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Strendur
Strendur ( da, Strænder) is a village on the Faroese island of Eysturoy, located along the Skálafjørður fjord. It is the seat and main settlement of the Sjóvar Municipality. The 2012 population was 785. Its postal code is FO 490. ''Strendur'' means ''beaches'' or ''strands'' in the Faroese language. The village is connected by road to Selatrað, Skáli and the rest of Eysturoy, and via the Eysturoyartunnilin to Runavík and Tórshavn. References External linksDanish site with photographs of Strendur See also * List of towns in the Faroe Islands This is a list of villages (and towns) of the Faroe Islands. :fo:Býir í Føroyum :de:Liste der Städte und Orte auf den Färöern References {{DEFAULTSORT:List Of Towns In The Faroe Islands Towns Faroe Islands The Faroe Isl ... Populated places in the Faroe Islands {{faroes-geo-stub ...
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Eysturoyartunnilin
The Eysturoyartunnilin (in English the Eysturoy Tunnel, earlier known as the Skálafjarðartunnilin) is a large undersea road tunnel under the Tangafjørður sound in the Faroe Islands, connecting the island of Streymoy to the island of Eysturoy. It also crosses the southern part of Skálafjørður, and connects the towns of Runavík on the eastern side and Strendur on the western side of the fjord, and includes the world's first undersea roundabout in the middle of the network. It is the largest ever infrastructure project in the Faroe Islands. Altogether, the three-branch sub-sea tunnel measures long, including the roundabout. Construction costs are estimated to be around a billion DKK. /sup> The roundabout features artwork, including large sculptures and light effects. The tunnel opened for traffic on 19 December 2020. History The idea for the Eysturoyartunnilin emerged during the construction of the Vágatunnilin and Norðoyatunnilin, opened in 2002 and 2006 respectiv ...
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Eysturoy
Eysturoy (pronounced estroimeaning 'East Island') is a region and the second-largest of the Faroe Islands, both in size and population. Description Eysturoy is separated by a narrow sound from the main island of Streymoy. Eysturoy is extremely rugged, with some 66 separate mountain peaks, including Slættaratindur, the highest peak in the archipelago at . The country's two longest fjords, Skálafjørður in the south and Funningsfjørður in the north, almost split the island in two halves. The isthmus in between, Millum Fjarða, is one of the flattest areas in the country. Important settlements on Eysturoy are Fuglafjørður in the north and the densely populated area of the municipalities of Runavík and Nes in the south. Eysturoy is connected with Streymoy by the Streymin Bridge over the Sundini. Leirvík on the east coast of the island is the gateway for transport connections to the north-eastern islands, particularly Klaksvík on the island of Borðoy, which is the Faroes' ...
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Sjóvar Municipality
Sjóvar Municipality ( Faroese: ''Sjóvar kommuna'') is a municipality of the Faroe Islands. The name of the municipality has its origins from the farm ''Sjógv á Strondum'' which gave name to Sjóvar parish. The name comes from the Faroese word for ''seawater'' (''sjógvur''). Sjóvar covers a part of the island of Eysturoy. It consists of the villages of Strendur, Innan Glyvur, Selatrað, Morskranes Morskranes ( da, Morskrenæs) is a village on the west coast of the Faroese island of Eysturoy in the Sjóvar Municipality. The 2013 population was 28. Its postal code is FO 496. Morskranes can translate roughly as "Moors of the Corner". Externa ... and Kolbanargjógv. References External linksOfficial website Municipalities of the Faroe Islands Eysturoy {{Faroes-geo-stub ...
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List Of Towns In The Faroe Islands
This is a list of villages (and towns) of the Faroe Islands. :fo:Býir í Føroyum :de:Liste der Städte und Orte auf den Färöern References {{DEFAULTSORT:List Of Towns In The Faroe Islands Towns Faroe Islands The Faroe Islands ( ), or simply the Faroes ( fo, Føroyar ; da, Færøerne ), are a North Atlantic island group and an autonomous territory of the Kingdom of Denmark. They are located north-northwest of Scotland, and about halfway bet ...
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Greenwich Mean Time
Greenwich Mean Time (GMT) is the Local mean time, mean solar time at the Royal Observatory, Greenwich, Royal Observatory in Greenwich, London, counted from midnight. At different times in the past, it has been calculated in different ways, including being calculated from noon; as a consequence, it cannot be used to specify a particular time unless a context is given. The term 'GMT' is also used as Western European Time, one of the names for the time zone UTC+00:00 and, in UK law, is the basis for civil time in the United Kingdom. English speakers often use GMT as a synonym for Coordinated Universal Time (UTC). For navigation, it is considered equivalent to UT1 (the modern form of mean solar time at 0° longitude); but this meaning can differ from UTC by up to 0.9s. The term GMT should thus not be used for purposes that require precision. Because of Earth's uneven angular velocity in its elliptical orbit and its axial tilt, noon (12:00:00) GMT is rarely the exact moment the S ...
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European Summer Time
Summer time in Europe is the variation of standard clock time that is applied in most European countries (apart from Iceland, Belarus, Turkey and Russia) in the period between spring and autumn, during which clocks are advanced by one hour from the time observed in the rest of the year, with a view to making the most efficient use of seasonal daylight. It corresponds to the notion and practice of daylight saving time (DST) to be found in many other parts of the world. In all locations in Europe where summer time is observed (the EU, EFTA and associated countries), European Summer Time begins at 01:00 UTC/Western European Time, WET (02:00 Central European Time, CET, 03:00 Eastern European Time, EET) on the last Sunday in March and ends at 01:00 UTC (02:00 Western European Summer Time, WEST, 03:00 Central European Summer Time, CEST, 04:00 Eastern European Summer Time, EEST) on the last Sunday in October each year; i.e. the change is made at the same absolute time across all time zone ...
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Köppen Climate Classification
The Köppen climate classification is one of the most widely used climate classification systems. It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, with several later modifications by Köppen, notably in 1918 and 1936. Later, the climatologist Rudolf Geiger (1894–1981) introduced some changes to the classification system, which is thus sometimes called the Köppen–Geiger climate classification system. The Köppen climate classification divides climates into five main climate groups, with each group being divided based on seasonal precipitation and temperature patterns. The five main groups are ''A'' (tropical), ''B'' (arid), ''C'' (temperate), ''D'' (continental), and ''E'' (polar). Each group and subgroup is represented by a letter. All climates are assigned a main group (the first letter). All climates except for those in the ''E'' group are assigned a seasonal precipitation subgroup (the second letter). For example, ''Af'' indi ...
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Oceanic Climate
An oceanic climate, also known as a marine climate, is the humid temperate climate sub-type in Köppen classification ''Cfb'', typical of west coasts in higher middle latitudes of continents, generally featuring cool summers and mild winters (for their latitude), with a relatively narrow annual temperature range and few extremes of temperature. Oceanic climates can be found in both hemispheres generally between 45 and 63 latitude, most notably in northwestern Europe, northwestern America, as well as New Zealand. Precipitation Locations with oceanic climates tend to feature frequent cloudy conditions with precipitation, low hanging clouds, and frequent fronts and storms. Thunderstorms are normally few, since strong daytime heating and hot and cold air masses meet infrequently in the region. In most areas with an oceanic climate, precipitation comes in the form of rain for the majority of the year. However, some areas with this climate see some snowfall annually during winter. M ...
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Faroe Islands
The Faroe Islands ( ), or simply the Faroes ( fo, Føroyar ; da, Færøerne ), are a North Atlantic island group and an autonomous territory of the Kingdom of Denmark. They are located north-northwest of Scotland, and about halfway between Norway ( away) and Iceland ( away). The islands form part of the Kingdom of Denmark, along with mainland Denmark and Greenland. The islands have a total area of about with a population of 54,000 as of June 2022. The terrain is rugged, and the subpolar oceanic climate (Cfc) is windy, wet, cloudy, and cool. Temperatures for such a northerly climate are moderated by the Gulf Stream, averaging above freezing throughout the year, and hovering around in summer and 5 °C (41 °F) in winter. The northerly latitude also results in perpetual civil twilight during summer nights and very short winter days. Between 1035 and 1814, the Faroe Islands were part of the Kingdom of Norway, which was in a personal union with Denmark from 1 ...
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Fjord
In physical geography, a fjord or fiord () is a long, narrow inlet with steep sides or cliffs, created by a glacier. Fjords exist on the coasts of Alaska, Antarctica, British Columbia, Chile, Denmark, Germany, Greenland, the Faroe Islands, Iceland, Ireland, Kamchatka, the Kerguelen Islands, Labrador, Newfoundland, New Zealand, Norway, Novaya Zemlya, Nunavut, Quebec, the Patagonia region of Argentina and Chile, Russia, South Georgia Island, Tasmania, United Kingdom, and Washington state. Norway's coastline is estimated to be long with its nearly 1,200 fjords, but only long excluding the fjords. Formation A true fjord is formed when a glacier cuts a U-shaped valley by ice segregation and abrasion of the surrounding bedrock. According to the standard model, glaciers formed in pre-glacial valleys with a gently sloping valley floor. The work of the glacier then left an overdeepened U-shaped valley that ends abruptly at a valley or trough end. Such valleys are fjords wh ...
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Faroese Language
Faroese ( ; ''føroyskt mál'' ) is a North Germanic language spoken as a first language by about 72,000 Faroe Islanders, around 53,000 of whom reside on the Faroe Islands and 23,000 in other areas, mainly Denmark. It is one of five languages descended from Old West Norse spoken in the Middle Ages, the others being Norwegian, Icelandic, and the extinct Norn and Greenlandic Norse. Faroese and Icelandic, its closest extant relative, are not mutually intelligible in speech, but the written languages resemble each other quite closely, largely owing to Faroese's etymological orthography. History Around 900 AD, the language spoken in the Faroes was Old Norse, which Norse settlers had brought with them during the time of the settlement of Faroe Islands () that began in 825. However, many of the settlers were not from Scandinavia, but descendants of Norse settlers in the Irish Sea region. In addition, women from Norse Ireland, Orkney, or Shetland often married native Scandinavian m ...
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Selatrað
Selatrað ( da, Selletræ) is a village on the west coast of the Faroese island of Eysturoy in Sjóvar Municipality. The name ''Selatrað'' refers to ''a breeding place for seals''. The 2010 population was 38. Its postal code is FO 497. The village's church, the first in the archipelago made from concrete, was built in 1927. The third biggest plantation in the Faroe Islands is in Selatrað. It was severely damaged in a hurricane in 1988, destroying 2/3 of it. However the biggest trees (20m in height) survived. Selatrað was once the parliamentary meeting place for the whole of Eysturoy. References External linksDanish site with photographs of Selatrað See also * List of towns in the Faroe Islands This is a list of villages (and towns) of the Faroe Islands. :fo:Býir í Føroyum :de:Liste der Städte und Orte auf den Färöern References {{DEFAULTSORT:List Of Towns In The Faroe Islands Towns Faroe Islands The Faroe Isl ... Populated places in the ...
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