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West Norwegian Fjords
The West Norwegian Fjords is the common name of two fjords in Norway listed as a World Heritage Site by UNESCO: the Geirangerfjord and the Nærøyfjord. Geography Location The World Heritage Site consists of two areas 120 km apart, located in south-west Norway, north-west of the city of Bergen, and part of the fjord landscape of western Norway extending over 500 km between Stavanger in the south and Åndalsnes in the north... The areas of Geirangerfjord and Nærøyfjordtotal 122 712 hectares (111 966 ha terrestrial and 10 746 ha marine). The Geirangerfjord area is situated 60 km inland and constitutes the Geirangerfjord itself as the upper end of Storfjorden as well as Tafjorden.. The heritage cite lies in the county of Møre og Romsdal, extending into the municipalities of Fjord and Stranda. It covers 51 802 ha, of which 46 151 ha are terrestrial and 5 651 ha are marine. The Nærøyfjord is situated 100 km inland and is the u ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
World Heritage Site
A World Heritage Site is a landmark or area with legal protection by an international convention administered by the United Nations Educational, Scientific and Cultural Organization (UNESCO). World Heritage Sites are designated by UNESCO for having cultural, historical, scientific or other form of significance. The sites are judged to contain " cultural and natural heritage around the world considered to be of outstanding value to humanity". To be selected, a World Heritage Site must be a somehow unique landmark which is geographically and historically identifiable and has special cultural or physical significance. For example, World Heritage Sites might be ancient ruins or historical structures, buildings, cities, deserts, forests, islands, lakes, monuments, mountains, or wilderness areas. A World Heritage Site may signify a remarkable accomplishment of humanity, and serve as evidence of our intellectual history on the planet, or it might be a place of great natural beauty. A ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sogn Og Fjordane
Sogn og Fjordane (; English: "Sogn and Fjordane") was, up to 1 January 2020, a county in western Norway, when it was merged to become part of Vestland county. Bordering previous counties Møre og Romsdal, Oppland, Buskerud, and Hordaland, the county administration was in the village of Hermansverk in Leikanger municipality. The largest town in the county was Førde. Although Sogn og Fjordane has some industry, predominantly hydroelectricity and aluminium, it is predominantly an agricultural area. Sogn og Fjordane is also home to the Urnes Stave Church and the Nærøyfjord, which are both listed by UNESCO as World Heritage Sites. The Western Norway University of Applied Sciences has campuses in Sogndal and Førde. Name The name ''Sogn og Fjordane'' was created in 1919; a literal translation is: ''Sogn and the fjords.'' The first element is the name of the region of Sogn, located in the southern part of the county. The last element is the plural definite form of ''fjord'', which ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
World Heritage Centre
UNESCO Headquarters, or Maison de l'UNESCO, is a building inaugurated on 3 November 1958 at number 7 Place de Fontenoy in Paris, France, to serve as the headquarters for the United Nations Educational, Scientific and Cultural Organization (UNESCO). It is a building that can be visited freely. Design The design of the UNESCO Headquarters building was the combined work of three architects: Bernard Zehrfuss (France), Marcel Breuer (Hungary), and Pier Luigi Nervi (Italy). Plans were also validated by an international committee of five architects composed of Lucio Costa (Brazil), Walter Gropius (Germany/United States), Le Corbusier (France), Sven Markelius (Sweden) and Ernesto Nathan Rogers (Italy), with the collaboration of Eero Saarinen (Finland). Description The main building, which houses the secretariat, consists of seven floors forming a three-pointed star. To this is added a building called the "accordion" and a cubic building, which is intended for permanent delegations and non ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Valley
A valley is an elongated low area often running between Hill, hills or Mountain, mountains, which will typically contain a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacier, glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these glaciation, glacially formed valleys may have been created or enlarged during ice ages but now are ice-free and occupied by streams or rivers. In desert areas, valleys may be entirely dry or carry a watercourse only rarely. In karst, areas of limestone bedrock, dry valleys may also result from drainage now taking place cave, underground rather than at the surface. Rift valleys arise principally from tectonics, earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited Summit (topography), summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are Monadnock, isolated summits, but most occur in mountain ranges. Mountain formation, Mountains are formed through Tectonic plate, tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through Slump (geology), slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce Alpine climate, colder climates than at sea level at similar latitude. These colder climates strongly affect the Montane ecosystems, ecosys ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Microclimate
A microclimate (or micro-climate) is a local set of atmospheric conditions that differ from those in the surrounding areas, often with a slight difference but sometimes with a substantial one. The term may refer to areas as small as a few square meters or square feet (for example a garden bed or a cave) or as large as many square kilometers or square miles. Because climate is statistical, which implies spatial and temporal variation of the mean values of the describing parameters, within a region there can occur and persist over time sets of statistically distinct conditions, that is, microclimates. Microclimates can be found in most places but are most pronounced in topographically dynamic zones such as mountainous areas, islands, coastal areas. Microclimates exist, for example, near bodies of water which may cool the local atmosphere, or in heavy urban areas where brick, concrete, and asphalt absorb the sun's energy, heat up, and re-radiate that heat to the ambient air: t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Continental Climate
Continental climates often have a significant annual variation in temperature (warm summers and cold winters). They tend to occur in the middle latitudes (40 to 55 north), within large landmasses where prevailing winds blow overland bringing some precipitation, and temperatures are not moderated by oceans. Continental climates occur mostly in the Northern Hemisphere due to the large landmasses found there. Most of northern and northeastern China, eastern and southeastern Europe, Western and north western Iran, central and southeastern Canada, and the central and northeastern United States have this type of climate. Continentality is a measure of the degree to which a region experiences this type of climate. In continental climates, precipitation tends to be moderate in amount, concentrated mostly in the warmer months. Only a few areas—in the mountains of the Pacific Northwest of North America and in Iran, northern Iraq, adjacent Turkey, Afghanistan, Pakistan, and Central Asia†... [...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] |
European Route E16
European route E16 is the designation of a main west-east road through Northern Ireland, Scotland, Norway and Sweden, from Derry to Gävle, via Belfast, Glasgow, Edinburgh, previously by ferry to Bergen, Voss, through the Gudvanga Tunnel and the Lærdal Tunnel (the world's longest road tunnel), Lærdal, over Filefjell to Fagernes, Hønefoss, Gardermoen and Kongsvinger. In Sweden, it passes Malung, Falun and ends in Gävle. United Kingdom *Northern Ireland **: Derry - **: - Antrim **: Antrim - Belfast (Multiplex with and between and Belfast) *Great Britain **: Glasgow (Interchange with at ) - Edinburgh (Interchange with at ) In Northern Ireland, it follows the A6 from Derry to Randalstown, then the M22 and M2 to Belfast. In Scotland it follows the M8 from Glasgow to Edinburgh. E16 meets the E1 and E18 in Belfast, the E5 in Glasgow, the E15 in Edinburgh. European routes are not signposted in the UK. There is no ferry anymore between the United Kingdom and Norw ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Voss
Voss () is a municipality and a traditional district in Vestland county, Norway. The administrative center of the municipality is the village of Vossevangen. Other villages include Bolstadøyri, Borstrondi, Evanger, Kvitheim, Mjølfjell, Oppheim, Stalheim, and Vinje. The municipality is the 35th largest by area of Norway's 356 municipalities. Voss is Norway's 77th most populous municipality, with a population of 15,875. Its population density is and its population has increased by 6.5% over the last 10 years. Municipal history The parish of Voss was established as a municipality on 1 January 1838 (see formannskapsdistrikt law). On 1 January 1867, a small area in northern Voss (population 28) was transferred to the municipality of Hosanger. On 1 January 1868, the municipality's northern district (population 2,009) was separated to form the new municipality of Vossestrand. This left 7,592 residents in Voss. On 21 August 1868, an unpopulated area of northern Voss was transfe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hordaland
Hordaland () was a county in Norway, bordering Sogn og Fjordane, Buskerud, Telemark, and Rogaland counties. Hordaland was the third largest county, after Akershus and Oslo, by population. The county government was the Hordaland County Municipality, which is located in Bergen. Before 1972, the city of Bergen was its own separate county, apart from Hordaland. On 1 January 2020, the county was merged with neighbouring Sogn og Fjordane county, to form the new Vestland county. Name and symbols Name Hordaland (Old Norse: ''Hǫrðaland'') is the old name of the region which was revived in 1919. The first element is the plural genitive case of ''hǫrðar'', the name of an old Germanic tribe (see Charudes). The last element is ''land'' which means "land" or "region" in the Norwegian language. Until 1919 the name of the county was ''Søndre Bergenhus amt'' which meant "(the) southern (part of) Bergenhus amt". (The old ''Bergenhus amt'' was created in 1662 and was divided into North ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lærdal
Lærdal is a municipality in Vestland county, Norway. It is located on the south side of the Sognefjorden in the traditional district of Sogn. The administrative center of the municipality is the village of Lærdalsøyri. The old Filefjell Kongevegen road passes through Lærdal on its way to Valdres and later to Oslo. The municipality is the 71st largest by area out of the 356 municipalities in Norway (with over half of this area consisting of mountains). Lærdal is the 274th most populous municipality in Norway with a population of 2,117. The municipality's population density is and its population has decreased by 4% over the previous 10-year period. The Lærdal river valley is long, running from Hemsedal (Høgeloft mountain) and the Filefjell mountains in the east to the Sognefjorden in the west. About half of the municipal residents live in the main village of Lærdalsøyri; the rest in the small villages in the surrounding valleys such as Borgund, Ljøsne, Tønjum, Erdal ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
