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Shenkursky District
Shenkursky District (russian: Ше́нкурский райо́н) is an administrative district (raion), one of the twenty-one in Arkhangelsk Oblast, Russia.Law #65-5-OZ As a municipal division, it is incorporated as Shenkursky Municipal District.Law #258-vneoch.-OZ It is located in the south of the oblast and borders with Vinogradovsky District in the north, Verkhnetoyemsky District in the east, Ustyansky District in the southeast, Velsky District in the south, Nyandomsky District in the west, and with Plesetsky District in the northwest. The area of the district is . Its administrative center is the town of Shenkursk. Population: The population of Shenkursk accounts for 37.5% of the district's total population. Geography The district is located in the valley of the Vaga River, a major left tributary of the Northern Dvina. A major tributary of the Vaga is the Led River (left). Some areas in the east, northeast, north, and west of the district lie in the basin of various le ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vaga River
The Vaga (russian: Вага) is a river in Totemsky, Syamzhensky, and Verkhovazhsky Districts of Vologda Oblast and in Velsky, Shenkursky, and Vinogradovsky Districts of Arkhangelsk Oblast in Russia. It is a left and the biggest tributary of the Northern Dvina. The length of the river is . The area of its basin . The main tributaries of the Vaga are the Pezhma (left), the Kuloy (right), the Vel (left), the Ustya (right), the Puya (left), and the Led (left). For Verkhovazhsky, Velsky, and Shenkursky Districts the Vaga is the main river, its valley being heavily populated, and the districts centers, the selo of Verkhovazhye (translated as ''on the Upper Vaga''), and the towns of Velsk and Shenkursk, are located on the banks of the Vaga. In these districts, one of the principal highways in Russia, M8 connecting Moscow and Arkhangelsk, has been built on the left bank of the Vaga. The source of the Vaga is located west of the village of Pakhtusovo, in the Totemsky District cl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tributary
A tributary, or affluent, is a stream or river that flows into a larger stream or main stem (or parent) river or a lake. A tributary does not flow directly into a sea or ocean. Tributaries and the main stem river drain the surrounding drainage basin of its surface water and groundwater, leading the water out into an ocean. The Irtysh is a chief tributary of the Ob river and is also the longest tributary river in the world with a length of . The Madeira River is the largest tributary river by volume in the world with an average discharge of . A confluence, where two or more bodies of water meet, usually refers to the joining of tributaries. The opposite to a tributary is a distributary, a river or stream that branches off from and flows away from the main stream. PhysicalGeography.net, Michael Pidwirny & S ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vazhsky Uyezd
Vazhsky (russian: Важский) is a rural locality (a settlement) in Kitskoye Rural Settlement of Vinogradovsky District, Arkhangelsk Oblast, Russia. The population was 423 as of 2010. There are 6 streets. Geography Vazhsky is located on the Vaga River, 32 km southeast of Bereznik Bereznik (russian: Березник) is the name of several inhabited localities in Russia. Arkhangelsk Oblast As of 2010, nineteen inhabited localities in Arkhangelsk Oblast bear this name. ;Urban localities *Bereznik, Vinogradovsky District, A ... (the district's administrative centre) by road. Bereznichek is the nearest rural locality. References Rural localities in Vinogradovsky District {{ArkhangelskOblast-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Grand Duchy Of Moscow
The Grand Duchy of Moscow, Muscovite Russia, Muscovite Rus' or Grand Principality of Moscow (russian: Великое княжество Московское, Velikoye knyazhestvo Moskovskoye; also known in English simply as Muscovy from the Latin ) was a Rus' principality of the Late Middle Ages centered on Moscow, and the predecessor state of the Tsardom of Russia in the early modern period. It was ruled by the Rurik dynasty, who had ruled Rus' since the foundation of Novgorod in 862. Ivan III the Great titled himself as Sovereign and Grand Duke of All Rus' (russian: государь и великий князь всея Руси, gosudar' i velikiy knyaz' vseya Rusi). The state originated with the rule of Alexander Nevsky of the Rurik dynasty, when in 1263, his son, Daniel I, was appointed to rule the newly created Grand Principality of Moscow, which was a vassal state to the Mongol Empire (under the "Tatar Yoke"), and which eclipsed and eventually absorbed its parent duchy ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Novgorod Republic
The Novgorod Republic was a medieval state that existed from the 12th to 15th centuries, stretching from the Gulf of Finland in the west to the northern Ural Mountains in the east, including the city of Novgorod and the Lake Ladoga regions of modern Russia. The Republic prospered as the easternmost trading post of the Hanseatic League and its Slavic, Baltic and Finnic people were much influenced by the culture of the Viking-Varangians and Byzantine people. Name The state was called "Novgorod" and "Novgorod the Great" (''Veliky Novgorod'', russian: Великий Новгород) with the form "Sovereign Lord Novgorod the Great" (''Gosudar Gospodin Veliky Novgorod'', russian: Государь Господин Великий Новгород) becoming common in the 15th century. ''Novgorod Land'' and ''Novgorod volost usually referred to the land belonging to Novgorod. ''Novgorod Republic'' itself is a much later term, although the polity was described as a republic as early a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Uralic Languages
The Uralic languages (; sometimes called Uralian languages ) form a language family of 38 languages spoken by approximately 25million people, predominantly in Northern Eurasia. The Uralic languages with the most native speakers are Hungarian (which alone accounts for more than half of the family's speakers), Finnish, and Estonian. Other significant languages with fewer speakers are Erzya, Moksha, Mari, Udmurt, Sami, Komi, and Vepsian, all of which are spoken in northern regions of Scandinavia and the Russian Federation. The name "Uralic" derives from the family's original homeland (''Urheimat'') commonly hypothesized to have been somewhere in the vicinity of the Ural Mountains. Finno-Ugric is sometimes used as a synonym for Uralic, though Finno-Ugric is widely understood to exclude the Samoyedic languages. Scholars who do not accept the traditional notion that Samoyedic split first from the rest of the Uralic family may treat the terms as synonymous. History Homeland ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shenkursk COA (Arkhangelsk Governorate) (1780)
Shenkursk (russian: Шенку́рск) is a town and the administrative center of Shenkursky District in Arkhangelsk Oblast, Russia, located on the right bank of the Vaga River. Population: Geography Climate History Shenkursk was first mentioned in documents of Novgorod merchants in 1229. In 1315, it was bought by a Novgorod ''posadnik''. Ivan the Terrible referred to this location as the town of Vaga and included it into his ''oprichnina''. At that time, there was a timber fort and a residence of local bishops. Tsar Feodor I made a grant of Shenkursk to his brother-in-law, Boris Godunov, who bequeathed it to his future son-in-law, Johan of Schleswig-Holstein, who died shortly after arriving to Russia. The Romanovs presented the area to Prince Dmitry Troubetskoy as his ''votchina''. Upon his death, the town was returned to the crown. In 1640–1643, the Tsar ordered a new fortress to be built in Shenkursk. Catherine the Great chartered Shenkursk in 1780, and She ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Swamp
A swamp is a forested wetland.Keddy, P.A. 2010. Wetland Ecology: Principles and Conservation (2nd edition). Cambridge University Press, Cambridge, UK. 497 p. Swamps are considered to be transition zones because both land and water play a role in creating this environment. Swamps vary in size and are located all around the world. The water of a swamp may be fresh water, brackish water, or seawater. Freshwater swamps form along large rivers or lakes where they are critically dependent upon rainwater and seasonal flooding to maintain natural water level fluctuations.Hughes, F.M.R. (ed.). 2003. The Flooded Forest: Guidance for policy makers and river managers in Europe on the restoration of floodplain forests. FLOBAR2, Department of Geography, University of Cambridge, Cambridge, UK. 96 p. Saltwater swamps are found along tropical and subtropical coastlines. Some swamps have hammock (ecology), hammocks, or dry-land protrusions, covered by aquatic vegetation, or vegetation that tolerates ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Floodplain
A floodplain or flood plain or bottomlands is an area of land adjacent to a river which stretches from the banks of its channel to the base of the enclosing valley walls, and which experiences flooding during periods of high discharge.Goudie, A. S., 2004, ''Encyclopedia of Geomorphology'', vol. 1. Routledge, New York. The soils usually consist of clays, silts, sands, and gravels deposited during floods. Because the regular flooding of floodplains can deposit nutrients and water, floodplains frequently have high soil fertility; some important agricultural regions, such as the Mississippi river basin and the Nile, rely heavily on the flood plains. Agricultural regions as well as urban areas have developed near or on floodplains to take advantage of the rich soil and fresh water. However, the risk of flooding has led to increasing efforts to control flooding. Formation Most floodplains are formed by deposition on the inside of river meanders and by overbank flow. Whereve ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Taiga
Taiga (; rus, тайга́, p=tɐjˈɡa; relates to Mongolic and Turkic languages), generally referred to in North America as a boreal forest or snow forest, is a biome characterized by coniferous forests consisting mostly of pines, spruces, and larches. The taiga or boreal forest has been called the world's largest land biome. In North America, it covers most of inland Canada, Alaska, and parts of the northern contiguous United States. In Eurasia, it covers most of Sweden, Finland, much of Russia from Karelia in the west to the Pacific Ocean (including much of Siberia), much of Norway and Estonia, some of the Scottish Highlands, some lowland/coastal areas of Iceland, and areas of northern Kazakhstan, northern Mongolia, and northern Japan (on the island of Hokkaidō). The main tree species, depending on the length of the growing season and summer temperatures, vary across the world. The taiga of North America is mostly spruce, Scandinavian and Finnish taiga consists of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake Lum
A lake is an area filled with water, localized in a basin, surrounded by land, and distinct from any river or other outlet that serves to feed or drain the lake. Lakes lie on land and are not part of the ocean, although, like the much larger oceans, they do form part of the Earth's water cycle. Lakes are distinct from lagoons, which are generally coastal parts of the ocean. Lakes are typically larger and deeper than ponds, which also lie on land, though there are no official or scientific definitions. Lakes can be contrasted with rivers or streams, which usually flow in a channel on land. Most lakes are fed and drained by rivers and streams. Natural lakes are generally found in mountainous areas, rift zones, and areas with ongoing glaciation. Other lakes are found in endorheic basins or along the courses of mature rivers, where a river channel has widened into a basin. Some parts of the world have many lakes formed by the chaotic drainage patterns left over from the last ic ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacial Lake
A glacial lake is a body of water with origins from glacier activity. They are formed when a glacier erodes the land and then melts, filling the depression created by the glacier. Formation Near the end of the last glacial period, roughly 10,000 years ago, glaciers began to retreat. A retreating glacier often left behind large deposits of ice in hollows between drumlins or hills. As the ice age ended, these melted to create lakes. This is apparent in the Lake District in Northwestern England where post-glacial sediments are normally between 4 and 6 metres deep. These lakes are often surrounded by drumlins, along with other evidence of the glacier such as moraines, eskers and erosional features such as striations and chatter marks. These lakes are clearly visible in aerial photos of landforms in regions that were glaciated during the last ice age. The formation and characteristics of glacial lakes vary between location and can be classified into glacial erosion lake, ice-bloc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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