Latourell Falls Makeover (Part 2)

January 8, 2013March 2, 2013 / Tom Kloster / 8 Comments

Latourell Falls

In the first part of this article, I focused on recent improvements that have greatly enhanced the Historic Columbia River Highway wayside at Latourell Falls. This article looks at the balance of Guy Talbot State Park, where a number of improvements are needed to keep pace with the ever-growing number of visitors who now hike the Latourell loop trail year-round.

Improving the Loop Trail

Hiking the loop in the traditional clockwise direction from the wayside, the first stop is bench located a few hundred yards up the trail. This memorial bench was donated by the Sierra Club, and though it’s not a great architectural fit for the area (a rustic style would be more appropriate), it’s still a welcome resting spot for casual hikers.

Memorial bench along the Latourell Loop Trail

Not coincidentally, the bench faces a lovely view of Latourell Falls, but there’s a story behind the view, as someone has made the effort to do some “scene management” for photographers. Take a look at the photo below, and you can appreciate the waterfall scene in its graceful glory, framed by firs and moss-covered maples. But a closer look reveals a sawed-off stump with a fresh cut. Why here? Because a trail steward (authorized or otherwise) trimmed off the broken shards of a maple that split off in an ice storm a few years ago — leaving a sore thumb that marred this classic view. You can see in these after/before comparisons from now and in 2010:

A beautiful scene as viewed in December 2012…

…and the sore thumb that once was…

…and the telltale stump!

If this was sanctioned “scene management” pruning, then kudos to the State Parks folks for putting classic views on their maintenance list. If this is a guerilla effort by a frustrated photographer, then perhaps State Parks managers will take note, and keep this view intact..!

Moving up the loop, the trail soon approaches a heavily trampled bluff above Latourell Falls. Here, the first apparent problem is a decades-old shortcut at the first switchback. A sign begs hikers to stay on the trail to protect “sensitive plants”, but so far, the boots are winning, despite logs and debris purposely scattered across the shortcut.

Tossing more logs across this shortcut might help, but borrowing an idea from the beautiful new stonework at the trailhead (or recently built stonework along the Bridal Veil Falls trail), and adding a rustic stone retaining wall here to corral traffic would be a nice option that would have lasting value.

A forlorn sign attempts to reason with trail-cutters

The viewpoint atop the well-worn bluff is really starting to show its age. The 1950s-vintage steel cable fence and mix of concrete and steel pipe posts were never a good aesthetic fit for the Gorge, but more importantly, they’re not doing anything. Visitors have recently pushed a scary boot path past the fence, and down to the brink of Latourell Falls (shown below), so a near-term fix is in order.

The overgrown, beleaguered viewpoint at the to of the falls is in need of some TLC!

The trail at the overlook has already been stomped into a wide “plaza” of sorts, and that would be a good design solution here, with a stone wall replacing the rickety old handrail. A layer of crushed gravel (another design feature of the recent improvements at Bridal Veil Falls) would further help minimize the mud slick that forms in wet months.

The lone (and beleaguered) wood bench at the overlook is well-used, and a redesign should include two or three places to sit and admire the view. For most visitors who venture beyond the lower falls overlook, this bluff above the falls is the turnaround point.

The boot path to the brink of the falls has become a heavily used liability in recent years

Adding a stone wall to better define the overlook would help curb foolhardy visitors from following the boot path to the falls brink. However, the overlook also needs some vegetation management in order to simply maintain the view back down to the trailhead — this is what most hikers who push beyond the handrails are looking for, after all.

A pair of reckless visitors in flip-flops spotted in 2010 at the bottom of the dangerous boot path, tempting fate…

A few steps beyond the bluff overlook, an unmarked trail forks to the right, descending to Latourell Creek. At first, this seems like another informal boot path, but a closer look reveals a well-constructed trail. In fact, this is where a lower loop once crossed the creek, connecting to the main loop where it returns (and is clearly visible) on the far side of the creek. This is an old idea that still makes sense, and should be embraced with a new bridge and refurbished connector trail.

This side trail (to the right) used to be part of a lower loop route

In reality, hikers are already using the lower loop, though a series of slick, dangerous logs a few yards upstream from the brink of Latourell Falls serve as the “bridge”. Reconnecting and restoring these old trail segments would be a good way to provide a shorter loop for less active hikers, and also resolve this hazardous crossing that is clearly too tempting for many hikers to resist.

Bridge needed! This old trail and the sketchy log crossing are an accident waiting to happen — and also an opportunity to provide an excellent short loop for hikers.

Moving along the loop to its upper end, the Latourell trail has a few issues at Upper Latourell Falls that deserve attention in the interest of protecting the lush landscape from being loved to death. For many years, this upper section of the trail was only lightly used, but the proximity of Talbot State Park to the Portland Metro region and the family-friendly nature of this trail has clearly made the full loop a very favorite destination.

Upper Latourell Falls

The trail approach on the east side of the falls is in good shape, but problems start to emerge on the west side of the footbridge. This is not coincidental, as an adventurous early trail once switch-backed up the slope on the west side, and led to a precarious bridge across the mid-section of the falls (shown below).

The location of this old trail was uncovered only recently. Century-old rockwork and obvious paths heading uphill from the falls have always hinted at an old trail, but a geocache has now been placed along the old path, drawing enough visitors up the slope to add some urgency to addressing the off-trail impacts here.

A century-old trail climbs the west slope at Upper Latourell Falls

The best solution here is to embrace the lowest segment of the old path by repairing the stonework, or perhaps adding steps where a shortcut has formed, and provide hikers with that close-up view from behind the falls that is responsible for the bulk of the off-trail traffic (the hikers in the photo above are making this irresistible trip).

The upper sections of the old trail are much less traveled, and a simple solution here might be to simply ask the geocache owner to remove the cache. The cache risks not simply re-opening the old trail, but also bringing inexperienced hikers to the potentially dangerous rock shelf where the log footbridge once stood. If the geocache is removed soon, it’s unlikely that visitors would even notice the upper portions of this trail.

This precarious bridge spanned the upper tier of Upper Latourell Falls in the early 1900s (courtesy U of O Archives)

Turning downstream along the west leg of the Latourell loop, the trail passes a couple of spots where some TLC is needed. First, another potentially dangerous log crossing (shown below) has drawn enough traffic to form its own boot path.

It could be decades before this old log finally collapses into the creek, so a better plan is needed to stem the damage now. Sawing out the log seems possible, and is a job that could be easily in early fall, when water levels are at their lowest, and fire danger has passed. This might even be a job for volunteer trail stewards with crosscut skills.

The other “bridge” on upper Latourell Creek…

A bit further downstream along the west leg, the loop trail passes the old trail leading to the former footbridge (described previously). Here, the new trail launches uphill along a steep, slick segment built to bypass the bridge.

Reopening the old trail section (and adding a new bridge) would therefore have a spinoff benefit here: not only would a shorter loop be possible (and safe), but the short, badly designed new section of the current trail (shown in yellow on the map, below) could be decommissioned, with the main route using the old section of trail, once again (shown in red). This would be a terrific project for volunteers, including bridge construction.

(click here for a large map)

Another scary feature suddenly appears as the west leg of the loop trail curves above Latourell Falls: an old viewpoint spur trail heads straight down to a very exposed, rocky outcrop rising directly above the falls. The view from this exposed landing is impressive, but completely unsafe, given the thousands of families with young kids that walk this loop each year. There is no railing and no warning of the extreme exposure for parents attempting to keep kids in tow.

The west overlook from the trail… yikes!

The safety hazards of the west overlook are twofold: certain death for someone slipping over the 280 foot sheer cliff to the north and a tempting, sloped scramble to the falls brink for daredevils and the foolhardy.

A simple solution could be a handrail or cable encircling the viewpoint, but a more elegant option would be a more permanent viewing platform in the stonework style of the improvements at the trailhead, serving both as a safety measure and to encourage visitors to comfortably enjoy the airy view.

The west overlook and falls brink from the east side

Next, the loop trail curves away from the creek and out of Latourell canyon, passing an overgrown viewpoint (that probably deserves to be retired), then descending in a long switchback to the Historic Columbia River Highway.

Here, the route crosses the road, and resumes on an attractive path that suddenly ends in the Talbot State Park picnic area. Though a bit of searching gets most hikers to the resumption of the loop hike, some signage would be helpful here — both to direct loop hikers back to the main trailhead, but also pointing picnickers to trail to both the upper and main waterfalls.

Heavy traffic has formed a boot-path at the base of Latourell Falls

Beyond the picnic area, the trail re-enters Latourell canyon and quickly descends to the base of Latourell Falls, the final area where loop trail improvements are sorely needed. At this point along the loop, we are within a few hundred yards of the main trailhead and wayside, so the crush of year-round visitors is evident everywhere — and thus the paved trail surface in this portion of the loop.

Most of the human impact is absorbed by the trail, but in recent years a messy boot path has developed along the west side of the creek, starting at the lower footbridge, and branching as it heads toward the base of the falls.

Looking back at the footbridge, and the extent of damage from the boot path

As it nears the falls, the boot path devolves into a web of muddy paths, where delicate ferns and wildflowers have been trampled

There isn’t a good way to convert this boot path into a formal spur or viewpoint because of the unstable slopes and visual impact it would create, so the challenge is how to best manage the off-trail activity. The simplest option would be an extension of the bridge hand-rail to block the boot path, making off-trail exploring a bit harder.

This mud patch at the east approach to the lower footbridge would make a perfect mini-plaza for visitors to spend time taking in the view

But there is also an opportunity to embrace the first part of the boot path, where a “mud plaza” of sorts has been stomped into the ground. This spot features one of the best angles for photographing the falls, after all, so a stone masonry mini-plaza with seating would be a terrific way to both discourage the off-trail travel, and give waterfall admirers an inviting place to stop and photograph the falls, out of the main flow of foot traffic.

Honoring Guy W. Talbot

One last bit of unfinished business at Talbot State Park is a debt of gratitude to Guy Talbot, himself. At the west end of the historic highway bridge, a large gravel pullout serves as overflow parking for this popular park. The loop trail crosses the highway near the pullout and in recent years, heavy use has turned this into an overflow trailhead, as well.

The wide pullout at the west end of the Latourell Bridge

At first glance, it seems nothing more than a broad, gravel shoulder. But upon closer inspection, it’s home to the only real monument to Guy Webster Talbot — the man whose profound generosity spared Latourell Falls from some other fate, and gave us the park that we know today. After all, the property wasn’t simply an undeveloped tract of forest, but rather, Talbot’s beloved country home. He gave the place he loved most to all Oregonians, in perpetuity.

Few traces of Talbot’s home and the surrounding estate survive, so this would be the perfect spot for a third interpretive sign (the first two are on the east end of the bridge, at the refurbished wayside) focused on Talbot, and why he was such an important historical figure in history of the area.

This plaque is the sole evidence of Guy Talbot’s grand gesture to the public

The pullout, itself, could also be improved to become a more formal secondary trailhead for the loop, as well — perhaps not as substantial as the newly rebuilt main trailhead and wayside at the other end of the bridge, but something better than the pothole-covered pullout that exists today.

The venerable Latourell Creek Bridge is among the most impressive on the old highway

Finally, there’s one more interpretive opportunity near the Guy Talbot memorial: a tale of two bridges. One is the towering, 300-foot long Latourell Bridge along the old highway, to the east. The unique history of its construction in 1914 is a story that should be told, especially since visitors can walk both sides of the bridge on the beautifully designed, original sidewalks.

The second bridge is a curious phantom of history — a former footbridge that once connected the two halves of the Talbot property in an elaborate, Venetian-style arch. Though long gone, the footings for the bridge can still be seen, and are a reminder of the elegance of days gone by.

The old footbridge over the highway was located just east of Latourell Creek

The good news is that both the Oregon State Parks and Oregon Department of Transportation (ODOT) are on a roll when it comes to enhancing the Historic Columbia River Highway trails and waysides. Many recent improvements to the Gorge parks and the old highway, itself, have already been completed in recent years, and more are already under construction.

Hopefully, polishing up the rest of the Latourell Falls loop and Talbot State Park can find its way into the State Parks and ODOT work program, too!

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Addendum: after posting this article, I heard from the owner of the geocache mentioned above Upper Latourell Falls. File this under the “small world” department, but it also happened to be someone I’ve known for many years, and who sets the highest standard for conservation ethics. Had I checked the cache ownership and known this, it would have erased any concerns about potential impacts the cache will have on the area. I now know it is in very good hands!

The cache owner also shared some numbers behind the cache that support that last point: only 50 users have logged it in the 3-plus years since it was placed, so not enough to have a noticeable impact on the terrain. Thus, the impacts that we’ve seen in recent years are likely just more of what we see elsewhere on the loop, where the crush of thousands off feet hitting this trail each year is running the landscape a bit ragged.

At its core, geocaching is a terrific way to introduce people (and especially children) to our public lands, which in turn, helps create advocates for conservation — something very much in line with this blog. Hopefully this article didn’t leave other geocachers thinking otherwise. After all, I own several caches myself, and like most cache owners, do my best to ensure they bring people into the wilds while also having minimal impact on the landscape.

Latourell Falls Makeover (Part 1)

December 26, 2012December 26, 2012 / Tom Kloster / 3 Comments

Today’s wayside is located at the east end of the Latourell Bridge, where the Falls Chalet roadhouse once stood in 1914 (shown here)

Over the past few years, Oregon Parks & Recreation has set the high bar for recreation improvements on the state lands it manages in the Columbia River Gorge Scenic Area. The latest project is a handsome, thoughtful makeover of the Latourell Falls wayside, located along the Historic Columbia River Highway (HCRH) in Talbot State Park.

The Latourell wayside serves thousands of Gorge tourists each year, and also functions as the trailhead for the very popular Latourell Falls loop trail. The site has a long history, and was once home to a pair of roadhouses during the heyday of Samuel Lancaster’s world-class highway in the early 1900s.

The Falls Villa roadhouse was located across the road from today’s wayside through the 1930s, now marked only by a stand of mature bigleaf maple

Modest improvements to the wayside over the years included interpretive historic signs added in the 1990s that tracked the colorful human history of the area, but for the most part, the site was dated and dingy. The restoration work completed last summer is thus a major upgrade that deserves a review here. The work was completed with a special grant secured by the Oregon State Parks department

Makeover Review

Front and center in the rebuilt wayside is the official state park sign, constructed in the standardized style used for both national forest and state park units throughout the Columbia Gorge National Scenic Area (CGNSA). The sign is mounted on a newly constructed basalt base, also designed in the uniform CGNSA style.

Welcome (again) to Guy W. Talbot State Park!

One missed opportunity in repurposing the existing entry sign was the chance to tell the story of Guy Talbot (picture below, in the early 1930s), one of the business titans of early Portland. Talbot donated the land containing Latourell Falls and the gorgeous canyon above the falls, so deserves more than passing mention in the human story of the area (along with other benefactors who donated the lands we now know as the state parks gems dotting the Historic Columbia River Highway).

Guy W. Talbot as he appeared in 1933 on the front page of the Oregonian, announcing his retirement

Two enamel interpretive panels installed at the wayside in the 1990s were salvaged and reinstalled in the new layout. One focuses on the history of the historic highway (the photos of the roadhouses, above, are from this display) and is now mounted in outside a new restroom (below). It’s a well-trafficked location, albeit sorely lacking in aesthetic appeal! The second interpretive sign is located at the main falls overlook, and briefly describes the history of private land donations for parks in the Gorge.

The new restroom is located at the east end of the wayside, tucked away from most of the picnic tables and a good distance from the new falls overlook plaza. While modern budgets probably require the low-maintenance advantage of pit toilets, the more civilized flush toilets that were removed were an aesthetic notch above the smelly nature of a chemical toilet.

The new restroom is (unfortunately) the standard pit-toilet style found elsewhere along the old highway

Considering the volume of visitors to this park, plumbed toilets may be essential — we shall find out soon enough! Fortunately, flush toilets at historic highway waysides still survive at Bridal Veil, Multnomah Falls, Ainsworth State Park, Eagle Creek, Bridge of the Gods and Starvation Creek.

But a major improvement that comes with the new restroom is the location on the south side of the old highway, adjacent to the parking area — the old restroom required crossing the highway. The new toilets are also ADA accessible, along with the drinking fountain located outside the restroom and two of the nearby picnic tables.

Accessible drinking fountain located outside the restroom

An unexpected benefit from the relocated restrooms: it turns out the old restrooms blocked a very nice view of the Latourell Bridge (below), framed by mossy bigleaf maple trees. The old restroom site is marked only by a flat spot below the highway. The low-headroom trail under the bridge that once accessed the restroom has also been decommissioned.

The view that used to be behind the restroom..!

Other details of the new wayside design include basalt curbs that edge the repaved parking area (below), and bicycle racks for cyclists touring the old highway to safely stop and admire the upper viewpoint, fill water bottles, picnic or use the restrooms.

Stone curbs show the attention to details paid by the designers

One thoughtful aspect of the new bicycle racks is the central location: too often, bicycle parking is relegated to an unused corner. This makes for much less secure parking than a more prominent location, where the public eye is more likely to deter sketchy behavior.

Centrally located bike racks front the main parking area

The west end of the wayside is the primary focus for visitors, with a handsome plaza and several new visitor amenities. A concrete-capped stone wall in the Gorge style wraps around the plaza, with notched insets for visitor information and interpretive sign installations.

An attractive, new visitor information sign (below) is an excellent addition to the wayside. While it contains the standard park information found at most state parks, an excellent trail map describing the Latourell Creek loop hike is also featured. Even better, the map isn’t of the cartoonish variety often found at tourist waysides. Instead, it shows accurate trail information and even includes elevation contours!

The handsome new visitor information sign at the Latourell wayside

The visitor map does a good job of showing the hiking options and trail highlights, as well as helpful tips on the multiple (and somewhat confusing) trailheads that provide access to the loop. A nice cartographic touch is attention to showing private lands that abut the park (though hopefully some future version of this map will show those lands in public ownership, through the Columbia Gorge Scenic Area acquisition program!)

The excellent, new Latourell Falls Loop map

One minor map glitch exists: the labeling of “Upper Falls” and “Lower Falls” may work for most people, but using the proper place name for Latourell Falls (instead of “Lower Falls”) would be more accurate and informative to those visiting the park for the first time (the upper falls is known unofficially as “Upper Latourell Falls”, so not an issue). There’s rarely a good reason to deviate from official geographic names on maps, after all.

A closer look at the excellent detail on the new park map

Hopefully, the State Parks folks will also provide a downloadable, online copy of this map at some point — one that non-profits like Portland Hikers could also offer on their user-created Field Guide, for example.

Another nice touch on the visitor information sign is the high-profile shout-out to the Columbia Group of the Sierra Club, the volunteer trail stewards for the Talbot State Park (thanks, Sierra Club!). Not only are the signs a welcome recognition of trail volunteers, but also a subtle tool for raising public awareness to the unfortunate reality that volunteers have become an essential partner to public agencies in keeping our trail system open.

Kudos to the Sierra Club volunteers!

The photo below shows the new visitor information sign from the perspective of the new plaza, with the restrooms visible in the far distance.

The view toward the visitor signboard and steps leading to the upper falls viewpoint from the new plaza (interpretive sign in foreground)

This view also shows the second notched inset in the curving basalt wall that defines the plaza overlook, where the second refurbished interpretive sign has been installed. This sign briefly describes how Latourell Falls and other nearby parks came into public ownership in the early 1900s, and is the only mention of Guy Talbot in the wayside beyond the entry signs — an oversight that is a missed opportunity in the redesign (more about that coming in Part 2 of this article).

Latourell Falls from the new plaza overlook (with the interpretive sign on the left)

The new plaza corrects many serious problems with the old design, starting with the need for a more spacious falls overlook that respects the historic design of the Samuel Lancaster’s Columbia River Highway. The new plaza meets this test with flying colors, including a subtle, but helpful detail of steps replacing ramps at both the upper and lower loop trailheads.

Another view from the plaza showing the interpretive sign (in the distance) and steps leading to the lower end of the Latourell Falls loop

Because the opening segments of the loop in both directions are paved, there has always been a temptation for people with strollers (or worse, wheelchairs) to assume the trail is safe for wheeled vehicles — it is not! Thus, the new steps will help visitors with strollers and mobility devices to avoid the dangerous mistake of venturing onto the loop trail.

The plaza forms a semi-circle in order to incorporate a second view of the spectacular Latourell Bridge in addition to the falls view. This is an unexpected discovery for visitors arriving over the bridge, unaware of its soaring height and graceful arches.

Wayside details: Samuel Lancaster would approve!

On this detail, the designers hit a home run, with a series of arches built into the basalt walls that beautifully echo the bridge design, and seamlessly tie the wayside into the highway, itself, as a natural extension of Samuel Lancaster’s masterpiece. Each arch also includes a painted steel grate – a nice detail that will keep kids and pets on the plaza-side of the stone walls.

A newly installed, arch-back bench at the head of the lower loop trailhead gives a similar nod to the historic bridge, while also helping terminate the decommissioned path that once accessed the old restroom, via a narrow, sketchy path that ducked beneath the bridge (the wood post rails in the photo below block the route of the old path).

This stately bench salutes the old highway bridge, a nice touch!

In the center of the new plaza, the designers have incorporated a long planter-bench (below) that will be a welcome respite for visitors to sit and enjoy the view. However, the design of the bench planter is problematic: The narrow planting compartment is not irrigated, and thus presents a tough landscape dilemma. The designers planted mahonia nervosa, or longleaf Oregon grape that should be drought-tolerant enough to survive, and compact enough to fit the narrow space. But it will also a prickly companion to share the bench with! Perhaps this was intentional (as a means to keep the plants from being crushed)?

The other dilemma with planters of this type is the frustrating reality that it will become an oversized ashtray over time. In the end, it might have made more sense to simply design a wide bench with a solid top for the plaza (which is certainly an option for retrofitting this bench, as needed).

A large planter bench anchors the new plaza

The revamped wayside also includes improvements to the popular upper viewpoint, located just east of the visitor information sign. The upper viewpoint path is also the trailhead for the upper portion of the Latourell Falls loop.

The stairway to the upper viewpoint path (below) also forms the terminus of the stone wall that defines around the plaza, and is nicely designed to simply lead wandering visitors to the overlook. Like the steps at the opposite end of the plaza that lead to the lower trail, these steps may help deter wheelchairs and strollers from the steep, unsafe climb to the upper viewpoint.

New steps leading to the upper falls viewpoint and loop trail

Unfortunately, the upper viewpoint path is one of the disappointments in the Latourell makeover. The short, existing section of paved trail to the viewpoint is steep and slick even for able-bodied hikers. Worse, it becomes a terrifying skating rink in winter ice conditions — which happens to be a time when the Gorge is often crowded with visitors admiring the spectacle of waterfalls transformed into ice cathedrals.

While the new handrails help, a home-run design here would have been a series of steps and landings all the way to the viewpoint — picture a scaled down version of the stairs approaching the lower Multnomah Falls viewpoint as an example. Instead, the improved steps at the base of the path taper onto the old path in a fairly awkward transition, an understandable budget constraint, no doubt, but a missed opportunity, nonetheless.

Unfortunately, this ugly, occasionally dangerous path remains a sore thumb…

After walking the brief section of old paving, visitors suddenly reach a completely reconstructed upper falls viewpoint (below) with nice attention paid to views. The basalt surround at the viewing platform has a subtle cutout where a steel fence allows the falls to be more fully viewed when approaching the overlook. This design replaces an old stone wall that once blocked the view from the trail, so is an especially thoughtful detail.

The revamped upper viewpoint platform is a major upgrade, albeit marred by the ugly approach on a steep, outmoded old trail

The awkward transition from the ugly remnant section of the old pathway to the new platform detracts from the otherwise beautiful scene, but is also something that can be remedied with future enhancement to the viewpoint.

The disappearing Latourell Falls view: a thorny problem?

Some unfinished business exists at the upper viewpoint, and it might fit into the State Parks operations budget: any photographer will attest to some much-needed “view management” here. Over the past decade or two, the brushy slope below the viewpoint (below) has swallowed up the bottom third of the falls. It’s something that a bit of pruning would greatly enhance. As recently as the 1990s the splash pool at the base of Latourell Falls was clearly visible from the viewpoint.

A Legacy Achievement

Though there will always more work to do in bringing the Gorge trails and byways closer to the national park standard, the Latourell Falls makeover is a terrific step in that direction. The project achieves a level of quality and permanence that few improvements manage.

Latourell Falls from the new wayside plaza

The new space created and constructed by the State Parks team will easily last for decades, joining the rest of the historic Columbia River Highway as a stunning blend of nature and architecture that continue to thrill visitors from around the world. It’s truly a legacy project, and all who were involved in the design and construction deserve our kudos – thank you!
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(Next up in the Part 2 of this article: a look at the Latourell Loop trail and possible improvements that would bring this popular trail to its full potential)
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Read an article on the Latourell wayside makeover

Read an article on the local stone masons uniquely skilled to do the kind of work on display at Latourell Falls

2013 Mount Hood National Park Calendar

November 23, 2012June 22, 2013 / Tom Kloster / 2 Comments

Each year at about this time I assemble the Mount Hood National Park Scenic Calendar. The proceeds are modest, but do help support the Mount Hood National Park Campaign website, WyEast Blog and related project expenses. But the main purpose is to simply promote the national park concept, and make the case for the campaign with pictures.

What the calendar looks like – oversized 11×17” pages you can actually use!

I’ve published the calendars since 2004, so this year’s calendar marks the ninth edition. All of the photos in the calendar are from trips and trails I’ve explored over the past year. I get a surprising number of questions about the photos, so in addition to simply announcing the 2013 calendar, this article tells a bit of the story behind the new images — and some are surprising!

The 2013 Scenes

The cover image for the 2013 calendar is Upper McCord Creek Falls, located just west of Cascade Locks. This is a popular destination for Columbia Gorge lovers, though often overshadowed by its more famous downstream sibling, Elowah Falls.

Cover Scene: Upper McCord Creek Falls

Upper McCord Falls is unique in that it flows as a twin cascade. A little known fact is that a third segment used to flow during the rainy season as recently as the 1970s, just to the left of the two segments shown in the photo (above). The third segment has since been blocked by stream debris, however, so for now, Upper McCord is best known as a twin cascade.

The falls is popular with photographers, but in 2010 was briefly obstructed by a large treetop that had split from atop a nearby maple, landing perfectly on its head, directly in front of the falls. While the local photography community simply grumped and groaned about this unfortunate development, Gorge waterfall explorer and photographer Zach Forsyth did something about it: he scrambled down the slope, and neatly tipped the 40-foot up-ended tree on its side. Thus, Zach made this year’s calendar cover possible – thanks, Zach!

Upper McCord Creek Falls with “the stump” in 2010

Upper McCord Creek Falls is tucked away in the hidden upper canyon of McCord Creek, just a few hundred yards from the brink of Elowah Falls. The trail to the upper falls is especially spectacular, following a ledge chiseled into sheer cliffs in the early 1900s to pipe water to the former Warrendale Cannery, below (portions of the pipe system can be seen along the trail). The falls is hidden from view until you abruptly arrive at the dramatic overlook, directly in front of the falls – one of the finest and most unexpected scenes in the Gorge.

The January calendar scene is a wintery view of the rugged west face of Mount Hood, just emerging from the clouds after a fresh snowfall. This view was captured just a few weeks ago near Lolo Pass, as the evening light was briefly catching the summit.

January Scene: West face after an early winter storm

Like most “mountain in the mist” images, this one was a reward for patience: I waited for two chilly hours for the clouds to clear! It worth the wait, though I’ve also had my share of disappointments when that glorious glimpse of the mountain didn’t materialize.

For the month of February, I picked an image from a trip last winter along the Little Zigzag River. I had planned to snowshoe to Little Zigzag Falls from the Kiwanis Camp, but there were only about 18 inches of snow on the ground, much of it fluffy and new. So, I simply trudged through leaving some very deep boot prints in my wake — and happily, the only footprints on the trail that afternoon.

February Scene: Little Zigzag River in winter

The weather was extremely cold on this visit, revealing one of the surprising effects of running water in winter: it turns out the sheer volume of relatively “warm” water (that is, above freezing) flowing down the Little Zigzag river actually heats the narrow canyon, much like an old steam radiator heats a room.

Following this radiator analogy, the temperate gradient is most noticeable when air temperatures are really cold. It was about 12º F that day, yet the air right next to the stream, and especially in front of Little Zigzag Falls measured in at a “balmy” 30º F. I found myself peeling off layers while shooting the stream and falls, only to hurriedly put them back on as I ventured back down the trail and into the real cold!

For the month of March I chose another waterfall scene, this time the lush, verdant base of popular Latourell Falls in the Columbia Gorge.

March Scene: Latourell Falls in spring

On this visit to the falls, Oregon State Parks construction crews were starting work on several major upgrades to viewpoints along this busy trail. As a result, the most popular trailhead at the Latourell Wayside was closed. Instead, I took a back route to the falls and had the place to myself for the better part of an hour — nearly unheard of on what should have been a busy spring weekend at Latourell Falls.

The April calendar scene is from Rowena Plateau at the McCall Preserve, in the dry, eastern Columbia Gorge. The iconic yellow balsamroot and blue lupine were in peak bloom on this sunny afternoon in mid-spring, and the glassy surface of the Columbia River in the background reveals a rare day of calm in the normally windy Gorge. The very tip of Mount Adams peeks over the hills on the horizon, on the Washington side of the river:

April Scene: Balsamroom and lupine on Rowena Plateau

The trip to Rowena was especially memorable for me, as I was hiking with an old college friend who was visiting Oregon for a few days. Rowena was a great place to catch up on news and old memories.

My friend also happens to be an eminent geologist working for the federal government, so we had a great conversation about the mystery of “desert mounds” (also known as “biscuit scablands”), which found on Rowena Plateau and in other areas in the Columbia Basin (watch for a future WyEast Blog article on this subject…).

Hikers passing one of the mysterious desert mounds on Rowena Plateau

Continuing the balsamroot-and-lupine theme, the May scene in the new calendar comes from Hood River Mountain, a tract of private land that is (for now) open to the public, but at risk of closure, due to heavy use by hikers.

This is one piece of land that will hopefully come into public ownership someday, before a less responsible private owner places trophy homes on these beautiful slopes. I wrote about this unfortunate oversight in the Columbia River Gorge Scenic Act in this article from a few years ago.

May Scene: Hood River Mountain in May

On Memorial Day last spring, I made a trip to Dry Creek Falls, a beautiful waterfall saddled with one of the most unfortunate and uninspiring place names in the Gorge! The June calendar image is from that trip, and captures Dry Creek rambling through the forest a few hundred yards below the falls.

June Scene: (not so) Dry Creek in spring

This area has a unique history: an old, derelict diversion dam and waterworks survives at the base of the falls, where the City of Cascade Locks once tapped the stream for municipal water in decades past. Perhaps this is the origin of “Dry Creek” name — did the stream below the diversion actually go dry when the dam was installed? Perhaps, but today it flows year-round, and makes for a beautiful streamside hike in spring.

Dry Creek Falls and the remains of the old diversion dam and waterworks

The July scene in the 2013 calendar is from a trip to Elk Cove last August. This is one of my annual pilgrimages, and I have photographed this particular spot just east of Cove Creek too many times to count — yet I’m always excited to get there, and recapture the stunning scene.

July Scene: Summer wildflowers at Elk Cove

The wildflower bloom on Mount Hood was delayed by several weeks this year, so even though I was a bit late in visiting Elk Cove, there was still a bumper-crop of purple aster mixing with the blue lupine and mop-heads of western anemone, or Old Man of the Mountain.

Not visible in the calendar view of Elk Cove are the blackened forests directly behind me: the Dollar Fire of 2011 swept across a 5-mile swath along the northern foot of Mount Hood, charring the northern fringes of Elk Cove, including several large stands of mountain hemlock that frame the view from 99 Ridge.

The Dollar Fire burned a 5-mile swath across the north slope Mount Hood

Though it’s initially shocking to see healthy forests killed by fire, it is also part of the natural cycle of forest renewal. Thus, we’ll now have a front-row seat to the fire recovery process that will unfold over the coming years along the popular north side trails. I wrote this blog article on the Dollar Fire earlier this year.

For the August calendar image, I picked a less familiar scene from an otherwise popular hike: the soaring trail to the 8,514’ summit of Cooper Spur. To beat the crowds, I set my alarm for 3 AM and raced to the trailhead at Cloud Cap. I was the first to arrive at the string of dramatic viewpoints along the trail, and caught the first rays of sun lighting up the northeast face of the mountain.

August Scene: Eliot Glacier from Cooper Spur

This view is from the north shoulder of Cooper Spur, just below the summit, and looking into the impressive jumble of crevasses and icefalls along the Eliot Glacier. Though the sky was crystal clear (you can see the moon setting to the left of the mountain), the winds from the south were strong and blustery. So, getting this shot from the lee side of the spur also meant enjoying some respite from the intense wind and blowing volcanic grit.

For the September image, I selected a lesser-known view of the mountain: the remote and rugged Newton Canyon, on the southeast side, where Mount Hood has a broad, massive profile.

September Scene: Rugged Newton Creek Canyon on the east side of Mount Hood

Glacial Newton Creek is best known for the havoc it brings far below, where the stream has repeatedly washed out Highway 35 with violent debris flows that toss Toyota-size boulders and whole trees across the road in their wake. Construction crews were busy this summer completing yet another repair, this time for damage that occurred in the 2006 floods. As always, the new road is bigger and higher than the old. We’ll see if Newton Creek is persuaded to flow through the new series of larger flood culverts this time…

The October scene is from Wahclella Falls on Tanner Creek, a popular family hike that also provides terrific viewing of spawning salmon and steelhead in early autumn.

October Scene: Wahclella Falls in autumn

Fall colors were somewhat muted in 2012, thanks to an unusually long, dry summer that extended well into October. As a result, the broadleaf trees in many areas had already dropped a lot of leaves due to the stress of the drought, before they would even have a change to change with the seasons.

While fall colors at Tanner Creek were less affected by the summer drought, the autumn scene in this year’s calendar has to make due without without the help of the particular tree, the Wahclella Maple I wrote about earlier this year. You can see the hole it left by comparing this year’s image (above) and a 2010 image (below).

Wahclella Falls in 2010 with the Wahclella Maple still standing above the footbridge

Since 2007, I’ve made annual trips with friends and volunteers to tend to the Old Vista Ridge Trail on the north side of Mount Hood. This historic gem from the early 1900s was an overgrown, forgotten victim of the Forest Service clear-cutting juggernaut for some 40 years, but somehow managed to escape their chainsaws.

Volunteers re-opened the Old Vista Ridge Trail in 2007, spurred in part by a Forest Service scheme to turn the area into a playground for dirt bikes and ATVs — an appalling plan that was eventually abandoned, in part because the rediscovered trail had revealed the beauty of the area to so many.

In 2010, the trail became the official northern boundary of the expanded Mount Hood Wilderness, when President Obama signed a new wilderness bill into law. This change should close the door on future Forest Service threats to the area, and today the hike into one of the best on the mountain.

November Scene: Mount Hood from Owl Point

The November calendar scene is from a viewpoint along the Old Vista Ridge Trail known as Owl Point, the rocky outcrop with stunning views of the mountain. Bright red huckleberries light up the foreground in this scene, and the first dusting of snow highlights the mountain. In the distance, you can also pick out the browned forests on the slopes of Mount Hood, where the Dollar Fire swept across the base of the mountain in 2011.

The final image in the new calendar is another taken from Lolo Pass, perhaps one of the most spectacular views of Mount Hood. This image was taken just before sundown after a fresh snowfall had blanketed the mountain.

December Scene: Winter arrives at Lolo Pass

I paid the price for taking in the sunset that night at Lolo Pass, as my car was broken into at the trailhead – something I’d somehow managed to avoid in all my years of hiking! As frustrating as it was to deal with the repairs and lost belongings… I’d do it all over again just to spend those magical hours watching the mountain that night — it was truly breathtaking! Here, take a closer look, and see for yourself:

Mount Hood from Lolo Pass | 2012
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The thirteen images I chose for the 2013 calendar are from a few thousand images I’ve taken this year on something just shy of 40 outings to Mount Hood and the Gorge — a bit less time on the trail than a typical year would allow, but no complaints! As always, these adventures took me to new places and discoveries, as well as fond visits to my favorite old haunts.

And as always, the magnificent scenery further confirmed my conviction that Mount Hood should (and will!) be set aside as our next National Park! Hopefully, the calendar makes the case, as well.

How can you get one, you ask?

The new calendars are available online:

2013 Mount Hood National Park Calendar at CafePress

They are large and functional, measuring 17” across by 22” tall when hung, with plenty of room for writing notes and scheduling activities. CafePress packages them carefully, with each calendar sealed against a corrugated cardboard backing for support.

The calendars sell for $29.99 + shipping, with about 25% of the proceeds going to support the Mount Hood National Park Campaign. They make terrific stocking stuffers (…although you’ll need an 11×17” stocking…), and CafePress now makes it even easier by offering PayPal as an option.

And as always, thanks for your support!
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Addendum: Gorge uber-Guru Scott Cook set me straight on a couple of comments in the above article:

Hey Tom, so of course I read your blog like a good Gorge denizen. A couple of points…I’m not trying to sound like a know-it-all…but I know that you do like to get at the bottom of things and eschew conjecture:

The pipes visible on the Upper McCord trail are from Myron Kelly’s pulp mill, not Warren’s cannery. There are some pix on my blog of Kelly’s mill and iterations of his pipes. I have another old pic too showing the pipe running along the cliff cleft, illustrating to me that the cleft was a pipeway instead of a WPA/CCC construction.

(author’s note: here’s a photo I shared with Scott that shows CCC crews clearing out the old waterline shelf to make way for the trail to Upper McCord Falls — note the Historic Columbia River Highway, far below, and the CCC crew bosses in full uniform)

…and, about Dry Creek falls, the Creek was called Dry Creek before the water works were installed. The reason is that just downstream of the PCT trail bridge, just down the access road 200yards, the creek dries up in the summer to nothing, just a dry creek bed as the creek goes subterranean until re-emerging downstream of the powerline corridor.

If you walk down the access road in the summer, the stream is of course flowing under the bridge, but when you walk downstream the sound goes away and you just figure the stream curved away from the road, but nope, if you bushwhack over just 100 feet you’ll see the dry stream…as you will if you continue down the access road also.

Down the (Dry Creek) access road is a bunker-looking building that was built in the 30’s to store the water from the stream’s waterworks for the city’s first municipal supply. The water shed is still in use today, but the water is pumped upwards into it from wells in the town below.

Next edition of Curious I’ll have Dry Creek Falls as a loop using the powerline access road…so people can learn the history and see the Dried-up Creek as well (cuz everyone loves a loop). Look for my pix on Google Earth of all this stuff and the dried-up creek. -Scott

Thanks, Scott!

Money Plant

November 4, 2012November 12, 2012 / Tom Kloster

Spring brings a stunning array of wildflowers to the Columbia River Gorge, and one of the most striking is the Money Plant (Lunaria annua), also known commonly as Silver Dollar Plant and Honesty. Its botanical name “lunaria” refers to its moon-shaped seed pods. But it turns out that Money Plant isn’t really a native — more about that in a moment.

This beautiful species produces lush purple, lilac and white blossoms on tall stalks in spring. But it is the namesake “silver dollar” seed pods — known as a “silique” — in fall and winter that are most familiar to us.

Money Plant typically grows in scattered roadside drifts, and can be found along the western sections of the Historic Columbia River Highway where it favors sites with rich soils and filtered sunlight.

Typical Money Plant coming into bloom in its second year

Money Plant is a biennial, which means it takes two years to complete its lifecycle from germination to flowering and seed production.

In its first year the Money Plant sprouts from seeds in early spring, and over the course of summer develops leaves, stems, and roots substantial enough to survive the subsequent winter, when the plant becomes dormant.

In its second year, the Money Plant emerges from dormancy and “bolts” to produce tall flowering stems by late spring. The blossoms open from the bottom of the emerging stalk, and proceed to bloom at the growing tip of the flower stem, even as the earliest flowers have transformed into green, developing seed pods.

Money Plants blooms come in purple, lilac …and white

By early summer, most of the blooms have dropped, and the flower stalks have transformed into a bouquet of flat, green discs. These are the pods, or “siliques”, that hold developing seeds, and will soon mature to become the more familiar “silver dollars”.

Middle stage: green “dollars” forming along the flower stalk

“Dollars” are already forming on this plant, even as the tip of each flower stalk continues to bloom

Close-up view of the young seed pods shows the tiny dots that will mature into pea-sized seeds

By late summer of their second year, Money Plants have put all of their energy into producing viable seeds, whereupon the plant dies and turns a tawny brown as it dries.

Finally, the outer skin of each seed pod shrinks enough to become brittle, eventually popping off to release the seeds. Two to four flat, kidney-shaped seeds adhere to the pair of outer skins, allowing them to carried a short distance from the mother plant in the first fall storms, with the skin serving as a mini-sail.

Mature seeds still attached to the mother plant

Some of the seeds have fallen from these pods, revealing the first few “silver dollars”

Close view of the two outer skins of a silique and the shiny inner membrane “dollar”

Once the outer skins are shed from the seed pods, the Money Plant takes on its most familiar form. Each pod has an iridescent central membrane that dries to form the “silver dollar” that is reveled when the outer skins and seeds have been shed. These “dollars” remain on the plant through the winter and beyond, and even have commercial value as floral material.

Money Plant at the end of its lifecycle, with all of its seeds shed, leaving only a skeleton of the plant (source: Wikimedia)

Surprisingly… not native!

As non-natives go, Money Plant looks right at home among the native wildflowers of the Columbia Gorge. The plants are attractive, aren’t particularly aggressive and tend form only scattered small drifts among our native species.

It’s no secret how Money Plant naturalized: you can find Money Plant sold as a garden ornamental around the world, as the appeal of the plant is universal: showy flowers, attracts butterflies, valued for its dried form and easily grown from seed.

In a garden center near you?

Thus, this native to the Balkans of Southeastern Europe has since naturalized throughout the world – including our own Columbia River Gorge.

The following map shows Money Plant naturalizing in pretty much every temperate state, but notably where winters are cool enough to trigger its biennial growth stages:

Source: USDA

In Oregon, the plant is listed as “moderately invasive” by numerous public land agencies and native plant organizations, though not on the “100 Worst List” of noxious species targeted by the State of Oregon for eradication.

Meanwhile, Money Plant seeds have found a new niche as a promotional gimmick, with marketers selling customized seed packets — most often for financial institutions, but also for other organizations.

It is therefore unlikely that Money Plant will ever be eradicated from Oregon — but also doesn’t seem to be a destructive invader. It thrives among native plants, but doesn’t seem to smother them. Compared to other, more aggressive invaders, Money Plant seems more “naturalized” than “invasive”.

Should you grow Money Plant?

So, now you’re feeling guilty about those Money Plant seeds you collected to plant in your garden, right? Clearly, millions of Americans have done the same — or simply purchased a pack of seeds at their local garden center (or received a pack from their bank – as I recently did).

Once planted, Money Plant is also very good at propagating itself in your garden – just as it does on roadsides. So, for most gardeners, that’s a benefit since the plant is a biennial and must be replanted annually, though that is also what makes the plant invasive.

Who wouldn’t want this flower in their garden..?

So, is it okay to grow an “invasive” species..? Generally, the answer is “no”. But here’s a responsible way to grow Money Plant in your garden: simply cut the drying seed stalks (whether from your own garden, or collected in the wild) as they’re beginning to turn yellow, but before they’ve become brittle enough to release seeds. This prevents the seeds from scattering on their own, potentially beyond your garden.

Next, hang the cut plants in a garage or basement to completely dry. Once dried, you can shake the outer silique skins (and seeds) from the plants into a paper bag, and use the shiny inner “silver dollars” that remain on the stems for decoration. This allows you to collect and sow the seeds you harvest where you can keep an eye on the plants, and carefully control where the seeds go.

If you’ve collected your seeds in the wild, then you get bonus points: in addition to having some beautiful flowers in your garden, you’ve also done your part to keep the naturalized population in check, as well. That should go a long way in easing your guilt..!

Warren Falls story airs October 25th on Oregon Field Guide!

October 21, 2012November 12, 2012 / Tom Kloster / 3 Comments

The Magnificent Seven ready to head to Warren Falls on May 12

If you’ve followed this blog for awhile, you may remember this article from last spring. This earlier article documents the field shoot at Warren Falls for a story on OPB’s Oregon Field Guide.

The segment finally airs this week at the following times on Oregon Public Broadcasting:

• Thursday, Oct. 25 at 8:30pm

• Sunday, Oct 28 at 6:30pm (repeat)

After the story airs, it will be viewable on the Oregon Field Guide website:

OFG Warren Falls Episode

Vince and Michael at work along Warren Creek

Thanks go out to Vince Patton and Michael Bendixen, the brave OFG crew who made a couple of trips to Warren Falls to capture the story. Along the way they braved an ice storm, waded through knee-deep poison oak, dodged cliffs and dangled beneath the huge “trash rack” that covers the top of the Warren Falls diversion. They are true adventurers to the core!

The crew spent two separate days on site, and captured what should be some very intriguing views of the Warren Falls diversion structure — including that glimpse under the weir, looking into the tunnel. The video from our earlier, icy winter trip should be interesting, with some surprises, I suspect.

OFG shooting at the base of Warren Falls last May (Photo: Adam Sawyer)

ODOT continues to move forward toward construction of the Historic Columbia River Highway State Trail segment from Starvation Creek to Warren Falls, so stay tuned! I’ll continue to post information on the effort to restore the falls on the blog, as well as on the Restore Warren Falls Facebook page:

Restore Warren Falls on Facebook

Our Gorge: Their Summer Destination..!

August 19, 2012 / Tom Kloster / 6 Comments

Look! Behind you… it’s Multnomah Falls!

Thanks to being one of the country’s original motoring routes, countless automobile ads have been filmed along the Mount Hood Loop Highway over the years. Usually, our world-class scenery is little more than an un-credited extra in the casting, though always a welcome affirmation of the national park qualities of Mount Hood and the Columbia Gorge!

But this summer, two new ads from Infiniti get more personal with the Gorge as “your summer destination”. True, it’s the luxury Infiniti G Sedan (and the affluent buyers they are courting) that the company has in mind, but like few ads before it, these 30-second spots use the Gorge setting as the main selling point. They’re fun to watch for local Gorge enthusiasts, especially some digital slight-of-hand for the sharp-eyed.

Cruising Waterfall Alley

The first ad opens with a stylish 30-something couple in a contemporary art gallery, admiring a metal sculpture. Behind them is a rather nice abstract painting of Multnomah Falls, featuring the Benson Bridge (was it created for the ad?).

After a brief daydream involving a cruise ship and spritely grandpa running by in a red Speedo, the couple turns toward the painting behind them and proclaims: “Let’s go on vacation there!”

Ah, now you see it! Nice painting, too…

Cut to a lovely summer view of Multnomah Falls and Benson Bridge… and a car zipping across the pedestrians-only bridge…? Clearly, a driving maneuver made possible through the miracle of computer generated imagery (CGI), but fun to see for those who know the location!

Look out, pedestrians! Luxury sedan coming through..!

Before your eyes can zero in on the car atop Benson Bridge, the scene cuts to the same car coming across the similarly arched Shepperd’s Dell bridge. For the national audience watching this ad, the two bridges do appear to be the one and the same, adding to the fun for local Gorge aficionados who know better.

Aren’t you going to slow down for the waterfall..?

From Shepperd’s Dell, the sleek new Infiniti now passes in front of Horsetail Falls as the fine print appears: “Professional driver. Closed course. Do not attempt.” Good advice… especially if you still owe on your $37,000 luxury sedan!

Nope, not stopping at this falls, either…

Next, the ad cuts to a section of historic highway that appears to be just east of Shepperd’s Dell, with a verdant green forest canopy reflecting off the hood of the well-polished Inifiti. A squiggly “sharp turns” sign completes the scene and message: sure, it looks like a sedan, but it drives like a sports car!

That squiggly arrow means “go faster”, right..?

Then, another abrupt U-turn, and we complete the high-speed tour of Waterfall Alley with a spin around Crown Point. The colors and river level in the background show this scene to have been filmed in the peak of spring in May or early June, under overcast skies, as were the previous clips in the sequence.

Hey, you’re speeding past a world-class viewpoint..!

The exception is the opening Multnomah Falls shot — the only clip without an actual vehicle operating in it. This clip appears to have been filmed later, possibly mid-summer, and clearly under sunny conditions, too. Could this be a stock video clip with the CGI added?

Here’s the complete video of “your summer destination” in Waterfall Alley – enjoy the ride!

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Cruising Rowena Crest

One of these ads would be fun enough for local Gorge junkies to study, but a twin ad filmed in the eastern Gorge is equally intriguing. This commercial begins with a somewhat younger 30-something couple (the Infiniti G is apparently an “entry level” luxury model… hmm…) this time admiring a mysterious coffee table book in an upscale bookstore (is this a film set, or real location..?)

Definitely not Powell’s, but the book looks interesting…

Like the first couple, this pair daydreams of a tropical vacation (on Bora Bora), then comes to their senses when a coconut thumps the hood of their hyper-polished Infiniti sedan. Startled from their daydream, they take a look at the two-page spread in the huge art book before them and proclaim: “Let’s go here!”

…now the book looks REALLY interesting!

The colossal book looks like it must be a custom-made prop, but does have a caption running down the left side that describes driving this scenic route in Oregon — perhaps this is a real book?

If so, the camera crews went to extraordinary efforts to match the location for the first shot in first video sequence — or is it the other way around? If the book was created as a prop for the ad, the stills of this scene for the book were clearly shot later in the summer than the filming of the driving sequences, as evidenced by the summer colors along the freeway and Sevenmile Hill, in the background.

A couple of quick cuts in the opening sequence along the historic highway show off a lovely section of Samuel Lancaster’s beautiful old road, featuring the artful stonework and remarkable effort to blend with the landscape that continues to make the Historic Columbia River Highway a “summer destination” for visitors from around the world.

Ah… you might want to slow down on this curve…

…or not… glad there’s a “professional” at the wheel…

Next, the still spotless Infiniti sedan makes another time-travel maneuver, appearing on the Rowena Loops, just to the east of the opening clip. This is one of the most photographed sections of the old highway for the purpose of selling fast cars, so an expected clip in this ad.

Clearly, he saw another squiggly arrow sign…

The next clip is back in geographic sequence, picking up the sedan as it passes another terrific Lancaster design feature: the graceful roadside viewpoint just below Rowena Crest. Though a bit sketchy for pulling off (especially with professional Infiniti drivers speeding by), this little overlook is one of the lovelier details along the historic highway.

Wait! Another view… point… eh… never mind.

The second ad ends up with another leap to the east, near Rowena, proper, just below the loops. The amazingly bug and dust free Inifiti zooms past a nice section of restored wooden historic highway guardrail before the commercial fades to text.

The shiniest car to ever visit Rowena?

Here’s the complete video for the second ad – another fun 30-second ride!

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Do these ads matter?

Beyond the welcome confirmation by Madison Avenue of the Gorge and Mount Hood as places of national park caliber (and generally assumed as such by most out-of-state visitors), these moments in the national spotlight have real benefits for our region. I tried a few web searches using the catch phrase from the ad, and found many queries and discussions from curious viewers trying to figure out where these ads were filmed.

A Google search for “Infiniti commercial” shows the waterfall spots to be popular

If ads like these translate into out-of-state visitors coming to experience the Columbia River Gorge and Mount Hood for themselves, it’s a big win for the local economy: visitors from outside our region spend much more than locals when they’re here, especially on lodging and dining.

That’s a good thing for the Gorge and Mount Hood communities, even if we can’t take credit for the free advertising — our breathtaking landscape gets star billing for that!

The Wahclella Maple

July 27, 2012July 7, 2013 / Tom Kloster / 3 Comments

Autumn sunburst lights up the Wahclella maple in late 2011

Sometime last winter a picturesque bigleaf maple framing Wahclella Falls tumbled into Tanner Creek, likely under the stress of heavy snow or ice. In any other spot, this event might have gone unnoticed, but the Wahclella maple had the distinction of a front row seat at one of the most visited and photographed waterfalls in the Columbia River Gorge.

“Change is the only constant. Hanging on is the only sin.”
-Denise McCluggage

Tanner Creek gorge is no stranger to change. In the spring of 1973, a massive collapse of the west wall, just below Wahclella Falls, sent a huge landslide into the creek, temporarily forming a 30-foot deep lake behind the jumble of house-size boulders. Today, the popular Wahclella Falls trail crosses the landslide, providing a close-up view of the natural forces that have created this magnificent place.

By contrast, the demise of the Wahclella maple is a very small change, indeed. But a closer look provides a glimpse into some of the more subtle changes that are part of the perpetually unfolding evolution this beautiful landscape. The following are nearly identical photos captured six years apart, in 2006 and 2012, and the changes over that short span are surprising:

[Click here for a larger view]

Comparing these images, one obvious change is in the stream, itself where (1) an enormous log has been pushed downstream by the force of Tanner Creek, testament to the power of high water. In the center of the scene (2) a young bigleaf maple has doubled in height, obscuring the huge boulder that once sheltered the tree, and on course to obscure the footbridge, as well. New growth is also filling in (3) along the new section of raised trail built on gabions in the 1990s (gabions are wire mesh baskets filled with rock, and were used to build up the trail along the edge of Tanner Creek)

The main change to this scene is the Wahclella maple (4), itself. Because the tree fell into a brushy riparian thicket, the fallen trunk and limbs have already been largely overtaken by lush spring growth of the understory. In a few short years, the fallen tree will disappear under a thick layer of moss and ferns, completing the forest cycle.

[Click here for a larger view]

But the story of the fallen Wahclella maple doesn’t end there, thanks to the unique adaptive abilities of bigleaf maple. Unlike most of our large tree species, bigleaf maple is prolific in sprouting new stems from stumps or upturned root balls. The massive, multi-trunked giants that appear in our forests are the result of this form of regeneration.

The Wahclella maple is already re-growing from its shattered trunk

[Click here for a larger view]

In this way, the Wahclella maple already seems to be making a comeback. With its former trunk still lying nearby, the shattered base of the tree has sprouted several new shoots this spring. In time, there’s a good chance that some of these shoots will grow to form a new, multi-trunked tree, perhaps one that is even more magnificent for future generations of photographers.

In the meantime, the old maple tree is a reminder that the beauty of the area is forever a work in progress, and how fortunate we are to watch the each stroke of nature unfold.

“The best thing about the future is that it comes only one day at a time.”
-Dean Acheson

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How to visit Wahclella Falls

Though hardly a secret anymore , the hike to Wahclella Falls remains a less traveled alternative to other short waterfall hikes in the Gorge. The trail is generally open year-round, though the best times for photography are in May/June, when spring greenery is at its peak, and in late October, when the bigleaf maples light up the forest with bright yellow and orange hues.

[Click here for a larger, printable version of this map]

This is a terrific family trail, thanks to several dramatic footbridges, two waterfalls, a staircase, caves (!) and several streamside spots safe for wading or skipping stones. Young kids should be kept close, however, since there are also some steep drop offs along sections of the trail. For kids, midweek in midsummer is a perfect time to visit.

Another fascinating time to visit with kids is during the fall spawning season, when the stream below the hatchery diversion dam is filled with returning salmon and steelhead within easy view of the trail.

Wahclella Falls is a family favorite

The trailhead for Wahclella Falls is easy to find. Follow I-84 east from Portland to Bonneville Dam (Exit 40), turning right at the first stop sign then immediately right into the trailhead parking area along Tanner Creek, where a Northwest Forest Pass is required. Portable toilets are provided at the trailhead from spring through early fall.

The trail begins at a gate at the south end of the parking area, and initially follows a rustic gavel road to a small diversion dam that provides water for the Bonneville Fish Hatchery. From here, the route crosses a footbridge in front of Munra Falls, and becomes a proper hiking path. Head right (downhill) at a fork in the trail 0.7 miles from the trailhead to begin the loop through the towering amphitheater surrounding Wahclella Falls, then retrace your steps 0.7 miles to the trailhead after completing the 0.6 mile loop portion of the trail. Enjoy!

After the Dollar Lake Fire

June 22, 2012July 11, 2012 / Tom Kloster / 15 Comments

The Dollar Lake Fire from Bald Butte on September 3, 2011

On August 26, 2011, a lightning strike ignited what was to become the Dollar Lake Fire, on Mount Hood’s rugged north side. The fire started in the Coe Branch canyon, just below the Elk Cove trail, and was spotted by numerous hikers.

Initially, it seemed small and manageable. But over the next few days and weeks, arid conditions and strong winds spread the fire from Stranahan Ridge on the east to Cathedral Ridge on the northwest side of the mountain, eventually consuming some 6,300 acres of high elevation forest. The blaze burned through September and into early October, when fall rains finally arrived.

Hot spot erupts along Stranahan Ridge on September 3, 2011

Some of the burn was of the beneficial form, a mosaic fire leaving islands of surviving trees, but much of the fire was too hot and the accumulated forest fuel too plentiful to prevent devastating crown fires from sweeping across the forest. Eventually, the fire destroyed most of the standing timber and burned the forest duff down to mineral soil throughout most of the burn area.

The fire was contained entirely within the Mount Hood Wilderness, thanks to the recent Clear Branch additions that expanded the wilderness boundary on the north to encompass the Clear Branch valley and the high country surrounding Owl Point, to the north. While this complicated fire fighting, it has also created a living laboratory for forest recovery, as the USFS is unlikely to assist the reforestation process inside the wilderness boundary. The Forest Service map, below, shows the broad extent of the fire.

Final extent of the Dollar Lake Fire (outlined in red)

Though the fire burned to the tree line in several spots, a surprising amount of terrain along the iconic Timberline Trail was somehow spared. While the burn touched Elk Cove and Cairn Basin, WyEast Basin and Barrett Spur are well beyond the burned area. The Clear Branch wilderness additions to the north were mostly spared, as well.

The New Vista Ridge: After the Fire

The following is a photo essay from my first visit to the burn, on June 22, 2012, and is the first in what will eventually be a series of articles on the aftermath of the fire.

The devastation left by the fire is awesome to witness, but also starkly beautiful when you consider the context of a forest fire. After all, this event is part of the natural rhythm of the forest just as much as the changing of seasons.

From this point forward, we will have a front-row seat to the miracle of life returning to the fire zone, much as we’ve watched life return to the Mount St. Helens blast zone over the past 32 years. And as my photos show, the rebirth of the forest ecosystem has already begun on Mount Hood’s northern slopes.

Untouched trailhead at Vista Ridge.

From the Vista Ridge trailhead, I followed the Vista Ridge Trail to the snow line, above about 5,000 feet. The Vista Ridge trailhead is completely untouched, though the fire swept through a vast area immediately to the south. Yet, no sign of the fire is evident at the trailhead marker (above).

A bit further up the trail, at the Old Vista Ridge trailhead, the fire zone comes into view. Where green forests existed last summer, browned foliage and a burned forest floor spread out east of the junction. This fringe of the fire is of the healthy “mosaic” form, sparing large trees, while clearing accumulated forest debris.

Old Vista Ridge trailhead spared by fire… just barely.

An unexpected benefit of the fire came last fall, when the USFS added the long-neglected Old Vista Ridge trail to official agency fire maps (below) released to the public. Volunteers began restoring this beautiful trail in 2007, but formal acknowledgement of the route on USFS maps is a welcome development.

Welcome development: Old Vista Ridge trail reappears on USFS fire fighting maps

Clearly, the restoration of the Old Vista Ridge trail helped fire fighters reach this area, and could have served as a fire line had the blaze swept north, across the Clear Branch. Hopefully this is an indication that the Old Vista Ridge trail will someday reappear on the USFS maintenance schedule, too.

Turning south on the Vista Ridge trail from the Old Vista Ridge junction, the wilderness registration box and map board seem to have received divine intervention from the fire — the blaze burned within a few feet of the signs, yet spared both. From here, the Vista Ridge trail abruptly leaves the scorched fringe of the fire, and heads into the most devastated areas.

Vista Ridge trail signs were spared… by divine guidance?

A few yards up the Vista Ridge trail, the devastation quickly intensifies.

From about the 4,700 foot level, the Dollar Lake Fire burned the forests along Vista Ridge to bare earth. In this area, the entire forest crowned, leaving only a scattering of surviving trees where protected by topography or sheer luck. Forest understory, woody debris and duff burned to mineral soil, leaving a slick, muddy surface of ash. For those who have hiked through the previous Bluegrass Fire or Gnarl Fire zones on the east slopes of Mount Hood, this eerie scene is familiar.

The surprisingly intact trail curves through the devastated forests along Vista Ridge.

Crown fires have killed almost all of the standing forests along Vista Ridge.

Amid the devastation in this hottest part of the Dollar Lake Fire, signs of life are already emerging. At this elevation, one of the toughest survivors is beargrass, a member of the lily family with a deep rhizome that allows plants to survive even the hottest fires. These plants are normally evergreen, but were completely scorched in the fire. The new grown in this photo (below) has emerged this spring.

Beargrass (Xerophyllum tenax) emerges from underground rhizomes protected from the fire.

Another surprise is avalanche lily, one of the more delicate flowers in the subalpine ecosystem. Like beargrass, these plants survive thanks to a bulb located deep enough in the soil to escape the heat of the fire. As one of the early bloomers in the mountain forests, these plants area already forming bright green carpets in the sea of fire devastation (below).

Avalanche Lily (Erythronium grandiflorum) emerging from the ashes.

A ribbon of green, these Avalanche Lilies are emerging along the Vista Ridge trail.

Another of the beneficial aspects of the fire comes into view a bit further up the trail: several sections of Vista Ridge had long been overgrown with thickets of overcrowded, stressed trees that were ripe for a burn.

Over the coming years, these areas are likely to evolve into beargrass and huckleberry meadows like those found at nearby Owl Point or along Zigzag Mountain, where fires have opened the landscape to sun-loving, early succession plants.

Unhealthy forest thickets cleared by fire — a beneficial outcome of the blaze.

One human artifact was uncovered by firefighters — a coil of what must be telephone cable (below). This is a first along the Vista Ridge trail, but makes sense given the insulators and cable found along the Old Vista Ridge trail.

It’s hard to know what this connected to, but on the north end, it served the old Perry Lake Guard Station and lookout, just east of Owl Point. It’s possible this line extended to the Bald Mountain lookout, though I have been unable to verify this on historic forest maps.

Telephone cable on Vista Ridge – gathered up and coiled by firefighters?

Though much of the devastation zone still consists of blackened trees and soil, some of the burned forest has begun to evolve into the uniquely attractive second phase. This happens when scorched bark peels away from trees to reveal the often beautiful, unburned wood beneath.

Soon, all of the trees in this forest will shed their bark. The skeletons of thousands of trees will emerge in colors of red, yellow and tan, then gradually fade to a bleached gray and white with time.

The burned trees of Vista Ridge are just beginning to shed their blackened bark, revealing beautiful trunks unscarred by the fire.

Mount Hood rises behind the new ghost forests of Vista Ridge

This second phase of the fire is helped along by winter snow. As the scene above shows, the freeze-thaw and compacting effects of the snow pack have already stripped many trees of their bark beneath the now-melted snowpack. Hot summer sun will continue this process, shrinking the remaining bark until it drops from the drying tree trunk.

This process of de-barking is the first in a post-fire sequence of events that will recycle much-needed organic matter to the forest floor. Twigs and tree limbs will soon fall, and over time, whole trees will begin to drop. This is a critical phase in stabilizing the forest soil, when low vegetation is still just beginning to re-establish in the fire zone.

Strips of tree bark are the first organic layer to accumulate on the floor of the burn zone.

The next few images show the extent of the Dollar Lake Fire, as viewed from Vista Ridge. To the east (below), The Pinnacle was mostly burned, but the fire somehow missed stand of trees just below the north summit.

These trees will play an important role in reforestation of the area, partly because so few trees survived the fire, but also because of their geographic location above the surrounding forest, where wind will widely scatter their seeds.

The Pinnacle, where a small grove of of trees on the north slope survived the fire.

To the south, the area above Elk Cove known as 99 Ridge (shown below) was partly spared, though the fire did scorch the east slopes of the ridge. From this side (to the west), the Timberline Trail corridor was almost completely spared. Ironically, Dollar Lake — the namesake for the fire — appears to have been spared, as well.

To the west of 99 Ridge, WyEast Basin was also spared, but the area along the Timberline Trail to the west of the basin, along the upper sections of Vista Ridge, was largely burned.

Forests along 99 Ridge were spared by the fire.

This panoramic view (below) encompasses the entire mid-section of the fire, from Stranahan Ridge on the horizon to Vista Ridge, on the right. This is a new viewpoint along a largely unnoticed rocky scarp on the east shoulder of Vista Ridge, now revealed thanks to the fire.

(Click here for a much larger panoramic view]

A Changed Landscape

Those who have explored Mount Hood’s north slopes over the years will surely mourn the loss of the beautiful forests of noble fir and mountain hemlock that once stood here — I certainly have. But this is also a chance to watch the ecosystem recover and restore itself over time, as it has for centuries. Among the surprising benefits are the new scenic vistas that are suddenly available, giving a bit more meaning to the name “Vista Ridge.”

The new views from Vista Ridge include Laurance Lake and Bald Butte, to the east.

By following the true ridge top of Vista Ridge, the new views extend east across Laurance Lake and the Clear Branch valley to Bald Butte and the Columbia Basin (above). Most of the area below the ridge is not burned, and this new perspective on the recent additions to the Mount Hood Wilderness is both unexpected and beautiful.

To the north, the new views include the rugged and little-known Owl Point area of the expanded Mount Hood Wilderness (reached by the Old Vista Ridge trail). Mount Adams rises in the distance, above the talus fields and meadows of Owl Point.

Owl Point and Mount Adams from newly revealed viewpoint on Vista Ridge.

This suddenly very scenic “true” ridge along the lower portion of Vista Ridge is easy enough to hike by simply following the ridge top where the existing trail heads into a narrow draw, about one-half mile from the Old Vista Ridge trail junction. It’s worth the visit if you’d like to inspect the scenery and Dollar Lake Fire up-close.

But in the spirit of recasting the Vista Ridge trail in the aftermath of the fire, and taking in these new views, now would be the perfect time to simply realign the trail along the ridge top. As shown on the map (below), this project could be done in a weekend by volunteers, if approved by the Forest Service.

(Click here for a larger map]

The fire has already done the heavy work of trail building by clearing the ground to mineral soil: designing and completing a realigned trail here would be quite straightforward. The slope of the ridge top, itself, is surprisingly gentle and would allow for an easy grade, similar to the current trail.

I hope to pitch this idea to the Forest Service, so if you’re interested in getting involved, watch the Portland Hikers forum for updates. That’s where volunteer work parties will be organized if there is interest from the USFS.

Until then, take the time to explore the fire zone, and watch the unfolding forest recovery firsthand. Visit the Portland Hikers Field Guide for directions to the Vista Ridge Trailhead.

10 Common Poison Oak Myths

May 28, 2012July 11, 2012 / Tom Kloster / 7 Comments

Spring in the Columbia River Gorge brings lush greens and a rainbow of wildflowers, but in this heavenly mix you will also find Toxicodendron diversilobum: Western poison oak.

If humans were as immune to the toxic oils of this plant as deer seem to be (they snack on the stuff!), we would simply admire it for the handsome foliage, and maybe even grow it in our gardens. After all, poison oak is an undeniably handsome plant… from a distance.

But instead, humans are prone to contact dermatitis when we encounter poison oak up-close, breaking out in itchy, blistering rashes that can take weeks to subside. Folklore on the cause and remedies for poison oak rash abound, and much of the information in this age of the internet is decidedly misleading.

Handsome devil: poison oak is as toxic as it is elegant.

Here are 10 common myths about poison oak — debunked — with information every hiker should know about this pesky plant:

Myth 1 – Many people are simply immune. I have hiked the poison oak-lined trails of the Columbia Gorge since the age of five, and thus have a 45-year streak of never reacting to it, despite some epic encounters. Am I immune? Maybe, but it turns out only about one-in-ten seem to have no reaction poison oak. Most of us who think we are immune have simply been careful enough — and lucky. If you have a perfect track record, assume it’s your reward for due caution, not immunity.

Myth 2 – Only the sap is toxic. Some believe it takes breaking a stem or crushing the leaves to release the toxic component of poison oak, a chemical called “urushiol” (pronounced “yoo-ROO-she-all”), and that simply brushing against it cannot transmit the toxin to your skin. In fact, urushiol is present throughout the plant, including the surface oils on the leaves and green stems of poision oak. This is especially true in spring, when new foliage literally glistens with toxic oils.

Poison oak usually looks like this in the Gorge: a spreading groundcover, 1-3 feet deep, and favoring open woods and forest margins.

Myth 3 – You’ll know you’ve got it by the next morning. While it takes only about 30 minutes for urushiol to penetrate your skin, the itchy, blistering skin reaction does not appear immediately. For most people, the symptoms are delayed at least 12 hours after exposure, and it usually takes up to 3 days for symptoms to appear — confounding hikers who think they’ve escaped a close encounter without consequence. For a first time sufferer, it generally takes even longer for the rash to appear – as much as 7 to 10 days!

Myth 4 – It takes a lot of exposure to cause a reaction. Poison oak is surprisingly toxic, and only a small amount of exposure can trigger a reaction. A single drop of urushiol on your skin contains more than enough toxin to cause a reaction, and a small amount is easily spread across your skin by perspiration or physical contact while you hike.

Myth 5 – Scratching will spread your rash. Scratching or rubbing a poison oak rash won’t make it spread to other parts of your body, assuming you’ve already washed thoroughly with soap and water. You can spread the rash if urushiol oil is still on your skin, of course. Scratching can lead to secondary skin infections, however, making your itchy misery a bit worse.

Poison oak is versatile, growing as a ground cover, shrub, or as a towering vine, as in this nightmarish scene along the McCord Creek trail.

Myth 6 – Breaking blisters will spread the rash. Breaking blisters won’t spread poison oak to other parts of your body, or other people. But open blisters can become infected and you may cause permanent scarring in the process. In very extreme cases, excessive fluid may need to be withdrawn by a doctor, though in most cases it’s best to simply let blisters heal on their own.

Myth 7 – Dead or leafless plants aren’t toxic. The bare winter stems of poison oak may look harmless, but still contain toxins. Urushiol oil has lasting power, and can stay active on any surface, including dead plants, for up to 5 years. Burning dead or dormant poison oak branches is an especially dangerous practice, as urushiol oils released in smoke can produce disastrous results, if inhaled.

Myth 8 – Dogs can’t get poison oak. Dogs are mostly protected from poison oak by their fur, though some can develop symptoms on their nose or underbelly. But all dogs can accumulate the oils on their fur, and transmit it to unwitting owners. This is especially true for off-leash dogs that might find a lush patch of poison oak just off the trail, but unseen by the dog’s owner.

The safest practice is to simply keep dogs on a leash when in poison oak country, so you know where they’ve been. Even better, give them a shampoo after the trip, as a precaution — or consider leaving Fido behind when you know you’re going to be in prolific poison oak country.

Poison oak growing in shrub form along the Rowena Plateau trail, showing the handsome bronze color of emerging leaves in spring — when the plant is especially toxic.

Myth 9 – You can develop immunity from exposure. False. With some 90% of humans allergic to urushiol, it’s only a matter of time before most of us will develop a reaction, and it turns out the more reactions you experience from exposure to urushiol, the more likely you are to react to with further exposure. But the reverse is also true: avoiding exposure (and outbreaks) reduces your susceptibility to a reaction. In other words, the myth has it backward: your best immunity comes from simply avoiding contact to begin with.

Sadly, the “develop your immunity” myth is among the more dangerous notions circulating on the internet, with countless testimonials on the “homeopathic” benefits of actually eating poison oak leaves in order to develop immunity. This is an incredibly foolhardy, dangerous idea that can lead to serious, life-threatening situations. Don’t even think about it!

Myth 10 – It’s just a rash. For most of us, this is true. But given the delayed (and varied) symptoms, poison oak reaction should always be taken seriously. As with any immune response to toxins, the symptoms can sometimes spiral out of control and become deadly. If you have a serious reaction, you need to see a doctor right away. Here are the American Academy of Dermatology guidelines for knowing if you’re having serious reaction:

• You should see a doctor if swelling persists, specially swelling that makes an eye swell shut or your face to swell.

• You should see a doctor if the rash covers a large part of your body, you have large blisters, or cannot sleep.

• If you have trouble breathing or swallowing, immediately go to an emergency room.

So, you’ve developed a rash from poison oak exposure, and it isn’t serious? Then you can treat it yourself. You can try one of these online resources for tips on managing your itchy journey ahead:

American Academy of Dermatology

Mayo Clinic

There are dozens of resources on the giving medical advice on treating poison oak rash, many with undocumented, anecdotal suggestions, so the best bet is to stick with these, or similarly respected clinical sources.

This impressive poison oak patch in the Viento area shows all three forms of the plant: groundcover, shrub and as a vine, climbing up the tree trunks.

Managing your Poison Oak exposure

The following hiking tips are adapted from recommendations by the American Academy of Dermatology and Mayo Clinic:

During your hike in poison oak country:

• If you are very sensitive, or heading into a lot of poison oak, consider one of the topical skin products containing bentoquatam, a non-prescription compound shown to protect the skin from absorbing urushiol.

• Wear long pants, long sleeves, boots, and gloves. Even when you apply a skin barrier that contains bentoquatam, you still need to cover your skin with clothing.

• Use hiking poles. They have the effect of keeping your hands up and in front of you, where you’re less likely to brush against poison oak.

• Keep your hands and arms away from your face.

• Rinse your skin right away with lukewarm water if you think you’ve been exposed. You may be able to rinse off the oil before the urushiol penetrates your skin.

Another view of an impressive patch of poison oak in the Viento area, growing in open Douglas fir forest.

After your hike in poison oak country:

• Take a shower — not a bath — with plenty of soap and lather.

• Wash all of the clothes you were wearing when you came into contact with poison oak with conventional laundry soap, set for two rinse cycles (if possible).

• Wash or wipe anything that may have urushiol oil on its surface with soap, including hiking poles, leashes, and your pet.

• Some hikers swear by Tecnu, an over-the-counter topical treatment for removing urushiol oils. Clinical tests show it to be somewhat more effective than plain soap, though neither a substitute for avoiding contact to begin with.

Learning to Recognize Poison Oak

Poison oak is easy to recognize: the old adage “leaves of three, let it be” applies, as poison oak generally has three leaflets per stem. With a bit of practice, you can learn to instantly recognize it as you hike, including the leafless stems in winter.

Here’s a close-up of the classic leaf shape (below), somewhat resembling an oak leaf, but with less pronounced lobes. In autumn, poison oak leaves take on striking hues of red and coral before dropping, leaving bare stems in winter. Note the tiny blossoms in the background — in summer, these will become clusters of greenish-white or tan berries.

Poison oak leaf detail: “Leaves of three, let it be..!”

Poison oak has several friends that it often grows with, and these plants can sometimes be confused with the real thing. They’re worth learning to identify, too, partly to know if you’ve been exposed to the real thing — but also because when you see these companion plants, you’re likely to be in poison oak habitat, and can keep an eye out for the genuine article.

One obvious example of a look-alike is the Oregon white oak (below), a classic companion of poison oak, and easily confused where brushy thickets of white oak grow in the eastern Columbia Gorge. Oak leaves are single, however, and usually larger with much deeper lobes than poison oak.

Oregon white oak can be confused with poison oak in the oak savannah country of the eastern Columbia River Gorge (courtesy PCC)

Another companion plant that is somewhat less common, but matches the “leaves of three” identifier is wild blackberry, or bramble (below). These plants are easily identified by their thorny, rambling stems that creep through the forest, small thorns on the underside of the leaves, and edible (and tasty) blackberries that form in summer.

Wild blackberry, or bramble, has “leaflets of three”, but is thorny, not smooth.

Still another companion plant that can be confused with poison oak is ocean spray, which prefers the same open woodland and forest margin habitat that poison oak enjoys. However, its leaves are single, and generally smaller than poison oak.

Ocean spray grows in dense clumps of arching stems, often reaching 8-10 feet in height. The name comes from “sprays” of hundreds of tiny, white blossoms in large clusters that cover plants in summer.

The leaves of ocean spray might initially look like poison oak, but are single and grow from a tall, arching thicket and have dramatic clusters of tiny white blossoms that give the plant its name.

Finally, snowberry is a companion plant of poison oak that normally has small, oval leaves, but in early spring grows larger, lobed leaves that can resemble poison oak at first glance. Snowberry can be identified by its thin, twiggy stems and white, inedible berries that give the plant its name. Most of its leaves are oval, and finely toothed, not lobed.

Early spring leaves on new growth are often exaggerated on snowberry, and can sometimes look like poison oak. The white berries on this plant distinguish it from the poison oak, and give the plant its name. In this view, the more typical oval leaves can bee seen in the background.

Where is Poison Oak Country?

Where can you expect to encounter poison oak? The answer is anywhere you might hike in the Gorge below an elevation of about 2,000 feet. It grows along most low-elevation trails throughout the Gorge, from Angels Rest on the west end to Dalles Mountain Ranch on the east.

Though the most prolific displays are east of Cascade Locks, you will find also lush bowers of poison oak draped over the rustic stone walls at Wahkeena Falls and Multnomah Falls, and along many sections of the popular Eagle Creek Trail (for Clackamas River hikers, it also grows in the lower canyon, under similar conditions).

Poison oak in early spring: new growth emerges in beautiful shades of copper, crimson and gold… though best appreciated from a distance!

The best bet is to assume its presence whenever hiking in the Gorge, and follow the simple precautions described in this article. It doesn’t have to ruin your hike: learning to recognize poison oak in its various forms is peace of mind, as you’ll be able to watch for it and manage your exposure with the knowledge that you know what you’re watching for.

Finally, if you’ve got small kids, there is no better way to teach them about plants than to start with identifying (and not touching!) poison oak. Print these photos of the plant (shown earlier in this article) for them to fold up and carry in a plastic sandwich bag on your next family hike:

(click here for a general view of poison oak)

(click here for a detailed view of the leaves)

It’s a great opportunity to teach young hikers to understand and respect nature, not fear it — and that goes for us grown-up hikers, too!

“Warren Falls, we’re ready for your close-up…”

May 20, 2012July 11, 2012 / Tom Kloster / 11 Comments

On May 12, Oregon Public Broadcasting’s popular Oregon Field Guide program travelled to the site of Warren Falls to film a story on the unique history of Warren Creek: the odd 1939 highway department project that silenced the falls, and the potential for restoring the falls to its former grandeur.

Michael Bendixen and Vince Patton on the chilly January trip to Warren Falls

This was the second trip to Warren Falls for Oregon Field Guide producer Vince Patton and videographer Michael Bendixen. Both had joined me for a first look at the area on a particularly icy January day last winter when the Gorge was at its worst — freezing rain and sleet over a crusty layer of snow.

Our May 12 trip would prove to be the welcome opposite: unseasonably warm, summerlike conditions, with trails lined with ferns and wildflowers instead of snow. Along for the trip were PortlandHikers.org friends Adam Sawyer and Jamie Chabot, and Kristen Stallman and Andy Johnson, representing the ODOT team that is steering the Historic Columbia River Highway restoration project.

(from left) Adam, me, Andy, Jamie, Kristen, Vince and Michael at the trailhead

We met at the Starvation Creek trailhead at 9 AM, and loaded up our packs with OPB gear before making the short hike to Warren Falls. Along the way, the OPB team shot a few trail scenes, but were interested in getting to Warren Falls and Hole-in-the-Wall Falls while the morning light lasted.

Vince and Michael working at the mighty basalt wall formed by Warren Falls

We soon reached the massive amphitheater created by Warren Falls, where the OPB crew filmed the haunting scene of the silenced waterfall, marked only by the trail of moss that marks where the waterfall once flowed. The group spent some time here discussing the strange project that diverted Warren Creek in 1939, and the mechanics of the diversion tunnel and accompany flume that has long since disappeared.

Warren Creek had overflowed Warren Falls several times over the course of our wet winter, and there were obvious signs that a large amount of water had coursed down the old streambed. But on this day, the stream was dry, with the eerie quiet that now exists here.

Michael filming at Hole-in-the-Wall Falls

We backtracked to Hole-in-the-Wall Falls for another session of shooting. Here, the rest of the group visited while Michael and Vince captured several angles of the odd, accidental waterfall.

Adam, Andy, Jamie & Kristen at Hole-in-the-Wall Falls

For a good look at the bypass tunnel that creates Hole-in-the-Wall Falls, we moved to the knoll above the footbridge. From this spot, it’s easy to imagine the wood flume that once attached to the tunnel exit and carried Warren Creek over the old highway and railroad, all the way to the Columbia River. Only when the old flume disappeared was today’s man-made falls created.

Pointing out the man-made features of the upper portion of Hole-in-the-Wall Falls

A wood flume originally connected to the tunnel opening, carrying Warren Creek over the old highway and to the Columbia

Next, we hiked up the Starvation Ridge Trail, heading for the brink of Warren Falls, and the huge steel weir at the head of the diversion tunnel.

The original plan was to scramble down Warren Creek from the Starvation Ridge Trail ford for the quarter mile of bushwhacking required to reach the brink of the falls. But Kristen had been to the diversion structure a few days earlier with an ODOT engineering crew, and they had found a faint boot path that dropped more directly from the Starvation Ridge Trail.

We voted on the two options at the Starvation Creek ford: wet feet and a rock hop along the stream or pushing through a hillside of poison oak along the boot path? The poison oak option won the day!

Weighing the alternative routes at the upper Warren Creek crossing

We backtracked to the jump-off point for the boot path, descended through a manageable patch of poison oak, and soon found ourselves curving around a steep, grassy bluff hanging directly above the 120-foot cliffs of Warren Falls.

From here, a dramatic view of the massive Warren Creek diversion structure suddenly came into view, and the OPB crew set up to shoot the scene.

Rounding the approach to the brink of Warren Falls

Michael shoots the diversion structure from the cliff top above Warren Falls

The diversion structure is much larger up-close than the historic drawings or a glimpse from below the falls would suggest. The tilted weir is made from sixty 20-foot steel beams laid across a 28-foot wide trench carved into the cliff. Beneath the mesh of steel rails, the trench leads directly to the bypass tunnel.

A close-up view reveals at least half the weir to be filled with loose rubble, to the extent that it is lush with a strange hanging garden of wildflowers, A thicket of willow has even become established in the upper right corner of the weir, suspended 15 feet above the diversion tunnel, below. The forces of nature are taking back Warren Creek Falls, slowly but surely.

Vince takes in the huge steel weir that covers the diversion tunnel opening, rushing directly below him

The up-close view also shows most of the beams to be twisted and buckled with the ravages of time, thanks to rocks and debris getting lodged between the beams, and the effects of freeze-thaw cycles in the harsh Gorge winters.

Still, the overall structure represents an amazing ingenuity of design and construction detail to have lasted 73 years, but is still functioning as intended. While nature is clearly winning this battle, the persistence of the diversion project is silent tribute to the designers and builders who created these structures in 1939.

Jamie exploring the steel weir from below — the top of Warren Falls is few feet beyond

Jamie peers through the weir into the opening of the diversion tunnel, directly below

Vince found an opening in the upper corner of the weir, and set up a compact camera mounted on a short arm to film the scene below

The OBP team used a compact video camera mounted on an arm to shoot under the weir. Vince found an opening at the upper west corner of the weir that gave access to the view from below the steel beams.

From this angle, Vince was shooting just below the upper edge of the weir, where a 15-foot rubble and masonry dam was constructed across the creek to elevate the angle of the weir structure toward Warren Falls. For 73 years, this design has allowed for loose debris to roll off the weir and over the natural falls, while filtering the waters of Warren Creek through the weir into the bypass tunnel that now forms Hole-in-the-Wall Falls.

Vince filming the tunnel below the weir with the compact camera

Next, we moved to the top of the weir, crossing to the upper east corner of the structure. The view from the top of the weir looking over the brink of Warren Falls is impressive, as is the view toward the Columbia River. From here, Dog Mountain fills the horizon across the river.

But the fact that the river can clearly be seen from the brink makes a good case that Warren Falls was one of the “four cascades caused by small streams falling from the mountainsides” in Captain William Clark’s journal entry of October 29, 1805. The other three were presumably the nearby falls on Starvation Creek, Cabin Creek and Lancaster Falls on Wonder Creek.

Looking down Warren Falls from the top of the weir

Dog Mountain dominates the view from the top of the Warren Creek diversion dam

The view from the top of the weir shows more wear and tear on the structure: the mortared lip of the rubble dam is badly weathered, fully exposing the ends of many of the 60 steel beams that connect to it, with only a rusty bolt anchoring them to the masonry wall.

Here, the decay of the diversion system seems to be moving close to structural failure — another argument for an orderly removal of the weir, and restoration of Warren Falls before it becomes impossible to safely do so.

Close-up of the top of the weir shows the wear-and-tear of 70 years

Vince and Michael planning the shoot from the top of the Warren Falls diversion dam

Jamie helps Michael set up at the top of the diversion structure

The group settled in for a lengthy shoot at the top of the falls, where Michael and Vince worked to capture the setting, and the rest of the group enjoyed the sylvan scene along Warren Creek.

Michael shooting from midstream, at the brink…

Michael posing for a certain Oregon Field Guide fan!

It’s a long drop: Michael shooting from the top of the diversion

The OPB crew wrapped up the day’s shooting with a few interviews and reflections of the group on the diversion project, and the future of Warren Falls. We soon packed up the video gear, and started up the canyon slope for the trail.

Adam shooting the OPB crew… shooting Warren Falls…

On the trip back to the trailhead, we ran into several groups of curious hikers, all familiar with Oregon Field Guide and excited to meet the crew.

One young woman asked what we were filming, and I explained the story to her — and asked her to go to Restore Warren Falls! on Facebook. Later, she approached me at the trailhead, and asked “Why are you focusing on this when there are so many global issues facing the world?”

Jamie muggles the geocache at Warren Falls. We signed it “Oregon Field Guide”

At the time I was somewhat startled, and replied that the project to restore the Historic Columbia River Highway provided a unique opportunity for funding the restoration of Warren Falls — a good argument, and one she seemed to accept. But I wish I’d simply said “We have to start somewhere, and right now, this is as good a place as any!”

“I wondered why somebody didn’t do something. Then I realized, I am somebody.”

~Author Unknown

(Special thanks to the Vince, Michael, Jamie, Adam, Andy and especially Kristen for another great day imagining the past and future Warren Falls)

___________________________

Previous articles on restoring Warren Falls:

Restoring Warren Falls
Warren Falls Lives! (temporarily, at least)
Warren Falls Mystery… Solved!
Warren Falls Solutions
Warren Falls Lives… Again?

Restore Warren Falls! on Facebook

Parkdale Lava Flow Revealed

April 28, 2012July 11, 2012 / Tom Kloster / 7 Comments

The new LIDAR data viewer created by Oregon’s Department of Geology and Mineral Industries (DOGAMI) offers a fascinating new look at familiar features in the Mount Hood region. This article focuses on the Parkdale Lava Flow, one of the formations where LIDAR offers an especially striking new look at the geologic story.

Four sections of the Parkdale flow (shown on the index map, below) are the focus of the article.

(for a larger LIDAR view of the entire flow, click here)

The Parkdale lava is of the A’a’ variety (pronounced “ah-ah”), characterized by a thick, pasty molten core carrying hardened chunks of cooled lava on its surface like a crusty skin. This floating skin of jagged, solidified rocks echoes the movement of the underlying flow, thus creating the flow lines. The LIDAR imagery beautifully illustrates these characteristics of an A’a’ flow, including the tall, steep edges of the flow that result from this dense, slow-moving form of lava.

Starting on the north end, at the toe of the Parkdale flow (Map A, below), the LIDAR imagery reveals the flow lines in the once-molten rock in great detail, when compared to traditional maps and air photos. Though the flow was generally heading downhill (the underlying valley floor drops about 250 feet per mile in this area), LIDAR shows it was spreading out, too, as evidenced in the many secondary lobes that formed at the terminus of the flow.

The gentle slope of the open valley floor was responsible for the broad toe of the lava flow, which spread out in the shape of a hand (or paw?) once it emerged from the confining canyon walls of the Middle Fork canyon.

In this lowest extent of the flow, it’s also clear that the lava covered most of the Middle Fork flood plain. Below the flow, the flood area averages about one-third mile in width, but where the channel along the west side of the lava flow, it measures only a out one-tenth of a mile in width.

Moving south to the middle of the Parkdale flow (Map B, below), the LIDAR image shows a powerful, quarter-mile wide stream of lava pushing down a channel at the center of the flow. This main channel also has well defined levees of solidified lava along its margins, a common feature on the more liquid Pahoehoe (pronounced pa-HOI-hoi) form of lava, but less so with the viscous A’a’ lava that makes up the Parkdale formation. More on that point, below.

This view also shows the first lateral lobes, splitting off the main flow as the molten lava reached the open floor of the Upper Hood River Valley, and where the volume of lava overtopped or burst through the levees along the main channel.

The view in Map B, above, also shows how the Parkdale flow pushed the Middle Fork Hood River against the foot of Blue Ridge, to the west. The oversteepened slopes along the west margin of the stream (shown as a distinct shadow) are the result of the Middle Fork continuing to cut away at the base of Blue Ridge, some 7,000 years after the lava flow formed.

Another view of the mid-section of the Parkdale flow (Map C, below) shows fascinating features along the west margin of the formation. Here, a lobe of lava pushed laterally (left) and uphill into the side canyon of Bear Creek, permanently diverting the Middle Fork Hood River in the process.

Molten lava on this scale would have instantly vaporized the Middle Fork as it flowed down valley. But LIDAR shows terraces in stream sediments along Bear Creek near the base of this lobe, suggesting that for some period after the lava cooled, the Middle Fork was backed up, forming a lake. The map below shows what a lake might have looked like, assuming a lava dam formed downstream where the main flow pushed the river high against the slopes of Blue Ridge, creating a 150-foot dam.

The resulting lake might have covered 40 acres and been more than 100 feet deep. The terraces in sediments along Bear Creek suggest the lake existed long enough for a few feet of debris to collect before the Middle Fork cut a path around the lava dam, and allowed Bear Creek to cut through the new layer of sediments.

Did a lava dam create an ancient lake at Bear Creek?

(Click here for a larger map)

The new LIDAR imagery is most interesting at the south end of the Parkdale flow (Map D, below), at the source of the lava. The LIDAR images clearly confirm a single, crescent-shaped volcanic dome that has long been suggested by surveyed contours on USGS topographic maps.

This area is now mostly forested, so the detail provided by LIDAR is the first good look at the radial spread of volcanic material from the vent, initially as more of a mound or cone. As the scale of the eruption grew, a massive stream of molten rock emerged from the north flank of the vent, and began to flow north and downhill, following the broad Middle Fork valley.

The eruption must have been a spectacular event, likely setting off forest fires and impressive steam explosions as the Middle Fork was pushed from its riverbed. It was almost certainly witnessed by Indians living along the Columbia River at the time — perhaps from somewhere in the Hood River Valley, even? It would have been a startling sight, especially at night, and could have lasted from a few days to a few weeks.

The LIDAR images of the vent area also make it easier to imagine the mechanics of the main lava flow. The flow lines on this portion of the flow curve upstream near the vent, as opposed to downstream for most of the flow, a pattern supported by elevation contours: in other words, the upper portion of the flow is concave, or slightly sunken, while the lower flow is convex, or arched upward.

This pattern results from the upper part of the flow deflating as the supply of new lava from the vent subsided, and some of the molten core of the lava flow drained back into the vent, while the rest continued to move downhill under the partially solidified skin. Thus, the upper part of the flow flattened out like a deflated balloon, reversing the flow lines in this section as the skin of solidified lava pulled backward against the hardened levees at the edge of the flow. The effect can be seen in the thickness of the flow: at the toe, the bulging lava flow is upwards of 200 feet thick, whereas the sagging upper portions are less than 100 feet thick near the source.

An analogy for this phenomenon is to half-fill a tube-shaped balloon with water, lay it on a plank, then gradually lift one end of the plank. The effect would be a pooling of water and rounding of the balloon at the low end, and a flattened balloon at the high end. This is how the flow dynamics of the Parkdale Lava Flow unfolded 7,000 years ago.

USGS maps have long suggested a volcanic dome at the head of the Parkdale Lava Flow (marked as point 2825)

As mentioned earlier, the main flow channel of the Parkdale Lava flow has many lateral levees of hardened rock that are more typical of Pahoehoe lava, and yet the rock that makes up the Parkdale flow is clearly of the A’a’ variety. Why was this A’a’ flow comparatively liquid compared to nearby lava flows at Mt. Adams and Indian Heaven, for example?

One reason is suggested in a recent Oregon State University study that shows Mount Hood to have a less explosive personality than most of the other volcano giants of the Cascade Range. Scientists now believe that regular mixing of magma inside the volcano produces a less viscous, less explosive lava than most of Mount Hood’s volcanic neighbors. This research might explain the fluidity of the Parkdale flow, as well.

Fire and Ice?

The new LIDAR images of the Parkdale flow beautifully illustrate how the eruption filled the broad glacial valley of the Middle Fork Hood River from edge-to-edge with lava. Because scientists have dated the flow to about 7,000 years ago, it clearly formed after the end of the Fraser Era glaciation, which ended about 10,000 years ago.

This means the Parkdale flow most likely erupted in the U-shaped valley left behind by the ancestral Coe glacier — a once massive river of ice that included arms reaching into the Eliot Branch, Pinnacle Creek and Clear Branch valleys, as well as the Coe Branch valley, proper. Though intriguing to imagine a volcanic event emerging beneath an ice-age glacier, the glaciers at the time of the Parkdale flow were more like the modern versions we see today on the north face of Mount Hood, high above their ice age extent.

Fire and ice… but not at the same time.

(Click here for larger map)

Though fire and ice did not co-exist here, the path left by ice age glaciers clearly shaped the Parkdale flow. The full extent of the ancestral Coe Glacier is difficult to estimate, partly because the Parkdale Flow has covered the floor of the valley created by the glacier. But the long, straight path of the Parkdale flow clearly follows flat, even terrain that is the hallmark of a glacial valley.

Another possibility is that the formation of the glacial valley, itself, might have triggered a lava eruption after the ice retreated, having carved a low spot where underlying magma could find its way to the surface. That could help explain the flow emerging from this spot on the mountain, far from the active volcanic vents on Mount Hood.

Fire, ice and more than coincidence that a volcanic vent emerged here?

(Click here for larger map)

Equally puzzling in this area is the gap leading to the Evans Creek drainage (marked with “?” on the map, above), which has all the features of a glacial valley, but is separated by a low, 150-foot high saddle from the main Middle Fork valley. Hopefully, the LIDAR imagery will help geoscientists untangle the mystery of these landforms.

LIDAR Art

The striking Parkdale Lava Flow caught the eye of cartographic artist Daniel Coe, and you can pick up his colorized interpretations of LIDAR imagery from the State of Oregon. Coe’s take on Mount Hood and the Parkdale Lava Flow is available in this poster form:

The poster image is also available as a postcard, along with this closer view of the flow:

To purchase these beautiful images, go to the DOGAMI website, and select from the posters and postcards.

To surf the LIDAR imagery yourself, go to the DOGAMI website, and launch the LIDAR Viewer.

Yocum Ridge Waterfalls

March 31, 2012July 20, 2020 / Tom Kloster / 4 Comments

Scores of little-known waterfalls hide in Mount Hood’s backcountry. Some are towering glacial torrents, while others are quiet forest cascades, framed in moss and maple leaves. But when conditions are right, few rival the towering trio of waterfalls that mark peak snowmelt on the upper ramparts of Yocum Ridge.

These waterfalls are unnamed and unmapped, but familiar to hikers crossing the Muddy Fork on the Timberline Trail or visiting McNeil Point, across the canyon. They completely disappear by autumn in dry years, but in early summer, they are Mount Hood’s roaring counterparts to the famous seasonal giants of Yosemite.

(Click here for a larger view)

These waterfalls originate from an unnamed glacial cirque, or bowl, high on the northern shoulder of Yocum Ridge, the massive spine that divides the Muddy Fork from the Sandy River, and extends to the summit of Mount Hood. Though they flow from a relatively small basin, the snowfields that accumulate in the cirque each winter generate a surprisingly powerful runoff.

In recent decades, the year-round snowfields in the basin have almost disappeared, compared to 1960s-vintage USGS maps (below). This seems to have opened a more direct snowmelt channel to the waterfalls, as they seem more prominent in recent years, while the perennial stream to the west, as shown on the USGS maps, has become much less prominent.

(Click here for a larger view)

The cirque is well below the tree line, so the lack of forests in this amphitheater is also a good indicator of both heavy snow accumulations and frequent winter avalanches.

The view (below) from across the canyon shows the waterfalls in relation to Yocum Ridge and the cirque. The low ridge to the right of the falls forms a lower cusp of the cirque, and this ridge serves as a dike that channels most of the spring runoff toward the waterfalls. The Yocum Ridge Trail (shown on the map, above) terminates at the rim of the cirque, in the extreme upper right corner of this view:

A closer look at the waterfalls, as viewed from below at the Muddy Fork crossing (below), shows the rugged upper crags of Yocum Ridge in the background, with the waterfalls tumbling from the cirque into the Muddy Fork canyon. The cirque is located to the right, just outside this frame.

Surprisingly, a sizeable forest is perched on the slopes to the left of the waterfalls, apparently spared by the most frequent avalanches that have cleared most of the slopes within the cirque.

(Click here for a larger view)

It’s somewhat unknown how the streams that feed these waterfalls originate, since they are not mapped, and perhaps not even explored. However, from Google Earth imagery, the trio of waterfalls seem to flow from three distinct sources, with the western falls draining the main portion of the cirque, and the middle and east segments draining directly off the upper slopes of Yocum Ridge.

A closer view (below) shows the trio of waterfalls in detail. The westernmost of the three (on the right) is by far the largest, dropping at least 700 feet in the main cascade, and arguably nearly 800 overall. This drop is on a scale with Multnomah Falls, which drops a total of 635 feet, by comparison.

The eastern segment (on the left) is next in size, and though dwarfed by its larger sister to the west, is quite large and drops at least 500 feet. The middle segment is a tall, thin slide that is nearly as tall as the western segment, albeit much less dramatic.

The towering western falls (left) starts out as a 100-foot slide, and quickly fans out for 150 feet before leaping over a wide, 400-foot plunge.

The falls collects in a steep amphitheater at the base of the main plunge before making a final 70-foot plunge into a roiling, narrow gorge.

A closer look at the main plunge of the western falls (below) reveals the raw power at work during peak snowmelt, with its roaring curtains of falling water.

Somehow, thickets of red alder cling to the cliffs around the falls, framing the scene. This spectacle persists for several weeks in early summer, yet nearly disappears in autumn and through the winter.

The following video captures this dramatic scene, as viewed from the Muddy Fork crossing on the Timberline Trail in July 2010:

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How to visit the Waterfalls

Viewing the Yocum Ridge Waterfalls up close makes for a terrific day hike, and the waterfalls are at their prime as soon as the trails open — usually late June or July. The recommended 5.4 mile (round-trip) hike shown on the map below starts at the usually crowded Top Spur Trailhead, near Lolo Pass. But most of the hikers are heading for McNeil Point, so you will see very few people beyond the series of junctions at Bald Mountain.

(Click here for a larger, printable map)

Starting at Top Spur, the trail climbs somewhat steeply for 0.4 to a signed junction with the Pacific Crest Trail (PCT). Turn right onto the PCT, and immediately reach a confusing 4-way junction with the Timberline Trail. Turn right onto the famed Timberline Trail, heading uphill and to the right, past a sign pointing to the Muddy Fork

The Timberline Trail climbs gently through noble fir forest, soon passing the unmarked junction with the Bald Mountain trail. A short distance beyond, the trail traverses across the steep meadows on the south face of Bald Mountain, with stunning views of Mount Hood and the Muddy Fork canyon.

Mount Hood and the Muddy Fork canyon from Bald Mountain

After re-entering the forest, the trail passes yet another junction, this time with the unsigned Bald Mountain Cutoff. Head straight, going through a log gate before making a very gradual descent to the Muddy Fork.

Once at the Muddy Fork, the trail enters the scene of a violent debris flow that crashed through the area in 2002, snapping thousands of mature trees like match sticks and pouring 20 feet of debris across the valley floor.

The Muddy Fork has made short work of the debris in the subsequent 10 years, cutting all the way down to its former stream level. This makes crossing difficult for Timberline Trail hikers, but that’s okay: the best view of the Yocum Ridge waterfalls is from one of the scores of boulders resting atop the debris flow, where you can relax and take in Mount Hood, the waterfalls and the roaring Muddy Fork, below.

Be sure to bring binoculars and a camera — and enjoy!

Warren Falls Lives… Again?

March 28, 2012November 27, 2016 / Tom Kloster / 2 Comments

March 16 was a good day for Warren Falls: in the morning, the Historic Columbia River Highway Advisory Committee (AC) allowed me time on their agenda for a second pitch to restore Warren Falls as part of the larger historic highway trail project. After the meeting, I visited Warren Falls and was able to capture it flowing, thanks to the unusually heavy rain we had experienced in early March. Here are the highlights:

HCRC Advisory Committee

Last summer, I made a pitch to the HCRC Advisory Committee (AC) to restore Warren Falls as part of the highway restoration project, and in my second appearance, was able to provide a much more polished case. The members of the AC were engaged and clearly interested in the idea, asking many questions after the presentation. However, they are also constrained by the tight budget and timeline they are working under to complete the highway restoration by the 2016 centennial of Samuel Lancaster’s “King of Roads.”

The HCRH trail design already includes a short trail and overlook at Warren Falls

The AC chair sent me a follow-up message after the meeting offering support for all of the proposals I had laid out at the meeting — except restoration of Warren Falls itself. While that last part was disappointing, it was helpful to at least have a sense of where the AC stood on the issue, since I can now focus efforts on finding the needed funding and perhaps a project partner for ODOT to pull off the Warren Falls restoration.

The good news is the AC is supportive of several accompanying proposals that I laid out in the presentation, including:

• designing the crossing of the original Warren Creek channel to resemble a “bridge” so that there will be a place for an interpretive panel describing the history of the area

• addition of a side trail to the original Warren Falls with an interpretive panel – albeit, with “volunteer work”

• Enhancing fish habitat downstream of Hole-in-the-Wall Falls as a proposed mitigation action related to construction of the next (unfunded) trail segment west of the Starvation-Lindsey segment currently being designed

• removal of invasive species in the area – mostly, English ivy, Himalayan blackberry and Scots broom.

So, despite the disappointment of not adding the falls restoration to the current ODOT project, the list of related restoration work supported by the AC is a big step forward. In their words, the AC is “supportive of [the] idea to bring water back to the original waterfall, but given our charge, we cannot offer any monetary or construction assistance”. A partial victory, to be sure, but also a challenge to help ODOT find funding for the Warren Falls restoration.

This historic streambed of Warren Creek, now permanently cut off from the stream, could have a “bridge-like” crossing and an interpretive sign describing the area history.

An interesting footnote to the meeting was a conversation I had afterward with a reader of this blog who had watched the presentation, and thought a much simpler solution was possible for restoring Warren Falls: simply pull out the “trash rack” grate, and let Warren Creek do the rest. The stream would surely plug the tunnel with debris and gradually start flowing over its original falls without an elaborate engineering solution for retiring the tunnel.

It’s a temptingly simple idea, and came from a person with a professional background as a hydrologist, no less. So, that scaled-back option will be my starting point as I look for additional funding for bringing back Warren Falls.

Warren Falls Lives!

After the HCRH Advisory Committee presentation, I bolted for the Starvation Creek trailhead, with a strong hunch that Warren Falls would be flowing that day. Despite the bright, blue skies on March 16, the previous week had seen an unusually cold and wet weather pattern, and the gorge waterfalls visible from the highway were roaring.

As hoped, when I arrived at Hole-in-the-Wall Falls, part of Warren Creek was flowing down the normally dry channel that leads to Warren Falls. I captured the following video as I walked along the temporary stream, then rounded a corner to find water flowing over Warren Falls, once again. Warren Falls lives!

As with previous visits when Warren Falls was flowing, the experience was magical. Instead of hearing the echoes of trucks on I-84 in the dry amphitheater surrounding the falls, I could hear only the sound of Warren Creek — or the overflowing part of it, at least — cascading over the 120-foot brink of the falls, then splashing down the normally dry streambed to the point where it re-joins the main stream of Warren Creek, at Hole-in-the-Wall Falls.

This clip marks the moment when a large rock came over the falls, in the background… CRACK!

The video still image, above, marks a somewhat jarring moment on this visit, however: if you listen closely at 0:47 you can hear a CRACK! in the background, then an abrupt end to that clip in the video. This is the sound of a soccer ball-sized rock coming over the top of the falls — just as designed — and landing in the debris pile near the base. It was not only startling to hear this, but also a bit ominous, considering that on previous visits I had been standing at the base of the falls shooting video and still photos. If you visit when Warren Falls is flowing, please don’t stand near the base of the falls!

Finally, there was a pleasant surprise on the way out that day. For some reason I had never noticed, but the USFS trailhead sign at Starvation Creek (pictured at the top of this article) actually lists Warren Falls as a destination! Clearly, the Forest Service meant Hole-in-the-Wall Falls, but I choose to look upon the sign as a good omen that the real Warren Falls will be restored!

Friends for Warren Falls

My month of Warren Falls adventures continued on March 25, when I guided a Friends of the Gorge hike on a tour of the Starvation-area waterfalls, including a visit to Warren Falls. At 24 hikers, the group was by far the largest I have led to the falls site!

Friends of the Gorge hike visits the site of Warren Falls

Warren Falls was once again dry on this visit, but the group was fascinated by the odd history of the diversion project, the obvious signs that Warren Falls had recently flowed, and the magnificence of the massive basalt amphitheater that frames the falls.

Restore Warren Falls on Facebook

I’ve had many people ask how they can support the effort to restore Warren Falls. In response, I have finally set up a Facebook page for people to track progress on the project and vote their support for the idea:

Warren Falls on Facebook

You can help out by stopping by the Facebook page, like it, and then forward the web link to like-minded friends. If the project picks up enough “likes”, it will help me make the case to ODOT and elected officials that popular support exists for the project.

Thanks go out to those who have already stopped by the Facebook page, and thanks, especially, to Scott Cook for speaking out in support of Warren Falls at both HCRH Advisory Committee meetings — very much appreciated, Scott!

Please watch the Warren Falls page on Facebook for more updates on the project as the it unfolds over the next several months.

Warren Falls Solutions

February 27, 2012July 11, 2012 / Tom Kloster / 2 Comments

The strange history of Warren Falls began shortly after completion of the Historic Columbia River Highway in the 1920s, when unruly Warren Creek repeatedly pushed debris against the modest new highway bridge that spanned the stream.

The first Warren Creek bridge was replaced as part of the waterfall diversion; no photos of the original structure survive

Oregon highway engineers subsequently diverted the creek in 1939 through a bizarre tunnel that survives to this day. The diversion created today’s manmade Hole-in-the-Wall Falls when an accompanying flume was removed sometime in the early 1960s, leaving an eerie, dry cliff where Warren Falls once thundered.

This article proposes a few solutions for restoring Warren Falls to its former glory in tandem with the ongoing ODOT project to restore the Historic Columbia River Highway.

Option A: Let Nature Take Her Course

The simplest solution for restoring Warren Falls is to simply wait for the “trash rack” diversion structure to rust away, eventually collapsing into the tunnel intake under the weight of a heavy winter flood or debris flow. Surprisingly, this hasn’t already happened over the 73-year life of the diversion project, but it is inevitable.

Debris flows periodically clog the brink of Oneonta Falls; a similar event is inevitable at Warren Falls

This is the least desirable option because it leaves the maintenance and safety liability of the diversion tunnel in ODOT’s hands, and the removal of obsolete structures to chance. The dry falls and diversion tunnel are visited regularly by curious hikers, canyoneers and rock climbers, so the unresolved safety liability the tunnel presents for ODOT is quite real.

Option B: A Large Cork

Short of waiting for the “trash rack” diversion structure to collapse on its own, the simplest option for restoring Warren Falls is to cork the tunnel intake. A vault carved like a rocky bathtub into the bedrock brink of the falls forms the tunnel intake, and provides for the “cork” solution.

Though the metal “trash rack” covers an opening of roughly 20×20 feet square, the rock vault is tapered in a v-shape, narrowing to the 5 foot width of the tunnel at the bottom of the vault. The “cork” would be a series of stacked basalt columns filling the vault and blocking the bypass tunnel opening. Approximately twenty 6-foot columns, each about 18 inches in diameter would do the job.

The 1939 construction drawings for the diversion project show the v-shaped vault carved into the lip of Warren Falls, leading to the diversion tunnel (cross-section view)

Mother Nature would provide the assist for this solution once the basalt columns are in place, with the hydraulic force of Warren Creek filling the spaces between columns with fine gravels and sediment over time. Eventually, the voids between the columns would fill completely, plugging the bypass tunnel to all but a small amount of seepage.

The lower end of the corked bypass tunnel would also be covered with a protective grate to prevent curious explorers from entering, just as a number of lava tubes in Oregon have been gated to public access. The bonus? A very large, secured bat cave is created in the process!

A stack of basalt columns like these would form the “cork” that plugs the bypass tunnel forever (Wikipedia)

How would the basalt columns get up there? The best plan would be an air crane, as the rock columns would be comparable in size and weight to the timber loads that are routinely lifted in Oregon’s helicopter logging operations.

ODOT maintains an open maintenance field just a few hundred yards from the falls site, with direct freeway access for delivering the columns to a staging area. On-the-ground workers could access the top of the falls from the Starvation Ridge Trail, but a mechanical lift from the base of the falls would be more practical.

Option C: Colossal Dental Work

The third option is the best plan for fully restoring Warren Falls to near-natural conditions. This design would “fill the cavity” of the entire bypass tunnel, permanently.

Construction detail of the lip of the masonry dam that supports the “trash rack” (cross-section view)

This solution uses the original masonry dam at the head of the bypass tunnel to temporarily pipe Warren Creek over the natural falls during the construction phase, allowing for concrete work to proceed within the bypass tunnel.

The tunnel would be plugged in two steps. First, a reinforced concrete plug would be poured at the lower opening of the bypass tunnel, sealing the tunnel exit. The plug would be disguised on the outside to match the color and texture of the basalt cliff.

Next, the rest of the tunnel would be filled with mixture of concrete and rock cobbles — roughly 100 cubic yards worth. Once the tunnel “cavity” is filled, the vault at the top of the falls would be filled with basalt columns, using the same method described in the “cork” scenario. In this case, they could be mortared in place, since this approach would already have concrete pouring equipment on site.

Wanted: dentist with masonry skills and a helicopter pilot license… (photo: Zach Forsyth)

The “dental work” option has the benefit of stabilizing basalt cliffs that form the western wall of Warren Falls by permanently filling the man-made cavity behind them. This option allows ODOT to walk away from the Warren Tunnel site forever, with almost no trace of the old stream diversion left behind.

How would ODOT move the concrete and rock to the top of the falls? Fortunately, much has changed since the tunnel was originally created, and today there is portable equipment specifically designed for the task.

First up is a truck-mounted concrete pump, normally used for precision pouring in building construction, but increasingly used to minimize environmental impacts at construction sites.

This truck-mounted concrete pump would easily reach the top of Warren Falls (Wikipedia)

Moving rock to the top of the falls would be a bit more cumbersome, but could employ a portable rock conveyor. These are widely used in commercial aggregate operations, and could conceivably be used at the Warren Falls site. A low-budget alternative is to us rock from Warren Creek’s streambed above the falls.

Moving heavy equipment to the site would drive up the cost of restoring Warren Falls, so the “dental work” option for completely decommissioning the old tunnel is probably the least viable alternative, given funding constraints. But it’s also possible that ODOT will already have equipment required to do the job in the area as part of the project to restore the historic highway.

A telescoping rock conveyor could be the solution for loading aggregate into the Warren Tunnel (Wikipedia)

Next Steps?

Why link restoration of Warren Falls to the Historic Columbia River Highway project? The answer lies in the intertwined history of the falls and the highway department: now is the time for ODOT to undo an unfortunate environmental travesty from another era.

The historic Columbia River Highway restoration project provides a once-in-a-lifetime opportunity to provide the resources needed to restore the falls. It also allows ODOT to demonstrate how much highway planning has evolved since the diversion project was conceived, more than 70 years ago.

I will be making another pitch to restore Warren Falls at the Historic Columbia River Highway advisory committee meeting on March 16 (in Hood River). Hopefully, I’ll be able to capture the imagination of the citizens and ODOT staff charged with returning the old highway to its former glory, and make the case that restoring Warren Falls ought to be part of the larger restoration effort.

More to come…

Warren Falls Mystery… Solved!

January 31, 2012July 11, 2012 / Tom Kloster / 1 Comment

(Click here for a larger view)

It was the summer of 1939, and Depression-era Americans were escaping the hard times with the theater releases of “Gone with the Wind” and “The Wizard of Oz”. In Europe, Hitler’s invasion of Poland in September of 1939 ignited World War II.

Against the sweeping backdrop of this pivotal year in history, a odd story was playing out on obscure Warren Creek, near Hood River in the Columbia River Gorge. This is the story of how today’s manmade Hole-in-the-Wall Falls was created, and Warren Falls was (temporarily, at least) lost to time. It all began 15,000 years ago…

15,000 Years Ago – The string of waterfalls on Warren Creek were formed as a result of the Bretz Floods. Also known as the Missoula Floods, these were a cataclysmic series of bursts from glacial Lake Missoula that scoured out the Columbia River Gorge over a 2,000 year span. The events finally ended with the ice age, about 13,000 years ago.

J. Harlen Bretz faced decades of controversy before his flood theory was accepted

Today’s rugged cliffs in the Columbia Gorge were over-steepened by the Bretz floods, leaving tributary streams like Warren Creek cascading down the layers of sheer, exposed basalt bedrock. Geologist J. Harlen Bretz published his theory describing the great floods in 1923, just a few years before Warren Falls would be diverted from its natural channel.

June 6, 1916 – Samuel Lancaster’s Columbia River Highway is dedicated, and immediately hailed as one of the pre-eminent roadway engineering feats in the world. The spectacular new road brings a stream of touring cars into the Gorge for the first time, with Portlanders marveling at the new road and stunning scenery.

Samuel Lancaster touring his beautiful new highway in 1916

Lancaster’s new highway passed Warren Falls under what is now I-84, crossing Warren Creek on a small bridge, and passing two homesteads, a small restaurant and service station that were once located near the falls. Today, this section of the old road is about to be restored as a multi-use path as part of the Historic Columbia River Highway project.

July 29, 1939 – Robert H. “Sam” Baldock is midway through his 24-year tenure as Oregon State Highway Engineer (1932-1956), an influential career spanning the formative era of the nation’s interstate highway era. Baldock advocated for the construction of what would eventually become I-84 in the Columbia Gorge, initially built as a “straightened” US 30 that bypassed or obliterated Samuel Lancaster’s visionary Columbia River.

Thirties-era Chiefs: Oregon Highway Engineer Sam Baldock (left) and Assistant Highway Engineer Conde B. McCullough (right)

In a letter to the Union Pacific Railroad, Baldock describes an ingenious “trash rack” and bypass tunnel at Warren Falls that had just been released to bid, on July 27. The project was designed to address an ongoing maintenance problem where Warren Creek had repeatedly clogged the openings on the old highway and railroad bridges with rock and log debris.

While the Baldock proposal for Warren Creek seems a brutal affront to nature by today’s standards, an irony in this bit of history is that his assistant highway engineer was none other than Conde B. McCullogh, the legendary bridge designer whose iconic bridges define the Oregon Coast Highway.

McCullough designed several bridges along the Columbia River Highway, as well, yet he apparently passed on the opportunity to apply a more elegant design solution to the Warren Creek flooding problem. Otherwise, we might have an intact Warren Falls today, perhaps graced by another historic bridge or viaduct in the McCullough tradition!

Historic site map of the Warren Falls diversion project (1939)

(Click here for a larger view of this map)

At the time of the Warren Falls diversion project, the railroad was located adjacent to the highway (it was later moved onto fill in the Columbia River when the modern I-84 alignment was built in the 1950s).

The Union Pacific had already attempted to address the Warren Creek issue with a flume built to carry the stream over the railroad and away from the railroad bridge. This initial effort by the railroad appears to have been the catalyst for a joint project with ODOT to build an even larger diversion.

This map blends historic information from ODOT site plans with the modern-day location of Warren Creek.

(Click here for a larger view of this map)

August 10, 1939 – Union Pacific Railroad Resident Engineer S. Murray responds to Baldock’s July 29 letter, praising the “trash rack” and tunnel design solution, but also offering an alternative approach to the tunnel scheme:

“I think possibly we have all approached this problem from the reverse end. Above the falls there is a deposit of gravel about 600 feet long and of varying widths and depths, and possibly there are 10,000 yards of it ready to move.

Would it not be practicable and sensible to simply hoist a cat up the cliff and into the canyon and push this material down over the falls and then away from the course of the water, and then construct a small barrier of creosoted timber so as to hold back future deposits until they accumulate in sufficient amount to justify their being moved again?”

In the letter, Murray suggests that Baldock’s Highway Department do a comparative cost analysis of this alternative, as he expected to “have difficulty in obtaining approval” of the Union Pacific’s participation in the project “under [the] present railroad financial situation.”

The Union Pacific proposed hoisting a bulldozer like this one to the top of Warren Falls and using it to push debris over the brink!

August 30, 1939 – In his response to Murray, Sam Baldock declines to consider the counter proposal to simply bulldoze the debris above Warren Falls as an alternative to the tunnel project, and instead, continues advancing a $14,896.27 construction contract to complete the diversion project for Warren Creek.

September 2, 1939 – Murray responds immediately to Baldock’s August 30 letter. With disappointment and surprising candor, he dryly quotes a 1934 letter where Baldock had proposed completely moving both the highway and railroad to the north, and away from Warren Falls, as a solution to the debris problem, apparently to underscore his belief that Baldock’s tunnel project would be a short-term, costly fix at best.

This earlier 1934 correspondence from Baldock turns out to be prophetic, of course, with the modern-day alignment of I-84 and the Union Pacific railroad ultimately carrying out Baldock’s vision.

Baldock’s faster, straighter version of the Columbia River Highway began to emerge in the 1940s (near Mitchell Point).

These proposals for altering Warren Creek may seem brazen and completely irresponsible by today’s environmental standards, but consider that at the time the dam building era on the Columbia River was just getting underway. By comparison, these “improvements” to nature were just another effort to conquer the land in the name of progress.

These schemes also underscore how visionary Samuel Lancaster really was: far ahead of his colleagues of the day, and some 75 years ahead of the 1990s reawakening among engineers to “context sensitive” design in the modern engineering profession.

Cross-section plans for the “trash rack” design at the head of the Warren Creek diversion tunnel; the odd structure still survives and continues to function today.

October 2, 1939 – Work on the Warren Falls diversion project begins. The full project includes the diversion tunnel and flume, plus reconstruction of a 0.69 mile section of Lancaster’s historic highway and two bridges. In the fall of 1939, the highway contractor built a highway detour road, new highway bridges, and excavated the flume ditch and relief channels.

Work on the “trash rack” and associated blasting for the diversion tunnel bogged down, however, with the contractor continuing this work through the winter of 1940. Despite the modest budget, ODOT records show that the contractor “made a very good profit” on the project, and completed work on September 21, 1940.

The budget for the project was as follows:

Compared to modern-day transportation projects that routinely run in the millions, seeing costs detailed to the penny seems almost comical. Yet, at the time both the Oregon Highway Department and Union Pacific Railroad were strapped for cash, and very cost-conscious about the project. A series of letters between the sponsors continued well beyond its completion to hash out an eventual 50/50 agreement to pay for construction and ongoing maintenance of the stream diversion structures.

After the 1940s – the reconstruction of the Columbia River Highway at Warren Creek was part of a gradual effort to widen and straighten US 30 along the Columbia River. Today’s eastbound I-84 still passes through the Tooth Rock Tunnel, for example, originally built to accommodate all lanes on the straighter, faster 1940s version of US 30.

The beginning of the end: construction of the “new” bridge at Oneonta Creek in 1948, one of many projects to make the old highway straighter and faster. Both this bridge, and the original Lancaster bridge to the right, still survive today.

By the early 1950s, most of Sam Lancaster’s original highway had been bypassed or obliterated by the modernized, widened US 30. Much of the new route was built on fill pushed into the Columbia River, in order to avoid the steep slopes that Lancaster’s design was built on.

Passage of the federal Interstate and Defense Highways Act in 1956 moved highway building in the Gorge up another notch, with construction of I-80N (today’s I-84) underway. The new, four-lane freeway followed much of the US 30 alignment, though still more of Lancaster’s original highway was obliterated during the freeway construction. This was the final phase of freeway expansion in the Gorge, and was completed by 1963.

In the Warren Creek area, interstate highway construction in the late 1950s finally achieved what Sam Baldock had envisioned back in his correspondence of 1932, with the Union Pacific railroad moved onto fill reaching far into the Columbia River, creating what is now known as Lindsay Pond, an inlet from the main river that Lindsay, Wonder and Warren creeks flow into today. The “improved” 2-lane US 30 of the 1940s had become today’s four-lane freeway by the early 1960s.

Coming Full Circle: Restoring Warren Falls

Since the mid-1990s, ODOT and the Friends of the Historic Columbia River Highway have worked to restore, replace and reconnect Samuel Lancaster’s magnificent old road. In some sections, the road continues to serve general traffic, though most of the restoration focus is on re-opening or re-creating formerly closed sections as a bike and pedestrian trail.

The trail segment in the Warren Falls vicinity is now entering its design phase, and is slated for construction as early as 2016, commemorating the centennial of Lancaster’s road. Though initially excluded from the plan, the restoration of Warren Falls is now shown as a “further study” item — a step forward, for sure, but still a long way from reality. The plan does call for an overlook of both the historic Warren Falls and Hole-in-the-Wall falls (shown below).

Proposed trail alignment along the reconstructed Historic Columbia River Highway.

(Click here for a larger view of the trail plan)

There are three key reasons to restore Warren Falls now:

1. Funding is Available: The nexus for incorporating the restoration of Warren Falls into the larger trail project is clear: the trail project will require environmental mitigation projects to offset needed stream crossings and other environmental impacts along the construction route. Restoring the falls and improving fish habitat along Warren Creek would be a terrific candidate for this mitigation work.

2. The Right Thing to Do: Restoring the falls is also an ethical imperative for ODOT. After all, it was the former Oregon Highway Department that diverted Warren Creek, and therefore it falls upon ODOT to decommission the diversion tunnel and restore the falls. Doing this work in conjunction with the nearby trail project only makes sense, since construction activity will already be occurring in the area. Most importantly, it also give ODOT an opportunity to simply do the right thing.

Ain’t no way to treat a lady: the obsolete Warren Creek diversion tunnel is not only a maintenance and safety liability for ODOT (photo by Zach Forsyth)

3. Saves ODOT Money: Finally, the restoration makes fiscal sense for ODOT. The Warren Creek diversion tunnel is still on the books as an infrastructure asset belonging to ODOT, which in turn, means that ODOT is liable for long-term maintenance or repairs, should the tunnel fail.

The tunnel also represents a safety liability for ODOT, as more rock climbers and canyoneers continue to discover the area and actually travel through the tunnel. Decommissioning the tunnel and diversion would permanently remove this liability from ODOT’s operating budget.

Not good enough: excerpt from the HCRC restoration mentions the “Historic Warren Falls site”, missing the opportunity to restore the falls to its natural state.

How can you help restore Warren Falls? Right now, the best forum is the Historic Columbia River Highway Advisory Committee, a mostly-citizen panel that advises ODOT on the trail project. A letter or e-mail to the committee can’t hurt, especially since the project remains a “further study” item. You can find contact information for the committee on the HCRH page on ODOT’s website.

But it is also clear that Oregon State Parks will need to be a project partner to restore Warren Falls. The best way to weigh in is an e-mail or letter to the office of Oregon State Parks & Recreation (OSPRD) director Tim Wood. You can find contact information on the Oregon State Parks website. This is one of those rare opportunities where a few e-mails could really make a difference, and now is the time to be heard!
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Special thanks go to Kristen Stallman, ODOT coordinator for the HCRH Advisory Committee, for providing a wealth of historic information on the Warren Creek bypass project.

To read Oral Bullards‘ 1971 article on Hole-in-the-Wall Falls, click here. Though largely accurate, note that Bullards’ article is based on interviews of ODOT employees at the time, and not the original project files that were the basis for this blog article.

Next: a simple, affordable design solution for restoring Warren Falls!

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