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The size, area, depth of landslide and its distribution significantly varies from place to place.
The largest depth of Landslide S4 is 200 m, and the largest volume is 50 × 109 m3 (Table 1).
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Fig. 13 Changes in the length and depth of Saddle River landslide lake since formation in June 1990.
The depth of coseismic landslides was larger than the depth of the rainfall-induced landslides.
The depth of coseismic landslides ranged from 0.8 to 4.6 m, with an average of 1.5 m.
Indeed, of the three seed lots trialled through to year 4, none had developed more than ~4% of their total below-ground biomass, 16% of their total root length and 4.5% of their total root CSA (vertical roots only) below the typical 1-m failure depth of shallow landslides.
Rainfall-induced landslide data of the Chengdu Land Resources Bureau show that the depth of rainfall-induced landslide in Dujiangyan is generally about 1 m.
The average depth of the coseismic landslides was 1.5 m, which is deeper than the depth of the rainfall-induced landslides prior to these.
The depth of the coseismic landslides reached > 3.0 m, with an average of 1.5 m, which is larger than the rainfall-induced landslide depth.
The depths of shallow landslides in USA and Japan used for the validations process are in the range of 0.5 to 5 m, but characteristic depths are less than 2 m.
However, 36 landslides had depths > 1.0 m, which is larger than the depth of the rainfall-induced landslides (Fig. 4).
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com