0000000000918513

AUTHOR

T. Macaluso

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The great landslide at Portella Colla (Madonie, Sicily)

1996

The South Western area of the Madonie Mountains is affected by large landslides; the major one developed starting from Portella Colla down to the Imera Settentrionale river, for a maximum length of about 6.2 km in a NE-SW direction. The study of the landslide, with the aim of reconstructing the geological, geomorphological and evolutionary aspects, has been carried out using integrated methodologies, including some geophysical investigations (in particular geoelectrical prospecting). The landslide is complex and characterized by superficial and deep gravitational deformations. The movement began in the Upper Pliocene and it is still active. The origin and evolution of the landslide are link…

Settore GEO/04 - Geografia Fisica E GeomorfologiaSettore GEO/11 - Geofisica ApplicataLandslide Deep-seated Gravitational Slope Deformations Madonie Sicily
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