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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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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