A mountain slope deformation in an alpine metaophiolitic massif (Ligurian Alps, Italy)
Deep-seated gravitational slope deformation (DsGSD) represents a relevant geological-geomorphological feature of the landscape and has drawn scientific attention for the past several decades. During a detailed fieldwork in the Ligurian Alps, we identified areas (larger than ca 5 km2), characterized...
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| Veröffentlicht in: | Journal of maps 2021-06, Vol.17 (3), p.77-89 |
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| creator | Faccini, F. Federico, L. Torchio, S. Roccati, A. Capponi, G. Crispini, L. |
| description | Deep-seated gravitational slope deformation (DsGSD) represents a relevant geological-geomorphological feature of the landscape and has drawn scientific attention for the past several decades. During a detailed fieldwork in the Ligurian Alps, we identified areas (larger than ca 5 km2), characterized by very low percentage of outcrops, with rock blocks on the watershed and many morpho-tectonic evidences. Through the integration of geological-geomorphological mapping, structural data, photo interpretation, GIS-based analyses, we identified a number of typical DsGSDs. The example here described is one major complex-sagging-type DsGSD that is not present in national land planning and/or management databases but that is likely at the origin of the large-scale landslides which affected the villages of the area. This DsGSD is also located within the Beigua UNESCO Global Geopark, in an area of unique natural and historical value. This study once again highlights the importance of ground truth observations as the basis for further investigations. |
| doi_str_mv | 10.1080/17445647.2020.1854130 |
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During a detailed fieldwork in the Ligurian Alps, we identified areas (larger than ca 5 km2), characterized by very low percentage of outcrops, with rock blocks on the watershed and many morpho-tectonic evidences. Through the integration of geological-geomorphological mapping, structural data, photo interpretation, GIS-based analyses, we identified a number of typical DsGSDs. The example here described is one major complex-sagging-type DsGSD that is not present in national land planning and/or management databases but that is likely at the origin of the large-scale landslides which affected the villages of the area. This DsGSD is also located within the Beigua UNESCO Global Geopark, in an area of unique natural and historical value. This study once again highlights the importance of ground truth observations as the basis for further investigations.</description><identifier>ISSN: 1744-5647</identifier><identifier>EISSN: 1744-5647</identifier><identifier>DOI: 10.1080/17445647.2020.1854130</identifier><language>eng</language><publisher>Abingdon: Taylor & Francis</publisher><subject>Deformation ; field survey ; Fieldwork ; Geological mapping ; Geomorphology ; Gravity ; Landslides ; Ligurian Alps ; Massifs ; morpho-tectonic ; Mountain slope deformation ; Mountains ; ophiolites ; Outcrops ; Tectonics ; Voltri Massif</subject><ispartof>Journal of maps, 2021-06, Vol.17 (3), p.77-89</ispartof><rights>2020 The Author(s). Published by Informa UK Limited, trading as Taylor & Francis Group on behalf of Journal of Maps 2020</rights><rights>2020 The Author(s). Published by Informa UK Limited, trading as Taylor & Francis Group on behalf of Journal of Maps. 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| subjects | Deformation field survey Fieldwork Geological mapping Geomorphology Gravity Landslides Ligurian Alps Massifs morpho-tectonic Mountain slope deformation Mountains ophiolites Outcrops Tectonics Voltri Massif |
| title | A mountain slope deformation in an alpine metaophiolitic massif (Ligurian Alps, Italy) |
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