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Volume 15, issue 6
Nat. Hazards Earth Syst. Sci., 15, 1265–1273, 2015
https://doi.org/10.5194/nhess-15-1265-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
Nat. Hazards Earth Syst. Sci., 15, 1265–1273, 2015
https://doi.org/10.5194/nhess-15-1265-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 17 Jun 2015

Research article | 17 Jun 2015

Dynamics of the Oso-Steelhead landslide from broadband seismic analysis

C. Hibert et al.

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Cited articles

Allstadt, K.: Extracting source characteristics and dynamics of the August 2010 Mount Meager landslide from broadband seismograms, J. Geophys. Res., 118, 1472–1490, https://doi.org/10.1002/jgrf.20110, 2013.
Brodsky, E. E., Gordeev, E., and Kanamori, H.: Landslide basal friction as measured by seismic waves, Geophys. Res. Lett., 30, 2236, https://doi.org/10.1029/2003GL018485, 2003.
Dammeier, F., Moore, J. R., Haslinger, F., and Loew, S.: Characterization of alpine rockslides using statistical analysis of seismic signals, J. Geophys. Res., 116, F04024, https://doi.org/10.1029/2011JF002037, 2011.
Deparis, J., Jongmans, D., Cotton, F., Baillet, L., Thouvenot, F., and Hantz, D.: Analysis of rock-fall and rock-fall avalanche seismograms in the French Alps, Bull. Seismol. Soc. Am., 98, 1781–1796, https://doi.org/10.1785/0120070082, 2008.
Dragovich, J., Stanton, B., Lingley Jr., W., Griesel, G., and Polenz, M.: Geologic Map of the Oso 7.5-Minute Quadrangle, Skagit and Snohomish Counties, Washington: Washington Division of Geology and Earth Resources Open-File Report 11, Washington Division of Geology and Earth Resources, Washington, 2003.
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We carry out a study of the seismic signals generated by the devastating Oso-Steelhead landslides. We invert the long-period seismic signals generated by the first main event and obtain estimates of its trajectory, kinematics and mass. No distinct long-period surface waves were recorded for the second failure, which prevents inversion for its source parameters. However, from the comparison of the energy of the short-period waves generated by both events, we can estimate the volume of the second.
We carry out a study of the seismic signals generated by the devastating Oso-Steelhead...
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