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Scientific Investigations Report 2010–5065

Channel Change and Bed-Material Transport in the Lower Chetco River, Oregon

Table 1. Summary of reach attributes for the study area, Chetco River, Oregon.

[Abbreviations: m, meter; m/m, meter per meter; FPkm, flood-plain kilometer]

Reach name Distance along floodplain axis (FPkm) General description Average water surface slope (2008)(m/m) Average flood plain width(m) Average width of low-flow channel (2008)(m) Instream gravel extraction sites (1995–2008)
Upper 13.2–16 Steep, narrow channel corridor where channel and gravel bars have remained fairly stable over time. 0.00138 213 45 Fitzhugh Bar (FPkm 15.4), operated by Tidewater Contractors, Inc.
Emily Creek 10.6–13.2 Similar planform and stability as Upper Reach, but wider valley bottom and increasing bar size. .00109 285 48 Tamba Bar (FPkm 11), operated by South Coast Lumber Co.
Mill Creek 7.6–10.6 Transition reach between the stable upper reaches and more dynamic North Fork Reach. .00072 474 56 No extraction
North Fork 4.3–7.6 Historically most dynamic of all reaches. Extensive in-stream gravel mining at multiple sites since 1930s. .00140 343 47 North Fork site 
(FPkm 7–7.8), operated by Freeman Rock, Inc.
Estuary 0–4.3 Tidally influenced, confined between steep valley walls. Mouth of river historically was dynamic but navigation improvements have stablized channel entrance. Extensive gravel mining along multiple sites prior to 1990s. .00015 329 96 Estuary Bar (FPkm 2.8), operated by Tidewater Contractors, Inc.

Revised July 2012

First posted May 26, 2010

For additional information contact:
Oregon Water Science Center, Director
U.S. Geological Survey
2130 SW 5th Avenue
Portland, Oregon 97201
http://or.water.usgs.gov

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