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Julsundet

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Julsundet is a 15-kilometre (9.3 mi) long strait connecting the Norwegian Sea to the Romsdalsfjorden . The strait is located about 10 kilometres (6.2 mi) west of the town of Molde in Møre og Romsdal county, Norway . The strait runs through the municipalities of Fræna , Aukra , Molde , and Midsund . The strait flows north–south from the village of Bud (in Fræna Municipality) to Julneset (in Molde Municipality). It flows between the Romsdal peninsula (on the east side) and the islands of Otrøya and Gossa (on the west side). The Frænfjorden empties into the Julsundet strait at the small island of Vågøya .

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24-453: The strait is up to 500 metres (1,600 ft) deep and it is 2 to 3 kilometres (1.2 to 1.9 mi) wide. It has a significant tidal current and is exposed to strong northerly winds. Julsundet was heavily fortified by the Germans during World War II . The mainland part of Aukra Municipality is also often referred to as Julsundet . This Møre og Romsdal location article is

48-416: A stub . You can help Misplaced Pages by expanding it . Strait A strait is a water body connecting two seas or two water basins. While the landform generally constricts the flow, the surface water still flows, for the most part, at the same elevation on both sides and through the strait in both directions. In some straits there may be a dominant directional current through the strait. Most commonly, it

72-492: A continuous line east to Seabird Point ( Discovery Island ), British Columbia, Cattle Point ( San Juan Island ), Washington, Iceberg Point ( Lopez Island ), Point Colville (Lopez Island), and then to Rosario Head ( Fidalgo Island ). The eastern boundary runs south from Rosario Head across Deception Pass to Whidbey Island , then along the western coast of Whidbey Island to Point Partridge , then across Admiralty Inlet to Point Wilson ( Quimper Peninsula ). The northern coast of

96-602: A dilemma for the federal government of Canada. If Canada holds that the principle of natural prolongation applies to the Juan de Fuca Canyon on its Pacific Ocean coast, the assertion could undermine Canada's argument in the Gulf of Maine boundary dispute . In this Atlantic Ocean context, Canada favours an outcome based on the principle of equidistance. In March 2008, the Chemainus First Nation proposed renaming

120-789: A part of high seas or an exclusive economic zone with the territorial sea of a coastal nation ( Straits of Tiran , Strait of Juan de Fuca , Strait of Baltiysk ) and (2) in straits formed by an island of a state bordering the strait and its mainland if there exists seaward of the island a route through the high seas or through an exclusive economic zone of similar convenience with respect to navigational and hydrographical characteristics ( Strait of Messina , Pentland Firth ). There may be no suspension of innocent passage through such straits. [REDACTED] Media related to Straits at Wikimedia Commons Strait of Juan de Fuca The Strait of Juan de Fuca (officially named Juan de Fuca Strait in Canada)

144-590: A resolution only recommending that the name be adopted by the Geographical Names Board of Canada , should its US counterpart approve the name-change. The United States Board on Geographic Names approved the name on November 12, 2009. Counties along the Strait of Juan de Fuca: Regional districts along the Strait of Juan de Fuca: Certain groups of seabirds called common murre migrate north by swimming. Some Pacific Coast murres paddle north to

168-668: Is a body of water about 96 miles (83 nmi; 154 km) long that is the Salish Sea 's main outlet to the Pacific Ocean . The international boundary between Canada and the United States runs down the centre of the Strait. It was named in 1787 by the maritime fur trader Charles William Barkley , captain of Imperial Eagle , for Juan de Fuca , the Greek navigator who sailed in a Spanish expedition in 1592 to seek

192-501: Is a narrowing channel that lies between two land masses . Some straits are not navigable, for example because they are either too narrow or too shallow, or because of an unnavigable reef or archipelago . Straits are also known to be loci for sediment accumulation. Usually, sand-size deposits occur on both the two opposite strait exits, forming subaqueous fans or deltas . The terms channel , pass , or passage can be synonymous and used interchangeably with strait , although each

216-562: Is sometimes differentiated with varying senses. In Scotland, firth or Kyle are also sometimes used as synonyms for strait. Many straits are economically important. Straits can be important shipping routes and wars have been fought for control of them. Numerous artificial channels, called canals , have been constructed to connect two oceans or seas over land, such as the Suez Canal . Although rivers and canals often provide passage between two large lakes, and these seem to suit

240-512: The California sea lion and Steller's sea lion , in addition to the gray whale , another cetacean with both residential and nomadic groups in the Strait. As migratory gray whales swim between Baja California and Alaska each year, they will often be seen in the Strait of Juan de Fuca, feeding on small marine creatures on the seafloor, and using the Strait as a sort of "rest stop" on their long journeys. They also socialize with and encounter

264-693: The Olympic Peninsula forms the southern boundary of the strait. In the eastern entrance to the Strait, the Race Rocks Archipelago is in the high current zone halfway between Port Angeles, Washington, and Victoria, BC. Like the rest of the Salish Sea and surrounding regions, the climate of the Strait is disputed, with the Köppen system classifying it as Mediterranean , but most regional climatologists preferring oceanic . While

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288-518: The Pacific Ocean between Vancouver Island , British Columbia, and the Olympic Peninsula , Washington, to Haro Strait , San Juan Channel, Rosario Strait , and Puget Sound . The Pacific Ocean boundary is formed by a line between Cape Flattery and Tatoosh Island , Washington, and Carmanah Point (Vancouver Island), British Columbia. Its northern boundary follows the shoreline of Vancouver Island from Carmanah Point to Gonzales Point, then follows

312-620: The Strait of Georgia and related waters under the more general name Salish Sea . This latter definition was made official in 2009 by geographic boards of Canada and the United States. In October 2009, the Washington State Board of Geographic Names approved the Salish Sea toponym , not to replace the names of the Strait of Georgia, Puget Sound, and Strait of Juan de Fuca, but instead as a collective term for all three. The British Columbia Geographical Names Office passed

336-576: The United States. In addition, the government of British Columbia has rejected both equidistant proposals, instead arguing that the Juan de Fuca submarine canyon is the appropriate "geomorphic and physiogeographic boundary". The proposed equidistant boundary currently marks the northern boundary of the Olympic Coast National Marine Sanctuary . British Columbia's position is based on the principle of natural prolongation which developed in international law . It poses

360-524: The United States. The dispute is only over the seaward boundary extending 200 nautical miles (370 km) west from the mouth of the strait. The maritime boundary within the strait is not in dispute. Both governments have proposed a boundary based on the principle of equidistance , but with different basepoint selections, resulting in small differences in the line. Resolution of the issue should be simple, but has been hindered because it might influence other unresolved maritime boundary issues between Canada and

384-623: The climate is mostly oceanic in nature, the dry summers result in the Mediterranean classification in the Köppen system. Rainfall ranges from over 100 inches (250 cm) ( temperate rainforest ) conditions at the west end to as little as 16 inches (410 mm) at the east end, near Sequim . Because it is exposed to the generally westerly winds and waves of the Pacific, seas and weather in Juan de Fuca Strait are, on average, rougher than in

408-583: The converse of isthmuses . That is, while a strait lies between two land masses and connects two large areas of ocean, an isthmus lies between two areas of ocean and connects two large land masses. Some straits have the potential to generate significant tidal power using tidal stream turbines . Tides are more predictable than wave power or wind power . The Pentland Firth (a strait) may be capable of generating 10  GW . Cook Strait in New Zealand may be capable of generating 5.6 GW even though

432-405: The fabled Strait of Anián . Barkley was the first recorded person to find the strait, unless Juan de Fuca's story was true. The strait was explored in detail between 1789 and 1791 by Manuel Quimper , José María Narváez , Juan Carrasco , Gonzalo López de Haro , and Francisco de Eliza . The United States Geological Survey defines the Strait of Juan de Fuca as a channel . It extends east from

456-475: The formal definition of strait, they are not usually referred to as such. Rivers and often canals, generally have a directional flow tied to changes in elevation, whereas straits often are free flowing in either direction or switch direction, maintaining the same elevation. The term strait is typically reserved for much larger, wider features of the marine environment. There are exceptions, with straits being called canals; Pearse Canal , for example. Straits are

480-581: The more protected waters inland, thereby resulting in a number of small-craft advisories , gale warnings , and storm warnings . An international vehicle ferry, the MV ; Coho , crosses the Strait from Port Angeles, Washington , to Victoria, British Columbia , several times each day. It began operating in 1959, replacing an earlier ferry, and remains privately owned; the Coho carried 475,000 passengers and 130,000 vehicles in 2018. A passenger-only ferry on

504-708: The same route, named the Victoria Express , operated from 1990 to 2011. Victoria is also the terminus of the Victoria Clipper , a passenger-only ferry from Seattle . Sidney, located northeast of Victoria, is served by a seasonal extension the Washington State Ferries system's route serving the San Juan Islands and Anacortes, Washington . This strait remains the subject of a maritime boundary dispute between Canada and

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528-484: The sheltered bays of the Strait of Juan de Fuca to feed on herring and other small fish. Humpback whales can be observed near the western end of the Strait of Juan de Fuca, mostly from June to November, especially in areas near Neah Bay and La Push . There is a resident (non-nomadic) population of killer whale in the Strait and surrounding waters, where they feed on spawning Chinook salmon . The migrating, so-called "transient" populations of killer whale often prey on

552-499: The strait the " Salish Sea ", an idea that reportedly met with approval by British Columbia's Aboriginal Relations Minister Mike de Jong , who pledged to put it before the BC cabinet for discussion. Making Salish Sea official required a formal application to the Geographical Names Board of Canada . A parallel American movement promoting the name had a different definition, combining of the Strait of Juan de Fuca and Puget Sound as well as

576-477: The total energy available in the flow is 15 GW. Straits used for international navigation through the territorial sea between one part of the high seas or an exclusive economic zone and another part of the high seas or an exclusive economic zone are subject to the legal regime of transit passage ( Strait of Gibraltar , Dover Strait , Strait of Hormuz ). The regime of innocent passage applies in straits used for international navigation (1) that connect

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