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Inlets Of Maine
An inlet is a (usually long and narrow) indentation of a shoreline, such as a small arm, bay, sound, fjord, lagoon or marsh, that leads to an enclosed larger body of water such as a lake, estuary, gulf or marginal sea. Overview In marine geography, the term "inlet" usually refers to either the actual channel between an enclosed bay and the open ocean and is often called an "entrance", or a significant recession in the shore of a sea, lake or large river. A certain kind of inlet created by past glaciation is a fjord, typically but not always in mountainous coastlines and also in montane lakes. Multi-arm complexes of large inlets or fjords may be called sounds, e.g., Puget Sound, Howe Sound, Karmsund (''sund'' is Scandinavian for "sound"). Some fjord-type inlets are called canals, e.g., Portland Canal, Lynn Canal, Hood Canal, and some are channels, e.g., Dean Channel and Douglas Channel. Tidal amplitude, wave intensity, and wave direction are all factors that influ ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bucht Am Golf Von Neapel
Bucht is a Swedish surname. Notable people with the surname include: * Gunnar Bucht (born 1927), Swedish composer and musicologist *Märta Bucht Märta Johanna Bucht (1882–1962) was a Swedish schoolteacher, suffragist and peace activist. From 1908, she chaired the Luleå branch of the Swedish Association for Women's Suffrage (FKPR). She was also active in the peace movement. In 1919, sh ... (1882–1962), Swedish schoolteacher, suffragist and peace activist * Sven-Erik Bucht (born 1954), Swedish politician of the Social Democrats {{surname Swedish-language surnames ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glaciation
A glacial period (alternatively glacial or glaciation) is an interval of time (thousands of years) within an ice age that is marked by colder temperatures and glacier advances. Interglacials, on the other hand, are periods of warmer climate between glacial periods. The Last Glacial Period ended about 15,000 years ago. The Holocene is the current interglacial. A time with no glaciers on Earth is considered a greenhouse climate state. Quaternary Period Within the Quaternary, which started about 2.6 million years before present, there have been a number of glacials and interglacials. At least eight glacial cycles have occurred in the last 740,000 years alone. Penultimate Glacial Period The Penultimate Glacial Period (PGP) is the glacial period that occurred before the Last Glacial Period. It began about 194,000 years ago and ended 135,000 years ago, with the beginning of the Eemian interglacial. Last Glacial Period The last glacial period was the most recent glacial period ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tropical Cyclone
A tropical cyclone is a rapidly rotating storm system characterized by a low-pressure center, a closed low-level atmospheric circulation, strong winds, and a spiral arrangement of thunderstorms that produce heavy rain and squalls. Depending on its location and strength, a tropical cyclone is referred to by different names, including hurricane (), typhoon (), tropical storm, cyclonic storm, tropical depression, or simply cyclone. A hurricane is a strong tropical cyclone that occurs in the Atlantic Ocean or northeastern Pacific Ocean, and a typhoon occurs in the northwestern Pacific Ocean. In the Indian Ocean, South Pacific, or (rarely) South Atlantic, comparable storms are referred to simply as "tropical cyclones", and such storms in the Indian Ocean can also be called "severe cyclonic storms". "Tropical" refers to the geographical origin of these systems, which form almost exclusively over tropical seas. "Cyclone" refers to their winds moving in a circle, whirling round ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Barrier Island
Barrier islands are coastal landforms and a type of Dune, dune system that are exceptionally flat or lumpy areas of sand that form by wave and tidal action parallel to the mainland coast. They usually occur in chains, consisting of anything from a few islands to more than a dozen. They are subject to change during storms and other action, but absorb energy and protect the coastlines and create areas of protected waters where wetlands may flourish. A barrier chain may extend uninterrupted for over a hundred kilometers, excepting the tidal inlets that separate the islands, the longest and widest being Padre Island of Texas, United States. Sometimes an important inlet may close permanently, transforming an island into a peninsula, thus creating a barrier peninsula, often including a beach, barrier beach. The length and width of barriers and overall morphology of barrier coasts are related to parameters including tidal range, wave energy, Sediment transport, sediment supply, Sea leve ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Douglas Channel
Douglas Channel is one of the principal inlets of the British Columbia Coast. Its official length from the head of Kitimat Arm, where the aluminum smelter town of Kitimat to Wright Sound, on the Inside Passage ferry route, is . The actual length of the fjord's waterway includes waters between there and the open waters of the Hecate Strait outside the coastal archipelago, comprising another for in total. Geography The Kitimat River flows into the Kitimat Arm portion of Douglas Channel. The channel is named in honour of Sir James Douglas, the first governor of the Colony of British Columbia. A major side-inlet, the Gardner Canal, is in length, and is accessed from the Kitimat Arm of Douglas Channel via Devastation Channel (), which is on the east side of Hawkesbury Island. South of Hawkesbury is Varney Passage (), which has a sidechannel, Ursula Passage (). Total waterway length of the fjord dominated by Douglas Channel is therefore, not counting smaller side-inlets, , longer tha ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dean Channel
Dean Channel is the upper end of one of the longest inlets of the British Columbia Coast, from its head at the mouth of the Kimsquit River. The Dean River, one of the main rivers of the Coast Mountains, enters Dean Channel about below the head of the inlet, at the community of Kimsquit. History Dean Channel was named by Captain Vancouver in 1793 after Rev. James King, Dean of Raphoe, Ireland. The channel was surveyed by Captain Richards in 1861 of HMS ''Hecate''. It is located within the Central Coast region. Branches Ending at the mouth of Cousins Inlet, which is the harbour for the abandoned town of Ocean Falls, the fjord's name changes to Fisher Channel down the west side of King Island. Below Fisher Channel's length the fjord merges with Burke Channel, which is a arm of the Dean/Fisher Channel on the east side of King Island, the name of the fjord changes to Fitz Hugh Sound, which is considerably wider than the upper part of the fjord at about in width and is itse ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hood Canal
Hood Canal is a fjord forming the western lobe, and one of the four main basins,Features Of Puget Sound Region: Oceanography And Physical Processes Chapter 3 of th King County Department of Natural Resources, Seattle, Washington, 2001. of in the US state of Washington. It is one ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lynn Canal
Lynn Canal is an inlet (not an artificial canal) into the mainland of southeast Alaska. Lynn Canal runs about from the inlets of the Chilkat River south to Chatham Strait and Stephens Passage. At over in depth, Lynn Canal is the deepest fjord in North America (outside Greenland) and one of the deepest and longest in the world. The northern portion of the canal braids into the respective Chilkat, Chilkoot, and Taiya Inlets. Lynn Canal was explored by Joseph Whidbey in 1794 and named by George Vancouver for his birthplace, King's Lynn, Norfolk, England. Lynn Canal was frequently visited by maritime fur traders from at least 1800. The '' Atahualpa'' visited in 1801 and its log mentions an earlier trading visit by an unidentified ship. In April 1811 the American maritime fur trader Samuel Hill Samuel Hill (13 May 1857 – 26 February 1931), usually known as Sam Hill, was an American businessman, lawyer, railroad executive, and advocate of good roads. He su ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Portland Canal
, image = Hyder Alaska IMG 0276 (22495379342).jpg , alt = , caption = Portland Canal from Hyder, Alaska , image_bathymetry = , alt_bathymetry = , caption_bathymetry = , location = Alaska and British Columbia , group = , coordinates = , type = Fjord , etymology = , part_of = Portland Inlet , inflow = , rivers = , outflow = , oceans = , catchment = , basin_countries = Canada and United States , agency = , designation = , date-built = , engineer = , date-flooded = , length = , width = , area = , depth = , max-depth = , volume = , residence_time = , salinity = , shore = , elevation = , temperature_high = , temperature_low = , frozen = , islands = , islands_category = , sections = , trenches = , benches = , cities = , pushpin_map = Canada British Columbia , pushpin_label_position = , pushpin_map_alt = , pushpin_map_caption = , website = , reference = Portland Canal is an arm of Portland Inlet, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canal
Canals or artificial waterways are waterways or engineered channels built for drainage management (e.g. flood control and irrigation) or for conveyancing water transport vehicles (e.g. water taxi). They carry free, calm surface flow under atmospheric pressure, and can be thought of as artificial rivers. In most cases, a canal has a series of dams and locks that create reservoirs of low speed current flow. These reservoirs are referred to as ''slack water levels'', often just called ''levels''. A canal can be called a ''navigation canal'' when it parallels a natural river and shares part of the latter's discharges and drainage basin, and leverages its resources by building dams and locks to increase and lengthen its stretches of slack water levels while staying in its valley. A canal can cut across a drainage divide atop a ridge, generally requiring an external water source above the highest elevation. The best-known example of such a canal is the Panama Canal. Many ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Scandinavian Languages
The North Germanic languages make up one of the three branches of the Germanic languages—a sub-family of the Indo-European languages—along with the West Germanic languages and the extinct East Germanic languages. The language group is also referred to as the Nordic languages, a direct translation of the most common term used among Danish, Faroese, Icelandic,Elfdalian,Norwegian, Gutnish, and Swedish scholars and people. The term ''North Germanic languages'' is used in comparative linguistics, whereas the term Scandinavian languages appears in studies of the modern standard languages and the dialect continuum of Scandinavia. Danish, Norwegian and Swedish are close enough to form a strong mutual intelligibility where cross-border communication in native languages is very common. Approximately 20 million people in the Nordic countries speak a Scandinavian language as their native language,Holmberg, Anders and Christer Platzack (2005). "The Scandinavian languages". ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Karmsund
Karmsund is a strait located in Rogaland county, Norway. The long strait separates the island of Karmøy on the west and the mainland of Norway and island of Vestre Bokn in the east. The strait runs through the municipalities of Haugesund, Karmøy, and Bokn. The town of Haugesund lies at the northern end of the strait and the town of Kopervik lies in the central part of the strait, and the town of Skudeneshavn lies near the southern end where the strait flows into the Boknafjorden. The Karmsund Bridge, a part of the European route E134 highway, links Karmøy to the mainland. The bridge was completed in 1955. The small islands of Vibrandsøy, Risøy, and Hasseløy lie in the strait at the northern end, just off shore from the town of Haugesund. Near the Norsk Hydro Factory on Karmøy, there are three powerlines that cross the Karmsund on tall electricity pylons, which are the tallest in Norway. A local newspaper in this area is named after the strait: ''Karmsund Avis''. His ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
