Shore-based monitoring of flow dynamics in a steep bedrock canyon river
The pace of landscape evolution is set by bedrock erosion in canyons. This phenomenon occurs by various geological processes including plucking of bedrock blocks and abrasion by saltating bedload and suspended load in highly turbulent flows. For a better understanding of the river flow characteristi...
Main Authors: | Ansari Saber, Rennie Colin D., Venditti Jeremy G., Kwoll Eva, Fairweather Kirsti |
---|---|
Format: | Article |
Language: | English |
Published: |
EDP Sciences
2018-01-01
|
Series: | E3S Web of Conferences |
Online Access: | https://doi.org/10.1051/e3sconf/20184006025 |
Similar Items
-
Bedrock rivers are steep but not narrow: hydrological and lithological controls on river geometry across the USA
by: Buckley, J, et al.
Published: (2024) -
Bedload transport and hydro-abrasive erosion at steep bedrock rivers and hydraulic structures
by: Mueller-Hagmann Michelle, et al.
Published: (2018-01-01) -
Rapid holocene bedrock canyon incision of Beida River, North Qilian Shan, China
by: Wang, Yiran, et al.
Published: (2023) -
Efficacy of bedrock erosion by subglacial water flow
by: F. Beaud, et al.
Published: (2016-01-01) -
High-resolution observations of the near-surface wind field over an isolated mountain and in a steep river canyon
by: B. W. Butler, et al.
Published: (2015-04-01)