Page 5: Research news on landslide

A landslide is a mass-movement phenomenon in which soil, rock, regolith, or debris moves downslope under the influence of gravity, often along a discrete shear surface or failure plane. It encompasses diverse mechanisms such as rotational and translational slides, debris flows, rockfalls, and avalanches, typically initiated when driving forces exceed resisting forces due to factors like pore-water pressure increase, seismic shaking, weathering, or anthropogenic slope modification. Landslides are characterized by rapid to extremely rapid kinematics, spatial heterogeneity of displacement, and strong dependence on lithology, structural discontinuities, hydrological conditions, and topography, and are central to geomorphological evolution and natural hazard assessment.

Why seismic waves are slower shortly after an earthquake

Solid as they are, rocks are not static materials with constant properties. Even small loads are enough to alter their mechanical properties; their reaction to being deformed is a loss of stiffness. Rocks which have been ...

When Martian ground falls apart

In its latest postcard from Mars, the European Space Agency's Mars Express returns to Acheron Fossae: a dramatic network of chasms carved into the surface of the red planet.

Landslide-prone Nepal tests AI-powered warning system

Every morning, Nepali primary school teacher Bina Tamang steps outside her home and checks the rain gauge, part of an early warning system in one of the world's most landslide-prone regions.

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