Friday, December 12, 2025

Lewis & Clark State Park

Next up we're visiting Lewis & Clark State Park, at the west end of the Columbia Gorge just across the Sandy River from downtown Troutdale. Let me start off by saying this post is not an adventure through pristine wilderness; the the park's essentially a glorified highway rest area -- it officially opened in October 1955 along with the nearby segment of I-84 -- surrounded by a few recreation options. (The park is classified as a "State Recreation Site", if we're going to split hairs.) The park is best known as a Sandy River access point for fishing and boating, and the high bluffs above the river have become a popular rock climbing spot in recent decades. The park is not famous for hiking, but it does have a few trails, and that's what we're here to check out. None of them are very long and most are easy, but one has sort of a weird mystery associated with it, which we'll get to in a bit. And don't miss the historical odds and ends down at the bottom, stuff that didn't fit anywhere else.

  1. Lewis & Clark Nature Trail
  2. Broughton Bluff Trail
  3. Lewis & Clark Trail No. 400

So the first trail, and the only one with a sign, is the "Lewis & Clark Nature Trail", which is a mostly-paved loop around the landscaped "rest area" part of the park, with a few signs describing various native plants. In practice I imagine it's largely used by people and dogs who need a stretch after a long drive along I-84. When I started writing this post I sort of assumed the trail and the dated, weathered sign were original features of the park, but it turns out they were added in 1980 for the 175th anniversary of the Lewis & Clark expedition camping here for a bit in November 1805. And yes, a bit of my surprise is due to being of just the right age where 1955 is ancient history, while 1980 is a year I have clear childhood memories of, and therefore things from then cannot possibly look dated or weathered. (And yes, I have yet another birthday this month, why do you ask?)

An April 1980 Oregon Journal article described the upcoming trail:

When completed, the trail will feature many of the 150 flowers, shrubs, and trees identified and described by Capts. Meriwether Lewis and William Clark in their journals which, besides an account of their travels, were a compendium of scientific data covering botany and other disciplines. The one-half mile loop trail, with a gravel covering, is in place and site preparation has been finished. Only a start has been made on the plantings.

The article then notes that they only had Oregon grapes in place so far, but a vine maple was coming soon. The article continued:

Plans are in progress for various planting areas to be “adopted” by garden clubs, civic and educational groups, each to plant and maintain its own plot. Twenty-two such groups have been enlisted so far. ... The nature trail is a project of the Oregon Lewis and Clark Trail Committee, chaired by Dr. E.G. Chuinard, Portland orthopedic surgeon. Dr. Chuinard is a nationally known Lewis and Clark scholar, and the trail has been a dream of his for many years.

The article goes on to mention that, as an orthopedic surgeon, he was proud that the new trail would be wheelchair-accessible, at least by the pre-ADA standards of 1980. Chuinard later wrote a book that more or less combined his professional and personal interests “Only One Man Died, the Medical Aspects of the Lewis & Clark Expedition”

An August 1979 Oregonian article described the proposal in similar terms, adding that this would be a great new use for the park, replacing the overnight campground that had been there since the park opened. Apparently the campground was considered a nuisance and drew 'undesirable' people to the area, though I'm not sure whether that meant partiers or something worse. A November 1978 letter to the Oregon Journal opposing removal of the campground explained that it was the only low-income camping option for people passing through the area in the summer, and Ainsworth was (and is) the closest alternative, much further from Portland and Troutdale. The Oregonian article went on to quote someone with the State Parks Division who hoped they'd be able to get rid of the adjacent dirt bike area just north of the park as that was considered a nuisance too.

1979, the oregonian editorialized in favor of the trail. The editorial board may not have paid close attention to the proposal up to this point, and it's hard to imagine a bunch of cynical old-school newspapermen caring a whit about gardening, but one historical constant about the Oregonian, from the 1850s to the present day, is that they will always endorse any proposal that involves being mean to poor people, whether as a deliberate goal, or as foreseeable collateral damage. So with this editorial, the project was virtually a done deal.

The nature trail was dedicated in October 1980. For the big event, the paper interviewed Roger Mackaness, a Corbett landscape architect, nursery owner, and part-time Job Corps instructor, who was handling the practical side of the project, translating Chuinard's daydream into an actual garden full of live plants.

“I can’t guarantee that anything will grow”, said Mackaness, explaining that certain plants such as sagebrush and prickly pear have to be grown from seed. “Eastern Oregon plants take special care.” Varieties of plants to be found on the trail include cliff dwellers, desert lovers, high mountain and shore plants, he said. Making the task even more difficult, the plants will be ordered in the manner in which Lewis and Clark discovered them, and each planting will be landscaped to mirror the topography found in the plant’s natural habitat. “This will be a trailhead for a 90 mile hike to The Dalles”, Mackaness said. “In the 1/4 mile nature trail you could see the same kind of plant life you’d see if you hiked to The Dalles.”

The article goes on to explain that the plantings should be complete in another two years or so. An Oregonian article on the trail dedication notes that the trail had been in the works since 1974, and the very first mention of it I saw came in a 1975 article by Chuinard, which mentions that a group in Charlottesville, VA was proposing an "all the Lewis & Clark plants" garden there.

In April 1982, a Lewis and Clark mini-garden opened at the Oregon Zoo, featuring some of the same plants, with Chuinard and other members of the trail committee in attendance. The Journal assured readers that

The new garden also is intended to complement, not compete with, the nature trail at Lewis and Clark State Park near the mouth of the Sandy River, which, when completed, will have examples of all or most of the plants identified in the Oregon country by the famous explorers. A sign in the zoo garden calls attention to the Sandy River project.

It's not clear what happened after that, as the Oregon Journal went out of business later that year and they covered the garden effort much more closely than the Oregonian ever did. Probably the same thing that often happens with efforts that start as one person's dream and that rely on volunteers to keep going. Especially when that one person was already a retiree and eventually retires "for real" from civic efforts too and moves out of the area to be near family, as the Chuinards did in 1987. He had already moved on to a new project at that point, trying to persuade the city to build a Lewis and Clark museum out at Kelley Point Park. He and the committee had originally wanted to build the museum here, piggybacking on a proposed ODOT port of entry, as Chuinard explained in a 1984 op-ed in the Oregonian.

He argued this was a great location for a museum (although the State Parks Division and environmental groups disagreed) and a logical follow-up for the still-incomplete nature trail. The museum would have been located in the still-barren 12 acre plot north of the 'main' park, between the railroad and I-84, which I think is where the county's short-lived offroad motorcycle park was located during the 1970s. an August 1985 article has more details about the proposal.

The problem with the trail, Chuinard said, is that the flowers do not bloom at the same time, and most are not at their peak during the short season of pleasant weather in the Columbia Gorge, when visitors are not subjected to rain or the cold east wind.

Which is true of the entire Northwest, frankly. He went on to suggest that we were rapidly falling behind Washington State in both quantity and quality of Lewis & Clark visitor centers, which is an odd sort of arms race to have. But I suppose that was how things got funded in 1984.

The present-day trail does not exactly look as though it has 22+ garden clubs and civic groups avidly maintaining their individual plots. Some of the signage has been updated fairly recently, though, possibly for the Lewis & Clark bicentennial in 2005. One of the newer signs concerns native medicinal plants, and has a sidebar snarking about the Lewis & Clark expedition dosing themselves to the gills with mercury and other toxic patent medicines of the era, I guess for a little contrast. Which is a fair point, and not one a circa-1980 sign would have mentioned, necessarily, even if the nature trail's main proponent wrote an entire book on the subject.


The second trail is an obvious but unnamed trail that heads south and upward from the landscaped area. This is the access trail for the popular rock climbing area along the southwest-facing part of Broughton Bluff. This area is enormously popular when weather permits, which was not the case the day I visited. Which is great if (like me) you just want to take photos of the rocks and not try going up them. I only followed the trail to the point where you're looking almost straight down at the old Columbia River Highway bridge over the Sandy River, but I gather it dead-ends at the state park property line, not much further south from there. The potentially-climbable cliffs continue for a while south from there, but they're on private property and it seems the owners don't want the liability issues, and also don't want to sell. In terms of the trail having other features, there's one small and (as far as I know) unnamed waterfall along the way. I don't know whether it runs year round or it's just seasonal. Either way, I can't say it's worth going out of your way to see if you aren't there to climb any rocks, given all of the vastly better hiking options a few miles to the east. Small bit of trivia here, the place is named for a junior officer on the the George Vancouver expedition who made it roughly this far upriver, and is best known for naming Mt. Hood and Mt. St. Helens, along with a bunch of other names that didn't stick, like calling the Sandy the "Barings River", after the British bank that imploded in 1995 after a rogue trader lost all their money. Broughton didn't name the bluff after himself, though. That came later, after a 1926 lobbying campaign by local Girl Scouts.

In addition to the main trail, a scramble route goes to the top of the bluff, starting right at the point where the main trail rounds the sharp corner from the north face of the bluff to the southwest face. I only found out this existed afterward so I don't have any photos from the top, but blog posts at Casing Oregon and Columbia River Gorgeous include photos from up there, and a video from TheCascadeHiker shows both trails, first the main one, then backtracking to the one to the top. Unfortunately the park boundary also runs along or very close to the top of the bluff so you can't really go anywhere once you've made it to the top. A century ago (early November 1920) you could take a streetcar here from downtown Portland, climb the bluff (which went by "Troutdale Butte" back then) and then east and up to the top of Chamberlain Hill and back, but I get the impression that hikers and climbers and random tourists wore out their welcome here decades ago. In any event it's just ordinary farm country up there once you're away from the edge, and not one of those weird Venezuelan islands in the sky, especially not the kind with dinosaurs. Could be worse, though; if Portland's urban growth boundary didn't exist, the entire top of the bluff would likely be a nasty gated community full of ugly McMansions, and security goons from the HOA would pour boiling oil down on anyone who dared to climb here. So there's that.

As it is, the top of the bluff is just ordinary farm country growing normal farm products. It did have one brief brush with semi-importance back in 1961, when the top of Broughton Bluff was part of an elaborate surveying project by the US Coast & Geodetic Survey, the agency behind all of those pre-GPS vintage survey markers. This project involved a team of engineers, families in tow, traveling from place to place, marking and surveying, building and disassembling survey towers, measuring and remeasuring until the exact position of everything was nailed down to 1/300th of an inch, then going somewhere else and starting the process all over again, like the world's nerdiest traveling circus. I imagine that probably made for a weird childhood. The article mentions that the survey had been delayed by higher-priority projects like laying out Cold War missile bases.

September 1974 article on climbing here, mentions in passing that there are a few other things to do, like smelt dipping (no longer possible since the smelt runs collapsed in the 80s), camping (replaced by the garden), and dirt bike riding (also abolished, and replaced by an empty lot). While chain smoking or working your way through a case of Blitz beer or both whenever you had a hand free.


And finally, at the far corner of the landscaped triangle, an unsigned trail heads east into the forest, and off the edge of most maps of the park. It's clearly a "real" trail, constructed by people who knew what they were doing, and not just a random use path, and it seems to get some level of regular maintenance, and you get the distinct impression that a trail like this is bound to go somewhere interesting, sign or no sign. So you keep going, doing a roughly flat, roughly straight traverse east, part of the way up the bluff and parallel to I-84 and the railroad (which you are never out of earshot of). But after a couple of miles it just sort of fades out and ends, and you can either turn back at that point or try bushwhacking further for a while and then turn back. The only real destination along the way is a stretch with several house-sized boulders toward the end of the (obvious) trail, known to local climbers as "The Zone". I can't say it's an amazing nature experience, but if you think of it as more of a very easterly city park along the lines of Portland's Forest Park, it's actually not that bad. I feel like I need to say this because the OregonHikers page about the trail snarks about it (which is quite uncharacteristic for them), saying they only did it just for the sake of completeness.

So why is there a trail here, if it just sort of ends at a random spot in the forest? That isn't typically what trails do. One clue is that although there's no sign for the trail in the park, if you look at the right maps you'll see occasional scattered references to it here and there calling it the "Lewis and Clark Trail 400" or some variation thereof. (I'm almost positive the name also appeared on an official PDF map of the park at one point, but I can't seem to find a link to that map now.) The "400" is the key detail: Under the longstanding trail numbering scheme in the Gorge (which I think is a Forest Service thing, although some trails on state land use it as well in the name of consistency), trails are all numbered 400-something, (other than the Gorge bit of the Pacific Crest Trail, which is #2000 for its whole length), and the number 400 was reserved early on for a hypothetical east-west trail stretching 90 miles or so from Portland out to Hood River or possibly The Dalles, depending on who you ask. This trail has never really existed over that full distance, but a few segments do, and it's slowly grown (and occasionally shrunk) over time when people take an interest in the idea for a while and funding becomes available. A couple of segments further east are known as the Gorge Trail #400, which I'm sure I've mentioned here once or twice. So right now the official west end of the westernmost existing chunk of Gorge Trail is at Angels Rest, which is obviously nowhere close to Troutdale, and that's how it's been for decades. That is, except for the obscure bit of dead-end trail we're visiting here. Which I guess makes it the trail equivalent of a freeway ghost ramp.

Note that Trail #400 is not the same thing as the under-construction Historic Columbia River Highway trail. It covers more or less the same ground but is a very different proposal, a paved path aimed primarily at road cyclists, often immediately next to the freeway, and encompassing surviving bits of the old highway where possible. I've walked on a few parts of it, and it's fine, I guess, but it's nobody's idea of a relaxing nature experience. And since the entire theme of the effort is around the old highway, the initial part of the route involves riding on the old road, sharing it with Winnebagos and monster SUVs and so forth. Which is not doable at all if you're on foot.

It's also not the same thing as the Hatfield Memorial Trail, which is supposed to be an east-west backcountry route, staying as far away from civilization as possible under the circumstances. A trail along these lines was proposed by the Sierra Club way back in 1971, and a fairly long route can be assembled out of parts of several existing trails, though some of these trails receive little or no Forest Service maintenance and it's an ongoing struggle to keep them from being taken back by the forest.

An early version of that idea (or part of it) was the proposed Talapus Trail, which would have connected Larch Mountain to Wahtum Lake by way of the Bull Run Watershed, a large area that's normally closed to all public access because it's the primary source of Portland's drinking water supply. I am not sure how that was supposed to work, whether they were going to tweak the closure boundary or just accept that a few backcountry hikers wouldn't be a problem, or they just hadn't figured that out yet. The notion being kicked around as early as 1974 (back when calling it "Hatfield Memorial" would have alarmed Senator Hatfield), and an August 1980 article was already looking ahead to a third east-west linkage once Gorge Trail #400 and the Talapus route were done and dusted. This third route would have run right along the Columbia shoreline, which isn't even on anyone's long-term ideas list anymore, as far as I've seen. It always shocks me to see how many grand plans of the 60s and 70s came to a crashing halt on election day 1980; I'm sure that there were a few clunker ideas in there, but I'd love to go visit the timeline where the entire Reagan Administration never happened, and the wingnuts and their ideas never took over, and just see how the year 2020 played out over there versus here. It can't have been worse, anyway

The notion of a Trail 400 that specifically started here seems to have burst onto the scene in 1979 with the state's new Columbia Gorge parks master plan, which envisioned what it called a "low-level gorge trail":

Proposed development of trail head parking for the "low level gorge trail", which, when fully completed, will complete a link for hikers from Troutdale to The Dalles, a distance of 90 miles. Portions of the trail have been completed, but access through some western properties is still being examined.

Toward the end of the article it mentions that funding was uncertain, and construction probably wouldn't begin until 1981-83 on any of the listed projects, and that was dependent on federal money coming through. Other interesting and sadly unbuilt ones include a trail between Rooster Rock and Latourell Falls, and a railroad underpass connecting Wahkeena Falls and Benson State Park. The plan mentions that the old Rooster Rock Wagon Road -- which we visited a few years ago in the Palisade Falls post -- would connect to the low-level trail as it passed through the area.

So the first problem with the trail and the rest of these grand plans was the date: 1979 was immediately before Ronald Reagan was elected and began slashing non-military budgets, and stomping on anything that looked vaguely environmental just to spite the hippies. The envisioned construction period also overlapped with Oregon's deep multiyear recession of the 1980s. So without money or political interest, the project fell by the wayside and has never been revived, just like other grand projects of the 1970s like switching to the metric system.

As for why it stops where it does, the current trail extends past the eastern edge of the park and out onto Forest Service land for a while, and remains largely federal as far as the Corbett area other than some assorted bits of ODOT-owned land and one stretch owned by the Union Pacific railroad. It's as if the state built as much as they could on their own and then the feds never picked up the baton. As for the railroad bit, I didn't see anything saying they were blocking the proposal, which I think would've been newsworthy if that had happened. I did see that they'd tried subdividing it into residential(?) lots at one point but didn't sell any of them, and the land hasn't been buildable since 1986 due to National Scenic Area rules). So maybe they'd still be up for selling that area, or at least doing an easement for a trail, though I obviously have no way to know that.

November 1981 - Multnomah County closed a mile of Henderson Road between Latourell & Bridal Veil, though holding on to the old right-of-way to maybe become part of trail #400 someday. The article mentions that the old road had once been part of the 1870s wagon road between the Sandy River and The Dalles. I gather the steep, long-closed, long-forgotten (but again never-vacated) Latourell Hill Road was once part of the old wagon route too, but I don't know if it was ever envisioned as a trail route.

Small calendar item from September 30th 1983, noting volunteers could come join a "work party clearing new low-level Gorge Trail No. 400 east from Lewis & Clark State Park".

Further east, the state was trying to arrange a land swap with the federal Bureau of Land Management for land further east along the proposed trail route; the article describes the 2 mile long parcel as 100 acres of steep north-facing bluffs next to the rail line, but I can't pin down which parcel they're talking about or who owns it now. The Friends of the Columbia Gorge was strongly opposed to the idea. It seems that a couple of rare and potentially endangered plants were known to live in the area: Sullivantia oregana and Dodecatheon dentatum, and the Friends figured they would no longer be protected properly with the plants in state hands. Thinking BLM would do a better job than the state would of protecting the environment seems a bit odd in the 2020s but maybe things were different back then.

The trail also ran into a degree of local opposition, as the park had a sketchy reputation back in those days, beyond the usual urban legends about highway rest areas. The trail was proposed around the same time the campground was removed, and the county-run dirtbike park next door was still there, and rural residents to the east found it easy to imagine the trail would funnel an urban crime wave in their direction. For example, a 1979 article about a longtime resident of the tiny town of Latourell (it's just downhill from Latourell Falls, but not visible from the Gorge highway) raised concerns about a proposal in the new state plan to turn a local historic house into a youth hostel for people through-hiking the new trail. Local residents strongly opposed the idea, the word "youth" being even more loaded then than it is now.

As another example, a 1982 article lamenting that 37 different government agencies were involved in managing the Sandy River area. mentioned rowdy campers at Dodge Park as one of the issues facing the area, holding all-night beer parties and such and driving away respectable visitors. A State Parks representative mentioned that similar problems had receded at Lewis & Clark after the campground had been removed. Other people wanted to talk about habitat protection, but the paper reported that toward the end, after the lurid stuff and the riling people up about big gummint bureaucrats.

By 1984 the Oregonian was wringing its hands again about the now campground-free, dirtbike-free park, as the area nearby saw its second homicide in as many years. I haven't looked up the news stories about those but it sounds like both were related to arguments between transients. The mayor of Troutdale was freaking out and blaming the park, conveniently outside city limits. A spokesman for the county sheriff's office explained that "Other than those two murders, we have no phenomenal problem at Lewis and Clark state park", to which the mayor responded "Don't you think one murder a year is too much?", as if this was now a long term trend. The article went on to lump in a recent homicide at a truck stop half a mile away, a sexual assault in Troutdale Community Park (now Glenn Otto Park) three years earlier, and the general unruly crowd atmosphere at Glenn Otto as if those were valid data points about Lewis & Clark being scary. I've complained before about how bad crime reporting was in the 80s, but it still startles me. Nobody was even trying to figure out actual cause and effect, just pointing fingers at everything randomly and freaking out even further when that approach didn't move the needle.

Despite all that, the effort forged ahead for another couple of years. Here's a 1985 interview with the Oregon State Parks regional administrator. The article explains that a trail from Troutdale to Hood River had been a longtime dream of his, noting however that some of the remaining parts would be expensive, like at Tooth Rock west of Eagle Creek. There's also a bit about another then-ongoing project to build a four-mile trail between Bridal Veil and Latourell Falls, with improved views of the falls at Shepperds Dell, which I imagine would have doubled as another Trail #400 segment. Seems this was never constructed either, which is a shame. The interview was in conjunction with the grand opening of another Gorge Trail segment further east, between Ainsworth and Yeon State Parks. Unfortunately that entire segment was destroyed by an enormous landslide in 1996 and has never been rebuilt.

Someone giving a presentation about the proposed trail at Portland State in 1986.

The 1986 talk was the last mention of the proposal that I could find in the newspaper archives, but I still had several open questions, like exactly what the intended route was, for example. I ended up looking for old planning documents to see if they offered any more clues, and luckily the 1994 state parks plan for the Gorge mentions the proposed trail a few times. (For whatever reason, all of the state parks department's master plan archives vanished off the net sometime in the last few months as part of a site redesign. But as usual, Archive.org has our back, or mine anyway.) From page 15:

Trail connections and/or trailhead development is proposed for a low elevation route from Lewis and Clark to the OPRD properties just west of Hood River via segments of the HCRH and via other new routes, and from the east side of Hood River to Mosier along the Historic Columbia River Highway (HCRH) to Mosier.

and then on page 26:

Trail use continues to be popular in the Gorge especially at the higher elevations. There has been an effort by recreationists for many years to see the establishment of a series of connections through the gorge at a lower elevation and along the river where possible. Most notable among these efforts are the Historic Columbia River Gorge Highway (HCRH) connection projects, the trail 400 project, and the Chinook Trail.

(If the name "Chinook Trail" is unfamiliar, you aren't alone; I had never heard of it before either, but it's a long-term effort to build a backcountry trail over on the Washington Side of the Gorge, eventually connecting with either the Gorge Trail, or the Hatfield Trail, or a fresh new backcountry trail on the Oregon side to form a big long loop.)

Anyway, in a later section of the plan, we finally get some details about what they had in mind. (The acronym NSA in this context means the then-new Columbia River Gorge National Scenic Area, not the shadowy intelligence agency.)

#1 Lewis and Clark to Portland Women's Forum, MP CRGNSA trail proposal No. T27. Trail Maps 1 and 2

OPRD's proposal for this trail deviates from the NSA proposal in that Chamberlain Road is used rather than trying to build a trail through the complex ownerships near Corbett Station. By constructing a pedestrian walk along the county road, a trail connection could be accomplished much sooner and at less expense. Easements will be needed across the north face of Chanticleer Point.

The connection of this trail to Portland Women's Forum cannot be accomplished until parking is expanded at Portland Women's Forum to accommodate the long term parking requirements of trail users. Additional trailhead parking could be developed at the Corbett Station quarry if a suitable trail route from the quarry to Portland Women's Forum or from the Lewis and Clark to Portland Women's Forum trail route could be found.

Google Books has the 1992 Federal management plan for the new scenic area, which describes that proposal in a couple of paragraphs:

Trail Description: The land is primarily in private ownership. This trail would provide a link between the Portland/Vancouver metropolitan area and the Scenic Area. The trail would provide views of both the Columbia River and the pastoral landscape of the western Gorge. This trail would form part of a loop trail that links to the Sandy River Delta Trail. Recreation Intensity Class: mostly 1. Development Proposal: Four miles of new trail are proposed to provide opportunities for hiking and scenic appreciation. There is an existing trailhead opportunity at Lewis and Clark State Park; a parking area is proposed at the existing borrow pit at Corbett Station in the GMA. Some sections of the trail traverse steep bluff lands and would require sophisticated design and construction.

For whatever reason, the Management Plan "as amended thru September 1st 2011" deletes the entire section of concrete proposals and just speaks somewhat vaguely about high level goals.

Getting back to the state plan, it has maps after page 100, which show the trail eventually connecting to the old wagon road between Portland Womens Forum and Rooster Rock, and then making its way over to the Vista House. The maps also show that the proposed trail would be both Trail 400 and the Chinook Trail; following the maps further east, the two routes diverge above Multnomah Falls, Trail 400 following its familiar (if currently closed) route, and the Chinook Trail taking a parallel route further south/uphill, and this arrangement continuing all the way to Hood River. I imagine this would let you hike to Hood River and back mostly as a loop (albeit a long, skinny sort of loop), or put together more reasonably-sized loops out of parts of the two plus connecting trails. The key detail here is that significant chunks of the Chinook route would be new construction, and as the first route to Hood River is not exactly making rapid progress, it feels like building a brand-new second route is a bit of a longer-term vision, to put it mildly. Maybe it'll be ready around the time the gorge has fully regrown from the Eagle Creek fire, who knows.

Metro's 1992 Metropolitan Greenspaces Master Plan described the proposal: "The Chinook Trail is a proposed Columbia River Gorge loop trail that will connect Vancouver Lake, Maryhill State Park, Biggs, and Portland. It will travel in part on existing trails. The concept was formalized in 1988 as a rim-top trail where possible."

These plans only get a very brief mention in the 2011 Master Plan for Lewis & Clark specifically, which mostly focuses on parking and congestion, and improved river access. It does acknowledge that the trail exists and ideas for it are out there, but doesn't propose doing anything about them.

[I]t is a hub for a series of existing and proposed trails that will eventually connect Portland with the City of Hood River. This includes an eventual link with the famous “40-Mile Loop” trail network on the east side of the Sandy River on federal and state land and with cycling routes along the Historic Columbia River Highway

and a few pages later:

There is a walking trail at the foot of Broughton Bluff along the edge of the lawn that extends northeast along the north face of the bluff at least as far as the eastern property boundary.

The state's 2015 Gorge master plan (which I guess supersedes the 1994 plan) more or less includes the 2011 plan by reference and repeats the ideas from there (chapter 8, pages 148-149, here). The map on page 149 incorrectly shows the trail heading off onto private property, which (as I noted above) is not actually true. Which is not an encouraging sign.

More recently, Metro -- Portland's regional government, which runs Oxbow Park further south on the Sandy (among many other things) -- has taken an interest in the long-running proposed trail, calling it the "Lower Columbia Gorge Trail". A 2014 map from Metro shows it as a "proposed regional trail" heading east off the map as a connection from Portland to the Gorge. The agency's 2017 "Green Trails" guide describes it as one of several future "inter-regional" trails, along with the Willamette Greenway south to Eugene-or-so, and two routes west to different destinations on the coast. The interesting thing about this is that, per a 2019 map, the "Sandy River Connections" project area is one of 24 "acquisition target areas" where they're interested in buying land or paying for easements. Historically they've just been interested in property along the Sandy, but the maps shows their "ok to buy within this area" radius, which looks like some number of miles past the urban growth boundary, and everything out to Rooster Rock seems to be fair game, in theory. And it's basically all state and federal land east of there, so that might be sufficient to fill in the gaps. Metro has local bond money specifically dedicated for this, too, where the state rarely does, and the feds are rarely interested these days (though that might change after the inauguration in January, unless Trump blows up the world before that.)

Which brings us to a "Now What?" section. For the sake of argument, let's assume first that schools, healthcare, housing, antipoverty programs and other concrete human needs are being funded properly, and there's money left over after that, and we don't need to have a zero-sum argument over what to cut in order to build something new. Let's also assume that within the recreation budget, maintenance and repair is already funded, so we aren't trading off against restoring Eagle Creek and other fire-damaged areas, reviving ones that were abandoned or relegated to unmaintained status like the old Perdition Trail at Multnomah Falls, the viewpoint at the top of Wahkeena Falls, and so on.

This is not the most wild or scenic stretch of the route. not aware of any key points of interest along the route, and land ownership around corbett is an issue. and I'm not personally sold that it would be important enough to buy except from willing sellers. the current thing that attracts funding is the bike-centric HCRH Trail, which follows the 1916 route of the old highway. eventually there may be an interest in doing the same thing for the circa-1940 pre-I-84 water-level route (per the Tunnel Point post), for cyclists who'd like to skip the tourist traffic (or just the additional elevation gain and loss) along the initial chunk of old highway. So a hiking trail could maybe piggyback on that in spots where there isn't space or money to build both. with or without HCRH trail involvement, one slightly-outside-the-box idea might be to cross the overpass at Corbett and walk along the river for a bit, either to Rooster Rock (where there's another existing overpass) or maybe to a new pedestrian bridge over I-84 at Tunnel Point and heading east from there to squeeze past Palisade Falls


  • The very first piece of the park that the state owned was actually the gravel parking area just across the river from Glenn Otto Park, purchased way back in July 1936, probably for the sake of public fishing access. They don't appear to have named it right away, and the old survey map for it just calls it "Parking Area".
  • land acquired in 1954 in a 3-way deal: Timber co. buys the land, swaps it for non-scenic BLM land elsewhere, BLM donates it to the state. Article says the goal was to eventually assemble a big park running the whole length of the gorge, which I suppose the National Scenic Area basically is.
  • September 1955 article on the soon-to-open park
  • An article from December 1965 about what would eventually become Estacada's Milo McIver State Park explained that it was needed as a safety valve because existing parks along the Sandy and Columbia were overflowing with visitors. Rooster Rock and Dabney each attracted 250k visitors that year, and Lewis & Clark pulled in 350k people, who were packed into the park's "anemic" 56 acres like an "outdoor sardine can". For contrast, in 2019 Rooster Rock was the 19th most visited state park with 667k visitors, down 29% from the previous year for some reason. I can't find numbers for the others since they didn't make the top 20, or the bottom 20.

    A 1965 article inventorying parks and recreational opportunities in East Multnomah County mentioned Lewis & Clark as one of the area's shiniest and newest parks, and explained that we would soon need even more parks like it. The author explained that in the time before white settlers arrived, local tribes had a word for the ennui that comes with having too much free time and no work that needed doing, in the months after the salmon and berries had been dried for the winter and so forth. He argued a similar situation was looming for Americans of the near future: "The Portland urban dweller of A.D. 2000 — perhaps even sooner — will find himself suffering from the same malady, what with the coming 30- and 20-hour week, the extended leisure time, and an increasingly easy life." .

  • October 1967, in the upcoming election Troutdale voters were being asked to approve a controversial sewer bond issue, which on one hand would result in the city no longer dumping raw sewage into the river, just upstream of the park's public beaches. On the other hand, doing this would cost money.
  • 1969, a Multnomah County Commissioner was bound and determined to site a new metro-area garbage dump in the sandy river delta, just downstream, although locals opposed the idea. Residents must have prevailed eventually, since there's no dump there now.
  • A 1969 article explained that conventional wisdom among local park rangers -- including one responsible for both Dabney and Lewis & Clark -- was that out-of-state visitors were typically cleaner and nicer than local residents, contradicting a widespread public notion of the time. A visiting family from Pendleton at Lewis & Clark reported that someone had knocked their tent over, accusing them of being Californians and demanding that they leave the state.
  • August 1970, county turned down a proposed rock quarry south of the park, after turning down another proposal in corbett, 2 miles from Crown Point. The developer couldn't see why people opposed the idea, explaining that the quarrying was temporary and he planned to build houses on the site as soon as the mining phase was done.
  • August 1971, park hosted a unit of Green Berets who were retracing the Lewis & Clark route for some reason.
  • October 1972, bit about historical sites being gobbled up by development. seemed to focus on lewis & clark sites, including here, which had no historical marker at the time. gov. mccall promised to fix that particular detail
  • May 1974 E.G. Chuinard of the Lewis & Clark Trail Committee (seen above/later) writes in response to an earlier editorial about typos on a sign at the park. He explains that the typos are how Lewis & Clark spelled things and are thus historical in nature and not incorrect.
  • the aforementioned editorial, titled "History in Misspelled Words".
  • the coming-soon article
  • the unveiling, with photo
  • December 1975, a columnist waxing on about a seasonal waterfall a bit upstream of the park. (w/ photo)
  • March 1976, the county had leased land for the motorcycle park as an alternative after passing a restrictive off-road vehicle ordinance. forgot to rezone the land for the new use at first. . a story on the same page mentions the shiny new Trojan Nuclear Plant was being swarmed by smelt and had to report it to the feds.
  • March 1977, report on the annual smelt run
  • September 1977: In an extremely 1970s episode, the park was the destination of a 5 mile river race from Dabney State Park, sponsored by the local 7-Up bottler and US Army recruiters, as one of many local festivities organized around the annual Jerry Lewis Telethon. (!!) Local telethon content was hosted by Ramblin' Rod. Other events included a 3-day CB radio jamboree, and a disco car wash at Beaverton Mall. leading up to this were a few weeks of danceathons, skateathons, bike races, raft races, waffle feeds, and shoot outs.
  • July 1978, mentioned on a list of good picnic spots around the state. The list is interesting. hagg lake, blue lake, baldock rest area were state parks, cook park was washington county, belle view point was publicly accessible
  • May 1981, legislative hearing endorses the so-called "40 mile loop", now "the intertwine", which
  • August 1981, adjacent county land had been operated as a motorcycle park, but closed due to budget cuts. Recall that the county had opened it after an ordinance cracked down on offroad motorcycles. But closing the motorcycle facility did not revive o

Saturday, December 06, 2025

Highland Butte

Visitors to Portland are generally subjected to a pile of trivia that's meant to show how weird and quirky we are. World's smallest city park, various things that were filmed here, donuts, Shanghai tunnels, quirky food carts. They're told to check out all the breweries, giggle about all the strip clubs, and so forth. The trivia will have a whole section on Local Nature Facts, so you'll hear about the coast and the gorge, and maybe something about Forest Park being the world's largest city park (which is not actually true), and sooner or later the list gets around to volcanoes.

This, admittedly, is not something you'll encounter in most major US cities. But we've been promoting it all wrong for the last century or so. The original claim was that Mt. Tabor was the only volcano within city limits anywhere in the world. Or at least anywhere in the US. Or, at minimum, in the US excluding Alaska and Hawaii. And obviously we're only talking about major cities here, and stipulating that little fun-sized lava domes like Mt. Tabor count as individual volcanoes (and volcanic vents in the West Hills don't). And then City Hall went and moved city limits outward, which brought a few more lava domes into the city, although they obviously don't count due to being east of I-205, or (in the case of Rocky Butte) just barely west of it, and still east of 82nd Avenue. Meanwhile, Gresham and Vancouver and even Lake Oswego expanded to include a few of their own, but any geologist will tell you that suburban volcanoes absolutely do not count, period. And technically most of the Northwest east of the Cascades sits on top of a deep layer of Columbia River flood basalts, but that doesn't count, because reasons, and the hair-splitting just goes on and on. Frankly this all seems like overkill, since the point of all of this is to impress random tourists and conventioneers from the Great State of Corn Rectangle, who have never seen a hill of any kind before.

Another approach is to forget about Mt. Tabor and run with Mt. St. Helens, which is obviously not within city limits but is at least visible from here. The winning move here is to point out the mountain and reassure your audience -- as nonchalantly as you possibly can -- that there's no need to worry, it hasn't erupted at all since way back in 2008, and that one was no big deal, and besides, we're upwind of the mountain and almost never get volcanic ash falling from the sky. This is their cue to look at each other and chuckle nervously, which is the effect you're going for. This will be great fun for a while, but there are a couple of potential downsides. First, your visitors from Corn Rectangle will see this as an opening to tell you about their many white-knuckle tornado encounters. Which is only fair, frankly. Second, it's 2025 now, and sooner or later an impertinent teen in your audience will agree that 2008 was a long, long time ago -- before they were born, in fact -- and so long ago that the mountain is probably extinct by now. And this will not only make you feel old, it might be enough to troll the volcano into erupting again.

And let's be honest here, neither Mt. Tabor or Mt. St. Helens is exactly on brand for us these days. Mt. Tabor is in a ritzy, unaffordable neighborhood and none of its superlatives are actually true, and St. Helens is in a whole other state -- a state with sales tax -- and biking to the top is probably a nightmare. They also have their own Wikipedia articles, and are featured prominently in coffee table books about the region, and just in general are way too mainstream, and thus desperately, terminally uncool.

So with all of that as an intro, it's time to meet Highland Butte, the subject of this post and an obscure local volcano you probably haven't heard of. It's not the tallest volcano in the Boring Lava Field -- Larch Mountain out in the Gorge wins that one by a wide margin -- and I've seen conflicting things on whether it's the southernmost, but it may be the oldest and widest of all of them. A 2009 paper on the Boring Lava Field notes that Highland Butte rocks have been dated to around 2.4-2.6 million years, making it the oldest, or among the oldest of the Boring volcanoes. A lot of other sources say it's around 3 million years old, but I don't know if that's from a different measurement or just someone rounding up to the nearest million. For comparison, Mount Hood is estimated to be no more than 1.3 million years old, Mount Tabor is a bit over 200,000, and Beacon Rock -- the youngest of the bunch -- is only around 57,000 years old.

The summit is a sort of Mt. Tabor-sized dome in a wider rural area known as "Upper Highland", but by the time you see that hill you've already been driving or riding on the volcano for several miles. It's a roughly circular area about 7 miles in diameter centered on the summit and gently sloping away from there, and all streams for miles around drain away from that point. Then there's an extension to the north all the way to Oregon City and the Willamette. I don't know if that's as far as the lava got, or that's where the river cut a path thru later, but it explains the present-day cliffs along the river, and probably the rocks that form Willamette Falls too. I had a vague recollection that I'd read something to the effect that the large rounded boulders here at the main entrance to the Clackamas Community College campus were thought to be volcanic bombs thrown to the campus from the summit, nine miles to the south. I finally located the article where I got that idea from, an April 1986 column about the boulders by the paper's geology columnist. He specifically ruled out the volcanic bomb theory on the grounds that the boulders were too big, and they lacked the distinctive markings rocks take on when they form as blobs of lava hurtling through the air. Instead, he explains, this is just a weathering pattern typical of Boring lava rocks when exposed to the elements, and they just sort of become spherical over time as their exteriors degrade into iron-rich red dirt. Apparently Columbia flood basalts (the other common type of basalt you'll see around here) are denser and darker and they just don't come apart like this.

The summit peak doesn't look all that impressive, but it's still the highest point for miles around, which is why you can visit the place now. First, nobody claimed it as farmland back in pioneer days, or at least nobody successfully claimed it, and the ill-fated Oregon & California Railroad seems to have had no better luck finding a buyer for it, so it was still federal land in the early 20th Century, at which point someone realized it would be a great place for a forest fire lookout.

So here's a 1927 article on the summit's brand new modern Forest Service fire lookout tower. The article explains that while this is the first tower, the summit had been a GLO fire lookout for years before that, in the form of a "peg tree". What you would do is pick out a tall tree near the summit, and hammer wooden pegs into the tree trunk in a spiral pattern, forming a sort of primitive spiral staircase up the tree, like something Ewoks would have in Return of the Jedi. In this case, the stairway used 114 pegs and circled the tree 5 times, taking the fire observer to a point in the treetops, 142' off the ground. Once you were up there, you would just sort of hang out in the top of the tree with a pair of binoculars looking for forest fires and swaying with the breeze. This doesn't sound like a very effective way to keep an eye on the horizon with binoculars, and a great way to get motion sick, but may have been all the GLO could afford. The forest service built a tower, plus a house at the base of the tower for the rest of the lookout crew when they were off shift, plus the road to the summit, and they were even considering putting in a telephone at the base so would-be visitors could call uphill and check if anyone was on the way downhill before trying to drive up.

The article included a photo of the peg tree, so it seems to have been spared when the summit was logged, sometime between 1911 and 1927. I was (and am) kind of curious whether that tree still exists (though I'm pretty sure the pegs either wouldn't be there anymore or wouldn't be climbable). I didn't see any one particular tree that was much bigger than the others, and didn't see one with a spiral of wooden pegs sticking out of it, so it's anybody's guess.

If you want to visit now, the road to the top is gated and locked, but it's simple to park so you aren't blocking the gate and then walk the rest of the way. Or you could come here by bike and ride to the top, though the fresh gravel along the road seemed to be of the especially sharp and tire-puncturey variety. Either way, the road is a bit steep at times, but it's not very long and you only go up a couple of hundred vertical feet from this point. One sort of unfortunate thing is that there isn't much of a view from the top at present due to all the trees in the way. I say "at present" because the land here is designated as part of the O&C Lands, and it's clearly been logged before and most likely will be again, and there will be more of a view from here once they get around to that. So I guess there's that to look forward to.

Over the years the lookout tower existed, Highland Butte was occasionally in the news. Not for erupting or anything earth-shaking like that, but minor news items came up every few years:

  • The summit was visited by a Trails Club hike in 1934, so there was presumably still a view at that point.
  • There was a small forest fire nearby in 1951. The article doesn't say whether the fire lookout helped or not.
  • A field trip by the Geological Society of the Oregon Country visited in 1957
  • The summit gained a second tower for a while starting in 1960, a microwave communication tower for an emergency system bypassing Portland in case the city was destroyed in World War III. The new tower would talk to another antenna to the south near Silverton, and one near Mt. Livingston to the north, somewhere out in the back of beyond due north of Camas.
  • A full-page photo of this tower with Mt. Hood in the background appeared in AT&T's 1962 corporate annual report, I guess as one of their more photogenic recent technological advancements, if you can avoid thinking about why it was built. Not quite photogenic enough to make the cover of the report, which features a phone operator wearing a headset and smiling while she pages through an enormous phone book.
  • The fire tower lasted until the 1962 Columbus Day Storm flattened it, and they never built a replacement, and after that the place languished in even deeper obscurity than before. Then sometime around 2019-2020 the summit got a new tower, this time a shiny new Clackamas County EMS radio tower, built to close some coverage gaps in this hilly, rural area.
  • You might have noticed that the BLM got the land back from the Forest Service at some point. I don't know any more details about it than that, but I can see that happening if it wasn't going to be used for a lookout tower anymore. There isn't any other Forest Service land nearby, while there's an actual BLM facility with actual people a few miles SE of here, namely the agency's Walter H. Horning Tree Seed Orchard. The sign at the front gate includes sort of a mission statement, which is readable on Street View: "To produce seed for growing trees of superior quality which will best use the productive capacity of forest lands.", and a few of its Google reviews indicate it also hosts trail rides by local equestrian clubs and even the occasional Civil War reenactment (!). In any event, it was probably just more practical for them to send somebody around to keep an eye on the place now and then instead of having the Forest Service do it.

McCord Creek RR Bridge

Ok, here's the next Columbia Gorge train bridge, and this is one I was initially not going to bother with, even in this already sort of dubious sub-project, because it sure looks like it's just a big concrete culvert under the tracks, and those don't count because there would be no end to this project if I did that. But I saw that the Federal Railroad Administration GIS layer for train bridges has a database entry for it, so I guess legally it counts as a bridge. And thanks to that db entry I can tell you it has a Design Type of "Unknown", and a UniqueID of "W31_OR79215". And more importantly, and regardless of whether it's really a bridge or not, this is a low-stakes and (as far as I can tell) completely harmless golden opportunity to shrug and publicly go along with at least one federal government decision that (just between us) may not be entirely fact-based, I mean, if you look at it from a pre-2016 standpoint.

If you'd like to go see it and decide for yourself whether you think it even counts as a bridge, one way to do that is to park at the Elowah Falls trailhead and take the HCRH Trail (i.e. the paved path next to the freeway) to the retro-styled trail bridge over the creek, or a short distance just past it, and look through the trees and under the freeway bridges, and this probably works best when the trees are bare. If you want a closer look, there's a small parking area under the I-84 overpasses that I think is usually used for fishing access. I've never actually been over there, and I'm not about to make a special trip just for this one blog post, but it looks like the access road for this parking area turns off of Warrendale Road at the first right just off the westbound Warrendale exit.

Tumalt Creek Railroad Bridge

Next up we're looking at yet another really obscure Columbia Gorge train bridge. This one is on Tumalt Creek, which is in the Dodson/Warrendale area just east of the main tourist corridor, and we're on a dead-end back road instead of continuing down the old highway since the road and train don't run parallel through here. This one is behind some trees and bushes and we can't see it as well, but the federal GIS system I'm getting this info from says that like the others we've looked at, it's single track, non-moveable, and this time the design type is just listed as "Unknown", with a unique ID of "W1007_OR24756". From what I could see of it, this one seems to be on a concrete beam instead of steel, and if I had to guess when it was built I would probably guess no earlier than the 1990s. The reason for that is the creek it's on, which is the largest of about a dozen in this stretch of the gorge, all of which are prone to massive landslides of mud and rocks and giant boulders, and this creek specifically was one of those involved in the 1996 slides that closed I-84 for weeks. I don't know whether this bridge was ever physically washed out at any point, but at minimum all that material coming down and trying to flow underneath is at least going to cause a bit of excess wear and tear over time.

The name "Tumalt" is not the result of Lewis & Clark trying to spell "tumult", although that would be a reasonable guess. This was one of the names bestowed in 1916 when the Mazamas (a prominent local mountaineering club) decided that prominent sights along the new Columbia River Highway should generally have Indian names, with a few melodramatic bits of European mythology tossed in. (Note that these were not actually what local tribes called these places before settlers showed up, but a selection of exotic-yet-pronounceable words, often with background stories that white people found appealing in 1916. In particular, the creek is named after Tumulth, a member of the Cascades tribe, and a tragic figure of the Yakima War of 1855-1858, and specifically the 1856 "Cascades Massacre", a raid on the white settlement of Cascades (near present-day North Bonneville, WA) by members of the Yakama and allied tribes. The local Cascades tribe was apparently not involved in this incident, but became the focus of settler retaliation afterward as they lived nearby and it was more convenient, and Tumulth was one of several men who were summarily hanged for their supposed involvement. Here are a few links for more info about him and the whole conflict:

Before the current name, the creek was widely known as "Devil's Slide Creek" due to its ongoing geological tendencies. Yet despite that name two distinct towns sprang up in the main landslide corridor, Dodson right around here, complete with its own train station, and Warrendale a mile or so to the east, both named after local canned salmon tycoons of the late 19th and early 20th centuries. Frank Warren, namesake of Warrendale, was possibly the biggest and wealthiest of them all, but his fishy empire quickly fell apart after his watery demise on the Titanic, which roughly coincided with a crash in the salmon population. Seriously. You can't make this stuff up. Or, I mean, technically you can, but reviewers will roll their eyes and make fun of your ridiculous hamfisted plot twists.

Sunday, November 30, 2025

Horsetail Creek Railroad Bridge

Next up we've got a few photos of the train bridge at Horsetail Creek, just down the tracks from the Oneonta Creek one we looked at in the last post, and just downstream from the HCRH Horsetail Creek Bridge, which we visited back in 2018. Federal railroad GIS says this one is like the others we've looked at today in that it carries a single set of tracks and is not a drawbridge or any other kind of moving bridge. Like its neighbor to the west, the ridge type is listed as "Regular Steel Beams/Girder + Misc. Steel bridges", and it has a UniqueID of "W811_OR24818", for whatever that's worth. This one does look different than the Oneonta one and I don't think it's of the exact same design, like it's being held up by multiple smaller steel beams rather than one large girder. Like the others I have no information on how old this bridge might be, and I don't think I could even guess a correct range of a few decades. Regardless of that, the sorta-handrail on this bridge looks like a later addition and may coincide with the advent of modern personal injury law.

I have two mildly interesting and not particularly old items to pass along this time around:

  • A 2012 Horsetail Creek floodplain restoration design doc. This project re-engineered the large low-lying area between the old highway and Interstate 84 to make it more friendly to baby salmon, implementing various things from the standard baby salmon playbook, like plenty of woody debris in the water. Regarding that, let me point you at this post from about a year ago -- it's technically about some new-ish salmon-themed art in the South Waterfront area, but while putting the post together I came across various sources indicating we don't actually understand the various needs of baby salmon anywhere near as well as we think we do. Also I think that post is one of my better recent ones, and is probably more entertaining than the one you're reading now. And if you're wondering why I'm mentioning all this stuff, the link to the 2012 plan came up in search results because the bridge here and the one on Oneonta Creek mark part of the boundary of the study area.
  • A 2009 Multnomah County planning approval doc for placing power lines underground, explaining how the proposed work complies with all sorts of regulations. A window into what it takes to get anything done when your proposed project is going to take place within both Multnomah County and the federal National Scenic Area. Behold and despair as a maze of agencies endlessly consult and re-consult with each other and struggle to get anything done, even though nobody actually objects to the proposal.

Oneonta Creek Railroad Bridge

So next we've got some photos of the train bridge at Oneonta Creek, continuing east on this little speedrun. We visited the ones at Bridal Veil and Wahkeena Creek in the previous two posts, and saw the one at Multnomah Falls back in 2018, so I guess this one is the logical next step. Federal railroad GIS says this one has a unique ID of "W925_OR24624", if that means anything to you, and lists the bridge design type as "Regular Steel Beams/Girder + Misc. Steel bridges", which I don't think is exactly a technical engineering term. You can see that this one is supported by a steel beam or girder underneath the bridge instead of two on the sides, and you can also see that it has substantially more clearance above the creek than the Bridal Veil one does, so the designers didn't have the same design constraints as the Bridal Veil bridge.

This one also sits just downstream of the two HCRH road bridges, which brings us to the one and only mildly unusual detail I have about this one. Before civil engineers got their hands on it, the Columbia River once ran fairly close to the bluffs at Oneonta Creek, close enough that at one spot just east of the creek the railroad took up all the usable space between the river and the cliff. A few decades later, when the Columbia River Highway got here, the railroad wouldn't budge and highway engineers ended up having to dig the Oneonta Tunnel to continue the road east from there. Eventually the state decided to build a river-level road to replace the winding and twisting old highway, which involved quarrying vast quantities of gravel and filling in some areas along the river where there was no existing flat land available. Once that had happened through here -- on the taxpayer dime -- the railroad was suddenly much more amenable to moving, and in 1948 a sort of switcheroo was arranged: New, rerouted tracks were built, and then the existing bridge was somehow moved sideways to the current bridge location, and train traffic was shifted over to there. Then a new stretch of road was built where the train used to run, complete with a shiny new modern bridge. And when that was finished, they shifted traffic to the new road around the cliff, blocked off the Oneonta Tunnel, and used the original 1914 highway bridge for parking.

That last detail actually resolved another problem with the original alignment, which was that there was nowhere to park if you wanted to stop and wade up Oneonta Gorge. As a 1946 doc explains, the state ended up leasing a bit of railroad land for a parking lot and grandly declared that little area to be a new state park, which then quietly fell off the rolls after the realignment.

The switcheroo details come from February 2000 nomination designating parts of the highway of as a "National Historic Landmark", which I gather is similar to the National Register of Historic Places but with stricter rules on how intact a thing has to be, such that the whole road qualified for the National Register, but only certain parts were good enough to be a Landmark. The doc went on to explain that the 1948 road bridge here was a "non-contributing structure", but its presence was not enough to derail the whole nomination since the original bridge was bypassed and left in place instead of being removed. So that's nice, I guess.

Wahkeena Creek Railroad Bridge

So next up we're looking at the little railroad bridge over Wahkeena Creek, which is the next train bridge east of the one at Bridal Veil that we just looked at. This one sits on top of a girder (either steel or concrete, I'm not sure which) instead of having two of them on the sides, and in general it looks like it might be a recent replacement of an older bridge, but I don't know that either because federal railroad GIS doesn't have that info. What I can tell you is that it has a unique ID of "W1012_OR24759", and a design type of "Unknown". If you had high hopes that this bridge was made with advanced alien technology or something you're likely to be disappointed. I think it just means the data entry intern didn't have that info or couldn't be bothered typing it in.

The one semi-interesting thing about this one is that the rail line also serves as a physical divider between the Wahkeena Falls area (the side I took these photos on), which is a Forest Service day use site, with free parking, and Benson State Park on the far side of the tracks, which has been a pay-to-park fee site as long as I can remember, long before anywhere else nearby was. This is possible because Benson is set up as sort of a walled garden, with no official trails (or, ideally, a railroad-approved skybridge over the tracks) between it and either Wahkeena Falls or Multnomah Falls next door. Otherwise people of the cheapskate persuasion could just park at Wahkeena Falls and haul an inflatable raft over to Benson Lake without paying the state a penny. And now it works both ways: During peak tourist season, the demand for parking at Multnomah Falls far exceeds the available supply, and if visitors could easily use Benson as overflow parking it would probably mess up the whole timed entry ticket scheme they've been using to try to manage crowds over there. And that demand would probably swamp the smaller numbers of people who just want to fish the lake or grill some burgers or whatever else there is to do at Benson itself. And I'm sure these are all very good and responsible reasons for things being how they are, and why they have to stay that way forever, but when you're standing on one side and you can easily see the park on the other side, and there are signs saying you are strictly forbidden from going over there, the whole arrangement just seems incredibly dumb.

Bridal Veil Railroad Bridge

This may surprise some of you, but not every weird project I have a go at turns out to be a winner. Some years ago, I did a series on old historic Columbia River Highway bridges, which was fun because they were all a little different, and the engineers who designed them had gone the extra mile to show off what was possible with modern concrete technology, where "modern" meant roughly 1914-1920. So I eventually ran out of those, or more to the point, I hit the long tail part where the remaining items on the list are either small and not very interesting, or far away and hard to visit, or often both. It occurred to me at some point that instead of driving for hours on end, further and further east out into the desert wastes, there was a whole second set of old bridges through the Gorge, used by the Union Pacific railroad that often ran right next to the old highway, and by and large they're at least as old as the highway ones, and it ought to be fairly straightforward to go see a bunch of them and then share some fair-to-middlin' photos and whatever fun trivia I can dig up. That formula usually works out ok; the problem this time around is that there seems to be precisely one interesting train bridge on the Oregon side of the Gorge, the Tanner Creek Viaduct, the big sorta-Roman-aqueduct structure next to Bonneville Dam, and we already visited it way back in 2014. The others fall into two basic categories: Rivers and larger creeks get a steel through truss bridge, like the one on the Sandy River (visited way back in 2009), and anything smaller gets a simple steel beam or girder design, like the one at Multnomah Falls, but without the vintage sign giving mileages by train to various semi-distant cities.

The bridge you see in the photos above is one of the latter category. This is the old railroad bridge at Bridal Veil, downstream of the falls and the trail and next to the site of the old Bridal Veil Lumber sawmill. What little info I know about it comes from a terse database entry in the Federal Railroad Administration's "Railroad Bridges" ArcGIS layer, which informs us this is a "Steel Through Plate Girder" bridge, it crosses over water, is "fixed - non-moveable" (as in not a drawbridge or something), carries one set of tracks, length is not specified, and has a UniqueID code of "W712_OR24695", whatever that means. And that may be all the info Uncle Sam knows about it. I think the db essentially has whatever info the railroad feels like sharing voluntarily, so no details about stuff like the last time a bridge built sometime around 1907 was inspected for rust and structural soundness and whatnot. And I'll just point you at the Steel Bridge and Portsmouth Cut posts if you want to know how things go when your city depends on railroad-owned critical infrastructure and they don't have to tell you anything if they don't want to. The state government knows how little leverage it has, which explains things like a state Fish & Wildlife map of Fish Passage Barriers, which flags every last tiny creek, stream, and seasonal rivulet as a potential fish barrier where it passes under I-84 or the old highway, but not where it passes under the railroad, like they know they can't do anything about that particular barrier and would rather not poke the bear if they can avoid it.

I did find a railfan page that briefly explains what a "Steel Through Plate Girder" bridge is and how it works. See those railings along the length of the bridge? They aren't a safety feature for derailments, and they aren't a pedestrian feature from the old days when passenger trains stopped here. No, those heavy duty "railings" are actually the main load-bearing structure of the bridge: Each girder has a post on each end that attaches it to the concrete bridge piers, and then the bridge deck is attached to the beams, and then the bridge deck is a relatively thin layer attached to the bases of the two girders. The page notes the main reason you might use this design is if you don't have a lot of clearance between track level and whatever it is your bridge needs to cross, which is certainly the case here. Listed along with that are several limitations: "Easy to damage", "Difficult to replace", and "Limited to one track between girders (two possible with depth increase)".

Those design concerns may also explain why I don't think I've ever seen a regular motor vehicle bridge of this design. For one thing, a road bridge is bound to have the occasional vehicle banging into the railing for any number of reasons, and it sounds like this could be rather consequential, both for the bridge and the driver, since these support girders probably don't have the same degree of give on impact that a regular highway guardrail would. And with a road bridge you can usually get around any clearance issues by just building the bridge higher up and putting a ramp at either end, which you can't really do with trains.

Anyway, those bridge design concerns probably explain why the line is single track over the bridge, but is double track for about a mile immediately east of the bridge, ending somewhere around Old Boneyard Road. This was probably done to accomodate freight trains that used to stop at the lumber mill that used to exist here, and the railroad still keeps Bridal Veil on the books as an official train station. This is per federal GIS data, again, which says the station's unique station ID is "UP06258853437", though before anyone gets excited about this, note there is no actual freight or passenger infrastructure in place. Maybe they do this on the off chance the Columbia Gorge timber industry stages a big comeback, or there's a huge boom in the mailing of wedding invitations from the tiny Bridal Veil post office here, or the Oregon side of the Gorge gets passenger rail service again, or who knows.

Saturday, November 15, 2025

Baker Creek Falls

Next up we're taking a peek at Baker Creek Falls, a small waterfall in rural Washington County, in the hilly area west of Sherwood. This is part of Metro's Baker Creek Canyon Natural Area, an obscure greeenspace area the agency purchased in 2011 or so. These late summer photos don't really do it justice; a Waymarking page for the falls has a photo of it when it was running at a much higher volume. I meant to go back on an early spring day and get better photos of it but getting there is a bit of a long drive to the far end of the metro area and then a few miles past there, almost into Yamhill County.

This a Metro Natural Area, as opposed to a Nature Park, so there are zero visitor facilities beyond the cute little Natural Area sign (if you can find it) and the agency does absolutely nothing to get the word out about it to potential visitors. Some Natural Areas like this may never get more development than they have now. Others will be upgraded to Nature Parks someday, but not during your lifetime or mine. The thing to understand here is that Metro takes a very long-term view of things, surprising for a government agency in this country. They prioritize buying land above building amenities, on the theory that nobody is making new undeveloped land; what's there now is as much as there will ever be, and it's not going to be any more affordable in the future than it is now.

The good news is that the falls are right next to a road and easy to get to, so you're not going to need much in the way of facilities. Have your favorite driving directions app guide you to the intersection of SW Kruger Rd. and Dutson Dr., which is right at a sorta-hairpin corner on Kruger. This is also where Baker Creek passes under the street. Just west of there, immediately past the bend, there's a flat stretch of shoulder on the westbound side of the road, on the inside of the turn, with enough space for maybe 2-3 regular-size vehicles, or quite a few bikes, or between 0.5 and 2 luxury SUVs. I mention that last bit because this area is a short distance from the vineyards of Yamhill County, and seems to be rapidly filling up with McMansions and hobby farms. So you can kind of sense the urgency of Metro's land-buying efforts here. On the positive side, on the way here you'll see lots of cute llamas and alpacas randomly hanging out watching the world go by, so you can look at them and just ignore the ghastly 6000 square foot Tuscan-Victorian chateaus and whatnot where their people live.

So assuming there's room to park, park there and look for a really obvious unofficial trail heading downhill to the creek. Follow it toward the creek, then look upstream for the waterfall. At this point you can decide for yourself whether it was worth the effort to get here, which is obviously going to depend on the season and how far you had to drive to get to this point. If you're just coming from Sherwood or maybe Tualatin, it probably counts as a cool local attraction, kind of like Cedar Hills Falls in Beaverton. If you're coming from downtown Portland, like I was, it's a lot of trouble to get to for how small it is. I thought it was still worth visiting, but I also recognize that doing things "for the sake of completeness" motivates me a lot more than it does most people, plus even if it had gone completely dry when I visited I'd still get a blog post out of it.

I don't have any news stories to share about the falls, or the creek, or the rest of the general area, but I did come up with a short list of Metro documents and press releases that refer to it, so here we go:

Beaver Creek Canyon, Troutdale OR

Next up we're doing the hike around Troutdale's Beaver Creek Canyon. This particular Beaver Creek is a large tributary of the Sandy River that begins somewhere south of Oxbow Park and flows north, roughly parallel to the Sandy River, eventually joining the river at Depot Park in downtown Troutdale. On its way there it flows thru a surprisingly deep and narrow canyon for a couple of miles. Surprising as in one stretch seems to be over 150' deep, so not on the same scale as the Columbia Gorge to the east of here, or the Sandy River Gorge south of here, but it's big enough to make you forget you're still technically in suburbia. Which you can do here because it's a Troutdale city park, and there's a trail through it, or at least part of it.

If you look at a map of the area, like the one above, you'd think this would be a straightforward hike: You'd park at Glenn Otto Park, which borders Beaver Creek for a bit, and the trail would head south from there. But right at the mouth of the canyon are several private landowners, served by a private road with a big "No Trespassing" sign posted. As far as I could tell there isn't an interesting or dramatic backstory to this situation, or if there is the story never made it into a newspaper with searchable archives. Whatever the exact details are, the 50,000 foot version is probably just landowners not wanting to sell, and/or the city not having the money to buy. In any case, the "actual" route is a bit longer but possibly more interesting than the direct route would have been.

So the route we're taking goes a lot like this: Starting at Glenn Otto, cross Beaver Creek on the pedestrian bridge and stroll along the sidewalk heading for downtown Troutdale. After a few blocks you'll see signs for the Harlow House Museum, a house belonging to the city's colorful founder. Behind the house, there's a small landscaped garden, and behind the garden you'll find a trailhead marked something like "Harlow Canyon". Because this initial stretch follows an entirely different creek with its own watershed. The trail heads uphill briefly, crosses the tiny canyon's tiny creek right where it makes a cute little mini-waterfall, and then ends at a trail junction. One option seems to dump you out onto a suburban city street, while the trail on the left continues in a narrow corridor right along the edge of the bluff, a near-sheer drop on one side, and a bunch of backyard fences on the other. There isn't a city parks page for this bit of trail, but it appears to be called the "Strawberry Meadows Greenway", named for the subdivision here. Which in turn (following the usual practice with subdivisions) was named for the strawberry farms that once dominated the area. This part is a fairly popular community walking trail, so you might get waylaid by chatty retirees unless you look like you need to be somewhere on a tight schedule. Eventually this trail ends too, I think right at the subdivision boundary, dumping you out on a regular suburban street, SE Beaver Creek Lane. Luckily this is the kind of suburb that has sidewalks, because that's the next phase of the hike. You're looking for either of two entrances to Beaver Creek Canyon, which start as nondescript paths between houses. There aren't any big signs announcing where they go, either. The first one is across the street from the intersection with Chapman Ave. The second one is across from tiny Weedin Park. Pick either one, and before you know it the concrete path becomes several flights of stairs down into the canyon.

Either entrance puts you on the same sloping trail down into the canyon, which brings you to the park's main trail junction. From here you can turn right and follow the creek south/upstream, or follow the trail as it turns left and follows the creek north/downstream. The exact distance you can go in either direction varies a lot over time, shrinking when a winter flood or landslide rolls through, and expanding when the city finds grant money or volunteers to repair flood and landslide damage, or even (once in a blue moon) to expand the trail network. There will be anywhere between zero and two footbridges over the creek; if the current number is one or more, you may have access to a parallel trail on the east bank of the creek, and -- if it's a good trail year -- that trail might connect to another entrance here. If there's currently a bridge in existence at both bridge sites (which is rarely true), you can do this part of the park as a loop. The southbound trail may also connect to trails in Kiku Park, depending on current landslide/repair conditions, which would be a third way in from the west side. I didn't check on this when I was there and it may have changed since then, and could change again between when I'm writing this and when you're reading it.

Even further south, there's yet another westside entrance here, which apparently goes to a small loop trail disconnected from the rest of the trail network. I didn't visit this area and have no photos of it. It's separated from the rest of the park by the deepest and narrowest stretch of the canyon, so I don't know whether connections to the rest of the park once existed and don't anymore, or whether they never got funding in the first place, or whether it's even physically possible to build a trail through that part. Upstream from there, Beaver Creek passes through a jumble of public land and farmland without trails, and the canyon starts somewhere in that area. Continuing upstream, Beaver Creek flows through a city park that's called either "Bellingham Greenway", "Mountain Vista Greenway", or "CEF Open Space" depending on whose map you're looking at, with an entrance here and another somewhere around here. And on the south side of SW Stark St. is the Mt. Hood Community College campus, which has a ~65 acre Metro wetland area running along either side of the creek, and a small trail system we'll meet in another post. South of the college, the creek runs more or less along the edge of suburbia (as of 2024) for a bit, incuding a few disconnected units of Gresham's Beaver Creek Management Area here, here, and here, the last two possibly with trails connecting them. Then it's just farmland all the way south to where the creek begins, a bit west of Oxbow Park.

The park is like this because of the Great Troutdale Land Rush of the late 1970s. Subdivisions sprouted like invasive weeds all across east Multnomah County generally, and Troutdale in particular. I think it was largely because it's where the large blocks of cheap land and motivated sellers were. The local strawberry industry had been rapidly outcompeted by larger, cheaper, and completely flavorless, styrofoam-like strawberries from California, mostly because their strawberry varieties can survive long bumpy journeys in an 18-wheeler while ours don't, and theirs hold up under being dipped in molten chocolate and then sitting on grocery shelves for weeks. And our strawberries... don't. Long story short, it was a great time to sell around here, and most of the land on either side of Beaver Creek became housing over a few short years, right up to Oregon's mega-recession of the early 1980s. It probably helped too that house hunting is largely a spring and summer phenomenon and prospective buyers wouldn't get to experience what Troutdale winters can be like until it's too late. In any case, the city responded to this wave by being surprisingly forward-looking by Portland suburb standards, and not immediately bowing down to whatever developers wanted. A 1977 Oregonian article, "Wilderness survives amidst housing" explains that the city generally required developers to hand over some land for city parks as part of getting your subdivision approved, and in this part of town that included any land in the canyon. You couldn't build there anyway, for flood control reasons. The city also required that private property along the canyon rim had to be in natural vegetation, to limit the visual impact of subdivisions up above. Which probably also reduced the risk of distracted gardeners taking a big tumble while weeding.

Somehow this actually worked, and the parts of the canyon that are protected now are protected because of adjacent subdivisions. This is not how things usually turn out, to put it mildly. But thanks to the county surveyor's office putting records online we can look at the subdivision plats for Sandee Palisades phases I (1/77), II (2/78), III (12/78), and IV (12/90) on the east side of the creek, and the ones for Corbeth (6/77), Rainbow Ridge (5/76), Kiku Heights (2/77), Beaver Creek Estates (2/78) Weedin Addition (7/77), Mountain Vista (1992), Bellingham Park (5/97) and Strawberry Meadows (4/95) on the west side, each one showing the concessions developers made in exchange for the privilege of building here. Not just donating land that was probably unbuildable anyway, but providing access points into the park.

The 70s were a time of grand plans, and there was indeed a grand plan for Beaver Creek. The hot new idea back then was the "40 Mile Loop", a future regional hike-n-bike trail network encircling the Portland metro area. Eventually someone remembered the "circumference equals Pi times two times radius" formula from high school and realized that encircling the metro area would involve quite a lot more than 40 miles of trails, and a few years ago they rebranded the concept as "The Intertwine". In any case, no version of this loop has never been anywhere near completion, but I would guess that it has a cameo in every last urban planning document produced in the Portland area since the Tom McCall era. I think the idea is to not do anything to preclude a future bit of Intertwine in your project area even though you aren't actively working on it just now. So the working idea has been that Troutdale's part of the loop follows Beaver Creek into town from the south, drops into the canyon at some point, and continues to the Sandy River and then along the Columbia on what eventually becomes the Marine Drive Trail, taking you back toward Portland. Or you could hang a right at Glenn Otto Park, cross the bridge, and follow either the HCRH Trail (i.e. bike in traffic until Elowah Falls) or get on Trail 400 at Lewis & Clark State Park (as soon as they get around to building that initial 5-10 mile stretch of trail) and follow it east to Cascade Locks where it intersects the Pacific Crest Trail, and simply walk to Canada or Mexico from there, as one does.

Which brings us to the usual timeline section of this post, which is basically a list of old news stories and other items I couldn't work into this post any other way. Nothing really earthshaking to share here, but you can see the decades-long pattern of the city scratching its head trying to figure out what to do about the place and how to pay for it.

  • 1978, meeting notice that Sandee Palisades III was in the city planning approval phase
  • 1982 article about the growing Troutdale park system. Mentions summer maintenance jobs were paid for with CETA grants. (CETA was the "Comprehensive Employment and Training Act of 1973", a late, lamented federal program that would pay for just about anything if you had a good grant writer.)
  • A similar 1983 article mentions the park briefly, director said the trails were too steep for bikes
  • Another article from around the same time noted the trail was now part of city's comprehensive plan, mentions that planned 40 Mile Loop route at the time was through the canyon.
  • Report on a mid-1990s project clearing invasive plants. Which sort of morphed into a restoration effort after the 1995-96 floods. A consultant told the city to move trails away from the creek and get rid of a bridge for causing erosion.
  • another project nearby in 1997, maybe in connection with the Strawberry Meadows subdivision going in.
  • 2004 city council minutes, discussion of parks master plan, with a member of the public blowing a gasket over another such proposed development deal, as it would be in exchange for low income housing this time. Thinks connecting the north & south chunks of park would cause crime, and if a park happens it should be a human exclusion area
  • Parks Master Plan, adopted 2006. The plan of record is to extend the existing trail along the creek in both directions, bypassing the current harlow creek / strawberry route. You could hike from Glenn Otto to MHCC. Discusses maybe obtaining easements for the gap to Glenn Otto vs buying, maybe owners aren't interested in selling or city can't afford
  • 2014 study connecting trail south to springwater corridor
  • 2020 OregonHikers thread about the park

HCRH Milepost 35

Continuing east, the next HCRH milepost on this weird little project is number 35, which -- conveniently -- is located right at the day use area portion of Ainsworth State Park, which we (as in, this humble blog here and its vast and rapidly growing global audience) last visited wayyy back in 2007. This milepost is unfortunately a bit worse for wear right now, or at least it was when I took the photos, and this one might just be reinforced concrete spalling, and not being sideswiped by some bro in a Hellcat trying to drift through here.

The park itself has an easy half-mile loop nature trail for the whole family, and Trail 400 passes through here too. Via the 400, to the west it's about half a mile to the Horsetail Falls trail and maybe onward to points west. To the east it's about a mile to the little-known, little-used Dodson Trailhead near Exit 35, and from there it isn't far to the rather un-picturesque setting of milepost 36. Not really a highlight of the Gorge, but if you're looking for unusual hike ideas, this is definitely one of them. If nothing else, it's a good trail to keep in mind if outdoor social distancing ever comes back.

If you aren't up for any hiking at all, it's probably a good spot to just hang out and watch the trains go by, if you're into that sort of thing.

For the higher difficulty levels, this is also where you would start if you're doing the legendary slash infamous Mystery Trail, or becoming one of the few people to ever climb St. Peter's Dome, or taking on the Ainsworth Left ice climbing route.

The park also has an overnight camping section, which might be the closest public camping site to Portland, with the sole exception of Oxbow Park. It wasn't always like this; until the late 1970s or early 1980s, there were plenty of others: Lewis & Clark State Park on the Sandy River at Troutdale; Dabney SP a bit further upriver, and Dodge Park even further south and east. Also Rooster Rock; the summit of Larch Mountain; and possibly Wahkeena Falls, though I'm less sure about that one. The powers that be decided this was attracting the wrong sort of person: Young, drunk, and disorderly partiers for one thing, but also people with nowhere else to go, and even people who were in town for the summer doing seasonal farm work, back when East Multnomah County was still largely rural. So now it costs enough to keep the poors out, and time limits ensure it's not a good option for seasonal workers, who instead get to live in whatever lightly-regulated housing a farmer feels like providing, out of sight and mind, and away from polite society.

Another nearby turnout has a roadside drinking fountain, fed by an underground spring. The Ainsworth page at Recreating the Columbia River Highway seems to indicate this is actually a bit older than the park itself, since the park was created in 1933 and the fountain was part of a statewide Highway Commission project in the 1920s. I think the "Sunset Springs" one on US 26 heading to the Coast is another survivor of this project, as was the recently-discontinued one on the HCRH across from Dabney State Park. Unlike those two, this one doesn't seem to have legions of devotees who come regularly to fill their VW Buses with multiple carboys of pure spring water. I'm not sure why not, though all the fancy stonework around might make it difficult to convince yourself you've come across a fountain "that was not made / by the hand of man", as the song goes.

The area is a bit thin on nearby historical events, but here's what I've got this time around:

  • For people planning their summer vacations, in June 1953 the Oregonian printed a list of state parks with a brief blurb about each. 46 acres, 37 miles east of Portland. U.S. 30, at the foot of St. Peter’s Dome. Ice-cold spring, footpaths, parking and picnic areas.
  • With later additions the park now comes to 171.97 acres. At least that's the number I come up with by adding up everything labeled "Ainsworth State Park" in the State Land Inventory System. That total includes a separate chunk of 25.08 acres along the river, directly north of I-84 Exit 35 and the railroad, which doesn't seem to be accessible, except maybe by boat. ODOT's Right-of-Way map and blueprint for the park shows the original park and the 1963 expansion
  • A month later (July 1953), an article about a land acquisition near Oneonta Creek mentioned a plan to somehow run a road up Oneonta Creek to Triple Falls, then cut over to Horsetail Creek to visit Ponytail Falls, rejoining the old highway somewhere near Ainsworth. I may have mentioned this proposal before; I keep coming across it when searching for other things, and it's just such a strange and alarming idea. I feel like I need to point out the bullets that were dodged when I run across them, I guess as a reminder that when a particular place or thing survives, that survival was often not automatic or guaranteed, and as inhabitants of the modern 21st century we are every bit as susceptible to harebrained schemes as our counterparts 50 or 100 years ago, and possibly even more so.
  • The state started talking about expanding the park in 1963, with the land to be used as a campground, and the expansion eventually opened in 1968.
  • October 1972 dueling pair of letters to the editor about the new campground. The first complains that the camping portion of the park was not natural enough and reminded them of a supermarket parking lot. The second letter, in response, claims to like it that way, insisting it's the nicest and cleanest state park around. I have never actually been to that part and have no personal opinion on the subject. Or, as real professional journalists like to say about everything, Both Sides Do It.
  • April 1985 interview with the Portland regional administrator for Oregon State Parks about his big plans for Trail 400, which was (and still kinda-sorta is) supposed to cover the whole distance between Troutdale and Hood River. The segment between Ainsworth and Elowah Falls / Yeon State Park had recently opened, and the next steps he had in mind were 1.) a route around Tooth Rock, between Tanner Creek and Eagle Creek, which was probably going to be expensive. 2.) A four-mile trail between Bridal Veil Falls and Latourell Falls, passing above Shepperds Dell and giving new views of the falls there. This was gated on some key land acquisitions and of course funding. 3.) A trail segment between Portland Womens Forum and Crown Point, which also needed some land acquisitions or easements. Something akin to item 1 happened in the late 1990s as the first segment of the bike-oriented HCRH State Trail. That project made its way around Tooth Rock via a segment of the old highway, rather than dynamiting a new ledge into the rock for the trail to use, while the Trail 400 that was eventually built makes its way from Tanner to Eagle Creek via a different route, with switchbacks on either end to gain/lose altitude, and then a roughly east-west route through the maze of existing Forest Service and BPA access roads in the area between the two creeks.