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 …

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 …

Strong earthquakes, especially on mountain slopes, can generate large amounts of
unconsolidated deposits, prone to remobilization by aftershocks and rainstorms. Assessing …

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 …

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 …

We release two datasets that track the enhanced landsliding induced by the 2008 M w 7.9
Wenchuan earthquake over a portion of the Longmen Mountains, at the eastern margin of …

Lithospheric organic carbon (“petrogenic”; OCpetro) is oxidized during exhumation and
subsequent erosion of mountain ranges. This process is a considerable source of carbon …

Major earthquakes in steep orogens can trigger extensive landsliding. Most of the landslide
bodies come to rest high on the slopes, but subsequent rainfalls can easily remobilize them …

Infrequent extreme events such as large earthquakes pose hazards and have lasting
impacts on landscapes and biogeochemical cycles. Sediments provide valuable records of …

Abstract The Araniko and Pasang Lhamu highways are two critical trading routes connecting
Nepal and China that are experiencing and are threatened by landsliding. The April 25 M w …