Geomorphological assessment as basic complement of InSAR analysis for landslide processes understanding
Landslide research has benefited greatly from advances in remote sensing techniques. However, the recent increase in available data on land surface movement provided by InSAR techniques can lead to identifying only those areas that were active during data acquisition as hazardous, overlooking other...
Gespeichert in:
Veröffentlicht in: | Landslides 2024-06, Vol.21 (6), p.1273-1292 |
---|---|
Hauptverfasser: | , , , , , , , , |
Format: | Artikel |
Sprache: | eng |
Schlagworte: | |
Online-Zugang: | Volltext |
Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
container_end_page | 1292 |
---|---|
container_issue | 6 |
container_start_page | 1273 |
container_title | Landslides |
container_volume | 21 |
creator | Torre, Davide Galve, Jorge Pedro Reyes-Carmona, Cristina Alfonso-Jorde, David Ballesteros, Daniel Menichetti, Marco Piacentini, Daniela Troiani, Francesco Azañón, José Miguel |
description | Landslide research has benefited greatly from advances in remote sensing techniques. However, the recent increase in available data on land surface movement provided by InSAR techniques can lead to identifying only those areas that were active during data acquisition as hazardous, overlooking other potentially unsafe areas or neglecting landslide-specific geological settings in hazard assessments. Here, we present a case study that serves as a reminder for landslide researchers to carefully consider the geology and geomorphology of study areas where complex active movements are detected using InSAR technology. In an area extensively studied using InSAR and UAV-related techniques, we provide new insights by applying classical approaches. The area is the coastal stretch of La Herradura, and its importance lies in the fact that it has served as an illustrative example in the Product User Manual of the European Ground Motion Service, a platform that provides ground motion data on a European scale. Our approach is to revisit the area and carry out qualitative geological and geomorphological assessments supported by UAV surveys and GIS spatial analysis on a broader scale than previously published investigations. Our classical approach has yielded the following new observations, crucial for risk assessment and land management: active landslides identified by InSAR techniques since 2015 are bodies nested within large mass movements that affect entire slopes. A variety of processes contribute to slope dynamics, such as large slumps, marble rock spreading and block sliding, and surface rock falls and topples. The revised delineation of the landslide bodies reveals an area almost five times larger than previously mapped. These new findings in a well-known area highlight (1) the importance of updating and downscaling previous maps and (2) the ongoing importance of classical fieldwork and desk studies as basic complements to modern InSAR analyses. |
doi_str_mv | 10.1007/s10346-024-02216-w |
format | Article |
fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_journals_3053347140</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>3053347140</sourcerecordid><originalsourceid>FETCH-LOGICAL-a337t-923539722a33132c9ac5f17d4db0d746f605b9c985254e9d5cdab505d6edf2c53</originalsourceid><addsrcrecordid>eNp9UFtLwzAYDaLgnP4BnwI-V3Np2uVxDN0GA8EL-BbSJK0dbVPzdYz9e7NV9M2Hj-92zuFwELql5J4Skj8AJTzNEsLSWIxmyf4MTWhGWSIonZ3_zuTjEl0BbAlhknA5QdXS-daH_tM3vqqNbrAGcACt64Y44kJDbbDxbd-4082XeN29zl-w7nRzgBpw6QNudGehqa3DffDGHSXwrrMuwBA_dVddo4tSN-BufvoUvT89vi1WyeZ5uV7MN4nmPB8SybjgMmcsrpQzI7URJc1tagti8zQrMyIKaeRMMJE6aYWxuhBE2MzZkhnBp-hu1I0-vnYOBrX1uxCtguJEcJ7mNCURxUaUCR4guFL1oW51OChK1DFQNQaqYqDqFKjaRxIfSRDBXeXCn_Q_rG_bTnrk</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>3053347140</pqid></control><display><type>article</type><title>Geomorphological assessment as basic complement of InSAR analysis for landslide processes understanding</title><source>SpringerLink Journals</source><creator>Torre, Davide ; Galve, Jorge Pedro ; Reyes-Carmona, Cristina ; Alfonso-Jorde, David ; Ballesteros, Daniel ; Menichetti, Marco ; Piacentini, Daniela ; Troiani, Francesco ; Azañón, José Miguel</creator><creatorcontrib>Torre, Davide ; Galve, Jorge Pedro ; Reyes-Carmona, Cristina ; Alfonso-Jorde, David ; Ballesteros, Daniel ; Menichetti, Marco ; Piacentini, Daniela ; Troiani, Francesco ; Azañón, José Miguel</creatorcontrib><description>Landslide research has benefited greatly from advances in remote sensing techniques. However, the recent increase in available data on land surface movement provided by InSAR techniques can lead to identifying only those areas that were active during data acquisition as hazardous, overlooking other potentially unsafe areas or neglecting landslide-specific geological settings in hazard assessments. Here, we present a case study that serves as a reminder for landslide researchers to carefully consider the geology and geomorphology of study areas where complex active movements are detected using InSAR technology. In an area extensively studied using InSAR and UAV-related techniques, we provide new insights by applying classical approaches. The area is the coastal stretch of La Herradura, and its importance lies in the fact that it has served as an illustrative example in the Product User Manual of the European Ground Motion Service, a platform that provides ground motion data on a European scale. Our approach is to revisit the area and carry out qualitative geological and geomorphological assessments supported by UAV surveys and GIS spatial analysis on a broader scale than previously published investigations. Our classical approach has yielded the following new observations, crucial for risk assessment and land management: active landslides identified by InSAR techniques since 2015 are bodies nested within large mass movements that affect entire slopes. A variety of processes contribute to slope dynamics, such as large slumps, marble rock spreading and block sliding, and surface rock falls and topples. The revised delineation of the landslide bodies reveals an area almost five times larger than previously mapped. These new findings in a well-known area highlight (1) the importance of updating and downscaling previous maps and (2) the ongoing importance of classical fieldwork and desk studies as basic complements to modern InSAR analyses.</description><identifier>ISSN: 1612-510X</identifier><identifier>EISSN: 1612-5118</identifier><identifier>DOI: 10.1007/s10346-024-02216-w</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>Aerial surveys ; Agriculture ; Civil Engineering ; Data acquisition ; Earth and Environmental Science ; Earth Sciences ; Fieldwork ; Geographical information systems ; Geography ; Geological surveys ; Geology ; Geomorphology ; Ground motion ; Hazard assessment ; Land management ; Landslides ; Landslides & mudslides ; Natural Hazards ; Original Paper ; Remote sensing ; Remote sensing techniques ; Risk assessment ; Rock falls ; Rocks ; Sensing techniques ; Slump structures ; Spatial analysis ; Synthetic aperture radar interferometry</subject><ispartof>Landslides, 2024-06, Vol.21 (6), p.1273-1292</ispartof><rights>The Author(s) 2024</rights><rights>The Author(s) 2024. This work is published under http://creativecommons.org/licenses/by/4.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-a337t-923539722a33132c9ac5f17d4db0d746f605b9c985254e9d5cdab505d6edf2c53</cites><orcidid>0000-0002-8325-4350 ; 0000-0001-8880-975X ; 0000-0002-5235-3882 ; 0000-0001-5780-821X ; 0000-0003-2901-0715 ; 0000-0002-2703-7730 ; 0000-0002-4554-1332 ; 0000-0001-7834-5816 ; 0000-0001-5642-4767</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s10346-024-02216-w$$EPDF$$P50$$Gspringer$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s10346-024-02216-w$$EHTML$$P50$$Gspringer$$Hfree_for_read</linktohtml><link.rule.ids>314,780,784,27924,27925,41488,42557,51319</link.rule.ids></links><search><creatorcontrib>Torre, Davide</creatorcontrib><creatorcontrib>Galve, Jorge Pedro</creatorcontrib><creatorcontrib>Reyes-Carmona, Cristina</creatorcontrib><creatorcontrib>Alfonso-Jorde, David</creatorcontrib><creatorcontrib>Ballesteros, Daniel</creatorcontrib><creatorcontrib>Menichetti, Marco</creatorcontrib><creatorcontrib>Piacentini, Daniela</creatorcontrib><creatorcontrib>Troiani, Francesco</creatorcontrib><creatorcontrib>Azañón, José Miguel</creatorcontrib><title>Geomorphological assessment as basic complement of InSAR analysis for landslide processes understanding</title><title>Landslides</title><addtitle>Landslides</addtitle><description>Landslide research has benefited greatly from advances in remote sensing techniques. However, the recent increase in available data on land surface movement provided by InSAR techniques can lead to identifying only those areas that were active during data acquisition as hazardous, overlooking other potentially unsafe areas or neglecting landslide-specific geological settings in hazard assessments. Here, we present a case study that serves as a reminder for landslide researchers to carefully consider the geology and geomorphology of study areas where complex active movements are detected using InSAR technology. In an area extensively studied using InSAR and UAV-related techniques, we provide new insights by applying classical approaches. The area is the coastal stretch of La Herradura, and its importance lies in the fact that it has served as an illustrative example in the Product User Manual of the European Ground Motion Service, a platform that provides ground motion data on a European scale. Our approach is to revisit the area and carry out qualitative geological and geomorphological assessments supported by UAV surveys and GIS spatial analysis on a broader scale than previously published investigations. Our classical approach has yielded the following new observations, crucial for risk assessment and land management: active landslides identified by InSAR techniques since 2015 are bodies nested within large mass movements that affect entire slopes. A variety of processes contribute to slope dynamics, such as large slumps, marble rock spreading and block sliding, and surface rock falls and topples. The revised delineation of the landslide bodies reveals an area almost five times larger than previously mapped. These new findings in a well-known area highlight (1) the importance of updating and downscaling previous maps and (2) the ongoing importance of classical fieldwork and desk studies as basic complements to modern InSAR analyses.</description><subject>Aerial surveys</subject><subject>Agriculture</subject><subject>Civil Engineering</subject><subject>Data acquisition</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Fieldwork</subject><subject>Geographical information systems</subject><subject>Geography</subject><subject>Geological surveys</subject><subject>Geology</subject><subject>Geomorphology</subject><subject>Ground motion</subject><subject>Hazard assessment</subject><subject>Land management</subject><subject>Landslides</subject><subject>Landslides & mudslides</subject><subject>Natural Hazards</subject><subject>Original Paper</subject><subject>Remote sensing</subject><subject>Remote sensing techniques</subject><subject>Risk assessment</subject><subject>Rock falls</subject><subject>Rocks</subject><subject>Sensing techniques</subject><subject>Slump structures</subject><subject>Spatial analysis</subject><subject>Synthetic aperture radar interferometry</subject><issn>1612-510X</issn><issn>1612-5118</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2024</creationdate><recordtype>article</recordtype><sourceid>C6C</sourceid><recordid>eNp9UFtLwzAYDaLgnP4BnwI-V3Np2uVxDN0GA8EL-BbSJK0dbVPzdYz9e7NV9M2Hj-92zuFwELql5J4Skj8AJTzNEsLSWIxmyf4MTWhGWSIonZ3_zuTjEl0BbAlhknA5QdXS-daH_tM3vqqNbrAGcACt64Y44kJDbbDxbd-4082XeN29zl-w7nRzgBpw6QNudGehqa3DffDGHSXwrrMuwBA_dVddo4tSN-BufvoUvT89vi1WyeZ5uV7MN4nmPB8SybjgMmcsrpQzI7URJc1tagti8zQrMyIKaeRMMJE6aYWxuhBE2MzZkhnBp-hu1I0-vnYOBrX1uxCtguJEcJ7mNCURxUaUCR4guFL1oW51OChK1DFQNQaqYqDqFKjaRxIfSRDBXeXCn_Q_rG_bTnrk</recordid><startdate>20240601</startdate><enddate>20240601</enddate><creator>Torre, Davide</creator><creator>Galve, Jorge Pedro</creator><creator>Reyes-Carmona, Cristina</creator><creator>Alfonso-Jorde, David</creator><creator>Ballesteros, Daniel</creator><creator>Menichetti, Marco</creator><creator>Piacentini, Daniela</creator><creator>Troiani, Francesco</creator><creator>Azañón, José Miguel</creator><general>Springer Berlin Heidelberg</general><general>Springer Nature B.V</general><scope>C6C</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>7UA</scope><scope>8FD</scope><scope>C1K</scope><scope>F1W</scope><scope>FR3</scope><scope>H96</scope><scope>KL.</scope><scope>KR7</scope><scope>L.G</scope><orcidid>https://orcid.org/0000-0002-8325-4350</orcidid><orcidid>https://orcid.org/0000-0001-8880-975X</orcidid><orcidid>https://orcid.org/0000-0002-5235-3882</orcidid><orcidid>https://orcid.org/0000-0001-5780-821X</orcidid><orcidid>https://orcid.org/0000-0003-2901-0715</orcidid><orcidid>https://orcid.org/0000-0002-2703-7730</orcidid><orcidid>https://orcid.org/0000-0002-4554-1332</orcidid><orcidid>https://orcid.org/0000-0001-7834-5816</orcidid><orcidid>https://orcid.org/0000-0001-5642-4767</orcidid></search><sort><creationdate>20240601</creationdate><title>Geomorphological assessment as basic complement of InSAR analysis for landslide processes understanding</title><author>Torre, Davide ; Galve, Jorge Pedro ; Reyes-Carmona, Cristina ; Alfonso-Jorde, David ; Ballesteros, Daniel ; Menichetti, Marco ; Piacentini, Daniela ; Troiani, Francesco ; Azañón, José Miguel</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a337t-923539722a33132c9ac5f17d4db0d746f605b9c985254e9d5cdab505d6edf2c53</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2024</creationdate><topic>Aerial surveys</topic><topic>Agriculture</topic><topic>Civil Engineering</topic><topic>Data acquisition</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Fieldwork</topic><topic>Geographical information systems</topic><topic>Geography</topic><topic>Geological surveys</topic><topic>Geology</topic><topic>Geomorphology</topic><topic>Ground motion</topic><topic>Hazard assessment</topic><topic>Land management</topic><topic>Landslides</topic><topic>Landslides & mudslides</topic><topic>Natural Hazards</topic><topic>Original Paper</topic><topic>Remote sensing</topic><topic>Remote sensing techniques</topic><topic>Risk assessment</topic><topic>Rock falls</topic><topic>Rocks</topic><topic>Sensing techniques</topic><topic>Slump structures</topic><topic>Spatial analysis</topic><topic>Synthetic aperture radar interferometry</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Torre, Davide</creatorcontrib><creatorcontrib>Galve, Jorge Pedro</creatorcontrib><creatorcontrib>Reyes-Carmona, Cristina</creatorcontrib><creatorcontrib>Alfonso-Jorde, David</creatorcontrib><creatorcontrib>Ballesteros, Daniel</creatorcontrib><creatorcontrib>Menichetti, Marco</creatorcontrib><creatorcontrib>Piacentini, Daniela</creatorcontrib><creatorcontrib>Troiani, Francesco</creatorcontrib><creatorcontrib>Azañón, José Miguel</creatorcontrib><collection>Springer Nature OA Free Journals</collection><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Technology Research Database</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Landslides</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Torre, Davide</au><au>Galve, Jorge Pedro</au><au>Reyes-Carmona, Cristina</au><au>Alfonso-Jorde, David</au><au>Ballesteros, Daniel</au><au>Menichetti, Marco</au><au>Piacentini, Daniela</au><au>Troiani, Francesco</au><au>Azañón, José Miguel</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Geomorphological assessment as basic complement of InSAR analysis for landslide processes understanding</atitle><jtitle>Landslides</jtitle><stitle>Landslides</stitle><date>2024-06-01</date><risdate>2024</risdate><volume>21</volume><issue>6</issue><spage>1273</spage><epage>1292</epage><pages>1273-1292</pages><issn>1612-510X</issn><eissn>1612-5118</eissn><abstract>Landslide research has benefited greatly from advances in remote sensing techniques. However, the recent increase in available data on land surface movement provided by InSAR techniques can lead to identifying only those areas that were active during data acquisition as hazardous, overlooking other potentially unsafe areas or neglecting landslide-specific geological settings in hazard assessments. Here, we present a case study that serves as a reminder for landslide researchers to carefully consider the geology and geomorphology of study areas where complex active movements are detected using InSAR technology. In an area extensively studied using InSAR and UAV-related techniques, we provide new insights by applying classical approaches. The area is the coastal stretch of La Herradura, and its importance lies in the fact that it has served as an illustrative example in the Product User Manual of the European Ground Motion Service, a platform that provides ground motion data on a European scale. Our approach is to revisit the area and carry out qualitative geological and geomorphological assessments supported by UAV surveys and GIS spatial analysis on a broader scale than previously published investigations. Our classical approach has yielded the following new observations, crucial for risk assessment and land management: active landslides identified by InSAR techniques since 2015 are bodies nested within large mass movements that affect entire slopes. A variety of processes contribute to slope dynamics, such as large slumps, marble rock spreading and block sliding, and surface rock falls and topples. The revised delineation of the landslide bodies reveals an area almost five times larger than previously mapped. These new findings in a well-known area highlight (1) the importance of updating and downscaling previous maps and (2) the ongoing importance of classical fieldwork and desk studies as basic complements to modern InSAR analyses.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/s10346-024-02216-w</doi><tpages>20</tpages><orcidid>https://orcid.org/0000-0002-8325-4350</orcidid><orcidid>https://orcid.org/0000-0001-8880-975X</orcidid><orcidid>https://orcid.org/0000-0002-5235-3882</orcidid><orcidid>https://orcid.org/0000-0001-5780-821X</orcidid><orcidid>https://orcid.org/0000-0003-2901-0715</orcidid><orcidid>https://orcid.org/0000-0002-2703-7730</orcidid><orcidid>https://orcid.org/0000-0002-4554-1332</orcidid><orcidid>https://orcid.org/0000-0001-7834-5816</orcidid><orcidid>https://orcid.org/0000-0001-5642-4767</orcidid><oa>free_for_read</oa></addata></record> |
fulltext | fulltext |
identifier | ISSN: 1612-510X |
ispartof | Landslides, 2024-06, Vol.21 (6), p.1273-1292 |
issn | 1612-510X 1612-5118 |
language | eng |
recordid | cdi_proquest_journals_3053347140 |
source | SpringerLink Journals |
subjects | Aerial surveys Agriculture Civil Engineering Data acquisition Earth and Environmental Science Earth Sciences Fieldwork Geographical information systems Geography Geological surveys Geology Geomorphology Ground motion Hazard assessment Land management Landslides Landslides & mudslides Natural Hazards Original Paper Remote sensing Remote sensing techniques Risk assessment Rock falls Rocks Sensing techniques Slump structures Spatial analysis Synthetic aperture radar interferometry |
title | Geomorphological assessment as basic complement of InSAR analysis for landslide processes understanding |
url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2024-12-24T02%3A58%3A53IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Geomorphological%20assessment%20as%20basic%20complement%20of%20InSAR%20analysis%20for%20landslide%20processes%20understanding&rft.jtitle=Landslides&rft.au=Torre,%20Davide&rft.date=2024-06-01&rft.volume=21&rft.issue=6&rft.spage=1273&rft.epage=1292&rft.pages=1273-1292&rft.issn=1612-510X&rft.eissn=1612-5118&rft_id=info:doi/10.1007/s10346-024-02216-w&rft_dat=%3Cproquest_cross%3E3053347140%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=3053347140&rft_id=info:pmid/&rfr_iscdi=true |