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Lower New York Bay

Bays of Kings County, New YorkBays of New JerseyBays of New York (state)Bays of Queens County, New YorkBodies of water of Brooklyn
Bodies of water of Monmouth County, New JerseyBodies of water of New York CityBodies of water of Queens, New YorkBodies of water of Staten IslandBorders of New JerseyBorders of New York (state)Estuaries of New JerseyEstuaries of New York (state)Hudson River
Wpdms ev26188 lowernewyorkbay
Wpdms ev26188 lowernewyorkbay

Lower New York Bay is a section of New York Bay south of the Narrows (the strait between Staten Island and Brooklyn). The eastern end of the Bay is marked by two spits of land, Sandy Hook, New Jersey, and Rockaway, Queens. The waterway between the spits connects the Bay to the Atlantic Ocean at the New York Bight. Traversing the floor of the Bay southeasterly from the Narrows to the Bight and beyond is Hudson Canyon. Roughly the northeastern portion of the Bay from the Narrows to Sandy Hook is known as the Lower Bay (named in relation to the neighboring Upper [New York] Bay); roughly the western portion of the Bay (including the portion at the mouth of New Jersey's Raritan River) is called Raritan Bay; and roughly the southeastern portion of the Bay (that is, the portion south and the portion southwest from Sandy Hook) is known as Sandy Hook Bay.

Excerpt from the Wikipedia article Lower New York Bay (License: CC BY-SA 3.0, Authors, Images).

Lower New York Bay
New York Staten Island

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Wikipedia: Lower New York BayContinue reading on Wikipedia

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Latitude Longitude
N 40.516666666667 ° E -74.049722222222 °
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Staten Island


New York, Staten Island
New York, United States
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Wpdms ev26188 lowernewyorkbay
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New York–New Jersey Harbor Estuary
New York–New Jersey Harbor Estuary

The New York–New Jersey Harbor Estuary, also known as the Hudson-Raritan Estuary, is in the northeastern states of New Jersey and New York on the East Coast of the United States. The system of waterways of the Port of New York and New Jersey forms one of the most intricate natural harbors in the world and one of the busiest ports of the United States. The harbor opens onto the New York Bight in the Atlantic Ocean to the southeast and Long Island Sound to the northeast. Although the overall form of the estuary remains unchanged from the time of Giovanni da Verrazzano's visit in 1524, all parts have changed at least a little, and some parts, such as Hell Gate and Ellis Island, have been almost completely altered. In the greatest hidden change, the navigational channels have been deepened from the natural 17 feet (5.2 m) depth to 45 feet (14 m). In some places this required blasting of bedrock.There is an extremely complex system of tides and currents. Both the Bight and the Sound are essentially marine bodies with tides and saltwater, but the Sound compared to the Atlantic is about 20–30% less saline (as an estuary), and the tide is about 3 hours later with as much as 70% more variation. Rivers add a fresher, non-tidal inflow although the tide and brackishness extend well up rivers throughout the extended hydrologic system from Albany to Montauk Point to the Hudson Canyon region of the New York Bight. The New York Harbor Observing and Prediction System (NYHOPS) utilizes information from sensors, weather forecasts, and environment models to provide real-time forecasts of meteorological and oceanographic conditions in the area. Since the Ash Wednesday Storm of 1962 beaches along the shores of the East Coast have been regularly replenished with sand pumped in from off-shore. The United States Army Corps of Engineers (USACE) coordinates the projects.In 2016, USACE and the Port Authority of New York and New Jersey produced a comprehensive restoration plan for the New York Harbor region, with proposals to mitigate the effects of sea level rise through projects to restore natural areas. In September the USACE released the New York New Jersey Harbor and Tributaries Study (HATS).

East Shore Seawall
East Shore Seawall

The East Shore Seawall, also known as Staten Island Multi-Use Elevated Promenade, is a 5.2-mile (8.4 km) long combined seawall and esplanade proposed for the eastern shoreline of Staten Island, New York. It would run along the Lower New York Bay linking sections of the Gateway National Recreation Area: Fort Wadsworth at the north, Miller Field, and Great Kills Park to the south. It will roughly parallel Father Capodanno Boulevard and the South Beach–Franklin Delano Roosevelt Boardwalk. The coastal engineering strategy is to address climate change and sea level rise, and improve resilience along the shoreline of the New York–New Jersey Harbor Estuary and Port of New York and New Jersey. It will be built up to 6 metres (20 ft) above sea level and protect communities from coastal flooding of up to 15.6 feet (4.8 m) (two feet higher than that caused by Hurricane Sandy in 2012). It will includes 4.5 miles (7.2 km) of buried seawall, 0.6 miles (0.97 km) of earthen levee tie-in, 0.35 miles (0.56 km) miles vertical flood wall, more than 300 acres (120 ha) of natural storage, approximately 180 acres (73 ha) of ponding areas and 40 acres (16 ha) acres of tidal wetlands. It will also function as a linear park/greenway with recreational amenities including a boardwalk, biking and walking paths, and will provide access to public beaches.The project, a collaboration between the US Army Corps of Engineers and the New York State Department of Environmental Conservation, was first announced in May 2017. In 2019, the city allocated $615 million for its design and construction.Conflicts over environmental remediation has stalled the building of the project, originally projected to be completed in 2024.Federal legislation to expedite the construction of the seawall was passed in June 2022. It is expected to cost $1.5 billion. Construction was slated to begin at the end of that year.