The design of sustainable early warning systems for landslide prone areas requires deep understanding of the kinematic of landslides with emphasis on the evolution of its movement. This is controlled by many factors, and creep is a major one. Creep is perceptively slow land sliding process where the movement is nearly imperceptible and occurring at a rate of millimetres (mm) per year. This article reports the results of investigations of the viscous shear behaviour of clayey geo-materials, in particular creep and relaxation, which were carried out using a direct shear box. The viscous behaviour was investigated by either measuring the decay in shear stress at constant relative horizontal displacement (stress relaxation test) or by measuring...
The displacement rate of the considered ancient clayey earth slide varies noticeably along its longi...
Deep and superficial displacements have been measured since 2005 in a slow active landslide that has...
Deep and superficial displacements have been measured since 2005 in a slow active landslide that has...
The design of sustainable early warning systems for landslide prone areas requires deep understandin...
Translational slides in clays are often characterized by long-lasting intermittent movements associa...
Translational slides in clays are often characterized by long-lasting intermittent movements associa...
Creep behavior of clayey soils plays an extremely important role in the landslide process. The soils...
Creep behavior of clayey soils plays an extremely important role in the landslide process. The soils...
The prediction of motion of slowly moving landslides, also referred to as creeping slopes, is import...
In the last two decades extensive research has been undertaken to characterize the time and rate dep...
In structural geology, viscous creep is generally recognized as the major deformation mechanism in t...
As a result of the scarcity of land for construction, a number of projects to construct man-made isl...
The coefficient of lateral earth pressure at rest (K0) is an important parameter in any geotechnical...
The displacement rate of the considered ancient clayey earth slide varies noticeably along its longi...
The displacement rate of the considered ancient clayey earth slide varies noticeably along its longi...
The displacement rate of the considered ancient clayey earth slide varies noticeably along its longi...
Deep and superficial displacements have been measured since 2005 in a slow active landslide that has...
Deep and superficial displacements have been measured since 2005 in a slow active landslide that has...
The design of sustainable early warning systems for landslide prone areas requires deep understandin...
Translational slides in clays are often characterized by long-lasting intermittent movements associa...
Translational slides in clays are often characterized by long-lasting intermittent movements associa...
Creep behavior of clayey soils plays an extremely important role in the landslide process. The soils...
Creep behavior of clayey soils plays an extremely important role in the landslide process. The soils...
The prediction of motion of slowly moving landslides, also referred to as creeping slopes, is import...
In the last two decades extensive research has been undertaken to characterize the time and rate dep...
In structural geology, viscous creep is generally recognized as the major deformation mechanism in t...
As a result of the scarcity of land for construction, a number of projects to construct man-made isl...
The coefficient of lateral earth pressure at rest (K0) is an important parameter in any geotechnical...
The displacement rate of the considered ancient clayey earth slide varies noticeably along its longi...
The displacement rate of the considered ancient clayey earth slide varies noticeably along its longi...
The displacement rate of the considered ancient clayey earth slide varies noticeably along its longi...
Deep and superficial displacements have been measured since 2005 in a slow active landslide that has...
Deep and superficial displacements have been measured since 2005 in a slow active landslide that has...