Landslide inventory and main geomorphological features affecting slope stability in the Picentino river basin (Campania, southern Italy)

The landslide inventory of the Picentino basin was realized at 1:25,000, with focus on main geomorphological features affecting slope stability. It is based on different sets of air-photos (scales 1:33,000–1:18,000, dated up to 1998), and on field surveys. Among shallow landslides, channelized debri...

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Main Authors: Valeria Lupiano, Valeria Rago, Oreste G. Terranova, Giulio Iovine
Format: Article
Language:English
Published: Taylor & Francis Group 2019-07-01
Series:Journal of Maps
Subjects:
Online Access:http://dx.doi.org/10.1080/17445647.2018.1563836
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spelling doaj-a5af79a579724bd5b42d1533b2ec0ec92020-11-25T04:05:31ZengTaylor & Francis GroupJournal of Maps1744-56472019-07-0115213114110.1080/17445647.2018.15638361563836Landslide inventory and main geomorphological features affecting slope stability in the Picentino river basin (Campania, southern Italy)Valeria Lupiano0Valeria Rago1Oreste G. Terranova2Giulio Iovine3CNR-IRPI (National Research Council, Research Institute for Geo-hydrological Protection)CNR-IRPI (National Research Council, Research Institute for Geo-hydrological Protection)CNR-IRPI (National Research Council, Research Institute for Geo-hydrological Protection)CNR-IRPI (National Research Council, Research Institute for Geo-hydrological Protection)The landslide inventory of the Picentino basin was realized at 1:25,000, with focus on main geomorphological features affecting slope stability. It is based on different sets of air-photos (scales 1:33,000–1:18,000, dated up to 1998), and on field surveys. Among shallow landslides, channelized debris flows strongly prevail, originated as debris slides on moderately steep slopes. Further sectors are affected by deeper slope movements of greater extent. Items related to tectonics, erosion processes, and anthropized sectors are also mapped. Relevant predisposing factors to slope instability are shown in 1:100,000 thematic maps. In addition, shallow landslides of the 1998 inventory were compared to those derived from two event-based inventories (PSAI 2002, PSAI 2011, dated 1998–2005 at 1:13,000–1:10,000). Discrepancies are mainly ascribable to types of employed air-photos, age of surveys, scale of mapping, and freshness of forms, remarking the relevance of suitable shallow-landslide inventories for susceptibility evaluations.http://dx.doi.org/10.1080/17445647.2018.1563836landslide inventoryshallow landslidespredisposing factorspicentino rivercampania
collection DOAJ
language English
format Article
sources DOAJ
author Valeria Lupiano
Valeria Rago
Oreste G. Terranova
Giulio Iovine
spellingShingle Valeria Lupiano
Valeria Rago
Oreste G. Terranova
Giulio Iovine
Landslide inventory and main geomorphological features affecting slope stability in the Picentino river basin (Campania, southern Italy)
Journal of Maps
landslide inventory
shallow landslides
predisposing factors
picentino river
campania
author_facet Valeria Lupiano
Valeria Rago
Oreste G. Terranova
Giulio Iovine
author_sort Valeria Lupiano
title Landslide inventory and main geomorphological features affecting slope stability in the Picentino river basin (Campania, southern Italy)
title_short Landslide inventory and main geomorphological features affecting slope stability in the Picentino river basin (Campania, southern Italy)
title_full Landslide inventory and main geomorphological features affecting slope stability in the Picentino river basin (Campania, southern Italy)
title_fullStr Landslide inventory and main geomorphological features affecting slope stability in the Picentino river basin (Campania, southern Italy)
title_full_unstemmed Landslide inventory and main geomorphological features affecting slope stability in the Picentino river basin (Campania, southern Italy)
title_sort landslide inventory and main geomorphological features affecting slope stability in the picentino river basin (campania, southern italy)
publisher Taylor & Francis Group
series Journal of Maps
issn 1744-5647
publishDate 2019-07-01
description The landslide inventory of the Picentino basin was realized at 1:25,000, with focus on main geomorphological features affecting slope stability. It is based on different sets of air-photos (scales 1:33,000–1:18,000, dated up to 1998), and on field surveys. Among shallow landslides, channelized debris flows strongly prevail, originated as debris slides on moderately steep slopes. Further sectors are affected by deeper slope movements of greater extent. Items related to tectonics, erosion processes, and anthropized sectors are also mapped. Relevant predisposing factors to slope instability are shown in 1:100,000 thematic maps. In addition, shallow landslides of the 1998 inventory were compared to those derived from two event-based inventories (PSAI 2002, PSAI 2011, dated 1998–2005 at 1:13,000–1:10,000). Discrepancies are mainly ascribable to types of employed air-photos, age of surveys, scale of mapping, and freshness of forms, remarking the relevance of suitable shallow-landslide inventories for susceptibility evaluations.
topic landslide inventory
shallow landslides
predisposing factors
picentino river
campania
url http://dx.doi.org/10.1080/17445647.2018.1563836
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