Landslide occurrence has become increasingly influenced by human activities. Accordingly,
changing land use and land cover (LULC) is an important conditioning factor in landslide …

Debris flows are the most dangerous geological hazard in steep terrain. For systematic
debris flow mitigation and management, debris flow evaluation is required. Over the past few …

Physical modelling is a useful method to examine how landslides deform and fail at the
laboratory scale. Reliable and accurate measurement systems are required for landslide …

Large wood (LW) is an important element in riparian and mountain ecosystems and
influences geomorphic controls, particularly in torrents and mountain rivers. Despite several …

We propose a mechanical explanation for the low basal shear resistance (about 50 kPa)
previously used to simulate successfully the complex, well-documented deposit morphology …

This special issue of Geomorphology includes 14 papers dealing with landslides selected
from two conferences of the International Association of Geomorphologists (IAG): the …

Tropical landslides are suitable locations to study short-term carbon (C) fluxes because of
the rapid changes that occur for the first few years following initial disruption of the slope …

When tests are conducted on the field slope under artificial rainfall, because artificial rainfall
is often limited to implementation in the mode of local rainfall, there is a boundary constraint …

Landslide hazard can be influenced by natural resource management and rural
development related activities, such as forest management, road construction, agricultural …

Repeated freeze–thaw cycles on slopes trigger sorting and solifluction mass movements,
while subsequent displacement of material modifies the geomorphology of slopes as well as …