the sliding movement of rock masses down a slope under the action of the force of gravity. Landslides occur on particular segments of an incline or slope as a result of unbalance of the rocks caused by an increase in the steepness of the slope through erosion by water, weakening of the rock by weathering or supersaturation by precipitation and groundwater, seismic shocks, or construction and economic activity carried out without consideration for the geological conditions of the terrain (breaking up slopes by road excavation, excessive watering of gardens and orchards on slopes, and so on).
Landslides most often occur on slopes composed of alternating impervious (clayey) and water-bearing rock (for example, sand and gravel or fissured limestone). The development of landslides is also promoted by types of bedding in which layers are inclined in the direction of the slope or are crossed by fissures going in the same direction. Landslides assume the form of a flow in strongly moistened clayey rock. A landslide is often semicircular in cross section (see Figure 1), forming a depression in the slope that is called the landslide cirque.
Landslides cause great damage to farmland, industrial enterprises, and populated areas. Reinforcement works and drainage structures are constructed to combat landslides, piles are driven to secure the slopes, and vegetation is planted.