Fig. 3From: Surface creep rate distribution along the Philippine fault, Leyte Island, and possible repeating of Mw ~ 6.5 earthquakes on an isolated locked patcha Topography map of the Leyte Island, shown with the Philippine fault traces mapped by Tsutsumi and Perez (2013) (black) and a branched trace mapped by Prioul et al. (2000) (red). b Elevation profiles across the fault (Tsutsumi and Perez 2013) along selected lines shown in a. The location of each line corresponds to the center of the boxes shown in later figuresBack to article page