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Inlets Of Alaska
An inlet is a typically long and narrow indentation of a shoreline such as a small arm, cove, 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 ... [...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 (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] |
Enclosed Bay
A bay is a recessed, coastal body of water that directly connects to a larger main body of water, such as an ocean, a lake, or another bay. A large bay is usually called a Gulf (geography), ''gulf'', ''sea'', sound (geography), ''sound'', or bight (geography), ''bight''. A ''cove'' is a small, circular bay with a narrow entrance. A ''fjord'' is an elongated bay formed by glacial action. The term ''embayment'' is also used for , such as extinct bays or freshwater environments. A bay can be the estuary of a river, such as the Chesapeake Bay, an estuary of the Susquehanna River. Bays may also be nested within each other; for example, James Bay is an arm of Hudson Bay in Atlantic Canada, northeastern Canada. Some large bays, such as the Bay of Bengal and Hudson Bay, have varied marine geology. The land surrounding a bay often reduces the strength of winds and blocks waves. Bays may have as wide a variety of shoreline characteristics as other shorelines. In some cases, bays have Bea ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Douglas Channel
Douglas Channel is one of the principal inlets (or fjords) of the British Columbia Coast, into which the Kitimat River flows. The channel was named in honour of Sir James Douglas, the first governor of the Colony of British Columbia. The official length, from the head of Kitimat Arm and the aluminum smelter town of Kitimat to Wright Sound (on the Inside Passage ferry route), is . The full length of the fjord's waterways includes waters between Kitimat and the open waters of the Hecate Strait, outside of the coastal archipelago, stretching for another , reaching in-total. Geography A major side-inlet, the Gardner Canal, is in length, accessible from the Kitimat Arm of the Douglas Channel via Devastation Channel (), on the east side of Hawkesbury Island. South of Hawkesbury is Verney Passage (), which has a side-channel called Ursula Passage (). Total length of the fjord waterway dominated by Douglas Channel is therefore (not counting smaller side-inlets) roughly , con ... [...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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hood Canal
Hood Canal is a fjord-like body of water that lies south of Admiralty Inlet in Washington State that some consider to be the western lobe and one of the five main basins of Puget Sound.Features Of Puget Sound Region: Oceanography And Physical Processes Chapter 3 of th King County Department of Natural Resources, Seattle, Washington, 2001. It is one of the minor bodies of water that constitute the Salish Sea. Maximum depth is 600 ft. Hood Canal is not a |
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. The Tlingit are the indigenous people of the Lynn Canal's shores and waterways. The inlet was explored for the Royal Navy 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, captain of ''Otter'', battled the Chilkat Tlingit in the Chilkat Inlet of Lynn Ca ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Portland Canal
Portland Canal is an arm of Portland Inlet, one of the principal inlets of the British Columbia Coast. It is approximately long. The Portland Canal forms part of the border between southeastern Alaska and British Columbia. The name of the entire inlet in the Nisga'a language is ', with meaning "at the back of (someplace)". The upper end of the inlet was home to the Tsetsaut ( in Nisgaʼa), who after being decimated by war and disease were taken under the protection of the Laxsgiik (Eagle) chief of the Nisgaʼa, who holds the inlet's title in native law. Despite its naming as a canal, the inlet is a fjord, a completely natural and not man-made geographic feature, and extends northward from the Portland Inlet at Pearse Island, British Columbia, to Stewart, British Columbia, and Hyder, Alaska. Observatory Inlet joins the Portland Canal at Ramsden Point, where both merge with Portland Inlet. Pearse Canal joins Portland Canal at the north end of Pearse Island. Portland C ... [...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 Can ... [...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, Norwegian, 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, particularly between the latter two. Approximately 20 million people in the Nordic countries speak a Scandinavian language as their native language,Holmberg, Anders and Christer Platzack (2005). "The Scandi ... [...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: ''Karmsun ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Howe Sound
Howe Sound (, ) is a roughly triangular sound (geography), sound, that joins a network of fjords situated immediately northwest of Vancouver, British Columbia, Canada. It was designated as a UNESCO Biosphere Reserve in 2021. Geography Howe Sound's mouth at the Strait of Georgia is situated between West Vancouver and the Sunshine Coast (British Columbia), Sunshine Coast. The sound is triangular, opening to the southwest into the Strait of Georgia, and extends northeast to its head at Squamish, British Columbia, Squamish. There are several islands in the sound, three of which are large and mountainous in their own right. The steep-sided mainland shores funnel the breezes as the daily thermals build the wind to or more at the northern end of the sound on a typical summer day. A small outcrop of volcanic rock is located on the eastern shore of Howe Sound called the Watts Point volcanic centre. History The history of Howe Sound begins with the Indigenous people, the Squamish people, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Puget Sound
Puget Sound ( ; ) is a complex estuary, estuarine system of interconnected Marine habitat, marine waterways and basins located on the northwest coast of the U.S. state of Washington (state), Washington. As a part of the Salish Sea, the sound (geography), sound has one major and two minor connections to the Strait of Juan de Fuca, which in turn connects to the open Pacific Ocean. The major connection is Admiralty Inlet; the minor connections are Deception Pass and the Swinomish Channel. Puget Sound extends approximately from Deception Pass in the north to Olympia, Washington, Olympia in the south. Its average depth is and its maximum depth, off Jefferson Point between Indianola, Washington, Indianola and Kingston, Washington, Kingston, is . The depth of the main basin, between the southern tip of Whidbey Island and Tacoma, Washington, Tacoma, is approximately . In 2009, the term Salish Sea was established by the United States Board on Geographic Names as the collective wate ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
