This project presents some aspects of the fields’ degradation by suffusion within the Eastern part of Southern Baragan.  The observations were performed in three points, in North, in Ciulnita Plain, in North-East and East of Hagieni Plain. Due to the precipitations’ water infiltrations on the abrupt front sides of the grounds and terraces there are some loess wells, which enable the torrential leakages and condition the formation of some tight and by stages with an aspect of  badlands.  The appearance of these geomorphologic processes determines practical problems by the degradation of sloping grounds.

loess; suffusion; degradation; Bărăgan

Presentation: oral