Efterpi Koskeridou

TL;DR: In this article, the influence of physical and anthropogenic factors in landslide activity was identified and combined with a geographic information system (GIS) to evaluate the collected data and determine the relationship between physical and human activities and landslide activity, and the results proved that Plio-Pleistocene fine-grained sediments and flysch, relatively steep slopes (15°-30°) and a rise in the amount of rainfall increase landslide frequency and density.

TL;DR: An analysis of the relationships between skeletal organisms and fossil leaves and rhizomes shows that the majority of them lived together in the same seagrass-vegetated environment, were transported a short distance from their natural habitat, and buried very rapidly in fine-grained sediments, thus preserving this remarkable assemblage almost intact.

TL;DR: In this paper, the authors used historical data and old topographic maps to identify the flood hazard by using historic data in the drainage basin of Pinios (Peneus) River, in Thessaly, central Greece.

TL;DR: In this article, an integrated study combining data from field investigations, sedimentology, bio- and magnetostratigraphy, radiometric dating, palaeoecology, and palynology is presented.

TL;DR: Pollen records, marine faunal associations and stable isotope compositions of sediments from Rhodes, Greece, have been determined to track environmental changes in the eastern Mediterranean during the Early and Middle Pleistocene as mentioned in this paper.