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.
|East Branch Reservoir|
|Location||Putnam County, New York|
|Primary inflows||East branch of the Croton River|
|Catchment area||75 sq mi (190 km2)|
|Basin countries||United States|
|Surface area||525 acres (2.12 km2)|
|Average depth||32 ft (9.8 m)|
The East Branch Reservoir has a surface area of 525 acres (2.12 km2), reaches a mean depth of 32 feet (10 m), and holds 5.2 billion US gallons (20,000,000 m3) at full capacity. It drains a 75-square mile (180 km²) area that includes Bog Brook Reservoir. Its water flows back into the East Branch of the Croton River south of the dam, then into The Diverting Reservoir, then via the Croton River to the Muscoot and the New Croton reservoirs, into the New Croton Aqueduct. Water from the aqueduct flows into the Jerome Park Reservoir in the Bronx for daily distribution.
One of two double reservoirs in NYC's system, it is connected to the Bog Brook impoundment via a 1,778-foot (547.07 m) tunnel. When the two were being built, the project's name was "Double Reservoir I". The second double reservoir project ("Double Reservoir II") would create the Croton Falls and Diverting reservoirs.
The village of Southeast Center, named for the town of Southeast, was leveled and flooded to create the reservoir. Parts of the village remain, including Sodom Rd, at the foot of the Sodom Dam, which holds the reservoir back.
Construction of the reservoir also flooded part of the village of Milltown, in the northeastern corner of Southeast, near present-day Deforest Corners. Many of the village's original buildings were moved to higher ground, onto present-day Milltown Rd, one of Southeast's longest roads running from New Fairfield, Connecticut to Route 22 in Southeast. The village of Milltown's 1-room schoolhouse still stands today as a private residence. Foundations, rock walls and roadbeds for both villages can still be seen during droughts.
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.
Its main function is to serve as a storage reservoir for the larger East Branch Reservoir, to which it is connected by a tunnel. The reservoir holds 4.4 billion US gallons (17,000,000 m3) of water at full capacity, and has a drainage basin of four square miles (10 km2).
The Bog Brook Reservoir is one of 12 reservoirs in the Croton Watershed.
From the East Branch Reservoir, the water flows into the continuation of the East Branch of the Croton River, then into The Diverting Reservoir, then via the Croton River to the Muscoot Reservoir and the New Croton Reservoir, into the New Croton Aqueduct, and finally to the Jerome Park Reservoir in the Bronx for distribution to New York City. It then flows through Manhattan, and mixes with the water from the Catskill Aqueduct.Claridon Township, Geauga County, Ohio
Claridon Township is one of the sixteen townships of Geauga County, Ohio, United States. As of the 2010 census the population was 3,205, of whom 2,865 lived in the unincorporated portions of the township.Cohoes Falls
Cohoes Falls [Kahon:ios, Mohawk for "Canoe Falls"] is a waterfall on the Mohawk River shared by the city of Cohoes and the town of Waterford, New York, United States. Discovered by the indigenous people, the falls were called Ga-ha-oose or Ga-ho'n'-yoos by the Mohawks, which is believed to mean "The Place of the Falling Canoe." Cohoes historian Arthur Masten wrote in his 1880 history that the phrase might mean "Potholes in the River," referring to the potholes that appear in the riverbed when it is dry. In the oral tradition of the Haudenosaunee (Iroquois), the Cohoes Falls are the site where The Great Peacemaker, performed a feat of supernatural strength, convincing the Mohawk people to become the founders of the Iroquois League of Nations or Confederacy. Some historians believe the Mohawks launched the Confederacy as early as 1142 CE, though other experts report dates ranging from 1450-1650.
Celebrated by 18th-century travelers in letters and journals, the Cohoes Falls, also called The Great Falls of the Mohawk, were regarded as the second-most beautiful cataract in New York State after Niagara. In 1804, the national poet of Ireland, Thomas Moore, visited Cohoes and wrote a paean to the waterfall's beauty: "Lines Written at the Cohos, or Falls of the Mohawk River."
In 1831, town leaders built a dam across the Mohawk River to harness the power of the falls to fuel the turbines of the city's burgeoning textile industry. Over the next several decades, the predominant company, Harmony Mills, became the largest manufacturer of cotton in the United States, thanks to its control of local water rights. When all the mills closed in the wake of the Great Depression, city leaders neglected the potential of the falls for tourism. They leased the flow rights to a series of power companies, including Niagara Mohawk and Orion Power.
The Erie Canal was planned to overcome the navigational barrier of the Cohoes Falls. The original "Clinton's Ditch", the Erie Canal of 1825, was built through the city of Cohoes. The later Enlarged Canal was realigned, yet still went through the City of Cohoes. The Barge Canal, which opened in 1918, bypasses Cohoes and runs though the Village of Waterford via the Waterford Flight of Locks.
The Cohoes Falls is 90 feet (28 m) high and 1,000 feet (305 m) wide. Its flow is most impressive in springtime, sometimes running at 90,000 cubic feet (2,500 m3) of water per second, but as the season changes, there is less water for the falls because so much of the flow is diverted at the Crescent Dam to the Barge Canal through Lock 6. Most of the water is still diverted for power generation; some is diverted for the Cohoes water supply. During the summer, the falls are virtually dry, revealing shale rock formations that have their own distinctive beauty. The 87-year average flow of the Mohawk River at Cohoes is 34,638 cubic feet per second, but this includes water diverted to the power plant and Erie Canal locks.East Branch Croton River
The East Branch Croton River is a tributary of the Croton River in Dutchess, Putnam, and Westchester counties in the state of New York. It lies within the Croton River watershed and is part of the New York City water supply system's Croton Watershed.East River
The East River is a salt water tidal estuary in New York City. The waterway, which is actually not a river despite its name, connects Upper New York Bay on its south end to Long Island Sound on its north end. It separates the borough of Queens on Long Island from the Bronx on the North American mainland, and also divides Manhattan from Queens and Brooklyn, which are also on Long Island. Because of its connection to Long Island Sound, it was once also known as the Sound River. The tidal strait changes its direction of flow frequently, and is subject to strong fluctuations in its current, which are accentuated by its narrowness and variety of depths. The waterway is navigable for its entire length of 16 miles (26 km), and was historically the center of maritime activities in the city, although that is no longer the case.Gerard Crane House
The Gerard Crane House is a private home located on Somerstown Turnpike (U.S. Route 202) opposite Old Croton Falls Road in Somers, New York, United States. It is a stone house dating to the mid-19th century, built by an early circus entrepreneur in his later years.
The house itself is an unusually sophisticated late application of the Greek Revival architectural style. The interior features a high level of decoration, particularly English Renaissance-style plaster moldings on the ceilings that are not commonly found in rural Greek Revival houses. It is the center of a 25-acre (10 ha) estate that includes not only the original outbuildings but an original section of Somerstown Turnpike and one of its mileposts.
It remains largely as it was originally built. In 1985 the area was designated a historic district and listed on the National Register of Historic Places. It is the northernmost such listing in Westchester County.Great Swamp (New York)
The Great Swamp in eastern Putnam and Dutchess counties is one of the largest wetlands in the U.S. state of New York.Interstate 684
Interstate 684 (I-684) is a 28.4 mile-long (45.7 km) north–south Interstate Highway in the state of New York and a short portion in Connecticut in the United States. The highway connects I-84 with I-287 and the Hutchinson River Parkway, primarily serving commuter traffic to and from the northern suburbs of the New York metropolitan area. The route of the highway was originally designated as part of I-87 during the 1960s. The first section of the roadway opened to traffic in October 1968, and the final segment was completed in December 1974.LaDue Reservoir
LaDue Reservoir is a reservoir located near Ohio State Route 44 and U.S. Route 422 in Auburn and Troy Townships in Geauga County, Ohio. Originally called the “Akron City Reservoir”, it was dedicated as the LaDue Reservoir on October 11, 1961, in honor of Wendell R. LaDue. The Geographic Names Information System recognized four variants names, including Akron City Reservoir, Bridge Creek Reservoir, Ladue Reservoir, and Wendell R. Ladue Reservoir.The reservoir is formed by the Bridge Creek Dam 41°24′16″N 81°11′2″W across Bridge Creek and the Black Brook Dike 41°21′4″N 81°12′36″W across Black Brook, both tributaries of the Cuyahoga River.
The reservoir was created in an area that was covered with ice during the Wisconsinan glaciation and contains numerous glacial sand and gravel deposits (kames) and glacial ponds (kettles). The lake bottom retains the same irregularities found before it was dammed.List of dams and reservoirs in New York
This is a list of dams and reservoirs in the State of New York.List of lakes in Ohio
The following is a list of lakes in Ohio. According to the Ohio Department of Natural Resources, there are approximately 50,000 lakes and small ponds in the U.S. state of Ohio, with a total surface area of about 200,000 acres (81,000 ha). About 2,200 of these lakes are 5 acres (2.0 ha) or greater, with a total surface area of 134,000 acres (54,000 ha). These 2,200 include both public and private lakes. The United States Environmental Protection Agency estimated (from an electronic file generated from 1:100,000 scale maps) that Ohio has 5,130 lakes totaling 188,461 acres (76,267 ha). The difference in the number of lakes estimated by USEPA and ODNR is likely related to numerous small ponds (high number, small acreage) not detected on the 1:100,000 scale maps.New York State Route 121
New York State Route 121 (NY 121) is a north–south state highway in the Hudson Valley of New York, United States. It begins in northern Westchester County at an intersection with NY 22 in Bedford and extends for 15.56 miles (25.04 km) to a junction with U.S. Route 6 and U.S. Route 202 (US 6 and US 202) east of the village of Brewster in Putnam County. As the route heads north, it briefly overlaps with NY 35 and NY 116 in Westchester County and connects to Interstate 84 (I-84) in Putnam County. NY 121 was assigned as part of the 1930 renumbering of state highways in New York.Peach Lake, New York
Peach Lake is a hamlet (and census-designated place) located mostly in the town of Southeast in Putnam County, New York; a portion of the CDP is in the town of North Salem in Westchester County. As of the 2010 census, the population was 1,629.The community of Peach Lake is located on the northeast side of a lake with the same name. The lake itself is in two counties. The community is south of Interstate 84.Putnam County, New York
Putnam County is a county located in the U.S. state of New York. As of the 2010 census, the population was 99,710. The county seat is Carmel. Putnam County formed in 1812 from Dutchess County and is named for Israel Putnam, a hero in the French and Indian War and a general in the American Revolutionary War.
Putnam County is included in the New York-Newark-Jersey City, NY-NJ-PA Metropolitan Statistical Area. It is located in the lower Hudson River Valley. Midtown Manhattan is around a one-hour drive, and Grand Central Terminal is approximately 1 hour, 20 minute train ride from the county.It is one of the most affluent counties in America, ranked 7th by median household income, and 43rd by per-capita income, according to the 2012 American Community Survey and 2009-2013 American Community Survey, respectively.Reservoir
A reservoir (from French réservoir – a "tank") is, most commonly, an enlarged natural or artificial lake, pond or impoundment created using a dam or lock to store water.
Reservoirs can be created in a number of ways, including controlling a watercourse that drains an existing body of water, interrupting a watercourse to form an embayment within it, through excavation, or building any number of retaining walls or levees.
Defined as a storage space for fluids, reservoirs may hold water or gasses, including hydrocarbons. Tank reservoirs store these in ground-level, elevated, or buried tanks. Tank reservoirs for water are also called cisterns. Most underground reservoirs are used to store liquids, principally either water or petroleum, below ground.Southeast, New York
Southeast is a town in Putnam County, New York, United States. The population was 18,404 at the 2010 census. The town is in the southeast part of the county. Interstate 84, Interstate 684, U.S. Route 202, and US Route 6 pass through the town.The Palisades (Hudson River)
The Palisades, also called the New Jersey Palisades or the Hudson River Palisades, are a line of steep cliffs along the west side of the lower Hudson River in Northeastern New Jersey and Southeastern New York in the United States. The cliffs stretch north from Jersey City about 20 miles (32 km) to near Nyack, New York, and visible at Haverstraw, New York. They rise nearly vertically from near the edge of the river, and are about 300 feet (90 m) high at Weehawken, increasing gradually to 540 feet (160 m) high near their northern terminus. North of Fort Lee, the Palisades are part of Palisades Interstate Park and are a National Natural Landmark.The Palisades are among the most dramatic geologic features in the vicinity of New York City, forming a canyon of the Hudson north of the George Washington Bridge, as well as providing a vista of the Manhattan skyline. They sit in the Newark Basin, a rift basin located mostly in New Jersey.
Palisade is derived from the same root as the word pale, ultimately from the Latin word palus, meaning stake. A "palisade" is, in general, a defensive fence or wall made up of wooden stakes or tree trunks. The Lenape called the cliffs "rocks that look like rows of trees", a phrase that became "Weehawken", the name of a town in New Jersey that sits at the top of the cliffs across from Midtown Manhattan.U.S. Route 202 in New York
U.S. Route 202 (US 202) is a part of the U.S. Highway System that runs from New Castle, Delaware, to Bangor, Maine. In the U.S. state of New York, US 202 extends 55.57 miles (89.43 km) from the New Jersey state line near Suffern to the Connecticut state line east of Brewster. While most of US 202 is signed north–south, the portion within New York is signed east–west. It drifts north slowly as it crosses southern New York. US 202 is the only road to cross New York between New Jersey and Connecticut and not pass through New York City on the way.
As it does in other states, Route 202 serves mainly as a local road in suburban and exurban communities along the outskirts of the metropolitan area, mostly two lanes with the exception of some four-lane sections and a brief concurrency onto an expressway in Peekskill. Its course along the Hudson River takes it first north up the west side, over the historic Bear Mountain Bridge, then south along the east side. It takes in many scenic areas, such as the Ramapo Mountains and Hudson Highlands, and two New York City reservoirs.
Its circuitous path across the state puts it on many concurrencies—only 14.5 miles (23.3 km), or 26%, of Route 202's mileage in New York is signed as US 202 alone. Among the roads it joins are three U.S. highways and two state routes. It forms four three-route conurrencies, including the only such grouping of three U.S. routes in the state, again in Peekskill.Washington Valley Park
Washington Valley Park is a 715-acre (2.89 km2) public park between the first and second Watchung mountain ridge in the Martinsville section of Bridgewater Township, New Jersey that is administered by the Somerset County Park Commission. It contains the Washington Valley Reservoir and the Chimney Rock Hawk Watch.
|Catskill & Delaware reservoirs|
Italics indicate a decommissioned site
Hudson River watershed