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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/564
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dc.contributor.authorallMora, P.; Dip. Scienze della Terra e Geologico-Ambientali, Universita` di Bologna, Via Zamboni 67, 40127 Bologna, Italyen
dc.contributor.authorallBaldi, P.; Dip. Fisica, Settore Geofisica, Universita` Bologna, Via C. Berti Pichat 8, 40127 Bologna, Italyen
dc.contributor.authorallCasula, G.; Istituto Nazionale Geofisica e Vulcanologia, Via di Vigna Murata 605, 00143 Rome, Italyen
dc.contributor.authorallFabris, M.; DAUR, Universita` di Padova, Via Marzolo 9, 35131 Padoua, Italyen
dc.contributor.authorallGhirotti, M.; Dip. Scienze della Terra e Geologico-Ambientali, Universita` di Bologna, Via Zamboni 67, 40127 Bologna, Italyen
dc.contributor.authorallMazzini, E.; Regione Emilia-Romagna, V.le Silvani 6, 40122 Bologna, Italyen
dc.contributor.authorallPesci, A.; Istituto Nazionale Geofisica e Vulcanologia, Via di Vigna Murata 605, 00143 Rome, Italyen
dc.date.accessioned2005-11-24T14:45:18Zen
dc.date.available2005-11-24T14:45:18Zen
dc.date.issued2003en
dc.identifier.urihttp://hdl.handle.net/2122/564en
dc.description.abstractAbstract A combination of digital photogrammetry and Global Positioning Systems (GPS) surveying has been used to measure landslide surface displacements and to estimate the volume involved in the movement. Ninety-eight percent of landslides mapped as active in the Emilia-Romagna region of northern Italy are reactivations of dormant mass movements. The Ca’ di Malta landslide, south of Bologna, was chosen to test this integrated system. A 0.5-m cellsize Digital Elevation Model (DEM) with vertical accuracy of 0.1 m was generated using digital photogrammetric techniques. We have used a combination of digital photogrammetry and three GPS techniques to monitor landslide movement. Rapid static surveying in which the survey observations are made for a period of minutes yielded sub-centimetre positions for several marked points distributed on a longitudinal axis along the landslide. Kinematic surveying, in which the observations are carried out continuously, in this case by a walking person, provided models of the surface (1 1 m grid) by measuring the position of irregularly distributed points. Continuous observations over 7 months were made between two GPS receivers. One positioned within the moving landslide body and the other at a fixed location outside the landslide. An automatic procedure was developed to download, process and compute relative movement at constant time intervals. The accuracy achieved with the GPS measurements ranges between several millimetres to a few centimetres for static and kinematic observations, respectively. This integrated survey technique is a cost-effective method that could be applied to other structural and morphological settings. The real-time monitoring could be coupled with a warning system for landslide hazard management and the repeated kinematic GPS surveys derive precise DEMs of a landslide, providing information on geometry, volumes and evolution of the phenomenon.en
dc.format.extent1219006 bytesen
dc.format.mimetypeapplication/pdfen
dc.language.isoEnglishen
dc.relation.ispartofEngineering Geologyen
dc.relation.ispartofseries/68(2003)en
dc.subjectGPSen
dc.subjectReal-time monitoring; DEM;en
dc.titleGlobal Positioning Systems and digital photogrammetry for the monitoring of mass movements:application to the Ca’ di Malta landslide (northern Apennines, Italy)en
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber(103-121)en
dc.subject.INGV04. Solid Earth::04.07. Tectonophysics::04.07.99. General or miscellaneousen
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dc.description.fulltextreserveden
dc.contributor.authorMora, P.en
dc.contributor.authorBaldi, P.en
dc.contributor.authorCasula, G.en
dc.contributor.authorFabris, M.en
dc.contributor.authorGhirotti, M.en
dc.contributor.authorMazzini, E.en
dc.contributor.authorPesci, A.en
dc.contributor.departmentDip. Scienze della Terra e Geologico-Ambientali, Universita` di Bologna, Via Zamboni 67, 40127 Bologna, Italyen
dc.contributor.departmentDip. Fisica, Settore Geofisica, Universita` Bologna, Via C. Berti Pichat 8, 40127 Bologna, Italyen
dc.contributor.departmentIstituto Nazionale Geofisica e Vulcanologia, Via di Vigna Murata 605, 00143 Rome, Italyen
dc.contributor.departmentDAUR, Universita` di Padova, Via Marzolo 9, 35131 Padoua, Italyen
dc.contributor.departmentDip. Scienze della Terra e Geologico-Ambientali, Universita` di Bologna, Via Zamboni 67, 40127 Bologna, Italyen
dc.contributor.departmentRegione Emilia-Romagna, V.le Silvani 6, 40122 Bologna, Italyen
dc.contributor.departmentIstituto Nazionale Geofisica e Vulcanologia, Via di Vigna Murata 605, 00143 Rome, Italyen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptDipartimento di Scienze della Terra e Geologico-Ambientali – University of Bologna (Italy-
crisitem.author.deptUniversità di Bologna, Dipartimento di Fisica, Settore Geofisica.-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Bologna, Bologna, Italia-
crisitem.author.deptDip. Scienze della Terra e Geologico-Ambientali, Universita` di Bologna, Via Zamboni 67, 40127 Bologna, Italy-
crisitem.author.deptRegione Emilia-Romagna, V.le Silvani 6, 40122 Bologna, Italy-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Bologna, Bologna, Italia-
crisitem.author.orcid0000-0001-7934-2019-
crisitem.author.orcid0000-0003-1863-3132-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
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