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Shoreline displacement and Pineios River diversions in NW Peloponnese (Greece) as result of the geology,active tectonics and human activity during the last 100 ky
  • Shoreline displacement and Pineios River diversions in NW Peloponnese (Greece) as result of the geology,active tectonics and human activity during the last 100 ky
  • Quaternary geomorphology in tectonically active areas with emphasis in fluvio-coastal processes
  • Alluvial plain ; Channel geometry ; Coastal environment ; Coastline ; Drainage network ; Fault ; Geoarchaeology ; Greece ; Human impact ; Longitudinal section ; Neotectonics ; Palaeogeography ; Peloponnese ; Salt tectonics ; Stream ; Tectonics
  • The lower alluvial Pineios River has reacted to major geological controls, surface deformation and uplift movements caused by the activity of the recently mapped Pineios normal fault zone and salt tectonics in Kyllini peninsula resulting
  • in the river flow diversion from north to south at completely different open sea areas. The effects of the geological, tectonic and neotectonic activity and the impact of the human presence and influence on the lower Pineios River are presented in this paper
  • [b1] Fac. of Geology and Geoenvironment, Dept. of Dynamic, Tectonic and Applied Geology, Univ., Athènes, Grece
Comments on the neotectonics of the coastal zone of western Messenia based on luminescence dating and geoarchaeological evidence
  • Quaternary geomorphology in tectonically active areas with emphasis in fluvio-coastal processes
  • in order to yield ages of tectonic and eustatic changes. Besides, the coastal areas of Navarino have exhibited evidence of human activity since prehistoric times. Ancient human activity was controlled by coastal processes and thus its remains may comprise
  • important indicators of coastal displacement. Specifically, Hellenistic and Roman archaeological sites are useful markers of tectonic subsidence and thus they demonstrate localised diversions from the general pattern of uplift.
  • [b2] Fac. of Geology and Geoenvironment, Dept. of Dynamic, Tectonic and Applied Geology, Univ., Athènes, Grece
Morphological analysis and related volcanic features of the Kolumbo submarine volcanic chain (NE of Santorini Island, Aegean Volcanic Arc)
  • Quaternary geomorphology in tectonically active areas with emphasis in fluvio-coastal processes
  • Aegean Sea ; Bathymetry ; Greece ; Mediterranean Sea ; Plate tectonics ; Sea floor ; Slope gradient ; Submarine geomorphology ; Volcanism ; Volcano
Exploring the Avyssos-Yali-Strogyli submarine volcanic complex at the eastern edge of the Aegean Volcanic Arc
  • Quaternary geomorphology in tectonically active areas with emphasis in fluvio-coastal processes
Hydrogeomorphological vulnerability in the Romanian Plain
  • Quaternary geomorphology in tectonically active areas with emphasis in fluvio-coastal processes
Automated identification of geomorphological and topographical features of the seabed by object based image analysis of digital terrain models
  • Quaternary geomorphology in tectonically active areas with emphasis in fluvio-coastal processes
Reconstruction of modern debris flow activity in the arctic environment with the use of dwarf shrubs (south-western Spitsbergen) – a new dendrochronological approach
  • Quaternary geomorphology in tectonically active areas with emphasis in fluvio-coastal processes