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Observational Evidence on the Effects of Mega-Fires on the Frequency Of
Science of the Total Environment 592 (2017) 262–276 Contents lists available at ScienceDirect Science of the Total Environment journal homepage: www.elsevier.com/locate/scitotenv Observational evidence on the effects of mega-fires on the frequency of hydrogeomorphic hazards. The case of the Peloponnese fires of 2007 in Greece Diakakis M. a,⁎, Nikolopoulos E.I. b,MavroulisS.a,VassilakisE.a,KorakakiE.c a Faculty of Geology and Geoenvironment, National & Kapodistrian University of Athens, Panepistimioupoli, Zografou GR15784, Greece b Department of Civil and Environmental Engineering, University of Connecticut, Storrs, CT, USA c WWF Greece, 21 Lembessi St., 117 43 Athens, Greece HIGHLIGHTS GRAPHICAL ABSTRACT • The mega fire of 2007 in Greece and its effects of hydrogeomorphic events are studied. • The frequency of such events over the period 1989–2016 is examined. • Results show an increase in floods by 3.3 times and mass movement events by 5.6. • Increase in frequency of such events is steeper in affected areas than unaf- fected. • Increases are found even in months that record a decrease in extreme rainfall. article info abstract Article history: Even though rare, mega-fires raging during very dry and windy conditions, record catastrophic impacts on infra- Received 6 January 2017 structure, the environment and human life, as well as extremely high suppression and rehabilitation costs. Apart Received in revised form 7 March 2017 from the direct consequences, mega-fires induce long-term effects in the geomorphological and hydrological Accepted 8 March 2017 processes, influencing environmental factors that in turn can affect the occurrence of other natural hazards, Available online xxxx such as floods and mass movement phenomena. -
Ganas, A., Serpelloni, E., Drakatos, G., Kolligri, M., Adamis, I., Tsimi, Ch
This article was downloaded by: [HEAL-Link Consortium] On: 20 October 2009 Access details: Access Details: [subscription number 772810551] Publisher Taylor & Francis Informa Ltd Registered in England and Wales Registered Number: 1072954 Registered office: Mortimer House, 37-41 Mortimer Street, London W1T 3JH, UK Journal of Earthquake Engineering Publication details, including instructions for authors and subscription information: http://www.informaworld.com/smpp/title~content=t741771161 The Mw 6.4 SW-Achaia (Western Greece) Earthquake of 8 June 2008: Seismological, Field, GPS Observations, and Stress Modeling A. Ganas a; E. Serpelloni b; G. Drakatos a; M. Kolligri a; I. Adamis a; Ch. Tsimi a; E. Batsi a a Institute of Geodynamics, National Observatory of Athens, Athens, Greece b Istituto Nazionale di Geofisica e Vulcanologia, Centro Nazionale Terremoti, Bologna, Italy Online Publication Date: 01 December 2009 To cite this Article Ganas, A., Serpelloni, E., Drakatos, G., Kolligri, M., Adamis, I., Tsimi, Ch. and Batsi, E.(2009)'The Mw 6.4 SW- Achaia (Western Greece) Earthquake of 8 June 2008: Seismological, Field, GPS Observations, and Stress Modeling',Journal of Earthquake Engineering,13:8,1101 — 1124 To link to this Article: DOI: 10.1080/13632460902933899 URL: http://dx.doi.org/10.1080/13632460902933899 PLEASE SCROLL DOWN FOR ARTICLE Full terms and conditions of use: http://www.informaworld.com/terms-and-conditions-of-access.pdf This article may be used for research, teaching and private study purposes. Any substantial or systematic reproduction, re-distribution, re-selling, loan or sub-licensing, systematic supply or distribution in any form to anyone is expressly forbidden. The publisher does not give any warranty express or implied or make any representation that the contents will be complete or accurate or up to date. -
Durham E-Theses
Durham E-Theses Archaeology in the community - educational aspects: Greece: a case-study Papagiannopoulos, Konstantinos How to cite: Papagiannopoulos, Konstantinos (2002) Archaeology in the community - educational aspects: Greece: a case-study, Durham theses, Durham University. Available at Durham E-Theses Online: http://etheses.dur.ac.uk/4630/ Use policy The full-text may be used and/or reproduced, and given to third parties in any format or medium, without prior permission or charge, for personal research or study, educational, or not-for-prot purposes provided that: • a full bibliographic reference is made to the original source • a link is made to the metadata record in Durham E-Theses • the full-text is not changed in any way The full-text must not be sold in any format or medium without the formal permission of the copyright holders. Please consult the full Durham E-Theses policy for further details. Academic Support Oce, Durham University, University Oce, Old Elvet, Durham DH1 3HP e-mail: [email protected] Tel: +44 0191 334 6107 http://etheses.dur.ac.uk 2 Konstantinos Papagiannopoulos Archaeology in the community - educational aspects. Greece: a case-study (Abstract) Heritage education in Greece reproduces and reassures the individual, social and national sel£ My purpose is to discuss the reasons for this situation and, by giving account of the recent developments in Western Europe and the new Greek initiatives, to improve the study of the past using non-traditional school education. In particular, Local History projects through the Environmental Education optional lessons allow students to approach the past in a more natural way, that is through the study of the sources and first hand material. -
Geomorphology and Archeology, Northwest Peloponnesos, Greece. Constantine Nicholas Raphael Louisiana State University and Agricultural & Mechanical College
Louisiana State University LSU Digital Commons LSU Historical Dissertations and Theses Graduate School 1968 Geomorphology and Archeology, Northwest Peloponnesos, Greece. Constantine Nicholas Raphael Louisiana State University and Agricultural & Mechanical College Follow this and additional works at: https://digitalcommons.lsu.edu/gradschool_disstheses Recommended Citation Raphael, Constantine Nicholas, "Geomorphology and Archeology, Northwest Peloponnesos, Greece." (1968). LSU Historical Dissertations and Theses. 1515. https://digitalcommons.lsu.edu/gradschool_disstheses/1515 This Dissertation is brought to you for free and open access by the Graduate School at LSU Digital Commons. It has been accepted for inclusion in LSU Historical Dissertations and Theses by an authorized administrator of LSU Digital Commons. For more information, please contact [email protected]. This dissertation has been microfilmed exactly as received 69-4498 RAPHAEL, Constantine Nicholas, 1937- GEOMORPHOLOGY AND ARCHEOLOGY, NORTH WEST PELOPONNESOS, GREECE. Louisiana State University and_Agricultural and Mechanical College, Ph.D., 1968 Geography University Microfilms, Inc., Ann Arbor, Michigan (c Copyright by CONSTANTINE NICHOLAS RAPHAEL 1969 Geomcrphology and Archeology, Northwest Peloponnesos, Greece A Dissertation Submitted to the Graduate Faculty of the Louisiana State University and Agricultural and Mechanical College in partial fulfillment of the requirements for the degree of Doctor of Philosophy in The Department of Geography and Anthropology by Constantine -
List of Bank Branches by Branch Name 31/12/2014
LIST OF BANK BRANCHES BY BRANCH NAME 31/12/2014 PIRAEUS BANK S.A. BRANCH NAMEHEBIC AREA ADDRESS TELEPHONE NUMBER / FAX 1866 SQUARE, CHANIA0172758 CHANIA 70, Chatzimichali Giannari str., 731 35 CHANIA tel.: 2821029100, fax: 2821050710 25TH AVGOUSTOU, HERAKLIO0172751 HERAKLEIO 39, 25th Avgoustou str., 712 02 HERAKLEIO tel.: 2810247610, fax: 2810228324 3RD SEPTEMVRIOU, OMONIA 0172039 ATHENS 28, 3rd Septemvriou & Kapodistriou str., 104 32 ATHENS BRANCH tel.: 2105205100, fax: 2105235138 62 MARTIRON HERAKLIOU0172761 HERAKLEIO 97, 62 Martiron Ave. & 1, Dionysiou Fragiadaki str., 713 04 HERAKLEIO tel.: 2810264330, fax: 2810255997 ABELONAS0171393 AMPELONAS 1, Goltsiou & 5, Thermopylon str., 404 00 AMPELONAS tel.: 2492306000, fax: 2492031402 ACHARNON0172058 ATHENS 421, Acharnon str., 111 43 ATHENS tel.: 2102588070, fax: 2102520490 ACHARNON STR.0171592 ATHENS 205, Acharnon & Niovis str.s., 104 46 ATHENS tel.: 2166008310, fax: 2168003817 AEGINA BRANCH0172124 AEGINA Dimokratias Coastal Ave. & Leonardou Lada str., 180 10 AEGINA tel.: 2297029890, fax: 2297028882 AG. ACHILLIOU0171563 LARISSA 146, El. Venizelou str., 412 22 LARISSA tel.: 2416000160, fax: 2416007111 AG. ANTONIOU, PERISTERI0172048 PERISTERI 33, Ethnarchou Makariou str., 121 31 PERISTERI tel.: 2105783020, fax: 2105773224 AG. DIMITRIOS0171555 AGIOS DIMITRIOS 266, Vouliagmenis Ave., 173 43 AGIOS DIMITRIOS tel.: 2160005020, fax: 2109765714 AG. DIMITRIOU0172085 AGIOS DIMITRIOS 173, Ag. Dimitriou Ave., 173 43 AGIOS DIMITRIOS tel.: 2109758170, fax: 2109764036 AG. DIMITRIOU, THESSALONIKI0172203 THESSALONIKI 77, Ag. Dimitriou str., 546 33 THESSALONIKI tel.: 2310254860, fax: 2310223843 AG. IOANNI RENTI SQ. BRANCH0172136 AG. I. RENTIS 4, Konstantinou Palaiologou str., Ag. I. Renti sq., 182 33 AG. I. RENTIS tel.: 2104838120, fax: 2104832389 AG. IOANNOU, AG. PARASKEVI0172010 AGIA PARASKEVI 40, Ag. Ioannou str., 153 42 AGIA PARASKEVI tel.: 2106085800, fax: 2106011128 AG. -
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Journal of Coastal Research 853-863 West Palm Beach, Florida Summer 2000 Geomorphological Observations in the Coastal Zone of Kyllini Peninsula, NW Peloponnesus-Greece, and their Relation to the Seismotectonic Regime of the Area Hampik Maroukian'[, Kalliopi Gaki-Papanastassiou'[, Dimitris Papanastassiouj and Nikolaos Palyvos] tDepartment of Geography :j:lnstitute of Geodynamics Climatology National Observatory of University of Athens Athens GR-15784 Athens, Greece GR-11810 Athens, Greece ABSTRACT . MAROUKIAN, H.; GAKI-PAPANASTASSIOU, K.; PAPANASTASSIOU, D., and PALYVOS, N., 2000. Geomorpholog .tflllllllt. ical observations in the coastal zone of Kyllini Peninsula, NW Peloponnesus-Greece, and their relation to the seis ~ motectonic regime of the area. Journal of Coastal Research, 16(3), 853-863. West Palm Beach (Florida), ISSN 0749 ~. 0208. ---- ~ ~ --~a-.__+; 1&--- The Kyllini Peninsula comprises an isolated hilly region and occupies the western part of the alluvial plain ofPeneios River. It owes its morphology to a Triassic salt dome intrusion active since Miocene times. During the Quaternary it was covered by the sea, became an island and was finally joined to Peloponnesus with the alluvial deposits ofPeneios River. In this study an attempt is made to correlate the coastal landforms with the seismotectonic regime of the broader area of Kyllini Peninsula. Raised Tyrrhenian shorelines occur at elevations ranging from sea-level up to 60 m. Holocene uplifted shorelines, wave cut benches, abrasion platforms and notches have been observed, at heights between 0.3 to 3 m. Furthermore, the coastal zone is characterized by beachrock and a series of dunes of two different generations as well as raised aeolianite. Geophysical investigations of the deep geological structure of the region have also revealed the offshore presence of salt diapirism as well as large faults in the area of Zakynthos Straits. -
Greek Railway Map
GREEK RAILWAY MAP SVILENGRAD ORMENIO (28+120) MARASIA (150+381=4+762) DIKEA B U L G A R I A (20+506) NEA VYSSA (137+951) NEA ORESTIADA (129+310) CHEIMONIO (123+010) EVROS KOULATA PYTHIO (112+017) (14+461) DIDYMOTEICHO KASTANOUSSA (98+265) (51+990) RODOPOLI PROMACHONAS DRAMA (61+639) (13+401) PARENESTIO NEOCHORI LAVARA MOURIES VYRONEIA (233+641) (247+217) XANTHI (83+710) (46+993) (84+597) STRIMONAS NORTH MACEDONIA STAUROUPOLI (94+351, 00+000) PLATANIA (256+437) (222+455) MANDRAKI DRAMA XANTHI DOIRANI (74+400) SIDIROKASTRO POLYANTHOS RODOPI LAGYNA GEVGELIJA (196+126) (291+453) (57+102) (33+700) (98+810) LIVERA (323+600) (78+666) NIKIFOROS (268+032) SKOTOUSSA (211+286) (110+741) KOMOTINI IDOMENI CALINDOIA (338+659) (61+114=26+566) GAZOROS FOTOLIVOS IASMOS (76+718) (149+162) LEUKOTHEA (183+467) POLYSITO (319+450) KILKIS SERRES (170+243) TOXOTES (307+400) MESTI PAIONIA METALLIKO (277+371) MONASTIRI (369+374) PEPLOS (64+726) (126+040) KAVALA (222+335) (50+367) CHRYSO VENNA (39+937) KIRKI (137+422) (354+859) PELLA KILKIS (KRISTONI) NEA ZICHNI DIMITRA (385+892) FERES POLYKASTRO (163+242) (28+509) KREMENICA NEOS KAFKASOS (56+747) (41+163) (158+200, 0+000) (206+070) (200+400) MYRKINOS POTAMOS ASPROS SERRES (6+182) (397+839) (43+628) GALLIKOS AMFIPOLI KASTANAS (28+755) MESONISIO ARNISSA AGRAS EDESSA LIMENAS (17+450) (36+346) (136+784) (119+091) AMFIPOLIS (187+464, 0+000) (110+700) FILADELFEIA (24+849) VEVI GEFYRA (20+899) FLORINA (178+490) SKYDRA (23+439) ALEXANDROUPOLI T U R K E Y (5+446) VEGORITIDA THESSALONIKI (95+774) ADENDRO AXIOS (0+362) (143+200) -
Synergy of Tectonic Geomorphology, Applied Geophysics and Remote Sensing Techniques Reveals New Data for Active Extensional Tectonism in NW Peloponnese (Greece)
Geomorphology 237 (2015) 52–64 Contents lists available at ScienceDirect Geomorphology journal homepage: www.elsevier.com/locate/geomorph Synergy of tectonic geomorphology, applied geophysics and remote sensing techniques reveals new data for active extensional tectonism in NW Peloponnese (Greece) Ioannis Fountoulis b,1, Emmanuel Vassilakis a,⁎, Spyridon Mavroulis b, John Alexopoulos c, Spyridon Dilalos c, Athanasia Erkeki d a National and Kapodistrian University of Athens, Faculty of Geology and Geoenvironment, Department of Geography & Climatology, Panepistimiopolis Zografou 15784, Greece b National and Kapodistrian University of Athens, Faculty of Geology and Geoenvironment, Department of Dynamic Tectonic Applied Geology, Panepistimiopolis Zografou 15784, Greece c National and Kapodistrian University of Athens, Faculty of Geology and Geoenvironment, Department of Geophysics-Geothermy, Panepistimiopolis Zografou 15784, Greece d National and Kapodistrian University of Athens, Faculty of Geology and Geoenvironment, Laboratory of Natural Hazards' Prevention & Management, Panepistimiopolis Zografou 15784, Greece article info abstract Article history: In tectonically active areas, such as in the northwest Peloponnese of western Greece, geomorphic processes are Received 3 April 2012 strongly influenced by active faulting; in many cases such faults cannot be easily identified. In this paper we Received in revised form 17 November 2014 apply multidisciplinary analysis (morphotectonic indices, neotectonic mapping, geophysical surveys and remote Accepted 25 November 2014 sensing techniques) to map the recently-recognized east–west trending Pineios River normal fault zone with a Available online 3 December 2014 high degree of accuracy, and to better understand its contribution to the evolution of the ancient region of Elis dur- ing Holocene time. Fault activity seems to be related to frequent changes in river flow patterns and to displacements Keywords: Morphotectonic indices of the nearby shoreline. -
Damaging Earthquakes Since 1909 – a Macroseismic Approach
REVISITING THE VARTHOLOMIO (W. PELOPONNESE) DAMAGING EARTHQUAKES SINCE 1909 – A MACROSEISMIC APPROACH Giannis MISAILIDIS1 Vasiliki KOUSKOUNA2 Eleftheria PAPADIMITRIOU3 ABSTRACT Macroseismic intensity data provide a useful tool for seismic hazard analysis and largely contribute to seismic risk assessment, when vulnerability classification is involved in a detailed manner as in the EMS98 scale. Therefore, relevant information is exploited for the Vartholomio area belonging to the western Peloponnese highly active seismicity zone, between the Ionian Islands and the Gulf of Corinth, and having experienced five damaging earthquakes since the beginning of the 20th century. For these events, a considerable number of macroseismic intensities are available, expressed in various intensity scales (Rossi-Forel, Modified Mercalli, EMS98). These earthquakes are revisited and an effort is made towards harmonization of the intensities expressed in different scales. Furthermore, contemporary newspaper earthquake reports (articles and photographic material) are extensively evaluated and used as additional sources of macroseismic information, in order to re-evaluate in the EMS98 scale and enrich the existing intensity data stock. INTRODUCTION Macroseismic intensity reports consist an indisputable measure of the earthquake via its effects used in various studies covering a wide range of seismological applications. For the pre-instrumental era in particular, but even in times when the seismological networks were inadequate to reliably determine focal parameters, the observed macroseismic intensities contribute to assess the epicentre, focal depth and magnitude of given event and/or amount of seismic energy released. It has to be particularly pointed out that macroseismic data are the only information describing earthquake damage of the historical earthquakes, for which no instrumental records exist. -
Synergy of Tectonic Geomorphology, Applied Geophysics and Remote Sensing Techniques Reveals New Data for Active Extensional Tectonism in NW Peloponnese (Greece)
GEOMOR-04985; No of Pages 13 Geomorphology xxx (2014) xxx–xxx Contents lists available at ScienceDirect Geomorphology journal homepage: www.elsevier.com/locate/geomorph Synergy of tectonic geomorphology, applied geophysics and remote sensing techniques reveals new data for active extensional tectonism in NW Peloponnese (Greece) Ioannis Fountoulis b,1, Emmanuel Vassilakis a,⁎, Spyridon Mavroulis b, John Alexopoulos c, Spyridon Dilalos c, Athanasia Erkeki d a National and Kapodistrian University of Athens, Faculty of Geology and Geoenvironment, Department of Geography & Climatology, Panepistimiopolis Zografou 15784, Greece b National and Kapodistrian University of Athens, Faculty of Geology and Geoenvironment, Department of Dynamic Tectonic Applied Geology, Panepistimiopolis Zografou 15784, Greece c National and Kapodistrian University of Athens, Faculty of Geology and Geoenvironment, Department of Geophysics-Geothermy, Panepistimiopolis Zografou 15784, Greece d National and Kapodistrian University of Athens, Faculty of Geology and Geoenvironment, Laboratory of Natural Hazards' Prevention & Management, Panepistimiopolis Zografou 15784, Greece article info abstract Article history: In tectonically active areas, such as in the northwest Peloponnese of western Greece, geomorphic processes are Received 3 April 2012 strongly influenced by active faulting; in many cases such faults cannot be easily identified. In this paper we Received in revised form 17 November 2014 apply multidisciplinary analysis (morphotectonic indices, neotectonic mapping, geophysical surveys and remote Accepted 25 November 2014 sensing techniques) to map the recently-recognized east–west trending Pineios River normal fault zone with a Available online xxxx high degree of accuracy, and to better understand its contribution to the evolution of the ancient region of Elis during Holocene time. Fault activity seems to be related to frequent changes in river flow patterns and to dis- Keywords: Morphotectonic indices placements of the nearby shoreline. -
AG 56.06.13 MAVROULIS Final:Layout 6
ANNALS OF GEOPHYSICS, 56, 6, 2013, S0681; doi:10.4401/ag-6239 Special Issue: Earthquake geology Seismic intensity assignments for the 2008 Andravida (NW Peloponnese, Greece) strike-slip event (June 8, Mw=6.4) based on the application of the Environmental Seismic Intensity scale (ESI 2007) and the European Macroseismic scale (EMS-98). Geological structure, active tectonics, earthquake environmental effects and damage pattern Spyridon D. Mavroulis1,*, Ioannis G. Fountoulis1, Emmanuel N. Skourtsos1, Efthymis L. Lekkas1, Ioannis D. Papanikolaou2 1 National and Kapodistrian University of Athens, Faculty of Geology and Geoenvironment, Department of Dynamic Tectonic Applied Geology, Panepistimiopolis, Athens, Greece 2 Agricultural University of Athens, Department of Geological Sciences and Atmospheric Environment, Laboratory of Mineralogy and Geology, Athens, Greece Article history Received October 19, 2012; accepted November 14, 2013. Subject classification: Active faults, Earthquake environmental effects, ESI 2007 intensity scale, EMS-98 intensity scale, Strike-slip earthquakes. ABSTRACT ance design. Correlation of all existing data shows that the geological struc- On June 8, 2008, a strike-slip earthquake (Mw=6.4) was generated NE ture, the active tectonics, and the geotechnical characteristics of the alpine of the Andravida town (NW Peloponnese, western Greece) due to the ac- and post-alpine formations along with the construction type of buildings tivation of the previously unknown western Achaia strike-slip fault zone were of decisive importance in the damage and the EEE distribution. (WAFZ). Extensive structural damage and earthquake environmental ef- fects (EEE) were induced in the NW Peloponnese, offering the opportunity 1. Introduction to test and compare the ESI 2007 and the EMS-98 intensity scales in a Earthquake environmental effects (EEE) have been moderate strike-slip event.