Focal mechanism, epicenter, landslide distribution and line-of-sight (LOS) displacements measured from InSAR. Shallow slip occurs along a strike-slip fault ~2 km into the hanging-wall of the North Waziristan-Bannu Thrust Fault, along the sharp eastern margin of the red LOS displacements. Landslides (black and orange dots) are clustered around the ruptured fault. Map compiled by S. Valkanotis using data from the European Space Agency and showing focal mechanism and epicenter from GFZ (German Research Centre for Geosciences, Potsdam).