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Múli
Múli (pronounced ; da, Mule) is a hamlet on the Island of Borðoy in the Norðoyar Region of the Faroes. Múli lies on the outermost northern edge of Borðoy's east coast. The origins of the settlement can be traced back to the 14th century. Múli became the last community in the archipelago to receive electricity in 1970. It was later connected with Norðdepil by Road 743 in an attempt to stop depopulation. Nevertheless, Múli has been considered abandoned since 2002, though there are still four registered residents. During the summer months, some of its former residents use their old houses as vacation homes. Nature The mountains around Múli are spectacular and do not offer any easy climbing. They are also the last stronghold of a contiguous population of Arctic Willow in the Faroe Islands. History The oldest record of Múli is to be found in the so-called ‘Hundabrævið’, the '' Dog letter'', a letter concerning the keeping of sheep dogs in the Faroe Islands in the 1 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Borðoy
Borðoy ( da, Bordø) is an island in the north-east of the Faroe Islands. Its name means 'headland island'. There are eight settlements: Klaksvík (the second largest town in the Faroes), Norðoyri, Ánir, Árnafjørður, Strond, Norðtoftir, Depil and Norðdepil. History There are also three abandoned settlements: Skálatoftir, Múli and Fossá, all in the north. Múli was one of the remotest settlements in the Faroes – there was no road link until 1989, before which goods had to be brought in via helicopter or boat. The last people left in 1994. A Klaksvík museum bought the Fossá area in 1969 with the plan of turning it into a typical Faroese Medieval village, though the plan never came to fruition. Important Bird Area The northern and south-eastern headlands of the island have been identified as an Important Bird Area by BirdLife International because of their significance as a breeding site for seabirds, especially European storm petrel The European storm pet ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Norðdepil
Norðdepil (pronounced ; da, Norddeble) is a town on the east coast of the island of Borðoy in the Norðoyar Region of the Faroe Islands. History Norðdepil was founded in 1866. Its school opened in 1895. On 18 August 1941, around noon, a German Junkers Ju 88 bomber crashed in heavy fog into the mountainside above the village. Norðdepil has been connected with the town of Hvannasund on Viðoy to the east by a causeway with a road on top since 1963. Because the two communities are located directly across from each other on opposite shores, they often act as one community. Since 1967, two single-lane tunnels have connected Norðdepil with the regional city of Klaksvík. Immediately bordering Norðdepil to its north is the abandoned settlement of Fossá, of which nothing remains. Fossá was named after some waterfalls. Further north on the east coast of Borðoy there is a road going from Norðdepil to the abandoned hamlet of Múli. Whaling station In 1897 the whaling stat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hvannasund
Hvannasund ( da, Kvannesund, older spelling: ''Quannesund'') is a village and municipality in the Faroe Islands, an autonomous region in Denmark. Hvannasund is located on the west coast of the island of Viðoy. It faces Norðdepil on Borðoy. The villages are connected to each other by a causeway. A large cracked rock rests in an area just north of Hvannasund. An old legend details that the rock, called Skrudhettan, broke the very moment that Jesus was born. On 26 May 2008, the ocean inexplicably receded 2½ – 3 metres before suddenly hitting the area with great strength. A couple of days later, it was reported that a mini-tsunami had hit Hvannasund. There were no injuries or fatalities. On 3 September 2008, a majority of the town council, notably excluding the mayor, announced that there would be a referendum on merging Hvannasund municipality with Klaksvík, the municipality of Klaksvík. The referendum was held on 17 September. Of the 321 eligible, 278 cast their vote ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Norðoyar
The six islands in the northeast of the Faroe Islands are together referred to as Norðoyar, i.e. the Northern Isles ( da, Norderøerne). These Islands from west to east are Kalsoy, Kunoy, Borðoy, Viðoy, Svínoy and Fugloy. Klaksvík Klaksvík is the second largest town of the Faroe Islands behind Tórshavn. The town is located on Borðoy, which is one of the northernmost islands (the Norðoyar). It is the administrative centre of Klaksvík municipality. History The first s ... is the biggest settlement of the region. Norðoyar is sometimes spelled Norðoyggjar. In the 1946 independence referendum, 67.3% of Norðoyar voters chose independence, the highest proportion out of any Faroese region. Direct Democracy Further reading * Christiansen, Hans ...[...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Faroes
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 13 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Municipalities Of The Faroe Islands
The Faroe Islands are administratively divided in 29 municipalities (''kommunur''), with about 120 cities and villages. Until December 31, 2008, there were 34 municipalities, and until December 31, 2004, there were 48 municipalities. In the coming years the number of Faroese municipalities is expected to drop to somewhere between 7 and 15, as there is currently a rationale towards municipal amalgamation and a decentralization of public services. In 1998 it was suggested that no municipality should have fewer than 2,000 inhabitants, but whether this will be true is a political question. The Faroese government has furthermore decided not to conduct forced, top-down amalgamation, but to leave the process to the free will of the municipalities. In many small municipalities there is some resistance to the amalgamation process, and as a result two kinds of municipalities are being created: large municipalities (town-municipalities) that are eager to attract smaller municipalities into ama ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Arctic Willow
''Salix arctica'', the Arctic willow, is a tiny creeping willow (family Salicaceae). It is adapted to survive in Arctic conditions, specifically tundras. Description ''S. arctica'' is typically a low shrub growing to only in height, rarely to , although it may reach in height in the Pacific Northwest. It has round, shiny green leaves long and broad; they are pubescent, with long, silky, silvery hairs. Like the rest of the willows, Arctic willow is dioecious, with male and female catkins on separate plants. As a result, the plant's appearance varies; the female catkins are red-coloured, while the male catkins are yellow-coloured.Jepson Flora''Salix arctica''/ref> Despite its small size, it is a long-lived plant, growing extremely slowly in the severe arctic climate; one in eastern Greenland was found to be 236 years old. Hybrids with '' Salix arcticola'' and ''Salix glauca'' are known. Distribution and habitat The Arctic willow grows in tundra and rocky moorland, and is th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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