This article needs additional citations for verification .(November 2024) |
Hop Brook Lake | |
---|---|
Location | New Haven County, Connecticut |
Coordinates | 41°30′49″N73°03′59″W / 41.51361°N 73.06639°W |
Type | reservoir |
Primary inflows | Hop Brook |
Primary outflows | Hop Brook |
Basin countries | United States |
Surface area | 16.4 sq mi (42 km2) |
Hop Brook Lake is spread over three communities in New Haven County, Connecticut, United States. These communities are Naugatuck, Middlebury, and Waterbury. A dam was created across Hop Brook in Naugatuck and the lake that was created is known as Hop Brook Lake. [1]
Construction of the dam commenced in December 1965 and was completed in December 1968, costing $6.2 million. The relocation of 1.8 miles (2.9 km) of Route 63 was required. [1] The project includes an earthfill dam with stone slope protection 520 feet (160 m) long and 97 feet (30 m) high; an earthfill dike measuring 400 feet (120 m) long and 33 feet (10 m) high; a gated rectangular 425-foot (130 m)-long concrete conduit three feet wide and five feet high; and a chute spillway edged in rock with a 200-footlong broad-crested weir. The weir's crest elevation is 17 feet (5.2 m) lower than the top of the dam.
The flood storage area of the project, which is normally empty and is only utilized to store floodwaters, is 1.5 miles (2.4 km) long and spreads out over 270 acres (1.1 km2). The project and associated lands total 553 acres (2.24 km2) throughout Naugatuck, Middlebury, and Waterbury. Hop Brook Lake can store up to 2.23 billion US gallons (8,400,000 m3) of water for flood control purposes. This is equivalent to eight inches (203 mm) of water covering its drainage area of 16.4 square miles (42 km2).
Hop Brook Lake contains a 21-acre (85,000 m2) recreation pool that has a maximum depth of 18 feet (5.5 m). [2]
Hop Brook Lake contains largemouth bass and panfish. The state stocks both the lake and its feeder streams with trout. Recreational development of the reservoir includes picnic sites, walking trails, a beach, ball field, drinking water, and sanitary and parking facilities. [1]
In 2002, a man drowned at Hop Brook Lake. [3]
Hop Brook Lake is controlled by the Army Corps of Engineers.
Naugatuck is a consolidated borough and town in New Haven County, Connecticut, United States. The town, part of the Naugatuck Valley Planning Region, had a population of 31,519 as of the 2020 Census.
Keystone Lake is a reservoir in northeastern Oklahoma on the Arkansas and Cimarron rivers. It is located upstream about 23 miles (37 km) from Tulsa. It was created in 1968 when the Keystone Dam was completed. The primary purposes are: flood control, hydroelectric power generation, wildlife management and recreation.
Fort Cobb Reservoir is a reservoir located in Caddo County in the U.S. state of Oklahoma. It impounds the waters of Cobb Creek, Lake Creek, and Willow Creek. The lake covers approximately 4,000 acres (16 km2) of water and 45 mi (72 km) of shoreline. Its drainage area is 285 square miles (740 km2). It was constructed in 1958. The towns of Carnegie, Fort Cobb, and Eakly are located nearby.
Sardis Lake is a 98,520-acre (398.7 km2) reservoir on the Tallahatchie River in Lafayette, Panola, and Marshall counties, Mississippi. Sardis Lake is impounded by Sardis Dam, located nine miles (14 km) southeast of the town of Sardis. It is approximately an hour drive from Memphis, Tennessee. The dam is 15,300 feet (4,700 m) long, has an average height of 97 feet (30 m), and a maximum height of 117 feet (36 m).
The Naugatuck River is a 40.2-mile-long (64.7 km) river in the U.S. state of Connecticut. Its waters carve out the Naugatuck River Valley in the western reaches of the state, flowing generally due south and eventually emptying into the Housatonic River at Derby, Connecticut and thence 11 miles (18 km) to Long Island Sound. The Plume and Atwood Dam in Thomaston, completed in 1960 following the Great Flood of 1955, creates a reservoir on the river and is the last barrier to salmon and trout migrating up from the sea.
The Ware River is a 35.4-mile-long (57.0 km) river in central Massachusetts. It has two forks, its West Branch, which begins in Hubbardston, Massachusetts, and its East Branch, which begins in Westminster, Massachusetts. The Ware River flows southwest through the middle of the state, joins the Quaboag River at Three Rivers, Massachusetts, to form the Chicopee River on its way to the Connecticut River.
The Barre Falls Dam is located on the Ware River in Barre, Massachusetts, about 0.3 miles (0.48 km) below the junction of the river's east and west branches and 13 miles (21 km) northwest of Worcester, Massachusetts.
Lake Livingston is a reservoir located in Piney Woods in Houston, Madison, Polk, San Jacinto, Trinity and Walker counties in east Texas, United States. Lake Livingston was built and is owned and operated by the Trinity River Authority (TRA) of Texas under contract with the City of Houston for water-supply purposes. The USCG Auxiliary Flotilla 6-9 is also stationed on the lake. The lake is the third-largest lake located in the state of Texas. The Livingston Dam, constructed across the Trinity River about 7 miles (11 km) southwest of the city of Livingston is 2.5 miles (4 km) in length and has an average depth of 55 feet (17 m).
Lake O’ the Pines is a reservoir on Big Cypress Bayou, also known as Big Cypress Creek, chiefly in Marion County, Texas, United States. The reservoir also occupies a small part of Camp, Upshur, and Morris Counties. The dam is located approximately 8.5 miles (13.7 km) west of Jefferson.
Mansfield Hollow Lake is a reservoir resting on the border of Windham County and Tolland County, Connecticut. The reservoir provides drinking water for Willimantic and helps control flooding in the 159-square-mile Thames River watershed. It was created by the Mansfield Hollow Dam and is entirely contained within Mansfield Hollow State Park and the Mansfield Hollow Wildlife Area. Designed and constructed by the United States Army Corps of Engineers, the dam substantially reduces flooding along the Quinebaug, Shetucket, and Thames rivers. Construction of the project began in 1949 with completion in 1952 at a cost of US$6.5 million. The Mansfield Hollow reservoir is located within the Shetucket River Watershed and is part of the Thames River Basin. Access to the site is available from US Route 6 and State Route 195. The damsite, covering an area of 25 acres (10 ha), was listed on the National Register of Historic Places in 2003.
The Conant Brook Dam is located on Conant Brook in Monson, Massachusetts, about 7.4 miles (11.9 km) upstream from the confluence of Conant Brook and the Quaboag River. It is approximately 15 miles (24 km) east of Springfield, Massachusetts.
The East Brimfield Dam is located on the Quinebaug River in Sturbridge, Massachusetts, approximately 20 miles (32 km) southwest of Worcester, Massachusetts.
The Westville Dam is located on the Quinebaug River between Southbridge and Sturbridge, about 1.3 miles (2.1 km) west of the Southbridge town center and 18 miles (29 km) southwest of Worcester, Massachusetts.
The Central Utah Project is a United States federal water project that was authorized for construction under the Colorado River Storage Project Act of April 11, 1956, as a participating project. In general, the Central Utah Project develops a portion of Utah's share of the yield of the Colorado River, as set out in the Colorado River Compact of 1922.
The Rio Grande Project is a United States Bureau of Reclamation irrigation, hydroelectricity, flood control, and interbasin water transfer project serving the upper Rio Grande basin in the southwestern United States. The project irrigates 193,000 acres (780 km2) along the river in the states of New Mexico and Texas. Approximately 60 percent of this land is in New Mexico. Some water is also allotted to Mexico to irrigate some 25,000 acres (100 km2) on the south side of the river. The project was authorized in 1905, but its final features were not implemented until the early 1950s.
Santa Fe Dam is a flood-control dam on the San Gabriel River located in Irwindale in Los Angeles County, California, United States. For most of the year, the 92-foot (28 m)-high dam and its reservoir lie empty, but can hold more than 45,000 acre-feet (56,000,000 m3) of water during major storms. During the dry season, the basin behind the dam is used for groundwater recharge, as well as various recreational activities.
Angostura Dam is an embankment dam across the Cheyenne River in Fall River County in southwestern South Dakota in the United States, about 75 miles (121 km) south of Rapid City. The dam consists of an earth-fill embankment with a concrete spillway section, 193 feet (59 m) high and 2,030 feet (620 m) long; it withholds the 195,121-acre-foot (0.240678 km3) Angostura Reservoir. The dam was conceived as early as 1913, but it was not until the 1930s when a regional drought caused crop failures that the project received widespread support from farmers. Built from 1946 to 1949, the dam is part of the Angostura Division of the Pick-Sloan Missouri Basin Program, and is operated by the U.S. Bureau of Reclamation.
The Mojave Forks Dam, most often known as the Mojave River Dam, is an earth-fill dry dam across the Mojave River in San Bernardino County, California in the United States. Completed in 1974 by the U.S. Army Corps of Engineers (USACE), the dam is located at the confluence of the West Fork Mojave River and Deep Creek, and can store approximately 179,400 acre⋅ft (221,300,000 m3) of water.
Wrightsville Reservoir is a reservoir located in Washington County, Vermont, United States, as a result of the construction of the Wrightsville Dam built from 1933 to 1935 after the Great Flood of 1927. It is located at the intersection of the municipal borders of three towns, Montpelier, Middlesex, and East Montpelier. It is a popular recreational spot in the summer, for swimming, boating, and fishing in the Montpelier area.
The Potomac River basin reservoir projects were U.S. Army Corps of Engineers programs that sought to regulate the flow of the Potomac River to control flooding, to assure a reliable water supply for Washington, D.C., and to provide recreational opportunities. Beginning in 1921 the Corps studied a variety of proposals for an ambitious program of dam construction on the Potomac and its tributaries, which proposed as many as sixteen major dam and reservoir projects. The most ambitious proposals would have created a nearly continuous chain of reservoirs from tidewater to Cumberland, Maryland. The 1938 program was focused on flood control, on the heels of a major flood in 1936. The reformulated 1963 program focused on water supply and quality, mitigating upstream pollution from sewage and coal mine waste.