Problems of Water Buffalo Breeding in Turkey and Suggestions for Its Development
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The European Union's Black Sea Region Policy*
* THE EUROPEAN UNION’S BLACK SEA REGION POLICY AVRUPA BİRLİĞİ’NİN KARADENİZ BÖLGESİ POLİTİKASI ПОЛИТИКА ЕВРОСОЮЗА К ЧЕРНОМОРСКОМУ РЕГИОНУ ** Assist. Prof. Dr. Haydar EFE ABSTRACT After Romania and Bulgaria entrance in to the EU, the Black Sea region has become very important for the European Union. First of all, stability and security in the Black Sea region is important for the EU. This region is also a main concern for the European Union regarding of preventing the spread of organized crime and terrorism. On the other hand, this region is an important hub for energy and transport flows for the EU. The EU is an important economic and trading partner for the Black Sea countries and makes many efforts to stimulate democratic and economic reforms and supports regional development of the whole region. In this context, “Black Sea Synergy” Programme as an EU initiative was launched in 2007, and finally in May 2009, the EU adopted the “Eastern Partnership” a plan to foster closer political and economic ties with these countries of the region. Key Words: European Union, Black Sea region, Black Sea Synergy, Eastern Partnership ÖZET Bulgaristan ve Romanya’nın AB’ye girmesinden sonra, Karadeniz bölgesi Avrupa Birliği için çok önemli hale geldi. İlk olarak, Karadeniz Bölgesinde istikrar ve güvenlik AB için önemlidir. Bu bölge organize suçlar ve terörizmin yayılmasını önlemede Avrupa Birliği için bir endişe kaynağıdır. Öte yandan, bu bölge AB için enerji ve ulaşım için önemli bir terminaldir. AB Karadeniz ülkelerinin önemli bir ekonomik ve ticari ortağıdır ve tüm bölgede bölgesel kalkınmayı desteklemekte ve demokratik ve ekonomik reformları teşvik etmek için çok çaba harcamaktadır. -
A 2020 Vision for the Black Sea Region a Report by the Commission on the Black Sea
A 2020 Vision for the Black Sea Region A Report by the Commission on the Black Sea www.blackseacom.eu An initiative of: The Black eaS Trust for Regional Cooperation A 2020 Vision for the Black Sea Region A Report by the Commission on the Black Sea Contents Why read this Report? 4 What is the Commission on the Black Sea? 7 Executive Summary 12 Резюме выводов 15 Yönetici Özeti 19 The Report Introduction: The State of Play 22 Peace and Security 28 Economic Development and Welfare 31 Democratic Institutions and Good Governance 34 Regional Cooperation 36 Conclusions 38 Policy Recommendations 40 The Black Sea in Figures 45 Abbreviations 65 Initiators 67 The Rapporteurs, Editor and Acknowledgements 69 Imprint 70 3 Why read this Report? Why read this Report? … because the Black Sea matters The Black Sea region is coming into its own - but it is a contested and sometimes dangerous neighbourhood. It has undergone countless political transformations over time. And now, once again, it is becoming the subject of an intense debate. This reflects the changing dynamics of the Black Sea countries and the complex realities of their politics and conflicts, economies and societies. Geography, the interests of others and the region’s relations with the rest of the world in large part explain its resurgence. Straddling Europe and Asia, the Black Sea links north to south and east to west. Oil, gas, transport and trade routes are all crucial in explaining its increasing relevance. In the last two decades the Black Sea has changed beyond recognition. We have witnessed the transformation of the former communist societies and the impact of globalisation. -
The Cole Collection
THE COLE COLLECTION If you would like more information on the collection or would like to access one of the documents, please send an email to [email protected] with the accompanying file number. A Zoryan Institute representative will get back to you within 48 hours. _________________________________________________________ THE COLE COLLECTION Journals, Letters, Lectures, Documents, Photographs, and Artifacts of Royal M. Cole and Lizzie C. Cole American Missionaries in Armenian and Kurdistan Turkey in the years 1868-1908 (c) 1996, M. Malicoat --------------- TABLE OF CONTENTS --------------- I. Royal Cole's journals: (a) Bound copy-book journals . p. 1 (b) Three smaller journals: 1. ‘Erzeroom Journal: War Times, 1877 - 1878’ . p. 7 2. ‘Travel Reminiscences’ . p. 7 3. Royal Cole’s personal diary of 1896: events at Bitlis, Van, and Moush; the Knapp affair: the persecution of American missionaries; relief work for Garjgan refugees . p. 7 II. Royal Cole’s copy-book journals: loose sheets: (a) Handwritten . p. 8 (b) Typed . p. 12 III. Drafts and notes for two projected volumes by Rev. Cole: (a) Dr. Cole’s Memoirs: ‘Interior Turkey Reminiscences, Forty Years in Kourdistan (Armenia)’ . p. 14 (b) ‘The Siege of Erzroom’; miscellaneous notes on The Russo-Turkish War . p. 15 IV. Newspaper articles by Royal Cole; miscellaneous newspaper articles on the subject of Armenian Turkey, in English, by various writers . p. 16 V. Lectures, essays, and letters by Mrs. Cole (Lizzie Cobleigh Cole) (a) Lectures . p. 17 (b) Copy-book journal loose-sheet essays and copy-book journal entries . p. 19 (c) Letters . p. 20 VI. Massacres in the Bitlis and Van provinces, 1894 - 1896: Sasun; Ghelieguzan; Moush; Garjgan sancak: charts, lists, maps . -
Climate Change Projections of Temperature and Precipitation In
Climate Change Projections of Temperature and Precipitation in the Eastern Black Sea Basin, Turkey by using Multivariate Adaptive Regression Splines Statistical Downscaling Method Sinan NACAR ( [email protected] ) Tokat Gaziosmanpaşa University https://orcid.org/0000-0003-2497-5032 Murat KANKAL Bursa Uludağ University Umut OKKAN Balıkesir University Research Article Keywords: Eastern Black Sea Basin, Climate Change, MARS, Statistical Downscaling Posted Date: August 17th, 2021 DOI: https://doi.org/10.21203/rs.3.rs-647619/v1 License: This work is licensed under a Creative Commons Attribution 4.0 International License. Read Full License Climate change projections of temperature and precipitation in the Eastern Black Sea Basin, Turkey by using multivariate adaptive regression splines statistical downscaling method Sinan NACAR*1, Murat KANKAL2, Umut OKKAN3 1Tokat Gaziosmanpaşa University, Department of Civil Engineering, 60150, Tokat, Turkey, [email protected] 2Bursa Uludağ University, Department of Civil Engineering, 16059, Bursa, Turkey, [email protected] 3Balıkesir University, Department of Civil Engineering, 10600, Balıkesir, Turkey, [email protected] *Corresponding author: Sinan Nacar, Ph.D. (Email: [email protected]) Author ORCID ID Sinan Nacar 0000-0003-2497-5032 Murat Kankal 0000-0003-0897-4742 Umut Okkan 0000-0003-1284-3825 Climate change projections of temperature and precipitation in the Eastern Black Sea Basin, Turkey by using multivariate adaptive regression splines statistical downscaling method Sinan Nacar*1, Murat Kankal2, Umut Okkan3 1Tokat Gaziosmanpaşa University, Department of Civil Engineering, 60150, Tokat, Turkey, [email protected] 2Bursa Uludağ University, Department of Civil Engineering, 16059, Bursa, Turkey, [email protected] 3Balıkesir University, Department of Civil Engineering, 10600, Balıkesir, Turkey, [email protected] *Corresponding author: Sinan Nacar, Ph.D. -
Where Is the Black Sea Region in Turkey's Foreign Policy?
TurcasIlan165x235mmENG copy.pdf 1 22.12.2014 15:12 WHERE IS THE BLACK SEA REGION IN TURKEY’S FOREIGN POLICY? C Black Sea regional analyses often assume that Turkey holds the role of a regional M leader pursuing its intra-regional interests. In contrast to this perspective, this article will present evidence verifying an absence of a Black Sea regional Y conception in Turkey’s foreign policy. It will show how Turkey’s vision related to CM the Black Sea is limited to maritime security and control of the Turkish Straits. As MY this study reveals, even if Turkey perceives itself as a regional leader, this region CY does not include the Black Sea; Ankara has far bigger ambitions, seeing itself in the center of the Afro-Eurasian geography. Such an approach to the Black Sea CMY region makes it very unlikely for Turkey to promote regional integration, much less K see itself as part of the region at all. Sophia Petriashvili* Fall 2015 * Dr. Sophia Petriashvili is an Assistant Professor in the International Relations Department, Faculty of Social and Political Sciences at Tbilisi State University, Georgia. 105 VOLUME 14 NUMBER 3 SOPHIA PETRIASHVILI ith the longest shoreline among all the Black Sea littoral states, Turkey’s outlook towards the Black Sea region is greatly preconditioned by its historical background. For centuries, starting from the conquest of W Crimea in 1475 up to 1774 when the Treaty of Küçük Kaynarca was signed, the Black Sea was regarded as an Ottoman lake and had gained the status of an inner sea of the Empire.1 The Ottoman Empire enjoyed the exclusive right to con- trol the Turkish Straits, which required all foreign vessels passing through the Straits to obtain permission from the Sublime Porte. -
Turkey and Black Sea Security 3
SIPRI Background Paper December 2018 TURKEY AND SUMMARY w The Black Sea region is BLACK SEA SECURITY experiencing a changing military balance. The six littoral states (Bulgaria, siemon t. wezeman and alexandra kuimova* Georgia, Romania, Russia, Turkey and Ukraine) intensified their efforts to build up their military potential after Russia’s The security environment in the wider Black Sea region—which brings takeover of Crimea and the together the six littoral states (Bulgaria, Georgia, Romania, Russia, Turkey start of the internationalized and Ukraine) and a hinterland including the South Caucasus and Moldova— civil war in eastern Ukraine is rapidly changing. It combines protracted conflicts with a significant con- in 2014. ventional military build-up that intensified after the events of 2014: Russia’s Although security in the takeover of Crimea and the start of the internationalized civil war in eastern Black Sea region has always Ukraine.1 Transnational connections between conflicts across the region been and remains important for and between the Black Sea and the Middle East add further dimensions of Turkey, the current Turkish insecurity. As a result, there is a blurring of the conditions of peace, crisis defence policy seems to be and conflict in the region. This has led to an unpredictable and potentially largely directed southwards, high-risk environment in which military forces with advanced weapons, towards the Middle East. including nuclear-capable systems, are increasingly active in close proxim- Russian–Turkish relations have been ambiguous for some years. ity to each other. Turkey has openly expressed In this context, there is an urgent need to develop a clearer understanding concern about perceived of the security dynamics and challenges facing the wider Black Sea region, Russian ambitions in the Black and to explore opportunities for dialogue between the key regional security Sea region and called for a actors. -
Thermochronology of the Miocene Arabia-Eurasia Collision Zone of Southeastern Turkey GEOSPHERE; V
Research Paper GEOSPHERE Thermochronology of the Miocene Arabia-Eurasia collision zone of southeastern Turkey GEOSPHERE; v. 14, no. 5 William Cavazza1, Silvia Cattò1, Massimiliano Zattin2, Aral I. Okay3, and Peter Reiners4 1Department of Biological, Geological and Environmental Sciences, University of Bologna, 40126 Bologna, Italy https://doi.org/10.1130/GES01637.1 2Department of Geosciences, University of Padua, 35131 Padua, Italy 3Eurasia Institute of Earth Sciences, Istanbul Technical University, Maslak 34469, Istanbul, Turkey 4Department of Geosciences, University of Arizona, Tucson, Arizona 85721, USA 9 figures; 3 tables CORRESPONDENCE: william .cavazza@ unibo.it ABSTRACT ocean, and has been linked to mid-Cenozoic global cooling, Red Sea rifting, extension in the Aegean region, inception of the North and East Anatolian CITATION: Cavazza, W., Cattò, S., Zattin, M., Okay, The Bitlis-Pütürge collision zone of SE Turkey is the area of maximum in- strike-slip fault systems, and development of the Anatolian-Iranian continental A.I., and Reiners, P., 2018, Thermochronology of the Miocene Arabia-Eurasia collision zone of southeast- dentation along the >2400-km-long Assyrian-Zagros suture between Arabia and plateau (e.g., Şengör and Kidd, 1979; Dewey et al., 1986; Jolivet and Faccenna, ern Turkey: Geosphere, v. 14, no. 5, p. 2277–2293, Eurasia. The integration of (i) fission-track analyses on apatites, ii( ) (U-Th)/He 2000; Barazangi et al., 2006; Robertson et al., 2007; Allen and Armstrong, 2008; https:// doi .org /10 .1130 /GES01637.1. analyses on zircons, (iii ) field observations on stratigraphic and structural rela- Yılmaz et al., 2010). The age of the continental collision has been the topic of tionships, and (iv) preexisting U-Pb and Ar-Ar age determinations on zircons, much debate, with proposed ages ranging widely from the Late Cretaceous to Science Editor: Raymond M. -
Ölüm Ve Zulmün Üç Hali: Birinci Dünya Savaşı'nda Bitlis
Akademik İncelemeler Dergisi (Journal of Academic Inquiries) 1 Cilt/Volume: 9, Sayı/Issue: 2, Yıl/Year: 2014 Ölüm ve Zulmün Üç Hali: Birinci Dünya Savaşı’nda Bitlis Cephesi Three State of Death and Oppression: Bitlis Front in World War I Adem Ölmez Özet Bu makalede Birinci Dünya Savaşı’nda Bitlis’te Müslümanların ve Erme- nilerin çektiği sıkıntılar, üç aşama/hal halinde anlatılmaktadır. Birinci aşa- ma, Rusların ilk taarruzları sırasında Müslümanlara yaptıkları katliamlardır. İkinci aşama, 1915 ortalarında yerli Ermenilerin çektiği sıkıntılardır. Bilin- diği gibi, Rusların geri çekilmesi üzerine bölgedeki Ermeniler korunmasız kaldılar. Bu süreçte Müslümanların saldırılarına maruz kaldılar ve göçe zor- landılar. Üçüncü hal ise, 1916 başlarında Rusların yeniden saldırıya geçme- leriyle başladı. 1916 başlarından itibaren Bitlis üzerinden güneye ilerlemeyi planladılar; ancak planları istedikleri gibi gitmedi. Bitlis’te düzenli ordularla milis güçlerinin ittifak ettiği büyük bir direnişle karşılaştılar. Rus-Ermeni bir- likleri Bitlis’i geçebilmek için büyük katliamlar yaptılar. Müslüman ahalinin yaşadığı yerlerde kadın, çocuk ve ihtiyarlardan oluşan grupları toplu olarak katlettiler. Rus Ermeni kuvvetleri yeniden Müslüman ahaliye zulmetmeye başladılar. Bu süreç Rusya’da Bolşevik devriminin belirtilerinin görülmeye başlamasına kadar devam etti. Ermenilerin Ruslarla birlikte hareket ederek eski komşuları olan Müslümanlara zulmetmesi Müslümanlar arasında Er- menilere karşı büyük nefretlerin oluşmasına zemin hazırladı. Daha sonraki olaylarda bu nefretlerin büyük payı oldu. Anahtar Kelimeler:Bitlis, Birinci Dünya Savaşı, Ermeni, Rus, Kürt Milis- leri. Doç. Dr., İstanbul Medeniyet Üniversitesi, Edebiyat Fakültesi, Tarih Bölümü, [email protected] Bu makale iThenticate sistemi tarafından taranmıştır. 2 Adem Ölmez Abstract In this paper describes in three phases, the suffering of Muslims and Arme- nians in Bitlis. The first stage are the massacres committed by the Russians against Muslims, during the first attack. -
Crustal Structure of the Eastern Anatolia Region (Turkey) Based on Seismic Tomography
geosciences Article Crustal Structure of the Eastern Anatolia Region (Turkey) Based on Seismic Tomography Irina Medved 1,2,* , Gulten Polat 3 and Ivan Koulakov 1 1 Trofimuk Institute of Petroleum Geology and Geophysics SB RAS, Prospekt Koptyuga, 3, 630090 Novosibirsk, Russia; [email protected] 2 Sobolev Institute of Geology and Mineralogy SB RAS, Prospekt Koptyuga, 3, 630090 Novosibirsk, Russia 3 Department of Civil Engineering, Yeditepe University, 26 Agustos Yerleskesi, 34755 Istanbul, Turkey; [email protected] * Correspondence: [email protected]; Tel.: +7-952-922-49-67 Abstract: Here, we investigated the crustal structure beneath eastern Anatolia, an area of high seismicity and critical significance for earthquake hazards in Turkey. The study was based on the local tomography method using data from earthquakes that occurred in the study area provided by the Turkiye Cumhuriyeti Ministry of Interior Disaster and Emergency Management Directorate Earthquake Department Directorate of Turkey. The dataset used for tomography included the travel times of 54,713 P-waves and 38,863 S-waves from 6355 seismic events. The distributions of the resulting seismic velocities (Vp, Vs) down to a depth of 60 km demonstrate significant anomalies associated with the major geologic and tectonic features of the region. The Arabian plate was revealed as a high-velocity anomaly, and the low-velocity patterns north of the Bitlis suture are mostly associated with eastern Anatolia. The upper crust of eastern Anatolia was associated with a ~10 km thick high-velocity anomaly; the lower crust is revealed as a wedge-shaped low-velocity anomaly. This kind of seismic structure under eastern Anatolia corresponded to the hypothesized existence of Citation: Medved, I.; Polat, G.; a lithospheric window beneath this collision zone, through which hot material of the asthenosphere Koulakov, I. -
The Black Sea Region — Shores and Delta
Black Sea region. page 1 European Environment Agency Europe’s biodiversity — biogeographical regions and seas Biogeographical regions in Europe The Black Sea Region — shores and delta Original contributions from ETC/NPB: Sophie Condé, Dominique Richard (coordinators) Nathalie Liamine (editor) Anne-Sophie Leclère (data collection and processing) Barbara Sotolargo (drafting) Ulla Pinborg (final co-editor) Map production: UNEP/GRID Warsaw (final production) Project manager: Tor-Björn Larsson, EEA ZooBoTech HB, Sweden, Linus Svensson (final edition) Black Sea region. page 2 Summary ............................................................................................................ 3 1. What are the main characteristics and trends of the Black Sea biogeographical region? ..................................................................................... 3 1.1 General characteristics.............................................................................. 3 1.1.1 Extent and limitations ............................................................................ 3 1.1.2 Geomorphological and topography ........................................................... 3 1.1.3 Soils .................................................................................................... 4 1.1.4 Climate ................................................................................................ 4 1.2 Present biodiversity status and trends: habitats, fauna and flora ............. 5 1.2.1 Habitats .............................................................................................. -
Displacement of the Buildings According to Site-Specific
Ŕ Periodica Polytechnica Displacement of the Buildings Civil Engineering According to Site-Specific Earthquake Spectra 60(1), pp. 37–43, 2016 DOI: 10.3311/PPci.7661 Ercan I¸sık, Mustafa Kutanis, Ihsan˙ Engin Bal Creative Commons Attribution RESEARCH ARTICLE Received 13-08-2014, revised 02-04-2015, accepted 30-05-2015 Abstract 1 Introduction The probabilistic seismic hazard curves were based on appro- The seismic risk of building stock is of growing interest for priate attenuation relationships at rock sites with a probability academia as well as for governments due to the increasing ur- of exceedance of 10% in 50 years in this study. Results from banization and concentration of populations in earthquake prone the model were compared to the response spectra proposed in and vulnerable areas. Since 1999 Izmit˙ earthquake, Turkey has Section 7 of TEC ‘07 and were found to differ in both ampli- become recognized as one of the most earthquake-prone regions tude and frequency content. The impact of these differences has in the world. This is true considering that most of the country been investigated with respect to building performance evalua- is mapped as having probabilities of peak ground acceleration tion. Specifically, modal capacity diagrams and response spec- PGA (up to 9.8 m/sec2). tra have been obtained for five buildings. Based on the dia- Seismic hazard analysis of the earthquake-prone Eastern Ana- grams and spectra, peak displacements have been calculated as tolia region of Turkey has become more important due to its well, revealing significant differences in the demand displace- growing strategic importance as a global energy corridor and ment curves of the buildings. -
The Geodynamics of the Aegean and Anatolia: Introduction
Downloaded from http://sp.lyellcollection.org/ by guest on September 27, 2021 The geodynamics of the Aegean and Anatolia: introduction T. TAYMAZ1, Y. YILMAZ2 & Y. DILEK3 1Department of Geophysical Engineering,˙ Istanbul Technical University, Maslak, TR–34469,˙ Istanbul, Turkey (e-mail: [email protected]) 2Kadir Has University, Fatih, I˙stanbul, Turkey 3Department of Geology, Miami University, Oxford, OH 45056, USA The complexity of the plate interactions and and volcanism in Anatolia and the Aegean region associated crustal deformation in the Eastern (Taymaz et al. 2004). Mediterranean region is reflected in many destruc- tive earthquakes that have occurred throughout Regional synthesis its recorded history, many of which are well documented and intensively studied. The Eastern Given its location in the Alpine–Himalayan Mediterranean region, including the surrounding orogenic belt, and at the collisional boundary areas of western Turkey and Greece, is indeed one between Gondwana and Laurasia, the geological of the most seismically active and rapidly deform- history of the Aegean region and Anatolia involves ing regions within the continents (Fig. 1). Thus, the Mesozoic–Cenozoic closure of several Neo- the region provides a unique opportunity to tethyan oceanic basins, continental collisions and improve our understanding of the complexities of subsequent post-orogenic processes (e.g. Sengo¨r continental tectonics in an actively collisional & Yılmaz 1981; Bozkurt & Mittwede 2001; Okay orogen. The major scientific observations from et al. 2001; Dilek & Pavlides 2006; Robertson & this natural laboratory have clearly been helping Mountrakis 2006). The opening of oceanic branches us to better understand the tectonic processes in of Neotethys commenced in the Triassic and active collision zones, the mode and nature of they closed during the Late Cretaceous to Eocene continental growth, and the causes and distribution time interval.