Fig. 6From: Shallow seismic reflection imaging of the Inabanga–Clarin portion of the North Bohol Fault, Central Visayas, Philippines(top) Topographic cross section and (bottom) interpreted CDP stacked section of the Caluwasan seismic line showing that the pressure ridge observed on the surface was caused by a flower structure in the subsurface. Vertical exaggeration for the topographic cross section is ×1, while the seismic profile has no vertical exaggerationBack to article page