Monitoring and Prevention of Debrisflows and Landslides in Tibet
CUI Peng;CHEN Xiao-Qing;CHENG Zun-Lan;CHEN Ning-Sheng;DANG Chao
2010, 32(1):
19-25.
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Tibet, the main part of the QinghaiTibet Plateau, is a hypersensitive terrain for the generation of debris flows and landslides, and is noteworthy for active tectonism, sharp changes in topography, and for cold, dry conditions at high elevations contrasting with intense rainfall in valleys. Widespread in Tibet, debris flows are triggered by glacial meltwater, glacial lake outburst floods, rainstorms and freezethaw activity. Thick deposits of large landslides, both modern and ancient, are common. In general, debris flows and landslides are associated with faults, seismic zones, deeply incised valleys, and road construction. The different types and scales of flows and slope failures occur in valley and highland areas. Construction activities in areas that are susceptible to debrisflow and landslide formation frequently result in major disasters in Tibet. The mountainous sections of the SichuanTibet Highway along the Polongzangbu valley and of the ChinaNepal Highway from Nielamu to the Friendship Bridge are selected as cases proposed for a hazard monitoring and warning system for highway safety. A total of 26 towns at risk of debrisflows and landslides have been identified, and a specific plan of risk reduction for the typical Tibetan town of Nielamu, site of a previous debrisflow disaster, has been prepared. The plan consists of a monitoring and warning system, engineering structures, and specific emergency countermeasures.