Discusses the results abtained from geomorphological and hydrological investigation conducted in order to point out the complex geomorphological evolution related to a large part of the Castronuovo S. Andrea (PZ) territory, to identify the landslide typology of two different mass movements under investigation, as well as the influence caused by the rainfall. The landslide under study occurred on two opposite slopes of the low valley of torrent Mastro Ciardi, characterised by the same stratigraphic-structural, hydrogeological and geotechnic environment. The first slope can be ascribed to a displacement of a first detachment, while the other one for at least 70% can be referred to a remobilization phenomenon; both landslides, to a variable extent, have been influenced by tectonic joints following two different directions: NE-SW and WNW-ESE. -from English summary
Geomorphological evolution of a Castronuovo S. Andrea (PZ): suburban area and rainfall influence on mass movements
D'Ecclesiis G.;Merenda L.;Polemio M.Penultimo
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1991
Abstract
Discusses the results abtained from geomorphological and hydrological investigation conducted in order to point out the complex geomorphological evolution related to a large part of the Castronuovo S. Andrea (PZ) territory, to identify the landslide typology of two different mass movements under investigation, as well as the influence caused by the rainfall. The landslide under study occurred on two opposite slopes of the low valley of torrent Mastro Ciardi, characterised by the same stratigraphic-structural, hydrogeological and geotechnic environment. The first slope can be ascribed to a displacement of a first detachment, while the other one for at least 70% can be referred to a remobilization phenomenon; both landslides, to a variable extent, have been influenced by tectonic joints following two different directions: NE-SW and WNW-ESE. -from English summaryI documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.
