Îles Grecques – Les Cyclades Et Athènes
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DESERTMED a Project About the Deserted Islands of the Mediterranean
DESERTMED A project about the deserted islands of the Mediterranean The islands, and all the more so the deserted island, is an extremely poor or weak notion from the point of view of geography. This is to it’s credit. The range of islands has no objective unity, and deserted islands have even less. The deserted island may indeed have extremely poor soil. Deserted, the is- land may be a desert, but not necessarily. The real desert is uninhabited only insofar as it presents no conditions that by rights would make life possible, weather vegetable, animal, or human. On the contrary, the lack of inhabitants on the deserted island is a pure fact due to the circumstance, in other words, the island’s surroundings. The island is what the sea surrounds. What is de- serted is the ocean around it. It is by virtue of circumstance, for other reasons that the principle on which the island depends, that the ships pass in the distance and never come ashore.“ (from: Gilles Deleuze, Desert Island and Other Texts, Semiotext(e),Los Angeles, 2004) DESERTMED A project about the deserted islands of the Mediterranean Desertmed is an ongoing interdisciplina- land use, according to which the islands ry research project. The “blind spots” on can be divided into various groups or the European map serve as its subject typologies —although the distinctions are matter: approximately 300 uninhabited is- fluid. lands in the Mediterranean Sea. A group of artists, architects, writers and theoreti- cians traveled to forty of these often hard to reach islands in search of clues, impar- tially cataloguing information that can be interpreted in multiple ways. -
MASS TOURISM and the MEDITERRANEAN MONK SEAL
MASS TOURISM and the MEDITERRANEAN MONK SEAL The role of mass tourism in the decline and possible future extinction of Europe’s most endangered marine mammal, Monachus monachus William M. Johnson & David M. Lavigne International Marine Mammal Association 1474 Gordon Street, Guelph, Ontario, Canada N1L 1C8 ABSTRACT Mass tourism has been implicated in the decline of the Mediterranean monk seal (Monachus monachus) since the 1970s, when scientists first began reviewing the global status of the species. Since then, the scientific literature, recognising the inexorable process of disturbance and loss of habitat that this economic and social activity has produced along extensive stretches of Mediterranean coastline, has consistently identified tourism as among the most significant causes of decline affecting this critically-endangered species. Despite apparent consensus on this point, no serious attempt has been made to assess the tourist industry’s role, or to acknowledge and discuss its moral and financial responsibility, in the continuing decline and possible future extinction of M. monachus. In view of this, The Monachus Guardian 2 (2) November 1999 1 we undertook a review of existing literature to identify specific areas in which tourism has impacted the Mediterranean monk seal. Our results provide compelling evidence that mass tourism has indeed played a major role in the extirpation of the monk seal in several European countries, that it continues to act as a significant force of extinction in the last Mediterranean strongholds of the species, and that the industry exerts a generally negative influence on the design and operation of protected areas in coastal marine habitats. There are compelling reasons to conclude that unless the tourist industry can be persuaded to become an active and constructive partner in monk seal conservation initiatives, it will eventually ensure the extinction of the remaining monk seals in the Mediterranean. -
A West-East Traverse Along the Magmatism of the South Aegean Volcanic Arc in the Light of Volcanological, Chemical and Isotope Data
65 A West-East Traverse along the magmatism of the south Aegean volcanic arc in the light of volcanological, chemical and isotope data L. Francalanci1,2,∗, G.E. Vougioukalakis 3, G. Perini1, P. Manetti1,2 1 Dipartimento di Scienze della Terra, Università degli Studi di Firenze, via La Pira, 4, I-50121, Firenze, Italy. 2 C.N.R., I.G.G., Sezione di Firenze, via La Pira 4, I-50121, Firenze, Italy. 3 I.G.M.E, Mesogeion, 70, Athens, Greece. ABSTRACT The volcanic rocks of the South Aegean arc (SAAVA) form a chain from the Gulf of Saronikos (Susaki, Egina, Poros, Methana) at West, to an area close to the Anatolian coast at East (Kos, Nisyros and minor islands), through the central part (Milos and Santorini island groups). The volcanic activity began in the Lower Pliocene at Egina (4.7 Ma) and lasted until present days, with the still active Methana, Milos, Santorini and Nisyros volcanoes. The beginning of volcanism is younger in the central sector of the arc. Volcanic center location was controlled by large tectonic lineaments, most of them still active, trending E-W to NW-SE for the western part and mainly NE-SW for the central and eastern parts of the arc. Volcanic fields developed along ellipse shaped areas with the longest axis oriented perpendicular to the subduction front. In the western volcanic fields (Susaki, Egina-Poros-Methana and Milos), volcanic centers are mostly monogenetic and no composite volcanic structures are present. In the eastern sector of the arc, Santorini and Nisyros are important composite volcanoes with caldera structures. -
Find Your Greek Island Love Match
6 *** Sunday 20 June 2021 The Sunday Telegraph The Sunday Telegraph Sunday 20 June 2021 *** 7 Greece Tile style: Pyrgi ciples – from Orthodox pilgrims to jet- Tinos by accident – they hopped over village in Chios is setting fashion editors – Patmos is the from Mykonos while waiting for a little known but full of character Alpha and Omega of Greek islands. delayed flight. “We’d visited lots of Patmos is an eight-hour ferry ride Aegean Islands, though Tinos, typified Find your At the helm: from Athens. The nearest international in guides as a Greek Lourdes, somehow island hop airport is five islands away. Scott got missed,” recalls Peter. “We found around the Williams (01749 812721; scottwilliams. beautiful landscapes, fields of arti - archipelago by co.uk) has a couple of handsome villas on chokes, heavenly beaches and excellent hiring a boat Patmos, from €2,900 (£2,490) per week. tavernas. In a green valley dotted with car-free villages, someone showed us an ancient, dilapidated house once the Greek island home of a bishop. It was for sale. Our life K suddenly changed – too big to restore is for Kea for just the two of us, we created a hotel set among quiet terraces.” Filled with The closest to Athens of all the Cyclades, contemporary art and design, local Kea is a game of two halves. The yacht marble, mosaics, and antiques, Xinara love match set flirt over lobster spaghetti in the bays House is one of the most exceptional of Vourkari and Koundouros, while pur- guesthouses in Greece. ists commune with nature in the oak- Prices per night (low season) from Quick fling or lengthy affair, you’ll find your ideal clad hills, where sheep huddle around €100 (£85) for 2-3 people, €375 (£320) ice-cold springs, and farmers till their for 8-10 people (xinarahouse.com). -
Griechenland 2 Attikaküste – Petalischer Golf Südlicher Euböa-Golf – Südteil Von Euböa – Kykladen
3 GERD RADSPIELER MELANIE HASELHORST KENNETH DITTMANN GRIECHENLAND 2 ATTIKAKÜSTE – PETALISCHER GOLF SÜDLICHER EUBÖA-GOLF – SÜDTEIL VON EUBÖA – KYKLADEN TÖRNFÜHRER DELIUS KLASING VERLAG P52028_Toernfüher_Griechenland_2_3_CC21.indd 3 08.03.21 14:44 5 INHALT Vorwort ...................................................... 6 Einführung ................................................... 7 Informationen vor der Reise ....................................... 8 Formalitäten ................................................... 9 Was man auch noch wissen sollte .................................. 12 Seekarten und Seebücher ........................................ 17 Wind und Wetter ............................................... 17 Seewetterbericht .............................................. 18 Küstenfunkstellen und Seenotrettungsdienst ......................... 21 Symbole in den Plänen .......................................... 21 Attikaküste .................................................. 22 Petalischer Golf – Südlicher Euböa-Golf – Südteil von Euböa ........... 48 Kykladen .................................................... 78 Insel Andros .................................................. 79 Insel Tinos ................................................... 89 Insel Syros ................................................... 94 Inseln Mykonos, Dilos und Rineia ................................. 109 Inseln Paros, Antiparos und Despotiko ............................. 120 Insel Naxos und die Erimonisia ................................... 130 Inselgruppe -
The Sanctuary of Despotiko in the Cyclades. Excavations 2001–2012
https://publications.dainst.org iDAI.publications ELEKTRONISCHE PUBLIKATIONEN DES DEUTSCHEN ARCHÄOLOGISCHEN INSTITUTS Dies ist ein digitaler Sonderdruck des Beitrags / This is a digital offprint of the article Yannos Kourayos – Kornelia Daifa – Aenne Ohnesorg – Katarina Papajanni The Sanctuary of Despotiko in the Cyclades. Excavations 2001–2012 aus / from Archäologischer Anzeiger Ausgabe / Issue 2 • 2012 Seite / Page 93–174 https://publications.dainst.org/journals/aa/123/4812 • urn:nbn:de:0048-journals.aa-2012-2-p93-174-v4812.0 Verantwortliche Redaktion / Publishing editor Redaktion der Zentrale | Deutsches Archäologisches Institut Weitere Informationen unter / For further information see https://publications.dainst.org/journals/aa ISSN der Online-Ausgabe / ISSN of the online edition 2510-4713 Verlag / Publisher Hirmer Verlag GmbH, München ©2017 Deutsches Archäologisches Institut Deutsches Archäologisches Institut, Zentrale, Podbielskiallee 69–71, 14195 Berlin, Tel: +49 30 187711-0 Email: [email protected] / Web: dainst.org Nutzungsbedingungen: Mit dem Herunterladen erkennen Sie die Nutzungsbedingungen (https://publications.dainst.org/terms-of-use) von iDAI.publications an. Die Nutzung der Inhalte ist ausschließlich privaten Nutzerinnen / Nutzern für den eigenen wissenschaftlichen und sonstigen privaten Gebrauch gestattet. Sämtliche Texte, Bilder und sonstige Inhalte in diesem Dokument unterliegen dem Schutz des Urheberrechts gemäß dem Urheberrechtsgesetz der Bundesrepublik Deutschland. Die Inhalte können von Ihnen nur dann genutzt und vervielfältigt werden, wenn Ihnen dies im Einzelfall durch den Rechteinhaber oder die Schrankenregelungen des Urheberrechts gestattet ist. Jede Art der Nutzung zu gewerblichen Zwecken ist untersagt. Zu den Möglichkeiten einer Lizensierung von Nutzungsrechten wenden Sie sich bitte direkt an die verantwortlichen Herausgeberinnen/Herausgeber der entsprechenden Publikationsorgane oder an die Online-Redaktion des Deutschen Archäologischen Instituts ([email protected]). -
Network Biogeography of a Complex Island System: the Aegean
Journal of Biogeography (J. Biogeogr.) (2016) ORIGINAL Network biogeography of a complex ARTICLE island system: the Aegean Archipelago revisited Konstantinos Kougioumoutzis1,2*, Anna Thalassini Valli1, Elisavet Georgopoulou3, Stylianos Michail Simaiakis4, Kostas A. Triantis2 and Panayiotis Trigas1 1Laboratory of Systematic Botany, Faculty of ABSTRACT Crop Science, Agricultural University of Aim The Aegean Archipelago has been the focal research area for identifying Athens, GR-118 55 Athens, Greece, 2 and testing several ecological and evolutionary patterns, yet its biogeographical Department of Ecology & Systematics, Faculty of Biology, National & Kapodistrian subdivision has been somewhat overlooked, with the processes driving the University of Athens, GR-157 03 Athens, assembly of the Aegean island plant communities still remaining largely Greece, 3Geological-Paleontological unclear. To bridge this gap, we identify the biogeographical modules (highly Department, Natural History Museum, 1010 linked subgroups of islands and plant taxa) within the Aegean Archipelago. 4 Vienna, Austria, Natural History Museum of Location The Aegean Archipelago, Greece. Crete, University of Crete, Heraklion GR- 71409 Crete, Greece Methods We used a network approach to detect island biogeographical roles and modules, based on a large and detailed database including 1498 Aegean endemic and subendemic plant taxa distributed on 59 Aegean Islands and five adjacent mainland areas. Results The Aegean was divided into six biogeographical modules; the net- work was significantly modular. None of the modules displayed all four possi- ble biogeographical roles (connectors, module hubs, network hubs, peripherals). Six new biogeographical regions in the Aegean were identified. Main conclusions The borders of the six biogeographical regions in the Aegean correspond well to the region’s palaeogeographical evolution from the middle Miocene to the end of the Pleistocene. -
Eruptive History and 40Ar/39Ar Geochronology of the Milos Volcanic 2 Field, Greece 3
https://doi.org/10.5194/gchron-2020-30 Preprint. Discussion started: 13 October 2020 c Author(s) 2020. CC BY 4.0 License. 1 Eruptive history and 40Ar/39Ar geochronology of the Milos volcanic 2 field, Greece 3 4 Xiaolong Zhou1, Klaudia Kuiper1, Jan Wijbrans1, Katharina Boehm1, Pieter Vroon1 5 1Department of Earth Sciences, VU University Amsterdam, De Boelelaan 1085, 1081 HV Amsterdam, The Netherlands. 6 Correspondence to: Xiaolong Zhou ([email protected]) 7 Abstract. High-resolution geochronology is essential to determine the growth-rate of volcanoes, which is one of the key factors 8 to establish the periodicity of explosive volcanic eruptions. However, there are less high-resolution eruptive histories (>106 9 years) determined for long-lived submarine arc volcanic complexes than for subaerial complexes, since the submarine 10 volcanoes are far more difficult to observe than subaerial ones. In this study, high-resolution geochronology and major element 11 data are presented for Milos Volcanic Field (VF) in the South Aegean Volcanic Arc, Greece. The Milos VF has been active 12 for over 3 Myrs, and the first two million years of its eruptive history occurred in a submarine setting that has emerged above 13 sea level nowadays. The long submarine volcanic history of the Milos VF makes it an excellent natural laboratory to study the 14 growth-rate of a long-lived submarine arc volcanic complex. This study reports twenty-one new high-precision 40Ar/39Ar ages 15 and major element compositions for eleven volcanic units of the Milos VF. This allows us to refine the volcanic evolution of 16 Milos into nine phases and five volcanic quiescence periods of longer than 200 kyrs, on the basis of age, composition, volcano 17 type and location. -
Elaphe Rechingeri Werner As an Endemic Species
HERPETOLOGICAL JOURNAL, Vol. 4, pp. 91-97 (1994) NEW OBSERVATIONS ON THE ELAPHE SNAKES FROM AMORGOS (CYCLADES, GREECE) AND THE VALIDITY OF ELAPHE RECHINGERI WERNER AS AN ENDEMIC SPECIES RICHARD CLARK Vollenetoppen 3, 4800 Arenda/, Norway Three specimens of Elaphe quatuorlineata (Lacepede) and three referable to the disputed taxon E/aphe rechingeri Werner were caught on the Cycladean island ofAmorgos in April 1993. Analysis of this and earlier material collected by the author reveals the taxa are non-synonymous and separable chromatically, morphologically and in head scalation. A new definition of E. rechingeri is given. The status of E. quatuorlineata is discussed but no decision taken pending the nee� for further research. The study is presented against past debate on the Amorgos E/aphe . snakes, island phys10graphy, sympatric herpetofauna andthe urgency forconservation measures. INTRODUCTION longissima with which Wettstein (1953) was in agree ment. Wettstein however relegated it to a subspecies of The type specimen of the Amorgos rat snake Elaphe E. longissima and it is so listed in Mertens & Wermuth rechingeri, described in 1932 by Werneras a new spe (1960). Buchholz (1961) examined the type and came cies endemic to the island of Amorgos, remained the to the conclusion that it stood nearer to E. only documented record of a snake of the genus Elaphe quatuorlineata than E. longissima, a viewpoint with from this island until 1966. In that year I collected two which Wettstein (1963) concurred afterreapprai sal. adult snakes of this genus on Amorgos, one agreeing The revelation in 1966 that there were two Elaphe with Werner's description of E. -
Paros Island Cyclades Islands Paros Sifnos Folegandros Santorini Amorgos Paros 7 Days Charter Sample Itinerary
7 DAYS SAMPLE ITINERARY STARTING FROM PAROS ISLAND CYCLADES ISLANDS PAROS SIFNOS FOLEGANDROS SANTORINI AMORGOS PAROS 7 DAYS CHARTER SAMPLE ITINERARY Please note that these is only to give you an idea. The final route will be decided on board in coordination with the Captain, tailor made to your preferences and the weather conditions at that time. THESSALONIKI THASSOS SAMOTHRAKI LIMNOS CORFU PSATHOURA SYVOTA GIOURA VOLOS KYRA PARGA PANAGIA PIPERI PAXOS ALONISSOS ANTIPAXOS PERISTERA SKIATHOS LESVOS SKOPELOS SKANTZOURA PREVEZA SPORADES IONIAN ISLANDS SEA SKYROS LEFKAS MEGANISI KALAMOS ARKOUDI KASTOS PSARA ATOKOS ITHAKA CHIOS NAFPAKTOS TRIZONIA GALAXIDI ANTIRIO RIO PATRA KEFALONIA KORINTHIAN GULF IONIAN ISLANDS ATHENS KYLLINI KORINTHOS ANDROS ZAKYNTHOS LAVRION AEGINA SAMOS KATAKOLO PELOPONNESE ANAVYSSOS AEGEAN AGHISTRI SOUNION ΜΟΝΙ SEA EPIDAVROS SARONIC METHANA KEA IKARIA NAFPLION GULF TINOS FOURNI POROS MYKONOS DELOS ASTROS KYTHNOS SYROS ARKI ARGOLIC RINIA PORTO ERMIONI GULF HELI PATMOS LIPSI KYPARISSIA DOKOS HYDRA SPETSES CYCLADES LEROS LEONIDION SERIFOS ISLANDS DONOUSA PAROS PROTI NAXOS KALAMATA LEVITHIA SIFNOS ANTIPAROS VOIDIKOILIA KALYMNOS KYPARISSI DESPOTIKO KEROS PSERIMOS PANTERONISIA PYLOS SCHINOUSA KOUFONISIA KOS HERAKLIA AMORGOS METHONI GERAKAS KORONI MYRTOAN KIMOLOS SEA POLYAIGOS GYTHION IOS SIKINOS DODECANESE MONEMVASIA MILOS ISLANDS XIFIAS FOLEGANDROS ASTYPALEA SIMI AG. FOKAS NISYROS NEAPOLI ELAFONISOS KASTELORIZO TILOS SANTORINI ANAFI SYRNA RHODES KYTHERA CHALKI ANTIKYTHERA KARPATHOS KASSOS CRETE CYCLADES PAROS ISLAND Paros is so fascinating on so many levels that many people love it having seen only one of its faces. Don’t jump to conclusions about what you like, get to know the island first and find your “own” Paros, the face that suits you best. No doubt, though, it will charm you even if you see a different side from the one expected. -
Morphotectonic Analysis Along the Northern Margin of Samos Island, Related to the Seismic Activity of October 2020, Aegean Sea, Greece
geosciences Article Morphotectonic Analysis along the Northern Margin of Samos Island, Related to the Seismic Activity of October 2020, Aegean Sea, Greece Paraskevi Nomikou 1,* , Dimitris Evangelidis 2, Dimitrios Papanikolaou 1, Danai Lampridou 1, Dimitris Litsas 2, Yannis Tsaparas 2 and Ilias Koliopanos 2 1 Department of Geology and Geoenvironment, National and Kapodistrian University of Athens, Panepistimioupoli Zografou, 15784 Athens, Greece; [email protected] (D.P.); [email protected] (D.L.) 2 Hellenic Navy Hydrographic Service, Mesogeion 229, TGN 1040 Cholargos, Greece; [email protected] (D.E.); [email protected] (D.L.); [email protected] (Y.T.); [email protected] (I.K.) * Correspondence: [email protected] Abstract: On 30 October 2020, a strong earthquake of magnitude 7.0 occurred north of Samos Island at the Eastern Aegean Sea, whose earthquake mechanism corresponds to an E-W normal fault dipping to the north. During the aftershock period in December 2020, a hydrographic survey off the northern coastal margin of Samos Island was conducted onboard R/V NAFTILOS. The result was a detailed bathymetric map with 15 m grid interval and 50 m isobaths and a morphological slope map. The morphotectonic analysis showed the E-W fault zone running along the coastal zone with 30–50◦ of Citation: Nomikou, P.; Evangelidis, slope, forming a half-graben structure. Numerous landslides and canyons trending N-S, transversal D.; Papanikolaou, D.; Lampridou, D.; Litsas, D.; Tsaparas, Y.; Koliopanos, I. to the main direction of the Samos coastline, are observed between 600 and 100 m water depth. The Morphotectonic Analysis along the ENE-WSW oriented western Samos coastline forms the SE margin of the neighboring deeper Ikaria Northern Margin of Samos Island, Basin. -
Strike Slip Tectonics and Transtensional Deformation in the Aegean Region and the Hellenic Arc: Preliminary Results
Bulletin of the Geological Society of Greece, vol. XLVII 2013 Δελτίο της Ελληνικής Γεωλογικής Εταιρίας, τομ. XLVII , 2013 th ου Proceedings of the 13 International Congress, Chania, Sept. Πρακτικά 13 Διεθνούς Συνεδρίου, Χανιά, Σεπτ. 2013 2013 STRIKE SLIP TECTONICS AND TRANSTENSIONAL DEFORMATION IN THE AEGEAN REGION AND THE HELLENIC ARC: PRELIMINARY RESULTS Sakellariou D.1, Mascle, J.2 and Lykousis V.1 1 Institute of Oceanography, Hellenic Centre for Marine Research, Greece, [email protected], [email protected] 2 Observatoire Océanologique de Villefranche, France, [email protected] Abstract Recently acquired offshore seismic and swath bathymetry data from the Hellenic Arc, the Ionian Sea and the South and North Aegean Sea, including the Hellenic Volcanic Arc and the Cyclades plateau, along with geological and tectonic data from Plio-Quaternary basins exposed on the Hellenic Arc indicate that strike slip tectonics has played a major role in the southwestward extension of the Aegean crustal block, the development of the offshore neotectonic basins and the spatial dis- tribution of the volcanic activity along the Volcanic Arc. Transtensional defor- mation, accommodated by (sinistral or dextral) strike slip zones and related exten- sional structures, prevail throughout Plio-Quaternary, since the North Anatolian Fault broke westwards into the North Aegean. Incipient collision of the Hellenic Forearc south of Crete with the Libyan promontory and consequent lateral escape tectonics led to the segmentation of the Hellenic Arc in distinct blocks, which