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Home arrow Papers arrow V.V.Surkov - Stratification of natural terrains in floodplains as a function of river bed evolution and hydrological processes
V.V.Surkov - Stratification of natural terrains in floodplains as a function of river bed evolution and hydrological processes PDF Print E-mail
Written by Джахангир   
Tuesday, 07 January 2014
Stratification of morphological structure of the floodplain landscapes is determined by reduced influence of fluvial factors and increased role of non-fluvial factors with distance from the river bed. With an increase in river’s water content, the landscape structure of floodplains becomes complicated and the quantity of layer options increases - from 1-2 in stream plains to 15-20 in the floodplains of large rivers. The type of stratification and altitude ranges of terrains are determined by vertical river bed deformations and river water regime. 


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Last Updated ( Tuesday, 07 January 2014 )
 
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