An Earthflow is a type of landslide characterized by the slow, continuous movement of saturated soil and rock downhill due to gravity. It typically occurs in areas with relatively gentle slopes and can be composed of a mixture of water, soil, and other materials, such as vegetation and rock fragments. Earthflows can be triggered by factors such as heavy rainfall, rapid snowmelt, or human activities that destabilize the slope, like construction or deforestation.
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