In 2009, the USGS completed a comprehensive study of gravel transport and storage along the lower Chetco River.
PROJECT DESCRIPTION
The Chetco River is a steep, gravel-bed river in southwestern Oregon that drains 914 km2 (354 mi2) of the rugged Klamath Mountains before emptying into the Pacific Ocean 5 km (3.1 mi) north of the California-Oregon border. The lower 18 km (11.2 mi) of the channel is a wandering gravel bed river flanked by abundant, large gravel bars.
The U.S. Army Corps of Engineers and other agencies charged with permitting instream gravel extraction in Oregon requested that the USGS conduct studies to characterize channel processes and gravel transport on the Chetco River and to also evaluate possible effects of gravel extraction on physical channel and aquatic habitat conditions. The study area for this project spans the lower 18 km (11.25 mi) of the Chetco River corridor, including the USGS streamflow gage at river kilometer 16.9 (river mile 10.7) and the extent of commercial gravel extraction.
In 2009, the USGS completed a comprehensive study of gravel transport and storage along the lower Chetco River. The objectives of the study were to:
- Determine the annual influx of bed-material sediment.
- Evaluate spatial and temporal variation in bed-material transport rates.
- Assess planform and vertical changes to the river channel.
- Provide digital maps of floodplain geomorphology and general vegetation conditions for different time periods.
DATA AVAILABILITY
Below are publications associated with this project.
Channel change and bed-material transport in the Lower Chetco River, Oregon
Estimation of bed-material transport in the lower Chetco River, Oregon, water years 2009-2010
Channel change and bed-material transport in the Lower Chetco River, Oregon
Below are partners associated with this project.
- Overview
In 2009, the USGS completed a comprehensive study of gravel transport and storage along the lower Chetco River.
PROJECT DESCRIPTION
The Chetco River is a steep, gravel-bed river in southwestern Oregon that drains 914 km2 (354 mi2) of the rugged Klamath Mountains before emptying into the Pacific Ocean 5 km (3.1 mi) north of the California-Oregon border. The lower 18 km (11.2 mi) of the channel is a wandering gravel bed river flanked by abundant, large gravel bars.
Location Map for Checto River Study(Public domain.) The U.S. Army Corps of Engineers and other agencies charged with permitting instream gravel extraction in Oregon requested that the USGS conduct studies to characterize channel processes and gravel transport on the Chetco River and to also evaluate possible effects of gravel extraction on physical channel and aquatic habitat conditions. The study area for this project spans the lower 18 km (11.25 mi) of the Chetco River corridor, including the USGS streamflow gage at river kilometer 16.9 (river mile 10.7) and the extent of commercial gravel extraction.
In 2009, the USGS completed a comprehensive study of gravel transport and storage along the lower Chetco River. The objectives of the study were to:
- Determine the annual influx of bed-material sediment.
- Evaluate spatial and temporal variation in bed-material transport rates.
- Assess planform and vertical changes to the river channel.
- Provide digital maps of floodplain geomorphology and general vegetation conditions for different time periods.
DATA AVAILABILITY
Download geodatabase Download metadata Download 2008 bathymetric survey metadata - Publications
Below are publications associated with this project.
Channel change and bed-material transport in the Lower Chetco River, Oregon
The lower Chetco River is a wandering gravel-bed river flanked by abundant and large gravel bars formed of coarse bed-material sediment. The large gravel bars have been a source of commercial aggregate since the early twentieth century for which ongoing permitting and aquatic habitat concerns have motivated this assessment of historical channel change and sediment transport rates. Analysis of histAuthorsJ. Rose Wallick, Scott W. Anderson, Charles Cannon, Jim E. O'ConnorEstimation of bed-material transport in the lower Chetco River, Oregon, water years 2009-2010
This assessment of bed-material transport uses methods developed in a previous study (Wallick and others, 2010) to estimate bed-material flux at the USGS Chetco River streamflow gaging station located at flood-plain kilometer 15 (14400000). On the basis of regressions between daily mean flow and transport capacity, daily bed-material flux was calculated for the period October 1, 2008 to March 30,AuthorsJ. Rose Wallick, Jim E. O'ConnorChannel change and bed-material transport in the Lower Chetco River, Oregon
The lower Chetco River is a wandering gravel-bed river flanked by abundant and large gravel bars formed of coarse bed-material sediment. Since the early twentieth century, the large gravel bars have been a source of commercial aggregate for which ongoing permitting and aquatic habitat concerns have motivated this assessment of historical channel change and sediment transport rates. Analysis of hisAuthorsJ. Rose Wallick, Scott W. Anderson, Charles Cannon, Jim E. O'Connor - Partners
Below are partners associated with this project.