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Structures & Hosting Facilities Capacity New
SUMMARY STATEMENT OF REFUGEE FLOWS AT 10.00 14.3.2017 STRUCTURES & HOSTING NEW GUESTS CAPACITY NOTES FACILITIES ARRIVALS UNTIL 07:30 * HOSTING EASTERN AEGEAN ISLANDS STRUCTURES FACILITIES LESVOS (TOTAL) 3459 1460 3500 0 * HOSTING FACILITIES CHIOS (TOTAL) 836 2462 1100 19 CAPACITY REFERS TO SAMOS (TOTAL) 1710 237 850 0 UNHCR AND OTHER STATE- LEROS (TOTAL) 621 304 1000 0 RUN FACILITIES AT THE KOS (TOTAL) 1748 640 1000 0 ISLANDS OTHER ISLANDS (TOTAL) 652 0 TOTAL ISLANDS 7208 5755 8759 19 NORTHERN GREECE POLYKASTRO (NEA KAVALA) 942 4200 PIERIA (IRAKLIS FARM) 38 200 VEROIA (ARMATOLOU KOKKINOU CAMP IMATHIA) 218 400 ALEXANDRIA IMATHIAS (G. PELAGOU CAMP) 365 1200 DIAVATA (ANAGNOSTOPOULOU 329 2500 CAMP) 74 850 DERVENI-ALEXIL (THESSALONIKI) SINDOS -FRAKAPOR 47 600 (THESSALONIKI) KORDELIO- SOFTEX 450 1900 (THESSALONIKI) SINATEX-KAVALARI (THESSALONIKI) 165 500 KORDOGIANNIS FARM - 50 1500 VASSILIKA DERVENI-DION AVETE 142 400 KONITSA (MUNICIPALITY) 130 200 DOLIANA IOANNINA 110 400 PREVEZA-FILIPIADA (PETROPOULAKI CAMP) 226 700 LAGADIKIA 213 TOTAL NORTHERN GREECE 3452 14950 CENTRAL GREECE LARISSA KOUTSOXERO EFTHIMIOPOULOU CAMP 1063 1500 VOLOS (MAGNESIA PREFECTURE) 108 200 TRIKALA-ATLANTIK 209 360 OINOI (OINOFYTA) VOIOTIA 600 600 EVOIA-RITSONA (A.F. CAMP) 679 1000 FTHIOTIDA-THERMOPYLAE 462 500 TOTAL CENTRAL GREECE 3121 4160 SOUTHERN GREECE ANDRAVIDA (MUNICIPALITY) 161 300 TOTAL SOUTHERN GREECE 161 300 ATTIKI ELAIONAS 1975 2500 SCHISTO 942 2000 SKARAMAGAS DOCK 3200 3200 MERCHANT MARINE ACADEMY (ELEFSINA) 320 346 MALAKASA 483 1500 RAFINA 111 120 LAVRIO -
It Is Quite Common for Confusion to Arise About the Process Used During a Hydrographic Survey When GPS-Derived Water Surface
It is quite common for confusion to arise about the process used during a hydrographic survey when GPS-derived water surface elevation is incorporated into the data as an RTK Tide correction. This article explains a little about the process. What we are discussing here might be a tide-related correction to a chart datum for coastal surveying – maybe to update navigational charts, or it might be nothing to do with tides at all. For example, surveying a river with the need to express bathymetry results as a bottom elevation on the desired vertical datum – not simply as “depth” results. Whether it is anything to do with tidal forces or not, the term “RTK Tide” is ubiquitous in hydrographic-speak to refer to vertical corrections of echo sounding data using RTK GPS. Although there is some confusing terminology, it’s a simple idea so let’s try to keep it that way. First keep in mind any GPS receiver will give the user basically two things in terms of vertical positioning: height above the GPS reference ellipsoid surface and height above Mean Sea Level (MSL) where ever he or she is on the Earth. How is MSL defined? Well, a geoid surface is a measure of the strength of gravity which in turn mostly controls the height of the sea; it is logical to say that MSL height equals the geoid height and vice versa. Using RTK techniques to obtain tide information is a logical extension of this basic principle. We are measuring the GPS receiver height above a geoid. -
Recent Geomorphic Evolution of the Fan Delta of the Mornos River, Greece: Natural Processes and Human Impacts
Δελτίο της Ελληνικής Γεωλογικής Εταιρίας τομ. ΧΧΧΧ, Bulletin of the Geological Society of Greece vol. XXXX, 2007 2007 Proceedings of the 11th International Congress, Athens, May, Πρακτικά 11ου Διεθνούς Συνεδρίου, Αθήνα, Μάιος 2007 2007 RECENT GEOMORPHIC EVOLUTION OF THE FAN DELTA OF THE MORNOS RIVER, GREECE: NATURAL PROCESSES AND HUMAN IMPACTS Karymbalis E., Gaki-Papanastassiou K.2, and Maroukian H.2 1 Harokopio University, Department of Geography, [email protected] National and Kapodistrian University of Athens, Faculty of Geology and Geoenvironment, Department of Geography and Climatology, [email protected], [email protected] Abstract The Mornos river fan delta is located on the northern side of the western Gulf of Corinth is a Gilbert-type fan delta with an arcuate form characterised by the abun dance of coarse sediments. In order to determine the processes which contributed in the configuration of the fan delta during the last two centuries a detailed geomor- phic map was prepared depicting both the deltaic plain and the coastal zone fea tures. Comparative examination of 1945, 1986 and 1998 aerial photographs and re liable maps of the last two centuries along with field observations detected recent changes of the fan delta. The construction of a dam in the upper reaches of the basin in 1980 has significantly decreased the sediment supply downstream and has slack ened the growth of the fan delta. After 1980 the eastern distributary has been aban doned causing a 120 m retreat at the river mouth. Although a progradation rate of 4 m/year has been observed for the western active distributary in the period between 1945 and 1986, no remarkable changes have occurred since that period. -
Are Landscapes Buffered to High-Frequency
Watkins et al. Are landscapes buffered to high-frequency climate change? A comparison of sediment fluxes and depositional volumes in the Corinth Rift, central Greece, over the past 130 k.y. Stephen E. Watkins1,†, Alexander C. Whittaker1, Rebecca E. Bell1, Lisa C. McNeill2, Robert L. Gawthorpe3, Sam A.S. Brooke1, and Casey W. Nixon3 1Department of Earth Science and Engineering, Imperial College London, Prince Consort Road, London, SW7 2AZ, UK 2Ocean and Earth Science, National Oceanography Centre Southampton, University of Southampton, Southampton, SO14 3ZH, UK 3Department of Earth Science, University of Bergen, Allégaten 41, 5007 Bergen, Norway ABSTRACT vary spatially around the gulf, and we used istics of sediment supply to depocenters (e.g., them to derive minimum catchment-aver- Humphrey and Heller, 1995; Allen and Dens- Sediment supply is a fundamental control aged denudation rates of 0.18–0.55 mm/yr. more, 2000; Gawthorpe and Leeder, 2000; on the stratigraphic record. However, a key Significantly, our time series of basin sedi- Densmore et al., 2003; Cowie et al., 2006; question is the extent to which climate affects mentary volumes demonstrate a clear reduc- Backert et al., 2010). However, the importance sediment fluxes in time and space. To address tion in sediment accumulation rates during of climate in controlling sediment fluxes from this question, estimates of sediment fluxes the last glacial period compared to the cur- catchments to depositional basins over a range can be compared with measured sediment rent interglacial. This implies that Holocene of timescales remains contentious (e.g., Collier volumes within a closed basin that has well- sediment fluxes must have increased rela- et al., 2000; Jerolmack and Paola, 2010; Simp- constrained tectonic boundary conditions tive to Late Pleistocene times. -
Nafpaktos Schräg Gegenüber Von Patras Liegt Ein Kleines Äußerst Malerisches Städtchen – Nafpaktos
Nafpaktos Schräg gegenüber von Patras liegt ein kleines äußerst malerisches Städtchen – Nafpaktos. Es hat einen winzigen Hafen, der durch eine Art Stadtmauer befestigt ist. Rechts und links der Hafeneinfahrt stehen kleine Türmchen auf der Mauer, ein sehr schönes Bild. Oberhalb des Städtchens liegt die Ruine einer ziemlich groß angelegten venezianischen Festung, deren Mauern bis hinunter zum Meer gehen. Und oberhalb gibt es eine wunderschöne Taverne, von der aus man einen einmaligen Blick auf die Stadt und den Golf von Patras hat. Und im Hafen gibt es ausgezeichnete Restaurants, man sitzt sozusagen auf der Stadtmauer und hat beim Essen einen wunderbaren Blick auf den kleinen Hafen. Was hat es auf sich mit Nafpaktos? Dazu muss man in die Geschichte zurückgehen – da hieß das Städtchen nicht Nafpaktos, sondern Lepanto. Nach der Eroberung Konstantinopels 1453 durch die Türken gab es ja immer wieder Versuche seitens der Türken/des Osmanischen Reiches, Griechenland und den Balkan – mit Ziel Europa insgesamt – zu erobern. Einer dieser Versuche endete am 7. Oktober 1571 in der Seeschlacht von Lepanto, unweit des heutigen Städtchens Nafpaktos. Es war die letzte Seeschlacht mit von Sklaven geruderten Galeeren. 212 Kriegsschiffe der „Heiligen Liga“ gegen 260 Kriegsschiffe der Osmanen; 68000 Spanier, Italiener, Österreicher, Venezianer und Soldaten des Papstes gegen 77000 Osmanen. Don Juan de Austria, ein Sohn des Habsburgerkaisers Karl V., führte die Koalition an. Diese hatte sich gebildet, weil die Osmanen Zypern erobert hatten, das bisher zu Venedig gehörte. Venedig wollte seinen Mittelmeerhandel erhalten und erweitern – der Papst hoffte auf eine Renaissance der Kreuzzüge gegen die „Ungläubigen“. Das Zweckbündnis hielt nicht lange, der Sieg festigte die europäische Vormachtstellung der Habsburger. -
Detailed Fact Sheet 19.Pdf
THE RESORT Imagine overlooking the azure sea sparkling from every angle you stand. Imagine sinking your toes in the warm sand, feeling carefree, and free to self-care. Even so, there are places that cannot be fully framed in our imagination. It is only the soul that can genuinely recognize their blessings emerging from their land, their skyline and the smile of their people. Miraggio Thermal Spa Resort is one of them, a luxury spa resort in Halkidiki; a Greek Eden of unpretentious comfort lying amphitheatrically at the tip of the Kassandra peninsula, an ideal destination for families. This seafront enclave of well being and countless amenities descends on a lovely hill slope across 330 acres at one of the most unspoiled and least exploited areas in North Greece. Location The region is situated at the northern Aegean sea and shaped like a three-fingers palm; Kassandra, Sithonia and Mount Athos are the names of its peninsulas and each one of them has something unique to offer. Due to its easy access from different parts of Europe and Thessaloniki, and thanks to its recognized and contemporary hospitality infrastructure, Halkidiki is one of the ideal locations for holidays, international conferences, incentives and cruises. Weather 280 sunny days per year; mild Mediterranean microclimate. Neighborhood & Access Miraggio Thermal Spa Resort abstains from Thessaloniki airport 120 km. The second largest city of Greece is charming, ancient and vibrant, lies on the shore of the Thermaic Gulf and welcomes warmly its visitors. 63085 Paliouri, Kanistro,Halkidiki GR Reservations: [email protected] T: +30 2374440 000 E: [email protected] F: +30 23744 40 001 W: www.miraggio.gr Dining & Bars At Miraggio Thermal Spa Resort, a marvelous array of kitchen venues, food services, and bars is offered. -
A Seamless Vertical-Reference Surface for Acquisition, Management and Display (Ecdis) of Hydrographic Data
SEAMLESS VERTICAL DATUM A SEAMLESS VERTICAL-REFERENCE SURFACE FOR ACQUISITION, MANAGEMENT AND DISPLAY (ECDIS) OF HYDROGRAPHIC DATA A report prepared for the Canadian Hydrographic Service under Contract Number IIHS4-122 David Wells Alfred Kleusberg Petr Vanicek Department of Geodesy and Geomatics Engineering University of New Brunswick PO. Box 4400 Fredericton, New Brunswick Canada E3B 5A3 FINAL REPORT (DRAFT) November 22, 2004 Page 1 SEAMLESS VERTICAL DATUM Final Report 15 July 1995 FINAL REPORT (DRAFT) November 22, 2004 Page 2 SEAMLESS VERTICAL DATUM TABLE OF CONTENTS Table of contents...........................................................................................................................2 Executive summary.......................................................................................................................5 Acronyms used in this report ........................................................................................................6 1. Introduction...............................................................................................................................8 1.1 Problem statement.......................................................................................................8 1.2 The role of vertical-reference surfaces in navigation..................................................8 1.3 Vertical-reference surface accuracy issues..................................................................9 1.3.1 Depth measurement errors .........................................................................10 -
Accuracy of Flight Altitude Measured with Low-Cost GNSS, Radar and Barometer Sensors: Implications for Airborne Radiometric Surveys
sensors Article Accuracy of Flight Altitude Measured with Low-Cost GNSS, Radar and Barometer Sensors: Implications for Airborne Radiometric Surveys Matteo Albéri 1,2,* ID , Marica Baldoncini 1,2, Carlo Bottardi 1,2 ID , Enrico Chiarelli 3, Giovanni Fiorentini 1,2, Kassandra Giulia Cristina Raptis 3, Eugenio Realini 4, Mirko Reguzzoni 5, Lorenzo Rossi 5, Daniele Sampietro 4, Virginia Strati 3 and Fabio Mantovani 1,2 ID 1 Department of Physics and Earth Sciences, University of Ferrara, Via Saragat, 1, 44122 Ferrara, Italy; [email protected] (M.B.); [email protected] (C.B.); fi[email protected] (G.F.); [email protected] (F.M.) 2 Ferrara Section of the National Institute of Nuclear Physics, Via Saragat, 1, 44122 Ferrara, Italy 3 Legnaro National Laboratory, National Institute of Nuclear Physics, Via dell’Università 2, 35020 Legnaro (Padova), Italy; [email protected] (E.C.); [email protected] (K.G.C.R.); [email protected] (V.S.) 4 Geomatics Research & Development (GReD) srl, Via Cavour 2, 22074 Lomazzo (Como), Italy; [email protected] (E.R.); [email protected] (D.S.) 5 Department of Civil and Environmental Engineering (DICA), Polytechnic of Milan, Piazza Leonardo da Vinci 32, 20133 Milano, Italy; [email protected] (M.R.); [email protected] (L.R.) * Correspondence: [email protected]; Tel.: +39-329-0715328 Received: 7 July 2017; Accepted: 13 August 2017; Published: 16 August 2017 Abstract: Flight height is a fundamental parameter for correcting the gamma signal produced by terrestrial radionuclides measured during airborne surveys. -
Newsletter August 2011 – December 2011
Program for the Education of Roma Children Regions of Central Macedonia, Western Macedonia, Eastern Macedonia and Thrace 21.09.2010 – 31.12.2013 Newsletter August 2011 – December 2011 Beginning of classes addressed Literacy courses for to students who had been grade adolescents retained in Dendropotamos, In the settlements of Agia Sofia Alexandria and Kymina- and Peraia, literacy courses for Malgara. illiterate Roma adolescents begin. A direct positive outcome of Three philologists and a support classes was that sixteen mathematician teach in these 3rd grade students of the Junior courses and 56 adolescents High School of Menemeni, in participate (Agia Sofia: 39 Dendropotamos passed to the 1st students, Peraia: 17 students). grade of Senior High School. The support for children in this transitory phase of their education is estimated to contribute to its continuation and completion. Thus, upon the children’s request and given the fact that support teaching is no longer offered to Junior and Senior High Schools, support classes are scheduled and take place during the whole academic year 2011-2012 in Junior and Senior High Schools in Menemeni, Alexandria, Kymina- Malgara and Kouloura October 2011 October 3 Introductory training for teachers in the primary schools and the kindergarten of Menemeni, in Dendropotamos. October 4 Introductory in-service training for teachers in the primary schools of Peraia and the cross-cultural primary school of Neoi Epivates. October 6 In-service training for philologists and mathematicians of the Program, regarding teaching approaches in mathematics and language. October 7 Introductory training in the primary and kindergarten schools of Veroia, Kouloura and Xehasmeni. -
Agricultural Practices in Ancient Macedonia from the Neolithic to the Roman Period
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by International Hellenic University: IHU Open Access Repository Agricultural practices in ancient Macedonia from the Neolithic to the Roman period Evangelos Kamanatzis SCHOOL OF HUMANITIES A thesis submitted for the degree of Master of Arts (MA) in Black Sea and Eastern Mediterranean Studies January 2018 Thessaloniki – Greece Student Name: Evangelos Kamanatzis SID: 2201150001 Supervisor: Prof. Manolis Manoledakis I hereby declare that the work submitted is mine and that where I have made use of another’s work, I have attributed the source(s) according to the Regulations set in the Student’s Handbook. January 2018 Thessaloniki - Greece Abstract This dissertation was written as part of the MA in Black Sea and Eastern Mediterranean Studies at the International Hellenic University. The aim of this dissertation is to collect as much information as possible on agricultural practices in Macedonia from prehistory to Roman times and examine them within their social and cultural context. Chapter 1 will offer a general introduction to the aims and methodology of this thesis. This chapter will also provide information on the geography, climate and natural resources of ancient Macedonia from prehistoric times. We will them continue with a concise social and cultural history of Macedonia from prehistory to the Roman conquest. This is important in order to achieve a good understanding of all these social and cultural processes that are directly or indirectly related with the exploitation of land and agriculture in Macedonia through time. In chapter 2, we are going to look briefly into the origins of agriculture in Macedonia and then explore the most important types of agricultural products (i.e. -
Flood Risk Perception and Adaptation Capacity
Flood risk perception and adaptation capacity: a contribution to the socio-hydrology debate Sven Fuchs, Konstantinos Karagiorgos, Kyriaki Kitikidou, Fotios Maris, Spyridon Paparrizos, Thomas Thaler To cite this version: Sven Fuchs, Konstantinos Karagiorgos, Kyriaki Kitikidou, Fotios Maris, Spyridon Paparrizos, et al.. Flood risk perception and adaptation capacity: a contribution to the socio-hydrology debate. Hydrology and Earth System Sciences, European Geosciences Union, 2017, 21 (6), pp.3183-3198. 10.5194/hess-21-3183-2017. hal-03226100 HAL Id: hal-03226100 https://hal.archives-ouvertes.fr/hal-03226100 Submitted on 16 May 2021 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Hydrol. Earth Syst. Sci., 21, 3183–3198, 2017 https://doi.org/10.5194/hess-21-3183-2017 © Author(s) 2017. This work is distributed under the Creative Commons Attribution 3.0 License. Flood risk perception and adaptation capacity: a contribution to the socio-hydrology debate Sven Fuchs1, Konstantinos Karagiorgos1, Kyriaki Kitikidou2, Fotios Maris3, Spyridon Paparrizos4,a, and -
Base Metal Mineralisation in the Evros and Rhodope
BASE METAL MINERALISATION IN THE EVROS REGION, THRACE, N.E. HELLAS K.L. Ashworth1, M.F. Billett1, D. Constantinides2, A. Demetriades2, 2 2 C. Katirtzoglou and C. Michael 1. Department of Geology, University of Southampton, Southampton, SO9 5NH, U.K. 2. Institute of Geology and Mineral Exploration, 70 Messoghion Ave., Athens, 115 27, Hellas In: G.H. Friedrich, P.M. Herzig (Editors), 1988. Base metal sulphide deposits in sedimentary and volcanic environments. Proceedings of the DMG-GDMB-SGA- Meeting Aachen, 1985. Special Publication No. 5 of the Society for Geology Applied to Mineral Deposits. Springer-Verlag, Berlin, Heidelberg, p.168-181. Abstract The stratiform and vein base metal sulphide mineralisation of the Evros region has been emplaced during three major metallogenetic periods: the Pre-, Early- and Mid-Alpidic orogenic era. The Pre-Alpidic mineralisation is associated with a metamorphosed ophiolitic mafic-ultramafic sequence (Rhodope Massif), the Early Alpidic with tholeiitic metabasalt (Circum-Rhodope Belt) and the Mid-Alpidic mineralisation has its major development in Tertiary sedimentary and calc-alkaline igneous rocks. These types of mineralisation, depending on their geotectonic setting, are considered to be similar to that of the Limassol Forest Plutonic Complex (Rhodope Massif), to volcanic-exhalative and analogous to Cyprus volcanogenic massive sulphides (Circum- Rhodope Belt), and to stratiform sediment hosted and veins of volcanic affiliation (Tertiary volcano-sedimentary basins). 1. Introduction The Evros region is situated in north-eastern Hellas and is bounded to the north and east by Bulgaria and Turkey (Fig. 1). It shows a history of some minor exploration and mining activity which started during the Turkish and Bulgarian occupation of Thrace in the late 19th and early 20th century.