1.
Finnmark
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Finnmark is a county in the extreme northeastern part of Norway. By land, it borders Troms county to the west, Finland to the south, and Russia to the east, and by water, the Norwegian Sea to the northwest, the county was formerly known as Finmarkens amt or Vardøhus amt. Since 2002, it has had two names, Finnmark and Finnmárku. It is part of the Sápmi region, which spans four countries, as well as the Barents Region, Vardø, the easternmost municipality in Norway, is located farther east than the cities of St. Petersburg and Istanbul. The Old Norse form of the name was Finnmǫrk, the first element is finn, the Norse name for the Sámi people. The last element is mǫrk which means woodland or borderland, in Norse times the name referred to any places where Sámi people were living. The coat of arms are black with a castle tower, technically described as Sable. The design is from 1967 and shows the old Vardøhus Fortress on the border with Russia. Finnmark is the northernmost and easternmost county in Norway, by area, Finnmark is Norways largest county, even larger than the neighboring country of Denmark. However, with a population of about 75,000, it is also the least populated of all Norwegian counties, Finnmark has a total coastline of 6,844 kilometres, including 3,155 kilometres of coastline on the islands. Nearly 12,300 people or 16.6 percent of the population in 2000 was living in the 100-meter belt along the coastline. Honningsvåg in Finnmark claims to be the northernmost city of the world, the coast is indented by large fjords, many of which are false fjords, as they are not carved out by glaciers. The highest point is located on the top of the glacier Øksfjordjøkelen, which has an area of 45 square kilometres, both Øksfjordjøkelen and Seilandsjøkelen are located in the western part of Finnmark. The Øksfjord plateau glacier calved directly into the sea until 1900, the central and eastern part of Finnmark is generally less mountainous, and has no glaciers. The land east of Nordkapp is mostly below 300 m, the nature varies from barren coastal areas facing the Barents Sea, to more sheltered fjord areas and river valleys with gullies and tree vegetation. About half of the county is above the line. This valley has the highest density of Brown bears in Norway, lynx and moose are common in large parts of Finnmark, but rare on the coast. The interior parts of the county are part of the great Finnmarksvidda plateau, with an elevation of 300 to 400 m, with numerous lakes, the plateau is famous for its tens of thousands of reindeer owned by the Sami, and swarms of mosquitos in mid-summer
2.
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
3.
Geographic coordinate system
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A geographic coordinate system is a coordinate system used in geography that enables every location on Earth to be specified by a set of numbers, letters or symbols. The coordinates are chosen such that one of the numbers represents a vertical position. A common choice of coordinates is latitude, longitude and elevation, to specify a location on a two-dimensional map requires a map projection. The invention of a coordinate system is generally credited to Eratosthenes of Cyrene. Ptolemy credited him with the adoption of longitude and latitude. Ptolemys 2nd-century Geography used the prime meridian but measured latitude from the equator instead. Mathematical cartography resumed in Europe following Maximus Planudes recovery of Ptolemys text a little before 1300, in 1884, the United States hosted the International Meridian Conference, attended by representatives from twenty-five nations. Twenty-two of them agreed to adopt the longitude of the Royal Observatory in Greenwich, the Dominican Republic voted against the motion, while France and Brazil abstained. France adopted Greenwich Mean Time in place of local determinations by the Paris Observatory in 1911, the latitude of a point on Earths surface is the angle between the equatorial plane and the straight line that passes through that point and through the center of the Earth. Lines joining points of the same latitude trace circles on the surface of Earth called parallels, as they are parallel to the equator, the north pole is 90° N, the south pole is 90° S. The 0° parallel of latitude is designated the equator, the plane of all geographic coordinate systems. The equator divides the globe into Northern and Southern Hemispheres, the longitude of a point on Earths surface is the angle east or west of a reference meridian to another meridian that passes through that point. All meridians are halves of great ellipses, which converge at the north and south poles, the prime meridian determines the proper Eastern and Western Hemispheres, although maps often divide these hemispheres further west in order to keep the Old World on a single side. The antipodal meridian of Greenwich is both 180°W and 180°E, the combination of these two components specifies the position of any location on the surface of Earth, without consideration of altitude or depth. The grid formed by lines of latitude and longitude is known as a graticule, the origin/zero point of this system is located in the Gulf of Guinea about 625 km south of Tema, Ghana. To completely specify a location of a feature on, in, or above Earth. Earth is not a sphere, but a shape approximating a biaxial ellipsoid. It is nearly spherical, but has an equatorial bulge making the radius at the equator about 0. 3% larger than the radius measured through the poles, the shorter axis approximately coincides with the axis of rotation
4.
Barents Sea
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The Barents Sea is a marginal sea of the Arctic Ocean, located off the northern coasts of Norway and Russia divided between Norwegian and Russian territorial waters. Known among Russians in the Middle Ages as the Murman Sea and it is a rather shallow shelf sea, with an average depth of 230 metres, and is an important site for both fishing and hydrocarbon exploration. Novaya Zemlya, an extension of the part of the Ural Mountains. The southern half of the Barents Sea, including the ports of Murmansk, in September, the entire Barents Sea is more or less completely ice-free. Until the Winter War, Finlands territory also reached to the Barents Sea, with the harbor at Petsamo being Finlands only ice-free winter harbor. There are three types of water masses in the Barents Sea, Warm, salty Atlantic water from the North Atlantic drift, cold Arctic water from the north, and warm. Between the Atlantic and Polar waters, a front called the Polar Front is formed, the lands of Novaya Zemlya attained most of their early Holocene coastal deglaciation approximately 10,000 years before present. The International Hydrographic Organization defines the limits of the Barentsz Sea as follows, On the west, on the northwest, The eastern shore of West Spitzbergen, Hinlopen Strait up to 80° latitude north, south and east coasts of North-East Land to Cape Leigh Smith. On the north, Cape Leigh Smith across the Islands Bolshoy Ostrov, Gilles and Victoria, on the east, Cape Kohlsaat to Cape Zhelaniya, west and southwest coast of Novaya Zemlya to Cape Kussov Noss and thence to western entrance Cape, Dolgaya Bay on Vaigach Island. Through Vaigach Island to Cape Greben, thence to Cape Belyi Noss on the mainland, on the south, The northern limit of the White Sea. Other islands in the Barents Sea include Chaichy and Timanets, most of its geological history is dominated by extensional tectonics, caused by the collapse of the Caledonian and Uralian orogenic belts and the break-up of Pangaea. These events created the rift basins that dominate the Barents Shelf, along with various platforms. Due to the North Atlantic drift, the Barents Sea has a high biological production compared to other oceans of similar latitude. The spring bloom of phytoplankton can start quite early close to the ice edge, the phytoplankton bloom feeds zooplankton such as Calanus finmarchicus, Calanus glacialis, Calanus hyperboreus, Oithona spp. and krill. The zooplankton feeders include young cod, capelin, polar cod, whales, the capelin is a key food for top predators such as the north-east Arctic cod, harp seals, and seabirds such as common guillemot and Brunnichs guillemot. The fisheries of the Barents Sea, in particular the cod fisheries, are of importance for both Norway and Russia. There is a genetically distinct polar bear population associated with the Barents Sea and its eastern corner, in the region of the Pechora Rivers estuary, has been known as Pechorskoye Morye, that is, Pechora Sea. This sea was given its present name in honor of Willem Barentsz, Barentsz was the leader of early expeditions to the far north, at the end of the sixteenth century
5.
Norwegian language
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Norwegian is a North Germanic language spoken mainly in Norway, where it is the official language. Along with Swedish and Danish, Norwegian forms a continuum of more or less mutually intelligible local and regional variants. These Scandinavian languages, together with Faroese and Icelandic as well as extinct languages. Faroese and Icelandic are hardly mutually intelligible with Norwegian in their spoken form because continental Scandinavian has diverged from them, as established by law and governmental policy, the two official forms of written Norwegian are Bokmål and Nynorsk. The official Norwegian Language Council is responsible for regulating the two forms, and recommends the terms Norwegian Bokmål and Norwegian Nynorsk in English. Two other written forms without official status also exist, one and it is regulated by the unofficial Norwegian Academy, which translates the name as Standard Norwegian. Nynorsk and Bokmål provide standards for how to write Norwegian, no standard of spoken Norwegian is officially sanctioned, and most Norwegians speak their own dialects in all circumstances. Thus, unlike in other countries, the use of any Norwegian dialect. Outside Eastern Norway, this variation is not used. From the 16th to the 19th centuries, Danish was the written language of Norway. As a result, the development of modern written Norwegian has been subject to strong controversy related to nationalism, rural versus urban discourse, historically, Bokmål is a Norwegianised variety of Danish, while Nynorsk is a language form based on Norwegian dialects and puristic opposition to Danish. The unofficial form known as Riksmål is considered more conservative than Bokmål, Norwegians are educated in both Bokmål and Nynorsk. A2005 poll indicates that 86. 3% use primarily Bokmål as their written language,5. 5% use both Bokmål and Nynorsk, and 7. 5% use primarily Nynorsk. Thus, 13% are frequently writing Nynorsk, though the majority speak dialects that resemble Nynorsk more closely than Bokmål. Broadly speaking, Nynorsk writing is widespread in western Norway, though not in major urban areas, examples are Setesdal, the western part of Telemark county and several municipalities in Hallingdal, Valdres, and Gudbrandsdalen. It is little used elsewhere, but 30–40 years ago, it also had strongholds in rural parts of Trøndelag. Today, not only is Nynorsk the official language of four of the 19 Norwegian counties, NRK, the Norwegian broadcasting corporation, broadcasts in both Bokmål and Nynorsk, and all governmental agencies are required to support both written languages. Bokmål is used in 92% of all publications, and Nynorsk in 8%
6.
Northern Sami
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Northern or North Sami, sometimes also simply referred to as Sami, is the most widely spoken of all Sami languages. The area where Northern Sami is spoken covers the parts of Norway, Sweden. The number of Northern Sami speakers is estimated to be somewhere between 15,000 and 25,000, about 2,000 of these live in Finland and between 5,000 and 6,000 in Sweden. Among the first printed Sami texts is Svenske och Lappeske ABC Book, written in Swedish and it was published in two editions in 1638 and 1640 and includes 30 pages of prayers and confessions of Protestant faith. It has been described as the first book with a regular Sami language form, Northern Sami was first described by Knud Leem in 1748 and in dictionaries in 1752 and 1768. The majority of his work has disappeared, en omarbejdelse af Prof. Knud Leems Lappiske grammatica in 1832. Rask opted for a phonemic orthographic system, following in the tradition of Rask meant that diacritics were used with some consonants, which caused data-processing problems before Unicode was introduced. Both Stockfleth and J. A. Friis went on to publish grammar books and it can be said that Northern Sami was better described than Norwegian was before Ivar Aasen published his grammar on Norwegian. Northern Sami was and is used in three countries, each of which used its own orthography for years, Friis orthography was used when work on translating the Bible into Northern Sami commenced, in the first Sami newspaper called Saǥai Muittalægje, and in the Finnemisjonens own newspaper Nuorttanaste. The groundwork for Northern Sami lexicography was laid by Konrad Nielsen who used an orthography of his own creation in his dictionary Lappisk ordbok, starting in 1948, the orthographies used in Norway and Sweden were combined into a single Bergsland-Ruong orthography. It was not greatly used in Norway, in addition, the authorities there instituted a policy that prohibited Sami from being used in practice. In Sweden, classes were taught in Sami in the Sami schools, in 1979, an official orthography for Northern Sami was adopted for use in Norway, Sweden and Finland. In Norway, Northern Sami is currently a language of two counties and six municipalities. The consonant inventory of Northern Sami is large, consisting of three different series of plosives/affricates and two series of nasals, in addition, length is contrastive for almost all consonants. /v/ is realised as a fricative in the syllable onset. Although is a fricative, it behaves phonologically like an approximant, all consonants can be geminated, except for /h/. This distinction is phonemically contrastive and widely productive as a grammatical feature, geminated glottalized nasals are realised with the glottalization in between the two consonants. In geminated preaspirated consonants, it is the preaspiration that lengthens rather than the occlusion, except for glottalized or preaspirated consonants, /h/, /j/ or /ʎ/, all consonants also possess a third overlong length
7.
Cape (geography)
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In geography, a cape is a headland or a promontory of large size extending into a body of water, usually the sea. A cape usually represents a change in trend of the coastline. Their proximity to the makes them prone to natural forms of erosion. This results in capes having a relatively short geologic lifespan, capes can be formed by glaciers, volcanoes, and changes in sea level. Erosion plays a role in each of these methods of formation. Eritrea–Sudan Ras Kasar Ghana Cape Coast Liberia Cape Mesurado - The Cape on which Monrovia is located, separates the Golden Horn Bay from the Sea of Marmara
8.
Northern Norway
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Northern Norway is the geographical region of Norway, consisting of the three northernmost counties Nordland, Troms and Finnmark, in total about 35% of the Norwegian mainland. Some of the largest towns in Northern Norway are Mo i Rana, Bodø, Narvik, Harstad, Tromsø, Northern Norway is often described as the land of the midnight sun and the land of the northern lights. Further north, halfway to the North Pole, is the Arctic archipelago of Svalbard, the region is multi-cultural, housing not just Norwegians but also the indigenous Sami people, Norwegian Finns and Russian populations. Finnish is spoken in only a few communities in the east of Finnmark, Northern Norway covers about a third of Norway. The southernmost part, roughly the part south of the Arctic Circle, is called Helgeland, the inland is covered with dense spruce forests and mountains near the Swedish border, some of the biggest rivers in the region are the Vefsna and the Ranelva. The highest mountain in Northern Norway is found here in the Okstindan range south of Mo i Rana with Oksskolten reaching 1,915 metres above sea level, the Saltfjellet range, with its Svartisen glacier and intersecting Arctic Circle, divides Helgeland from the next region, called Salten. Notable peaks in Salten are the Børvasstindan south of Bodø, Suliskongen near Fauske, the Steigartindan, between Saltfjellet and eastern Finnmark, Norway spruce trees have originally been planted and are mostly privately owned. The older plantations are now producing lumber,80 years after planted, Lofoten is a chain of peaks that jut out of the ocean. From the mainland side it looks very barren, but behind the violet-black peaks there are also flatlands with good grazing for sheep, the Vesterålen islands consist of smaller and bigger islands with a huge variation in landscape. There are also glaciers, like Frostisen and Blåisen, big islands like Senja, Kvaløya and Ringvassøya have green, forested interiors and a barren, mountainous coastline, with smaller islands offshore. The Lyngen Alps are the highest mountains of the area, rising to 1,833 metres, the 269 metres Mollisfossen waterfall in Nordreisa is the highest waterfall in the north, while Målselvfossen is Norways national waterfall. Finnmark county has fjords and glaciers in the far southwest, the inland is covered by Finnmarksvidda, a relatively barren plateau about 300 to 400 metres high, with many lakes and rivers like Alta-Kautokeino and Tana/Deatnu. Even at this latitude, pine forests grow naturally in lowland areas inland, east of Honningsvåg, there are no islands protecting the barren coasts that rise directly up from the sea. The landscape towards the Russian border is comparatively flat, Finnmark is situated north of northernmost Finland, and to the east Norway has a 196 kilometres border with Russia. The oldest known historical culture in the region is called Komsa, the first people possibly arrived around 12–13,000 years ago, but it is uncertain whether they came from southern Norway or from the Kola Peninsula. Today the rock carvings at Hjemmeluft in Alta or at Leknes in Nordland are among the remainders of the Stone Age cultures, showing reindeer swimming across the fjords. A significant find area is between the river Tana and the fjord of Varanger, where the reindeer probably ran over the isthmus on the way between the winter and summer grazing, metals were introduced around 500 BC. The Sami culture can be traced back at least 2,000 years, there is also some archeological evidence of Bronze Age agricultural settlements about 2,500 years old, as in Steigen and Sømna
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Nordkapp travel guide from Wikivoyage
