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Alazeya
The Alazeya ( rus, Алазея, r=; sah, Алаһыай, translit=Alahıay) is a river in the northeastern part of Yakutia, Russia which flows into the Arctic between the basins of the larger Indigirka to the west and the Kolyma to the east. Mount Kisilyakh-Tas is a notable kigilyakh site on the right bank of the Alazeya River at . Geography The river is long. The area of its basin is . The Alazeya is formed at the confluence of the Nelkan and Kadylchan rivers in the slopes of the Alazeya Plateau. It crosses roughly northwards through the tundra meandering among the flat, marshy areas of the Kolyma Lowland, part of the greater East Siberian Lowland. Finally the Alazeya drains into the Kolyma Bay of the East Siberian Sea, close to Logashkino. The river freezes in late September through early October and stays icebound until late May through early June. There are more than 24,000 lakes in its basin.Google Earth [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Buor-Yuryakh
The Buor-Yuryakh (russian: Буор-Юрях; sah, Буор-Үрэх) 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 bends northwards to t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alazeya Plateau
The Alazeya Plateau ( rus, Алазейское плоскогорье) is a mountain plateau in the Sakha Republic, Far Eastern Federal District, Russia. The area is named after river Alazeya, which has its source in the plateau. There are kigilyakhs in the Alazeya Plateau. The particularity of the kigilyakhs found in this location is that their lower part (corresponding to the legs) is thinner than the upper part. Geography The Alazeya Plateau is located in eastern Sakha Republic, between the Indigirka, Kolyma, Alazeya and Ozhogina rivers. The average height of the plateau surface is around . There are slightly higher tableland type elevations cutting across the plateau area; the highest point is a high unnamed summit. The plateau is limited by the Yana-Indigirka Lowland, including the Aby Lowland, to the west, with rivers Yana and Indigirka, the Ozhogina to the south, and the Kolyma Lowland with the Kolyma to the east and northeast.Google Earth Besides the Alazeya, the Se ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rassokha
The Rassokha (russian: Рассоха, also Россоха; sah, Рассоха) is a river in the northeastern part of Yakutia, Russia. It is the major tributary of the Alazeya.Google Earth Geography The river is long. The area of its basin is . The Rassokha is formed by the confluence of the rivers Ilin-Yuryakh and Arga-Yuryakh in the Kolyma Lowland. The original sources of the uppermost river in the network are in the Ulakhan-Sis Range. The Rassokha flows across the Middle Kolyma District and the Lower Kolyma District in an area marked by permafrost, with numerous swamps and lakes. Finally it joins the left bank of the Alazeya from its mouth.Rossokha - Water (in Russian) The Rassokha has 145 tributaries that are longer than ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kolyma Lowland
The Kolyma Lowland (russian: Колымская низменность) is a lowland plain in the northeastern parts of Sakha Republic in the basin of the Alazeya, Bolshaya Chukoch'ya and lower reaches of the Kolyma rivers. The lowland is formed by fluvio-lacustrine loam soil about 120 m thick. The climate is subarctic. Geography The Kolyma Lowland stretches for along the Kolyma River from the East Siberian Sea to the Chersky Range, between the Alazeya and Yukagir plateaus. Besides the Kolyma, other rivers in the lowland include the Alazeya, its tributary Rossokha, and the Chukochya. The average elevation of the Kolyma lowland is with occasional heights, such as the high Suor Uyata.Google Earth The Kolyma Lowland is part of the wider Yana-Kolyma system of lowlands, which include the Aby to the south of the Polousny Range and the Yana-Indigirka on the northern and western sides.Oleg Leonidovič Kryžanovskij, ''A Checklist of the Ground-beetles of Russia and Adjacent Lands.' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 |
Kolyma River
The Kolyma ( rus, Колыма, p=kəlɨˈma; sah, Халыма, translit=Khalyma) is a river in northeastern Siberia, whose basin covers parts of the Sakha Republic, Chukotka Autonomous Okrug, and Magadan Oblast of Russia. The Kolyma is frozen to depths of several metres for about 250 days each year, becoming free of ice only in early June, until October. Course The Kolyma begins at the confluence of the Kulu and the Ayan-Yuryakh, originating in the Khalkan Range and flows across the Upper Kolyma Highlands in its upper course. Leaving the mountainous areas it flows roughly northwards across the Kolyma Lowland, a vast plain dotted with thousands of lakes, part of the greater East Siberian Lowland. The river empties into the Kolyma Gulf of the East Siberian Sea, a division of the Arctic Ocean. The Kolyma is long. The area of its basin is . The average discharge at Kolymskoye is , with a high of reported in June 1985, and a low of in April 1979. Tributaries The m ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kisilyakh-Tas
Kisilyakh-Tas ( rus, гора Кисилях-Тас) is a mountain in Yakutia, Far Eastern Federal District, Russia. Administratively it belongs to the Lower Kolyma District. This mountain is one of the renowned places of Yakutia where kigilyakhs are found. The largest of them are between and in height. Kigilyakhs are rock formations that are held in high esteem by Yakuts. ''Kisilyakh'' means "Mountain having a man" or "Mountain married" in the Yakut language. Geography Mount Kisilyakh-Tas is a small, isolated mountain massif of the Kolyma Lowland, located east of the Suor Uyata range. It rises above the tundra on the right bank of the Alazeya, roughly south of the river's mouth in the shores of the East Siberian Sea. Kisilyakh-Tas is located in a flat area, where there are only two other mountains nearby, a higher one to the SW and a smaller one to the west, both on the other side of the river. The three mountains are roughly at the same distance from each other. Andr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kigilyakh
Kigilyakh or kisiliyakh ( rus, кигиляхи; sah, киһилээх, meaning "stone person") are tall, pillar-like natural rock formations looking like tall monoliths standing more or less isolated. Usually they are composed of granite or sandstone shaped as a result of cryogenic weathering. Most kigilyakhs formed during the Cretaceous period and are about 120 million years old. Cultural significance and etymology These anthropomorphic rock pillars are an important feature in Yakut culture. Often they are slightly scattered, protruding from the surface of smooth mountains and giving the impression of a standing crowd of people. According to Yakut legends kigilyakhs originated in very ancient people. The Yakut word ''"kisiliy"'' means "a place where there are people". ''Kisilyakh'' means "mountain having a man" or "mountain married". The term "kigilyakh" is a distorted form of the original Yakut ''"kisilyakh"''. Locations Such stones are found in different places of Sakha ( ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
East Siberian Sea
The East Siberian Sea ( rus, Восто́чно-Сиби́рское мо́ре, r=Vostochno-Sibirskoye more) is a marginal sea in the Arctic Ocean. It is located between the Arctic Cape to the north, the coast of Siberia to the south, the New Siberian Islands to the west and Cape Billings, close to Chukotka, and Wrangel Island to the east. This sea borders on the Laptev Sea to the west and the Chukchi Sea to the east. This sea is one of the least studied in the Arctic area. It is characterized by severe climate, low water salinity, and a scarcity of flora, fauna and human population, as well as shallow depths (mostly less than 50 m), slow sea currents, low tides (below 25 cm), frequent fogs, especially in summer, and an abundance of ice fields which fully melt only in August–September. The sea shores were inhabited for thousands of years by indigenous tribes of Yukaghirs, Chukchi and then Evens and Evenks, which were engaged in fishing, hunting and reindeer husbandry. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sakha Republic
Sakha, officially the Republic of Sakha (Yakutia),, is the largest republic of Russia, located in the Russian Far East, along the Arctic Ocean, with a population of roughly 1 million. Sakha comprises half of the area of its governing Far Eastern Federal District, and is the world's largest country subdivision, covering over 3,083,523 square kilometers (1,190,555 sq mi). ''Sakha'' following regular sound changes in the course of development of the Yakut language) as the Evenk and Yukaghir exonyms for the Yakuts. It is pronounced as ''Haka'' by the Dolgans, whose language is either a dialect or a close relative of the Yakut language.Victor P. Krivonogov, "The Dolgans’Ethnic Identity and Language Processes." ''Journal of Siberian Federal University'', Humanities & Social Sciences 6 (2013 6) 870–888. Geography * ''Borders'': ** ''internal'': Chukotka Autonomous Okrug (660 km)(E), Magadan Oblast (1520 km)(E/SE), Khabarovsk Krai (2130 km)(SE), Amur Oblast (S ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Yakutia
Sakha, officially the Republic of Sakha (Yakutia),, is the largest republic of Russia, located in the Russian Far East, along the Arctic Ocean, with a population of roughly 1 million. Sakha comprises half of the area of its governing Far Eastern Federal District, and is the world's largest country subdivision, covering over 3,083,523 square kilometers (1,190,555 sq mi). ''Sakha'' following regular sound changes in the course of development of the Yakut language) as the Evenk and Yukaghir exonyms for the Yakuts. It is pronounced as ''Haka'' by the Dolgans, whose language is either a dialect or a close relative of the Yakut language.Victor P. Krivonogov, "The Dolgans’Ethnic Identity and Language Processes." ''Journal of Siberian Federal University'', Humanities & Social Sciences 6 (2013 6) 870–888. Geography * ''Borders'': ** ''internal'': Chukotka Autonomous Okrug (660 km)(E), Magadan Oblast (1520 km)(E/SE), Khabarovsk Krai (2130 km)(SE), Amur Oblast (S ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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