Assoc. Prof. Topçu Ahmet ERTEK

Total Page:16

File Type:pdf, Size:1020Kb

Assoc. Prof. Topçu Ahmet ERTEK Assoc. Prof. Topçu Ahmet ERTEK OPfefricseo Pnhaol nIen:f +or9m0 2a1t2io 4n55 5700 Extension: 15767 WEmeabi:l :h tatpe:r/t/[email protected]/taertek/ Aİsdtadnrbeusls. : İstanbul Üniversitesi Edebiyat Fakültesi Coğrafya Bölümü Fiziki Coğrafya Anabilim Dalı Ordu Caddesi,34459,Beyazıt / Education Information UDnodcteorrgartaed, uİsattaen, bİsutla Ünbnuivle Ürnsiitveesri,s Ditesnii, zF Baciluimltyle orif VLeit eCroağtruarfey, aC Eonğrsatiftyüas,ü T, uJerokmeyo 1rf9o7lo4j i- A1n9a7b8ilim Dalı, Turkey 1979 - 1990 FEnogrliesihg, nB1 L Iantnegrmueadgiaetse Dissertations EDnoscttiotürsaüte, ,J eKoomcaoerlfi oYlaorjiı mAnadabasilıi'mnı nD aKluı, z1e9y9d0oğu Kesiminin Jeomorfolojisi, Istanbul University, Deniz Bilimleri Ve Coğrafya RSoecsiael aSrcicehnc Aesr aenads Humanities, Geography, Physical Geography Ascsaodcieatme Picro Tfeistsloers, I/s tTanabsukl sUniversity, Faculty of Literature, Coğrafya Bölümü, 2019 - Continues RAessiesatarcnht PArsosfisetsasnotr, ,İ Issttaannbbuul lÜ Unniviveerrssititeys,i ,F Faaccuultlyty o of fL Litieterraatuturree, ,C Cooğğrraafyfyaa B Böölülümmüü, ,1 1999832 - -2 1091983 Courses JTeüorlkoijyike vSeu lJaero mCooğrrfaoflyoajiskı H(Taürirtkailyaer , GPöolsletgrri)a, dUunadte,r 2gr0a1d7u -a 2te0, 128017 - 2018 JUeyogmuolarmfoalloı jJieyoe mGoirrişfo, Ulonjid veer gÇreaşditulia Tteo, p2o0g1r7a f-y 2a0la1r8da Uygulamalı Jeomorfoloji Sorunları, Postgraduate, 2017 - 2018 KJeıoyım Jeoorfmoolorjfio, Ulonjidsei,r Ugnraddeurgartea,d 2u0a1te7, -2 2001178 - 2018 JUeyogmuolarmfoalloı jJiedoem Roardfyoolomjie, tDriokc Ytoarşa Ttea,y 2in0l1e7ri ,- D2o0c1t8orate, 2016 - 2017 Jeomorfolojik Tip Bölgeler, Undergraduate, 2016 - 2017 Toüprkriayke CJeooğmraofyrafoslıo, Ujisnidnedreg Nraedouteakteto, 2n0ik1, 6U n- d2e0r1g7raduate, 2016 - 2017 Türkiye KSuıylaı rJe Coomğorarfoyalosjıi s(iT, üProksityger aAdkuaartseu, l2a0rı1)3, U -n 2d0e1r4graduate, 2016 - 2017 BAurazzuil ÇJeaolımşmoarlfaorloı vjiesi ,P Ulanndlaemrgarsaıd, Uuantdee, r2g0r1a3d u- a2t0e1, 24013 - 2014 Haidrritoag Brailfgyiasi, Unygduelragmraadlauraı,t eU, n2d0e1r3g r-a 2d0u1a4te, 2013 - 2014 SJetroümkotürrfoallo Jjeinoimn oPrrfeonlosjiip, lUenrid, eUrngdreardguraatdeu, 2at0e1, 32 0- 1230 1- 42014 HKarsitta J eBoilmgiosir, fUonlodjeisrig, Uranddueartger, a2d0u1a3te -, 20143 - 2014 SKpıyeıl eJeoolomjio (rMfoalğoajirsai,b Piloimst)g,r Dadouctaotera, 2te0, 1230 1- 32 0- 124014 MGeinerl aJel ovelo Kji,a Uyançdlearg, Uranddueartger, a2d0u1a3te -, 22001143 - 2014 Advising Theses ERTEK T. A. , GMearrgmera rvae BYöalkgıens Çi Cevorğersaifni iKna (nEalal zPırğo Lje4l2er-di 4ve p Oaflatassı ıEntıkni)le Jreio., mPoosrtfgorloadjisuia (tAe,d Mııy.SaÜmZaEnR)(.,S Ptuodstegnrta)d, Cuoatnet,inues ER.GTÜENKD TÜ. ZA(. S, tPuldeeisntot)s, eCno Snotinruaessı Orta Anadolu’da Coğrafi Ortam Şartlarının Değişimi ve Kültür Ortamının Gelişimi EARraTsEınKd Ta.k Ai .İ l, iKşkızilıelırr,m Paoks tHgraavdzausaıtneı,n M U.Nğuerbliu(dStauğd-Benayt)a, tC-Koanrtginı-uOessmancık arasındaki Kesiminin Jeomorfolojisi (Çorum), EDRoTctEoKr aTt.e A, M. , .KTaİLsKatİu(Sratu Kdöernfte)z, iC-Rounmtineuliefesneri Arasındaki Kıyı Bölgesinin Jeomorfolojisi ve Kıyı Alanları Yönetimi Modeli, EPRosTtEgKra Td.u Aa.t ,e İ, sKta.KnUbRuUl İMlinAiHn MBUatTı (KSetusidmeinnti)n, CJeoonmtionrufeoslojisi, Doctorate, T.ŞENSU(Student), Continues İEliRşTkiEleKr iT.,. PAo. s, tAgkrdadenuiazt eH, aGv.AzaLsPı'(nSdtua dHeonlto)s, eCno nKtıiynıu Çeiszgisi Değişimleri ile İklim Değişikliği ve Arkeolojik Yerleşmelerin SE.RATTEICKI (TS. tAu.d ,e Tnut)z, GCöolnüt iGnüuneesyinde 2000’li Yıllarda Oluşan Obrukların Jeomorfometrik Özellikleri, Postgraduate, TE.RSTEEKKM TE.N A(.S ,t Audneandto)l,u 2 F0e1n9eri-Ağva Arasındaki Kıyı Bölgesinin Jeomorfolojisi, Gelişimi ve Değişimi, Postgraduate, E.RKTILEIKÇ (TS. tAu.d , eKnatp),ı d2a0ğ1 9Yarımadası ve Güney Marmara Adalarının Jeomorfolojisi ve Kuaterner'deki Evrimi., Doctorate, ERTEK T. A. , İAsntatrnobpuol jBeonğika zJeı oKmıyoı rBföollgoejisnininin İ kJleimom Doerğfoişliokjliisğii,n Gee Elitşkimilei rvi,e P Doesğtgişriamdiu, aPtoes, tEg.rGaİdZuDaEtŞe(, SAt.uMdeesnutd)(, S2t0u1d8ent), 2018 BER.STOELK(S Ttu. Ad.e ,n Mt)u, d2u0r1n7u Çayı Havzası'nın (Taşburnu - Abant Gölü Batısı Arası) Flüvyo-Tektonik Jeomorfolojisi, Doctorate, 2E0R1T3EK T. A. , İstanbul Boğazında Deniz Kazaları ve Çevre Sorunları-Jeomorfoloji İlişkisi, Postgraduate, E.YASTI(Student), BER.STOELK(S Ttu. Ad.e ,n Gt)ü, m20ü1şy1aka-Eminönü Arasındaki Kıyı Bölgesinin Jeomorfolojisi, Gelişimi ve Değişimi, Postgraduate, BER.KTAEFKE STO. AĞ.L , UK(aSdtuıkdöeyn-Tt)u, z2l0a 1A0rasındaki Kıyı Bölgesinin Jeomorfolojisi, Gelişimi ve Değişimi, Postgraduate, ERTEK T. A. , BAilgtıan kÇuamyı (BKaKtıT KCe)s vime iÇneinv rJesoimnionr Jfeoolomjiosir, fDoloocjtisoir, aPtoes, tAg.rŞaEdNuCaAteN, (NS.tÇuAdĞeLnAt)R, (2S0t0u7dent), 2009 ERTEK T. A. , SOarkhaarnyeal iN Çeahyrı iH - aGvözyansıünkın Ç Aayşaı ğ- ıÇ Kaetaskim Çianyinı AJeroasmınodrafo Kloajliasni ( SBauhrasnaı)n, DKoarcstot rMaoter,f Aol.Eovjirsei n(B(Silteucdike)n, tD),o 2c0to0r5ate, EKR.TTUENKC TE.R A(.S ,t Mudoernfot)d, i2n0a0m4ik Süreçlere Dayanarak 1/50.000 ölçekli İstanbul İli ve Yakın Çevresinin Jeomorfoloji Haritası E(ARğTvEaK P Ta.f Ata. s, ıK) avrea Adçeınkilza mKıaysılıa, Prıomsıtzgdra dRuaadtyeo, Em.KeItLriIkÇ (YSatşu Tdaeynitn)l, e2r0in0e4 Dayalı Denizel Taraçaların Korelasyonu ve ENReToEteKk tTo. nAik. , YMoorrufmodui,n Paomstikg rSaüdrueaçtle,r Ae .DAYayTaAnÇa(rSatku d1e/n5t0).,0 20000 ö3lçekli İstanbul İli ve Yakın Çevresinin Jeomorfoloji Haritası E(KR.TÇEeKkm Te. cAe. ,P Mafotarfsoı)d vinea Amçiıkk lSaümraesçıl,e Preo sDtgaryaadnuaartaek, Ç1./Ü5S0K.0Ü0P0L ÜöOlçĞekLlUi (İsSttaundbeunlt )İl,i 2v0e0Y3akın Çevresinin Jeomorfoloji Haritası E(İRsTtaEnKb uTl. AB.o ,ğ Daezıv Preakft avseı )Ç evver Aeçsıiknlianm Jeaosım, Poorsfotglorajidsiu (aZteo,n Dg.uYlIdLaDkI)R, IPMo(sStgturaddeunat)te, 2, T0.0K2ESİK(Student), 2001 2E0R0T1EK T. A. , Kocaçay Havzasının Yukarı Kesiminin Jeomorfolojisi (İvrindi/Balıkesir), Doctorate, K.GÜLÜM(Student), (EŞRilTeE PKa Tft.a Ası. ), Mveo Arfçoıkdlianmamasiık, PSoüsrtegçrleardeu aDtaey, aAn.Eavrraekn 1(/S5tu0d.0e0n0t) ö, 2lç0e0k0li İstanbul İli veYakın Çevresinin Jeomorfoloji Haritası ERTEK T. A. , Kİzınrkikg öGzö lKüa Çyenvarkelasrinı d(Ae nYtaallıytaaş)ı vOel uYşaukmınl aÇreı,v Proesitngirna dKuaartset , JSe.oAmYDorINfo(lSotjuisdi,e Dnot)c, t2o0ra0t0e, İ.KOÇAK(Student), 2000 (ETRuTzElaK PTa. fAta. s, ıM) overf Aodçıiknlaammiaks Sı, üProesçtlgeraed Duaaytea,n Ta.rDaUkR 1S/U5N0(.0S0tu0d öelnçte)k, l2i 0İs0ta0nbul İli veYakın Çevresinin Jeomorfoloji Haritası (EBR.TÇEekKm Te. cAe. ,P Mafotarsfoı)d vinea Amçiıkk lSaümraesçıl,e Proe sDtgaryaadnuaartaek, H1/.K5A0Y.0A0(0S töuldçeknlti) İ, s1ta9n9b9ul İli ve Yakın Çevresinin Jeomorfoloji Haritası 1E9R9T9EK T. A. , Bartın Çayı Ağzı-Amasra-Çakraz Koyu Arasının Kıyı Jeomorfolojisi, Postgraduate, A.DEMİRCA(Student), ERTEK T. A. , GKearpeısdue- Gveü bÇlev Çraeysiın Ainra Jseıonmıno Krıfyoıl oJejiosmi (oBrofolulo),j iPsoi (sCtgidraed/uKatset,a Am.SoAnVuA),Ş P(oSstutgdreandtu),a 1te9, 9A8.ERGİN(Student), 1998 1E9R9T7EK T. A. , Verçenik Dağı-Tatos Dağları Arasının Glasyal Morfolojisi (Rize/Erzurum), Postgraduate, M.Kemal(Student), ERTEK T. A. , UYelaş-iYlheirskaers Kiku Azeryaisnıninın J eKoamrsotr Mfoolorjfioslio (jKisai y(sMeuriğ)l,a P)o, Pstogsrtagdruadatuea, tAe.,B KO.TZUDNACĞE(RSt(uSdtuednet)n, t1),9 199695 ERTEK T. A. , DÜzeüğmirmcüe nÇdayeır eH aHvazvazsaınsıını nJe Joemomorofrofloljoisjii s(iB (aTlrıkaebszior)n,) P, oPsotsgtrgardaudautaet,e S, .EŞ.UBLüEle(nSt(uSdteundte)n, 1t)9, 915995 JDuorctyo rMate,m Tebze srasvhunipmsası, İstanbul Üniversitesi Deniz Bilimleri ve İşl. Enst., January, 2020 2P0o1st8 Graduate, Tez Savunma Jürisi, İstanbul Üniversitesi, 2017, İstanbul Üniversitesi Sosyal Bilimler Enstitüsü, February, BDiolicmtolerrait eE,n Dstoitkütosüra, J Tanezu aSrayv,u 2n0m1a8 Jürisi, Çanakkale Onsekiz Mart Üniv. 2017, Çanakkale Onsekiz Mart Üniversitesi, Sosyal Post Graduate, YTüezk sSeakv uLnismanas J üterzis si,a İvsutannmbauslı ,Ü İnstivaenrbsuitle Üsni, i2v0er1s7it, eİ.sÜi .Sosyal Bilimler Enstitüsü, OJacntoubareyr,, 20187 Doctorate, DTeozk tSoarvau Tnemza S Jaüvruisnim, İsat aJünrbisuil, ÜFınriavte Ürsniitveesri,s 2it0e1si7 S, oİ.Üsy.Saol sByialilm Bleilrim Elnesrt E. 2n0st1it6ü, sEüla, Ozıcğt-oFbıreart, Ü20n1iv7ersitesi, Sosyal DBiolicmtolerra tEen, Dstoitkütsoür,a D Teecze mSabveurn, m20a1 J6ürisi, Çanakkale Onsekiz Mart Üniv. 2017, Çanakkale Onsekiz Mart Üniversitesi, Fen DBiolicmtolerrait eE,n Dsotiktütosüra, JTaenzu aSrayv,u 2n0m1a6 Jürisi, ÇOMÜ Sosyal Bilimler Enst., May, 2013 Post Graduate, Yüksek Lisans Tez Savunma Jürisi, ÇİsOtaMnÜb uSlo Üsynaivl eBrisliimtelseir, JEansuta.,r Sye, p2t0e1m2ber, 2011 Post Graduate, Yüksek Lisans Tez Savunma Jürisi, İstanbul Üniversitesi Deniz Bilimleri ve İşlet. Enst., June, 2011 DPoosctt oGrraatdeu, Datoek, tYoürkas Teekz L Sisaavnusn Tmeaz JSüarvisuin, İmstaa nJübruisl iÜ, İnsitvaenrbsuitle Üsin, Fiveebrrsuitaersyi,, J2u0n1e1, 2011 Doctorate, Doktora Tez Savunma Jürisi, İstanbul Üniversitesi ADdelni iTz ıBp iElimnslte.,r Ni voev eİşmlebt.e Er,n 2s0t.,1 D0ecember, 2010 Post Graduate, Yüksek Lisans Tez Savunma Jürisi, İstanbul Üniversitesi, SNeopvteemmbbeerr,, 22001100 Post Graduate, Yüksek Lisans Tez Savunma Jürisi, İstanbul Üniversitesi, Apurgiul,s 2t,0 210010 DPoosctt oGrraatdeu, Datoek, tYoürkas Teekz L Sisaavnusn Tmeaz JSüarvisuin, İmstaa nJübruisl iÜ, İnsitvaenrbsuitle Üsin, Nivoevrseimtebsei rD, e2n0i0z 9Bilimleri ve İşlet. Enst., November, 2009 Post Graduate, Yüksek Lisans Tez Savunma Jürisi, ÇİsOtaMnÜb uFle Ünn Bivliemrsleitrei
Recommended publications
  • 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]
  • Evaluation of Forest Management Plans in Conjunction with the Cadastral Information: the Case of Agva and Beykoz, Istanbul
    Journal of the Faculty of Forestry Istanbul University 2016, 66(2): 641-648 JOURNAL OF THE FACULTY OF FORESTRY ISTANBUL UNIVERSITY İSTANBUL ÜNİVERSİTESİ ORMAN FAKÜLTESİ DERGİSİ ISSN: 0535-8418 e-ISSN: 1309-6257 Online available at / Çevrimiçi erişim Research Article / Araştırma Makalesi http://dergipark.ulakbim.gov.tr/jffiu - http://dx.doi.org/10.17099/jffiu.77941 Evaluation of forest management plans in conjunction with the cadastral information: The case of Agva and Beykoz, Istanbul Gunay Cakir 1* , Alptug Guler 2 , Hayati Zengin 3 , Ahmet Salih Degermenci 3 1 Gumushane University, Graduate School of Natural and Applied Sciences, Department of Forestry and Environmental Science, 29100, Gumushane, Turkey 2 Turkish General Directorate of Forestry, Duzce Forest Enterprise, 81100, Duzce, Turkey 3 Duzce University, Faculty of Forestry, Department of Forest Engineering, 81620 Duzce, Turkey * Corresponding author e-mail (İletişim yazarı e-posta): [email protected] Received (Geliş): 19.01.2016 - Revised (Düzeltme): 01.02.2016 - Accepted (Kabul): 22.02.2016 Abstract: Determination of land ownership and boundaries is one of the most important purposes of the urban and rural land laws. There can be some boundary problems while preparing forestry area of any urban area when there is not consistency between the borders constructed by different state organizations like land cadastre, forest cadastre and forest management and planning teams. This study aims to illustrate these conflicts in forestry applications process of two different areas (Ağva and Beykoz) having different characteristics. The study was carried out in Ağva and Beykoz districts in the province of Istanbul and focused on the integration in the land and forest cadastral systems.
    [Show full text]
  • An Attempt to Revitalize Part of an Island in a New Integrated System
    Sustainable Development and Planning IV, Vol. 2 703 An attempt to revitalize part of an island in a new integrated system M. Şahin Yeditepe University, Faculty of Architecture, Istanbul, Turkey Abstract The main objective of this paper is to represent a revitalization project, aiming at recombining all valuable yet disintegrated cultural and natural components of a certain place, in a new coherent system. Covering 23 acres of land in a non-populated part of the island of Büyükada (Prinkipo), one of the few islands boasted by Istanbul, the private property in question has now been the subject of a revitalization project. The premises include two dilapidated ancient brick furnaces, a farm, a farmhouse, a family manor in a relatively fit state (the latter converted from a farm building in 1936 by Sedad Hakkı Eldem, one of the most prominent figures in modern Turkish architecture), a large vineyard once used by monks of the nearby St. George Monastery, and diverse flora and fauna. Firstly, all the natural and cultural aspects of the site, having evolved over a long period of time, were registered and re-evaluated by the owners, artists, architecture students and experts in the interrelated disciplines of archeology, architecture, landscaping, tourism and engineering. Secondly, all the rundown components of the site were remapped and redesigned to yield a new meaning, in an attempt to create physical, visual, functional and economic integrity, consequent to considerable discussion regarding relevant issues, such as sustainable development, revitalization and adaptive re-use, restoration and development. While preserving the distinct character of the place with a minimum of intervention, a number of fruitful propositions were developed.
    [Show full text]
  • Environmental and Social Impact Assessment for the Eurasia Tunnel Project Istanbul
    Environmental and Social Impact Assessment for the Eurasia Tunnel Project Istanbul, Volume II Main Report Final Draft January 2011 ERM Group, Germany and UK ELC-Group, Istanbul Delivering sustainable solutions in a more competitive world Main ESIA Report DRAFT REPORT Avrasya Tüneli İşletme İnşaat ve Yatırım A.Ş. (ATAŞ - the Eurasia Tunnel Operation, Construction and Investment Inc. Co.) Eurasia Tunnel Environmental and Social Impact Assessment Volume II Main Report January 2011 For and on behalf of Environmental Resources Management Approved by: _________________ Karen Raymond Signed: Position: ______________________Principal Partner Date: _________________________ 28st January 2011 This report is confidential to the client and we accept no responsibility of whatsoever nature to third parties to whom this report, or any part thereof, is made known. Any such party relies on the report at their own risk. This report has been prepared by Environmental Resources Management the trading name of Environmental Resources Management Limited, with all reasonable skill, care and diligence within the terms of the Contract with the client, incorporating our General Terms and Conditions of Business and taking account of the resources devoted to it by agreement with the client. We disclaim any responsibility to the client and others in respect of any matters outside the scope of the above. ERM GmbH ELC Group Ltd. Siemensstrasse 9 Kavacık Mah. Şehit Mustafa D-63263 Neu-Isenburg Yazıcı Sok. No:20 Tel.: +49 (0) 61 02/206-0 KAVACIK/ ISTANBUL Fax.: +49 (0) 61 02/206-202 (+9)0 216 465 91 30 (pbx) E-Mail: [email protected] (+9)0 216 465 91 39 (fax) http://www.erm.com E-Mail: [email protected] http://www.elcgroup.com.tr/ Project No.
    [Show full text]
  • 9.0 Geology and Soils
    AECOM Final Report Environment 9-1 9.0 GEOLOGY AND SOILS 9.1 Introduction This section discusses environmental issues associated with geology, soils, hydrogeology (groundwater) and waste management conditions relating to the Project. The current conditions within the route corridor are described below and likely effects of the development on potentially sensitive receptors assessed. These impacts have been divided into two categories: • Short-term construction impacts; and • Permanent and operational impacts. The potential impacts during construction and operational activities and mitigation measures proposed for each parameter are described. Some of the impacts are indirect impacts; some of them are direct impacts. For direct impacts, the Project site and development of the Project affect the issue directly. For indirect impacts, the Project site and development of the Project do not affect the issue directly, in the other words, if mitigation measures do not apply for these issues, there will be possible negative consequences and these cause negative impacts on the environmental issues. Note that some of the conditions and effects described, particularly with regard to contamination and hydrogeology, may interact with other parameters such as ecology and surface water. Such interactions are described where appropriate. 9.2 Approach and Methods 9.2.1 Baseline Methods This section explains the potential impacts on ground (Geology & Soil, Hydrogeology and Waste Management) conditions with the proposed Project. Potential impacts within the Project sites as well as adjacent receptors have been considered. In addition, potential impacts associated with the construction phase of the Project have been considered as well as potential impacts associated with permanent infrastructure and operational activities.
    [Show full text]
  • Berriasian Rudist Faunas and Micropalaeontology of Stramberk Type Carbonate Exotics from the Lycian Nappes, Bodrum Peninsula, So
    Cretaceous Research 56 (2015) 76e92 Contents lists available at ScienceDirect Cretaceous Research journal homepage: www.elsevier.com/locate/CretRes Berriasian rudist faunas and micropalaeontology of Stramberk type carbonate exotics from the Lycian nappes, Bodrum Peninsula, southwest Turkey * € Jean-Pierre Masse a, , Mükerrem Fenerci-Masse a, Sacit Ozer b, Talip Güngor€ b, Cüneyt Akal b a CEREGE, Aix-Marseille University, Centre Saint-Charles, 13331 Marseille Cedex 3, France _ b Dokuz Eylul University, Engineering Faculty, Geological Engineering Department, Tınaztepe Campus, Buca, 35160 Izmir, Turkey article info abstract Article history: Megablocks of coral-rudist bearing platform limestone, of Stramberk type, are present as exotics in upper Received 15 December 2014 SantonianeCampanian flysch-like deposits of the Karabortlen€ formation, near Bodrum. These beds Accepted in revised form 23 March 2015 belong to the Lycian nappes and the palaeogeographic origin of the megablocks is unclear. The micro- Available online paleontological assemblage of benthic foraminifera, calcareous green algae and problematica of the blocks indicates a Berriasian age, and has a Mediterranean character. Rudists are essentially represented Keywords: by Heterodiceras luci (Epidiceratidae) and Hypelasma salevensis (Requieniidae), commonly found in the Rudist bivalves Upper TithonianeBerriasian of the European margin of the Mediterranean Tethys. The Lycian specimens Micropalaeontology fi Palaeogeography of Hypelasma represent the rst record of this taxon on the southern Tethyan margin whereas Hetero- fi fi Palaeobiogeography diceras has been reported from the peri-Adriatic regions but is identi ed for the rst time in Turkey. Lower Cretaceous © 2015 Elsevier Ltd. All rights reserved. Turkey 1. Introduction and requieniids have been mentionned (Altıner et al., 1991; Masse € and Ozer, unpublished observations).
    [Show full text]
  • ETİ Elektrik Üretim A.Ş
    AKINCI 13.1) Environmental Impact Assessment (EIA) regarding AKINCI HES project has been completed and enclosed approved report and details can be analyzed. ETİ Elektrik Üretim A.Ş. Sahrayıcedit. Man., Omca Sk. No 37, Golden Plaza E Blok, Kat: 1 D: 3-4 Tel. : 0 216 355 16 30 34734 Kozyatağı – İSTANBUL Fax : 0 216 355 16 39 Form No : G 604 1 T.R. Ministry of Environment and Forestry General Directorate of Environmental Impact Assessment and Planning Date of decision : 18/03/2008 Decision No: 1457 EIA Certificate In accordance with article 14 of Environmental Impact Assessment Regulation coming into force through publication on 16.12.2003 dated and 25318 numbered Official Gazette, "Akıncı HES Facilities and Material Mines" project has been approved positive in terms of Environmental Impact Assessment. Owner of the project: Eti Elektrik Üretim A.Ş. Location of the project: Tokat province, Reşadiye and Niksar districts 2 ETI ELEKTRİK ÜRETİM A.Ş. Final EIA Report Regarding AKINCI HES Facilities and Material Mines TOKAT PROVINCE NİKSAR and REŞADİYE DISTRICTS KELKİT STREAM ROGHT COAST LOCALITY DERYA MÜHENDİSLİK MÜŞAVİRLİK İNŞAAT SANAYİ VE TİCARET ANONİM ŞİRKETİ İSTANBUL-2008 3 ETİ Elektrik Üretim A.Ş. Akıncı HES Plants and Material Centres Final ÇED (Environmental Effect Assessment) Report Name of the project owner ETİ ELEKTRİK ÜRETİM A.Ş. Address SAHRAYICEDIT.OMCA SK.No:37 GOLDEN PLAZA E BLOK KAT:1 DAİRE:3 - 4 KADIKÖY/İSTANBUL Phone and Fax numbers TEL: +90(216)355 16 30 FAX: +90(216) 355 16 39 Name of the project TOKAT PROVINCE AKINCI HES FACILITIES AND MATERIAL MINES Open address of the location selected for TOKAT PROVINCE NİKSAR and the project (province, district, region, REŞADİYE DISTRICTS KELKİT locality) STREAM RIGHT COATS LOCALITY Name of the company/study group DERYA MÜHENDİSLİK arranging the report MÜŞAVİRLİK İNŞAAT SANAYİ VE TİCARET ANONİM ŞİRKETİ (Derya Engineering Consultancy Construction Industry and Trade Inc.
    [Show full text]
  • A Pelagic Upper Devonian Sequence in Sarıyer, İstanbul
    Turkish Journal of Earth Sciences Turkish J Earth Sci (2020) 29: 785-797 http://journals.tubitak.gov.tr/earth/ © TÜBİTAK Research Article doi:10.3906/yer-2001-25 A pelagic Upper Devonian sequence in Sarıyer, İstanbul 1,2, 3 2 Aral I. OKAY *, Ayşe ATAKUL-ÖZDEMİR , Nilgün OKAY 1 Eurasia Institute of Earth Sciences, İstanbul Technical University, İstanbul, Turkey 2 Department of Geology, Faculty of Mines, İstanbul Technical University, İstanbul, Turkey 3 Department of Geophysical Engineering, Van Yüzüncü Yıl Üniversitesi, Van, Turkey Received: 28.01.2020 Accepted/Published Online: 04.05.2020 Final Version: 01.07.2020 Abstract: The Palaeozoic sequence in the İstanbul region is made up of a continuous transgressive sedimentary series extending from Ordovician continental clastic rocks to Lower Carboniferous turbidites. The middle part of this sequence consists predominantly of carbonates ranging from shallow marine Upper Silurian limestones to latest Devonian to earliest Carboniferous deep marine limestones and shales. Here, we describe a new Upper Devonian deep marine limestone-siltstone section from the Sarıyer region in the European part of İstanbul. The 37-m thick section located in the campus of the İstanbul Technical University consists at the base of dark micritic limestones interbedded with carbonate-rich siltstones, which pass up into siltstones with rare micritic limestone lenses and beds. Conodonts indicate a late Famennian (latest Devonian) age for the İTÜ campus section; 5 conodont biozones are documented; Pseudopolygnathus granulosus, Polygnathus styriacus, Palmatolepis gracilis manca, Palmatolepis gracilis expansa, and Bispathodus aculeatus aculeatus. The Late Devonian fauna from the İTÜ Campus section are dominated by the important marker species of Palmatolepis, Bispathodus and Polygnathus.
    [Show full text]
  • Determination of Cr (Vi) in Creeks Discharge to Izmit Gulf (Kocaeli, Turkey)
    Journal of Scientific Perspectives Volume 3, Issue 3, Year 2019, pp. 201-206 E - ISSN: 2587-3008 URL: http://ratingacademy.com.tr/ojs/index.php/jsp DOİ: https://doi.org/10.26900/jsp.3.020 Research Article DETERMINATION OF CR (VI) IN CREEKS DISCHARGE TO İZMIT GULF (KOCAELI, TURKEY) Kadriye OKTOR * * Assist. Prof. Dr., Department of Environmental Engineering, Engineering Faculty, Kocaeli University, TURKEY, e-mail: [email protected] ORCID ID: https://orcid.org/0000-0002-7217-4371 Received: 28 June 2018; Accepted: 9 July 2019 ABSTRACT With increasing industrialization, environmental pollution has become a threat to human health. The heavy metal pollution, especially from industrial waste water, is the best example of this. Chromium holds a special position among living organisms because on its species it can be either essential or toxic. Cr (VI) even at very low concentrations is harmful and carcinogenic, while Cr(III) is a necessary microelement for cellular metabolism. Therefore, it is very important to determine the chromium metal found in the wastewater of leather, paint and iron - steel industries. Four main creeks discharges located in the important industrial area in Kocaeli Province are made to the Gulf of İzmit. In this study, Cr (VI) was measured by the spectrophotometer S.M.3500-Cr B. Calorimetric Method sampled from four main streams Saz, Dil, Narca (Bağ) and Ambar (Ulupınar) Creeks samples and the results were found to be <0.02 mg / L. With these values it is observed that there is a visible improvement in the pollution of the creeks. Keywords: Creek, Water pollution, Heavy metal, Chromium (VI) OKTOR / Determination of Cr (VI) in Creeks Discharge to İzmit Gulf (Kocaeli, Turkey) 1.
    [Show full text]
  • Special Issue 2015 January
    Journal Home page : www.jeb.co.in E-mail : [email protected] JEB ISSN: 0254-8704 (Print) ISSN: 2394-0379 (Online) Journal of Environmental Biology CODEN: JEBIDP Woody vegetation of Şile and its environs (Istanbul/Turkey) and destruction of the area Y. Sezer12 , V. Altay *, I.I. Ozyigit 1 and C. Yarci 1 1Biology Department, Faculty of Science & Arts, Marmara University, Goztepe-Istanbul, 34722, Turkey. 2Biology Department, Faculty of Science & Arts, Mustafa Kemal University, Antakya-Hatay, 31040, Turkey *Corresponding Author E-mail: [email protected] Abstract Publication Info The woody vegetation of Şile district (Istanbul/Turkey), and its characteristics in conjunction with its Paper received: environs are presented in this study. The field studies were performed using classic Braun-Blanquet 02 July 2013 method during 2003-2010 periods. In the present study three associations, two from forest vegetation and one from maquis vegetation, were characterized in the field. One of these associations is new and its Revised received: description, typification and syntaxonomy was proposed. Phytosociological and phytoecological features of all three associations were compared with their relatives and related discussion was done accordingly. 10 November 2013 The associations described in the present study were as follows: Phillyreo-Lauretum nobilis, Smilaco- Castanetum sativae, Fago orientalis-Quercetum ibericae ass. nova. Furthermore, some soil properties Re-revised received: such as saturation, organic matter, pH, CaCO32 , K O and P 25 O were
    [Show full text]
  • Pre-Alpide Palaeozoic and Mesozoic Orogenic Events in the Eastern Mediterranean Region
    Pre-Alpide Palaeozoic and Mesozoic orogenic events in the Eastern Mediterranean region A. I. OKAY1, M. SATIR2 & W. SIEBEL2 1I˙stanbul Teknik U¨ niversitesi, Avrasya Yerbilimleri Enstitu¨su¨, Ayazag˘a 80626, I˙stanbul Turkey (e-mail: [email protected]) 2Institut fu¨r Geowissenschaften, Universita¨tTu¨bingen, Wilhelmstraße 56, D-72074 Tu¨bingen, Germany Abstract: We review the Palaeozoic–Early Mesozoic evolution of the Eastern Mediterranean–Balkan region with special reference to Anatolia, and provide new isotopic data on the Palaeozoic magmatic and metamorphic rocks. The pre-Alpide evolution of the region involves episodic growth of Laurussia by accretion of oceanic terranes and Gondwana-derived microcontinents. Terrane accretion, associated with deformation, magmatism and regional metamorphism, took place in the Late Ordovician–Early Silurian, Carboniferous, Late Triassic–Early Jurassic and Mid-Jurassic. The Late Ordovician–Early Silurian accretion is inferred from strati- graphic and faunal records in the Pontides; other evidence for it is buried under young cover on the northern margin of the Black Sea. The Carboniferous orogeny is related to southward subduction and continental collision on the southern margin of Laurussia. It is marked in the Pontides by high-grade regional metamorphism, north-vergent deformation and post-orogenic latest Carboniferous– Early Permian plutonism. The latest Triassic–Early Jurassic Cimmeride orogeny involved the collision and amalgamation of an oceanic plateau to the southern margin of Laurasia. It is represented by voluminous accretionary complexes with Late Triassic blues- chists and eclogites. Late Jurassic regional metamorphism and deformation is confined to the Balkans, and is the result of continental collision between the Rhodope–Serbo-Macedonian and Strandja blocks in the Late Jurassic.
    [Show 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.
    [Show full text]