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Outer Banks
The Outer Banks (frequently abbreviated OBX) are a string of barrier islands and spits off the coast of North Carolina and southeastern Virginia, on the east coast of the United States. They line most of the North Carolina coastline, separating Currituck Sound, Albemarle Sound, and Pamlico Sound from the Atlantic Ocean. A major tourist destination, the Outer Banks are known for their wide expanse of open beachfront and the Cape Hatteras National Seashore. The seashore and surrounding ecosystem are important biodiversity zones, including beach grasses and shrubland that help maintain the form of the land. The Outer Banks were sites of early European settlement in the United States and remain important economic and cultural sites. Most notably the English Roanoke Colony vanished from Roanoke Island in 1587 and was the first location where an English person, Virginia Dare, was born in the Americas. The hundreds of shipwrecks along the Outer Banks have given the surrounding seas th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wright Flyer
The ''Wright Flyer'' (also known as the ''Kitty Hawk'', ''Flyer'' I or the 1903 ''Flyer'') made the first sustained flight by a manned heavier-than-air powered and controlled aircraft—an airplane—on December 17, 1903. Invented and flown by Wright brothers, Orville and Wilbur Wright, it marked the beginning of the Aviation in the pioneer era, pioneer era of aviation. The Wright brothers flew the ''Wright Flyer'' four times that day on land now part of the town of Kill Devil Hills, North Carolina, Kill Devil Hills, about south of Kitty Hawk, North Carolina. The aircraft was preserved and is now exhibited in the National Air and Space Museum in Washington, D.C. Design and construction The ''Flyer'' was based on the Wrights' experience testing gliders at Kitty Hawk between 1900 and 1902. Their last glider, the 1902 Wright Glider, 1902 Glider, led directly to the design of the ''Wright Flyer''. The Wrights built the aircraft in 1903 using Sitka spruce, spruce for straight ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bogue Banks
Bogue Banks form a barrier island off the mainland of North Carolina in Carteret County. The island, separated from the mainland by Bogue Sound, runs east to west, with the ocean beaches facing due south. Bogue Banks is the only island on the Carteret County shore that has been developed with housing: numerous communities are located on the island and can be accessed by one of two bridges across Bogue Sound, either from Morehead City to Atlantic Beach, which is the more heavily traveled bridge, or from Cape Carteret to Emerald Isle. The communities of Bogue Banks are the most prominent of the Crystal Coast. NC 58 traverses a majority of the island's length. There are several hotels that dot the island, but most of the land contains private houses, some of which are rented out during the summer, or maritime forest. Stores and other commercial properties are limited to the five main communities. History During a survey titled "The Greater Beaufort Area at 1800" completed by th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Crystal Coast
In North Carolina, the Crystal Coast is an 85-mile stretch of coastline that extends from the Cape Lookout National Seashore, which includes 56 miles of protected beaches, southwestward to the New River. The Crystal Coast is a popular area with tourists and second-home owners in the summer. The absolute boundaries of this coast are often disputed, but the main area includes all the major Carteret County beaches (those on Bogue Banks, which face south). It also includes eastern portions of Carteret County, such as Harkers Island, Down East and Shackleford Banks, as well as the northern Onslow County beaches (Bear Island/Hammock's Beach), and a few ports along the Intracoastal Waterway. Some tourism marketing describes the region as the Southern Outer Banks, to draw a connection to the main barrier islands of the Outer Banks. The main communities include the coastal resorts of Atlantic Beach, Emerald Isle, Indian Beach, Pine Knoll Shores and Salter Path, as well as the inl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Core Banks
The Core Banks are barrier islands in North Carolina, part of the Outer Banks and Cape Lookout National Seashore. Named after the Coree tribe, they extend from Ocracoke Inlet to Cape Lookout, and consist of two low-relief narrow islands, North Core Banks and South Core Banks, and, since September 2011, two smaller islands. New Drum Inlet, Old Drum Inlet and Ophelia Inlet now separate the islands. The Core Banks are now uninhabited. However, Portsmouth, at the north end of the North Core Banks, was once a substantial port, and Cape Lookout Village, about one and half miles south of the Cape Lookout Lighthouse, contains the historic Lookout Life-Saving Station, a U.S. Coast Guard Station, and several island homes. Access Islands can be reached by two vehicle ferries. One ferry crosses Core Sound from Atlantic to North Core Banks, and another crosses the sound from Davis to South Core Banks. There are no roads on the islands: vehicles use the beach and four wheel drive tr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Core Banks, North Carolina
The Core Banks are barrier islands in North Carolina, part of the Outer Banks and Cape Lookout National Seashore. Named after the Coree tribe, they extend from Ocracoke Inlet to Cape Lookout, and consist of two low-relief narrow islands, North Core Banks and South Core Banks, and, since September 2011, two smaller islands. New Drum Inlet, Old Drum Inlet and Ophelia Inlet now separate the islands. The Core Banks are now uninhabited. However, Portsmouth, at the north end of the North Core Banks, was once a substantial port, and Cape Lookout Village, about one and half miles south of the Cape Lookout Lighthouse, contains the historic Lookout Life-Saving Station, a U.S. Coast Guard Station, and several island homes. Access Islands can be reached by two vehicle ferries. One ferry crosses Core Sound from Atlantic to North Core Banks, and another crosses the sound from Davis to South Core Banks. There are no roads on the islands: vehicles use the beach and four wheel drive ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hurricane Irene
Hurricane Irene was a large and destructive tropical cyclone which affected much of the Caribbean and East Coast of the United States during late August 2011. The ninth named storm, first hurricane, and first major hurricane of the 2011 Atlantic hurricane season, Irene originated from a well-defined Atlantic tropical wave that began showing signs of organization east of the Lesser Antilles. Due to development of atmospheric convection and a closed center of circulation, the system was designated as Tropical Storm Irene on August 20, 2011. After intensifying, Irene made landfall in St. Croix as a strong tropical storm later that day. Early on August 21, the storm made a second landfall in Puerto Rico. While crossing the island, Irene strengthened into a Category 1 hurricane. The storm paralleled offshore of Hispaniola, continuing to slowly intensify in the process. Shortly before making four landfalls in the Bahamas, Irene peaked as a Category 3 hurricane. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tropical Cyclones And Climate Change
Climate change can affect tropical cyclones in a variety of ways: an intensification of rainfall and wind speed, a decrease in overall frequency, an increase in the frequency of very intense storms and a poleward extension of where the cyclones reach maximum intensity are among the possible consequences of human-induced climate change. Tropical cyclones use warm, moist air as their source of energy or "fuel". As climate change is warming ocean temperatures, there is potentially more of this fuel available. Between 1979 and 2017, there was a global increase in the proportion of tropical cyclones of Category 3 and higher on the Saffir–Simpson scale. The trend was most clear in the North Atlantic and in the Southern Indian Ocean. In the North Pacific, tropical cyclones have been moving poleward into colder waters and there was no increase in intensity over this period. With warming, a greater percentage (+13%) of tropical cyclones are expected to reach Category 4 and 5 strength ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hatteras Island
Hatteras Island (historically Croatoan Island) is a barrier island located off the North Carolina coast. Dividing the Atlantic Ocean and the Pamlico Sound, it runs parallel to the coast, forming a bend at Cape Hatteras. It is part of North Carolina's Outer Banks and includes the communities of Rodanthe, Waves, Salvo, Avon, Buxton, Frisco, and Hatteras. It contains the largest part of the Cape Hatteras National Seashore. Prior to European settlement the island was inhabited by Croatoan Native Americans. The island has a land area of and a population of 4,322, as of the 2010 census. It lies in parts of Kinnakeet Township and Hatteras Township in Dare County, and Ocracoke Township in Hyde County. Hatteras Island is known for sport fishing, surfing, windsurfing and kiteboarding, and Hatteras Village is known as the "Blue Marlin Capital of the World". The island is one of the longest in the contiguous United States, measuring along a straight line from end to end, or ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Coastal Management
Coastal management is defence against flooding and erosion, and techniques that stop erosion to claim lands. Protection against rising sea levels in the 21st century is crucial, as sea level rise accelerates due to climate change. Changes in sea level damage beaches and coastal systems are expected to rise at an increasing rate, causing coastal sediments to be disturbed by tidal energy. Coastal zones occupy less than 15% of the Earth's land area, while they host more than 40% of the world population. Nearly 1.2 billion people live within 100 km of shoreline and 100 m of sea level, with an average density 3 times higher than the global average for population. With three-quarters of the world population expected to reside in the coastal zone by 2025, human activities originating from this small land area will impose heavy pressure on coasts. Coastal zones contain rich resources to produce goods and services and are home to most commercial and industrial activities. Hi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Climate Change In North Carolina
Climate change in North Carolina is of concern due to its impacts on the environment, climate, people, and economy of North Carolina. "Most of the state has warmed one-half to one degree (F) in the last century, and the sea is rising about one inch every decade." North Carolina, along with the rest of the Southeastern United States, has warmed less than the rest of the country. Temperature and climate Around the year 2080, "temperatures are likely to rise above 95°F approximately 20 to 40 days per year in most of the state, compared with about 10 days per year" in 2016. If current warming trends continue, by 2080 "North Carolina will likely feel like the Florida Panhandle or possibly like northern Mexico within a generation." The State Climate Office predicts as of 2020 that temperatures will increase 4-10 degrees Fahrenheit by the end of the century. Coastline "The United States Geological Survey estimates that the lightly developed Outer Banks between Nags Head and Ocr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Coastal Erosion
Coastal erosion is the loss or displacement of land, or the long-term removal of sediment and rocks along the coastline due to the action of waves, currents, tides, wind-driven water, waterborne ice, or other impacts of storms. The landward retreat of the shoreline can be measured and described over a temporal scale of tides, seasons, and other short-term cyclic processes. Coastal erosion may be caused by hydraulic action, abrasion, impact and corrosion by wind and water, and other forces, natural or unnatural. On non-rocky coasts, coastal erosion results in rock formations in areas where the coastline contains rock layers or fracture zones with varying resistance to erosion. Softer areas become eroded much faster than harder ones, which typically result in landforms such as tunnels, bridges, columns, and pillars. Over time the coast generally evens out. The softer areas fill up with sediment eroded from hard areas, and rock formations are eroded away. Also erosion com ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
