Abstract:
The planimetric position of the river banks is a main parameter in detecting the areas affected by erosion and sediment
deposition, but also for studying the morph dynamics of the river bed. In order to measure, quantify, calculate and
monitor the statistics of the modification rate of the shore line, many researchers have used the software Digital
Shoreline Analysis System (DSAS) which works as an extension of the software Environmental System Research
Institute (ESRI) ArcGIS and which is using for this kind of statistics the multiple lines of the shore recorded at different
dates in time and obtained from different sources. Taking into account that the DSAS software uses polyline layers as a
representation of a certain shoreline at a certain time, we have used the polylines which represent the geographical
position in time of the right bank of the river Prut. The resulted statistics are the following: Net Shoreline Movment
(NSM), Shoreline Change Envelope (SCE), End Point Rate (EPR) and Linear Regression Rate (LRR). This provides a
thorough analysis of the change in time of the right bank of the river Prut, but cannot establish the force of the morpho
dynamics of the river bed.