DOCSLIB.ORG

Geomorphological Features of Marmara Sea Islands

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Geomorphological Features of Marmara Sea Islands ISSN: 2148-9173 Vol: 6 Issue:1 April 2019 International Journal of Environment and Geoinformatics (IJEGEO) is an international, multidisciplinary, peer reviewed, open access journal. Geomorphological features of Marmara Sea Islands Hakan KAYA Chief in Editor Prof. Dr. Cem Gazioğlu Co-Editor Prof. Dr. Dursun Zafer Şeker, Prof. Dr. Şinasi Kaya, Prof. Dr. Ayşegül Tanık and Assist. Prof. Dr. Volkan Demir Editorial Committee (2019) Assos. Prof. Dr. Abdullah Aksu (TR), Prof. Dr. Bedri Alpar (TR), Prof. Dr. Lale Balas (TR), Prof. Dr. Levent Bat (TR), Prof. Dr. Paul Bates (UK), Prof. Dr. Bülent Bayram (TR), Prof. Dr. Luis M. Botana (ES), Prof. Dr. Nuray Çağlar (TR), Prof. Dr. Sukanta Dash (IN), Dr. Soofia T. Elias (UK), Prof. Dr. A. Evren Erginal (TR), Assoc. Prof. Dr. Cüneyt Erenoğlu (TR), Dr. Dieter Fritsch (DE), Assos. Prof. Dr. Çiğdem Göksel (TR), Prof.Dr. Lena Halounova (CZ), Dr. Hakan Kaya (TR), Assoc. Prof. Dr. Maged Marghany (MY), Prof. Dr. Michael Meadows (ZA), Prof. Dr. Nebiye Musaoğlu (TR), Prof. Dr. Erhan Mutlu (TR), Prof. Dr. Masafumi Nakagawa (JP), Prof. Dr. Hasan Özdemir (TR), Prof.Dr. Chryssy Potsiou (GR), Prof. Dr. Erol Sarı (TR), Prof. Dr. Maria Paradiso (IT), Prof. Dr. Petros Patias (GR), Prof. Dr. Elif Sertel (TR), Prof. Dr. Nüket Sivri (TR), Assoc. Prof. Dr. Füsun Balık Şanlı (TR), Prof. Dr. Uğur Şanlı (TR), Assoc. Prof. Dr. Oral Yağcı (US), Prof. Dr. Seyfettin Taş (TR), Assoc. Prof. Dr. Ömer Suat Taşkın (TR), Dr. İnese Varna (LV), Dr. Petra Visser (NL), Prof. Dr. Selma Ünlü (TR), Assoc. Prof. Dr. İ. Noyan Yılmaz (AU), Prof. Dr. Murat Yakar (TR), Assit. Prof. Dr. Sibel Zeki (TR) Abstracting and Indexing: DOAJ, Index Copernicus, OAJI, Scientific Indexing Services, JF, Google Scholar International Journal of Environment and Geoinformatics 6(1): 57-66 (2019) Reaserch Article Geomorphological features of Marmara Sea Islands Hakan Kaya Istanbul University, Institute of Marine Sciences and Management, 34134 VEFA Fatih Istanbul TR Received 28 Feb 2019 E-mail:[email protected] Accepted 26 March 2019 How to cite: Kaya, H.(2019). Geomorphological features of Sea of Marmara Islands, International Journal of Environment and Geoinformatics (IJEGEO), 6(1): 57-66. DOI: 10.30897/ijegeo.533694 Abstract The Sea of Marmara is located on a continental crust. The Sea of Marmara, which is a remnant of the Sarmasien period of the Miocene Sea, is an inland sea (Okay, 2007). It opens to the Black Sea with the Bosphorus and the Aegean Sea with the Dardanelles. Its surface area is 11 111 km2 (Gazioğlu, et al., 2002) and its average depth ranges from -200 to -500 m (Doğanay, 1997). At the end of the third time, and at the beginning of the fourth time, there were crumbs and crashes arising from the earth crust movements in and around, where this sea lies today (İzbırak, 1996). In the Marmara Sea, the oldest sediments were deposited as a result of the transformation of the Marmara Sea from a lacustrine environment to a marine environment with the Mediterranean Tyrenian transgression at the end of Middle Pleistocene. When the sea level in the Sea of Marmara is at the same or higher than the present day, water passage from the Black Sea has occurred. At the beginning of Late Pleistocene, as a result of a sudden drop in world sea level, the water passage from the Marmara Sea to the Mediterranean was cut and the marine sedimentation environment was replaced by lacustrine sedimentation. At the beginning of Late Pleistocene (between 64.000-59.000 BC), Mediterranean waters entered the Sea of Marmara and the Black Sea with the sudden rise of sea level (Algan, et al., 2011 ). After the transgression, the gulfs and islands in the Sea of Marmara were formed. Keywords: Sea of Marmara Islands, Marmara, Avşa, Paşalimanı, Büyükada, Heybeliada Introduction The Sea of Marmara is an inland sea in NW Anatolia, Mediterranean waters entered the Sea of Marmara and which is located between the Aegean Sea in the south the Black Sea with the sudden rise of sea level (Algan et and the Black Sea in the north. It has a surface area of 11 al., 2011; Gazioğlu et al., 2010). After the transgression, 110 km2 (max. 280 km. long, max. 80 km. wide) and the gulfs and islands in the Sea of Marmara were formed. lies along east-west direction. It has broad shelf in the The Sea of Marmara can be considered in two groups south (38% proportion to total Sea of Marmara area and regarding its islands. Northern Marmara and South 69% proportion to shelves) and narrower shelf in the Marmara islands. South Marmara islands are; Marmara north area (17% proportion to total Sea of Marmara area Island (117.2 km2), Paşalimanı Island (21.4 km2), Avşa and 31% proportion to shelves). Shelf area has a largest Island (20.6 km2), Koyun, Ekinlik, Yer, Mamalı, proportion among the other morphologic units in the Sea Tavşan, Fener, (Asmalı), Hayırsız, Haliada, Eşek Islands of Marmara (Gazioğlu, et al., 2002; 2017). The E–W- of Balıkesir Province, and İmralı Island (9.98 km2) of oriented basin chain between the Gulf of zmit and the İ Bursa. North Marmara Islands are Büyükada (5.4 km2), Ganos Mountain System is called here the "Marmara Heybeliada (2.5 km2), Burgaz (1.5 km2), Eşek, Sedef, Trough". The four basins are separated by ridges Pide (Kaşık), Kınalıada, Sivriada, and Yassıada constituted in the E-W direction of Marmara Trough (Doğanay, 1997). In this study, physical geography which coincides with the northern branch of the North features of these islands were analysed. Anatolian Fault Zone (NAFZ) (Gazioğlu, et al., 2005; 2014; 2016). Geological Evolution In the Sea of Marmara, the oldest sediments The Sea of Marmara is located in a geologically complex were deposited as a result of the transformation of the area. The formation of the Sea of Marmara, which is Sea of Marmara from a lacustrine environment to a much younger than the Black Sea and the Mediterranean marine environment with the Mediterranean Sea, began with the arrival of the North Anatolian Fault Tyrenian transgression at the end of Middle in the Miocene - Pliocene. The Sea of Marmara consists Pleistocene. When the sea level in the Sea of Marmara of three pits with a depth exceeding one thousand meters is at the same or higher than the present day, water and shelves surrounding these pits. These deep pits are passage from the Black Sea has occurred. At the also basins with Plio-Quaternary sedimentations with a beginning of Late Pleistocene, as a result of a sudden thickness of several kilometers. The pits of the Sea of drop in world sea level, the water passage from the Marmara are deepening and filling grabens due to the Sea of Marmara to the Mediterranean was cut and the movement of the North Anatolian Fault which cuts marine sedimentation environment was replaced by across the Sea of Marmara (Doğanay, 1997; Kaya & lacustrine sedimentation. At the beginning of Late Gazioğlu, 2015). The very narrow northern shelf of the Pleistocene (between 64.000-59.000 BC), 57 Kaya / IJEGEO (6)1: 57-66 (2019) Sea of Marmara is rising due to the movements of the years ago (Görür et al., 1997; Sakınç et al., 1999; Kaya North Anatolian Fault. The much larger southern shelf is et al., 2008; Burak et al., 2009). The Sea of Marmara had shaped by normal faults. Elevations such as Marmara been a terrestrial area covered with lakes and rivers. Island and Kapıdağ form the base blocks of active Following the arrival of the North Anatolian Fault in the normal faults. The Sea of Marmara is a very young region, the basins were formed as a result of the vertical geological area that is formed by the effect of the North movements along the fault, and the Sea of Marmara Anatolian Fault. Although the formation of the Black (Okay, 2007; Gökaşan eta l., 2001; İsmail & Gazioğlu, Sea and the Eastern Mediterranean reaches 80 million 2019) was formed as a result of the invasion of those years ago, Sea of Marmara is not present 10 million basins by the sea. Sea of Marmara Figure 1. Study Areas. Geological Features Sedef Island and in the Northeast of Büyükada. In the south of the Büyükada, there is the Kartal member of the Northern Marmara Islands that have been formed in a Pendik formation, which consists of limestones with large time interval from the early Paleozoic to the limestone inter-bedded with mica scaly, clay-mile and present, covers a large number of rock-stratigraphy units thin clastic rocks. Another formation observed at the (İ.B.B, 2009). However, Büyükada is very diverse in southwest of Büyükada is the Denizli Village Formation. geologically. This formation consists of limestone, clayey limestone, nodular limestone, and lidites. In some places, there is The most common observed formation in the islands is inter-bedded thin shale. Slope debris is frequently Kınalıada Formation. This formation consists of encountered on the slopes of the high sections of the sandstone - milestone with feldspar. The whole of northern Marmara islands. Especially east and north- Kinaliada and Burgazada and the major part of facing slopes of Kınalıada there is debris fan that has Heybeliada and the northern half of the Büyükada is been developed starting from the sea coast, reaching up composed of this formation. The Aydos Formation, to 40-50 m altitudes, becoming steeper as ascending which is composed of quartzites, has been distributed in down, and reaching the thickness of 20-30 m (Özgül, the high sections in the southern part of Büyükada. 2011; İ.BB, 2009).
Load more

Recommended publications
  • The Mark of the Japanese Murrelet (Synthliboramphus Wumizusume): a Study of Song and Stewardship in Japan’S Inland Sea
    Claremont Colleges Scholarship @ Claremont Pomona Senior Theses Pomona Student Scholarship 2019 The aM rk of the Japanese Murrelet (Synthliboramphus wumizusume): A study of song and stewardship in Japan’s Inland Sea Charlotte Hyde The Mark of the Japanese Murrelet (Synthliboramphus wumizusume): A study of song and stewardship in Japan’s Inland Sea Charlotte Hyde In partial fulfillment of the Bachelor of Arts Degree in Environmental Analysis, 2018-2019 academic year, Pomona College, Claremont, California Readers: Nina Karnovsky Wallace Meyer Acknowledgements I would first like to thank Professor Nina Karnovsky for introducing me to her work in Kaminoseki and for allowing me to join this incredible project, thereby linking me to a community of activists and scientists around the world. I am also so appreciative for her role as my mentor throughout my years as an undergraduate and for helping me develop my skills and confidence as a scholar and ecologist. Thank you also to my reader Wallace Meyer for his feedback on my writing and structure. I am so thankful for the assistance of Char Miller, who has worked tirelessly to give valuable advice and support to all seniors in the Environmental Analysis Department throughout their thesis journeys. Thank you to Marc Los Huertos for his assistance with R and data analysis, without which I would be hopelessly lost. I want to thank my peers in the Biology and Environmental Analysis departments for commiserating with me during stressful moments and for providing a laugh, hug, or shoulder to cry on, depending on the occasion. Thank you so much to my parents, who have supported me unconditionally throughout my turbulent journey into adulthood and who have never doubted my worth as a person or my abilities as a student.
    [Show full text]
  • COPYRIGHTED MATERIAL 04 518823-Ch01.Qxp 9/24/088:11Pmpage2
    04_518823-ch01.qxp 9/24/08 8:11 PM Page 1 1 Family Highlights of Turkey COPYRIGHTED MATERIAL 04_518823-ch01.qxp 9/24/08 8:11 PM Page 2 TURKEY 0 100 mi R U S S I A 0 100 km BLACKB L A C K SEAS E A BULGARIAB U L G A R I A G E O R G I A EdirneEdirnEdirne SinopSinop 16 AmasraAmasra 4 ZonguldakZonguldak BartinBartin Bafra Family Highlights of Turkey KastamonuKastamonu Artvin SafranboluSafranbolu Ardahan TerkirdaTerkirdağ IstanbulIstanbul EregliEregli 27 KeKeşanan 1 30 20 Samsun Trabzon Rize KarabukKarabuk Ünye Ordu SeaSea ofof MMarmaraarmara GebzeGebze KocaelKKocaeliocaeli SakaryaSakarya DüzceDüzceüzce Kars GallipoliGallipoli 28 BoluBolu Giresun A R M E N I A AegeanAegean YalovYYalovaalova 32 ÇankiriÇankiri SeaSea IIznikznik ÇorumÇorum Amasya Gümüşhane Yerevan IznikIznik22 9 12 BandirmaBandirma GölüGölü Tokat Bayburt 11 ÇanakkaleÇanakkale Turhal BursaBursa InegolInegol Erzurum SincanSincan Karakose BalıkesirBalıkesir ş AnkaraAnkara Doğubayazıt BozüyükBozBozüyüküyük EskiEski ehirehir 5 YozgatYozgat 7 KirikkaleKirikkale Sivas Erzincan PolatliPolatli LesboLLesbosesbos KütahyaKütahya TURKEYT U R K E Y Kemaliye Erçis AkhisarAkhisar Tunceli I R A N KirKirşehirehir Bingol ManisaManisa Mus Uşakak AfyonAfyon Van Gölü ş IzmirIzmir TurgutluTurgutlu KayseriKayseri Van ÇeÇe meme 21 TuzTuz GGölüölü Bitlis SalihliSalihli ÜrgüpÜrgüp Elazığ 14 13 3 AkAkşehirehir 17 OOdOdemisdemismis AksarayAksaray Malatya AegeanAegean ş DinarDinar KuKu adasiadasi 19 HoyranHoyran Siirt SeaSea 24 AydinAydin Diyarbakır SamosSamos 26 GölüGölü NiNiğdede Göksun Batman KonyaKonya
    [Show full text]
  • Assessment of Social Vulnerability Using Geographic Information Systems: Pendik, Istanbul Case Study
    Assessment of Social Vulnerability Using Geographic Information Systems: Pendik, Istanbul Case Study Zeynep Haki, Zuhal Akyürek, Şebnem Düzgün Middle East Technical University, Natural and Applied Sciences, Geodetic and Geographic Information Technologies 06531- Ankara, Turkey [email protected], [email protected], [email protected] SUMMARY This study aims to develop a methodology to define vulnerable groups in terms of their social conditions for any possible hazard, with Geographical Information Systems (GIS) technology, in the case study area of earthquake-prone Pendik, Istanbul. In the calculation of social vulnerability certain indicators were estimated and used as criterion data. Criterion standardization, weighting and combining were accomplished by means of multi-criteria evaluation (MCE) methods, the theoretical background being based on the multi-attribute utility theory (MAUT). In order to avoid the subjectivity of the assessment, 10 more evaluations are utilized. The results show that, the income- and educational-level indicators are the most important factors in defining the social vulnerability. These outputs are supported with some explorative spatial data analyses to understand global trends and spatial interactions in order to be used in pre- and post-disaster planning. Besides, to determine the physical effects of basic services and transportation, some GIS Analyses are applied. The objectivity of the assessment and the complicated structure of the study data are discussed for an effective disaster management. The main outcomes of the methodology and its applications show that, the southwest part of Pendik is socially vulnerable to any possible hazard. KEYWORDS: Social Vulnerability Assessment, Pre- and Post-Disaster Planning, Disaster Management, Spatial Data Analysis, GIS, Pendik-İstanbul INTRODUCTION Natural hazards are the reality of today’s world, which considerably affect people’s living conditions.
    [Show full text]
  • Late Cretaceous–Eocene Geological Evolution of the Pontides Based on New Stratigraphic and Palaeontologic Data Between the Black Sea Coast and Bursa (NW Turkey)
    Turkish Journal of Earth Sciences (Turkish J. Earth Sci.), Vol.Z. ÖZCAN 21, 2012, ET pp. AL. 933–960. Copyright ©TÜBİTAK doi:10.3906/yer-1102-8 First published online 25 April 2011 Late Cretaceous–Eocene Geological Evolution of the Pontides Based on New Stratigraphic and Palaeontologic Data Between the Black Sea Coast and Bursa (NW Turkey) ZAHİDE ÖZCAN1, ARAL I. OKAY1,2, ERCAN ÖZCAN2, AYNUR HAKYEMEZ3 & SEVİNÇ ÖZKAN-ALTINER4 1 İstanbul Technical University (İTÜ), Eurasia Institute of Earth Sciences, Maslak, TR−34469 İstanbul, Turkey (E-mail: [email protected]) 2 İstanbul Technical University (İTÜ), Faculty of Mines, Department of Geology, Maslak, TR−34469 İstanbul, Turkey 3 General Directorate of Mineral Research and Exploration (MTA Genel Müdürlüğü), Geological Research Department, TR−06520 Ankara, Turkey 4 Middle East Technical University (METU), Department of Geological Engineering, Ünversiteler Mahallesi, Dumlupınar Bulvarı No. 1, TR−06800 Ankara, Turkey Received 17 February 2011; revised typescript receipt 04 April 2011; accepted 25 April 2011 Abstract: Th e Late Cretaceous–Eocene geological evolution of northwest Turkey between the Black Sea and Bursa was studied through detailed biostratigraphic characterization of eleven stratigraphic sections. Th e Upper Cretaceous sequence in the region starts with a major marine transgression and lies unconformably on a basement of Palaeozoic and Triassic rocks in the north (İstanbul-type basement) and on metamorphic rocks and Jurassic sedimentary rocks in the south (Sakarya-type basement). Four megasequences have been diff erentiated in the Late Cretaceous–Eocene interval. Th e fi rst one, of Turonian to Late Campanian age, is represented by volcanic and volcanoclastic rocks in the north along the Black Sea coast, and by siliciclastic turbidites and intercalated calcarenites in the south, corresponding to magmatic arc basin and fore-arc basin, respectively.
    [Show full text]
  • Modeling of the Turkish Strait System Using a High Resolution Unstructured Grid Ocean Circulation Model
    Journal of Marine Science and Engineering Article Modeling of the Turkish Strait System Using a High Resolution Unstructured Grid Ocean Circulation Model Mehmet Ilicak 1,* , Ivan Federico 2 , Ivano Barletta 2,3 , Sabri Mutlu 4 , Haldun Karan 4 , Stefania Angela Ciliberti 2 , Emanuela Clementi 5 , Giovanni Coppini 2 and Nadia Pinardi 3 1 Eurasia Institute of Earth Sciences, Istanbul Technical University, Istanbul 34469, Turkey 2 Fondazione Centro Euro-Mediterraneo sui Cambiamenti Climatici, Ocean Predictions and Applications Division, 73100 Lecce, Italy; [email protected] (I.F.); [email protected] (I.B.); [email protected] (S.A.C.); [email protected] (G.C.) 3 Department of Physics and Astronomy, Universita di Bologna Alma Mater Studiorum, 40126 Bologna, Italy; [email protected] 4 TUBITAK MRC Environment and Cleaner Production Institute, Kocaeli 41470, Turkey; [email protected] (S.M.); [email protected] (H.K.) 5 Fondazione Centro Euro-Mediterraneo sui Cambiamenti Climatici, Ocean Modeling and Data Assimilation Division, 40126 Bologna, Italy; [email protected] * Correspondence: [email protected] Abstract: The Turkish Strait System, which is the only connection between the Black Sea and the Mediterranean Sea, is a challenging region for ocean circulation models due to topographic constraints and water mass structure. We present a newly developed high resolution unstructured finite element grid model to simulate the Turkish Strait System using realistic atmospheric forcing and lateral open boundary conditions. We find that the jet flowing from the Bosphorus Strait into the Marmara creates Citation: Ilicak, M.; Federico, I.; an anticyclonic circulation. The eddy kinetic energy field is high around the jets exiting from the Barletta, I.; Mutlu, S.; Karan, H.; Ciliberti, S.A.; Clementi, E.; Coppini, Bosphorus Strait, Dardanelles Strait, and also the leeward side of the islands in the Marmara Sea.
    [Show full text]
  • Paleoseismology of the North Anatolian Fault at Güzelköy
    Paleoseismology of the North Anatolian Fault at Güzelköy (Ganos segment, Turkey): Size and recurrence time of earthquake ruptures west of the Sea of Marmara Mustapha Meghraoui, M. Ersen Aksoy, H Serdar Akyüz, Matthieu Ferry, Aynur Dikbaş, Erhan Altunel To cite this version: Mustapha Meghraoui, M. Ersen Aksoy, H Serdar Akyüz, Matthieu Ferry, Aynur Dikbaş, et al.. Pale- oseismology of the North Anatolian Fault at Güzelköy (Ganos segment, Turkey): Size and recurrence time of earthquake ruptures west of the Sea of Marmara. Geochemistry, Geophysics, Geosystems, AGU and the Geochemical Society, 2012, 10.1029/2011GC003960. hal-01264190 HAL Id: hal-01264190 https://hal.archives-ouvertes.fr/hal-01264190 Submitted on 1 Feb 2016 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. Article Volume 13, Number 4 12 April 2012 Q04005, doi:10.1029/2011GC003960 ISSN: 1525-2027 Paleoseismology of the North Anatolian Fault at Güzelköy (Ganos segment, Turkey): Size and recurrence time of earthquake ruptures west of the Sea of Marmara Mustapha Meghraoui Institut de Physique du Globe de Strasbourg (UMR 7516), F-67084 Strasbourg, France ([email protected]) M. Ersen Aksoy Institut de Physique du Globe de Strasbourg (UMR 7516), F-67084 Strasbourg, France Eurasia Institute of Earth Sciences, Istanbul Technical University, 34469 Istanbul, Turkey Now at Instituto Dom Luiz, Universidade de Lisboa, P-1750-129 Lisbon, Portugal H.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • PENDIK MUNICIPALITY | Erasmus+ Projects
    PENDIK MUNICIPALITY | Erasmus+ Projects The Organisation Erasmus+ Projects in last three years Legal Name Pendik Belediyesi EU Program Year Project ID Applicant / Beneficiary Legal Name (EN) Pendik Municipality Erasmus+ 2017 2017-1-TR01-KA105-044661 Pendik Municipality Address Yeni Mah. Stadyum Sk. No:18 34893 Pendik – Istanbul Erasmus+ 2017 2017-2-TR01-KA105-047556 Pendik Municipality City Istanbul Erasmus+ 2017 2017-2-TR01-KA105-047587 Pendik Municipality Country Turkey Erasmus+ 2017 2017-3-TR01-KA105-048383 Pendik Municipality Website Www.pendik.bel.tr Erasmus+ 2018 2018-3-TR01-KA347-061747 Pendik Municipality E-mail [email protected] Erasmus+ 2018 2018-3-RO01-KA105-061290 Asociatia Be You Phone +90 216 585 11 66 Erasmus+ 2019 2019-1-HU01-KA104-060383 Jó munka szociális szövetkezet Fax +90 216 585 14 86 Erasmus+ 2019 2019-1-TR01-ESC11-065100 Pendik Municipality Type Local Public Body Erasmus+ 2019 2019-1-TR01-KA204-074520 Pendik Municipality Accreditation ESC Erasmus+ 2019 6132019-EPP-1-2019-1-TR-SPO-SSCP Pendik Municipality The LEAR Rüveyda Güzel graduated from Selçuk University International Relations BA degree. She has been working as project specialist since 2012 and leading Project Managemant Unit. Title Mr. She has experience in preparing, implementing, and managing different projects both at Name & Surname Abdulkadir COŞKUN national and international level. She is the coordinator of latest E+ Sport project as well. Position Strategy Development Manager Sümeyye Topal gained her BA from Istanbul Bilgi University – Public Relations and her Phone & Fax +90 216 585 11 00 +90 216 585 14 86 MA Gebze Technical University on Project Management.
    [Show full text]
  • Composition and Abundance of Octocorals in the Sea of Marmara, Where the Mediterranean Meets the Black Sea
    SCIENTIA MARINA 79(1) March 2015, 125-135, Barcelona (Spain) ISSN-L: 0214-8358 doi: http://dx.doi.org/10.3989/scimar.04120.09A Composition and abundance of octocorals in the Sea of Marmara, where the Mediterranean meets the Black Sea Eda N. Topçu 1,2, Bayram Öztürk 1,2 1 Istanbul University Fisheries Faculty, Ordu cad No 200 Laleli, 34470 Istanbul, Turkey. E-mail: [email protected] 2 Turkish Marine Research Foundation, No 10, Beykoz, 81650, Istanbul, Turkey. Summary: Species composition and abundance of octocoral assemblages were investigated in the Sea of Marmara, which forms the connection between the Mediterranean and the Black Seas, two semi-enclosed seas with peculiar oceanographic conditions. Fourteen octocoral species were collected in the saline layer of the Marmara Sea (20-40 m), with a mean coral abundance of 5.21±5.11 colonies m–2 (mean ± SD) calculated from a total of 1390 colonies counted in transects. In spite of severe anthropogenic disturbances, dense assemblages of corals/gorgonians were observed during this study. The coral- ligenous communities—one of the most valuable structures of the Mediterranean Sea—harbored either Eunicella cavolini or Paramuricea macrospina as the dominant gorgonian in the Marmara Sea. Furthermore, the gorgonian assemblages of the Marmara Sea differed from those of the Mediterranean in their high abundance of P. macrospina and Spinimuricea klavereni, two species rarely encountered in the Mediterranean Sea at the studied depth range. The factors behind the observed differ- ences are discussed in regard to the particular oceanographic conditions of the Marmara Sea. Finally, we revised the main threats to corals/gorgonians in the Marmara Sea and provided some insights on management recommendations for coral conservation in this area.
    [Show full text]
  • 'ISLANDER 'IDENTITIES: the CASES of HEYBELIADA and BURGAZADA
    KADİR HAS UNIVERSITY SCHOOL OF GRADUATE STUDIES PROGRAM OF ARCHITECTURE AND URBAN STUDIES ‘ISLANDER ’IDENTITIES: THE CASES of HEYBELIADA and BURGAZADA EYLÜL ŞENSES MASTER’S THESIS ISTANBUL, JANUARY, 2020 Eylül Şenses Master’s Thesis 2020 ‘ISLANDER ’IDENTITIES: THE CASES of HEYBELIADA and BURGAZADA EYLÜL ŞENSES MASTER’S THESIS Submitted to the School of Graduate Studies of Kadir Has University in partial fulfillment of the requirements for the degree of Master of Science in Architecture and Urban Studies Master Program. ISTANBUL, JANUARY, 2020 DECLARATION OF RESEARCH ETHICS / METHODS OF DISSEMINATION I, EYLÜL ŞENSES, hereby declare that; • this Master’s Thesis is my own original Work and that due references have been appropriately provided on all supporting literature and resources; • this Master’s Thesis contains no material that has been submitted or accepted for a degree or diploma in any other educational institution; • I have followed “Kadir Has University Academic Ethics Principles” prepared in accordance with the “The Council of Higher Education’s Ethical Conduct Principles” In addition, I understand that any false claim in respect of this Work will result in disciplinary action in accordance with University regulations. Furthermore, both printed and electronic copies of my Work will be kept in Kadir Has Information Center under the following condition as indicated below: The full content of my thesis/project will not be accessible for 6 months. If no extension is required by the end of this period, the full content of my thesis/project will be automatically accessible from everywhere by all means. EYLÜL ŞENSES __________________________ January 2020 KADİR HAS UNIVERSITY SCHOOL OF GRADUATE STUDIES ACCEPTANCE AND APPROVAL This Work entitled ISLANDER IDENTITY: THE CASE of HEYBELIADA and BURGAZADA of ISTANBUL prepared by EYLÜL ŞENSES has been judged to be successful at the defense exam held on December, 2019 and accepted by our jury as MASTER’S THESIS.
    [Show full text]
  • Adalara Göç Profili
    1 Eser Adı: Göç Bağlantıları 2012 Projesi | Adalar_Kreuzberg_Stockholm_Xanthi Migration Connections 2012 Project | Princes’ Islands_Kreuzberg_Stockholm_Xanthi ISBN: 978-975-9119-34-8 Editör Editor Deniz Koç Yayınlayan Publisher Adalı Yayınları Tel Phone +90 216 382 64 30 Faks Fax +90 216 382 52 90 Tarih Date 2012 Dili Language Türkçe-İngilizce Baskı Print Tüm Baskı (Seçil Ofset) Basım Yeri Printed in İstanbul Tasarım ve Grafik Uygulama Design and Graphic ApplicationArne Uebel Gülşah Sağlam Uebel [email protected] [email protected] Bu kitapçıkta kullanılan görsel malzemelerden bağışçıları belirtilmeyenler Adalar Müzesi arşivlerinden sağlanmıştır. Bunlar ve diğer görsel malzemeler Adalar Müzesi’nden yazılı izin alınmadan hiçbir şekilde kullanılamaz. The donators of the visual materials who were not indicated in this catalog were provided from the Museum of the Princes’ Islands archives.These and other visual materials cannot be used in any way without the written approval of the Museum of the Princes’ Islands. 2 Bu program AB veTürkiye Cumhuriyeti tarafından ortaklaşa finanse edilmektedir. This Program is co-funded by the European Union and the Republic ofTurkey. Kurucular Founders İşbirliği ile In cooperation with Bu yayının içeriğinden yalnızca Adalar Müzesi sorumlu olup, herhangi bir şekilde AB’nin görüşlerini yansıttığı şeklinde yorumlanamaz. The content of this publication is the sole responsibility of Museum of the Princes’ Islands and can in no way be taken to reflect the views of the EU. 3 4 Göç Bağlantıları Sergisi 2012 Projesi
    [Show full text]