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 interpretation of theoretical and methodological concepts and results of
contemporary scientific literature. In this paper, on specific sections of
the South Morava River (Serbia), the values of maximum lateral migration
over different time periods are determined. Three representative river
sectors were singled out, spatial and temporal dynamic was determined, while
the process of lateral channel migration was presented quantitatively and
graphically. Based on the obtained data, a comparative analysis showed
significant riverbank changes for the observed meanders, within the period
1924-2020. Special emphasis is on the analysis of the lateral channel
migration in the last decade of the mentioned period. The obtained results
can be further used in order to develop and implement plans of water and
land management, environmental protection and socio-economic development
strategies. [Project of the Serbian Ministry of Education, Science and Technological Development, Grant no. 176017]