Lake Shawnee (New Jersey)
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Lake Shawnee (New Jersey)
Lake Shawnee is a small private Lake located in Jefferson Township, New Jersey, United States. Its outsourcing is Beaver Brook, which flows into Lake Hopatcong, New Jersey's largest lake. Lake Shawnee and its watershed are the headwaters of the Musconetcong River watershed. The Lake Shawnee Reservation, as it is known, was developed in 1946 by the Arthur D. Crane Company of Sparta, real estate developers, which incorporated the Lake Shawnee Club and began selling home sites on the Lake many of which were originally summer homes. By 1948, the first two homes were built and during the next 15 years the Club reached its peak of 562 resident members. The clubhouse was then constructed and First Beach, not included in the original deeds, was subsequently purchased from the Crane Company with funds raised from within the membership. Carl Peterson was instrumental in developing the Third Beach area and was known as Mr. Shawnee among local residents. The Lake Shawnee dam was damaged dur ...
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Jefferson Township, New Jersey
Jefferson Township is the northernmost township in Morris County, New Jersey, United States. As of the 2010 United States Census, the township's population was 21,314, having increased by 1,597 (+8.1%) from the 19,717 counted in the 2000 Census, which had in turn increased by 1,892 (+10.6%) from the 17,825 counted in the 1990 Census. Jefferson Township was formed as a township by an act of the New Jersey Legislature on February 11, 1804, from portions of Pequannock Township and Roxbury Township.Snyder, John P''The Story of New Jersey's Civil Boundaries: 1606-1968'' Bureau of Geology and Topography; Trenton, New Jersey; 1969. p. 193. Accessed October 26, 2012. The township was named after Thomas Jefferson, the President of the United States at the time the Township was created. The township is situated in the northernmost part of Morris County bordering both Passaic and Sussex counties. Geography According to the United States Census Bureau, the township had a total area of ...
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Reservoir
A reservoir (; from French ''réservoir'' ) is an enlarged lake behind a dam. Such a dam may be either artificial, built to store fresh water or it may be a natural formation. 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. In other contexts, "reservoirs" may refer to storage spaces for various fluids; they may hold liquids 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. Types Dammed valleys Dammed reservoirs are artificial lakes created and controlled by a dam A dam is a barrier that stops or restricts the flow of surface water or underground streams ...
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Beaver Brook (New Jersey)
Beaver Brook is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map, accessed April 1, 2011 tributary of the Pequest River in western New Jersey in the United States.Gertler, Edward. ''Garden State Canoeing'', Seneca Press, 2002. Beaver Brook originates near Blairstown and terminates at its confluence with the Pequest River near Belvidere. See also *List of rivers of New Jersey This is a list of streams and rivers of the U.S. state of New Jersey. List of New Jersey rivers includes streams formally designated as rivers. There are also smaller streams (''i.e.,'' branches, creeks, drains, forks, licks, runs, etc.) in the ... References External linksU.S. Geological Survey: NJ stream gaging stations Rivers of New Jersey Tributaries of the Delaware River Rivers of Warren County, New Jersey {{NewJersey-river-stub ...
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Lake Hopatcong
Lake Hopatcong is the largest freshwater body in New Jersey, United States, about in area. Located from the Delaware River and from Manhattan, New York City, the lake forms part of the border between Sussex and Morris counties in the state's northern highlands region. Lake Hopatcong was produced by damming and flooding of two ponds, known as the Great Pond and Little Pond, and the Musconetcong River, its natural outlet. Historically known as a resort lake for vacationing New Yorkers, it is now a mostly suburban residential lake. Name The exact origin of the name Hopatcong is unknown, though it is most commonly attributed to the Lenape Indian word for "stone water," or "stone over water". Some linguists believe "Hopatcong" to be a derivative of the Lenape word ''hapakonoesson'', meaning "pipe stone". One explanation of the origin of the word ''Hopatcong'' is that it was a derivation from the Lenni Lenape word ''Huppakong'' meaning "honey waters of many coves," but this wording ...
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Musconetcong River
The Musconetcong River is a tributary of the Delaware River in northwestern New Jersey in the United States.U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map accessed April 1, 2011 It flows through the rural mountainous country of northwestern New Jersey. The name derives from the Lenape words ''moschakgeu'' meaning "clear" and ''hannek'' meaning "stream". Part of it is a National Wild and Scenic River. It rises out of Lake Hopatcong, on the border between the borough of Hopatcong in Sussex County and the township of Roxbury in Morris County. It flows through Lake Musconetcong, then flows southwest, past Stephensburg and New Hampton, passing south of Washington then along the southeastern side of the Pohatcong Mountain ridge. It joins the Delaware at Riegelsville, approximately 10 mi (16 km) south of Phillipsburg. The river does not flow through any large population center and has been the site of relatively lit ...
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Lakes Of Morris County, New Jersey
A lake is an area filled with water, localized in a basin, surrounded by land, and distinct from any river or other outlet that serves to feed or drain the lake. Lakes lie on land and are not part of the ocean, although, like the much larger oceans, they do form part of the Earth's water cycle. Lakes are distinct from lagoons, which are generally coastal parts of the ocean. Lakes are typically larger and deeper than ponds, which also lie on land, though there are no official or scientific definitions. Lakes can be contrasted with rivers or streams, which usually flow in a channel on land. Most lakes are fed and drained by rivers and streams. Natural lakes are generally found in mountainous areas, rift zones, and areas with ongoing glaciation. Other lakes are found in endorheic basins or along the courses of mature rivers, where a river channel has widened into a basin. Some parts of the world have many lakes formed by the chaotic drainage patterns left over from the last ice ...
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