Giant palaeo-landslide dammed the Yangtze river

Field evidence is presented to demonstrate that a very large landslide blocked the Jinsha River (the main stem of the Yangtze) near the present day town of Qiaojia, Yunnan Province. The discovery is significant because no persistent river-blocking landslide has been reported so far downstream in a m...

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Main Authors: Higgitt, David L., Zhang, Xinbao, Liu, Weiming, Tang, Qiang, He, Xiubin, Ferrant, Sylvain
Format: Article
Published: SpringerOpen 2014
Online Access:https://eprints.nottingham.ac.uk/47254/
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author Higgitt, David L.
Zhang, Xinbao
Liu, Weiming
Tang, Qiang
He, Xiubin
Ferrant, Sylvain
author_facet Higgitt, David L.
Zhang, Xinbao
Liu, Weiming
Tang, Qiang
He, Xiubin
Ferrant, Sylvain
author_sort Higgitt, David L.
building Nottingham Research Data Repository
collection Online Access
description Field evidence is presented to demonstrate that a very large landslide blocked the Jinsha River (the main stem of the Yangtze) near the present day town of Qiaojia, Yunnan Province. The discovery is significant because no persistent river-blocking landslide has been reported so far downstream in a major catchment. At the location of the landslide dam the upstream catchment area is 445 × 103 km^2. Sediments deposited behind the dam indicate that the minimum crest height was approximately 200 m with a lake volume of 11.4 +/− 1.3 km^3. The landslide occurred on the western (Sichuan) side of the river and displaced an estimated volume of at least 3.75 km^3, with material riding up to 550 m above the river on the eastern (Yunnan) side of the valley. The location is at the intersection of the Xiaojiang and Zemuhe fault zones which form part of the eastern boundary fault of the Sichuan-Yunnan Fault Block, an area where many earthquakes exceeding magnitude 7.0 have been documented in the historical record.
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spelling nottingham-472542020-05-04T16:47:03Z https://eprints.nottingham.ac.uk/47254/ Giant palaeo-landslide dammed the Yangtze river Higgitt, David L. Zhang, Xinbao Liu, Weiming Tang, Qiang He, Xiubin Ferrant, Sylvain Field evidence is presented to demonstrate that a very large landslide blocked the Jinsha River (the main stem of the Yangtze) near the present day town of Qiaojia, Yunnan Province. The discovery is significant because no persistent river-blocking landslide has been reported so far downstream in a major catchment. At the location of the landslide dam the upstream catchment area is 445 × 103 km^2. Sediments deposited behind the dam indicate that the minimum crest height was approximately 200 m with a lake volume of 11.4 +/− 1.3 km^3. The landslide occurred on the western (Sichuan) side of the river and displaced an estimated volume of at least 3.75 km^3, with material riding up to 550 m above the river on the eastern (Yunnan) side of the valley. The location is at the intersection of the Xiaojiang and Zemuhe fault zones which form part of the eastern boundary fault of the Sichuan-Yunnan Fault Block, an area where many earthquakes exceeding magnitude 7.0 have been documented in the historical record. SpringerOpen 2014-04-07 Article PeerReviewed Higgitt, David L., Zhang, Xinbao, Liu, Weiming, Tang, Qiang, He, Xiubin and Ferrant, Sylvain (2014) Giant palaeo-landslide dammed the Yangtze river. Geoscience Letters, 1 (1). p. 6. ISSN 2196-4092 https://geoscienceletters.springeropen.com/articles/10.1186/2196-4092-1-6 doi:10.1186/2196-4092-1-6 doi:10.1186/2196-4092-1-6
spellingShingle Higgitt, David L.
Zhang, Xinbao
Liu, Weiming
Tang, Qiang
He, Xiubin
Ferrant, Sylvain
Giant palaeo-landslide dammed the Yangtze river
title Giant palaeo-landslide dammed the Yangtze river
title_full Giant palaeo-landslide dammed the Yangtze river
title_fullStr Giant palaeo-landslide dammed the Yangtze river
title_full_unstemmed Giant palaeo-landslide dammed the Yangtze river
title_short Giant palaeo-landslide dammed the Yangtze river
title_sort giant palaeo-landslide dammed the yangtze river
url https://eprints.nottingham.ac.uk/47254/
https://eprints.nottingham.ac.uk/47254/
https://eprints.nottingham.ac.uk/47254/