The rate of bank retreat was measured using erosion pins on the alluvial banks rivers in Podhale region (the boundary zone between Central and Outer Carpathians) during hydrological year 2013/2014. During winter half-year (November–April), mainly caused by processes related to freezing thawing ground (swelling, creep, downfall). summer (May–October), fluvial mass movements such as lateral erosi...