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Fisher's Island
Fishers Island (Pequot: ''Munnawtawkit'') is an island that is part of Southold, New York, United States at the eastern end of Long Island Sound, off the southeastern coast of Connecticut across Fishers Island Sound. About long and wide, it is about from the tip of Long Island at Orient Point, each from Napatree Point at the southwestern tip of Rhode Island and Groton Long Point in Connecticut, and about southeast of New London, Connecticut. It is accessible from New London by plane and regular ferry service. The island is part of the town of Southold in Suffolk County. It is a census-designated place (CDP). As of the 2010 census, there were 236 people living year-round on of land. The population rises to about 2,000 during peak summer weekends, as throngs disembark on the island from Connecticut. Geography According to the United States Census Bureau, the CDP has a total area of , of which is land and , or 3.48%, is water. Fishers Island represents a section of th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Census-designated Place
A census-designated place (CDP) is a Place (United States Census Bureau), concentration of population defined by the United States Census Bureau for statistical purposes only. CDPs have been used in each decennial census since 1980 as the counterparts of incorporated places, such as self-governing city (United States), cities, town (United States), towns, and village (United States), villages, for the purposes of gathering and correlating statistical data. CDPs are populated areas that generally include one officially designated but currently unincorporated area, unincorporated community, for which the CDP is named, plus surrounding inhabited countryside of varying dimensions and, occasionally, other, smaller unincorporated communities as well. CDPs include small rural communities, Edge city, edge cities, colonia (United States), colonias located along the Mexico–United States border, and unincorporated resort and retirement community, retirement communities and their environs. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Napatree Point
Napatree Point in Rhode Island, often referred to simply as Napatree, is a long sandy spit created by a geologic process called longshore drift. Up until the Hurricane of 1938, Napatree was sickle-shaped and included a 1.5-mile (2.4 km) long northern extension called Sandy Point. Napatree now extends 1.5 miles (2.4 km) westward from the business district of Watch Hill, a village in Westerly, Rhode Island forming a protected harbor. It is the southernmost and westernmost point of mainland Rhode Island. Name origin Reportedly, the name "Napatree" derives from Nap or Nape (Neck) of Trees. Napatree Point was once heavily wooded. However, when the Great September Gale of 1815 struck the area, the trees were destroyed."Watch Hill In The Hurricane of September 21st, 1938" a special pictorial issue of Seaside Topics published November 1938. Geography and geology Napatree Point is a slender, 1.5 mile long peninsula in Block Island Sound. To the north of the peninsula is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rip Current
A rip current, often simply called a rip (or misleadingly a ''rip tide''), is a specific kind of water current that can occur near beaches with breaking waves. A rip is a strong, localized, and narrow current of water which moves directly away from the shore, cutting through the lines of breaking waves like a river running out to sea. The current in a rip is strongest and fastest next to the surface of the water. Rip currents can be hazardous to people in the water. Swimmers who are caught in a rip current and who do not understand what is happening, or who may not have the necessary water skills, may panic, or they may exhaust themselves by trying to swim directly against the flow of water. Because of these factors, rip currents are the leading cause of rescues by lifeguards at beaches, and in the United States, they are the cause of an average of 46 deaths by drowning per year. A rip current is not the same thing as undertow, although some people use the term incorrectly whe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The Race (Long Island Sound)
Race, RACE or "The Race" may refer to: * Race (biology), an informal taxonomic classification within a species, generally within a sub-species * Race (human categorization), classification of humans into groups based on physical traits, and/or social relations * Racing, a competition of speed Rapid movement * The Race (yachting race) * Mill race, millrace, or millrun, the current of water that turns a water wheel, or the channel (sluice) conducting water to or from a water wheel * Tidal race, a fast-moving tide passing through a constriction Acronyms * RACE encoding, a syntax for encoding non-ASCII characters in ASCII * Radio Amateur Civil Emergency Service, in the US, established in 1952 for wartime use * Rapid amplification of cDNA ends, a technique in molecular biology * RACE (Remote Applications in Challenging Environments), a robotics development center in the UK * RACE Racing Academy and Centre of Education, a jockey and horse-racing industry training centre in Kildare ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake Connecticut
Glacial Lake Connecticut formed over what is now Long Island Sound and coastal Connecticut at the fore edge of the ice sheet of the Wisconsin glaciation, as the lobe of the Laurentide Ice Sheet began to retreat, some 18 to 20,000 years before present. It was dammed by the terminal moraine that now forms the spine of Long Island and Fishers Island. About 15,000 BP, the moraine dam that impounded Lake Connecticut failed; the outlet, known as The Race for its tidal rip currents, lies between the North Fork of Long Island and Fishers Island. For a time, much of the lake bed was exposed to wind-driven erosion: the cue is found in soundings that reveal regional unconformities in the sediment bed of Long Island Sound. The fore-edge lake formed by glacial meltwater expanded to be about the same size as present-day Long Island Sound; it may have been connected at times with similar freshwater lakes in Block Island Sound and Buzzards Bay, while sea level was low. The fairly shallow averag ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wisconsin Glaciation
The Wisconsin Glacial Episode, also called the Wisconsin glaciation, was the most recent glacial period of the North American ice sheet complex. This advance included the Cordilleran Ice Sheet, which nucleated in the northern North American Cordillera; the Innuitian ice sheet, which extended across the Canadian Arctic Archipelago; the Greenland ice sheet; and the massive Laurentide Ice Sheet, which covered the high latitudes of central and eastern North America. This advance was synchronous with global glaciation during the last glacial period, including the North American alpine glacier advance, known as the Pinedale glaciation. The Wisconsin glaciation extended from approximately 75,000 to 11,000 years ago, between the Sangamonian Stage and the current interglacial, the Holocene. The maximum ice extent occurred approximately 25,000–21,000 years ago during the last glacial maximum, also known as the ''Late Wisconsin'' in North America. This glaciation radically altered the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Watch Hill, Rhode Island
Watch Hill is an affluent coastal neighborhood and census-designated place in the town of Westerly, Rhode Island. The population was 154 at the 2010 census. It sits at the most-southwestern point in all of Rhode Island. It came to prominence in the late 19th and early 20th century as an exclusive summer resort, with wealthy families building sprawling Victorian-style "cottages" along the peninsula. Watch Hill is characterized by ''The New York Times'' as a community "with a strong sense of privacy and of discreetly used wealth," in contrast with "the overpowering castles of the very rich" in nearby Newport. History The area was occupied by Niantic Indians in the 17th century, led by Harman Garrett. Colonists used the hill as an important lookout point during the French and Indian War and the Revolutionary War, hence the community's name. Some landmarks in the village include the Watch Hill Lighthouse, the first of which was built in 1745; 1880s The Flying Horse Carousel, th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
North Fork, Suffolk County, New York
The North Fork is a 30-mile- (48 km) long peninsula in the northeast part of Suffolk County, New York, U.S., roughly parallel with a longer peninsula known as the South Fork, both on the East End of Long Island. Although the peninsula begins east of Riverhead hamlet, the term ''North Fork'' can also refer collectively to the towns of Riverhead and Southold in their entirety. Beginning about 75 miles (120 Kilometers) east of Manhattan, the North Fork is the easterly part of the North Shore of Long Island. Along with The Hamptons, the area is also part of Long Island's "East End". Geography At Riverhead proper, Long Island splits into two tines, hence the designations of the South Fork and the North Fork. The dividing line between the two forks in the west is the Peconic River. The North Fork is composed of all of the Town of Southold in the east and part of the Town of Riverhead in the west. The body of water north of this region is Long Island Sound. The sou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Terminal Moraine
A terminal moraine, also called end moraine, is a type of moraine that forms at the terminal (edge) of a glacier, marking its maximum advance. At this point, debris that has accumulated by plucking and abrasion, has been pushed by the front edge of the ice, is driven no further and instead is deposited in an unsorted pile of sediment. Because the glacier acts very much like a conveyor belt, the longer it stays in one place, the greater the amount of material that will be deposited. The moraine is left as the marking point of the terminal extent of the ice. Formation As a glacier moves along its path, the surrounding area is continuously eroding. Loose rock and pieces of bedrock are constantly being picked up and transported with the glacier. Fine sediment and particles are also incorporated into the glacial ice. The accumulation of these rocks and sediment together form what is called glacial till when deposited. Push moraines are formed when a glacier retreats from a previo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
United States Census Bureau
The United States Census Bureau (USCB), officially the Bureau of the Census, is a principal agency of the U.S. Federal Statistical System, responsible for producing data about the American people and economy. The Census Bureau is part of the U.S. Department of Commerce and its director is appointed by the President of the United States. The Census Bureau's primary mission is conducting the U.S. census every ten years, which allocates the seats of the U.S. House of Representatives to the states based on their population. The bureau's various censuses and surveys help allocate over $675 billion in federal funds every year and it assists states, local communities, and businesses make informed decisions. The information provided by the census informs decisions on where to build and maintain schools, hospitals, transportation infrastructure, and police and fire departments. In addition to the decennial census, the Census Bureau continually conducts over 130 surveys and p ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Census-designated Place
A census-designated place (CDP) is a Place (United States Census Bureau), concentration of population defined by the United States Census Bureau for statistical purposes only. CDPs have been used in each decennial census since 1980 as the counterparts of incorporated places, such as self-governing city (United States), cities, town (United States), towns, and village (United States), villages, for the purposes of gathering and correlating statistical data. CDPs are populated areas that generally include one officially designated but currently unincorporated area, unincorporated community, for which the CDP is named, plus surrounding inhabited countryside of varying dimensions and, occasionally, other, smaller unincorporated communities as well. CDPs include small rural communities, Edge city, edge cities, colonia (United States), colonias located along the Mexico–United States border, and unincorporated resort and retirement community, retirement communities and their environs. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Southold (town), New York
The Town of Southold is one of ten towns in Suffolk County, New York, United States. It is located in the northeastern tip of the county, on the North Fork of Long Island. The population was 23,732 at the 2020 census. The town also contains a hamlet named Southold, which was settled in 1640. History Algonquian-speaking tribes, related to those in New England across Long Island Sound, lived in eastern Long Island before European colonization. The western portion of the island was occupied by bands of Lenape, whose language was also one of the Algonquian languages. In surrounding areas, the Dutch colonists had established early settlements to the northwest: on the upper Hudson River was Fort Orange, founded in 1615 (later renamed Albany by the English); and New Amsterdam (later renamed Manhattan) in 1625. Lion Gardiner established a manor on Gardiners Island in East Hampton in 1639. Just across from Long Island, the Connecticut Colony, or Connecticut River Colony, was establ ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
