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University of Hull
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Erosion of the Holderness cliffs is a cyclic, four stage process:
- The soft Boulder Clay cliffs become saturated with rain water and lose their strength.
- The cliff is too steep and fails either as a block of material or as a slurry slide
- Cliff failure reduces the angle and prevents further erosion but …
- Large waves from the North East remove the debris in longshore drift to the South and the cliff oversteepens, rain falls and the cycle begins again.
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