1.
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
2.
Russia
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Russia, also officially the Russian Federation, is a country in Eurasia. The European western part of the country is more populated and urbanised than the eastern. Russias capital Moscow is one of the largest cities in the world, other urban centers include Saint Petersburg, Novosibirsk, Yekaterinburg, Nizhny Novgorod. Extending across the entirety of Northern Asia and much of Eastern Europe, Russia spans eleven time zones and incorporates a range of environments. It shares maritime borders with Japan by the Sea of Okhotsk, the East Slavs emerged as a recognizable group in Europe between the 3rd and 8th centuries AD. Founded and ruled by a Varangian warrior elite and their descendants, in 988 it adopted Orthodox Christianity from the Byzantine Empire, beginning the synthesis of Byzantine and Slavic cultures that defined Russian culture for the next millennium. Rus ultimately disintegrated into a number of states, most of the Rus lands were overrun by the Mongol invasion. The Soviet Union played a role in the Allied victory in World War II. The Soviet era saw some of the most significant technological achievements of the 20th century, including the worlds first human-made satellite and the launching of the first humans in space. By the end of 1990, the Soviet Union had the second largest economy, largest standing military in the world. It is governed as a federal semi-presidential republic, the Russian economy ranks as the twelfth largest by nominal GDP and sixth largest by purchasing power parity in 2015. Russias extensive mineral and energy resources are the largest such reserves in the world, making it one of the producers of oil. The country is one of the five recognized nuclear weapons states and possesses the largest stockpile of weapons of mass destruction, Russia is a great power as well as a regional power and has been characterised as a potential superpower. The name Russia is derived from Rus, a state populated mostly by the East Slavs. However, this name became more prominent in the later history, and the country typically was called by its inhabitants Русская Земля. In order to distinguish this state from other states derived from it, it is denoted as Kievan Rus by modern historiography, an old Latin version of the name Rus was Ruthenia, mostly applied to the western and southern regions of Rus that were adjacent to Catholic Europe. The current name of the country, Россия, comes from the Byzantine Greek designation of the Kievan Rus, the standard way to refer to citizens of Russia is Russians in English and rossiyane in Russian. There are two Russian words which are translated into English as Russians
3.
Federal districts of Russia
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The federal districts are groupings of the federal subjects of Russia. Plenipotentiary Representatives are appointed by the President and are employees of the Presidential Administration, source, President Vladimir Putin established seven federal districts in May 2000. On January 19,2010 the new North Caucasian Federal District split from the Southern Federal District, on March 2014, after the Russian military intervention in and annexation of Crimea, the Crimean Federal District was established. The legality of this annexation is disputed by most states as well as NATO, on July 28,2016 the Crimean Federal District was abolished and merged into the Southern Federal District in order to improve the governance
4.
Economic regions of Russia
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No federal subject can belong to more than one economic region. Economic regions are grouped into economic zones. An economic region or its parts can belong to more than one economic zone, establishment and abolition of economic regions and economic zones or any changes in their composition are decided upon by the federal government of Russia. The following is the list and composition of the economic regions, sorted by population
5.
Northern economic region (Russia)
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Northern Economic Region is one of twelve economic regions of Russia. Arkhangelsk Oblast Republic of Karelia Komi Republic Murmansk Oblast Nenets Autonomous Okrug Vologda Oblast Northern economic region accounted for almost 4 per cent of the national GRP in 2008. In the partly arctic zone of Russia, monthly wages appear much higher than the national average, a higher proportion in the region are employed in a state enterprise, and a lower proportion are secure in their jobs. Unemployment is more than one fifth higher in the region than across Russia as a whole, although climatic conditions can be daunting, the life expectancy in the Northern region is almost exactly the national average for both men and women. Youths ambitious for a higher education tend to leave the region, and, for those who live in the region, the expectation of life improving is lower than the national average
6.
Murmansk
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The city is named for the Murman Coast, Murman is itself an older Russian term for Norwegians. Although Murmansks population is in decline—299,148,307, 257 ,336, 137 ,468, Murmansk was the last city founded in the Russian Empire. On June 29,1916, Russian Transport Minister Alexander Trepov petitioned to grant urban status to the railway settlement, on July 6,1916, the petition was approved and the town was named Romanov-on-Murman, after the imperial Russian dynasty of Romanovs. On September 21,1916, the ceremony was performed. After the February Revolution of 1917, on April 3,1917, in the winter of 1917 the British North Russia Squadron under Rear Admiral Thomas Kemp was established at Murmansk. From 1918 to 1920, during the Russian Civil War, the town was occupied by the Western powers, who had allied in World War I. On February 13,1926, local self-government was organized in Murmansk for the first time, during a session of the Murmansk City Soviet. Prior to this, the city was governed by the authorities of Alexandrovsky Uyezd, while this plan was not confirmed by the Leningrad Oblast Executive Committee, in 1935–1937 several rural localities of Kolsky and Polyarny Districts were merged into Murmansk anyway. According to the Presidium of the Leningrad Oblast Executive Committee resolution of February 26,1935, however, the provisions of the resolution were not fully implemented, and due to military construction in Polyarnoye, the administrative center was instead moved to Murmansk in the beginning of 1935. In addition to being the center of Murmansk Okrug, Murmansk also continued to serve as the administrative center of Polyarny District until September 11,1938. This status was retained when Murmansk Okrug was transformed into Murmansk Oblast on May 28,1938, the supplies were brought to the city in the Arctic convoys. For the rest of the war, Murmansk served as a point for weapons. This unyielding, stoic resistance was commemorated at the 40th anniversary of the victory over the Germans in the designation of Murmansk as a Hero City on May 6,1985. During the Cold War Murmansk was a center of Soviet submarine, after the dissolution of the Soviet Union, the nearby city and naval base of Severomorsk remains the headquarters of the Russian Northern Fleet. In 1974, a massive 35. 5-meter tall statue Alyosha, in 1984, the Hotel Arctic, now known as Azimut Hotel Murmansk, opened and became the tallest building above the Arctic Circle. Within the framework of administrative divisions, it is incorporated as the City of Murmansk—an administrative unit with the equal to that of the districts. As a municipal division, the City of Murmansk is incorporated as Murmansk Urban Okrug and they were abolished on June 2,1948. The same city districts were created for the time on June 23,1951
7.
Marina Kovtun
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Marina Vasilievna Kovtun is the current Governor of Murmansk Oblast. She worked in various Murmansk government agencies, including tourism management, Kovtun is the first female leader of Murmansk Oblast. In 2001 she was graduated from North-West Academy for State Services as a specialist in Municipal, from 1986 she worked in the Murmansk District Committee of the Komsomol, and she was the head of Kola District. From 1994 to 2005 she worked as deputy chairman of the Physical Culture, Sport, from 2005 she was the Chief Deputy of the local Department of the Federal Tourism Agency. From 2006 til 2009 she led the Department for Tourism Development of the Directorate for Economics in the Murmansk Oblast Administration, until 2011 she was the deputy chairman of the Kola GMK Company. In December 2011 she was elected to the Murmansk Oblast Duma, in April 2012, Russian president Dmitry Medvedev appointed Kovtun as acting governor of Murmansk Oblast, when the previous governor, Dmitry Dmitriyenko, resigned from office
8.
Federal subjects of Russia
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Since March 18,2014, the Russian Federation constitutionally consists of 85 federal subjects, although the two most recently added subjects are internationally recognized as part of Ukraine. Three Russian cities of importance have a status of both city and separate federal subject which comprises other cities and towns within federal city keeping old structure of postal address. In 1993, there were 89 federal subjects listed, by 2008, the number of federal subjects had been decreased to 83 because of several mergers. In 2014, Sevastopol and the Republic of Crimea became the 84th and 85th federal subjects of Russia, every federal subject has its own head, a parliament, and a constitutional court. Federal subjects have their own constitution and legislation, subjects have equal rights in relations with federal government bodies. The federal subjects have equal representation—two delegates each—in the Federation Council and they do, however, differ in the degree of autonomy they enjoy. Composition of post-Soviet Russia was formed during the history of the Russian Soviet Federative Socialist Republic within the USSR, the Federation Treaty was included in the text of the 1978 Constitution of the Russian SFSR. In the late 1990s and early 2000s, the system became de jure closer to other modern federal states with a republican form of government in the world. There are several groupings of Russian regions, Federal subjects should not be confused with the eight Federal districts which are not subdivisions of Russia, are much larger and each encompass many federal subjects. Federal districts were created by Executive Order of the President of Russia specially for presidential envoys, an official government translation of the Constitution of Russia in Article 5 states,1. Another translation of the Constitution of Russia gives for article 65, each federal subject belongs to one of the following types, b. ^ According to Article 13 of the Charter of Leningrad Oblast, however, St. Petersburg is not officially named to be the administrative center of the oblast. ^ According to Article 24 of the Charter of Moscow Oblast, however, Moscow is not officially named to be the administrative center of the oblast. ^ Not recognized internationally as a part of Russia, the merging process was finished on March 1,2008. No new mergers have been planned since March 2008, Федерального конституционного закона №7-ФКЗ от30 декабря2008 г. Вступил в силу со дня официального опубликования, Опубликован, Российская газета, №237,25 декабря1993 г
9.
Time in Russia
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There are eleven time zones in Russia, which currently observe times ranging from UTC+02,00 to UTC+12,00. Daylight saving time is not used in Russia, since 4 December 2016, the time zones are as follows, Daylight saving time in Russia was originally introduced on 30 June 1917 by a decree of the Russian Provisional Government. However, it was abandoned by a Decree of the Soviet government five months later, Daylight saving time was re-introduced in the USSR on 1 April 1981, by a decision of the Council of Ministers of the USSR. The usage of daylight saving time continued after the Soviet collapse but ended in 2011, on 27 March 2011, clocks were advanced as usual, but they did not go back on 30 October 2011, effectively making Moscow Time UTC+4 permanently. In the Russian Empire, most of the observed solar time. During the late 19th century, Moscow Mean Time was introduced on 1 January 1880,2,30,17 corresponds to 37. 6166667°, the longitude of Moscow. Other parts of Russia kept solar time for several years. At this time, Russia had the Julian calendar with 12 or 13 days less date compared to Western Europe, so it is possible to say the Moscow actually had GMT-285,29,43, GMT-309,29,43 and GMT-309,28,41. Russia adopted the Gregorian calendar on Thursday,14 February 1918, after the Soviet Union was created, Moscow Time became UTC+2 and the various other time zones were introduced throughout Russia and the rest of the Soviet Union, for example Irkutsk Time GMT+7. Between 1917-1922 the time was ordered, with daylight savings time some of those years. On 21 June 1930, the Soviet Union advanced all clocks by one hour, Moscow Time was now GMT+3 and Irkutsk Time GMT+8. On 1 April 1981, daylight saving time was re-introduced, clocks were moved one hour forward on 1 April, on 1 April 1981,00,00,00, Oymyakonsky District changed its time zone from MSK+6 to MSK+8. The change occurred during DST effectively changing the offset from UTC+9 to UTC+12, on 1 April 1982,00,00,00, Chukotka Autonomous Okrug changed its time zone from MSK+10 to MSK+9, thus eliminating Anadyr Time. The change occurred during DST effectively changing the offset from UTC+14 to UTC+13, on 27 March 1988,02,00,00, Saratov and Volgograd oblasts changed its time zone from MSK+1 to MSK. The change occurred during DST effectively changing the offset from UTC+5 to UTC+4, on 23 May 1993,00,00,00, Novosibirsk Oblast changed its time zone from MSK+4 to MSK+3. The change occurred during DST effectively changing the offset from UTC+8 to UTC+7, on 28 May 1995,00,00,00, Altai Krai and Altai Republic changed its time zone from MSK+4 to MSK+3. On 30 March 1997,02,00,00, Sakhalin Oblast changed its time zone from MSK+8 to MSK+7, on 1 May 2002,03,00,00, Tomsk Oblast changed its time zone from MSK+4 to MSK+3. On 1 January 2004,00,00,00, New Siberian Islands, Tomponsky District, the following time zone changes occurred on 28 March 2010, which, in particular, led to abolition of two of the eleven time zones
10.
Vehicle registration plates of Russia
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Vehicle registration plates are the mandatory number plates used to display the registration mark of a vehicle, and have existed in Russia for many decades. Most motor vehicles which are used on roads are required by law to display them. The current format uses a letter followed by 3 digits and two more letters, to improve legibility of the numbers for Russian cars abroad, only a small subset of Cyrillic characters that look like Latin characters are used. Finally, the number and letters RUS are included, as well as the national flag. There is a different format for trailers, motorcycles, mopeds and scooters plates are made of square reflective plates and its format is 4 digits at the top and two letters at the bottom. Some autonomous regions are not required to have the flag on the licence plates, vehicles used by certain organisations or categories of persons carry special plates, Special plates in the above categories never carry the Russian flag, except for trailers. There are special reserved for government officials. The license plates for government officials originally had a larger flag instead of the regional code. Rich businessmen, prominent politicians and crime lords often use para-legally acquired special licence plates to get preferential treatment from the transport police, often, this is used in conjunction with a flashing siren. The Society of Blue Buckets is a protest movement that opposes this trend, as of 2014, there are new codes for Russian plates, number 82 for the Republic of Crimea and 92 for Sevastopol. The Russian Federation then officially annexed Crimea from Ukraine and now administers it as two federal subjects, the Republic of Crimea and the city of Sevastopol. Ukraine, backed by most of the community, refuses to accept the annexation. As per GOST provision, only 1,726,272 combinations may be issued within one administration unit, in certain regions, the amount of vehicles exceeds that number, and the combination may not be reused after a vehicle was taken off the registration. All this creates an issue of running out of numbers, a short-term solution was introducing more codes for those regions. Introduction of new license plate is being considered as a future solution. In the following years some codes were reassigned or discontinued, as the populous regions started running out of license plate combinations, new codes past code 89 were assigned to them as well. Additional triple-digit codes were created by adding a 1 or a 7 to the regional code. According to the Ministry of Internal Affairs Order 282 from March 28,2002, 1Code 059 is a former code for Syria
11.
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
12.
Romanization of Russian
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Romanization of the Russian alphabet is the process of transliterating the Russian language from the Cyrillic script into the Latin alphabet. Scientific transliteration, also known as the International Scholarly System, is a system that has used in linguistics since the 19th century. It is based on the Czech alphabet and formed the basis of the GOST, OST8483 was the first Soviet standard on romanization of Russian, introduced in 16 October 1935. This standard is an equivalent of GOST 16876-71 and was adopted as a standard of the COMECON. GOST7. 79-2000 System of Standards on Information, Librarianship and it is the official standard of both Russia and the Commonwealth of Independent States. Machine readable passports is an adoption of an ICAO stadards for travel documents and it was used in Russian passports for a short period during 2010–2013. The standard was substituted in 2013 by GOST R ISO/IEC 7501-1-2013, which does not contain romanization, ISO/R9, established in 1954 and updated in 1968, was the adoption of the scientific transliteration by the International Organization for Standardization. It covers Russian and seven other Slavic languages, ISO9,1995 is the current transliteration standard from ISO. It is based on its predecessor ISO/R9,1968, which it deprecates, for Russian, the UNGEGN, a Working Group of the United Nations, in 1987 recommended a romanization system for geographical names, which was based on the 1983 version of GOST 16876-71. It may be found in some international cartographic products, American Library Association and Library of Congress romanization tables for Slavic alphabets are used in North American libraries and in the British Library since 1975. The formal, unambiguous version of the system requires some diacritics and two-letter tie characters, British Standard 2979,1958 is the main system of the Oxford University Press, and a variation was used by the British Library to catalogue publications acquired up to 1975. The BGN/PCGN system is relatively intuitive for Anglophones to read and pronounce, the portion of the system pertaining to the Russian language was adopted by BGN in 1944 and by PCGN in 1947. In Soviet international passports, transliteration was based on French rules, in 1997, with the introduction of new Russian passports, a diacritic-free English-oriented system was established by the Ministry of Internal Affairs, but this system was also abandoned in 2010. In 2006, GOST52535. 1-2006 was adopted, which defines technical requirements and standards for Russian international passports, in 2010, the Federal Migratory Service of Russia approved Order No. 26, stating that all names in the passports issued after 2010 must be transliterated using GOST52535. 1-2006. The standard was abandoned in 2013, finally in 2013, Order No.320 of the Federal Migratory Service of Russia came into force. It states that all names in the passports must be transliterated using the ICAO system. This system differs from the GOST52535. 1-2006 system in two things, ц is transliterated into ts, ъ is transliterated into ie, Scholarly ¹ Some archaic letters are transcribed in different ways
13.
Russian Census (2010)
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The Russian Census of 2010 is the first census of the Russian Federation population since 2002 and the second after the dissolution of the Soviet Union. Preparations for the census began in 2007 and it took place between October 14 and October 25, the census was originally scheduled for October 2010, but was moved to 2013 allegedly for financial reasons, although it was also speculated that political motives were influential in the decision. However, in late 2009 Russian Prime Minister Vladimir Putin announced that the Government of Russia allocated 10.5 billion rubles in order to conduct the census as originally scheduled, Results showed the population to stand at 142.9 million. Since the previous 2002 census, population has decreased by 2.3 million, according to the 2010 census, urban population is 105.3 million, rural population is 37.5 million. The urbanisation rate is currently 73. 7%, the median age is 38 years. The ethnic composition is dominated by Russians, demographics of Russia Russian Census 2010 final results Results of 2010 All-Russia population census Official website of the 2010 Census
14.
Kola Peninsula
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The Kola Peninsula is a peninsula in the far northwest of Russia. The city of Murmansk is the most populous human settlement on the peninsula, summers are rather chilly, with the average July temperature of only 11 °C. The peninsula is covered by taiga in the south and tundra in the north, the peninsula supports a small variety of mammals, and its rivers are an important habitat for the Atlantic salmon. The Kandalaksha Nature Reserve, established to protect the population of eider, is located in the Kandalaksha Gulf. However, by the 1st millennium CE only the Sami people remained and this changed in the 12th century, when Russian Pomors discovered the peninsulas game and fish riches. Soon after, the Pomors were followed by the tribute collectors from the Novgorod Republic, no permanent settlements, however, were established by the Novgorodians until the 15th century. The Novgorod Republic lost control of the peninsula to the Grand Duchy of Moscow in 1471, several new settlements were established during the 16th century, and the Sami and Pomor people were forced into serfdom. The original administrative and economic center of the area was Kola, however, in 1916, Romanov-na-Murmane was founded and quickly became the largest city and port on the peninsula. The Soviet period saw an increase of the population, although most of it remained confined to urbanized territories along the sea coast. As a result, the ecology of the peninsula suffered major damage, including contamination by military nuclear waste. After the dissolution of the Soviet Union, the economy went into decline, between 1989 and 2002, Murmansk Oblast lost almost a quarter of its population, and almost 100,000 more between 2002 and 2010. Nevertheless, the economy rebounded somewhat in the first decade of the 2000s, the peninsula is located in the far northwest of Russia, almost completely inside the Arctic Circle and is washed by the Barents Sea in the north and the White Sea in the east and southeast. Geologically, the peninsula occupies the edge of the Baltic Shield. Under a more restrictive definition, the covers a area of about 100,000 square kilometers. The northern coast is steep and high, while the southern coast is flat, the Keyvy drainage divide lies in the central part. The mountainous reliefs of the Murman and Kandalaksha Coasts stretch from southeast to northwest, deposits of construction materials such as granite, quartzite, and limestone are also abundant. Diatomaceous earth deposits are common near lakes and are used to produce insulation, cyclones are typical during the cold seasons, while the warm seasons are characterized by anticyclones. Monsoon winds are common in most areas, with south and southwesterly winds prevailing in winter months, strong storm winds blow for 80–120 days a year
15.
Arctic Circle
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The Arctic Circle is the most northerly of the abstract five major circles of latitude as shown on maps of the Earth. The region north of this circle is known as the Arctic, the position of the Arctic Circle is not fixed, as of 7 April 2017, it runs 66°33′46. 6″ north of the Equator. Its latitude depends on the Earths axial tilt, which fluctuates within a margin of 2° over a 40, 000-year period, consequently, the Arctic Circle is currently drifting northwards at a speed of about 15 m per year. The word arctic comes from the Greek word ἀρκτικός and that from the word ἄρκτος, directly on the Arctic Circle these events occur, in principle, exactly once per year, at the June and December solstices, respectively. That is true at sea level, those limits increase with elevation above sea level, tens of thousands of years ago, waves of people migrated from eastern Siberia across the Bering Strait into North America to settle. Much later, in the period, there has been migration into some Arctic areas by Europeans. The largest communities north of the Arctic Circle are situated in Russia and Norway, Murmansk, Norilsk, Tromsø, rovaniemi in Finland is the largest settlement in the immediate vicinity of the Arctic Circle, lying slightly south of the line. In contrast, the largest North American community north of the Arctic Circle, of the Canadian and United States Arctic communities, Barrow, Alaska is the largest settlement with about 4,000 inhabitants. The Arctic Circle is roughly 16,000 kilometres, the area north of the Circle is about 20,000,000 km2 and covers roughly 4% of Earths surface. The Arctic Circle passes through the Arctic Ocean, the Scandinavian Peninsula, North Asia, Northern America, the land within the Arctic Circle is divided among eight countries, Norway, Sweden, Finland, Russia, the United States, Canada, Denmark, and Iceland. In the interior, summers can be warm, while winters are extremely cold
16.
Republic of Karelia
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The Republic of Karelia is a federal subject of Russia, located in the northwest of Russia. Its capital is the city of Petrozavodsk and its population in 2010 was 643,548. From 1940 to 1956, it was known as the Karelo-Finnish Soviet Socialist Republic, in 1956, it was once again an autonomous republic and remains as part of Russia after the dissolution of the Soviet Union in 1991. The republic is in the part of Russia, taking intervening position between the White and Baltic Seas. The White Sea has a line of 630 kilometers. It has an area of 172,400 km2 and it shares internal borders with Murmansk Oblast, Arkhangelsk Oblast, Vologda Oblast, and Leningrad Oblast, and it also borders Finland, the borders measure 723 km. The main bodies of water next to Karelia are the White Sea to the north-east and Lake Onega and its highest point is the Nuorunen peak at 576 m. This area is the largest contiguous Archaean outcrop in Europe and one of the largest in the world, There are about 27,000 rivers in Karelia. Major rivers include, Vodla River Kem River Kovda River Shuya River Suna River with Kivach Falls Vyg River There are 60,000 lakes in Karelia, the republics lakes and swamps contain about 2,000 km³ of high-quality fresh water. Lake Ladoga and Lake Onega are the largest lakes in Europe, other lakes include, Nyukozero Pyaozero Segozero Syamozero Topozero Vygozero Lakes Ladoga and Onega are located on the south of the republic. Vodlozero National Park Kalevala National Park Paanajärvi National Park The majority of the territory is composed of state forest stock. The total growing stock of resources in the forests of all categories and ages is 807 million m³. The mature and over mature tree stock amounts to 411.8 million m³, fifty useful minerals are found in Karelia, located in more than 400 deposits and ore bearing layers. Natural resources of the republic include iron ore, diamonds, vanadium, molybdenum, the Republic of Karelia is located in the Atlantic continental climate zone. Average temperature in January is −8.0 °C and +16.4 °C in July, average annual precipitation is 500–700 mm. Historically, Karelia was a region to the northwest of Russia, east of present-day Finland, controlled by the Novgorod Republic. From the 13th century and onwards, various parts were conquered by Sweden, in 1920, the province became the Karelian Labour Сommune. In 1923, the became the Karelian Autonomous Soviet Socialist Republic. Annexed territories were incorporated into Karelo-Finnish SSR, but after the Continuation War the Karelian Isthmus was incorporated into the Leningrad Oblast and its status was changed back to an ASSR in 1956
17.
Lapland (Finland)
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Lapland is the largest and northernmost region of Finland. The municipalities in the region cooperate in a Regional Council, Lapland borders the region of Northern Ostrobothnia in the south. It also borders the Gulf of Bothnia, Norrbotten County in Sweden, Finnmark County and Troms County in Norway, and Murmansk Oblast and the Republic of Karelia in Russia. The area of Lapland region is 100,367 km², which consists of 92,667 km²of dry land,6,316 km² fresh water and 1,383 km² of sea areas. In south it borders Northern Ostrobothnia region, in west Sweden, in north and west Norway and its borders follow three rivers, Tana, Muonio and Torne. The largest lake is Lake Inari,1,102 km², highest point is on Halti, which reaches 1,324 m on Finnish side of the border. There are eight national parks in Lapland, Bothnian Bay, Lemmenjoki, Oulanka, Pallas-Yllästunturi, Pyhä-Luosto, Riisitunturi, Syöte, the very first snowflakes fall to the ground in late August or early September over the higher peaks. The first ground-covering snow arrives in average in October or late September, permanent snow cover comes between mid-October and end of November, significantly earlier than in southern Finland. The winter is long, approximately seven months, the snow cover is usually thickest in early April. Soon after that the snow starts to melt fast. The thickest snow cover ever was measured in Kilpisjärvi in 19 April 1997, due to the warming effect of the Arctic Sea, the coldest spot is not located in northernmost Lapland but in the north-western corner. The annual mean temperature varies from a couple of degrees below zero in Northwest to a couple of degrees above zero in the southwest, the area of Lapland was split between two counties of the Swedish Realm from 1634 to 1809. The northern and western areas were part of Västerbotten County, while the areas were part of Ostrobothnia County. The northern and western areas were transferred in 1809 to Oulu County, under the royalist constitution of Finland during the first half of 1918, Lapland was to become a Grand Principality and part of the inheritance of the proposed king of Finland. Lapland Province was separated from Oulu Province in 1938, during the Interim Peace and beginning of the Continuation War the government of Finland allowed the Nazi German Army to station itself in Lapland as a part of Operation Barbarossa. After Finland made a peace with the Soviet Union in 1944. The result was the Lapland War, during which almost the whole population of Lapland was evacuated. The Germans used scorched earth tactics in Lapland, before they withdrew to Norway, ninety percent of Rovaniemi, the capital of Lapland, was burned to the ground, with only a few pre-war buildings surviving the destruction
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Finland
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Finland, officially the Republic of Finland, is a sovereign state in Northern Europe. A peninsula with the Gulf of Finland to the south and the Gulf of Bothnia to the west, the country has borders with Sweden to the northwest, Norway to the north. Estonia is south of the country across the Gulf of Finland, Finland is a Nordic country situated in the geographical region of Fennoscandia, which also includes Scandinavia. Finlands population is 5.5 million, and the majority of the population is concentrated in the southern region,88. 7% of the population is Finnish people who speak Finnish, a Uralic language unrelated to the Scandinavian languages, the second major group are the Finland-Swedes. In terms of area, it is the eighth largest country in Europe, Finland is a parliamentary republic with a central government based in the capital Helsinki, local governments in 311 municipalities, and an autonomous region, the Åland Islands. Over 1.4 million people live in the Greater Helsinki metropolitan area, from the late 12th century, Finland was an integral part of Sweden, a legacy reflected in the prevalence of the Swedish language and its official status. In the spirit of the notion of Adolf Ivar Arwidsson, we are not Swedes, we do not want to become Russians, let us therefore be Finns, nevertheless, in 1809, Finland was incorporated into the Russian Empire as the autonomous Grand Duchy of Finland. In 1906, Finland became the nation in the world to give the right to vote to all adult citizens. Following the 1917 Russian Revolution, Finland declared itself independent, in 1918, the fledgling state was divided by civil war, with the Bolshevik-leaning Reds supported by the equally new Soviet Russia, fighting the Whites, supported by the German Empire. After a brief attempt to establish a kingdom, the became a republic. During World War II, the Soviet Union sought repeatedly to occupy Finland, with Finland losing parts of Karelia, Salla and Kuusamo, Petsamo and some islands, Finland joined the United Nations in 1955 and established an official policy of neutrality. The Finno-Soviet Treaty of 1948 gave the Soviet Union some leverage in Finnish domestic politics during the Cold War era, Finland was a relative latecomer to industrialization, remaining a largely agrarian country until the 1950s. It rapidly developed an advanced economy while building an extensive Nordic-style welfare state, resulting in widespread prosperity, however, Finnish GDP growth has been negative in 2012–2014, with a preceding nadir of −8% in 2009. Finland is a top performer in numerous metrics of national performance, including education, economic competitiveness, civil liberties, quality of life, a large majority of Finns are members of the Evangelical Lutheran Church, though freedom of religion is guaranteed under the Finnish Constitution. The first known appearance of the name Finland is thought to be on three rune-stones. Two were found in the Swedish province of Uppland and have the inscription finlonti, the third was found in Gotland, in the Baltic Sea. It has the inscription finlandi and dates from the 13th century, the name can be assumed to be related to the tribe name Finns, which is mentioned first known time AD98. The name Suomi has uncertain origins, but a candidate for a source is the Proto-Baltic word *źemē, in addition to the close relatives of Finnish, this name is also used in the Baltic languages Latvian and Lithuanian
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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
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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
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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
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White Sea
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The White Sea is a southern inlet of the Barents Sea located on the northwest coast of Russia. It is surrounded by Karelia to the west, the Kola Peninsula to the north, the whole of the White Sea is under Russian sovereignty and considered to be part of the internal waters of Russia. Administratively, it is divided between Arkhangelsk and Murmansk Oblasts and the Republic of Karelia, the major port of Arkhangelsk is located on the White Sea. For much of Russias history this was Russias main centre of maritime trade. In the modern era it became an important Soviet naval and submarine base, the White Sea-Baltic Canal connects the White Sea with the Baltic Sea. The White Sea is one of four seas named in English after common colour terms — the others being the Black Sea, the Red Sea, the International Hydrographic Organization defines the northern limit of the White Sea as A line joining Svyatoi Nos and Cape Kanin. There are four main bays or gulfs on the White Sea and these bays connect with the funnel-shaped opening to the Barents Sea via a narrow strait called gorlo. Kandalaksha Gulf lies in the part of the White Sea, it is the deepest part of the sea. On the south, Onega Bay receives the Onega River, to the southeast, the Dvina Bay receives the Northern Dvina River at the major port of Arkhangelsk. On the east side of the gorlo, opposite the Kola peninsula, is Mezen Bay and it receives the Mezen River and the Kuloy River. Other major rivers flowing into the sea are the Vyg, Niva, Umba, Varzuga and Ponoy. The seabed of the part and Dvina Bay is covered in silt and sand, whereas the bottom of the northern part. Ice age deposits often emerge near the sea shores, northwestern coasts are tall and rocky but the slope is much weaker at the southeastern side. The White Sea contains a number of islands, but most of them are small. The main island group is the Solovetsky Islands, located almost in the middle of the sea, kiy Island in Onega Bay is significant due to a historic monastery. Velikiy Island, located close to the shore, is the largest island in the Kandalaksha Gulf, the White Sea is a water-filled depression in the block of a continental shelf known as the Baltic Shield. Its bottom is very uneven and contains the Kandalaksha Hollow in the northwest, also, the Onega Bay has many small underwater elevations. The opening and the gorlo of the sea are rather shallow, in addition, there is an underwater ridge in the northern part of the gorlo, resulting in maximum depths of 40 metres in that part
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Arkhangelsk Oblast
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Arkhangelsk Oblast is a federal subject of Russia. It includes the Arctic archipelagos of Franz Josef Land and Novaya Zemlya, Arkhangelsk Oblast also has administrative jurisdiction over Nenets Autonomous Okrug. Including Nenetsia, Arkhangelsk Oblast has an area of 587,400 km2 and its population was 1,227,626 as of the 2010 Census. The city of Arkhangelsk, with a population of 348,716 as of the 2010 Census, is the center of the oblast. The second largest city is the nearby Severodvinsk, home to Sevmash, Plesetsk Cosmodrome is one of three spaceports in Russia. Arkhangelsk Oblast, which includes Nenets Autonomous Okrug, borders Kirov Oblast, Vologda Oblast, the Republic of Karelia, the Komi Republic, Cape Fligely in Franz Josef Land and Cape Zhelaniya in Novaya Zemlya are both located within Arkhangelsk Oblast. Arkhangelsk Oblast is located on the East European Plain, and most of it represents forested hilly landscape, the north-eastern part belongs to the Timan Ridge, a highland mostly situated east from the oblast. The Nenets Autonomous Okrug is essentially a flat tundra with several hill chains like Pay-Khoy Ridge, the Arctic islands including Novaya Zemlya and Franz Joseph Land are mountainous with glaciers and eternally snow-covered. This region has a distinct population of polar bears associated with the Barents Sea area. Almost all of the area of the Oblast belongs to the basin of the Arctic Ocean, with the rivers being Onega River, Northern Dvina River, Kuloy River, Mezen River. A minor area in the west of the Oblast, most notably the basin of the Ileksa River, drains into the Lake Onega and eventually to the Baltic Sea. A very minor area in Kargopolsky District in the south-west of the Oblast drains into the Kema River which belongs to the basin of the Caspian Sea. The area in the Onega River basin containing the biggest lakes in the oblast, such as Lake Lacha, Lake Kenozero, Lake Undozero, the tundra of the Nenets Autonomous Okrug also contains a number of bigger lakes. The river basin of the Pinega is characteristic of the karst, the White Sea coast within the Oblast is split into the Onega Bay, the Dvina Bay, and the Mezen Bay. Solovetsky Islands, as well as a number of islands, are located in the Onega Bay. The Onega Bay and the Dvina Bay are separated by the Onega Peninsula, the Mezen Bay is separated from the main body of the White Sea by Morzhovets Island. Almost all of the oblast is covered by taiga, the coniferous forest dominated by pine, spruce, large areas in the middle of taiga are devoid of trees and covered by swamps. In the floodplains of the rivers, there are meadows, a number of areas in Arkhangelsk Oblast have been designated as protected natural areas
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Khibiny Mountains
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The massif is of oval shape of about 1,300 km2. and occupies the central part of the peninsula at a relative elevation of 900–1000 m above the surrounding plain. The mountains are not particularly high, the two highest peaks are the Yudychvumchorr, which stands 1,201 metres, and the Chasnachorr, the average elevation is 1,116 metres. The mountains form the shape of a horseshoe topped by a high plateau, the peaks are of plateau type, with steep slopes, with glaciers, icefields and snowfields in some places. The overall terrain is alpine tundra, the second, and similar mountain range of the Kola Peninsula, the Lovozero Tundras, is located about 5 km east from the easternmost point of Khibiny. The Khibiny range is rich in minerals, mainly apatite. 477 valid minerals have been reported and 108 of those are type localities or minerals first described in the Khibiny, the range is also seismically active. Khibiny mountains are mostly uninhabited, except for one of the worlds richest mineral quarries, one of the minerals discovered there is reported to have a potential as a nuclear waste radioactivity absorbent. By the foot of the massif the cities of Apatity and Kirovsk are situated, the Khibiny Mountains lie within the Kola Peninsula, a large peninsula extending from northern Russia into the Barents and White seas. The total land area of the peninsula is approximately 100,000 square kilometres and it is rich in minerals due to the removal of a layer of soil during the last ice age. Khibiny have an Arctic-moderate climate, with a winter temperature of −5 °C. However, the temperature can drop to −30 °C during the night. The Gulf Stream, which brings water to the Kolsky Peninsula from the north, moderates the climate, making it slightly warmer than other Arctic regions. info Khibiny geology
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Lovozero Massif
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The slopes are covered mainly with spruce and pine. The highest point is Mount Angvundaschorr, the area around the lake is inhabited by Saami, and many place names are of non-Russian origin. The Lovozero Massif is underlain by a complex of agpaitic to hyperagpaitic rocks containing minerals as eudialyte, loparite, natrosilite, at least 105 valid minerals have been described in the massif and 39 minerals were initially discovered there. The only other areas with similar geology and mineralogy are Khibiny Massif, Ilimaussaq in SW Greenland and Mont-Saint-Hilaire, Quebec, the area is relatively well accessible from railroads. In winter the area is accessible from Khibiny Mountains via the ice of Umbozero, in summer there are usable mountain roads and trails. P. Mineralogy of Hyperagpaitic Alkaline Rocks Clarendon Press 1995 Lovozero Tundras, In Russian Geology and minerals
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Sea level
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Mean sea level is an average level of the surface of one or more of Earths oceans from which heights such as elevations may be measured. A common and relatively straightforward mean sea-level standard is the midpoint between a low and mean high tide at a particular location. Sea levels can be affected by factors and are known to have varied greatly over geological time scales. The careful measurement of variations in MSL can offer insights into ongoing climate change, the term above sea level generally refers to above mean sea level. Precise determination of a sea level is a difficult problem because of the many factors that affect sea level. Sea level varies quite a lot on several scales of time and this is because the sea is in constant motion, affected by the tides, wind, atmospheric pressure, local gravitational differences, temperature, salinity and so forth. The easiest way this may be calculated is by selecting a location and calculating the mean sea level at that point, for example, a period of 19 years of hourly level observations may be averaged and used to determine the mean sea level at some measurement point. One measures the values of MSL in respect to the land, hence a change in MSL can result from a real change in sea level, or from a change in the height of the land on which the tide gauge operates. In the UK, the Ordnance Datum is the sea level measured at Newlyn in Cornwall between 1915 and 1921. Prior to 1921, the datum was MSL at the Victoria Dock, in Hong Kong, mPD is a surveying term meaning metres above Principal Datum and refers to height of 1. 230m below the average sea level. In France, the Marégraphe in Marseilles measures continuously the sea level since 1883 and it is used for a part of continental Europe and main part of Africa as official sea level. Elsewhere in Europe vertical elevation references are made to the Amsterdam Peil elevation, satellite altimeters have been making precise measurements of sea level since the launch of TOPEX/Poseidon in 1992. A joint mission of NASA and CNES, TOPEX/Poseidon was followed by Jason-1 in 2001, height above mean sea level is the elevation or altitude of an object, relative to the average sea level datum. It is also used in aviation, where some heights are recorded and reported with respect to sea level, and in the atmospheric sciences. An alternative is to base height measurements on an ellipsoid of the entire Earth, in aviation, the ellipsoid known as World Geodetic System 84 is increasingly used to define heights, however, differences up to 100 metres exist between this ellipsoid height and mean tidal height. The alternative is to use a vertical datum such as NAVD88. When referring to geographic features such as mountains on a topographic map, the elevation of a mountain denotes the highest point or summit and is typically illustrated as a small circle on a topographic map with the AMSL height shown in metres, feet or both. In the rare case that a location is below sea level, for one such case, see Amsterdam Airport Schiphol
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Tundra
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In physical geography, tundra is a type of biome where the tree growth is hindered by low temperatures and short growing seasons. The term tundra comes through Russian тундра from the Kildin Sami word tūndâr uplands, there are three types of tundra, Arctic tundra, alpine tundra, and Antarctic tundra. In tundra, the vegetation is composed of shrubs, sedges and grasses, mosses. Scattered trees grow in tundra regions. The ecotone between the tundra and the forest is known as the line or timberline. Arctic tundra occurs in the far Northern Hemisphere, north of the taiga belt, the word tundra usually refers only to the areas where the subsoil is permafrost, or permanently frozen soil. Permafrost tundra includes vast areas of northern Russia and Canada, the polar tundra is home to several peoples who are mostly nomadic reindeer herders, such as the Nganasan and Nenets in the permafrost area. Arctic tundra contains areas of landscape and is frozen for much of the year. The soil there is frozen from 25–90 cm down, and it is impossible for trees to grow, instead, bare and sometimes rocky land can only support low growing plants such as moss, heath, and lichen. There are two seasons, winter and summer, in the polar tundra areas. During the winter it is cold and dark, with the average temperature around −28 °C. However, extreme temperatures on the tundra do not drop as low as those experienced in taiga areas further south. During the summer, temperatures rise somewhat, and the top layer of seasonally-frozen soil melts, the tundra is covered in marshes, lakes, bogs and streams during the warm months. Generally daytime temperatures during the rise to about 12 °C. Arctic tundras are sometimes the subject of conservation programs. In Canada and Russia, many of areas are protected through a national Biodiversity Action Plan. Tundra tends to be windy, with winds often blowing upwards of 50–100 km/h, however, in terms of precipitation, it is desert-like, with only about 15–25 cm falling per year. Although precipitation is light, evaporation is also relatively minimal, there is a natural pattern of accumulation of fuel and wildfire which varies depending on the nature of vegetation and terrain
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Taiga
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Taiga also known as boreal forest or snow forest, is a biome characterized by coniferous forests consisting mostly of pines, spruces and larches. The taiga is the worlds largest biome apart from the oceans, in North America it covers most of inland Canada and Alaska as well as parts of the extreme northern continental United States, where it is known as the Northwoods or North woods. However, the tree species, the length of the growing season. Hoffman discusses the origin of this use in North America. Although at high elevations taiga grades into alpine tundra through Krummholz, it is not an alpine biome only like subalpine forest, Taiga is the worlds largest land biome, and makes up 29% of the worlds forest cover, the largest areas are located in Russia and Canada. The taiga is the terrestrial biome with the lowest annual average temperatures after the tundra, extreme winter minimums in the northern taiga are typically lower than those of the tundra. The lowest reliably recorded temperatures in the Northern Hemisphere were recorded in the taiga of northeastern Russia, the taiga or boreal forest has a subarctic climate with very large temperature range between seasons, but the long and cold winter is the dominant feature. This climate is classified as Dfc, Dwc, Dsc, Dfd and Dwd in the Köppen climate classification scheme, meaning that the summer lasts 1–3 months. In Siberian taiga the average temperature of the coldest month is between −6 °C and −50 °C, the mean annual temperature generally varies from -5 °C to 5 °C, but there are taiga areas in eastern Siberia and interior Alaska-Yukon where the mean annual reaches down to -10 °C. According to some sources, the boreal forest grades into a mixed forest when mean annual temperature reaches about 3 °C. The winters, with temperatures below freezing, last five to seven months. Temperatures vary from −54 °C to 30 °C throughout the whole year, the summers, while short, are generally warm and humid. In much of the taiga, -20 °C would be a winter day temperature and 18 °C an average summer day. In Canada, Scandinavia and Finland, the season is often estimated by using the period of the year when the 24-hour average temperature is +5 °C or more. For the Taiga Plains in Canada, growing season varies from 80 to 150 days, some sources claim 130 days growing season as typical for the taiga. Other sources mention that 50–100 frost-free days are characteristic, data for locations in southwest Yukon gives 80–120 frost-free days. The closed canopy boreal forest in Kenozersky National Park near Plesetsk, Arkhangelsk Province, Russia, the longest growing season is found in the smaller areas with oceanic influences, in coastal areas of Scandinavia and Finland, the growing season of the closed boreal forest can be 145–180 days. High latitudes mean that the sun not rise far above the horizon
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Gulf Stream
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The process of western intensification causes the Gulf Stream to be a northward accelerating current off the east coast of North America. At about 40°0′N 30°0′W, it splits in two, with the stream, the North Atlantic Drift, crossing to Northern Europe and the southern stream. The Gulf Stream influences the climate of the east coast of North America from Florida to Newfoundland, and it is part of the North Atlantic Gyre. Its presence has led to the development of strong cyclones of all types, the Gulf Stream is also a significant potential source of renewable power generation. The Gulf Stream may be slowing down as a result of climate change, the Gulf Stream is typically 100 kilometres wide and 800 metres to 1,200 metres deep. The current velocity is fastest near the surface, with the maximum speed typically about 2.5 metres per second. European discovery of the Gulf Stream dates to the 1512 expedition of Juan Ponce de León and its existence was also known to Peter Martyr dAnghiera. Benjamin Franklin became interested in the North Atlantic Ocean circulation patterns, Franklin asked Timothy Folger, his cousin twice removed, a Nantucket Island whaling captain, for an answer. Franklin worked with Folger and other experienced ship captains, learning enough to chart the Gulf Stream and he offered this information to Anthony Todd, secretary of the British Post Office, but it was ignored by British sea captains. Franklins Gulf Stream chart was published in 1770 in England, where it was mostly ignored, subsequent versions were printed in France in 1778 and the U. S. in 1786. The Gulf Stream proper is a current, driven largely by wind stress. The North Atlantic Drift, in contrast, is largely thermohaline circulation–driven, in 1958 the oceanographer Henry Stommel noted that very little water from the Gulf of Mexico is actually in the Stream. By carrying warm water northeast across the Atlantic, it makes Western, a river of sea water, called the Atlantic North Equatorial Current, flows westward off the coast of Central Africa. When this current interacts with the northeastern coast of South America, one passes into the Caribbean Sea, while a second, the Antilles Current, flows north and east of the West Indies. These two branches north of the Straits of Florida. The trade winds blow westward in the tropics, and the westerlies blow eastward at mid-latitudes and this wind pattern applies a stress to the subtropical ocean surface with negative curl across the north Atlantic Ocean. The resulting Sverdrup transport is equatorward, the conservation of potential vorticity also causes bends along the Gulf Stream, which occasionally break off due to a shift in the Gulf Streams position, forming separate warm and cold eddies. This overall process, known as western intensification, causes currents on the boundary of an ocean basin, such as the Gulf Stream
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Precipitation
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In meteorology, precipitation is any product of the condensation of atmospheric water vapor that falls under gravity. The main forms of precipitation include drizzle, rain, sleet, snow, graupel, Precipitation occurs when a portion of the atmosphere becomes saturated with water vapor, so that the water condenses and precipitates. Thus, fog and mist are not precipitation but suspensions, because the vapor does not condense sufficiently to precipitate. Two processes, possibly acting together, can lead to air becoming saturated, Precipitation forms as smaller droplets coalesce via collision with other rain drops or ice crystals within a cloud. Short, intense periods of rain in scattered locations are called showers, moisture that is lifted or otherwise forced to rise over a layer of sub-freezing air at the surface may be condensed into clouds and rain. This process is active when freezing rain is occurring. A stationary front is often present near the area of freezing rain, provided necessary and sufficient atmospheric moisture content, the moisture within the rising air will condense into clouds, namely stratus and cumulonimbus. Eventually, the droplets will grow large enough to form raindrops. Lake-effect snowfall can be locally heavy, thundersnow is possible within a cyclones comma head and within lake effect precipitation bands. In mountainous areas, heavy precipitation is possible where upslope flow is maximized within windward sides of the terrain at elevation, on the leeward side of mountains, desert climates can exist due to the dry air caused by compressional heating. The movement of the trough, or intertropical convergence zone. Precipitation is a component of the water cycle, and is responsible for depositing the fresh water on the planet. Approximately 505,000 cubic kilometres of water falls as precipitation each year,398,000 cubic kilometres of it over the oceans and 107,000 cubic kilometres over land. Given the Earths surface area, that means the globally averaged annual precipitation is 990 millimetres, Climate classification systems such as the Köppen climate classification system use average annual rainfall to help differentiate between differing climate regimes. Precipitation may occur on celestial bodies, e. g. when it gets cold, Mars has precipitation which most likely takes the form of frost. Precipitation is a component of the water cycle, and is responsible for depositing most of the fresh water on the planet. Approximately 505,000 km3 of water falls as precipitation each year,398,000 km3 of it over the oceans, given the Earths surface area, that means the globally averaged annual precipitation is 990 millimetres. Mechanisms of producing precipitation include convective, stratiform, and orographic rainfall, Precipitation can be divided into three categories, based on whether it falls as liquid water, liquid water that freezes on contact with the surface, or ice
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Murman Coast
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The Murman Coast is a coastal area in Murmansk Oblast in northwest Russia. It is located on the side of the Barents Sea. The major rivers flowing to the sea at the coast are the Tuloma, administratively, the Murman Coast is shared between Pechengsky, Kolsky and Lovozersky Districts of Murmansk Oblast and Zaozyorsk, Vidyayevo, Aleksandrovsk, Murmansk, Severomorsk, Ostrovnoy. The cities of Zaozyorsk, Gadzhiyevo, Polyarny, Snezhnogorsk, Murmansk Oblast, Murmansk, Kola, Severomorsk, the coast was populated not later than 13th century by the Pomors and Norwegians. Murman Coast is included into border security zone, intended to protect the borders of Russian Federation from unwanted activity, in order to visit the zone, a permit issued by the local FSB department is required
32.
Sami people
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The Sami people are an indigenous Finno-Ugric people inhabiting the Arctic area of Sápmi, which today encompasses parts of far northern Norway, Sweden, Finland, and the Kola Peninsula of Russia. The Sami are the indigenous people of Scandinavia recognized and protected under the international conventions of indigenous peoples. Sami ancestral lands are not well-defined and their traditional languages are the Sami languages and are classified as a branch of the Uralic language family. Traditionally, the Sami have pursued a variety of livelihoods, including fishing, fur trapping. Their best-known means of livelihood is semi-nomadic reindeer herding, currently about 10% of the Sami are connected to reindeer herding, providing them with meat, fur, and transportation. 2,800 Sami people are involved in herding on a full-time basis. For traditional, environmental, cultural, and political reasons, reindeer herding is legally reserved only for Sami people in regions of the Nordic countries. The Sámi are often known in other languages by the exonyms Lap, Lapp, some Sami regard these as pejorative terms, while others do not. Finn was the originally used by Norse speakers to refer to the Sami, as attested in the Icelandic Eddas. As Old Norse gradually developed into the separate Scandinavian languages, Swedes apparently took to using Finn exclusively to refer to inhabitants of Finland, Finnish immigrants to Northern Norway in the 18th and 19th centuries were referred to as Kvens to distinguish them from the Sami Finns. Ethnic Finns are a group from Sami. In fact, Saxo never explicitly connects the Sami with the two Laplands, there is another suggestion that it originally meant wilds. In Finland and Sweden, Lapp is common in names, such as Lappi, Lappeenranta and Lapinlahti in Finland. As already mentioned, Finn is an element in Norwegian place names. In the North Sámi language, láhppon olmmoš means a person who is lost, Sámi refer to themselves as Sámit or Sápmelaš, the word Sámi being inflected into various grammatical forms. It has been proposed that Sámi, Häme, and perhaps Suomi are of the origin and ultimately borrowed from the Baltic word *žēmē. The Baltic word is cognate with Slavic земля, which means land. The Sámi institutions—notably the parliaments, radio and TV stations, theatres, etc. —all use the term Sámi, including when addressing outsiders in Norwegian, Swedish, Finnish, or English
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Russians
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Russians are an East Slavic ethnic group native to Eastern Europe. The majority of Russians inhabit the state of Russia, while notable minorities exist in Ukraine, Kazakhstan. A large Russian diaspora exists all over the world, with numbers in the United States, Germany, Israel. Russians are the most numerous group in Europe. They are predominantly Orthodox Christians by religion, the Russian language is official in Russia, Belarus, Kazakhstan, Kyrgyzstan, and Tajikistan, and also spoken as a secondary language in many former Soviet states. There are two Russian words which are translated into English as Russians. One is русские, which most often means ethnic Russians, another is россияне, which means citizens of Russia. The former word refers to ethnic Russians, regardless of what country they live in, under certain circumstances this term may or may not extend to denote members of other Russian-speaking ethnic groups from Russia, or from the former Soviet Union. The latter word refers to all people holding citizenship of Russia, regardless of their ethnicity, translations into other languages often do not distinguish these two groups. The name of the Russians derives from the Rus people, the name Rus would then have the same origin as the Finnish and Estonian names for Sweden, Ruotsi and Rootsi. According to other theories the name Rus is derived from Proto-Slavic *roud-s-ь, the modern Russians formed from two groups of East Slavic tribes, Northern and Southern. The tribes involved included the Krivichs, Ilmen Slavs, Radimichs, Vyatiches, genetic studies show that modern Russians do not differ significantly from Belarusians and Ukrainians. Some ethnographers, like Zelenin, affirm that Russians are more similar to Belarusians, such Uralic peoples included the Merya and the Muromians. Outside archaeological remains, little is known about the predecessors to Russians in general prior to 859 AD when the Primary Chronicle starts its records and it is thought that by 600 AD, the Slavs had split linguistically into southern, western, and eastern branches. Later, both Belarusians and South Russians formed on this ethnic linguistic ground, the same Slavic ethnic population also settled the present-day Tver Oblast and the region of Beloozero. With the Uralic substratum, they formed the tribes of the Krivichs, in 2010, the worlds Russian population was 129 million people of which 86% were in Russia,11. 5% in the CIS and Baltic countries, with a further 2. 5% living in other countries. Roughly 111 million ethnic Russians live in Russia, 80% of whom live in the European part of Russia, ethnic Russians historically migrated throughout the area of former Russian Empire and Soviet Union, sometimes encouraged to re-settle in borderlands by the Tsarist and later Soviet government. On some occasions ethnic Russian communities, such as Lipovans who settled in the Danube delta or Doukhobors in Canada, after the Russian Revolution and Russian Civil War starting in 1917, many Russians were forced to leave their homeland fleeing the Bolshevik regime, and millions became refugees
34.
Murmansk Okrug
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Murmansk Okrug was an administrative division of the Russian SFSR, Soviet Union, which existed in 1927–1938. According to these resolutions, Murmansk Governorate was transformed into Murmansk Okrug, the okrug was not contiguous with the rest of Leningrad Oblast and was separated from it by the territory of the Karelian Autonomous Soviet Socialist Republic. Upon the transformation, the structure of the okrug has also been changed. Instead of the nine volosts into which Murmansk Governorate was divided and this time, however, the ethnic composition of the territory became a priority. On May 30,1927, the provision was extended to cover the Lapps, until 1928, the Sami and Samoyeds used the same forms of government as elsewhere on the Kola Peninsula—the selsoviets and the district executive committees. On October 25,1928, the list was reviewed by the Selsoviet Review Commission of the Organizational Department of Leningrad Oblast Executive Committee, in addition to these eight, Peyvo-Yarvinsky Selsoviet of Kolsko-Loparsky District was granted the status of the national Finnish selsoviet. The creation of the proposed ethnic Sami selsoviets was found to be impractical. The only exception was Babinsky Selsoviet, the creation of which did not succeed, the first scenario suggested the creation of the district on the territories of Ponoysky and Lovozersky Districts, with Ponoysky Selsoviet being left out. The second one suggested the creation of the district on parts of the territories of Ponoysky and Lovozersky Districts, namely in Iokangsky, Kamensky, Lumbovsky, Semiostrovsky, at the same time, the creation of another ethnic Sami district to the west was suggested. Zapadno-Laplandsky District, on the territories of Kolsko-Loparsky District where the Sami population was predominant, on December 25,1929, this project was amended and approved by the Administrative-Legislative Commission of the Committee of the North. Zapadno-Laplandsky District was to include the following selsoviets and settlements, Kildinsky, Notozersky, Babinsky, the territories of the Sami people, Girvasky, Pulozersky, Sami in Motovsky Selsoviet would remain in Alexandrovsky District. On January 10,1930 the Presidium of the VTsIK issued a letter on the procedures for establishing special ethnic administrative-territorial units for the ethnic minorities. By April 1,1930, seven ethnic Finnish selsoviets and one ethnic Norwegian selsoviet were established in Murmansk Okrug, discussions of the possibilities of establishing more ethnic selsoviets was ongoing in the executive committees of various levels. With the task of creating ethnic selsoviets completed, on May 26,1930 the okrug administrative commission returned to the discussion of the proposed ethnic districts. Ponoysky and Sosnovsky Selsoviets of Ponoysky District would be merged into Tersky District and this proposal was approved and sent on for further consideration to the administrative commission of the Leningrad Oblast Executive Committee. The proposal for creation of Zapadno-Laplandsky District, on the hand, was declined and returned to the Committee of the North as needing a revision. The discussion of the possibility of creating an ethnic Finnish district was postponed, the administrative commission of the Leningrad Oblast Executive Committee reviewed the proposal on July 31,1930. Alexandrovsky District within its borders was granted the status of an ethnic Finnish district
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Leningrad Oblast
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Leningrad Oblast is a federal subject of Russia. It was established on August 1,1927, although it was not until 1946 that the borders had been mostly settled in their present position. The oblast was named after the city of Leningrad, the first governor of Leningrad Oblast was Vadim Gustov. The current governor, since 2012, is Alexander Drozdenko, the oblast has an area of 84,500 square kilometers and a population of 1,716,868, up from 1,669,205 recorded in the 2002 Census. The most populous town of the oblast is Gatchina, with 88,659 inhabitants, Leningrad Oblast is located around the Gulf of Finland and south of two great lakes of the European Part of Russia, Lake Ladoga and Lake Onega. Its northeastern part, between the Gulf of Finland and Lake Ladoga, occupies the Karelian Isthmus, some islands in the Gulf of Finland and Lake Ladoga also belong to the oblast. Much of the area of the oblast belongs to the basin of the Neva. Whereas the Neva, which flows to the Gulf of Finland is relatively short, its basin is enormously big and includes Lake Onega. The Svir and the Volkhov flow from Lake Onega and Lake Ilmen, respectively, other major tributaries of Lake Ladoga include the Vuoksi and the Syas. Rivers in the part of the oblast flow to the Gulf of Finland. Minor areas in the east of the oblast belong to the basin of the Chagodoshcha, a tributary of the Mologa. Thus, the divide between the basins of the Baltic and Caspian Seas crosses the oblast, the Karelian Isthmus is a rocky terrain which hosts a lake district. The biggest lakes on the Karelian Isthmus are Lake Vuoksa, Lake Sukhodolskoye, the rest of the area of the oblast is essentially flat. The exception is the Tikhvin Ridge, a chain of hills in the east of the oblast, most of the area is covered by forests and swamps. The most taxonomically diverse vascular plant families are Asteraceae, Cyperaceae, Poaceae and Rosaceae, by far the most diverse genus is Carex. The territory has no endemic plant taxa, the territory of present-day Leningrad Oblast was populated shortly after the end of the Weichsel glaciation and now hosts numerous archaeological remnants. The Volga trade route and trade route from the Varangians to the Greeks crossed the territory, staraya Ladoga, the first capital of legendary Rurik, founded in the 8th-9th century, is situated in the east of the oblast, on the Volkhov River. During the Russo-Swedish Wars of the 15th-17th centuries, the border moved back, ingrian Finns soon became the dominant ethnic group
36.
Kolsky District
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Kolsky District is an administrative district, one of the six in Murmansk Oblast, Russia. As a municipal division, it is incorporated as Kolsky Municipal District and it is located in the northwest of the oblast, partially lies on the Kola Peninsula, and borders with the Barents Sea in the north and Finland in the west. The area of the district is 27,600 square kilometers and its administrative center is the town of Kola. The population of Kola accounts for 23. 4% of the total population. Kolsky District is bordered on the west by Pechengsky District, on the southwest by Finland, the terrain is mostly flat forest and rocky tundra. The district mostly covers the Tuloma River and the Kola River, which flow north into Kola Bay, the Tuloma River flows out of Lake Notozero, which in turn is fed from the southwest by the Nota River and the Lutto. According to these resolutions, Murmansk Governorate was transformed into Murmansk Okrug, the administrative center of the district was in the selo of Kola. Upon establishment, the territory of the former Kolsko-Loparskaya Volost and of Minkinsky Selsoviet of the former Alexandrovskaya Volost were included into the district, according to this proposal, Kolsko-Loparsky District was to be abolished, with Kirovsky and Kolsky Districts to be established in its place. On February 15,1935, the VTsIK approved the redistricting of the okrug into seven districts, Minkinsky Selsoviet of Kolsko-Loparsky District was transferred to Polyarny District, and Kildinsky Selsoviet—to Lovozersky District. Kolsky, Notozersky, Peyvo-Yarvinsky, and Pulozersky Selsoviets, as well as the part of Ekostrovsky Selsoviet remained in Kolsko-Loparsky District. The administrative center of Kolsky District was slated to be moved to the station of Laplandiya, on June 1,1936, the renaming of the district was approved by the Resolution of the VTsIK. The provisions of the February 26,1935 Resolution, however, were not fully implemented, the station of Laplandiya ultimately never became the administrative center of the district, because Kola was not included into Murmansk as originally intended. On November 25,1935, the Presidium of the VTsIK granted work settlement status to the locality of Moncha-Guba. At the same time, it was transferred from Kolsky to Kirovsky District, when Polyarny District was abolished on July 9,1960, a part of its territory was transferred to Kolsky District. However, this only lasted for less than two years. By the August 2,1965 Presidium of the Supreme Soviet of the RSFSR Decree, Kolsky District has many natural resources, including forests, ore deposits and water life. Atlantic salmon is fished in the rivers of the district, ore deposits include copper, nickel, and titanium. The area also produces construction materials, the local representative body is the Council of Deputies of Kolsky District
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Lovozersky District
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Lovozersky District is an administrative district, one of the six in Murmansk Oblast, Russia. Municipally, it is incorporated as Lovozersky Municipal District and it occupies most of the central and northeastern parts of the Kola Peninsula. The area of the district is 53,800 square kilometers and its administrative center is the rural locality of Lovozero. The population of Lovozero accounts for 24. 3% of the total population. The territory of the district encompasses almost the entire half of the Kola Peninsula. The Ponoy and Yokanga Rivers flow through the districts territory, the Kandalaksha Nature Reserve, a federal-level strict ecological reserve, covers a portion of the Barents Sea coast on the north of Lovozersky District. According to these resolutions, Murmansk Governorate was transformed into Murmansk Okrug, the administrative center of the district was established in the selo of Lovozero. On July 31,1930, the commission of the Leningrad Executive Committee granted the district an ethnic status. The Presidium of the Leningrad Oblast Executive Committee confirmed this decision on January 7,1931, on February 15,1935, the VTsIK approved the redistricting of the okrug into seven districts, although it did not specify what territories the new districts were to include. However, Chalmny-Varrsky and Semiostrovsky Selsoviets of Lovozersky District were transferred to Saamsky District, Chalmny-Varrsky Selsoviet, however, did not remain in Saamsky District for long—the VTsIK Resolution of September 10,1937 transferred it back to Lovozersky District. When Saamsky District was abolished on January 26,1963, its selsoviets were transferred to Lovozersky District, however, this classification only lasted for less than two years. Some of the population is Sámi. Закон №96-01-ЗМО от6 января1998 г, «Об административно-территориальном устройстве Мурманской области», в ред. Закона №1953-01-ЗМО от24 декабря2015 г, «О внесении изменений в Закон Мурманской области Об административно-территориальном устройстве Мурманской области». Закон №574-02-ЗМО от29 декабря2004 г, «О статусе, наименованиях и составе территорий муниципального образования Ловозерский район и муниципальных образований, входящих в его состав», в ред. Закона №1156-01-ЗМО от23 ноября2009 г «Об упраздении некоторых населённых пунктов Мурманской области и внесении изменений в отдельные законодательные акты Мурманской области», Вступил в силу1 января2005 г. Решение №64 от24 января2006 г, «Устав муниципального образования Ловозерский район Мурманской области», в ред.10.2003 Об общих принципах организации местного самоуправления в Российской Федерации». Вступил в силу после официального опубликования
Media related to Murmansk Oblast at Wikimedia Commons
