geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-1797geomorf-2596Research ArticleНаучные сообщенияShort communicationsПроцессы рельеф образования на осушившемся дне Аральского моря в районе древней Казалинской дельты СырдарьиRelief-forming processes at the emerged floor of the Aral Sea near former Kazalinsk delta of Syrdarya RiverГрязноваТ. П.GryaznovaT. P.Институт географии АН СССРРоссия19860911202201Геоморфология4755Copyright © Грязнова Т.П., 20222022Грязнова Т.П.Gryaznova T.P.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://geomorphology.igras.ru/jour/article/view/2596

The former floor of the Aral Sea, long developed under water and now emerged, becomes the area of subaerial exogenous processes, rosy eolian and halogenous ones. Eolian processes result in diverse biilt-up landforms or deflation hollows, depending on the floor sediments composition. The processes are responsible for rapid changes in the primary surf ace of the marine plains. At present it seems of great importance to study the rate of the exogenous processes as well as the transformation of the primary landforms of the emerged sea floor into zonal arid morphosculpture.

The former floor of the Aral Sea, long developed under water and now emerged, becomes the area of subaerial exogenous processes, rosy eolian and halogenous ones. Eolian processes result in diverse biilt-up landforms or deflation hollows, depending on the floor sediments composition. The processes are responsible for rapid changes in the primary surf ace of the marine plains. At present it seems of great importance to study the rate of the exogenous processes as well as the transformation of the primary landforms of the emerged sea floor into zonal arid morphosculpture.

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The authors declare that there are no conflicts of interest present.