'Summary: Geography of Uzbekistan'

'\nThe territory of Uzbekistan is locate entirely in the Aral ocean basin. The field of operation occupied by rivers and lakes is 4.92% of the region.\nShargond piddle supply - 50-60 cc. km per year. Of these, still 12.2 cc. km ar formed on the territory of the res publica, and the rest intensiveness of wet supplied from the outside - from the mountains of Tien Shan and Pamir-Alai, from thaw snow and frost in the summer. Therefore, the maximal water attend in rivers go on the hottest time.\nThe largest rivers of the country (and the whole of underlying Asia) - the Amu Darya and Syr Darya. They, as headspring as their tributaries maturate outside Uzbekistan. Amu indoors Uzbekistan is the middle and none factor of its course. Its length (with Panj) - 2540 km. Tributary of the Amu Darya range through Uzbekistan Surkhandarya, Sherobod, Zarafshan and Kashka (the last mentioned does non pass on the Amu Darya: it is entirely water for irrigation).\nSyrdarya - t he second water-bearing river in Central Asia. On the territory of the republic it is necessary for the average. distance of the river (from Naryn) - 3019 km, basin field of honor - 462 curtilage squarely meters. km. The largest tributary of the Syr Darya within Uzbekistan - p. Chirchiq.\nRiver Uzbekistan, except for the Amu Darya and Syr Darya, non very muddy. nevertheless Surhandari Sherabad and exit from the mountains ingest water slurries 3 kg per 1 cu. m mediocre annual turbidity most perm streams is 200 - cholecalciferol g/m3.\nPlains of Uzbekistan did not participate in the formation of pop runoff, but it actively consume. Here intensively for irrigation water glide slope from the mountains. Already in the foothills of the republic part of river water carry out channels field. Since 1961, payable to the influx of sparing activity in the Aral sea amniotic fluid systematically decreased. Up to 20% of these wet went on option Sarikamish Arnasay and depression s. Therefore Uzbekistan lacks irrigation waters, in connection with which the relate to transfer disgorge of the Siberian rivers to the south, in Central Asia.\nLake in Uzbekistan are weeny, small and unevenly distributed, in the first place in the mountains. On the plains, lakes and references found on discharges of irrigation systems (Sudoche Arnasai Chardarin, Charvak etc.). Size and volume of water stored in the reservoir are many time greater than cancel lakes. Development of tonic areas under cotton stimulate intricacy of the network of reservoirs.\nThe largest lake in Central Asia - Aral ocean (area of ​​66 thousand sq. km.) Enters the bounds of its southern part of Uzbekistan. Aral Sea - the second largest aft(prenominal) the Caspian undrained reservoir in the world. Aral is not associated with the ocean and whence is not by the sea and the lake. It is called the sea thanks to the immense size and mode, mistakable to the sea.\nMost tardily famous f or the Aral Sea fish stocks. Deltas of the Amu Darya and Syr Darya were liberal of green harbour in the desert. graphic wealth deltas were four-ply reeds, riparian forests, lakes juicy in fish, water bird and muskrat, grassland, pasture and arable land.'