Retrieved from: Seattle times
“The sediment loads in the Elwha River are spiking because the reservoir behind former Elwha Dam is now completely gone. That means the settling of fines that used to occur in the lake is no longer happening so all that material is pouring into the river, and heading on down to the Strait of Juan de Fuca. It’s a dramatic sight.
“The distinct line is caused by the difference in density between the fresh water of the Elwha and the salt water of the Strait of Juan de Fuca. The heavy sediment loading is coming primarily from the area that used to be Elwha Dam. In this photo the Elwha River, right, meets the Strait of Juan de Fuca. The plume is flowing east with the tide — up, in this photograph, as Roorda flies north.
“And while the amount of sediment is large — about 50 times normal levels for the Elwha — don’t call it mud. Sediment is a single word for a whole range of material that the river has been depositing behind the two dams for the past 100 years: rocks, gravel, cobble, sand, silt, and clay. About 40 percent of that material is expected to eventually make its way out to sea.
“Restarting the river’s natural transport capacity is one of the most important aspects of Elwha River recovery. Big mountain rivers like the Elwha eat a steady diet of wood and rocks and sand and gravel, moving the material with the energy of their perpetual flow down gradient to the sea. Wood and sediment rebuild the natural structure and complexity of the riverbed: meanders, side channels, gravel bars, pools and riffles. A big mountain river like the Elwha naturally transports a fantastic amount of material — but it’s all been stuck up behind the dams, some 24 million cubic yards worth. Well now with the dams coming out — and Elwha Dam already completely gone — that material is on the move.”
Read more: Seattle times








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