DOCUMENTS of the SAMOTHRACIAN LANGUAGE 95 Their Contents Were Mostly Archaic and Together They Include the Largest Amount of the Material Submitted Here
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Poison King: the Life and Legend of Mithradates the Great, Rome's
Copyrighted Material Kill em All, and Let the Gods Sort em Out IN SPRING of 88 BC, in dozens of cities across Anatolia (Asia Minor, modern Turkey), sworn enemies of Rome joined a secret plot. On an appointed day in one month’s time, they vowed to kill every Roman man, woman, and child in their territories. e conspiracy was masterminded by King Mithradates the Great, who communicated secretly with numerous local leaders in Rome’s new Province of Asia. (“Asia” at this time referred to lands from the eastern Aegean to India; Rome’s Province of Asia encompassed western Turkey.) How Mithradates kept the plot secret remains one of the great intelli- gence mysteries of antiquity. e conspirators promised to round up and slay all the Romans and Italians living in their towns, including women and children and slaves of Italian descent. ey agreed to confiscate the Romans’ property and throw the bodies out to the dogs and crows. Any- one who tried to warn or protect Romans or bury their bodies was to be harshly punished. Slaves who spoke languages other than Latin would be spared, and those who joined in the killing of their masters would be rewarded. People who murdered Roman moneylenders would have their debts canceled. Bounties were offered to informers and killers of Romans in hiding.1 e deadly plot worked perfectly. According to several ancient histo- rians, at least 80,000—perhaps as many as 150,000—Roman and Italian residents of Anatolia and Aegean islands were massacred on that day. e figures are shocking—perhaps exaggerated—but not unrealistic. -
European Court of Human Rights Examines Living Conditions in Hotspots Moria, Pyli & Vial
This project has been supported by the European Programme for Integration and Migration (EPIM), a collaborative initiative of the Network of European Foundations (NEF). The sole responsibility for the project lies with the organiser(s) and the content may not necessarily reflect the positions of EPIM, NEF or EPIM’s Partner Foundations. For immediate release EUROPEAN COURT OF HUMAN RIGHTS EXAMINES LIVING CONDITIONS IN HOTSPOTS MORIA, PYLI & VIAL Chios, Kos & Lesvos, January 20, 2021 While the situation on the East Aegean islands received particular attention after the outbreak of the fire in Moria, it has subsided more recently. At the same time, living conditions on the islands continue to be catastrophic. People have little access to medical care, wash facilities, and proper shelter, and are regularly forced to sleep in tents that flood easily in the winter rains. Particularly vulnerable people are not exempt from these conditions. Even in times when the Covid-19 was and is on the verge of an outbreak in the camps, members of at-risk groups continue to live exposed to these conditions without protection. The European Court of Human Rights has now asked the Greek government questions regarding the treatment of a total of eight people, all of whom were living in one of the so-called EU hotspots and had pre-existing medical conditions or were particularly vulnerable. In total, the Court connected 8 cases involving Chios, Kos, Lesvos and Samos, i.e. 4 out of 5 EU hotspots. These cases therefore demonstrate the structural illegality and impossibility to implement the hotspot approach and border procedures in a way that does not violate human rights. -
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. -
Greece • Crete • Turkey May 28 - June 22, 2021
GREECE • CRETE • TURKEY MAY 28 - JUNE 22, 2021 Tour Hosts: Dr. Scott Moore Dr. Jason Whitlark organized by GREECE - CRETE - TURKEY / May 28 - June 22, 2021 May 31 Mon ATHENS - CORINTH CANAL - CORINTH – ACROCORINTH - NAFPLION At 8:30a.m. depart from Athens and drive along the coastal highway of Saronic Gulf. Arrive at the Corinth Canal for a brief stop and then continue on to the Acropolis of Corinth. Acro-corinth is the citadel of Corinth. It is situated to the southwest of the ancient city and rises to an elevation of 1883 ft. [574 m.]. Today it is surrounded by walls that are about 1.85 mi. [3 km.] long. The foundations of the fortifications are ancient—going back to the Hellenistic Period. The current walls were built and rebuilt by the Byzantines, Franks, Venetians, and Ottoman Turks. Climb up and visit the fortress. Then proceed to the Ancient city of Corinth. It was to this megalopolis where the apostle Paul came and worked, established a thriving church, subsequently sending two of his epistles now part of the New Testament. Here, we see all of the sites associated with his ministry: the Agora, the Temple of Apollo, the Roman Odeon, the Bema and Gallio’s Seat. The small local archaeological museum here is an absolute must! In Romans 16:23 Paul mentions his friend Erastus and • • we will see an inscription to him at the site. In the afternoon we will drive to GREECE CRETE TURKEY Nafplion for check-in at hotel followed by dinner and overnight. (B,D) MAY 28 - JUNE 22, 2021 June 1 Tue EPIDAURAUS - MYCENAE - NAFPLION Morning visit to Mycenae where we see the remains of the prehistoric citadel Parthenon, fortified with the Cyclopean Walls, the Lionesses’ Gate, the remains of the Athens Mycenaean Palace and the Tomb of King Agamemnon in which we will actually enter. -
Investment Profile of the Chios Island
Island of Chios - Investment Profile September 2016 Contents 1. Profile of the island 2. Island of Chios - Competitive Advantages 3. Investment Opportunities in the island 4. Investment Incentives 1. Profile of the island 2. Island of Chios - Competitive Advantages 3. Investment Opportunities in the island 4. Investment Incentives The island of Chios: Οverview Chios is one of the largest islands of the North East Aegean and the fifth largest in Greece, with a coastline of 213 km. It is very close to Asia Minor and lies opposite the Erythraia peninsula. It is known as one of the most likely birthplaces of the ancient mathematicians Hippocrates and Enopides. Chios is notable for its exports of mastic and its nickname is ”The mastic island”. The Regional Unit of Chios includes the islands of Chios, Psara, Antipsara and Oinousses and is divided into three municipalities: Chios, Psara and Oinouses. ➢ Area of 842.5 km² ➢ 5th largest of the Greek islands ➢Permanent population: ➢52.574 inhabitants (census 2011) including Oinousses and Psara ➢51.390 inhabitants (only Chios) Quick facts The island of Chios is a unique destination with: Cultural and natural sites • Important cultural heritage and several historical monuments • Rich natural environment of a unique diversity Archaeological sites: 5 • Rich agricultural land and production expertise in agriculture and Museums: 9 livestock production (mastic, olives, citrus fruits etc) Natura 2000 regions: 2 • RES capacity (solar, wind, hydro) Beaches: 45 • Great concentration in fisheries and aquaculture Source: http://www.chios.gr • Satisfactory infrastructure of transport networks (1 airport, 2 ports and road network) • Great history, culture and tradition in mercantile maritime, with hundreds of seafarers and ship owners Transport infrastructure Chios is served by one airport and two ports (Chios-central port and Mesta-port) and a satisfactory public road network. -
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 Chios, Greece Earthquake of 23 July 1949: Seismological Reassessment and Tsunami Investigations
Pure Appl. Geophys. 177 (2020), 1295–1313 Ó 2020 Springer Nature Switzerland AG https://doi.org/10.1007/s00024-019-02410-1 Pure and Applied Geophysics The Chios, Greece Earthquake of 23 July 1949: Seismological Reassessment and Tsunami Investigations 1 2 3,4 1 5 NIKOLAOS S. MELIS, EMILE A. OKAL, COSTAS E. SYNOLAKIS, IOANNIS S. KALOGERAS, and UTKU KAˆ NOG˘ LU Abstract—We present a modern seismological reassessment of reported by various agencies, but not included in the Chios earthquake of 23 July 1949, one of the largest in the Gutenberg and Richter’s (1954) generally authorita- Central Aegean Sea. We relocate the event to the basin separating Chios and Lesvos, and confirm a normal faulting mechanism tive catalog. This magnitude makes it the second generally comparable to that of the recent Lesvos earthquake largest instrumentally recorded historical earthquake located at the Northern end of that basin. The seismic moment 26 in the Central Aegean Sea after the 1956 Amorgos obtained from mantle surface waves, M0 ¼ 7 Â 10 dyn cm, makes it second only to the 1956 Amorgos earthquake. We compile event (Okal et al. 2009), a region broadly defined as all available macroseismic data, and infer a preference for a rupture limited to the South by the Cretan–Rhodos subduc- along the NNW-dipping plane. A field survey carried out in 2015 tion arc and to the north by the western extension of collected memories of the 1949 earthquake and of its small tsunami from surviving witnesses, both on Chios Island and nearby the Northern Anatolian Fault system. -
Constructing Crisis at Europe's Borders
CONSTRUCTING CRISIS AT EUROPE'S BORDERS The EU plan to intensify its dangerous hotspot approach on Greek islands JUNE 2021 Table of contents 1 Executive Summary 4 Introduction 5 The EU hotspot: containment strategy on the Greek islands 7 The Human Cost of Containment 8 Mental health deterioration among adults 10 Children at risk: mental health 11 Children at risk: physical health and well-being 11 Sexual violence and a chronic lack of protection 12 Systematic gaps in healthcare 13 The COVID-19 effect: conflation of public health and migration control 14 The ‘Shield’ of Europe: Normalisation of Push-backs and Violence at Borders 16 The EU’s Dangerous Hotspot Experiment 16 The everyday violence of containment 18 Failure to identify and protect vulnerable people 20 Erosion of asylum: ‘Fast track’ procedures and return 21 The expansion of detention 22 Moving Forward: EU Intensifies its Dangerous Approach 22 The renewed and intensified hotspot approach: MPRIC red flags 26 Conclusion 28 References 30 Annex: Reported Deaths in Hotspots Cover: Asylum seekers behind a razor wire fence in Vathy hotspot, Samos, March 2016, © GUILLAUME BINET/MYOP |2 CONSTRUCTING CRISIS AT EUROPE’S BORDERS Executive Summary Over the past five years, an entirely avoidable and the situation, the EU and its member states intend predictable policy-driven humanitarian crisis to intensify and institutionalise its containment has been unfolding in the Greek islands of Lesvos, and deterrence strategy. Samos, Chios, Leros, and Kos, with devasting consequences for the people trapped there. After In September 2020, the notorious Moria RIC fleeing their homes and surviving harrowing was burned to the ground in a destructive and journeys to Europe, the indefinite containment, symbolic moment. -
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). -
Announcement
COMMUNICATION Application of Residential Off-Peak Rates for the winter period 2019- 2020 Residential off-peak rates will apply between 01.11.2019 and 30.04.2020 as follows: 1. For residential customers 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, Thiva, Iasmos, Ioannina,Kavala, Kalamata, Kalambaka, Kanalaki, Karditsa, Karpenisi, Kassandria, Kastoria, Katerini, Kiato, Kilkis, Kozani, Komotini, Korinthos, Kranidi, Kyparissia, Lagadas, Lagadia (Arkadia), Lamia, Larisa, 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; on the islands of Alonissos, Antiparos, Evia, Zakynthos, Heraklia, Ios, Kea, Corfu, Cephalonia, Koufonisi, Lefkada, Mykonos, Naxos, Paros, Sikinos, Skiathos, Skopelos, Syros, Schoinousa, Folegandros. the off-peak rate shall apply on the basis of 2 different time frames: 1.1. Continuous period (23:00–07:00): applies for 8 hours. It applies for consumers who are already using this option and wish to keep it as is. 1.2. The split-hour option timetable, i.e. 2 hours in the afternoon (15:00-17:00) and 6 hours at night (02:00–08:00), i.e. a total of 8 hours. This shall apply to the following consumer groups: Consumers who have already used the 02:00-08:00 and 15:00-17:00 option until 30.04.2019; New consumers applying for off-peak rates who can use solely this option; Consumers who use the continuous option but wish to move to the split-hour option (users of this category shall not be able to return to the continuous option).