Fig. 5From: Paleotsunami history of Hachinohe, northern Japan: a multiproxy analysis and numerical modeling approachMagnetic susceptibility landward changes along with the core samples H02, H03, H04, and H06. Note that it is a graphic representation of the MS intensity only in the sand layers, and the thickness of the sand layers is not at scale. MS values of the mud layers were not plottedBack to article page