translational landslide

A translational landslide occurs when a mass of soil or rock moves downhill along a flat or gently sloping surface, typically caused by gravity and factors like heavy rain, earthquakes, or human activities. In this type of landslide, the movement is relatively quick and occurs in a more horizontal direction, as opposed to rotating or tumbling. Unlike other landslides that may involve chaotic movement, translational landslides often maintain their shape and can emerge suddenly, posing risks to structures and ecosystems below. Proper drainage and land management can help reduce their occurrence.