Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
8907901 | Geomorphology | 2018 | 55 Pages |
Abstract
Among principal outcomes is the recognition, by field observations, stratigraphic and inclinometer data as well as slope stability modelling, of a basal sheared and softened band, made chiefly of remoulded mudrocks, which constrains the current landslide failure surface. Such basal band can be considered an inherited landslide structure, formed during the original paroxysmal stage of the Lemeglio landslide, which controls the current residual kinematics of the landslide deposits throughout the foot, depending also on the coastal marine erosion acting along the landslide toe.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
A. Cevasco, F. Termini, R. Valentino, C. Meisina, R. Bonì, M. Bordoni, G.P. Chella, P. De Vita,