NELSON CREEK

River Runs Kayaking Whitewater
November 21, 2024

SUMMARY

Last Updated 2024-09-23
River Levels 3 cfs (2.22 ft)
Percent of Normal 43%
Status
Class Level iii-iv
Elevation ft
Streamflow Discharge cfs
Gauge Height ft
Reporting Streamgage
USGS 14306340

The Nelson Creek segment of the Whitewater River in Oregon is a popular destination for kayaking and rafting. The ideal streamflow range for this section is between 400-800 cfs, as water levels below 400 cfs may be too low to navigate and levels above 800 cfs may be too dangerous. The segment covers approximately 6 miles and is rated as a Class III-IV difficulty level, with several challenging rapids such as "Toilet Bowl" and "Pinball."

As with all whitewater runs, safety is a top priority. Kayakers and rafters should wear helmets and personal flotation devices at all times and be familiar with rescue techniques. The Nelson Creek segment is also subject to specific regulations, including a permit requirement for all commercial outfitters. Additionally, the use of motorized watercraft is not permitted on this section of the river.

Overall, the Nelson Creek segment of the Whitewater River provides a thrilling and challenging experience for experienced kayakers and rafters. It is important to consider water levels and safety regulations before embarking on any whitewater adventure.

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Watershed River Levels

29500

Cubic Feet Per Second

4920

Cubic Feet Per Second

25600

Cubic Feet Per Second

11000

Cubic Feet Per Second

Point of Interest

Erratic Rock State Natural Site

Erratic Rock State Natural Site

Erratic Rock State Natural Site is a geological wonder located in the state of Oregon. It is situated in the Willamette Valley and is known for its unique rock formations. There are plenty of reasons to visit this natural site, including experiencing the beauty of the rocks and the stunning views of the surrounding landscape. One of the best points of interest at Erratic Rock State Natural Site is the erratic rock itself. This is a large boulder that was transported to the site by a glacier over 10,000 years ago. The rock is estimated to weigh over 90 tons ...