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Durham E-Theses
Durham E-Theses Neolithic and chalcolithic cultures in Turkish Thrace Erdogu, Burcin How to cite: Erdogu, Burcin (2001) Neolithic and chalcolithic cultures in Turkish Thrace, Durham theses, Durham University. Available at Durham E-Theses Online: http://etheses.dur.ac.uk/3994/ Use policy The full-text may be used and/or reproduced, and given to third parties in any format or medium, without prior permission or charge, for personal research or study, educational, or not-for-prot purposes provided that: • a full bibliographic reference is made to the original source • a link is made to the metadata record in Durham E-Theses • the full-text is not changed in any way The full-text must not be sold in any format or medium without the formal permission of the copyright holders. Please consult the full Durham E-Theses policy for further details. Academic Support Oce, Durham University, University Oce, Old Elvet, Durham DH1 3HP e-mail: [email protected] Tel: +44 0191 334 6107 http://etheses.dur.ac.uk NEOLITHIC AND CHALCOLITHIC CULTURES IN TURKISH THRACE Burcin Erdogu Thesis Submitted for Degree of Doctor of Philosophy The copyright of this thesis rests with the author. No quotation from it should be published without his prior written consent and information derived from it should be acknowledged. University of Durham Department of Archaeology 2001 Burcin Erdogu PhD Thesis NeoHthic and ChalcoHthic Cultures in Turkish Thrace ABSTRACT The subject of this thesis are the NeoHthic and ChalcoHthic cultures in Turkish Thrace. Turkish Thrace acts as a land bridge between the Balkans and Anatolia. -
93 Fari Dismessi. Dall'abbandono Alla
Annali del Turismo, V, 2016, n.1 Edizioni Geoprogress FARI DISMESSI. DALL’ABBANDONO ALLA RIGENERAZIONE Antonietta Ivona Abstract Lighthouses decommissioned. From abandonment to regeneration. - The Italian legislation on cultural heritage introduced, a few years ago, the concept of enhancement and enjoyment of cultural heritage through the outsourcing of cultural assistance and hospitality services for the public. Particularly, the national Project "Valore Paese" of the Agenzia del Demanio is dedicated to lighthouses and it intends to encourage the promotion of the Italian public real estate through the synergy between the sectors of tourism, art and culture, economic and territorial cohesion. In this sense, the recovery of public assets owned by the State and local authorities has the possibility to be considered not only in terms of cost to the community, but also as a significant lever for territorial and social development, in a logic of public- private partnership. 1. I fari nel tempo Opere di ingegneria umana, ammantate di miti e leggende, i fari sono parte della storia della navigazione. Dai bagliori dei primi fuochi accesi sulle torri di avvistamento fino ai recenti dibattiti sul futuro della rete dei fari, essi hanno da sempre rappresentato anche luoghi identitari. I primi fari che la storia conosce non erano altro che falò di legna accatastata situati nei luoghi più pericolosi per segnalare la rotta ai naviganti. “I primi fuochi, che dovevano restare accesi tutta la notte, richiedevano continua cura: occorreva combustibile, sapienza tecnica, presenza costante dell’uomo” (Mariotti, 2013, p. 10). Con l’evolversi della navigazione commerciale, occorse sostituire i falò con strumenti di segnalazione più sicuri e, quindi, più potenti da ubicare nei porti lungo le nuove rotte commerciali. -
Challenges and Opportunities for Sustainable Management of Water Resources in the Island of Crete, Greece
water Review Challenges and Opportunities for Sustainable Management of Water Resources in the Island of Crete, Greece V. A. Tzanakakis 1,2,*, A. N. Angelakis 3,4 , N. V. Paranychianakis 5, Y. G. Dialynas 6 and G. Tchobanoglous 7 1 Hellenic Agricultural Organization Demeter (HAO-Demeter), Soil and Water Resources Institute, 57001 Thessaloniki, Greece 2 Department of Agriculture, School of Agricultural Science, Hellenic Mediterranean University, Iraklion, 71410 Crete, Greece 3 HAO-Demeter, Agricultural Research Institution of Crete, 71300 Iraklion, Greece 4 Union of Water Supply and Sewerage Enterprises, 41222 Larissa, Greece; [email protected] 5 School of Environmental Engineering, Technical University of Crete, 73100 Chania, Greece; [email protected] 6 Department of Civil and Environmental Engineering, University of Cyprus, Nicosia 1678, Cyprus; [email protected] 7 Department of Civil and Environmental Engineering, University of Davis, Davis, CA 95616, USA; [email protected] * Correspondence: [email protected] Received: 12 April 2020; Accepted: 16 May 2020; Published: 28 May 2020 Abstract: Crete, located in the South Mediterranean Sea, is characterized by long coastal areas, varied terrain relief and geology, and great spatial and inter-annual variations in precipitation. Under average meteorological conditions, the island is water-sufficient (969 mm precipitation; theoretical water potential 3284 hm3; and total water use 610 hm3). Agriculture is by far the greatest user of water (78% of total water use), followed by domestic use (21%). Despite the high average water availability, water scarcity events commonly occur, particularly in the eastern-south part of the island, driven by local climatic conditions and seasonal or geographical mismatches between water availability and demand. -
Palaeogeography, Harbour Potential and Salt Resources Since the Greek and Roman Periods at the Promontory of Pachino
Palaeogeography, harbour potential and salt resources since the Greek and Roman periods at the promontory of Pachino. Preliminary results and perspectives Salomon Ferréol, Darío Bernal-Casasola, Cécile Vittori, Hatem Djerbi To cite this version: Salomon Ferréol, Darío Bernal-Casasola, Cécile Vittori, Hatem Djerbi. Palaeogeography, harbour potential and salt resources since the Greek and Roman periods at the promontory of Pachino. Pre- liminary results and perspectives. Darío Bernal-Casasola; Daniele Malfitana; Antonio Mazzaglia; José Juan Díaz. Le cetariae ellenistiche e romane di Portopalo (Sicilia) / Las cetariae helenisticas y ro- manas de Portopalo (Sicilia), Supplement – 1, pp.217-233, 2021, HEROM - Journal on Hellenistic an Roman material culture, 2294-4273. hal-03230863 HAL Id: hal-03230863 https://hal.archives-ouvertes.fr/hal-03230863 Submitted on 20 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. Palaeogeography, harbour potential and salt resources since the Greek and Roman periods at the promontory of Pachino. Preliminary results and perspectives Ferréol Salomon, Darío Bernal-Casasola, Cécile Vittori and Hatem Djerbi Introduction Cicogna was surveyed along with the Pantano Morghella part of the Riserva naturale orientate ai Pantani della Sicilia Sud-Orientale. -
Strong Ground Motion Characteristics from the 17 August 1999 Kocaeli, Turkey Earthquake
BOLLETTINO DI GEOFISICA TEORICA ED APPLICATA VOL. 43, N. 1-2, PP. 37-52; MAR.-JUN. 2002 Strong ground motion characteristics from the 17 August 1999 Kocaeli, Turkey earthquake A. AKINCI Istituto Nazionale di Geofisica e Vulcanologia, Roma, Italy (Received July 2, 2001; accepted December 21, 2001) Abstract - The 17 August 1999 Kocaeli, Turkey earthquake (Mw.=.7.4, USGS) occurred in the western part of the North Anatolian Fault Zone about 80 km east of Istanbul. The mechanism of the main event was almost a pure right-lateral strike- slip, and the aftershock distribution indicates that the rupture was located toward the western end of the North Anatolian Fault Zone. The earthquake affected a wide area in the Marmara region, as well as the city of Istanbul. Most of the damage and fatalities occurred in towns located on the narrow, flat shoreline of the Sea of Marmara. Since the broken fault segment traversed the densely populated and industrialized east Marmara region, damage was enormously high. Widespread liquefactions caused bearing capacity losses and consequent foundation failu- res in the Adapazari region, as well as extensive subsidence along the shoreline in Gölcük (Gulf of Izmit) and Sapanca. The earthquake struck also the western suburbs of Istanbul, the Avcilar region, causing severe damage on buildings even though the distance from the epicenter was about 80 km. In this study, we discuss the ground motion characteristics, as well as directivity and soil effects of recorded ground acceleration of the Kocaeli earthquake. Strong-motion data were obtained from the networks managed by the Bogaziçi University, Kandilli Observatory and Earthquake Research Institute and by the General Director of Disaster Affairs, Earthquake Research Department. -
Clusters of Megaearthquakes on Upper Plate Faults Control the Eastern 1
Originally published as: Mouslopoulou, V., Nicol, A., Begg, J. G., Oncken, O., Moreno, M. (2015): Clusters of mega-earthquakes on upper-plate faults control the Eastern Mediterranean hazard. - Geophysical Research Letters, 42, 23, pp. 10282—10289. DOI: http://doi.org/10.1002/2015GL066371 PUBLICATIONS Geophysical Research Letters RESEARCH LETTER Clusters of megaearthquakes on upper plate faults 10.1002/2015GL066371 control the Eastern Mediterranean hazard Key Points: Vasiliki Mouslopoulou1, Andrew Nicol2, John Begg3, Onno Oncken1, and Marcos Moreno1 • Uplift along the Hellenic forearc transient due to earthquake clustering 1German Research Centre for Geosciences, GFZ Helmholtz Centre Potsdam, Germany, 2Department of Geological Sciences, • Earthquakes occur mostly on upper 3 plate faults rather than the plate University of Canterbury, Christchurch, New Zealand, GNS Science, Lower Hutt, New Zealand interface • Seismic hazard in Eastern Mediterranean underestimated Abstract The Hellenic subduction margin in the Eastern Mediterranean has generated devastating historical earthquakes and tsunamis with poorly known recurrence intervals. Here stranded paleoshorelines indicate – Supporting Information: strong uplift transients (0 7 mm/yr) along the island of Crete during the last ~50 kyr due to earthquake • Supporting Information S1 clustering. We identify the highest uplift rates in western Crete since the demise of the Minoan civilization and • Table S1 along the entire island between ~10 and 20 kyr B.P., with the absence of uplifted Late Holocene paleoshorelines in the east being due to seismic quiescence. Numerical models show that uplift along the Hellenic margin is Correspondence to: V. Mouslopoulou, primarily achieved by great earthquakes on major reverse faults in the upper plate with little contribution [email protected] from plate-interface slip. -
Block and Boulder Accumulations on the Southern Coast of Crete (Greece): Evidence for the 365 CE Tsunami in the Eastern Mediterranean
Boulton & Whitworth, 2016 Boulder deposits, Crete Block and boulder accumulations on the southern coast of Crete (Greece): evidence for the 365 CE tsunami in the Eastern Mediterranean. Sarah J. Boulton1*, Michael R.Z. Whitworth1, 2, 1School of Geography, Earth and Environmental Sciences, Plymouth University, Plymouth, Devon, PL4 8AA, U.K. 2 AECOM, Mayflower House, Armada Way, Plymouth, Devon, PL1 1LD. *Correspondence ([email protected]) The Eastern Mediterranean is one of the most seismically active regions in Europe. Crete, located in the centre of the Eastern Mediterranean, should experience tsunamis resulting from large magnitude earthquakes or volcanic eruptions. At three locations boulders were observed that may relate to tsunami or storm events. At Lakki, the size of the boulders slightly favours a tsunami origin for deposition. By contrast, at Kommos boulder size and geomorphology is consistent with storm parameters in the Mediterranean. The most compelling evidence for tsunami transport is found at Diplomo Petris, where a lithologically varied grouping of large boulders (≤ 690 t) is exposed at sea level. The calculated storm wave heights (15 m) required to transport the observed boulders significantly exceeds winter averages; therefore, these accumulations are interpreted as tsunami deposits. Radiocarbon dating of encrusting biological material was undertaken to constrain periods of boulder motion. Encrustations from Diplomo Petris and Lakki pre-date the 365 CE earthquake suggesting that this event transported the largest boulders; the first time boulder deposits have been identified on Crete from this tsunami. Therefore, these data are important for developing local and regional hazard assessments but also to inform numerical models of tsunami propagation in the Mediterranean. -
Earthquake Source Parameters Along the Hellenic Subduction Zone and Numerical Simulations of Historical Tsunamis in the Eastern Mediterranean
Tectonophysics 536–537 (2012) 61–100 Contents lists available at SciVerse ScienceDirect Tectonophysics journal homepage: www.elsevier.com/locate/tecto Earthquake source parameters along the Hellenic subduction zone and numerical simulations of historical tsunamis in the Eastern Mediterranean Seda Yolsal-Çevikbilen ⁎, Tuncay Taymaz Istanbul Technical University, the Faculty of Mines, Department of Geophysical Engineering, Maslak TR-34469, Istanbul, Turkey article info abstract Article history: We studied source mechanism parameters and slip distributions of earthquakes with Mw ≥5.0 occurred dur- Received 25 March 2011 ing 2000–2008 along the Hellenic subduction zone by using teleseismic P- and SH-waveform inversion Received in revised form 26 January 2012 methods. In addition, the major and well-known earthquake-induced Eastern Mediterranean tsunamis Accepted 13 February 2012 (e.g., 365, 1222, 1303, 1481, 1494, 1822 and 1948) were numerically simulated and several hypothetical tsu- Available online 25 February 2012 nami scenarios were proposed to demonstrate the characteristics of tsunami waves, propagations and effects of coastal topography. The analogy of current plate boundaries, earthquake source mechanisms, various Keywords: Active tectonics earthquake moment tensor catalogues and several empirical self-similarity equations, valid for global or Earthquakes local scales, were used to assume conceivable source parameters which constitute the initial and boundary Eastern Mediterranean conditions in simulations. Teleseismic inversion results showed that earthquakes along the Hellenic subduc- Slip distribution tion zone can be classified into three major categories: [1] focal mechanisms of the earthquakes exhibiting E– Source rupture parameters W extension within the overriding Aegean plate; [2] earthquakes related to the African–Aegean convergence; Tsunamis and [3] focal mechanisms of earthquakes lying within the subducting African plate. -
Greece) - in Situ Conserva Tion Required
Erwin Bergmeier Seasonal pools in the vegetation of Gavdos (Greece) - in situ conserva tion required Abstract Bergmeier, E.: Seasonal pools in the vegetation of Gavdos (Greece) - in situ conservation required. - Bocconea 13: 511-516. 2001. - ISSN 1120-4060. Flora, vegetation, and inundation regime of rock pools on Gavdos, the southemmost European island, are described in detail. Requirements for nature conservation are also addressed. The seasonally water-filled cavities provide habitat for several rare species, inc1uding Calli/riche pulchra, and Ma/ricaria aurea with their single Greek locali ti es in the island. Five plant com munities may be distinguished along an ecological gradient of decreasing water level and inun dation periodo Introduction 2 Gavdos (32 km ) IS the southernmost European island (34°48-52'N 24°02-08'E). Although geographically (37 km) close to western Crete, it shows important differences in floristics and vegetation. The vascular flora consists of some 460 taxa, c. 30 (6 %) of which do not occur in western Crete but are chiefly south Mediterranean/north African species at their northern border of distribution (Bergmeier & al. 1997). Mean annual precipitation in Gavdos is less than 400 mm. Geological formations inclu de tertiary sediments with sandy soils in the northeast, crystalline limestone in the south west, and minor ares with flysch and ophiolithic substrata (Vicente 1970). Gavdos inhabi tants have decreased to less than 50 to date but summer tourism is esxpanding. Extensive grazing by goats and sheep occurs throughout the island. Most remarkable among the unique features of the island are small karstic rock pools and depressions seasonally filled with rain water which were already noticed as important plant habitats by Dorfler when collecting on the island in 1904 (Vierhapper & Rechinger 1935). -
Assessment of Tsunami-Related Geohazard Assessment for Hersek Peninsula and Gulf of İzmit Coasts Cem Gazioğlu
ISSN:2148-9173 IJEGEO Vol: 4(2) May 2017 International Journal of Environment and Geoinformatics (IJEGEO) is an international, multidisciplinary, peer reviewed, open access journal. Assessment of Tsunami-related Geohazard Assessment for Hersek Peninsula and Gulf of İzmit Coasts Cem Gazioğlu Editors Prof. Dr. Cem Gazioğlu, Prof. Dr. Dursun Zafer Şeker, Prof. Dr. Ayşegül Tanık, Assoc. Prof. Dr. Şinasi Kaya Scientific Committee Assoc. Prof. Dr. Hasan Abdullah (BL), Assist. Prof. Dr. Alias Abdulrahman (MAL), Assist. Prof. Dr. Abdullah Aksu, (TR); Prof. Dr. Hasan Atar (TR), Prof. Dr. Lale Balas (TR), Prof. Dr. Levent Bat (TR), Assoc. Prof. Dr. Füsun Balık Şanlı (TR), Prof. Dr. Nuray Balkıs Çağlar (TR), Prof. Dr. Bülent Bayram (TR), Prof. Dr. Şükrü T. Beşiktepe (TR), Dr. Luminita Buga (RO); Prof. Dr. Z. Selmin Burak (TR), Assoc. Prof. Dr. Gürcan Büyüksalih (TR), Dr. Jadunandan Dash (UK), Assist. Prof. Dr. Volkan Demir (TR), Assoc. Prof. Dr. Hande Demirel (TR), Assoc. Prof. Dr. Nazlı Demirel (TR), Dr. Arta Dilo (NL), Prof. Dr. A. Evren Erginal (TR), Dr. Alessandra Giorgetti (IT); Assoc. Prof. Dr. Murat Gündüz (TR), Prof. Dr. Abdulaziz Güneroğlu (TR); Assoc. Prof. Dr. Kensuke Kawamura (JAPAN), Dr. Manik H. Kalubarme (INDIA); Prof. Dr. Fatmagül Kılıç (TR), Prof. Dr. Ufuk Kocabaş (TR), Prof. Dr. Hakan Kutoğlu (TR), Prof. Dr. Nebiye Musaoğlu (TR), Prof. Dr. Erhan Mutlu (TR), Assist. Prof. Dr. Hakan Öniz (TR), Assoc. Prof. Dr. Hasan Özdemir (TR), Prof. Dr. Haluk Özener (TR); Assoc. Prof. Dr. Barış Salihoğlu (TR), Prof. Dr. Elif Sertel (TR), Prof. Dr. Murat Sezgin (TR), Prof. Dr. Nüket Sivri (TR), Assoc. Prof. Dr. Uğur Şanlı (TR), Assoc. -
USGS Circular 1193
FOLD BLEED BLEED BLEED BLEED U.S. Geological Survey Implications for Earthquake Risk Reduction in the United States from the — Kocaeli, Turkey, Earthquake Implications for Earthquake Risk Reduction in the U.S. from Kocaeli, of August 17, 1999 T urkey , Earthquake — U.S. Geological Survey Circular 1 U.S. Geological Survey Circular 1193 193 U.S. Department of the Interior U.S. Geological Survey BLEED BLEED BLEED FOLD BLEED FOLD BLEED BLEED Cover: Damage in Korfez, Turkey, following the August 17 Kocaeli earthquake. Photograph by Charles Mueller Cover design by Carol A. Quesenberry Field investigations were coordinated with the U.S. Army Corps of Engineers and National Institute of Standards and Technology BLEED BLEED FOLD FOLD BLEED BLEED Implications for Earthquake Risk Reduction in the United States from the Kocaeli, Turkey, Earthquake of August 17, 1999 By U.S. Geological Survey U.S. Geological Survey Circular 1193 U.S. Department of the Interior U.S. Geological Survey BLEED FOLD BLEED FOLD BLEED BLEED BLEED BLEED U.S. Department of the Interior Contributors Bruce Babbitt, Secretary Thomas L. Holzer, Scientific Editor, U.S. Geological Survey U.S. Geological Survey Aykut A. Barka, Istanbul Technical University, Turkey Charles G. Groat, Director David Carver, U.S. Geological Survey Mehmet Çelebi, U.S. Geological Survey Edward Cranswick, U.S. Geological Survey Timothy Dawson, San Diego State University and Southern California Earthquake Center James H. Dieterich, U.S. Geological Survey William L. Ellsworth, U.S. Geological Survey Thomas Fumal, U.S. Geological Survey John L. Gross, National Institute of Standards and Technology Robert Langridge, U.S. -
Myanmar: the Golden Land
VOL. 16, NO. 1 – 2019 GEOSCIENCE & TECHNOLOGY EXPLAINED geoexpro.com GEOEDUCATION Creating Excitement in the EXPLORATION Geosciences Myanmar: The Golden Land GEOTOURISM Australia’s Big Outdoor Museum TECHNOLOGY The Pre-Drill Prediction Toolbox HISTORY OF OIL Mr Five Per Cent Make Better Decisions on Indonesia Exploration Opportunities North Sumatra South Makassar 3D acquisition ongoing Fast-track available Q2 2019 North Madura West Timor PSTM and PSDM High density fast-track available now available Q2 2019 Broadband Data Available for Viewing The latest PGS MultiClient 3D GeoStreamer surveys enable a better understanding of the plays and prospectivity oshore Indonesia. To find out more about these surveys and new acquisition plans, visit our website or contact [email protected]. A Clearer Image | www.pgs.com/Indonesia Previous issues: www.geoexpro.com Contents Vol. 16 No. 1 This edition of GEO ExPro focuses on Australasia and South East Asia, New GEOSCIENCE & TECHNOLOGY EXPLAINED Technologies, and Training Geoscientists. 5 Editorial ; 6 Regional Update Gulbenkian: Revealing the man behind the myths. 8 Licensing Update 10 A Minute to Read 14 Cover Story Exploration: Myanmar - The Golden Land v 18 Hot Spot: Great Expectations PetroEDGE Virtual field trips offer an integrated and flexible 20 Seismic Foldout: learning resource. Gippsland Basin Rejuvenated 26 GEO Education: Creating Excitement in the Geosciences Y 30 History of Oil: Mr Five per Cent, The last frontier in seismic Calouste Gulbenkian interpretation is getting a step closer. 34 GEO Education: Eliis Field Trips in a Virtual World I 38 Technology Explained: Robert Hall East Indonesian geology suggests The Pre-Drill Prediction Toolbox that relatively recent tectonic events had spectacular consequences on 42 Seismic Foldout: palaeogeography and life.