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Assessment of Tsunami-related Geohazard Assessment for Coasts of Hersek Peninsula and Gulf of İzmit

Year 2017, Volume: 4 Issue: 2, 63 - 78, 15.05.2017
https://doi.org/10.30897/ijegeo.312554

Abstract

Tsunamis are one of
the most dreadful natural disasters; they could cause abysmal damage to all
kind of lives in the hinterland within instantly. It is a major right-lateral
moving fault that runs along the tectonic boundary between the Eurasian Plate
to the north and the Anatolian Plate to the south. The western segment of the North
Anatolian Fault splits into three main branches. The northern one of NAF is
generally subdivided in several subsegments that have been the source of
frequent large historical earthquakes. The Sea of Marmara coasts is located on
the western extension of the NAFZ which is one of the most important active
faults with strike-slip characteristics, which are not likely to generate
tsunami. However, in the light of tsunami catalogs based on historical
documents, it is possible to say that Sea of Marmara has tsunamigenic potential.
The İstanbul shorelines, Gemlik Bay, Kapıdağ N-NE shores, Gelibolu, Hersek
Peinsula and Gulf of İzmit are one of the most significant geohazards in Sea of
Marmara due to the tsunami effect.

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Year 2017, Volume: 4 Issue: 2, 63 - 78, 15.05.2017
https://doi.org/10.30897/ijegeo.312554

Abstract

References

  • Abalı, H. (2005). Tsunami danger evaluation of Marmara sea coasts, Univerity of Istanbul, Institute of Marine Sciences and Management, Department of Marine Environment MSc. Thesis, 96p. Aksu A.E., Hiscott, R.N. and Yaşar, D. (1999). Oscillating Quaternary water levels of the Marmara Sea and vigorous outflow into the Aegean Sea from the Marmara Sea Black Sea Drainage Corridor, Mar. Geol. 153:275-302.
  • Aksu, A.E., Calon, T.J. and Hiscott, R.N. (2000). Anatomy of the North Anatolian Fault Zone in the Marmara Sea, western Turkey: extensional basins above a continental transform, GSA Today, 10(6): 3–7.
  • Aksu, A.E., Hiscott, RN., Kaminski, MA., Mudie, PJ., Gillespie, H., Abrajano, T. and Yaşar, D. (2002). Last Glacial-Holocene Paleoceanography of the Black Sea and Marmara Sea: Stable İsotopic, Foraminiferal and Coccolith Evidence, Mar. Geol. 190 (1- 2):119-149.
  • Alpar, B. and Güneysu, AC. (1999): Evolution of the Hersek Delta (İzmit Bay), Turk. J. Mar. Sci., 5: 57–74. Alpar, B., Altınok, Y., Gazioğlu, C. and Yücel, ZY. (2003). Tsunami hazard assessment in Istanbul, Turk. J. Mar. Sci., 9(1): 3–29.
  • Alpar, B., Erel, L., Gazioğlu, C., Gökaşan, E., Adatepe, FM., Demirel, S. and Algan, O. (1998). Plio-Quaternary evolution of the Enez Delta, NE Aegean Sea. Turkish J. Marine Sciences Vol. 4(1-2): 11-28. Alpar, B., Gazioğlu, C., Altınok, Y., Yücel, ZY. and Dengiz, Ş. (2004). Tsunami hazard assessment in Istanbul using by high resolution satellite data (IKONOS) and DTM. XXth Congress of the ISPRS, Istanbul, 2004.
  • Alpar, B., Yüksel, Y., Doğan, E., Gazioğlu, C., Çevik, E. and Altınok, Y. (2001). An estimate of detailed depth soundings in Izmit Bay before and after 17 August 1999 earthquake, Turkish Journal of Marine Sciences, 7(1): 3-18 . Altınok, Y. and Ersoy, Ş. (2000). Tsunamis observed on and near the Turkish Coast, Nat. Hazards, 21:185–205.
  • Altınok, Y., Alpar, B., Özer, N. and Aykurt, H. (2011). Revision of the tsunami catalogue affecting turkish coasts and surrounding regions, Nat Hazards Earth Syst Sci. Vol.11:273-291.
  • Altınok, Y., Ersoy, Ş., Yalçıner, A.C., Alpar, B. and Kuran, U. (2001). Historical tsunamis in the Sea of Marmara. Proceedings of the International Tsunami Symposium 2001, August 7–10 2001, Seattle, WA: 527–534.
  • Altınok, Y., Tinti, S., Alpar, B., Yalçıner, AC., Ersoy, Ş., Bortolucci, E. and Armigliato, A. (2001). The tsunami of August 17, 1999 in İzmit Bay, Turkey, Nat. Hazards, 24: 133–146.
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  • Ambraseys, NN. and Jackson, JA. (2000): Seismicity of the Sea of Marmara (Turkey) since 1500 Geophys. J. Int., 141:F1–F6.
  • Ambraseys, NN. (2002). The seismic activity of the Marmara Sea region over the last 2000 years, Bull. Seismol. Soc. Am., 92(1): 1–18.
  • Ardel, A. (1959). İzmit Körfezi’nden İznik Gölüne Morfolojik Müşahadeler, İstanbul Üniversitesi Coğrafya Enstitüsü Dergisi, Sayı 10: 145-151.
  • Armijo, R., Meyer, B., Navarro, S., King, G. and Barka, AA. (2002), Assymetric slip partitioning in the Sea of Marmara pull-apart: A clue to propagation processes of the North Anatolian Fault? Terra Nova, 14: 80–86.
  • Armijo, R., Meyer, B., Hubert, A. and Barka, AA. (1999). Westward propagation of the North Anatolian Fault into the northern Aegean: timing and kinematics. Geology, 27: 267–270.
  • Aytöre, B., Yalçıner, AC., Zaytsev, A., Çankaya, ZC. and Süzen, ML. (2016). Assessment of tsunami resilience of Haydarpaşa Port in the Sea of Marmara by high-resolution numerical modeling. Earth, Planets and Space (2016) 68:139.
  • Bargu, S. (1997). İzmit Körfezindeki Pleistosen Taraçaları ve Tektonik Özellikler, İstanbul. Üniv. Müh. Fak. Yerbilimleri Dergisi, Sayı 10:1-33.
  • Barka, AA. (1996). Slip distribution along the North Anatolian Fault associated with the large earthquakes of the period 1939 to 1967 Bull. Seismol. Soc. Am., 86: 1238–1254.
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Details

Journal Section Research Articles
Authors

Cem Gazioğlu

Publication Date May 15, 2017
Published in Issue Year 2017 Volume: 4 Issue: 2

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APA Gazioğlu, C. (2017). Assessment of Tsunami-related Geohazard Assessment for Coasts of Hersek Peninsula and Gulf of İzmit. International Journal of Environment and Geoinformatics, 4(2), 63-78. https://doi.org/10.30897/ijegeo.312554