Skip to main content

Part of the book series: NATO Science Series: IV: Earth and Environmental Sciences ((NAIV,volume 9))

Abstract

Review of the available data suggests that there is a threat of tsunami inundation to the coasts of the Sea of Marmara and Gulf of Izmit. The tsunami may be the result of shaking from the next major earthquake or more probably, the secondary effect of sediment slumping on the seabed. This assessment is based on the extensive historical database available for the region and is supported by earthquake probability analysis, geological interpretation of the offshore area and preliminary mathematical simulations. In spite of the evidence, there are still too few focussed tsunami studies, and thus tsunami source mechanisms, propagation and onshore run-up remain poorly researched and largely unknown. The most recent tsunami event was associated with the Izmit earthquake of August 1999, when a tsunami wave up to 6.0 metres high inundated the coastal areas in the central part of the Gulf of Izmit. By contrast, earthquake risk has been well studied. The probability of a progressive westward shift in major earthquakes along the east-west trending North Anatolian Fault over the past 60 years indicates that the next major shock will be located offshore in the eastern part of the Sea of Marmara or the Gulf of Izmit. An earthquake located offshore in the eastern area will almost certainly generate a tsunami that will attack the eastern coasts, some of the most populated and industrial areas of Turkey. The areas most threatened by tsunamis are in the eastern Sea of Marmara and Gulf of Izmit. The southern areas of Istanbul would be at risk. An assessment of the limited database available suggests that the sediment slumps located on the marginal slopes of the deep basinal areas of the Sea of Marmara as well as the deeper areas of the Gulf of Izmit are probable tsunami source locations. A tsunami sourced from any of these basins has the potential to strike surrounding coasts but its magnitude will depend on the actual source location, propagation direction and local run-up. The tsunami source will be seabed displacement either by faulting or, more probably, sediment slumping.

This is a preview of subscription content, log in via an institution to check access.

Access this chapter

Chapter
USD 29.95
Price excludes VAT (USA)
  • Available as PDF
  • Read on any device
  • Instant download
  • Own it forever
eBook
USD 84.99
Price excludes VAT (USA)
  • Available as EPUB and PDF
  • Read on any device
  • Instant download
  • Own it forever
Softcover Book
USD 109.99
Price excludes VAT (USA)
  • Compact, lightweight edition
  • Dispatched in 3 to 5 business days
  • Free shipping worldwide - see info
Hardcover Book
USD 109.99
Price excludes VAT (USA)
  • Durable hardcover edition
  • Dispatched in 3 to 5 business days
  • Free shipping worldwide - see info

Tax calculation will be finalised at checkout

Purchases are for personal use only

Institutional subscriptions

Preview

Unable to display preview. Download preview PDF.

Unable to display preview. Download preview PDF.

Similar content being viewed by others

References

  1. Reilinger, R., Toksoz, N., McCluskey, S. and Barka, A. (2000) 1999 Izmit, Turkey earthquake was no surprise, GSA Today 10.

    Google Scholar 

  2. Stein, R.S., Barka, A.A. and Dieterich, J.H. (1997) Progressive failure on the North Anatolian fault since 1939 by earthquake stress triggering, Geophysical Journal International 128, 594–604.

    Article  Google Scholar 

  3. Parsons, T, Toda, S., Stein, R., Barka, A. and Dieterich, J.H. (2000) Heightened odds of Large Earthquakes Near Istanbul: An Interaction-Based Probability Calculation, Science 288, 661–665.

    Article  Google Scholar 

  4. Alpar, B. (1999) Underwater signatures of the Kocaeli Earthquake (August 17th 1999), Turkish Journal of Marine Sciences 5, 111–129

    Google Scholar 

  5. Altinok, Y., Alpar, B., Ersoy, S. and Yalciner, A.C. (1999) Tsunami generation of the Kocaeli earthquake (August 17th 1999), Turkish Journal of Marine Sciences 5, 130–148.

    Google Scholar 

  6. Yalciner, A.C., Synolakis, C., Borrero, J., Altinok, Y., Watts, P., Imamura, F., Kuran, U., Ersoy, S., Kanoglu, U. and Tinti, S. (1999) Tsunami generation in Izmit Bay by the 1999 Izmit Earthquake, Conference on 1999 Kocaeli Earthquake. ITU Konferansi, p. 217–221.

    Google Scholar 

  7. Şengör, A.M.C., Görür, N. and Saroglu, F. (1985) Strike-slip faulting and related basin formation in zones of tectonic escape: Turkey as a case study, SEPM Special Publication. 37, 227–264.

    Google Scholar 

  8. Barka, A.A. and Kadinsky-Cade, K. (1988) Strike-slip geometry in Turkey and its influence on earthquake activity, Tectonics 7, 663–684.

    Article  Google Scholar 

  9. McGrory, D. (1999) The Times August 20th

    Google Scholar 

  10. Yalciner, A.C., Synolakis, C.E., Alpar, B., Borrero, J.C, Altinok, Y., Imamura, F., Tinti, S., Ersoy, S., Kuran, U., Pamakcu, S. and Kanoglu, U. (2001) Field surveys and modeling of the 1999 Izmit tsunami. ITS 2001 Proceedings, Session 4, Number 4-6.

    Google Scholar 

  11. Altinok, Y. and Ersoy, S. (2000) Tsunamis observed on and near the Turkish Coast, Natural Hazards, 21, 185–205.

    Article  Google Scholar 

  12. Ambraseys, N.N and Finkel, C.F. (1990) The Marmara Sea earthquake of 1509, Terra Nova, 2, 167–174.

    Article  Google Scholar 

  13. Ambraseys, N.N and Finkel, C.F. (1991) Long term seismicity of Istanbul and the Marmara Sea region, Terra Nova 3, 527–539.

    Article  Google Scholar 

  14. Ambraseys, N.N and Finkel, C.F. (1995) The seismicity of Turkey and adjacent areas: a historical review, 1500-1800, Muhittin Salin EREN, Istanbul, Turkey.

    Google Scholar 

  15. Ambraseys, N. N. (2001) Seismic Sea-Waves in the Marmara Sea region during the last 20 centuries. Proceedings of the NATO Advanced Workshop “Underwater Ground Failures on Tsunami Generation, Modeling, Risk and Mitigation. P. 193–194.

    Google Scholar 

  16. Altinok, Y., Ersoy, S., Yalciner, A.C., Alpar, B. and Kuran, U. (2001) Historical tsunamis in the Sea of Marmara. ITS 2001 Proceedings, Session 4, Number 4-2.

    Google Scholar 

  17. Bakun, W.H. and Wentworth, C.M. (1997) Estimating earthquake location and magnitude from seismic intensity data, Bulletin of the Seismological Society of America 87, 1502–1521.

    Google Scholar 

  18. Parke, J.R., Minshull, T.A., Anderson, G, White, R.S., McKenzie, D., Kusco, I., Bull, J.M., Gorur, N. and Sengor C. (1999) Active faults in the Sea of Marmara, western Turkey, imaged by seismic reflection profiles, Terra Nova 11, 223–227.

    Article  Google Scholar 

  19. Alpar, B., Yalciner, A.C., Imamura, F. and Synolakis, C.E. (2001) Determination of probable underwater failures and modeling of tsunami propagation in the Sea of Marmara. ITS 2001 Proceedings, Session 4, Number 4-3.

    Google Scholar 

  20. 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.

    Google Scholar 

  21. Wong, H.K., Lüdmann, T., Ulug, A. and Görür, N. (1995) The Sea of Marmara: a plate boundary sea in as escape tectonic regime. Tectonophysics 244, 231–250.

    Article  Google Scholar 

  22. Okay, A.I., Demirbag, E., Kurt, H., Okay, N. and Kuscu, I. (1999) An active, deep marine strike-slip basin along the North Anatolian Fault in Turkey, Tectonics 18, 129–147.

    Article  Google Scholar 

  23. İmren, C., Le Pichon, X., Rangin, C., Demirbağ, E., Ecevitoğlu, B. and Görür, N. (2001) The North Anatolian Fault within the Sea of Marmara: a new interpretation based on multi-channel seismic and multi-beam bathymetry data. Earth and Planetary Science Letters, 186, 143–158.

    Article  Google Scholar 

  24. Turner, A. K. and Schuster, R. L. (1996) Landslides: Investigation and mitigation, Special Report 247, Transactions Research Board, National Academy Press, Washington, D.C

    Google Scholar 

  25. Kawata, Y., Benson, B. C, Borrero, J. L., Davies, H. L., de Lange, W. P., Imamura, F., Letz, H., Nott, J. and Synolakis C. (1999) Tsunami in Papua New Guinea was as intense as first thought, Eos, Transactions American Geophysical Union, 80(9), 101,104-105.

    Article  Google Scholar 

  26. Tappin, D.R., Matsumoto, T. and Shipboard scientists. (1999) Offshore Surveys Identify Sediment Slump as Likely Cause of Devastating Papua New Guinea Tsunami 1998, Eos Transactions. American Geophysical Union, 80(30), 329, 334, 340.

    Google Scholar 

  27. Tappin, D.R., Watts, P., McMurtry, G. M., Lafoy, Y. and Matsumoto, T. (2001) The Sissano, Papua New Guinea tsunami of July 1998 — offshore evidence on the source mechanism. Marine Geology 175, 1–23.

    Article  Google Scholar 

  28. Yalciner, A.C., Alpar, B., Ozbay, I., Altinok, Y. and Imamura, F. (2001) Tsunami generation and coastal amplification in the Sea of Marmara. Proceedings of the NATO Advanced Workshop “Underwater Ground Failures on Tsunami Generation, Modeling, Risk and Mitigation, p. 138–146.

    Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Editor information

Editors and Affiliations

Rights and permissions

Reprints and permissions

Copyright information

© 2002 Kluwer Academic Publishers

About this chapter

Cite this chapter

Tappin, D.R., GöRür, N., Watts, P., Musson, R.M.W., Evans, R. (2002). The Tsunami Threat in the Sea of Marmara, Turkey: A Review. In: Görür, N., Papadopoulos, G.A., Okay, N. (eds) Integration of Earth Science Research on the Turkish and Greek 1999 Earthquakes. NATO Science Series: IV: Earth and Environmental Sciences, vol 9. Springer, Dordrecht. https://doi.org/10.1007/978-94-010-0383-4_7

Download citation

  • DOI: https://doi.org/10.1007/978-94-010-0383-4_7

  • Publisher Name: Springer, Dordrecht

  • Print ISBN: 978-1-4020-0653-1

  • Online ISBN: 978-94-010-0383-4

  • eBook Packages: Springer Book Archive

Publish with us

Policies and ethics