ACMG Mountain Conditions Report Summary for the Coastal Mountains issued April 28, 2010S.COAST AND N.CASCADES RANGES:Cool and unsettled conditions prevailed this past week. Alpine areas received periodic snow flurries resulting in some lingering storm snow over a generally moist snow-pack. A weak ridge of high pressure is forecast to build onto the coastal areas this weekend. Perhaps we will see clear skies, and an overnight freeze. Avalanche activity; was generally limited to cornice failures and surface layers of the snow-pack. However some large avalanches have been reported, including a size 4 avalanche in the Hurley Pass area. The east side of the coast range, such as the Southern Chicotin region, the snow-pack probably still has lingering mid pack weaknesses. On the east side of the Cascades around Leavensworth, multi-pitch rock climbing routes out of Icicle creek drainage have had ascents in the past week,... presumably the snow line is retreating to treeline elevations. CENTRAL COAST REGION: The past week was reported to have drier conditions than South Coast. areas. Avalanche activity; the usual spring cycle will be underway, with wet slides running into valley bottoms. Avalanches and cornice falls have triggered deeper layers in the form of slabs in the drier side of the range, indicating a lingering Persistent Weakness Layer are still a concern on the drier east side slopes of the Coast Range. The alpine snowpack seems to be above average this year, many of the glaciers observed have an increase in crevasses. Ski touring activity is reported to be way up this year, with the number of groups flying in for trips approaching the busy days of the 1980's! NORTH COAST RANGES; Unlike the south Coast, the north coast has below average snowpack this winter. I didn't have much information at this time, but hopefully more info in the coming weeks. WEEKEND OUTLOOK If the skies do start to clear into the weekend, a nice melt-freeze travelling crust may form. The weather forecast seems to change daily, however at this time, Saturday looks like a lovely day for the South and Central coast areas. However, given the uncertain forecast, the safe bet might be rock-climbing in the rain shadow areas such as Pavillion, Skaha, or Leavensworth. Better bring a toque and sweater! Paul Berntsen, Mountain Guide | |
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These observations and opinions are those of the person who submitted them. The ACMG and its members take no responsibility for errors, omissions, or lapses in continuity. Conditions differ greatly over time and space due to the variable nature of mountain weather and terrain. Application of this information provides no guarantee of increased safety. Do not use the Mountain Conditions Report as the sole factor in planning trips or making decisions in the field. Please check out http://acmg.ca/mcr for more information. |
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Friday, April 30, 2010
[MCR] ACMG Mountain Conditions Report Summary for the Coastal Mountains issued April 28, 2010
Thursday, April 29, 2010
[MCR] ACMG Mountain Conditions Report Summary for the Rockies and Columbia Mountains issued April 29th, 2010
ACMG Mountain Conditions Report Summary for the Rockies and Columbia Mountains issued April 29th, 2010ACMG Mountain Conditions Summary for the Rockies and Columbia Mountainsissued April 29th, 2010. This is the first ACMG Mountain Conditions Summary for 2010. Periodic avalanche bulletins from the Canadian Avalanche Center, Mountain National Parks and Kananaskis country will continue for awhile yet. Last weeks heat wave seems to have had a dramatic effect on the mountain snowpack. Observations are limited as most backcountry ski operations are closed for the winter. However, the limited observations all point to a strong, surface, melt freeze crust throughout the Rockies and Columbia mtns. from that warm period. This melt freeze crust, along with the large scale avalanche cycle that occurred during the heat, has taken most of the sting out of the persistent weak layers from the winter. However, there is no question that some BIG avalanches, releasing deep in the snowpack, will continue to occur with rapid warming from daytime heating or big rains for awhile. The melt freeze crust is presently being buried by snow and this trend is likely to continue given the forecast. As often happens in the spring, it is dumping in the Eastern Rockies and things are much drier along the Divide of the Rockies and in the Columbia mtns. Kananaskis country is reporting 50cms of new snow as of this morning(thursday) and it was still snowing at 10am. The wind is probably blowing and K Country's avalanche forecasters are calling the avalanche danger EXTREME in the alpine and treeline for tomorrow and saturday! Much less snow has fallen along the Rockies Divide (3 cm wednesday night at Lake Louise, 6cm at Sunshine, 10cm at Parkers Ridge) and in the Columbia mtns. In these areas, the few people reporting talk about good "dust on crust" skiing treeline and above. Below treeline, especially in well travelled places like Rogers Pass, it is either skiing in frozen debris, alders and ruts or isothermal wallowing when things warm up. Most valley bottom locati ons have reported rain rather than snow. Alpine climbing conditions WERE pretty good for awhile but we will have to see how much new snow we get through the extended period of grey forecasts. Assume that all cornices are massive and wobbly until you have observed them to be otherwise. >From all reports, it seems glacier travel conditions are pretty good in the Columbia Mountains and along the Rockies Divide from Mt. Robson to the Wapta. The notable exception seems to be Mt. Athabasca North Face area with a very thin snowpack. Lots of talk of bare ice in the steepish Rockies glaciers and ice faces. The wind did blow up high this winter! Ice climbing is almost done but climbable ice persists in some very shady locations for shady climbers. The usual caveats about warm temperatures, weak ice, hanging daggers, cornices, avalanche hazard etc obviously apply even more as we get into spring. Snow line is just above my house in Canmore as of 1pm thursday. The local mountains look more snowy than they have all winter. The scrambling and long rock routes on the east slope of the Rockies will need some much better weather to dry them out. Low elevation cragging will probably work this weekend if you don't mind climbing in down with a heat pack in your chalk bag:) Skiing could be good but I am trying to be a patient grasshopper, waiting for the glory of corn right from the top of a BIG peak. Hopefully that happens SOON! Larry Stanier ACMG/IFMGA Mountain Guide | |
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These observations and opinions are those of the person who submitted them. The ACMG and its members take no responsibility for errors, omissions, or lapses in continuity. Conditions differ greatly over time and space due to the variable nature of mountain weather and terrain. Application of this information provides no guarantee of increased safety. Do not use the Mountain Conditions Report as the sole factor in planning trips or making decisions in the field. Please check out http://acmg.ca/mcr for more information. |
Monday, April 26, 2010
[MCR] Rockies, Wapta traverse April 23-26
Sunday, April 25, 2010
[MCR] South Coast conditions
The beginning of the week saw weak to non-existant overnight freezes and an isothermal snowpack extending from roadside elevations (~1300m) up to treeline. During the days, weak surface crusts formed overnight would breakdown quickly and avalanche hazard increased rapidly with daytime heating and solar input. Weak and newly enlarged cornices (from a major storm event the previous week) were our major concern-- from exposure to the cornices themselves and as triggers for slopes below.
Wednesday, April 22nd saw a major rainfall event with rain extending to 1800/2000m in most locations. This saturated the upper 50cm of the snowpack and produced many loose snow avalanches on all aspects from below treeline to ridgetop. A major natural avalanche on Chipmunk Mtn, (sz 4 with a 1-2m deep crownline extending 550m across) occurred during this period.
Thursday and Friday (22nd and 23rd) saw stronger overnight freezes and generally cooler temperatures during the days. This resulted in the development of a 5-10cm thick crust layer at the snow surface which helped stabilize the snowpack. However, weak and saturated snow still exists below this crust and when temperatures rise and solar input increases, expect this surface crust to weaken and stability to decrease rapidly.
Cornices remain a major concern, especially when exposed to sun and rising daytime temperature. The major avalanche that occurred during the rain event also indicates that deep instabilities in the snowpack can "wake up" during periods of higher freezing levels and increased precipitation (rain).
Saturday, April 24, 2010
[MCR] Juan de Fuca Trail
Hi, This past week I hiked the Juan de Fuca trail from Botanical Bay to Mile 13 and thought it worthy to note that the trail has had some improvements made to the existing structures. Although the mud puddles are still big it looks like the wood work like bridges and cat walks have been straightened out and some reinforces. Most old wash outs are fixed. The trail seemed cleaned up (although there are a few new windfalls from this past winter) and it walked considerably better than previous Springs.
Dave Sarkany
SG
Thursday, April 22, 2010
[MCR] Frank Mackie Traverse - NW Coast Ranges. Bell 2/Stewart, BC
Completed the traverse in 3 travel days, and 2 weather days over 80km, Through the Treaty-Knipple-Frank Mackie-Salmon Glaciers. Travel days were generally good weather, mixed in with storms, including a day of rain at 5500' on the Frank Mackie. Travel was fast on A.M. Crusts, and degraded in the PM with heating. Lack of overnight freeze now would be very miserable. Coverage is good up high, but lots of slots open in weird places, were one would not suspect them, and the Salmon is quite open, and lots of recent bridge failures under previous sled tracks from the rain event. Surprisingly little avalanche activity after the rain event.. Low elevation snowpack is going fast, and don't think the exit off the Salmon moraines will be in for much longer. Granduc Rd is a mess of low elev avalanches from the rain event, and lots of bare patches opening. Feels a good month ahead of normal.
Thanks to LFH for the Heli Flight.
Sean Fraser, Lucas Holtzman, Olivia Sofer
Sean Fraser
ACMG Ski Guide
CAA Professional Member
Smithers, BC
250-643-0505
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[MCR] waddington angel glacier image
These observations and opinions are those of the person who submitted them. The ACMG and its members take no responsibility for errors, omissions, or lapses in continuity. Conditions differ greatly over time and space due to the variable nature of mountain weather and terrain. Application of this information provides no guarantee of increased safety. Do not use the Mountain Conditions Report as the sole factor in planning trips or making decisions in the field.
Please check out http://acmg.ca/mcr for more information.
[MCR] Waddington conditions
Waddington to the Dias Glacier area. Other than the ski quality the
area around the regular base-camp on the Dias is in good shape.
From the limited probing that I did on the Franklin, Finality and
Angel glacier there is well over 3m in the area. Having said this
though, there is widespread evidence of an extreme wind event in the
past few weeks which has stripped much snow off ridge tops and made
snow conditions on north faces, bullet proof!
We managed to be in the area right when most snow surfaces were going
though its first transition into a spring snow cycle. This meant that
we used ski crampons on almost all of our travel however the snow
never really turned into a skiable form of corn snow due to the powder
like conditions underneath. On most days this meant we were rewarded
with a beautiful breakable crust or schmoo for skiing.
We did mange to bag the false summit of the NW peak of Waddington in
our short stay. In my 15 years of skiing in the area I have never seen
the Angle glacier in such difficult conditions. The Seracs have become
very active and personally are almost a bit much for a ski route. The
attached photo is from our flight into the area on the evening of the
14th, however when we climbed up there two days later there had been a
serac fall from high on the glacier in the center. This large icefall
did not cause any real avalanche, but it did leave a 2-3m deep trench
down the entire glacier and left debris field 30-40m wide.
Also of note the NW summit of Waddington was also in difficult
conditions with mostly blue ice and two near vertical steps just below
the summit. Defiantly not skiable as it usually is at this time of the
year. Ski and boot crampons were a must for our whole route up from
the Dias as would be a few more ice screws and a real ice axe and
crampons for the NW summit.
With a forecast of warming temps and poor weather we headed out a few
days earlier than planed. I'd bet with the warm temps there would be
bit of an avalanche cycle going right now until the temps cooled off
again.
Craig McGee, Mountain guide.
Whistler BC
craigskibum@yahoo.com
_______________________________________________
These observations and opinions are those of the person who submitted them. The ACMG and its members take no responsibility for errors, omissions, or lapses in continuity. Conditions differ greatly over time and space due to the variable nature of mountain weather and terrain. Application of this information provides no guarantee of increased safety. Do not use the Mountain Conditions Report as the sole factor in planning trips or making decisions in the field.
Please check out http://acmg.ca/mcr for more information.
Wednesday, April 21, 2010
[MCR] Coast Mountains, Hope Creek, Large Avalanche
With this came reports of large slides off the North face of Mt Currie.
Be carefull out there! Watch the temperatures and the influence of the sun and rain on the slopes around you. This happened this morning with rapid rain loading.
Conny Amelunxen
MG
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Monday, April 19, 2010
[MCR] Singing Pass Trail
The Singing Pass trail is still in very passable form. Harmony Creek bridge is melting out and usable. Lots of expectable forest debris on mid third of trail. Ditches on road are much like they where through the winter, some are still crossable. Near the village the road has a few dirt patches of no more than 15m across.
Dave Sarkany SG
[MCR] North Blue River, Cariboos
Sunday, April 18, 2010
[MCR] South Coast Spearhead Traverse
Did a lap through the Spearhead Traverse over the last 4 days.
The snow from yesterday made for very good skiing this morning in the higher alpine, but this all turned to mashed potatoes later (except on true north aspects above 1800m).
Earlier in the trip ski crampons where useful for cutting trail on all S aspects in the AM, and N aspects maintained good snow for skiing. Cornices are really big.
Great traverse conditions, barely saw any recent avalanche activity - Accept for a fairly recent size 3+ that appeared to start from Benvolio’s summit cornice. It took out a slab (where the traverse line crosses) and then spilled over a large portion of the Fitzsimmons ice fall and stopped ¾ km further down the lower Fitz Gl.
Dave Sarkany
SG
[MCR] Pantheon Range, Coast Mountains, April 11-17th, 2010
ACMG/IFMGA Mountain Guide
www.conradjanzenguiding.com
[MCR] More Wapta
Skied in the Wapta area April 12-16. Peyto-Bow-Balfour-Bow and out to Bow Lake. The morraines climbing up to Peyto glacier were still mostly covered in hard packed snow. Boot packing was the easiest way to climb up. We saw lots of slab avalanches from the storm about a week ago on various aspects all over between the Peyto and Balfour Hut area. Some released naturally, some were triggered by cornice or serac fall. We also noted many point releases on sunny aspects that step down to deeper layers and released decent size slab avalanches. On thinner spots around morrainal features some 'whumpf' sounds confirmed the still unstable layering of the snowpack. Again I had to turn away from Balfour High Col. Still large open and some barely covered cravesses, serac and cornice fall, and still the potential of skier triggering the deeper unstable layers was beyond our risk tolerance, even though it was a blue bird day and other un-guided parties decided to take the risk (or were not aware of it). See picture in previous Wapta posting. Enjoy the spring Thomas Exner Mountain Guide, IFMGA, ACMG www.ontopmountaineering.com (403) 678 2717 |
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[MCR] Rockies, Kid Goat, Twilight Zone.
Saturday, April 17, 2010
[MCR] Rockies, Easy Street, Mt Yamnuska
Thursday, April 15, 2010
[MCR] Rockies, Nemesis
Wednesday, April 14, 2010
[MCR] Rockies, Yamnuska and front ranges. april 14th, 2010
The front ranges you see from Yam still looked very snowy at the treeline and above. Given the forecast of sun and warmish temps, wet avalanches and rockfall will likely be a bit of a concern in those hills for a few days. If the weather forecast is correct, I would work hard to avoid being in the fall line of any front range snow in the heat of the day through the weekend.
Larry Stanier
ACMG/IFMGA Mountain Guide
laristan@telus.net
_______________________________________________
These observations and opinions are those of the person who submitted them. The ACMG and its members take no responsibility for errors, omissions, or lapses in continuity. Conditions differ greatly over time and space due to the variable nature of mountain weather and terrain. Application of this information provides no guarantee of increased safety. Do not use the Mountain Conditions Report as the sole factor in planning trips or making decisions in the field.
Please check out http://acmg.ca/mcr for more information.
[MCR] Rockies: Cirque Peak
Saturday, April 10, 2010
[MCR] Wapta conditions.
changed again and not for the better as we thought "could" happen
leaving on April 4th. Travelling up Peyto was good, probably the
best day was on April 4th.
April 5th at about 1100hrs noted the slab come out on Trappeur peak
while hanging around the hut doing some skills stuff. Later that day
did a quick profile under Thompson and still found instabilities
down about 70cm on an old facet or SH interface. This was on the easy
side of a moderate compression. Also some instabilities in the newer
storm snow.
Climbed Rhonda south on the 6th. The ridge was generally scoured but
loading on the lee side which was variable, not slabbed yet.
The summit ridge was quite windblown and rimed and I thought quite
well covered and without many exposed rocks. Still good skiing down
the ramp and over to Bow hut, not much wind affect.
On April 7th headed over to Balfour hut. A few cm of new snow at Bow
that morning, strong winds picking up and continued most of the day.
It seems like 20-30cm of new snow blown in on the Vulture glacier,
little to no visibility for rest of day. moderate to strong winds
continued with snowfall overnight and all day on the 8th.
We stretched our legs going over to the Diaberlet glacier but barely
got out of the flats as another wave of weather hit by mid day.
Significant subsidences in Balfour pass. We turned around just above
the pass due to the poor light and changing conditions.
Came out to Bow again on the morning of the 9th. -15 at Balfour hut
with a stiff northwesterly wind.Visibility still generally poor but
signs of newer activity on Olive were noted. A size 2 slab had pulled
out on the Bow head wall as well. the slopes above Bow were quite
wind affected with whales of soft slab getting stiffer the higher you
got. The slope below the hut was not wind affected when we came down.
The canyon was generally good with little wind affect, but still some
isolated small slabs in the canyon walls.
Didn't see much of Mt Balfour in the 2 days we were there, and it
wouldn't have mattered much. I would suspect the full traverse would
be quite scary right now and "definitely" not recommended.
Peter
Peter Amann
Mountain Guide
pamann@incentre.net
Friday, April 9, 2010
[MCR] Avalanche Control Mount Stephen/Bosworth Sat. April 10
[MCR] Spray road avalanche control.
Mike Koppang SG
Kananaskis Public Safety
_______________________________________________
These observations and opinions are those of the person who submitted them. The ACMG and its members take no responsibility for errors, omissions, or lapses in continuity. Conditions differ greatly over time and space due to the variable nature of mountain weather and terrain. Application of this information provides no guarantee of increased safety. Do not use the Mountain Conditions Report as the sole factor in planning trips or making decisions in the field.
Please check out http://acmg.ca/mcr for more information.
Thursday, April 8, 2010
[MCR] Duffy Lake Area
Evan Stevens
Mountain Guide
evan_stevens@hotmail.com
evanstevens.blogspot.com
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Wednesday, April 7, 2010
[MCR] Cerise Creek
If you are planning on visiting Keith's Hut, a few friendly reminders. Bring your own TP, and plan on burning it thoroughly either in the wood stove or by hand. There has been big piles of half burned teepee left in the outhouse. Don't expect much firewood. All that is left was a few huge burls/knots, and is really hard to chop, and there is not much left! Please do some shoveling and leave the place cleaner than when you found it as well! This place is heavily used. Also, bring a newspaper in if you want to start a fire, instead of tearing pages out of books, magazines and log books left in the hut.
Have fun out there.
Evan Stevens
Mountain Guide
evan_stevens@hotmail.com
evanstevens.blogspot.com
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[MCR] Rockies: Nemesis, Stanley Headwall (April 7)
route. Having said that, it looks like everything is to change
tomorrow with a weather forecast of snow, rain, wind and warm
temperatures. Parks Canada is forecasting the avalanche hazard to go
to HIGH with this storm so it will be a while before I would want to
head back up to the Stanley Headwall.
Hanging daggers on the left side of Nemesis threaten the first two
pitches to the halfway ledge. They are worth considering if it gets
really warm. They get direct sun for about an hour mid-morning.
The lower portion of the trail is well packed and could be walked, but
once you hit treeline it would be post-holing. We skied the whole way.
My client saw a large Grizzly yesterday digging by the side of the
road across from the Stanley parking lot so we decided to carry bear
spray. No sign of the bruin today, but they are definitely awake and
hungry.
Sean Isaac
ACMG Alpine Guide
_______________________________________________
These observations and opinions are those of the person who submitted them. The ACMG and its members take no responsibility for errors, omissions, or lapses in continuity. Conditions differ greatly over time and space due to the variable nature of mountain weather and terrain. Application of this information provides no guarantee of increased safety. Do not use the Mountain Conditions Report as the sole factor in planning trips or making decisions in the field.
Please check out http://acmg.ca/mcr for more information.
Tuesday, April 6, 2010
[MCR] Southern Selkirks, Remote triggering potential
We spent the last couple of days (April 5th/6th) ski touring tree line and alpine terrain on southerly aspects near Gimli and Presley peaks in Valhalla provincial park of the Southern Selkirks.
Given the time of year, we were very pleased to find excellent powder skiing on southerly aspects above 1800m with up to 20cm of new light density snow in past two days. This new snow combined with the previous storm snow made for 30cm to 60cm of recent storm snow, consolidating into a stiffening slab, and overlying a 4cm thick pencil resistance crust above the said elevation. On Monday (April 5th), we saw significant wind transport in the alpine with consistent moderate easterly winds loading westerly aspects and cross loading undulating southerly terrain.
For the most part, all of this new snow seemed to be bonding reasonably well to the crust at treeline and below with stability test showed moderate to hard (resistant) shears. In the alpine things are different. Most of the shear results on that layer were in the moderate range with sudden collapse characteristics. Of note at the interface was a thin (1cm thick) softer faceted layer just above the previously mentioned crust.
Today (April 6th), while skiing a lower angled bench on a west aspect in the alpine we started noticing some cracking and whumpfing in the upper snowpack. One of these whumpf remotely triggered a slab avalanche 100m away in nearby steeper terrain. This size 2 avalanche was 30 to 70cm deep (on the crust), about 80m wide and 100m long. Luckily our terrain choice lead us to be safe at that moment but had we been more exposed/closer the steeper terrain things could have been worse.
Up until now this layer had been more of a concern on northerly aspects. Given the significant recent snowfall, wind transport and poor bond with the underlying crust in the alpine, this layer deserve more respect on southerly aspects too. With a weather forecast promising more snow in the next few days this layer will get deeper and could reach critical load, it is bound to become more reactive naturally and to skier traffic. I believe it is time to avoid exposure to any avalanche terrain in the alpine for the next little while. Cool temps and continued precipitation will likely keep fantastic skiing options in the trees.
Be safe and enjoy a great Spring!
Perhaps winter is finally getting here...
David Lussier
IFMGA-ACMG-CAA
www.summitmountainguides.com
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[MCR] Valkyr Lodge, Southern Selkirks, March 29-April 5, 2010
ACMG/IFMGA Mountain Guide
www.conradjanzenguiding.com
Monday, April 5, 2010
[MCR] Rockies, Coire Dubh, Doors of Perception, Bow Valley snow line, April 5th, 2010
It was very clear from the views that it is still very wintery above treeline in the Bow Valley. Yamnuska trails, all routes and the backside are almost completely dry, but when you go west and higher expect some snow.
Larry Stanier
ACMG/IFMGA Mountain Guide
_______________________________________________
These observations and opinions are those of the person who submitted them. The ACMG and its members take no responsibility for errors, omissions, or lapses in continuity. Conditions differ greatly over time and space due to the variable nature of mountain weather and terrain. Application of this information provides no guarantee of increased safety. Do not use the Mountain Conditions Report as the sole factor in planning trips or making decisions in the field.
Please check out http://acmg.ca/mcr for more information.
[MCR] This House of Sky, The Ghost, Canadian Rockies (April )
Sunday, April 4, 2010
[MCR] Mt. Hector
steep section where the crags start) and turned back mainly out of
concern for avalanche hazard on the steep upper pitches.
The snowpack in this area is as scary as reported elsewhere in the
Rockies and Hector cannot be recommended as a destination now or in
the foreseeable future. On non-solar slopes 20-40cm of wind affected
storm snow overlies a windcrust which overlies weak, large facet
crystals. We experienced frequent whoomfing and shooting cracks
between treeline at 2200m and about 2700m (the toe of the glacier).
Solar aspects had wind hammered storm snow seemingly well bonded to a
bulletproof crust below.
The snow depths were variable and shallow, ranging from 0-150cm below
the glacier and from 0-250cm on the glacier. Average snow depth above
2800m was about 250cm.
The N facing slopes that threaten the route as you exit the approach
gulley/waterfall at treeline have not avalanched and look ripe &
windloaded with a large cornice overhead. The N-NE facing slopes off
Hector's NW outlier peak that threaten the route between the moraine
and the glacier showed evidence of widespread avalanche & cornice
activity to size 3.0 in the past 72hrs.
One whoomf as we crested the moraine at ~2500m resulted in a large (sz
3.0) remote avalanche (crown 7m below our track) that ran far. Crown
was ~100m wide, 20 to 60cm thick, NE aspect, steep, convex and
windloaded. Impressive.
Skiing was good on the glacier, albeit worrying with the shallow
snowpack and recent storm snow and wind likely concealing crevasses.
Below the glacier -- well, bring your rock skis and your 6th sense if
you're dumb enough to go after reading this. Nasty skiing.
Temps ranged from -1 to -12C with moderate W winds and broken cloudy
skies. Solar aspects were softening later in the afternoon but the
snow below treeline was still supportive and almost skiable.
No evidence of natural avalanche activity today.
Regards,
Tom Wolfe
ASG/AAG
_______________________________________________
These observations and opinions are those of the person who submitted them. The ACMG and its members take no responsibility for errors, omissions, or lapses in continuity. Conditions differ greatly over time and space due to the variable nature of mountain weather and terrain. Application of this information provides no guarantee of increased safety. Do not use the Mountain Conditions Report as the sole factor in planning trips or making decisions in the field.
Please check out http://acmg.ca/mcr for more information.
[MCR] Intercoastal Range ~ Duffey Lake area
The skies opened today and it was a pleasant day to be in the high places while turning the legs over.
The snow turned moist quickly once the sun began heating things up. Dry snow is still accessible on true north-facing terrain with good powder that's 20-25cm deep. At open below treeline locations on north aspects, this powder snow is sitting on a crust located 25-30cm below the surface. Tests showed a clean, 'sudden' result where this recent storm snow rests on the crust. Fortunately, the snow at these particular below treeline locations was still quite soft so the hazard is a little lower. As you climb to treeline, and just above, the snow (and hazard) changes.
A party of recreational tourers skier-triggered a healthy size 2 slab avalanche (large enough to bury a person) today on an east (with a little north-facing bias) aspect at an elevation where the treeline thins and the alpine begins. I strongly suspect that this slab ran on a crust. The interesting thing about the terrain, from which the slab was triggered, was that the avalanche began much lower in the start zone on a large convex feature. Essentially, the very strong winds that we recently had relocated much of that snow lower into avalanche start zone locations than usual. As such, it seems that it may be possible to trigger an avalanche from lower down. The slide ran from an adjacent steep cross-loaded slope into a gully-like feature that they were attempting to ski. It was triggered where the gully met the cross-loaded slope.
Cornices continue to be a significant overhead hazard and so, too, are large sun-baked slopes.
On the drive home to Whistler, the clouds were thickening to the west and wind speeds in the mountains had begun to increase. The next system approaches!
'So foul a sky clears not without a storm.'
~ 'Yep', Shakespeare....
Hoping this finds Everyone keeping well and enjoying the Spring touring season....
Best regards,
Dale Marcoux
ACMG Asst. Ski Guide
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[MCR] Rockies: Wapta, again
Saturday, April 3, 2010
[MCR] Rockies, King Creek, Magic touch
[MCR] Hydrophobia-April 4
All the best,
Marco Delesalle
IFMGA/ACMG Mountain Guide
www.greatdividemountaineering.com
_______________________________________________
These observations and opinions are those of the person who submitted them. The ACMG and its members take no responsibility for errors, omissions, or lapses in continuity. Conditions differ greatly over time and space due to the variable nature of mountain weather and terrain. Application of this information provides no guarantee of increased safety. Do not use the Mountain Conditions Report as the sole factor in planning trips or making decisions in the field.
Please check out http://acmg.ca/mcr for more information.
[MCR] Kananaskis Country Avalanche Conditions
The Kananaskis region is currently experiencing somewhat unusual avalanche conditions. The snowpack this season has several persistent weak layers of buried surface hoar which continue to be reactive in stability tests and are responsible for a number of avalanches. In addition, the snowpack above these persistent weak layers has sufficient density to allow for wide propagation if an avalanche is initiated. Although it is currently slightly more difficult to trigger an avalanche (as compared to last week), the likelihood of generating a large and destructive avalanche is high. It is expected that the persistent weak layers will remain a problem for the rest of the ski season. It is not a normal spring snowpack.
For more information please check the Kananaskis Country Avalanche Bulletin at
http://tpr.alberta.ca/parks/kananaskis/backcountryreport.asp
Play safe!
Jeremy Mackenzie
Kananaskis Country Public Safety
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[MCR] South Coast conditions
Here is a summary of the conditions observed by the Assistant Ski Guide exam this past week:
Dates: 27 March – 02 April
Region: Duffey Lake & Blackcomb backcountry
Weather was generally unsettled and overcast with moderate to strong winds from the south and south west accompanied by moderate to heavy precipitation resulting in 60-80cm of storm snow. Freezing levels fluctuated between valley bottom and 2,000 metres producing a fairly widespread temperature crust on east, south and west aspects up to 2,000 m.
Cornices were one of the main concerns of the week and this was reinforced by a size 2.5 that we remotely triggered in the Blackcomb backcountry.
Despite significant amounts of precip and wind transport, stability was fair to good throughout the week with very little avalanche activity and although storm snow was a 'concern' it was generally bonding well to old surfaces with stability tests producing moderate to hard resistant results.
Earlier in the week, isothermal conditions were encountered below 1400m and did not inspire confidence on open or exposed slopes. By week's end, ski quality on north aspects was excellent above 1500m. .
Ski crampons were essential on southerly aspects earlier in the week and ski pen was up to 30-40 in the alpine and lee aspects..
Cover on glaciers was generally good with snow depth ranging from 250cm to 300cm +.
Sylvain Hebert
ACMG Ski Guide
Friday, April 2, 2010
[MCR] Rockies, Coirre Dubh and environs
[MCR] Ghost River rock and the Sorcerer
Sorcerer was in REALLY good shape today and it stayed cool and breezy all day. I imagine it will disappear fast if and when it heats up. One small droopy cornice on top and no hanging death daggers as of 2pm. Lots of melted out Abalakov's and our screws were melting a bit in the am sun. As dangerous places go though, it felt good to be there today:)
Roads are in good shape too. Lots of potholes and a couple of big puddles on the main road. The big hill is good and there are currently no real river crossings to get to the Silver Tongue Devil crossing/parking.
Snowpack tests generally showed there to be no snowpack. Yippee!
Larry Stanier
ACMG/IFMGA Mountain Guide
laristan@telus.net
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These observations and opinions are those of the person who submitted them. The ACMG and its members take no responsibility for errors, omissions, or lapses in continuity. Conditions differ greatly over time and space due to the variable nature of mountain weather and terrain. Application of this information provides no guarantee of increased safety. Do not use the Mountain Conditions Report as the sole factor in planning trips or making decisions in the field.
Please check out http://acmg.ca/mcr for more information.
Thursday, April 1, 2010
[MCR] rockies, Healy Pass area
[MCR] Have a safe Easter
We are very busy here at the CAC and I don't have time to do an in-depth update. I do want to remind people that even though avalanches are much harder to trigger now than they were even a week ago and we are seeing far less slides in recent days, there are still signs that the weak layers we've been talking about since February are still capable of producing very large, destructive avalanches.
Our February/March avalanche photo gallery is at:
http://www.avalanche.ca/cac/library/avalanche-image-galleries/feb-march-2010
Take a look at the two most recent photos the gallery:
http://www.avalanche.ca/uploads/gallery/2/MPS-1.jpg
http://www.avalanche.ca/uploads/gallery/2/MPS-4.jpg
While isolated incidents, these are indicative of the potential that still exists out there.
Please be careful if you are considering going into the following mountains this weekend:
· North Rockies (north and east of Prince George to the Alberta border.
· Columbia Mountains south of highway 16 to the US border, between Quesnel, Williams Lake, Kamloops, and Osyoos on the west and Valemount, Blue River, Golden, and Cranbrook on the east.
· South Chilcotin Mountains north of Pemberton and east of the South Coast Mountain divide.
In these areas, the advice provided here: http://www.avalanche.ca/cac/library/researchandarticles/PWLpaper0910 is applicable.
The CAC Avalanche Forecasts at: http://www.avalanche.ca/cac/bulletins/regions provide information that is updated daily to help you make informed decisions if you plan to go into the mountains.
Have a great Easter weekend and Easter holidays but play safe.
Please send this on or repost in other venues freely.
Karl Klassen
Mountain Guide
Public Avalanche Bulletins Manager
Canadian Avalanche Centre