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- W277797828 abstract "This work is based on a multi-scale experimental approach applied on the “Vence” landslide (South-eastern France, Mediterranean climate) which is characterised by a sandy-clay sliding mass of Lower Eocene. It is considered as a translational landslide including 1.2×10m of material. This landslide affects an inhabited area about 250 m large by 350 m long, with an average slope of 12 /14 . The present day landslide activity is underlined by a variety of failure surfaces appearing in the landscape morphology: tension cracks, scarps, disorders affecting human activity and particularly the deviation of the “Lubiane” river at the foot of the slope." @default.
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- W277797828 date "2010-05-01" @default.
- W277797828 modified "2023-09-23" @default.
- W277797828 title "A Stacked aquifer system controlling the Vence landslide site (French Alps) revealed by hydrogeophysical surveying" @default.
- W277797828 hasPublicationYear "2010" @default.
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