Independence Day of the Republic of Kazakhstan
Kazakhstan, also spelled Kazakstan, officially Republic of Kazakhstan, Kazakh Qazaqstan Respublikasï, country of Central Asia. It is bounded on the northwest and north by Russia, on the east by China, and on the south by Kyrgyzstan, Uzbekistan, the Aral Sea, and Turkmenistan; the Caspian Sea bounds Kazakhstan to the southwest.
Kazakhstan is the largest country in Central Asia and the ninth largest in the world. Between its most distant points, Kazakhstan measures about 1,820 miles (2,930 kilometres) east to west and 960 miles north to south. While Kazakhstan was not considered by authorities in the former Soviet Union to be a part of Central Asia, it does have physical and cultural geographic characteristics similar to those of the other Central Asian countries. The capital is Nur-Sultan (formerly Astana, Aqmola, and Tselinograd), in the north-central part of the country. Kazakhstan, formerly a constituent (union) republic of the U.S.S.R., declared independence on December 16, 1991.
Kazakhstan’s great mineral resources and arable lands have long aroused the envy of outsiders, and the resulting exploitation has generated environmental and political problems. The forced settlement of the nomadic Kazakhs in the Soviet period, combined with large-scale Slavic in-migration, strikingly altered the Kazakh way of life and led to considerable settlement and urbanization in Kazakhstan. The Kazakhs’ traditional customs uneasily coexist alongside incursions of the modern world.
Land - Relief
Lowlands make up one-third of Kazakhstan’s huge expanse, hilly plateaus and plains account for nearly half, and low mountainous regions about one-fifth. Kazakhstan’s highest point, Mount Khan-Tengri (Han-t’eng-ko-li Peak) at 22,949 feet (6,995 metres), in the Tien Shan range on the border between Kazakhstan, Kyrgyzstan, and China, contrasts with the flat or rolling terrain of most of the republic. The western and southwestern parts of the republic are dominated by the low-lying Caspian Depression, which at its lowest point lies some 95 feet below sea level. South of the Caspian Depression are the Ustyurt Plateau and the Tupqaraghan (formerly Mangyshlak) Peninsula jutting into the Caspian Sea. Vast amounts of sand form the Greater Barsuki and Aral Karakum deserts near the Aral Sea, the broad Betpaqdala Desert of the interior, and the Muyunkum and Kyzylkum deserts in the south. Most of these desert regions support slight vegetative cover fed by subterranean groundwater.
Depressions filled by salt lakes whose water has largely evaporated dot the undulating uplands of central Kazakhstan. In the north the mountains reach about 5,000 feet, and there are similar high areas among the Ulutau Mountains in the west and the Chingiz-Tau Range in the east. In the east and southeast, massifs (enormous blocks of crystalline rock) are furrowed by valleys. The Altai mountain complex to the east sends three ridges into the republic, and, farther south, the Tarbagatay Range is an offshoot of the Naryn-Kolbin complex. Another range, the Dzungarian Alatau, penetrates the country to the south of the depression containing Lake Balkhash. The Tien Shan peaks rise along the southern frontier with Kyrgyzstan.
Drainage
Kazakhstan’s east and southeast possess extensive watercourses: most of the country’s 7,000 streams form part of the inland drainage systems of the Aral and Caspian seas and Lakes Balkhash and Tengiz. The major exceptions are the great Irtysh, Ishim (Esil), and Tobol rivers, which run northwest from the highlands in the southeast and, crossing Russia, ultimately drain into Arctic waters. In the west the major stream, the Ural (Kazakh: Zhayyq) River, flows into the Caspian Sea. In the south the waters of the once-mighty Syr Darya have, since the late 1970s, scarcely reached the Aral Sea at all.
The torrent of the Irtysh River pours some 988 billion cubic feet (28 billion cubic metres) of water annually into the vast West Siberian catchment area. In the late 1970s Soviet authorities developed extensive plans to tap the Irtysh River for use in irrigating the arid expanses of Kazakhstan and Uzbekistan, but the scheme was killed in 1986 because of the large investment required and concern for the project’s possible adverse ecological consequences. This left southern and western Kazakhstan, as before, greatly in need of additional water resources. Kazakhstan also suffers from the disastrous depletion and the contamination (by pesticides and chemical fertilizers) of the Syr Darya flow, on which the republic depends greatly for crop irrigation.
The Caspian Sea, the largest inland body of water in the world, forms Kazakhstan’s border for 1,450 miles of its coastline. Other large bodies of water, all in the eastern half of the country, include Lakes Balkhash, Zaysan, Alaköl, Tengiz, and Seletytengiz (Siletiteniz). Kazakhstan also wraps around the entire northern half of the shrinking Aral Sea, which underwent terrible decline during the second half of the 20th century: as freshwater inflow was diverted for agriculture, the salinity of the sea increased sharply, and the receding shores became the source of salty dust and polluted deposits that ruined the surrounding lands for animal, plant, or human use.
Climate
Kazakhstan’s climate is sharply continental, and hot summers alternate with equally extreme winters, especially in the plains and valleys. Temperatures fluctuate widely, with great variations between subregions. Average January temperatures in northern and central regions range from −2 to 3 °F (−19 to −16 °C); in the south, temperatures are milder, ranging from 23 to 29 °F (−5 to −1.4 °C). Average July temperatures in the north reach 68 °F (20 °C), but in the south they rise to 84 °F (29 °C). Temperature extremes of −49 °F (−45 °C) and 113 °F (45 °C) have been recorded. Light precipitation falls, ranging from 8 to 12 inches (200 to 300 millimetres) annually in the northern and central regions to 16 or 20 inches in the southern mountain valleys.
Soils
Very fertile soils characterize the lands from far northern Kazakhstan down to the more infertile, alkaline soils of the middle and southern areas. The vast stretches of arable land in the northern plains are the most intensely cultivated and productive. Other cultivated areas fringe the mountains in the south and east; irrigation and reclamation, when feasible, extend along river valleys into the deserts. Nuclear bomb testing conducted during the Soviet period near Semey (Semipalatinsk) contaminated the soils in the vicinity.
Plant and animal life
The vegetation on plains and deserts includes wormwood and tamarisk, with feather grass on drier plains. Kazakhstan has very little wooded area, amounting to only about 3 percent of the territory. Many animals, including antelope and elk, inhabit the plains. The wolf, bear, and snow leopard, as well as the commercially important ermine and sable, are found in the hills. Fishermen take sturgeon, herring, and roach from the Caspian Sea. In parts of northeastern and southwestern Kazakhstan, where commercial fishing collapsed as a result of industrial and agricultural pollution, efforts to revive fish populations have shown some success. In 2008 Kazakhstan’s Naurzum and Korgalzhyn state nature reserves were named a UNESCO World Heritage site; both are important habitats for migrating birds, as well as for many other animal species.
People of Kazakhstan - Ethnic groups
Fewer than one-fifth of the more than eight million ethnic Kazakhs live outside Kazakhstan, mainly in Uzbekistan and Russia. During the 19th century about 400,000 Russians flooded into Kazakhstan, and these were supplemented by about 1,000,000 Slavs, Germans, Jews, and others who immigrated to the region during the first third of the 20th century. The immigrants crowded Kazakhs off the best pastures and watered lands, rendering many tribes destitute. Another large influx of Slavs occurred from 1954 to 1956 as a result of the Virgin and Idle Lands project, initiated by the Soviet premier Nikita Khrushchev, himself a Slav. This project drew thousands of Russians and Ukrainians into the rich agricultural lands of northern Kazakhstan. By 1989, however, Kazakhs slightly outnumbered Russians.
In the early years of independence, significant numbers of ethnic Russians in Kazakhstan emigrated to Russia. This emigration, along with a return to the country of ethnic Kazakhs, changed the demographic makeup of Kazakhstan: by the mid-1990s the Kazakh proportion was approaching half the total population, while that for the Russians was closer to one-third.
The trend persisted into the 21st century, as the Kazakh population neared two-thirds of the country’s total population while the Russian community represented just over one-fifth. Other ethnic groups in Kazakhstan include Uzbeks, Uighurs, and Tajiks, along with Ukrainians, Germans, Tatars, and Koreans.
The urban areas of Kazakhstan are still home to more Slavs than Kazakhs. Kazakhs constitute about half the inhabitants of Almaty, the country’s largest city and, until 1997, its capital. About three-fifths of Kazakh families live in rural areas. Urbanization in Kazakhstan involves much more immigration of foreigners than movement of Kazakhs from the countryside into the cities.
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Source: https://www.britannica.com/place/Kazakhstan