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Lake Inari
Lake Inari (, , , , , ) 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 Sámi 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 Cenozoic The Cenozoic Era ( ; ) is Earth's current geological era, representing the last 66million years o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Inari, Finland
Inari (; ; ; ; Norwegian language, Norwegian and ) is Finland's largest Municipalities of Finland, 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), Siida museum in the Inari (village), village of Inari, it is a center of Sámi peoples, Sámi culture, widely known as the "capital of Sámi culture". The Ivalo Airport, airport in Ivalo and the country's key north-south European route E75, European Route E75 (Finnish national road 4, 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#Territorial claims, Quisling regime during the Nazi occupation of Norway. Geography Inari is the List of Finnish ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ukonkivi
Ukonkivi ("Ukko's rock") is located on the island of Ukonsaari in lake Lake Inari, Inari, Lapland (Finland), Finnish Lapland. The Inari Sámi language, Inari Sámi name for the island is Äijih. The area of the lake is called Ukonselkä. Ukonkivi was considered by the local Inari Sámi people, Inari Sámi to be an extremely important ''sieidi'' (, ), or sacred natural formation, and was used as a sacrificial site, perhaps as recently as in the 19th century. The names "Ukko" and "Äijih" refer to sky deities in the Finnish mythology, Finnish and Sámi mythology, Sámi mythologies, respectively. The island is about high, broad and a long. The distance from the village of Inari (village), Inari to Ukonkivi is approximately . There are guided tours to the site during the summer from the harbour of the Sámi museum, Siida. There are two known siedis at Ukonsaari. The first one to be studied was a sacrificial cave. One of the most important archaeological findings in Sápmi (area) ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of Lapland (Finland)
A landform is a land feature on the solid surface of the Earth or other planetary body. They may be natural or may be anthropogenic (caused or influenced by human activity). 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 oceanic basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, structure stratification, rock exposure, and soil type. Gross physical features or landforms include intuitive elements such as berms, cliffs, hills, mounds, peninsulas, ridges, rivers, valleys, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Paatsjoki Basin
The Paatsjoki River (, , , , , , ''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. Five of those sevenhttps://www.dagsavisen.no/nyheter/2023/12/03/samarbeid-med-russland-lagt-pa-is-et-tap/. Dagsavisen.no. Retrieved 2023-12-04 power stations, are Russian. 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake Inari Missile Incident
The P-5 ''Pityorka'' (), also known by the NATO reporting name SS-N-3 Shaddock for submarine-launched versions and SS-N-3 Sepal for ship and coastal defence versions, is a Cold War era turbojet-powered cruise missile of the Soviet Union, designed by the Vladimir Chelomei, Chelomey design bureau. Originally designed as a strategic nuclear weapon, it entered service in 1963 with the Soviet Navy. All ship and submarine launched versions remained in service until 1994, while coastal defence batteries remain in limited service with the Russian Navy. Overview The SS-N-3 Shaddock and Sepal missiles are long with a body diameter of . Two swept-wings long unfold forward after launch. A turbojet engine and an air inlet are located at the rear of the missile, while two solid propellant motors boost the missile during launch. The missile can cruise at altitudes of , , or at a maximum speed of 1.3 Mach. After the boosters are jettisoned, the turbojet powers the missile for the rest of ... [...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. points out that similar substrate words are present in Finnic languages as well, but in much smaller numbers. The proposed substrate influence in Finnic may have been related either by borrowing or a direct genetic relationship to the languages that influenced Saami. 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-Europe ... [...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 Schildts in five volumes during 2003 to 2007. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cenozoic
The Cenozoic Era ( ; ) is Earth's current geological era, representing the last 66million years of Earth's history. It is characterized by the dominance of mammals, insects, birds and angiosperms (flowering plants). It is the latest of three geological eras of the Phanerozoic Eon, preceded by the Mesozoic and Paleozoic. The Cenozoic 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 and to some extent South America) in the Southern Hemisphere. The extinction of many groups allowed mammals and birds to greatly diversify so that large m ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fault (geology)
In geology, a fault is a Fracture (geology), planar fracture or discontinuity in a volume of Rock (geology), rock across which there has been significant displacement as a result of rock-mass movements. Large faults within Earth's crust (geology), crust result from the action of Plate tectonics, plate tectonic forces, with the largest forming the boundaries between the plates, such as the megathrust faults of subduction, 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 (geometry), 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 geological maps to represent a fault. A ''fault zone'' is a cluster of parallel faults. However, the term is also used for the zone ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Graben
In geology, a graben () is a depression (geology), depressed block of the Crust (geology), crust of a planet or moon, bordered by parallel normal faults. Etymology ''Graben'' is a loan word from German language, German, meaning 'ditch' or 'trench'. The first known usage of the word in the geologic context was 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 Horst (geology), horsts. Horst and graben structures indicate tensional forces and crustal stretching. Graben are produced by sets of normal faults that have parallel fault traces, 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 t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Barents Sea
The Barents Sea ( , also ; , ; ) 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 earlier among Russians as the Northern Sea, Pomorsky Sea or 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, 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 Kara Sea. Although part of the Arctic Ocean, the Barents Sea ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Varangerfjord
The Varangerfjord (; ; ; ) is the easternmost fjord in Norway, north of Finland. The fjord is located in Finnmark county between the Varanger Peninsula and the mainland of Norway. Extents 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. Older Russian Imperial and Soviet sources also included its natural extension up to the Russian Rybachy Peninsula on the southern shore and the easternmost part of the Varanger Peninsula on the northern shore. History During the first half of the 19th century, the possibility ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
