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Soil erosion is a natural process that models the land surface, building large geological ensembles and erosion relief from the most trivial to the most obvious forms of erosion that gives the characteristic note of geographical landscapes. Subjected to a continuous disintegration, fragments of rock and fine particles of soil are detached and transported by the movement of diverse masses of material: blown or taken from rainwater, and then transported by streams and rivers and finally submitted along river valleys...