The main aim this paper is to reveal the hydrological impacts on the social and economic processes over the Dráva flood plain. AA. demonstrate how water regime and the micro relief have been influencing the economic and settlement relations
in Drava field have been performed in order to prevent the dispersion of farming land into smaller pieces and to increase the yield. The paper talks about the transformation of agriculture in Drava and Ptuj field after the year 1991 and evaluates the impact
commassation has on structural as well as productional changes in agriculture. The difference in the size of farms so far are due to social as well as landownership development, various land measures, earlier urbanization of Drava field, the geographical
Geomorphology and environmental history in the Drava valley, near Berzence
The geomorphological and environmental history case study aims at reconstructing the environmental conditions and the different ways of land use in the surroundings of Berzence in the Drava valley (S-Hungary). The area’s geomorphological evolution
Correlation of quaternary sediments and tectonic activity of the eastern part of the Drava river depression
Les sédiments de l'Holocène, du Pléistocène supérieur et moyen dans l'est de la dépression de la Drava sont composés, dans la partie inférieure, principalement de vases et d'argiles et, dans la partie supérieure de sables. Les données collectées
A jelenkori tektonika hatása a Duna, a tisza és a Dráva hidrológiai folyamataira
, 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 temperature and, resultantly, of the density of uplifting dacite- and other intrusions which have not metamorphosed the surrounding sediments. On the Pohorje by the river Drava (hereinafter the Drava Pohorje), the drainage network does not match the orography
, because, between the Vuzenica-Radlje basin and Fala, the Drava epigenetically deepened its gorge into the marginal range of Kobansko. Modest plateaus on the ridge of the Pohorje originate from the time when the base level maintained a cover of the so