The wide range of both spatial and temporal scales distinguishes landslide processes
significantly from other natural processes such as floods, earthquake shaking or tsunamis …

Although it is generally assumed that the internal structure of a slope (eg lithology and rock
mass properties, inherited faults and heterogeneities, etc.) is preponderant for the …

Landslide erosion has an established history in New Zealand. Some broad estimates of
economic costs for short-term event damage, long-term landslide damage, and proactive …

The paper deals with the relationship between the temporal occurrence of landslides and
climatic changes in the Italian Dolomites since the Late glacial. After an introduction on the …

Debris flow initiation by channel bed mobilization is a common process in high mountainous
areas. Initiation is more likely to occur at the outlet of small, steeply sloping basins where …

Geomorphology has now reached a certain level where the methodology, scientific content
and resultsbeing published in the field make it worthy of being considered as a major …

This study investigates the relationships between climate changes and hillslope evolution in
the Dolomites (eastern Alps, Italy), during the Late Quaternary, with particular attention paid …

A continuous recording of landslide displacements is often required in order to better
understand the complex relationship between the triggering factors and the dynamics of the …

Soil properties of major landslides that occurred recently on the mid-altitude slopes of Mount
Elgon, eastern Uganda were analysed. A mudflow, located at the Kitati protected forest site …

Rainfall and its consequences are usually considered as the major factor triggering slope
instabilities within clay deposits. The link between rainfall, water infiltration and landslide …