The Camporaghena landslide, situated in the Northern Apennines, is a typical example of complex landslide in a high seismicity area. The hillslope stability is controlled by climatic, geological, morphological, structural and geotechnical factors; results of static, pseudostatic and dynamic stability analyses are presented and discussed.

  • INTRODUCTION

  • GEOLOGIC AND CLIMATIC OUTLINES

  • GEOTECHNICAL / GEOMECHANICAL PROPERTIES

  • SEISMIC STUDY

  • STABILITY ANALYSES

  • DISCUSSION

  • REFERENCES

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