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Uyandina River
The Uyandina (russian: Уяндина; sah, Уйаандьы, translit=Uyaancı) is a river in Yakutia, Russia, a tributary of the Indigirka. The length of the Uyandina is . The area of its drainage basin is . Course The river is formed by the confluence of the long Irgichyan originating in the NW Selennyakh Range and the long Baky, which has its source in Lake Baky, located at the junction of the western end of the Polousny Range and the Kyun-Tas. After flowing in a roughly southern direction in its upper course, the Uyandina flows then eastwards through the Aby Lowland. Finally it meets the left bank of the Indigirka from its mouth. Google Earth The Uyandina freezes up in October and remains icebound until late May or early June. Tributaries The biggest tributaries of the Uyandina are the long Khatyngnakh and long Khachimcher from the left, as well as the long Buor-Yuryakh from the right. See also *List of rivers of Russia Russia can be divided into a European ...
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Polousny Range
The Polousny Range ( rus, Полоусный кряж; sah, Полоуснай томтороот) is a mountain range in the Sakha Republic, Far Eastern Federal District, Russia.Полоусный кряж (Polousny Range) / Great Soviet Encyclopedia; in 35 vols. / Ch. ed. Yu. S. Osipov. 2004—2017. This range is one of the areas of Yakutia where kigilyakhs are found. History The area of the Polousny Range was first mapped by geographer and ethnologist Baron Gerhard von Maydell (1835–1894) during his pioneering research of East Siberia. The Chondon mammoth was discovered in 2013, at the feet of the Polousny Range in the Chondon basin, 66 km south-west of the village of Tumat. Geography The Polousny Range is part of the Momsko-Chersk Mountain Region (russian: Момско-Черская область). It rises in the southern area of the Yana-Indigirka Lowland, north of the Aby Lowland in the Sakha region. It is made up of mountains of middle height and smooth slopes. I ...
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Buor-Yuryakh (Uyandina)
The Buor-Yuryakh (russian: Буор-Юрях; sah, Буор-Үрэх, ''Buor-Ürex'') is a river in the Sakha Republic (Yakutia), Russia. It is the second largest tributary of the Alazeya. The river has a length of and a drainage basin area of . The Buor-Yuryakh flows north of the Arctic Circle, across desolate territories of the Srednekolymsky District. The name of the river comes from the Yakut "Буор Үрэх" ''"Buor"'' = earth, clay / ''"Yurekh"'' = river. Course The Buor-Yuryakh is a right tributary of the Alazeya. It has its sources in the Kolyma Lowland, off the southern foothills of the Alazeya Plateau. The river flows across a floodplain among numerous lakes forming meanders all along its course. It heads first in a roughly southeastward direction. South of the area of lake Ilka it bends and turns east. Then it turns northeastwards to the east of the lake, bending again eastwards after a stretch, leaving lake Balyma to the south. Finally the Buor-Yuryakh b ...
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Khatyngnakh (river)
The Khatyngnakh (russian: Хатынгнах; sah, Хатыҥнаах, ''Xatıŋnaax''), or Khatynnakh (Хатыннах), is a river in the Sakha Republic (Yakutia), Russia. It is the longest tributary of the Uyandina. The river has a length of — together with the Donskaya— and a drainage basin area of . The Khatyngnakh is fed by snow and rain. It flows north of the Arctic Circle, across desolate territories of the Aby District. Course The Khatyngnakh is a left tributary of the Uyandina. It is formed by the confluence of the long Donskaya from the left and the long 2nd Nonchondzhya (2-я Нонгонджя) from the right, both rivers having their sources in the southern slopes of the Polousny Range range. The Khatyngnakh flows meandering roughly southwards across a vast floodplain in the northern sector of the Aby Lowland, where there are innumerable lakes and swamps. Finally the river joins the left bank of the Uyandina from its mouth in the Indigirka.Google Earth ...
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Google Earth
Google Earth is a computer program that renders a 3D computer graphics, 3D representation of Earth based primarily on satellite imagery. The program maps the Earth by superimposition, superimposing satellite images, aerial photography, and geographic information system, GIS data onto a 3D globe, allowing users to see cities and landscapes from various angles. Users can explore the globe by entering addresses and coordinates, or by using a Computer keyboard, keyboard or computer mouse, mouse. The program can also be downloaded on a smartphone or Tablet computer, tablet, using a touch screen or stylus to navigate. Users may use the program to add their own data using Keyhole Markup Language and upload them through various sources, such as forums or blogs. Google Earth is able to show various kinds of images overlaid on the surface of the earth and is also a Web Map Service client. In 2019, Google has revealed that Google Earth now covers more than 97 percent of the world, and has c ...
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Aby Lowland
The Aby Lowland (russian: Абыйская низменность; sah, Абый Намтала, translit=Abıy Namtala) is a low alluvial plain located in the Sakha Republic, Far Eastern Federal District, Russia. Administratively most of the territory of the lowland is part of Aby District ''(Aby Ulus)''. Geography The lowland is crossed by the Indigirka River in its middle course. Besides many smaller rivers and streams, three large left hand tributaries of the great river flow into it, the Selennyakh, Uyandina (with the Khatyngnakh) and Druzhina rivers. The Badyarikha limits the area in the east. The area is flat and mostly marshy, the average height of the plain being between and above sea level. The rivers are generally slow-flowing and meandering, connected by channels and with very boggy shores. The Aby Lakes, mostly small and numbering over 15,000, are dotting the lowlands. The largest are Lake Ozhogino
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Kyun-Tas
Kyun-Tas ( rus, Кюн-Тас; sah, Күн Таас) is a mountain range in the Sakha Republic, Far Eastern Federal District, Russia. The Kyun-Tas is one of the mountain areas of Yakutia where there are kigilyakh rock formations. Geography The Kyun-Tas is located northeast of Deputatsky, between the Selennyakh Range and the western end of the Polousny Range. It rises at the southern limit of the Yana-Indigirka Lowland, northwest of the Aby Lowland. It is a broad massif with mountains of middle height and smooth slopes. The main ridge stretches in a roughly southeast/northwest direction west of the eastern slopes of the Selennyakh Range for about .Google Earth Although the range is smaller, the highest summits of the Kyun-Tas are higher than those of the neighboring Polousny Range. The highest peak, located in the northern part, is high; there is another high peak at the southeastern end that is . Hydrography The long Nuchcha, a tributary of the Chondon, originates in the ...
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Baky (Uyandina)
The Baky (russian: Бакы; sah, Бакы) is a river in the Sakha Republic (Yakutia), Russia. It is one of the northern tributaries of the Yana. The river has a length of and a drainage basin area of . The river flows north of the Arctic Circle. Its basin falls within Verkhoyansky District. Course The Baky is a left tributary of the Yana. It has its sources in the northwestern slopes of the Khayrdakh Ridge (Хайырдахский кряж), part of the Kular Range of the Verkhoyansk system. The river flows first northeastwards, skirting the mountain area. It meanders within a wide valley heading in an eastern direction in its lower course. Osokhtokh village is located by the banks of the Baky in its last stretch, where the river meanders very strongly. Near the left bank of the Yana the Baky divides into three branches, joining the river from its mouth. Google Earth Tributaries The main tributaries of the Baky are the long Tulluk (Туллук), the long Yuyuteer ...
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Baky (river)
The Baky (russian: Бакы; sah, Бакы) is a river in the Sakha Republic (Yakutia), Russia. It is one of the northern tributaries of the Yana. The river has a length of and a drainage basin area of . The river flows north of the Arctic Circle. Its basin falls within Verkhoyansky District. Course The Baky is a left tributary of the Yana. It has its sources in the northwestern slopes of the Khayrdakh Ridge (Хайырдахский кряж), part of the Kular Range of the Verkhoyansk system. The river flows first northeastwards, skirting the mountain area. It meanders within a wide valley heading in an eastern direction in its lower course. Osokhtokh village is located by the banks of the Baky in its last stretch, where the river meanders very strongly. Near the left bank of the Yana the Baky divides into three branches, joining the river from its mouth. Google Earth Tributaries The main tributaries of the Baky are the long Tulluk (Туллук), the long Yuyuteer ...
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Selennyakh Range
The Selennyakh Range (russian: Селенняхский хребет, ''Selennyakhsky Khrebet''; sah, Силээннээх) is a range of mountains in far North-eastern Russia. Administratively the range is part of the Sakha Republic of the Russian Federation.''Selennyakhsky Khrebet'' / Great Soviet Encyclopedia; in 35 vols. / Ch. ed. Yu. S. Osipov. 2004–2017. The town of Deputatsky, capital of the Ust-Yansky District, is located in the area of the range. Geography The Selennyakh Range extends from NNW to SSE for almost north of the northern end of the Moma Range and east of the Khadaranya Range. It is parallel to the latter and separated from it by the Moma-Selennyakh Depression, a wide intermontane basin, where the river Selennyakh flows and that continues southeastwards along the western side of the Moma Range. The Aby Lowland lies to the east and to the north the Yana-Indigirka Lowland. To the northeast it connects with the Kyun-Tas, at the western end of the Polousny Rang ...
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Drainage Basin
A drainage basin is an area of land where all flowing surface water converges to a single point, such as a river mouth, or flows into another body of water, such as a lake or ocean. A basin is separated from adjacent basins by a perimeter, the '' drainage divide'', made up of a succession of elevated features, such as ridges and hills. A basin may consist of smaller basins that merge at river confluences, forming a hierarchical pattern. Other terms for a drainage basin are catchment area, catchment basin, drainage area, river basin, water basin, and impluvium. In North America, they are commonly called a watershed, though in other English-speaking places, "watershed" is used only in its original sense, that of a drainage divide. In a closed drainage basin, or endorheic basin, the water converges to a single point inside the basin, known as a sink, which may be a permanent lake, a dry lake, or a point where surface water is lost underground. Drainage basins are similar ...
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