Articles | Volume 10, issue 2
Solid Earth, 10, 463–486, 2019
https://doi.org/10.5194/se-10-463-2019
Solid Earth, 10, 463–486, 2019
https://doi.org/10.5194/se-10-463-2019

Research article 04 Apr 2019

Research article | 04 Apr 2019

Effects of finite source rupture on landslide triggering: the 2016 Mw 7.1 Kumamoto earthquake

Sebastian von Specht et al.

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Sebastian von Specht on behalf of the Authors (15 Feb 2019)  Author's response    Manuscript
ED: Publish as is (19 Feb 2019) by Ulrike Werban
ED: Publish as is (27 Feb 2019) by CharLotte Krawczyk(Executive Editor)
Download
Short summary
We show the landslide response to the 2016 Kumamoto earthquake (Mw 7.1) in central Kyushu (Japan). Landslides are concentrated to the northeast of the rupture, coinciding with the propagation direction of the earthquake. This azimuthal variation in the landslide concentration is linked to the seismic rupture process itself and not to classical landslide susceptibility factors. We propose a new ground-motion model that links the seismic radiation pattern with the landslide distribution.