Dome Col Traverse: Glacier Skiing At Its Finest

The last day of temperature inversion called for a proper adventure. We decided on completing the Dome Col Traverse. Our route would take us up the Lily Glacier in the Loop Brook Valley, through the col, and down the Dome Glacier in the Asulkan Valley. It’s an ultra-scenic ski tour that takes you through one of Rogers Pass’ famed perch. With the right glacier travel and crevasse rescue training, I highly recommend the Dome Col Traverse to anyone looking for spectacular views and a good push.

Related: Sapphire Col Traverse: An Alpine High

skier racing down a glacier
Fred, skiing down the characteristic roll of the Dome Glacier. Photo: The Uptrack

Report from December 3, 2020

I assembled the team: Iannick and Freddy, two experienced backcountry skiers that I would trust with my life if shit was to hit the fan. Our day began at the Loop Brook parking lot, frozen solid by the cold morning breeze. It’s no understatement that this drainage is an ice-box, being surrounded by some very serious glaciers. After a prompt transceiver check, we slogged up the Loop Brook, crossing fast-moving water at the Elephant Trunk. From there, we were but a short bushwhack away from the narrow moraine leading up to the Lily Glacier. Let’s call that one the Lily Moraine.

two men skiing up the loop brook drainage
Iannick and Freddy, moments before reaching the Lily Moraine. Photo: The Uptrack

Along the way, we observed the presence of surface hoar, on sheltered aspects, noticeable by the magical glimmer the crystals produce as they reflect sunlight. We quickly hopped on the Lily Moraine, a high-ground route that would negate the overhead avalanche hazard from the exposed west slope of Mt Afton. The Bonney massif stood high above us with its heavily-crevassed glacier lying at the base of its headwall. From our perch, we could spot the Dome and its col, the high point of the Dome Col Traverse.

Surface Hoar Facts
Surface hoar, otherwise know as hoar frost, is a bitch. That’s a common saying for ski tourers around the world. Those delicate frost crystals are formed at night during periods of calm winds, high humidity, clear skies, and sub-zero temps. They usually form during bouts of good touring weather in sheltered areas. It’s no surprise that the Selkirks and Monashees (basically inland rainforests) harbor tons of surface hoar, especially at treeline and below. Once buried, surface hoar is preserved under additional snowfall, can support large vertical loads, and rarely break down naturally. Since the snowpack is unable to bond to the buried hoar, the crystals form a persistent weak layer, waiting to be triggered by unaware skiers.
ascent to the dome col through the lily glacier lower section
Our route up the Dome Col in the Loop Brook Valley. Taken from the Lily Moraine. Photo: The Uptrack

We shimmied along the Lily Moraine until we cleared the hazard posed by Mt Afton as the tree cover started to thin out. From there, we traversed through the low ground and connected with yet another moraine, looker’s left of the Lily Glacier, which was barely in our view at that point. This was a painful reminder of global warming’s impact on small glaciers. The small toe had receded halfway up the valley, now only a few hundred meters below the Lily Col.

ascent to the dome col through the lily glacier upper section
Our route up the Lily Glacier on the Dome Col Traverse. Taken from the higher moraine. Photo: The Uptrack

Eventually, the height-of-land walk came to an end as we reached the end of the moraine, just a little above treeline. We now faced the rocky, wind-scoured west face of the Rampart, a broken, knife-edge ridge that looks like the back of a stegosaurus. Let my nerdy Jurassic reference sink in with you a bit!

view of the lily glacier with route to dome col and sapphire col
Possible uptracks on the Lily Dome Traverse. Photo: The Uptrack

Since we planned on traversing below the slope, the overhead hazard was worth discussing. Things were looking good: the natural avalanche cycle happened more than a week ago, the aspect, albeit solar, wasn’t warmed up enough by the low-lying December sun and the ridgetop winds would remain calm for the foreseeable future. Excellent! During a brief lunch break, we met two aspiring ski guides, Jeff and Joe, people I consider friends and touring partners to this day. They unintentionally joined us for the ascent since we advanced at nearly the same pace.

two male skiers walking up below the west slopes of mt afton
Jeff, followed by Joe, below the Rampart. Photo: The Uptrack

We began the uneventful crossing under the west face of the Rampart. Uneventful is good! The katabatic winds had done a number on the snow’s surface. The 20cm of dry powder below turned into a hard crust. It took all the edging I could muster to maintain traction on the wind-affected snow. I was damning myself for now bringing ski crampons. Somehow, Iannick had no trouble dealing with the side-hilling as he bolted way past us on his fruitless quest to drain his infinite supply of energy.

Katabatic Wind Facts
Katabatic winds are generated when a cold, high-density air mass at elevations moves downslope into a warm low-density air mass at the bottom of valleys. This is felt like an icy breeze heading down and away from glaciers, commonly at nighttime and in the early mornings when the glacial slopes radiate their heat into the open skies and cool off.
solo skier with the dome behind him
Iannick, leading the charge on the icy crust below the west face of the Rampart. Photo: The Uptrack

We escaped the Rampart’s crosshair just as the snow was visibly warming up, a reminder that moist snow spells disaster. We pressed on towards the upper bench of the Lily Glacier. As we crossed above the Lily Col (2480m), the winds, funneled through the terrain constriction, dramatically picked up to the point where they almost knocked Freddy over. We felt like one of those polar explorers forging a path through a frozen landscape riddled with sastrugi.

solo skier walking up the lily glacier in high winds
Fred, bracing himself in the gale-force winds above the Lily Col (2480m). Photo: The Uptrack

Once we reached the toe of the upper Lily Glacier, we donned the glacier travel and crevasse rescue equipment, aka all the dangly bits. After a short refresher on glacier rope management, we began the short pilgrimage up the glacier, now roped up. It’s worth noting we roped up for practice since the Lily Glacier is barely crevassed. Usually, I don’t bring the gear up there but it doesn’t hurt to be on the cautious side.

Glacier Travel Basics
I cannot overstate the importance of taking a glacier travel and crevasse rescue course before jumping on glaciers, no matter how mellow they are. On top of that, first-hand knowledge of the specific glacier on which you would be traveling is paramount. Consider hiring a certified mountain guide as they know the ins and outs of glaciers such as where the crevasses are located and which slopes to avoid.
two roped up mountaineers walking towards the dome col
The charge up the Lily Glacier to the Dome Col. Photo: The Uptrack

We eventually reached the base of the Dome Col, caked with faceted snow. I knew the sugary snow would make booting up the rock slab a chore. We packed away our glacier gear and prepped our backpacks for the short stint up the col, now lying in the shadow of the Dome.

fred booting across the dome
Freddy, leaving the Lily Glacier on his way to the Dome Col. Photo: The Uptrack

To my surprise, the bootpack was easier than expected. Jeff and Joe made short work of it, following a well-established track that was put in a few days ago. Within minutes, Jeff and Joe who were now standing proudly at the top of the col. Looking back, the views of Rogers Pass were absolutely stunning. This is a one-of-a-king valley!

group of skiers and splitboarders climbing the dome col
Jeff and Joe, climbing the Dome Col. Photo: The Uptrack

With much time to spare, we gained the Dome Col and peered past the Dome Col into Asulkan Valley, magical as always. A hundred meters away, our impromptu partners were perched above the Asulkan Glacier on a prominent ridge dividing the latter from the Dome Glacier, called the Cleaver. The Jupiter massif was standing high in the distance, towering over the Asulkan, a view that granted me a good bit of insight into the surrounding terrain. Those terrain photos will come in handy when I’ll be attempting the Jupiter Traverse in spring.

view from the top of the dome glacier with the asulkan glacier below
Jeff and Joe, chilling on top of the Cleaver at the Dome Col. Photo: The Uptrack

After a good fifteen minutes of rest, we clipped in our bindings and transitioned from the Cleaver onto the Dome Glacier through a precarious wind-battered ramp. This was now the second part of the Dome Col Traverse. The snow was without a doubt gross, an unavoidable fact of life when skiing exposed alpine terrain. Slow, cautious turns were the names of the game.

skier craving a turn in shit snow with glacier national park in the background
Freddy, carving a couple of turns in the shit snow at the ramp above the Dome Glacier. Iannick, in the distance. Photo: The Uptrack

Surface conditions improved past the ramp. The wind-affected snow turned into light, fluffy powder. Based on our local observations as well as the avalanche forecast which indicated a “moderate” hazard at al[pine elevations, we decided on skiing the Dome Roll, a large convexity leading into a steep glacial slope. Otherwise, we would have veered right following the Cleaver and dropped into a mellower grade.

descent on the dome glacier from the dome col with overlay V2
The descent on the Dome Glacier, part two of the Dome Col Traverse. Photo: The Uptrack

From the top of the glacier, the slope seemed to roll off into the unknown. I’ve got a particular dislike for rolling glaciers since I don’t get to scope out the crevasses below. After sending it off a serac in Chamonix on one of those, I learned my lesson. Nonetheless, the slope’s grade past the convexity took me by surprise, at which point I gained a little too much speed for my lightweight skis to handle. Luckily, conditions were prime for a quick brake as soon as I realized my predicament.

skier slashing powder on the dome glacier in rogers pass
Freddy, slashing some pow midway down the Dome Roll. Photo: The Uptrack

After sharing our stoke at the bottom of the glacier, we sneaked through a narrow, icy choke, located skier’s left of the Dome Headwall, a steep rock slab below the glacier’s toe. I was struck by the beauty of this feature, covered in clear blue ice! How pretty! We traversed a series of convoluted moraines towards the foothill of Mt Afton, only to burst through a pillow field right above the Asulkan Brook. From there, we performed the usual slog out of the Asulkan Valley and traversed back along the highway to the Loop Brook parking lot in the dark with the loud rumble of trucks whizzing by us.

With good terrain knowledge and proper training, the Dome Col Traverse is an accessible, uber-scenic alpine traverse along with the Little Sifton Traverse and the Sapphire Col Traverse. Highly recommended, go do it! Hire a guide if necessary. It’s worth its weight in gold.

Route Info