In a homogeneous earthfill dam responsible for the water supply of a private company, an initial process of internal erosion was observed near the base of the downstream slope, which is listed as one of the main dam failures causes in the world. Although this problem has been correctly solved at the studied structure, this thesis aimed to find the causes for the detected anomaly in order to increase knowledge about this subject. To do so, the history of the structure was investigated, undisturbed samples were collected near the region of interest to carry out laboratory tests to characterize the soil, determine the physical parameters, measure permeability coefficients under different effective stresses and find its characteristic curve (SWCC) through filter paper tests. With the results of the tests, computational models were elaborated under different scenarios to investigate the behavior of hydraulic gradients. The software Plaxis LE was used in this work. It was evaluated whether the adoption of unsaturated parameters or 3D analysis would promote any change in the flow pattern in the studied structure, which did not occur. It was also considered whether the soil-atmosphere interaction could generate critical hydraulic gradients through rainfall and evaporation cycles, but there were no critical results either. Although, permeability seems to have a an inversely proportional relationship with hydraulic gradient. Thus, it is understood that the formation of organic soils at the toe of the downstream slope may have led to the observed internal erosion process.