The morphological evolution of the fluvial relief in the lowland areas is determined by the dynamic of the lateral channel migration process. River meandering and lateral channel migration represent continuous, dynamic and complex processes, which intensity modifies alluvial plains. Accordingly, it is a current topic observed from the domain of various scientific disciplines and practices, including the geographical aspect of the study. Directly or indirectly, variations of natural and anthropogenic processes affect changes in the lateral migration intensity, which is later manifested through permanent consequences for the environment. The aim of this paper is to investigate the process of lateral channel migration, through the review and i...
River channels are dynamic landforms that play an important role in understanding the alluvial chang...
River bank erosion, accretion and lateral channel migration are the most important geomorphological ...
River bank erosion, accretion and lateral channel migration are the most important geomorphological ...
The morphological evolution of the fluvial relief in the lowland areas is determined by the dynamic ...
Riverbank erosion and lateral channel migration are important geomorphological processes which cause...
The fluvial process is characterized by an intense meandering riverbed. The aim of this study was to...
Freely meandering (quasi)natural reaches of lowland rivers represent a rare phenomenon in Central Eu...
The fluvial process is characterized by an intense meandering riverbed. The aim of this study was to...
The river channel dynamics are result of the complex interaction between natural and human impact...
Lateral adjustments of Timiș river channel between 1965-2015. Until now, most of the studies regardi...
The bank erosion area, rate of bank retreat and overall geomorphological and financial effects of ch...
This thesis characterises and quantifies the influence of lateral ground-tilting on rivers in terms ...
The quasi-natural meandering type of alluvial rivers is quite unusual in Central European watersheds...
Since the 1990s, nature and water management policies have attempted to re-create natural rivers sys...
The bank erosion area, rate of bank retreat and overall geomorphological and financial effects of ch...
River channels are dynamic landforms that play an important role in understanding the alluvial chang...
River bank erosion, accretion and lateral channel migration are the most important geomorphological ...
River bank erosion, accretion and lateral channel migration are the most important geomorphological ...
The morphological evolution of the fluvial relief in the lowland areas is determined by the dynamic ...
Riverbank erosion and lateral channel migration are important geomorphological processes which cause...
The fluvial process is characterized by an intense meandering riverbed. The aim of this study was to...
Freely meandering (quasi)natural reaches of lowland rivers represent a rare phenomenon in Central Eu...
The fluvial process is characterized by an intense meandering riverbed. The aim of this study was to...
The river channel dynamics are result of the complex interaction between natural and human impact...
Lateral adjustments of Timiș river channel between 1965-2015. Until now, most of the studies regardi...
The bank erosion area, rate of bank retreat and overall geomorphological and financial effects of ch...
This thesis characterises and quantifies the influence of lateral ground-tilting on rivers in terms ...
The quasi-natural meandering type of alluvial rivers is quite unusual in Central European watersheds...
Since the 1990s, nature and water management policies have attempted to re-create natural rivers sys...
The bank erosion area, rate of bank retreat and overall geomorphological and financial effects of ch...
River channels are dynamic landforms that play an important role in understanding the alluvial chang...
River bank erosion, accretion and lateral channel migration are the most important geomorphological ...
River bank erosion, accretion and lateral channel migration are the most important geomorphological ...