The Shanklin cliffs are a fine example of soft rock cliffs protected from marine erosion but still subject to degradational activity albeit at a slow rate. Past development in the area has discounted the long-term evolutionary consequences of the slope movements, especially in respect of the outgrowth of the talus slope. The resulting planning and engineering problems will be relevant to other cases of protected soft rock cliffs in urban areas.

  • INTRODUCTION

  • SLOPE MOVEMENTS

  • THE CLIFF FACE AND FALL ADJACENT TO THE LIFT SHAFT (1987)

  • THE BURIED ROCKFACE

  • THE LONG-TERM EVOLUTION OF THE SHANKLIN CLIFF AND TALUS SLOPE

  • PLANNING AND ENGINEERING ASPECTS

  • CONCLUSIONS

  • ACKNOWLEDGEMENTS

  • REFERENCES

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