It is here presented the geological mapping of a deposit portion of Vajont landslide which took place on October 9, 1963, in order to define the asset of the involved formations and of the quaternary. The measurements have been performed on outcrops selected in such a way to permit the characterization of the major blocks constituted by different lithological units belonging to the Calcare di Socchèr, with particular interest in the Colle Isolato. Moreover, it was performed a 155 meter long geoelectrical mapping along the road leading to Pineda, employing a PASI computer resistivity meter in order to define the electric resistive tomography (ERT) and evaluate the resistivity of different types of deposits
Rilevamento geologico-strutturale e indagine geoelettrica della porzione Nord Occidentale della frana del Vajont nelle Prealpi Venete = Geological-Structural Mapping And Geoelectrical investigation of the North-Occidental portion of the Vajont landslide in the Venetian Prealps
Carli, Marco
2011/2012
Abstract
It is here presented the geological mapping of a deposit portion of Vajont landslide which took place on October 9, 1963, in order to define the asset of the involved formations and of the quaternary. The measurements have been performed on outcrops selected in such a way to permit the characterization of the major blocks constituted by different lithological units belonging to the Calcare di Socchèr, with particular interest in the Colle Isolato. Moreover, it was performed a 155 meter long geoelectrical mapping along the road leading to Pineda, employing a PASI computer resistivity meter in order to define the electric resistive tomography (ERT) and evaluate the resistivity of different types of depositsFile | Dimensione | Formato | |
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Frana_del_Vaiont.pdf
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https://hdl.handle.net/20.500.12608/15127