Results coming from both DlnSAR and A-DlnSAR analyses allowed to define the deformation pattern of the areas including the active glacier flowing aside the morein, thus defining the behavior of this geomorphological structure. Thanks to the capability of satellite SAR systems, able to acquire information both during night and day and to penetrate the cloud coverage, information for the whole 2-years period was acquired despite the long polar-night period and the presence of not good visibility.