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<!DOCTYPE article SYSTEM "http://www.nat-hazards-earth-syst-sci.net/inc/nhess/copernicus.dtd">
<article language="en">
	<journal>
		<journal_title>Natural Hazards and Earth System Science</journal_title>
		<journal_url>www.nat-hazards-earth-syst-sci.net</journal_url>
		<issn>1561-8633</issn>
		<eissn>1684-9981</eissn>
		<volume_number>6</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2006</publication_year>
	</journal>
	<doi>10.5194/nhess-6-55-2006</doi>
	<article_url>http://www.nat-hazards-earth-syst-sci.net/6/55/2006/</article_url>
	<abstract_html>http://www.nat-hazards-earth-syst-sci.net/6/55/2006/nhess-6-55-2006.html</abstract_html>
	<fulltext_pdf>http://www.nat-hazards-earth-syst-sci.net/6/55/2006/nhess-6-55-2006.pdf</fulltext_pdf>
	<start_page>55</start_page>
	<end_page>61</end_page>
	<publication_date>2006-01-16</publication_date>
	<article_title content_type="html">Investigation and monitoring in support of the structural mitigation of large slow moving landslides: an example from Ca&apos; Lita (Northern Apennines, Reggio Emilia, Italy)</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>A. Corsini</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>L. Borgatti</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>G. Caputo</name>
		</author>
		<author numeration="4" affiliations="2">
			<name>N. De Simone</name>
		</author>
		<author numeration="5" affiliations="2">
			<name>G. Sartini</name>
		</author>
		<author numeration="6" affiliations="2">
			<name>G. Truffelli</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Dipartimento di Scienze della Terra, Università di Modena e Reggio Emilia, Largo S. Eufemia, 19, 41100 Modena, Italy</affiliation>
		<affiliation numeration="2" content_type="html">Regione Emilia Romagna, Servizio Tecnico Bacini Enza e sinistra Secchia, Via Emilia S. Stefano, 25, 42100 Reggio Emilia, Italy</affiliation>
	</affiliations>
	<abstract content_type="html">The Ca&apos; Lita landslide is a large and deep-seated mass movement located in
the Secchia River Valley, in the sector of the Northern Apennines falling
into Reggio Emilia Province, about 70 km west of Bologna (Northern Italy).
It consists of a composite landslide system that affects Cretaceous to
Eocene flysch rock masses and chaotic complexes. Many of the components
making up the landslide system have resumed activity between 2002 and 2004,
and are now threatening some hamlets and an important road serving the upper
watershed area of River Secchia, where many villages and key industrial
facilities are located.

&lt;P  style=&quot;line-height: 20px;&quot;&gt;
This paper presents the analysis and the quantification of displacement
rates and depths of the mass movements, based on geological and
geomorphological surveys, differential DEM analysis, interpretation of
underground stratigraphic and monitoring data collected during the
investigation campaign that has been undertaken in order to design
cost-effective mitigation structures, and that has been conducted with the
joint collaboration between public offices and research institutes.</abstract>
	<references>
	</references>
</article>

