There have been major improvements in instrumentation, field survey design and data
inversion techniques for the geoelectrical method over the past 25 years. Multi-electrode …

In the context of in-situ geophysical methods the Electrical Resistivity Tomography (ERT) is
widely used for the near-surface exploration of landslide areas characterized by a complex …

Deep-seated gravitational slope deformations (DSGSDs) are slow moving, hillslope-scale
mass movements featuring characteristic landforms such as double-crested ridges and …

Pakhi landslide is one of the major debris slides of retrogressive nature along national
highway (NH-58) corridor from Rishikesh to Badrinath in Garhwal Himalayas, India. The …

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 …

Climatic factors are considered major causes and triggers of slope instability, but the
palaeoclimatic implications of landslides have not yet been systematically reviewed. As …

Abstract The Heifangtai terrace, in Northwest China, is a typical area where loess landslides
have been induced by agricultural irrigation, and many of the landslides are prone to …

Toppling is the foremost failure pattern of anaclinal rock slopes, and deep-seated toppling
deformations (DSTDs) are common on high anaclinal slopes on the sides of gorges in …

The deformation process of soil slopes observed during a landslide can have progressive
characteristics, which can be quantified through acoustic emission (AE) monitoring. A model …

The large-scale deformation of high mountain slopes finds its origin in many phenomena
(inherent parameters, external stresses) with very different time constants (instantaneous to …