Fig. 5From: Investigation of the subsurface structure at the target site in Kumamoto, Japan, and the distributed data of the blind prediction exercise: report for the experiments for the 6th international symposium on effects of surface geology on seismic motionPS logging results performed for every 0.5 m in depth, for the whole 39 m compared with layering obtained from the boring log in the left side of the figure. Data of P- and S- wave velocities are presented in Table 2Back to article page