Dylan works hard to keep pace with Ty as we skin up Spruce Peak.
By this morning, enough snow had accumulated that we decided to head up to the higher elevations and check it out. Without much of a base, we didn’t expect the skiing to be too great, but it would be a good chance for Dylan to get on his skins and see how everything was working for him.
We first stopped in up at Bolton Valley, where accumulations appeared to be in the 2-3 inch range at the main base (~2,100’). I took a look around to see if any manmade snow had been put down outside the areas of current snowmaking operations, but didn’t see any on the lower mountain. A good amount of snow had been made in the Mighty Mite learning area, a fan gun was blowing snow above the lodge, and I could see at least one other gun going underneath the Mid Mountain Chair. The snow was certainly light and dry, and the powder had accumulated up to a foot in some areas. We hung out for a bit and let the boys play in the snow, then we headed off to Stowe to see if any ski options were available atop manmade base snow at Spruce Peak.
As we drove toward Stowe, we could see that the valley snow accumulations were quite variable. We had an inch or two at our house on the Waterbury/Bolton line, and there was a bit less in the center of Waterbury. North of Colbyville however, the ground was bare, and between there and the Stowe’s Lower Village, there was only the occasional dusting visible on the ground. As Powderfreak had mentioned in one of his reports to Americanwx.com, we saw a sharp increase in snowfall amounts as one entered the center of Stowe, where they had picked up a fluffy few inches earlier in the morning.
Up at the mountain base, accumulations were similar to what we’d seen at Bolton, with roughly 2 to 3 inches on the ground at the Mt. Mansfield Ski Club building. We were surprised to see that lift-served skiing was going on over at Spruce (Easy Street area), so we decided to skin up above that elevation and check out the options. We headed up toward the Sunny Spruce Quad, and found about 4 to 5 inches of fluff as we approached the top of East Run. The snow was definitely fluffy, so good turns could be had on grassy slopes, but beyond that it was sketchy. It was definitely rock ski/junkboard territory, although with all of the extra snow we’ve had in the past couple of days, that will be changing. To continue with the rest of the text and see all the pictures, click through to the Stowe trip report from today.
Ty skiing some October snow on Perry Merrill at Stowe Mountain Resort
Even before the storm existed, the formation of the season’s first Nor’easter had appeared likely for several days, and with it, the appearance of at least a few flakes in the higher elevations of the Northeast seemed like a good bet. However, the question of the whether or not we’d see our first decent dump of skiable snow took a few more days to settle out. Eventually, the mountain forecasts came into focus, and it looked like the Greens were going to get good elevation snows up and down the spine. The Northern Greens seemed to be in a good spot for precipitation, but the Central and Southern Greens were likely to be closest to the core of cold air that would support the most early season snow. On Wednesday the 13th, Scott Braaten did a nice job of alerting everyone about the setup through SkiVT-L and Lionel Hutz was all over it at the FIS website.
On Friday, October 15th, the storm was underway, and morning reports were already coming in about snow falling in the Southern and Central Greens. The pictures from the Killington web cam were looking quite wintry even at the lower elevations, and when Paul Terwilliger sent in his Friday Killington trip report to SkiVT-L and said he’d already found 18 inches at the summit, it was clear that the area was getting a good shot of snow. By that point the temperatures indicated that the Northern Greens were getting plenty of snow as well, but if they weren’t going to catch up to the Killington area, I was thinking that it might be a good time to mix things up and head a bit south for turns.
My thoughts of heading south to Killington were suppressed somewhat around 8:30 P.M. that evening. After checking on our rain gauge a couple of hours earlier, I hadn’t looked outside at all, as a massive sword and ball battle had kept me busy in the basement with the boys. When I finally did look out back, I was very surprised to see that it was snowing… all the way down at our elevation of roughly 500 feet. The air temperature had dropped to 33.3 F and the precipitation was big flakes of snow, without even any rain mixed in. The snowfall lasted for a couple of hours, long enough to put down 0.3 inches of slushy accumulation on the snowboard and coat the ground white. Eventually as the precipitation slowed down, the temperature began to warm up and it all changed back over to rain. I knew that if we were getting snow all the way down to the lower valleys though, then the local mountains must have been getting pounded, so I suspected that Mt. Mansfield would come through with sufficient snow to make it worth skiing.
The next morning we had steady rain at the house, and valley temperatures in the low 40s F as Ty and I headed off to Stowe. The snow level had clearly risen up overnight, as we didn’t see any signs of snow at all until the slopes of Spruce Peak came into view. We headed to the base of the Gondola (~1,600’) which seemed to have the best accumulations of snow at low elevations. The temperature was in the upper 30 s F, and there was a gusty wind in the parking lot. Although a little thin, coverage was still enough that one could start skinning from the lot if they wanted, but we decided to hike for a bit to get some variety in the ascent. Snow depth at the bottom of Perry Merrill was 2-3 inches, but with the warming temperatures any disruptions in the snow were seeding its melting. The footprints of earlier hikers were already holes in the snow with colorful foliage showing through. To continue with the full text and all of the pictures, click through to the full trip report from today at Stowe.
Ty out there ripping up some of the powder on Bald Hill today
Saturday was another potentially good day for some backcountry skiing in Northern/Central Vermont, since snowfall had again been rather minimal in the area during the preceding week. At the house in Waterbury, we’d picked up just 1.4 inches of snow in the Sunday/Monday range from a storm that favored parts of Maine and Southern New Hampshire with up to a foot, and then 1.6 inches of snow in the Tuesday/Wednesday timeframe from an upper level low coming out of the Great Lakes. As for the mountains, I saw accumulations topping out in the 4 to 5 inch range for the Bolton through Sugarbush stretch, with amounts tapering off to the north. The forecast on Saturday called for a cold start in the 0 F range, but brilliant sunshine and eventual temperatures in the 20s F. Weather wise, it was an excellent time to get outside.
“The combination of settling and the thin breakable crust in some spots made things tricky at times, but it was all soft and fun.”
With the snowfall thoughts in mind, the plan was to do some skiing off the west side of the Camel’s Hump/Mt. Ethan Allen area. Unfortunately, on Friday we found out that Tom had tweaked his knee and ankle at soccer, so the ski group for the day was going to be just James, Ty, and myself. We met up with James in Huntington Center a bit after 9:00 A.M., and decided on an initial plan of heading up the Forest City Trail to do some skiing on the lower flanks of Mt. Ethan Allen (3,674’), the next prominent peak south of Camel’s Hump. We headed up Camel’s Hump Road, finding that the access to the Forest City trailhead was going to be difficult because the road there wasn’t plowed in the winter. There was a little room along the snowbank to potentially park a couple of cars, but a more important factor in our case was the added distance to get to the trailhead. Ty’s backcountry range is not that great yet, so we weren’t looking for a big approach. There was the option to connect over to the Forest City Trail from the Burrows Trailhead area, but we decided to just do something simple off the Burrows Trail. James had commented to me earlier that there was going to be a temperature inversion in effect, and that was indeed what we saw on our ascent of Camel’s Hump Road. From down in Huntington Center (690’) where the temperature was somewhere in the middle single digits, the temperature was up around 10-11 F at the trailhead parking area (~1,900’). The lot was about half full, and while we geared up, we could see that several parties of people were heading out for hikes on snowshoes.
Some of the powder stacked along the Burrows Trail
Starting up on the Burrows Trail, I checked the snowpack and found a couple inches of fluff on top of a generally thin crust, atop a lot more settled powder. A few of the lower elevation stream crossings on the trail were open with small gaps, and that represented a bit of a challenge for Ty, but he managed well. We didn’t have any lofty goals in mind other than getting in a little skiing, since our ultimate destination would likely be affected by Ty’s mood and stamina. Our pace was pretty slow with Ty taking his time, but it was an easy go, and everyone’s skins were working well on the packed trail. There were lots of dogs, lots of people on snowshoes (including a bigger group that seemed to be from the UVM Outing Club), and we also saw a party of about four skiers that passed us on their way up the trail. One of the more interesting sights was a woman coming down trail at breakneck speed on a sled that looked like a booster seat. We made sure to move out of her way, but she seemed to be very conscious of the uphill traffic and stopped easily. James inquired about how her sled worked, and she demonstrated that for braking, you just lean back. I know that people like to use those Mad River Rocket-style sleds on the trail and elsewhere, but this was the first time I’d seen what this woman had.
Ty and James ascend Bald Hill.
Up to about the 2,300’ elevation mark the surrounding vegetation was on the brushy side, but above that point it began to thin out and the potential for skiable lines looked a little better. Off to our right, we could see some open, moderate angle slopes across the big gully that had begun to parallel the trail, and off to the left we could see the more obvious lines that steepened on the way up to Bald Hill (3,041’). Ty had some good bursts of skinning speed when we kept him motivated, but as inquiries about how far we were going and when we would get to ski became more frequent, we decided it was time to think about our descent route. Heading off to the left for the lower slopes of Bald Hill was going to make things easiest for getting back to the trailhead for Ty, so a bit above 2,500’ when we hit one of the skin tracks breaking off the Burrows Trail and going in that direction, we took it. The change of scene was enough to keep Ty motivated for a little bit longer, since we were able to tell him that we’d be able to descend soon.
We headed up into the glades a little farther, reaching an elevation of about 2,700’ before Ty seemed to be getting just a bit too antsy. There were plenty of good lines available with untracked snow, but we could see that taking them would mean dropping right back down to the Burrows Trail almost immediately. So, we continued to contour westward to get something that might drop a little more directly to the trailhead. We could only traverse so far though, since Ty knew we were close to skiing and his inquiries started up again. When we finally called it on the traverse, James and I skinned up a little farther to catch a nice looking line, while Ty waited just below us.
Jay enjoys some turns in the beautiful powder out there on Bald Hill.
The skiing was good, and definitely worth the hike, but certainly not perfect or quite up to what I’d found off the Monroe Trail the previous weekend. The combination of settling and the thin breakable crust in some spots made things tricky at times, but it was all soft and fun. Ty stuck with just alpine turns, but had a lot of fun catching air and working on his jumping technique. Our extra traversing had bought us a little longer descent, but we still dropped back to the Burrows Trail pretty quickly. Instead of trying to ski on and near the trail, we took a traverse out to the west with the aim of eventually dropping back down to the parking lot to finish our run. I used the GPS for route finding, and as is often the case, James went by his natural sense of direction. The biggest issue with the traverse was that like on the Burrows Trail itself, a few streams were still open from the previous warm weather. They weren’t too hard to cross since there were still snow bridges around, but Ty’s smaller skis definitely set him at a disadvantage for spanning some gaps. We helped him across when needed. Even with the aid of the GPS, I overshot the parking area by about 100 feet or so and had to swing back during my final descent, while James nailed it right on.
The GPS tracking data from today’s ski tour plotted on Google Earth
Views of the glades along the Monroe Trail on Camel’s Hump
From what I’d been hearing, ski conditions were generally decent around the area this week, but new snowfall was sparse. Subsequent to the 9 inches of snow that Bolton picked up last weekend, they’d only reported 2 to 3 inches of additional accumulation. Down at the house in Waterbury (495’), we picked up 4.8 inches of snow from that weekend event, and then smaller events on Monday and Wednesday dropped 1.2 inches each. It was enough to keep things fresh, but it was rather dry snow that probably didn’t add too much new substance to the snowpack.
The end of the week also saw an increase in temperatures, with our location in the valley getting up to around 40 F at times. It was a little hard to get a sense of what had gone on with the weather in the mountains, since I heard talk of a crust in the Mt. Mansfield area, but Paul Terwilliger’s report from Central Vermont suggested that the powder was great down there. Unsure of whether I was going to encounter, powder, crust, mush, or who knows what, I chose to keep it simple and earn some turns close to home. I decided to check out some terrain right across the Winooski in North Duxbury below Camel’s Hump. From the Winooski Valley, at an elevation of about 400’ or so, the Camel’s Hump Road heads southward up into the mountains for several miles to an elevation of about 1,500’ where there is access to Camel’s Hump State Park and various hiking trails. My friend Weston used to live right up near the top of the road, and told me that there were plenty of glades up above him along the route to Camel’s Hump. I took a peek at my copy of David Goodman’s backcountry skiing book for Vermont, and he also speaks of the various glade skiing options along the Monroe Trail.
This was actually my first time driving up Camel’s Hump Road in the winter, so it was neat to get the perspective with the snow. The drive offered great views of Ridley Brook, which flows near the road throughout the drive. I always get a kick out of some of the funky houses along the road: some that seem to be accessed by unique bridges, and others with their own quirks, like one that seems to be some sort of partially underground structure with a flat roof. At this time of the year, the very top part of the road is closed, so I had to park in the winter parking area at ~1,200’. From a temperature of ~38-39 F down at the house, the temperature dropped to ~36 F at the parking area, and in terms of snow conditions, I hoped that the temperature would continue to drop as I ascended.
With skins on, I quickly made it up the rest of the snow-covered road to the main parking area and trailhead at around 1,500’. I checked out the plaque near the trailhead commemorating the 1944 bomber crash on the mountain, and then I was on my way up the trail. I began checking the consistency of the snow, and it seemed like the powder was dense, but not really wet, and there was no detectable crust. Within a few minutes of being on the Monroe Trail, I began to see obvious glades up above me as Weston had suggested. The Monroe Trail didn’t really attack the fall line, instead it seemed to gradually contour up and to the left in a southwesterly direction. I figured that one approach to skiing the glades would be to see if I could gain some elevation on the Monroe Trail and eventually traverse back in a northeasterly direction for a fall-line style descent back to the trail, but I wanted to see where the Monroe Trail would take me on its own before I started breaking snow on a new route. The trail was well packed, and plenty wide as David Goodman suggests in his book, so it’s really easy to cruise along with skins. I was happy to have full-width skins in a few spots where the trail gets steep, but one could certainly make due with less as long as the snow consistency supported good grip. There were a few ski tracks where skiers had come out of some of the glades, and tracks suggested that a few more folks seemed to have skied on and around the trail, but I didn’t see any skiers during my tour. I did see a lot of people on snowshoes: one group of 6 to 8 people, a few couples, and a couple of other groups.
The trail continued it’s mostly gradual, southwesterly ascent, and at around 1,800’ I noticed that the trees seemed to have more brush in them than I’d seen in the earlier part of the climb. At 2,300’ in elevation, I reached the junction of the Monroe and Dean Trails, and direction-wise, continuing on the Monroe Trail was the obvious choice for what I wanted to ski. The Monroe Trail had been starting to wrap around toward a more northwesterly direction, getting more in line with my efforts to eventually head to the northeast, while the Dean Trail headed southwest. Not far above the junction, the forest began to turn into a beautiful combination of birches and evergreens, and I could see some nice ski lines for folks that opted for the skiing in the trail area. Then, a little above the 2,500’ elevation mark, I hit the frost line and everything began to turn white, changing the look of things again. Ascending farther, the forest transformed back into more hardwoods again with some decent open ski lines paralleling the trail, and I could see that a few people had used them. Finally, as I approached the 2,800’ level, the trail was actually starting to almost make a north/northeasterly jog and far above I could see huge cliffs on the eastern face of Camel’s Hump directly ahead of me. The forest quickly transformed yet again into an area of almost exclusively evergreens.
Traversing through the higher elevations of Camel’s Hump
It was after 3:00 P.M. by that point, and as I didn’t want to push the available daylight, I began to look for the best route to traverse northeastward for my descent. I followed the Monroe Trail for as far as it seemed to jive with my plan, and when it really seemed to head southward I had to begin my traverse. I traversed north/northeastward among the evergreens, and down below the cliffs the trees were often quite open. If the snow was elevation-dependent, or if one wanted to simply stick in this terrain, I could easily see this area being used for some great laps of skiing. Indeed, I saw various tracks of previous skiers scattered around, suggest that folks had had some fun. As I made my traverse through the evergreen forest, I came across various tracks of people that had either been descending or ascending, but I eventually picked up a skin track that seemed to be very much in line with my plan. I followed the track through the evergreens until it broke back out into a lot of birches, crossing what looked like an interesting trail marked with blue flagging tape. That blue-flagged route looked intriguing, but it ran literally perpendicular to where I wanted to go, so I had to pass it by and chock it up to future exploration. I checked several times with my GPS compass to ensure that the track I was following was legitimate, and not something left over by somebody that had simply been lost, but it stayed on course.
After another couple of minutes of traveling through some flat, very open terrain, I noticed that the skier/rider before me had started to make a couple of turns, so I decided it was time to take of my skins and focus on the descent. I was excited about the skiing prospects, even if only due to the snow depths and consistency I’d see on the ascent. I had little idea about what I might find for slope continuity or vegetation below. In terms of snow quality, there had been no sign of a crust aside from a couple of isolated spots that had a thin coating that must have been from the sun. And, throughout the trip I’d been checking on snow depths, finding anywhere from 14 to 26 inches of settled powder atop the base snow.
Some of the ski terrain out there on the tour today
You don’t always know quite how snow is going to ski until you actually get on it, but as soon as I dropped that first knee into a turn all questions were answered. The powder was dense as expected, and I was only sinking in about 4 to 5 inches, but the density made the turns really smooth. I continued on with turns, checking my GPS every couple hundred vertical or so to ensure that I was on track to hit the glades near the start of the Monroe Trail. There were some steeper options off to my left (north) but with the tree spacing they would be best for deeper/lighter powder. I found the conditions perfect for the moderate and low angle slopes that I encountered. Ultimately, my descent was not as fall line as I was initially hoping for, and I really had to keep pulling left throughout the descent to stay on target, but I was pretty happy with it for a first shot. I occasionally saw a couple of other tracks in the area as our paths crisscrossed, so obviously some others (presumably at least that track I’d followed) had done something similar. As far as tree spacing went, it wasn’t a brush-fest, and there were a few more open areas, but nothing extraordinary relative to what I’ve seen around here for what appears to be nature taking its typical course. If one didn’t have to check on or correct their route, most competent tree skiers could enjoy a fairly continuous ride without having to constantly hit the brakes for brush. A couple more feet of base would help a little on the bush front, but not too much from what I could see, and it’s certainly not needed in terms of coverage. With the base snow plus all the settled powder, coverage was absolutely bomber on everything I found on my ascent. I was able to pop off small boulders etc. and never heard a thing from my skis. The most consistently open glades on my descent were the terrain I’d seen down near the Monroe Trail, and I actually still came up just shy of one of the shots I’d been aiming for. Looking at my GPS/Google Earth plot, I can see that a longer traverse up high would be needed for a more direct fall line descent, but that’s something to strive for in a future trip. It does remind me of a quote from David Goodman’s chapter on the Monroe Trail, where he says “The quest for the perfect glade run will keep you coming back to Camel’s Hump time and again…”
The GPS track of today’s tour on Camel’s Hump in the Monroe Trail area plotted on Google Earth
So, both the base and ski conditions in the Monroe Trail section of Camel’s Hump State Park were great as of yesterday at all elevations I skied off piste (1,500’ – 2,800’). We picked up 1.4 inches of snow from last night’s activity, so that area should have picked up something in the 1 to 3 inch range as well, and I can’t imagine that would be anything but a positive on top of the conditions I experienced.
Looking back at the resort trails today as I head up into the alpine
The boys were more interested in planting flowers with Mom on Saturday than skiing, so unfortunately I couldn’t interest them in going out for some turns. This meant that I was on a solo outing, but the upside was that I’d be able to do a much bigger tour than I would have been able to with Ty, or especially with Dylan. The skies were clear and blue all Saturday morning on what was likely our warmest day of the spring up to that point. The temperature was already around 80 F when I pulled into Stowe’s Midway lot (~1,700’) in the early afternoon, and with the forecast for temperatures in that range, I hadn’t been too optimistic about the snow quality. My major goal was to at least get in a good workout, so I was willing to negotiate some sloppy snow on the descent if that was the way it had to be.
Snow was available right from the Midway Lodge elevation, with just a couple hundred feet of fairly flat walking on grass to get on it from the parking lot. I was immediately surprised when I got on the snow and found that it wasn’t sloppy at all; it was all corn with just the top inch or so loosened up. That’s the sort of corn that seems to provide some of the easiest turns, so I was immediately enthusiastic about the potential for a quality descent. There wasn’t much of a breeze in the lower elevations, but the snow helped keep the air temperature a bit cooler and the ascent was very enjoyable. For ascent attire I’d gone about as minimally as I felt comfortable doing, with a short sleeve polypropylene T-shirt and my ski pants with the side zippers fully open, and that worked out to be a comfortable setup for the temperature. I hadn’t made a non-powder ascent on skins in a while, and I was quickly reminded how the lightness of Telemark gear allows you to simply fly up the slopes. Before I knew it I was up at the Cliff House (3,625’) and feeling great, so I decided to keep going up into the alpine.
I set my skis onto my pack and hit the climbing gully. There was a bit of rotten snow in spots, and as I didn’t immediately find a boot ladder, I had visions of an inefficient, sloppy climb with lots of post-holing. I’d already post-holed a few times in the outskirts of the gully (it only took one of those to remind me to get my ski pants zipped up at least halfway) but fortunately, about 50 feet up the climbing gully I found a boot ladder made by some nice big feet. That made the going fairly smooth, and the views of the Green and White Mountains continued to improve with each step. Near the top of the gully, I ran into a guy about to descend. He had spent an overnight or two on the mountain, and said that he’d been amazed to find fresh powder on Friday morning when he’d started skiing. It sounds like along with Thursday morning, Friday morning had also been good in the higher elevations with regard to fresh snow. The downside of the fresh snow was that conditions in the alpine were still a bit sloppy. The new snow had not yet cycled to corn in the highest elevations, so it just wasn’t going to provide an optimal surface. By the time I departed from my conversation in the gully, I was moments from the Mansfield ridge line. Up on the ridge I enjoyed the new westerly views of the Champlain Valley and Adirondacks, and decided to stop in at the top of The Chin (4,395’) since I was so close. There was a small group of college students enjoying the popular leeward side of the summit, and there was a pleasant breeze of probably 15 MPH or so. The high temperature for the day at the Mt. Mansfield Stake came in at 67 F, so I suspect that the summit maximum temperature was probably close to that. Getting an April day like that at the top of The Chin is certainly a treat.
For my descent, I wasn’t able to ski right in the summit or the West Chin area due to lack of snow, but I was able to ski down the gully where the Long Trail drops away from The Chin as it heads south. It was quite a perspective to see the snow create a flat surface through the gully, when in the off season it’s a 10-foot deep chasm containing the hiking trail. I had to remove my skis to descend the very top of the climbing gully, but below that point one could keep them on continuously. As expected, the new snow up high that hadn’t fully cycled to corn wasn’t as nice as the corn snow on the bottom 2,000’, but I actually had some fun turns in the climbing gully, and it let me work on Telemark turns in steeper, tighter confines. I still had to make some alpine turns and throw in some side slipping up there since some areas were just so tight, but overall the gully allowed a good mix of styles. The crème de la crème of snow surfaces for the day was probably the top half of the Gondolier descent. There must have been very little traffic up there because most of the snow surface was just a smooth layer of ripe corn. The lower half of Gondolier still had nice corn snow, but the surface wasn’t as smooth as the top half of trail. Perhaps the lower elevations had experienced more melting that started forming aberrations in the surface. Based on my GPS data, it looks like my descent was 2,720’, not quite what you can get for vertical in the winter when you head all the way back down to Route 108, but still a decent run. There were still about 7 feet of snow at the stake on Saturday, and even though that level has dropped some with the recent warmth we’ve had, skiing should available on Mt. Mansfield for a while.
A Google Earth/GPS map of today’s ski tour up to the Chin of Mt. Mansfield – Click the image for a full size map
Bolton is starting off this storm cycle with about a foot of powder to greet midweek visitors.
By the time I’d left the house (495’) at 7:30 A.M. this morning, we’d picked up 0.6 additional inches of snow since the 6:00 A.M. snowboard clearing, bringing the event total to 4.1 inches. It had been snowing lightly at the house when I left, but when I arrived up at the Bolton Valley Village area (2,100’) it was snowing moderately and still accumulating. The mountain had reported 7 inches of new snow as of their 6:45 A.M. update, but I suspected I’d find a bit more based on the way it was coming down. The lifts weren’t going to start loading until 9:00 A.M., so I kicked off the morning off by skinning for some turns, taking the route straight up Beech Seal. I first checked the consistency of the snow near the base area; I couldn’t quite make a snowball out of it in my hand, so I guess I’d describe it as medium weight powder. Beech Seal had been groomed at some point earlier, but I found about 2 to 4 inches of additional new snow on top of the groomed base.
“…today Spillway offered up some gorgeous steep powder.”
When I reached mid mountain (2,500’) I checked the depth of the powder in an undisturbed location and it came in right at 12 inches. That should represent the combination of powder from last week’s midweek system (~6 inches) as well as whatever had come down up to that point with this new event, so that seemed reasonable. Wind doesn’t appear to have been much a factor with this system, so getting measurements was easy. I was thinking of skinning up in the Cobrass area, but there was enough powder to keep me following one of the snowmobile tracks for my ascent. At about 9:00 A.M. I’d reached the top of Vermont 200 (~3,000’), and when I checked the depth of the new snow there I found that it was at 9 inches.
“It was really nice to see all the visitors getting rewarded with such a splendid day on the slopes.”
I enjoyed first tracks down Vermont 200, and this new round of snow had settled in nicely. The medium-density powder was just what the doctor had ordered in terms of getting the windswept steeps back into shape. I was on my Telemark skis, and found that the consistency of the snow made for really easy turns. After my initial descent I stayed around for some rides on the lift, and unquestionably the trail pick of the day for me was Spillway. Usually I avoid it like the plague between its man-made snow, exposure to the wind, and traffic, but today Spillway offered up some gorgeous steep powder. The fact that it has seen grooming in the past made the subsurface the most consistent and provided lots of nice bottomless turns, and since there didn’t appear to be much wind with this event, there were no issues on that front. I had to hit it twice because it was so good, and I’d say it was better than even Hard Luck or Vermont 200. The Wilderness Lift opened right around 10:00 A.M., and I was fortunate to catch one of the first few chairs. The way the steeper trails had been skiing so nicely, I opted for Bolton Outlaw from the Wilderness Summit, and it was in great shape. After that descent I traversed back toward the main mountain. I followed a random set of tracks off New Sherman’s Pass and found a nice region of glades that I’d never explored before.
Things were looking great on Bolton Outlaw today
The mountain definitely had more than its usual midweek handful of people this morning. A lot of the extra folks I saw were children, and I think some of the schools in the Northeast have vacation right now because I heard what sounded like a Boston-style accent on a couple of occasions. It was really nice to see all the visitors getting rewarded with such a splendid day on the slopes.
The moderate snowfall had gradually tapered off through the morning, and when I left the mountain around 10:40 A.M. there was just light snow and the temperature at my car (~2,100’) was 34 F. The temperature stayed fairly stable through most of the descent down the Bolton Valley Access Road, but at the bottom (340’) it was up to 35 F. The precipitation was light snow as I drove westward through the Winooski Valley to the center of Richmond. The temperature there was up to 36 F however, and I was surprised to see that Richmond appeared to have picked up little if any snow from this event. When I’d reached the I-89 rest area in Williston, the temperature was up to 37 F and the precipitation was over to rain, which was coming down at moderate intensity for a while. In the South Burlington area the temperature was up to 38 F, and when I finally arrived at the UVM campus it had hit 39 F.
Bolton Valley was officially reporting 8 inches from this event as of their 10:05 A.M. update, so I don’t think we’ll have any trouble getting into Scott’s 10-20” inch prediction range with some upslope. It sounds like this is one of the best upslope setups we’ve seen this season, so it should be fun to see how it plays out for the mountains and even the mountain valleys over the next couple of days. It’s expected to start up tonight so I’ll certainly report on whatever makes it down to our elevation in Waterbury. Images from today can be found in the gallery below, and full size versions are also available in the report to SkiVT-L from today.
Today I headed out for some backcountry exploration in the Bolton area. I was sure that James would still be resting his ankle, so once again I made it a solo outing. After exploring part of the Cotton Brook drainage the previous week, I decided to switch it up and check out something on the other side of the valley. A convenient starting area for reaching the terrain on the western side of the valley is one of the VAST (Vermont Association of Snow Travelers) access points. The ample parking lot sits at an elevation of roughly 1,000 feet on the Bolton Valley Access Road. My plan was to start out on the VAST trail that heads west from the parking area, and make my way up to the ridge line that extends north from Stimson Mountain. The summit of Stimson Mountain is at 2,002 feet, and the ridge maintains roughly that elevation for several miles as it heads northward toward the Bolton Mountain area. If I was able to find a suitable route to the ridge, and the terrain was appropriate, the tour would provide about 1,000 vertical feet of skiing.
I arrived at the trailhead in late morning to sunny skies and a temperature of 19 degrees F. There was only one snowmobile trailer in the lot at that time, so the lot looked pretty deserted. I started skinning westward on the nicely maintained VAST trail, which at first had a fairly gradual slope. Then, I crossed a large bridge, and the trail steepened. After maybe 50-100 vertical feet, the trail flattened out and turned to the south. At that point I decided to break away from the VAST trail and head westward up the ridge. The going would be slower once I had to get off the trail and break my own way through the powder, but as far as I could tell without a VAST map, the VAST trail headed more southward and was not going to get me up the ridge where I wanted to be. I finally broke off the VAST trail at the intersection with an old logging road. There was a sign indicating that the logging road was not open for VAST travel.
Despite breaking my own trail, the going was pretty smooth. I’d checked the depth of the powder just after I started my hike, and found it to be 9 inches over whatever thicker layer was below it. At the bottom of the logging road, the snow was still in the 9-12-inch range, so I wasn’t bogged down by too much depth. I continued upward, following a network of logging roads and taking the route that seemed to best direct me toward my destination on the ridge. I spied plenty of great ski lines along the way, and I marked a few of the more attractive ones on my GPS. The logging road seemed to have been maintained and it made for quick travel; at least it appeared that way with the snowpack at the time. If there was a forest of saplings growing on the road, they were long buried under the snowpack. There was only one obstacle that forced me to detour from the logging roads, a huge tree that lay across the trail near the middle of the hike. It took a few extra minutes to work my way around that one. Currently, with the additional 3 to 4 feet of new snow from Wednesday’s storm, that tree is probably not even an issue.
My route took me generally westward up the ridge, with a bit of northward movement toward the end. About 2/3 of the way through the hike, I came across a large flat area, and above it was some of the steepest terrain I’d seen on the day. The terrain there actually looked a bit too steep and rocky for skiing, so the slight northward trend worked well to keep me in more skiable terrain. Near the top of the hike I attained nice views of the Timberline area across the valley. I could even hear the announcer for the ski race that was taking place over there. The race was presumably a continuation of the event that Ty and I had seen the previous day. High clouds had been building in throughout my trip, so at that point the sunshine was no longer as brilliant as it had been when I started the hike.
After several minutes of additional climbing, I finally hit the ridge. While the powder just below the ridge had built up to a depth of around 15 inches, on the ridge itself, the snow was heavily compacted and drifted. In some places, the snow had been scoured down to just a few inches in depth. Small trees all across the ridgeline had been bent over and snapped by the strong prevailing winds that raked the area. To the west below me was Bolton Notch, and I could see what looked like some skiable lines dropping eastward toward the Bolton Notch Road. I actually thought I heard the voices of a couple of people below me in the notch, but it was very faint and I couldn’t get a fix on their location. I hiked around the summit ridge for a bit while I had a snack and a drink, then removed my skins and started down.
To ensure that I’d be able to get right back to the car without having to do any hiking along the access road, I followed a downhill route in the same general area as my skin track. Sometimes I traversed out above my skin track and skied back down to it, but for much of the run I was able to stay off to the skier’s left of my skin track and follow the natural contour of the terrain. Even with the snowpack below average (as gauged by the snow depth at the stake on Mt. Mansfield being at only ~54 inches), one could pretty much ski anywhere in the area I explored. There were always some lines that seemed to be the pick of the crop, but there were few areas where the vegetation was too thick for turns. There was plenty of powder for bottomless turns throughout the descent, and the depth of the base let me tackle the lines with a fair degree of confidence. With the potential for 3 to 4 feet of snow from the storm this coming Wednesday, I suspect there will be even more wide open lines. A storm of the size expected would likely bring the snow depth at the Mt. Mansfield stake close to 80 inches, which would actually be above average for this time of year.
For the final pitch down to the VAST trail, I actually skied the last part of the logging road I’d ascended. It was steep enough that it made for some pretty nice turns. The Avocet recorded 920 vertical feet of descent and the Suunto recorded 958 vertical feet of descent, a difference of 4.0%. The high clouds had continued to build in throughout the tour, so the temperature at the end of my run was pretty much the same as it had been when I started skinning. It was a fun and easy trip with great access.
Jay enjoying some powder during today’s ski tour on Gilpin Mountain after Jay Peak recently received 2 1/2 feet of new snow
For years I’ve driven along Route 242 to get to Jay Peak, often remarking about the intriguing ski terrain that dropped to the road from both sides. This was always on the way to ski the resort of course, and thoughts of exploring those backcountry goodies had to wait. Since Jay Peak had received 2 ½ feet of new snow in the past few days (much more than anyone else locally for us), and it was a holiday weekend, I decided it was time to explore the goods off Route 242. This realization came to me on Friday morning when I awoke, and I soon sent out a secret message to a local band of agents informing them of a Mission Impossible. This mission, which James, Erica, and Dave chose to accept, wasn’t really all that impossible, it was more just unknown. Mission Impossible sounded fun though.
A topographic map of the Gilpin Mountain area showing Route 242 (gray) and the approximate ascent (thick blue line) and descent (thick white line) routes used during today’s ski tour
At the crest of Route 242 (elevation ~2,250′), The Long Trail crosses the road, and along with the trailhead there’s a parking area (see the red dot at the lower left corner of the topographic map provided with this report), so this appeared to be a good place to start a hike. My initial plan was to head south along The Long Trail (note on the map where the gray-dashed Long Trail heads south from the red dot) toward Domeys Dome (elevation 2,913’ – not visible on map) and ski down from there to Route 242 where we would have a second car waiting (elevation ~1,500′ – off the map to the south). This would provide a roughly 1,400′ vertical run, with a calculated pitch of around 23 degrees.
When we actually arrived to surveil the area though, we discovered that what looked good on paper didn’t look as enticing in real life. The parking at the bottom was quite far away, and the slope leveled out too quickly to a very low angle. In 10 degree temperatures and brisk winds, we gathered together in one of our cars at the top of Route 242 and consulted the maps for new guidance.
We decided to drive the car along Route 242 to the northeast (in the direction of the Jay Peak base area) as the road descended toward the resort, while we looked for potential ski lines. There were plenty of lines off to our right, as well as a second parking area for cars (yellow dot on the map) at the next low point of Route 242 (elevation ~1,950′). This setup seemed almost too perfect. I say “almost”, because unfortunately The Long Trail doesn’t go in that direction at all, and we assumed we’d have to blaze our own path through deep powder to get to where we wanted to go. We had seen what appeared to be a trail heading off in the direction we wanted, very wide (10 feet or so on average), but we were still unsure if it would work for us. As we got closer, we could see that someone already had a skin track heading that way; we’d found our hiking route.
From the top of Route 242, we got our gear together, threw on our snowshoes, and headed out along the trail (our ascent route is roughly marked by the thick blue line on the map). The image of the group heading out shows the general look of the terrain at the start of the trail. I soon noticed from the blazes that this was The Catamount Trail (the HUGE cross-country ski trail that travels the whole length of the state). The upward slope of the trail was very slight, but as we continued on our ascent, Route 242 quickly fell away to our left and we could watch the vertical drop for our potential ski run grow rapidly. At an elevation of around 2,400′, we broke uphill of The Catamount Trail (following the switchbacks of another skin track) to gain some additional vertical. It turned out that other folks had been in the area today, as shown by the skin tracks, ski tracks, and the people themselves. We continued to hike up to around the 2,600′ mark, and then as the slope started to mellow out, we decided to boot up and test out the terrain. A group of about five Telemark skiers passed by on their way up, one of them deciding to cash in at that point and start his descent as well.
Dave slices his way through some branches as he encounters a brushy area on one of our ski runs.
It’s amazing to think that last weekend had been a situation of rain, warm temperatures, and a refreeze that turned the entire snowpack into a solid, crusty mess. From where we were standing, it was basically bottomless powder, a situation in which removal of snowshoes or skis meant trouble standing. The pitch of our descent started off mellow, with various areas of hardwood glades and some underbrush at times. The snow was nice and light; I’d estimate its density at somewhere in the 5-7% H2O range. The slope gradually got steeper as we picked lines along the way that looked good and headed in the general direction of our lower shuttle vehicle. Our general descent route is marked by the thick white line on the map. Even with the deep snow, some areas had enough underbrush that they made picking lines difficult. Some areas we quite clear, but a bit of scouting was needed to find them. James picked direction with his usual finesse, and guided us right down to the parking area and our waiting vehicle (Dave’s pickup truck).
A scene from the lower parking area on Route 242 where many people finished off their ski runs, with skiers of all types constantly coming and going
Our total vertical skied was approximately 700 feet, which was a nice run for only about 400 vertical feet of very easy hiking. At the parking area it felt like the local version of Grand Central Station for backcountry skiing. There were numerous cars, lots of people hanging out, and skiers pouring down off of both sides of the road enjoying the powder. James said it felt like a local backcountry Mecca (in reference to the number of people). Although a few of the people were from our side of the road, most came down from the Jay Peak side, riding the lifts and then catching a beautiful long run all the way down to Route 242. Some people had cars waiting for them, some hitched rides, and some looked like they had no idea where they were. It was an awesome scene to see though, with all those folks out there enjoying the snow. I’m thankful we weren’t skiing the other side of the road though (the Jay Peak side), as the number of skiers on those slopes had even that vast amount of terrain tracked up quite well. I had always thought of heading that way when skiing Jay Peak, and had no idea how many people did it. There was a continuous flux of people coming through that area all day long, with cars pulling in, parking, leaving, people looking for rides, giving rides, looking for people that they had lost, etc. etc. etc.
Catching a ride back up to the top of the pass in the back of Dave’s pickup truck
Using our vehicles, we shuttled our crew up to the top of the pass, and started for another run from the upper parking area. Unlike the lower parking area, there were only a few cars there, and no people. The wind was blowing and the temperature had stayed around 10 degrees the whole day, but the sun had come out for a while during our first trek, and it had made that a great hike. We had a snack in the car, and headed off along The Catamount Trail for round two. Our first run had tuned us into the lay of the land its terrain nuances even better, and now James had plans for some even sweeter lines. We hiked the same general route (much easier at this point with the presences of our tracks and those of numerous others who had been up). We cut upward off The Catamount Trail a bit earlier, and topped off near the same elevation as before. This time we found some lines that were even more open, although we did still had to pass through some brushy sections.
James helping out with some footage for our crash reel!
I’m not sure how good the ski touring in this area would be with low snowpack, since even with four feet of base, there was still brush in some areas, but it was certainly good skiing with our usual midwinter base depths. Some of the most fun we had was due to spectacular falls, with all four of us getting in on the act by diving into the powder. We shot about 30 minutes of video, hopefully enough to have a segment in this year’s ski movie. We’ll have to see, but either way, we got some of our best falls for this season’s crash reel! 🙂
