El paleomovimiento de Fonfría (Villablino, Cordillera Cantábrica)
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Abstract
La cartografía geomorfológica permite clasificar el movimiento
de ladera de Fonfría como un paleomovimiento paraglaciar, complejo e inactivo, al menos hasta el año 2000, en la fase previa a la
explotación minera de carbón de Fonfría. Posteriormente, durante
la fase de actividad minera y después, el movimiento empieza a ser
afectado por estructuras de deformación gravitacional, reactivándose parcialmente
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
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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