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  5. A map for volcaniclastic debris flow hazards in Apennine areas surrounding the Vesuvius volcano (Italy)
 
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A map for volcaniclastic debris flow hazards in Apennine areas surrounding the Vesuvius volcano (Italy)

Author(s)
Bisson, M.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Pisa, Pisa, Italia  
Zanchetta, G.  
Dipartimento di Scienze della Terra, Università di Pisa  
Sulpizio, R.  
Dipartimento di Scienze della Terra e Geoambientali, Università di Bari  
Demi, F.  
Dipartimento di Scienze della Terra, Università di Pisa  
Language
English
Obiettivo Specifico
3V. Dinamiche e scenari eruttivi
4V. Vulcani e ambiente
Status
Published
JCR Journal
JCR Journal
Peer review journal
Yes
Journal
Journal of maps  
Issue/vol(year)
2/ 9 (2013)
ISSN
1744-5647
Electronic ISSN
1744-5647
Publisher
Kingston University
Pages (printed)
230-238
Date Issued
2013
DOI
10.1080/17445647.2013.768948
URI
https://www.earth-prints.org/handle/2122/9581
Subjects
04. Solid Earth::04.08. Volcanology::04.08.08. Volcanic risk  
Subjects

volcaniclastic debris...

Abstract
Volcaniclastic debris flows are dangerous natural phenomena that originate in volcanic areas not only during or shortly after an eruption but also during a period of volcanic quiescence,when heavy and/or persistent rains remobilize unconsolidated pyroclastic deposits. In Italy, one of the areas most affected by these phenomena is that of the Apennine Mountains which border the southern Campania Plain surrounding the Vesuvius volcano. Historical accounts record in these areas that more than 500 debris flow events occurred during the last five centuries. These events caused very dangerous consequences such as loss of life and serious damage to property. An example is the devastating event of Sarno of 5 May 1998 which caused the death of more than 150 people and considerable damage to villages
located at the foot of the Apennine Hills. In order to contribute to the assessment and
mitigation of the debris flow risk, we propose a zonation map that identifies the areas more
prone to generation and invasion by volcaniclastic flows. This map is based on field
investigations and morphometric analyses derived from a digital elevation model with
spatial resolution of 10 meters.
Type
article
File(s)
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Name

bisson et al JOM 2013.pdf

Size

512 KB

Format

Adobe PDF

Checksum (MD5)

859dba3e00e2cf0fac812318c3dfc08d

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