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Lake Inari
Lake Inari ( fi, Inarijärvi/Inarinjärvi, se, Anárjávri, smn, Aanaarjävri, sms, Aanarjäuʹrr, sv, Enare träsk, no, Enaresjøen) is the largest lake in Sápmi and the third-largest lake in Finland. It is located in the northern part of Lapland, north of the Arctic Circle. The lake is above sea level, and is regulated at the Kaitakoski power plant in Russia. The freezing period normally extends from November to early June. The best-known islands of the lake are Hautuumaasaari ("Graveyard Island"), which served as a cemetery for ancient Sami people, and Ukonkivi ("Ukko's Stone"), a sacrificial place of the ancient inhabitants of the area. There are over 3,000 islands in total. Trout, lake salmon, Arctic char, white fish, grayling, perch and pike are found in Lake Inari. The lake covers . It empties northwards through the Paatsjoki at the mouth of the Varangerfjord, which is a bay of the Barents Sea. The lake depression is a graben bounded by faults active in the Cen ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Inari, Finland
Inari (; smn, Aanaar; sms, Aanar; sme, Anár ; Norwegian and Swedish: ''Enare'') is Finland's largest municipality by area (but one of the most sparsely populated), with four official languages, more than any other in the country. Its major sources of income are tourism, service industry and cold climate testing. With the Siida museum in the village of Inari, it is a center of Sami culture, widely known as the "capital of Sámi culture". The airport in Ivalo and the country's key north-south European Route E75 ( Finland's National Road 4) bring summer and winter vacationers seeking resorts with access to a well-preserved, uncrowded natural environment. History The municipality was established in 1876. It was claimed from about 1942 to 1945 by the Quisling regime during the Nazi occupation of Norway. Geography Inari is the largest municipality by area in Finland. Located in Lapland, it covers an area of , of which is water. With an area of , Lake Inari is the third largest ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ukko
Ukko (), Äijä or Äijö (Finnish for 'male grandparent', 'grandfather', 'old man'), parallel to Uku in Estonian mythology, is the god of the sky, weather, harvest and thunder in Finnish mythology. Ukkonen, the Finnish word for thunder, is the diminutive form of the name ''Ukko''.Compare to English ''thunder'' (< ''þunor'') and ''donner'' (< ''donar'') both derived from ''*þunraz'' and originally synonymic with appellations of the |
Landforms Of Lapland (Finland)
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are the fou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Paatsjoki Basin
The Paatsjoki River ( fi, Paatsjoki, sms, Paaččjokk, sme, Báhčaveaijohka, no, Pasvikelva, sv, Pasvik älv, russian: Паз or Патсойоки, ''Paz or Patsoyoki'') is a river that flows through Finland, Norway, and Russia. Since 1826, the river has marked parts of the Norway–Russia border, except from 1920 to 1944 when it was along the Finland–Norway border. The river is the outlet from the large Lake Inari in Finland and flows through Norway and Russia to discharge into the Bøkfjorden (which later flows into the Varangerfjorden and then the Barents Sea), not far from the town of Kirkenes. The river has a watershed of , and is long. A series of hydroelectric stations, known as the Paatsjoki River Hydroelectric Plants, are along the river. The river provides good fishing opportunities for Atlantic salmon The Atlantic salmon (''Salmo salar'') is a species of ray-finned fish in the family Salmonidae. It is the third largest of the Salmonidae, behind Siberi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Soviet Union
The Soviet Union,. officially the Union of Soviet Socialist Republics. (USSR),. was a transcontinental country that spanned much of Eurasia from 1922 to 1991. A flagship communist state, it was nominally a federal union of fifteen national republics; in practice, both its government and its economy were highly centralized until its final years. It was a one-party state governed by the Communist Party of the Soviet Union, with the city of Moscow serving as its capital as well as that of its largest and most populous republic: the Russian SFSR. Other major cities included Leningrad (Russian SFSR), Kiev (Ukrainian SSR), Minsk ( Byelorussian SSR), Tashkent (Uzbek SSR), Alma-Ata (Kazakh SSR), and Novosibirsk (Russian SFSR). It was the largest country in the world, covering over and spanning eleven time zones. The country's roots lay in the October Revolution of 1917, when the Bolsheviks, under the leadership of Vladimir Lenin, overthrew the Russian Provisional Government ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pre-Finno-Ugric Substrate
Pre-Finno-Ugric substrate refers to substratum loanwords from unidentified non-Indo-European and non-Uralic languages that are found in various Finno-Ugric languages, most notably Sami. The presence of Pre-Finno-Ugric substrate in Sami languages was demonstrated by Ante Aikio. Janne Saarikivi points out that similar substrate words are present in Finnic languages as well, but in much smaller numbers. The number of substrate words in Sámi likely exceeds one thousand words. Borrowing to Saami from Paleo-Laplandic probably still took place after the completion of the Great Saami Vowel Shift. Paleo-Laplandic likely became extinct about 1500 years ago. The Nganasan language also has many substrate words from unknown extinct languages in the Taimyr peninsula. Theories According to Aikio, the speakers of the Proto-Samic language arrived in Lapland around 650 BC and fully assimilated the local Paleo-European populations by the middle of 1st millennium AD. In his opinion, the d ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Uppslagsverket Finland
''Uppslagsverket Finland'' ('Encyclopedia Finland') is a Swedish-language encyclopedia with a focus on Finland and in particular Finland-Swedish subjects. The encyclopedia is published by initiative of an association dedicated to this task, ('the Finnish-Swedish Encyclopedia Association'). The initiative to the publication was taken in 1969, and the first edition was published in three volumes in 1982 to 1985.Uppslagsverket Finlands historia Accessed 2016-07-16. A second edition was published by in five volumes during 2003 to 2007. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cenozoic
The Cenozoic ( ; ) is Earth's current geological era, representing the last 66million years of Earth's history. It is characterised by the dominance of mammals, birds and flowering plants, a cooling and drying climate, and the current configuration of continents. It is the latest of three geological eras since complex life evolved, preceded by the Mesozoic and Paleozoic. It started with the Cretaceous–Paleogene extinction event, when many species, including the non-avian dinosaurs, became extinct in an event attributed by most experts to the impact of a large asteroid or other celestial body, the Chicxulub impactor. The Cenozoic is also known as the Age of Mammals because the terrestrial animals that dominated both hemispheres were mammalsthe eutherians (placentals) in the northern hemisphere and the metatherians (marsupials, now mainly restricted to Australia) in the southern hemisphere. The extinction of many groups allowed mammals and birds to greatly diversify so that l ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fault (geology)
In geology, a fault is a planar fracture or discontinuity in a volume of rock across which there has been significant displacement as a result of rock-mass movements. Large faults within Earth's crust result from the action of plate tectonic forces, with the largest forming the boundaries between the plates, such as the megathrust faults of subduction zones or transform faults. Energy release associated with rapid movement on active faults is the cause of most earthquakes. Faults may also displace slowly, by aseismic creep. A ''fault plane'' is the plane that represents the fracture surface of a fault. A ''fault trace'' or ''fault line'' is a place where the fault can be seen or mapped on the surface. A fault trace is also the line commonly plotted on geologic maps to represent a fault. A ''fault zone'' is a cluster of parallel faults. However, the term is also used for the zone of crushed rock along a single fault. Prolonged motion along closely spaced faults can blur the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Graben
In geology, a graben () is a depressed block of the crust of a planet or moon, bordered by parallel normal faults. Etymology ''Graben'' is a loan word from German, meaning 'ditch' or 'trench'. The word was first used in the geologic context by Eduard Suess in 1883. The plural form is either ''graben'' or ''grabens''. Formation A graben is a valley with a distinct escarpment on each side caused by the displacement of a block of land downward. Graben often occur side by side with horsts. Horst and graben structures indicate tensional forces and crustal stretching. Graben are produced from parallel normal faults, where the displacement of the hanging wall is downward, while that of the footwall is upward. The faults typically dip toward the center of the graben from both sides. Horsts are parallel blocks that remain between graben; the bounding faults of a horst typically dip away from the center line of the horst. Single or multiple graben can produce a rift valley. Half-g ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Barents Sea
The Barents Sea ( , also ; no, Barentshavet, ; russian: Баренцево море, Barentsevo More) is a marginal sea of the Arctic Ocean, located off the northern coasts of Norway and Russia and divided between Norwegian and Russian territorial waters.World Wildlife Fund, 2008. It was known among Russians in the Middle Ages as the Murman Sea ("Norse Sea"); the current name of the sea is after the historical Netherlands, Dutch navigator Willem Barentsz. The Barents Sea is a rather shallow Continental shelf, shelf sea, with an average depth of , and it is an important site for both fishing and hydrocarbon exploration.O. G. Austvik, 2006. It is bordered by the Kola Peninsula to the south, the shelf edge towards the Norwegian Sea to the west, and the archipelagos of Svalbard to the northwest, Franz Josef Land to the northeast and Novaya Zemlya to the east. The islands of Novaya Zemlya, an extension of the northern end of the Ural Mountains, separate the Barents Sea from the Kar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Varangerfjord
The Varangerfjord ( en, Varanger Fjord; russian: Варангер-фьорд, Варяжский залив; fi, Varanginvuono; sme, Várjavuonna) is the easternmost fjord in Norway, north of Finland. The fjord is located in Troms og 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 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 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. History The ''Kven'' residents of ''Varangerfjord'' are largely descendants of Finnish immigrants who arrived to the area during the 19th century from Finland and northe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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