Channel‐planform evolution in four rivers of Olympic National Park, Washington, USA: the roles of physical drivers and trophic cascades


World Heritage Site: Olympic National Park

Publication Year: 2016

Publication Type: Article

Publication Identifier: WHEEDE6759927

Summary

A 74-year analysis of four rivers in Olympic National Park reveals that physical factors, such as flood history and sediment supply, dominate channel planform evolution over ecological drivers like elk impacts. Contrary to expectations, the study found no significant correspondence between channel morphology and elk abundance, which had been linked to trophic cascades following wolf extirpation. Instead, recent widening and increased braiding in rivers like the Hoh and Elwha correlate with flood activity and sediment supply changes, including glacial retreat and landslide responses. These findings contrast with similar studies in Yellowstone National Park, highlighting the influence of hydrologic regime and large-wood availability on fluvial dynamics.

Citation

East, A. E., Jenkins, K. J., Happe, P. J., Bountry, J. A., Beechie, T. J., Mastin, M. C., Sankey, J. B., & Randle, T. J. (2016). Channel‐planform evolution in four rivers of Olympic National Park, Washington, USA: the roles of physical drivers and trophic cascades. Earth Surface Processes and Landforms, 42(7), 1011–1032. Portico. https://doi.org/10.1002/esp.4048

You are here:
World Heritage Explorer > World Heritage Research > Publications > Channel‐planform evolution in four rivers of Olympic National Park, Washington, USA: the roles of physical drivers and trophic cascades

This website includes data sources licensed under CC BY-SA 4.0. Additional original content by World Heritage Explorer, also licensed under CC BY-SA 4.0. WHE is not affiliated with UNESCO or the World Heritage Committee. Legal Notice. Privacy Policy.

Open Data for an Open World