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 …

Here we assess earthquake volume balance and the growth of mountains in the context of a
new landslide inventory for the Mw 7.9 Wenchuan earthquake in central China. Coseismic …

Large, compressional earthquakes cause surface uplift as well as widespread mass
wasting. Knowledge of their trade‐off is fragmentary. Combining a seismologically …

Potentially active faults are exposed in the steep glaciated topography of the central
Southern Alps, New Zealand, immediately adjacent to the Alpine Fault plate boundary. Four …

Large earthquakes rapidly denude hillslopes by triggering thousands of coseismic
landslides. The sediment produced by these landslides is initially quickly mobilised from the …

Individual, large thrusting earthquakes can cause hundreds to thousands of years of
exhumation in a geologically instantaneous moment through landslide generation. The …

Large dip‐slip earthquakes have a major contribution to mountain building while earthquake‐
induced landslides lower mountains simultaneously. The amount of the coseismic uplift and …

2008 年MW 7.9 汶川地震导致龙门山断裂发生强烈地壳变形, 同时引发的巨量同震滑坡加速了
该地区的地表剥蚀和河流侵蚀. 然而, 目前尚缺少系统的数据定量研究滑坡物质的运移以及河流 …

The widely held notion about the relationship between reverse‐faulting earthquakes and
mountain building has been challenged by recent studies suggesting a net coseismic …

Landscape evolution in active orogen region is inevitably affected by landslides associated
with strong earthquakes, rain or storm. However, quantitative studies of the orogenic or …