Colorado Backcountry Turns All Year: Year 1, Months 7-9 (2021)

I am not the first person to try and ski every month of the year in Colorado. While the overall numbers aren’t many, there are people who have done this thing every month for decades or more. And while the elevation of the Centennial State guarantees turns through mid-July at hundreds of locations, by the time August and September roll around, you’re options become really limited. Additional limiting factors include the rate of recent snowmelt and the previous season’s snowpack. Luckily for me, I decided to ski in a year that only managed an average winter snowpack and experienced a warmer than average June/July…wheee.

Faced with dwindling options, I honed my focus on the areas of Colorado that seem to hold onto snow the most. In the northern Front Range, those areas are high, cold, sun-starved alpine cirques. Some of these feature permanent snowfields, and some feature the occasional glacier. For August and September, those became my focus while I clung to the hope that October might signal the return of accumulating alpine snow.

This is part of an ongoing series, for parts one and two, click on the links below.

Table of Contents

Backcountry Warning and Resources

If you’re tip-toeing into backcountry skiing, there are a ton of resources and education that I would consider mandatory before taking it to the hills. I’ve compiled a list below.

  • Avalanche training (look up Avvy 1 certifications near you).
  • Avalanche gear (shovel, probe, beacon, radio).
  • Regular ski gear plus skins, frame/tech bindings.
  • Orienteering skills (download offline maps, have a GPS watch, or bring a physical map and a compass).
  • Scout your line before committing.
  • Ski with partners when able (if not able, compensate by only attempting on the best day conditions wise). This is a touchy point, many refuse to attempt without a partner, and I accept that, but if you have a flexible risk tolerance and can accept more risk in one area (solo journeys), you have to compensate by nailing down all other aspects of the planning process to make the risk defensible.
  • Check the weather up until the moment you leave.
  • Leave your plan with a loved one and have that plan include emergency contact info should you miss a predetermined rendezvous time.
  • Here are some Colorado-focused resources I use: OpensnowFront Range Skimo, Mountain Weather Forecasts (click here), CAIC (they have an Instagram page, and there are other associated avalanche pages to follow as well), NWS.
  • For added info on planning and gear, please visit these two articles I wrote for an outdoor website called SkyblueOverland. The topics covered are crucial for any aspiring backcountry skier/rider. Essential Backcountry Gear, and Guide to Planning a Backcountry Adventure.
  • Additionally, I wrote an overview of Colorado Snow, which has a bunch of additional information pertinent to centennial state winters.
  • Jump to Table of Contents

Month 7: August 25, 2021 (Ptarmigan Glacier)

Ptarmigan Glacier, tucked into the Continental Divide between Flattop Mt. (left) and Notchtop (right).

After a successful July ski of Andrews Glacier, I began looking at the rest of Rocky Mountain National Park in search of other permanent pieces of snow. I’d passed by Ptarmigan Glacier (a name that doesn’t usually show up on official maps but has been recorded in many user trip reports and blogs) the year prior when I scrambled up Little Matterhorn. It’s not too terribly far from the Bear Lake Trailhead (roughly similar to Andrews, just the opposite direction), and from what I’d researched, stays snowy all year. Good enough for me

So, one late August day, after delaying what I knew would be a taxing journey with skis on my back, I finally committed.

Views toward Estes Park as the day slowly dawned.

Like Andrews, I used the Bear Lake Trailhead. This time, however, I went north, around the bulk of FLattop Mt. and the Banana Bowls (another lower angle backcountry area in the winter/spring), and continued as if heading towards Odessa Gorge. The whole Odessa area is magnificent, from the lakeshore to the views of Notchtop; it’s all National Park-level beauty.

Notchtop (and Notchtop Spire) from just above the Odessa Lake trail.

The established trail ascends gently to a saddle near Joe Mills Mountain and then drops into the gorge before finding the shores of Odessa Lake. My turnoff into the backcountry was at the saddle, where a noticeable but unsigned path leads south to Lake Helene, a shallow pond that acts as a great marker.

Lake Helene and the not-so-flat sides of Flattop Mt.

I followed the use trail around the right shore of the lake until a series of paths began veering uphill. Using a combination of a few, I found a route that ascends away from the lake and higher into the gorge. This part was a bit frustrating because Krumholtz kept catching my skis, but I soldiered through, following the occasional cairn, until I broke into the alpine.

As you can see in the picture above, stubborn vegetation gives way to two separate snowfields. Up until July, they are more or less connected. The upper field is what’s generally referred to as the glacier, although both fields are large enough to last all year. The navigation was never really hard on this trip, but it was a taxing approach nonetheless. As the terrain changed to talus and scree, my pace slowed to a crawl to make sure I wasn’t misstepping or taking a long rocky ride down a loose slope.

I broke out the crampons and climbed the first snowfield, thankful to be on more of a solid surface. All around the snowfield were large pieces of talus on unstable slopes. The whole area looked like it moved with some regularity, so I was keen to avoid any suspicious-looking areas. Using the crampons to bypass a particularly perilous-looking hogback saved me time and worry.

Looking back at a couple unnamed tarns as I get ready to climb the first snowfield.
Climbing up the first snowfield, notice the layers of windswept dirt on top of the snow. Not only is summer skiing limited to existing snowfields, but in a lot of cases, you have to deal with dirt, exposed rocks, ice, slush, and rockfall. Just because avalanche danger is low to non-existent doesn’t mean there is no danger.

Between the two snowfields, I chose an angling ascent over loose ground until I could traverse over to the second, larger snowfield, aka Ptarmigan Glacier, and put my crampons back on.

Ptarmigan Glacier.

As far as permanent snowfields go, Ptarmigan didn’t look as sad as some of the others I’d seen; the top half looked fairly cohesive and nice, but the bottom half bled into a talus field with plenty of scree poking up out of the snow. The skiing looked like it would be challenging, which felt appropriate since it was late August. I channeled some energy and spike-stepped my way up.

Up we go.

As I mentioned in a previous post, the ideal time to hit these slopes is before the afternoon sun creates slush out of the top layers of snow. This process slows when you have temperatures that dip below freezing the night before. Well, in the middle of summer, that doesn’t happen often, so, even though I made good time getting to the glacier, the climb was slushy and uncomfortable. I had to brace a few times to stop from sliding.

Interesting looking crevasse near the top.

I made it one piece and allowed myself a bit of time to prepare but wanted to turn around and start skiing soon because the slush issue was only going to become more pronounced as the day warmed up.

Top-down view.

To be honest, the skiing was a bit terrifying. I connected ~10 turns, but the top was a mixed bag of hard snow ridges and sun-cupped BS, the middle was slushy, and the bottom was a minefield of fist-size rocks that could really screw up my skis. I threaded together as many safe turns as I could but ultimately had to take my skis off and boot pack down the last hundred feet; there was just too much detritus to avoid.

It was too dangerous of a ski to film with my phone so this is the only “mid-action” photo I have. I think this day convinced me to start looking at Go-Pros, which I would eventually get by the year’s end.

So, yeah, I skied in August on a dwindling glacier in a National Park. It was harrowing, steep (~42-45 degrees at its steepest pitch), and riddled with debris that would’ve destroyed my skis had I not been paying attention. I don’t think It’ll be on the repeat list anytime soon, but it was a good reminder that while dirty snow can be skied, it’s really tricky.

I also finally got a good idea of what a “rock” glacier is, which I thought was pretty cool.

As yearly erosion dumps more rock and debris into valleys and cirques, they end up covering the top of the ice. The ice doesn’t really go anywhere; it just hangs out under accruing layers of rocks and dirt. Practically, this makes the terrain on top of the ice exceptionally loose and subject to sliding; as far as climate change goes, the layers of rocks actually help hide the glacial layers from direct sun exposure. So, even though you may not see a bunch of ice and snow above ground, in some areas, you can bet that the ice still exists; it’s just hiding below the rocks i.e., rock glacier.

What’s interesting about Ptarmigan (Taylor Glacier is also a good example) is that a substantial portion of the ice is still visible, so you get the above surface “glacier,” and you can see the transition zone into the sub-surface “rock glacier.” Cool stuff.

Here’s what you’re looking at. A roughly 20 foot wide, 8-foot tall chunk of ice covered by dirt and scree. In fact, everything in this picture is resting on top of ice. The only reason this piece is exposed is because the summer snowmelt creates a runoff stream from the glacier; as the water moves, it carries debris down the slope, opening up a channel to sun exposure. Between where I took this photo and the ice chunk, is a ravine about 10 feet deep that leads to a running stream on top of more ice layers. There was no way I was walking up to the edge, so this is as close I got.

Rock Glaciers are exceptionally unstable (because it’s all resting on ice) and demand careful footfalls and risk management. Naturally, I traversed it in ski boots.

Another instance of debris on top of visible ice.

The “rock glacier” continued pretty much right up to the lower snowslope. As I carefully made my way to it, I started to tire of the tedious footing and thought it may be worth it to grab a few extra turns on the lower snowfield and drop a couple of hundred feet relatively quickly.

To my surprise, the snow surface was much more agreeable on this field, and I actually made some half-decent turns without feeling like I was two steps away from dying.

Slide the bar to see roughly where I made my turns. You can see where the snow is disturbed from the turns but it’s not immediately obvious.

After managing a handful of extra turns on the lower snowfield, I felt accomplished enough to call the outing a success. I made my way to the tarn at the base of the lower snowfield and collapsed on a nice, sunny rock. Compelled to celebrate in some way, I stripped down to my birthday suit and got into the water.

Hand down one of the top five coldest water experiences of my entire life, and I’ve jumped into the Arctic Ocean before!

The tarn is only exposed enough to get into for maybe two months out of the year, so it’s all frigid snowmelt. Despite the shock, I didn’t freeze to death and let the sun dry me. A few confused and concerned rock climbers descending from Notchtop probably got more of a show from my naked lounging than they would’ve liked, but hey, after hauling my skis all the way up to Ptarmigan and faced with the daunting prospect of hauling them back to the car, I can’t say I was in much of a caring mood.

Cold, cold water.

After my quick water refresh, I summoned as much energy as I could, strapped down all my gear, and dragged myself back to the parking lot. Unlike the hundreds of questions I had to field coming back from Andrews, I only spoke to a handful of people. There were still hordes of visitors near the trailhead, but I think they were too shocked at my appearance to even let some questions out, fine by me, haha. August ski down!

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Month 8: September 16, 2021 (Knobtop Icefield)

The previous October, I hiked Little Matterhorn, a Class 3 scramble overlooking the Odessa Lake area of Rocky Mountain National Park, and just a stellar adventure all around. While on the ridgeline to the summit, I noticed a large snowfield hiding under the bulk of Knobtop, a relatively ill-defined area with a flat top, gentle western slopes, and a precipitous eastern and northern wall. The snowfield looked large and interesting, so I decided to revisit the area and see if my observation last year held up to skiing scrutiny.

Not bad; decent vertical to boot.

So, a little less than a month after my Ptarmigan Glacier descent, I saddled up for an attempt of the Knobtop Icefield.

I really wanted the snowfield to be exactly the way I’d seen it the year prior, but that turned out to be pretty optimistic on my part.

The approach was fairly benign until I broke from the trail around Lake Helene as I’d done for the previous hike. Instead of heading up into the Ptarmigan Glacier area, I traversed underneath a small headwall and descended below Hope falls. Technically, this is the same gorge that originates near Ptarmigan, but the headwall is a significant enough obstacle to legitimately call them two separate things (Odessa Gorge and Ptarmigan Cirque, for example).

Little Matterhorn and the Gables from near Lake Helene.

After descending below Hope Falls and crossing the stream, I found myself in a familiar talus field and slope (the same approach that I’d used to climb Little Matterhorn the year prior). This part I knew wasn’t terribly long but featured some serious elevation gain that I had to do with skis. It was a long, and grinding ascent, but I stuck to areas that I thought looked the most stable and slowly made my way higher.

Generalized ascent path, turns out, not the easiest way, but certainly the most direct.

My path was…ok, I mean, I arrived where I wanted to, but the loose rocks and steep slope angle made me a bit nervous, and if you’ve ever tried to hike anything with skis on your back, you’ll know how easily you can get off balance. So, I stumbled, cursed, and dragged myself up the rise, hoping to reach what I knew would be a relatively flat talus field leading up to the edge of the icefield.

The first views of the icefield were…not super inspiring.

Oof, dirty and a lot smaller than last year’s observations.

Feeling the looming specter of failure creep in, I resolved to at least scout the whole field from its base to see if there were any places I could rope together a measly five turns. The longest part of the icefield looked initially good but led right to a rockfall chute, and after watching countless fist-sized rocks scream down the icefield and crash into the talus below, I was keen to avoid that part.

I did find one section that looked relatively clean and was tucked up underneath a solid-looking rock wall with nothing overhung above it. To be honest, the whole area was a huge rockfall hazard, but I angled towards an area that looked white (so not a lot of surface debris) and got as close as I could to the start before getting my climbing gear on and preparing for a steep ascent.

Certainly not pretty, but clean enough to ski.

My crampons got their money’s worth as the terrain steepened quickly past 40 degrees. It wasn’t an altogether long ascent, but the sun-cupped surface, steep profile, and constant rockfall danger kept me plenty focused. I angled towards a large bergschrund (specifically, a randkluft in my case) between the top of the icefield and the solid rock walls behind it. In that pocket, I awkwardly got ready.

This is not beginner territory.

Also, in case you are unaware of what a bergschrund or randkluft are, this still shot from a video I took should provide some context. In no way was this a comfortable changeover from crampons to skis.

As the summer sun melts snow slopes, the snow can pull away from the walls behind them, creating a gap or a bergschrund. Technically, since this was the gap between stagnant ice and rocks as opposed to a moving glacier and stagnant ice, the appropriate term is a randkluft, but the key element is the same: a crevasse-like gap between ice and other stuff.
In the randkluft.

After a few trying minutes, I got all my gear ready and awkwardly sidestepped from the lower part of the randkluft up to the crest and gently, nervously, stepped my skis over. I was leaning so much on my inside edges I thought I’d fall right back into the randkluft, but it all held together, and I slid forward to a patch of clean snow.

Yeah, so, perhaps unsurprisingly, this was not a banner skiing day, but in the middle of the summer, beggars can’t be choosers. Would I ever repeat it though? ….Uhm.

I didn’t take any pictures on the way down but did manage to put together a set of turns that actually made me really proud. Despite my wonky start, I settled in quickly and hit the skiable bit with the same confidence I had at Andrews Glacier, which is saying something. I hated the rockfall danger and looming sense of potential catastrophe, but I skied better this day than I did on Ptarmigan in August.

I did get some perspective shots from further back and could trace my lines, which was neat.

Gotta love old iPhone pic quality. Below the red line, I unstrapped and just carefully heel kicked my way down, far too much debris.

Below is a different perspective from farther away. I drew in the lines using a computer mouse, so there may be small differences between representations, but you can clearly see my first few turns in the shade on the undrawn version.


The skiing was strangely better than August, but this was by far the most dangerous ski of the year.

Although I made it down the ski slope just fine, I had another couple of heart-stopping moments when chunks of rocks cascaded down from higher elevations. Hearing a rock pick up speed, hitting what looked like 60-80 mph, and then split into a thousand pieces when it hits a piece of talus bigger than an SUV certainly leaves an impression.

Luckily, I had scouted potential lower-risk escape routes, and because I had already identified the problem spots above me, I knew I wasn’t in immediate danger. With barely any wind that day, the biggest factors were sun-melt on the ice and rockfall from gullies and slots that broke through the walls above me. I could tell where those gullies emptied out because of how the snow looked (darker=more debris covered), and you can see that in the picture below. Purposely picking my line to ski the best conditions, as opposed to the longest vertical, saved my skis from getting too beat up and kept me in one physical piece.

Left pic, no markup. Right pic, Red arrows=most likely rockfall direction based on my observations. Blue=the area where I skied. PLEASE NOTE: all of this was completely dangerous, I just worked with the best option.

Still, having a bunch of rocks break a few dozen meters away from you is not a calming experience. I kept my helmet on for the majority of the return hike to lake Helene and only stowed it when I was safely back on established trails.

The hike back felt somehow more exhausting and challenging than last month’s outing; my ski straps kept loosening, so I had to do a bunch of re-adjusts, and talus hopping with skis on just beats you up. I did make it back successfully, and despite the rapidly forming blisters, felt pretty good about how I’d managed what is definitely one of the craziest backcountry adventures I’ve done.

Quick PSA: This is all completely nuts, and I think that should be noted somewhere in every piece I write about this kinda stuff. I am a competent skier and mountaineer with decades of experience; I’m also a 6-year ski instructor; additionally, I have years of trail-building and months of alpine camping/living under my belt. I make it my business to understand the mountains and the hazards they harbor, and I have turned around on many adventures when the conditions weren’t right.

I really like being alive, but I also intimately understand my personal thresholds because I have that conversation with myself often. Like most aspects of life, thresholds change over time. As silly as it sounds, the best advice when you’re pushing yourself in the outdoors is to get right with yourself, figure out what you can and won’t do, and identify the gray area where you can build skills into. After all the years I’ve spent in the outdoors (along with the hundreds of Colorado mountains I’ve climbed), I felt that I could handle the risks presented to me on this day, but I am always preparing for the day when that’s no longer the case.

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Month 9: October 28, 2021 (Shrine Pass Meadows)

When we talk about the alpine in Colorado, there’s usually a period of time in the autumn when a series of high elevation storms bring the first snow of the year. Most of this is unskiable from resorts, and there’s a fair amount of melting between storms because the sun angle is still high, but it signals the inevitable arrival of colder weather. Well, this year, that first bout of snow took its sweet time showing up. There were a few anemic spurts in early October, but finally, towards the back half of the month, a stronger storm targeting the western slope dropped up to a foot on the mountains around Vail Pass. My time had arrived.

By this time, I’d also managed to wrestle down the inevitable criteria I would use for the challenge. With an understanding that I’d elected to keep my skiing limited to the I-70 corridor and north, I figured exploring a small section west of Vail Pass would make for a nice excursion. I knew the road to Shrine Pass was skiable, so I planned for that.

The new snow, while copious for October, was also still drivable, so I ended up giving the ole snow tires a workout and chugged up the Shrine Pass Road, looking specifically for low-angle grassy slopes where the chances of skiing rocks was a lot lower.

I had no illusions that this was going to be a short outing. Already limited by early season snowfall, my hope was to just recycle a few slopes until I felt like I’d made my five requisite turns. All in all, I found three separate “runs” and pieced together about 20 turns between them.

Easy and it counts.

There were a few people out skiing the road, but after driving over some bare patches, it looked, to me, like it would still mess up a pair of skis, so I was relatively excited to find soft slopes without surprise gravel under them.

There were a couple of times I broke through the snow, but luckily the surface was soft underneath. If you strain, you can see at least five turns in this photo.

This day wasn’t anything to shout about, but after languishing through the first part of October, wondering if I’d get to ski fresh snow or be forced to have another experience like August and September, I was just happy to be able to ski something soft.

I think from start to finish, I was on my skis for maybe 90 minutes total, and a lot of that was just soaking up being outside.

Yeah, no real issues, just enjoyed some high-altitude October turns under cloudy skies and on top of fresh snow.

Naturally, thoughts turned towards the following month since another storm was set to hit, and I wanted to take advantage but I also took a moment to give myself a high five, month 9 of backcountry turns complete! Only three more before I’d skied a whole year!

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Colorado Backcountry Turns All Year: Year 1, Months 4-6 (2021)

April 2021 was a breakout backcountry ski month for me. While I only managed three days out in the hills, they were all exceptionally satisfying, and my confidence rose accordingly. As I mentioned in my previous turns all year post, by early May, the idea of doing a full year of backcountry skiing still hadn’t made it to the forefront of my brain. As a kind of interim goal, I’d resolved to keep the skis out of storage until at least June. In fact, I already had an idea of what the ski adventure could look like. As for July and beyond? Hadn’t even considered it yet.

From late April through mid-May, my wife and I had a few trips we needed to take (family visits and a sister’s graduation from college), so backcountry took a backseat. However, as May wound down and I found myself with a solid week and a half weather window, the pressure to go do something epic began to ratchet up in my head. And while the winter of 2020/2021 was average in pretty much every sense of the word, the spring of 2021 was temperate and wet, with a lot of alpine spring snow available for the taking.

Table of Contents

Backcountry Warnings and Resources

If you’re tip-toeing into backcountry skiing, there are a ton of resources and education that I would consider mandatory before taking it to the hills. I’ve compiled a list below.

  • Avalanche training (look up Avvy 1 certifications near you).
  • Avalanche gear (shovel, probe, beacon, radio).
  • Regular ski gear plus skins, frame/tech bindings.
  • Orienteering skills (download offline maps, have a GPS watch, or bring a physical map and a compass).
  • Scout your line before committing.
  • Ski with partners when able (if not able, compensate by only attempting on the best day conditions wise). This is a touchy point, many refuse to attempt without a partner, and I accept that, but if you have a flexible risk tolerance and can accept more risk in one area (solo journeys), you have to compensate by nailing down all other aspects of the planning process to make the risk defensible.
  • Check the weather up until the moment you leave.
  • Leave your plan with a loved one and have that plan include emergency contact info should you miss a predetermined rendezvous time.
  • Here are some Colorado-focused resources I use: Opensnow, Front Range Skimo, Mountain Weather Forecasts (click here), CAIC (they have an Instagram page, and there are other associated avalanche pages to follow as well), NWS.
  • For added info on planning and gear, please visit these two articles I wrote for an outdoor website called SkyblueOverland. The topics covered are crucial for any aspiring backcountry skier/rider. Essential Backcountry Gear, and Guide to Planning a Backcountry Adventure.
  • Additionally, I wrote an overview of Colorado Snow, which has a bunch of additional information pertinent to centennial state winters.
  • Jump to Table of Contents

Month 4: May 22, 2021 (Tyndall Glacier & Gorge)

Rocky Mountain National Park is one of the top 5 most-visited national parks in the country, and for good reason, it’s really pretty and less than two hours from a large metro area. The park is an outdoor mecca, and that means winter recreation as well. The Bear Lake Road corridor is a particular highlight, and any casual outdoor Instagram follower will have seen a ton of #inspiring/#grateful posts featuring a lake, pinnacles to the right, and a tilted blocky looking mountain to the left. The gorge in-between them is Tyndall Gorge, and if you hike up to the headwall, you get Tyndall Glacier. Ever since seeing the view from Dream Lake (picture below), I’d wanted to do a couple of things, ski Tyndall Glacier and climb Chaos Couloir up Hallett Peak. This year I’d do both, but since the snow was starting to melt lower down, skiing became the top priority.

Bam. While you can’t quite see the glacier yet, you get an idea of the gorge run (down the middle), Hallett Peak (left), and the Pinnacles to the right that house two gnarly ski mountaineering routes: Dragontail Couloir and Dead Elk Couloir.

With an elevation above 9k, the top of Bear Lake Road is the perfect place to explore some spring skiing. While there are many ways to access Tyndall Glacier, I wanted to skin up from the bottom because I hadn’t skied in the upper part of the gorge, and I wanted to see it before dropping in. When I arrived at the parking lot, there was enough snow about 1/4 mile from the trailhead to strap skins on, which I gratefully did. Not that carrying skis is overly complicated; they’re just heavy. So, I was keen to take any chance to connect snowfields without the extra weight.

On the way in, you pass three lakes, Nymph Lake, Dream Lake, and Emerald Lake. Beyond Emerald, the terrain steepens sharply, the crowds fall to the wayside, and you feel as though you’re back in the wild. Starting early enough, I’d already beaten most of the day-trippers, but crowd avoiding is a big part of my outdoor ethos. Not that I mind people beholding magnificent scenery, but for a serious outdoor adventure, you don’t necessarily want a huge audience watching your every move. Unfortunately, my head was so focused on speeding up to the start of the line that I took an ill-advised shortcut across a corner of Nymph Lake. In my defense, the ice was thick when I stepped onto it, but after crossing the lake, I had to get back on dry land, and the edge had a weak ice layer that was rapidly melting. My weight sent my skis through, and before I could curse, both boots were in the drink.

Soaked and a little pissed, I took stock of the damage, dried the boots as best I could, slapped a new pair of socks on, and continued. The weather was supposed to be a warm 50 degrees with ample sunshine (and no humidity because Colorado is high and dry), so I figured I wasn’t going to freeze to death, and the thought of being defeated by four feet of water didn’t leave a particularly great taste in my mouth. So, I soldiered on.

National Park-worthy scenery almost every step of the way.
If you look closely, you can see at least three climbers on the lower/mid portion of Dragontail Couloir.

The two other lakes passed in quick succession, and before I knew it, I was scrambling over some boulders near Emerald Lake, looking to gain elevation for the eventual ascent into the gorge. As predicted, the crowds vanished after Emerald until it was just me and a handful of other backcountry hopefuls, each set on their own objectives.

Dead Elk Couloir (L.), and DragonTail Couloir (R.).

I saw a group peel off to the East Couloir, a 45-degree option that attacked the ridge of Hallett Peak, and another group further ahead, heading for Tyndall Couloir. In the Tyndall area alone, there are at least eight well-established backcountry ski lines, and the variety is pretty spectacular. My goal, Tyndall Glacier, is one of the few alpine glaciers left in Colorado. There are a handful of them on the eastern slope of the northern Front Range, which is peculiar because the eastern side of the Front Range doesn’t get as much snow as the Western Slope. The glacier’s location can be explained by looking at the wind scouring that happens in this part of the state.

Quick weather PSA, for the full scoop, read this piece. Colorado winters are variable; storms roll in (very, very generally) from west to east. So, snow slams into the western slope first. However, the wind really kicks up over the northern Front Range. That wind, ruthless as it is, steals snow from the Western Slope and lobs it over the continental divide until it settles in high, cold, east, and north-facing alpine basins. These areas, consequently, have the most consistent snow. Colorado also isn’t as far north as people think, which means the sun factor is more critical. An eastern and northern aspect helps shield these areas from sun-melt. All of this is, of course, subject to climate change, but for now, these areas of snow and ice are the last vestiges of Colorado’s glacial history. Back during the last mini ice age, glaciers in Northern Colorado were huge and helped shape the gnarled-looking valleys of the Indian Peaks and RMNP. Estes Park and its world-famous rock climbing areas were carved out by advancing and retreating glaciers.

ANYWAY, Tyndall was one of a few left, and I kind of wanted to see them all, which of course led to a follow-up thought, “Hey, I wonder if you can ski any of them.” As evidenced by multiple trip reports, blogs, websites, and guidebooks, the answer to that is absofreakinglutely. Tyndall made sense because it was in the middle of a well-traveled and well-documented area, had a low avalanche rating due to snowpack consolidation and nightly freezes, was supposedly an enjoyable descent, and since I hit it early enough in the year, there was enough snow to take me from the top of the glacier on a more than a mile-long journey to the shores of Emerald Lake. (Quick aside: Tyndall Glacier slides every year, so a scouting trip is HIGHLY recommended before you commit.)

I found it astounding that this run even existed because if you’ve only been as far as Emerald Lake, you’d think the valley simply ended on the other side of the lake. You can’t see over the slope in front of you, so you assume it stops. In reality, there’s at least another mile of terrain between you and what’s left of the glacier.

The upper part of the gorge with a small tarn visible. The glacier is nestled up against the headwall (hard to see when most things are covered in snow).

So after a lot of grunting and sweating, I arrived at the base of the glacier and then faced the daunting task of climbing it. I had followed a set of previous skin tracks that ultimately broke up to Tyndall Couloir, so I approached the glaciers steeper south side (45-50 degrees). Armed with a trusty ice axe, crampons, and general mountain enthusiasm, I resolved to climb the steeper portion of the glacier and ski the mellower part.

Hallett Peak frames the southern side of the gorge rim.

This was a steep climb, made harder by the rising temperature and slushy snow. The biggest concern in spring is the idea of a wet avalanche, where the sun melts the top layers of snow, and they gradually sluff off the slope. Usually, if you have a good freeze overnight (which I did), you can get to the top of your line and ski it before the sun increases the wet slide risk. I made the timing work, but it was a bit later than I would’ve liked, with the slush making upward progress more difficult.

You can see my ascent tracks heading diagonally right to avoid the cornices up top.

By the time I reached the very top, I was down to shorts and a t-shirt. With added effort, I managed to crest the top, avoid the cornices, and take in the beauty of the alpine.

Looking northward around the rim of the gorge—the Mummy Range is in the background.

I took a little time to rest at the top and snap some photos of the surround. After some food, water, and a bit of stretching, I got ready to descend. The first set of turns I made were simple, just along the top of the glacier angling towards the mellower north side. I used those first turns to test my gear and then made necessary adjustments to my bindings before pouring into the gorge.

First few turns from the top of my climb.

Once I felt I had made all necessary adjustments, I swallowed a rapidly expanding bubble of anxiety (pretty common when you think about any crazy outdoor activity you’re about to do) and ripped into my descent. It went perfectly. The turns were soft but not too soft, and the snow held without sending me any wet avalanche signs.

Looking up to my ascent tracks (left) and where I skied down (hard to see my tracks through the darker patches).

Now, Tyndall Glacier descends into a formidable terrain trap. A terrain trap is simply a set of features preventing a continuous ski. In my case, the steeper side of the glacier bled into a large bowl rimmed by talus. If I skied the way gravity wanted me to, I’d end up in it, have to put my skis on my back, and hike out to the nearest continuous snow line. Well, all of that sounded awful, so about 2/3 of the way down, I made an abrupt left-hand turn and aimed for a 10-20 foot wide snow chute that offered the best chance for continuous skiing.

Slide the bar to see my marked-up ascent/descent routes.

Luckily, the little slot I’d chosen held just enough snow for me to ski through some chokepoints and continue unhindered. Turning the glacier into a continuous descent down the gorge was a game-changer and the only times I stopped were to take pictures, say “wow” under my breath, and, occasionally, catch my breath when I needed to.

Slushy turns.

At one point, I had to ski on one ski to fit through a section, and at another, lost all my momentum; but, after some sidestepping and huffing, I was able to keep connecting continuous snow-fields. I think another day or two after I went, and the snowmelt would’ve made that impossible.

The last part of the descent is interesting because you bulldoze into view of everyone down at Emerald Lake. You can’t hear them if you’re skiing and making turns, but boy, can they see you. I managed to make it all the way down to the shore and scooted around it until running into the crowds. I could feel eyes on me but only really began to field questions when I stowed all the gear that could be stowed, got out my hikers/crampons, and fastened my skis to my backpack.

Here’s a generalized drawing of the last part of the run down to Emerald Lake. I traded emails with a girl from Virginia who sent me this picture. It’s hard to see, but the skier in the circle is me.

All told, I skied more than a mile and dropped 2,300 feet over the course of my run, and I could not be happier. While conditions may have been better overall for April, skiing down an alpine cirque glacier in a National Park will always be a top memory for me. What a day, and to think I almost quit when I fell into Nymph Lake! Granted, my pruney and smelly feet had a lot to say about that choice, but I took a week and a half to lick my wounds before attacking my June ski.

From the top of the Glacier, looking down the gorge, Emerald Lake is hidden from view.

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Month 5: June 2, 2021 (Sundance Mt. North Face)

Longs Peak, seen from near the start of my ski line down Sundance Mountain.

Even though the summer solstice doesn’t occur until the end of June, you could tell that warm weather was on its way. After a wet and cool April-May, the heat was coming. Following an upper elevation snowstorm (11k and above), the weather forecast looked dry and sunny. I wanted to take advantage of a couple of things, ease of access, high altitude, and good weather. I came up with Sundance Mountain.

Trail Ridge Road is the primary road bisecting Rocky Mountain National Park and closes down over the winter. When it opens back up (around Memorial Day, weather permitting), there are still large snowfields left above treeline that the road gets very close to. One of those is Sundance Mountain’s north face. The year prior, I’d taken my parents through the park, and near the highest part of the road is a small trail to the Toll Memorial. It was on this trail that my dad and I noticed some skiers, and ever since, I thought that it would be the perfect early summer Colorado ski candidate. I was right.

Let’s get it.

Armed with a June plan and still high off my Tyndall Glacier descent, I finally committed to the ski all-year challenge and was eager to try some summer backcountry skiing. I had only skied in June once before, in 2019, the year A-Basin stayed open to July 4th. My friends and I skied on a few inches of fresh powder on June 23rd, which was my current record for latest season ski. While I wouldn’t break that with an early June ski, I was confident I’d find the snow.

June 23, 2019, A-Basin.

So, June 2 rolls around, and I bulldoze up the recently opened Trail Ridge Road to just beyond its highest point. I was the first car in the parking lot, and that’s always strange, especially with an area as popular as Trail Ridge, but I was thankful for the solitude as it allowed me to futz with my gear and take oodles of pictures of mountains.

The Mummy Range from the Toll Memorial Trail.

There are a couple of ways that you can ski Sundance Mountains North Face. The top of the run gives you more than 700 vertical feet of super easy 20-25 degrees slopes. This is where most people ski. When the slope narrows and steepens (to the tune of 45 degrees), most people find a stopping point, slap some skins on, and recycle the upper portion. Well, I’d just skied a glacier; there was no way I was going to let a juicy 45-degree slope go to waste.

So, I skied the upper portion on a cold morning and enjoyed the fresh crunch under my boots while making wide GS turns. As all the other reports I’d seen indicated, it was fairly obvious when the slope angle steepened past the point of many people’s comfort zone. And, while unfortunate to discuss, people have died on the lower portion of this particular run, so you really need to “know thyself” before making critical terrain choices.

The beautiful and effortless upper portion of Sundance.

Having said that, when I finally got a good look at the lower portion, I knew I had to ski it. I had years of experience and had skied similar slopes recently. I knew I could handle the slop angle and the conditions. So, when I passed the logical point of no return, I flashed a smile and began slicing my way down.

The snow didn’t really soften up until the bottom half, so I wouldn’t say it was the best day out for the type of snow surface encountered, but just like Tyndall, I surprised myself with how smooth my turns ended up being. Aside from one break to scout my line through the bottom section, I skied a 2,000-foot slope without stopping.

Yeah, it gets steep. The line ends at the foot of the large meadowy patch of snow at the bottom left.

By the time I reached a logical end-point, I collapsed into the snow and practiced breathing for a while. The run only took about 10-12 minutes, but that is a significant time for continuous skiing. Once I collected myself, I took a shot from the bottom-up.

Runs like Sundance North have obvious benefits. Since Trail Ridge climbs up beyond the start, you can be out of your car and skiing within a few minutes. However, if you want to ski the whole line, and unless you car positioned, you have to reclimb the slope. Needless to say, this bit took a lot longer than the skiing, but the temperature began to moderate, and it was nice to feel my muscles working. About halfway up, I was surprised by the presence of a Coyote. I stopped and watched him stick his nose in a Pika nest, pull one out and devour it. Nature is beautiful, but she can be cruel.

Who wants Pika for breakfast?

Eventually, the coyote noticed me and began to saunter off, but not before I grabbed a few more pictures. Even in a state like Colorado, where wildlife is abundant, it’s always so cool to see big animals roaming around.

Lookin good fella.

Seeing the coyote actually gave me a nice break, which I used to adjust the weight I was carrying and eventually make it back up to the starting point. For the bottom portion, I had to use my crampons and carry my skis, but after the Coyote sighting, the slope angle lessened enough for me to reapply skins. By the time I reached the top, at least a handful of other skiers were out and about enjoying the day. The gawking from the masses on the way back to my car was a bit much, but I shoved some earbuds in, smiled when someone looked at me and kept moving.

Sadly, only a week later, another skier died on the lower portion of Sundance, which by slope degree alone is easily a Black Diamond or Double Black Diamond run at any ski resort. I began wondering if the ease of access and gentle upper portion were fooling people into thinking they could do all of it. Was this slope only being advertised as beginner terrain? And by advertised, I mean by word of mouth, which is really how this stuff spreads.

This is the point of no return, or as close to it as I thought made sense to photograph. Once you pass that rock, you are committing to a steep and dangerous slope.

I don’t know; I guess hearing about another death in a year that had already killed more backcountry enthusiasts than any other in the last 50+ years made me wonder if those risks aren’t being communicated effectively enough. In reality, it’s just the top snowfield that can support those easier turns; once you commit to the bottom, you absolutely need to know what you’re doing. I hope that people are accurately conveying not only the rewards of backcountry but the risks as well; there are a lot of them.

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Month 6: July 25, 2021 (Andrews Glacier)

Andrews Glacier

After my early June ascent, I turned my attention to other outdoor opportunities.

  • I took on Hallett Peaks Chaos Couloir, a fantastic mixed climb up an iconic peak, on June 8th.
  • I scrambled across the Gorge Lakes Rim, which included Mt. Ida, Chief Cheley, Cracktop, and Mt. Julian on June 14th.
  • I scrambled up a Class 4 route on the Spearhead, one of the more vertigo-inducing summits in RMNP, on June 30.
  • I scrambled a Class 3+/4 route up Lead Mt. in the Never Summers, one of the true hidden-gems of the area and a bear to get to.
  • I also hiked a few area favorites with my wife and had a banner scrambling day on Horsetooth Peak, a little known Boulder County mountain with an outrageous Class 4 option that I thoroughly enjoyed.

I was having so much fun embracing summer that by the time the last week and a half of July rolled around, I realize I hadn’t gotten my July ski in yet! A quick bout of panic turned into an opportunity when I settled on a trip to Andrews Glacier.

Andrews is in Rocky Mountain National Park and a fairly popular place; however, since it’s on the way to Sky Pond (arguably the prettiest lake on the eastern side of the park), it tends to draw far fewer people.

My wife and I hiked in and had most of the trail to ourselves once we took the cutoff away from Sky Pond. I’m glad I had gotten all the hikes in that I did since Sundance, so my body could handle carrying skis for 4+ miles because there was zero snow up until the foot of the glacier.

As far as alpine glaciers are concerned, Andrews still shows signs of movement and is generally considered an active glacier (unlike other nearby pieces of snow like Moomaw Glacier, St. Marys Glacier, and Skyscraper Glacier). Throughout most of the summer, the snow reaches down to a beautiful tarn at its base. By mid-August, the glacier retreats to above the tarn, but when we arrived, there was still a twenty-foot snow connection to the shores of the lake, which made for a much more aesthetically pleasing descent.

Andrews is not a steep glacier and has a maximum pitch of maaaaaybe 33 degrees. Most of the run is in the high 20’s, making it easy to connect soft, satisfying turns all the way down.

The conditions were typical for the summer, with some firm patches on the way up, bowing to warm slush by the time I made it to the top and clipped in. Even still, I had a great time slicing down the slope and made a series of excellent turns. It’s not often you can say that you backcountry skied in Colorado on July 25th!

Perhaps the most unexpected part of the adventure was the sheer number of people who could not believe that I had actually found snow. For many, this was their first time in Rocky Mountain National Park, so they wore clear expressions of deep confusion when they saw a sweaty man with a pair of skis on his back passing them. Everyone was friendly, though, and on a beautiful summer day, it’s not hard to smile and field a couple of questions.

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Final Thoughts

With Andrews being such an easy ski (and a tough but manageable approach), I began thinking about the next three months, and a bit of worry crept in. I’d always heard that August and September can be the toughest months to ski in Colorado because even after a heavy previous winter, the snow is more or less gone (except for the 100 or so permanent snowfields left in the state), and the conditions on what’s left can be quite dangerous. And while the high peaks can see snowflakes any month of the year, skiable accumulations don’t really occur until mid-late October, which presented a bit of a logistical problem. I had to find two skiable candidates during the two driest months in the state….hurray.

So, despite my elation at making it this far into my challenge, I began to wonder how difficult the next couple of adventures would end up being… One thing was for certain, now that I’d committed, I’d be hunting snow in August, September, and October, no matter how hard it ended up being.

I hope you tune back to read the next part of this ongoing series!