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| Content Provider | Springer Nature Link |
|---|---|
| Author | Runqiu, Huang |
| Copyright Year | 2009 |
| Abstract | Landslides occur frequently in China. Especially, in the western part of China, large-scale landslides are notable for their scale, complex formation mechanism, and serious destruction. This paper presents some typical large-scale landslides that occurred in the southwest of China since the beginning of the twentieth century but were rarely reported worldwide. These cases represent different geological conditions and different triggering factors and mechanisms. The analysis shows that about 80% of large-scale landslides occurred in the first slope-descending zone along the eastern margin of Tibet Plateau, which is tectonically very active. The intensive interactions between the endogenic and epigenetic geological process cause serious dynamic change on the high steep slope and then result in the development of large-scale landslides. Strong earthquakes are also common in this area, and repetitive seismic activities make the slopes unstable and more vulnerable to failures. Besides earthquake, the area also experiences high rainfall, which is also responsible for triggering some of the large landslides. |
| Starting Page | 69 |
| Ending Page | 81 |
| Page Count | 13 |
| File Format | |
| ISSN | 1612510X |
| Journal | Landslides |
| Volume Number | 6 |
| Issue Number | 1 |
| e-ISSN | 16125118 |
| Language | English |
| Publisher | Springer-Verlag |
| Publisher Date | 2009-02-24 |
| Publisher Place | Berlin, Heidelberg |
| Access Restriction | One Nation One Subscription (ONOS) |
| Subject Keyword | Large-scale landslides Case study Triggering mechanism China Geography (general) Civil Engineering Agriculture Natural Hazards |
| Content Type | Text |
| Resource Type | Article |
| Subject | Geotechnical Engineering and Engineering Geology |
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