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
A jelenkori tektonika hatása a Duna, a tisza és a Dráva hidrológiai folyamataira
Impact de l’activité tectonique à l’Holocène sur les processus hydrologiques du Danube, de la Tisza et de la Drave
Accumulation fluviatile ; Danube ; Distribution spatiale ; Drave ; Holocène ; Hongrie ; Hydrologie ; Plaine d'inondation ; Rupture de pente ; Tectonique ; Tisza ; Versant
, on the other hand, indicate very slight subsidence of basin lowlands in the Tisza and Drava valleys. The major area of Holocene accumulation on the active Danube floodplain is in the Paks-Mohács depression of prolonged subsidence in the Holocene, while
in the Tisza Valley it coincides with the North-Hungarian fault zone of NE to SW direction. - (AM)