Samothrace:Sixth Preliminaryreport
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With Samos & Kuşadası
GREECE with Samos & Kuşadası Tour Hosts: Prof. Douglas Henry & MAY 27 - JUNE 23, 2018 Prof. Scott Moore organized by Baylor University in GREECE with Samos & Kuşadası / MAY 27 - JUNE 23, 2018 Corinth June 1 Fri Athens - Eleusis - Corinth Canal - Corinth - Nafplion (B,D) June 2 Sat Nafplion - Mycenaean Palace and the Tomb of King Agamemnon - Epidaurus - Nafplion (B, D) June 3 Sun Nafplion -Church of Agia Fotini in Mantinea- Tripolisand Megalopolis-Mystras-Kalamata (B,D) BAYLOR IN GREECE June 4 Mon Kalamata - Drive by Methoni or Koroni to see the Venetian fortresses - Nestor’s Palace in Pylos (B,D) Program Directors: Douglas Henry and Scott Moore June 5 Tue Pylos - Tours in the surrounding area - more details will follow by Nick! (B,D) MAY 27 - JUNE 23, 2018 June 6 Wed Pylos - Gortynia - Dimitsana - Olympia (B, D) June 7 Thu Olympia - Temple of Zeus, the Temple of Hera, Museum - Free afternoon. Overnight Olympia (B,D) Acropolis, Athens June 8 Fri Olympia - Morning drive to the modern city of Corinth. Overnight Corinth. (B,D) June 9 Sat Depart Corinth for Athens airport. Fly to Samos. Transfer to hotel. Free afternoon, overnight in Samos (B,D) June 10 Sun Tour of Samos; Eupalinos Tunnel, Samos Archaeological Museum, walk in Vathi port. (B,D) June 11 Mon Day trip by ferry to Patmos. Visit the Cave of Revelation and the Basilica of John. Return Samos. (B,D) June 12 Tue Depart Samos by ferry to Kusadasi. Visit Miletus- Prienne-Didyma, overnight in Kusadasi (B,D) Tour Itinerary: May 27 Sun Depart USA - Fly Athens May 28 Mon Arrive Athens Airport - Private transfer to Hotel. -
Review of Samothrace 3: the Hieron, by Phyllis Williams Lehmann Brunilde S
Bryn Mawr College Scholarship, Research, and Creative Work at Bryn Mawr College Classical and Near Eastern Archaeology Faculty Classical and Near Eastern Archaeology Research and Scholarship 1971 Review of Samothrace 3: The Hieron, by Phyllis Williams Lehmann Brunilde S. Ridgway Bryn Mawr College, [email protected] Let us know how access to this document benefits ouy . Follow this and additional works at: http://repository.brynmawr.edu/arch_pubs Part of the Classical Archaeology and Art History Commons, and the History of Art, Architecture, and Archaeology Commons Custom Citation Ridgway, Brunilde S. 1971. Review of Samothrace 3: The Hieron, by Phyllis Williams Lehmann. American Journal of Archaeology 75:100-102. This paper is posted at Scholarship, Research, and Creative Work at Bryn Mawr College. http://repository.brynmawr.edu/arch_pubs/73 For more information, please contact [email protected]. 100 AMERICAN JOURNAL OF ARCHAEOLOGY [AJA 75 ing health of Professor Schweitzer forced him to cease tion, the painstaking presentation of evidence and espe- writing in 1964. Research into the nature of geo- cially the elegant format of these three volumes. For metric art has proceeded at an extremely fast pace since such typographical quality it is perhaps a small price that time, and it is regrettable that more of the re- to pay that the book took several years in printing cent studies could not have been incorporated into this (the Preface is dated July 1965), although some re- volume. However, an interpretation of the period as cent publications could not therefore be taken into ac- it was known in 1964 is not without value, although count. -
THE NATURE of the THALASSOCRACIES of the SIXTH-CENTURY B. C. by CATHALEEN CLAIRE FINNEGAN B.A., University of British Columbia
THE NATURE OF THE THALASSOCRACIES OF THE SIXTH-CENTURY B. C. by CATHALEEN CLAIRE FINNEGAN B.A., University of British Columbia, 1973 A THESIS SUBMITTED IN PARTIAL FULFILMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF ARTS in the Department of CLASSICS We accept this thesis as conforming to the required standard THE UNIVERSITY OF BRITISH COLUMBIA October, 1975 In presenting this thesis in partial fulfilment of the requirements for an advanced degree at the University of British Columbia, I agree that the Library shall make it freely available for reference and study. I further agree that permission for extensive copying of this thesis for scholarly purposes may be granted by the Head of my Department or by his representatives. It is understood that copying or publication of this thesis for financial gain shall not be allowed without my writ ten pe rm i ss ion . Department of plassips. The University of British Columbia 2075 Wesbrook Place Vancouver, Canada V6T 1W5 Date October. 197 5. ~t A ~ A A P. r~ ii The Nature of the Thalassocracies of the Sixth-Century B. C. ABSTRACT The purpose of this thesis is to study the nature and extent of the sixth century thalassocracies through the available ancient evidence, particularly the writings of Herodotus and Thucydides. In Chapter One the evidence for their existence is established and suggested dates are provided. Chapter Two is a study of their naval aspects and Chapter Three of their commercial aspects. This study leads to the conclusion that these thalassocracies were unaggressive mercantile states, with the exception of Samos during Polycrates' reign. -
Greece): Results from Geomorphological Studies and Fission-Track Analysis
© Österreichische Geologische Gesellschaft/Austria; download unter www.geol-ges.at/ und www.biologiezentrum.at fission-track dating geomorphology palaeokarst neotectonics . Hellenides Cretaceous Palaeokarst and Cenozoic Erosion of the North Sporades (Greece): Results from Geomorphological Studies and Fission-Track Analysis EWALD HEJL1, HELMUT RIEDL2 AND HERBERT WEINGARTNER2 9 Figures and 2 Tables Content Zusammenfassung 67 Abstract .' 67 1. Introduction 68 2. Geological setting 68 3. Palaeokarst features 69 3.1 Bauxite karst and laterite karst 69 3.2 Preflysch karst 72 4. Neogene-Quaternary planation surfaces of Skopelos Island 72 4.1 Planation system A 72 4.2 Planation system B 72 4.3 Planation system C 72 4.4 Pediment system D 74 4.5 Coastal marginal pediment system E 74 5. Apatite fission-track analysis 74 6. Discussion of thermochronological data 75 7. Conclusions 81 8. Acknowledgements 81 References 81 Der kreidezeitliche Paläokarst und die känozoische Reliefgeschichte der Nordsporaden (Griechenland): Geomorphologische Befunde und Spaltspurenanalysen Zusammenfassung Die Reliefentwicklung der Magnesischen Inseln (Nordsporaden) wurde anhand geomorphologischer Geländebeobachtungen auf Skopelos und mittels Spaltspurdatierungen an Gesteinen von Skiathos, Skopelos und Alonnisos untersucht. Die gemessenen Spaltspuralter und modellierten Abkühlpfade weisen auf regionale und zeitliche Schwankungen der posteozänen Abtragungsgeschwindigkeiten hin. Zwei präeozäne Generationen von Paläokarst sind auf Skopelos zu beobachten. Die erste entwickelte sich während der Unterkreide auf triadischen Dolomiten des alten pelagonischen Schelfs. Die Bauxite und Laterite, mit denen dieser Palaeokarst versiegelt ist, sind aus verschwemmtem Material der Eohellenischen Decke hervorgegangen. Eine zweite Generation von Paläokarst entwickelte sich auf oberkretazi- schen Rudistenkalken und wurde unter palaeogenem Flysch begraben. Drei Generationen neogener Verflachungen treten auf Skopelos oberhalb von 300 m Seehöhe auf. -
The Molasse of Paros Island, Aegean Sea
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Annalen des Naturhistorischen Museums in Wien Jahr/Year: 1980 Band/Volume: 83 Autor(en)/Author(s): Dermitzakis M., Papanikolaou D. Artikel/Article: The Molasse of Paros Island, Aegean Sea. 59-71 ©Naturhistorisches Museum Wien, download unter www.biologiezentrum.at Ann. Naturhist. Mus. Wien 83 59-71 Wien, Dezember 1980 The Molasse of Paros Island, Aegean Sea By M. DEEMITZAKIS & D. PAPANIKOLAOU X) with contributions of S. THEODOBIDIS and R. MIRKOU (With 7 textfigures) Manuscript received on 17th of March 1980 Zusammenfassung Auf der Insel Paros bildet die Molasse die höchste Formation der Marmara-Decke. Diese ist ein Teil der regionalen Kykladen-Decke und umfaßt alle vorobermiozänen, nichtmetamorphen Gesteine des Gebietes. Das Alter der Molasse und ihrer Transgression auf den Ophiolithen wurde mit Foraminiferen und kalkigem Nannoplankton als Burdiga- lien bestimmt. Daraus ergibt sich eine Platznahme der Kykladen-Decke in der Zeit nach dem Burgidalien und vor dem Messinien, da die frühesten autochthonen Sedimente auf Milos dieses Alter haben. Die Kykladen-Decke stammt wahrscheinlich aus einem Gebiet südlich der Kykladen, etwa aus dem jetzigen Kreta-Becken. Abstract The Molasse of Paros Island is the upper formation of Marmara nappe, which is part of the regional Cycladic nappe comprising all the pre-upper Miocene non-metamorphic rocks of the area. The age of the Molasse as well as of its transgression on the ophiolites was determined by foraminifera and calcareous nannoplankton as Burdigalian. Hence, the emplacement of the Cycladic nappe is of post-Burdigalian and of pre-Messinian age (from the age of the first autochthonous sediments of Milos). -
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. -
Mycenaean Reminiscence in the Area Samothrace – Hemus Valeria Phol
Mycenaean Reminiscence in the area Samothrace – Hemus Valeria Phol (Summary) The report represents the hypothesis about the Samothrace as an area center between Ida in Phrygia, Aton and Thrace of the oral mysterious – consecrated belief, formed during the Mycenaean period in the Aegean Sea cultural area. In the earliest period the ceremonial is implemented in rock formed belief topos, modified and updated during and after the Classical Era in Hellenes cultural – linguistic area. In Thrace clear clues from the Mycenaean period are preserved because of the social – political kingdoms structure. Because of the Samothrace location against the outflow of Maritsa river – “the door” of the Aegean Sea toward the European Thrace, it can be characterized even in the Mycenaean period as a key center of oral mysterious belief and the king ideology with influence onto wide group of believers until the Early Christian Era. (TEXT) The Mycenaean traditions in which belongs the Thrace are stick in belief topos from the Ancient times, which fall into the Hellenes cultural – linguistic area through the first 2-3 centuries of 1 millennium B.C. The traditions accepted their Hellenes Classical character around 5 century B.C. In Thrace the Mycenaean traditions in political structure and religiosity continuous their existence even after 5 century B.C. The process of cultural – historic and religious continuity, which is implemented by Hellenization between Mycenaean, Geometric, Archaic and Classical Eras are not interrupted during the following periods. In Southeast Europe they can be followed with relatively enough written, archaeological, graphic, and epigraphic materials for a long period of time of one of the most important belief toposes, in which is the transition from abstract belief toward the personified religiosity. -
Sustainable Energy Production and Consumption in Greece: a Review
RECENT ADVANCES in ENVIRONMENT, ECOSYSTEMS and DEVELOPMENT Sustainable energy production and consumption in Greece: A review V. Vita, M. Peikou, P. Kaltakis, A. Goutis, L. Ekonomou A.S.PE.T.E. - School of Pedagogical and Technological Education, Department of Electric Educators, Ν. Ηeraklion, 141 21 Athens, Greece e-mail: [email protected] Abstract: Electricity is considered to be one of the most important and vital goods. Each country should be energy independent and efficient in order to cope with its citizens needs and abstain political, economical and social after effects. Greek electrification initiated and evolved in a much slower pace than the rest of Europe. The foundation of the Public Power Cooperation S.A. (PPC) in 1950 was one of the most significant steps for essential, more organized and further growth of electrification. In this paper a thorough analysis of the Greek electrical energy sources, such as lignite, oil, natural gas, hydroelectric power and renewable energy sources is made and their percentage participation in electrical energy production is examined. After obtaining a broad picture of the current electrical energy production state in Greece, it is concluded that there is the need for the development of environmental friendly unexploited energy forms. Several measures towards that direction combined with Greek policy and objectives are demonstrated. Key-Words: Production; Renewable Energy Sources (RES); Public Power Corporation S.A. (PPC); Policy. 1. Introduction 2. Historical energy retrospection of Greece The advantages of electric energy against other 2.1 Period before the foundation of the Public forms of energy are: a) the instantly transformation Power Cooperation S.A. -
3Rd HELLENIC SCIENTIFIC CONFERENCE in APICULTURE- SERICULTURE Thessaloniki 21-22 April 2007
3rd HELLENIC SCIENTIFIC CONFERENCE IN APICULTURE- SERICULTURE Thessaloniki 21-22 April 2007 HELLENIC SCIENTIFIC SOCIETY OF APICULTURE- SERICULTURE NUMBER OF DRONE CELLS IN THE NATURAL-BUILT HONEYCOMBS OF A. M. MACEDONICA Goras G., Dislis S., Konstas N., Thrasyvoulou A. Laboratory of Apiculture – Sericulture, Faculty of Agriculture, Aristotle University of Thessaloniki, . [email protected] Beekeeping as a biological agriculture requires the replacement of all of the honeycombs. Using frames with foundation comb provides uniformity with minimal structure of dronecells but biological wax is limited and it is not always free of residues. As a solution it could be proposed to “force” bees to build the frames without using foundation combs, but in this case, the number of dronecells would be higher. This number depends on the bee race but there in no paper that it refers to this characteristic for the indigenous of Greece. In this paper present the first data concerns the production of dronecells in beecolonies with and without foundation comb. The experimental group provided with frames with foundation comb, produced less drone cells (0,03% per bee colony) in relation to the second group, which built natural honeycombs and so produced more dronecells (20,6% per bee colony). These average numbers present significant differences and this is also occurs after the comparison of the number of worker cells that the two experimental groups produced. First group produced mainly worker cells (99,97% per colony), while the second group produced 79,3% worker cells per colony. Finally we can establish that in each experimental group there is a great variance among the colonies that concerns the number of dronecells, regardless of the use (CV% : 316,7%) or not (CV% : 67%) foundation combs. -
Naxos, Cyclades, Greece
Retrogression of a high-temperature metamorphic core complex Low-grade retrogression of a high-temperature metamorphic core complex: Naxos, Cyclades, Greece Shuyun Cao1,2,†, Franz Neubauer1, Manfred Bernroider1, Johann Genser1, Junlai Liu3, and Gertrude Friedl1 1Department of Geography and Geology, University of Salzburg, Hellbrunnerstrasse 34, A-5020 Salzburg, Austria 2State Key Laboratory of Geological Processes and Mineral Resources, School of Earth Sciences, China University of Geosciences, Wuhan 430074, China 3State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China ABSTRACT metapelites (at temperatures of ~350–130 °C) sion of metamorphic complexes along the in the metamorphic core complex core re- upper margins, particularly close to the brittle- Retrogressive deformation and metamor- sulted mainly from late-stage E-W shorten- ductile boundary (e.g., Siebenaller et al., 2013; phism are often reported from the main ing and folding. Late-stage flow of hydrous Whitney et al., 2013; Gébelin et al., 2014; low-angle shear zones and detachments of fluids resulted in resetting of fabrics and Methner et al., 2015, and references therein). metamorphic core complexes, but their im- enhancement of ductile deformation. The Low-temperature retrogressive deformation portance is not sufficiently emphasized for middle–late Miocene retrogression events and metamorphism of high-grade metamorphic the footwall interior. In order to contribute are also reflected by a similarly aged tectonic fabrics are often reported from detachments of to a better understanding of exhumation- collapse basin in the hanging-wall unit above metamorphic core complexes (e.g., Mehl et al., related retrogression processes within and at the detachment. -
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.