DOI: 10.1007/s11069-020-04461-3
论文题名: Activity maps of multi-source mudslides from the Daunia Apennines (Apulia, southern Italy)
作者: Spalluto L. ; Fiore A. ; Miccoli M.N. ; Parise M.
刊名: Natural Hazards
ISSN: 0921030X
出版年: 2021
卷: 106, 期: 1 起始页码: 277
结束页码: 301
语种: 英语
中文关键词: Apulia
; Daunia apennines
; Landslide activity map
; Multi-temporal analysis
; Reactivated mudslide
英文关键词: aerial photograph
; digital elevation model
; field survey
; geological mapping
; hazard assessment
; landslide
; mudflow
; slope failure
; spatiotemporal analysis
; Apennines
; Italy
; Puglia
英文摘要: Multi-source mudslides are common in the Daunia Apennines, i.e., the Apulian sector of the Southern Apennines of Italy, and play an important role in the historical evolution of the landscape, with significant impact on the social and economic activities of the area. They also represent the most relevant geological hazard along the front of the Apennine Chain and expose to a considerable risk the local population and infrastructures. The outer sector of the Daunia Apennines is part of the foreland thrust belt system, made up of fissured fine-grained materials, belonging to the Daunia tectonic unit formations. Concerning landslide typology, the most frequent slope movements are represented by flows and composite mudslides, the latter typically starting as slumps evolving from flows. This paper deals with the production of landslide activity maps of three case studies of composite mudslides from the front of the Daunia Apennines. The maps were produced integrating traditional interpretation of multi-year aerial photograph coverage and field surveys with the available digital elevation models to analyze surface morphology. Each landslide activity map corresponds to multi-temporal landslide inventories compiled for the last 15–20 years. This paper outlined that in the last 20 years the front of the Daunia Apennines underwent a significant reactivation of slope failure phenomena after years of quiescence, or of limited activity. The three case studies clearly confirm that: (i) the active portions of the mudslides are located inside or near preexisting slope failures, and (ii) the spatial distribution of instability phenomena is strictly dependent upon the presence of older, larger and dormant, phenomena. Landslide activity maps are an important tool for the evaluation of landslide susceptibility and hazard in the study area, and for quantitative geomorphological analyses it aimed at understanding the long-term geomorphological evolution of this portion of the Southern Apennines. Moreover, we argue that high-quality multi-temporal inventories could have positive effects on all derivative products and analyses, including erosion studies and landscape modeling, susceptibility and hazard assessments, and risk evaluations as well. © 2021, The Author(s), under exclusive licence to Springer Nature B.V. part of Springer Nature.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/169379
Appears in Collections: 气候变化与战略
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作者单位: Autorità di Bacino Distrettuale dell’Appennino Meridionale - Sede Puglia, c/o INNOVAPUGLIA (Ex Tecnopolis CSATA) Str. Prov. per Casamassima, Km 3, Valenzano, Bari 70010, Italy; Dipartimento di Scienze della Terra e Geoambientali, Università degli Studi di Bari Aldo Moro, Via E. Orabona, 4, Bari, 70125, Italy; Consiglio Nazionale delle Ricerche, Istituto di Ricerca per la Protezione Idrogeologica, Via Amendola, 122, Bari, 70126, Italy
Recommended Citation:
Spalluto L.,Fiore A.,Miccoli M.N.,et al. Activity maps of multi-source mudslides from the Daunia Apennines (Apulia, southern Italy)[J]. Natural Hazards,2021-01-01,106(1)