José Luis Peña Monné, Morgan de Dapper, Ana Constante, Beata de Vliegher, K. Pavlopoulos
It have been analyzed the Dystos karst landscape in the island of Euboia (Greece). The objectives of research have been karst landforms spatial analysis, producing geomorphological maps, to establish the spatial delimitation of palaeopoljes, and their temporal evolution. We have studied on the evolution of Dystos poljes the effects of geological structure and climate influence. To do this analysis, poljes have been grouped in eleven units separated accordingly topographic criteria. The sequence of flattening and incision processes could be related with climate evolution and also tectonic activity during the Quaternary. Finally, we compared the results with similar landforms from Iberian Peninsula and other areas of Mediterranean Basin.
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