E and I headed out to Stowe yesterday for the school program training session, wondering what we were going to experience in terms of weather. Happily, the first flakes appeared just after we arrived at around 8:00 A.M., the snowfall quickly ramped up in intensity, and then it dumped hard all morning and into the afternoon to make for great riding conditions.
Stan Biasini fills us in on how teach novice snowboarders at Stowe, Vermont.
This year we both decided to go with the snowboard training session, since out of necessity E seems to spend most of her time boarding instead of skiing, and it would supply me with some additional tools to serve as an alternate snowboarding coach when needed. We joined up with Stan Biasini’s group, since he would be advising everyone on how to work with the students that were early in their snowboard progression. We started out with techniques for the “never evers” at the Magic Carpet, then stepped it up to Inspiration, followed by the Alpine Double, and finally the Sunny Spruce Quad. We got a raft of good teaching techniques, and Stan made ample time to ensure that everyone got plenty of their own instruction as well. I learned that Stowe no longer requires leashes for snowboards, and that the slope of the Inspiration trail is an impressively consistent 8% grade for teaching. Continue reading the text and see all the pictures by going to the full trip report from Stowe today.
The morning’s outdoor adventures got started right on the ascent of the Bolton Valley access road. Once we got up to the big steep S-curve pitch at around 1,200’, we could see that traffic was stopped. It turned out that a couple of cars were struggling with the ascent. The road didn’t seem that bad from our perspective, but I later heard some comments suggesting that it wasn’t prepared as well as usual. In any event, the benefits of 4WD/AWD were obvious, not just for getting up the slick road, but having the ability to start right back up and get going from a dead stop on a steep slope. I met Stephen right in the parking lot as he was getting out of his car, and we made plans to meet up later.
While I was parking the car, the boys had warmed up on the Mighty Mite, and then I brought E and the boys right over to Wilderness based on my experiences from the previous day. I knew that the fresh snow and moderate pitch over there would be great for E to work on here Telemark turns off the groomed. In places that had seen some traffic, we found about 4 inches of new, but there were still spots that hadn’t been touched on Friday and had a good foot of powder. To check out the rest of the story and see the pictures, click through to the full report from today at Bolton Valley.
Some nice powder turns were made at Bolton Valley this morning.
This morning I headed up to Bolton to catch some opening day turns and check out the four feet of new snow they’d picked up over the week. On the way up I could see that Timberline was just loaded with tracks from all the folks that had been earning turns there. We’d had our coldest temperatures of the season this morning, and although it was still somewhere in the single digits when I arrived at the mountain, the wind was calm and it turned out to be very comfortable.
They had the usual early season options going, but also some natural snow terrain such as the lower part of Wilderness. I saw that VT 200 was open at the top, but it still looked somewhat bony. I found that Wilderness and the routes over there were the places to be though, one could get some nice steeper turns in about a foot or so of powder in the junction areas of Swing, Lower Crossover, and Work Road, and then down on the Wilderness lift line it was mellow powder cruising. To check out the rest of the details and see all the pictures from the day, head to the full Bolton Valley Trip Report from today.
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.
We found lots of options for great turns on Mt. Washington’s snowfield’s this weekend.
The Mount Washington Auto Road was finally open for business by the weekend of May 22nd – 23rd, but since E was out of town, Memorial Day weekend was our first opportunity for a ski trip. As always, weather was an important determinant in whether or not we would try to take the boys up the mountain, but as the weekend grew closer, the good forecasts continued to hold. None of the days looked like a total washout, but Saturday looked like the best bet since the NWS point forecast indicated the chance for gusts as high as 100 MPH in the higher elevations of the Presidential Range on Sunday, and Monday had higher potential for precipitation. On Friday evening we put ice packs in the freezer, charged batteries, and planned to make a final check on the forecast in the morning.
Saturday morning’s forecast still looked decent; there was a chance of precipitation in the afternoon, but winds were expected to be low with comfortable temperatures. I reserved a campsite for Saturday night, and we spent most of the morning getting things together for the trip and taking care of other stuff around the house. We finally headed out in the late morning under mostly cloudy skies, but no signs of precipitation.
Once we’d reached the base of the Mount Washington Auto Road, we stopped in at the Great Glen Lodge to hit the restrooms and check on the summit weather. We were excited to see that the summit weather board indicated winds of just 4 to 12 MPH and a temperature of 50 F. Even better though, was being able to look up toward the higher elevations to the west to see blue skies. Last year’s trip featured 50 MPH winds and fog, conditions that were more amenable to playing in the strong gusts on the deck of the observatory than skiing with the boys. From our views along Routes 2 and 16, the snow up high looked less plentiful than we’ve often seen at this time of year. The level of the snowpack was potentially due to at least a couple of factors. Although there were some nice snowy storms in April and May, too many of the midwinter storms skirted off to the south of Northern New England this season, and more recently we’d seen warm, or even hot, dry weather with lots of sun. One never really knows quite what the snow situation is going to be until they get up on the mountain though, and based on the Mt. Washington web cam images, we knew there was going to be plenty of terrain to ski.
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The fair weather made for an enjoyable drive up the Auto Road, and the views were stupendous as usual. We stopped in just briefly at the summit, and got an overview of the various eastern snowfields on the drive back down the road. We could see that there were plenty of options, and continued our drive down to the parking area below Ball Crag where we’d based ourselves before.
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Consistent with the faster depletion of the snow this season, although potentially due to seasonal variability as well, the snowfield that we’d skied with the boys in May of 2008 was absent. But, based on the boy’s enthusiasm, along with their improved endurance and ski abilities, we were looking to hit some different snowfields this season anyway. The plan was to head up the Nelson Crag Trail for a bit as we’d done on our last ski trip to the area, and then traverse generally southward below Ball Crag to search out some snowfields that would work well for everyone.
Our equipment setup from our last Mount Washington ski trip had worked well, so we used a similar configuration with just a couple of changes. I carried the big SLR in my photo/ski pack, which is also set up well to carry multiple pairs of skis, so I carried mine as well as the boy’s. E and I simply hiked in our Telemark boots, but since the boys would be skiing in alpine ski boots, they wore their hiking boots to make their traveling much easier, and along with her skis, E carried their ski boots in her pack. The boys had their poles for hiking, and a new addition this time was that they carried their water, food, clothing, and helmets in/on their packs.
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We hiked roughly two tenths of a mile up the Nelson Crag trail before breaking off and contouring southward. The boys were very mobile in their hiking boots and light packs, and they moved along at a great pace. Compared to our last ski outing on Mount Washington, Ty was much more comfortable traveling through the alpine setting; he was well ahead of the rest of the group and opted for a much higher traverse. I knew that we would eventually run into the main portion of the east snowfield if we didn’t run into any other snowfields first, but there turned out to be earlier options. Ty was the first to spot some of the bigger snowfields below us along the Upper portion of the Huntington Ravine Trail, and we planned to work our way toward those after seeing what we found ahead of us. After only about a tenth of a mile of traversing, we hit a small snowfield, and the group, which had become a bit scattered during the traverse, got back together to start the descent.
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That first snowfield was moderately steep, perhaps in the 30 degree range or so. Since it was steep and rather short, the boys decided to wait until one of the bigger snowfields to start skiing. They opted to simply do some sliding on the snow. E and I mentioned that it was likely to be easier to ski than slide since they would have edges to control their descent, but they were having fun. E and I skied the snowfield, and then we all traversed over to a much larger snowfield off to the north. When we’d arrived at the initial snowfield, there had been a couple of people skiing laps on the edge of the larger snowfield below, but by the time we got there they were gone, and we had the whole thing to ourselves. In fact, they were the only people we’d seen on any of the snowfields in that area. We were surprised by the lack of people since it was Memorial Day weekend, but perhaps everyone had already done their skiing the previous weekend. The weather continued to feature interludes of sunny and cloudy periods, and although we’d seen what looked like thicker clouds and showers off to the Green Mountains in the west, no precipitation materialized in our area.
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Ty and Dylan were the first to ski the larger snowfield, and it was fun to watch Dylan follow Ty through the terrain. The snowfield wasn’t quite as steep as the first one, and it was a fun experience for the boys to have the whole face to themselves with the ability to decide what route they wanted to take. The boys stopped about 2/3 of the way through the descent to wait for us, then E joined them, and I skied all the way to the bottom to get some pictures from below.
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From the bottom of that snowfield we traversed north and slightly upward to another snowfield section that was connected to the first. At that point we were on the long collection of snowfields that sits above Huntington Ravine. The next section of snow didn’t provide quite as much vertical drop, but it didn’t seem like it had seen any skier traffic in quite a while, so it was extremely smooth. I made a boot ladder that was spaced well for the boys, and we hiked up to the top of that section. The boys had been happy with their earlier turns, and were most excited to play on the rocks and stairs of the Huntington Ravine Trail, so they switched back to their hiking boots and played around while E and I did a bit more skiing. Those turns were a lot of fun, and E got the time she’d been looking for that let her practice and dial in some smoother Telemark turns.
I hadn’t really been following the recent freeze thaw cycles up on Mt. Washington prior to our outing, but looking back at the Mount Washington summit weather archive, it says that the lows for the two nights before our trip were only down to 35 F, and the nights prior to that were even warmer. Apparently, once the corn is formed, it doesn’t necessarily matter if the temperatures go below freezing nightly or not in terms of maintaining quality conditions for spring skiing. We never encountered sticky, rotten, or mushy snow, just good corn with a peel away layer on the surface. I’m sure it would have been much less enjoyable for the boys if the snow had been difficult, but thinking back, I can’t recall any really tough snow in our Mount Washington outings at this time of year. Perhaps the snowpack is dense enough by this point in the season that freezing cycles aren’t as critical.
It was only a few minutes of hiking to get back to the car from there, and it really had been an efficient outing; for all the skiing we’d done, it had only required about ¾ of a mile worth of total travel. Although I’m sure Dylan was a bit tired, both boys were still bounding around on the final leg back to the car, so the distance had clearly been good for them. Just as we were about finished changing clothes and packing the gear back into the car, one of the Auto Road vans came by and let us know that he was the last one heading down. It was just about 6:00 P.M. by that point. We didn’t dawdle on the way down so that we wouldn’t hold up the final van, but there were plenty of people still out of their cars below us as we passed by, and even a pair of hikers just below our parking area that seemed to be making their final descent via the road.
After an enjoyable Auto Road descent with more fun views, we headed over to Shelburne, NH and checked in at White Birches Camping Park. We’d reserved a grassy site, and they’ve got some nice ones right on the edge of an evergreen forested area that contains access to the Shelburne Basin Trails. The evening’s burgers were some of the best in a while, and there were no complaints from me when Ty couldn’t quite polish his off burger or sausage.
In the morning, we had some breakfast and broke camp, then the boys went off with E for a while to go swimming and play on the campground’s equipment while I worked on repacking the gear. The weather was still nice, so we decided to take a circuitous route home and see some sights. We headed back to Gorham, then north along the Androscoggin through Berlin, past Umbagog Lake, and up to Lake Aziscohos. North of Berlin, we were certainly in the land of lakes, loons and logs; houses seemed just as likely to have a loaded logging truck in their yard as anything else. Between the abundance of big rivers, dams, and lakes, it’s quite a water paradise. We saw several groups of flat water and whitewater boats, and lots of fly fishing taking place. At Aziscohos we were getting close to the Saddleback/Sugarloaf zone, although we didn’t head quite that far into Maine.
After lunch at the picnic area on the south shore of Aziscohos, we headed west through Dixville Notch and got to take in its impressive craggy views. We also stopped in to check out The Balsams Resort Hotel and The Balsams Wilderness Ski Area, which we’d never visited before. The ski area isn’t huge, offering just over 1,000 feet of vertical, but from everything I’ve heard, it’s very much the type of ski area we enjoy. Akin to some of our favorite local ski areas like Lost Trail Powder Mountain in Montana and Bolton Valley in Vermont, it’s got low skier traffic, low speed lifts to keep it that way, and decent snowfall. Wilderness doesn’t quite get the 300+ inches of annual snowfall that Bolton and Lost Trail do, but knowing the snow trends for northernmost New Hampshire, I suspect they do decently on snow preservation like Saddleback and Sugarloaf. Based on an article I found by David Shedd on easternslopes.com[SJ2] , it sounds like minimal skier traffic helps out in maintaining the powder and general snow quality as well. The 1,000 feet of vertical at Wilderness is said to be nicely sustained, with no runouts, and that was definitely the impression we had when we drove to the bottom of the lifts and looked around. E and I have been thinking it would be nice to do a ski trip coupling Wilderness, Saddleback, and Sugarloaf together. Of the three areas, we’ve only been to Sugarloaf, and only in the spring. It’s usually hard to leave Northern Vermont’s snow during the middle of the ski season, but a good time to go east would be when one of those storm cycles comes through that focuses on Northern New Hampshire and Western Maine.
We got back into Vermont in the far northeast part of the Kingdom, and took the northerly route to I-91 along the Canadian border past Wallace Pond. It’s not a huge body of water, and it was fun pointing out to the boys that the houses just a couple hundred yards away on the other side of it were actually in Canada. We also passed Great Averill Pond, Norton Pond, and finally Seymour Lake, where we stopped for a few minutes. We went through Derby, but didn’t quite get up to Derby Line to show the boys how the library/opera house is split by the international border. At some point we will have to get them up there. Once on I-91, we were pretty quickly back in our own neck of the woods, and I’d say one of the more surprising things that we discovered was how close Balsams Wilderness Ski Area is to our location. Being so far north in New Hampshire, and mentioned so infrequently, it seemed to be on another planet. But, barring horrible road conditions, it should only be two to three hours from Waterbury. After our visit to the area, it has certainly moved up higher on my hit list.
Below I’ve added a web cam image of the east side of Mt. Washington from last weekend, showing the various areas of snow that were present at the time. The longest runs up near the summit still seemed to be off the main east snowfield that we didn’t visit. We haven’t had any of the hot temperatures that we had the week before our visit, and things have been much more seasonable, so there should still be some decent easy access skiing up there at this point.
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 down Stowe's Hayride ski trail at the fresh October snow and brilliant fall foliage
For quite a while, the local weather gurus had been talking about the potential for local snow at the end of September/beginning of October. Yesterday, reports started coming in of white in the mountains, and from UVM I could see the tendrils of snowfall crashing out along the Green Mountain spine. It was looking like this morning would feature some real accumulations of snow, but yesterday evening the snowfall seemed to come to a halt. I started to reconsider my thoughts of taking a morning trip up to Mt. Mansfield, but sometime after dark I checked the local radar and it looked like snowfall was blooming again. I awoke this morning to see that there were still echoes on the radar, the temperature at the house was ~41 F, and our back deck was wet. I suspected there had been some additional snow on Mansfield, so I hopped in the car and decided that I’d at least go for a hike before work.
While I couldn’t see much white at all on my drive to the mountain, as I finally got close to Mt. Mansfield, I could see that there was a good covering of snow from about the middle elevations of Spruce Peak on up. I parked in the upper lot of the gondola (~1,600’) and there were a half dozen cars that looked like they could belong to other early morning folks checking out the snow. Snow was falling all around me, and while it wasn’t sticking at the base, I could see white on the ground not far above. At some point after 7:30 A.M., I strapped my skis on my pack and headed up Nosedive, hitting the snow line right around 1,800’. The depth of the snow didn’t increase too quickly, only up to maybe ½ to 1 inch in depth by the 2,000’ mark. I thought that the snow would probably be great for the junkboarders, but I wasn’t quite sure about those who were on regular skis. Not long after I had that thought though, I met three skiers coming down Nosedive, right around the intersection with National. They clearly seemed to be making due on regular skis and seemed to be enjoying it. During my ascent it snowed most of the time, and occasionally the snow came down with moderate to heavy intensity. Being starved for a bit of winter weather, I loved it.
Even by the top of Nosedive (~3,600’) the snow was only up to about 3 inches in depth, but I hiked on a bit farther to check out the Mt. Mansfield Stake. There was some vegetation in front of the stake (~3,700’) that hadn’t let the snow settle all the way to the ground, but the depth of the snow was clearly less than 6 inches. At least one vehicle had driven on the Toll Road, but I still popped on my old Telemark skis and did a little gliding in the untouched snow outside the tire tracks. That was quite pleasant, although due to the minimal snowfall, there was the occasional crunch of a piece of gravel. Not wanting to deal with the hassle of negotiating the steep terrain of Nosedive with somewhat minimal snow, I continued on the Toll Road and into the Ridge View area before deciding to take off my skis. I had even made a few Tele turns on the snowy grass, but by around the 3,000’ elevation, a combination of wanting to head back in the direction of the Gondola via steeper terrain, and not wanting to put any real damage into my skis saw me strapping them back on my pack. I’m not totally ready to commit the Hellgates to official rock ski status just yet.
Hiking up had been really enjoyable (I think it was the first time I’d hiked such a long distance in Tele boots without switching to skinning) but the vistas on the descent were spectacular. With the dramatic scenes of white surrounding me, and the brilliant colors in the valley, I stopped frequently to pull out the camera. My descent was somewhat meandering, taking me down through the Hayride and Lookout areas, before making it down to Crossover and down to the gondola lot. The snow level on Mansfield looked like it had crept up a few hundred feet since my ascent, so it was certainly warming up. Insofar as I can recall, I think today’s outing was the first time that things came together to allow me to ski on my birthday, so that made it even more of a treat that usual. To check out all the pictures from the day, head to the Stowe trip report from today.
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
