Checking for non-preferred file/folder path names (may take a long time depending on the number of files/folders) ...
This resource contains some files/folders that have non-preferred characters in their name. Show non-conforming files/folders.
This resource contains content types with files that need to be updated to match with metadata changes. Show content type files that need updating.
| Authors: |
|
|
|---|---|---|
| Owners: |
|
This resource does not have an owner who is an active HydroShare user. Contact CUAHSI (help@cuahsi.org) for information on this resource. |
| Type: | Resource | |
| Storage: | The size of this resource is 12.1 KB | |
| Created: | Nov 24, 2021 at 6:24 p.m. | |
| Last updated: | Nov 24, 2021 at 6:54 p.m. | |
| Citation: | See how to cite this resource |
| Sharing Status: | Public |
|---|---|
| Views: | 716 |
| Downloads: | 5 |
| +1 Votes: | Be the first one to this. |
| Comments: | No comments (yet) |
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.
Subject Keywords
Content
How to Cite
This resource is shared under the Creative Commons Attribution CC BY.
http://creativecommons.org/licenses/by/4.0/
Comments
There are currently no comments
New Comment