Elaphe Rechingeri Werner As an Endemic Species
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Îles Grecques – Les Cyclades Et Athènes
Îles grecques Les Cyclades et Athènes Y VOIR L’ESSENTIEL M VIVRE LE MEILLEUR Marathonas Elefsina (Éleusis) ATHÈNES Megara p.46 Rafina Karistos Pireas (Le Pirée) SALAMINA + ANDROS ATHÈNES AU QUOTIDIEN / Gavrio L’ACROPOLE / Andros MUSÉE ARCHÉOLOGIQUE NATIONAL MAKRONISSI Egina G OLFE SA RONIQ Lavrio ANGISTRI UE KEA Korissia GIAROS Methana CAP Ioulida SOUNION P Poros É LO PO N POROS NÈ Ermo SE Merichas SYROS+ Hydra DOKOS KYTHNOS M SERFOPOULA E R D SERIFOS E Livadi M Y R T ANTIPAR O Kamares Apollonia CYCLADES OCCIDENTALES +SIFNOS DESPOTIK VELOPOULA p.164 KIMOLOS FALKONERA ANTIMILOS Plaka POLIEGOS Adamas MILOS Folegandros FOLEGANDROS+Karavosta TURQUIE E OP LES CYCLADES EUR ET ATHÈNES IRA GRÈCE ASIE AFRIQUE M E R É G É Gavrio ANDROS E Andros CYCLADES SEPTENTRIONALES p.98 GIAROS +TINOS IKARIA Tinos Mykonos Ermoupoli + SYROS+ MYKONOS RINIA + DELOS LA Naxos DONOUSSA Parikia + ANTIPAROS NAXOS s KINAROS Apollonia KOUFONISSIA +SIFNOS PAROS KEROS DESPOTIKO +AMORGOS IRAKLIA Katapola Amorgos SCHINOUSSA LIEGOS SIKINOS IOS Ios Kastro Alopronia Folegandros ANUDROS ANDROS+Karavostassis ASTIPALEA CYCLADES ORIENTALES p.206 Oia FIRASSIA ANAFI Fira + Anafi SANTORIN CHRISTIANI N 25 km Îles grecques Les Cyclades et Athènes BIENVENUE DANS LES… es maisons chaulées de blanc dégringolant d’une colline, vers une mer d’un bleu aussi D intense que l’azur du ciel… Voici l’image éternelle des Cyclades, archipel aux 250 îles de toutes tailles disséminées dans la mer Égée. Chacune pourrait être une perle d’un komboloï, ce chapelet grec dont le nœud de fixation serait Athènes, la capitale, berceau culturel de l’Europe, sur laquelle veille la silhouette mythique de l’Acropole. -
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. -
The Primal Greece : Between Dream and Archaeology
The primal Greece : between dream and archaeology Introduction The Aegean civilisations in the French National Archaeological Museum « This unusual form […] reveals an unknown Greece within Greece […] as solemn, profound and colossal as the other is radiant, light and considered; […] all here meets the reputation of the Atrids and brings back the horror of the Achaean fables », wrote on 1830 in front of the walls of Mycenae, the traveller Edgard Quinet, who was passionate about Greek tragedies. Like other travellers before him, he was aware of approaching the memory of an unknown past, of a primal Greece, but he would never have believed that this Greece dated from prehistoric times. It will be the end of the 19th century before the pioneers of archaeology reveal to the world the first civilisations of the Aegean. The « Museum of National Antiquities» played then a key role, spreading the knowledge about these fabulous finds. Here, as well as in the Louvre, the public has been able to meet the Aegean civilisations. The Comparative Archaeology department had a big display case entirely dedicated to them. The exhibition invites visitors back to this era of endless possibilities in order to experience this great archaeological adventure. Birth of a state, birth of an archaeology As soon as it becomes independent (1832), Greece is concerned with preserving its antiquities and creates an Archaeological Service (1834). Shortly afterwards, Ephemeris Archaiologike, the first Greek archaeological review, is founded, at the same time as the Archaeological Society at Athens. The French School at Athens is founded in 1846 in order to promote the study of antiquities, and is followed by a German study Institute in 1874; many other countries will follow the example of France and Germany. -
CYCLADES 1 WEEK Dazzling White Villages, Golden Beaches and Clear Azure Water Are Just the Start of What These Islands Have to Offer
Hermes Yachting P.C. 92-94 Kolokotroni str., 18535 Piraeus, Greece Tax No. EL801434127 Tel. +30 210 4110094 E-mail: [email protected] Web: www.hermesyachting.com CYCLADES 1 WEEK Dazzling white villages, golden beaches and clear azure water are just the start of what these islands have to offer. Within easy reach of Athens, these are the Aegean’s most precious gems. Ancient Greek geographers gave this unique cluster of islands the name Cyclades because they saw that they formed a circle (kyklos) of sorts around the sacred island of Delos. According to myth, the islands were the debris that remained after a battle between giants. In reality, they resulted from colossal geological events like earthquakes and volcanic eruptions. Their colours are blue and white like the Greek flag. The islands come in all sizes and, though the ingredients are the same – incomparable light, translucent water, heavenly beaches, lustrous white buildings and bare rock, each one has its own distinct character. The group’s stars, Mykonos and Santorini, need no introduction but the lesser-known islands, big and small, are just as rewarding. For starters, try aristocratic Syros, cosmopolitan Paros, the sculptors’ paradise of Tinos, bountiful Naxos, exotic Milos and historic Delos, not to mention the ‘hidden gems’ that adorn the Aegean, such as Tzia/Kea, Kythnos, Sifnos, Serifos, Amorgos, Sikinos, Anafi and Folegandros. Whether you’re travelling with your family, friends or sweetheart, you’re bound to find your summer paradise in the sun in the Cyclades. Beaches of indescribable beauty in the Cyclades What’s your idea of the perfect beach? Green-blue water and white sand? Beach bars and water sports? Framed by rocks for snorkelling and scuba diving? Is a secret Aegean cove accessible only on foot or by boat? No matter what your ideal is, you’ll find it in the Cyclades. -
Seismotectonic Setting of Santorini-Amorgos Zone and the Surrounding Area Revealed from Crustal Earthquakes Relocation and Vp/Vs Distribution
EGU2020-6589 https://doi.org/10.5194/egusphere-egu2020-6589 EGU General Assembly 2020 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Seismotectonic setting of Santorini-Amorgos zone and the surrounding area revealed from crustal earthquakes relocation and Vp/Vs distribution Ratri Andinisari1, Konstantinos I. Konstantinou1, Pratul Ranjan1,2, and Qori F. Hermawan1 1Department of Earth Sciences, National Central University, Chungli, Taoyuan, Taiwan 2Taiwan International Graduate Program–Earth System Science (TIGP–ESS), Taipei, Taiwan The Santorini-Amorgos zone represents right-lateral transtensional regime from NE of Santorini to the south of Amorgos which also hosts Kolumbo submarine volcano. A total number of 1869 crustal events from 2002 to 2019 were recorded by permanent and temporal seismic networks deployed in southern Aegean. Absolute locations of these events were obtained by utilizing the probabilistic nonlinear algorithm NonLinLoc. Precise relative relocation by using double-difference algorithm with catalog and cross-correlation differential times was later performed, resulting in 1455 locations with horizontal and vertical uncertainties of less than 0.3 km. Clusters of earthquakes relocated between Naxos and Paros as well as north of Astypalaia do not coincide with any fault in the area. Similarly, the relocated crustal events across Santorini-Amorgos zone show that most of the earthquake clusters do not coincide with any of the existing faults. The distribution of Vp/Vs ratios in the area were investigated based on the P and S-wave travel times of all the events. Vp/Vs ratios in the area vary between 1.67 and 2.03 with errors less than 0.04. -
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. -
Herpetological Notes on the Island of Amorgos (Cyclades, Greece)
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Herpetozoa Jahr/Year: 2007 Band/Volume: 20_1_2 Autor(en)/Author(s): Broggi Mario F. Artikel/Article: Herpetological notes on the island of Amorgos (Cyclades, Greece) 94-96 ©Österreichische Gesellschaft für Herpetologie e.V., Wien, Austria, download unter www.biologiezentrum.at 94 SHORT NOTE HERPETOZOA 20 (1/2) Wien, 30. Juli 2007 SHORT NOTE ment. Washington, D.C. (IUCN, Conservation Inter- (1938) who had visited the island and listed national, NatureServe) [Accessed on December 2006]. McDiARMiD, R. W. & ALTIG, R. (1990): Description of from Amorgos what he called Bufo viridis a bufonid and two hylid tadpoles from western LAURENT], 1768, Rana ridibunda PALLAS, Ecuador.- Alytes, Paris; 8 (2): 51-60. METTER, D. E. 1771, Gymnodactylus kotschyi STEINDACH- (1964): A morphological and ecological comparison of NER, 1870, Hemidactylus turcicus (LINNAE- two populations of the tailed frog, Ascaphus truei STEJNEGER.-Copeia, Washington, D.C.; 1964: 181-195. US, 1758), Lacerta erhardi amorgensis WER- NUSSBAUM, R. A. & BRODIE, E. D., Jr. & STORM, R. M. NER, 1933, Eryx jaculus (LINNAEUS, 1758) (1983): Amphibians and reptiles of the Pacific north- and Elaphe rechingeh WERNER, 1933. He west. Idaho (University Press of Idaho), 168 pp. RON, believed to have seen also Laudakia stellio S. R. & CANNATELLA, D. C. & COLOMA, L. A. (2004): (LINNAEUS, Two new species of Physalaemus (Anura: Leptodacty- 1758), but the presence of this lidae) from western Ecuador.- Herpetologica, Johnson species was never confirmed. Mauremys ri- City; 60: 261-275. SAVAGE, J. M. (2002): The amphib- vulata (VALENCIENNES, 1833) was cited by ians and reptiles of Costa Rica. -
Contemporary Kinematics of the South Aegean Area (Greece) Detected with Continuous GNSS Measurements
EGU2020-7656, updated on 03 Oct 2021 https://doi.org/10.5194/egusphere-egu2020-7656 EGU General Assembly 2020 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Contemporary Kinematics of the South Aegean Area (Greece) Detected with Continuous GNSS Measurements Vassilis Sakkas, Chrysa Doxa, Andreas Tzanis, and Haralambos Kranis National & Kapodistrian University of Athens, Department of Geology and the Geoenvironment, Athens, Greece ([email protected]) We examine the kinematic characteristics of the crustal deformation in the broader southern Aegean region using 47 permanent GNNS stations distributed across the eastern Peloponnesus, Attica, Cyclades, Dodecanese, Crete and the coast of western Anatolia. Our analysis is based on the study of velocity vectors relative to local reference points at the western and eastern halves of the study area, as well as on the strain field calculated from absolute velocity vectors across the study area. We demonstrate that the South Aegean region undergoes complex distributed block deformation. At the eastern end of the study area this varies from N210°-N220° extension and with crustal thinning across NE Peloponnesus – Attica, to N210°-N220° compression between the central- eastern Peloponnesus and western Crete, both consistent with the geodynamic setting of the Hellenic Subduction System. A principal feature of the S. Aegean crust appears to be a broad shear zone extending between the islands of Samos/Ikaria and Kalymnos, Paros/Naxos and Amorgos and Milos – Santorini; It exhibits left-lateral kinematics and its southern boundary appears to coincide with the Amorgos – Santorini ridge and comprise the Anhydros basin and associated volcanic field (including Columbo and Santorini). -
View Our Greece Brochure
Greece Nowhere else in the world are the grand sweep of history and the magnificence of nature so intertwined as in Greece. Journey to the birthplace of Western civilization; where the sparkling azure waters of the Aegean Sea create a beautiful backdrop to it all. Athens is a spellbinding destination, with the majestic Acropolis looking down upon the city. A thriving metropolis has risen around these treasured ruins, where the days of exploration through the remains of Greece’s golden age lead to nights filled with fine cuisine, glittering nightclubs and soulful music. Greece WorthAvenueYachts.com FYR BULG ARIA The Cyclades Islands MACEDONIA The most famous of the Greek Islands, the Cyclades are composed of 39 islands. The most well-known ones are ALBANIA Amorgos, Andros, Antiparos, Delos, Ios, Kea, Folegandros, Milos, Mykonos, Naxos, Paros, Santorini, Serifos, Sifnos, TH ESSALY Syros and Tinos. EPIRUS Aegean Sea TU RKEY STEREA ELLADA Athens Gulf Pira eus of Corinth Mykonos C PELO PONNESE Saronic y Gulf c la Patm os Ionian d e Sea s Must see Thira The Cyclades offer turquoise (S anto rini) Rhodes waters and white sandy beaches Sea of Crete that make them one of the finest sailing destinations worldwide. Medite rra nean Sea Crete Greece 1/8 2 3 7 4 5 6 Sample Itinerary Cyclades Island Day 1 Day 2 Day 3 Day 4 FYR BULG ARIA Athens to Kea. Expe- Kea to Tinos and Mykonos to Delos to Paros to Ios. Ios is MACEDONIA rience the Parthenon Mykonos. Be sure Paros. Stop into the the heart of the Cy- before boarding and ALBANIA to visit the Church sacred island of Delos clades and said to be starting the 4 hour of Panagia before before our short trip to the sland of youth. -
Opening Speech
II. National Symposium On The Aegean Islands, 2-3 July 2004, Gökçeada - Çanakkale OPENING SPEECH Ali KURUMAHMUT Prime Ministry of Navigation Counsellorship Marine Transportation General Manager The Aegean Sea lies between the Turkish and the Greek main lands, as well as between the Morea peninsular and the southwestern edges of the Anatolian coasts, with the extension of the islands of Çuha, Küçük Çuha, Girit, Kaşot, Kerpe and Rodos that constitute its outer natural boundaries. In terms of the geographical structure, the Aegean, a semi-closed sea, has geological and geo-morphological characteristics peculiar to itself: it has about 1800 islands, islets and rocks of various sorts, as well as a number of geographical formations, scattered al over the Sea. There is little wonder that all these characteristics make the Aegean Sea a special one. The Aegean dispute between Greece and Turkey has been complicated for a number of reasons: for instance, there are many islands in the Aegean that Turkey ceded to Greece through international treaties. And these islands lying in the natural extension of the Turkish mainland surround Anatolia from north to the south. But Athens makes claims of sovereignty over many islands, islets, and rocks though Ankara never ceded any of them to Greece officially. The most obvious and famous case would be the Kardak rocks crisis that erupted between Turkey and Greece at the beginning of 1996. These complications make the Aegean a sea that is of special importance among the seas of the world. It is possible to divide the Aegean Islands into five categories in terms of their geographical locations, geological and geo-morphological characteristics, the historical perspectives of the sovereign powers to which they belonged, the manner in which the sovereignty over them was determined through international treaties, as well as their importance for geo-political and strategic purposes. -
Sifnos, Milos Et Kimolos, Merveilles Cycladiques
TOUR INFORMATIONS Cyclades : Naxos, Amorgos /Kélifos Sunset at Portara © François Ribard at Portara © François Ribard Sunset - Naxos SUMMARY Greece • Cyclades Self guided hike 8 days 7 nights Semi-itinerant trip Nothing to carry 2 / 5 CYCLP0009 HIGHLIGHTS Hiking holidays in 2 splendid Cycladic islands from mountainous Naxos to wild Amorgos A simple paradise where an authentic everyday life prevails A good mix of walking, swimming, relaxing and visits of sites www.kelifos.travel +30 698 691 54 80 • [email protected] • CYCGP0018 1 / 15 MAP www.kelifos.travel +30 698 691 54 80 • [email protected] • CYCGP0018 2 / 15 P R O P O S E D ITINERARY Born in the mythical waters of the Aegean, these are two very different islands, in the matter of geology, landscape, and history. Naxos, the largest, is also the most wooded. Composed of granite, marble and limestone, bordered by beautiful sandy beaches near its attractive capital, Chora (6500 inhabitants), it is home to Mount Zas (1001 m), the highest peak of Cyclades islands. Amorgos is located further east. This long though narrow rocky island, lying in the sea is less populated. This fascinating island offers austere and grandiose scenery promise of sumptuous treks. This austerity is softened by the charm of the villages and the hilltop capital, Chora, with typical Cycladic architecture. Amorgos is also known for the extraordinary image of his monastery Chozoviotissa, stuck in the cliff. An image that many European people discovered in 1988 in the movie "The Big Blue". Many scenes of Luc Besson's film have been shot in Amorgos.