Геоморфологические условия процесса подтопления на территории г. Волгограда
Аннотация
The significance of topography in the waterlogging process is analysed with reference to the Volgograd territory at the right bank of the Volga. Special features of the water logging process are described which result from natural and artificial factors and also from their joint impact. Certain clusters of waterlogged sites are outlined.
Рецензия
Для цитирования:
Севостьянов В.В. Геоморфологические условия процесса подтопления на территории г. Волгограда. Геоморфология. 1990;(1):40-44.
For citation:
Sevostyanov V.V. Geomorphic conditions of waterlogging process in the city of Volgograd. Geomorfologiya. 1990;(1):40-44. (In Russ.)