Spatiotemporal Properties of Seismicity
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A Checklist of Greek Reptiles. II. the Snakes 3-36 ©Österreichische Gesellschaft Für Herpetologie E.V., Wien, Austria, Download Unter
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Herpetozoa Jahr/Year: 1989 Band/Volume: 2_1_2 Autor(en)/Author(s): Chondropoulos Basil P. Artikel/Article: A checklist of Greek reptiles. II. The snakes 3-36 ©Österreichische Gesellschaft für Herpetologie e.V., Wien, Austria, download unter www.biologiezentrum.at HERPETOZOA 2 (1/2): 3-36 Wien, 30. November 1989 A checklist of Greek reptiles. II. The snakes Liste der Reptilien Griechenlands. II. Schlangen BASIL P. CHONDROPOULOS ABSTRACT: The systematic status and the geographical distribution of the 30 snake taxa occurring in Greece are presented. Compared to lizards, the Greek snakes show a rather reduced tendency to form subspecies; from the total of 21 species listed, only 5 are represented by more than one subspecies. No endemic species has been recorded, though at the subspecific level 8 endemisms are known in the Aegean area. Many new locality records are provided. KURZFASSUNG: Der systematische Status und die geographische Verbreitung der 30 in Griechenland vorkommenden Schlangentaxa wird behandelt. Verglichen mit den Eidechsen zeigen die Schlangen in Griechenland eher eine geringe Tendenz zur Ausbildung von Unterarten; von ins- gesamt 21 aufgeführten Arten sind nur 5 durch mehr als eine Unterart repräsentiert. Keine endemi- sche Art wurde bisher beschrieben, obwohl auf subspezifischem Niveau 8 Endemismen im Raum der Ägäis bekannt sind. Zahlreiche neue Fundorte werden angegeben. KEYWORDS: Ophidia, Checklist, Greece INTRODUCTION The Greek snake fauna consists of 21 species belonging to 4 families: Typh- lopidae (1 species), Boidae (1 species), Colubridae (14 species) and Viperidae (5 species). Sixteen species are either monotypic or each one is represented in Greece by only one subspecies while the remaining rest is divided into a sum of 14 subspecies. -
Passive Seismic Interferometry & Shear Wave Splitting In
ΠΑΝΕΠΙΣΤΗΜΙΟ ΠΑΤΡΩΝ ΤΜΗΜΑ ΓΕΩΛΟΓΙΑΣ ΤΟΜΕΑΣ ΕΦΑΡΜΟΣΜΕΝΗ ΓΕΩΛΟΓΙΑΣ & ΓΕΩΦΥΣΙΚΗΣ ΕΡΓΑΣΤΗΡΙΟ ΣΕΙΣΜΟΛΟΓΙΑΣ Παθητική Σεισμική Συμβολομετρία & Ανισοτροπία Εγκαρσίων Κυμάτων στη διερεύνηση του Γήινου φλοιού ΔΗΜΗΤΡΙΟΣ Ν. ΓΙΑΝΝΟΠΟΥΛΟΣ Γεωλόγος, M.Sc. Εφαρμοσμένης Γεωλογίας & Γεωφυσικής Διδακτορική Διατριβή ΠΑΤΡΑ 2016 Passive Seismic Interferometry & Shear Wave Splitting in the investigation of the Earth's crust: application to the Corinth Rift, Greece a dissertation presented by Dimitrios N. Giannopoulos to The University of Patras, Department of Geology, Seismological Laboratory in partial fulfillment of the requirements for the degree of Doctor of Philosophy in Seismology Patras 2016 Frontpiece* © Alexandros Maragos ΗΡΑΚΛΕΙΤΟΣ, 535 - 475 Π.Κ.Χ. HERACLITUS, 535 - 475 BCE v University of Patras Faculty of Sciences Department of Geology Sector of Applied Geology & Geophysics Laboratory of Seismology Supervisory Committee Members: Ass. Prof. Efthimios Sokos (Supervisor) (Department of Geology, University of Patras) Prof. G-Akis Tselentis (National Observatory of Athens - Institute of Geodynamics) Prof. Georgios Oikonomou (Department of Physics, University of Patras) This to certify that we have read this dissertation and that in our opinion it is fully adequate, in scope of quality, as a dissertation for the degree of Doctor of Philosophy. Examining Committee Members: Assoc. Prof. Efthimios Sokos (Supervisor) (Department of Geology, University of Patras) ________________ Prof. G-Akis Tselentis (Department of Geology, University of Patras | National Observatory of Athens - Institute of Geodynamics) ________________ Prof. Georgios Oikonomou (Department of Physics, University of Patras) ________________ Prof. Ioannis Koukouvelas (Department of Geology, University of Patras) ________________ Prof. Anastasia Kiratzi (Department of Geophysics, Aristotle University of Thessaloniki) ________________ Prof. Panayiotis Papadimitriou (Faculty of Geology-Geoenvironment, University of Athens) ________________ Ass. -
Field Trip Guide, 2011
Field Trip Guide, 2011 Active Tectonics and Earthquake Geology of the Perachora Peninsula and the Area of the Isthmus, Corinth Gulf, Greece Editors G. Roberts, I. Papanikolaou, A. Vött, D. Pantosti and H. Hadler 2nd INQUA-IGCP 567 International Workshop on Active Tectonics, Earthquake Geology, Archaeology and Engineering 19-24 September 2011 Corinth (Greece) ISBN:ISBN: 978-960-466-094-0 978-960-466-094-0 Field Trip Guide Active Tectonics and Earthquake Geology of the Perachora Peninsula and the area of the Isthmus, Corinth Gulf, Greece 2nd INQUA-IGCP 567 International Workshop on Active Tectonics, Earthquake Geology, Archaeology and Engineering Editors Gerald Roberts, Ioannis Papanikolaou, Andreas Vött, Daniela Pantosti and Hanna Hadler This Field Trip guide has been produced for the 2nd INQUA-IGCP 567 International Workshop on Active Tectonics, Earthquake Geology, Archaeology and Engineering held in Corinth (Greece), 19-24 September 2011. The event has been organized jointly by the INQUA-TERPRO Focus Area on Paleoseismology and Active Tectonics and the IGCP-567: Earthquake Archaeology. This scientific meeting has been supported by the INQUA-TERPRO #0418 Project (2008-2011), the IGCP 567 Project, the Earthquake Planning and Protection Organization of Greece (EPPO – ΟΑΣΠ) and the Periphery of the Peloponnese. Printed by The Natural Hazards Laboratory, National and Kapodistrian University of Athens Edited by INQUA-TERPRO Focus Area on Paleoseismology and Active Tectonics & IGCP-567 Earthquake Archaeology INQUA-IGCP 567 Field Guide © 2011, the authors I.S.B.N. 978-960-466-094-0 PRINTED IN GREECE Active Tectonics and Earthquake Geology of the Perachora Peninsula and the area of the Isthmus, Corinth Gulf, Greece (G. -
Sedimentary Impacts of Recent Moderate Earthquakes from the Shelves to the Basin floor in the Western Gulf of Corinth
MARGO-05536; No of Pages 22 Marine Geology xxx (2016) xxx–xxx Contents lists available at ScienceDirect Marine Geology journal homepage: www.elsevier.com/locate/margo Sedimentary impacts of recent moderate earthquakes from the shelves to the basin floor in the western Gulf of Corinth Arnaud Beckers a,b,⁎, Christian Beck b, Aurelia Hubert-Ferrari a, Jean-Louis Reyss c, Clément Mortier a, Paola Albini d, Andrea Rovida d, Anne-Lise Develle e, Efthymios Tripsanas f, Dimitris Sakellariou g, Christian Crouzet b,OonaScottih a Dept of Geography, University of Liège, allée du 6 août 2, 4000 Liège, Belgium b ISTerre, CNRS UMR 5275, University of Savoie, F-73376 Le Bourget du Lac, France c LSCE, CNRS UMR 8212, avenue de la Terrasse, 91198, F-91191 Gif-sur-Yvette, France d Istituto Nazionale di Geofisica e Vulcanologia, Via E. Bassini, 15, 20133 Milano, Italy e EDYTEM, University of Savoie/CNRS, Le Bourget du Lac, France f Shell U.K. Limited, London, United Kingdom g Institute of Oceanography, Hellenic Center for Marine Research, GR-19013 Anavyssos, Greece h Institut de Radioprotection et de Sûreté Nucléaire (IRSN), Fontenay-aux-Roses, France article info abstract Article history: In seismically active areas, long term records of large earthquakes are indispensable to constrain reccurence pat- Received 28 October 2015 terns of large earthquakes. In the western Corinth Rift, one of the most active areas in Europe in terms of seismic- Received in revised form 30 September 2016 ity, data about ancient earthquakes are still insufficient, despite historical records covering the last two millenia Accepted 29 October 2016 and several studies in onshore paleoseimology. -
Entipo-Toutist.Pdf
Εύηνος… «Το ποτάμι λεωφόρος των βουνών» Evinos… the river “avenue” of the mountains Φαράγγι Βουραϊκού… Mαγεμένοι από το τοπίο, συνεπαρμένοι από την ιστορία. Vouraikos Gorge …enchanted by the landscape, overwhelmed by the history Αλφειός... O ερωτευμένος ποταμός! Alfios…the river in love! Αχελώος… Το Κέρας της Αμάλθειας είναι ο ίδιος ο ποταμός, που θα σας μαγέψει .... Acheloos…the river is the Horn of Plenty itself, it will enchant you…. Εύηνος… «Το ποτάμι λεωφόρος των βουνών» Evinos… the river “avenue” of the mountains Φαράγγι Βουραϊκού… Mαγεμένοι από το τοπίο, συνεπαρμένοι από την ιστορία. Vouraikos Gorge …enchanted by the landscape, overwhelmed by the history Αλφειός... O ερωτευμένος ποταμός! Alfios…the river in love! Αχελώος… Το Κέρας της Αμάλθειας είναι ο ίδιος ο ποταμός, που θα σας μαγέψει .... Acheloos…the river is the Horn of Plenty itself, it will enchant you…. EvinosΕύηνος Στο ρου του Ευήνου The flow of Evinos Ο Εύηνος είναι το ποτάμι της Ναυπακτίας που διατρέχει διαγώνια τη γη Evinos is the river of Nafpaktia, which crosses its land diagonally, with της με κατεύθυνση από τα ΒΑ προς τα ΝΔ. Οι πηγές του εντοπίζονται στα a direction from NE to SW. Its spring is found on Vardousia, Sarantena όρη Βαρδούσια, Σαράνταινα και Κοκκινιάς και διανύει 113 χλμ. ως την and Kokkinia Mts and it runs 113 kilometers before flowing into Patraikos εκβολή του στον Πατραϊκό κόλπο. Ο Εύηνος συνδέεται με πολλούς αρχαι- Gulf. Evinos is related to many ancient Greek myths, to Ancient Aetolia, as οελληνικούς μύθους, την Αρχαία Αιτωλία, την κοινωνική και οικονομική well as to the social and economic life of the area. -
Print Sheet Remote1
Отдалечени места към Зона I, II и III П.Код Населено място П.Код Населено място П.Код Населено място П.Код Населено място 11361 KICELI 27100 KERAMIDIA 44015 LAGKADA 70004 KSEROKABOS 12351 AGIA VARVARA 27100 MONI FRAGKOPIDIMATOS 44015 LIKORRAXI 70004 PERVOLA 13561 AGII ANARGIRI 27100 TRAGANO 44015 OKSIA 70004 PEFKOS 13672 PARNITHA 27200 AGIA MARINA 44015 PLAGIA 70004 SKAFIDIA 13679 AGIA TRIADA PARNITHAS 27200 ANALICI 44015 PLIKATI 70004 STAFRIA 13679 KSENIA PARNITHAS 27200 ASTEREIKA 44015 PIRSOGIANNI 70004 SIKOLOGOS 14451 METAMORFOSI 27200 PALEOLANTHI 44015 XIONADES 70004 SINDONIA 14568 KRIONERI 27200 PALEOXORI 44017 AGIA VARVARA 70004 TERTSA 15342 AGIA PARASKEFI 27200 PERISTERI 44017 AGIA MARINA 70004 FAFLAGKOS 18010 AGIA MARINA 27300 AGIA MAFRA 44017 VEDERIKOS 70004 XONDROS 18010 AGKISTRI 27300 KALIVIA 44017 VERENIKI 70004 CARI FORADA 18010 EGINITISSA 28080 AGIOS NIKOLAOS 44017 VROSINA 70005 AVDOU 18010 ALONES 28080 GRIZATA 44017 VRISOULA 70005 ANO KERA 18010 APONISOS 28080 DIGALETO 44017 GARDIKI 70005 GONIES 18010 APOSPORIDES 28080 ZERVATA 44017 GKRIBOVO 70005 KERA 18010 VATHI 28080 KARAVOMILOS 44017 GRANITSA 70005 KRASIO 18010 VATHI 28080 KOULOURATA 44017 DIXOUNI 70005 MONI KARDIOTISSAS 18010 VIGLA 28080 POULATA 44017 DOVLA 70005 MOXOS 18010 VLAXIDES 28080 STAVERIS 44017 DOMOLESSA 70005 POTAMIES 18010 GIANNAKIDES 28080 TZANEKATA 44017 ZALOGO 70005 SFENDILI 18010 THERMA 28080 TSAKARISIANOS 44017 KALLITHEA 70006 AGIA PARASKEFI 18010 KANAKIDES 28080 XALIOTATA 44017 KATO VERENIKI 70006 AGNOS 18010 KLIMA 28080 XARAKTI 44017 KATO ZALOGO -
Influence of Bottom Currents on the Sedimentary Processes At
Marine Geology 378 (2016) 312–332 Contents lists available at ScienceDirect Marine Geology journal homepage: www.elsevier.com/locate/margo Influence of bottom currents on the sedimentary processes at the western tip of the Gulf of Corinth, Greece A. Beckers a,b,⁎, C. Beck b, A. Hubert-Ferrari a, E. Tripsanas c, C. Crouzet b, D. Sakellariou d, G. Papatheodorou e, M. De Batist f a Department of Geography, University of Liège, Liège B-4000, Belgium b ISTerre, CNRS UMR 5275, University Savoie Mont Blanc, Le Bourget du Lac F-73376, France c Shell U.K. Limited, Specialist Geology Team, Aberdeen AB12 3FY, UK d Institute of Oceanography, Hellenic Center for Marine Research, Anavyssos GR-19013, Greece e Laboratory of Marine Geology and Physical Oceanography, Department of Geology, University of Patras, Patras 26500, Greece f Renard Centre of Marine Geology, University of Gent, Gent B-9000, Belgium article info abstract Article history: We investigated the sedimentary processes that were active during the Holocene in the Gulf of Corinth, using Received 10 May 2015 high-resolution seismic reflection profiles and gravity cores. Seismic reflection data clearly show the presence Received in revised form 31 January 2016 of shallow-water sediment drifts at the western end of the Gulf, close to the Rion sill that links the Gulf to the Accepted 3 March 2016 Ionian Sea. Short cores indicate that drifts are composed of homogenous bioturbated mud in their upper part. Available online 4 March 2016 The drift deposits flank a wide central area where the seafloor is eroded and where pre-Holocene deposits locally Keywords: outcrop. -
Late Quaternary and Holocene Faults of the Northern Gulf of Corinth Rift, Central Greece
Δελτίο της Ελληνικής Γεωλογικής Εταιρίας, τόμος L, σελ. 164-172 Bulletin of the Geological Society of Greece, vol. L, p. 164-172 Πρακτικά 14ου Διεθνούς Συνεδρίου, Θεσσαλονίκη, Μάιος 2016 Proceedings of the 14th International Congress, Thessaloniki, May 2016 LATE QUATERNARY AND HOLOCENE FAULTS OF THE NORTHERN GULF OF CORINTH RIFT, CENTRAL GREECE Valkaniotis S.1 and Pavlides S.1 1Aristotle University of Thessaloniki, Department of Geology, 54124, Thessaloniki, Greece, [email protected], [email protected] Abstract New results for the recent tectonic activity in the northern part of the Gulf of Corinth rift are presented. Geological mapping and morphotectonic study re-populate the area of study with numerous active and possible active faults. The area is dominated by individual and segmented normal faults along with major structures like Marathias and Delphi-Arachova faults. The results are in accordance with recent studies that reveal a more complex and wider structure of Corinth Rift to the north. Keywords: Active Tectonics, Seismic Hazard, Normal Faults, Extension, Delphi Fault. Περίληψη Νέα δεδομένα για την πρόσφατη τεκτονική δραστηριότητα στο βόρειο τμήμα του βυθίσματος του Κορινθιακού Κόλπου παρουσιάζονται. Με βάση γεωλογική χαρτογράφηση και λεπτομερή μορφοτεκτονική μελέτη, η περιοχή μελέτης εμπλουτίζεται με πολυάριθμα ενεργά και πιθανά ενεργά ρήγματα. Στην περιοχή επικρατούν μεμονωμένα και συνενωμένα κανονικά ρήγματα, καθώς και μεγάλες κύριες τεκτονικές δομές όπως τα ρήγματα Μαραθιά και Δελφών-Αράχωβας. Ta αποτελέσματα έρχονται σε συμφωνία με πρόσφατες μελέτες που αποκαλύπτουν μια περίπλοκη και πιο ευρεία δομή της τάφρου του Κορινθιακού στα βόρεια. Λέξεις κλειδιά: Ενεργός τεκτονική, Σεισμική Επικινδυνότητα, Κανονικά Ρήγματα, Εφελκυσμός, Ρήγμα Δελφών. 1. Introduction The Gulf of Corinth Rift is a rapidly expanding intra-continental extensional rift in a W-E setting, across the Alpine formations of the External Hellenides Geotectonic units of Pindos, Vardoussia, Parnassos and Beotia (Celet, 1962; Doutsos et al., 1988; Ori, 1989; Armijo et al., 1996). -
Appendix 1 Q Q Qip Q
APPENDIX 1 MAIN PARAMETERS OF TSUNAMIS IN THE MEDITERRANEAN SEA• Coordinates Max. Cause of earthquake Magni- Site of intensity Reliabi- Year of or volcano, tude, manifestation of lity of tsunami deg. of tsunami tsunami data N I E M iiiiiiJ< The Sea of Marmara (SM) 120 E 40.7 29.1 7.2 2 p 447 E? 40.2 28.0. 7.3 4 LIR 542 - 40.3 27.8 6.8 4 L/R 558? 40.9 28.8 7.0 - p 740 E 40.7 29.3 7.3 3 L 975? ? --- 3 p 1039 E? 38.4 27.3 6.8 - Q 1265 E 40.7 27.4 6.6 2 p 1332 E 40.9 28.9 6.8 3+ p 1344 E 40.8 28.8 6.9 4 LIR 1509 E 40.8 28.1 7.7 3- L 1646 E --- 3 p 1766 E 40.8 29.0 6.5 2 p 1829 E 41.1 24.3 7.3 2 p 1857 E 40.2 29.0 - - Q 1878 E 40.8 29.0 6.7 3 QIP 1894 E 40.6 28.7 6.7 3 p 1912 E 40.6 27.2 7.6 - p 1999 E 40.7 29:8 7.4 - p North Greece (NG) ' -479 E 39.7 23.3 6.7 Chalkidiki Peninsula 3 L 1902 E 40.8 23.4 6.6 Thessaloniki 2 L 1928 E 40.8 26.8 6.2 Gulf of Strimon 2 p 1932 E 40.5 23.9 7.0 Chalkidiki Peninsula 3 R 1978 E 40.8 23.2 6.5 Gulf of Strimon 2- p East Greece (EG) -426 E? 38.9 22.7 7.1 Gulf of Euboea 4 L 426 E --- Gulf of Euboea 4- L 552 E+L 38.4 22.3 7.1 Gulf of Euboea 4- p 1853 E 38.3 23.4 7.0 Gulf of Euboea 3+ p 1859 ? --- Piraeus 2- Q 1894 E+L 38.7 23.1 7.0 Gulf of Euboea 4 R 1928 E+L 38.0 23.0 5.0 Chalkida 3 L 1956 E 39.3 23.1 5.6 Volos 3 L • Symbols are listed after the table. -
BEACHES 15 MARINAS FLAG SUSTAINABLE TOURISM &1TOURISM BOAT Chanioti 1 35
519 BLUE BEACHES 15 MARINAS FLAG SUSTAINABLE TOURISM &1TOURISM BOAT Chanioti 1 35. Vari-Voula-Vouliagmeni EVROS R.U. [2] Chanioti 3/Grecotel Pella Beach Municipality 3 1. Alexandroupoli 6 14. Polygyros Municipality Asteras Vouliagmenis/Astir 5 Municipality Beach Vouliagmenis 7 Gerakini/Ikos Olivia Alexandroupollis Municipal Varkiza 2 WERE AWARDED Sargani/Blue Dolphin 4 Beach Voula A 9 1 Kyani Akti 15. Nea Propontida Vouliagmeni 10 Municipality BLUE FLAGS IN RODOPI R.U. [4] 36. Glyfada Municipality 11 Agios Mamas 8 Glyfada 15 2. Komotini Municipality Vergia 14 Glyfada A Arogi Geoponika-Mykoniatika 16 Glyfada B Mesi Dionysiou 12 Fanari/Camping Eleonas/Ikos Oceania 37. Aegina Municipality 1 Fanari/Ioulia 17 3 Nea Heraklia Agia Marina 63 1 XANTHI R.U. [5] Nea Heraklia-Sahara 38. Poros Municipality 18 2 13 3. Topiros Municipality Nea Kallikratia Askeli/Nea Egli 11 98 Erasmio Nea Moudania 39. Kythira Municipality 62 Mangana Nea Plagia 2018 Kakia Lagada Nea Potidea Propontidas 19 Kapsali 61 4. Avdira Municipality Nea Potidea/Portes Beach 21 Avdira/Porto Molo Nea Potidea-East of the KORINTHIA R.U. [7] 20 22 Mandra Toroneo Canal 40. Loutraki - Agii Theodori 60 www.blueflag.gr Myrodato 23 Portaria Municipality 9 97 KAVALA R.U. [11] Sozopoli Centre Loutraki 1 10 4 5. Nestos Municipality Sozopoli/Naftilos Loutraki 2 64 www.eepf.gr/blueflag Triglia Ammoglossa-Keramoti 1 Loutraki-Boutsi/Poseidon Resort 24 Flogita Ammoglossa-Keramoti 2 59 26 41. Velo-Vocha Municipality 27 28 25 30 PIERIA R.U. [12] Vrahati www.blueflag.global 6. Kavala Municipality 96 Kalamitsa 16. Katerini Municipality Kokkoni 65 29 Batis Kallithea 42. -
Deformation Estimation of an Earth Dam and Its Relation with Local
Deformation estimation of an earth dam and its relation with local earthquakes, by exploiting multitemporal synthetic aperture radar interferometry: Mornos dam case (Central Greece) Spiros Neokosmidis Panagiotis Elias Issaak Parcharidis Pierre Briole Spiros Neokosmidis, Panagiotis Elias, Issaak Parcharidis, Pierre Briole, “Deformation estimation of an earth dam and its relation with local earthquakes, by exploiting multitemporal synthetic aperture radar interferometry: Mornos dam case (Central Greece),” J. Appl. Remote Sens. 10(2), 026010 (2016), doi: 10.1117/1.JRS.10.026010. Deformation estimation of an earth dam and its relation with local earthquakes, by exploiting multitemporal synthetic aperture radar interferometry: Mornos dam case (Central Greece) Spiros Neokosmidis,a,* Panagiotis Elias,b Issaak Parcharidis,a and Pierre Briolec aHarokopio University of Athens, Department of Geography, El. Venizelou 70, Athens 17672, Greece bNational Observatory of Athens, Institute of Astronomy, Astrophysics, Space Applications and Remote Sensing, I. Metaxa & Vas. Pavlou, Penteli 152 36, Greece cCNRS, Ecole Normale Superieure, Department of Geosciences, Paris 75231, France Abstract. Monitoring dam performance is a critical parameter in maintaining a safe dam. Safety concerns include seepage, internal erosion, and seismic issues in the case that the dam is located in high seismic hazard areas. Seismic considerations for dam safety among others includes the expected dam’s performance during seismic events. The scope of this research work concerns the capability to record potential deformation on the Mornos earth dam (central Greece) induced by major earthquake events that occurred in the broader area. For this purpose, a hybrid interfer- ometry synthetic aperture radar (InSAR) method was applied using elements of conventional differential InSAR, short baseline interferometry approaches, and persistent scatterers interfer- ometry. -
Beaches Marinas
BLUE FLAG MARINAS BEACHES 3 7 6 12 9 8 4 2 486 10 1 11 12 5 WERE AWARDED BLUE FLAGS IN 16 15 www.blueflag.gr 2017 17 13 www.eepf.gr/blueflag Sani Dunes Loutra Kyllinis 1/Grecotel 18 EVROS [2] VIOTIA [2] Olympia Riviera Oasis 63 1 1. Alexandroupoli Municip. Sani Asterias 30. Distomo- Arachova-Antikyra 2 Kanistro/Miraggio Loutra Kyllinis 2/Grecotel 8 19 14 Alexandroupollis Municipal Municipality 96 www.blueflag.global Elani/Elani Bay Resort Olympia Riviera Thalasso Beach Agios Isidoros 20 Fourka/Olympion Sunset ACHAIA [7] 62 Kyani Akti 31. Tanagra Municipality Kallithea/Ammon Zeus 57. Dytiki Achaia Municipality 21 Kallithea-Municipal Bar Plaka Dilessiou 61 23 RODOPI [4] Kalogria/Kalogria Beach Pefkochori-Fyki Beach 22 2. Komotini Municipality EVIA [3] Niforeika 24 Posidi Centre 95 Arogi Lakkopetra/Lakopetra Beach 60 Siviri Centre 32. Chalkida Municipality 25 Fanari/Ioulia Tigania 6 Posidi-Egeopelagitika Alykes Drosias Fanari/Camping Lefkandi 58. Egialia Municipality 7 Mesi Loutra Agias Paraskevis 64 Polychrono-Cocones Beach Asteria Chalkidas Alyki 26 XANTHI [5] 15. Polygyros Municipality ATTIKI [16] Digeliotika Pounda 59 28 Beaches 3. Topiros Municipality Sargani/Blue Dolphin 33. Marathonas Municipality 29 30 27 32 Mangana Gerakini/Ikos Olivia Schinias/Karavi AETOLOAKARNANIA [3] 94 Marinas Erasmio 16. Nea Propontida Municip. 34. Markopoulo Mesogeas 59. Nafpaktos Municipality 31 4. Avdira Municipality 57 58 Eleonas/Ikos Oceania Municipality Psani 65 38 33 Avdira/Porto Molo Nea Potidea/Portes Beach Avlaki Kryoneri 42 Myrodato 56 37 34 Nea Potidea-East of the 35. Saronikos Municipality Kato Vasiliki 55 44 91 Mandra Toroneou Canal 43 39 35 Mavro Lithari/Eden Beach PREVEZA [8] 54 5 KAVALA [15] Sozopoli/Naftilos 40 4 90 Sozopoli Centre Lagonissi 1-Grand Beach/ 60.