Through its relatively low precipitation and good preservation of minor geomorphic features, particularly those formed by past landslides, this region provides opportunities for detailed study of the internal structure of landslide bodies.
- Summarizes the present-day knowledge of bedrock landslide distribution in the Dzungaria, Tien Shan and Pamir mountains
- Describes case studies illustrating both general characteristics of large bedrock landslides and other specific features, allowing comparative analysis of numerous case studies
- Presents the classification of bedrock landslides and related models based on deposits, morphology and internal structures that can be applied to global locations
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