Omoloy
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Omoloy
The Omoloy (russian: Омолой sah, Омолой) is a river in Siberia, flowing into the Laptev Sea east of the river Lena. It is long, and has a drainage basin of . Administratively the basin of the Omoloy is part of the Sakha (Yakutia) administrative region of Russia. There is a protected area in the basin of the river.The now extinct Beringian steppe bison used to have its habitat in the area of the Omoloy. Course It flows roughly northwards across the tundra along a valley limited by the Sietinden Range to the west and the Kular Range to the east. Both ranges are part of the Verkhoyansk Range system. The Omoloy flows through the East Siberian Lowland into the Laptev Sea. Its mouth is located in the eastern coast of the Buor-Khaya Gulf. The river freezes up in October and stays under ice until late May or early June. Tributaries The main tributaries of the Omoloy are the long Kuranakh-Yuryakh, the long Arga-Yuryakh, the long Bukhuruk (Бу­ху­рук) and the lon ...
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Ulakhan-Kyuegyulyur
The Ulakhan-Kyuegyulyur (russian: Улахан-Кюэгюлюр; sah, Улахан Күөгүлүүр, ''Ulaxan Küögülüür'') is a river in Sakha Republic (Yakutia), Russia. It is one of the major tributaries of the Omoloy. The river has a length of and a drainage basin area of . The river flows north of the Arctic Circle, across desolate tundra territories of the East Siberian Lowland. Its basin falls within Ust-Yansky District. Course The Ulakhan-Kyuegyulyur is the largest right tributary of the Omoloy. It has its sources in the western slopes of the Kular Range of the Verkhoyansk Range system. The river flows roughly in a NNE direction flanking the feet of the range. After it descends into the East Siberian Lowland, it heads in a northern direction until the end of its course. The river flows roughly parallel to the Omoloy further west, meandering in the floodplain. Finally the Ulakhan-Kyuegyulyur joins the right bank of the Omoloy from its mouth. The confluence is ups ...
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Arga-Yuryakh
The Arga-Yuryakh (russian: Арга-Юрях; sah, Арҕаа Үрэх, ''Arğaa Ürex'') is a river in Sakha Republic (Yakutia), Russia. It is one of the major tributaries of the Omoloy. The river has a length of and a drainage basin area of . The river flows north of the Arctic Circle, across desolate tundra territories of the East Siberian Lowland. Its basin falls within Ust-Yansky and Bulunsky districts. The name of the river comes from the Yakut ''"Arğaa-ürex"'' ''(Арҕаа-үрэх)'', meaning "western river". Course The Arga-Yuryakh is a left tributary of the Omoloy. It has its sources at the confluence of the long Mundukan and the long Khadarynnya in the eastern slopes of the Orulgan Range of the Verkhoyansk Range system. The river flows roughly in an ENE direction and when it descends into the East Siberian Lowland, it bends and heads in a NNE direction until the end of its course. In its last stretch the river flows roughly parallel to the Omoloy further east, ...
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Kuranakh-Yuryakh
The Kuranakh-Yuryakh (russian: Куранах-Юрях or Кураанах-Юрэх; sah, Кураанах Үрэх, ''Kuraanax Ürex'') is a river in Sakha Republic (Yakutia), Russia. It is one of the major tributaries of the Omoloy. The river has a length of — together with the Nyolu— and a drainage basin area of . The lower stretch of its course is also known as Altan. The Kuranakh-Yuryakh flows north of the Arctic Circle, across desolate tundra territories of the East Siberian Lowland. Its basin falls within Ust-Yansky and Bulunsky districts. Course The Kuranakh-Yuryakh is a left tributary of the Omoloy. It has its sources in the eastern slopes of the Orulgan Range of the Verkhoyansk Range system. The river flows roughly northeastwards across mountainous terrain, bound in the east by the Sietinden Range, then it heads eastwards along a wide valley. As it descends into the floodplain of the East Siberian Lowland, it turns again in a northeastern direction, flowing slowly ...
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Laptev Sea
The Laptev Sea ( rus, мо́ре Ла́птевых, r=more Laptevykh; sah, Лаптевтар байҕаллара, translit=Laptevtar baỹğallara) is a marginal sea of the Arctic Ocean. It is located between the northern coast of Siberia, the Taimyr Peninsula, Severnaya Zemlya and the New Siberian Islands. Its northern boundary passes from the Arctic Cape to a point with co-ordinates of 79°N and 139°E, and ends at the Anisiy Cape. The Kara Sea lies to the west, the East Siberian Sea to the east. The sea is named after the Russian explorers Dmitry Laptev and Khariton Laptev; formerly, it had been known under various names, the last being Nordenskiöld Sea (russian: link=no, мо́ре Норденшёльда), after explorer Adolf Erik Nordenskiöld. The sea has a severe climate with temperatures below 0 °C (32 °F) over more than nine months per year, low water salinity, scarcity of flora, fauna and human population, and low depths (mostly less than 50 meters) ...
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Sietinden Range
The Sietinden Range (russian: Сиетиндэнский хребет; sah, Сиэтэндэ) is a range of mountains in far North-eastern Russia. Administratively the range is part of the Sakha Republic, Russian Federation.Verkhoyansk Range
/ ; in 35 vols. / Ch. ed. Yu. S. Osipov. 2004—2017.
, the only permanent settlement in the area, lies off the southeastern slopes of the range.


History

Previously uncharted, this range was ...
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Buor-Khaya Gulf
The Buor-Khaya Gulf or Buor-Khaya Bight (russian: Губа Буор-Хая) is one of the most important gulfs of the Laptev Sea. Administratively the Buor-Khaya Gulf belongs to the Sakha Republic (Yakutia) of the Russian Federation. There is an abandoned polar station in the shores of the Buor-Khaya Gulf. Geography It lies at the western end of the Yana-Indigirka Lowland, between the eastern side of the Lena delta on its western side and Cape Buor-Khaya at its NE end. Tiksi Bay and the Bykovsky Peninsula are on the western shores of the Buor-Khaya Gulf.Google Earth Heavily eroded Muostakh Island, the remainder of an ancient great plain, is located roughly in the midst of the gulf. The Omoloy River is the only large river flowing into the Buor-Khaya Gulf, its mouth is located halfway up the eastern coast. The sea in this gulf is frozen for about nine months every year and often clogged with ice floes. See also *List of research stations in the Arctic A number of government ...
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Verkhoyansk Range
The Verkhoyansk Range (russian: Верхоянский хребет, ''Verkhojanskiy Khrebet''; sah, Үөһээ Дьааҥы сис хайата, ''Üöhee Chaangy sis khaĭata'') is a mountain range in the Sakha Republic, Russia near the settlement of Verkhoyansk, well-known for its frigid climate. It is part of the East Siberian Mountains. The range lies just west of the boundary of the Eurasian and the North American tectonic plates. The mountains were formed by folding, and represent an anticline. The Verkhoyansk Range was covered by glaciers during the Last Glacial Period and the mountains in the northern section, such as the Orulgan Range, display a typical Alpine relief. There are coal, silver, lead, tin and zinc deposits in the mountains. Geography Rising from the shores of the Buor-Khaya Gulf in the north, it runs southwards spanning roughly 1000 km (600 mi.) across Yakutia, east of the Central Yakutian Lowland, and west of the Chersky Range, reaching the ...
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Kular Range
The Kular Range (russian: хребет Кулар, ''Khrebet Kular''; sah, Кулар сис, Kular Sis) is a range of mountains in far North-eastern Russia. Administratively the range is part of the Eveno-Bytantaysky National District of the Sakha Republic, Russian Federation.Kular (mountains)
/ ; in 35 vols. / Ch. ed. Yu. S. Osipov. 2004—2017.
This range is one of the places in Yakutia where are found.
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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 drained into the Arctic Ocean and the Pacific Ocean. Notable rivers of Russia in Europe are Volga (which is the longest river in Europe), Pechora, Don, Kama, Oka and the Northern Dvina, while several other rivers originate in Russia but flow into other countries, such as the Dnieper and the Western Dvina. In Asia, important rivers are the Ob, the Irtysh, the Yenisei, the Angara, the Lena, the Amur, the Yana, the Indigirka, and the Kolyma. In the list below, the rivers are grouped by the seas or oceans into which they flow. Rivers that flow into other rivers are ordered by the proximity of their point of confluence to the mouth of the main river, i.e., the lower in the list, the more upstream. There is an alphabetical list of rivers at the end of ...
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East Siberian Lowland
The East Siberian Lowland ( rus, Восточно-Сибирская низменность), also known as Yana-Kolyma Lowland,Oleg Leonidovič Kryžanovskij, ''A Checklist of the Ground-beetles of Russia and Adjacent Lands.'' p. 16 is a vast plain in Northeastern Siberia, Russia.Yana-Indigirka and Kolyma lowlands (physical map, scale 1: 2 500 000)
// National Atlas of Russia . - M .: Roskartografiya, 2004. - T. 1. - S. 260—261. - 496 p. -
The territory of the lowland is one of the . Administratively it is part of the

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Great Soviet Encyclopedia
The ''Great Soviet Encyclopedia'' (GSE; ) is one of the largest Russian-language encyclopedias, published in the Soviet Union from 1926 to 1990. After 2002, the encyclopedia's data was partially included into the later ''Bolshaya rossiyskaya entsiklopediya'' (or '' Great Russian Encyclopedia'') in an updated and revised form. The GSE claimed to be "the first Marxist–Leninist general-purpose encyclopedia". Origins The idea of the ''Great Soviet Encyclopedia'' emerged in 1923 on the initiative of Otto Schmidt, a member of the Russian Academy of Sciences. In early 1924 Schmidt worked with a group which included Mikhail Pokrovsky, (rector of the Institute of Red Professors), Nikolai Meshcheryakov (Former head of the Glavit, the State Administration of Publishing Affairs), Valery Bryusov (poet), Veniamin Kagan (mathematician) and Konstantin Kuzminsky to draw up a proposal which was agreed to in April 1924. Also involved was Anatoly Lunacharsky, People's Commissar of Education ...
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