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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". External links Personal Danish site with photographs of Morskranes 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 Isla ... Populated places in the Faroe Islands {{faroes-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...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] |
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' ... [...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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