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Lake Pocotopaug is an unincorporated village and census-designated place (CDP) in the town of East Hampton in Middlesex County, Connecticut, United States. As of the 2020 census, it had a population of 4,901, [3] up from 3,436 in 2010. [4] It is named for the large local lake, which for years has been a popular resort area.
The lake has average and maximum depths of 56 feet (17 m) and 163 feet (50 m), respectively. There are three public boat launch locations, [1] and ice fishing is permitted from January through March. [1] Outflow of the lake into the Connecticut River is controlled via the First Lake Dam, [1] located near U.S. Route 3 at the southwestern shore.
Comerford Reservoir is a 1,029-acre (4 km 2) [1] impoundment located on the Connecticut River on the boundary between Vermont and New Hampshire in the United States. The reservoir is formed by the Frank D. Comerford Dam in the towns of Monroe, New Hampshire, and Barnet, Vermont, and impounds water into the towns of Littleton, New Hampshire, and Waterford, Vermont, nearly to the Moore Reservoir ...
Killingly Pond State Park is a public recreation area encompassing 162 acres (66 ha) in the town of Killingly, Connecticut. [1] The state park sits on the western side of Killingly Pond, a 122-acre (49 ha) body of water that straddles the state line between Connecticut and Rhode Island. [4]
Burr Pond State Park is a public recreation area covering 438 acres (177 ha) adjacent to Paugnut State Forest in the town of Torrington, Connecticut.The state park surrounds Burr Pond, an 85-acre (34 ha), [3] man-made body of water with facilities for swimming, boating, and fishing.
Lake Pocotopaug is a site that has been mentioned in many different accounts of the Wangunk people as an area that they frequented for fishing and hunting. [57] It is located in what is now called East Hampton, and is approximately 9 miles in circumference. [58] Many arrowheads have been found along the banks of the river.
Bathymetric charts showcase depth using a series of lines and points at equal intervals, called depth contours or isobaths (a type of contour line). A closed shape with increasingly smaller shapes inside of it can indicate an ocean trench or a seamount, or underwater mountain, depending on whether the depths increase or decrease going inward.
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