Paros Island Cyclades Islands Paros Sifnos Folegandros Santorini Amorgos Paros 7 Days Charter Sample Itinerary
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Announcement
ANNOUNCEMENT Application of Residential Off-Peak Rates during winter 2017-2018 Residential Off-peak rates will apply between 01.11.2017 and 30.04.2018 as follows: 1. For residential users registered: in all Municipalities and Communities across the Prefecture of Attica in the wider regions of: Agrinio, Aiginio, Aigio, Aitoliko, Aktio, Alexandroupoli, Almyros (Magnisia), Amaliada, Amyntaio, Amfiklia, Amfilochia, Amfissa, Axioupoli, Argos, Arta, Astros, Veria, Volos, Giannitsa, Grevena, Didimoticho, Distomo, Domokos, Drama, Edessa, Elassona, Eliki, Epidavros, Igoumenitsa, Zakynthos, Thiva, Iasmos, Ioannina,.Kavala, Kalamata, Kalambaka, Kanalaki, Karditsa, Karpenisi, Kassandria, Kastoria, Katerini, Kefallonia, Kiato, Kilkis, Kozani, Komotini, Korinthos, Kranidi, Kyparissia, Lagadas, Lagadia (Arkadia), Lamia, Larisa, Lefkada, Livadia, Nikiti, Methana, Metsovo, Molaoi, Moudania, Nafpaktos, Nafplio, Naousa, Nevrokopi, Xanthi, Xylokastro, Patra, Platamonas, Polygyros, Preveza, Provatonas, Ptolemaida, Pylos, Pyrgos, Oinofyta, Orestiada, Servia, Serres, Sidirokastro, Sofades, Skala, Skydra, Sparti, Stageira, Stylida, Schimatari, Trikala, Tripoli, Florina in the islands of Evia, Kea, Corfu, Skiathos, Skopelos and Alonnisos there will be two different off-peak periods: 1.1. Continuous time (23:00–07:00): applies for 8 hours, for consumers who are already using this option and wish to keep it as is. 1.2. Split time, i.e. 2 hours in the afternoon (15:00-17:00) and 6 hours in the evening (02:00–08:00) - 8 hours total. Applies for: Consumers who used the 02:00-08:00 and 15:00-17:00 option until 30.04.2017. New consumers/applicants of off-peak rates. Users of this category can use this option only. Consumers who use the continuous option but wish to move to the split-hour option (users of this category will not be able to return to the continuous option). -
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. -
Cupellation at Kea: Investigating Potential Applications of the Minoan Conical Cup
Cupellation at Kea: Investigating Potential Applications of the Minoan Conical Cup A Thesis Presented to the Faculty of the Graduate School of Cornell University in Partial Fulfillment of the Requirements for the Degree of Master of Arts by William Joseph Mastandrea February 2016 © 2016 William Joseph Mastandrea ABSTRACT For several decades, a full understanding of the Minoan Conical cup, its uses, and the social environment in which it was used has remained largely a mystery. Appearing first in the Early Minoan Period (EM; 31002100/2050 BCE), the conical cup seems to have been a vessel which was prevalent in the daily life of those living in the Bronze Age Aegean. It is not until the Late Minoan Period (LM; 1700/16751075/1050 BCE), that the conical cup production standardizes and vessels are found in large concentrations across the Aegean from Crete, Kea, Kythera, and Melos, to Thera, Mainland Greece, and portions of Western Anatolia (Gillis 1990b, 1). Yet over the past thirty years, physical descriptions and discussions of production of the conical cups have outnumbered explanations of their use and influence. Studies of standardization (Davis 1985; Gillis 1990b; Gillis 1990c; Berg 2004; Hilditch 2014), transmission (Gillis 1990a; Gillis 1990c; Knappett 1999) and regional distribution (Wiener 1984; Gillis 1991a; Gillis 1990b; Wiener 2011) are more numerous than those which address questions surrounding their use (Schofield 1990b). This thesis seeks to understand the spatial distribution and application of the handleless cup/conical cup in daily social practices taking place in the context of House A at Ayia Irini, Kea during the Period VI occupation (LM IA, LH I, LC I)1. -
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. -
Chronological Constraints of Pyroclastic Deposits on Anafi Island
15th International Congress of the Geological Society of Greece Athens, 22-24 May, 2019 | Harokopio University of Athens, Greece Bulletin of the Geological Society of Greece, Sp. Pub. 7 Ext. Abs. GSG2019-160 Chronological constraints of pyroclastic deposits on Anafi Island, (Cyclades, Greece): Are they Minoan? Katerina Theodorakopoulou1, Konstantinos Kyriakopoulos1, Kostas Stamoulis2, Magali Rizza3, Roberto Sulpizio4, M. Cihat Alçiçek4, Constantin D. Athanassas6 1 Department of Geology and Geoenvironment, National and Kapodistrian University of Athens, Greece, [email protected] 2 University of Ioannina-Archaeometry Center, Greece 3 Centre Européen de Recherche et d’Enseignement des Géosciences de l’Environnement, Aix-en-Provence, France 4 Department of Earth and Geo-environmental Sciences, University of Bari Aldo Moro, Italy, 5 Department of Geology, Pamukkale University, Denizli, Turkey 6 Department of Geological Sciences, School of Mining and Metallurgical Engineering, National Technical University of Athens, Greece This study attempts to clarify whether formerly-documented pyroclastic deposits (Keller et al. 2014, McCoy and Dunn, 2002) belong to the Minoan eruption of Santorini or an earlier event. The ‘Minoan’ eruption, occurred in the 17th century BCE (1627–1600 BCE, Friedrich et al., 2006) and had widespread impacts on the civilization of the Aegean an Eastern Mediterranean (Marinatos, 1939). Anafi Island could be a key site for the dispersal of Minoan tephra as it is the most nearby island of Santorini. Despite its proximity, only a few spots with pyroclastic deposits have been found on the island (Keller et al. 2014, McCoy and Dunn, 2002). The occurrence of tephra layers of the Minoan eruption on Rhodes, Kos and western Turkey (Keller, 1980; Eastwood et al., 1999), suggests that Anafi must have covered by Minoan tephra, which was probably eroded and swept away afterwards (Keller et al., 2014). -
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. -
THE DONOUSA MIRACLE a Scientist Bio-Interview with Prof
THE DONOUSA MIRACLE A Scientist Bio-Interview with Prof. Leonidas A. Papakonstantinidis. https://www.researchgate.net/profile/Leonidas_Papakonstantinidis https://researchleap.com/wp- content/uploads/2018/02/04_A_Social_Welfare_Economics_Proposal.edited.pdf Interviewer: Stephen I. Ternyik, Techno-Logos, Inc. (-1985) https://www.sociostudies.org/authors/ternyik_stephen_i/ Sudden mind changes seem to happen by a rapid transformation of the heart beat frequency. Such a deep psychological moment happened to you, when you visited Donousa island in 1979. You came as developmental and academic bureaucrat from the capital (Athens) and you were a bit over 30 years. What did strike you, the young careerist, so much, in that geo-meta-physical location? Yes, I came as a developmental and academic bureaucrat (Agricultural Bank of Greece, Direction of Studies and Planning) from the capital Athens to report on the small Cyclades-Aegean islands, and I started from Donousa. My turning point in the mind was a scene with the mute coachman driving the mule, as opposed to the limousine, which took us from Brussels airport to the building of the European Commission, called the Berlaymont. This was the period (1976-1979) of Greece’s accession to the EEC (now EU). The population of Donousa was fully isolated from what is called ‘quality of life’ or standard of living. I had no idea on how these people faced their day-to- day problems, especially those related to health. No electricity, no water, no infrastructure, no roads, no official port; it was a boat that brought guests to the island. It then literally clicked in me, and I refused my predetermined career, while all other bank direction members (27) became high profile academics or politicians. -
Travel Itinerary for Your Trip to Greece Created by Mina Agnos
Travel Itinerary for your trip to Greece Created by Mina Agnos You have a wonderful trip to look forward to! Please note: Entry into the European countries in the Schengen area requires that your passport be valid for at least six months beyond your intended date of departure. Your Booking Reference is: ITI/12782/A47834 Summary Accommodation 4 nights Naxian Collection Luxury Villas & Suites 1 Luxury 2-Bedroom Villa with Private Pool with Breakfast Daily 4 nights Eden Villas Santorini 1 Executive 3-BR Villa with Outdoor Pool & Caldera View for Four with Breakfast Daily 4 nights Blue Palace Resort & Spa 1 2 Bedroom Suite with Sea View and Private Heated Pool for Four with Breakfast Daily Activity Naxos Yesterday & Today Private Transportation Local Guide Discover Santorini Archaeology & Culture Private Transportation Entrance Fees Local Guide Akrotiri Licensed Guide Knossos & Heraklion Discovery Entrance Fees Private Transportation Local Guide Spinalonga, Agios Nikolaos & Kritsa Discovery Entrance Fees Private Transportation Local Guide Island Escape and Picnic Transportation Private Helicopter from Mykonos to Naxos Transfer Between Naxos Airport & Stelida (Minicoach) Targa 37 at Disposal for 8 Days Transfer Between Naxos Port & Stelida (Minicoach) Santorini Port Transfer (Mini Coach) Santorini Port Transfer (Mini Coach) Transfer Between Plaka and Heraklion (Minivan) Transfer Between Plaka and Heraklion (Minivan) Day 1 Transportation Services Arrive in Mykonos. Private Transfer: Transfer Between Airport and Port (Minivan) VIP Assistance: VIP Port Assistance Your VIP Assistant will meet and greet you at the port, in which he will assist you with your luggage during ferry embarkation and disembarkation. Ferry: 4 passengers departing from Mykonos Port at 04:30 pm in Business Class with Sea Jets, arriving in Naxos Port at 05:10 pm. -
Evolution of the Serifos Metamorphic Core Complex
Journal of the Virtual Explorer, 2007 Volume 27 Paper 2 http://virtualexplorer.com.au/ Evolution of the Serifos Metamorphic Core Complex Bernhard Grasemann Department of Geodynamics and Sedimentology, University of Vienna, Austria ([email protected]) K. Petrakakis Department of Geodynamics and Sedimentology, University of Vienna, Austria Keywords: Aegean, Cyclades, Serifos, metamorphic core complex, plutonism, low-angle normal fault, high-angle normal fault Evolution of the Serifos Metamorphic Core Complex Page 1 Journal of the Virtual Explorer, 2007 Volume 27 Paper 2 http://virtualexplorer.com.au/ Abstract: Serifos is located in the Aegean Sea, 100 km southeast of Athens and belongs to the Cycladic Islands. Geologically, Serifos belongs to the Attic-Cycladic massif and the island is largely dominated by a Late Miocene shallow-level I-type granodiorite pluton in the central and SE portion of the island. The pluton intruded into mylonitized orthogneisses, amphibolites, schists, calc-silicates, marbles and marble meta-conglom- erates. Because the host-rocks near the largely undeformed granodiorite pluton contain weakly deformed Ca-Fe-Mg high-temperature skarns, Fe-ores and extensive hydrother- mal alteration, the intrusion has been generally considered to be post-tectonic. Although the granodiorite intrusion clearly crosscuts the regional metamorphic fabric, the uppermost structural levels of the granodiorite, together with its host-rocks, are strongly overprinted by networks of greenschist-facies to cataclastic shear zones that record a notably consistent stretching lineation direction, associated with non-coaxial SSW-directed shear. The immediate host-rocks near the intrusion are mainly mylonitic orthogneisses and amphibolites that were highly deformed at temperatures > 450 °C. -
Greeka Guide to Anafi
Anafi in Cyclades Information about villages, beaches, sightseeing, restaurants, activities and more... All the information is this guide is sorted by popularity. For more information please visit our section of Anafi on Greeka.com. What is Greeka.com? Greeka.com is just the most popular website about Greece and the Greek Islands. What to do after you trip? Just visit www.greeka.com and write about your experience, rate the locations you visited and upload your pictures. Map of Anafi Organize your trip to Anafi Greeka.com can also help you organize your entire holiday in Anafi. Thousands of people use our services every year. You can use Greeka.com to: - Buy your ferry tickets online - Book your car rentals - Organize your transfers by taxi and bus - Create a custom island hopping package - Visit Greek areas in an organized tour Anafi p 2/6 Anafi Guide About Anafi Anafi is a small island, located to the east of Santorini. Its shape is triangular and its land is mostly rocky. This island, because of its size, hasn't been too much developed in tourism so it is a great destination for peace and quiet seekers. According to the myth, Anafi rose from the sea to provide shelter for the Argonatus and to protect them from the wild sea. It has got a semi-mountainous structure with Vigla, Kalamos and Agios Ioannis Theologos being their highest peaks. Anafi has many beaches, most of them with fine soft sand and some others pebbled. The port of Agios Nikolaos is the busiest part of Anafi.