During rainy events it can occur water flow in the interior of the soil erosions, thus carrying great amount from sediments, that are deposited in lower areas. The soil erosions go in accordance with to differentiate of the ravinas the width and depth. Some classifications in the world exist on these limits, but optimum it is to analyze and to establish the differences between these two erosive processes for distinct regions (WAR, 1998). Effect of the erosions in sheet with formation of soil erosions quarter Garden of the Buritis the effect of the erosions laminar or sheet for the convergent regimen of torrent waters, generally transform into ravinamento and soil erosions, in the quarter in question in this convergent regimen of torrent waters by means of the public ways (streets) and side streets in the city of Buritizeiro had taken the formation of two great soil erosions resulted of the displacement of waters of the quarters highest. Due to perenidade of the spring and for the place to be inhabited, the urbanstico sector constructed a bridge in order to facilitate to the life of the inhabitants and passer-bys of that quarter.
Therefore since its headboard until the area of sedimentation of material of the eroded material, housings in the neighborhoods of the edge of the soil erosion exist, in for some residence had to proceed been from attention for the evolutivo picture of the same one. Most of this area of contribution is constructed area that generally canalizes waters of rains streets, serving only of water collectors. The vacant lots and streets without pavement are a positive factor in the process of infiltration of waters of rains, having to brighten up the effect of the contribution areas. The ground of the area of contribution of waters and the areas of the soil erosions is the arenaceous Lotossolo and deep, that favors infiltration, but if worked correctly it does not favor the formation of laminar erosions, as it is perceived in the streets with formation of ravinas and soil erosions.