CRL School 2018 Corinth Rift Observatory
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SUSTAINABILITY REPORT 1 1 2 at a Glance Message 06 07 from the CEO
The best travel companion 2018 ANNUAL www.neaodos.gr SUSTAINABILITY REPORT 1 1 2 Message from the CEO 06 07At a glance Nea Odos11 21Awards Road Safety 25 37 Corporate Responsibility 51 High Quality Service Provision 3 69Human Resources Caring for the Enviment81 Collaboration with Local Communities 93 and Social Contribution 4 Sustainable Development Goals in103 our operation 107Report Profile GRI Content Index109 5 Message from the CEO Dear stakeholders, The publication of the 5th annual Nea Odos Corporate Responsibility Report constitutes a substantial, fully documented proof that the goal we set several years ago as regards integrating the principles, values and commitments of Corporate Responsibility into every aspect of our daily operations has now become a reality. The 2018 Report is extremely important to us, as 2018 signals the operational completion of our project, and during this year: A) Both the construction and the full operation of the Ionia Odos motorway have been completed, a project linking 2 Regions, 4 prefectures and 10 Municipalities, giving a boost to development not only in Western Greece and Epirus, but in the whole country, B) Significant infrastructure upgrade projects have also been designed, implemented and completed at the A.TH.E Motorway section from Metamorphosis in Attica to Scarfia, a section we operate, maintain and manage. During the first year of the full operation of the motorways - with 500 employees in management and operation, with more than 350 kilometres of modern, safe motorways in 7 prefectures of our country with a multitude of local communities - we incorporated in our daily operations actions, activities and programs we had designed, aiming at supporting and implementing the key strategic and development pillars of our company for the upcoming years. -
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Mediterranean Marine Science Vol. 14, 2013 Zooplankton diversity and distribution in a deep and anoxic Mediterranean coastal lake KEHAYIAS G. Department of Environmental and Natural Resources Management, University of Western Greece, Seferi 2, 30 100, Agrinio, Greece RAMFOS A. Department of Aquaculture and Fisheries Management, Technological Educational Institute of Messolonghi, 30200 Messolonghi, Greece IOANNOU S. Department of Environmental and Natural Resources Management, University of Western Greece, Seferi 2, 30 100, Agrinio, Greece BISOUKI P. Department of Environmental and Natural Resources Management, University of Western Greece, Seferi 2, 30 100, Agrinio, Greece KYRTZOGLOU E. Department of Environmental and Natural Resources Management, University of Western Greece, Seferi 2, 30 100, Agrinio, Greece GIANNI A. Department of Environmental and Natural Resources Management, University of Western Greece, Seferi 2, 30 100, Agrinio, Greece ZACHARIAS I. Department of Environmental and Natural Resources Management, University of Western Greece, Seferi 2, 30 100, Agrinio, Greece https://doi.org/10.12681/mms.332 Copyright © 2013 http://epublishing.ekt.gr | e-Publisher: EKT | Downloaded at 04/10/2021 13:17:24 | To cite this article: KEHAYIAS, G., RAMFOS, A., IOANNOU, S., BISOUKI, P., KYRTZOGLOU, E., GIANNI, A., & ZACHARIAS, I. (2013). Zooplankton diversity and distribution in a deep and anoxic Mediterranean coastal lake. Mediterranean Marine Science, 14(1), 179-192. doi:https://doi.org/10.12681/mms.332 http://epublishing.ekt.gr | e-Publisher: EKT | Downloaded at 04/10/2021 13:17:25 | Research Article Mediterranean Marine Science Indexed in WoS (Web of Science, ISI Thomson) and SCOPUS The journal is available on line at http://www.medit-mar-sc.net http://dx.doi.org/10.12681/mms.332 Zooplankton diversity and distribution in a deep and anoxic Mediterranean coastal lake G. -
D. Giannopoulos , E. Sokos , K. Konstantinou , A. Lois , G-Akis Tselentis (Email: [email protected]) Crustal Dynamics Vs Anisotropy
Temporal variation of shear-wave splitting parameters related to Movri Mountain earthquake in northwest Peloponnese (Greece) (1) University of Patras, (2) Institute of Geophysics, Department of Geology, National Central University, (1) (1) (2) (1) (1) EGU2012-8549 Seismology Laboratory, Taiwan GD2.2/GMPV6.5/SM3.7/TS3.8 Greece D. Giannopoulos , E. Sokos , K. Konstantinou , A. Lois , G-Akis Tselentis (email: [email protected]) Crustal Dynamics vs Anisotropy 21o20’ 21o30’ 21o40’ ABSTRACT Patraikos Gulf Patras DATA RESULTS For the purpose of this study three-component recordings are needed from stations in continuous operation during the periods before and after the occurrence After the analysis we obtained valid results (ö, dt) from 10 seismic events On June 8, 2008, at 12:25 GMT, a Mw 6.4 earthquake occur- Kefallonia of the Movri Mountain earthquake. The only station in the study area that satisfied the above criterion was Riolos station (RLS) which is operating since the for the period before the occurrence of the Movri Mountain earthquake Ionian red in the area of northwest Peloponnese, western Greece. Thrust July of 2001. No other seismological station around the epicenter was equipped with three-component seismometers and operating continuously in the and from 122 seismic events for the period after the earthquake (Fig. 2, 3). Ionian Sea Araxos Kato Achaia The epicenter was located in the municipality of Movri 35km H studied time period. The station is part of the seismological network of the Institute of Geodynamics, National Observatory of Athens (GI-NOA) and the e l Peloponnese le Polarization directions. Before the earthquake, the polarization southwest of Patras. -
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. -
Surface Deformation During the Mw 6.4 (8 June 2008) Movri Mountain Earthquake in the Peloponnese, and Its Implications for the Seismotectonics of Western Greece
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/233447964 Surface deformation during the Mw 6.4 (8 June 2008) Movri Mountain earthquake in the Peloponnese, and its implications for the seismotectonics of western Greece Article in International Geology Review · February 2010 DOI: 10.1080/00206810802674329 CITATIONS READS 28 94 3 authors: Ioannis Koukouvelas Sotirios Kokkalas University of Patras Khalifa University 109 PUBLICATIONS 1,865 CITATIONS 70 PUBLICATIONS 1,003 CITATIONS SEE PROFILE SEE PROFILE P. Xypolias University of Patras 69 PUBLICATIONS 1,102 CITATIONS SEE PROFILE Some of the authors of this publication are also working on these related projects: Palaeoseismological investigation of faults in Greece View project Tectonometamorphic evolution of the Hellenides during the Late Cretaceous to Eocene View project All content following this page was uploaded by Ioannis Koukouvelas on 31 May 2014. The user has requested enhancement of the downloaded file. This article was downloaded by: [HEAL-Link Consortium] On: 25 November 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 International Geology Review Publication details, including instructions for authors and subscription information: http://www.informaworld.com/smpp/title~content=t902953900 Surface deformation during the Mw 6.4 -
Geophysical Journal International - Supplementary Material For
1 Geophysical Journal International - Supplementary material for 2 3 The GPS velocity field of the Aegean. New observations, contribution of the earthquakes, 4 crustal blocks model. 5 6 Briole, P., Ganas, A., Elias, P & Dimitrov, D. 7 8 SUMMARY 9 10 The analysis of the secular component of the velocity field of the Aegean presented, discussed and 11 modelled in the main text, requires the accurate determination of the transient part of the velocity 12 field. This transient part is dominated by the coseismic displacements produced by the major 13 earthquakes that occurred in the area during the analysed time window. Another significant 14 component is due to the postseismic relaxations associated with those earthquakes. In this 15 supplementary material we review the coseismic and postseismic displacements induced by the 16 crustal earthquakes of magnitude Mw ≥ 5.3 during the period 2000-2020. In addition, several GPS 17 stations have their time series disrupted by other sources of transients with different origins, that we 18 also present and discuss. Once the transient velocity field is estimated it can be removed from the 19 total velocity field to extract what can be considered as the secular velocity field. We discuss the 20 gradients of this secular velocity field as they are measured along three sections originated at the 21 Euler pole of rotation Anatolia-Eurasia. 22 23 24 S1. INTRODUCTION 25 1 26 During the period 2000-2020 several strong earthquakes occurred in the Aegean region, with a 27 concentration in western Greece around and near the Ionian Islands: Lefkada 2003, Movri 2008, 28 Cephalonia doublet 2014, Lefkada 2015, and Zakynthos 2018. -
Temporal and Spatial Distribution of Physico-Chemical Parameters in an Anoxic Lagoon, Aitoliko, Greece
107 © 2012 Triveni Enterprises J. Environ. Biol. Vikas Nagar, Lucknow, INDIA 33, 107-114 (2012) [email protected] ISSN: 0254-8704 Full paper available on: www.jeb.co.in CODEN: JEBIDP Temporal and spatial distribution of physico-chemical parameters in an anoxic lagoon, Aitoliko, Greece Author Details Areti Gianni Department of Environmental and Natural Resources Management, University of Ioannina, 2 Seferi Str., 30100 Agrinio, Greece George Kehayias Department of Environmental and Natural Resources Management, University of Ioannina, 2 Seferi Str., 30100 Agrinio, Greece Ierotheos Zacharias Department of Environmental and Natural Resources Management, University of Ioannina, (Corresponding author ) 2 Seferi Str., 30100 Agrinio, Greece e-mail: [email protected] Abstract Temporal and spatial distribution of physico-chemical and water quality parameters and their correlation with meteorological and hydrological data, was investigated for anoxic lagoons, in Greece. Monthly variations of Publication Data parameters like temperature, salinity, dissolved oxygen, chlorophyll- a, total phosphorus etc. , along the Aitoliko lagoon water column, were recorded and studied at 14 stations. Throughout the sampling period, in Paper received: lagoon’s water column three layers were determined: the surface low density layer (11.49-16.15), the layer 07 April 2010 with the steep density gradient and the deep dense (19.78-20.62) water below the depth of 20 m. The depth of the surface and pycnocline layers depends on seasonal surface salinity (20.53-22.43‰) and temperature Revised received: (12.48-28.40 oC) alterations. Lagoon’s monimolimnion was extended, below the depth of 20 m and had 15 November 2010 constant temperature and salinity equal to about 13oC and 27‰ respectively. -
Spatiotemporal Properties of Seismicity
Spatiotemporal Properties of Seismicity and Variations of Shear-Wave Splitting Parameters in the Western Gulf of Corinth (Greece) Vasilis Kapetanidis, Georgios Michas, George Kaviris, Filippos Vallianatos To cite this version: Vasilis Kapetanidis, Georgios Michas, George Kaviris, Filippos Vallianatos. Spatiotemporal Properties of Seismicity and Variations of Shear-Wave Splitting Parameters in the Western Gulf of Corinth (Greece). Applied Sciences, MDPI, 2021, 11 (14), pp.6573. 10.3390/app11146573. hal-03304262 HAL Id: hal-03304262 https://hal.archives-ouvertes.fr/hal-03304262 Submitted on 28 Jul 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. Distributed under a Creative Commons Attribution| 4.0 International License Article Spatiotemporal Properties of Seismicity and Variations of Shear‐Wave Splitting Parameters in the Western Gulf of Corinth (Greece) Vasilis Kapetanidis 1, Georgios Michas 1, George Kaviris 1 and Filippos Vallianatos 1,2,* 1 Section of Geophysics—Geothermics, Department of Geology and Geoenvironment, National and Kapodistrian -
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. -
Integrated Wastewater Management on a County Basis
03-Tzimas.qxd 9/11/2005 9:33 Page 15 Global Nest: the Int. J. Vol 5, No 1, pp 15-22, 2003 Copyright© 2003 GLOBAL NEST Printed in Greece. All rights reserved INTEGRATED WASTEWATER MANAGEMENT ON A COUNTY BASIS A. TZIMAS Sanitary Engineering Laboratory, E. GAVALAKI Department of Water Resources Hydraulics and Maritime Works, School of Civil Engineering, A. ANDREADAKIS* National Technical University of Athens 5, Iroon Polytechneiou street, Zografou 15773, Athens Selected from papers presented at the 7th Conference *to whom all correspondence should be addressed: on Environmental Science and Technology, fax: +(30) 2106528078, 210772 2899 3-6 September 2001, Ermoupolis, Syros island, Greece. e-mail: [email protected] ABSTRACT The paper discusses a methodology for integrated municipal wastewater management. In compliance to the EU Directive 91/271, there is a legal binding to ensure that all agglomerations with populations over 2000 are provided with wastewater collecting system and adequate treatment. The conditions for optimum application of the Directive in Greece, especially in the light of the recent administrative reor- ganization, and the management of small rural communities not covered by the Directive are addressed, with reference to a case study application in the Achaia County. In compliance to the EU Directive 91/271, it is estimated that collecting systems and treatment should expand to at least 70% of the total population. However, due to the expanding touristic activity, the limited availability of land, environmental considerations, and favorable population characteristics (high density, relatively large communities) and morphological and socioeconomical conditions, it is proposed that coverage can reach to 85% of the total population. -
Improving the Tools for the Social Inclusion and Non-Discrimination of Roma in the EU
Improving the tools for the social inclusion and non-discrimination of Roma in the EU Summary and selected projects This publication is commissioned under the European Union Programme for Employment and Social Solidarity PROGRESS (2007-2013). This programme is managed by the Directorate-General for Employment, social affairs and equal opportunities of the European Commission. It was established to financially support the implementation of the objectives of the European Union in the employment and social affairs area, as set out in the Social Agenda, and thereby contribute to the achievement of the Europe 2020 goals in these fields. The seven-year Programme targets all stakeholders who can help shape the development of appropriate and effective employment and social legislation and policies, across the EU-27, EFTA-EEA and EU candidate and pre-candidate countries. PROGRESS mission is to strengthen the EU contribution in support of Member States’ commitments and efforts to create more and better jobs and to build a more cohesive society. To that effect, PROGRESS is instrumental in: — providing analysis and policy advice on Progress policy areas; — monitoring and reporting on the implementation of EU legislation and policies in Progress policy areas; — promoting policy transfer, learning and support among Member States on EU objectives and priorities; and — relaying the views of the stakeholders and society at large. For more information see: http://ec.europa.eu/progress Improving the tools for the social inclusion and non-discrimination of -
ESCUTIS Greece Study.Pdf
The Educational Approaches to Virtual Reality Laboratory, University of Ioannina, Ioannina, Greece University of Cyprus, Nicosia, Cyprus The Euromediterranean Cultural Heritage Agency, Lecce, Italy Educational Software Development Laboratory, University of Patras, Patras, Greece Contact: The Educational Approaches to Virtual Reality Laboratory University of Ioannina GR-451 10 Ioannina, Greece Tel.: +30 26510 95697 Fax: +30 26510 95854 Email: [email protected] Url: http://earthlab.uoi.gr © copyright 2008 ISBN: 978-960-233-187-3 Design ang layout: Afroditi Zouki Printing: Livanis Publishing Organization S.A., Athens Co - financed by the European Regional Development Fund (ERDF) and by national funds of Greece, Italy and Cyprus Elevating and Safeguarding Culture Using Tools of the Information Society: Dusty traces of the Muslim culture ESCUTIS The Educational Approaches to Virtual Reality Laboratory (EARTHLAB) The University of Ioannina, Ioannina, Greece (Lead Partner) Prof. Tassos A. Mikropoulos, Project Coordinator, Scientific Responsible Prof. George Smyris, Scientific consultant - Researcher Dr. Eleni Pintela, Researcher Nikiforos Papachristos, Administrative and technical support Afroditi Zouki, Graphic designer Margareth Swanberg, Editing Sofia Pegka, Digitization Marikelly Staikopoulou, English-Greek translator Ioannis Vrellis, Technical consultant – QTVR & 3D development Comitech S.A., Dynamic website and Hypermedia development The Euromediterranean Cultural Heritage Agency, Lecce, Italy Lecce, Italy Mauro Martina, Project Manager Prof.