Gravity Observations on Santorini Island (Greece): Historical and Recent Campaigns
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Santorini the Unique World ...Land of Lava!!
Santorini the unique world ...land of lava!! Santorini is one of the best places on earth as far as sunset viewing is concerned. In fact few places can match the sheer beauty of Santorini’s sunset views. Visitor to the island fallen in love with bewitchingly beautiful sunsets that can be savored from many vantage positions in the island, such as Imerovigli. Santorini Sunsets over Caldera are the best in the world!! Santorini is perhaps the most fascinating and most talked about island of Greece in the Aegean. Only the name of the island is enough to unfold in mind pleasurable connotations, volcanic landscape, gray and red beaches, dazzling white houses, terraces with panoramic sea views, stunning sunsets, wild fun. All this, together with remnants of lost civilizations discovered in the volcanic ash justify the epithets with which visitors identify Santorini and fairly is called, magical, indescribable, astonishing. The volcano is still active, and the last eruption was in 1950, causing an earthquake which destroyed many villages on the island. The island's official name is Thira and its main town, Fira, is also the capital of the Cyclades islands. Santorini became from the local “Santa Irini”. Oia (Ia) Village is one of the most beautiful villages of the island, carved out of the cliffs and clinging to the edge. The architecture is amazing and is highlighted by the stark white of the buildings and the contrasting colorful doors and window shutters. It has often been compared to the eagle's nest! Enjoy the panoramic view of caldera, the volcano, Thirassia Island, and the rest of Santorini looking back toward the capital, Fira. -
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. -
September 2017 • Price: 2€
The Responsible Travelers’ Newspaper • #19 • September 2017 • Price: 2€ SEPTEMBER CULTURAL AGENDA SAVE AKROTIRI DR. WALTER FRIEDRICH: STRATIGRAPHY OF THE VOLCANO PASSENGERS RIGHTS MAP OF SANTORINI NEW GUIDE TO AKROTIRI HIDDEN GEMS SEPTEMBER 2017 Read & keep, recycle or pass it on to another traveler... L A A I R O O T T I D E E 02 CONTENTS Santo Traveler September 2017 Picture of the month Hidden in plain site PAGE 04 Old villages of Santorini, like Pyrgos, Em - The best way to discover them is on foot, poreio and Megalochori, located not at the using your camera and your intuition! A Major Change in the Stratigraphy PAGE of the Santorini Volcano in Greece 06 Caldera but on the hinterland, can show you the traditional architecture of Cy - PAGE SANTORINI VIDEO TOUR 2017 An Australian in Greece: Why i clades: small and narrow paths, medieval keep coming back to Greece 10 santotraveler.com/tv castles and houses with several colour PAGE Map of Santorini combinations. 12 ODYSSEYS: The new exhibition of PAGE the National Archaeological 14 Museum PAGE Passengers rights 16 SantoTraveler _The Responsible Travelers’ Newspaper Save Akrotiri: PAGE Publisher & Director: Nikos Psarros 50 yeras of excavations 18 Editorial group: Carolina Rikaki, Yannis Papafiggos, Danae Bosler, Lefteris Zorzos, Walter L. Friedrich, Annette H jen S rensen, J. Richard Wil - PAGE son, Michael Fytikas, Spyridon Pavlides, Samsoøn Katsøipis, Vangelis I. Paravas, New guide to Akrotiri Yannis Pananakis, Christos Alexandris. 20 P.O. BOX E109, Emporio, Santorini, Greece 84703 • t: +30 22860 83481 E: [email protected] • E: [email protected] September in Santorini: PAGE Cultural agenda & events santofriends 21 © 2017- 2018. -
VU Research Portal
VU Research Portal Dynamics of magma generation and differentiation in the central-eastern Aegean arc: Klaver, M. 2016 document version Publisher's PDF, also known as Version of record Link to publication in VU Research Portal citation for published version (APA) Klaver, M. (2016). Dynamics of magma generation and differentiation in the central-eastern Aegean arc: A geochemical and petrological study of Quaternary arc volcanism in Greece. General rights Copyright and moral rights for the publications made accessible in the public portal are retained by the authors and/or other copyright owners and it is a condition of accessing publications that users recognise and abide by the legal requirements associated with these rights. • Users may download and print one copy of any publication from the public portal for the purpose of private study or research. • You may not further distribute the material or use it for any profit-making activity or commercial gain • You may freely distribute the URL identifying the publication in the public portal ? Take down policy If you believe that this document breaches copyright please contact us providing details, and we will remove access to the work immediately and investigate your claim. E-mail address: [email protected] Download date: 26. Sep. 2021 10 | CHAPTER 1 INTRODUCTION | 11 12 | CHAPTER 1 Previous pages: Santorini caldera right after sunset on a clear evening as seen from Fira town where the Nea Kameni dacites, the youngest volcanic deposits, have been emplaced in the centre of the caldera. The Christiani islands can be seen in the distance. INTRODUCTION | 13 1. -
The Cryptotephta Record of the Marine Isotope
POST-PRINT The cryptotephra record of the Marine Isotope Stage 12 to 10 interval (460–335 ka) at Tenaghi Philippon, Greece: Exploring chronological markers for the Middle Pleistocene of the Mediterranean region Polina Vakhrameeva1, Andreas Koutsodendris1, Sabine Wulf1,2, William J. Fletcher3, Oona Appelt4, Maria Knipping5, Ralf Gertisser6, Mario Trieloff1, Jörg Pross1 1 Institute of Earth Sciences, Heidelberg University, Im Neuenheimer Feld 234-236, D- 69120 Heidelberg, Germany 2 Department of Geography, University of Portsmouth, Buckingham Building, Lion Terrace, Portsmouth, PO1 3HE, United Kingdom 3 Department of Geography, School of Environment, Education and Development, University of Manchester, Manchester, M13 9PL, United Kingdom 4 Helmholtz Centre Potsdam, GFZ German Research Centre for Geosciences, Section 4.3 Chemistry and Physics of Earth Materials, Telegrafenberg, D-14773 Potsdam, Germany 5 Institute of Botany, University of Hohenheim, Garbenstraße 30, D-70593 Stuttgart, Germany 6 School of Geography, Geology and the Environment, Keele University, Keele, Staffordshire, ST5 5BG, United Kingdom Keywords: Tephrostratigraphy; Italian and Aegean Arc volcanism; Marine Isotope Stages 10, 11 and 12; Eastern Mediterranean; land-sea correlation; Tenaghi Philippon Highlights: • 18 cryptotephra layers identified for the 460–335 ka interval at Tenaghi Philippon. • Major- and trace-element compositions reveal Italian and Aegean Arc sources. • One cryptotephra can be traced to the Santorini Cape Therma 1 eruption. • Nine cryptotephras originate from a yet unknown Eastern Mediterranean source. • Cryptotephra ages derived from orbitally tuned high-resolution pollen data. 1 POST-PRINT Abstract Precise chronologies that allow direct correlation of paleoclimate archives are a prerequisite for deciphering the spatiotemporal characteristics of short-term climate variability. Such chronologies can be established through the analysis of tephra layers that are preserved in the respective sedimentary archives. -
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Santorini Field Guide
MeMoVolc short course, Santorini, 2015 Field guide to Santorini Volcano T.H. Druitt (LMV, Clermont-Ferrand, France), with contributions from L. Francalanci (University of Florence, Italy) and G. Fabbro (EOS, Singapore). INTRODUCTION HISTORICAL AND GEOGRAPHICAL PERSPECTIVES Santorini has fascinated and stimulated explorers and scholars since ancient times. Jason and the Argonauts Lying in the southern Aegean sea, 107 km north of were apparently visitors to the islands and described a Crete, Santorini has played an important role in the giant called Talos. Molten metal flowed from his feet cultural development of the region and has a history of and he threw stones at them. The legend of Atlantis is occupation stretching far back in time. The traditional plausibly based upon the great Bronze-Age eruption of names of Strongyle (the round one) or Kallisti (the Santorini. The geographer Strabo described the eruption fairest one) reflect the shape and unquestionable beauty of 197 BC in the following way: of the island cluster. '…for midway between Thera and Therasia fire broke Although firm evidence of human occupation dates to forth from the sea and continued for four days, so that only 3000-2000 BCE, obsidian finds show that the the whole sea boiled and blazed, and the fires cast up volcanic Cyclades were being visited by people from an island which was gradually elevated as though by mainland Greece as early as the 7th millennium before levers and consisted of burning masses…'. Christ. By the time of the late-Bronze-Age eruption, an advanced people contemporaneous with the Minoan It was Ferdinand Fouqué (1879) who made the first civilisation on Crete was established in the ancient town detailed geological study of Santorini, distinguishing of Akrotiri, on the southern coast of the volcano. -
Temple Reuse in Late Antique Greece
Temple Reuse in Late Antique Greece Stefan Moffat Thesis submitted to the Faculty of Graduate and Postdoctoral Studies in partial fulfillment of the requirements for the Master of Arts Degree in Classics Supervisor: Dr. Geoffrey Greatrex Department of Classics and Religious Studies Faculty of Arts University of Ottawa July 2017 © Stefan Moffat, Ottawa, Canada, 2017 Abstract The subject of this thesis is the variety of ways that temples were reused by Romans, both Christian and non-Christian, at the end of Antiquity in the present-day country of Greece. It discusses these means of reuse using principally archaeological evidence as a means of countering interpretations of the material culture that temples were either destroyed or reused as churches. These interpretations are based on the assumption that contemporary written sources such as Saints’ ‘Lives’ (the literary genre known as hagiography) are an accurate portrayal of temple reuse in Late Antiquity, without taking into consideration the legendary nature of hagiography. On the other hand, they do not account for potentially contradictory evidence of temple reuse derived from archaeological excavation. It is argued in this thesis that archaeological evidence provides an alternative outcome to that described in contemporary written sources such as hagiography, one that emphasizes practical forms of temple reuse rather than religious. The evidence for this argument is presented at both a geographic level and as discreet categories of forms of reuse of both a religious and practical nature, as a first glimpse of the nuanced image of temple reuse in Greece. Specific examples of the evidence are then cited in a number of case studies to be further developed as a valid attribute in the characterisation of the Late Antique sacred landscape at the level of the Roman Empire. -
Tectonic Deformation in the Santorini Volcanic Complex (Greece) As Inferred by Joint Analysis of Gravity, Magnetotelluric and DGPS Observations
Geophys. J. Int. (2020) 220, 461–489 doi: 10.1093/gji/ggz461 Advance Access publication 2019 October 14 GJI Geodynamics and tectonics Tectonic deformation in the Santorini volcanic complex (Greece) as inferred by joint analysis of gravity, magnetotelluric and DGPS observations A. Tzanis , S. Chailas, V.Sakkas and E. Lagios Section of Geophysics, Department of Geology and Geoenvironment, National and Kapodistrian University of Athens, Panepistimiopolis, Zografou 157 84, Greece. E-mail: [email protected] Downloaded from https://academic.oup.com/gji/article-abstract/220/1/461/5586995 by guest on 13 November 2019 Accepted 2019 October 11. Received 2019 March 17; in original form 2019 September 23 SUMMARY Tectonic activity is very difficult to study in the Santorini volcanic complex (SVC) as it comprises a cluster of small/awkwardly shaped islands covered by pyroclastic deposits from which tell-tale markers are swiftly erased, while seismicity is generally absent. We address the problem by combining geophysical exploration methods to evaluate the long-term effects of tectonic deformation and time-lapse differential GPS to directly evaluate the magnitude and kinematics of present-day deformation. The former comprise 3-D gravity modelling to investigate the footprint of tectonics on the pre-volcanic Alpine basement and natural-field EM induction to map conductivity anomalies epiphenomenal to fluid circulation in faults. Our analysis identified the following principal tectonic elements: The Trans-Santorin Divide (TSD), a segmented NNW–SSE dextral strike-slip fault splitting the SVC sideways of the line joining Cape Exomytis, the Kammeni Islets and the Oia–Therassia Strait. It is collocated with a major vertical conductive zone and forms a series of dents and depressions in the basement. -
Map Imerovigli
/ m o c . s o e - i n i r o t n a s / / : p t t C. Mavropetra h B. Baxedes m o c . s o e - i n i r o t n a s @ o f n i Useful Numbers Ε 3 1 0 0 0 0 6 8 2 2 0 3 + B. Paradisos F • General Hospital: 22860 36111 9 1 5 2 2 0 6 8 2 2 0 3 + B. Kolumbos T • Police: 22860 22649 e c e e r G 0 0 7 4 8 i n i r o t n a S , i l g i v o r e m C. Kolumbos I 1.SIGALAS • Port Authority: 2286022239 • Fire Service: 22860 33087 • Aegean Airlines: 22860 28500 • Taxi Service: 22860 22555 B. Katharos Finikia • Bus Service (KTEL): 22860 25404 sets B. Pori Ambient sun Oia • Municipality of Thira (city Hall): 22860 22231 Ammoudi Bay Wineries 1. SIGALAS Riva 2. WINE MUSEUM B. Xiropigado 3. ROUSSOS WINERY Isl. Thirasia 4. ARGYROS ESTATE B. Vourvoulos 5. SANTO WINES 6. VENETSANOS Imerovigli Manolas Vourvoulos Korfos Food - Coffe - Drink C. Tourlos 1. GIORGAROS, Firostefani Fish Tavern 2. TRANQUILO, FIRA Beach Bar no Active volca B. Monolithos Isl. NEA KAMENI Karterados C. Alonaki EUM Legend Mesaria 2.WINE MUS TO WINES WINERY main road 5.SAN 3.ROUSSOS Isl. PALIA KAMENI Vothonas TE GYROS ESTA second road 4.AR Exo Gonia Athinios Port B. Avis LEtGreEkkNinD g trail OS 6.VENETSAN BBEeAaCcH h Isl. Aspronisi Pyrgos ARCHAEOLOGICAL SITE arcaeological site Episkopi Megalochori B. Kamari Gonias Zoodochos AIRPORT Pigi airport Ag. -
Santorini Volcanic Field Using a New Oxygen Fugacity Method
An Examination of the Evolution of the Santorini Volcanic Field Using a New Oxygen Fugacity Method Presented in Partial Fulfillment of the Requirements for Graduation with a Bachelor of Science in Geological Sciences in the undergraduate colleges of The Ohio State University Susan M. Karberg The Ohio State University June 2006 Dr. Michael Barton Advisor Table of Contents Acknowledgements………………………………………………………………………iii Abstract…………………………………………………………………………………...iv Santorini Volcanic Field…………………………………………………………………..1 Geography…………………………………………………………………………1 Tectonics…………………………………………………………………………..3 Geologic History…………………………………………………………………..8 Oxygen Fugacity…………………………………………………………………………..9 Olivine-Melt Equilibrium………………………………………………………………..11 Olivine-Melt Method…………………………………………………………………….13 Results……………………………………………………………………………………14 Discussion .………………………………………………………………………………17 References………………………………………………………………………………..19 Appendix: Thin-Section Descriptions.………………….………………………………21 ii Acknowledgements: I want to dedicate this thesis to my parents who have provided me with a quality education. I would like to thank Dr. Barton for suggesting this project and providing methods and samples, answering all of my questions about source material, and the grateful review of the many parts of this thesis. Graduate student Scott Drew, and Jeff Ziga for their help with review of this thesis, abstract and poster preparations. iii Abstract: Volcanism on Santorini has occurred over the last ~600,000 years. During this interval most of the erupted lavas have evolved -
Prospectus Okeanis Eco Tankers Corp
PROSPECTUS OKEANIS ECO TANKERS CORP. (Incorporated under the laws of the Republic of the Marshall Islands with registration number 96382) Listing of the Company’s shares on the Oslo Axess __________ The information contained in this prospectus (the “Prospectus”) relates to the listing and admission to trading of common shares, each with a par value of USD 0.001 (the “Shares”) in Okeanis Eco Tankers Corp. (the “Company” or “OET”), a limited corporation incorporated under the laws of the Marshall Islands (together with its consolidated subsidiaries, the “Group” or “Okeanis”), on Oslo Axess, a regulated marked operated by Oslo Børs ASA (“Oslo Axess”) (the “Listing”). __________ The board of directors of the Oslo Stock Exchange approved the Company's listing application at a board meeting held on or about 5 March 2019, subject to fulfilment by the Company of the Oslo Axess listing requirements. __________ Beneficial interests in all of the Shares are registered with the Norwegian Central Securities Depository (Nw. Verdipapirsentralen) (the “VPS”) in book-entry form. All the Shares will rank in parity with one another and carry one vote per Share. Trading in the Shares on Oslo Axess is expected to commence on or about 7 March 2019, under the trading symbol “OET”. __________ For the definitions of capitalised terms used throughout this Prospectus, see Section 17 “Definitions”. Investing in the Shares involves risks; see Section 2 “Risk Factors” beginning on page 9. The date of this Prospectus is 28 February 2019. IMPORTANT INFORMATION This Prospectus has been prepared in order to provide information about the Company and its business in relation to the Listing of the Shares and to comply with the Norwegian Securities Trading Act of 29 June 2007 no.