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Earth Surface Dynamics An interactive open-access journal of the European Geosciences Union
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© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 26 Nov 2018

Research article | 26 Nov 2018

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This discussion paper is a preprint. A revision of the manuscript is under review for the journal Earth Surface Dynamics (ESurf).

Seismic and geologic controls on spatial clustering of landslides in three large earthquakes

Claire Rault1, Alexandra Robert2, Odin Marc3, Niels Hovius4,5, and Patrick Meunier1 Claire Rault et al.
  • 1Laboratoire de Géologie, Ecole Normale Supérieure Paris, Paris, 75005, France
  • 2Géosciences Environnement Toulouse, Observatoire Midi-Pyrénées, Toulouse, 31400, France
  • 3Ecole et Observatoire des Sciences de la Terre, Strasbourg, 67084, France
  • 4GFZ German Research Center for Geosciences, Potsdam, 14473, Germany
  • 5Institute for Earth and Environmental Sciences, University of Potsdam, 14476, Germany

Abstract. The large, shallow earthquakes at Northridge, California (1994), Chi-Chi, Taiwan (1999) and Wenchuan, China (2008) each triggered thousands of landslides. We have determined the position of these landslides along hillslopes, normalizing for statistical bias. The landslide patterns have a co-seismic signature, with clustering at ridge crests and slope toes. A cross check against rainfall-induced landslide inventories confirms that crest-clustering is specific to seismic-triggering. In our three study areas, seismic ground motion parameters, and lithologic and topographic features have limited bearing on the observed patterns of landslide clustering. However, we show that at the scale of the epicentral area, crest- and toe-clustering occur in areas with specific geological features. Toe-clustering of seismically-induced landslides tends to occur along major faults. Crest-clustering is concentrated at sites where the lithology along hillslopes is approximately uniform, or made of alternating soft and hard strata, and without strong overprint of geological structures. Although earthquake-induced landslides locate higher on hillslopes in a statistically significant way, geological features strongly modulate the landslide position along the hillslopes. As a result the observation of landslide clustering on topographic ridges cannot be used directly as an indicator of seismic parameters such as ground shaking.

Claire Rault et al.
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Status: final response (author comments only)
Status: final response (author comments only)
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Claire Rault et al.
Claire Rault et al.
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