The fluctuation of water levels and its amplitude especially is the importent factors for rising of sliding deformation in the banks. Rapid drawdown of the water level is the most frequent example. It is typical of slightly peremeable clayey and silty or sand rocks.
The fluctuation of water levels and its amplitude especially is the importent factors for rising of sliding deformation in the banks. Rapid drawdown of the water level is the most frequent example. It is typical of slightly peremeable clayey and silty or sand rocks. (en)