Yangtze floods recorded on Mt. Mufu and Swallow Cliff in Nanjing, China

The Yangtze drainage basin is the most densely populated and prosperous area of China; however, it is frequently threatened by floods. The Holocene flood lines of the Yangtze River have been preserved on Mt. Mufu and Swallow Cliff in north-eastern Nanjing, and they are characterised by the presence...

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Main Authors: Huachun He, Haiyu Lee
Format: Article
Language:English
Published: Taylor & Francis Group 2017-12-01
Series:Geomatics, Natural Hazards & Risk
Subjects:
Online Access:http://dx.doi.org/10.1080/19475705.2017.1284161
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author Huachun He
Haiyu Lee
author_facet Huachun He
Haiyu Lee
author_sort Huachun He
collection DOAJ
description The Yangtze drainage basin is the most densely populated and prosperous area of China; however, it is frequently threatened by floods. The Holocene flood lines of the Yangtze River have been preserved on Mt. Mufu and Swallow Cliff in north-eastern Nanjing, and they are characterised by the presence of particular colour tones and the horizontal arrangement of erosional pits and holes. Four major paleo-flood lines at altitudes of 8.51, 9.43, 10.47, and 12.84 m were identified via a field survey along the river bank. Historical literature and instrumental flood records extend the paleo-flood stage to the contemporary era and indicate that the highest flood line of 12.84 m represents a maximum limit for future floods. Besides, the flood line at 10.47 m can be regarded as a foreseeable extreme flood risk level with a recurrence interval of 100–200 years, especially considering the current circumstances of rising sea levels and decreasing flood storage capacities caused by human activities.
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spelling doaj.art-40a7935e7e00459d9cc6340e9981113b2022-12-21T18:29:29ZengTaylor & Francis GroupGeomatics, Natural Hazards & Risk1947-57051947-57132017-12-018290591710.1080/19475705.2017.12841611284161Yangtze floods recorded on Mt. Mufu and Swallow Cliff in Nanjing, ChinaHuachun He0Haiyu Lee1Nanjing UniversityNanjing UniversityThe Yangtze drainage basin is the most densely populated and prosperous area of China; however, it is frequently threatened by floods. The Holocene flood lines of the Yangtze River have been preserved on Mt. Mufu and Swallow Cliff in north-eastern Nanjing, and they are characterised by the presence of particular colour tones and the horizontal arrangement of erosional pits and holes. Four major paleo-flood lines at altitudes of 8.51, 9.43, 10.47, and 12.84 m were identified via a field survey along the river bank. Historical literature and instrumental flood records extend the paleo-flood stage to the contemporary era and indicate that the highest flood line of 12.84 m represents a maximum limit for future floods. Besides, the flood line at 10.47 m can be regarded as a foreseeable extreme flood risk level with a recurrence interval of 100–200 years, especially considering the current circumstances of rising sea levels and decreasing flood storage capacities caused by human activities.http://dx.doi.org/10.1080/19475705.2017.1284161yangtze riverpaleo-floodflood linecavecliff
spellingShingle Huachun He
Haiyu Lee
Yangtze floods recorded on Mt. Mufu and Swallow Cliff in Nanjing, China
Geomatics, Natural Hazards & Risk
yangtze river
paleo-flood
flood line
cave
cliff
title Yangtze floods recorded on Mt. Mufu and Swallow Cliff in Nanjing, China
title_full Yangtze floods recorded on Mt. Mufu and Swallow Cliff in Nanjing, China
title_fullStr Yangtze floods recorded on Mt. Mufu and Swallow Cliff in Nanjing, China
title_full_unstemmed Yangtze floods recorded on Mt. Mufu and Swallow Cliff in Nanjing, China
title_short Yangtze floods recorded on Mt. Mufu and Swallow Cliff in Nanjing, China
title_sort yangtze floods recorded on mt mufu and swallow cliff in nanjing china
topic yangtze river
paleo-flood
flood line
cave
cliff
url http://dx.doi.org/10.1080/19475705.2017.1284161
work_keys_str_mv AT huachunhe yangtzefloodsrecordedonmtmufuandswallowcliffinnanjingchina
AT haiyulee yangtzefloodsrecordedonmtmufuandswallowcliffinnanjingchina