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Balkhash-Alakol Basin
The Balkhash-Alakol Basin or Balkhash-Alakol Depression( kk, Балқаш-Алакөл ойысы; rus, Балхаш-Алакольская котловина), is a flat structural basin in southeastern Kazakhstan.Балхаш-Алакольская котловина '''' in 30 vols. — Ch. ed. . - 3rd ed. - M. Soviet Encyclopedia, 1969-1978. (in Russian) |
Karaganda Region
Karaganda Region ( kk, Qarağandy oblysy; russian: Карагандинская область, translit=Karagandinskaja oblast′), also spelled Qaraghandy Region, is a region of Kazakhstan. Its capital is Karaganda. On 17 March 2022 it was announced that Karaganda would be divided, with the formation of the Ulytau Region. This officially came into force on 8 June 2022. History The region was the site of intense coal mining during the days of the Soviet Union and also the site of several Gulag forced labor camps. Following World War II, Joseph Stalin, leader of the Soviet Union, had many ethnic Germans deported to the area. There have been constant border changes within the region's history. The first took place in 1954 when it was ceded parts of Kustanay Oblast and parts of Taldy-Kurgan Oblast. In 1973, Dzhezkazgan Oblast was split off from Karaganda Oblast making it a fraction of the size it once was. In 1986, Karaganda Oblast was given the southern part of Tselinograd Obl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake Zaysan
Lake Zaysan (, ''Zaısan kóli'', زايسان كؤلئ, ; , ''Zaisan nuur'', en: ''Noble lake''; , ''Ozero Zajsan''; , Xiao'erjing: جَىْصْا پْ; dng, Җэсонпә) is a freshwater lake, ca. 1,810 km² (700 mi²), in eastern Kazakhstan, in a hollow between the Altai and the Tarbagatai Mountains. It is the largest lake in the East Kazakhstan Region. The lake lies at an altitude of 420 m, is 105 km long and 22–48 km wide, with a maximum depth of 15 m. Its major tributaries are the ''Kara Irtysh'' (Black Irtysh) and Kendyrlyk from the east; its only outlet is the Irtysh River (or White Irtysh). The lake is generally frozen from the beginning of November to the end of April, but still has an abundance of fish. Since the construction of the Bukhtarma dam on the Irtysh downstream from the Zaysan, the lake has risen 6 m (20 ft) above its natural level. As the result, the area of lake essentially increased (nearly doubled: from about 1,800 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dzungarian Alatau
The Dzungarian Alatau ( mn, Зүүнгарын Алатау, ''Züüngaryn Alatau''; ; kk, Жетісу Алатауы, ''Jetısu Alatauy''; russian: Джунгарский Алатау, ''Dzhungarskiy Alatau'') is a mountain range that lies on the boundary of the Dzungaria region of China and the Zhetysu region of Kazakhstan. It has a length of and a maximum elevation of . Features The Dzhungraian Alatau consists of foothills, ridges, forts, and alpine meadows of the Northern Tian Shan (Trans-Ili Alatau, Ktmen). It is located at an altitude of 2,000m above sea level, and is over 400km long in the latitudinal direction. The Dzhungraian Alatau consists of two ranges that are distinctly parallel to each other: the northern (or main), and the southern range. The area includes several sub-parallel high mountain ranges, accompanied by low and short ranges and their spurs. It also holds the largest waterfall in Central Asia. A distinctive feature of the Dzunguarain Alatau is a seri ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tarbagatai Mountains
The Tarbagatai Mountains ( mn, , , translit. ''Tarvagatai nuruu'', literally: "range with marmots"; ; kk, Тарбағатай жотасы, ''Tarbağatai jotasy'') are a range of mountains located in the north-western parts of Xinjiang, China, and the Abai Region of East Kazakhstan. The name of the mountain derived from Mongolian word: in Traditional Mongolian alphabet: mn, ( "tarvaga", meaning "marmot") with suffix mn, ( "-tai"; literally "to have" or "with"). Many Tarbagan marmot live in this mountain range. Their name does not have a direct translation from the English in Mongolian, as it would mean "marmot's marmot". An eastern extension of the Tarbagatai is the Saur Range. Drainage As it is common for mountain ranges, there is more precipitation in the Tarbagatai mountains than in the adjacent flatlands. The mountains are thus an important watershed. Streams from the northern slopes of the Tarbagatai flow into Lake Zaysan, which eventually drains (via the Irtysh ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Artesian Basin
An artesian aquifer is a confined aquifer containing groundwater under positive pressure. An artesian aquifer has trapped water, surrounded by layers of impermeable rock or clay, which apply positive pressure to the water contained within the aquifer. If a well were to be sunk into an artesian aquifer, water in the well-pipe would rise to a height corresponding to the point where hydrostatic equilibrium is reached. A well drilled into such an aquifer is called an ''artesian well''. If water reaches the ground surface under the natural pressure of the aquifer, the well is termed a ''flowing artesian well''. Fossil water aquifers can also be artesian if they are under sufficient pressure from the surrounding rocks, similar to how many newly tapped oil wells are pressurized. From the previous statement, it can be inferred that not all aquifers are artesian (i.e., water table aquifers occur where the groundwater level at the top of the aquifer is at equilibrium with atmosphe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tarbagatai Range
The Tarbagatai Mountains ( mn, , , translit. ''Tarvagatai nuruu'', literally: "range with marmots"; ; kk, Тарбағатай жотасы, ''Tarbağatai jotasy'') are a range of mountains located in the north-western parts of Xinjiang, China, and the Abai Region of East Kazakhstan. The name of the mountain derived from Mongolian word: in Traditional Mongolian alphabet: mn, ( "tarvaga", meaning "marmot") with suffix mn, ( "-tai"; literally "to have" or "with"). Many Tarbagan marmot live in this mountain range. Their name does not have a direct translation from the English in Mongolian, as it would mean "marmot's marmot". An eastern extension of the Tarbagatai is the Saur Range. Drainage As it is common for mountain ranges, there is more precipitation in the Tarbagatai mountains than in the adjacent flatlands. The mountains are thus an important watershed. Streams from the northern slopes of the Tarbagatai flow into Lake Zaysan, which eventually drains (via the Irt ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pleistocene
The Pleistocene ( , often referred to as the ''Ice age'') is the geological Epoch (geology), epoch that lasted from about 2,580,000 to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations. Before a change was finally confirmed in 2009 by the International Union of Geological Sciences, the cutoff of the Pleistocene and the preceding Pliocene was regarded as being 1.806 million years Before Present (BP). Publications from earlier years may use either definition of the period. The end of the Pleistocene corresponds with the end of the last glacial period and also with the end of the Paleolithic age used in archaeology. The name is a combination of Ancient Greek grc, label=none, πλεῖστος, pleīstos, most and grc, label=none, καινός, kainós (latinized as ), 'new'. At the end of the preceding Pliocene, the previously isolated North and South American continents were joined by the Isthmus of Panama, causing Great American Interchang ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pliocene
The Pliocene ( ; also Pleiocene) is the epoch in the geologic time scale that extends from 5.333 million to 2.58See the 2014 version of the ICS geologic time scale million years ago. It is the second and most recent epoch of the Neogene Period in the . The Pliocene follows the Epoch and is followed by the Epoch. Prior to the 2009 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
