The development and relationship between an alluvial plain and a neighboring alluvial fan was evaluated in the paper on the case of the Lower Tisza Region and the Maros alluvial fan. The paleo-channels on the surface differ in their size and channel
The Lower Tisza floodplain can be divided based on height conditions. The lower floodplain was probably the result of tectonic movement and river incision during the Late Pleistocene or the Holocene. However, the exact date and circumstances of its