Of all the volcanoes in the northern Cascades, Mt. St. Helens is by far the easiest to climb. For starters, the most common route, Monitor Ridge on the south flank, is non-technical, eliminating the need for specialized gear or advanced mountaineering skills. At just 8,366 feet, its summit elevation post-1980 eruption places it several thousand feet lower than neighbors such as Mt. Adams, Mt. Baker, and Mt. Rainier, essentially taking the ill effects of altitude out of the equation. However, at 10 miles round trip and with about 5,000 feet of elevation gain, it’s still a robust day hike.
After numerous trips to the base of Mt. St. Helens over the years, reaching the summit of this active volcano has long been on my to-do list. When we moved back to Washington last summer, I knew I might finally get my chance. The Gifford Pinchot National Forest limits the number of climbers to 100 per day in the summer months, and the permits sell out quickly when they go on sale in March. Sadly, I missed the initial sale this year, leaving me to obsessively check every few days for cancellations. Eventually I got lucky and spotted two permits up for grabs in late-July. A few minutes later, they were mine.
From a distance and elevation gain standpoint, the hike up Monitor Ridge is comparable to many of Colorado’s famous “Fourteeners”. One major difference: on Mt. St. Helens we would be topping out at a lower elevation than one starts most Fourteener climbs at. The other big difference would be the terrain. Most Fourteeners have a fairly distinct path a good way up the mountain and are on reasonably solid rock (my dislike of exposure and falling means I haven’t done any of the ones on rotten rock). On Mt. St. Helens, after a brief foray through the forest, the climb traverses a mixture of large lava boulders and a loose scree consisting of pumice and volcanic ash. This is a hike where a mask was on the suggested gear list before they were cool!
To the hike! As the National Weather Service had accurately predicted several days in advance, the morning of our climb dawned with some fairly dense fog at the Climbers Bivouac trailhead where we had camped the previous night. We hit the trail at 6:00 am, anticipating that it would take us 4-5 hours to reach the summit. The first two miles of trail climbs gently through a moist and somewhat unremarkable second growth forest. At timberline is where the route changes from a well-maintained trail to the aforementioned scree and boulder scramble. Wooden posts serve as guides for the remainder of the climb, but following them too closely didn’t always make for the most sensible route. In places there is a fairly obvious path, while in others (particularly in the boulder fields), you just sort of have to find what works best. Just before arriving at timberline, we began to emerge from the clouds, revealing views of Mt. Adams to the east and the extremely conical Mt. Hood to the south that we enjoyed the rest of the day. Once above the trees, our pace slowed significantly, but before too long we were several hundred feet above the cloud deck we had been immersed in a short time earlier:
We made fairly good time through the ~2 miles of boulder fields. The final mile through a deep and loose mixture of volcanic ash and pumice was definitely the most challenging part of the hike. With masks on to prevent inhaling clouds of ash kicked up by our feet (and the wind), it was somewhat analogous to hiking up a sand dune: two steps forward, one step back, repeat. After about four hours, we were standing on the crater rim.
The first view northward into the bowels of Mt. St. Helens was stunning, and definitely one of the most dramatic viewpoints I can recall. Unlike many lesser peaks in the Cascades, or most peaks in the Rockies, where you are often surrounded by other peaks of comparable elevation, Mt. St. Helens stands alone. On this volcano, you are standing on what is, by far, the highest point for dozens of miles in any direction, with only the other volcanoes exceeding you in height. Looking down onto the crater formed by the 1980 eruption, the lava domes that are slowly rebuilding the summit, and the Crater Glacier (one of the few alpine glaciers in the world that is actually advancing) was spectacular. Cornices of hard-packed, dirty snow clung to the nearly vertical slopes of the crater walls just beneath our feet, necessitating caution as we moved our way along the rim. Gentle puffs of steam were visible on portions of the lava dome, a gentle reminder that we were standing at the summit of one of the most active volcanoes in the world. The dull roar of rock and ice fall from the crater walls was nearly constant for the hour we spent taking in the view from the summit.
While the hike up had been relatively uneventful, the journey down was definitely less pleasant. Hiking poles are a must for the descent due to the steep, loose, and rocky terrain. This is definitely one of those hikes where coming down is exponentially more difficult than going up!
Compared to our experience hiking Fourteeners in Colorado, the significantly lower elevation of this hike makes a huge difference and in my opinion dramatically lowers the overall difficultly of this route. There is a big difference between inching your way up a scree slope at 13,000′ and having to stop every few steps to take in oxygen, and doing the same at 8,000′ where breathing isn’t as much of an issue. While the terrain was definitely more difficult than your average hike with similar specs, in the end we felt like the difficulty of the Monitor Ridge route was somewhat over-hyped based on some of the accounts we read in advance. We wouldn’t hesitate to do it again. As far as special gear, a mask was definitely helpful for both COVID and volcanic ash purposes. Hiking poles were more or less useless on the way up, as the boulder fields often required the use of hands to navigate, but essential on the way down. Other sources recommended bringing garden gloves to protect against cuts on the sharp volcanic rocks. We bought some cheap ones and definitely found them useful. I never actually put mine on during the ascent, and made it to the summit with only one small abrasion on the back of my hand. Long pants are also a must if you don’t want your lower legs ripped to shreds by the rocks.
With Mt. St. Helens checked off, next up on the to-do list is Mt. Adams, which is also a non-technical climb at the right time of year, albeit longer. We may not get to that one this summer…perhaps our goal will be to climb one Cascade volcano per year!
The last destination on our Alaskan journey was the Kenai Peninsula and the town of Seward. After a few days respite from the wildfire smoke in Wrangell-St. Elias, it returned with a vengeance as we headed back to Anchorage and down to the the coast:
After baking in the heat of the Alaskan interior for the last week, the marine climate of Seward was a welcome change. We even had a bit of rain for one of the few times in our entire trip.
While temperatures in Seward we’re somewhat more mild, the coastal location meant the humidity was not. On our first day in Seward, we partook in a brutal hike up to the Harding Icefield in Kenai Fjords National Park. The hike itself was not abnormally difficult, but we were definitely not used to the combination of heat and humidity, leaving me feeling physically ill at several points during the slog up the mountain. The day had started off overcast, but as we climbed, the clouds evaporated leaving us with stellar views of the rapidly retreating Exit Glacier and the Harding Icefield from which it originates. An icefield is essentially a large mass of interconnecting glaciers. The Harding Icefield is the largest — and one of only four — remaining icefields in the United States. The Exit Glacier itself has retreated more than a mile in the last 200 years, leaving trees and other vegetation to begin re-occupying it’s former valley.
The white and blue ice of the glacier made for a stellar contrast with the lush green vegetation of the alpine zone:
The wet climate of coastal Alaska results in extremely heavy snowfalls, making this one of only a handful of places in the world where glaciers flow all the way down to sea level to meet the ocean. Known as tidewater glaciers, these glaciers exhibit complex patterns of advance and retreat that, unlike standard alpine glaciers, are not purely the result of variations in climate. While warmer temperatures or prolonged drought can certainly reduce their mass, the movement of tidewater glaciers is also subject to complex interactions between the ice, the geomtery of the ocean floor, and the depth of the water into which they flow.
On our second day in Seward, we took a water taxi into the heart of Kenai Fjords National Park and then kayaked to within about a quarter mile of the terminus of Holgate Glacier. Tidewater glaciers have a tendency to “calve”, in which large chunks of ice break off the glacier and fall into the ocean, necessitating a safe distance. Glacier “social distancing” if you will. It is not hard to find videos on YouTube of people getting too close to calving tidewater glaciers, with quite predictable results. From our safe distance, we observed and heard several calving events in the few hours we were kayaking around the bay, but unfortunately I was not adept enough at kayaking into position quickly enough to actually capture one on camera.
Our boat ride back to Seward through Resurrection Bay also resulted in sightings of sea lions, seals, puffins, and even two pods of orcas: an exciting end to the trip!
With one job ending in June and the next not starting until September, we spent most of this past summer on the road. It’s now mid-October, and I’m finally getting the chance to seriously sort through the resulting pictures.
Our last big stop of the summer was Glacier National Park in Montana and neighboring Waterton Lakes National Park in Canada. Glacier was one of the few remaining national parks in the west I had yet to visit, so I was excited that we were able to squeeze this trip in. Despite uncharacteristically foul weather for mid-August, a harrowing experience on the park shuttle bus, campgrounds with problem bears (and problem campers), and an unscheduled detour to an auto parts store in Cardston, Alberta, we managed to get in 60+ miles of hiking among some truly first-class scenery. Our most memorable hike was the trek to Grinnell Glacier in the northeast corner of the park. Here are a few photos from that journey:
We recently returned from a week in Italy; a refreshing change of pace, both scenically and climatically, from winter in the Utah desert! While we spent the majority of the trip enjoying the historic sights of Florence and Rome, just a handful of hours after touching down in Italy, we were aboard a high-speed train bound for the Cinque Terre, a rugged section of Ligurian Sea coastline where we spent the first several days of our trip hiking, exploring, and ingesting some of the best seafood of our lives. The Cinque Terre (“five lands”) consists of five small villages clinging to the rocky shore, surrounded by ancient stone terraces, vineyards, and olive groves, and crisscrossed by a network of hiking trails that, since 1999, have been part of the Cinque Terre National Park. A hot tourist spot in peak summer season, in March, with the temperatures still far too cold and the skies much too drizzly for a dip in the sea, the streets and trails were definitely still enjoying the relative calm of the off-season. On the stormiest day, we struggled to find an open restaurant or market to grab a bite to eat!
The five villages (from south to north: Riomaggiore, Manarola, Corniglia, Vernazza, and Monterosso al Mare) are spread out along a six mile stretch of shoreline. A regular train connects the five villages to one another and the larger cities of Liguria, making its way along the coast via a series of long, dark tunnels, only to pop out into the open briefly to stop at the station adjacent to each town. Coming from La Spezia (the closest major city to the Cinque Terre), we hopped off the train at Manarola, our home base for our all-too-short stay:
Like the other four towns, the colorful buildings of Manarola cling to the hillsides in impressive fashion. The terrain, while steep, is relatively easy to traverse thanks to the vast network of dry stone terraces, originally built centuries ago. Not only do the terraces help minimize erosion of the precipitous slopes, the treads provide flat surfaces on which grapes, olives, lemons, and other food products are grown. Most of the trails that wind through the Cinque Terre follow these historic terraces, providing an easy walking path, great views, and an up-close look at many of the vineyards which are still operated to this day.
Despite the convenience of the train, the most enjoyable way to travel between the towns is to walk. Hiking is one of the primary attractions here, and the five villages are connected by a famous 7-mile long coastal trail that follows the curves of the shoreline in dramatic fashion. So dramatic in fact, that many segments have been closed for years due to landslides that have made them dangerous and impassible. On day two, we struck out from Manarola to hike to the next village to the north: Corniglia. With the direct route along the coast closed indefinitely, we undertook a more circuitous route up through the vineyards and terraces to the village of Volastra, then back down a steep grade to Corniglia. The views of the Ligurian Sea from this trail were phenomenal, despite the occasional rain & thunder.
After enjoying a picnic in Corniglia, we opted for a short rest and utilized the train to reach the next town of Vernazza. Vernazza was by far the busiest and most active town we visited; it was hard to imagine what the crowds would be like in the sweltering heat and humidity of summer. Interestingly, Cinque Terre, which attracts ~2.5 million visitors each year, faces many of the same challenges as Zion National Park in our own backyard: namely, lots of visitors and not a lot of room for them to spread out. The peak-season crowding has gotten bad enough that the Cinque Terre National Park, much like Zion, has begun exploring the use of reservation systems and other strategies to mitigate the crowds in peak season. Another parallel between Cinque Terre and Zion: deadly flash floods. In 2011, heavy rains swelled many of the streams that the villages are built along (or literally over in many places), killing several and burying the main streets of Vernazza and Monterosso in over a dozen feet of mud. While the towns have mostly recovered, the reality is that this will always be a very geologically active place. Nature doesn’t like near-vertical terrain.
On our final day, we left the Cinque Terre proper and headed to the small town of Levanto, just to the north. Our plan was to hike a lesser known section of the coastal trail that traverses a wide peninsula jutting out into the Ligurian Sea, and then back to the Cinque Terre and Monterosso via Punta Mesco. Oddly, we saw far more people along this stretch of trail than we seen the past few days in the Cinque Terre, including an excursion of an Italian hiking club numbering at least 100 people. After a few dreary days, we finally got to bask in the beautiful Mediterranean sun on this trek, and were rewarded near the end with exquisite views of the entire Cinque Terre coast from Punta Mesco.
A few days hiking (and eating) in the quiet and laid-back Cinque Terre were a great way to kick off our trip and ease us into tackling the hustle and bustle of Italy’s larger cities!
Golden Larches at Blue Lake in the North Cascades.
Still reeling from the disappointment of having to leave Colorado a mere fortnight before the world’s largest Aspen forests exploded into their annual displays of color, I was determined to find some similar photo opportunities in Washington this fall. The “Aspen of the Pacific Northwest” is arguably the Western Larch. Most common in the Northern Rockies, a handful of Western Larch stands can be found east of the Cascade Crest in Washington state. Tall but unassuming for 50 weeks out of the year, and then drop-dead spectacular for two, the Western Larch looks all for the world like an evergreen, but it is decidedly deciduous. Most high-altitude Pacific Northwest forests are all evergreen, so unless seeing dead and decaying brown pine-needles pile up on the forest floor is your thing, autumn up in the high Cascades isn’t anything to get too excited about. Add larch though and it’s a different story. The yellowish-green needles of the larch go out with a bang, turning a glittering golden-yellow for just a few short weeks in the late fall before leaving the tree buck naked until the following spring.
Golden larch season in the Cascades is an event that generally attracts hordes of needle-peeping Seattleites to the mountains. My hope was that the several feet of early-season snow the mountains had received in late September would be deep enough to temper the crowds. I was wrong. The parking lot at the Blue Lake Trailhead off of Highway 20 in the Okanogan National Forest was completely full, forcing us to park alongside the highway. Fortunately, photographers are born with an innate desire to bask in late-afternoon light which meant we were headed up the trail to Blue Lake late enough that most other folks were already on their way down. One advantage to having lots of folks on the trail was that we were alerted to the presence of a solitary mountain goat scrambling along a rocky gully a few hundred feet above the trail.
The lower portion of the trail was snow-free, but by the time we reached the goat and the larch groves, it was several feet deep. The main trail was hard-packed snow and ice due to all of the foot traffic but wandering off trail trying to take pictures of the larches sans people would definitely have been easier with a pair of snowshoes. The larches were nothing short of spectacular, especially against the snowy-white backdrop. In the late afternoon sun, the color of the needles was so resplendent that you could have painstakingly coated each needle in gold leaf and not known the difference. Individual larches on mountain ridges miles away could easily be picked out, their needles back lit by the sun, shining like beacons in a sea of mountains.
A surprisingly sunny and warm October afternoon in the North Cascades is perfect for larch hunting.
Exploring off trail, gazing out at the Cascades through the larches.
Later in the evening, headed to a lower-elevation (read: warmer) camping spot, I was able to catch the very last rays of sunlight on Liberty Bell Mountain. And just in case larches and a spectacular sunset weren’t enough, the clear skies and nearly full moon were ideal conditions for some nightscapes of the North Cascades!
Sunset along the North Cascade Highway.
The constellation of Aquila sets over North Cascade peaks illuminated by the Full Moon .
Driving west on Highway 2 over Stevens Pass last spring, I kept catching glances of what appeared to be some sort of elongate, dark grey, overgrown, man-made structure paralleling the highway on the opposite site of the Tye River valley. Whatever it was, only isolated chunks of it were visible through the dense vegetation and the deep, late-season snowpack. It appeared to me to be made of concrete, although it was hard to be 100% sure given that my primary goal at the time was to prevent a van full of people from careening off the highway and plummeting into the gorge below. Ironically, little did I know that the very existence of the mysterious object I was seeing was the result of a passenger train carrying hundreds of people doing exactly that 113 years earlier.
Walking through a large concrete snowshed along the Iron Goat Trail, built at the site of the 1910 Wellington disaster to prevent future avalanches from sweeping trains and passengers off the rails.
It didn’t take long after getting home to my internet connection to figure out that what I was seeing was the old grade of the Great Northern Railway, the northernmost of the transcontinental railway routes in the U.S. The Great Northern reached Seattle in 1893 and the route it took across the Cascades can best be described as “gnarly”. A series of extremely steep switchbacks, and eventually a 2.60 mile long tunnel completed in 1900, funneled trains safely, if not easily, over Stevens Pass to Seattle. In the summer at least. The biggest danger of the route lay in the combination of heavy winter snows and steep rugged topography. The railway built a number of snowsheds, large concrete or timber structures which covered the rails in avalanche prone areas to protect the locomotives. Avalanches don’t always play nicely though, and in March of 1910, during a storm in which 11 feet of snow fell in one day, a 10′ thick slab of snow detached from Windy Mountain several hundred feet above the tracks and swept two trains off the tracks just outside the railroad town of Wellington, Washington. 96 people perished in what remains the deadliest avalanche in U.S. history, and one of the worst railroad disasters in the country’s history to boot.
Despite the somber backstory, the old railroad grade has been turned into what has to be one of the most fascinating hiking trails in Washington: the Iron Goat Trail. Taking its name from the mountain goat on the logo of the Great Northern Railway, the Iron Goat trail follows the portion of the railroad grade that was abandoned in 1929 after the 8-mile long Cascade Tunnel (still in use by the BNSF today) opened, which for the first time allowed trains to bypass the pass and its deadly avalanche chutes entirely.
Looking into the abandoned Windy Point Tunnel along the Iron Goat Trail
While this hike may not provide a wilderness experience (Highway 2 and the associated drone of motor vehicles is just a stone’s throw away across the valley), it does provide a heavy dose of history and just enough eeriness to keep you from ever wanting to spend the night. In between the Wellington disaster and the opening of the Cascade Tunnel, a span of just 19 years, the Great Northern Railway heavily fortified the section of rails near Stevens Pass in an attempt to prevent another disaster. I hiked the four mile section of the trail from Highway 2 to the Wellington Townsite and nearly the entire stretch was engineered in some way: tunnels, timber snowsheds, concrete snowsheds, you name it, the Great Northern Railway spared no expense in attempting to tame the mountains and make this a viable travel route over the Cascades. They even gave the town of Wellington a new name, “Tye”, because of all the bad publicity. Ultimately though, the mountains emerged victorious: the line was abandoned in favor of the tunnel less than 30 years after it was first constructed, leaving the man-made structures built in response to the Wellington disaster to slowly decay and become re-assimilated into the mountain.
This process is already well underway. After decades of enduring heavy winter snows, timber snowsheds are now unrecognizable piles of rotting wood. Concrete snowsheds are crumbling, exposing their innards in a scene that my hiking partners likened to the post-apocalyptic visuals of the Hunger Games.
Deep snow and avalanches ultimately get the better of anything man builds to lessen their impact
Many of the tunnels have partially collapsed, including the Old Cascade Tunnel, the longest in the world when it opened at the beginning of the 20th Century. In 2007, a portion of the roof collapsed, creating an unstable dam of debris which occasionally likes to rupture and send a deadly torrent of water rushing out the west end of the tunnel without warning. The Windy Point Tunnel, built to keep trains from derailing around a particularly sharp curve, is also slowly crumbling away while the entrances are slowly reclaimed by the forest:
Moss and debris slowly reclaims the old grade of the Great Northern railway at the entrance to the Windy Point Tunnel
Portions of the Windy Point Tunnel have been heavily damaged by rockfall. Thankfully, Gary and the fall foliage escaped unscathed.
After a somewhat strenuous 700 foot climb from the trailhead up to the Windy Point Tunnel, the hike follows the gentle grade of the old rail bed for several miles in either direction. Thanks to impressive work by local volunteer groups, the trail is well-maintained and a series of interpretive signs explain the history of the Great Northern Railroad and the chain of events that led to the Wellington disaster. Several spots on the trail have great views of the Tye River valley and the surrounding peaks in the Cascades making for a beautiful, intriguing, and incredibly diverse hike. But stay away during the winter for obvious reasons, and like I said, not really somewhere you’d want to spend the night…
Fun graffiti inside the concrete snowshed
For more info, trail maps, and directions, check out http://www.irongoat.org/
Out of all of the numerous ruin and rock art sites in the Sedona area, Red Tank Draw is one of the least known, most remote, and difficult to find sites. Red Tank Draw is a tributary canyon of Wet Beaver Creek about a half hour’s drive south of Sedona. The wash that runs along the bottom of Red Tank Draw, which is bone dry for probably 90% or more out of any given year, today looked like this:
Unseasonably warm temperatures combines with lots of snowpack to the north near Flagstaff meant that the normally dry stream bed was a veritable raging river today. Given that the petroglyphs are located along both the east and west sides of the draw, the high water level made things difficult to say the least. Several dirt roads lead right up to the western rim of the draw but we were unable to find a single crossing point along about a 2 mile stretch of the draw. We briefly considered simply wading across the stream but given that the water was moving surprisingly swiftly and any crossing would have involved wading through waist deep water, we decided this was probably a bad idea.
Fortunately for us, the largest and most spectacular panel is located on the side of the creek that was accessible to us. After several hours of bushwhacking our way in and out of the draw, we came across a finally found a fairly well defined path that led us on a short scramble down into the draw and spit us out right in front of the petroglyphs. The main panel is located at the base of a large and impressive rockfall. The rockfall must have occured relatively recently since many of the petroglyphs are actually located on huge blocks of sandstone that have clearly fallen from the cliffs above. Several additional Volkswagon sized angular boulders are precariously perched on the cliffs above the petroglyph panel and look as though a strong breeze would send them crashing down as well.
Overall, the petroglyphs are extremely well preserved. Unfortunately, there have been problem with vandalism at this site in the past, but surprisingly there is actually a Forest Service register at the base of the cliff. The sheer size of some of the carvings is what impressed me most. At the upper left of the main panel is an enourmous Elk petroglyph, more than two feet from tail to antler tip. Supposedly there are a number of other panels scattered along the draw nearby but we were not able to access any others due to the high water level in the creek.