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Fig. 1 | Earth, Planets and Space

Fig. 1

From: Relationship between pressure variations at the ocean bottom and the acceleration of its motion during a submarine earthquake

Fig. 1

Relief of ocean bottom in installation region of DONET observatories. The radii of circular marks at each station equal 1, 2 and 3 ocean depths at the installation points of the stations. The distribution of depths (isolines in steps of 100 m) and the absolute value of the depth gradient (color scale) are shown in the map in accordance with JODC-Expert Grid data for geography (J-EGG500). The absolute value of the ocean depth gradient (bottom slope) is shown in accordance with the color scale at the bottom of the figure

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