Puyallup, Washington, US
|
|
1 - Niesson Creek to Electron (Puyallup Gorge)
| Usual Difficulty |
V (for normal flows) |
| Length |
9 Miles |
| Avg. Gradient |
120 fpm |
Gauge Information
| Name |
Range |
Difficulty |
Updated |
Level |
|
PUYALLUP RIVER NEAR ELECTRON, WA
|
|
usgs-12092000 |
300 - 1000 cfs
|
V |
00h38m |
389
cfs
(rc= 0.1 ) |
Most of the time the flow is 400 cfs less than reported on this gauge because flows are diverted to the powerhouse. Gauge (92.8 sq.mi. drainage). |
River Description
Descending the west flank of Mount Rainier, after meandering for miles, the Puyallup River flows
through a narrow and dramatic canyon. After reading comparisons to the incomparable Carbon Gorge,
I had to go see it. You shouldn’t have to decide on such things, but I think the Carbon is
more awesome. But not by much. Both have a unique combination of rapids and geology that make
them truly special. The whitewater on the Puyallup is good, with ten or more challenging rapids
in an extremely committing setting. What prevents this run from being a Seattle-area
ultra-classic is one issue: access. The timber company that owns the area has completely
restricted a large swath of the upper Puyallup watershed. If you want to drive in via the road
right along the river, you must purchase a $360/year pass. If you are caught on the property
hiking or sitting in the car of someone with a pass, you could be given a $500 fine. Word has it
the area is regularly patrolled.
Fortunately,
there are ways to paddle this stretch. With an early start it can reasonably be done in a day via
the Mowich River, accessed near the west entrance to Mount Rainier National Park. Beginning the
hike at 9 got us to the takeout at 3. In 2006 another group put onto the larger South Fork
Puyallup using West Side Road; that involves a long hike and paddle-in. Getting down to the
Mowich is not bad, but the first part of the river is awful. The wide glacial valley accumulates
logs and disperses the river. With the gauge reading 850 at Electron, it took a couple hours to
get to the lower section of the Mowich, which thankfully is relatively unobstructed class III.
Hiking into the lower portion of the Mowich from 165 would be extremely difficult due to the
towering cliffs on river right. Almost immediately after the Mowich meets the Puyallup you come
to the diversion dam, final destination of the “World’s Crookedest Railway”.
You can visually check that the diversion is occurring, although try to find this out ahead of
time (Puget Sound Energy, Electron Powerhouse), because an extra 400 CFS in the gorge could spell
disaster.
The
rapids, with one exception, are manageable. After five or so big rapids there is a river-wide
hole at a point where the canyon narrows to ten feet. It lurks right behind a right bend that has
a gravel bar on river-left at the top of the entry rapid. Maybe you could scout the hole if you
climbed up the wall a bit, where there’s some evidence of a past landslide. With 450-500
cfs in the gorge, I got stuck after running the hole on the right and landing in the river-right
eddy. It took a few tries to paddle out. Not as bad as Rick’s Slide on the Carbon, but
similar enough to be a little eerie. This hole should be run center going straight across the
boil. I consider this the crux of the run, and it would likely get even more dangerous with
higher water.
Directions
to Takeout:
Head
south on Orville road from Highway 162. After 6.7 miles there is a turnout on the left, with
large boulders blocking a road that goes through the forest to the river. It is a little more
than a half-mile north of Electron road. At Electron road there is another road leading to a
bridge directly upstream of the takeout. If you crossed this bridge and headed upriver, it would
lead you to an easy put-in above the gorge. Absolutely no trespassing allowed
here.
Directions
to Putin Via Mowich River
Drive
North on Orville Rd. Take a right on 162 (E), right on 165 (S). Putin is down the 2nd to last
road on the right before you get to a “Mount Rainier” sign. Hike down the right fork
and then follow the switchbacks until the road is gone. Follow the lightly used trail down to an
old road. Stay on the road until it hits a floatable section of the
river.
StreamTeam Status: Not Verified
Last Updated: 2011-03-02 04:52:32
User Comments
accessing via West Side Road in the park. The road was closed to motorized vehicles due to a
wash-out, but we fabricated a "kayak" trailer from a bicycle baby carrage and had one guy peddle
the bike while two pushed from behind. You go up over one easy pass - historical in that it's
famous for the crash of a large military plane - and then you get a fun down hill screamer to the
SF Puyallup bridge. You can probably expect 2-3 hours hiking / biking from the start of WS road to
the bridge. If the road is open to vehicles, you're golden. Boating from this point down to the
main canyon is unique, lonely (you're in the park for the first bit), but not what I would consider
outstanding. The glacier till raised river beds are fun, as you're floating along at the crest of
these huge gravel deposits. It's a strange feeling to be floating HIGHER than the surrounding land.
There is also an upper vertical walled gorge probably less than a mile long - that would be
stellar. But alas, wood kept us on the rim. Once you get past this gorge, you'll have miles of
wilderness class 2 before the main canyon. Unless you get to the river at daybreak, expect to spend
the night. Also expect wildlife - we saw bear, deer, elk, etc. The canyon is fantastic - deeper
than the Carbon, vertical in spots, and quite dramatic. Most of the drops were straight-forward. We
did encounter a fresh and rather large land slide that created a class 6 mess (think Sultan), with
an easy carry on RL. Just below, we eddied at the brink of a class 5ish drop, walled in on both
sides, with fresh rock and wood from the slide impeading the line. There was one small eddy RR that
allowed us step out and teather our boats in a gully. Portaging on shore was not an option. Neither
was going up the walls or paddling back upstream to a potential exit from the canyon. This was
likely the biggest "now what" moment in my paddling career. Of course, cool heads prevailed, and we
were able to rig a tag line to a mid-river rock that luckily had a hidden but nice seal launch
shelf on the downstream side. This dropped us into the latter part of the rapid, below the crux
move that was jammed with wood and sharp rock. All is well that ends well. My guess is that both
these drops will have cleaned up with years of flow. Jon