Assessment of Sedimentation Changes in the Nehelam Bay, Oregon
This study will provide the Port of Nehalem with an assessment of the magnitude, spatial patterns, and volumetric rates of sedimentation in the Nehalem Bay from 1891 to 2012 through comparison of U.S. Coast and Geodetic Survey (USCGS). Systematically identifying locations of sedimentation and quantifying the rate of change over time will provide a baseline for understanding the extent and rate of sedimentation. Motivation for this study stems from observations of aggradation by the Port of Nehalem in recent decades. These observations are consistent with a qualitative review of the nautical charts from the USCGS from 1891 and 2012, which indicates decreases in water depth from Wheeler to Fishery Point in the Nehalem Bay, and a recent USGS study1 that documented increases in gravel bar area and decreases in channel width in the Nehalem Bay between 1939 and 2009. Bay aggradation may result in potential impacts to river navigation, reductions in estuarine habitats for juvenile salmonids, and flood risks for infrastructure near the City of Wheeler, including private docks, marinas, motels, and storm water outlets. Results from this study will be helpful to the Port of Nehalem as it seeks to communicate sedimentation observations to federal and state agencies.
Below are multimedia items associated with this project.
Below are publications associated with this project.
Preliminary assessment of channel stability and bed-material transport in the Tillamook Bay tributaries and Nehalem River basin, northwestern Oregon
- Overview
Assessment of Sedimentation Changes in the Nehelam Bay, Oregon
Aerial view of Nehalem Bay.(Public domain.) This study will provide the Port of Nehalem with an assessment of the magnitude, spatial patterns, and volumetric rates of sedimentation in the Nehalem Bay from 1891 to 2012 through comparison of U.S. Coast and Geodetic Survey (USCGS). Systematically identifying locations of sedimentation and quantifying the rate of change over time will provide a baseline for understanding the extent and rate of sedimentation. Motivation for this study stems from observations of aggradation by the Port of Nehalem in recent decades. These observations are consistent with a qualitative review of the nautical charts from the USCGS from 1891 and 2012, which indicates decreases in water depth from Wheeler to Fishery Point in the Nehalem Bay, and a recent USGS study1 that documented increases in gravel bar area and decreases in channel width in the Nehalem Bay between 1939 and 2009. Bay aggradation may result in potential impacts to river navigation, reductions in estuarine habitats for juvenile salmonids, and flood risks for infrastructure near the City of Wheeler, including private docks, marinas, motels, and storm water outlets. Results from this study will be helpful to the Port of Nehalem as it seeks to communicate sedimentation observations to federal and state agencies.
- Multimedia
Below are multimedia items associated with this project.
- Publications
Below are publications associated with this project.
Preliminary assessment of channel stability and bed-material transport in the Tillamook Bay tributaries and Nehalem River basin, northwestern Oregon
This report summarizes a preliminary study of bed-material transport, vertical and lateral channel changes, and existing datasets for the Tillamook (drainage area 156 square kilometers [km2]), Trask (451 km2), Wilson (500 km2), Kilchis (169 km2), Miami (94 km2), and Nehalem (2,207 km2) Rivers along the northwestern Oregon coast. This study, conducted in coopera-tion with the U.S. Army Corps of EngAuthorsKrista L. Jones, Mackenzie K. Keith, Jim E. O'Connor, Joseph F. Mangano, J. Rose Wallick