Significant rainfall over the past week has increased soil moisture to high levels across western Washington. Additional rainfall of 1 to 2 inches is expected through Friday. This amount of rain will continue to put extra pressure on soil instability, leading to an increased threat of landslides and debris flows, especially from recent burned areas, with this new rainfall acting as a trigger. Numerous landslides have already occurred in Whatcom, Skagit, King Counties and others. More landslides continue to be possible. Areas most susceptible to landslides debris flows under these conditions are steep coastal bluffs, other steep hillsides or road cuts, and recent burned areas. A diminishing threat of landslides and debris flows will continue for several days after the rain ends. For more information about current conditions, visit www.weather.gov/seattle, select Hydrology, and then scroll down for the links to the landslide information pages. For more information on landslides, visit the website for the Washington State Department of Natural Resources landslide geologic hazards at: http://bit.ly/2mtA3wn
The ideal streamflow range for this run is between 400-800 cubic feet per second (cfs), which provides Class III-IV rapids. The segment mileage of this run is around 6.5 miles, leading from the Headwaters to the Former Backwaters of Lake Mills created by the Former Glines Canyon Dam.
There are several notable rapids and obstacles on this run, including the Class III+ "S-Turn" rapid and the Class IV "Widowmaker" rapid. Additionally, paddlers must navigate through several boulder gardens and tight channels throughout the run.
The area is regulated by the Olympic National Park, which requires a permit for all overnight camping in the area. Additionally, paddlers are required to practice Leave No Trace principles and to respect the natural environment of the park.
| Last Updated | |
| River Levels | 725 cfs (539.27 ft) |
| Percent of Normal | +100% |
| Optimal Range | 400-800 cfs |
| Status | Too Low |
| Class Level | iii-iv |
| Elevation | ft |
| Run Length | 29.0 Mi |
| Streamflow Discharge | cfs |
| Gauge Height | ft |
| Reporting Streamgage | USGS 12044900 |
| Location | Reservations | Toilets |
|---|---|---|
Dodger Point Camp
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Elk Lake Campground
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13.3 Miles Camp
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13.2 Miles Camp
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12.4 Miles Camp
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Lewis Campsite
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Headwaters To Former Backwaters Of Lake Mills Created By The Former Glines Canyon Dam
Headwaters At About 4500 Feet In The Queets Basin From Glaciers On The Mount Olympus Massif And From The Queets Glacier On Mount Queets. To Southwestern Boundary Of Olympic National Park At End Of "Queets Corridor"
Headwaters And Includes All Tributaries To Confluence With Hoh River
Headwaters And Includes All Tributaries To Confluence With Elwha River
Headwaters To End Of North Fork Quinault Road