Subject: | [MCR] Rocky & Purcell mountains |
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Date: | Mon, 15 Dec 2014 21:45:13 -0700 |
Hello all, I taught an AST2 course for the UofC Outdoor Center Dec12-14th. My students have prepared this (slightly edited) report. As politicians say....I approve this message. Nov 12, 2014 Jimmy Simpson Glades, south of Bow Summit Widespread whomphing while crossing a 2000m meadow. Temp crust up to 2100m. An extended column test was done on a lee(NE) 30 degree slope in the glades. 95cm deep snowpack. We had an alarming shooting failure crack through the whole block with a hard hit down 55cm on the late Nov. facets. We noticed small (size 1.5-2) avalanches on NE aspects that did not trigger the late November or Nov 6 (rain crust) weak layers. Ski quality was very good above 2100 m, with approx 10-15cm of lighter snow over a consolidated storm slab of approx 40 cm. Below 2100 m snow was heavy and temp crust led to difficult skiing. Nov 13, 2014 Rudi's Ridge, Kicking Horse Slackcountry Freezing level was around 2000m with surface crust below and no crust above that elevation. Snowpack was around 125 cm above 2000m and quickly shrunk to 50cm at 1800m. Compression test on a South aspect 25 degree open slope at 2200m yielded a sudden failure below the Nov 6 crust layer. The S slope of rudi's ridge was crossloaded by previous SW winds creating a bit of a wind crust. It was a bluebird day so steeper solar aspects may have developed a sun crust. East and SE slopes yielded the best ski quality. A size two slab avalanche was noticed on a lee (N) alpine slope. It was more than 48 hours old. Nov 14, 2014 Lipilian Subpeak, Lake Louise (1700 to 2450m) While breaking trail in a 2200 meadow we were creating some shooting cracks, but no whoomphing. Steep south slopes were quite bare. A previous size 2.5 avalanche on a crossloaded south aspect petered out a few hundred meters above the 2200m hanging valley. Approx 60 cm snowpack. Evidence of old( >4days) size 1.5 avalanches on cross loaded NW alpine aspects which did not step down to deeper layers. Very thick and strong wind crust on alpine ridges provided easy and fast travel. No avalanches present in bowl below Lipilian Subpeak. Drifted snow on top of the hard windcrust snow made for nice skiing on the descent. New surface hoar was noted an all aspects and elevations traveled. _______________________________________________ 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. See http://acmg.ca/mcr for more information. See http://informalex.org/subscribe.shtml#unsubscribe to remove your name from this list. |
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