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Kobyaysky Ulus
Kobyaysky District (russian: Кобяйский улу́с; sah, Кэбээйи улууһа, ''Kebeeyi uluuha'', ) is an administrativeConstitution of the Sakha Republic, Article 45 and municipalLaw #172-Z #351-III district (raion, or ''ulus''), one of the thirty-four in the Sakha Republic, Russia. It is located in the center of the republic on the Vilyuy River, by road north of the republic's capital of Yakutsk. The area of the district is .Registry of the Administrative-Territorial Divisions of the Sakha Republic Its administrative center is the urban-type settlement of Sangar. As of the 2010 Census, the total population of the district was 13,680, with the population of Sangar accounting for 32.0% of that number. Geography Mountainous areas are located in the north and northeast of the district, with the Kuturgin Range, Muosuchan Range, Munni Range and Ust-Vilyuy Range, subranges of the Verkhoyansk Range, while the rest of the district is part of the Central Yaku ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sangar, Sakha Republic
Sangar (russian: Санга́р; sah, Сангаар, translit=Sangaar) is an urban locality (an urban-type settlement) and the administrative center of Kobyaysky District of the Sakha Republic, Russia. As of the 2010 Census, its population was 4,377. Geography Sangar is located on the right bank of the Lena River, on the opposite bank of the mouth of the Tyugyuene, by road from Yakutsk, the capital of the republic. Google Earth History It was established in 1928 as a mining settlement. The name originates from the nearby Sangar-Khaya Mountain. On February 10, 1930, the Yakut Autonomous Soviet Socialist Republic was split into districts (uluses) and Sangar became a part of newly established Namsky District. In 1934, the mine was transferred to the Chief Directorate of the Northern Sea Route, which at the time administrated most of the industrial activity in the north of the Soviet Union. Coal from Sangar was transported to Tiksi on the coast of the Arctic Ocean ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Central Yakutian Lowland
The Central Yakutian LowlandJohn Kimble (ed.), ''Cryosols: Permafrost-Affected Soils'' or Central Yakutian Lowlands (russian: Центральноякутская равнина; sah, Саха сирин ортоку намтала), also known as Central Yakut Plain or Vilyuy Lowland, is a low alluvial plain in Siberia, Russia. Administratively the territory of the lowland is part of the Sakha Republic (Yakutia). It is an extensive plain located in the transition zone between Central and Eastern Siberia and is one of the Great Russian Regions. The main city is Yakutsk, with a number of settlements near it, but the area of the lowland is largely uninhabited elsewhere. Google Earth Geography The Central Yakutian Lowlands extend along the middle basin of the Lena River and partly further downstream and are about in length and wide. They drop gradually from the Central Siberian Plateau to the west and the Lena Plateau to the south and southwest. To the northwest the lowland me ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nedzheli
Nedzheli (russian: Ниди́ли or Ниджили; sah, Нидьили, ''Nicili'') is a lake in Kobyaysky District, Sakha Republic (Yakutia), Russia. The lake is a protected area of regional significance. Geography Nedzheli is located near the Lena, about —in a straight line— southwest of the village of Sangar. It is the largest lake in the Central Yakut Plain (Leno-Vilyui interfluve) and the 9th largest in Yakutia. The lake is elongated in an east to west direction. It is fed mainly by snow and freezes between late September / early October and mid June. Flora and fauna The vegetation of the area surrounding the Nedzheli is mainly larch and pine taiga. The lake is rich in fish. The crucian carp variety of the Nedzheli is highly appreciated in Yakutia and has been introduced to other lakes in the region. Siberian cranes, black-headed gulls, river terns, Eurasian teals, ruffs and diving ducks are common in the shores of the lake. In former times the Nedzheli used to b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nuora
The Nuora (russian: Нуора; sah, Нуора) is a river in the Sakha Republic (Yakutia), Russia, a right tributary of the Tumara, of the Aldan basin, part of the Lena basin. It has a length of and a drainage basin area of . The Nuora flows across an area of the Kobyaysky District that is wholly mountainous and desolate. Segyan-Kyuyol village, the closest inhabited place, lies to the south of its confluence with the Tumara. Google Earth The river is a destination for rafting. The name of the river comes from the Yakut language. Course The Nuora is a mountain river that originates south of the Arctic Circle near the Arkachan Plateau, central part of the southern Verkhoyansk Range. In the uppermost stretch of its course the river flows southwards. As it meets the Kelter Range, it bends roughly southeastwards, flowing below the northeastern slopes of the range within a deep valley. Finally the Nuora meets the right bank of the Tumara River, a little upstream from where it cut ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tumara
The Tumara (russian: Тумара; sah, Тумара) is a river in the Sakha Republic (Yakutia), Russia, a right tributary of the Aldan, part of the Lena basin. It flows across an area that is largely desolate, except for Segyan-Kyuyol village. Google Earth The Tumara has a length of and a drainage basin area of . The river is a destination for rafting. The name of the river comes from the Yakut language ''tumara'', meaning "tundra".Murzaev EM, ''Turkic place names'' / Baskakov NA . - Moscow: Eastern Literature RAS, 1996 .-- P. 149 .-- 254 p. - 500 copies. - ISBN 5-02-016806-8 . Course The Tumara originates in the slopes of the southwestern Verkhoyansk Range. In the upper section of its course the river displays all the characteristics of a mountain river, flowing roughly southwards within a deep and narrow valley bound by steep slopes that cuts across the Kelter (Көлтөр) and Munni (Мунний) ranges. After leaving the mountainous area in its middle course the Tumara ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Belyanka (river)
The Belyanka (russian: Белянка; sah, Белянка) is a river in the Sakha Republic (Yakutia), Russia, a right tributary of the Lena. It has a length of — counting the Munni at its head— and a drainage basin area of . There are no settlements in the basin of the river. The nearest village is Batamay, located to the east of its mouth in the Lena.Google Earth Course The Belyanka originates in the Munni Range at the confluence of rivers Munni from the west and Tagyndzha from the east in the southwestern area of the Verkhoyansk Range. The Munni flows from the slopes of the Tagindzhin Range and its valley is bound by the eastern end of the Muosuchan Range. In the upper section of its course the Belyanka river cuts across the mountainous terrain of the Sorkin Range heading roughly southwards in a narrow valley. Soon it leaves the mountainous area and flows southwards flowing slowly and dividing into branches across the Central Yakutian Lowland in a wide floodplain. Cl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Khanchaly
The Khanchaly (russian: Ханчалы; sah, Ханчылы, ''Xançılı'') is a river in Yakutia (Sakha Republic), Russia. It is a left tributary of the Lena with a length of . Its drainage basin area is . The river flows across the Gorny, Namsky and Kobyaysky districts of Yakutia. Google Earth Course The entire length of the course of the Khanchaly falls within the Central Yakutian Lowland. Its source is in an area of lakes, the largest of which is lake Chabyda (Чабыда), a protected area located to the west of Yakutsk. The river flows first northeastwards, then it bends northwards, flowing parallel to the Kenkeme all along its middle and lower course. The Khanchaly heads steadily in a northern direction within poorly drained flatland until its mouth in the Lena. The confluence of the Khanchaly with the Lena is from its mouth. There are many small lakes in the Khanchaly basin, especially on the western side, to the east of the course of the Sitte. The river ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tympylykan
The Tympylykan (russian: Тымпылыкан, sah, Тымпылыкаан, ''Tımpılıkaan'') is a river in the Sakha Republic (Yakutia), Russia. It is a left tributary of the Lena. Its length is and the area of its basin is . The basin of the Tympylykan falls fully within the Central Yakutian Lowland. It flows across the Kobyaysky and Vilyuysky districts. The banks of the river are uninhabited. Geography The Tympylykan originates in an area of swamps and small lakes of the Central Yakutian Lowland. It flows first in a SSE direction and then roughly southeastwards to the south of the Linde within a wide floodplain. Towards the last stretch of its course it bends and flows northeastwards, meandering among marshes and lakes. Finally it meets the left bank of the Lena upstream of its mouth in the Laptev Sea. The Lyapiske has its mouth roughly on the opposite side of the Lena. Google Earth The main tributaries of the Tympylykan are the long Achchygyi-Tympylykan and long Ko ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sitte (river)
The Sitte (russian: Ситте; sah, Сииттэ, ''Siitte'') is a river in Yakutia (Sakha Republic), Russia. It is a left tributary of the Lena with a length of . Its drainage basin area is . The name of the river is based on the Yakut word ''"satyy"'' (сатыы), meaning "low". Course The Sitte has its sources in a marshy area near Kiriyestyakh, at the northern edge of the Lena Plateau. It soon leaves the plateau area and flows across the Central Yakutian Lowland in a roughly northern direction. The river forms meanders as it heads north within a floodplain with oxbows and small thermokarst lakes to the east of the Tyugyuene and west of the Khanchaly. Close to the final stretch of its course the Sitte enters the Lena floodplain, dotted with a multitude of larger lakes and marshes. Finally it meets an arm of the left bank of the Lena, from its mouth. The Sitte river is fed by rain and snow. Floods are common in the spring, but the rest of the warm season its channel ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tyugyuene
The Tyugyuene (russian: Тюгюэне or Тюгене; sah, Түгүөнэ, ''Tügüöne'') is a river in Yakutia (Sakha Republic), Russia. It is a tributary of the Lena with a length of and a drainage basin area of . The river marks the border between Gorny and Kobyaysky Districts in a stretch of its middle course. The name of the river is based on the Evenk word ''"tagin"'' (тагин), meaning "swamp". Course The Tyugyuene is a left tributary of the Lena. It has its origin at the confluence of the long Ysyakh-Yuryage and Kupsuyu-Yuryakh streams, at an altitude of about in the northeastern part of the Lena Plateau, southwest of the abandoned village of Abaranda. It heads first a roughly northern direction to the east of the Lungkha in its upper course, then it bends northeastwards in its middle course across the Central Yakutian Lowland, changing again to northwards. There are small lakes in the broad floodplain of the lower course of the river, and it meanders s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kenkeme
The Kenkeme (russian: Кенкеме; sah, Кэҥкэмэ, ''Keŋkeme'') is a river in Yakutia (Sakha Republic), Russia. It is a tributary of the Lena (river), Lena with a length of — together with the Yagas-Yyaabyt at its head— and a drainage basin area of . The Mirny, Sakha Republic, Mirny — Yakutsk stretch of the A331 highway (Russia), A331 highway has a bridge over the Kenkeme. The river flows across a desolate region. The only inhabited place in its basin is an Evenks, Evenk settlement in the middle course. Since it is not far from Yakutsk, the Kenkeme is a popular summer destination for kayaking and rafting. Course The Kenkeme originates in the northeastern edge of the Lena Plateau, at the confluence of the Yagas-Yyaabyt (Ыагас-Ыйаабыт) and Yolyong-Yurege (Ёлёнг-Юрэгэ) rivers. Is sources are about to the west of Yakutsk in a straight line. It heads first in a southeastern direction, bending to the east and then to the north, forming meanders ... [...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] |
