The East Coast of the United States, also known as the Eastern Seaboard, the Atlantic Coast, and the Atlantic Seaboard, is the coastline along which the Eastern United States meets the North Atlantic Ocean. The eastern seaboard contains the coastal states and areas east of the Appalachian Mountains that have shoreline on the Atlantic Ocean, namely, Maine, New Hampshire, Massachusetts, Rhode Island, Connecticut, New York, New Jersey, Delaware, Maryland, Virginia, North Carolina, South Carolina, Georgia, and Florida.[2] Toponymy and composition[edit]The place name "East Coast" derives from the idea that the contiguous 48 states are defined by two major coastlines, one at the western edge and one on the eastern edge. Other terms for referring to this area include the "Eastern Seaboard" ("seaboard" being American English for coast), "Atlantic Coast", and "Atlantic Seaboard" (because the coastline lies along the Atlantic Ocean). The 14 states that have a shoreline on the Atlantic Ocean are, from north to south, Maine, New Hampshire, Massachusetts, Rhode Island, Connecticut, New York, New Jersey, Delaware, Maryland, Virginia, North Carolina, South Carolina, Georgia, and Florida.[2] In addition, Pennsylvania and the District of Columbia border tidal arms of the Atlantic (the Delaware River and the Potomac River, respectively). The states of Alabama, Mississippi, Louisiana, and Texas (via the Gulf of Mexico), as well as the territories of Puerto Rico, the US Virgin Islands and Navassa Island (the latter only bordering the Caribbean Sea) have Atlantic coastline, but are not included in the definition. Although Pennsylvania, Vermont, and West Virginia have no Atlantic coastline, they are grouped with the Eastern Seaboard states because of their locations in the Mid-Atlantic, New England, and the Old South,[3] and their history as part of the land base of the original Thirteen Colonies (viz. the Colony of New Hampshire, the Colony of New York, and the Colony of Virginia). The Eastern Panhandle of West Virginia is drained by the Potomac River into Chesapeake Bay. Colonial history[edit]The original Thirteen Colonies of Great Britain in North America all lay along the East Coast.[a] Two additional U.S. states on the East Coast were not among the original Thirteen Colonies: Maine (became part of the English colony of Massachusetts in 1677)[4] and Florida (part of New Spain until 1821, though held by the British from after the end of the French and Indian War until 1781). Florida's written history begins with the arrival of Europeans; the Spanish explorer Juan Ponce de León in 1513 made the first textual records. The state received its name from this Spanish conquistador, who called the peninsula La Pascua Florida in recognition of the verdant landscape and because it was the Easter season, which the Spaniards called Pascua Florida (Festival of Flowers).[5] The Middle Colonies (New Jersey, Pennsylvania, New York, and Delaware) had been owned by the Dutch as New Netherland, until they were ceded to the English in the mid- to late 17th century.[citation needed] Climate and physical geography[edit] Three basic climate regions occur on the East Coast according to the Köppen climate classification and four occur according to the Trewartha climate classification from north to south based on the monthly mean temperature of the coldest month (January) and the number of months averaging above 50°F (10°C), respectively: The region from northern Maine and Upstate New York south to southern Connecticut, most of northern New Jersey, and western Maryland has a humid continental climate (Dfa/Dfb/Dc), with warm-to-hot summers, cold and snowy winters with at least one month averaging below freezing, and four to seven months warmer than 50°F. The area from Long Island and New York City south to southern Delaware and western North Carolina has a temperate climate (Cfa/Do in the Trewartha climate classification), with long and hot summers with at least one month over 22°C (71.6°F,) cool winters with all months over freezing, and six to seven months above 50°F. [1] The area from the southern Delmarva Peninsula, SE Virginia, and central NC south to central Florida is subtropical (Cfa/Cf), with hot and rainy summers, mild and drier winters, and eight to twelve months above 50°F. Around south-central Florida southward (from the line from Stuart to Fort Myers south through the Florida Keys) exists a tropical climate (Af/Aw/Ar) which is usually frost-free, is warm to hot all year, and has all months averaging above 18°C (64.4°F). [2] This is the only tropical climate in the continental US. The least common climate on the East Coast is the oceanic (Cfb/Do), which is only found on Block Island and Nantucket and in areas of the southern Appalachian Mountains. This zone has all monthly averages between 0 and 22°C and six to seven months above 50°F. Seasonally, average monthly precipitation ranges from a slight late fall (November) maximum from Massachusetts northward (as at Portland, Maine), to a slight summer maximum in the Mid-Atlantic states from southern Connecticut south to Virginia (as at Wilmington, Delaware and Norfolk, Virginia), to a more pronounced summer maximum from Cape Hatteras, North Carolina, southward along the Southeastern United States coast to Savannah, Georgia. The Florida peninsula has a sharp wet-summer/dry-winter pattern, with 60 to 70% of precipitation falling between June and October in an average year and a dry, and sunny late fall, winter, and early spring. Although landfalls are rare, the Eastern Seaboard is susceptible to hurricanes in the Atlantic hurricane season, officially running from June 1 to November 30, although hurricanes can occur before or after these dates.[6] Hurricanes Hazel, Hugo, Bob, Isabel, Irene, and Sandy, and most recently Florence, Isaias, Henri, and Ida are some of the more significant storms to have affected the region.[3] The East Coast (except for eastern Maine) is a low-relief, passive margin coast.[7] It has been shaped by the Pleistocene glaciation in the far northern areas in New England, with offshore islands such as Nantucket, Martha's Vineyard, Block Island, and Fishers Island. From around northern New Jersey southward, the coastal plain broadens southwards, separated from the Piedmont region by the Atlantic Seaboard fall line of the East Coast rivers, often marking the head of navigation and prominent sites of cities. The coastal areas from Long Island south to Florida are often made up of barrier islands that front the coastal areas, with the long stretches of sandy beaches. Many of the larger capes along the lower East Coast are in fact barrier islands, like the Outer Banks of North Carolina and Cape Canaveral, Florida. The Florida Keys are made up of limestone coral and provide the only coral reefs on the US mainland. Demographics[edit]In 2010, the population of the states that have shoreline on the East Coast was estimated at 112,642,503 (36% of the country's total population). New York City is both the largest city and the largest metropolitan area on the East Coast. The East Coast is the most populated coastal area in the United States.[8]
Transportation[edit]The primary Interstate Highway along the East Coast is Interstate 95, completed in 2018,[9][10] which replaced the historic U.S. Route 1 (Atlantic Highway), the original federal highway that traversed all East Coast states, except Delaware.[11] By water, the East Coast is connected from Boston, Massachusetts to Miami, Florida, by the Intracoastal Waterway, also known as the East Coast Canal, which was completed in 1912.[12][13] Amtrak's Downeaster and Northeast Regional offer the main passenger rail service on the Seaboard. The Acela Express offers the only high-speed rail passenger service in the Americas. Between New York and Boston the Acela Express has up to a 54% share of the combined train and air passenger market.[14][15] Some of the largest airports in the United States are located along the East Coast of the United States, such as John F. Kennedy International Airport in New York, Logan International Airport in Boston, Newark Liberty Airport in Newark, New Jersey, Philadelphia International Airport in Philadelphia, Baltimore–Washington International Airport near Baltimore, Washington-Dulles International Airport near Washington, D.C., Hartsfield–Jackson International Airport in Atlanta, Miami International Airport in Miami, Charlotte Douglas International Airport in Charlotte, Tampa International Airport in Tampa and Orlando International Airport in Orlando, Florida. Culture[edit]As the first spot in the United States that immigrants arrived and the close proximity of Europe, the Caribbean and Latin America, the East Coast is home to a diverse population and home to multi-cultures when compared to the rest of the US. From the strong Latin culture in southern Florida and New York City, to the 200-year-old Gullah culture of the low country coastal islands of Georgia and South Carolina, to the many historic cities in the Middle Atlantic where a strong English, German, Italian, Irish, and French culture are present, the East Coast is significantly more diverse than the rest of the United States. Numerous Chinatowns in New York City, and Little Havana in Miami, are examples of such cultural centers in the bigger cities. The East Coast is home to much of the political and financial power of the United States, as well as the center for resort and travel destinations in the United States. New York City is the largest city and financial center of the world. Seventy-one of the world's Fortune 500 companies have their corporate headquarters in New York City, while Midtown Manhattan with 400 million square feet of office space in 2018, is the largest central business district in the world. Washington, D.C. is the capital and political nerve center of the United States. Many organizations such as defense contractors, civilian contractors, nonprofit organizations, lobbying firms, trade unions, industry trade groups and professional associations have their headquarters in or near Washington, D.C., in order to be close to the federal government. Miami and Florida are two of the top domestic and international travel destinations in the United States. Miami is the warmest major city in the United States in winter, this factor contributes to it being a major tourism hub for international visitors. Miami has one of the largest concentrations of international banks in the United States, and the third tallest skyline in the U.S. with over 300 high-rises, 55 of which exceed 490 ft (149 m). The port of Miami is the busiest cruise port in the world in both passenger traffic and cruise lines, with over 5.5 million cruise passengers passing through the port each year. The center for tropical plant culture and research in the United States is based in Miami at Fairchild Tropical Botanic Garden, while the state of Florida is the number two producer of oranges in the world behind Brazil. See also[edit]
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References[edit]
What is the main difference between airports of the early 1920's and international airports of the 1930's?What is the main difference between airports of the early 1920s and international airports of the 1930s? Airports in the early 1920s catered to municipal and regional travel, while airports in the 1930s served as hubs for travel between countries.
How did Airports encourage city growth quizlet?How did airports encourage city growth? They promoted the building of hotels, restaurants, services, and rapid transit to accommodate travelers.
Was one of the world's first subway systems opening in 1863?The London Underground, which opened in 1863, was the world's first underground railway system. More than 30,000 passengers tried out the Tube on the opening day and it was hailed by the Times as “the great engineering triumph of the day”.
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Major cities in the western us are more likely to be older than major cities on the atlantic coast.
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