Fig. 3From: Temporal changes in the internal stresses and pore pressures in a large-scale submarine mass transport depositPhotograph of the fault observed in the coastal outcrop of the Akkeshi Formation (modified from Naruse and Otsubo 2011a). A minor deformed structure of beddings at the right end of the fault and the fact that the fault does not continue to the external matrix indicate that this fault is syn-sedimentary origin. The white circle shows a scale (1Â m)Back to article page