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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. -
How to Cite Complete Issue More Information About This Article
International Journal of Professional Business Review ISSN: 2525-3654 Universidade da Coruña Tzedopoulos, Yorgos; Kamara, Afroditi; Lampada, Despoina; Ferla, Kleopatra THERMALISM IN GREECE: AN OLD CULTURAL HABITUS IN CRISIS International Journal of Professional Business Review, vol. 3, no. 2, 2018, July-December, pp. 205-219 Universidade da Coruña DOI: https://doi.org/10.26668/businessreview/2018.v3i2.83 Available in: https://www.redalyc.org/articulo.oa?id=553658822005 How to cite Complete issue Scientific Information System Redalyc More information about this article Network of Scientific Journals from Latin America and the Caribbean, Spain and Journal's webpage in redalyc.org Portugal Project academic non-profit, developed under the open access initiative Responsible Editor: Maria Dolores Sánchez-Fernández, Ph.D. Associate Editor: Manuel Portugal Ferreira, Ph.D. Evaluation Process: Double Blind Review pelo SEER/OJS THERMALISM IN GREECE: AN OLD CULTURAL HABITUS IN CRISIS TERMALISMO NA GRÉCIA: UM HÁBITO CULTURAL ANTIGO EM CRISE Yorgos Tzedopoulos ¹ ABSTRACT 2 This paper examines thermalism in Greece both in its historical development and in the context of current challenges engendered Afroditi Kamara by economic recession. The authors’ intention is to discuss bathing in thermal springs as a sociocultural practice deeply rooted in 3 history and collective experience (Erfurt-Cooper & Cooper, 2009), to follow its transformations in the course of time, and to Despoina Lampada analyze the complexity of its present state. The latter issue, which is dealt with in more detail, is explored through academic 4 Kleopatra Ferla literature, the evaluation of quantitative and qualitative data, and empirical research. The last part of the paper discusses the conclusions of our study of the Greek case with a view to contributing to the overall assessment of popular thermalism in Europe. -
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 -
Dirfys-Messapia FY R O M
Montenegro Bulgaria Dirfys-Messapia FY R O M Activation ID: EMSN-025 Albania Glide Number: N/A P roduct N.: 04DIR FY S, v1, English Legend Greece Hazard Level Points of Interest Transportation Hazard Level Fire Ex tent Greece LU/LC (sqkm) Turkey Dirfys - Greece Null IC H ospital Secondary V ery Low Very Low Low Medium High Very High Fire station Tertiary Soil Erosion Hazard Zones Low Places ×Ñ Medium !. Education Local and Service Detail Tile 4009 V illage IH Olive groves - 0,089 0,104 0,098 - H igh Track !. Toponym V ery H igh (!S Sports P roduction date: 27/7/2016 Bridge & overpass Pastures - Úð Industrial facilities - 0,022 - - Greece Mitigation Measures Utility network Buildings Electricity infrastructure !( ô!E Cartographic Information Mulch treatment H igh voltage grid Commercial, P ublic & Coniferous forest 0,213 0,476 0,339 0,006 - !n Dam P rivate Services 4009 Full color A1, high resolution (300dpi) 1:5.000 Physiography Hydrography Industry & U tilities Sclerophyllous vegetation - 0,069 0,008 - - 300 P rimary R iver P lace of worship 0 0,05 0,1 0,2 0,3 0,4 Secondary Stream Transitional woodland/shrub - 0,067 0,140 - - U nclassified Km # ± H eight spots Coastline Areas affected by fire - 0,047 0,709 0,287 0,309 Grid: GGR S87 (H ellenic Geodetic R eference System 1987) Tick marks: W GS 84 geographical coordinate system 476500 477000 477500 478000 478500 479000 23°44'0"E 23°44'30"E 23°45'0"E 23°45'30"E 0 0 0 0 5 5 6 6 7 7 2 2 4 4 N " N " 0 4 ' 0 0 0 ' 8 8 3 00 ° 5 5 3 ° 8 00 8 3 3 0 0 0 0 0 0 6 6 7 7 2 2 4 524m 4 0 0 5 400 M e -
El Sistema De Poljes De La Región De Dystos-Almyropotamos (Isla De Eubea, Grecia): Cartografía Y Evolución Geomorfológica*
GEOGRAPHICALIA (2008), 53, 143-161 EL SISTEMA DE POLJES DE LA REGIÓN DE DYSTOS-ALMYROPOTAMOS (ISLA DE EUBEA, GRECIA): CARTOGRAFÍA Y EVOLUCIÓN GEOMORFOLÓGICA* J. L. Peña-Monné(1), M. de Dapper(2), A. Constante(1), B. de Vliegher(2) y K. Pavlopoulos(3) (1) Dpto. de Geografía y Ordenación del Territorio. Universidad de Zaragoza, 50009. Zaragoza (España). [email protected] [email protected] (2) Dpt. of Geography. Ghent University. Krijgslaan, 281 (S8). B-9000 Gent (Bélgica) [email protected] [email protected] (3) Dpt. of Geography. Harokopio University. 70 El. Benizelou St. 17671 Athenas (Grecia) [email protected] Resumen: Se presenta la cartografía de la zona kárstica desarrollada sobre már- moles y esquistos del sector central de la isla de Eubea. Destaca en primer lugar el sistema de poljes, relacionados con la estructura geológica y la evolución cli- mática de la isla durante el Cuaternario. De los 12 poljes diferenciados, tres de ellos se mantienen todavía en situación cerrada. Estas depresiones presentan extensos desarrollos de superficies de aplanamiento y conos rocosos generados por procesos de criptocorrosión kárstica en diferentes momentos de su evolu- ción cuaternaria. Por otra parte, las áreas de cumbre aparecen con restos de superficies aplanadas heredadas, afectadas por campos de lapiaz y dolinas. Se propone un modelo evolutivo y se relaciona con otras áreas kársticas del ámbito mediterráneo. Palabras clave: Grecia, Karst, poljes, Cuaternario. Abstract: A geomorphological mapping of a karstic area developed on marbles and schists in the central sector of the island of Eubea is presented. The system of poljes constitutes the main geomorphological feature. -
Journal of Geophysical Research Earth Surface 120 1 2015.Pdf
PUBLICATIONS Journal of Geophysical Research: Earth Surface RESEARCH ARTICLE Geomorphic constraints on fault throw rates and 10.1002/2014JF003318 linkage times: Examples from the Northern Key Points: Gulf of Evia, Greece • Footwall relief reflects fault segmentation for the studied Alexander C. Whittaker1 and A. Sofia Walker1 faults <60 km long • Knickpoints are generated by fault 1Department of Earth Science and Engineering, Royal School of Mines, Imperial College, London, UK linkage and their heights scale with footwall relief • Fault throw rates calculated from knickpoint heights and footwall relief Abstract We evaluate how the growth and interaction of active normal faults in the Sperchios Basin and Northern Gulf of Evia, Greece, are recorded by the landscape. We demonstrate that patterns in footwall relief along the faults reflect fault segmentation, and we show that in this study area, fault throw is 2 to 3 times the maximum footwall relief. Rivers crossing the faults typically have two knickpoints, which are unrelated to Correspondence to: A. C. Whittaker, lithology. However, their heights, measured from the active fault trace, vary systematically. The height of the [email protected] upper set of knickpoints scales linearly with the footwall relief of the faults and is typically >85% of the maximum relief. The height of the lower set of knickpoints also scales with footwall relief, but the heights Citation: are consistently lower. The existence of two sets of knickpoints suggests that the rivers have been perturbed Whittaker, A. C., and A. S. Walker (2015), by two changes in tectonic rates during faulting. We interpret the upper knickpoints to represent the Geomorphic constraints on fault throw initiation and growth of fault-generated topography, while the lower set of knickpoints reflects a throw rate rates and linkage times: Examples from the Northern Gulf of Evia, Greece, increase due to fault linkage. -
The August 9, 2020 Evia (Central Greece) Flood
ISSN 2653-9454 Issue No.19 | August 2020 The August 9, 2020 Evia (Central Greece) Flood Prof. Efthymis Lekkas PhD c Nafsika-Ioanna Spyrou PhD c Evelina Kotsi PhD c Christos Filis Dr. Michalis Diakakis Prof. Contantinos Cartalis Ass. Prof. Emmanuel Vassilakis MSc Thalia Mavrakou BEng Panagiotis Sartabakos PhD c Marilia Gogou PhD c Kat.-Navs. Katsetsiadou MSc Vanessa Barsaki Dr. Kostis Lagouvardos Dr. Vassiliki Kotroni Dr. Athanasios Karagiannidis MSc Stavros Dafis Prof. Isaak Parcharidis MSc Andreas Karavias MSc Despoina Bafi MSc Ioannis Gougoustamos ISSN 2653-9454 Issue No. 19, August 2020 | 2 About Non-periodic publication of the Post-graduate Studies Publishers: Program “Environmental Disasters & Crises Dr. Efthymis Lekkas Management Strategies" of the National & Kapodistrian Dr. Nikolaos Voulgaris University of Athens, issued after significant events for Dr. Stylianos Lozios the immediate information of the scientific community and the general public. The publication includes also Technical Editing: scientific data from various research teams from PhD c. Spyridon Mavroulis universities, organizations and research institutes. Communication: PhD c. Spyridon Mavroulis ([email protected]) MSc Alexia Grambas ([email protected]) MSc Katerina-Nafsika Katsetsiadou ([email protected]) Scientific Mission Copyrights Of the National and Kapodistrian University of Athens, Faculty of Geology All copyrights of scientific data belong to their and Geoenvironment, Department of Dynamic Tectonic Applied Geology respective owners, while the copyrights of this publication belong to the publishers. Contributors Dr. Efthymis Lekkas, Professor of Dynamic, Tectonic & Applied Geology & Natural Disaster Management Dr. Konstantinos Lagouvardos, Director of Research IERSD/National Observatory of Athens Cited as Dr. Constantinos Cartalis, Professor of Environmental Physics at the University of Athens Lekkas, E., Spyrou N-I., Kotsi E., Filis, Ch., Diakakis, M., Dr. -
Photo: Elliniko Panorama Evia Nean, Creating Emporia (Trade Centres)
FREE www.evia.gr Photo: Elliniko Panorama Evia nean, creating emporia (trade centres). Athenian League, especially during the During the rule of Venice, Evia was known The Ippovotes the aristocracy have by Peloponnesian War, apostatise, fighting for their as Negroponte. “Of the seven islands nature now replaced the Mycenaean kings, and their independence, and the island becomes a In early June 1407, Mehmed II The made… Evia is the fifth, narrow…” power, as well as their commercial ties with battlefield. Conqueror takes over Evia, which is (Stefanos Byzantios, under the entry “Sicily”) the Mediterranean civilisations, is reflected in The Evian Commons, a type of confederation renamed Egipoz or Egripos, and becomes the findings from the tomb of the Hegemon in of the city-states of Evia, was founded in 404 BC. the pashalik of Egripos. Evia owes its name to the healthy cattle Leukanti (now divided between the After the battle of Chaironeia in 338 BC, Evia On the 8th of May 1821, the revolution grazing on its fertile land. Eu + bous = good Archaeological Museums of Athens and comes under the rule of Phillip the 2nd and breaks out first in Ksirochori, led by chieftain cattle. Eretria). Macedonian guard are installed in all of its cities. Angelis Govgios, and then in Limni and In the 8th century BC large city states are After the death of Alexander, the island Kymi. It is not long, however, before it is The history of Evia or Avantis or Makris founded, the most important of which are becomes the apple of discord among his stamped out. -
Camp Sites & Lodgings
ATTICA - EPIRUS • CAMP SITES & LODGINGS Map Guide Cyclades Islands MARAGAS CAMPING Thrace 843 00 Agia Anna - Naxos Macedonia Tel 2285042599, 2285042552, Fax 2285024552 e-mail: [email protected] , web: www.maragascamping.gr Winter Tel 2285024096 RegCo Maragas S.A., VAT 094227300 (Naxos) Mgr Kyriakos Kalogitonas North Epirus Thessalia Open May-Oct, Bedtends, Rooms 6, Studios 15, Apts 9 Aegean Distances: City center 6km, Airport 4km, Beach 10m Islands Ionian Reception, (Breakfast) Bar with satellite TV, Tavern (also with take away), Islands Central Greece Supermarket, Playground, Basket, Intl. Card Phone, Safety boxes, Post box, Book & magazine swap, Credit cards acceptable, Exchange, Car & motorbike hire, Internet connection, Laundry service (wash/dry/iron), Fax, Rental tents, Sleeping Attica Peloponissos bags & mats for hire. Studios & Apts with airconditioning, shower & toilet, kitchenette, fridge, private veranda, TV. MILOS ACHIVADOLIMNI CAMPING cat C Cyclades 848 00 Milos Islands Tel 2287031410, Fax 2287031412 Dodecanissos e-mail: [email protected] , web: www.miloscamping.gr Islands Winter: 240, Attalias Street, 181 22 Korydallos Tel 2104976857, Fax 2104942369 Crete RegCo Doriki S.A. VAT 094291197 (Milos) Mgr Antonis Chronis Blt 1998, Ren 2004, Open May-Sep, Bgls 12 Distances: City center 5km, Beach 150m, Airport 2.5km, Port 6km Restaurant, Pool bar, Lounge bar, Beach bar, Cafeteria, Outdoor swimming pool, Childrens' playground, Wi-Fi internet access, Kitchen/Shower for common use, Laundry, Safes, Beach volley, Mini market, Tranfers, -
The Universidad Autónoma De Madrid and Fourteenth Ephorate Epicnemidian Locris Project FINAL REPORT
The Universidad Autónoma de Madrid and Fourteenth Ephorate Epicnemidian Locris Project FINAL REPORT (1) (2) Jose Pascual and Maria-Foteini Papakonstantinou (1) Department of Ancient History. Universidad Autónoma de Madrid (2) Fourteenth Ephorate of Prehistoric and Classical Antiquities Twenty-Fourth Ephorate of Byzantine Antiquities The area that was known as Epicnemidian Locris in Antiquity is a region of central Greece lying on the eastern seaboard of the Balkan Peninsula, on the shores of the Aegean Sea. Its borders probably coincided, approximately, with Mount Cnemis in the east, the Callidromus massif in the south and the Spercheius river basin in the west. The waters of the Malian Gulf and the Island of Euboea lay to the North (Figures 1 and 2). From 2004, as part of Research Projects BHA2001-0157, HAR2008- 04081/HIST and HAR2011-25443, subsidised by the Spanish Ministry of Education and Science, of the Agreement number 028700 (Universidad Autónoma de Madrid and Company Ontex Peninsular S.A.), subsidised by the Company Ontex Peninsular S.A. and the Agreement of the Ministry of Culture of the Hellenic Republic Αρ.Πρωτ. ΥΠΠΟ/ΓΔΑΠΚ/ΑΡΧ/Α2/Φ15/73900π.ε./31/2-3-2004, a Spanish-Greek team from the Fourteenth Ephorate of Prehistoric and Classical Antiquities and the Universidad Autónoma de Madrid, under the direction of Maria-Foteini Papakonstantinou and from the side of University of the staff of the Department of Ancient History,1 has developed a research project in Epicnemidian Locris (see also A.J. Domínguez, Teiresias 35, part 1, 2005). Τhis is the first historic-topographical research in the region and the first joint official Greek-Spanish field work in Greek territory. -
Bulletin of the Geological Society of Greece
Bulletin of the Geological Society of Greece Vol. 40, 2007 NEOTECTONIC BASIN EVOLUTION IN CENTRAL- EASTERN MAINLAND GREECE: AN OVERVIEW Kranis H. National and Kapodistrian University of Athens, Faculty of Geology and Geoenvironment, Department of Dynamic, Tectonic & Applied Geology http://dx.doi.org/10.12681/bgsg.16621 Copyright © 2018 H. Kranis To cite this article: Kranis, H. (2007). NEOTECTONIC BASIN EVOLUTION IN CENTRAL-EASTERN MAINLAND GREECE: AN OVERVIEW. Bulletin of the Geological Society of Greece, 40(1), 360-373. doi:http://dx.doi.org/10.12681/bgsg.16621 http://epublishing.ekt.gr | e-Publisher: EKT | Downloaded at 11/01/2020 00:09:18 | Δελτίο της Ελληνικής Γεωλογικής Εταιρίας τομ. ΧΧΧΧ, 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 NEOTECTONIC BASIN EVOLUTION IN CENTRAL-EASTERN MAINLAND GREECE: AN OVERVIEW Kranis H.1 1 National and Kapodistrian University of Athens, Faculty of Geology and Geoenvironment, Department of Dynamic, Tectonic & Applied Geology, [email protected] Abstract The neotectonic evolution of central-eastern mainland Greece (Sterea Hellas) is documented in the result of local extensional tectonics within a regional transten- sional field, which is related to the westward propagation of the North Anatolian Fault. The observed tectonic structures within the neotectonic basins and their mar gins (range-bounding faults and fault zones, rotation of tectonic blocL·) suggest a close relation to the Parnassos Detachment Fault (PDF), which is a reused alpine thrust surface. Lokris basin (LB) occupied a central position in this neotectonic con figuration, having received its first sediments in the Uppermost Miocene and subse quently been greatly affected by tectonic episodes, which continue until nowadays. -
Greek Island 8
©Lonely¨Planet¨Publications¨Pty¨Ltd Evia & the Sporades Why Go? Evia ...........................439 Evia (Εύβοια) and the four Sporades islands (Οι Σποράδες) The Sporades ............444 remain largely off the beaten island path, though two bridg- es at Halkida join Evia to the mainland. But away from its Skiathos ....................444 commercial hub of Halkida, the pace slows as the landscape Skopelos ....................448 stretches out, dotted by hilltop monasteries, small farms, Alonnisos ...................452 vineyards and not a few curious goats. Skyros ........................ 457 The Sporades (‘scattered ones’) seem like extensions of the forested Pelion Peninsula, and, in fact, they were joined in prehistoric times. Skiathos, easily the most developed of the group, claims the sandiest beaches in the Aegean. Best Places to Eat Low-key Skopelos kicks back with a postcard-worthy har- ¨¨Dina’s Amfilirion bour and forest meadows. Remote Alonnisos anchors the Restaurant (p441) National Marine Park of the Northern Sporades. Skyros, the southernmost of the chain, is known for its culinary and ar- ¨¨Taverna-Ouzerie tistic traditions that date from Byzantine times when these Kabourelia (p446) islands were home to rogues and pirates. ¨¨Nastas Ouzerie (p450) ¨¨Hayati (p456) ¨¨Taverna Mouries (p462) When to Go Skíathos Town Best Places to °C/°F Temp Rainfall inches/mm Stay 40/104 0.79/20 ¨¨Hotel Nefeli (p459) 30/86 0.39/15 ¨¨Atrium Hotel (p448) 20/68 ¨¨Pension Sotos (p450) 0.2/5 10/50 ¨¨Liadromia Hotel (p454) 0/32 0 ¨¨Perigiali Hotel & Studios J F M A M J J A S O N D (p460) Feb & Mar Carni- Apr & May Spring Jun & Sep val season keeps is in the air and Perfect tempera- things warm with Easter festivities tures and clear plenty of merry- linger long into skies – ideal hik- making.