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 …
Mountains, erosion and the carbon cycle
Mountain building results in high erosion rates and the interaction of rocks with the
atmosphere, water and life. Carbon transfers that result from increased erosion could control …
atmosphere, water and life. Carbon transfers that result from increased erosion could control …
Landslide mobilization rates: A global analysis and model
Landslides are a main driver of landscape evolution and a dominant sediment source in
many regions worldwide. Nevertheless, their role in sediment mobilization and denudation …
many regions worldwide. Nevertheless, their role in sediment mobilization and denudation …
An unshakable carbon budget for the Himalaya
The erosion and weathering of mountain ranges exert a key control on the long-term (105–
106 yr) cycling of carbon between Earth's surface and crust. The net carbon budget of a …
106 yr) cycling of carbon between Earth's surface and crust. The net carbon budget of a …
Inversions of landslide strength as a proxy for subsurface weathering
Distributions of landslide size are hypothesized to reflect hillslope strength, and
consequently weathering patterns. However, the association of weathering and critical zone …
consequently weathering patterns. However, the association of weathering and critical zone …
Topographic stress control on bedrock landslide size
Landslides are a major natural hazard and act as a primary driver of erosion, chemical
weathering and organic carbon transfer in mountain ranges. Evaluating the impact of …
weathering and organic carbon transfer in mountain ranges. Evaluating the impact of …
Seismic cycles, earthquakes, landslides and sediment fluxes: Linking tectonics to surface processes using a reduced-complexity model
In tectonically active mountain ranges, landslides triggered by earthquakes mobilise large
volumes of sediment that affect river dynamics. This sediment delivery can cause …
volumes of sediment that affect river dynamics. This sediment delivery can cause …
Increased landslide activity on forested hillslopes following two recent volcanic eruptions in Chile
O Korup, J Seidemann, CH Mohr - Nature Geoscience, 2019 - nature.com
Large explosive eruptions can bury landscapes beneath thick layers of tephra. Rivers
subsequently overloaded with excess pyroclastic sediments have some of the highest …
subsequently overloaded with excess pyroclastic sediments have some of the highest …
Long-term patterns of hillslope erosion by earthquake-induced landslides shape mountain landscapes
Widespread triggering of landslides by large storms or earthquakes is a dominant
mechanism of erosion in mountain landscapes. If landslides occur repeatedly in particular …
mechanism of erosion in mountain landscapes. If landslides occur repeatedly in particular …
Landslides: An emerging model for ecosystem and soil chronosequence research
O Rasigraf, D Wagner - Earth-Science Reviews, 2022 - Elsevier
Erosion by landslides is a common phenomenon in mountain regions around the globe,
affecting all climatic zones. Landslides facilitate bedrock weathering, pedogenesis and …
affecting all climatic zones. Landslides facilitate bedrock weathering, pedogenesis and …