Yana Plateau
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Yana Plateau
The Yana Plateau ( rus, Янское плоскогорье, sah, Дьааҥы хаптал хайалара) is a mountain plateau in the Sakha Republic, Far Eastern Federal District, Russia. Google Earth The plateau lies in an uninhabited area where solitude prevails. It was first surveyed and mapped in 1868 by Gerhard von Maydell (1835–1894), a Russian government officer in East Siberia of Estonian descent.Gerhard Baron von Maydell (1835–1894) und die Bedeutung seiner Forschungen in Nordost-Sibirien


Geography

The Yana Plateau is located in the middle basin of the

Russia
Russia (, , ), or the Russian Federation, is a transcontinental country spanning Eastern Europe and Northern Asia. It is the largest country in the world, with its internationally recognised territory covering , and encompassing one-eighth of Earth's inhabitable landmass. Russia extends across eleven time zones and shares land boundaries with fourteen countries, more than any other country but China. It is the world's ninth-most populous country and Europe's most populous country, with a population of 146 million people. The country's capital and largest city is Moscow, the largest city entirely within Europe. Saint Petersburg is Russia's cultural centre and second-largest city. Other major urban areas include Novosibirsk, Yekaterinburg, Nizhny Novgorod, and Kazan. The East Slavs emerged as a recognisable group in Europe between the 3rd and 8th centuries CE. Kievan Rus' arose as a state in the 9th century, and in 988, it adopted Orthodox Christianity from t ...
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Yana River
The Yana ( rus, Я́на, p=ˈjanə; sah, Дьааҥы, ''Caañı'') is a river in Sakha in Russia, located between the Lena to the west and the Indigirka to the east. Course It is long, and its drainage basin covers . Including its longest source river, the Sartang, it is long. Its annual discharge totals approximately . Most of this discharge occurs in May and June as the ice on the river breaks up. The Yana freezes up on the surface in October and stays under the ice until late May or early June. In the Verkhoyansk area, it stays frozen to the bottom for 70 to 110 days, and partly frozen for 220 days of the year. The river begins at the confluence of the rivers Sartang and Dulgalakh in the Yana-Oymyakon Highlands. It flows north across the vast Yana-Indigirka Lowland, part of the greater East Siberian Lowland, shared with the Indigirka to the east. As the river flows into the Yana Bay of the Laptev Sea, it forms a huge river delta covering .
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Dulgalakh
The Dulgalakh ( rus, Дулгалах; sah, Дулҕалаах, ''Dulğalaax'') is a river in Yakutia, the left, western source river of the Yana. Its length is and its basin size . Course The Dulgalakh rises on the central Verkhoyansk Range, south of the southern slopes of the Arkachan Plateau. It flows through Kobyaysky and Verkhoyansky districts. Above Verkhoyansk it merges with the Sartang forming the Yana.Дулгалах — ''статья из Большой советской энциклопедии''. Great Soviet Encyclopedia See also *List of rivers of Russia *Yana Plateau The Yana Plateau ( rus, Янское плоскогорье, sah, Дьааҥы хаптал хайалара) is a mountain plateau in the Sakha Republic, Far Eastern Federal District, Russia. Google Earth The plateau lies in an uninhabited ar ... * Yana-Oymyakon Highlands§Hydrography References {{Reflist Rivers of the Sakha Republic Verkhoyansk Range ...
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Sartang River
The Sartang ( rus, Сартанг; sah, Сартаҥ) is a river in the Republic of Sakha in Russia. It is the eastern, right source river of the Yana, and is long, with a drainage basin of .Сартанг — ''статья из Большой советской энциклопедии''. Great Soviet Encyclopedia Course The river begins in the Verkhoyansk Range at an elevation of . From this area, the Sartang heads north along the Barylas, and continues north along the Yana Plateau between the Verkhoyansk Range to the west and the Chersky Range to the east. Around southwest of Verkhoyansk, the Sartang joins the river Dulgalakh to form the river Yana. The area around the Sartang consists of taiga. See also *List of rivers of Russia Russia can be divided into a European and an Asian part. The dividing line is generally considered to be the Ural Mountains. The European part is drained into the Arctic Ocean, Baltic Sea, Black Sea, and Caspian Sea. The Asian part is d ...
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Tuostakh
, name_native = , name_native_lang = Yakut , image = Kisilyakh Mountains - ONC C-6.jpg , image_size = , image_caption = Map section showing part of the course of the Tuostakh in the lower center , pushpin_map = Russia Sakha Republic , pushpin_map_size = , pushpin_map_caption= Mouth location in Yakutia, Russia , source1_location = Confluence of rivers Khara-Sala and Boldymba , source1_coordinates = , source1_elevation = , mouth = Adycha , mouth_location = , mouth_coordinates = , mouth_elevation = , progression = , subdivision_type1 = Federal subject , subdivision_name1 = Yakutia, Russia , length = , discharge1_avg = , basin_size = The Tuostakh ( rus, Туостах; sah, Туостаах) is a river in the Verkhoyansk District, Sakha (Yakutia), Russia. It is a left hand tributary of the Adycha, of the Yana basin. Th ...
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Nelgese
The Nelgese ( rus, Нельгесе; sah, Нэльгэһэ, ''Nelgehe'') is a river in the Republic of Sakha in Russia. It is a left hand tributary of the Adycha, of the Yana basin. It is long, with a drainage basin of . The river flows across a desolate area of severe climate, with continuous permafrost. Course The Nelgese is the longest tributary of the Adycha. It begins between two high ranges of the Verkhoyansk Range, running approximately from north to south to the west of the Khunkhadin Range. It heads roughly north across the Yana Plateau of the Yana-Oymyakon Highlands in a wide, swampy area dotted with ancient lakes. Then it turns northeast between the Nelgesin Range and the Tirekhtyakh Range, flowing through a narrow valley before it joins the Adycha 78 km downstream from the mouth of the Derbeke and 13 km upstream from the mouth of the Charky. The Nelgese has many tributaries. The main ones are the Sordong and the Kordekan; the latter is the only one exceedi ...
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Derbeke
The Derbeke ( rus, Дербеке; sah, Дэрбэкэ) is a river in the Republic of Sakha in Russia. It is a left hand tributary of the Adycha, of the Yana basin. It is long, with a drainage basin of . It is an excellent river for boating, but it flows in an area without permanent population. Course The river begins in a rocky gorge in the eastern flank of the Khunkhadin Range, part of the southern section of the Verkhoyansk Range. It heads roughly north and northeast, leaving the Verkhoyansk mountains, and meandering slowly across a swampy area in the Yana Plateau with numerous lakes, including Lake Emanda ( sah, Эмандьа). The river gains speed again in its lower course at the feet of the southeastern side of the Nelgesin Range when it flows through a narrow mountain valley. Finally it joins the Adycha upstream from the Nelgese, the largest tributary.Derbeke — Great Soviet Encyclopedia in 30 vols. / Ch. ed. A.M. Prokhorov - 3rd ed. - M, 1969-1978. The main ...
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Adycha
The Adycha (russian: Адыча; sah, Адыаччы) is a river in the Republic of Sakha in Russia. It is a right hand tributary of the Yana, and is long, with a drainage basin of . At the end of the Soviet period, a big dam with a hydroelectric station was planned to be built on the river, but following perestroika and economic difficulties in the country the project was given up. Course The river begins in the western flank of the Chersky Range at an elevation of . It heads roughly north and northwest across a wide river valley where taiga and forest tundra predominate, bending around the northern end of the Tirekhtyakh Range. Finally, after flowing across the western end of the Kisilyakh Range, it joins river Yana from the right about to the north of Batagay and roughly to the south of the confluence with the Oldzho. The river is also known as "Borong" (Russian: Боронг) in a section of its upper course.Adycha — ''статья из Большой советско ...
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Borulakh
The Borulakh ( rus, Борулах; sah, Боруулаах, ''Boruulaax'') is a river in the Republic of Sakha in Russia. It is a left hand tributary of the Adycha, of the Yana basin. It is long, with a drainage basin of . The river is not navigable. It usually freezes in October and stays under thick ice until June. Course The river begins in the Yana Plateau and flows all the way along it. It heads first roughly north strongly meandering in its middle and lower course then is bends to the northeast around the Tirekhtyakh Range mountain area. Finally it joins the Adycha downstream from the Nelgese, the largest tributary.Borulakh — Great Soviet Encyclopedia in 30 vols. / Ch. ed. A.M. Prokhorov - 3rd ed. - M, 1969-1978. There are about 350 lakes in the river basin. The main tributaries of the Borulakh are the Kaltysy and Khatyngnakh. See also *List of rivers of Russia Russia can be divided into a European and an Asian part. The dividing line is generally considered ...
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Tectonic
Tectonics (; ) are the processes that control the structure and properties of the Earth's crust and its evolution through time. These include the processes of mountain building, the growth and behavior of the strong, old cores of continents known as cratons, and the ways in which the relatively rigid plates that constitute the Earth's outer shell interact with each other. Tectonics also provide a framework for understanding the earthquake and volcanic belts that directly affect much of the global population. Tectonic studies are important as guides for economic geologists searching for fossil fuels and ore deposits of metallic and nonmetallic resources. An understanding of tectonic principles is essential to geomorphologists to explain erosion patterns and other Earth surface features. Main types of tectonic regime Extensional tectonics Extensional tectonics is associated with the stretching and thinning of the crust or the lithosphere. This type of tectonics is fo ...
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Yana–Oymyakon Highlands
The Yana-Oymyakon Highlands ( rus, Яно-Оймяконское нагорье; sah, Дьааҥы хаптал хайалара), also known as Oymyakon Highlands ( rus, Оймяконское нагорье),Soviet General Topographic Maps P-54-V,VI are a mountainous area in the Sakha Republic, Khabarovsk Krai and Magadan Oblast, Far Eastern Federal District, Russia. The area is named after the main features of the highlands. Kigilyakhs are found in some places of the plateaus. These are rock formations that are valued in Yakut culture. Geography The Yana-Oymyakon Highlands are a mountain region of the East Siberian System located between the southern reaches of the Verkhoyansk Range to the west, the Suntar-Khayata Range to the southwest and the Chersky mountain range to the northeast. The main highland features are the vast Yana Plateau in the northwest, the Elgi Plateau in the middle and the Oymyakon Plateau in the southeast. The highlands include the Kuydusun and Aga ...
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Elgi Plateau
The Elgi Plateau ( rus, Эльгинское плоскогорье;Soviet General Topographic Maps P-54-V,VI sah, Эльгэ хаптал хайалаах сир) is a plateau in the Sakha Republic, Far Eastern Federal District, Russian Federation. The area is named after the Elgi River, a left tributary of the Indigirka. Formerly there was the Elginsky urban-type settlement by the left bank of river Elgi. It belonged to the Oymyakon District and was abolished in 2007. Geography The Elgi Plateau covers the central Yana-Oymyakon Highlands, in the upper Elgi, Tompo and Delinya River basins. The plateau is bound by the Verkhoyansk Range to the west and the Chersky Range to the northeast, the Yana Plateau to the northwest, the Suntar-Khayata Range to the southwest and the Oymyakon Plateau to the southeast.Geographical Atlas of Russia. - Federal Agency for Geodesy and Cartography , AST, 2010. - pp. 118-119 The average height of the plateau surface is between and . Dome-sh ...
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