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Stykkið
Stykkið ( da, Stykket) is a village on the west coast of the Faroese island Streymoy in Kvívík Municipality. The 2005 population was 42. Its postal code is FO 330. Stykkið was founded in 1845. 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 ... External linksDanish site with photographs of Stykkið Populated places in the Faroe Islands {{faroes-geo-stub ... [...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] |
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 ... [...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] |
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