Earthquake‐induced chains of geologic hazards: Patterns, mechanisms, and impacts

X Fan, G Scaringi, O Korup, AJ West… - Reviews of …, 2019 - Wiley Online Library
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 …

[HTML][HTML] The role of infrequently mobile boulders in modulating landscape evolution and geomorphic hazards

CM Shobe, JM Turowski, R Nativ, RC Glade… - Earth-Science …, 2021 - Elsevier
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 …

The size, distribution, and mobility of landslides caused by the 2015 Mw7. 8 Gorkha earthquake, Nepal

K Roback, MK Clark, AJ West, D Zekkos, G Li… - Geomorphology, 2018 - Elsevier
Coseismic landslides pose immediate and prolonged hazards to mountainous communities,
and provide a rare opportunity to study the effect of large earthquakes on erosion and …

Landslides after wildfire: Initiation, magnitude, and mobility

FK Rengers, LA McGuire, NS Oakley, JW Kean… - Landslides, 2020 - Springer
In the semiarid Southwestern USA, wildfires are commonly followed by runoff-generated
debris flows because wildfires remove vegetation and ground cover, which reduces soil …

The problem of predicting the size distribution of sediment supplied by hillslopes to rivers

LS Sklar, CS Riebe, JA Marshall, J Genetti, S Leclere… - Geomorphology, 2017 - Elsevier
Sediments link hillslopes to river channels. The size of sediments entering channels is a key
control on river morphodynamics across a range of scales, from channel response to human …

River profile response to normal fault growth and linkage: An example from the Hellenic forearc of south-central Crete, Greece

SF Gallen, KW Wegmann - Earth Surface Dynamics, 2017 - esurf.copernicus.org
Topography is a reflection of the tectonic and geodynamic processes that act to uplift the
Earth's surface and the erosional processes that work to return it to base level. Numerous …

Fracture density and grain size controls on the relief structure of bedrock landscapes

RA DiBiase, MW Rossi, AB Neely - Geology, 2018 - pubs.geoscienceworld.org
Quantifying how rock properties influence landscape evolution is an outstanding challenge
that confounds attempts to generalize relationships between topography and erosion rate …

Reconceptualising flood risk assessment by incorporating sediment supply

H Liu, J Du, Y Yi - Catena, 2022 - Elsevier
Sediments seriously increase flood risk. The lack of sediment data, as well as uncertainty in
sediment yield and transport modeling, hampers the incorporation of sediment into flood risk …

Fluvial archives, a valuable record of vertical crustal deformation

A Demoulin, A Mather, A Whittaker - Quaternary Science Reviews, 2017 - Elsevier
The study of drainage network response to uplift is important not only for understanding river
system dynamics and associated channel properties and fluvial landforms, but also for …

Sediment controls on the transition from debris flow to fluvial channels in steep mountain ranges

AB Neely, RA DiBiase - Earth Surface Processes and …, 2023 - Wiley Online Library
Steep channel networks commonly show a transition from constant‐gradient colluvial
channels associated with debris flow activity to concave‐up fluvial channels downstream …