Fig. 8From: Unified approach for evaluation of horizontal site amplification factors with special reference to history of studies on the effects of surface geology on seismic motionObserved seismograms during the foreshock of the 1930 Kita-Izu earthquake of M7.3 at the University of Tokyo (after Imamura 1931). Mainshock records were all off-scale. We can see a very prominent phase of surface waves in the later part (from about 4 times the S-P time), especially in the NS componentBack to article page