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The databases that these empirical indices are derived from include a wide range of landslide types (from slow, smaller soil slides to large, rapid rock avalanches), and the determined thresholds might not be appropriate for the Peace River region's dams.
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Fen et al. ([1994]) discovered a wide range of submarine landslide at the outer continental shelf and upper continental slope of NSCS, at the depth of about 180-650 m.
The inversion is based on the assumption that the spatial range of the landslide should be small compared with the distance between the seismic stations and the event, since the method treats the landslide seismic source as a time-varying point force.
Red lines with arrows depict the path of the landslide; gray solid lines depict the spatial ranges of the landslide area; gray dashed lines depict Zones I V; the three stages recognized from estimated source time functions are also depicted using semi-transparent yellow arrows.
Peat has distinct geotechnical properties that influence its stability and govern the range of impacts of landslide events.
A total of 36 seismic stations are deployed by the China Earthquake Networks Centers CENCC) within the 400 km range of the Wulong landslide, and their locations are shown in Fig. 2.
The range of hazards related to landslide dams in the Qiaojia area will soon be supplemented.
Soil erosion processes and a range of natural hazards particularly landslides that transpire in mountain landscapes have been invoked in support of the unsustainable and non-resilient paradigm.
This specific sediment yield ranks among the top 20% globally, while the intensity-duration curve of the rainstorm is similarly in the upper percentile range of storms that had triggered landslides.
Statistical analysis reveals a significant correlation (r = 0.55; p < 0.001) between total landslide volume and mean annual precipitation, with 98% of landslide volume occurring along the windward, high-precipitation side of the range during the 25-year interval.
Each thematic layer were given weight ranging from 0 to 10 depending upon the degree of their effect for the occurrence of landslide.
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