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The document describes the process of cliff collapse in three steps: soft, impermeable clay cliffs hold rainwater which saturates the clay while the base of the cliff is eroded by the sea, forming a notch; the saturated clay develops a slip plane under the weight of the cliff material; and the cliff then slumps or collapses as a result. It then provides background details on a case study of cliff collapse along the Holderness Coast, noting the area contains high chalk cliffs that are more resistant to erosion than the surrounding boulder clay cliffs.










