The bachelor thesis is focused on lateral movement of water in disturbed soil environment. Such disturbance in the sloping terrain can be a sloping forest path. In our research, the slopes of the forest paths served as an example of such disturbance. This disturbance can lead to the transformation of the subsurface flow into the surface, which means the loss of water in the water balance of the forest ecosystem and ultimately also to cause considerable property damage. In order to influence the impaired environment on the water movement, we performed electrical resistivity tomography measurements in Laudstoch in the cadastral area of Banská Belá. The measured results show that after the rainfall in the shallow layers of the soil, the infiltration water moves along the slope and, at the site of disturbance, is transformed into a surface runoff. The transformation of the flow is strongly dependent on the soil characteristics of the area and can occur at relatively short distances.