Earthquake‐induced chains of geologic hazards: Patterns, mechanisms, and impacts
Large earthquakes initiate chains of surface processes that last much longer than the brief
moments of strong shaking. Most moderate‐and large‐magnitude earthquakes trigger …
moments of strong shaking. Most moderate‐and large‐magnitude earthquakes trigger …
Research on geological and surfacial processes and major disaster effects in the Yellow River Basin
Abstract The Yellow River Basin (YRB) is characterized by active geological and tectonic
processes, rapid geomorphological evolution, and distinct climatic diversity …
processes, rapid geomorphological evolution, and distinct climatic diversity …
A review of recent earthquake-induced landslides on the Tibetan Plateau
Earthquake-induced landslides, also called seismic landslides (SLs), are some of the most
catastrophic natural hazards on the Tibetan Plateau (TP). They have frequently caused …
catastrophic natural hazards on the Tibetan Plateau (TP). They have frequently caused …
Coseismic landslides triggered by the 8th August 2017 Ms 7.0 Jiuzhaigou earthquake (Sichuan, China): factors controlling their spatial distribution and implications …
On 8th August 2017, a magnitude M s 7.0 earthquake struck the County of Jiuzhaigou, in
Sichuan Province, China. It was the third M s≥ 7.0 earthquake in the Longmenshan area in …
Sichuan Province, China. It was the third M s≥ 7.0 earthquake in the Longmenshan area in …
Spatio-temporal evolution of mass wasting after the 2008 Mw 7.9 Wenchuan earthquake revealed by a detailed multi-temporal inventory
Strong earthquakes in mountainous areas can trigger a large number of landslides that
generate deposits of loose and unconsolidated debris across the landscape. These deposits …
generate deposits of loose and unconsolidated debris across the landscape. These deposits …
[HTML][HTML] Long-term erosion of the Nepal Himalayas by bedrock landsliding: The role of monsoons, earthquakes and giant landslides
In active mountain belts with steep terrain, bedrock landsliding is a major erosional agent. In
the Himalayas, landsliding is driven by annual hydro-meteorological forcing due to the …
the Himalayas, landsliding is driven by annual hydro-meteorological forcing due to the …
Surface temperature controls the pattern of post-earthquake landslide activity
The patterns and controls of the transient enhanced landsliding that follows strong
earthquakes remain elusive. Geostatistical models can provide clues on the underlying …
earthquakes remain elusive. Geostatistical models can provide clues on the underlying …
[HTML][HTML] The role of infrequently mobile boulders in modulating landscape evolution and geomorphic hazards
A landscape's sediment grain size distribution is the product of, and an important influence
on, earth surface processes and landscape evolution. Grains can be large enough that the …
on, earth surface processes and landscape evolution. Grains can be large enough that the …
The sha** of erosional landscapes by internal dynamics
Erosional landscapes transport sediment downstream, host natural hazards and are
geologically active. While perturbations in external forcing, particularly climate and tectonics …
geologically active. While perturbations in external forcing, particularly climate and tectonics …
The art of landslides: How stochastic mass wasting shapes topography and influences landscape dynamics
Bedrock landslides shape topography and mobilize large volumes of sediment. Yet,
interactions between landslide‐produced sediment and fluvial systems that together govern …
interactions between landslide‐produced sediment and fluvial systems that together govern …