Received: 28 June 2019 Revised: 3 September 2019 Accepted: 13 October 2019 DOI: 10.1002/gj.3684 SPECIAL ISSUE ARTICLE Diversion of the paleo‐Yellow River channel in the Qingtongxia area of Ningxia, China: Evidence from terraces and fluvial landforms Hong Chen1,2 | Guo‐dong Bao1 | Wei Shi1,2 | Jian‐min Hu1,2 1 Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing, China The Qingtongxia Grand Canyon (QGC) of the Yellow River is a region of intense tec- 2 Key Laboratory of Paleomagnetism and tonic deformation that is located in the southern Yinchuan Basin, at the junction of Tectonic Reconstruction of Ministry of Natural Resources, Beijing, China the western margin of the Ordos Plateau and the northeast arcuate structural belt of the Qinghai–Tibetan Plateau. The Yellow River makes a 90° turn as it traverses Correspondence Hong Chen, Institute of Geomechanics, the Qingtongxia area, incising the hard Ordovician sandstones of Niushou Mountain, Chinese Academy of Geological Sciences, while leaving the relatively soft Quaternary sediments on the northern side of the No.11 Minzudaxue South Road, Haidian District. Beijing 100081, China. channel undisturbed. Despite this apparent inconsistency with the expected pattern Email:
[email protected] of river erosion, there has been no significant research to date on the formation of Funding information the QGC. Here, we utilize remote sensing, surficial geomorphology, and shallow cor- Geological Survey Project of the Geological ing to confirm the evolution of the Yellow River channel and formation of the QGC. Survey of China, Grant/Award Numbers: – ‐ DD20160060 and DD20190018; Special Using Landsat Thermic Mapper and ASTER imagery, we identified a N S oriented Funds for Basic Scientific Research Operation zone of high water‐content in the northern part of the QGC that is characterized at Fees of the Chinese Academy of Geosciences, Grant/Award Number: YYWF201616 the surface by marsh and wetlands.