Homeric Towns in East Lokris Problems of Identification
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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. -
And Aegean Bronze Age Archaeology
AEGAEUM28 Annales d'archeologie egeenne de l'Universite de Liege et UT-PASP EPOS RECONSIDERING GREEK EPIC AND AEGEAN BRONZE AGE ARCHAEOLOGY Proceedings of the 11th International Aegean Conference / lIe Rencontre egeenne internationale Los Angeles, UCLA - The J. Paul Getty Villa, 20-23 April 2006 Edited by Sarah P. MORRIS and Robert LAFFINEUR Universite de Liege Histoire de l'art et archeologie de la Grece antique University of Texas at Austin Program in Aegean Scripts and Prehistory 2007 Illustration: on cover pages: Palace of Nestor at Pylos, the Lyer-player fresco (watercolor Piet de Jong) Courtesy of the Department of Classics, University of Cincinnati D-2007 0480 33 Printed in Belgium by KLIEMO SA B4700 Eupen Publie avec l'aide financiere du Fonds de la Recherche Scientifique - FNRS All rights reserved. No part of this book 'may be reproducted in any form without written permission of the editors: R. LAFFINEUR, Universite de Liege, Service d'Histoire de l'art et d'archeologie de la Grece antique, Quai Roosevelt lb, B-4000 LIEGE (Belgique) Th.G. PALAIMA, Program in Aegean Scripts and Prehistory, The University of Texas at Austin, Department of Classics, WAG 123, AUSTIN, Tx '78712-1181 (U.S.A) THE SITE OF MITROU AND EAST LOKRIS IN "HOMERIC TIMES"* The area of East Lokris on the North Euboean Gulf is surprisingly prominent in Homer's Iliad, in contrast to its low status as a backwater in later historical times (PI. LX). East Lokris is the home of not one but two important Homeric heroes: Patroclus and Ajax "the lesser," son of Oileus. -
The Cognitive Benefits of Learning Native Language
Short Communication Open Access J Neurol Neurosurg Volume 10 Issue 3 - March 2019 DOI: 10.19080/OAJNN.2019.10.555788 Copyright © All rights are reserved by Genc Struga The Cognitive Benefits of Learning Native Language Genc Struga1* and Thomas Bak2 1Department of Neuroscience, University Hospital Mother Teresa, Albania 2Department of Psychology, Psychology and Language Sciences University of Edinburgh, UK Submission: February 05, 2019; Published: March 26, 2019 *Corresponding author: Genc Struga, Department of Neuroscience, University Hospital Mother Teresa, Albania Abstract Background The cognitive benefits of learning native language and bilingualism project focuses on Arvanites, a bilingual population in Greece that speak theAvantika, ability a for dialect further of learningAlbanian and language acquisition still spokenof other in languages. vast areas of Greece. It is classified as a minority and an endagered language and is considered in risk of extinction. The project aims to examine possible cognitive benefits of bilingualism in native speakers of Avantika, including Method We aim to achieve statistically important number of Arvanites equal Bilingual and monolingual to be interview using a up to date questionnaire and TEA or TEA like cognitive screening. This is a cross-sectional population study including bilingual and monolingual speakers orwithout 15% ofexclusion population. criteria and with respects to gender equality, stratified random sampling responders in the areas where Arvanite population traditionally lived achieving -
Selido3 Part 1
ΔΕΛΤΙΟ ΤΗΣ ΕΛΛΗΝΙΚΗΣ ΓΕΩΛΟΓΙΚΗΣ ΕΤΑΙΡΙΑΣ Τόμος XLIII, Νο 3 BULLETIN OF THE GEOLOGICAL SOCIETY OF GREECE Volume XLIII, Νο 3 1 (3) ΕΙΚΟΝΑ ΕΞΩΦΥΛΛΟΥ - COVER PAGE Γενική άποψη της γέφυρας Ρίου-Αντιρρίου. Οι πυλώνες της γέφυρας διασκοπήθηκαν γεωφυ- σικά με χρήση ηχοβολιστή πλευρικής σάρωσης (EG&G 4100P και EG&G 272TD) με σκοπό την αποτύπωση του πυθμένα στην περιοχή του έργου, όσο και των βάθρων των πυλώνων. (Εργα- στήριο Θαλάσσιας Γεωλογίας & Φυσικής Ωκεανογραφίας, Πανεπιστήμιο Πατρών. Συλλογή και επεξεργασία: Δ.Χριστοδούλου, Η. Φακίρης). General view of the Rion-Antirion bridge, from a marine geophysical survey conducted by side scan sonar (EG&G 4100P and EG&G 272TD) in order to map the seafloor at the site of the construction (py- lons and piers) (Gallery of the Laboratory of Marine Geology and Physical Oceanography, University of Patras. Data acquisition and Processing: D. Christodoulou, E. Fakiris). ΔΕΛΤΙΟ ΤΗΣ ΕΛΛΗΝΙΚΗΣ ΓΕΩΛΟΓΙΚΗΣ ΕΤΑΙΡΙΑΣ Τόμος XLIII, Νο 3 BULLETIN OF THE GEOLOGICAL SOCIETY OF GREECE Volume XLIII, Νο 3 12o ΔΙΕΘΝΕΣ ΣΥΝΕΔΡΙΟ ΤΗΣ ΕΛΛΗΝΙΚΗΣ ΓΕΩΛΟΓΙΚΗΣ ΕΤΑΙΡΙΑΣ ΠΛΑΝHΤΗΣ ΓH: Γεωλογικές Διεργασίες και Βιώσιμη Ανάπτυξη 12th INTERNATIONAL CONGRESS OF THE GEOLOGICAL SOCIETY OF GREECE PLANET EARTH: Geological Processes and Sustainable Development ΠΑΤΡΑ / PATRAS 2010 ISSN 0438-9557 Copyright © από την Ελληνική Γεωλογική Εταιρία Copyright © by the Geological Society of Greece 12o ΔΙΕΘΝΕΣ ΣΥΝΕΔΡΙΟ ΤΗΣ ΕΛΛΗΝΙΚΗΣ ΓΕΩΛΟΓΙΚΗΣ ΕΤΑΙΡΙΑΣ ΠΛΑΝΗΤΗΣ ΓΗ: Γεωλογικές Διεργασίες και Βιώσιμη Ανάπτυξη Υπό την Αιγίδα του Υπουργείου Περιβάλλοντος, Ενέργειας και Κλιματικής Αλλαγής 12th INTERNATIONAL CONGRESS OF THE GEOLOGICAL SOCIETY OF GREECE PLANET EARTH: Geological Processes and Sustainable Development Under the Aegis of the Ministry of Environment, Energy and Climate Change ΠΡΑΚΤΙΚΑ / PROCEEDINGS ΕΠΙΜΕΛΕΙΑ ΕΚΔΟΣΗΣ EDITORS Γ. -
Locris, Central Greece) Earthquake Sources Through Coeval Records on Macroseismic Effects by Paola Albini and Daniela Pantosti
Bulletin of the Seismological Society of America, Vol. 94, No. 4, pp. 1305–1326, August 2004 The 20 and 27 April 1894 (Locris, Central Greece) Earthquake Sources through Coeval Records on Macroseismic Effects by Paola Albini and Daniela Pantosti Abstract Newly retrieved coeval records on the effects of the two large earth- quakes of 20 and 27 April 1894 in Locris (central Greece) have been analyzed to assess macroseismic intensities according to the European Macroseismic Scale (Gru¨nthal, 1998). An intensity equal or higher than 8 has been estimated at 70 dif- ferent places. The two earthquakes were close in time and both focused on the same area; this asked for an interpretation free, as much as possible, from the prejudice due to the accumulative descriptions implied, for instance, by the 1894 scientists’ reports. To image the earthquake sources and derive the main seismic parameters, we processed the macroseismic intensity data by using the Boxer method proposed by Gasperini et al. (1999). On the basis of this approach and our new sets of data, we obtain M 6.4 and 6.5 for the 20 and 27 April earthquakes, respectively, the latter being substantially smaller than the estimates proposed in previous works. Results obtained from the processing of macroseismic data have been tested and compared to recent geological data. Our preferred interpretation is that the 20 and 27 April 1894 earthquakes ruptured together the whole Atalanti fault. The internal structural complexity of the Atalanti fault appears to have controlled the rupture propagation: the change in strike of the fault trace along with its intersection with the Malesina fault, near Proskinas, is interpreted as a geometric barrier that is the boundary be- tween the two individual earthquake sources. -
Papanastassiou Et Al Arkitsa Preprint.Pdf
1 The uplifted terraces of the Arkitsa region, NW Evoikos Gulf, Greece: a 2 result of combined tectonic and volcanic processes? 3 4 Dimitris Papanastassiou1, A. B. Cundy2*, K. Gaki-Papanastassiou3, M. R. Frogley4, K. 5 Tsanakas3, H. Maroukian3 6 7 8 1 Institute of Geodynamics, National Observatory of Athens, Gr 11810 Athens, Greece 9 2 School of Environment and Technology, University of Brighton, Brighton, BN2 4GJ, UK 10 3 Department of Geography-Climatology, University of Athens, Gr 15784 Athens, Greece 11 4 Department of Geography, University of Sussex, Falmer, Brighton, BN1 9QJ, UK 12 * Corresponding author: School of Environment and Technology, University of Brighton, Brighton, BN2 13 4GJ, UK. Email: [email protected]; Tel: +44 1273 642270; Fax: +44 1273 642285 14 ABSTRACT 15 The Arkitsa-Kamena Vourla area of central Greece occupies a zone of accommodation 16 between the two tectonic provinces of the North Aegean Trough (the extension of the 17 North Anatolian fault system) and the Gulf of Corinth, and is characterised by a series 18 of very prominent tectonic landforms, notably the large (ca. 1000 m elevation) 19 footwall ridge of the Arkitsa-Kamena Vourla fault system. Despite the highly prominent 20 nature of this footwall ridge and the presence of very fresh tectonic landforms this 21 fault system is not known to have hosted any major historical earthquakes, and the 22 tectonic and geomorphic evolution of the Arkitsa-Kamena Vourla area remains poorly 23 constrained. This paper utilises a combined geomorphological, sedimentological and 24 macro-/micro-fossil approach to evaluate the Late Quaternary evolution of the Arkitsa 25 area, in the eastern part of the fault system, focussing on prominent uplifted terraces 26 present in the hangingwall of the Arkitsa fault. -
The Locrians and the Sea*
ADOLFO J. DOMÍNGUEZ The Locrians and the Sea* As is well known, the Locrians occupied two different territories in central Greece, although for both the relationship with the sea was intense. Eastern Lo- cris occupied a stretch of about 80 km. as the crow flies on the Gulf of Northern Euboea while Western Locris occupied a similar distance along the north coast of the Gulf of Corinth. In this paper I shall analyse the information we have about the relationship of these two territories with the sea. We shall begin our analysis with Eastern Locris. Although I shall not dwell too long on the period following the end of the Mycenaean age, we do need to consider an interesting piece of evidence. Exca- vations carried out in Pyrgos Livanates have shown, in the phase beginning after a mid-twelfth century earthquake, important elements linking this site to the sea. Thus, along with miniature models of commercial and war vessels, some craters with painted decoration depicting scenes of naval battles have been found. Since it seems that the pottery was manufactured in situ we can assume that it proba- bly depicts actual acts of naval war and/or piracy, which would have been fre- quent in this turbulent period1. Some possible relationships, perhaps of an economic nature, between Lo- cris and the eastern and northeastern Aegean during the Protogeometric Age had been suggested by the discovery at Troy of amphorae with parallels that indicate a place of production in the Locrian territory or neighbouring regions2, although new researches suggest that at least part of them were locally manufactured in the Troad; however there are other wares in Troy (e.g. -
II. MITTELGRIECHENLAND 1. Boiotien Besiedlung
II. MITTELGRIECHENLAND Zu den Grabungen bis 1979 siehe auch Leekley – Efstratiou 1980. 1. Boiotien Besiedlung Lit.: Konsola 1981, 33–47; 52–58. Fossey 1988, 407–419. Chronologie: Maran 1998, 54–73. Zusammenfassend: van Effenterre H. 1989, 39–45. Die Arbeiten von Konsola und Fossey enthalten Zusammenstellungen der früh- helladischen Fundorte Boiotiens. Fossey kennt 60 frühhelladische Fundorte, von denen 31 in FH I, 34 in FH II und 19 in FH III datieren. Gegenüber dem Neolithi- kum nimmt die Besiedlung deutlich zu, und zwischen FH I und II ist Siedlungskon- tinuität zu beobachten. In FH III findet ein Siedlungsrückgang statt, jedoch werden bedeutende Fundorte auch noch in dieser Periode genutzt. Aussagen über einen möglichen Bruch am Ende von FH III sind hingegen nicht mit Sicherheit möglich.1 Das Siedlungsmuster zeigt während der Frühbronzezeit weiterhin nur eine geringe Besiedlung um die Kopais, während die Zunahme von Fundorten am Hylike- und Paralimni-See sowie am Golf von Euboia in Zusammenhang mit den Beziehungen zu den aufblühenden Siedlungen auf Euboia und ihren Verbindungen zu den Kyk- laden zu sehen ist. Die boiotischen Siedlungen lagen an natürlichen Wegen, die das Landesinnere, und damit auch Theben mit dem Golf von Euboia verbanden.2 Theben (Taf. 42) Lit.: Zusammenfassend: Konsola 1981, 103–111; 117–126; 143–152; 159–166. Symeonoglou 1985, 15–19; siehe auch S. 213–309, catalogue of sites, site nos. 1–6, 12, 13, 18, 51, 88, 101, 110, 112, 121, 131, 166, 171, 179, 184, 186, 205, 208, 245, 268. Demakopoulou – Konsola 1981. Forsén J. 1992, 130–135. Farakla 1998, 179–181; 193–205. -
New Mycenaean Pottery Production Centers from the East
NEW MYCENAEAN POTTERY PRODUCTION CENTERS FROM THE EAST ERN PART OF CENTRAL GREECE OBTAINED BY NEUTRON ACTIVATION ANALYSIS & & # H Mommsen A Hein D Ittameier J Maran and Ph Dakoronia Institut fur Strahlen und Kernphysik Universitat Bonn Nuallee Bonn & Institut fur Ur und Fruhgeschichte Universitat Heidelb erg Marstallhof th # Heidelb erg and Ephorate of Antiquities Lamia Greece November Abstract Neutron activation analysis results of a set of more than sherds and whole vessels including misred pieces from Lo cris Phthiotis and Southwestern Thessaly are presented The material covers the time p erio d Middle Helladic to Late Helladic I I IC Several new patterns are detected some of which can b e assigned with high probability to that region A sp ecial result concerns several fragments of pictorial craters depicting ships and sea battles found in LHI I IC Middle levels at LivanatesKynos As suggested by our data they originate from a manufacturing place in Eastern Lo cris Introduction Since the midies our archaeometry group is working on a pro ject concerning the classication and provenance determination of Aegean Bronze Age p ottery which has b een a fo cus of archaeological interest for more than a years Of all the dierent p ottery classes used during the Bronze Age sp ecial attention was paid to the ne decorated p ottery of the Greek Mainland and adjacent regions The p erio d of the Late Bronze Age the Mycenaean p erio d is esp ecially well investigated and this for the following reasons Mycenaean decorated p ottery shows -
Segment Boundaries, the 1894 Ruptures and Strain Patterns Along the Atalanti Fault, Central Greece
.I. Geodynnmics Vol. 26, No. 24, pp. 461486, 1998 0 1998 Published by Elsevier Science Ltd Pergamon All rights reserved. Printed in Great Britain PII: SO264-3707(!W)ooo66-5 0X&3707/98 $19.00+0.00 SEGMENT BOUNDARIES, THE 1894 RUPTURES AND STRAIN PATTERNS ALONG THE ATALANTI FAULT, CENTRAL GREECE ATHANASSIOS GANAS,‘* GERALD P. ROBERTS2 and TZETTA MEMOU3 ‘Department of Geography, University of Reading, Whiteknights, Reading RG6 6AB, U.K. *The Research School of Geological and Geophysical Sciences, Birkbeck and University College London, Gower Street, London WClE 6BT, U.K. ‘Division of Geophysics, IGME, 70 Messoghion Str., 115 27 Athens, Greece (Received 27 April 1997; revised 2 June 1997; accepted 5 June 1997) Abstract-The Atalanti Fault is a large active normal fault segment inside the Gulf of Evia Rift system (Central Greece), that last ruptured during the April 1894 earthquake sequence. Using structural and geomorphological interpretations of digitally processed Landsat TM satellite imagery, two regions of i) low topography, ii) minimum hinterland development and iii) transverse bedrock ridge development, 34 kilometres apart were identified; these regions are suggested to be segment boundaries constraining the length of the fault. From throw profiles and displaced syn-rift strata, we estimate a minimum slip of 810m at the central region of the fault (Tragana), increasing to a value of 1200 meters within the Asprorema embayment area. These figures averaged over a time span of 3 million years (age of oldest offset syn-rift), yield mean slip rates of at least 0.27 to 0.4 mm/year. Field studies were also conducted along the length of the Atalanti Fault Segment to re- examine and map the 1894 ruptures. -
Paleoseismological Trenching Across the Atalanti Fault (Central Greece): Evidence for the Ancestors of the 1894 Earthquake During the Middle Ages and Roman Times by D
Bulletin of the Seismological Society of America, Vol. 94, No. 2, pp. 531–549, April 2004 Paleoseismological Trenching across the Atalanti Fault (Central Greece): Evidence for the Ancestors of the 1894 Earthquake during the Middle Ages and Roman Times by D. Pantosti, P. M. De Martini, D. Papanastassiou, F. Lemeille, N. Palyvos,* and G. Stavrakakis Abstract The Atalanti fault bounds to the southwest the Evoikos Gulf, one of the major extensional basins of central Greece. This fault ruptured during the 1894 earth- quakes, producing at the surface a complex, ca. 30-km-long rupture. Paleoseismo- logical trenching performed at three sites along this fault provided the first insights on its seismogenic behavior. Unfavorable trench stratigraphy and scarcity of datable material made the identification and characterization of individual paleoearthquakes quite difficult. However, by integrating paleoseismological, geological, historical, and archaeoseismological data, we defined three surface-faulting earthquakes. The most recent event is the 1894 earthquake; the penultimate occurred during the Middle Ages between A.D. 770 and 1160, whereas the third event back occurred in Roman times between 50 B.C. and A.D. 230 and is interpreted to be the Opus earthquake of A.D. 105. These results suggest that 1894-type earthquakes repeat each 660–1120 yr. The average minimum slip per event and vertical slip rates are of the order of 45 cm and 0.4–1.6 mm/yr, respectively. These values are in agreement with other geological estimates and with geodetic measurements. Because of the short time elapsed since the 1894 earthquake, the Atalanti fault does not appear to contain an important seis- mogenic potential. -
Copyright© 2017 K. Tsanakas, K. Gaki-Papanastassiou, SE Poulos, H
Bulletin of the Geological Society of Greece Vol. 43, 2010 GEOMORPHOLOGY AND SEDIMENTOLOGICAL PROCESSES ALONG THE COASTAL ZONE BETWEEN LIVANATES AND AGIOS KONSTANTINOS (N. EVOIKOS GULF, CENTRAL GREECE) Tsanakas K. National and Kapodistrian University of Athens, Faculty of Geology and Geoenvironment, Department of Geography and Climatology Gaki-Papanastassiou K. National and Kapodistrian University of Athens, Faculty of Geology and Geoenvironment, Department of Geography and Climatology Poulos S.E. National and Kapodistrian University of Athens, Faculty of Geology and Geoenvironment, Department of Geography and Climatology Maroukian H. National and Kapodistrian University of Athens, Faculty of Geology and Geoenvironment, Department of Geography and Climatology http://dx.doi.org/10.12681/bgsg.11201 Copyright © 2017 K. Tsanakas, K. Gaki- Papanastassiou, S.E. Poulos, H. Maroukian To cite this article: Tsanakas, K., Gaki-Papanastassiou, K., Poulos, S., & Maroukian, H. (2010). GEOMORPHOLOGY AND SEDIMENTOLOGICAL PROCESSES ALONG THE COASTAL ZONE BETWEEN LIVANATES AND AGIOS http://epublishing.ekt.gr | e-Publisher: EKT | Downloaded at 01/08/2019 17:29:48 | KONSTANTINOS (N. EVOIKOS GULF, CENTRAL GREECE). Bulletin of the Geological Society of Greece, 43(1), 506-515. doi:http://dx.doi.org/10.12681/bgsg.11201 http://epublishing.ekt.gr | e-Publisher: EKT | Downloaded at 01/08/2019 17:29:48 | Δελτίο της Ελληνικής Γεωλογικής Εταιρίας, 2010 Bulletin of the Geological Society of Greece, 2010 Πρακτικά 12ου Διεθνούς Συνεδρίου Proceedings of the 12th International