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Shalkarteniz Basin
Shalkarteniz ( kk, Шалқартеңіз; russian: Шалкартениз) is an extensive Salt pan (geology), salt flat and seasonal lake in the Yrgyz District, Aktobe Region, Kazakhstan. The Shalkarteniz lies in the northeastern sector of the Turan Depression, northwest of the city of Aralsk. It is part of the Kazakh semi-desert ecoregion. There are no settlements in the immediate vicinity. History Until the end of the 16th century, the Shalkarteniz basin was regularly filled by the formerly more abundant waters of the Turgay (river), Turgay river, which at that time reached the Aral Sea. In the centuries that followed the river became shallow and carried less water, so the Shalkarteniz could not overflow. Thus the Turgay stopped flowing south and the depression lost its connection with the Aral Sea. By the 20th century, at the time of the Kazakh SSR, the degradation of the forest cover and extraction of water from the Turgay (river), Turgay and Irgiz (Turgay), Irgiz rivers inc ...
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Turgay Basin
Turgay is a Turkish given name for males. People named Turgay include: * Turgay Avcı, Turkish Cypriot politician * Turgay Bahadır, Turkish-Austrian footballer * Turgay Gemicibasi, Turkish footballer * Turgay Semercioğlu, Turkish footballer * Turgay Şeren, Turkish football manager Turgay may also refer to: * Turgay (river), a river in northern Kazakhstan * Turgay Depression, a structural basin in Kazakhstan * Turgay Plateau, in northern Kazakhstan * Turgay Oblast (Russian Empire), a former administrative division See also * Tugay (other) * Turgai (other) Turgai may refer to: * Turgay Oblast (Russian Empire), an administrative unit of the Russian Empire * Torgay Region, a former administrative unit in Kazakhstan * Turgay (river), a river-valley system in Kazakhstan * Turgai Sea The Turgai Sea, also ... {{given name Turkish masculine given names ...
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Endorheic Lake
An endorheic lake (also called a sink lake or terminal lake) is a collection of water within an endorheic basin, or sink, with no evident outlet. Endorheic lakes are generally saline as a result of being unable to get rid of solutes left in the lake by evaporation. These lakes can be used as indicators of anthropogenic change, such as irrigation or climate change, in the areas surrounding them. Lakes with subsurface drainage are considered cryptorheic. Components of endorheic lakes The two main ways that endorheic lakes accumulate water are through river flow into the lake (discharge) and precipitation falling into the lake. The collected water of the lake, instead of discharging, can only be lost due to either evapotranspiration or percolation (water sinking underground, e.g., to become groundwater in an aquifer). Because of this lack of an outlet, endorheic lakes are mostly salt water rather than fresh water. The salinity in the lake gradually builds up through years as wate ...
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Lakes Of Kazakhstan
Excluding the northernmost districts, Kazakhstan consists of endorheic basins, where rivers flow into one of the numerous lakes. The most important drainage system is known as Yedisu, meaning "seven rivers" in Turkic languages. Below is the list of the more important lakes, some of which are shared (Caspian Sea, Lake Aral, Lake Aike, etc.) with the neighbouring countries. References {{Europe topic, List of lakes of * Lakes 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 ...
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Shalkarteniz Basin
Shalkarteniz ( kk, Шалқартеңіз; russian: Шалкартениз) is an extensive Salt pan (geology), salt flat and seasonal lake in the Yrgyz District, Aktobe Region, Kazakhstan. The Shalkarteniz lies in the northeastern sector of the Turan Depression, northwest of the city of Aralsk. It is part of the Kazakh semi-desert ecoregion. There are no settlements in the immediate vicinity. History Until the end of the 16th century, the Shalkarteniz basin was regularly filled by the formerly more abundant waters of the Turgay (river), Turgay river, which at that time reached the Aral Sea. In the centuries that followed the river became shallow and carried less water, so the Shalkarteniz could not overflow. Thus the Turgay stopped flowing south and the depression lost its connection with the Aral Sea. By the 20th century, at the time of the Kazakh SSR, the degradation of the forest cover and extraction of water from the Turgay (river), Turgay and Irgiz (Turgay), Irgiz rivers inc ...
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List Of Lakes Of Kazakhstan
Excluding the northernmost districts, Kazakhstan consists of endorheic basins, where rivers flow into one of the numerous lakes. The most important drainage system is known as Yedisu, meaning "seven rivers" in Turkic languages. Below is the list of the more important lakes, some of which are shared (Caspian Sea, Lake Aral, Lake Aike, etc.) with the neighbouring countries. References {{Europe topic, List of lakes of * Lakes 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 ...
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Kamyshlov Log
The Kamyshlov Log ( rus, Камышловский лог or ''Урочище Камышловский лог''; kk, Камыстысай), is a former river valley of Siberia. Administratively it falls within Omsk Oblast, Siberian Federal District, of the Russian Federation, as well as the North Kazakhstan Region of Kazakhstan.Google Earth The first geographical observations about the Kamyshlov Log in the early 18th century described it as a flowing river, consisting in a chain of long lakes interconnected by channels, which seasonally dried up, but flowed again during periods of high water. However, by the 19th century most of the surrounding steppe was converted into agricultural fields and the flow between the lakes gradually stopped. The runoff along an almost imperceptible channel last took place in 1865 when the water reached the village of Poludino. Geography The Kamyshlov Log is part of the Ishim Plain, West Siberian Plain. It is the long ancient valley of the Kamyshlo ...
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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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Great Soviet Encyclopedia
The ''Great Soviet Encyclopedia'' (GSE; ) is one of the largest Russian-language encyclopedias, published in the Soviet Union from 1926 to 1990. After 2002, the encyclopedia's data was partially included into the later ''Bolshaya rossiyskaya entsiklopediya'' (or '' Great Russian Encyclopedia'') in an updated and revised form. The GSE claimed to be "the first Marxist–Leninist general-purpose encyclopedia". Origins The idea of the ''Great Soviet Encyclopedia'' emerged in 1923 on the initiative of Otto Schmidt, a member of the Russian Academy of Sciences. In early 1924 Schmidt worked with a group which included Mikhail Pokrovsky, (rector of the Institute of Red Professors), Nikolai Meshcheryakov (Former head of the Glavit, the State Administration of Publishing Affairs), Valery Bryusov (poet), Veniamin Kagan (mathematician) and Konstantin Kuzminsky to draw up a proposal which was agreed to in April 1924. Also involved was Anatoly Lunacharsky, People's Commissar of Education ...
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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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Karakol (lake)
Karakol ( ky, Каракол, Karakol, قاراقول, ; zh, 卡拉科尔), formerly Przhevalsk (russian: Пржевальск), is the fourth-largest city in Kyrgyzstan, near the eastern tip of Lake Issyk-Kul, about from the Kyrgyzstan–China border and from the capital Bishkek. It is the administrative capital of Issyk-Kul Region. Its area is , and its resident population was 84,351 in 2021 (both including Pristan'-Przheval'sk). To the north, on highway A363, is Tüp, and to the southwest Jeti-Ögüz resort. History A Russian military outpost founded on 1 July 1869, Karakol grew in the 19th century after explorers came to map the peaks and valleys separating Kyrgyzstan from China. In the 1880s Karakol's population surged with an influx of Dungans, Chinese Muslims fleeing warfare in China. In 1888, the Russian explorer Nicholay Przhevalsky died in Karakol of typhoid, while preparing for an expedition to Tibet; the city was renamed Przhevalsk in his honor. After local pr ...
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Bittern (salt)
Bittern (pl. bitterns), or nigari, is the salt solution formed when halite (table salt) precipitates from seawater or brines. Bitterns contain magnesium, calcium, and potassium ions as well as chloride, sulfate, iodide, and other ions. Bittern is commonly formed in salt ponds where the evaporation of water prompts the precipitation of halite. These salt ponds can be part of a salt-producing industrial facility, or they can be used as a waste storage location for brines produced in desalination processes. Bittern is a source of many useful salts. It is used as a natural source of Mg2+, and it can be used as a coagulant both in the production of tofu and in the treatment of industrial wastewater. History Bittern has been extracted for a long time, at least several centuries. The Dutch chemist Petrus Jacobus Kipp (1808–1864) experimented with saturated solutions of bittern. The term for the solution is a modification of "bitter". Uses Salt derivation Bittern is a source ...
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