The influence of lithology on channel geometry and bed sediment organization in mountainous hillslope‐coupled streams-Reference-Cited by-同舟云学术

The influence of lithology on channel geometry and bed sediment organization in mountainous hillslope‐coupled streams

Published:2020-06-14 Issue:10 Volume:45 Page:2365-2379
ISSN:0197-9337
Container-title:Earth Surface Processes and Landforms
language:en
Short-container-title:Earth Surf. Process. Landforms

Author:

Fratkin Michael Mulugetta¹²,Segura Catalina¹^ORCID,Bywater‐Reyes Sharon³^ORCID

Affiliation:

1. Forest Engineering, Resources, and Management Oregon State University Corvallis OR USA

2. Water Resources Graduate Program Oregon State University Corvallis OR USA

3. Department of Earth and Atmospheric Sciences University of Northern Colorado Greeley CO USA

Funder

National Science Foundation

Publisher

Wiley

Subject

Earth and Planetary Sciences (miscellaneous),Earth-Surface Processes,Geography, Planning and Development

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/esp.4885

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3. AttalM LavéJ.2006.Changes of bedload characteristics along the Marsyandi River (central Nepal): implications for understanding hillslope sediment supply sediment load evolution along fluvial networks and denudation in active orogenic belts.Special Paper 398: Tectonics Climate and Landscape Evolution. Geological Society of America: Boulder CO.

4. Impact of change in erosion rate and landscape steepness on hillslope and fluvial sediments grain size in the Feather River basin (Sierra Nevada, California)

5. Deep-Seated Landslides Drive Variability in Valley Width and Increase Connectivity of Salmon Habitat in the Oregon Coast Range

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