The Cases of Evros and the Aegean Sea. Research Notes from Greece
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Flood Risk Perception and Adaptation Capacity
Flood risk perception and adaptation capacity: a contribution to the socio-hydrology debate Sven Fuchs, Konstantinos Karagiorgos, Kyriaki Kitikidou, Fotios Maris, Spyridon Paparrizos, Thomas Thaler To cite this version: Sven Fuchs, Konstantinos Karagiorgos, Kyriaki Kitikidou, Fotios Maris, Spyridon Paparrizos, et al.. Flood risk perception and adaptation capacity: a contribution to the socio-hydrology debate. Hydrology and Earth System Sciences, European Geosciences Union, 2017, 21 (6), pp.3183-3198. 10.5194/hess-21-3183-2017. hal-03226100 HAL Id: hal-03226100 https://hal.archives-ouvertes.fr/hal-03226100 Submitted on 16 May 2021 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Hydrol. Earth Syst. Sci., 21, 3183–3198, 2017 https://doi.org/10.5194/hess-21-3183-2017 © Author(s) 2017. This work is distributed under the Creative Commons Attribution 3.0 License. Flood risk perception and adaptation capacity: a contribution to the socio-hydrology debate Sven Fuchs1, Konstantinos Karagiorgos1, Kyriaki Kitikidou2, Fotios Maris3, Spyridon Paparrizos4,a, and -
Base Metal Mineralisation in the Evros and Rhodope
BASE METAL MINERALISATION IN THE EVROS REGION, THRACE, N.E. HELLAS K.L. Ashworth1, M.F. Billett1, D. Constantinides2, A. Demetriades2, 2 2 C. Katirtzoglou and C. Michael 1. Department of Geology, University of Southampton, Southampton, SO9 5NH, U.K. 2. Institute of Geology and Mineral Exploration, 70 Messoghion Ave., Athens, 115 27, Hellas In: G.H. Friedrich, P.M. Herzig (Editors), 1988. Base metal sulphide deposits in sedimentary and volcanic environments. Proceedings of the DMG-GDMB-SGA- Meeting Aachen, 1985. Special Publication No. 5 of the Society for Geology Applied to Mineral Deposits. Springer-Verlag, Berlin, Heidelberg, p.168-181. Abstract The stratiform and vein base metal sulphide mineralisation of the Evros region has been emplaced during three major metallogenetic periods: the Pre-, Early- and Mid-Alpidic orogenic era. The Pre-Alpidic mineralisation is associated with a metamorphosed ophiolitic mafic-ultramafic sequence (Rhodope Massif), the Early Alpidic with tholeiitic metabasalt (Circum-Rhodope Belt) and the Mid-Alpidic mineralisation has its major development in Tertiary sedimentary and calc-alkaline igneous rocks. These types of mineralisation, depending on their geotectonic setting, are considered to be similar to that of the Limassol Forest Plutonic Complex (Rhodope Massif), to volcanic-exhalative and analogous to Cyprus volcanogenic massive sulphides (Circum- Rhodope Belt), and to stratiform sediment hosted and veins of volcanic affiliation (Tertiary volcano-sedimentary basins). 1. Introduction The Evros region is situated in north-eastern Hellas and is bounded to the north and east by Bulgaria and Turkey (Fig. 1). It shows a history of some minor exploration and mining activity which started during the Turkish and Bulgarian occupation of Thrace in the late 19th and early 20th century. -
New Species of Dolichopoda Bolívar, 1880 (Orthoptera, Rhaphidophoridae) from the Aegean Islands of Andros, Paros and Kinaros (Greece)
DIRECTEUR DE LA PUBLICATION : Bruno David Président du Muséum national d’Histoire naturelle RÉDACTRICE EN CHEF / EDITOR-IN-CHIEF : Laure Desutter-Grandcolas ASSISTANTS DE RÉDACTION / ASSISTANT EDITORS : Anne Mabille ([email protected]), Emmanuel Côtez MISE EN PAGE / PAGE LAYOUT : Anne Mabille COMITÉ SCIENTIFIQUE / SCIENTIFIC BOARD : James Carpenter (AMNH, New York, États-Unis) Maria Marta Cigliano (Museo de La Plata, La Plata, Argentine) Henrik Enghoff (NHMD, Copenhague, Danemark) Rafael Marquez (CSIC, Madrid, Espagne) Peter Ng (University of Singapore) Norman I. Platnick (AMNH, New York, États-Unis) Jean-Yves Rasplus (INRA, Montferrier-sur-Lez, France) Jean-François Silvain (IRD, Gif-sur-Yvette, France) Wanda M. Weiner (Polish Academy of Sciences, Cracovie, Pologne) John Wenzel (The Ohio State University, Columbus, États-Unis) COUVERTURE / COVER : Female habitus of Dolichopoda kikladica Di Russo & Rampini, n. sp. Photo by G. Anousakis. Zoosystema est indexé dans / Zoosystema is indexed in: – Science Citation Index Expanded (SciSearch®) – ISI Alerting Services® – Current Contents® / Agriculture, Biology, and Environmental Sciences® – Scopus® Zoosystema est distribué en version électronique par / Zoosystema is distributed electronically by: – BioOne® (http://www.bioone.org) Les articles ainsi que les nouveautés nomenclaturales publiés dans Zoosystema sont référencés par / Articles and nomenclatural novelties published in Zoosystema are referenced by: – ZooBank® (http://zoobank.org) Zoosystema est une revue en flux continu publiée par les Publications scientifiques du Muséum, Paris / Zoosystema is a fast track journal published by the Museum Science Press, Paris Les Publications scientifiques du Muséum publient aussi / The Museum Science Press also publish: Adansonia, Anthropozoologica, European Journal of Taxonomy, Geodiversitas, Naturae. Diffusion – Publications scientifiques Muséum national d’Histoire naturelle CP 41 – 57 rue Cuvier F-75231 Paris cedex 05 (France) Tél. -
Greece): Results from Geomorphological Studies and Fission-Track Analysis
© Österreichische Geologische Gesellschaft/Austria; download unter www.geol-ges.at/ und www.biologiezentrum.at fission-track dating geomorphology palaeokarst neotectonics . Hellenides Cretaceous Palaeokarst and Cenozoic Erosion of the North Sporades (Greece): Results from Geomorphological Studies and Fission-Track Analysis EWALD HEJL1, HELMUT RIEDL2 AND HERBERT WEINGARTNER2 9 Figures and 2 Tables Content Zusammenfassung 67 Abstract .' 67 1. Introduction 68 2. Geological setting 68 3. Palaeokarst features 69 3.1 Bauxite karst and laterite karst 69 3.2 Preflysch karst 72 4. Neogene-Quaternary planation surfaces of Skopelos Island 72 4.1 Planation system A 72 4.2 Planation system B 72 4.3 Planation system C 72 4.4 Pediment system D 74 4.5 Coastal marginal pediment system E 74 5. Apatite fission-track analysis 74 6. Discussion of thermochronological data 75 7. Conclusions 81 8. Acknowledgements 81 References 81 Der kreidezeitliche Paläokarst und die känozoische Reliefgeschichte der Nordsporaden (Griechenland): Geomorphologische Befunde und Spaltspurenanalysen Zusammenfassung Die Reliefentwicklung der Magnesischen Inseln (Nordsporaden) wurde anhand geomorphologischer Geländebeobachtungen auf Skopelos und mittels Spaltspurdatierungen an Gesteinen von Skiathos, Skopelos und Alonnisos untersucht. Die gemessenen Spaltspuralter und modellierten Abkühlpfade weisen auf regionale und zeitliche Schwankungen der posteozänen Abtragungsgeschwindigkeiten hin. Zwei präeozäne Generationen von Paläokarst sind auf Skopelos zu beobachten. Die erste entwickelte sich während der Unterkreide auf triadischen Dolomiten des alten pelagonischen Schelfs. Die Bauxite und Laterite, mit denen dieser Palaeokarst versiegelt ist, sind aus verschwemmtem Material der Eohellenischen Decke hervorgegangen. Eine zweite Generation von Paläokarst entwickelte sich auf oberkretazi- schen Rudistenkalken und wurde unter palaeogenem Flysch begraben. Drei Generationen neogener Verflachungen treten auf Skopelos oberhalb von 300 m Seehöhe auf. -
Covid19 and a New Quality-Of-Life Tourism Model for the Greek Islands
International Journal of Cultural and Digital Tourism Volume 6, Spring 2020 (Special Issue) Copyright © IACUDIT ISSN (Online): 2241-9705 ISSN (Print): 2241-973X Accessibility, Tourism and Social Welfare: Covid19 and a new Quality-of-Life Tourism Model for the Greek islands Elen-Paraskevi Paraschi1* 1Dept. of Tourism Management,University of Patras, Greece Tel. 6973460338, email: [email protected] Abstract This paper aims to draw attention on the insularity issue faced by many Greek islands and to discuss how the challenges connected with insularity are affected by the Covid19 pandemic and the mobility restrictions measures imposed by the central government. Given that the current tourism pattern of Europe and Greece in particular is going to alter, this paper proposes a new tourism model that could improve the competitive position of the remote Greek islands, while enhancing the total social welfare. This Quality-of-Life Tourism Model (QoLTM) exploits the unique features of the small islands, transforming insularity into a tourist competitive advantage. The proposed QoL tourism model is consistent with the Sustainable Development Goals of the United Nations and aims to improve the well-being of both visitors and island residents. Keywords: Insularity, Accessibility, Sustainable Development, Quality of Life Tourism, Covid19. JEL Classification: Z32, Tourism and Development 1. Introduction Greek tourism industry has experienced a continuous growth in the last decade, with tourist arrivals crossing the of 30 million border line in 2018 and following the same rising trend in 2019, too. However, the situation in 2020 will be dramatically different. Tourism industry is facing an unprecedented challenge from Coronavirus disease 2019 (Covid19) which has grounded airplanes, shut down hotels, and cancelled the vacation plans of millions of people. -
Downloaded from the NOA GNSS Network Website (
remote sensing Article Spatio-Temporal Assessment of Land Deformation as a Factor Contributing to Relative Sea Level Rise in Coastal Urban and Natural Protected Areas Using Multi-Source Earth Observation Data Panagiotis Elias 1 , George Benekos 2, Theodora Perrou 2,* and Issaak Parcharidis 2 1 Institute for Astronomy, Astrophysics, Space Applications and Remote Sensing (IAASARS), National Observatory of Athens, GR-15236 Penteli, Greece; [email protected] 2 Department of Geography, Harokopio University of Athens, GR-17676 Kallithea, Greece; [email protected] (G.B.); [email protected] (I.P.) * Correspondence: [email protected] Received: 6 June 2020; Accepted: 13 July 2020; Published: 17 July 2020 Abstract: The rise in sea level is expected to considerably aggravate the impact of coastal hazards in the coming years. Low-lying coastal urban centers, populated deltas, and coastal protected areas are key societal hotspots of coastal vulnerability in terms of relative sea level change. Land deformation on a local scale can significantly affect estimations, so it is necessary to understand the rhythm and spatial distribution of potential land subsidence/uplift in coastal areas. The present study deals with the determination of the relative vertical rates of the land deformation and the sea-surface height by using multi-source Earth observation—synthetic aperture radar (SAR), global navigation satellite system (GNSS), tide gauge, and altimetry data. To this end, the multi-temporal SAR interferometry (MT-InSAR) technique was used in order to exploit the most recent Copernicus Sentinel-1 data. The products were set to a reference frame by using GNSS measurements and were combined with a re-analysis model assimilating satellite altimetry data, obtained by the Copernicus Marine Service. -
The Geodynamics of the Aegean and Anatolia: Introduction
Downloaded from http://sp.lyellcollection.org/ by guest on September 27, 2021 The geodynamics of the Aegean and Anatolia: introduction T. TAYMAZ1, Y. YILMAZ2 & Y. DILEK3 1Department of Geophysical Engineering,˙ Istanbul Technical University, Maslak, TR–34469,˙ Istanbul, Turkey (e-mail: [email protected]) 2Kadir Has University, Fatih, I˙stanbul, Turkey 3Department of Geology, Miami University, Oxford, OH 45056, USA The complexity of the plate interactions and and volcanism in Anatolia and the Aegean region associated crustal deformation in the Eastern (Taymaz et al. 2004). Mediterranean region is reflected in many destruc- tive earthquakes that have occurred throughout Regional synthesis its recorded history, many of which are well documented and intensively studied. The Eastern Given its location in the Alpine–Himalayan Mediterranean region, including the surrounding orogenic belt, and at the collisional boundary areas of western Turkey and Greece, is indeed one between Gondwana and Laurasia, the geological of the most seismically active and rapidly deform- history of the Aegean region and Anatolia involves ing regions within the continents (Fig. 1). Thus, the Mesozoic–Cenozoic closure of several Neo- the region provides a unique opportunity to tethyan oceanic basins, continental collisions and improve our understanding of the complexities of subsequent post-orogenic processes (e.g. Sengo¨r continental tectonics in an actively collisional & Yılmaz 1981; Bozkurt & Mittwede 2001; Okay orogen. The major scientific observations from et al. 2001; Dilek & Pavlides 2006; Robertson & this natural laboratory have clearly been helping Mountrakis 2006). The opening of oceanic branches us to better understand the tectonic processes in of Neotethys commenced in the Triassic and active collision zones, the mode and nature of they closed during the Late Cretaceous to Eocene continental growth, and the causes and distribution time interval. -
Assessment of the Greek Ramsar Wetlands
Assessment of the Greek Ramsar wetlands Panagiota Maragou and Daphne Mantziou WWF-Greece Athens, 2000 Current status of Greek Ramsar wetlands This report was prepared during the project “Scoring a wetland” that was executed by WWF-Greece and funded by the MAVA Foundation and the WWF European Freshwater Programme. The report should be referred to as Maragou P. and Mantziou D. (2000) Assessment of the Greek Ramsar wetlands, WWF-Greece, pp 59 + Answered questionnaires pp 118 2 WWF Greece TABLE OF CONTENTS ASSESSMENT OF THE GREEK RAMSAR WETLANDS................................................................. 1 Introduction........................................................................................................................................ 5 The elaboration of the assessment criteria ............................................................................ 5 Ramsar wetlands.................................................................................................................... 6 Report on the Answers ..................................................................................................................... 9 Site Description ................................................................................................................................. 9 Ownership status.................................................................................................................... 9 Legal status ......................................................................................................................... -
Network Biogeography of a Complex Island System: the Aegean
Journal of Biogeography (J. Biogeogr.) (2016) ORIGINAL Network biogeography of a complex ARTICLE island system: the Aegean Archipelago revisited Konstantinos Kougioumoutzis1,2*, Anna Thalassini Valli1, Elisavet Georgopoulou3, Stylianos Michail Simaiakis4, Kostas A. Triantis2 and Panayiotis Trigas1 1Laboratory of Systematic Botany, Faculty of ABSTRACT Crop Science, Agricultural University of Aim The Aegean Archipelago has been the focal research area for identifying Athens, GR-118 55 Athens, Greece, 2 and testing several ecological and evolutionary patterns, yet its biogeographical Department of Ecology & Systematics, Faculty of Biology, National & Kapodistrian subdivision has been somewhat overlooked, with the processes driving the University of Athens, GR-157 03 Athens, assembly of the Aegean island plant communities still remaining largely Greece, 3Geological-Paleontological unclear. To bridge this gap, we identify the biogeographical modules (highly Department, Natural History Museum, 1010 linked subgroups of islands and plant taxa) within the Aegean Archipelago. 4 Vienna, Austria, Natural History Museum of Location The Aegean Archipelago, Greece. Crete, University of Crete, Heraklion GR- 71409 Crete, Greece Methods We used a network approach to detect island biogeographical roles and modules, based on a large and detailed database including 1498 Aegean endemic and subendemic plant taxa distributed on 59 Aegean Islands and five adjacent mainland areas. Results The Aegean was divided into six biogeographical modules; the net- work was significantly modular. None of the modules displayed all four possi- ble biogeographical roles (connectors, module hubs, network hubs, peripherals). Six new biogeographical regions in the Aegean were identified. Main conclusions The borders of the six biogeographical regions in the Aegean correspond well to the region’s palaeogeographical evolution from the middle Miocene to the end of the Pleistocene. -
The Dadia–Lefkimi–Soufli Forest National Park, Greece: Biodiversity, Management and Conservation
THE DADIA–LEFKIMI–SOUFLI FOREST NATIONAL PARK, GREECE: BIODIVERSITY, MANAGEMENT AND CONSERVATION Edited by Giorgos Catsadorakis and Hans Källander Illustrations by Paschalis Dougalis WWF Greece Athens 2010 5 THE DADIA–LEFKIMI–SOUFLI FOREST NATIONAL PARK, GREECE: BIODIVERSITY, MANAGEMENT AND CONSERVATION Editors: Giorgos Catsadorakis, Hans Källander, P.O. Box 403, Villavägen 6, Dadia, SE-240 35 Harlösa, GR-68 400 Soufli, SWEDEN GREECE [email protected] [email protected] Suggested citation: Author’s name. 2010. Title of paper. – In: Catsadorakis, G. and Källander, H. (eds). The Dadia–Lefkimi–Soufli Forest National Park, Greece: Biodiversity, Management and Conservation. WWF Greece, Athens, pp. 000–000. © 2010, WWF Greece Published by: WWF Greece, 26 Filellinon str., GR-105 58 Athens, Greece Tel:+30 2103314893, fax: +302103247578 e-mail: [email protected] http://www.wwf.gr ISBN 978-960-7506-10-8 Typeset by ZooBo Tech, Torna Hällestad, Sweden Printed by Schema + Chroma, GR-574 00 Sindos, Thessaloniki, http://www.kethea-print.gr Illustrations by Paschalis Dougalis Maps on pages 18–28, 36, 42, 86, 89, 217 and 231–243 prepared by Nikolaos Kasimis, those on pages 23, 27 and 232 by Konstantinos Poirazidis. The book was printed on130 g FSC-certified Sappi Era Silk paper. Cover photo: Giorgos Catsadorakis. 6 A regional-historical approach to the high raptor diversity of the Dadia–Lefkimi–Soufli Forest National Park Giorgos Catsadorakis Potential reasons underlying the high diversity and abundance of raptorial birds in DNP are explored with emphasis on larger temporal and spatial scales. In terms of food resources for these birds, the DNP and the surrounding area support high reptile densities and offer a regular supply of livestock carcasses. -
RIS3 Regional Assessment: South Aegean
Smart Specialisation Strategies in Greece – expert team review for DG REGIO RIS3 Regional Assessment: South Aegean A report to the European Commission, Directorate General for Regional Policy, Unit I3 - Greece & Cyprus December 2012 (final version) Alasdair Reid, Nicos Komninos, Jorge-A. Sanchez-P., Panayiotis Tsanakas Table of Contents 1. Executive summary: Overall conclusions and recommendations 1 2. Regional Innovation Performance and potential 3 2.1 Regional profile and specialisation 3 2.2 The strengths and weaknesses of the regional innovation system 5 3. Stakeholder involvement and governance of research and innovation policies 6 3.1 Stakeholder involvement in strategy design and implementation 6 3.2 Vision for the Region 7 4. Towards a smart specialisation strategy 8 4.1 The regional research and innovation policy 8 4.2 Cluster and entrepreneurship policies 11 4.3 Digital economy and ICT policies 13 5. Monitoring and evaluation 14 Appendix A List of people attending regional workshop 15 Appendix B List of key documents and reference materials consulted 15 Appendix C Key Actors in the regional innovation system 16 Appendix D Regional RTDI funding under the OP Competitiveness and Innovation 18 Appendix E Total Gross value added at basic prices – South Aegean 19 Appendix F Relative regional specialisation in 20 industries – South Aegean 20 Figures Figure 1 Summary benchmark of regional innovation performance ............................... 3 Figure 2: SWOT of regional innovation potential and specialisation .............................. 4 Figure 3: Priorities and funding of OP South Aegean 2007-2013 ....................................8 Figure 4: regional priorities of research and innovation 2007-13.................................... 9 Figure 5:Innovation priorities 2014-2020 ........................................................................ -
Strike Slip Tectonics and Transtensional Deformation in the Aegean Region and the Hellenic Arc: Preliminary Results
Bulletin of the Geological Society of Greece, vol. XLVII 2013 Δελτίο της Ελληνικής Γεωλογικής Εταιρίας, τομ. XLVII , 2013 th ου Proceedings of the 13 International Congress, Chania, Sept. Πρακτικά 13 Διεθνούς Συνεδρίου, Χανιά, Σεπτ. 2013 2013 STRIKE SLIP TECTONICS AND TRANSTENSIONAL DEFORMATION IN THE AEGEAN REGION AND THE HELLENIC ARC: PRELIMINARY RESULTS Sakellariou D.1, Mascle, J.2 and Lykousis V.1 1 Institute of Oceanography, Hellenic Centre for Marine Research, Greece, [email protected], [email protected] 2 Observatoire Océanologique de Villefranche, France, [email protected] Abstract Recently acquired offshore seismic and swath bathymetry data from the Hellenic Arc, the Ionian Sea and the South and North Aegean Sea, including the Hellenic Volcanic Arc and the Cyclades plateau, along with geological and tectonic data from Plio-Quaternary basins exposed on the Hellenic Arc indicate that strike slip tectonics has played a major role in the southwestward extension of the Aegean crustal block, the development of the offshore neotectonic basins and the spatial dis- tribution of the volcanic activity along the Volcanic Arc. Transtensional defor- mation, accommodated by (sinistral or dextral) strike slip zones and related exten- sional structures, prevail throughout Plio-Quaternary, since the North Anatolian Fault broke westwards into the North Aegean. Incipient collision of the Hellenic Forearc south of Crete with the Libyan promontory and consequent lateral escape tectonics led to the segmentation of the Hellenic Arc in distinct blocks, which