Slope instability in the Bastardo Basin (Umbria, Central Italy) – The landslide of Barattano

The Bastardo Basin is one of the classics Apenninic intermontane basins of central Italy. They are en-closed tectonic basins (graben and semigraben) with high anthropization, but with high vulnerability, too (seismic, hydrogeological and geomorphological).</p> <p style='line-heig...

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Main Authors: C. Cencetti, P. Conversini
Format: Article
Language:English
Published: Copernicus Publications 2003-01-01
Series:Natural Hazards and Earth System Sciences
Online Access:http://www.nat-hazards-earth-syst-sci.net/3/561/2003/nhess-3-561-2003.pdf
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author C. Cencetti
P. Conversini
author_facet C. Cencetti
P. Conversini
author_sort C. Cencetti
collection DOAJ
description The Bastardo Basin is one of the classics Apenninic intermontane basins of central Italy. They are en-closed tectonic basins (graben and semigraben) with high anthropization, but with high vulnerability, too (seismic, hydrogeological and geomorphological).</p> <p style='line-height: 20px;'>The paper concerns some aspects about slope instability in the Bastardo Basin as part of a wider research, which aims to actually define the characteristics of the liability to landslides of the Apenninic intermontane basins. In particular lithological, stratigraphical and hydrogeological conditions are analysed under which a landslide near village of Barattano has developed.</p> <p style='line-height: 20px;'>This mass movement, at different times, produced partial or total occlusion of the torrent Puglia. Here geognostic investigations together with laboratory tests and subsequent monitoring of landslide area were carried out.&nbsp;</p> <p style='line-height: 20px;'>A back analysis, based on limit equilibrium solutions for the factor of safety of the slope, provided the residual strenght properties of the soil mass along the sliding surface.&nbsp;&nbsp;</p> <p style='line-height: 20px;'>The landslide of Barattano is representative of a very frequent situation (in terms of type, factors and causes of the movement, possible development of the movement) not only within Bastardo Basin, but in general within Apenninic intermontane basins, too.&nbsp;</p> <p style='line-height: 20px;'>The study of landslide and the design of appropriate remedial measures are of great importance in terms of prevention and mitigation of geologic-hydraulic risk in Apenninic intermontane basins.
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spelling doaj.art-23329b72268143f6b0f44ce49533b76d2022-12-22T02:44:01ZengCopernicus PublicationsNatural Hazards and Earth System Sciences1561-86331684-99812003-01-0136561568Slope instability in the Bastardo Basin (Umbria, Central Italy) – The landslide of BarattanoC. CencettiP. ConversiniThe Bastardo Basin is one of the classics Apenninic intermontane basins of central Italy. They are en-closed tectonic basins (graben and semigraben) with high anthropization, but with high vulnerability, too (seismic, hydrogeological and geomorphological).</p> <p style='line-height: 20px;'>The paper concerns some aspects about slope instability in the Bastardo Basin as part of a wider research, which aims to actually define the characteristics of the liability to landslides of the Apenninic intermontane basins. In particular lithological, stratigraphical and hydrogeological conditions are analysed under which a landslide near village of Barattano has developed.</p> <p style='line-height: 20px;'>This mass movement, at different times, produced partial or total occlusion of the torrent Puglia. Here geognostic investigations together with laboratory tests and subsequent monitoring of landslide area were carried out.&nbsp;</p> <p style='line-height: 20px;'>A back analysis, based on limit equilibrium solutions for the factor of safety of the slope, provided the residual strenght properties of the soil mass along the sliding surface.&nbsp;&nbsp;</p> <p style='line-height: 20px;'>The landslide of Barattano is representative of a very frequent situation (in terms of type, factors and causes of the movement, possible development of the movement) not only within Bastardo Basin, but in general within Apenninic intermontane basins, too.&nbsp;</p> <p style='line-height: 20px;'>The study of landslide and the design of appropriate remedial measures are of great importance in terms of prevention and mitigation of geologic-hydraulic risk in Apenninic intermontane basins.http://www.nat-hazards-earth-syst-sci.net/3/561/2003/nhess-3-561-2003.pdf
spellingShingle C. Cencetti
P. Conversini
Slope instability in the Bastardo Basin (Umbria, Central Italy) – The landslide of Barattano
Natural Hazards and Earth System Sciences
title Slope instability in the Bastardo Basin (Umbria, Central Italy) – The landslide of Barattano
title_full Slope instability in the Bastardo Basin (Umbria, Central Italy) – The landslide of Barattano
title_fullStr Slope instability in the Bastardo Basin (Umbria, Central Italy) – The landslide of Barattano
title_full_unstemmed Slope instability in the Bastardo Basin (Umbria, Central Italy) – The landslide of Barattano
title_short Slope instability in the Bastardo Basin (Umbria, Central Italy) – The landslide of Barattano
title_sort slope instability in the bastardo basin umbria central italy the landslide of barattano
url http://www.nat-hazards-earth-syst-sci.net/3/561/2003/nhess-3-561-2003.pdf
work_keys_str_mv AT ccencetti slopeinstabilityinthebastardobasinumbriacentralitalythelandslideofbarattano
AT pconversini slopeinstabilityinthebastardobasinumbriacentralitalythelandslideofbarattano