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The area crossed by the Tisza River has been con- tinuously subsiding during the Quaternary and is filled up by sediment of the rivers flowing from the Carpathians. The av- erage Quaternary subsidence rate was multiplied by the in- creased sediment compaction caused by the water and hy- drocarbon exploitation after river regulation. The rate of this subsidence shows a characteristic spatial variation. In the most subsiding areas this process increases the effect of the silting up of the floodway between the dykes and the occur- rence of thresholds in the longitudinal profile. These pro- cesses influence the mid- and long-term flood security of the region and a solution system is proposed here to handle the increased flood hazard. Besides this, the geomorphology of the Mid-Tisza region is shown by a detailed digital elevation model of a smaller area offering a tool for the re-assessment of the plans of flood control systems.

The effects of neotectonic and hydrological processes on the flood hazard of the Tisza region (East Hungary)