Consequence of the morphological changes that took place in the High Khonsu bank during the perihelion passage. (a) May 2, 2015, UTC 15:09 (F41-F23-F24); (b) August 1, 2015, UTC 08:00 (F22); (c) and January 1, 2016, UTC 01:48 (F41-F23-F24). Description: (a) Landmark F1 (retreating wall) and the two 20-m-sized boulders near an ancient cliff collapseobserved at better illumination conditions. (b) The High bank observed from an S/C distance of 215 km. Landmark F1 is still observable, and no deformation (yellow line) of the equatorial cliff is detected. (c) Jumping boulder 2 under better illumination conditions. F1 has vanished, and two 20-m-sized boulders are now found to have fallen onto the deposit. Deformation caused by jumping boulder 2 is marked by a yellow line.