Measurement of Input Usage Efficiency in Cotton Production in Diyarbakir Province, Turkey
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Special Issue “The Next Marmara Earthquake: Disaster Mitigation
Hori et al. Earth, Planets and Space (2017) 69:65 DOI 10.1186/s40623-017-0648-9 PREFACE Open Access Special issue “The next Marmara earthquake: disaster mitigation, recovery, and early warning” Takane Hori1*, Ali Pinar2, Ocal Necmioglu2, Muneo Hori3 and Azusa Nishizawa4 Te Marmara Sea, accommodating the fault segments of with Mw = 7.25 on the Main Marmara Fault is expected a major transform fault, is well known as a seismic gap to heavily damage or destroy 2–4% of the near 1,000,000 along the North Anatolian Fault (NAF), running through buildings in Istanbul, which has a population of around the northern part of Turkey and connecting the East 13 million, with 9–15% of the buildings receiving Anatolian convergent area with the Hellenic subduction medium damage and 20–34% of the buildings lightly zone (e.g., Pınar 1943; Toksöz et al. 1979; Pondard et al. damaged (Erdik 2013). 2007; Şengör et al. 2014). It is obvious from historical Te aim of this special issue is to gather information records spanning more than 2000 years that the region about the risk of another Marmara earthquake from the is subject to frequent strong shaking that is likely associ- latest geophysical, geological, geotechnical, computa- ated with tsunami waves, threatening heavily populated tional, and building science research results to discuss and industrialized locations (Ambraseys 2002; Erdik et al. ways of mitigating disaster in advance. Te collection 2004; Hébert et al. 2005). In the twentieth century, mag- of 12 papers constituting this special issue is based on nitude (M) 7-class earthquakes sequentially occurred recent research on imaging the crustal structure, the from east to west along the NAF zone, as shown in Fig. -
Assessing Urbanization Dynamics in Turkey's Marmara Region Using CORINE Data Between 2006 and 2018
remote sensing Article Assessing Urbanization Dynamics in Turkey’s Marmara Region Using CORINE Data between 2006 and 2018 Özlem Altınkaya Genel 1,2 and ChengHe Guan 3,4,* 1 Kenniscentrum NoorderRuimte, Hanze University of Applied Sciences, Groningen Zernikeplein 1, 9747 AS Groningen, The Netherlands; [email protected] 2 Faculty of Architecture and Design, Özye˘ginUniversity, Orman Sk.13, Istanbul˙ 34794, Turkey 3 Arts and Sciences, New York University Shanghai, 1555 Century Avenue, Pudong New District, Shanghai 200122, China 4 Shanghai Key Laboratory of Urban Renewal and Spatial Optimization Technology, Tongji University, Shanghai 200122, China * Correspondence: [email protected] Abstract: This study investigated the urban growth dynamics of urban regions. The study area was the Marmara Region, one of the most densely populated and ecologically diverse areas in Turkey. Using CORINE land cover data for 2006, 2012, and 2018, the study utilized multiple correspondence analyses and cluster analyses, to analyze land cover changes. The resulting maps, visualized in GIS, revealed the rapid urban transformation of the regional structure, formerly comprised of four distinct areas, into a more complex structure, in which densification and sprawl occur simultaneously. Our findings demonstrated a dissonance between the spatial dynamics of the Marmara Region during the study period, and the capacity and scope of the simultaneously initiated regional policies and mega-projects. This uncoordinated approach has endangered the region’s sustainable development. The paper, therefore, discusses the importance of land use planning and transboundary collaboration Citation: Genel, Ö.A.; Guan, C. for sustainable regional development. Beyond the local case, the results contribute to critical theories Assessing Urbanization Dynamics in in regional planning by linking theory and practice. -
The Potential of Regional Centers in Turkey Related to Growth of the Core Regions
A Service of Leibniz-Informationszentrum econstor Wirtschaft Leibniz Information Centre Make Your Publications Visible. zbw for Economics Gezici, Ferhan Conference Paper The Potential of Regional Centers in Turkey Related to Growth of the Core Regions 39th Congress of the European Regional Science Association: "Regional Cohesion and Competitiveness in 21st Century Europe", August 23 - 27, 1999, Dublin, Ireland Provided in Cooperation with: European Regional Science Association (ERSA) Suggested Citation: Gezici, Ferhan (1999) : The Potential of Regional Centers in Turkey Related to Growth of the Core Regions, 39th Congress of the European Regional Science Association: "Regional Cohesion and Competitiveness in 21st Century Europe", August 23 - 27, 1999, Dublin, Ireland, European Regional Science Association (ERSA), Louvain-la-Neuve This Version is available at: http://hdl.handle.net/10419/114244 Standard-Nutzungsbedingungen: Terms of use: Die Dokumente auf EconStor dürfen zu eigenen wissenschaftlichen Documents in EconStor may be saved and copied for your Zwecken und zum Privatgebrauch gespeichert und kopiert werden. personal and scholarly purposes. Sie dürfen die Dokumente nicht für öffentliche oder kommerzielle You are not to copy documents for public or commercial Zwecke vervielfältigen, öffentlich ausstellen, öffentlich zugänglich purposes, to exhibit the documents publicly, to make them machen, vertreiben oder anderweitig nutzen. publicly available on the internet, or to distribute or otherwise use the documents in public. Sofern die Verfasser die Dokumente unter Open-Content-Lizenzen (insbesondere CC-Lizenzen) zur Verfügung gestellt haben sollten, If the documents have been made available under an Open gelten abweichend von diesen Nutzungsbedingungen die in der dort Content Licence (especially Creative Commons Licences), you genannten Lizenz gewährten Nutzungsrechte. -
Republic of Turkey Ministry of Transport General Directorate of Highways
MOTORWAY DEVELOPMENT PROGRAM of TURKEY HEEP AREA V ANNUAL MEETING Suceava, ROMANIA 13/18‐06‐2011 MOTORWAY DEVELOPMENT PROGRAM of TURKEY OUTLINE 1. Turkish Road Network 2. General Overview of Road Investments 3. Target PPP Motorway Projects‐Vision 2023 4. Decision Making Procedure of PPP Motorway Projects in Turkey 5. Financial Feasibility of PPP Motorway Projects 6. Gebze ‐İzmir Motorway Project 7. North Marmara Motorway Project 8. Conclusion MOTORWAY DEVELOPMENT PROGRAM of TURKEY 1. Turkish Road Network • The lands of Turkey are located at a point where the three continents; Asia, Africa and Europe are closest to each other, and straddle the point where Europe and Asia meet. • Being located on a passing channel of intercontinental links Turkey has always been an important channel of international trade links MOTORWAY DEVELOPMENT PROGRAM of TURKEY 1. Turkish Road Network • The public roads in Turkey classified in four-tier system: motorways (multi-lane access-controlled highways), state roads, provincial roads and rural roads. •General Directorate of Turkish Highways ( KGM) is responsible for the planning, maintenance, construction and operation of motorways, state and provincial roads. •Special Provincial Administration is in the charge of village and forest roads. • Urban roads are under the administration of municipal authorities. • The road network excluding urban roads is about 354000 km in length. MOTORWAY DEVELOPMENT PROGRAM of TURKEY 1. Turkish Road Network • Motorways are the divided state roads with full control of access and two or more lanes for the exclusive use of traffic in each direction to provide uninterrupted flow, on which opposing traffic is separated by a median and collection of tolls are performed at designated points. -
An Earthquake Gap South of Istanbul
ARTICLE Received 23 Jan 2013 | Accepted 9 May 2013 | Published 18 Jun 2013 DOI: 10.1038/ncomms2999 An earthquake gap south of Istanbul Marco Bohnhoff1,2, Fatih Bulut1, Georg Dresen1, Peter E. Malin3, Tuna Eken1 & Mustafa Aktar4 Over the last century the North Anatolian Fault Zone in Turkey has produced a remarkable sequence of large earthquakes. These events have now left an earthquake gap south of Istanbul and beneath the Marmara Sea, a gap that has not been filled for 250 years. Here we investigate the nature of the eastern end of this gap using microearthquakes recorded by seismographs primarily on the Princes Islands offshore Istanbul. This segment lies at the western terminus of the 1999 Mw7.4 Izmit earthquake. Starting from there, we identify a 30-km-long fault patch that is entirely aseismic down to a depth of 10 km. Our evidence indicates that this patch is locked and is therefore a potential nucleation point for another Marmara segment earthquake—a potential that has significant natural hazards implications for the roughly 13 million Istanbul residents immediately to its north. 1 Helmholtz-Centre Potsdam German Centre for Geosciences GFZ, Telegrafenberg, 14473 Potsdam, Germany. 2 Department of Earth Sciences, Freie Universita¨t Berlin, Malteser Strasse 74-100, 12249 Berlin, Germany. 3 Institute of Earth Science and Engineering, University of Auckland, Auckland, New Zealand. 4 Kandilli Observatory and Earthquake Research Institute, Bogazici University, 34342 Bebek, Cengelko¨y, Istanbul, Turkey. Correspondence and requests for materials should be addressed to M.B. (email: [email protected]). NATURE COMMUNICATIONS | 4:1999 | DOI: 10.1038/ncomms2999 | www.nature.com/naturecommunications 1 & 2013 Macmillan Publishers Limited. -
Frictional Strength of North Anatolian Fault in Eastern Marmara Region Ali Pınar* , Zeynep Coşkun, Aydın Mert and Doğan Kalafat
Pınar et al. Earth, Planets and Space (2016) 68:62 DOI 10.1186/s40623-016-0435-z FULL PAPER Open Access Frictional strength of North Anatolian fault in eastern Marmara region Ali Pınar* , Zeynep Coşkun, Aydın Mert and Doğan Kalafat Abstract Frequency distribution of azimuth and plunges of P- and T-axes of focal mechanisms is compared with the orientation of maximum compressive stress axis for investigating the frictional strength of three fault segments of North Anato- lian fault (NAF) in eastern Marmara Sea, namely Princes’ Islands, Yalova–Çınarcık and Yalova–Hersek fault segments. In this frame, we retrieved 25 CMT solutions of events in Çınarcık basin and derived a local stress tensor incorporating 30 focal mechanisms determined by other researches. As for the Yalova–Çınarcık and Yalova–Hersek fault segments, we constructed the frequency distribution of P- and T-axes utilizing 111 and 68 events, respectively, to correlate the geometry of the principle stress axes and fault orientations. The analysis yields low frictional strength for the Princes’ Island fault segments and high frictional strength for Yalova–Çınarcık, Yalova–Hersek segments. The local stress ten- sor derived from the inversion of P- and T-axes of the fault plane solutions of Çınarcık basin events portrays nearly horizontal maximum compressive stress axis oriented N154E which is almost parallel to the peak of the frequency dis- tribution of the azimuth of the P-axes. The fitting of the observed and calculated frequency distributions is attained for a low frictional coefficient which is about μ 0.1. Evidences on the weakness of NAF segments in eastern Marmara Sea region are revealed by other geophysical≈ observations. -
Joint Meeting and Field Trip of IGCP 610 and INQUA POCAS Focus Group, Antalya, Turkey, 14-21 October 2018
Joint Meeting and Field Trip of IGCP 610 and INQUA POCAS Focus Group, Antalya, Turkey, 14-21 October 2018 TECTONICALLY MODIFIED COASTAL SHORELINE IN THE MARMARA REGION, NW TURKEY: EVIDENCE FROM THE ARCHEOLOGICAL SITE Koral, H. 1, Tur, H.2 Aydıngün, Ş. 3, and İşbil, D., 1 1Istanbul University, Department of Geological Engineering, Istanbul, Turkey 34320, hkoral @istanbul.edu.tr ; [email protected] 2İstanbul University, Department of Geophysical Engineering, Istanbul, Turkey 34320 [email protected] 3Kocaeli University, Department of Archaeology, Izmit, Turkey 41380 [email protected] Keywords: Coastal modification, North Anatolian Fault Zone, Prince Islands, KüçükÇek- mece Lagoon, Iznik Lake, Byzantine Establishment Active tectonic structures are present along the coast of the Marmara Sea and surrounding areas, extensively modifying the Neogene-Quaternary sequence (e.g., Barka and Ka- dinsky-Cade,1988, Koral and Şen, 1995, Koral, 1998). The units were folded and faulted by neotectonic structures, some of which are linked to the seismically active North Anato- lian Fault Zone (NAFZ). Proximity of a submerged or elevated ancient settlement to the nearby active tectonic feature is evidence for a tectonically induced coastal change in the Marmara region (Fig. 1). A small submerged rocky mass named ‘Yıldız Kayalıkları/Vordonisi’ is one the Prince Islands, located about 1 km south of the Asian coast of the city of Istanbul in the Marmara Sea (Fig. 1). The Prince Islands comprise nine closely spaced islands with unique tectonic geological features (e.g., Isbil, 2012; Tur, 2007). Historical records and underwater searches indicate ‘Vordonisi’ is said to have supported a monastery during the Byzantine time, circa 850 AD, which now lies submerged under several meters of water (Meriç, 2010). -
Neotectonics of the Southeast Marmara Region, NW Anatolia, Turkey
Journal of Asian Earth Sciences 21 (2003) 1041–1051 www.elsevier.com/locate/jseaes Neotectonics of the southeast Marmara region, NW Anatolia, Turkey O¨ mer Feyzi Gu¨rer*, Nuretdin Kaymakc¸ı, S¸erafeddin C¸ akır, Muzaffer O¨ zburan Kocaeli University, Engineering Faculty, Department of Geology, Kocaeli TR 41100, Turkey Received 26 October 2001; revised 24 May 2002; accepted 4 September 2002 Abstract The North Anatolian Fault Zone (NAFZ) bifurcates into three branches in the Marmara Region, which is a transition zone between the strike–slip tectonics manifested by the NAFZ and the N–S directed extensional regime of western Anatolia. The southern Marmara region is characterized by the middle and the southern branches while the northern branch controls the north Marmara region. The south Marmara region is characterized by approximately E–W trending rhomb-like horst and graben complexes bounded by strike slip-faults with normal component, striking mainly in E–W direction. This study documents the geometry and the structural characteristics of the NAFZ in the southeast Marmara region and discusses the commencement age of the strike–slip tectonics using deformation patterns of Neogene units and information available in the literature. q 2002 Elsevier Science Ltd. All rights reserved. Keywords: Marmara sea; Neotectonics; North Anatolian fault zone; Extensional regime 1. Introduction regime which causes N–S extension of western Anatolia and the Aegean Sea area and (2) the strike–slip tectonics exerted Turkey has suffered two severe earthquakes that occurred by the NAFZ. The former is effective in a broad zone from along two segments of the North Anatolian Fault Zone Bulgaria in the north to the Hellenic trench in the south (NAFZ) on 17 August 1999 (Mw 7.4) and 12 November (McKenzie, 1972). -
Drilling the North Anatolian Fault
Part 2 : Overview of Recent Projects Drilling the North Anatolian Fault CZ(FPSH%SFTFO .VTUBGB"LUBS .BSDP#PIOIPGG BOE)BMVL&ZJEPHBO BOE )BMVL &ZJEPHBO EPJJPEQTET The North Anatolian Fault Zone (NAFZ) represents a Dardanelles Peninsula merging with the Ganos Fault. Here, ~1400-km-long plate boundary that slips at an average rate of the last M>7 earthquake occurred in 1912 rupturing approxi- 20–30 mm yr-1. It separates the westward moving Anatolian mately 60 km into the Sea of Marmara. block in the south from Eurasia in the north (McClusky et al., 2000). Comparison of long-term slip rates (6.5 mm yr-1 for In the eastern Sea of Marmara, five seismic events with the last 13 Ma, 17 mm yr-1 for the last 5 Ma,) with Holocene M>6 have occurred since 1509. The events in 1509, 1754, and GPS-derived slip rates (20–25 mm yr-1) indicate an accel- 1766, and 1894 generated tsunamis with waves exceeding erated movement in the recent geological past. During the 6 m in height in some cases. Also, the 1999 Izmit earthquake, twentieth century, the NAFZ has ruptured over 900 km of its reflecting pure strike-slip faulting, generated a minor length. A series of large earthquakes starting in 1939 near tsunami with local wave heights >2 m. Erzincan in eastern Anatolia propagated westward towards the Istanbul-Marmara region in northwestern Turkey. A Current seismic activity in the eastern Marmara Sea large part of the Sea of Marmara today represents a seismic indicates the seismic gap south of Istanbul and a complex gap along a ≥100-km-long segment which did not rupture fault network active at the transition between the western since 1766 and may have accumulated a slip deficit of 4–5 m. -
The Status of Diurnal Birds of Prey in Turkey
j. RaptorRes. 39(1):36-54 ¸ 2005 The Raptor ResearchFoundation, Inc. THE STATUS OF DIURNAL BIRDS OF PREY IN TURKEY LEVENT TURAN 1 HacettepeUniversity, Faculty of Education, Department of BiologyEducation, 06532 Beytepe,Ankara, Turkey ABSTRACT.--Here,I summarize the current statusof diurnal birds of prey in Turkey This review was basedon field surveysconducted in 2001 and 2002, and a literature review.I completed661 field surveys in different regionsof Turkey in 2001 and 2002. I recorded37 speciesof diurnal raptors,among the 40 speciesknown in the country In addition, someadverse factors such as habitat loss, poisoning, killing, capturingor disturbingraptors, and damagingtheir eggswere seen during observations. KEYWORDS: EasternEurope,, population status; threats;, Turkey. ESTATUSDE LASAVES DE PRESADIURNAS EN TURQUiA RESUMEN.--Aquiresumo el estatusactual de las avesde presa diurnas en Turquia. Esta revisi6nest2 basadaen muestreosde campo conducidosen 2001 y 2002, yen una revisi6nde la literatura. Complet• 661 muestreosde campo en diferentesregiones de Turquia en 2001 y 2002. Registr• 37 especiesde rapacesdiurnas del total de 40 especiesconocidas para el pals. Ademfis,registra algunos factores ad- versoscomo p•rdida de hfibitat, envenenamiento,matanzas, captura o disturbiode rapacesy dafio de sus huevos durante las observaciones. [Traducci6n del equipo editorial] Turkey, with approximately454 bird species,has servations of diurnal raptors collected during a relatively rich avian diversity in Europe. Despite 2001-02 from locationsthroughout Turkey. recognized importance of the country in support- METHODS ing a significantbiodiversity, mapping of the avi- fauna has not occurred and there are few data on Turkey is divided into sevengeographical regions (Fig. the statusof birds in Turkey. 1; Erol et al. 1982) characterizedby variable landscape types,climate differences,and a rich diversityof fauna Among the birds of Turkey are included 40 di- Field data were obtained from surveysconducted in all urnal birds of prey and 10 owls. -
Regional Disparities and Territorial Indicators in Turkey: Socio-Economic Development Index (SEDI)
A Service of Leibniz-Informationszentrum econstor Wirtschaft Leibniz Information Centre Make Your Publications Visible. zbw for Economics Ozaslan, Metin; Dincer, Bulent; Ozgur, Huseyin Conference Paper Regional Disparities and Territorial Indicators in Turkey: Socio-Economic Development Index (SEDI) 46th Congress of the European Regional Science Association: "Enlargement, Southern Europe and the Mediterranean", August 30th - September 3rd, 2006, Volos, Greece Provided in Cooperation with: European Regional Science Association (ERSA) Suggested Citation: Ozaslan, Metin; Dincer, Bulent; Ozgur, Huseyin (2006) : Regional Disparities and Territorial Indicators in Turkey: Socio-Economic Development Index (SEDI), 46th Congress of the European Regional Science Association: "Enlargement, Southern Europe and the Mediterranean", August 30th - September 3rd, 2006, Volos, Greece, European Regional Science Association (ERSA), Louvain-la-Neuve This Version is available at: http://hdl.handle.net/10419/118537 Standard-Nutzungsbedingungen: Terms of use: Die Dokumente auf EconStor dürfen zu eigenen wissenschaftlichen Documents in EconStor may be saved and copied for your Zwecken und zum Privatgebrauch gespeichert und kopiert werden. personal and scholarly purposes. Sie dürfen die Dokumente nicht für öffentliche oder kommerzielle You are not to copy documents for public or commercial Zwecke vervielfältigen, öffentlich ausstellen, öffentlich zugänglich purposes, to exhibit the documents publicly, to make them machen, vertreiben oder anderweitig nutzen. publicly available on the internet, or to distribute or otherwise use the documents in public. Sofern die Verfasser die Dokumente unter Open-Content-Lizenzen (insbesondere CC-Lizenzen) zur Verfügung gestellt haben sollten, If the documents have been made available under an Open gelten abweichend von diesen Nutzungsbedingungen die in der dort Content Licence (especially Creative Commons Licences), you genannten Lizenz gewährten Nutzungsrechte. -
Maritime Traffic Regulations for the Turkish Straits and the Marmara Region, Entered Into Force on 1 July 1994
Page 1 Maritime Traffic Regulations for the Turkish Straits and the Marmara Region, entered into force on 1 July 1994 PART I PURPOSE, SCOPE AND DEFINITIONS Purpose and scope Article 1 The purpose of these Regulations, which shall apply to all ships navigating in the Straits and the Sea of Marmara, is to regulate the maritime traffic scheme in order to ensure the safety of navigation, life and property and to protect the environment in the region. Definitions Article 2 For the purposes of these Regulations: (a) "Administration" means T.C. Basbakanlik Denizcilik Müstesarligi (Under-Secretariat for Maritime Affairs); (b) "The Straits and the Marmara region" means the maritime area comprising the Sea of Marmara, the Strait of Istanbul (the Bosphorus), the Strait of Canakkale (the Dardanelles) and the coastlines surrounding this area; (c) "The Straits" mean the area within the boundaries of the Strait of Istanbul and the Strait of Canakkale; (d) "Vessel" means any vehicle able to navigate at sea except craft under oars; (e) "Vessel in transit" means a vessel, the passage of which shall be innocent, continuous, expeditious and without delay. The passage through the Straits and the Marmara region shall be planned so as not to stop at any port, berth or any other place, and a notification to that effect shall have been made by the master of the vessel to the Turkish authorities before entering into the Straits; (f) "A vessel interrupting its transit passage" means a vessel the master or commander of which has notified during passage that the vessel has given up its transit passage; (g) "Vessel whose transit passage has been interrupted" means a vessel, which, due to maritime accidents such as collision and grounding, or for other reasons, is subject to investigations, legal proceedings and inquiries carried out by the Turkish administrative or legal authorities; (h) Nuclear-powered vessels or vessels carrying nuclear, noxious and dangerous goods and wastes mean: 1.