Ephemeral seafloor sedimentation during dam removal: Elwha River, Washington. (1st November 2017)

• Record Type: Journal Article
• Authors: Foley, Melissa M.; Warrick, Jonathan A.
• Is Part Of: Continental shelf research. Volume 150(2017)
• Page Start: 36
• Page End: 47
• Publication Date: 2017-11-01
• Subjects: Sediment deposition -- Sediment dynamics -- Benthic habitats -- Dam removal -- Photo time-series -- Elwha; Continental shelf -- Periodicals; Submarine geology -- Periodicals; 551.41
• DOI: 10.1016/j.csr.2017.09.005
• Languages: English
• ISSNs: 0278-4343

Abstract

Abstract: The removal of the Elwha and Glines Canyon dams from the Elwha River in Washington, USA, resulted in the erosion and transport of over 10 million m 3 of sediment from the former reservoirs and into the river during the first two years of the dam removal process. Approximately 90% of this sediment was transported through the Elwha River and to the coast at the Strait of Juan de Fuca. To evaluate the benthic dynamics of increased sediment loading to the nearshore, we deployed a tripod system in ten meters of water to the east of the Elwha River mouth that included a profiling current meter and a camera system. With these data, we were able to document the frequency and duration of sedimentation and turbidity events, and correlate these events to physical oceanographic and river conditions. We found that seafloor sedimentation occurred regularly during the heaviest sediment loading from the river, but that this sedimentation was ephemeral and exhibited regular cycles of deposition and erosion caused by the strong tidal currents in the region. Understanding the frequency and duration of short-term sediment disturbance events is instrumental to interpreting the ecosystem-wide changes that are occurring in the nearshore habitats around the Elwha River delta. Highlights: Frequency of sediment deposition increased as dam removal progressed. Seafloor sedimentation was ephemeral; most events lasted less than four hours. Seafloor sedimentation was correlated with river supply (+) and shear stress (−).