Howsons, but the skiing was excellent, with no less than 1200 m skied
every day. On Friday, the winds were moderate to strong from the NW with
steady snowfall. The temperatures dropped to -21C. The wind reversed
direction Friday night, but the snowfall and low temperatures persisted
until noon on Sunday. There were 40 cm of snow on the storm board by the
end of the week. It snowed much more, but much of that had been blown away.
A test profile at 1650 m in a wind exposed area, W aspect, showed about 
50 cm of storm snow over last week. There were several sudden planar 
moderate to hard shears on decomposing and fragmented grains in the 
storm snow. There is a crust/ facet layer 100 cm down that is producing 
hard sudden planar shears. There was some whumpfing in glades below 
treeline. Ski cutting produced no results.
Our avalanche observations were mostly acoustic as the visibility was 
poor throughout the week. Several size 2 and 3 came off the Hut Cliffs 
and Polemic Glacier through the week.
Today, as we saw the sun for the first time all week, we observed one 
size 3 natural slab in a south aspect on Hut Peak and several natural 
size 2 slabs, some triggered by cornice falls, on the flight out in the 
Telkwa Range.
-- 
Christoph Dietzfelbinger
IFMGA/ UIAGM Mountain Guide - Bear Mountaineering and the Burnie Glacier Chalet
Box 4222	Smithers, B.C.		V0J 2N0	Canada
tel. 250-847-3351/ fax 250-847-2854 
info@bearmountaineering.ca		www.bearmountaineering.ca
_______________________________________________
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.