Uly-Zhylanshyk
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Uly-Zhylanshyk
The Uly-Zhylanshyk ( kk, Ұлы Жыланшық; russian: Улы-Жыланшык) is a river in Kazakhstan. It is long and has a catchment area of . It is one of the rivers of the Turgay Depression, flowing across the Amangeldi and Zhangeldi districts of the Kostanay Region, Kazakhstan. Its waters are used for irrigation. Course The river is formed at the confluence of rivers Dulygaly-Zhylanshyk from the right and the Ulken-Zhylanshyk from the left. Both have their sources in the Ulutau range of the Kazakh Uplands. The Uly-Zhylanshyk flows roughly westwards all along its course, sometimes bending northwest for a certain distance and others to the southwest. As it reaches its last stretch the river meanders strongly. Finally it flows into the northeastern shore of lake Akkol, an endorheic salt lake located in Zhangeldi District, north of Shalkarteniz. The Uly-Zhylanshyk is fed mainly by snow.
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Akkol (lake)
Akkol, meaning "White Lake" ( kk, Ақкөл; russian: Акколь), is a salt lake in Zhangeldi District, in the SW sector of the Kostanay Region, Kazakhstan.Google Earth Local authorities try to promote tourism in the lake, but the area lacks the necessary infrastructure. The nearest inhabited locality is Akhmeta Baytursynuly to the east of the eastern shore. Geography Akkol is located in the southern part of the Turgay Depression at above sea level. It is an endorheic lake sharing the same depression as smaller lakes and salt pans nearby. A projecting spit in the northwestern shore of the lake divides the northern side into two bays. The lake lies about to the NNE of the northern end of the Shalkarteniz lake. Much smaller lakes Uziksor and Karaksor are located to the southeast, close to its shores. There is a hot spring from the lake where the water temperature reaches
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Ulutau
Ulutau ( kk, Ұлытау; russian: Улытау) is a range of mountains in Kazakhstan. Administratively the range is part of the Ulytau District, Karaganda region.Улытау
'''' in 30 vols. — Ch. ed. A.M. Prokhorov. - 3rd ed. - M. Soviet Encyclopedia, 1969–1978. (in Russian)


Geography

The Ulutau is one of the subranges of the Kazakh Upland system. The range stretches from north to south for about . Its highest point is high
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Kazakh Uplands
The Kazakh Uplands ( kk, Сарыарқа, ''Saryarqa'' - "Yellow Ridge", russian: Казахский мелкосопочник, Kazakhskiy Melkosopochnik), also known as the Kazakh Hummocks, is a large peneplain formation extending throughout the central and eastern regions of Kazakhstan.Казахский мелкосопочник (Kazakh Uplands)
'''' in 30 vols. — Ch. ed. . - 3rd ed. - M. Soviet Encyclopedia, 1969-1978. (in Russian)
Administratively the Kazakh Uplands stretch acros ...
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Turgay Depression
The Turgay Depression, also known as Turgay Basin, Turgay Trough, and Turgay Hollow ( kk, Торғай қолатый; rus, Тургайская ложбина), is a structural basin in Kazakhstan.Тургайская ложбина
'''' in 30 vols. — Ch. ed. . - 3rd ed. - M. Soviet Encyclopedia, 1969-1978. (in Russian)
The depression is named after the
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List Of Rivers Of Kazakhstan
This is a list of rivers of Kazakhstan, arranged by drainage basin. Tributaries are listed in order from mouth to source. Flowing into the Arctic Ocean Ob Irtysh (''Ertis'') River *Tobol **Ubagan ** Ayat ** Uy ** Syntasty * Ishim ** Imanburlyq ** Aqqanburlyq ** Terisaqqan ** Qalqutan * Shagan **Ashchysu * Uba * Ulba *Bukhtarma ** Lukina *Naryn *Kürshim Flowing into endorheic basins Caspian Depression *Volga River **Akhtuba (''distributary'') ***Kigach (''distributary'') *Ural River ** Shagan **Utva (''Shynghyrlau'') ** Ilek ***Kargaly ** Or * Bolshoy Uzen (''Ülken Özen'') * Maly Uzen (''Kishi Özen'') * Emba * Aschiagar River * Saghyz * Uil Aral Sea Syr Darya * Sarysu * Chu (''Shu'') ** Talas ***Asa ** Ak-Suu ** Kichi-Kemin * Bögen * Arys ** Badam *** Sayramsu ** Mashat **Boralday *Keles Akkol * Uly-Zhylanshyk Shalkarteniz * Turgay ** Irgiz **Ulkayak *Tegene *Zhyngyldyozek *Kalmakkyrgan *Baikonyr *Zhymyky Lake Tengiz * Nura Balkhash-Alakol Basin *Ili ** Charyn ** Chilik ** Es ...
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Rivers Of Kazakhstan
This is a list of rivers of Kazakhstan, arranged by drainage basin. Tributaries are listed in order from mouth to source. Flowing into the Arctic Ocean Ob Irtysh (''Ertis'') River * Tobol ** Ubagan ** Ayat ** Uy ** Syntasty * Ishim ** Imanburlyq **Aqqanburlyq **Terisaqqan **Qalqutan * Shagan **Ashchysu * Uba * Ulba *Bukhtarma ** Lukina *Naryn *Kürshim Flowing into endorheic basins Caspian Depression *Volga River **Akhtuba (''distributary'') ***Kigach (''distributary'') *Ural River ** Shagan ** Utva (''Shynghyrlau'') ** Ilek ***Kargaly ** Or * Bolshoy Uzen (''Ülken Özen'') * Maly Uzen (''Kishi Özen'') * Emba * Aschiagar River * Saghyz * Uil Aral Sea Syr Darya * Sarysu * Chu (''Shu'') ** Talas ***Asa ** Ak-Suu ** Kichi-Kemin * Bögen * Arys ** Badam *** Sayramsu ** Mashat **Boralday *Keles Akkol * Uly-Zhylanshyk Shalkarteniz * Turgay ** Irgiz ** Ulkayak *Tegene *Zhyngyldyozek *Kalmakkyrgan *Baikonyr *Zhymyky Lake Tengiz * Nura Balkhash-Alakol Basin *Ili ** Charyn ** Chilik ** ...
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Kazakhstan
Kazakhstan, officially the Republic of Kazakhstan, is a transcontinental country located mainly in Central Asia and partly in Eastern Europe. It borders Russia to the north and west, China to the east, Kyrgyzstan to the southeast, Uzbekistan to the south, and Turkmenistan to the southwest, with a coastline along the Caspian Sea. Its capital is Astana, known as Nur-Sultan from 2019 to 2022. Almaty, Kazakhstan's largest city, was the country's capital until 1997. Kazakhstan is the world's largest landlocked country, the largest and northernmost Muslim-majority country by land area, and the ninth-largest country in the world. It has a population of 19 million people, and one of the lowest population densities in the world, at fewer than 6 people per square kilometre (15 people per square mile). The country dominates Central Asia economically and politically, generating 60 percent of the region's GDP, primarily through its oil and gas industry; it also has vast mineral ...
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Amangeldi District
Amangeldi ( kk, Аманкелді ауданы, ) is a district of Kostanay Region in northern Kazakhstan Kazakhstan, officially the Republic of Kazakhstan, is a transcontinental country located mainly in Central Asia and partly in Eastern Europe. It borders Russia to the north and west, China to the east, Kyrgyzstan to the southeast, Uzbeki .... The administrative center of the district is the selo of Amangeldi. Population: References Districts of Kazakhstan Kostanay Region {{Kazakhstan-geo-stub ...
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Zhangeldi District
Zhangeldi ( kk, Жангелді ауданы, ) is a district of Kostanay Region in northern Kazakhstan. The administrative center of the district is the selo of Torgay. Population: Geography Lakes Kushmurun and Sarykopa Sarykopa ( kk, Сарықопа; russian: Сарыкопа) is a Bittern (salt), bittern salt lake in the Kostanay Region, Kazakhstan. Sarykopa lies in the steppe of the central sector of the Turgay Basin in Zhangeldi District, in the southern are ... are located in the district. References Districts of Kazakhstan Kostanay Region {{Kazakhstan-geo-stub ...
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Kostanay Region
Kostanay Region ( kk, Қостанай облысы, translit=Qostanai oblysy; russian: Костанайская область, translit=Kostanayskaya oblast) is a region of Kazakhstan. Its administrative center is the city of Kostanay. The population of the region is 900,300. The population living in Kostanay is 207,000 which is equivalent to 23% of the region. Geography Kostanay Region is adjacent to the Russian federal subjects Orenburg Oblast, Chelyabinsk Oblast, Kurgan Oblast, and is near the Ural Mountains. It also touches four other Kazakh regions: Aktobe Region to the southwest, Karaganda Region to the south, Akmola Region to the southeast, and North Kazakhstan Region to the northeast. The Tobol (Tobyl) River, a tributary of the Irtysh River, starts in and flows through the region on its way to Russia. Kostanay Region's area is 197,000 square kilometers, making it the sixth largest of the Kazakh regions. Flora and fauna Resources of an animal and flora of Kostan ...
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Meanders
A meander is one of a series of regular sinuous curves in the channel of a river or other watercourse. It is produced as a watercourse erodes the sediments of an outer, concave bank (cut bank) and deposits sediments on an inner, convex bank which is typically a point bar. The result of this coupled erosion and sedimentation is the formation of a sinuous course as the channel migrates back and forth across the axis of a floodplain. The zone within which a meandering stream periodically shifts its channel is known as a meander belt. It typically ranges from 15 to 18 times the width of the channel. Over time, meanders migrate downstream, sometimes in such a short time as to create civil engineering challenges for local municipalities attempting to maintain stable roads and bridges.Neuendorf, K.K.E., J.P. Mehl Jr., and J.A. Jackson, J.A., eds. (2005) ''Glossary of Geology'' (5th ed.). Alexandria, Virginia, American Geological Institute. 779 pp. Charlton, R., 2007. ''Fundamentals o ...
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Endorheic
An endorheic basin (; also spelled endoreic basin or endorreic basin) is a drainage basin that normally retains water and allows no outflow to other external bodies of water, such as rivers or oceans, but drainage converges instead into lakes or swamps, permanent or seasonal, that equilibrate through evaporation. They are also called closed or terminal basins, internal drainage systems, or simply basins. Endorheic regions contrast with open and closed lakes, exorheic regions. Endorheic water bodies include some of the largest lakes in the world, such as the Caspian Sea, the world's largest inland body of water. Basins with subsurface outflows which eventually lead to the ocean are generally not considered endorheic; they are cryptorheic. Endorheic basins constitute local base levels, defining a limit of erosion and deposition processes of nearby areas. Etymology The term was borrowed from French ''endor(rh)éisme'', coined from the combining form ''endo-'' (from grc, ἔν ...
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