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Fault-zone controls on the spatial distribution of slow-moving landslides
Fault-zone controls spatial distribution slow-moving landslides
2014/4/9
Slow-moving landslides (earth flows) can dominate hills lope sediment flux and landscape erosion in hilly terrain with mechanically weak, fine-grained rock. Controls on the occurrence of slow-moving ...
Fault-zone controls on the spatial distribution of slow-moving landslides
Fault-zone controls spatial distribution slow-moving landslides
2014/4/8
Slow-moving landslides (earthfl ows) can dominate hillslope sediment fl ux and landscape erosion in hilly terrain with mechanically weak, fi ne-grained rock. Controls on the occurrence of slow-moving ...
Assessing the capability of terrestrial laser scanning for monitoring slow moving landslides
capability terrestrial laser slow moving landslides
2009/12/10
Digital elevation models (DEM) are widely used to determine characteristics of mass movement processes such as accumulation and deposition of material, volume estimates or the orientation of discontin...
Assessing the capability of terrestrial laser scanning for monitoring slow moving landslides
terrestrial laser scanning slow moving landslides
2009/12/31
Digital elevation models (DEM) are widely used to determine characteristics of mass movement processes such as accumulation and deposition of material, volume estimates or the orientation of discontin...
Investigation and monitoring in support of the structural mitigation of large slow moving landslides:an example from Ca' Lita (Northern Apennines,Reggio Emilia,Italy)
Investigation monitoring structural mitigation large slow moving landslides
2009/12/29
The Ca' Lita landslide is a large and deep-seated mass movement located in the Secchia River Valley, in the sector of the Northern Apennines falling into Reggio Emilia Province, about 70 km west of Bo...