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EnglishDuring the last 30 years of studies in the field of mass movements located in the calcareous-marly and marly-sandy Apennines (Umbria-Marches and Latium-Abruzzi regions), over to a large number of landslides with different dimensions, even a lot of deep-seated gravitational slope deformations (DSGSDs) have been recognized and analysed. These phenomena are also located in that sector of central Italy affected by a cold climate during the past and actually temperate (central Apennine chain).
| Titolo: | DSGSDs induced by post-glacial decompression in central Apennine (Italy) | |
| Autori: | ||
| Data di pubblicazione: | 2013 | |
| Abstract: | During the last 30 years of studies in the field of mass movements located in the calcareous-marly and marly-sandy Apennines (Umbria-Marches and Latium-Abruzzi regions), over to a large number of landslides with different dimensions, even a lot of deep-seated gravitational slope deformations (DSGSDs) have been recognized and analysed. These phenomena are also located in that sector of central Italy affected by a cold climate during the past and actually temperate (central Apennine chain). | |
| Handle: | http://hdl.handle.net/11564/442886 | |
| ISBN: | 978 3 642 31337 0 | |
| Appare nelle tipologie: | 4.1 Contributo in Atti di convegno |
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