Tjørnuvík
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Tjørnuvík
Tjørnuvík ( da, Tjørnevig) is the northernmost village on Streymoy in Sunda Municipality, Faroe Islands. As of the 2006 census, the population has a total of 71 people. The town uses the Stakkur sea stack for sheep grazing, accessed by cable car. The Risin og Kellingin sea stacks are visible across the Sundini strait. A 5 km single-lane dead-end road (route 594) from Haldórsvík Haldórsvík ( da, Haldersvig), also Haldarsvík, is a village located on the north-east coast of Streymoy in the Sunda Kommuna municipality. In the centre of the village there is a small waterfall. The stone church in the village is from 185 ... is the only way to reach Tjørnuvík. Tourists clogged the road in summer, before a traffic control system improved conditions in 2022. Gallery File:Tjørnuvík, Faroe Islands.JPG File:Is03080-Tjornuvik.jpg File:Is03073-Tjornuvik.jpg File:Gongutúrur yvir Tjørnuvík (2).jpg See also * Towns of the Faroe Islands References External linksP ...
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Sunda, Faroe Islands
Sunda is a municipality in the Faroe Islands, loosely centered around the Sundini sound between the islands of Streymoy and Eysturoy. History Sunda is an amalgamation of the former municipalities of Hósvíkar, Hvalvíkar, Saksunar, Haldarsvíkar, (former) Sunda and Gjáar kommuna, which merged in 2005. The mayor as of 2020 is Heðin Zachariasen, who was also the first mayor, from 2005 to 2009. Geography The region in which Sunda kommuna is situated is referred to as Sundalagið, centered around the Sundini (''The Narrows'') between the islands of Streymoy and Eysturoy. The region also includes Eiðis kommuna, while strictly speaking Gjógv does not belong to Sundalagið, though is part of Sunda kommuna. The villages Selatrað, Morskranes and Kolbeinagjógv are also situated on the Sundini but not considered part of Sundalagið region. Sunda kommuna contains the following villages: *Hósvík *Norðskáli *Hvalvík * Streymnes *Haldórsvík *Oyri *Oyrarbakki *Tjørnuvík *Gjógv ...
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Sundini
280px, The Streymin Bridge crosses the Sundini at its narrowest point Sundini is the northern section of the sound separating the islands of Streymoy and Eysturoy in the Faroe Islands. The southern section of the strait is named Tangafjørður. Name ''Sund'' is the Faroese word for ''sound'' or ''strait''. Sundini is the plural definite of ''Sund'', hence translating as ''The Sounds'' or ''The Straits'' in English. An alternative suggested translation would be ''The Narrows''. Geography The Sundini separates Streymoy and northern Eysturoy. In the north, bordering Eiðisflógvi gulf (part of the Atlantic Ocean), Sundini starts between Tjørnuvík and Eiðiskollur (near Eiði). It merges with the much wider Tangafjørður strait between Norðuri í Sundum ( Kollafjørdur) and Morskranes. Its length is in an equidistant line. The deepest point is northwest of Morskranes at . Sundini is at its widest around Selatrað at . The shallowest and narrowest point is situated at Við Str ...
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Streymoy
Streymoy ( da, Strømø) is the largest and most populated island of the Faroe Islands. The capital, Tórshavn, is located on its southeast coast. The name means "island of currents". It also refers to the largest region of the country that also includes the islands of Hestur, Koltur and Nólsoy. Geography The island is oblong in shape and stretches roughly in northwest–southeast direction with a length of and a width of around . There are two deeply-indented fjords in the southeast: Kollafjørður and Kaldbaksfjørður. The island is mountainous (average height is 337 meter ), especially in the northwest, with the highest peak being Kopsenni (). That area is dominated by over cliffs. The area is known as Vestmannabjørgini, which means Cliffs of Vestmanna. The beaches of Tórshavn, Vestmanna, Leynar, Kollafjørður, Hvalvík (meaning Whale Bay) and Tjørnuvík are officially approved ''grind'' beaches for whaling. Like the rest of the Faroe Islands there are numerous shor ...
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Stakkurin
Stakkurin is the sea stack at the northernmost point of the island of Streymoy in the Faroe Islands. The owners of Stakkurin have sheep farming Sheep farming or sheep husbandry is the raising and breeding of domestic sheep. It is a branch of animal husbandry. Sheep are raised principally for their meat (lamb and mutton), milk (sheep's milk), and fiber (wool). They also yield sheepskin an ... on top of the sea stack, and once a year they go out and bring back the sheep and sell them at an auction in the village Tjörnuvík. The money from auction goes to benefit the whole community, such as the community house. The sea stack can be reached by a cable from Streymoy. References {{coord missing, Denmark Streymoy Stacks of the Faroe Islands ...
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Risin Og Kellingin
Risin og Kellingin (Risin and Kellingin) are two sea stacks just off the northern coast of the island of 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 ... in the Faroe Islands close to the town of Eiði. The name ''Risin og Kellingin'' means ''The Giant and the Witch'' (or ''Hag'') and relates to an old legend about their origins. The Giant (Risin) is the 71m stack further from the coast, and the witch (Kellingin) is the 68m pointed stack nearer land, standing with her legs apart. Legend of the Giant and the Witch A legend tells how, once upon a time, the giants in Iceland were envious and decided that they wanted the Faroes. So the giant and the witch (his wife in some versions of the story) were sent down to the Faroe Islands to bring them back. They reached the north- ...
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Towns Of 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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Tundra
In physical geography, tundra () is a type of biome where tree growth is hindered by frigid temperatures and short growing seasons. The term ''tundra'' comes through Russian (') from the Kildin Sámi word (') meaning "uplands", "treeless mountain tract". There are three regions and associated types of tundra: Arctic tundra, alpine tundra, and Antarctic tundra. Tundra vegetation is composed of dwarf shrubs, sedges, grasses, mosses, and lichens. Scattered trees grow in some tundra regions. The ecotone (or ecological boundary region) between the tundra and the forest is known as the tree line or timberline. The tundra soil is rich in nitrogen and phosphorus. The soil also contains large amounts of biomass and decomposed biomass that has been stored as methane and carbon dioxide in the permafrost, making the tundra soil a carbon sink. As global warming heats the ecosystem and causes soil thawing, the permafrost carbon cycle accelerates and releases much of these soil-contained g ...
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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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Stack (geology)
A stack or sea stack is a geological landform consisting of a steep and often vertical column or columns of rock in the sea near a coast, formed by wave erosion. Stacks are formed over time by wind and water, processes of coastal geomorphology."Sea stacks"
britannica.com They are formed when part of a headland is by , which is the force of the sea or water crashing against the rock. The force of the water weakens cracks in the headland, causing them to later collapse, formi ...
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