Multnomah Falls

Multnomah Falls

2.5 miles round trip, 850 feet elevation gain
Difficulty: Easy-moderate
Access: Paved road to trailhead, no fee required

620-foot tall Multnomah Falls is the highest waterfall in Oregon and one of the most stunning falls in the Pacific Northwest; it's also astonishingly easy to access, as it's less than an hour east of Portland directly off I-84. This beautiful double-tiered waterfall drops down the basalt walls of the Columbia River Gorge and can be seen without having to do any real hiking; the hike detailed here climbs from the base of the falls to a viewpoint at the top of the upper falls. As the falls are one of the most popular locations in the Columbia River Gorge, this hike offers a good way to see the falls while escaping the crowds at the base and at the bridge above the lower falls.

I hiked this trail in December after a rare low-elevation snowstorm paralyzed Portland and the Columbia River Gorge. My initial plan was to hike the Wakheena Falls Loop, but I-84 was closed due to snow and ice on the morning of the day of my hike, as was the Columbia River Highway, so I found myself just east of Portland, stuck in traffic with a line of tractor-trailers, with no way to head east. My backup plan of exploring Fort Vancouver National Historic Site fell apart once I discovered that the park's visitor facilities were closed on Sundays. I instead decided to take a day drive east along the Washington side of the Columbia River Gorge, which had stayed open despite the buildup of ice and snow in the gorge. After spending much of my afternoon touring the Bonneville Dam- the furthest downstream of the many hydroelectric projects along the Columbia River- I looked across the river and saw that traffic had resumed on I-84, so I decided that I would spend some time on the Oregon side of the gorge after all. I crossed the Bridge of the Gods into Oregon and then took I-84 west until reaching the Multnomah Falls parking area, which is sandwiched between the eastbound and westbound lanes of I-84. It's also possible to access the lodge at the base of the falls by driving the Columbia River Highway. Parking at Multnomah Falls can be very difficult on weekends and throughout the summer- in fact, it's a good idea to avoid this hike during peak tourist times as traffic jams can snarl the Columbia River Highway near the falls.

From the parking lot in the middle of I-84, I followed the underpass below the eastbound lanes of the interstate over to Multnomah Falls Lodge, where the hike started. From the lodge, a wide, paved, and flat path led about 50 meters to a clear viewpoint of this towering waterfall. The upper falls was the more impressive drop here, plunging 540 feet in a single go down a massive basalt cliff. The lower falls were much smaller, at just 70 feet tall, but still made a pretty drop down to a pool at the base of the cliffs. A pretty, arched footbridge spanned the gorge directly above the lower falls. The high basalt cliffs here were adorned with moss and on the winter day when I visited there was snow clinging to nooks in the cliff. The lower viewpoint is usually very crowded, as this is one of the most popular viewpoints in the state of Oregon.

From the lower viewpoint, a paved path led uphill to the right, making some switchbacks as it climbed steadily uphill to reach the footbridge over the lower falls in 0.2 miles. From the bridge, there was a view back down to the Multnomah Falls Lodge and the viewpoint at the base of the falls, as well as a close-up view of the towering upper falls, which were too tall to fit into a single camera frame. This is truly an impressive waterfall- in the contiguous United States, only the waterfalls of Yosemite have have combined such height with robust flow. During my visit, a wispy minor waterfall also tumbled off the cliffs to the right of the main Multnomah Falls.

Upper drop of Multnomah Falls

Most casual visitors to Multnomah Falls don't bother to go any further than the footbridge; hikers who choose to go further can experience the falls with just a fraction of the crowds. The paved path continued up the mountainside from the bridge, reaching a junction with the Gorge Trail at 0.4 miles; here, I stayed on the main paved path, making a sharp switchback and continuing uphill through forested slopes. The trail was paved but steep as it ascended through a series of switchbacks over the next 0.6 miles.

In September 2017, the forest around Multnomah Falls was badly damaged by the Eagle Creek Fire. The fire started when teenagers hiking the Eagle Creek Trail a bit to the east in the Columbia River Gorge set off fireworks in the forest, igniting an intense blaze that ripped through the Oregon side of the gorge. Hikers enjoying their Labor Day weekend were trapped by the flames and the Multnomah Falls Lodge was threatened but ultimately saved; ash rained from the sky as far away as Seattle, where I lived at the time. While the forest here was badly damaged by that fire and many of the trees that once grew on this slope are gone, the landscape is now in the process of recovering and the greenery will return. 

When I hiked here, the landscape was coated in fresh snow. This trailhead is generally accessible in winter, but hikers who come when there is snow or ice should bring traction devices like microspikes or Yaktrax, especially as the trail is quite steep.

Snow-covered trail

While ascending up the 11 switchbacks on this stretch of the hike, there were some good views out into the Columbia River Gorge. Cloud cover was low on the day of my visit, limiting the extent of views, but I was still impressed by the cliffs of Hamilton Mountain rising across the river and Beacon Rock, a large basalt outcrop rising directly above the Columbia. The Columbia River's near sea level crossing of the Cascades makes for steep terrain changes where the mountains meet the Columbia, which is responsible for the many impressive waterfalls found in the gorge, including Multnomah Falls.

Columbia River Gorge

A mile from the trailhead, I reached and then crossed a small saddle that marked the high point of the hike. From here, the trail descended slightly to a junction, just uphill from Multnomah Creek. The left fork headed off towards Larch Mountain, a local high point and the headwaters of Multnomah Creek. The right fork- which I took- was a short spur trail leading out to the Multnomah Falls Viewpoint. The trail was probably paved through here, but it was a bit difficult for me to tell due to the thick snow cover. The spur descended gently over the next 1/5 of a mile until it ended at a viewpoint at the very lip of the falls. There was a nice view at this observation platform of a very pretty cascade on Multnomah Creek just above the upper falls. After passing through this small cascade, Multnomah Creek then rushed downstream until it leaped into the air, its water droplets almost hanging in the air before wafting down to the basin far below. While I couldn't see the lower falls at all, Multnomah Falls Lodge, the viewpoint at the base, I-84, and the Columbia River Gorge were all visible. 

Cascade just above Multnomah Falls

The top of Multnomah Falls

Columbia River Gorge from the top of Multnomah Falls

On a snowy December day with just minutes of daylight left, I had the viewing platform at the top of the falls all to myself. If you come on a weekend or in the summer you'll undoubtedly have company as this Multnomah Falls is an extraordinary popular spot. Still, the top of the falls will be much less crowded than the base and the nice views of the Columbia River and the chance to see the waterfall from above make it a rewarding way to experience Oregon's tallest waterfall.

Table Mountain (Columbia River Gorge)

Mount Hood the Columbia River Gorge from Table Mountain

16 miles loop, 4200 feet elevation gain
Difficulty: Strenuous
Access: Paved road to trailhead, Northwest Forest Pass required

Soaring cliffs of columnar basalt make Table Mountain one of the most impressive peaks on the Washington side of the Columbia River Gorge. The views from this peak are stellar, sweeping over the length of the gorge and extending to the four nearby Cascade volcanoes; however, the approach to Table Mountain via the Pacific Crest Trail somehow manages to be long, a bit boring, and extraordinarily steep all at the same time. Experienced hikers may not mind the slog to get to Table Mountain's great views, but novice hikers and visitors to the Columbia River Gorge may be better off doing a more rounded and rewarding hike like nearby Hamilton Mountain. Hikers who do choose to come will find a trail that's relatively quiet despite its proximity to Portland and observe firsthand the landsape created by the Bonneville Landslide.

The long trail to Table Mountain can be broken down into a lengthy 6.5 mile approach to the base of Table Mountain and a extremely steep loop that ascends to Table Mountain's summit, visits some viewpoints, and returns to its base in 3 miles. Although Table Mountain is just 3420 feet high, the hike starts just above sea level and the undulating trail on the approach makes the cumulative elevation gain much more substantial. The approach trail spends most of its time traveling through clearcuts.

I hiked Table Mountain during an early November trip to the Columbia River Gorge. From Portland, I took I-205 north across the Columbia River into Washington and exited onto Washington Highway 14 heading east. I followed Highway 14 past Camas, Washougal, and North Bonneville to the Bonneville Trailhead, which was on the north (left) side of the highway just across from the entrance to the Washington side of the Bonneville Dam. The trailhead was well signed from the road and had a vault toilet and parking for about 20 cars; I put up my Northwest Forest Pass here after parking.

I started the hike out on the Tamanous Trail, a gravel path which initially paralleled a railroad track in a clearing before cutting to the right and beginning a gentle ascent into the forest as the railroad disappeared into a tunnel. The trail ascended about 200 feet to gain the top of a low, wooded ridge and then followed this ridge north to reach a junction with the Pacific Crest Trail at 0.6 miles. The forest on the Tamanous Trail was reasonably nice, with some scattered deciduous trees providing nice pockets of fall color during my November visit.

Forest along the Pacific Crest Trail

Reaching the PCT, I took the left fork to follow the famed trail northbound. You might think that being on the PCT should mean that there might be some better scenery, but you would be wrong; what followed was perhaps the least scenic stretch of the PCT in Washington State. For the next 1.7 miles, the PCT passed through a series of clearcuts, so the trail surroundings alternated between tree stumps, crowded growth of 10-foot tall conifers, and forest that looked to be fourth or fifth growth at this point. Occasional views of Table Mountain, the pyramidal rocky peak with a massive basalt southeast face that was my destination of the day, were the saving grace of this stretch of hike. The trail occasionally crossed the logging roads that run through this area and there was no sustained elevation gain or loss, although there were plenty of little ups and downs as the trail traveled through an undulating landscape.

At 2.4 miles from the trailhead, I crossed a logging road and came upon Gillete Lake, one of the many small pothole lakes that dot the landscape near Table Mountain. There were nice views here of Table Mountain rising above the lake and the scene was quite pleasant despite much of the surrounding area being clearcut. Power lines ran directly above the lake, ferrying hydroelectricity from the Bonneville Dam to points east. The trail descended and circled around the lake to the north, where a spur path led to the lakeshore.

Gillette Lake and Table Mountain

Leaving Gillette Lake, the trail crossed Gillette Creek and then continued through the patchwork landscape of clearcuts. Land ownership is quite complex along the PCT in this area: there is a mix of federal, state, and private land here, with different land managers subscribing to different forestry practices. After a gentle ascent up from Gillette Lake, the PCT followed a logging road for a hundred meters before a single-track trail split off to the right of the road; be sure to pay attention for the trail here. Passing by another pond, another logging road, and more clearcut, the trail reached a well built bridge over Greenleaf Creek at 3.5 miles from the trailhead.

Bridge over Greenleaf Creek

Greenleaf Creek marked the boundary of Gifford Pinchot National Forest and the conclusion of the clearcuts that dominated the early stretches of the hike. From here on, the surroundings felt much more natural. The trail switchbacked uphill for a bit before leveling out as it contoured along the side of a hill, passing a clearing with a view of the Columbia River Gorge. This stretch of the trail, which was forested but had partial views out to the gorge, was quite pleasant. At 4.5 miles, I passed a junction with the Two Chiefs Trail, which was an old road trace. 

Views of the Columbia River Gorge from the forested PCT

The trail was fairly flat until I reached the 5 mile mark of the hike, where the trail crossed a creek and then began a switchback climb up to a low ridge. Once atop the ridge, the PCT headed north while ascending steadily, eventually intesecting a road trace; the trail and the road trace paralleled each other briefly, so following either path is fine. The trail and the road trace soon combined as I reached the base of Table Mountain and the PCT began climbing more steeply along the lower slopes of Table Mountain.

At 6.4 miles from the trailhead, the PCT came to a junction with the Heartbreak Ridge Trail, which was marked by a large information board. From here, the Heartbreak Ridge Trail broke off to the right, headed towards the summit of Table Mountain. I hiked a loop here to get up and down Table Mountain: I chose to ascend the Heartbreak Ridge Trail and then to do a counterclockwise loop around the summit viewpoints before descending on the West Table Mountain Trail and then following the PCT back to this junction. That loop only covers about 3 miles of hiking but includes over 1600 feet of elevation gain.

I turned right at the junction to start up the Heartbreak Ridge Trail. After 6.4 miles of flat to moderate hiking, the trail became serious here: this is one of the steepest trails in the Columbia River Gorge. This not just an aggressive ascent: the trail is brutally steep, eschewing switchbacks in favor for a direct, full-on assault of Table Mountain's slopes. The trail ascended a net of 1400 feet in one mile along the Heartbreak Ridge Trail and that eye-popping stat doesn't even begin to really explain the steepness: perhaps it is more useful to note that there is a relatively flat 0.4 mile stretch in the middle of this hike that actually includes some downhill, meaning that the 1400 feet of elevation gain is packed into about just 0.6 miles, a grade as steep as the trail to Aasgard Pass in the Enchantments.

The Heartbreak Ridge Trail made its first 700 feet of ascent in 0.3 miles in the forest before flattening out to reach a brushy saddle. Here, the first of this hike's multiple excellent views opened up. This saddle between Table Mountain and the lower Sacaquawea Rock had a stunning view of the mountain's immense basalt cliffs, perhaps the most massive vertical cliff of columnar basalt in the United States. The Columbia River flowed in the gorge down below, bending around Oregon's Mount Defiance to the east. Sacaquawea Rock was another sharp and impressive basalt outcrop just to the south.

Basalt cliffs of Table Mountain

After I passed the saddle, the trail descended briefly- surely the advertised heartbreak, after such a strenuous ascent- before it went right back into the relentless uphill. The final 700 feet of uphill on the Heartbreak Ridge Trail were covered in another 0.3 miles, meaning there was no time for switchbacks, with the trail plowing straight uphill first through the forest and then through a talus slope. There's not much of a real trail through the talus slope, so I picked my way through the rocks while following a number of poles that marked the route. After the trail returned to the forest, it curved to the left and continued the morale-destroying uphill until it ended at an intersection. Here, the left fork promised a return to the PCT on the West Table Mountain Trail, while the right fork led towards the Gorge Overlook. I took the right fork. While the grade on this trail was still quite steep- ascending 150 feet in 200 meters- it felt like a relief after coming off the brutal ascent of the Heartbreak Ridge Trail. At the top of this short uphill, I arrived on Table Mountain's flat summit plateau and came to the Table Mountain Trail. While the left fork here led to the high point of Table Mountain, I took the right fork first to head to an overlook over the Columbia River Gorge.

The side trail to the Gorge Overlook was tremendously scenic. The trail followed the top of a ridge that was open to the south, providing sweeping views to the southwest over the Columbia River Gorge. Towards the end of the ridge, the trail narrowed as it passed directly above the massive basalt cliffs of Table Mountain's southeast face. The trail ended when the ridge did, above the steep, thousand-foot cliffs at the top of Table Mountain's great basalt pyramid.

Atop the great cliffs of Table Mountain

The view from here was jaw-dropping; this is one of the most commanding views in the entire Columbia River Gorge. The view of the individual basalt columns on the cliffs was extraordinary. There was so much air below the viewpoint as Table Mountain's slopes plunged to the forested landscape of the Bonneville Landslide below. The Bonneville Dam held back the Columbia River and Mount Hood rose above the Oregon side of the Gorge. Views stretched west towards Larch Mountain, although forest on the northeast side of Table Mountain's ridge blocked views to the east.

Mount Hood and the Bonneville Dam

This is perhaps the best viewpoint from which to appreciate the immensity of the Bonneville Landslide, an enormous mass wasting event in the Columbia River Gorge in parts of Table Mountain and nearby Greenleaf Mountain collapsed into the gorge. This landslide- or perhaps a series of landslides- is a geoloically recent event, having occurred sometime between 1100 and 1700 CE. The slide brought down massive amounts of rock from the two peaks, filling the valley below and blocking the flow of the Columbia River. Native peoples have oral records of this event, which created a massive natural dam on the Columbia that became known as the Bridge of the Gods. The great erosive power of the Columbia eventually wore away this dam, forming the Bonneville rapids; those rapids then made this site an attractive spot for the lowest dam on the Columbia River.

The source of these massive landslides may be linked to past megathrust earthquakes in the Pacific Northwest, perhaps the 1700 Cascadia earthquake that was the last known quake of such magnitude on the Cascadia subduction zone. As the Juan de Fuca Plate is still actively subducting beneath the North American Plate, it is all but certain that more such earthquakes will rock the Northwest.

After enjoying the view from the Gorge Overlook, I headed north along the Table Mountain Trail to explore other areas of the summit. As the mountain's name suggests, the summit area is a flat plateau. I hiked to the north end of the mountain, passing Table Mountain's high point along the way in a forested area. When the main trail began to loop around at the north end of the mountain, I took the spur trail that led me to the edge of the peak's north ridge. From here, there were great views to the north and east. The views to the north encompassed the three great volcanoes of southern Washington State: Mount St. Helens, Mount Rainier, and Mount Adams, rising above the forested ridges of the South Cascades. All had donned their winter snowcoats by early November.

Looking north to St. Helens, Rainier, and Adams

To the east, I could see the Columbia River flowing out of the deep gorge near Mount Defiance into the gentler landscape near Cascade Locks and Stevenson. Eagle Creek is almost directly across the Columbia River from Table Mountain on the Oregon side: that watershed was responsible for two very destructive historical wildfires. One of the worst wildfires- the Yacolt Burn- was sparked on the Oregon side of the Gorge near Eagle Creek in September 1902. The fire leaped the gorge and set ablaze a half million acres of forest in southwest Washington, casting smoke clouds that completely darkened the skies over Portland and Seattle and depositing a half inch of ash in the Portland streets. In September 2017, another fire was sparked near Eagle Creek when a teenage hiker threw fireworks into bone dry forest, igniting a 50000 acre inferno that burned much of the Oregon side of the Columbia River Gorge and that once again rained ash in Seattle and Portland. As of early 2021, many of the trails damaged during that fire- including the once famed Eagle Creek Trail- have still not reopened.

Mount Defiance rises over the Columbia River Gorge

After thoroughly enjoying the summit views, I completed the loop around the summit, following the West Table Mountain Trail along the west side of the mountaintop and past a large basalt ledge with good views of the volcanoes. Past the ledge, the West Table Mountain Trail started its steep descent. Shortly afterwards, I passed an intersection with a trail that led to the left back towards the Heartbreak Ridge Trail; I continued forward on the West Table Mountain Trail, which descended steeply through forest along the mountain's western south ridge. This descent was just as steep as the Heartbreak Ridge Trail: in 0.8 miles, the West Table Mountain Trail dropped 1200 feet to rejoin the PCT. As I descended, the trail broke back out into the open along the top of the rocky ridge, delivering some final views on the hike. In addition to lovely views of Mount Hood and the Columbia River Gorge here, I also had nice views east to Heartbreak Ridge, along which I had ascended. I could see the high overlook over the Gorge atop Table Mountain's cliffs as well as the sharp profile of Sacaquawea Rock.

Descent along the West Table Mountain Trail

Mount Hood and the Columbia River Gorge from the West Table Mountain Trail

The trail was composed of loose rock along much of the West Table Mountain Trail, making footing treacherous and forcing me to pay total attention on the trail. Tackling such a steep downhill grade with poor footing was just as difficult as the lung-busting ascent. When I finally exited the talus slope, I had a final steep descent through the forest before the West Table Mountain Trail ended at a junction with the PCT.

Back on the PCT, I breathed a sigh of relief as I returned to a properly graded trail. I followed the PCT gently downhill through the forest on the lower slopes of Table Mountain and passed the Heartbreak Ridge junction after a half mile; from there, I retraced my steps for the final, long 6.4 miles back to the trailhead. I saw just a single other hiker all day, although I'm sure that this hike will be a bit more popular than that in summer. I rewarded my long day's effort when I returned to Portland with dinner at Bollywood Theatre (it was okay) and by watching Alex Honnold climb El Capitan in Free Solo.

The views atop Table Mountain are magnificent, but I'm still not prepared to recommend this hike to most people. The neverending approach and its ugly clearcuts and the brutal steepness of the Heartbreak Ridge and West Table Mountain Trails combined to make this a tough hike. I'm glad I saw Table Mountain's sweeping panoramas but I'm in no hurry to return to this corner of the Columbia River Gorge.

Hamilton Mountain (Columbia River Gorge)

Hamilton Mountain rises above the Columbia River Gorge

7.5 miles loop, 2100 feet elevation gain
Difficulty: Moderate
Access: Paved road to trailhead, Washington State Parks Discover Pass required

The massive basalt cliffs of Hamilton Mountain provide marvelous views over the Columbia River Gorge, making it one of the most popular hikes on the Washington State side of the gorge. This hike in Beacon Rock State Park visits some pretty waterfalls en route to the views from Hamilton's big cliffs; the variety on the hike makes it one of the more enjoyable hikes in the Columbia River Gorge. Its location overlooking the Bonneville Dam, just an hour from Portland, makes it an extremely popular destination with local hikers.

I hiked Hamilton Mountain during an early November trip to the Columbia River Gorge, hoping to see some fall color on the deciduous trees in the area. From Portland, I took I-205 north across the Columbia River into Washington and exited onto Washington Highway 14 heading east. I followed Highway 14 past Camas and Washougal, enjoying the views at Cape Horn before continuing onward to Beacon Rock State Park. At Beacon Rock State Park, immediately after passing a sign welcoming me to the park on the left side of the road, I made a left turn onto a side road that was only marked by a sign that said "Camping"; I followed this road uphill and took the first right turn, which brought me into a sizeable parking lot that was the trailhead for the Hamilton Mountain hike. As this was a Washington State Park, I displayed my Discover Pass before starting the hike. On a sunny and cold November weekend, the parking lot was full.

I left the parking lot on the trail to Rodney Falls and Hamilton Mountain. The trail started out with a gentle ascent through the forest for the initial 0.3 miles before emerging into a power line clearing. The clearing provided a clear view due east down to the Bonneville Dam on the Columbia River, from which these power lines emanated, carrying hydroelectric power to Vancouver, Washington and beyond. In this clearing, the Hamilton Mountain Trail intersected with the Hadley Trail, which led off to the left towards the Beacon Rock State Park campground. I stayed the course, returning into the forest on the Hamilton Mountain Trail. The trail continued making a gentle ascent through the forest and came to a junction with a spur trail to Hardy Falls at 0.9 miles.

The spur trail to Hardy Falls branched off to the right of the trail and dropped about 50 feet in elevation; however, it was not a particularly worthwhile detour as there are not good views of the falls from the trail. Prettier waterfalls lay just ahead on the trail and were more enjoyable stops. Shortly after passing the Hardy Falls spur trail, I came to another spur trail on the left that led to the Pool of the Winds. This short side trail ended at a cliff walkway above Rodney Falls and a view into a beautiful gorge where a waterfall on Hardy Creek plunged powerfully into the Pool of the Winds. The force of the waterfall indeed resulted in gusts blowing out of the pocket gorge. This spot had the feel of a slot canyon and is one of the prettiest waterfalls on the Washington side of the Columbia River Gorge.

Pool of the Winds

I returned to the main trail, which crossed Hardy Creek on a well-built bridge just below Rodney Falls, a pretty cascade, at the one mile mark of the hike. This is a popular spot; expect the bridge to be crowded on a nice weekend day.

Rodney Falls

From Hardy Creek, the trail began to ascend more steeply, passing a gap in the trees with a view down to the Columbia River and Beacon Rock. At 1.2 miles from the trailhead, I passed an intersection with the Hardy Creek Trail, which split off to the left. I would return on the Hardy Creek Trail as this was a loop hike, but on the way in I continued uphill on the Hamilton Mountain Trail. The amusing trail sign here labeled the two routes as being "Difficult" and "More Difficult." The "More Difficult" route lived up to its billing, embarking on a steep switchback climb up the slopes of Hamilton Mountain.

View of Beacon Rock and the Columbia River from the Hamilton Mountain Trail

The Hamilton Mountain Trail switchbacked up to a bald, rocky ridge stretching south from the main mountain, reaching the top of that ridge at 1.7 miles. This ridge had arguably the best views of the hike: the massive basalt cliffs of Hamilton Mountain rose above, while the Columbia River Gorge was laid out below, with the mightiest river of the Northwest cutting its way through the Cascades. Deciduous trees were intermixed into the conifer forests below, providing pockets of yellow autumn color that spiced up the scenery. The mountains on the Oregon side of the river rose steeply from the Columbia, creating the dramatic topographic relief that makes possible the many waterfalls on the Oregon side, which include Multnomah Falls, Oregon's tallest drop.

Basalt cliffs of Hamilton Mountain

The Bonneville Dam held back the Columbia River just to the east of Hamilton Mountain. The Bonneville Dam is the last of the many dams on the Columbia River before its waters finally reach the Pacific Ocean. The nearly 200-foot high dam holds back the Columbia River to generate renewable and cheap hydroelectricity for the Northwest and to protect downstream communities from floods that previously ravaged the towns along the Columbia. Started as a New Deal project in the Great Depression, the Bonneville Dam- along with the Grand Coulee Dam- was one of the first major hydroelectric projects along the main trunk of the Columbia River. The slackwater reservoirs held back by this dam and seven others between here and Hells Canyon allow for barge traffic as far inland as Lewiston, Idaho. The power generated from this dam has helped keep electricity prices in the Northwest lower than just about anywhere else in the country.

The Columbia River is just barely above sea level at the downstream side of the dam: sea lions from the Pacific swim upstream as far as the base of the Bonneville Dam. Salmon swim to this dam each year, too, on their way back to their spawning grounds higher up the river. Fish ladders help the salmon surmount the dam, but this dam and the numerous others upstream make the journey more difficult and have altered the river's natural flow, which has severely impacted the salmon runs on the Columbia River. The salmon runs each summer and fall now are just fractions of the size of the monumental salmon migrations that nourished Native peoples all across the Northwest and that amazed Lewis and Clark.

Bonneville Dam on the Columbia River

I followed this ridge north to reach the base of the main cliffs of Hamilton Mountain. Here, the trail began switchbacking aggressively again as it ascended another 600 feet to reach the summit of Hamilton Mountain. Early in this ascent, the trail switchbacked through a clearing with views west along the gorge as the Columbia River flowed by the bases of Larch Mountain and Beacon Rock. I didn't realize it at the time, but this would actually be the last good view in a while, as the views are actually quite limited at Hamilton Mountain's true summit.

Beacon Rock and the Columbia River Gorge

The trail returned to the forest for the remainder of the ascent until it reached the summit ridge of Hamilton Mountain at 2.8 miles from the trailhead. There was an unmarked intersection at the top of the ridge; the trail to the right led to a dead end at the 2438-foot summit, where there were no real views to speak of. I followed the trail to the left, which continued north along the summit ridge; unfortunately, vegetation was quite tall here and views were quite limited, though not nonexistent. After 0.2 miles along the ridge, I came to a raised rock ouctrop by the trail; hopping on the outcrop, I found some nice views, most notably to the northeast of Table Mountain's impressive columnar basalt cliffs and Mount Adams in the distance. Table Mountain's cliffs were massive, dwarfing the basalt cliffs on Hamilton Mountain. The basalts that make up Table Mountain, Hamilton Mountain, and Beacon Rock are a result of the Columbia River Flood Basalts rather than volcanism in the Cascades. Volcanic activity from a hot spot over what is now eastern Washington and Oregon resulted in massive eruptions of low-viscosity lava that flooded the Columbia Basin and flowed west along the Columbia River Gorge, forming thick layers of flood basalts.

Table Mountain and Mount Adams from Hamilton's summit ridge

Leaving the rocky viewpoint, I continued north along the ridge, which was generally forested. The trail then descended off the ridge to the west and traversed slopes just below the ridge to reach an open, rocky saddle at 3.7 miles from the trailhead. There were good views from this saddle: Table Mountain towered over the Columbia River to the east, while the rocky ridge of Hamilton Mountain that I had just hiked rose to the south, with Mount Hood's snowy summit peeking out behind the mountains on the Oregon side of the Columbia River Gorge. This was a nice, quieter spot on the trail with plenty of room to spread out, sit, and enjoy the scenery; it was also the last major viewpoint on the hike.

Table Mountain and the Columbia River Gorge

Mount Hood and Hamilton Mountain

When I soaked in enough of the views, I decided to complete the loop to get back to the trailhead. From the saddle, I walked north to the edge of the clearing, where I came to a well signed junction; here, I took the left fork for the Equestrian Trail, a road trace which began to descend into the forest. I followed the Equestrian Trail gently downhill for a mile through a broad switchback, dropping into a deciduous forest where the trees were displaying beautiful fall colors in the late afternoon lighting. I passed by a junction to the right of the trail for Don's Cutoff and a mile after leaving the saddle I came to another junction with the Upper Hardy Creek Trail at the bottom of a valley. Here, 4.8 miles from the trailhead, I turned left to follow the Upper Hardy Creek Trail south.

Descent along the Hardy Creek drainage

I followed the Upper Hardy Creek Trail briefly to a small clearing with a picnic table. Here, I headed to the left at the junction with the Hardy Creek Trail, leaving the Equestrian Trail. I followed the Hardy Creek Trail through the forest on the lower slopes of Hamilton Mountain for the next 1.2 miles, passing through beautifully illuminated autumn woods. The trail passed a few clearings with limited views en route and dropped steeply at the end as it descended to rejoin with the Hamilton Mountain Trail. From there, I followed the Hamilton Trail for the final 1.2 miles back to the trailhead.

Autumn woods near Hardy Creek

The views of the Columbia River Gorge and the Bonneville Dam from Hamilton Mountain were quite good, although the best views did not come from the summit. The waterfalls en route- especially the Pool of the Winds- gave this hike plenty of variety. The fall colors in November visible both in the forests along Hardy Creek and in the Columbia River Gorge below were surprisingly nice. The hike is a bit on the popular side so it might not be so fun during peak summer hiking season, but I found it to be an enjoyable experience during the shoulder season.

McCall Point

Balsamroot blooming at McCall Point

3.6 miles round trip, 1000 feet elevation gain
Difficulty: Easy-moderate
Access: Paved road to trailhead, no parking fee

McCall Point is a low peak rising over the grassy Rowena Plateau at the eastern end of the Oregon side of the Columbia River Gorge, a short drive from the town of the Dalles. Each spring, the grassy slopes of McCall Point erupt with a riot of color as balsamroot and other wildflowers bloom in one of the most spectacular flower shows in the state. The balsamroot bloom of the eastern Cascades is a stunning sight that every resident of the Northwest should see in their lifetimes and McCall Point is as good a place as any to see these stunning wildflowers. The excellent views of Mount Hood, Mount Adams, and the Columbia River Gorge still makes this a rewarding hike at other times of year.

I visited McCall Point on a late April weekend, when the annual balsamroot display in the meadows here typically peak. April and May are the best months to visit this part of the Columbia River Gorge, when the grasslands are green and filled with wildflowers. The Tom McCall Preserve is closed from November 1 to March 1 each year to prevent erosion in the area when the ground is muddy.

The hike is about an 80 minute drive east of Portland. To reach the trailhead at the Rowena Crest Viewpoint from the city, follow I-84 east to exit 76 for the Historic Columbia River Highway and Rowena; upon exiting the interstate, bear right and follow signs to take US 30 (the Historic Columbia River Highway) east for 3 miles, making a number of switchbacks to reach the top of a plateau, where the turnoff for the Rowena Crest is on the left side of the road. I parked in the large cul-de-sac loop of the viewpoint; after checking out the view below of the winding highway that I had just driven, I walked over to the McCall Point trailhead at the other end of the parking loop.

The wide dirt trail left the parking lot and initially skirted the edge of the basalt cliffs defining the Rowena Plateau, providing some additional views of the curving switchbacks of the Old Columbia River Highway below as well as of the Columbia River itself flowing past basalt cliffs and green, grassy hills in the distance. The trail- flat for the first third of a mile- then crossed a broad meadow that was covered with brilliantly yellow blooms of balsamroot.

Balsamroot in bloom on the Rowena Plateau

After 1/3 of a mile, the trail made two broad, 180-degree turns and then began ascending along the east side of the ridge leading up to McCall Point. Here, the trail passed above incredible fields of balsamroot, paired with open views of the Columbia River below and the town of Lyle and the basalt cliffs of Dalles Mountain in Washington State across the river.

Balsamroot blooming above the Columbia River

Trailside vegetation was lush in late April as I climbed through oaks, patches of balsamroot and lupine, and desert parsley that had not yet bloomed.

Lush springtime vegetation along the McCall Point Trail

The trail ascended steadily through the forest above the grassy bench for a bit before climbing up onto the open, grassy slopes below McCall Point at 0.6 miles. The fields here were also packed with blooming balsamroot, lupine, irises, and paintbrush- not only were the nearby meadows blooming with wildflowers, but I could see the fields of yellow on the slopes of the nearby Memaloose Hills. The trail ascended steadily through this meadow via a set of switchbacks; views were amazing the entire way up, stretching to Mount Defiance rising sharply up the Columbia River Gorge to the west.

Balsamroot blooms along the trail

Balsamroot, irises, and paintbrush

As the trail switchbacked up the slopes on a still-moderate but increasingly aggressive grade, McCall Point itself rose ahead. The summit of McCall Point is protected in a preserve managed by the Nature Conservancy; the peak is an offshoot of Seven Mile Hill, which itself is part of the Columbia Hills, a range of rolling, high hills and basalt cliffs that is cut through by the Columbia just downstream of the Dalles. McCall Point is named after Tom McCall, a former governor of Oregon in the late 1960s and early 70s known for his towering environmental legacy in this state.

McCall Point rises in front of the trail

At a little over a mile from the trailhead, the trail reentered forest, embarking on a slightly steeper climb. At 1.5 miles, the trail reemerged into the meadows from the forest. The trail made a final few switchbacks on these open, high slopes as it made the final ascent to the summit. The views from these open slopes here were the best of the hike- even better than the views at the very top. Green meadows featuring bursts of yellow balsamroot blooms covered much of the Rowena Plateau below me, with black basalt cliffs dropping from the plateau down to the Columbia River below. A similar landscape lay on the opposite side of the river in Washington State and I saw occasional barges heading up or downstream on the Columbia past the town of Lyle. On a clear day, visitors can see Mount Adams rising to the north across the Columbia; on the day of my visit, I was only able to spot the snowy base of the massive volcano as there was still quite a bit of cloud cover. 

Columbia River Gorge views from the high grassy slopes of McCall Point

Mount Adams across the Columbia River Gorge

At 1.8 miles, I arrived at the top of McCall Point, which was a rounded, grassy summit. The flowers at the summit were just as good as the fields of flowers I had hiked through on the way up. McCall Point was not the high point of Seven Mile Hill- in fact, it is just a knoll on a ridge extending from that hill and a social path appeared to lead further up the hill, but crest of the hill to the south had dense tree cover and would not have provided the same views that I had at McCall Point.

Trees on the north side of the point actually obstructed views to the north and east from the very summit, although there were sweeping views to the west of Mount Defiance rising over the Columbia River and the nearby grasslands exploding with yellow patches of balsamroot. While I enjoyed the view from here, the clouds parted briefly to reveal Mount Hood, the sharp, glacier-covered volcanic pyramid that is the highest peak in Oregon. 

Balsamroot and the Columbia River

Mount Hood peeks out from the clouds

Following a social path from the very high point of McCall Point around the trees on the northeastern side of the summit, I came to a point with fairly nice views to the northeast. From here, I could look along the length of the Columbia Hills, with Seven Mile Hill on the Oregon side of the River and Dalles Mountain rising above the basalt cliffs on the Washington side of the river. Upstream of here, the Columbia River simply cuts through the basalt layers of the Columbia Plateau; but here, the Columbia River cuts through its first water gap downstream of Wallula Gap, launching it into its spectacular, nearly sea-level crossing of the Cascades.

Dalles Mountain rises above the Columbia River

There were a good number of other hikers on the trail at the time of my visit- spring is by far the most popular time to visit here because of the amazing wildflower blooms. Despite the crowds at that time of year, the balsamroot blooms here are truly impressive and I can't recommend enough visiting this corner of the Columbia River Gorge in late April and early May. 

Catherine Creek-Coyote Wall

Balsamroot grow along the Coyote Wall, high above the Columbia River

11 miles loop, 2700 feet elevation gain
Difficulty: Moderate-strenuous
Access: Paved road to trailhead, no parking fee

Packed with views of snowy Mount Hood, the great cliffs of Coyote Wall, and the mighty Columbia River, the loop hike from the Catherine Creek Trailhead to Coyote Wall is one of the best hikes on the Washington State side of the Columbia River Gorge. In spring, the landscape around Coyote Wall explodes with wildflowers, turning an already excellent hike into one of the finest in the Pacific Northwest at that time of year. If you're looking for variety, you'll find it on this hike: in addition to the features mentioned above, hikers can enjoy the waterfalls of the Labyrinth, a natural arch at Catherine Creek, and fabulously green grassy meadows on the slopes above the Columbia River.

Spring is the best time of year to do this hike, especially in the months of April and May. The grasslands of this landscape turn brown later in the season and the area is not quite as charming without its magnificent floral displays. Temperatures are also more moderate during the spring, as the area can get quite hot in summer. Watch out for poison oak and ticks; also, keep an eye out for rattlesnakes on the open, south-facing slopes of this hike.

I hiked the Catherine Creek-Coyote Wall loop on a sunny late April Sunday, when the spring wildflower bloom of the Columbia River Gorge was in full swing. From Portland, it was an 80 minute drive to reach the Catherine Creek Day Use area trailhead: I followed I-84 east to Hood River, taking exit 64 and then crossing the Columbia on the Hood River Bridge, which charged a $2 passenger car toll at the time of writing. Once across the bridge, I turned right onto Washington Highway 14 and followed it east for 6 miles, passing beneath Coyote Wall. I turned left onto Old Highway No. 8 when Highway 14 reached Rowland Lake; I followed Old Highway No. 8 around Rowland Lake and then steeply uphill through two sets of basalt cliffs to the Catherine Creek Trailhead, where there was ample parking along the north side of the road. The hike started from the far (east) end of the parking area.

Two trails branched out from the trailhead into the grasslands that lay uphill: the Bitterroot Trail, which led to the left, and Atwood Road (also signed as FR 020), a former road trace that headed uphill and to the right. The first stretch of this hike followed Atwood Road, so I took the right fork. Less than a hundred yards from the trailhead, I passed a junction with the Catherine Creek Loop Trail; I stayed on Atwood Road, which continued north into a canyon, soon entering the woodlands along Catherine Creek. After following Atwood Road a quarter mile from the trailhead, I came to a second junction with FR 021, which split off to the right. Here, I took a brief detour from the main trail to visit Catherine Creek Arch. I took the right fork and crossed Catherine Creek and then followed the trail a fifth of a mile north along the base of a large cliff of columnar basalt. A fifth of a mile from the junction, just before the road trace began a steep ascent, I came to an old corral on the right side of the trail. Looking up from here, I spotted Catherine Creek Arch, a natural arch of columnar basalt. While it's not the most visually impressive arch, as it is separated from the basalt wall behind it by just a narrow crack, it was still an interesting phenomenon to see, as basalt arches are not terribly common.

Catherine Creek Arch

Returning down FR 021 to the junction with Atwood Road, I continued uphill along Atwood Road, which began to ascend more steeply on the most extended ascent of the hike. Initially, the road trace stayed in bottom of Catherine Creek Canyon, but the road soon began to ascend away from the creek, following the base of the basalt walls on the canyon's west side. As I made my way uphill, I looked back for some nice views of Catherine Creek Arch. Soon, the trail entered a thick forest as it made a steady ascent, passing under some power lines and reaching a junction with Old Stove Road at just under 2 miles into the hike. At this junction, I took the left fork to stay on Atwood Road, which made a 180-degree turn and then emerged out from the forest into the open grasslands of Sunflower Hill at 2.2 miles from the trailhead. 

Arriving at Sunflower Hill, views opened up as I hiked through the meadows, which were a vibrant green with fresh grass in April. Snowy Mount Hood rose ahead of the trail above the green meadows, but the heart of the view lay to the east, where the Columbia River began its dramatic journey through the Cascades by cutting a water gap between Dalles Mountain and McCall Point. Tiered basalt cliffs lined the river on both sides, evidence of the massive and frequent flood basalt eruptions that shaped the Columbia Plateau millions of years ago. Memaloose Island lay at the heart of the Columbia River: this island was once a burial ground for the native peoples of the Columbia River. Based on native customs in the region, the dead were not buried and instead were wrapped in blankets and left on the island with funerary items.

The Columbia River flows past the Dalles

The trail- Atwood Road- passed a junction with the Bitterroot Trail as it crossed the meadows of Sunflower Hill and also passed underneath a set of power lines. After that, the trail returned to the woods briefly, crossing Rowland Creek and passing by another junction with the Rowland Wall Trail. At both junctions, I stayed on Atwood Road, continuing west; the road gradually narrowed into a single track trail. At 2.8 miles, the trail reentered a green meadow on the slopes high above the Columbia River. Over the next mile, the hiking on Atwood Road was extremely enjoyable: I followed the single track trail through open meadows, with small, profusely blooming wildflowers mixed in with the grass. The trail undulated as it crossed these high slopes, with some gradual ups and downs but little net elevation gain or loss. At 3.3 miles, I passed a junction with the Upper Labyrinth Trail; I continued forward on Atwood Road. 

Views from the meadows above the Columbia River

As I hiked through these high meadows, views of Mount Hood, across the river in Oregon and the highest peak in that state, gradually improved. 

Mount Hood rises above the Columbia River

At 3.6 miles into the hike, the trail passed through the scenic ravine of Labyrinth Creek. Further downstream, this creek carves out of the prettiest landscapes of the eastern Columbia River Gorge, but there was little hint of what was further downslope from this position. Entering the oak woodlands in the ravine, I crossed Labyrinth Creek on a small footbridge.

The upper canyon of Labyrinth Creek

Shortly after crossing the Labyrinth Creek ravine, the Atwood Road came to a junction with the Old Ranch Road, now 3.7 miles into the hike. After following Atwood Road for such a long distance from the trailhead, I finally left that trail for Old Ranch Road, taking a left at the junction and descending downhill. Although Atwood Road does continue west towards Coyote Wall, it passes over private land; the hike utilizes Old Ranch Road as a detour to prevent trespassing on private property. Old Ranch Road headed back out into an open meadow as it descended steeply, dropping 120 feet in just over a tenth of a mile with sweeping views towards Mount Hood. Along this stretch, I could see the house on nearby private property and hear lawnmowing on the nice spring day. 

Old Ranch Road then flattened out and turned to the right; at 4 miles into the hike, I came to a junction between the Old Ranch Road and the Traverse to Coyote Wall. At this junction, I took the right fork for the Traverse Trail, which ascended briefly via switchbacks to regain the elevation lost on the Old Ranch Road. I passed a number of junctions with road traces and trails after this, staying left at every junction to remain on the Traverse Trail. I traversed across grassy slopes with great views of Mount Hood until I finally came to a junction with the Coyote Wall Trail, 4.7 miles into the hike. This junction was obvious, as the traversing trail ended with a massive cliff to the west.

Meadows, Mount Hood

Two trails ran along the Coyote Wall: a path running directly along the cliff and another path set back about 50 meters from the edge. From the junction, I headed uphill towards the top of the wall first; I took the trail removed from the edge on the way up and then hiked down along the trail following the cliff. Here, I finally arrived at the great balsamroot blooms for which the eastern Columbia River Gorge is known. The meadows along the Coyote Wall were brimming with the big, yellow flowers of the balsamroot, a splendid sight that eased the steep uphill ascent up the hill near the wall.

Balsamroot meadows at the Coyote Wall

Although the path I followed uphill was slightly set back from the edge of the Coyote Wall, the scenery was still incredible; the steep slopes of the hill here were coated in balsamroot and then dropped precipitously off a nearby edge, with snowy Mount Hood towering beyond the drop. The trail here was quite steep as it climbed about 300 feet uphill over a third of a mile, with the two trails along the Coyote Wall coming together at the top of the Coyote Wall, a little over 5 miles from the trailhead.

View of Mount Hood and balsamroot on the rim of the Coyote Wall

From the top of the Coyote Wall, I admired the view of forest directly below the massive columnar basalt cliffs with Mount Hood in the distance; however, the view down the wall from here was not as great. I started following the wall-side trail downhill, which delivered constantly amazing views of the huge cliff, until I came to a viewpoint where I could see down the entire length of the wall, its massive basalt columns lining up all the way down to the Columbia River. 

Coyote Wall and the Columbia

I hiked along the Coyote Wall Trail down the length of the cliff for the next 1.5 miles. There were frequent trail junctions along the way, including a point where the Coyote Wall Trail briefly joined the switchbacking Old Ranch Road; at every junction, I took the fork that kept me closer to the cliff. The views were glorious the entire way down as the full length of the wall was in the open and covered with meadows bursting with balsamroot blooms. The mighty Columbia passed below at the end of the wall and Mount Hood rose above it all. I also had great views back up the length of the impressive cliff.

Looking up the length of the Coyote Wall

At 6.5 miles into the hike, as I approached the bottom of the Coyote Wall, the trail veered to the left away from the cliff and completed the 1500-foot descent from the top of the wall by switchbacking through pretty grasslands displaying blooming desert parsley and interspersed with small basalt outcrops. At 6.8 miles, the Coyote Wall Trail ended by joining Old Ranch Road, which I continued to follow downhill through a long switchback. I ignored the junction with the Little Maui Trail and after 7.3 miles of hiking I reached the roadbed of Old Highway 8, which has become part of the hiking trail system here.

Columbia River at the bottom of the Coyote Wall

I turned left at the junction with Old Highway 8 and followed it east for 0.3 miles, paralleling WA Highway 14, the railroad, and the Columbia River below. Desert parsley and gentian grew in the grasslands along the former road, along with a few California poppies, which are rare to spot this far north.

Gentian growing along Old Highway 8 near the Columbia River

At 7.6 miles into the hike, I took the Labyrinth Trail, which split off to the left and headed uphill from Old Highway 8. The Labyrinth Trail- true to its name- immediately dove into a maze of basalt buttes and oak woodlands. A little ways up the Labyrinth Trail, I passed a junction with the Little Maui Trail, bearing right at this intersection to stay on the Labyrinth Trail. Over the next mile, I hiked through the Labyrinth, a very scenic ravine that was another of this hike's many highlights. The trail followed Labyrinth Creek for a while up the canyon as it passed a number of waterfalls where the creek dropped down columnar basalt ledges. The prettiest of these waterfalls came about 0.4 miles up into the Labyrinth, where the creek cascaded down an angled basalt face into a pool below before flowing further down the rocky but green canyon to the Columbia River past patches of blooming desert parsley and balsamroot.

View of the Columbia River from the Labyrinth

Columnar basalt and waterfalls in the Labyrinth

At a half mile up the Labyrinth Trail, I crossed Labyrinth Creek while following the trail steadily uphill through the mixed oak woodlands and balsamroot grasslands of the canyon. Columnar basalt cliffs rose above the ravine, providing a stark and angular contrast to the lushness and rounded slopes of the canyon bottom. I saw some extremely geometric examples of columnar basalt in the Labyrinth- some of the walls displayed perfectly straight, evenly-size, and hexagonal columns with clean jointing, a sight that is still fairly rare in the area despite the omnipresence of basalt throughout the Columbia River Gorge and Columbia Plateau. Indeed, some of these examples looked as perfect as those found at Devil's Postpile in California or at other more famous columnar basalt sites.

Columnar basalt cliffs in the Labyrinth

Perfectly geometric columnar basalt

As I ascended through the Labyrinth, the trail left the creek and made its way uphill through a canyon of alternating woods and small meadows. Here, in the shadow of the basalt buttes and oaks, I found a handful of blooming chocolate lilies. These lilies, which have spotted brown petals, are a rare wildflower treat- I have only ever seen them here in the Labyrinth, although they occur across much of the North American west coast.

Chocolate lilies

The trail continued ascending until exiting the canyon and emerging into the grasslands above the Labyrinth. After 8.8 miles of hiking and after 700 feet of elevation gain after leaving Old Highway 8, I came to a junction with the Desert Parsley Trail. At this unmarked junction, I took the right fork to follow the Desert Parsley Trail east. The Desert Parsley Trail followed the contours of the hill through open, grassy slopes for a half mile, providing excellent views east to Rowland Wall and down to Rowland Lake below. Rowland Lake is actually an arm of the flooded Columbia River that became separated from the rest of the Columbia's slackwater reservoir by causeways carrying Highway 14 and the railroad.

Rowland Lake and the Columbia River

While traversing these open grasslands on the Desert Parsley Trail, I spotted a snake crossing the trail. I gave it some space and continued onwards after it had completed its crossing, but it was a good reminder to keep my eyes open: the warm, south-facing open slopes here are popular with snakes, including rattlesnakes.

Snake along the Desert Parsley Trail

The Desert Parsley Trail met up with the Shoestring Trail at 9.3 miles into the hike in a forest. The trail junction was unmarked; here, I chose to stay on the Desert Parsley Trail, which made a sharp switchback to the right and started descending via switchbacks, first through meadows and then through forest. After a third of a mile of descent, the trail reentered the open on a basalt talus slope. Here, the trail passes through an area known as Indian Pits: the talus structures near the trail were created by Native peoples of the Columbia River. The trail continued descending steeply as it passed Indian Pits, all the while providing constant views of Rowland Wall. Like Coyote Wall, Rowland Wall is a columnar basalt cliff, but it is not nearly as impressive as its better known cousin to the west.

Rowland Wall and the Columbia River Gorge

The trail approached the base of Rowland Wall, passing through beautiful slopes of desert parsley and lupine, and intersected with the old road trace of the Raptor Trail, now 10 miles into the hike. The Raptor Trail led downhill to the road but was closed at the time of my visit for peregrine falcon nesting; it is off limits to hikers between February and May each year. Instead, I took the single track that branched off to the left here, leading up and over the Rowland Wall.

Lupine-lined trail near Rowland Wall

Once atop the Rowland Wall, the connector trail brought me to the Rowland Wall Trail. I took the right fork here to head downhill for the final mile of the hike. Initially, this trail followed the rim of the Rowland Wall and was not unlike the Coyote Wall Trail; I enjoyed nice views to the west of Rowland Lake and the Columbia. The Rowland Wall Trail then turned to the east away from the cliffside, crossing the grassy slopes of lower Sunflower Hill. The trail passed through multiple fields of blooming camas here, a final wildflower treat of the journey's floral feast. At the final trail junction with the Bitterroot Trail, the Catherine Creek parking lot was already in view in the distance; I turned right at this intersection and followed the Bitterroot down the last grassy hill to complete the loop.

Camas near Catherine Creek

What a hike! While the Pacific Northwest is best known for moist conifer forests, soaring rocky peaks above glaciers, and alpine lakes nestled amidst huckleberry and heather meadows, the Catherine Creek-Coyote Wall showcases some of the best of what you can see east of the Cascades. The endless wildflowers, the spectacular basalt formations, the mighty Columbia- hike here to appreciate all this beauty. The area is quite popular with day hikers from Portland, especially the Coyote Wall portion of the hike, which can be accessed by a shorter hike from a different trailhead, but it's undoubtedly worth visiting.