Striped Dolphin Home Ranges Within the IMMA and Natura 2000 Area
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Nafpaktos Schräg Gegenüber Von Patras Liegt Ein Kleines Äußerst Malerisches Städtchen – Nafpaktos
Nafpaktos Schräg gegenüber von Patras liegt ein kleines äußerst malerisches Städtchen – Nafpaktos. Es hat einen winzigen Hafen, der durch eine Art Stadtmauer befestigt ist. Rechts und links der Hafeneinfahrt stehen kleine Türmchen auf der Mauer, ein sehr schönes Bild. Oberhalb des Städtchens liegt die Ruine einer ziemlich groß angelegten venezianischen Festung, deren Mauern bis hinunter zum Meer gehen. Und oberhalb gibt es eine wunderschöne Taverne, von der aus man einen einmaligen Blick auf die Stadt und den Golf von Patras hat. Und im Hafen gibt es ausgezeichnete Restaurants, man sitzt sozusagen auf der Stadtmauer und hat beim Essen einen wunderbaren Blick auf den kleinen Hafen. Was hat es auf sich mit Nafpaktos? Dazu muss man in die Geschichte zurückgehen – da hieß das Städtchen nicht Nafpaktos, sondern Lepanto. Nach der Eroberung Konstantinopels 1453 durch die Türken gab es ja immer wieder Versuche seitens der Türken/des Osmanischen Reiches, Griechenland und den Balkan – mit Ziel Europa insgesamt – zu erobern. Einer dieser Versuche endete am 7. Oktober 1571 in der Seeschlacht von Lepanto, unweit des heutigen Städtchens Nafpaktos. Es war die letzte Seeschlacht mit von Sklaven geruderten Galeeren. 212 Kriegsschiffe der „Heiligen Liga“ gegen 260 Kriegsschiffe der Osmanen; 68000 Spanier, Italiener, Österreicher, Venezianer und Soldaten des Papstes gegen 77000 Osmanen. Don Juan de Austria, ein Sohn des Habsburgerkaisers Karl V., führte die Koalition an. Diese hatte sich gebildet, weil die Osmanen Zypern erobert hatten, das bisher zu Venedig gehörte. Venedig wollte seinen Mittelmeerhandel erhalten und erweitern – der Papst hoffte auf eine Renaissance der Kreuzzüge gegen die „Ungläubigen“. Das Zweckbündnis hielt nicht lange, der Sieg festigte die europäische Vormachtstellung der Habsburger. -
Kleonai, the Corinth-Argos Road, And
HESPERIA 78 (2OO9) KLEONAI, THE CORINTH- Pages ioj-163 ARGOS ROAD, AND THE "AXIS OF HISTORY" ABSTRACT The ancient roadfrom Corinth to Argos via the Longopotamos passwas one of the most important and longest-used natural routes through the north- eastern Peloponnese. The author proposes to identity the exact route of the road as it passed through Kleonaian territoryby combining the evidence of ancient testimonia, the identification of ancient roadside features, the ac- counts of early travelers,and autopsy.The act of tracing the road serves to emphasizethe prominentposition of the city Kleonaion this interstateroute, which had significant consequences both for its own history and for that of neighboring states. INTRODUCTION Much of the historyof the polis of Kleonaiwas shapedby its location on a numberof majorroutes from the Isthmus and Corinth into the Peloponnese.1The most importantof thesewas a majorartery for north- south travel;from the city of Kleonai,the immediatedestinations of this roadwere Corinthto the north and Argos to the south.It is in connec- tion with its roadsthat Kleonaiis most often mentionedin the ancient sources,and likewise,modern topographical studies of the areahave fo- cusedon definingthe coursesof these routes,particularly that of the main 1. The initial fieldworkfor this Culturefor grantingit. In particular, anonymousreaders and the editors studywas primarilyconducted as I thank prior ephors Elisavet Spathari of Hesperia,were of invaluableassis- part of a one-person surveyof visible and AlexanderMantis for their in- tance. I owe particulargratitude to remainsin Kleonaianterritory under terest in the projectat Kleonai,and Bruce Stiver and John Luchin for their the auspicesof the American School the guardsand residentsof Archaia assistancewith the illustrations. -
The World View of the Anonymous Author of the Greek Chronicle of the Tocco
THE WORLD VIEW OF THE ANONYMOUS AUTHOR OF THE GREEK CHRONICLE OF THE TOCCO (14th-15th centuries) by THEKLA SANSARIDOU-HENDRICKX THESIS submitted in the fulfilment of the requirements for the degree DOCTOR OF ARTS in GREEK in the FACULTY OF ARTS at the RAND AFRIKAANS UNIVERSITY PROMOTER: DR F. BREDENKAMP JOHANNESBURG NOVEMBER 2000 EFACE When I began with my studies at the Rand Afrikaans University, and when later on I started teaching Modern Greek in the Department of Greek and Latin Studies, I experienced the thrill of joy and the excitement which academic studies and research can provide to its students and scholars. These opportunities finally allowed me to write my doctoral thesis on the world view of the anonymous author of the Greek Chronicle of the Tocco. I wish to thank all persons who have supported me while writing this study. Firstly, my gratitude goes to Dr Francois Bredenkamp, who not only has guided me throughout my research, but who has always been available for me with sound advice. His solid knowledge and large experience in the field of post-classical Greek Studies has helped me in tackling Byzantine Studies from a mixed, historical and anthropological view point. I also wish to render thanks to my colleagues, especially in the Modern Greek Section, who encouraged me to continue my studies and research. 1 am indebted to Prof. W.J. Henderson, who has corrected my English. Any remaining mistakes in the text are mine. Last but not least, my husband, Prof. B. Hendrickx, deserves my profound gratitude for his patience, encouragement and continuous support. -
Maritime Areas, Ports and Sea Routes: Defining Space and Connectivity Between Malta and the Eastern Mediterranean 1770-1820
Journal of Maltese History, volume 5, number 2 (2018) Maritime Areas, Ports and Sea Routes: Defining Space and Connectivity between Malta and the Eastern Mediterranean 1770-1820 Frank Theuma Independent Researcher Introduction The numerous ships that arrived in Malta from eastern Mediterranean points of origin and were recorded systematically in the quarantine and arrival registers1 [henceforth QR] of Malta reveal an intense maritime traffic (1770-1815). They reveal a substantial connection between a large number of eastern Mediterranean commercial nodes and ports and the port of Malta. These ports and nodes were dotted over a wide geographical expanse, they differed widely in scale and importance, and presented different economic profiles, that changed and evolved along the years. Some rose from nothing, like the Black Sea port of Odessa.2 Some expanded in their operation, others contracted and declined. Some were massive trading hubs, like Smyrna, Salonica and Alexandria, with a wide range of far-flung sea and land connections, and from where hundreds of sailing voyages started, some of which found themselves sailing into the port of Malta. These hubs dealt with equally massive amounts of cargo consisting of a wide diversity of products that originated from proximal and distant locations in their extensive hinterlands. Others, like a number of locations that dotted the coasts of Epirus, the gulf of Arta, on the western coast of Greece, or the Gulf of Patras were mere beaches; landings that served as an outlet for a local product. At the latter, mariners anchored or beached their small vessels to take on board cargo that was limited in both variety and quantity. -
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. -
Sar Monitoring of Progressive Ground Deformation in Etoliko Using the Persistent Scatterers and Sbas Techniques
SAR MONITORING OF PROGRESSIVE GROUND DEFORMATION IN ETOLIKO USING THE PERSISTENT SCATTERERS AND SBAS TECHNIQUES. Gkartzou E., Parcharidis I. and Karymbalis E. Harokopio University of Athens, Department of Geography, El. Venizelou 70, 17671 Athens, Greece, [email protected], [email protected], [email protected] ABSTRACT The Messolonghi-Etoliko lagoons complex is located in the north part of the Gulf of Patras in the central west coast of Greece. It is one of the most important Mediterranean lagoons for both environmental and financial reasons. It is a shallow area of 150 km2, extended between the Acheloos and Evinos rivers, it is protected by the Ramsar Convention and it is also included in the Natura 2000 network. The town of Etoliko, known as the Little Venice of Greece, is a municipal section of Messolonghi municipality with a population of 5,349 inhabitants, ten kilometers northwest of Messolonghi. Etoliko is developed on a small island rooted in water in the middle of the lagoon. It is connected east and west to the mainland by two stone arched bridges with original length of about 300 meters each. This paper studies the ground deformation of the town of Etoliko using Multitemporal SAR Interferometry techniques and more precisely, the Persistent Scatterers Interferometry Technique (PSInSAR) and Small Baseline Subset (SBAS), which have proven a remarkable potential for mapping ground deformation phenomena. This approach allows to make accurate measurements very close to its theoretical limit (in the order of 1 mm), and to obtain from the numerous radar targets very precise displacement information. We applied the PS approach (Gamma-IPTA chain) and an ad-hoc SBAS approach on 105 SAR images from the European Remote Sensing satellites ERS-1, ERS-2 and 55 ENVISAT images that cover the two time periods, 1992-2000 and 2002-2009, to map the Etoliko subsidence. -
Geological Identification of Historical Tsunamis in the Gulf of Corinth, Central Greece S
Geological identification of historical tsunamis in the Gulf of Corinth, Central Greece S. Kortekaas, G. A. Papadopoulos, A. Ganas, A. Cundy, A. Diakantoni To cite this version: S. Kortekaas, G. A. Papadopoulos, A. Ganas, A. Cundy, A. Diakantoni. Geological identification of historical tsunamis in the Gulf of Corinth, Central Greece. Natural Hazards and Earth System Sci- ences, Copernicus Publ. / European Geosciences Union, 2011, 11 (7), pp.2029-2041. 10.5194/nhess- 11-2029-2011. hal-01465531 HAL Id: hal-01465531 https://hal.archives-ouvertes.fr/hal-01465531 Submitted on 12 Feb 2017 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. Nat. Hazards Earth Syst. Sci., 11, 2029–2041, 2011 www.nat-hazards-earth-syst-sci.net/11/2029/2011/ Natural Hazards doi:10.5194/nhess-11-2029-2011 and Earth © Author(s) 2011. CC Attribution 3.0 License. System Sciences Geological identification of historical tsunamis in the Gulf of Corinth, Central Greece S. Kortekaas1, G. A. Papadopoulos2, A. Ganas2, A. B. Cundy3, and A. Diakantoni4 1Fugro Engineers B.V., Veurse Achterweg 10, 2264 AG Leidschendam, The Netherlands 2Institute of Geodynamics, National Observatory of Athens, 11810 Athens, Greece 3School of Environment and Technology, University of Brighton, UK 4Dept. -
Deliverable No. 3.1 Census of Needs/Mapping of Existing Systems for Coastal Management
Project acronym: TRITON Project title: Development of management tools and directives for immediate protection of biodiversity in coastal areas affected by sea erosion and establishment of appropriate environmental control systems Deliverable No. 3.1 Census of needs/mapping of existing systems for coastal management Delivery date: 23/07/2019 1 PROGRAMME Interreg V-A Greece-ItalyProgramme2014-2020 AXIS Axis 2 (i.e. Integrated Environmental Management) THEMATIC OBJECTIVES 06 – Preserving and protecting the environment and promoting resource efficiency PROJECT ACRONYM TRITON PROJECT WEBSITE URL www.interregtriton.eu DELIVERABLE NUMBER No. 3.1 TITLE OF DELIVERABLE Census of needs/mapping of existing systems for coastal management WORK PACKAGE/TASK N° WP3 Mapping and Planning of tools and framework; Task 3.1 NAME OF ACTIVITY Census of needs/mapping of existing system for coastal management PARTNER IN CHARGE (AUTHOR) PB2 PARTNERS INVOLVED LB1, PB4 STATUS Final version DUE DATE Third semester ADDRESSEE OF THE DOCUMENT1 TRITON PROJECT PARTNERS; INTERREG V-A GREECE-ITALY PROGRAMME DISTRIBUTION2 PP Document Revision History Version Date Author/Reviewer Changes 1.0 – Final 24/06/2020 PB2- CMCC 0.6 - Draft 21/06/2020 PB5 - UoP Version revised by PB5 and sent to LB1 for afinal check 0.5 - Draft 19/07/2019 PB2- CMCC Version revised by PB2 and sent to LB1 and PB4 for their check 1WPL (Work Package Leaders); PB (Project Beneficiaries); AP (Associates); Stakeholders; Decision Makers; Other (Specify) 2PU (Public); PP (Restricted to other program participants); -
Wind-Induced Upwellings and Currents in the Gulfs of Patras, Nafpaktos and Korinthos, Western Greece
____________________________________o_c_EA_N __ O_LO_G __ JC_A_A_C_T_A __ 19_8_9_-_v_o_L_._1_2_-_N __ 3~~r----- Greek straits Sea surface temperature Upwellings Wind-induced upwellings Eddies · Baroclinic motions and currents Détroits grecs Température superficielle Remontées d'eau in the gulfs of Patras, Nafpaktos Tourbillon and Korinthos, Western Greece Mouvement barocline 11 Alexander LASCARATOS •, Ettore SALUSTI , Georgia PAPAGEORGAKI • a University of Athens, Department of Applied Physics, Laboratory of Meteorology, 33 lppocratous Str., 10680 Athens, Greece. b Istituto Nazionale de Fisica Nucleare (INFN), Department of Physics, Universita "La Sapienza", P.A. Moro, 1-00185, Roma, Italia. Received 12/1/88, in revised form 26/9/88, accepted 9/12/88. ABSTRACT With the use of 152 NOAA-6 and NOAA-7 satellite infrared images taken over the gulfs of Patras, Nafpaktos and Kqrinthos in Western Greece, a relatively complete description of sea surface temperature features and their evolution in time is obtained for these three marine basins. The satellite data, discussed in the light of recent theories on wind-induced marine upwellings near capes (Crépon and Richez, 1982 and Crépon et al., 1984), allow us to provide a general picture of wind-induced movements and upwellings. Oceanologica Acta, 1989. 12, 3, 159-164. RÉSUMÉ Remontées d'eau induites par le vent et courants dans les golfes de Patras, Nafpaktos et Corinthe, Grèce La structure thermique superficielle des golfes de Patras, Nafpaktos et Corinthe (Grèce) et son évolution sous l'effet du vent sont présentées. Les données de 152 thermographies des satellites NOAA-6 et NOAA-7 sont confrontées aux théories récentes sur les remontées d'eau au voisinage des caps (Crépon et Richez, 1982; Crépon et al., 1984); elles conduisent à une description générale des mouvements marins et des remontées d'eau dues aux vents dans la région. -
On the Hydrodynamic Geometry of Flow-Through Versus Restricted Lagoons
water Article On the Hydrodynamic Geometry of Flow-Through versus Restricted Lagoons Nikolaos Th. Fourniotis 1,2,*, Georgios M. Horsch 1 and Georgios A. Leftheriotis 1 1 Department of Civil Engineering, University of Patras, University Campus, 265 00 Patras, Greece; [email protected] (G.M.H.); [email protected] (G.L.A.) 2 Department of Civil Engineering, Technological Educational Institute of Western Greece, Megalou Alexandrou 1, 263 34 Patras, Greece * Correspondence: [email protected]; Tel.: +30-2610-996519 Received: 19 January 2018; Accepted: 17 February 2018; Published: 25 February 2018 Abstract: The classification of a lagoon as a restricted lagoon is shown to depend not solely on its geometry but also on the tidal hydraulics. By numerically simulating the tidal exchange of two lagoons of similar geometrical dimensions, the Nidova lagoon and the Papas lagoon, in Western Greece, subject to very similar tidal forcing, applied to the two tidal inlets in the first case and three in the second, very different residence times are found, namely 2.5 days for the Nidova and 25–30 days for the Papas lagoon. This large difference is attributed to the fact that whereas the Papas lagoon functions as a typical restricted lagoon, in which the water renewal is achieved by mixing in the lagoon of the tidal prism water exchanged within a tidal cycle, the Nidova lagoon functions as a flow-through system because of the differential arrival of the tide at its two tidal inlets. It is suggested that this way of enhancing the flushing rate of a lagoon be considered, whenever possible, when creating a new tidal inlet to the lagoon. -
Parnassus, Delphi, and the Thyiades Mcinerney, Jeremy Greek, Roman and Byzantine Studies; Fall 1997; 38, 3; Proquest Pg
Parnassus, Delphi, and the Thyiades McInerney, Jeremy Greek, Roman and Byzantine Studies; Fall 1997; 38, 3; ProQuest pg. 263 Parnassus, Delphi, and the Thyiades Jeremy McInerney AN INTERNATIONAL SANCTUARY, Delphi helped bring a bout the transition within the emerging poleis of the ~ Archaic period to what Fran~ois de Polignac has called a "more finished, <adult' stage of society and institutions. "1 Delphi's business was international in scope: the sanctuary was involved in colonization, arbitration, and panhellenism.2 Yet one important aspect of Delphi's emergence as a panhellenic sanc tuary rarely studied is the impact of this extraordinary status on the community of Delphi and its surrounding region. In this paper I propose that, as the sanctuary of Delphi came to repre sent order, conciliation, and mediation to the Greeks, the local topography of the region was made to reflect these same themes. Delphi and Mt Parnassus became, through myth and ritual, a landscape in which tensions between wildness and civilization-a polarity at the heart of the culture of the polis could be narrated, enacted, and organized. Delphi and Parnas sus stood for the polarities from which the polis was construc ted. On the one side was Delphi, representing the triumph of order over chaos, as expressed in the myth of the sanctuary's foundation, when Apollo destroys Pytho and brings culture to the original inhabitants of Parnassus (Strab. 9.3.12). On the other side was Mt Parnassus, the wilderness tamed by Apollo. These 1 F. de Polignac, UMediation, Competition, and Sovereignty: The Evolution of Rural Sanctuaries in Geometric Greece,» in S. -
Active Tectonics of the Corinth Gulf, Greece, the Fastest Growing Rift on Planet Earth
Active tectonics of the Corinth Gulf, Greece, the fastest growing rift on planet Earth (Dr. Athanassios Ganas) Abstract: Since the beginning of the instrumental seismology in Greece, the most intense seismic activity has been recorded within the Corinth rift and its vicinity such as the central Ionian Sea. This rift is the most active continental seismic region of the Mediterranean and one of the fastest opening continental rifts in the world. Its seismic history since the nineteenth century has exhibited more than 10 shallow events with M>6.0. A dense GPS velocity field is used to model the present-day deformation by means of a continuous strain and rotation rate field. The geodetic results quantify and refine previous findings as well as yield new insights for the present-day deformation pattern in the Gulf of Corinth rift. The consistency of the contemporary deformation field with earthquake activity is also evaluated by the calculation of geodetic moment rates and comparison with moment rates determined from earthquake catalogs. In this café, Dr. Athanassios Ganas presented briefly why Corinth Gulf is known as the fastest growing rift on planet earth by the support of his recent research results. Host: Good evening ladies and gentlemen. This is English GeoScience Café session 18. It’s a great pleasure for me to introduce our speaker tonight, who is going to talk to us about “Active tectonics of the Corinth Gulf, Greece, the fastest growing rift on planet Earth”. We are honored and delighted to have Dr. Athanassios Ganas with us today. Dr. Athanassios Ganas completed his PhD in Geological Remote Sensing from the University of Reading, UK.