Timing of exotic, far-traveled boulder emplacement and paleo-outburst flooding in the central Himalayas

• Published in: Earth surface dynamics 2020-09, Vol.8 (3), p.769-787
• Main Authors: Huber, Marius L, Lupker, Maarten, Gallen, Sean F, Christl, Marcus, Gajurel, Ananta P
• Format: Article
• Language: English
• Subjects: Aquatic reptiles; Bedrock; Boulders; Channel morphology; Channels; Chronology; Clustering; Computational fluid dynamics; Discharge; Earth Sciences; Earthquakes; Evolution; Exposure; Flood discharge; Flooding; Floods; Fluid flow; Geological hazards; Glacial lakes; Glaciers; Holocene; Hydraulic geometry; Lakes; Landscape; Landscape evolution; Lithology; Morphology; Mountain regions; Newtonian fluids; Preservation; Rivers; Sciences of the Universe; Topography; Transport; Turbulent flow; Valleys
• ISSN: 2196-632X; 2196-6311; 2196-632X
• DOI: 10.5194/esurf-8-769-2020

Large boulders, ca. 10 m in diameter or more, commonly linger in Himalayan river channels. In many cases, their lithology is consistent with source areas located more than 10 km upstream, suggesting long transport distances. The mechanisms and timing of “exotic” boulder emplacement are poorly constrained, but their presence hints at processes that are relevant for landscape evolution and geohazard assessments in mountainous regions. We surveyed river reaches of the Trishuli and Sunkoshi, two trans-Himalayan rivers in central Nepal, to improve our understanding of the processes responsible for exotic boulder transport and the timing of emplacement. Boulder size and channel hydraulic geometry were used to constrain paleo-flood discharge assuming turbulent, Newtonian fluid flow conditions, and boulder exposure ages were determined using cosmogenic nuclide exposure dating. Modeled discharges required for boulder transport of ca. 103 to 105 m3 s−1 exceed typical monsoonal floods in these river reaches. Exposure ages range between ca. 1.5 and 13.5 ka with a clustering of ages around 4.5 and 5.5 ka in both studied valleys. This later period is coeval with a broader weakening of the Indian summer monsoon and glacial retreat after the Early Holocene Climatic Optimum (EHCO), suggesting glacial lake outburst floods (GLOFs) as a possible cause for boulder transport. We, therefore, propose that exceptional outburst events in the central Himalayan range could be modulated by climate and occur in the wake of transitions to drier climates leading to glacier retreat rather than during wetter periods. Furthermore, the old ages and prolonged preservation of these large boulders in or near the active channels shows that these infrequent events have long-lasting consequences on valley bottoms and channel morphology. Overall, this study sheds light on the possible coupling between large and infrequent events and bedrock incision patterns in Himalayan rivers with broader implications for landscape evolution.