Abstract
The geographical history of the Doñana National Park during the Quaternary is viewed as a necessary background to understanding the actual morphology and principal processes. At present, the geomorphology of the Doñana National Park is classified into three morphogenetic systems: aeolian, estuarine and littoral. This paper describes the geomorphological classification of the aeolian system (the eldest one) down to the level of morphoedaphic elements, which are recognized through a soil classification and vegetation study.
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