Geological and oceanographic data determining the foreshore zone according to the Greek legislation

The available scientific field data of the marine and the coastal enviroment, (wind and wave field data, shallow area bathymetry, coastal area geomorphology and topography, etc.), in addition to deep and shallow wave prediction numerical modelling (by means of wind and bathymetry measurements), calc...

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Main Authors: K.G. PEHLIVANOGLOU, M. RAPPOU, M. MARTSOUKOU
Format: Article
Language:English
Published: Hellenic Centre for Marine Research 2006-06-01
Series:Mediterranean Marine Science
Online Access:https://ejournals.epublishing.ekt.gr/index.php/hcmr-med-mar-sc/article/view/12146
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spelling doaj-0d5410e32d2c4c99b4bc15d711ecdd8a2020-11-24T22:08:56ZengHellenic Centre for Marine ResearchMediterranean Marine Science1108-393X1791-67632006-06-0171152610.12681/mms.17410598Geological and oceanographic data determining the foreshore zone according to the Greek legislationK.G. PEHLIVANOGLOU0M. RAPPOU1M. MARTSOUKOU2The Greek Ombudsman, Independent Authority, Quality of Life Department, 5, Hatzigianni Mexi, 11528, AthensThe Greek Ombudsman, Independent Authority, Quality of Life Department, 5, Hatzigianni Mexi, 11528, AthensThe Greek Ombudsman, Independent Authority, Quality of Life Department, 5, Hatzigianni Mexi, 11528, AthensThe available scientific field data of the marine and the coastal enviroment, (wind and wave field data, shallow area bathymetry, coastal area geomorphology and topography, etc.), in addition to deep and shallow wave prediction numerical modelling (by means of wind and bathymetry measurements), calculation of the nearshore wave height and maximum wave run up, were used to support the mapping of the innermost limit of the foreshore zone according to Greek legislation which defi nes that ‘the foreshore is the zone of land wetted by the highest however unexceptional sea wave run up’ and the Supreme Administrative Court standard case law. These methods were applied for two areas, which completely differ as regards the wind and the wave field, the geomorphological and topographical characteristics of the coastal area, suggesting different procedures for the determination of the innermost limit of the foreshore zone. The limits of the foreshore zones for both areas, resulting from the study, are compared to the limits set out by the authorised Administrative Commissions, which were published in the Official Gazette and also were applied by the local authorities for the management of the coastal area.https://ejournals.epublishing.ekt.gr/index.php/hcmr-med-mar-sc/article/view/12146
collection DOAJ
language English
format Article
sources DOAJ
author K.G. PEHLIVANOGLOU
M. RAPPOU
M. MARTSOUKOU
spellingShingle K.G. PEHLIVANOGLOU
M. RAPPOU
M. MARTSOUKOU
Geological and oceanographic data determining the foreshore zone according to the Greek legislation
Mediterranean Marine Science
author_facet K.G. PEHLIVANOGLOU
M. RAPPOU
M. MARTSOUKOU
author_sort K.G. PEHLIVANOGLOU
title Geological and oceanographic data determining the foreshore zone according to the Greek legislation
title_short Geological and oceanographic data determining the foreshore zone according to the Greek legislation
title_full Geological and oceanographic data determining the foreshore zone according to the Greek legislation
title_fullStr Geological and oceanographic data determining the foreshore zone according to the Greek legislation
title_full_unstemmed Geological and oceanographic data determining the foreshore zone according to the Greek legislation
title_sort geological and oceanographic data determining the foreshore zone according to the greek legislation
publisher Hellenic Centre for Marine Research
series Mediterranean Marine Science
issn 1108-393X
1791-6763
publishDate 2006-06-01
description The available scientific field data of the marine and the coastal enviroment, (wind and wave field data, shallow area bathymetry, coastal area geomorphology and topography, etc.), in addition to deep and shallow wave prediction numerical modelling (by means of wind and bathymetry measurements), calculation of the nearshore wave height and maximum wave run up, were used to support the mapping of the innermost limit of the foreshore zone according to Greek legislation which defi nes that ‘the foreshore is the zone of land wetted by the highest however unexceptional sea wave run up’ and the Supreme Administrative Court standard case law. These methods were applied for two areas, which completely differ as regards the wind and the wave field, the geomorphological and topographical characteristics of the coastal area, suggesting different procedures for the determination of the innermost limit of the foreshore zone. The limits of the foreshore zones for both areas, resulting from the study, are compared to the limits set out by the authorised Administrative Commissions, which were published in the Official Gazette and also were applied by the local authorities for the management of the coastal area.
url https://ejournals.epublishing.ekt.gr/index.php/hcmr-med-mar-sc/article/view/12146
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