Correlation of Structural Seismic Damage with Fundamental Period of RC Buildings
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Some Attic Walls Author(S): Merle K
Some Attic Walls Author(s): Merle K. Langdon Source: Hesperia Supplements, Vol. 19, Studies in Attic Epigraphy, History and Topography. Presented to Eugene Vanderpool (1982), pp. 88-98+215-219 Published by: The American School of Classical Studies at Athens Stable URL: http://www.jstor.org/stable/1353974 . Accessed: 04/09/2013 21:21 Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at . http://www.jstor.org/page/info/about/policies/terms.jsp . JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range of content in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new forms of scholarship. For more information about JSTOR, please contact [email protected]. The American School of Classical Studies at Athens is collaborating with JSTOR to digitize, preserve and extend access to Hesperia Supplements. http://www.jstor.org This content downloaded from 63.110.229.170 on Wed, 4 Sep 2013 21:21:44 PM All use subject to JSTOR Terms and Conditions SOMEATTIC WALLS (PLATES7-11) "The Attic landscape ... possesses an aris- tocraticgrace and ease: the frugal, arid land, the gracefulcurves of Hymettos and Penteli- kon, the silver-leaved olive trees, the slen- der ascetic cypresses, the playful glare of rocks in the sun, and above all the buoyant diaphanous,completely spiritual light which dresses and undressesall things." N. Kazantzakis,Report to Greco F ROMTHE THRIASIAN PLAIN on the west to the gulf of Euboiaon the east the landwardborders of Atticawere guardedby impressivefortifications in antiquity. -
Psomopoulos, C.S
CONSTANTINOS S. PSOMOPOULOS Assistant Professor T.E.I. Piraeus 1. PERSONAL INFORMATION Name CONSTANTINOS S. PSOMOPOULOS Address 250, Thivon St., Aigaleo, GR-12244, ATHENS, GREECE Telephone +30-2105381182, +30-6974509948 Fax +30-2105381321 E-mail [email protected] , [email protected] Marital Status Married, 1 child Nationality Hellenic Date of birth 16/ 07/1973 2. EDUCATION AND TRAINING • 1998-2002 National Technical University of Athens, School of Electrical and Computer Engineering Ph.D. on Electrical and Computer Engineering • 1992-1997 National Technical University of Athens, School of Electrical and Computer Engineering Diploma on Electrical and Computer Engineering 3. WORK EXPERIENCE •4/10/2007-today TEI of Piraeus - Electrical Engineering Department Assistant Professor - Courses: Electric Power Systems I (Power Generation and Energy Economics) High Voltage Engineering Special Issues in High Voltage Engineering High Voltage Laboratory Electric Measurements - Head of High Voltage Laboratory - Head of the Electric Power Division of the Electrical Engineering Department - Member of Electrical Engineering Department Council - Head of environmental and recycling policies of Electrical Engineering Department • 05/2007-2009 NRG-Orion-Thomas Matopoulos SA (Energy saving & Photovoltaic’s) Consultant in issues regarding - Design, construct and installation of customized electrical – electronic components for Energy Saving Systems in industry - Overvoltage protection systems for photovoltaic parks - Earthing systems • 2003-2007 EPTA Ltd (Environmental -
The Government of Greece Cycle 2009
25/05/09 RAP/Cha/GR/XIX(2009) EUROPEAN SOCIAL CHARTER 19th report on the implementation of the European Social Charter and 5th report on the implementation of the 1988 Additional Protocol submitted by THE GOVERNMENT OF GREECE (Articles 3, 12 and 13 for the period 01/01/2005 – 31/12/2007; Articles 11, 14 and Article 4 of the Additional Protocol for the period 01/01/2003 – 31/12/2007) _________ Report registered at the Secretariat on 19/05/2009 CYCLE 2009 EUROPEAN SOCIAL CHARTER 19th GREEK REPORT ARTICLES 3, 11, 12, 13, 14 AND 4 OF THE ADDITIONAL PROTOCOL Reference period 2005-2007 (for articles 3, 12, 13) 2003-2007 (for articles 11, 14, 4) ATHENS MAY 2009 Table of Contents Article 3 The right to safe and healthy working conditions.....................................4 Paragraph 1 .............................................................. 4 Paragraph 2 .............................................................14 Paragraph 3 .............................................................19 Article 11 The right to protection of health.............................................................20 Paragraph 1 .............................................................20 Paragraph 2 .............................................................34 Paragraph 3 .............................................................39 Article 12 The right to social secutity.......................................................................62 Paragraph 1 .............................................................62 Paragraph 2 .............................................................70 -
A Hydrogeotechnical Integrated System for Water Resources 3 Management of Attica – Greece
A Hydrog eotechnical Integrated System for Water Resources Management of Attica – Greece Dr. Costas Sachpazis , M.Sc., Ph.D. Associate Professor, Department of Geotechnology and Environmental Engineering, Technological Educational Institute of West Macedonia, Koila 50100, Kozani, Greece. e-mail: [email protected] Dr. Odysseus Manoliadis, M.Sc., Ph.D. Associate Professor, Department of Geotechnology and Environmental Engineering, Technological Educational Institute of West Macedonia, Koila 50100, Kozani, Greece. e-mail: [email protected] Athina Baronos , M.Sc. , Ph.D. Candidate Senior Lecturer, Department of Industrial Engineering and Design, Technological Educati onal Institute of West Macedonia, Koila 50100, Kozani, Greece. e-mail: [email protected] Chrysanthy Tsapraili , M.Sc. Assisting Laboratory Lecturer, Faculty of Management and Economy, Technological Educationa l Institute of West Macedonia, Koila 50100, Kozani, Greece. e-mail: [email protected] Abstract : In this paper an information management system used in Attica Greece that combines modeling with the integrated management of water, sewerage and storm water infrastructure is presented. From this information management system there are proposed certain public works that are grouped in two categories, i.e. works that are needed for the entire Attica district and have a general character for the whole region (1 st category works) and then, works that are specifically needed for every particular and individual municipality (2 nd category works). The first category consists of: Collection and Treatment of the Used Water Works, and Reuse of at least a portion of the Treated Wastewater Works, and the second category consists of: Flood Protection through Stormwater Storage Works, Artificial Recharge of Groundwater Aquifers Works, 1 2 Dr. -
Examples of Manuscript Components and Description of Electronic
Proceedin gs Third UJNR Workshop on Soil-Structure Interaction, March 29-30, 2004, Menlo Park, California, USA. Strong Motion Site Effects in the Athens, 1999 Earthquake Dominic Assimaki,a) and Eduardo Kausel b) During the 1999 Athens Earthquake, the town of Adàmes, located on the eastern side of the Kifissos river canyon, experienced unexpectedly heavy damage. Despite the significant amplification potential of the slope geometry, topography effects cannot alone explain the uneven damage distribution within a 300m zone behind the crest, characterized by a rather uniform structural quality. This paper illustrates the important role of soil stratigraphy, material heterogeneity and soil-structure interaction on the formulation of surface ground motion. For this purpose, we first perform elastic two-dimensional wave propagation analyses based on available local geotechnical and seismological data, and validate our results by comparison with aftershock recordings. Next, we conduct nonlinear time-domain simulations that include spatial variability of soil properties and soil-structure interaction effects, to reveal their additive contribution in the topographic motion aggravation. INTRODUCTION It has been long recognized that topography can significantly affect the amplitude and frequency characteristics of ground motion during seismic events. In the recent past, documented observations from destructive seismic events show that buildings located at the tops of hills, ridges and canyons, suffer more intense damage than those located at the base: -
Greece) Michael Foumelis1,*, Ioannis Fountoulis2, Ioannis D
ANNALS OF GEOPHYSICS, 56, 6, 2013, S0674; doi:10.4401/ag-6238 Special Issue: Earthquake geology Geodetic evidence for passive control of a major Miocene tectonic boundary on the contemporary deformation field of Athens (Greece) Michael Foumelis1,*, Ioannis Fountoulis2, Ioannis D. Papanikolaou3, Dimitrios Papanikolaou2 1 European Space Agency (ESA-ESRIN), Frascati (Rome), Italy 2 National and Kapodistrian University of Athens, Department of Dynamics Tectonics and Applied Geology, Athens, Greece 3 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 May 20, 2013. Subject classification: Satellite geodesy, Crustal deformations, Geodynamics, Tectonics, Measurements and monitoring. ABSTRACT while there are sufficient data for the period after 1810 A GPS-derived velocity field is presented from a dense geodetic network [Ambraseys and Jackson 1990]. Reports on damage and (~5km distance between stations) established in the broader area of displacement of ancient monuments [Papanastassiou Athens. It shows significant local variations of strain rates across a major et al. 2000, Ambraseys and Psycharis 2012] suggest in inactive tectonic boundary separating metamorphic and non-metamor- turns that Attica region has experienced several strong phic geotectonic units. The southeastern part of Athens plain displays earthquakes in the past. It is interesting that despite the negligible deformation rates, whereas towards the northwestern part unexpected catastrophic seismic event of September 7, higher strain rates are observed, indicating the control of the inactive tec- 1999, Mw=6.0 [Papadimitriou et al. 2002], no further tonic boundary on the contemporary deformation field of the region. monitoring of the region was held. -
Networking UNDERGROUND Archaeological and Cultural Sites: the CASE of the Athens Metro
ing”. Indeed, since that time, the archaeological NETWORKING UNDERGROUND treasures found in other underground spaces are very often displayed in situ and in continu- ARCHAEOLOGICAL AND ity with the cultural and archaeological spaces of the surface (e.g. in the building of the Central CULTURAL SITES: THE CASE Bank of Greece). In this context, the present paper presents OF THE ATHENS METRO the case of the Athens Metro and the way that this common use of the underground space can have an alternative, more sophisticated use, Marilena Papageorgiou which can also serve to enhance the city’s iden- tity. Furthermore, the case aims to discuss the challenges for Greek urban planners regarding the way that the underground space of Greece, so rich in archaeological artifacts, can become part of an integrated and holistic spatial plan- INTRODUCTION: THE USE OF UNDERGROUND SPACE IN GREECE ning process. Greece is a country that doesn’t have a very long tradition either in building high ATHENS IN LAYERS or in using its underground space for city development – and/or other – purposes. In fact, in Greece, every construction activity that requires digging, boring or tun- Key issues for the Athens neling (public works, private building construction etc) is likely to encounter an- Metropolitan Area tiquities even at a shallow depth. Usually, when that occurs, the archaeological 1 · Central Athens 5 · Piraeus authorities of the Ministry of Culture – in accordance with the Greek Archaeologi- Since 1833, Athens has been the capital city of 2 · South Athens 6 · Islands 3 · North Athens 7 · East Attica 54 cal Law 3028 - immediately stop the work and start to survey the area of interest. -
UN/LOCODE) for Greece
United Nations Code for Trade and Transport Locations (UN/LOCODE) for Greece N.B. To check the official, current database of UN/LOCODEs see: https://www.unece.org/cefact/locode/service/location.html UN/LOCODE Location Name State Functionality Status Coordinatesi GR 2NR Neon Rysion 54 Road terminal; Recognised location 4029N 02259E GR 5ZE Zervochórion 32 Road terminal; Recognised location 3924N 02033E GR 6TL Lití 54 Road terminal; Recognised location 4044N 02258E GR 9OP Dhílesi 03 Road terminal; Recognised location 3821N 02340E GR A8A Anixi A1 Road terminal; Recognised location 3808N 02352E GR AAI Ágioi Anárgyroi 31 Multimodal function, ICD etc.; Recognised location 3908N 02101E GR AAR Acharnes A1 Multimodal function, ICD etc.; Recognised location 3805N 02344E GR AAS Ágios Athanásios 54 Road terminal; Recognised location 4043N 02243E GR ABD Abdera 72 Road terminal; Recognised location 4056N 02458E GR ABO Ambelókipoi Road terminal; Recognised location 4028N 02118E GR ACH Akharnaí A1 Rail terminal; Road terminal; Approved by national 3805N 02344E government agency GR ACL Achladi Port; Code adopted by IATA or ECLAC 3853N 02249E GR ADA Amaliada 14 Road terminal; Recognised location 3748N 02121E GR ADI Livádia 31 Road terminal; Recognised location 3925N 02106E GR ADK Ano Diakopto 13 Road terminal; Recognised location 3808N 02214E GR ADL Adamas Milos 82 Port; Request under consideration 3643N 02426E GR ADO Áhdendron 54 Rail terminal; Road terminal; Recognised location 4040N 02236E GR AEF Agia Efimia Port; Code adopted by IATA or ECLAC 3818N -
Vassilis Arapoglou,* Thomas Maloutas**
The Greek Review of Social Research, special issue 136 C´, 2011, 135-155 Vassilis Arapoglou,* Thomas Maloutas** SEGREGATION, INEQUALITY AND MARGINALITY IN CONTEXT: THE CASE OF ATHENS ABSTRACT This paper focuses on the contextual factors that shape the dynamics and the patterns of segregation in Athens. Migration and changes in the ethnic composition of the working class have not produced more segregation and widespread marginality, because employment opportunities and affordable housing were available in socially mixed areas. Attention, is drawn, however, to the dynamics of social polarization, the concentration of housing inequality and deprivation which have been reshaping the social map of the city since the 1990s. The suburbanization of higher social categories has been enhancing isolation of wealthy enclaves in the east and in parts of the centre. The indigenous working class population on the western periphery has become socially and spatially entrapped. At the same time a deprived and ethnically diverse population, has been concentrating in central, north-western and south-western districts. Keywords: segregation, immigration, ethnic segregation, Athens 1. INTRODUCTION: SEGREGATION IN THE INTERNATIONAL LITERATURE The definition of segregation is simple according to human geography dic- tionaries (Johnston et al., 1986: 424) and seems to have a general, inter- contextual, applicability (“The residential separation of subgroups within a wider population”). This simple metaphor from genetics, that subsequently *Assistant Professor of Sociology, University of Crete, Greece. ** Professor of Social Geography, Ηarokopio University, Greece. 136 VASSILIS ARAPOGLOU, THOMAS MALOUTAS became the dominant meaning of the term, owed its success to the fact that it reflected the conditions of the booming American metropolis of the first half of the 20th century. -
Stiff Soil Amplification Effects in the 7 September 1999 Athens (Greece)
Soil Dynamics and Earthquake Engineering 21 2001) 671±687 www.elsevier.com/locate/soildyn Stiff soil ampli®cation effects in the 7 September 1999 Athens Greece) earthquake G.D. Bouckovalas*, G.P. Kouretzis Geotechnical Division, Department of Civil Engineering, National Technical University of Athens, Patission 42, 10682 Athens, Greece Accepted 13 July 2001 Abstract The Athens, Greece, earthquake of 7 September 1999 provided a number of reliable strong motion recordings and well-de®ned patterns of damage at sites with known geological and geotechnical conditions. Joint evaluation of this evidence shows that the very stiff soils of the Athens basin, compared to the nearby outcropping soft rocks, have ampli®ed the peak horizontal acceleration by an average of 40% or more and have shifted elastic response spectra to higher periods. US and the European seismic code provisions NEHRP-97 and EC-8), place stiff soils and soft rocks at the same site category and consequently fail to predict these adverse effects. A larger number of site categories and new site coef®cients that depend on the seismic excitation frequency appear necessary in order to overcome this de®cit of the codes. q 2001 Elsevier Science Ltd. All rights reserved. Keywords: Athens earthquake; Site characterization; Seismic codes; Soil ampli®cation 1. Introduction speculation for rupture directivity and local site ampli®cation phenomena. On 7 September 1999 11:56:50.5 GMT) a violent earth- Following a brief seismological review, this paper quake of Ms 5.9 struck the western bounds of the greater presents results from a site-speci®c analysis of main-shock metropolitan area of Athens, at 18 km distance from the strong motion recordings and the on-going correlation of historical center. -
Generation 2.0 for Rights, Equality & Diversity
Generation 2.0 for Rights, Equality & Diversity Intercultural Mediation, Interpreting and Consultation Services in Decentralised Administration Immigration Office Athens A (IO A) January 2014 - now On 1st January 2014, the One Stop Shop was launched and all the services issuing and renewing residence permits for immigrants in Greece were moved from the municipalities to Decentralised Administrations. Namely, the 66 Attica municipalities were shared between 4 Immigration Offices of the Attic Decentralised Administration. a) Immigration Office for Athens A with territorial jurisdiction over residents of the Municipality of Athens, Address: Salaminias 2 & Petrou Ralli, Athens 118 55 b) Immigration Office for Central Athens and West Attica, with territorial jurisdiction over residents of the following Municipalities; i) Central Athens: Filadelfeia-Chalkidona, Galatsi, Zografou, Kaisariani, Vyronas, Ilioupoli, Dafni-Ymittos, ii) West Athens: Aigaleo Peristeri, Petroupoli, Chaidari, Agia Varvara, Ilion, Agioi Anargyroi- Kamatero, and iii) West Attica: Aspropyrgos, Eleusis (Eleusis-Magoula) Mandra- Eidyllia (Mandra - Vilia - Oinoi - Erythres), Megara (Megara-Nea Peramos), Fyli (Ano Liosia - Fyli - Zefyri). Address: Salaminias 2 & Petrou Ralli, Athens 118 55 c) Immigration Office for North Athens and East Attica with territorial jurisdiction over residents of the following Municipalities; i) North Athens: Penteli, Kifisia-Nea Erythraia, Metamorfosi, Lykovrysi-Pefki, Amarousio, Fiothei-Psychiko, Papagou- Cholargos, Irakleio, Nea Ionia, Vrilissia, -
Assessment of Seismic Risk for Museum Artifacts 1 2 3 C.C
th The 14 World Conference on Earthquake Engineering October 12-17, 2008, Beijing, China ASSESSMENT OF SEISMIC RISK FOR MUSEUM ARTIFACTS 1 2 3 C.C. Spyrakos , Ch.A. Maniatakis and I.M. Taflampas 1 Professor, Dept. of Civil Engineering, Laboratory for Earthquake Engineering National Technical University, Athens, Greece 2 Civil Engineer, PhD Candidate, Dept. of Civil Engineering, Laboratory for Earthquake Engineering National Technical University, Athens, Greece 3 Civil Engineer, Dept. of Civil Engineering, Laboratory for Earthquake Engineering National Technical University, Athens, Greece Email: [email protected], [email protected], [email protected] ABSTRACT: The protection of several types of museum collections against seismic hazard is increasingly gaining the interest of scientists and governments, as their damage is in many cases irreparable. Special programs of earthquake preparedness are conducted in order to mitigate the expected hazard, especially for earthquake - prone countries, such as the countries of eastern Mediterranean. In this study several types of art object failures caused by earthquakes are presented and risk mitigation methods are described. The magnitudes of Peak Ground Acceleration (PGA) and Peak Ground Velocity (PGV) that can cause failure are determined for a sample of representative artifacts applying suitable criteria. Several earthquakes are considered to determine the distance from the causative fault at which failure is expected using appropriate attenuation relationships and theoretical models for both near- and far-fault regions. KEYWORDS: museum artifacts, seismic risk, failure criteria, attenuation relationships, near-far fault regions 1. INTRODUCTION 1.1 Seismicity in Greece The eastern Mediterranean Sea including Italy, Balkan countries, Cyprus and Turkey is well known for the noteworthy history of the native civilizations.