1. The Lasting Legacy of Megaflood Boulder Deposition in Mountain Rivers.
- Author
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Morey, S. M., Shobe, C. M., Huntington, K. W., Lang, K. A., Johnson, A. G., and Duvall, A. R.
- Subjects
BOULDERS ,GLACIAL lakes ,FLUVIAL geomorphology ,SWIMMING pools ,COMPUTER simulation ,HYDROELECTRIC power plants ,EROSION - Abstract
Infrequent, large‐magnitude discharge (>106 m3/s) outburst floods—megafloods—can play a major role in landscape evolution. Prehistoric glacial lake outburst megafloods transported and deposited large boulders (≥4 m), yet few studies consider their potential lasting impact on river processes and form. We use a numerical model, constrained by observed boulder size distributions, to investigate the fluvial response to boulder deposition by megaflooding in the Yarlung‐Siang River, eastern Himalaya. Results show that boulder deposition changes local channel steepness (ksn) up to ∼180% compared to simulations without boulder bars, introducing >100 meter‐scale knickpoints to the channel that can be sustained for >20 kyr. Simulations demonstrate that deposition of boulders in a single megaflood can have a greater influence on ksn than another common source of fluvial boulders: incision‐rate‐dependent delivery of boulders from hillslopes. Through widespread boulder deposition, megafloods leave a lasting legacy of channel disequilibrium that compounds over multiple floods and persists for millennia. Plain Language Summary: Megafloods (discharge equivalent to ≥400 instantaneously draining Olympic‐sized swimming pools per second) can transport a lot of material, including car‐ to house‐sized boulders. Because these boulders are so big, they remain in the channel until the next megaflood or until they weather into smaller pieces. We use a computer model to understand the impact of these megaflood deposited boulders on mountain river processes. We find that megaflood boulders can protect the river from being eroded, causing other processes, like tectonic uplift, to outcompete erosion. Megaflood boulders cause small steps to form within the river. Our modeling shows that these effects can be felt for >20,000 yrs after a single flood. We suggest that megaflood deposition (in addition to erosion) can cause a significant, unique change in mountain river processes. Key Points: We studied channel response to megaflood boulder deposition in the eastern Himalaya using a numerical modelMegaflood boulder deposition locally changes channel steepness up to 180%, creating >100 knickpointsThe compounding effect from multiple megaflood boulder deposits in rapid succession perturbs channel form for many thousands of years [ABSTRACT FROM AUTHOR]
- Published
- 2024
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