The Fonfría paleolandslide (Villablino, Cantabrian Mountains)
DOI:
https://doi.org/10.55407/geogaceta98194Keywords:
paraglacial landslide, conditioning factors, propagation mechanisms, mining activity, Cantabrian MountainsAbstract
The Fonfría landslide is classified by geomorphological mapping as a paraglacial paleolandslide, complex and inactive, at least until 2000, before the Fonfría mining activity. Later, during and after the mining activity, the landslide started to be partially affected by new landslides and gravitational-deformation structures.
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