Iindaba kunye noMbuthoUbume

Umlambo waseKuban - ukusuka e-Elbrus ukuya eAzov

Eyona nxalenye esezantsi kwezona zinkulu zamanzi zaseRashiya - uMlambo waseKuban - uchongiwe ngokufanelekileyo umlambo omkhulu eNtshona Caucasus. Emva kokuthatha ixesha elide (malunga neekhilomitha eziliwaka) ukusuka emithambekeni eqingqiweyo yase-Elbrus kunye neendawo ezininzi zokuhamba kweStropol kunye neKrasnodar Territory, izisa amanzi ayo kwiTreeuk Bay ye-Azov Sea. Phantse zonke iinduna zeKuban ziqala ezintanjeni ze-Greater Caucasus kwaye zithwale amanzi azo ukusuka kwicala lasebhanini lasekhohlo. Ngakwesokudla, akukho ukuphuma okuphawulekayo okugeleza kuyo, kwaye ngoko ke umlambo umlambo uchaneka ngokukodwa kwesakhiwo sakhe. Ukuqala ukusuka kumthombo, i-Kuban ngumlambo weentaba, kwaye kumacandelo aphakathi kwaye aphantsi. Amanzi kuwo aphawulekayo ngenxa yobuthakathaka bawo. Ngomnyaka malunga neetoni ezili-9 ezilwanyana ezinqunyanyisiweyo zithwele emlonyeni. Phantse iikhilomitha ezilikhulu ukusuka emlanjeni woMlambo waseKuban, uhlukaniswe ngumkhono wesandla se-right of Protoka. Ukusuka kule ndawo uqala u-delta obanzi, indawo apho engaphezu kweekhilomitha ezili-4 zeekhilomitha. Le nto idla ngokukhukula iindawo ezinqabileyo zibizwa ngokuba zizikhukhula zeBuban.

Ukususela apho umlambo uKuban wawuthatha khona igama, akuqondwa ngokupheleleyo. Kukholelwa ukuba livela kwigama eliguqulelwe igama lesiTurkey lomlambo waseManan (oku kuthetha "umlambo"). Kwixesha elidala lalibizwa ngokuba nguHopanis (ekuguquleleni kweGrike yamandulo - "udlame, olunamandla umlambo"). Kwakhona kuthiwa yi-Psydzh (eguqulelwe ukusuka e-Adyghe njengowomlambo wasendulo), omnye uguquko "umlambo wamanina").

Ngokuhamba kwexesha, kungekhona nje igama lomlambo elitshintshileyo, kodwa nekhosi yalo. Apho i-delta yaseKuban itholakala khona ngoku, kwakukho iGulf enkulu yoLwandle lwaseAzov, esuka eTaman ukuya eKrasnodar. Nangona kunjalo, ngokuhamba kwexesha, ngokuyinhloko ngenxa yezizathu ze-tectonic kunye nangenxa yezikhunta zamadaka, intsimi yeTan Peninsula yatshintsha indawo yayo. Ngenxa yoko, esikhundleni sendawo, i-lagoon yakhiwa, yahlanjululwa ibhuloho yomhlaba, ekugqibeleni yaba enkulu. Isiphumo kukuba ngoku kwisayithi yolwandle i-delta. Kodwa kwi-XIX leminyaka uMlambo waseKuban waphuma waya kwi-Black Sea e-Kiziltash esitrateni ngokusebenzisa i-Old Kuban. Emva koko, umendo wakhe kule ndlela yavalwa.

Umlambo ubalulekile kuwo wonke ummandla waseNyakatho yeCaucasus. Kubonakaliswa ngumoya onobundlobongela kunye nokuhamba ngokukhawuleza kwinqanaba eliphezulu, njengoko lifikelela kuLwandle lwaseAzov, luya kuhlala luzolile, kwaye luye ngaphantsi komzi wase-Ust-Labinsk, iBuban ihamba ngomkhumbi. Ukongezelela, uMlambo waseKuban ungumthombo wamanzi aphelileyo, kwaye uqhuba nee-turbines zezikhululo zamandla ombane amaninzi, ezinika ummandla ngombane. Isithethe esasisiseko sokuhlala kwimida yamanzi, ngokukodwa, kwiKuban, yanika ubomi kwiidolophu ezinkulu kunye ezincinci: iArmavir, iKrasnodar, iNevinnomyssk, i-Slavyansk-kuban kunye nabanye abaninzi.

Kuban yindawo enhle yokuphumla. Umlambo udume kakhulu phakathi kwabalandeli ukuba bahambe kunye nokuhamba. Ukongezelela, iyaziwayo kwiintlanzi zayo. Apha kukho i-sturgeon stellate, i-sturgeon, i-bream, i-pike-perch, inkunzi yegusha, i-roach, i- zeirich, i-carp, i-cruciri, i-perch kunye nezinye iintlobo zeentlanzi.

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