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 …
Times associated with source-to-sink propagation of environmental signals during landscape transience
Sediment archives in the terrestrial and marine realm are regularly analyzed to infer
changes in climate, tectonic, or anthropogenic boundary conditions of the past. However …
changes in climate, tectonic, or anthropogenic boundary conditions of the past. However …
The gravel-sand transition and grain size gap in river bed sediments
EH Dingle, KM Kusack, JG Venditti - Earth-Science Reviews, 2021 - Elsevier
River bed sediments typically fine downstream, where fining of median grain sizes are often
described as exponential, except where fine gravel abruptly transitions to sand. Across the …
described as exponential, except where fine gravel abruptly transitions to sand. Across the …
Tectonic accretion controls erosional cyclicity in the Himalaya
The evolution of Earth's climate over geological timescales is linked to surface erosion via
weathering of silicate minerals and burial of organic carbon. However, methodological …
weathering of silicate minerals and burial of organic carbon. However, methodological …
Alluvial cover controlling the width, slope and sinuosity of bedrock channels
JM Turowski - Earth Surface Dynamics, 2018 - esurf.copernicus.org
Bedrock channel slope and width are important parameters for setting bedload transport
capacity and for stream-profile inversion to obtain tectonics information. Channel width and …
capacity and for stream-profile inversion to obtain tectonics information. Channel width and …
Long-profile evolution of transport-limited gravel-bed rivers
AD Wickert, TF Schildgen - Earth Surface Dynamics, 2019 - esurf.copernicus.org
Alluvial and transport-limited bedrock rivers constitute the majority of fluvial systems on
Earth. Their long profiles hold clues to their present state and past evolution. We currently …
Earth. Their long profiles hold clues to their present state and past evolution. We currently …
Characterising groundwater-surface water connectivity in the lower Gandak catchment, a barrage regulated biodiversity hotspot in the mid-Gangetic basin
The alluvial aquifer system of the Indo-Gangetic Basin (IGB) is one of the world's most
important freshwater resources, sustaining humans and river ecosystems. Understanding …
important freshwater resources, sustaining humans and river ecosystems. Understanding …
Sediment dynamics across gravel-sand transitions: Implications for river stability and floodplain recycling
The gravel-sand transition (GST) is commonly observed along rivers. It is characterized by
an abrupt reduction in median grain size, from gravel-to sand-size sediment, and by a shift in …
an abrupt reduction in median grain size, from gravel-to sand-size sediment, and by a shift in …
Downvalley fining of hillslope sediment in an alpine catchment: implications for downstream fining of sediment flux in mountain rivers
The size distributions of sediment delivered from hillslopes to rivers profoundly influence
river morphodynamics, including river incision into bedrock and the quality of aquatic …
river morphodynamics, including river incision into bedrock and the quality of aquatic …
[HTML][HTML] Sediment size on talus slopes correlates with fracture spacing on bedrock cliffs: Implications for predicting initial sediment size distributions on hillslopes
The detachment of rock fragments from fractured bedrock on hillslopes creates sediment
with an initial size distribution that sets the upper limits on particle size for all subsequent …
with an initial size distribution that sets the upper limits on particle size for all subsequent …