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A zone of high density landsliding (> 10% landslide surface area affected) stretches for ~ 240 km along the earthquake region, in proximity to the Yingxiu, Beichuan and Pennguan faults, which ruptured during the earthquake.
The landslide surface area A t ranges between 500 m2 and 3 km2, covering a total area of 8.1 km2, that is, 1/12th of the total studied area.
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As shown in Fig. 11b, these land subsidence areas are not included in the area of landslide surface deformation along the east and west riverbanks of the Bishnumati River.
Most of the landslides (12 coseismic cases are confirmed with a surface area of 1 10 ha) occurred during the earthquake or immediately after it, while only a few (namely 4) acted as post-seismic failures (24 h to 5 weeks).
This deformation cannot be explained by simple land subsidence; the lateral spread that caused the landslide surface deformation along the Bishnumati River was the same as that in the SE area of TIA.
Subtracting Fig. 9a from Fig. 8a, we obtained Fig. 10a for area C (i.e., the EW component of the resulting landslide surface deformation).
The exponent of the power law is >1, meaning that the mean depth is increasing with the surface area, which is in good agreement with previous observations (e.g., Larsen et al. 2010) and landslide models (Klar et al. 2011).
And 60percentt of the surface area downtown is surface parking.
Fig. 10 Landslide surface deformation by 2.5D analysis.
High surface area.
More surface area to contain the flood.
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