During the Quaternary, eolian processes had dominantly morphological
importance in shaping of southeastern Banat. In morphology of this region,
therefore, dominates loess plains, Zagajica's ridge and Deliblato and
Banatian dune field. About the genesis of loess plains, Zagajica's ridge and
Deliblato dune field are different, very often opposite opinions. Meanwhile,
during the geomorphologic mapping of Vojvodina, at the end of nineties years
of last century and at the beginning of 21st century, the author of this
paper came to new conclusions, so he explains his opinion about relief of
southeastern Banat. Special attention was paid on morphology and
morphogenesis of Deliblato dunes field and Zagajica's ridge.
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