Sifnos, Milos Et Kimolos, Merveilles Cycladiques
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And Macedonia (Pp
Summer 2018 - Greece (pp. 1-9) and Macedonia (pp. 9 -16) - Elly’s notes I traveled to Greece for a second summerschool (see here for the first). I left Arizona on a Monday morning and arrived in Thessaloniki on Tuesday afternoon before traveling on to Naxos on Wednesday. Thessaloniki is the second largest city in Greece and the capital of the Greek province of Macedonia. After Naxos, I would be traveling to the Republic of Macedonia which, under Greek pressure, may be changing its name to the Republic of Northern Macedonia (more below). Of course, some Greek nationalists don’t want the name Macedonia mentioned at all and some Macedonians don’t like the change either. When I was here, a scandal erupted of meddling by the Russians who don’t want this `deal’ either since it will pave the way for Macedonia to join NATO. Thessaloniki was built and rebuilt many times: it went from a pre-historic settlement to Macedonian, Roman, Byzantine, and Ottoman rule. Its fire in 1917 made it possible to plan a new city (see picture below). It was on the Via Egnatia (as is Ohrid) which connected Rome to Istanbul and is now a footpath. Old city walls are still around. Thessaloniki’s grid Typical building 1 More varied building styles Thessaloniki citywalls From Thessaloniki, I went to Naxos for the summer school (with some 35 participants some of whom are shown below). Naxos continues to be a wonderful place: lots of history, swimming, and hiking. Some highlights follow below. Summer school (these two pictures are by Kristel Fischer) 2 Moni Chrisostomou overlooks the chora of Naxos; two nuns remain in the monastery, which has a most beautiful church. -
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 - Greece 7 Days Charter Itinerary Cyclades - Greece 2
Cyclades - Greece 7 days Charter Itinerary Cyclades - Greece 2 Tessaly Evia GREECE TURKEY North Aegean Attica Andros Piraeus Aegina Kea Tinos Poros Mykonos Kythnos Syros Delos Peloponnese Hydra Spetses Seriphos Aegean Sea Paros Naxos Sifnos Milos Schinoussa Kos Ios Santorini Cyclades - Greece 3 Ports and distances Day Ports Distance in n.m. 1 Athens-Kea 49 2 Kea-Tinos-Mykonos 63 3 Mykonos-Delos-Paros 32 4 Paros-Ios-Santorini 73 5 Santorini-Milos 51 6 Milos-Sifnos 29 7 Sifnos-Seriphos-Kythnos 45 8 Kythnos-Piraeus 53 Total distance - 395 n.m. Cyclades - Greece 4 Athens Te Capital of Greece. Within the sprawling city of Athens it is easy to imagine the golden age of Greece when Pericles had the Parthenon (the most eminent monument of the ancient Greek architecture) built. Athens is built around the Acropolis and the pinnacled crag of Mt. Lycabettus, which the goddess Athena was said to have dropped from the heavens as a bulwark to defend the city. Te suburbs have covered the barren plain in all directions and the city is packed with lively taverns and bustling shops. Cyclades - Greece 5 Kea An exceptionally picturesque island. On the south side of Nikolaos Bay - which was a pirate stronghold in the 13th c. - is the little port of Korissia, built on the side of ancient Korissia. Tere are remains of the ancient town walls and a Sanctuary of Apollo. Te famous lion - carved from the native rock in the 6th c. BCE - can be seen just north-east of Kea town. Another highlight is the beautiful anchorage of Poleis. -
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. -
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. -
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. -
Accommodation | Rooms in Sifnos A/A Name Phone Email Address Coordinates 1 Test Property +3021021021 My.Cloudflare
Accommodation | Rooms in Sifnos A/A Name Phone Email Address Coordinates 1 Test Property +3021021021 my.cloudflare. Athens 37.983917,23. 0 domains@gm 7293599 ail.com 2 Iliofegaro +30 22840 info@iliofegar Kamares 36.991847625 Rooms 33595 o.com 128,24.68206 2279684 3 Nymfes +30.22840 info@nymfes. Kamares 36.992404630 31269 gr 714,24.68183 6974127 4 Mosha +30 22840 info@moshasi Kamares 36.992391776 Pension 31269 fnos.gr 785,24.68176 7236693 5 Akrogiali 22840 31269 info@akrogiali Platis Gialos 36.931638302 Pension sifnos.gr 954,24.72899 8234255 6 Kamaroti 22840 32069 info@kamarot Artemonas 36.980059144 Suites Hotel i.com 538,24.73446 6469928 7 Kampos 22840 31439 info@kampos Apollonia 36.976720512 Home home.gr 334,24.72263 6132927 8 Prasini Gonia 2284071247 margaritasirig Platis Yialos 36.934223961 [email protected] 439,24.73467 om 9152948 9 Holiday Home holidayhomesi Apollonia 36.977539043 Apollonia fnos@noemail 413,24.72502 Sifnos Cycl .com 8663368 with Fireplace IX 10 Casa Selene casaselenesif Apollonia 36.972546295 Sifnos nos@noemail. 454,24.72773 com 2330055 11 Lazarou 22840 71210 lazarousifnos Platis Gialos 36.926831232 Beach @hotmail.com 105,24.72547 Apartments 3811609 12 Aristeides - 2284071252 iriniathimariti Platis Gialos 36.932133572 Moscha & @gmail.com 689,24.73014 Accommodation | Rooms in Sifnos A/A Name Phone Email Address Coordinates Apartments 2284071319 2196399 13 Agnanti & 22840 32314 info@agnanti- Kastro 36.976294611 Agnanti sifnos.gr 688,24.74107 Traditional 9514789 14 Nikoletta 22840 31538 nikoletagiama Apollonia 36.972222719 -
Sailing in the Cyclades 2022
BEARING TRUE SOUTH PC Lykourgou 16, 19016, Artemis, Attica, Greece G.N.T.O. Number: 0208E60000443301 VAT Number 800622939 www.bearingtruesouth.com [email protected] +30 229 404 9993 +30 697 743 3391 +30 698 416 9994 SAILING IN THE CYCLADES CONTENTS 1. SAMPLE ITINERARY 2. OUR FLEET 3. WHAT PEOPLE SAY ABOUT US 4. OUR CANCELLATION POLICY 5. PRICING AND AVAILABILITY FOR 2022 1. SAMPLE ITINERARY Contents A. Tour Overview B. Tour Highlights C. Sample Day to Day Itinerary D. Extra Information E. Tour Information F. What’s Included / Not included A. Tour Overview One of the most famous archipelagos in the world, the Cyclades have way more to offer than pristine beaches, crystal clear waters and amazing sailing experiences. They are the cradle of over ten millennia of rich history, boast extreme geographical diversity, abundant marine wildlife and feature the best of traditional Aegean architecture and Mediterranean cuisine. This sailing adventure goes far beyond mere island hopping, giving you a chance to explore way beyond each island's marina, as well as immerse in local culture, savor the local flavors and learn a thing or two about the history of this immensely beautiful part of the world. And did we mention that it provides you with the opportunity to actively engage yourself in sailing, whether you have done it before or not? The Aegean archipelago, with its clear deep blue waters, is the ideal place to get acquainted with the basics of sailing and our skippers are always happy to show you the ropes! B. Tour Highlights ● Immerse -
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.