Rainfall induced landslides in December 2004 in south-western Umbria, central Italy: types, extent, damage and risk assessment

The autumn of 2004 was particularly wet in Umbria, with cumulative rainfall in the period from October to December exceeding 600 mm. On 4–6 December and on 25–27 December 2004, two storms hit the Umbria Region producing numerous landslides, which were abundant near the town of Or...

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Main Authors: M. Cardinali, M. Galli, F. Guzzetti, F. Ardizzone, P. Reichenbach, P. Bartoccini
Format: Article
Language:English
Published: Copernicus Publications 2006-01-01
Series:Natural Hazards and Earth System Sciences
Online Access:http://www.nat-hazards-earth-syst-sci.net/6/237/2006/nhess-6-237-2006.pdf
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spelling doaj-7bf0979d86eb494d8a2fc4fa8784dd282020-11-25T00:47:53ZengCopernicus PublicationsNatural Hazards and Earth System Sciences1561-86331684-99812006-01-0162237260Rainfall induced landslides in December 2004 in south-western Umbria, central Italy: types, extent, damage and risk assessmentM. CardinaliM. GalliF. GuzzettiF. ArdizzoneP. ReichenbachP. BartocciniThe autumn of 2004 was particularly wet in Umbria, with cumulative rainfall in the period from October to December exceeding 600 mm. On 4–6 December and on 25–27 December 2004, two storms hit the Umbria Region producing numerous landslides, which were abundant near the town of Orvieto where they affected volcanic deposits and marine sediments. In this work, we document the type and abundance of the rainfall-induced landslides in the Orvieto area, in south-western Umbria, we study the rainfall conditions that triggered the landslides, including the timing of the slope failures, we determine the geotechnical properties of the failed volcanic materials, and we discuss the type and extent of damage produced by the landslides. We then use the recent event landslide information to test a geomorphological assessment of landslide hazards and risk prepared for the village of Sugano, in the Orvieto area. Based on the results of the test, we update the existing landslide hazards and risk scenario for extremely rapid landslides, mostly rock falls, and we introduce a new landslide scenario for rapid and very rapid landslides, including soil slides, debris flows and debris avalanches.http://www.nat-hazards-earth-syst-sci.net/6/237/2006/nhess-6-237-2006.pdf
collection DOAJ
language English
format Article
sources DOAJ
author M. Cardinali
M. Galli
F. Guzzetti
F. Ardizzone
P. Reichenbach
P. Bartoccini
spellingShingle M. Cardinali
M. Galli
F. Guzzetti
F. Ardizzone
P. Reichenbach
P. Bartoccini
Rainfall induced landslides in December 2004 in south-western Umbria, central Italy: types, extent, damage and risk assessment
Natural Hazards and Earth System Sciences
author_facet M. Cardinali
M. Galli
F. Guzzetti
F. Ardizzone
P. Reichenbach
P. Bartoccini
author_sort M. Cardinali
title Rainfall induced landslides in December 2004 in south-western Umbria, central Italy: types, extent, damage and risk assessment
title_short Rainfall induced landslides in December 2004 in south-western Umbria, central Italy: types, extent, damage and risk assessment
title_full Rainfall induced landslides in December 2004 in south-western Umbria, central Italy: types, extent, damage and risk assessment
title_fullStr Rainfall induced landslides in December 2004 in south-western Umbria, central Italy: types, extent, damage and risk assessment
title_full_unstemmed Rainfall induced landslides in December 2004 in south-western Umbria, central Italy: types, extent, damage and risk assessment
title_sort rainfall induced landslides in december 2004 in south-western umbria, central italy: types, extent, damage and risk assessment
publisher Copernicus Publications
series Natural Hazards and Earth System Sciences
issn 1561-8633
1684-9981
publishDate 2006-01-01
description The autumn of 2004 was particularly wet in Umbria, with cumulative rainfall in the period from October to December exceeding 600 mm. On 4–6 December and on 25–27 December 2004, two storms hit the Umbria Region producing numerous landslides, which were abundant near the town of Orvieto where they affected volcanic deposits and marine sediments. In this work, we document the type and abundance of the rainfall-induced landslides in the Orvieto area, in south-western Umbria, we study the rainfall conditions that triggered the landslides, including the timing of the slope failures, we determine the geotechnical properties of the failed volcanic materials, and we discuss the type and extent of damage produced by the landslides. We then use the recent event landslide information to test a geomorphological assessment of landslide hazards and risk prepared for the village of Sugano, in the Orvieto area. Based on the results of the test, we update the existing landslide hazards and risk scenario for extremely rapid landslides, mostly rock falls, and we introduce a new landslide scenario for rapid and very rapid landslides, including soil slides, debris flows and debris avalanches.
url http://www.nat-hazards-earth-syst-sci.net/6/237/2006/nhess-6-237-2006.pdf
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