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Landslides are a growing threat in mountainous areas. The current observable state of the climate, with intensification of rainfall instead of snowfall, and increasing urbanization are expanding areas prone to soil slide. In the presented case, in Cisiec (Southern Poland), anthropogenic and natural factors cause the formation and evolution of a landslide in the area of a ski slope. 5 years of multimethod geophysical observations, allowed us to estimate the variability in the study zone, along with an understanding of the triggering factors and their impact. The acquired knowledge has important applications in similar cases, which are increasingly recorded on a global scale.