Skip to main content
Log in

Source Characterization and Tsunami Modeling of Submarine Landslides Along the Yucatán Shelf/Campeche Escarpment, Southern Gulf of Mexico

  • Published:
Pure and Applied Geophysics Aims and scope Submit manuscript

Abstract

Submarine landslides occurring along the margins of the Gulf of Mexico (GOM) represent a low-likelihood, but potentially damaging source of tsunamis. New multibeam bathymetry coverage reveals that mass wasting is pervasive along the Yucatán Shelf edge with several large composite landslides possibly removing as much as 70 km3 of the Cenozoic sedimentary section in a single event. Using GIS-based analysis, the dimensions of six landslides from the central and northern sections of the Yucatán Shelf/Campeche Escarpment were determined and used as input for preliminary tsunami generation and propagation models. Tsunami modeling is performed to compare the propagation characteristics and distribution of maximum amplitudes throughout the GOM among the different landslide scenarios. Various factors such as landslide geometry, location along the Yucatán Shelf/Campeche Escarpment, and refraction during propagation result in significant variations in the affected part of the Mexican and US Gulf Coasts. In all cases, however, tsunami amplitudes are greatest along the northern Yucatán Peninsula.

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

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Institutional subscriptions

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6
Fig. 7
Fig. 8
Fig. 9

Similar content being viewed by others

References

  • Adatte, T., Stinnesbeck, W., & Keller, G. (1996). Lithostratigraphic and mineralogic correlations of near K/T boundary clastic sediments in northeastern Mexico: Implications for origin and nature of deposition. In G. Ryder, D. Fastovsky, S. Gartner (Eds.), The Cretaceous–Tertiary event and other catastrophes in earth history: Boulder, Colorado, Geological Society of America Special Paper 307, 211–226.

  • Amante, C., & Eakins, B.W. (2009). ETOPO1 1 arc-minute global relief model: Procedures, data sources and analysis. NOAA Technical Memorandum NESDIS NGDC-24. National Geophysical Data Center, NOAA. doi:10.7289/V5C8276M.

  • Bourgeois, J. T., Hansen, A., Wiberg, P. L., & Kauffman, E. G. (1988). A tsunami deposit at the Cretaceous–Tertiary boundary in Texas. Science, 241, 567–570.

    Article  Google Scholar 

  • Bryant, W. R., Meyerhoff, A. A., Brown, N. K., Furrer, M., Pyle, T., & Antoine, J. W. (1969). Escarpments reef trends, and diapiric structures, eastern Gulf of Mexico. Bulletin American Association of Petroleum Geologists, 53, 2506–2542.

    Google Scholar 

  • Chaytor, J. D., ten Brink, U. S., Solow, A. R., & Andrews, B. D. (2009). Size distribution of submarine landslides along the US Atlantic margin. Marine Geology, 264(1–2), 16–27.

    Article  Google Scholar 

  • Chaytor, J.D., Twichell, D.C., Lynett, P., & Geist, E.L. (2010). Distribution and tsunamigenic potential of submarine landslides in the Gulf of Mexico. In: D.C. Mosher, L. Moscardelli, R.C. Shipp, J.D. Chaytor, C.D. Baxter, H.J. Lee, & R. Urgeles (Eds.), Submarine mass movements and their consequences, advances in natural and technological hazards research (745–754), vol 28. Springer, Netherlands.

  • Dalle Valle, G., & Gamberi, F. (2011). Pockmarks and seafloor instability in the Olbia continental slope (northeastern Sardinian margin, Tyrrhenian Sea). Marine Geophysical Researches, 32, 193–205.

    Article  Google Scholar 

  • Denne, R. A., Scott, E. D., Eickhoff, D. P., Kaiser, J. S., Hill, R. J., & Spaw, J. M. (2013). Massive Cretaceous-Paleogene boundary deposit, deep-water Gulf of Mexico: New evidence for widespread Chicxulub-induced slope failure. Geology, 41, 983–986.

    Article  Google Scholar 

  • Ewing, M., Worzel, J. L., Beall, A. O., et al. (1969). Initial reports of the deep sea drilling project (Vol. 1). Washington D.C.: U.S. Government Printing Office.

    Google Scholar 

  • Geist, E. L., Lynett, P. J., & Chaytor, J. D. (2009). Hydrodynamic modeling of tsunamis from the Currituck landslide. Marine Geology, 264, 41–52.

    Article  Google Scholar 

  • Horrillo, J., Wood, A., Kim, G. B., & Parambath, A. (2013). A simplified 3-D Navier Stokes numerical model for landslide-tsunami: Application to the Gulf of Mexico. Journal Geophysical Research, 118, 6934–6950.

    Google Scholar 

  • Horrillo, J.J., Wood, A.L., Williams, C., Parambath, A., & Kim, G.-B. (2010). Construction of tsunami inundation maps in the Gulf of Mexico, Tech. Rep, National Tsunami Hazard Mitigation Program (NTHMP), National Weather Service Program Office, NOAA.

  • Lawton, T. F., Shipley, K. W., Aschoff, J. L., Giles, K. A., & Vega, F. J. (2005). Basinward transport of Chicxulub ejecta by tsunami-induced backflow, La Popa basin, northeastern Mexico, and its implications for distribution of impact-related deposits flanking the Gulf of Mexico. Geology, 33, 81–84.

    Article  Google Scholar 

  • Lindsay, J. F., Shipley, T. H., & Worzel, J. L. (1975). Role of canyons in the growth of the Campeche Escarpment. Geology, 3, 533–536.

    Article  Google Scholar 

  • Locker, S. D., & Buffler, R. T. (1983). Comparison of lower Cretaceous carbonate shelf margins, northern Campeche Escarpment and northern Florida Escarpment, Gulf of Mexico. American Association of Petroleum Geologists. Studies in Geology, 15, 123–128.

    Google Scholar 

  • López-Venegas A.M., ten Brink U.S., Geist E.L (2008). Submarine landslide as the source for the October 11, 1918 Mona Passage tsunami: Observations and modeling. Marine Geology, 254(1), 35–46.

  • Lynett, P., & Liu, P. L. F. (2002). A numerical study of submarine landslide generated waves and runup. Proceedings of the Royal Society of London, Ser. A, 458, 2885–2910.

    Article  Google Scholar 

  • Lynett, P., & Liu, P. L. F. (2005). A numerical study of the run-up generated by three-dimensional landslides. Journal of Geophysical Research: Oceans, 110, C03006. doi:10.1029/2004JC002443.

    Article  Google Scholar 

  • Mulder, T. (2011). Gravity processes and deposits on continental slope, rise and abyssal plains. In H. Huneke & T. Mulder (Eds.), Deep-sea sediments (pp. 25–125). Amsterdam: Elsevier.

    Chapter  Google Scholar 

  • National Geophysical Data Center/World Data Service (NGDC/WDS): Global Historical Tsunami Database. National Geophysical Data Center, NOAA. doi:10.7289/V5PN93H7.

  • Pampell-Manis, A., Horrillo, J., Shigihara, Y., & Parambath, L. (2016). Probabilistic assessment of landslide tsunami hazard for the northern Gulf of Mexico. Journal of Geophysical Research Oceans. doi:10.1002/2015JC011261.

    Google Scholar 

  • Parsons, T., Geist, E. L., Ryan, H. F., Lee, H. J., Haeussler, P. J., Lynett, P., et al. (2014). Source and progression of a submarine landslide and tsunami: The 1964 Great Alaska earthquake at Valdez. Journal Geophysical Research. doi:10.1002/2014JB011514.

    Google Scholar 

  • Paull, C. K., Caress, D. W., Gwiazda, R., Urrutia-Fucugauchi, J., Rebolledo-Vieyra, M., Lundsten, E., et al. (2014). Cretaceous–Paleogene boundary exposed: Campeche Escarpment, Gulf of Mexico. Marine Geology, 357, 392–400.

    Article  Google Scholar 

  • Paull, C. K., Freeman-Lynde, R., Bralower, T. J., Gardemal, J. M., Neumann, A. C., D’Argenio, B., et al. (1990a). Geology of the strata exposed on the Florida Escarpment. Marine Geology, 91, 177–194.

    Article  Google Scholar 

  • Paull, C. K., Spiess, F. N., Curray, J. R., & Twichell, D. (1990b). Origin of Florida Canyon and the role of spring sapping on the formation of submarine box canyons. Geological Society of America Bulletin, 102, 502–515.

    Article  Google Scholar 

  • Shaw, C. E., & Benson, L. (2015). Possible tsunami deposits on the Caribbean coast of the Yucatán Peninsula. Journal of Coastal Research, 31, 1306–1316.

    Article  Google Scholar 

  • ten Brink, U. S., Geist, E. L., & Andrews, B. D. (2006). Size distribution of submarine landslides and its implication to tsunami hazard in Puerto Rico. Geophysical Research Letters, 33, L11307.

    Article  Google Scholar 

  • Twichell, D. C., Parson, L. M., & Paull, C. K. (1990). Variations in the styles of erosion along the Florida Escarpment, eastern Gulf of Mexico. Marine and Petroleum Geology, 7, 253–266.

    Article  Google Scholar 

  • Ward, S. N. (2001). Landslide tsunami. Journal of Geophysical Research: Solid Earth, 106(B6), 11201–11215.

    Article  Google Scholar 

  • Worzel, J.L., Bryant, W., Beall Jr., A.O., Capo, R., Dickinson, K., Foreman, H.P., Laury, R., McNeely, B.W., & Smith, L. (1970). Site 86 Initial Reports of the Deep Sea Drilling Project 10, Texas A & M University, Ocean Drilling Program, College Station, TX, United States, pp 25–47.

Download references

Acknowledgments

We would like to acknowledge the assistance of the Schmidt Ocean Institute, the captain and crew of the R/V Falkor, the David and Lucile Packard Foundation, Eve Lundsten, Krystle Anderson, and Brian Andrews. Nathan Miller, Uri ten Brink, David Tappin, and three anonymous reviewers provided helpful reviews which improved the manuscript. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the US Government.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Jason D. Chaytor.

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Chaytor, J.D., Geist, E.L., Paull, C.K. et al. Source Characterization and Tsunami Modeling of Submarine Landslides Along the Yucatán Shelf/Campeche Escarpment, Southern Gulf of Mexico. Pure Appl. Geophys. 173, 4101–4116 (2016). https://doi.org/10.1007/s00024-016-1363-3

Download citation

  • Received:

  • Revised:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s00024-016-1363-3

Keywords

Navigation