the New York City water supply system's Croton Watershed.