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- W2022977535 abstract "Details are presented of a double undercliff, an unusual landform feature on the coast of Southeast Devon. The double undercliff is the result of two separate landslides on argillaceous formations within the 127 m high cliffs. The upper undercliff is probably of great antiquity, whereas the lower undercliff formed as recently as 1969. The double undercliff dies out as the lower argillaceous formation dips below sea level, to the east, and is faulted out to the west. The stability of the slopes in each case depended on the shear strength of bedding laminations, and hence upon very low or zero cohesion. A back analysis suggests a mobilised angle of shearing resistance as low as 13°C for the lower undercliff. The future stability of the undercliffs is dependent mainly upon undrained crown loading, for the upper undercliff from the degradation of the backscar, and for the lower undercliff from the landslide above." @default.
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- W2022977535 date "1986-04-01" @default.
- W2022977535 modified "2023-10-14" @default.
- W2022977535 title "The form and stability of a double undercliff: An example from South-West England" @default.
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- W2022977535 doi "https://doi.org/10.1016/0013-7952(86)90023-2" @default.
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