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Par Collection Par Auteur- VÖTT, A. (3)
- BARETH, G. (2)
- CURDT, C. (2)
- HADLER, H. (2)
- PAPANIKOLAOU, I., (Directeur de publication) (2)
- REICHERTER, K., (Directeur de publication) (2)
- VÖTT, A., (Directeur de publication) (2)
- HOFFMEISTER, D. (2)
- AASEN, H. (1)
- BRÜCKNER, H. (1)
- HOUBEN, P., (Editeur scientifique) (1)
- NTAGERETZIS, K. (1)
- REICHERTER, K. (1)
- TILLY, N. (1)
- WILLERSHÄUSER, T. (1)
- WUNDERLICH, J., (Editeur scientifique) (1)
- KOSTER, B. (1)
- Années 2009-2011 ; Balayage laser terrestre ; Bilan sédimentaire ; Bloc ; Dynamique littorale ; Grèce ; Ile ; Littoral ; Mer Ionienne ; Modèle ; Pelopónnisos ; Tsunami ; Télédétection ; Vague (1)
- Atlantique ; Distribution spatiale ; Espagne ; GPR ; Golfo de Cádiz ; Grèce ; Géophysique ; Littoral ; Pelopónnisos ; Stratigraphie ; Sédimentologie ; Tsunamite (1)
- Atlántico ; Distribución espacial ; España ; Estratigrafía ; Geofísica ; Grecia ; Litoral ; Peloponeso ; Sedimentología (1)
- Balance sedimentario ; Dinámica litoral ; Grecia ; Isla ; Litoral ; Mar Ioniena ; Modelo ; Ola ; Peloponeso ; Teledetección ; Tsunami (1)
- Balayage laser terrestre ; Bloc ; Dislocation ; Dynamique littorale ; Grèce ; Kefallonia ; Littoral ; Modèle ; Pelopónnisos ; Technique de recherche ; Vague (1)
- Boulder ; Coastal dynamics ; Coastal environment ; Dislocation ; Greece ; Model ; Peloponnese ; Research technique ; Terrestrial laser scanning ; Wave (1)
- Boulder ; Coastal dynamics ; Coastal environment ; Greece ; Ionian Sea ; Island ; Model ; Peloponnese ; Remote sensing ; Sediment budget ; Terrestrial laser scanning ; Tsunami ; Wave (1)
- Dinámica litoral ; Grecia ; Litoral ; Modelo ; Ola ; Peloponeso ; Técnica de investigación (1)
- Reconstructing and modeling of paleotsunami events. Multi-proxy approaches, geophysical studies, numerical simulations (2)
- 3D model-based estimations of volume and mass of high-energy dislocated boulders in coastal areas of Greece by terrestrial laser scanning (1)
- Application of GPR for visualising spatial d distribution and internal structures of tsunami deposits ? Case studies from Spain and Greece (1)
- Monitoring annual changes of the coastal sedimentary budget in western budget Greece by terrestrial laser scanning terrestrial scanning (1)
- Past to present Quaternary landform change : natural and anthropogenic drivers (1)
- 3D model-based estimations of volume and mass of high-energy dislocated boulders in coastal areas of Greece by terrestrial laser scanning
- Boulder ; Coastal dynamics ; Coastal environment ; Dislocation ; Greece ; Model ; Peloponnese ; Research technique ; Terrestrial laser scanning ; Wave
- Boulders of 2 coastal areas (Cape Skalas in southern Lakonia, Peloponnese; Cape Gerogombos on Paliki Peninsula in western Greece were surveyed within their topographical context using a laser scanner in combination with a DGPS. 3D reconstruction
- allows the determination of highly accurate volumetric data, as well as the extraction of further parameters, such as elevation above sea level, inclination and distance to the sea for each boulder. The results show that terrestrial laser scanning
- the common method in scientific studies on boulder dislocation. The AA. found that volume data based on axes measurements together with density approximations result in a considerable overestimation of the mass of dislocated boulders.
- Boulder ; Coastal dynamics ; Coastal environment ; Greece ; Ionian Sea ; Island ; Model ; Peloponnese ; Remote sensing ; Sediment budget ; Terrestrial laser scanning ; Tsunami ; Wave
- to 2011. A Riegl LMS-Z420 i laser scanner was used in combination with a DGPS. Moreover, TLS-based volume and mass data of dislocated boulders encountered at several sites were incorporated into tsunami wave transport equations and compared to buoy data
- . High-energy dislocated boulders showed no movement during the monitoring period. Thus, it is assumed that they were been transported inland by extreme events, which were stronger than the average coastal dynamics between 2009 and 2011. Both
- the orientation and the spatial distribution pattern of the dislocated boulders match with observations of boulders dislocated by tsunami impact.
- covering wide areas of the harbour. GPR data indicate the variable thickness of tsunamigenic layers, channel-like structures of backwash deposits, and a non-planar erosion basement. Abrasion-scours were detected in various places and boulder accumulations