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A translational slide, also known as a lateral slide or a translational movement, occurs when a mass of rock or soil moves horizontally along a slope without significant rotation or tilting. This type of landslide typically happens when the material fails due to factors like saturation from rainfall or seismic activity. The movement is characterized by the material sliding over a defined surface, often resulting in a relatively uniform displacement. Translational slides can pose significant risks to structures and landscapes in their path.

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3w ago

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