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Verification of Vulnerable Zones Identified Under the Nitrate Directive \ and Sensitive Areas Identified Under the Urban Waste W
CONTENTS 1 INTRODUCTION 1 1.1 THE URBAN WASTEWATER TREATMENT DIRECTIVE (91/271/EEC) 1 1.2 THE NITRATES DIRECTIVE (91/676/EEC) 3 1.3 APPROACH AND METHODOLOGY 4 2 THE OFFICIAL GREEK DESIGNATION PROCESS 9 2.1 OVERVIEW OF THE CURRENT SITUATION IN GREECE 9 2.2 OFFICIAL DESIGNATION OF SENSITIVE AREAS 10 2.3 OFFICIAL DESIGNATION OF VULNERABLE ZONES 14 1 INTRODUCTION This report is a review of the areas designated as Sensitive Areas in conformity with the Urban Waste Water Treatment Directive 91/271/EEC and Vulnerable Zones in conformity with the Nitrates Directive 91/676/EEC in Greece. The review also includes suggestions for further areas that should be designated within the scope of these two Directives. Although the two Directives have different objectives, the areas designated as sensitive or vulnerable are reviewed simultaneously because of the similarities in the designation process. The investigations will focus upon: • Checking that those waters that should be identified according to either Directive have been; • in the case of the Nitrates Directive, assessing whether vulnerable zones have been designated correctly and comprehensively. The identification of vulnerable zones and sensitive areas in relation to the Nitrates Directive and Urban Waste Water Treatment Directive is carried out according to both common and specific criteria, as these are specified in the two Directives. 1.1 THE URBAN WASTEWATER TREATMENT DIRECTIVE (91/271/EEC) The Directive concerns the collection, treatment and discharge of urban wastewater as well as biodegradable wastewater from certain industrial sectors. The designation of sensitive areas is required by the Directive since, depending on the sensitivity of the receptor, treatment of a different level is necessary prior to discharge. -
Comparison of T1 FLAIR BLADE with and Without Parallel Imaging Against T1 Turbo Spin Echo in the MR Imaging of Lumbar Spine in the Sagittal Plane
Lavdas et al., J Radiat Res Imaging 2021; Journal of Radiation Research and 1(1):33-40. Imaging Research Article Comparison of T1 FLAIR BLADE with and without parallel imaging against T1 turbo spin echo in the MR imaging of lumbar spine in the sagittal plane Eleftherios Lavdas1,2, Eleonora Giankou3, Panos Papanikolaou4, Aleksandra Tsikrika5, Maria Papaioannou2, Violeta Roka6, Vasiliki Chatzigeorgiou3, Georgios Batsikas3, Spiros Kostopoulos7, Dimitrios Glotsos7, Athanasios Bakas1, Panayiotis Mavroidis8* 1University of West Attica, Department Abstract of Biomedical Sciences, Athens, Greece Purpose: Spinal cord and nerves are best visualized by MRI, which is able to show structural and functional 2Animus Kyanoys Stavros, Department anomalies of the spine. The primary objective of this study is to identify advantages or disadvantages of of Radiology, Larissa, Greece the T1-weighted fluid attenuated inversion recovery (FLAIR) sequence with BLADE technique (T1W-FLAIR BLADE), with and without parallel imaging when compared with T1 Turbo Spin Echo (T1 TSE) sequence 3Department of Medical Imaging, IASO Thessalias Hospital, Larissa, Greece when performing MRI examination of the lumbar spine in a sagittal view. 4Long School of Medicine, University Methods: L-spine examinations with T1W-FLAIR BLADE (with and without parallel imaging) and T1 TSE of Texas Health at San Antonio, San were acquired on 44 patients using a 1.5T scanner. These sequences were assessed by two radiologists Antonio, TX, USA a) quantitatively by comparing the signal-to-noise ratio (SNR), contrast-to-noise ratio (CNR) and relative contrast (ReCon) measurements and b) qualitatively based on different features of the images such as 5 Department of Radiology, University cerebrospinal fluid (CSF) nulling. -
Preliminary Results Regarding the Rock Falls of December 17, 2009 at Tempi, Greece
Bulletin of the Geological Soci- Δελτίο της Ελληνικής Γεωλογικής ety of Greece, 2010 Εταιρίας, 2010 Proceedings of the 12th Interna- Πρακτικά 12ου Διεθνούς Συνεδρί- tional Congress, Patras, May, ου, Πάτρα, Μάιος 2010 2010 PRELIMINARY RESULTS REGARDING THE ROCK FALLS OF DECEMBER 17, 2009 AT TEMPI, GREECE Christaras B.1, Papathanassiou G.1, Vouvalidis K.2, Pavlides S.1 1 Aristotle University of Thessaloniki, Department of Geology, 54124 Thessaloniki, Greece, [email protected], [email protected], [email protected] 2 Aristotle University of Thessaloniki, Department of Physical and Environmental Geography, 54124 Thessaloniki, Greece, [email protected] Abstract On December 17, 2009, a large size rock fall generated at the area of Tempi, Central Greece causing one casualty. In particular, a large block was detached from a high of 70 meters and started to roll downslope and gradually became a rock slide. About 120 tones of rock material moved downward to the road resulting to the close of the national road. Few days after the slope failure, a field survey organized by the Department of Geology, AUTH took place in order to evaluate the rock fall hazard in the area and to define the triggering causal factors. As an out- come, we concluded that the heavily broken rock mass and the heavy rain-falls, of the previous days, contribute significantly to the generation of the slope failure. The rocky slope was limited stable and the high joint water pressure caused the failure of the slope. Key words: rock fall, Tempi, engineering geology, hazard, Greece 1. Introduction A rock fall is a fragment of rock detached by sliding, toppling or falling that falls along a vertical or sub-vertical cliff, proceeds down slope by bouncing and flying along ballistic trajectories or by rolling on talus or debris slopes (Varnes, 1978). -
Grand Tour of Greece
Grand Tour of Greece Day 1: Monday - Depart USA Depart the USA to Greece. Your flight includes meals, drinks and in-flight entertainment for your journey. Day 2: Tuesday - Arrive in Athens Arrive and transfer to your hotel. Balance of the day at leisure. Day 3: Wednesday - Tour Athens Your morning tour of Athens includes visits to the Tomb of the Unknown Soldier, Panathenian Stadium, the ruins of the Temple of Zeus and the Acropolis. Enjoy the afternoon at leisure in Athens. Day 4: Thursday - Olympia CORINTH Canal (short stop). Drive to EPIDAURUS (visit the archaeological site and the theatre famous for its remarkable acoustics) and then on to NAUPLIA (short stop). Drive to MYCENAE where you visit the archaeological site, then depart for OLYMPIA, through the central Peloponnese area passing the cities of MEGALOPOLIS and TRIPOLIS arrive in OLYMPIA. Dinner & Overnight. Day 5: Friday – Delphi In the morning visit the archaeological site and the museum of OLYMPIA. Drive via PATRAS to RION, cross the channel to ANTIRION on the "state of the art" new suspended bridge considered to be the longest and most modern in Europe. Arrive in NAFPAKTOS, then continue to DELPHI.. Dinner & Overnight. Day 6: Saturday – Delphi In the morning visit the archaeological site and the museum of Delphi. Rest of the day at leisure. Dinner & Overnight in DELPHI. Day 6: Sunday – Kalambaka In the morning, start the drive by the central Greece towns of AMPHISSA, LAMIA and TRIKALA to KALAMBAKA. Afternoon visit of the breathtaking METEORA. Dinner & Overnight in KALAMBAKA. Day 7: Monday - Thessaloniki Drive by TRIKALA and LARISSA to the famous, sacred Macedonian town of DION (visit).Then continue to THESSALONIKI, the largest town in Northern Greece. -
(Selido ΤΟϜϟϣ 4
Δελτίο της Ελληνικής Γεωλογικής Εταιρίας, 2010 Bulletin of the Geological Society of Greece, 2010 Πρακτικά 12ου Διεθνούς Συνεδρίου Proceedings of the 12th International Congress Πάτρα, Μάιος 2010 Patras, May, 2010 GROUNDWATER QUALITY OF THE AG. PARASKEVI/TEMPI VALLEY KARSTIC SPRINGS - APPLICATION OF A TRACING TEST FOR RESEARCH OF THE MICROBIAL POLLUTIO (KATO OLYMPOS/NE THESSALY) Stamatis G. Agricultural University of Athens, Institute of Mineralogy-Geology, Iera Odos 75, GR-118 55 Athens, [email protected] . Abstract The study of the Kato Olympos karst system, based on the implementation of tracer tests and hydro- chemical analyses, is aimed at the investigation of surface-groundwater interaction, the delineation of the catchment area and the detection of the surface microbial source contamination of the Tempi karst springs. The study area is formed by intensively karstified carbonate rocks, metamorphic for- mations, Neogene sediments and Quaternary deposits. The significant karst aquifer discharges through karst springs in Tempi valley and in Pinios riverbed. The karst springs present important seasonal fluctuations in discharge rate, moderate mineralization with TDS between 562 to 630 mg/l + + - - and they belong to Ca-HCO3 water type. The inorganic pollution indicators, such as Na , K , Cl , NO3 + 3 , NH4 , PO4 , show low concentrations and do not reveal any surface influences. On the other hand, the presence of microbial parameters in karst springs proclaims the high rate of microbial contami- nation of karst aquifer. Tracer tests reveal hydraulic connection between the surface waters of Xirorema – Rapsani basin and the karst aquifer. The high values of groundwater flow velocity upwards of 200 m/h, show the good karstification rate of the carbonate formations and the cavy structure dom- inated in the study area, as well as the low self purification capability of the karst aquifer. -
Areas “Affected” by Malaria in Greece 2019 Season, May 2019
1 Areas “affected” by malaria in Greece 2019 season, May 2019 The “Working Group (WG) for the designation of areas affected by vector-borne diseases” of the National Committee for the Prevention and Control of Tropical Diseases of the Ministry of Health has convened and decided upon which areas should be designated as “affected”, following the recording of an introduced P.vivax malaria case (1st generation of transmission) in 2019. The WG of experts has carefully examined the following data: the total epidemiological data concerning malaria in Greece since 2009, the number and characteristics of all cases reported to the National Public Health Organization (N.P.H.O.) up to 24th May 2019, the characteristics of the population to which they correspond, and the geomorphological characteristics of the corresponding areas, the available entomological data for the years 2011-2019, especially for the area with the introduced case, and the literature concerning the flight range of mosquito vectors, especially Anopheles sacharovi, which is considered to be the main malaria vector in our country. According to the suggestion of European experts, an “affected area” is defined as falling within a radius of 2-6 km around the probable place of exposure of the locally acquired cases. In Greece, an affected area is usually defined by a radius of 6 km around the probable place of exposure. However, if this defined circle includes sections of large urban centres or cities (that cannot be easily divided) or if a smaller radius is deemed adequate (e.g. based on entomological data, history of cases in an area, geomorphology, etc.), the WG - following risk assessment – decides upon the exact designation of the affected area. -
DKV Stations, Sorted by City
You drive, we care. GR - Diesel & Services Griechenland / Ellás / Greece Sortiert nach Ort Sorted by city » For help, call me! DKV ASSIST - 24h International Free Call* 00800 365 24 365 In case of difficulties concerning the number 00800 please dial the relevant emergency number of the country: Bei unerwarteten Schwierigkeiten mit der Rufnummer 00800, wählen Sie bitte die Notrufnummer des Landes: Andorra / Andorra Latvia / Lettland » +34 934 6311 81 » +370 5249 1109 Austria / Österreich Liechtenstein / Liechtenstein » +43 362 2723 03 » +39 047 2275 160 Belarus / Weißrussland Lithuania / Litauen » 8 820 0071 0365 (national) » +370 5249 1109 » +7 495 1815 306 Luxembourg / Luxemburg Belgium / Belgien » +32 112 5221 1 » +32 112 5221 1 North Macedonia / Nordmazedonien Bosnia-Herzegovina / Bosnien-Herzegowina » +386 2616 5826 » +386 2616 5826 Moldova / Moldawien Bulgaria / Bulgarien » +386 2616 5826 » +359 2804 3805 Montenegro / Montenegro Croatia / Kroatien » +386 2616 5826 » +386 2616 5826 Netherlands / Niederlande Czech Republic / Tschechische Republik » +49 221 8277 9234 » +420 2215 8665 5 Norway / Norwegen Denmark / Dänemark » +47 221 0170 0 » +45 757 2774 0 Poland / Polen Estonia / Estland » +48 618 3198 82 » +370 5249 1109 Portugal / Portugal Finland / Finnland » +34 934 6311 81 » +358 9622 2631 Romania / Rumänien France / Frankreich » +40 264 2079 24 » +33 130 5256 91 Russia / Russland Germany / Deutschland » 8 800 7070 365 (national) » +49 221 8277 564 » +7 495 1815 306 Great Britain / Großbritannien Serbia / Serbien » 0 800 1975 520 -
GOVERNMENT GAZETTE Series B- 5922/31.12.2018
69941 GREEK GOVERNMENT GAZETTE Series B- 5922/31.12.2018 TRUE COPY 69941 OF THE ORIGINAL DOCUMENT Greek Government Gazette December 31st 2018 SERIES B Issue No. 5922 Β' 464/19-4-2010). DECISIONS 9. The provisions of ministerial decision “Natural Gas Dec. No 1314/2018 Licensing Regulation” ref. no. 178065 (Government Gazette Β' 3430/17.08.2018, hereinafter referred to as For the granting of a Natural Gas Distribution “Licensing Regulation”). License to the company under the trade name 10. The Tariffs Regulation for the Main Distribution “Gas Distribution Company Thessaloniki- Activity of distribution networks in Attica, Thessaloniki, Thessaly S.A.” and the distinctive title “EDA Thessaly and other Greece (Government Gazette Β' THESS”. 3067/26.09.2016) (hereinafter referred to as “Tariffs Regulation”). THE REGULATORY AUTHORITY FOR ENERGY 11. The RAE's Decision No 346/2016 on the Approval Taking into consideration the following: of the Tariff for the Charge of the Main Natural Gas 1. The provisions of Law 4001/2011 “For the Distribution Activity on Thessaloniki distribution network operation of the Energy Markets of Electricity and (Government Gazette Β' 3490/31.10.2016). Natural Gas, for Research, Production and transmission 12. The RAE's Decision No 347/2016 on the Approval networks of Hydrocarbons and other arrangements” of the Tariff for the Charge of the Main Natural Gas (Government Gazette A’179/22.08.2011), as amended Distribution Activity on Thessaly distribution network and in force (hereinafter referred to as “the Law”), and (Government Gazette Β'3537/03.11.2016). especially articles 13 and 80C thereof. -
Nikos Skoulikidis.Pdf
The Handbook of Environmental Chemistry 59 Series Editors: Damià Barceló · Andrey G. Kostianoy Nikos Skoulikidis Elias Dimitriou Ioannis Karaouzas Editors The Rivers of Greece Evolution, Current Status and Perspectives The Handbook of Environmental Chemistry Founded by Otto Hutzinger Editors-in-Chief: Damia Barcelo´ • Andrey G. Kostianoy Volume 59 Advisory Board: Jacob de Boer, Philippe Garrigues, Ji-Dong Gu, Kevin C. Jones, Thomas P. Knepper, Alice Newton, Donald L. Sparks More information about this series at http://www.springer.com/series/698 The Rivers of Greece Evolution, Current Status and Perspectives Volume Editors: Nikos Skoulikidis Á Elias Dimitriou Á Ioannis Karaouzas With contributions by F. Botsou Á N. Chrysoula Á E. Dimitriou Á A.N. Economou Á D. Hela Á N. Kamidis Á I. Karaouzas Á A. Koltsakidou Á I. Konstantinou Á P. Koundouri Á D. Lambropoulou Á L. Maria Á I.D. Mariolakos Á A. Mentzafou Á A. Papadopoulos Á D. Reppas Á M. Scoullos Á V. Skianis Á N. Skoulikidis Á M. Styllas Á G. Sylaios Á C. Theodoropoulos Á L. Vardakas Á S. Zogaris Editors Nikos Skoulikidis Elias Dimitriou Institute of Marine Biological Institute of Marine Biological Resources and Inland Waters Resources and Inland Waters Hellenic Centre for Marine Research Hellenic Centre for Marine Research Anavissos, Greece Anavissos, Greece Ioannis Karaouzas Institute of Marine Biological Resources and Inland Waters Hellenic Centre for Marine Research Anavissos, Greece ISSN 1867-979X ISSN 1616-864X (electronic) The Handbook of Environmental Chemistry ISBN 978-3-662-55367-1 ISBN 978-3-662-55369-5 (eBook) https://doi.org/10.1007/978-3-662-55369-5 Library of Congress Control Number: 2017954950 © Springer-Verlag GmbH Germany 2018 This work is subject to copyright. -
Geodetic Evidence for Active Uplift of the Olymbus Mt
∆ελτίο της Ελληνικής Γεωλογικής Εταιρίας τοµ. XXXVI, 2004 Bulletin of the Geological Society of Greece vol. XXXVI, 2004 Πρακτικά 10ου ∆ιεθνούς Συνεδρίου, Θεσ/νίκη Απρίλιος 2004 Proceedings of the 10th International Congress, Thessaloniki, April 2004 GEODETIC EVIDENCE FOR ACTIVE UPLIFT OF THE OLYMBUS MT, GREECE Stiros S.1, and Triantafillides P.1, and Chasapis A.2 1 Department of Civil Engineering, University of Patras, 26500, Patras, [email protected], [email protected] 2 I.G.M.E., Mesogion Str. 70, 115 27, Athens ABSTRACT Repeated leveling data collected between 1964-1989 along a traverse crossing the Tempi Val- ley and the Olymbus Mt (Greece) domal uplift testify to a small, though significant (4-21±1.2- 4.7mm) bulging of the central part of the traverse relative to its edges. In combination with coastal observations indicating land uplift at the eastern part of the traverse, as well as with structural and engineering geology observations excluding the possibility the overall pattern of observed dis- placements to reflect local instability effects, leveling data probably indicate a small amplitude do- mal uplift. The later is likely to reflect the continuation of the process responsible for the formation of the Olymbus-Ossa Mts, for uncovering of upper mantle rocks and for the impressive incision in the Tempi Valley. Furthermore, the lack of seismicity during the period covered by leveling data indi- cates that the Olymbus uplift is at least partly associated with aseismic processes. 1 INTRODUCTION Mount Olymbus in northern Greece (Fig.1), famous from the ancient Greek mythology, has long been recognized as a “tectonic window”, i.e. -
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. -
Optitrans Baseline Study Thessaly
OPTITRANS BASELINE STUDY THESSALY Version 1.0 Date: February 2019 Contents 1 Introduction ............................................................................................................................................ 5 2 Population and Territorial Characteristics ............................................................................................. 6 2.1 Regional Unit of Larissa ................................................................................................................. 9 2.2 Regional Unit of Trikala ................................................................................................................ 10 2.3 Regional Unit of Karditsa .............................................................................................................. 11 2.4 Regional Unit of Magnesia ........................................................................................................... 12 2.5 Regional Unit of Sporades ........................................................................................................... 13 3 Mobility and Transport Infrastructure ................................................................................................... 14 3.1 Road Transport ............................................................................................................................. 14 3.2 Rail Transport ............................................................................................................................... 17 3.3 Sea Transport ..............................................................................................................................