Cupsogue Beach County Park
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Cupsogue Beach County Park
Cupsogue Beach County Park is a park at the eastern end of Fire Island and the western end of Westhampton Island, known locally as Dune Road, one of Long Island's easternmost barrier islands. The Atlantic Ocean, Moriches Inlet and Moriches Bay surround the park. Location Though the park exists on both sides of the Moriches Inlet and is located entirely within the Town of Brookhaven, it is only accessible from the western terminus of Dune Road, which itself is in the Town of Southampton. The closest bridge to the park is for Jessup Lane in the village of Westhampton Beach between Moriches Bay and Moneybogue Bay. The park's eastern border is the Brookhaven/Southampton town line and the village of West Hampton Dunes. Park description This barrier beach park offers lifeguard-supervised swimming, sunbathing, fishing, scuba diving, and special events. A food concession, restrooms, a first aid center (staffed by an EMT during the summer months), showers and changing rooms are all si ...
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Hurricane Jose (2017)
Hurricane Jose was a powerful and erratic tropical cyclone which was the longest-lived Atlantic hurricane since Hurricane Nadine in 2012. Jose was the tenth named storm, fifth hurricane, and third major hurricane of the 2017 Atlantic hurricane season. Jose developed into a tropical storm on September 5 from a tropical wave that left the west coast of Africa nearly a week prior. A period of rapid intensification ensued on September 6, when Jose reached hurricane intensity. On September 8, it reached its peak intensity as a high-end Category 4 hurricane with 1-minute sustained winds of 155 mph. However, due to wind shear, Jose weakened over the next few days as it completed an anti-cyclonic loop north of Hispaniola. Despite weakening to a tropical storm on September 14, Jose managed to regain hurricane intensity the next day as it began to curve northwards. Never strengthening above Category 1 status for the remainder of its lifespan, Jose degraded ...
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Westhampton Beach, New York
Westhampton Beach is an incorporated village in the Town of Southampton, in Suffolk County, on the South Shore of Long Island, in New York, United States. As of the 2010 census, the population was 1,721. History The village of Westhampton Beach was incorporated in 1928. In 1938, almost all summer homes on its barrier beach were obliterated by a hurricane resulting in twenty-nine local deaths. Like most of the shoreline of southern Long Island, the beach at Westhampton Beach was eroding shoreward. This became a political issue in the 1960s. The project to protect the beaches in the area from further erosion was started by the Army Corps of Engineers in 1966, but was only partially completed because of the failure to secure funds from the state and local government. In addition the project design was seriously flawed. As a result, there was increased erosion at the beaches in Westhampton Beach while, up current, the beaches actually grew. During the late 1970s and throug ...
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Southampton (town), New York
Southampton, officially the Town of Southampton, is a Administrative divisions of New York#Town, town in southeastern Suffolk County, New York, Suffolk County, New York, partly on the South Fork, Suffolk County, New York, South Fork of Long Island. As of the 2020 United States census, 2020 U.S. census, the town had a population of 69,036. Southampton is included in the stretch of shoreline prominently known as The Hamptons. Stony Brook Southampton, Stony Brook University's Southampton campus is located in Southampton. History The town was founded in 1640, when settlers from Lynn, Massachusetts, Lynn, Massachusetts established residence on lands obtained from local Shinnecock Indian Nation. The first settlers included eight men, one woman, and a boy who came ashore at Conscience Point. These men were Thomas Halsey (1591-1679), Thomas Halsey, Edward Howell (died 1655), Edward Howell, Edmond Farrington, Allen Bread, Edmund Needham, Abraham Pierson, the elder, Abraham Pierson the ...
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Beaches Of Suffolk County, New York
A beach is a landform alongside a body of water which consists of loose particles. The particles composing a beach are typically made from rock, such as sand, gravel, shingle, pebbles, etc., or biological sources, such as mollusc shells or coralline algae. Sediments settle in different densities and structures, depending on the local wave action and weather, creating different textures, colors and gradients or layers of material. Though some beaches form on inland freshwater locations such as lakes and rivers, most beaches are in coastal areas where wave or current action deposits and reworks sediments. Erosion and changing of beach geologies happens through natural processes, like wave action and extreme weather events. Where wind conditions are correct, beaches can be backed by coastal dunes which offer protection and regeneration for the beach. However, these natural forces have become more extreme due to climate change, permanently altering beaches at very rapi ...
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The Hamptons
The Hamptons, part of the East End of Long Island, consist of the towns of Southampton and East Hampton, which together comprise the South Fork of Long Island, in Suffolk County, New York. The Hamptons are a popular seaside resort and one of the historical summer colonies of the northeastern United States. The Montauk Branch of the Long Island Rail Road, the Montauk Highway, and private bus services connect the Hamptons to the rest of Long Island and to New York City, while ferries provide connections to Shelter Island, New York and Connecticut. Stony Brook University's Southampton campus is located in the Hamptons. West to east The Hamptons include the following hamlets and villages in the town of Southampton: * Eastport (hamlet) * Speonk (hamlet) * Remsenburg (hamlet) * Westhampton (hamlet) * West Hampton Dunes (village) * Westhampton Beach (village) * Quogue (village) * East Quogue (hamlet) * Hampton Bays (hamlet) **Places of Interest: Shinnecock Bay * Shinne ...
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Hurricane Sandy
Hurricane Sandy (unofficially referred to as ''Superstorm Sandy'') was an extremely destructive and strong Atlantic hurricane, as well as the largest Atlantic hurricane on record as measured by diameter, with tropical-storm-force winds spanning . The storm inflicted nearly $70 billion (2012 USD) in damage and killed 233 people across eight countries from the Caribbean to Canada. The eighteenth Tropical cyclone naming, named storm, tenth Atlantic hurricane, hurricane, and second major hurricane of the 2012 Atlantic hurricane season, Sandy was a List of Category 3 Atlantic hurricanes, Category 3 storm at its peak intensity when it made landfall in Cuba, though most of the damage it caused was after it became a Category 1-equivalent extratropical cyclone off the coast of the Northeastern United States. Sandy developed from a tropical wave in the western Caribbean Sea on October 22, quickly strengthened, and was upgraded to Tropical Storm Sandy six hours later. Sandy moved s ...
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Boardwalk
A boardwalk (alternatively board walk, boarded path, or promenade) is an elevated footpath, walkway, or causeway built with wooden planks that enables pedestrians to cross wet, fragile, or marshy land. They are also in effect a low type of bridge. Such timber trackways have existed since at least Neolithic times. Some wooden boardwalks have had sections replaced by concrete and even "a type of recycled plastic that looks like wood." History An early example is the Sweet Track that Neolithic people built in the Somerset levels, England, around 6000 years ago. This track consisted mainly of planks of oak laid end-to-end, supported by crossed pegs of ash, oak, and lime, driven into the underlying peat. The Wittmoor bog trackway is the name given to each of two prehistoric plank roads, or boardwalks, trackway No. I being discovered in 1898 and trackway No. II in 1904 in the ''Wittmoor'' bog in northern Hamburg, Germany. The trackways date to the 4th and 7th century AD, both linked ...
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Nor'easter
A nor'easter (also northeaster; see below), or an East Coast low is a synoptic-scale extratropical cyclone in the western North Atlantic Ocean. The name derives from the direction of the winds that blow from the northeast. The original use of the term in North America is associated with storms that impact the upper north Atlantic coast of the United States and the Atlantic Provinces of Canada. Typically, such storms originate as a low-pressure area that forms within of the shore between North Carolina and Massachusetts. The precipitation pattern is similar to that of other extratropical storms. Nor'easters are usually accompanied by heavy rain or snow, and can cause severe coastal flooding, coastal erosion, hurricane-force winds, or blizzard conditions. Nor'easters are usually most intense during winter in New England and Atlantic Canada. They thrive on converging air masses—the cold polar air mass and the warmer air over the water—and are more severe in winter when t ...
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Shorebird
245px, A flock of Dunlins and Red knots">Red_knot.html" ;"title="Dunlins and Red knot">Dunlins and Red knots Waders or shorebirds are birds of the order Charadriiformes commonly found wikt:wade#Etymology 1, wading along shorelines and mudflats in order to foraging, forage for food crawling or burrowing in the mud and sand, usually small arthropods such as aquatic insects or crustaceans. The term "wader" is used in Europe, while "shorebird" is used in North America, where "wader" may be used instead to refer to long-legged wading birds such as storks and herons. There are about 210 species of wader, most of which live in wetland or coastal environments. Many species of Arctic and temperate regions are strongly migratory, but tropical birds are often resident, or move only in response to rainfall patterns. Some of the Arctic species, such as the little stint, are amongst the longest distance migrants, spending the non-breeding season in the southern hemisphere. Many of the sm ...
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Piping Plovers
The piping plover (''Charadrius melodus'') is a small sand-colored, sparrow-sized wader, shorebird that nests and feeds along coastal sand and gravel beaches in North America. The adult has yellow-orange-red legs, a black band across the forehead from eye to eye, and a black stripe running along the breast line. This chest band is usually thicker in males during the breeding season, and it is the only reliable way to tell the sexes apart. The bird is difficult to see when it is standing still, as it blends well with open, sandy beach habitats. It typically runs in short, quick spurts and then stops. There are two subspecies of piping plovers: the eastern population is known as ''Charadrius melodus melodus'' and the mid-west population is known as ''C. m. circumcinctus''. The bird's name is derived from its plaintive bell-like whistles which are often heard before the bird is visible. Total population is currently estimated to be between 7600 - 8400 individuals. Intensive conserva ...
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Smith Point County Park
Smith Point County Park is a beachfront park facing the Atlantic Ocean on the east end of Fire Island, along the central south shore of Long Island, near Shirley, New York, United States. It is the largest park owned by Suffolk County. The park derives its name from Smith Point, a peninsula on the Long Island mainland that extends into Bellport Bay. The peninsula was named for William "Tangier" Smith, who in the 17th century owned of ocean-front property in the Manor of St. George. The park is not on the Smith Point peninsula. Overview Smith Point Park, located on the barrier island of Fire Island, is a haven for sportsmen, surfers and beach lovers. An extremely popular facility, the park has white sands, rolling Atlantic surf and an adjoining camping facility that attract both Suffolk County residents and tourists each summer. Reservations are required for all the sites in the campground. All sites have water, and many have electric hookups and sewers. Outer beach camping ...
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Slack Tide
Slack water is a short period in a body of tidal water when the water is completely unstressed, and there is no movement either way in the tidal stream, and which occurs before the direction of the tidal stream reverses. Slack water can be estimated using a tidal atlas or the tidal diamond information on a nautical chart. The time of slack water, particularly in constricted waters, does not occur at high and low water, and in certain areas, such as Primera Angostura, the ebb may run for up to three hours after the water level has started to rise. Similarly, the flood may run for up to three hours after the water has started to fall. In 1884, Thornton Lecky illustrated the phenomenon with an inland basin of infinite size, connected to the sea by a narrow mouth. Since the level of the basin is always at mean sea level, the flood in the mouth starts at half tide, and its velocity is at its greatest at the time of high water, with the strongest ebb occurring conversely at low water ...
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