Earthquake-Induced Landslide Susceptibility and Hazard Assessment Approaches

Sepúlveda, Sergio A.

doi:10.1007/978-981-19-6597-5_14

Cited by 3 publications

(1 citation statement)

References 100 publications

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“…Ground motion variability is known to influence landslide susceptibility (e.g. Sepúlveda, 2022;Massey et al, 2022) but remains challenging to estimate on a regional scale. Outside of applying regional ground motion intensity estimates (PGA/PGV from the USGS ShakeMap), this analysis does not investigate the role of site-specific ground motion.…”

Section: Factors Controlling Increased Coastal Landslide Densitymentioning

confidence: 99%

Coastal earthquake-induced landslide susceptibility during the 2016 M_w 7.8 Kaikōura earthquake, New Zealand

Bloom,

Singeisen,

Stahl

et al. 2023

Nat. Hazards Earth Syst. Sci.

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Abstract. Coastal hillslopes often host higher concentrations of earthquake-induced landslides than those further inland, but few studies have investigated the reasons for this occurrence. As a result, it is unclear if regional earthquake-induced landslide susceptibility models trained primarily on inland hillslopes are effective predictors of coastal susceptibility. The 2016 Mw 7.8 Kaikōura earthquake on the northeastern South Island of New Zealand resulted in ca. 1600 landslides > 50 m2 on slopes > 15∘ within 1 km of the coast, contributing to an order of magnitude greater landslide source area density than inland hillslopes within 1 to 3 km of the coast. In this study, logistic regression modelling is used to investigate how landslide susceptibility differs between coastal and inland hillslopes and to determine the factors that drive the distribution of coastal landslides initiated by the 2016 Kaikōura earthquake. Strong model performance (area under the receiver operator characteristic curve or AUC of ca. 0.80 to 0.92) was observed across eight models, which adopt four simplified geology types. The same landslide susceptibility factors, primarily geology, steep slopes, and ground motion, are strong model predictors for both inland and coastal landslide susceptibility in the Kaikōura region. In three geology types (which account for more than 90 % of landslide source areas), a 0.03 or less drop in model AUC is observed when predicting coastal landslides using inland-trained models. This suggests little difference between the features driving inland and coastal landslide susceptibility in the Kaikōura region. Geology is similarly distributed between inland and coastal hillslopes, and peak ground acceleration (PGA) is generally lower in coastal hillslopes. Slope angle, however, is significantly higher in coastal hillslopes and provides the best explanation for the high density of coastal landslides during the 2016 Kaikōura earthquake. Existing regional earthquake-induced landslide susceptibility models trained on inland hillslopes using common predictive features are likely to capture this signal without additional predictive variables. Interestingly, in the Kaikōura region, most coastal hillslopes are isolated from the ocean by uplifted shore platforms. Enhanced coastal landslide susceptibility from this event appears to be a legacy effect of past erosion from wave action, which preferentially steepened these coastal hillslopes.

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Section: Factors Controlling Increased Coastal Landslide Densitymentioning

confidence: 99%

Coastal earthquake-induced landslide susceptibility during the 2016 M_w 7.8 Kaikōura earthquake, New Zealand

Bloom,

Singeisen,

Stahl

et al. 2023

Nat. Hazards Earth Syst. Sci.

View full text Add to dashboard Cite

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Spatial Prediction of Earthquake-Induced Landslide Susceptible Zones—A Case Study from Indian Himalaya

Kumar,

Kaushik

et al. 2023

Advances in Natural and Technological Hazards Research

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Effect of geometry on the natural frequency and seismic response characteristics of slopes subjected to pulse-like ground motions

Antwi Buah,

Zhang,

Abdulrazig

et al. 2024

Computers and Geotechnics

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Earthquake-Induced Landslide Susceptibility and Hazard Assessment Approaches

Cited by 3 publications

References 100 publications

Coastal earthquake-induced landslide susceptibility during the 2016 M_w 7.8 Kaikōura earthquake, New Zealand

Coastal earthquake-induced landslide susceptibility during the 2016 M_w 7.8 Kaikōura earthquake, New Zealand

Spatial Prediction of Earthquake-Induced Landslide Susceptible Zones—A Case Study from Indian Himalaya

Effect of geometry on the natural frequency and seismic response characteristics of slopes subjected to pulse-like ground motions

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Earthquake-Induced Landslide Susceptibility and Hazard Assessment Approaches

Cited by 3 publications

References 100 publications

Coastal earthquake-induced landslide susceptibility during the 2016 Mw 7.8 Kaikōura earthquake, New Zealand

Coastal earthquake-induced landslide susceptibility during the 2016 Mw 7.8 Kaikōura earthquake, New Zealand

Spatial Prediction of Earthquake-Induced Landslide Susceptible Zones—A Case Study from Indian Himalaya

Effect of geometry on the natural frequency and seismic response characteristics of slopes subjected to pulse-like ground motions

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Product

Resources

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Coastal earthquake-induced landslide susceptibility during the 2016 M_w 7.8 Kaikōura earthquake, New Zealand

Coastal earthquake-induced landslide susceptibility during the 2016 M_w 7.8 Kaikōura earthquake, New Zealand