Uda River (Republic Of Buryatia)
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Uda River (Republic Of Buryatia)
The Uda ( ; ) is a river in the Buryat Republic, Russia. It is a right tributary of the Selenga, which it meets near the city Ulan-Ude. Its length is , and it has a drainage basin of . The Uda basin lies in the Tuguro-Chumikanskiy region. The word ''Uda'' is derived from the Yakut word ''ud'', meaning "milk". The name was conferred on the river owing to a nearby milk-colored lake. Fish The Uda is a prime habitat for the pink, chum, red, and coho salmons. Other fish species found in the Uda include the Siberian taimen, two forms of lenok, and Amur grayling. The river is especially important as it remains one of the last strongholds of taimen, which have dwindled in other Siberian rivers. Taimens grow to huge sizes here; specimens weighing have been caught here. See also *Selenga Highlands *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 int ...
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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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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."opposite to a tributary"
PhysicalGeography.net, Michael Pidwir ...
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Selenga Highlands
The Selenga Highlands (russian: Селенгинское среднегорье) are a mountain area in Buryatia and the southwestern end of Zabaykalsky Krai, Russia. The highlands are named after the Selenga River. Protected areas in the highlands include the Baikal Nature Reserve and the Altacheysky Reserve. Geography The Selenga Highlands are located in central and southern Buryatia. They rise in the area of the basin of the Selenga River, including its large tributaries – Dzhida, Temnik, Chikoy, Khilok and Uda. From the north, the highlands are limited by the valleys of the Khamar-Daban and Ulan-Burgas ranges; in the east they are bound by the watershed of the Uda, Vitim and Shilka, bordering on the Vitim Plateau; in the southeast they limit with the Khentei-Daur Highlands; in the south lies the Mongolia–Russia border and in the southwest and west, the Selenga Highlands are bounded by the northern slopes of the Dzhidinsky Range and the southwestern slopes of t ...
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Valley Of The Uda River Near The Village Of Khorinsk
A valley is an elongated low area often running between Hill, hills or Mountain, mountains, which will typically contain a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacier, glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these glaciation, glacially formed valleys may have been created or enlarged during ice ages but now are ice-free and occupied by streams or rivers. In desert areas, valleys may be entirely dry or carry a watercourse only rarely. In karst, areas of limestone bedrock, dry valleys may also result from drainage now taking place cave, underground rather than at the surface. Rift valleys arise principally from tectonics, earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms th ...
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