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List Of Rivers In 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 state. Major rivers include the Manasquan, Maurice, Mullica, Passaic, Rahway, Raritan, Musconetcong, Hudson and Delaware rivers. Historically, the Delaware and Raritan rivers have provided transportation of goods and people inland from the Atlantic Ocean, and were once connected by the Delaware and Raritan Canal. Today, these rivers, and the streams that feed them, provide sport and recreation for many people. By drainage basin Hudson River Basin * North River (Lower Hudson) **Hudson River ***Sparkill Creek ***Rondout Creek (NY) ****Wallkill River *****Pochuck Creek ****** Black Creek ******Wawayanda Creek *****Papakating Creek ******Clove Brook ******Neepaulakating Creek ******West Branch Papakating Creek Newark Bay *Kill Van K ...
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Stream
A stream is a continuous body of water, body of surface water Current (stream), flowing within the stream bed, bed and bank (geography), banks of a channel (geography), channel. Depending on its location or certain characteristics, a stream may be referred to by a variety of local or regional names. Long large streams are usually called rivers, while smaller, less voluminous and more intermittent river, intermittent streams are known as streamlets, brooks or creeks. The flow of a stream is controlled by three inputs – surface runoff (from precipitation or meltwater), daylighting (streams), daylighted subterranean river, subterranean water, and surfaced groundwater (Spring (hydrology), spring water). The surface and subterranean water are highly variable between periods of rainfall. Groundwater, on the other hand, has a relatively constant input and is controlled more by long-term patterns of precipitation. The stream encompasses surface, subsurface and groundwater fluxes th ...
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Sparkill Creek
Sparkill Creek, is a tributary of the Hudson River in Rockland County, New York and Bergen County, New Jersey in the United States. It flows through the Sparkill Gap in the Hudson Palisades, which was created by a fault line which provided the only sea-level break in the Palisades."Piermont Pier and Marsh"
Rockland Aubudubon Society
Sparkill Creek is long and drains of watershed. It begins from runoff from Clausland Mountain in , New York. Small tributaries feed the creek as it flows through the hamlets of ,
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Hackensack River
The Hackensack River is a river, approximately 45 miles (72 km) long, in the U.S. states of New York and New Jersey, emptying into Newark Bay, a back chamber of New York Harbor. The watershed of the river includes part of the suburban area outside New York City just west of the lower Hudson River, which it roughly parallels, separated from it by the New Jersey Palisades. It also flows through and drains the New Jersey Meadowlands. The lower river, which is navigable as far as the city of Hackensack, is heavily industrialized and forms a commercial extension of Newark Bay. Once believed to be among the most polluted watercourses in the United States, it staged a modest revival by the late 2000s. The river is divided into the upper river, north of the Oradell Reservoir and Oradell Dam, and lower river, south of the reservoir and dam. Description The Hackensack River rises in southeastern New York, in Rockland County, in the Sweet Swamp, just west of the Hudson Riv ...
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Tidal Strait
A tidal strait is technically not a river but a strait connecting two oceans or seas. Tidal straits are narrow seaways through which tidal currents flow. Tidal currents are usually unidirectional but sometimes are bidirectional. They are frequently of tectonic origin. In them, currents develop because of elevation differences between the water basins at both ends. Tides sometimes allow sediments to collect in tidal straits. See also * Sediment trap (geology) * Tidal circularization Tidal circularization is an effect of the tidal forces between an orbiting body and the primary object that it orbits, whereby the eccentricity of the orbit is reduced over time so that the orbit becomes less and less elliptical. In figure 1 let ... References External links A facies‐based depositional model for ancient and modern, tectonically–confined tidal straitsDeltas sourcing tidal straits: observations from some field case studiesNotes on shipwrecks in the Arthur Kill ship gravey ...
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Kill Van Kull
__NOTOC__ The Kill Van Kull is a tidal strait between Staten Island, New York and Bayonne, New Jersey in the United States. It is approximately long and wide and connects Newark Bay with Upper New York Bay. The Robbins Reef Light marks the eastern end of the Kill, Bergen Point its western end. It is spanned by the Bayonne Bridge and is one of the most heavily traveled waterways in the Port of New York and New Jersey. Historically, it has been one of the most important channels for the commerce of the region, providing a passage for marine traffic between Upper New York Bay and the industrial towns of northeastern New Jersey. During the colonial era, it played a significant role in travel between New York and the southern colonies, with passengers changing from ferries to coaches at Elizabethtown (now Elizabeth). Since the final third of the 20th century, it has provided the principal access for oceangoing container ships to Port Newark-Elizabeth Marine Terminal, the bus ...
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Newark Bay
Newark Bay is a tidal bay at the confluence of the Passaic and Hackensack Rivers in northeastern New Jersey. It is home to the Port Newark-Elizabeth Marine Terminal, the largest container shipping facility in Port of New York and New Jersey, the second busiest in the United States. An estuary, it is periodically dredged to accommodate seafaring ships. Geography Newark Bay is rectangular, approximately long, varying in width from . It is enclosed on the west by the cities of Newark and Elizabeth, and on the east by Jersey City and Bayonne. At the south is Staten Island, New York and at the north Kearny Point and Droyer's Point mark the mouth of the Hackensack. Shooters Island is a bird sanctuary where the borders of Staten Island, Bayonne and Elizabeth meet at one point. The southern tip of Bergen Neck, known as Bergen Point, juts into the bay and lent its name to the former Bergen Point Lighthouse. Built offshore in 1849 it was demolished and replaced with a skeletal tower i ...
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West Branch Papakating Creek
West Branch Papakating Creek is a tributary of Papakating Creek located in Frankford and Wantage townships in Sussex County, New Jersey, in the United States. See also * Clove Brook * Neepaulakating Creek * Wallkill River * List of rivers in 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 ... Rivers of Sussex County, New Jersey Papakating Creek watershed Rivers of New Jersey Tributaries of the Wallkill River {{NewJersey-river-stub ...
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Neepaulakating Creek
Neepaulakating Creek is a 2.4-mile long (3.8 km) tributary of Papakating Creek in Wantage Township in Sussex County, New Jersey in the United States.United States Geological Survey, Geographic Names Information SystemFeature Detail Report for: Neepaulakating Creek Retrieved June 26, 2015.United States Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map Retrieved June 26, 2015. Note: The upper elevation of its headwaters is approximately 640 feet above mean sea level derived from a reading of the USGS NHD topographic map. The NHD information provides the elevation the mouth at 395 feet above mean sea level. See also: United States Geological Survey, ''Hamburg, NJ Quadrangle USGS 1:24 Topographic Map 41074B5'' and ''Branchville, NJ Quadrangle USGS 1:24 Topographic Map 41074B4''. It is one of three streams feeding the Papakating Creek, a major contributor to the Wallkill River. Although the stream was dammed in the 1950s to create Lake ...
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Clove Brook
Clove Brook is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map, accessed October 3, 2011 tributary of Papakating Creek in Sussex County, New Jersey in the United States.Gertler, Edward. ''Garden State Canoeing'', Seneca Press, 2002. Clove Brook, previously known as ''Bastions Brook'', ''Clove Creek'', ''Clove River'', and ''Deep Clove River'', rises from north of Colesville and travels in a southeasterly direction, predominantly on the north side of State Route 23, down through the Clove Valley toward Sussex Borough. The brook enters the north end of Clove Acres Lake, passes over the dam, and proceeds through the center of the Borough of Sussex. Leaving the borough, the brook turns south and joins Papakating Creek just north of Lewisburg. The name Bastions Brook was noted as a part of the description of a parcel of land in a deed signed by Peter Decker in the eighteenth century. See also *List of rivers of New Jersey *West B ...
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Papakating Creek
Papakating Creek is a tributary of the Wallkill River located in Frankford and Wantage townships in Sussex County, New Jersey in the United States. The creek rises in a small swamp located beneath the eastern face of Kittatinny Mountain in Frankford and its waters join the Wallkill to the east of Sussex borough. Papakating Creek and its three major tributaries drain the northern portion of New Jersey's Kittatinny Valley a fertile valley underlain by shale and limestone of the Ordovician Martinsburg Formation and soils deposited by retreating glaciers in the last ice age. The region which the Papakating Creek and its tributaries drain is largely rural farmland and forests with a few low-density residential communities. The New Jersey Department of Environmental Protection reports that phosphorus and fecal coliform from agricultural or residential runoff as well as arsenic from agricultural pesticide applications or regional mineralogy impair the creek. Within the watershed are ...
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Wawayanda Creek
Wawayanda Creek (pronounced "way way yonda") is the name of Pochuck Creek above its confluence with the tributary Black Creek.Gertler, Edward. ''Garden State Canoeing'', Seneca Press, 2002. It is long.U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map accessed October 3, 2011 Wawayanda Creek, via Pochuck Creek, is a tributary of the Wallkill River in Sussex County, New Jersey in the United States. It starts northeast of Warwick, New York, and runs southwest, mostly within Orange County, flowing into New Jersey for several miles to its confluence with Black Creek just north of Highland Lakes, forming Pochuck Creek, which flows north back into New York. See also *List of rivers of New Jersey *List of rivers of New York This is a list of rivers in the U.S. state of New York. By drainage basin This list is arranged by drainage basin, with respective tributaries indented by order of confluence with their main stem, from mouth to ...
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Black Creek (New Jersey)
Black Creek is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map, accessed October 3, 2011 tributary of Pochuck Creek in Sussex County, New Jersey in the United States.Gertler, Edward. ''Garden State Canoeing'', Seneca Press, 2002. 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 th ... References Rivers of New Jersey Rivers of Sussex County, New Jersey Tributaries of the Wallkill River {{NewJersey-river-stub ...
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