Municipality of Acharnes Conclusion
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Department Town Address Postcode Telephone Etoloakarnania Agrinio
Department Town Address Postcode Telephone Etoloakarnania Agrinio 1, Eirinis square, Dimitrakaki street 301 00 2641046346 Etoloakarnania Mesologgi 45, Charilaou Trikoupi street 302 00 2631022487 Etoloakarnania Nafpaktos 1, Athinon street 303 00 2634038210 Etoloakarnania Amfilohia Vasileos Karapanou street 305 00 2642023302 Argolida Argos 12, Danaou street 212 00 2751069042 Argolida Nafplio 35, Argous street 211 00 2752096478 Argolida Porto Heli Porto Heli Argolidas 210 61 2754052102 Arkardia Megalopoli 15, Kolokotroni street 222 00 2791021131 Arkardia Tripoli 48, Ethinikis Antistaseos street 221 00 2710243770 Arta Arta 129, Skoufa street 471 00 2681077020 Attica Athens 316, Acharnon street & 26 Atlantos street 112 52 2102930333 Attica Agios Dimitrios 54, Agiou Dimitriou street 173 41 2109753953 Attica Agios Dimitrios 276, Vouliagmenis avenue 173 43 2109818908 Attica Agios Dimitrios 9 - 11, Agiou Dimitriou street 173 43 2109764322 Attica Agia Paraskevi 429, Mesogeion avenue 153 43 2106006242 Attica Athens - Piraeus 153, Piraeus Avenue 118 53 2104815333 Attica Athens - Aristeidou 1, Aristeidou street 105 59 2103227778 Attica Athens 79, Alexandras avenue 114 74 2106426650 Attica Athens - Plateia Viktorias 2, Victoria square 104 34 2108220800 Attica Athens - Stadiou 7, Stadiou street 105 62 2103316892 Attica Egaleo 266, Iera Odos street 122 42 2105316671 126, Vasilissis Sofias street & 2, Feidippidou Attica Abelokipoi street 115 27 2106461200 Attica Amfiali 32, Pavlou Fissa street 187 57 2104324300 Attica Palaio Faliro 82, Amfitheas avenue -
Registration Certificate
1 The following information has been supplied by the Greek Aliens Bureau: It is obligatory for all EU nationals to apply for a “Registration Certificate” (Veveosi Engrafis - Βεβαίωση Εγγραφής) after they have spent 3 months in Greece (Directive 2004/38/EC).This requirement also applies to UK nationals during the transition period. This certificate is open- dated. You only need to renew it if your circumstances change e.g. if you had registered as unemployed and you have now found employment. Below we outline some of the required documents for the most common cases. Please refer to the local Police Authorities for information on the regulations for freelancers, domestic employment and students. You should submit your application and required documents at your local Aliens Police (Tmima Allodapon – Τμήμα Αλλοδαπών, for addresses, contact telephone and opening hours see end); if you live outside Athens go to the local police station closest to your residence. In all cases, original documents and photocopies are required. You should approach the Greek Authorities for detailed information on the documents required or further clarification. Please note that some authorities work by appointment and will request that you book an appointment in advance. Required documents in the case of a working person: 1. Valid passport. 2. Two (2) photos. 3. Applicant’s proof of address [a document containing both the applicant’s name and address e.g. photocopy of the house lease, public utility bill (DEH, OTE, EYDAP) or statement from Tax Office (Tax Return)]. If unavailable please see the requirements for hospitality. 4. Photocopy of employment contract. -
The Hadrianic Aqueduct
Proceedings of the 14th International Conference on Environmental Science and Technology Rhodes, Greece, 3-5 September 2015 THE HADRIANIC AQUEDUCT CHRISTAKI M.1, STOURNARAS G.1 and NASTOS P.2 1 National and Kapodistrian University of Athens, Faculty of Geology and Geoenvironment, Department of Dynamic Tectonic Applied Geology, Panepistimiopolis Zografou, 15784, 2 National and Kapodistrian University of Athens, Faculty of Geology and Geoenvironment, Department of Geography and Climatology, Panepistimiopolis Zografou, 15784 E-mail: [email protected] ABSTRACT Since prehistoric times, the city of Athens and the wider region of Attica did not contain many natural water sources so aquatic reserves were never adequate to meet the needs of residents, as these changed through time. The construction of aqueducts was part of a more organized effort to address the water needs of the Attica basin area since prehistoric times. A key step in developing the city’s water infrastructure took place during the Roman occupation of Athens when the Hadrianic aqueduct and the Hadrianic reservoir were built. Construction began in 125 AD and was completed in 140 AD The Hadrianic was underground with natural flow requiring a small and continuous slope along the aqueduct. Wells, communicated through the aqueduct, were placed at regular intervals. The main branch of the aqueduct - the central part of the Hadrianic, consists of the main tunnel, approximately 20 Km which starts from the foot of Mount Parnitha in the Olympic Village and ends up in the reservoir of Lycabettus, exploiting the water sources of Parnitha, Penteli and the Kifissos River. Gravity collected water from the water sources in the main tunnel and there was also the contribution of smaller aqueducts along the route. -
Selected Land Opportunities About Us
Selected Land Opportunities About us holds a wide range of properties available for sale and for rent across Greece and Cyprus in most asset classes. Our dedicated transaction professionals are available to provide additional information on all of the properties being marketed and ready to support you throughout the process from your first inquiry through to sale completion. Athens Office Thessaloniki Office 7, Stadiou Str. 1st & 4th Floor Ptolemaion 11, 1st Floor 10562, Athens, Greece 54630, Thessaloniki, Greece +30 216 800 1799 +30 231 053 3678 www.delfiproperties.gr www.delfiproperties.gr [email protected] [email protected] Information contained in our published works have been obtained from sources believed to be reliable at the time of publication. However, we do not guarantee the accuracy or completeness of any information published herein and shall not be held responsible for any changes, errors, omissions, or claims for damages arising out of use, inability to use, or with regard to the accuracy or sufficiency of the information contained in this publication. 2 Land Plot, Sifnos €500,000 NOT SUBJECT TO VAT DP01996/ELP_080 https://bit.ly/2G4ZaB2 The asset is an amazing land of 6424 sq.m. located in Sifnos, Cyclades in a unique spot which offes spectacular views to the Aegen sea. Also it is only a 10 minute walking distance from Chrisopigi beach. A property up to 230 sq.m. can be built in Coverage Density this plot. - - Zone Land Area Touristic 6424 m² Beach Front Land Plot, Patmos €750,000 NOT SUBJECT TO VAT DP02020/APV142 https://bit.ly/2HEniLq The buildings that can be constructed are as follows: 1.Land plot 2.010,00sq.m., within the planning zone of Skala Patmos, can build up to 400,00sq.m. -
Spatial Correlation Between Interferometric Stacking Pattern Deformation and Damage Distribution of Athens 7-9-99 Earthquake and Its Seismic Sequence
SPATIAL CORRELATION BETWEEN INTERFEROMETRIC STACKING PATTERN DEFORMATION AND DAMAGE DISTRIBUTION OF ATHENS 7-9-99 EARTHQUAKE AND ITS SEISMIC SEQUENCE M. Foumelis a , D. Raucoules b, Is. Parcharidis c *, D. Feurer b, S. Le Mouelic b, C. King b., C. Carnec b, E. Lagios a a ITU, National Kapodistrian University of Athens, Department of Geophysics & Geothermics, Laboratory of Geophysics, Space Applications Research Unit in Geosciences, Panepistimiopolis - Ilissia, 157 84 Athens, Greece b BRGM, 117 avenue de Luminy, 13276 Marseille cedex 09 – France c Harokopio University, , Faculty of Geography, El. Venizelou 70, 176 71 Athens, Greece KEY WORDS: Earthquake, Urban Area, Ground Deformation, Interferometry, GPS, GIS, Athens ABSTRACT: The study presents an attempt to correlate the spatial distribution of damages and the ground deformation measure by SAR interferometric stacking technique in the case of Athens 7-9-99 earthquake. Damage maps were created for building collapsed and affected areas, built in a GIS environment. The location of the collapsed building was identified using a portable GPS resever and introduced as point thematic map in the GIS. The interferometric images show a clear deformation pattern of fringes mainly in the Thriassio Pedion basin as well as in Athens basin. Comparing the damage maps with the pattern deformation of the interferometric image in the GIS it appears that there in not a clear correlation between the amplitude of deformation and the observed damages. Other parameters seems to affect the distribution of damages the most importannt of which should be the local geological conditions and the vulnerability of the buildings . 1. INTRODUCTION geographic variability and arrangement both on macro and microscale and the parametters that control the damage Athens basin constitutes the most populated basin of Greece distribution were alpine and post-alpine macrostructure, the with the cities of Athens and Pireaus. -
The Athens Earthquake (7 September 1999): Intensity Distribution and Controlling Factors
Engineering Geology 59 (2001) 297±311 www.elsevier.nl/locate/enggeo The Athens earthquake (7 September 1999): intensity distribution and controlling factors E. Lekkas* Department of Geology, University of Athens, Panepistimioupoli Zografou, 15784 Athens, Greece Received 20 June 2000; accepted for publication 14 December 2000 Abstract The Athens earthquake, Ms 5:9, that occurred on 7th September 1999 with epicenter located at the southern ¯ank of Mount Parnitha (Greece, Attiki) according to instrumental data, is attributed to the reactivation of an ESE±WNW south- dipping fault without sur®cial expression. The earthquake caused a large number of casualties and extensive damage within an extended area. Damage displayed signi®cant differentiation from place to place, as well as a peculiar geographic distribution. Based on geological, tectonic and morphological characteristics of the affected area and on the elaboration of damage recordings for intensity evaluation, it can be safely suggested that intensity distribution was the result of the combination of a number of parameters both on macro and microscale. On the macroscale, the parameters are the strike of the seismogenic fault, seismic wave directivity effects and to an old NNE±SSW tectonic structure, and they are also responsible for the maximum intensity arrangement in two perpendicular directions ESE±WNW and NNE±SSW. On the microscale, site foundation formations, old tectonic structures buried under recent formations and morphology are the parameters that differentiated intensities within the affected area. q 2001 Elsevier Science B.V. All rights reserved. Keywords: Athens; Earthquake; Intensity; Distribution; Tectonics; Fault 1. Introduction collapsed, including industrial installations, causing 140 deaths. The strongly affected area is inhabited On September 7, 1999 at 14:56 local time (11:56 by about 1 million people, 10% of whom are GMT), the City of Athens was rocked by an earth- estimated to be homeless. -
Rituals of Death and Dying in Modern and Ancient Greece
Rituals of Death and Dying in Modern and Ancient Greece Rituals of Death and Dying in Modern and Ancient Greece: Writing History from a Female Perspective By Evy Johanne Håland Rituals of Death and Dying in Modern and Ancient Greece: Writing History from a Female Perspective, by Evy Johanne Håland This book first published 2014 Cambridge Scholars Publishing 12 Back Chapman Street, Newcastle upon Tyne, NE6 2XX, UK British Library Cataloguing in Publication Data A catalogue record for this book is available from the British Library Copyright © 2014 by Evy Johanne Håland All rights for this book reserved. No part of this book may be reproduced, stored in a retrieval system, or transmitted, in any form or by any means, electronic, mechanical, photocopying, recording or otherwise, without the prior permission of the copyright owner. ISBN (10): 1-4438-6127-8, ISBN (13): 978-1-4438-6127-4 TABLE OF CONTENTS List of Figures........................................................................................... viii A Note on Transliteration ......................................................................... xiii Acknowledgements ................................................................................... xv Introduction ................................................................................................. 1 Chapter One ................................................................................................. 6 Death Rituals and the Cult of the Dead in Greece From death in general to Greek women and death in particular -
The Fault That Caused the Athens September 1999 Ms = 5.9 Earthquake: Field Observations
Natural Hazards 27: 61–84, 2002. 61 © 2002 Kluwer Academic Publishers. Printed in the Netherlands. The Fault that Caused the Athens September 1999 Ms = 5.9 Earthquake: Field Observations S. B. PAVLIDES1, G. PAPADOPOULOS2 and A. GANAS2 1Department of Geology, University of Thessaloniki, 54006, Greece E-mail: [email protected]; 2Geodynamics Institute, National Observatory of Athens, PO Box 20048, 11810 Athens, Greece Received: 18 October 2000; accepted in revised form: 5 November 2001 Abstract. On 7 September 1999 the Athens Metropolitan area (Greece) was hit by a moderate size (Ms = 5.9) earthquake. The severely damaged area is localized in the northwestern suburbs of the ◦ ◦ city, at the foothills of Mt. Parnitha (38.1 N, 23.6 E), about 18 km from the historic centre of Athens. In this paper, we present our results on the surface expression of the seismogenic structure. Methods applied were: field observations, geological mapping, fault geometry and kinematics, evaluation of macroseismic data, interpretation of LANDSAT images, construction of a DEM and application of shading techniques. Aftershock distribution and fault plane solutions were also considered. Our results suggest that the earthquake source is located within the NW-SE trending valley bearing a few outcrops of Neogene- Quaternary sediments across the south foothills of Mt. Parnitha, never known in the past to have been activated by such strong earthquakes. The earthquake occurred along ◦ ◦ ◦ ◦ a 10 km long normal fault, striking N110 –133 and dipping 64 –85 SW, extending from the Fili Fort (4th century BC) in the NNW to the Fili town and then to Ano Liossia, to the SSE. -
Gek Terna Societe Anonyme Holdings Real Estate Constructions
GEK TERNA SOCIETE ANONYME HOLDINGS REAL ESTATE CONSTRUCTIONS 85 Mesogeion Ave., 115 26 Athens Greece General Commercial Registry No. 253001000 (former S.A. Reg. No. 6044/06/Β/86/142) ANNUAL FINANCIAL REPORT for the period 1 January to 31 December 2017 In accordance with article 4 of L. 3556/2007 and the relevant executive Decisions by the Board of Directors of the Hellenic Capital Market Commission GEK TERNA GROUP Annual Financial Statements of the financial year 1 January 2017 - 31 December 2017 (Amounts in thousands Euro, unless otherwise stated) CONTENTS I. STATEMENTS BY MEMBERS OF THE BOARD OF DIRECTORS .............................................. 4 II. INDEPENDENT AUDITOR'S REPORT .................................................................................. 5 III. REPORT ON SEPARATE AND CONSOLIDATED FINANCIAL STATEMENTS .............................. 5 IV. ANNUAL REPORT OF THE BOARD OF DIRECTORS FOR THE FINANCIAL YEAR 2017 ............ 12 V. ANNUAL FINANCIAL STATEMENTS SEPARATE AND CONSOLIDATED OF 31 DECEMBER 2017 (1 JANUARY - 31 DECEMBER 2017) ........................................................................................ 51 STATEMENT OF FINANCIAL POSITION.................................................................................... 52 STATEMENT OF COMPREHENSIVE INCOME ........................................................................... 54 STATEMENT OF CASH FLOWS ................................................................................................ 56 STATEMENT OF CHANGES IN EQUITY ................................................................................... -
33 Tectonic Structure F Central-Western Attica.Pdf
Δελτίο της Ελληνικής Γεωλογικής Εταιρίας τομ. XXXX, Bulletin of the Geological Society of Greece vol. XXXX, 2007 2007 Proceedings of the 11th International Congress, Athens, May, Πρακτικά 11ου Διεθνούς Συνεδρίου, Αθήνα, Μάιος 2007 2007 TECTONIC STRUCTURE OF CENTRAL-WESTERN ATTICA (GREECE) BASED ON GEOPHYSICAL INVESTIGATIONS-PRELIMINARY RESULTS Papadopoulos T.D.1, Goulty N.2, Voulgaris N. S. 1, Alexopoulos J.D.1, Fountoulis I. 1, Kambouris P.1, Karastathis V. 3, Peirce C. 2, Chailas S.1, Kassaras J. 1, Pirli M.1, Goumas G.1 & Lagios E. 1 1 National and Kapodistrian University of Athens, Faculty of Geology and Geoenvironment, 15784 Zografou, GREECE 2 University of Durham, Department of Geological Sciences, UK 3 National Observatory of Athens, Geodynamic Institute, 118 10 Athens, GREECE Abstract In an effort to investigate the deep geological structure in the broader area of cen- tral-western Attica, that suffered severe damage during the destructive Athens earth- quake of September 7th, 1999, the Department of Geophysics-Geothermics of the Faculty of Geology and Geoenvironment of Athens University, in collaboration with the Geodynamic Institute of National Observatory of Athens and the Department of Geological Sciences of Durham University, carried out a combined geophysical survey. For the first time in Attica, seismic and gravity geophysical methods were applied along profiles, in such an extensive scale. Within the framework of this investigation the following tasks were accomplished: a) Three (3) seismic lines of about 30 kilometres of total length, two (2) in the area of Thriassion plain and one (1) along the Parnitha-Krioneri-Drosia-Ekali-Dionysos axis (Attica plain) and b) 338 gravity measurements distributed along eight (8) gravity profiles, four (4) of which in Thriassion plain, three (3) in Petroupoli-Aharnes-Thrakomakedones region (Attica plain) and one (1) along Parnitha-Krioneri-Drosia-Ekali-Dionysos axis (At- tica plain). -
Visa & Residence Permit Guide for Students
Ministry of Interior & Administrative Reconstruction Ministry of Foreign Affairs Directorate General for Citizenship & C GEN. DIRECTORATE FOR EUROPEAN AFFAIRS Immigration Policy C4 Directorate Justice, Home Affairs & Directorate for Immigration Policy Schengen Email: [email protected] Email: [email protected] www.ypes.gr www.mfa.gr Visa & Residence Permit guide for students 1 Index 1. EU/EEA Nationals 2. Non EU/EEA Nationals 2.a Mobility of Non EU/EEA Students - Moving between EU countries during my short-term visit – less than three months - Moving between EU countries during my long-term stay – more than three months 2.b Short courses in Greek Universities, not exceeding three months. 2.c Admission for studies in Greek Universities or for participation in exchange programs, under bilateral agreements or in projects funded by the European Union i.e “ERASMUS + (placement)” program for long-term stay (more than three months). - Studies in Greek universities (undergraduate, master and doctoral level - Participation in exchange programs, under interstate agreements, in cooperation projects funded by the European Union including «ERASMUS+ placement program» 3. Refusal of a National Visa (type D)/Rights of the applicant. 4. Right to appeal against the decision of the Consular Authority 5. Annex I - Application form for National Visa (sample) Annex II - Application form for Residence Permit Annex III - Refusal Form Annex IV - Photo specifications for a national visa application Annex V - Aliens and Immigration Departments Contacts 2 1. Students EU/EEA Nationals You will not require a visa for studies to enter Greece if you possess a valid passport from an EU Member State, Iceland, Liechtenstein, Norway or Switzerland. -
GR-Acharnes: Summary of Statute of Association of the European
OJ/S S183 22/09/2012 Member states - Not applicable - European company - Not applicable 1/3 299402-2012-EN This notice in TED website: http://ted.europa.eu/udl?uri=TED:NOTICE:299402-2012:TEXT:EN:HTML GR-Acharnes: Summary of Statute of Association of the European Grouping of Territorial Cooperation (E.G.T.C.) in the form of an Urban Non Profit Enterprise under the name "E.G.T.C. EFXINI POLI - Network of European Cities for Sustainable Development" with the distinguished title "EGTC Efxini Poli - SolidarCity Network" 2012/S 183-299402 According to the 30635/02-08-2012 (FEK 2307/6-8-2012) decision of the Minister of Internal Affairs of Greece and was published at the Protodikio Athinon (Athens Courts of Justice) with the General Number 132/2012/28-08-2012, and under the regulation EC 1082/2006, the establishment of the E.G.T.C. EFXINI POLI - NETWORK OF EUROPEAN CITIES FOR SUSTAINABLE DEVELOPMENT was approved, with the following identification. NAME: "E.G.T.C. EFXINI POLI - NETWORK OF EUROPEAN CITIES FOR SUSTAINABLE DEVELOPMENT" with the distinguished title "EGTC – Efxini Poli - SolidarCity NETWORK" HEAD OFFICE: As head office of the "E.G.T.C. EFXINI POLI - SOLIDARCITY NETWORK", is defined the Municipality of Acharnes Attica, Address: 60 Thessalias St., 13674Acharnes, Attica Greece, Tel. ++30 2102486041(1)45, Fax. ++30 2102486046, e- mail: [email protected], www.efxini.gr MISSION: 1. The main mission of the E.G.T.C. EFXINI POLI - SOLIDARCITY NETWORK is the living of all the people of the European Union in an environment of permanent peace and sustainable development, economically efficient, socially just and environmentally sustainable, with cohesion and safety of their regions.