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Gongzheng Ma, Linsen Zhan, Hailong Lu and Guiting Hou
Geological structure changes, including deformations and ruptures, developed in shallow marine sediments are well recognized but were not systematically reviewed in previous studies. These structures, generally developed at a depth less than 1000 m below...
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Rossella Bovolenta, Alessandro Iacopino, Roberto Passalacqua and Bianca Federici
Monitoring changes in soil saturation is important for slope stability analyses. Soil moisture capacitive sensors have recently been developed; their response time is extremely fast, they require little maintenance, and they are relatively inexpensive. T...
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Cristina Gordo, José Luís Zêzere and Rui Marques
The hydrographic basin of Ribeira Grande (S. Miguel Island, Azores) has a set of characteristics that enhance the occurrence of shallow slides that have been triggered by rainfall and earthquakes. Two landslide inventories were built according to the lan...
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Salvatore Martino, Simona Battaglia, Josè Delgado, Carlo Esposito, Guido Martini and Cristina Missori
The PARSIFAL (Probabilistic Approach to pRovide Scenarios of earthquake-Induced slope FAiLures) approach was applied in the basin of Alcoy (Alicante, South Spain), to provide a comprehensive scenario of earthquake-induced landslides. The basin of Alcoy i...
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Raül Oorthuis, Marcel Hürlimann, Alessandro Fraccica, Antonio Lloret, José Moya, Càrol Puig-Polo and Jean Vaunat
Slope mass-wasting like shallow slides are mostly triggered by climate effects, such as rainfall, and soil?vegetation?atmosphere (SVA) interactions play a key role. SVA interactions are studied by a full-scale embankment with different orientations (Nort...
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J. Michael Johnson and Hugo A. Loáiciga
Shallow translational slides are common in slopes during heavy rainfall. The classic model for the occurrence of translational slides in long slopes assumes rising saturation above a slip surface that reduces the frictional strength by decreasing the eff...
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The approach of tropical cyclone (TC) Juliette, in 2001, to the Baja California Peninsula triggered at least 419 landslides. Most of the landslides were shallow slips and debris slides of limited areal extent, which were converted rapidly into debris flo...
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Sergio A. Sepulveda,Alejandra Serey
Pág. 131 - 136
The April 21, 2007 shallow crustal earthquake (Mw 6.2) in the Aisén Fjord area triggered hundreds of landslides around the epicentral zone. Among those, several rock slope failures such as rock slides, rock falls and rock avalanches were induced on the s...
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