Baldface Creek

Day One

Forest Service road 4402. Access to Baldface Trail (#1215).
Direct vehicular access is now restricted in order to prevent root disease in Port Orford Cedar.
Burn from the Biscuit Fire.
The Baldface Trail is 6.8 miles long; distance to Baldface is 5 miles.
Snags are dead/dying trees that, despite still standing, are missing smaller branches and/or their tops.
Joseph Vaile of KS Wild and Zach Collier of NW Rafting.
The Baldface Creek drainage is covered in Serpentine Forest, which grows on ultramafic rock that originated in the Earth's mantle. While this area is one of the wettest regions in Oregon, the harsh landscape appears more like a desert—some call it a "Red Rock Rainforest."
Jeffery Pine and Incense Cedar are predominant.
The Baldface Trail descends Biscuit Hill.
There are more rare plant varieties in the Klamath-Siskiyou region than any other in the United States—particularly notable are the 36 individual species of conifers.
Prevailing trail conditions due to maintenance shortfalls in the last decade have complicated navigation. Topographic maps are necessary both off and on river, in particular for plotting river access points.
Hardwoods in the area include but are not limited to tanoak, Canyon Live Oak, California Laurel, Chinkapin, madrone, and Ceanothus.
Our first look at Baldface Creek confirmed it was swollen from recent rainfall and unnavigable without a raft.
Madrone, Port Orford Cedar and Pacific Yew surround one of the many fast-flowing but small creeks in the Kalmiopsis.
Streams and rivers in the Kalmiopsis typically look prototypical of temperate rainforests.
The put-in.
Zach Collier makes the first of many transitions between Transportation Modes: Wet and "Dry."
Swift, clear water and a variety of vegetation are Baldface Creek's hallmarks.
In addition to animal sign, we found archaeological evidence of recent Redneck and Miner populations.
The Biscuit Creek drainage.
Looking up the Biscuit Creek drainage at the confluence of Biscuit and Baldface Creeks.
A few miles further downstream, Taylor Creek joins Baldface. Upstream Taylor Creek is one of the proposed nickel mine sites. Past the confluence, the canyon narrows and the rapids increase in magnitude.
Zach Collier making the day's final crossing of Baldface Creek to reach camp.

Day Two

We made camp on a gravel bar downstream of the Taylor Creek confluence, in the vicinity of another proposed nickel mine site.
The improper use and execution of a Trucker's Hitch.
The first of several dozen river crossings throughout the day. "Dry Mode."
This slide (top right), visible from Google Earth, signals the beginning of the lower canyon.
Natural springs are commonplace along the steep canyon walls of Baldface Creek.
The sixteenth or seventeenth river crossing of the day. "Wet Mode."
The nineteenth crossing. Large, violent rapids are typically inadvisable in a packraft, necessitating short portages around them.
One of the steepest, most continuous sections of Baldface Creek.
The last mile of Baldface Creek, where the rock becomes more blue than the aforementioned red, is home to one of the most difficult rapids to navigate.
The lower canyon's geology is typical of the Smith River.
YJ's run down Baldface Creek ended here at Major Moore's, a popular put-in for the North Fork of the Smith River.
Bearfoot Brad—kind hearted, hard working—is the go-to shuttle for rides into and out of anywhere in the DFKWA.

DFKWA Fact Sheet – Baldface Creek

Geology: Serpentine.
Annual Precipitation: ~120 in.
Gradient: 126 ft/mi.
Rapids: Class IV+.
Notable Fish: Steelhead, coho salmon, chinook salmon.
Notable Flora: Darlingtona, rare serpentine endemics (no comprehensive study exists).
Notable Trees: Port Orford cedar, Jeffery pine, incense cedar, Douglas fir, tanoak, Canyon Live oak, Pacific yew.
Primary Threats: Large-scale nickel strip mines and Port Orford cedar root disease.


Smaller creeks like Baldface are temperamental and fickle in regards to navigability, flow, CFS, etc. What’s possible, what’s not possible, what’s safe, what’s not safe, can and will change, essentially, in lock-step with current weather and temperature conditions—the changes aren’t just immediate, they are, like weather itself, hyper-localized. Late winter and early spring, the most dynamic (dynamic weather = dynamic creek flow) and unpredictable time of year in terms of precipitation, snowmelt and accurate weather forecasting, is the only time of year Baldface is boatable. In this regard Baldface is problematic but not unlike many other creeks in the De Facto Kalmiopsis watershed.

The road conditions into Baldface, coupled with aforementioned unpredictable/temperamental flow is what makes it a particularly difficult creek to recon. Typically, when the creek is at perfect height to float/boat, either of the two roads into the trailhead/put-in are still buried under several feet of snow. And where there isn't snow (south facing sections), there is mud. At the very least the way in requires a legitimate 4-wheel drive truck. And but even then it’s at best a serious challenge, and at normal/worst it’s still often impossible short of towing in sleds—and then there is the issue of getting the sleds out.

The issue of getting both into and out-of further complicates a Baldface recon. Getting dropped off and picked up requires planning, logistics, coordination and help. You can’t just get off the river and picked up anywhere. Once “in” and committed from the top, it takes no less than 12 miles of floating and/or hiking to make it to the first take-out, which take-out is located several miles past the confluence with the Smith. Because even in the best of conditions it takes 2-3 hours to drive and 2-3 hours to hike just to get the Baldface put-in, and because the best time of year to recon is late winter when daylight is limited, it’s a two-day trip—which means packing food and equipment for at least one night of camping.

Further complicating floating and/or reconning Baldface, you need to be dropped off at “the top” and picked up downriver, on the Smith.

In February of 2001, Zach Collier and Super Kev (aka Beefcake) attempted to drive to the put-in from the North Fork of the Smith River. While the approach was promising at first, especially at lower elevations and on predominately south facing slopes, they were eventually turned around less than five miles from the trailhead because 5-6 foot deep snowbanks covering the road.

In March of 2007, Zach Collier and J.R met Bearfoot Brad, “the” local shuttle driver, at his house at five in the morning. This time they tried to drive in from the East up Patrick Creek. Three miles up Patrick Creek one of Brad’s truck’s wheel (yes the whole wheel) came off and rolled down a hill, and almost when into the creek. After some hitchhiking and a phone call they were able to make it back to Zach’s truck in Cave Junction. Now way behind schedule, they drove up Patrick’s Creek again until they were turned around 12 miles from the put-in because of snow drifts and snow pack.

In March of 2013, Zach Collier and YJ, with help from Joseph Vaile of KS Wild, made it all the way up and in, and down and out.

On the way in we were forced to park about two miles from the trailhead because of snow and hike the rest of the way. The snow was mostly packed and easy to navigate. A few miles beyond the trailhead we started to descend Biscuit Hill, at this point we were well below the snow line. On on the creek, we had planed to hike across and through and, when necessary, actually down or with the river when the banks became too steep or walled-in and walking alongside the creek was impossible or problematic. However, the creek was much higher than we had expected, and impossible to safely navigate through or across on foot. In anticipation of this problem we packed in Alpacka Packrafts, breakdown paddles and PFDs. What we thought would be an emergency tool, was in fact our primary mode of transportation. While inflating a packraft is relatively easy and quick, all the packing and repacking and reorganization required when transitioning between Float and Foot mode, is beyond a bummer. For two days we struggled floated, forged, hiked, backpacked, cris-crossed, bushwacked, humped, dragged, scrambled, ran, and boated our way down Baldface, often in a dry suit and backpacking boots.
 

Back To Index

 

The DFKWA is made possible with the support, financial and otherwise, of the Klamath-Siskiyou Wildlands Center, the Geos Institute, Northwest Rafting Company and Watershed, and in conjunction with the Siskiyou Mountain Club.