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| Created: | Nov 24, 2021 at 6:24 p.m. | |
| Last updated: | Nov 24, 2021 at 6:54 p.m. | |
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Abstract
The model presented here explores one-dimensional river profile evolution in a lithologically heterogeneous setting, where bedrock erosion is modulated by a variably thick layer of gravel-size alluvium. The model combines theory for bedload transport in equilibrium gravel-bed channels with bedrock incision by plucking and abrasion. We explore a scenario in which gravel-sized sediment derives exclusively from a “hard” geologic unit in the upstream part of the fluvial system, which is transported downstream to create an alluvial blanket across a “soft,” fine-grained geologic unit.
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This resource is shared under the Creative Commons Attribution CC BY.
http://creativecommons.org/licenses/by/4.0/
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