Fig. 2From: Surface creep rate distribution along the Philippine fault, Leyte Island, and possible repeating of Mw ~ 6.5 earthquakes on an isolated locked patchHypocenters of the 1947 and 2017 earthquakes from the PHIVOLCS catalog (yellow stars), hypocenter of the 1947 earthquake relocated by Lumbang and Hurukawa (2014) (yellow-filled circle), and GCMT solution for the 2017 earthquake. Plotted together are Philippine fault traces (red lines), seismicity of shallower than 50 km in 2000–2017 (PHIVOLCS catalog, color dots), and scene areas of PALSAR data used for the creep analysisBack to article page