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.
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
3.
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
4.
Counties of Norway
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Norway is divided into 19 administrative regions, called counties, until 1918, they were known as amter. The counties form the first-level subdivisions of Norway and are divided into 428 municipalities. Svalbard and Jan Mayen are outside the county division and ruled directly on national level, the capital Oslo is considered both a county and a municipality. In 2017 the government decided to abolish the current counties and to them with fewer, larger administrative regions. Below is a list of the Norwegian counties as they have been since 1919, note that the counties are administered both by appointees of the national government and to a lesser extent by their own elected bodies. The county numbers are from the numbering system ISO 3166-2, NO. The number 13 was dropped from the system when the city of Bergen was merged into Hordaland in 1972, from the consolidation to a single kingdom, Norway was divided into a number of geographic regions that had its own legislative assembly or Thing, such as Gulating and Frostating. The second-order subdivision of these regions was into fylker, such as Egdafylke and Hordafylke, in 1914, the historical term fylke was brought into use again to replace the term amt introduced during the union with Denmark. Current day counties often, but not necessarily, correspond to the historical areas. Finnmark, the Faroe Islands, the Orkney Islands, Shetland, the Hebrides, Isle of Man, Iceland and Greenland were Norwegian skattland, from the end of the 12th century, Norway was divided into several syssel. The head of the various syssel was the syslemann, who represented the king locally, the following shows a reconstruction of the different syssel in Norway c. 1300, including sub-syssel where these seem established, from 1308, the term len in Norway signified an administrative region roughly equivalent to todays counties. The historic len was an important administrative entity during the period of Dano-Norwegian unification after their amalgamation as one state, which lasted for the period 1536–1814. At the beginning of the 16th century the political divisions were variable, up to 1660 the four principal len were headquartered at the major fortresses Bohus Fortress, Akershus Fortress, Bergenhus Fortress and the fortified city of Trondheim. The sub-regions corresponded to the districts for the Lutheran church in Norway. Båhus len Akershus len Trondheim len Bergenhus len These four principal len were in the 1530s divided into approximately 30 smaller regions. From that point forward through the beginning of the 17th century the number of subsidiary len was reduced, from 1660 Norway had nine principal len comprising 17 subsidiary len, Len written as län continues to be used as the administrative equivalent of county in Sweden to this day. Each len was governed by a lenman, with the royal decree of February 19,1662, each len was designated an amt and the lenmann was titled amtmann, from German Amt, reflecting the bias of the Danish court of that period
5.
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
6.
Districts of Norway
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The country Norway is historically divided into a number of districts. Many districts have deep roots, and only partially coincide with todays administrative units of counties and municipalities. The districts are defined by geographical features, often valleys, mountain ranges, fjords, plains, or coastlines, many such regions were petty kingdoms up to the early Viking age. A high percentage of Norwegians identify themselves more by the district live in or come from. Thus, dialects and regional commonality in folk culture tended to correspond to those same geographical units, the construction of railroads between distant parts of the country. The opening of dozens of new airports all over the country through the 1960s and 1970s, the release of private cars from government rationing and import restrictions from the 1950s onwards. A concrete display of the Norwegian habit of identifying themselves by district can be seen in the many regional costumes, called bunad, the following list is non-exhaustive and partially overlapping. The first name is the name in Bokmål, the second Nynorsk, helgeland Lofoten Ofoten Salten Vesterålen See also Finnmark, Hålogaland and Troms
7.
Daylight saving time
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Daylight saving time is the practice of advancing clocks during summer months by one hour so that evening daylight lasts an hour longer, while sacrificing normal sunrise times. Typically, regions that use Daylight Savings Time adjust clocks forward one hour close to the start of spring, American inventor and politician Benjamin Franklin proposed a form of daylight time in 1784. New Zealander George Hudson proposed the idea of saving in 1895. The German Empire and Austria-Hungary organized the first nationwide implementation, starting on April 30,1916, many countries have used it at various times since then, particularly since the energy crisis of the 1970s. The practice has both advocates and critics, DST clock shifts sometimes complicate timekeeping and can disrupt travel, billing, record keeping, medical devices, heavy equipment, and sleep patterns. Computer software often adjusts clocks automatically, but policy changes by various jurisdictions of DST dates, industrialized societies generally follow a clock-based schedule for daily activities that do not change throughout the course of the year. The time of day that individuals begin and end work or school, North and south of the tropics daylight lasts longer in summer and shorter in winter, with the effect becoming greater as one moves away from the tropics. However, they will have one hour of daylight at the start of each day. Supporters have also argued that DST decreases energy consumption by reducing the need for lighting and heating, DST is also of little use for locations near the equator, because these regions see only a small variation in daylight in the course of the year. After ancient times, equal-length civil hours eventually supplanted unequal, so civil time no longer varies by season, unequal hours are still used in a few traditional settings, such as some monasteries of Mount Athos and all Jewish ceremonies. This 1784 satire proposed taxing window shutters, rationing candles, and waking the public by ringing church bells, despite common misconception, Franklin did not actually propose DST, 18th-century Europe did not even keep precise schedules. However, this changed as rail transport and communication networks came to require a standardization of time unknown in Franklins day. Modern DST was first proposed by the New Zealand entomologist George Hudson, whose shift work job gave him time to collect insects. An avid golfer, he also disliked cutting short his round at dusk and his solution was to advance the clock during the summer months, a proposal he published two years later. The proposal was taken up by the Liberal Member of Parliament Robert Pearce, a select committee was set up to examine the issue, but Pearces bill did not become law, and several other bills failed in the following years. Willett lobbied for the proposal in the UK until his death in 1915, william Sword Frost, mayor of Orillia, Ontario, introduced daylight saving time in the municipality during his tenure from 1911 to 1912. Starting on April 30,1916, the German Empire and its World War I ally Austria-Hungary were the first to use DST as a way to conserve coal during wartime, Britain, most of its allies, and many European neutrals soon followed suit. Russia and a few other countries waited until the year
8.
Central European Summer Time
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It corresponds to UTC + two hours. Other names which have been applied to Central European Summer Time are Middle European Summer Time, Central European Daylight Saving Time, and Bravo Time. Since 1996 European Summer Time has been observed between 1,00 UTC on the last Sunday of March and 1,00 on the last Sunday of October, the following countries and territories use Central European Summer Time. In addition, Libya used CEST during the years 1951–1959, 1982–1989, 1996–1997, European Summer Time Other countries and territories in UTC+2 time zone Other names of UTC+2 time zone
9.
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
10.
Russian language
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Russian is an East Slavic language and an official language in Russia, Belarus, Kazakhstan, Kyrgyzstan and many minor or unrecognised territories. Russian belongs to the family of Indo-European languages and is one of the four living members of the East Slavic languages, written examples of Old East Slavonic are attested from the 10th century and beyond. It is the most geographically widespread language of Eurasia and the most widely spoken of the Slavic languages and it is also the largest native language in Europe, with 144 million native speakers in Russia, Ukraine and Belarus. Russian is the eighth most spoken language in the world by number of native speakers, the language is one of the six official languages of the United Nations. Russian is also the second most widespread language on the Internet after English, Russian distinguishes between consonant phonemes with palatal secondary articulation and those without, the so-called soft and hard sounds. This distinction is found between pairs of almost all consonants and is one of the most distinguishing features of the language, another important aspect is the reduction of unstressed vowels. Russian is a Slavic language of the Indo-European family and it is a lineal descendant of the language used in Kievan Rus. From the point of view of the language, its closest relatives are Ukrainian, Belarusian, and Rusyn. An East Slavic Old Novgorod dialect, although vanished during the 15th or 16th century, is considered to have played a significant role in the formation of modern Russian. In the 19th century, the language was often called Great Russian to distinguish it from Belarusian, then called White Russian and Ukrainian, however, the East Slavic forms have tended to be used exclusively in the various dialects that are experiencing a rapid decline. In some cases, both the East Slavic and the Church Slavonic forms are in use, with different meanings. For details, see Russian phonology and History of the Russian language and it is also regarded by the United States Intelligence Community as a hard target language, due to both its difficulty to master for English speakers and its critical role in American world policy. The standard form of Russian is generally regarded as the modern Russian literary language, mikhail Lomonosov first compiled a normalizing grammar book in 1755, in 1783 the Russian Academys first explanatory Russian dictionary appeared. By the mid-20th century, such dialects were forced out with the introduction of the education system that was established by the Soviet government. Despite the formalization of Standard Russian, some nonstandard dialectal features are observed in colloquial speech. Thus, the Russian language is the 6th largest in the world by number of speakers, after English, Mandarin, Hindi/Urdu, Spanish, Russian is one of the six official languages of the United Nations. Education in Russian is still a choice for both Russian as a second language and native speakers in Russia as well as many of the former Soviet republics. Russian is still seen as an important language for children to learn in most of the former Soviet republics, samuel P. Huntington wrote in the Clash of Civilizations, During the heyday of the Soviet Union, Russian was the lingua franca from Prague to Hanoi
11.
Varangerfjord
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The Varangerfjord is the easternmost fjord in Norway. The fjord is located in Finnmark county between the Varanger Peninsula and the mainland of Norway, the fjord flows through the municipalities of Vardø, Vadsø, Nesseby, and Sør-Varanger. The fjord is approximately 100 kilometres long, emptying into the Barents Sea, in a strict sense, it is a false fjord, since it does not have the hallmarks of a fjord carved by glaciers. Its mouth is about 70 kilometres wide, located between the town of Vardø in the northwest and the village of Grense Jakobselv in the southeast, the fjord stretches westwards inland past the town of Vadsø to the village of Varangerbotn in Nesseby Municipality. The Kven residents of Varangerfjord are largely descendants of Finnish immigrants who arrived to the area during the 19th century from Finland, media related to Varangerfjorden at Wikimedia Commons
12.
Kirkenes Church
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It is located in the town of Kirkenes, just off the European route E6 highway. In 1857, it was decided that a church should be built on the side of the Varangerfjorden. After some discussion about the location to build on, planners settled on a site on the Piselvnes peninsula at the mouth of the Pasvikelva river where it meets the Bøkfjorden. The parish was named Sydvaranger, and after the church was built its site was renamed Kirkenes, the first church building was completed in 1862. It stood almost until the end of World War II, when in 1944 it was subjected to heavy bombing, the old church spire survived, though, and was incorporated into its replacement. As was common to two-thirds of post-war church construction in Norway, reinforced concrete bricks were used as a principal material, interior decoration and furnishings reflect a traditional strongly sacred character. The present church building was completed in 1959, it seats about 275 people
13.
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
14.
Headland
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A headland is a coastal landform, a point of land usually high and often with a sheer drop, that extends out into a body of water. It is a type of promontory, a headland of considerable size often is called a cape. Headlands are characterised by high, breaking waves, rocky shores, intense erosion, headlands and bays are often found on the same coastline. A bay is surrounded by land on three sides, whereas a headland is surrounded by water on three sides, headlands and bays form on discordant coastlines, where bands of rock of alternating resistance run perpendicular to the coast. Bays form where weak rocks are eroded, leaving bands of rocks forming a headland. Through the deposition of sediment within the bay and the erosion of the headlands, coastlines eventually straighten out then start the same process all over again
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Kirkenes (help·info) (Northern Sami: Girkonjárga, Finnish and Kven: Kirkkoniemi, Russian: Киркенес) is a town in Sør-Varanger Municipality in Finnmark county, in the far northeastern part of Norway. The town lies on a peninsula along the Bøkfjorden, an arm of the large Varangerfjorden. The main church for Kirkenes is Kirkenes Church, located in the Haganes area of the town.
