1.
Norway
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The Antarctic Peter I Island and the sub-Antarctic Bouvet Island are dependent territories and thus not considered part of the Kingdom. Norway also lays claim to a section of Antarctica known as Queen Maud Land, until 1814, the kingdom included the Faroe Islands, Greenland, and Iceland. It also included Isle of Man until 1266, Shetland and Orkney until 1468, Norway has a total area of 385,252 square kilometres and a population of 5,258,317. The country shares a long border with Sweden. Norway is bordered by Finland and Russia to the north-east, Norway has an extensive coastline, facing the North Atlantic Ocean and the Barents Sea. King Harald V of the Dano-German House of Glücksburg is the current King of Norway, erna Solberg became Prime Minister in 2013, replacing Jens Stoltenberg. A constitutional monarchy, Norway divides state power between the Parliament, the Cabinet and the Supreme Court, as determined by the 1814 Constitution, the kingdom is established as a merger of several petty kingdoms. By the traditional count from the year 872, the kingdom has existed continuously for 1,144 years, Norway has both administrative and political subdivisions on two levels, counties and municipalities. The Sámi people have an amount of self-determination and influence over traditional territories through the Sámi Parliament. Norway maintains close ties with the European Union and the United States, the country maintains a combination of market economy and a Nordic welfare model with universal health care and a comprehensive social security system. Norway has extensive reserves of petroleum, natural gas, minerals, lumber, seafood, the petroleum industry accounts for around a quarter of the countrys gross domestic product. On a per-capita basis, Norway is the worlds largest producer of oil, the country has the fourth-highest per capita income in the world on the World Bank and IMF lists. On the CIAs GDP per capita list which includes territories and some regions, from 2001 to 2006, and then again from 2009 to 2017, Norway had the highest Human Development Index ranking in the world. It also has the highest inequality-adjusted ranking, Norway ranks first on the World Happiness Report, the OECD Better Life Index, the Index of Public Integrity and the Democracy Index. Norway has two names, Noreg in Nynorsk and Norge in Bokmål. The name Norway comes from the Old English word Norðrveg mentioned in 880, meaning way or way leading to the north. In contrasting with suðrvegar southern way for Germany, and austrvegr eastern way for the Baltic, the Anglo-Saxon of Britain also referred to the kingdom of Norway in 880 as Norðmanna land. This was the area of Harald Fairhair, the first king of Norway, and because of him
2.
Fosen
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Fosen is a traditional district in Trøndelag, consisting of the municipalities Osen, Roan, Åfjord, Bjugn, Ørland, Rissa, Agdenes, Snillfjord, Hemne, Hitra and Frøya. The district is dominated by forested valleys, lakes, coastal cliffs but also shallow areas, the western coast has many skerries and some islands, such as Stokkøya in Åfjord. There are some good salmon rivers, and sea eagles and other sea birds are common along the coast. The west coast has mild winters, and some locations receive on more than 2,000 mm of precipitation per year. Part of the Scandinavian coastal conifer forests are located on the peninsula, the largest nature reserve is Øyenskavelen, with many nature types including undisturbed forest, some of it classified as rainforest. Fosen also has a folkehøgskole, Fosen Folkehøgskole and it teaches unusual subjects such as sailing and building traditional Norwegian boats, organic agriculture, traditional Norwegian arts and crafts, nature life, etc. The district is named after the island Storfosna in Ørland, the Old Norse form of the name was Fólgsn
3.
Island
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An island or isle is any piece of sub-continental land that is surrounded by water. Very small islands such as emergent land features on atolls can be called islets, skerries, an island in a river or a lake island may be called an eyot or ait, and a small island off the coast may be called a holm. A grouping of geographically or geologically related islands is called an archipelago, an island may be described as such, despite the presence of an artificial land bridge. Example, Singapore and its causeway, or the various Dutch delta islands, there are two main types of islands in the sea, continental and oceanic. The word island derives from Middle English iland, from Old English igland, Old English ieg is actually a cognate of Swedish ö and German Aue, and related to Latin aqua. There is a difference between islands and continents in terms of geology, continents sit on continental lithosphere which is part of tectonic plates floating high on Earths mantle. Oceanic crust is also part of tectonic plates, but it is denser than continental lithosphere, Islands are either extensions of the oceanic crust or geologically they are part of some continent sitting on continental lithosphere. This holds true for Australia, which sits on its own continental lithosphere, continental islands are bodies of land that lie on the continental shelf of a continent. A special type of island is the microcontinental island, which is created when a continent is rifted. Examples are Madagascar and Socotra off Africa, the Kerguelen Islands, New Caledonia, New Zealand, another subtype is an island or bar formed by deposition of tiny rocks where water current loses some of its carrying capacity. While some are transitory and may disappear if the volume or speed of the current changes, others are stable, oceanic islands are islands that do not sit on continental shelves. The vast majority are volcanic in origin, such as Saint Helena in the South Atlantic Ocean, the few oceanic islands that are not volcanic are tectonic in origin and arise where plate movements have lifted up the ocean floor above the surface. Examples are Saint Peter and Paul Rocks in the Atlantic Ocean, one type of volcanic oceanic island is found in a volcanic island arc. These islands arise from volcanoes where the subduction of one plate under another is occurring, examples are the Aleutian Islands, the Mariana Islands, and most of Tonga in the Pacific Ocean. The only examples in the Atlantic Ocean are some of the Lesser Antilles, another type of volcanic oceanic island occurs where an oceanic rift reaches the surface. There are two examples, Iceland, which is the second largest volcanic island, and Jan Mayen. A third type of oceanic island is formed over volcanic hotspots. A hotspot is more or less stationary relative to the tectonic plate above it
4.
Red deer
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The red deer is one of the largest deer species. The red deer inhabits most of Europe, the Caucasus Mountains region, Asia Minor, Iran, parts of western Asia and it also inhabits the Atlas Mountains region between Morocco and Tunisia in northwestern Africa, being the only species of deer to inhabit Africa. Red deer have been introduced to areas, including Australia, New Zealand, United States, Canada, Peru, Uruguay, Chile. In many parts of the world, the meat from red deer is used as a food source, Red deer are ruminants, characterized by a four-chambered stomach. Genetic evidence indicates the red deer as traditionally defined is a group, rather than a single species. It is probable that the ancestor of all red deer, including wapiti, originated in central Asia, although at one time red deer were rare in parts of Europe, they were never close to extinction. The red deer is the fourth-largest deer species behind moose, elk and it is a ruminant, eating its food in two stages and having an even number of toes on each hoof, like camels, goats and cattle. European red deer have a long tail compared to their Asian. The deer of Central and Western Europe vary greatly in size, large red deer stags, like the Caspian red deer or those of the Carpathian Mountains, may rival the wapiti in size. Female red deer are smaller than their male counterparts. The male red deer is typically 175 to 250 cm long and weighs 160 to 240 kg, the tail adds another 12 to 19 cm and shoulder height is about 95 to 130 cm. In Scotland, stags average 201 cm in length and 122 cm high at the shoulder. Size varies in different subspecies with the largest, the huge but small-antlered deer of the Carpathian Mountains, weighing up to 500 kg. At the other end of the scale, the Corsican red deer weighs about 80 to 100 kg, European red deer tend to be reddish-brown in their summer coats. The males of many subspecies also grow a short neck mane during the autumn, the male deer of the British Isles and Norway tend to have the thickest and most noticeable manes. Male Caspian red deer and Spanish red deer do not carry neck manes, male deer of all subspecies, however, tend to have stronger and thicker neck muscles than female deer, which may give them an appearance of having neck manes. Red deer hinds do not have neck manes, the European red deer is adapted to a woodland environment. Only the stags have antlers, which growing in the spring and are shed each year
5.
Labour Party (Norway)
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The Labour Party, formerly the Norwegian Labour Party, is a social-democratic political party in Norway. It was formerly the senior partner of the governing Red-Green Coalition, the party is currently led by Jonas Gahr Støre. The Labour Party is officially committed to social-democratic ideals and its slogan since the 1930s has been everyone shall take part, and the party traditionally seeks a strong welfare state, funded through taxes and duties. During the first Stoltenberg government, the policies were inspired by Tony Blairs New Labour. The party has frequently described as increasingly neoliberal since the 1980s. The Labour Party profiles itself as a party that subscribes to cooperation on a national as well as international level. Its youth wing is the Workers Youth League, the party is a full member of the Party of European Socialists and Progressive Alliance, and is an observer member of the Socialist International. The Labour Party has always been a supporter of Norways NATO membership and has supported Norwegian membership in the European Union during two referendums. Founded in 1887, the party increased in support until it became the largest party in Norway in 1927. This year also saw the consolidation of surrounding the party during the 1920s following its membership in the Comintern from 1919 to 1923. It formed its first government in 1928, and has led the government for all but 16 years since 1935, from 1945 to 1961, the party had an absolute majority in the Norwegian parliament, the only time this has ever happened in Norwegian history. The domination by the Labour Party, during the 1960s and early 1970s, was broken by competition from the left. From the end of the 1970s however, the party started to lose voters to the right, in 2001 the party achieved its worst electoral results since 1924. Between 2005 and 2013, Labour returned to power after committing to an agreement with other parties in order to form a majority government. Since losing 9 seats in the 2013 election, Labour has been in opposition, the party was founded in 1887 in Arendal and first ran in elections to the Parliament of Norway in 1894. It entered Parliament in 1904 after the 1903 election, and steadily increased its vote until 1927, the party were members of Comintern, a Communist organisation, between 1918 and 1923. From the establishment of Vort Arbeide in 1884, the party had a growing and notable organisation of newspapers, the party press system eventually resulted in Norsk Arbeiderpresse. In January 1913 the party had 24 newspapers, and 6 more newspapers were founded in 1913, the party also had the periodical Det 20de Aarhundre
6.
Skerry
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A skerry is a small rocky island, usually defined to be too small for human habitation, it may simply be a rocky reef. A skerry can also be called a low sea stack, the term skerry is derived from the Old Norse sker, which means a rock in the sea. The Old Norse term sker was brought into the English language via the Scots language word spelled skerrie or skerry. In Scottish Gaelic, it appears as sgeir, e. g. Sula Sgeir, in Irish as sceir, in Welsh as sgeri, a skerry may have vegetative life such as moss and small, hardy grasses. They also, in areas of the world, are rested upon by animals such as seals or birds. Skerries are most commonly formed at the outlet of fjords where submerged glacially formed valleys at right angles to the coast join with other cross valleys in a complex array. By this channel one can travel through a protected passage almost the entire 1,600 km route from Stavanger to North Cape, the Blindleia is a skerry-protected waterway that starts near Kristiansand in southern Norway, and continues past Lillesand. The inside passage provides a route from Seattle, Washington to Skagway. Yet another such skerry-protected passage extends from the Straits of Magellan north for 800 km along the west coast of the South American continent, the Swedish coast along Bohuslän is likewise guarded by skerries. Even the east coast of Sweden, in the Baltic Sea, has many big skärgårdar, the southwestern coast of Finland also has a great many skerries, so many, in fact, that they form an archipelago. This area is experiencing post-glacial rebound that connects the islands as they break sea level, revealing till deposits. The skerries exist as small islands before uplift of adjacent terrain changes the classification of this landform into a tombolo. The most southerly skerries are perhaps the Skrap Skerries off South Georgia
7.
Population density
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Population density is a measurement of population per unit area or unit volume, it is a quantity of type number density. It is frequently applied to living organisms, and most of the time to humans and it is a key geographical term. Population density is population divided by land area or water volume. Low densities may cause a vortex and lead to further reduced fertility. This is called the Allee effect after the scientist who identified it, commonly this may be calculated for a county, city, country, another territory, or the entire world. The worlds population is around 7,000,000,000, therefore, the worldwide human population density is around 7,000,000,000 ÷510,000,000 =13.7 per km2. If only the Earths land area of 150,000,000 km2 is taken into account and this includes all continental and island land area, including Antarctica. If Antarctica is also excluded, then population density rises to over 50 people per km2, thus, this number by itself does not give any helpful measurement of human population density. Several of the most densely populated territories in the world are city-states, microstates, cities with high population densities are, by some, considered to be overpopulated, though this will depend on factors like quality of housing and infrastructure and access to resources. Most of the most densely populated cities are in Southeast Asia, though Cairo, for instance, Milwaukee has a greater population density when just the inner city is measured, and the surrounding suburbs excluded. Arithmetic density, The total number of people / area of land, physiological density, The total population / area of arable land. Agricultural density, The total rural population / area of arable land, residential density, The number of people living in an urban area / area of residential land. Urban density, The number of people inhabiting an urban area / total area of urban land, ecological optimum, The density of population that can be supported by the natural resources. S. States by population density Selected Current and Historic City, Ward & Neighborhood Density
8.
Fillan, Norway
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Fillan is a village and former municipality in Sør-Trøndelag county, Norway. The village is also the center of the present-day municipality of Hitra. It is located on the shore of Hitra island, about 5 kilometres south of Ansnes. The 0. 84-square-kilometre village has a population of 744, the former municipality included the northeastern part of the island of Hitra surrounding the Fillfjorden, plus about 100 islands, islets, and skerries—the largest of which is Fjellværsøya. For the first part of its existence, Fillan also included the Sandstad area along the part of Hitra. Villages in the municipality included Ansnes, Fillan, Nordbotn, the former municipality had a church and a chapel in it, both of which now form a parish in present-day Hitra. The Fillan church is located in the village of Fillan and the Nordbotn chapel is located on the island of Fjellværsøya, the municipality of Fillan was established on 1 January 1886 when it was separated from Hitra to form a municipality of its own. The initial population of the new municipality was 2,241, on 1 July 1914, the southern district of Sandstad was separated from Fillan to form its own municipality, leaving 1,543 residents in Fillan. On 1 January 1964, the municipalities of Fillan, Sandstad, Kvenvær, and Hitra were merged back together to re-form the old pre-1886 Hitra municipality
