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Simple rules to minimise exposure to coseismic landslide hazard

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Figure

Figure 1. Schematic view of the different topographic metrics tested here. (a) Perspective view of a landscape with each cell shaded accordingto its local slope from light (steep) to dark (gentle)
Figure 2. SHALRUN-EQ hazard area calculations for a simplified (steepest flow path) example with an initiation angle of 40contributing area steeper than 40stopping angle of 10flow paths from cell to cell;◦ and a◦: (a) elevations from a 30 m resolution digital
Figure 3. Landslide hazard defined as conditional probability(c)slopes iniscontributing area normalised by the upslope contributing area of the inflection in average slope
Figure 4. Two-dimensional plots of landslide hazard defined as con-upslope contributing area per unit cell width
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