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GO for IT! Swim
CATCH TASTE THE WAVE PATROL Where to Sea, Eat like a local: Sun, Surf & Fun Roadmap for the most KEFALONIA, Στις ωραιότερες ISSUE 04 delicious flavours παραλίες CORFU, Οι συντεταγμένες της SUMMER 2019 - ZAKYNTHOS WINTER 2020 & AKTION τοπικής γαστρονομίας MADE OF KEFALONIA GODS HISTORY Local products & WALKS producers behind the Monuments you must label. Ποιοι κρύβονται see. Βόλτες στην Ιστορία πίσω από τα τοπικά προϊόντα; THE WEST EDITION HIP HOTELS To connect more deeply with your destination THE WEST EDITION Στα καλύτερα ξενοδοχεία FRAPORT GREECE OFFICIAL MAGAZINE του Ιονίου WHERE TO MAKE YOUR EURO GO FURTHER Shop and indulge your way. Οι διευθύνσεις της καλής ζωής ISSUE 04 SUMMER 2019 - WINTER 2020 THE WHITE HOUSE EXPERIENCE Be a Durrell for a day (or more) Στην Κέρκυρα των Durrell 120’ FREE VIDEO COPY INSIDE GO FOR IT! Swim. Explore. Dine. Drink. Relax. Shop. The islands’ go-to list 40 Lithostroto Str., Argostoli, Kefalonia, tel.: +30 26710 28665, +30 26710 24329. tzannatos.com Tzannatos Jewellers Since 1904 tzannatos_jewellers TzannatosAD.indd All Pages 29/7/2019 1:48:45 µµ 40 Lithostroto Str., Argostoli, Kefalonia, tel.: +30 26710 28665, +30 26710 24329. tzannatos.com Tzannatos Jewellers Since 1904 tzannatos_jewellers TzannatosAD.indd All Pages 29/7/2019 1:48:45 µµ OPENING SUMMER 2020 MarBella Elix A MARBELLA COLLECTION HOTEL Karavostasi Beach – Perdika, GR46100 – Thesprotia. Tel.: +30 26610 71123. Email: [email protected] www.marbellacollection.gr/marbella-elix/ LIVE THE ELIX LIFE! SPACIOUS. LUXURIOUS. GORGEOUS. MarbellaSALONIfinal.indd All Pages 29/7/2019 1:53:21 µµ OPENING SUMMER 2020 MarBella Elix A MARBELLA COLLECTION HOTEL Karavostasi Beach – Perdika, GR46100 – Thesprotia. -
The Ionian Islands COPY
∆ΩΡΕΑΝ ΑΝΤΙΤΥΠΟ FREE COPY PUBLICATION GRATUITE FRA OPUSCOLO GRATUITO ITA The Ionian Islands EJEMPLAR ESP GRATUITO GRATIS- www.visitgreece.gr AUSGABE Распространяется бесплатно GREEK NATIONAL TOURISM ORGANISATION THE IONIAN ISLANDS GREEK NATIONAL TOURISM ORGANISATION 04Corfu (Kerkyra) 22Diapontia Islands 26Paxoi (Paxi) 32Lefkada 50Kefalonia 68Ithaca (Ithaki) 74Zakynthos (Zante) CONTENTS 1. Cover page: Zakynthos, Navagio beach. Its white sand and turquoise waters attract thousands of visitors each year. Ionian Islands The Ionian Islands have a temperate climate, seawaters as deep as they are refreshing, in the area, reaching 4,406 m., registered as the greatest in the Mediterranean. verdant mountains, a rich cultural heritage and a carefree spirit; the ideal combination for Their mild, temperate climate makes them the ideal choice for vacation or permanent stay. your holidays during which you will enjoy a well-developed tourism infrastructure, hotels, In the wintertime, the mainland’s mountains buffer the bitter northern winds blowing to the restaurants, water sports centres, cultural events and numerous sights, historic monuments, direction of the islands while the hot summer weather is tempered by the mild northwestern and museums. meltemia winds and the sea breeze. The area’s air currents have turned many of the Ionian Scattered along the mainland’s western coastline, the Ionian Islands are a cluster of 12 Islands’ beaches into worldwide known destinations for windsurfing. large and small islands covering an area of 2,200 sq. km. There are six large ones: Zakynthos The Ionian Islands have been inhabited since the Paleolithic times. Since then, numerous (Zante), Ithaki (Ithaca), Kerkyra (Corfu), Kefalonia (Cephallonia), Lefkada (Leucas), and invaders and cultural influences have left their stamp on the islands. -
GUIDE to GREEK RETREAT VENUES for Your Next Retreat
Discover the Perfect Venue GUIDE TO GREEK RETREAT VENUES For Your Next Retreat RETREATS AND VENUES INDEX INDEX Contents 02 - 03 04 - 05 06 08 - 09 10 - 11 12 - 13 19 - 20 20 - 21 22 - 23 23 - 36 36 - 59 59 - 64 64 - 66 66 - 76 76 - 78 78 - 83 84 - 85 86 86 - 88 88 90 RETREAT AND VENUES Choose from a 1000+ venues vetted by www.retreatsandvenues.com our community of over 750 retreat leaders. 2 | © RETREATSANDVENUES © RETREATSANDVENUES | 3 ABOUT US ABOUT US Discover Your Perfect RETREATS Choose from a 1000+ venues & VENUES vetted by Retreat Venues our community of over 750 retreat leaders. FIND A VENUE e help retreat leaders find their perfect venue for free. Browse our Then our retreat venue experts will curate a custom list of venues that match website or book a discovery call today for a more personalized your retreat vision. We then work 1 on 1 with you to help you book or hold Wtouch. We will start by learning more about your retreat vision on your perfect venue. a discovery call (15 to 30 minutes). 4 | © RETREATSANDVENUES © RETREATSANDVENUES | 5 GREECE ORIZONTES DELUXE RESIDENCE Orizontes Deluxe Residence 9 PEOPLE 4 ROOMS CHQ VILLA RETHYMNO, CRETEF LEARN MORE Orizontes Deluxe Residence promises a one of a kind accommodation experience to the visitors of Crete and Rethymno, who look forward to Discover Your taking a vacation with their family or friends in Next Retreat Venue a high architectural and aesthetic aspirations property, which combines luxury, privacy, GREECE serenity and a magnificent view, all in one. -
Herpetological Observations on the Greek Islands of Kefallinia and Zakynthos
Herpetological observations on the Greek islands of Kefallinia and Zakynthos MATT J. WILSON 48 Harehill RD, Littleborough, Lancashire OL15 9HE, UK E-mail: [email protected] CQUIRING information on the herpetofauna GEOGRAPHY Aof Kefallinia and neighbouring islands is Kefallinia is the largest of the Ionian Islands and somewhat difficult, and when this information is is almost twice the size of neighbouring Lefkada, located, it is not in plentiful supply. Very little has with a distance of 90 kilometres from the Skala been published on reptiles and amphibians in the region in the far southeast to Fiskardo at its most Ionian Islands, except Corfu, probably due to the northerly point. The island has very cold winters, variety of species present there. Relatively recent contrasted by very hot, dry summers during which contributions on the islands of Kefallinia and – as elsewhere in Greece – the majority of water Zakynthos include that of Clark (1970), sources dry-out. Kefallinia is a mountainous “Observations of the lizard and snake fauna of the island, and is generally drier than others in the islands Kephallinia and Zakynthos, Ionian Sea, Ionian group. The most evident and impressive Greece”, and also of significance is that by peak is Mount Ainos, which reaches a height of Keymar (1986), “Amphibians of the Ionian almost 1630 metres. This mountain is a National region: their origin, distribution and future”. Park and was declared so in 1962, not due to its Mention must also be made of D. Kock, whose herpetofauna but the Cephalonian fir (Abies work elsewhere in the Ionian group is also cephalonica), which covers the majority of the considerable. -
Sur Quelques Sources Littorales Et Sous-Marines Autour De La Méditerranée
3 É tudes de Géographie Physique, n° XXXVI, 2009 SUR QUELQUES SOURCES LITTORALES ET SOUS-MARINES AUTOUR DE LA MÉDITERRANÉE Jean NICOD (1) (1) : Florida 1, 35 Avenue du 24 Avril 1915, 13012 MARSEILLE. RÉSUMÉ : Cette étude rassemble des informations et discussions, d'après de nombreux auteurs, sur diverses sources karstiques littorales, d'eau douce ou saumâtre, et émergences sous-marines, dans leur contexte hydrogéologique, géomorphologique et environnemental. La position par rapport au niveau marin des principales sources est précisée (Tab. I) et on rappelle brièvement leur origine et le fonctionnement des émergences, ainsi que les difficultés de captage, du fait des intrusions d'eau marine. On a particulièrement analysé le fonctionnement de Font Estramar et Font-Dame, sur la bordure de l'étang de Salses, en rapport avec le karst des Corbières, le cas analogue de l'alimentation du Lac Siutghiol sur le littoral de la Dobrodgea, le problème classique des "Moulins de la Mer" d'Argostoli et de l'hydrosystème de l'île de Céphalonie, et d'autres problèmes des karsts littoraux (covas de Majorque, etc.). MOTS-CLÉS : Karst littoral, paléo-hydrologie, sources littorales, sources sous-marines. ABSTRACT : This study produces some informations and discussions, after numerous authors, on various fresh water ore brackish (almyros) karstic coastal springs, and submarine springs (vrulja), in their hydrogeological and geomorphological environment. The position of main springs with the present sea level is analysed (tabl. 1), and the genesis and explanation of the brackish and submarine springs is brievly discussed, as well as the difficulties of catching because sea water intrusions. Are particularly showed the connections of Font Estramar and Font-Dame, the springs in the border of Salses lagoon, with the Corbières karstic area, the similar case of supply of the Siutghiol Lake in the Dobrodgea, the classical problem of the "sea mills" of Argostoli and the hydrosystem in the Kephallinia Island, and other problems in some coastal karst (covas of Mallorca...). -
Ionian Sea, Western Greece) Earthquake Sequence: Damage Pattern on Buildings
16th World Conference on Earthquake, 16WCEE 2017 Santiago Chile, January 9th to 13th 2017 Paper N° 414 THE JANUARY-FEBRUARY 2014 CEPHALONIA (IONIAN SEA, WESTERN GREECE) EARTHQUAKE SEQUENCE: DAMAGE PATTERN ON BUILDINGS S. Mavroulis(1), V. Alexoudi(2), A. Grambas(3), E. Lekkas(4), P. Carydis(5) (1) MSc Geologist, Department of Dynamic Tectonic Applied Geology, Faculty of Geology and Geoenvironment, School of Sciences, National and Kapodistrian University of Athens, Greece, [email protected] (2) MSc Engineer, Department of Dynamic Tectonic Applied Geology, Faculty of Geology and Geoenvironment, School of Sciences, National and Kapodistrian University of Athens, Greece, [email protected] (3) MSc Geologist, Department of Dynamic Tectonic Applied Geology, Faculty of Geology and Geoenvironment, School of Sciences, National and Kapodistrian University of Athens, Greece, [email protected] (4) Professor of Dynamic Tectonic Appleid Geology and Disaster Management, Department of Dynamic Tectonic Applied Geology, Faculty of Geology and Geoenvironment, School of Sciences, National and Kapodistrian University of Athens, Greece, [email protected] (5) Professor Emeritus, National Technical University of Athens,Greece, [email protected] Abstract The early 2014 Cephalonia earthquake sequence comprised two main shocks with almost the same magnitude (Mw 6.0) occurred successively in short time (January 26, February 3) and space (western Cephalonia, Paliki peninsula). The first event caused damage mainly in the Paliki peninsula, while the second aggravated damage induced by the first. The dominant buildings types are masonry, reinforced concrete (RC) and monumental buildings. Masonry buildings suffered the most due to their high vulnerability. RC buildings showed good performance due to their good construction quality. -
Derived from New Seismological and Geodetic Data on the Ionian Islands, Greece
data Article Characteristics of Recent Aftershocks Sequences (2014, 2015, 2018) Derived from New Seismological and Geodetic Data on the Ionian Islands, Greece Alexandra Moshou 1,* , Panagiotis Argyrakis 1 , Antonios Konstantaras 2 , Anna-Christina Daverona 3 and Nikos C. Sagias 4 1 Institute of Geodynamics, National Observatory of Athens, Lofos Nymphon, 11810 Athens, Greece; [email protected] 2 Department of Electronic Engineering, Hellenic Mediterranean University, 3 Romanou Str., Chalepa, 73133 Chania, Crete, Greece; [email protected] 3 Department of Surveying and Geoinformatics Engineers, Faculty of Engineering, Egaleo Park Campus, University of West Attica, Ag. Spyridonos Street, Aigaleo, 12243 Athens, Greece; [email protected] 4 Department Informatics and Telecommunications, Faculty of Economics and Technology, University of the Peloponnese, Akadimaikou G. K. Vlachou Street, GR-22131 Tripoli, Greece; [email protected] * Correspondence: [email protected]; Tel.: +30-21-0349-0152 Abstract: In 2014–2018, four strong earthquakes occurred in the Ionian Sea, Greece. After these events, a rich aftershock sequence followed. More analytically, according to the manual solutions of the National Observatory of Athens, the first event occurred on 26 January 2014 in Cephalonia Island with magnitude ML = 5.8, followed by another in the same region on 3 February 2014 with magnitude ML = 5.7. The third event occurred on 17 November 2015, ML = 6.0 in Lefkas Island and the last on 25 October 2018, ML = 6.6 in Zakynthos Island. The first three of these earthquakes caused moderate structural damages, mainly in houses and produced particular unrest to the local population. This Citation: Moshou, A.; Argyrakis, P.; work determines a seismic moment tensor for both large and intermediate magnitude earthquakes Konstantaras, A.; Daverona, A.-C.; (M > 4.0). -
Seismic Hazard Analysis in the Ionian Islands Using Macroseismic Intensities*
Project 34 N:17 2/14/11 10:22 PM Page 239 Hellenic Journal of Geosciences, vol. 45, 239 Seismic hazard analysis in the Ionian Islands using macroseismic intensities* Georgios Sakkas, Vicki Kouskouna & Kostas Makropoulos Department of Geophysics, Faculty of Geology & Geoenvironment, University of Athens, Panepistimiopolis, 157 84, Zographou, Athens, Greece ABSTRACT : The seismic hazard of Greece has been studied mainly through methods using maximum expected magnitude and peak ground accel - eration. However, few studies that have taken into account macroseismic intensity data appear in the bibliography. In this paper , a seismic hazard analy - sis based on Gumbel’s approach to PSHA for the Ionian Islands Corfu, Zakynthos, Leukada and Cephalonia is performed , using all the available macroseismic intensity data for the time period 1950 - todate. The macroseismic intensity values, as well as the corresponding locality (name and ge - ographical coordinates) were introduced into a database as Intensity Data Points. For approximately 60 years of observation period, the maximum intensity I max of each locality was identified and probabilistic seismic hazard analy - sis using the HAZAN algorithm is performed. The output of the analysis consists of the most probable maximum intensity for the next 25 years (25 years mode). Key-words : seismic hazard analysis, macroseismic intensities . Περίληψη: Στη βιβλιογραφία οι µελέτες σεισµικής επικινδυνότητας για τον Ελληνικό χώρο εστιάζουν κυρίως στο µέγιστο αναµενόµενο σεισµικό µέγεθος και τη µέγιστη αναµενόµενη εδαφική επιτάχυνση, ενώ σπανίζουν αυτές που πραγµατεύονται τη µακροσεισµική ένταση ως το κύριο στοι - χείο της ανάλυσης. Στην παρούσα εργασία µελετάται η σεισµική επικινδυνότητα των Ιονίων Νήσων, Κέρκυρας, Κεφαλλονιάς, Λευκάδας και Ζα - κύνθου, βασιζόµενη στην πρώτη ασύµπτωτη του Gumbel και χρησιµοποιώντας όλα τα διαθέσιµα µακροσεισµικά δεδοµένα από το 1950 έως και σήµερα. -
Präsentiert Den Reiseführer Für Insel Kefalonia
präsentiert den Reiseführer für Insel Kefalonia Die immergrüne Inseln Kefalonia Wunderschöne Landschaften, phantastische Strände, ein reiches Kulturerbe, bedeutende Monumente, Berge, Burgen, abgelegene Klöster und fröhliche, gastfreundliche Menschen; diese sind die wertvollen Schätze, die Kefalonia zu einem der attraktivsten Urlaubsziele machen. Es handelt sich um die größte Insel des Ionischen Meeres, am Ausgang zum Golf von Patras gelegen, zwischen den Inseln Zakynthos und Lefkada. Die Gesamtfläche der bei Griechenland Reisen noch nicht von den Massen eroberte Insel beträgt 904 qkm, mit einer Küstenlänge von circa 250 km. Die Insel hat eine wunderbare natürliche Schönheit und eine vielfältige geologische Struktur mit zahllosen kleinen Buchten und einer großartigen Vegetation; außerdem imponiert das Gebirgsmassiv Ainos (Nationalpark seit 1962, mit reicher Flora und Fauna) schon von weitem. Kefalonia wurde während der byzantinischen Zeit in die Provinz Achaia eingegliedert und gehörte administrativ zum östlichen Illyrikon. Im Laufe der Zeit wurde die Insel von Nomaden, Franken, Venezianern und Türken erobert. Die Vereinigung mit Griechenland und den restlichen Eptanisa- Inseln erfolge am 21. Mai 1864. Der Widerstand der Bewohner gegen die Italiener und die Deutschen während des zweiten Weltkrieges war sehr groß. Eine Geschichte aus der Zeit des Widerstands wird im Spielfilm „Corellis Mandoline“ wieder erzählt, der auf der Insel an Originalschauplätzen gedreht wurde. © Priv.-Doz. Dimitrios Zachos griechenlandabc.de Argostoli ist seit 1757 die Inselhauptstadt. Es geht um eine moderne Stadt, die Elemente der traditionellen Architektur erhalten hat. Ähnlich wie Amphitheater erbaut und mit Blick auf die Koutavou Lagune, die eine Zwischenstation für die Zugvögel ist. Die Stadt rühmt sich vieler neoklassizistischen Bauten, große Plätze, Kirchen und ein nennenswertes kulturelles Leben, nicht zuletzt mit ihrem bedeutenden Philharmonischen Orchester, den Chören und Theatergruppen. -
The Cephalonia, Ionian Sea (Greece), Sequence of Strong
Research in Geophysics 2014; volume 4:5441 The Cephalonia, Ionian tion. The rupture was directed upwards which along with the shallow focus (~5 km) and the Correspondence: Gerassimos A. Papadopoulos, Sea (Greece), sequence of simple source time function may explain the Lofos Nymfon, Thission, PC 11810, Athens, strong earthquakes significantly larger (0.77 g) PGA recorded with Greece. of January-February 2014: the second earthquake with respect to the one E-mail: [email protected] recorded (0.56 g) with the first earthquake. a first report Key words: Ionian Sea, Cephalonia Transform Most of the slip was concentrated on a 12x6 km Fault Zone, 2014 earthquakes, relocation, focal fault rupture. Maximum seismic intensity (I ) Gerassimos A. Papadopoulos,1 m mechanisms, strike-slip faulting, rupture histo- of level VII and VIII to VIII+ was felt in Lixouri ries, macroseismic intensity, ground failures. Vassilios K. Karastathis,1 town and the nearby villages from the first and Ioannis Koukouvelas,2 Maria Sachpazi,1 the second earthquake, respectively. The rup- Acknowledgements: this paper is a contribution 1 Ioannis Baskoutas, ture histories and the increased building vul- to the EU FP7-PEOPLE-2013-ITN Project ZIP 1 (Zooming In between Plates: deciphering the Gerassimos Chouliaras, nerability after the damage caused by the first Apostolos Agalos,1 Eleni Daskalaki,1 nature of the plate interface in subduction shock may account for the larger Im caused by zones), contract no. 604713, and to the internal 1 1 George Minadakis, Alexandra Moshou, the second shock. However, the ground fail- research project EARTHWARN of the Institute of Aggelos Mouzakiotis,1 ures area of the second earthquake was nearly Geodynamics, National Observatory of Athens, Katerina Orfanogiannaki,1 half of that of the first earthquake, which is Greece. -
On “Arogi” Buildings' Structural System and Construction
heritage Article On “Arogi” Buildings’ Structural System and Construction Procedure after the 1953 Earthquake in Kefalonia Eleni Theotokatou NTUA Architect, 17562 Athens, Greece; [email protected] Received: 27 June 2019; Accepted: 22 July 2019; Published: 26 July 2019 Abstract: After the series of earthquakes in August 1953, most of Kefalonia’s building stock totally collapsed. The buildings that emerged as a result of a collective effort are commonly referred to as “arogi” buildings, with the term arogi meaning help or assistance. In this way, merely referring to these structures is a direct mention to the circumstances under which they were constructed. The reconstruction of the building stock of the island was based in a series of building types proposed from the authorities, and proceeded replacing the richness of the architectural forms that stood before the earthquake, with austere but necessary settlements. Nevertheless, it is these buildings that constitute today’s image of the island. This study wishes to introduce us to the “arogi” buildings structural system, as it was applied in Kefalonia after the 1953 earthquake, with reference to recent bibliography and the recent experience of the 2014 earthquake. The purpose of setting the grounds for such research would be to highlight the effectiveness of this structural system. Moreover, to emphasize the fact that “arogi” buildings and their construction procedure incorporate Kefalonia’s recent history and have eventually produced today’s available “traditional” architecture of the island. Keywords: arogi buildings; 1953 earthquake; confined masonry; Kefalonia 1. Introduction The Ionian Islands stand in a remarkably seismic area, with Kefalonia literally standing on the Greek trench, i.e., where Eurasian and African lithospheric plates come to meet. -
Le Isole Ionie.Pdf
∆ΩΡΕΑΝ ΑΝΤΙΤΥΠΟ FREE COPY PUBLICATION GRATUITE FRA OPUSCOLO GRATUITO ITA EJEMPLAR ESP GRATUITO GRATIS- AUSGABE Распространяется бесплатно Le Isole Ionie www.visitgreece.gr ENTE NAZIONALE ELLENICO DEL TURISMO LE ISOLE IONIE ENTE NAZIONALE ELLENICO DEL TURISMO 04Corfù (gr. Kérkyra) 22Isole Diapontia 26Paxì 32Leucade (gr. Lefkàda) 50Cefalonia (gr. Kefalonià) 68Itaca (gr. Ithàki) 74Zante (gr. Zàkynthos) INDICE 1. (copertina). Zante. La spiaggia Navayo, con la sabbia bianca e l’acqua verde-azzurra, attira ogni anno migliaia di visitatori. Le Isole Ionie Le Isole Ionie, con un clima eccezionale, il mare profondo e fresco, le montagne e il verde, 4.406 m, è la maggiore di tutto il Mediterraneo. il patrimonio culturale ma anche il buon umore degli abitanti, sono un luogo ideale per Godono di un clima temperato e mite, che le rende ideali per vacanze e residenza. In inverno vacanze e riposo. E a tutto ciò si abbina un’ottima infrastruttura turistica, con alberghi, i monti della Grecia continentale impediscono l’azione dei venti freddi provenienti da Nord; ristoranti, centri per immersioni e sport nautici, manifestazioni culturali e bellezze naturali, in estate il caldo viene moderato da deboli venti etesii (meltemia) che arrivano da Nord- monumenti storici e musei. Ovest ed anche dalla brezza marina. A causa di questi venti diverse spiagge dell’Eptaneso Sparse lungo le coste occidentali della Grecia continentale, le Isole Ionie, come sono cono- sono diventate centri di windsurfing noti in tutto il mondo. sciute, costituiscono un arcipelago di dodici isole piccole e grandi, con un’estensione totale Le Isole Ionie furono abitate fin dal Paleolitico e da allora hanno vissuto varie forme di di 2.200 Kmq.