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reasoning behind this has been that in a cold, thin snow-
pack not enough skier compaction can be guaranteed in
the early season when the skiing was poor. If an area is
kept closed until more snow arrives and then openedlater
in the season, there is potential for a long term instability
to become buried, only to react later in the winter. There
have been instancesof avalanchesoccurringeven after ski
compaction has taken place, and each year isothermal
avalanchesrunat ground level in many heavilycompacted
areas. Deep release events in the mid-winter are not com-
mon but always a concern in areas of less compaction.
Over the past few years we havebegun to re-think tradi-
tional closures. Whereas before, a "buffer zone" of less
serious terrain on the edge of the closure ensured most
closure violators would remain away from the main area
of concern, we began to see more and more serious infrac-
tions occur deep within the closures. This culminated in
several serious avalancheinvolvements in permanent clo-
sure areas. The most notable of these was the complete
burial of a "poacher"resultingfrom the triggering of a deep
instability that had not reacted to explosives a few hours
earlier. Luckily the victim was rescued with no injuries,
but this type of event was clearly unacceptable even if it
did occur in a closed area.
More closure signs and a zero-tolerance enforcement
policy helped to a point. We also considered opening
some closures when stability was rated Good or Very
Good, but the risk of a forecasting error, or of a tempo-
rary closure not being respected because the slope
would only be open infrequently, seemed to be too high.
In the end, we feel the best way to deal with the situation
is to have these areas fully compacted, resulting in easily
forecasted surface instabilities being the only concern
for the majority of the winter and the areas being open
more often than closed.
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Could we do this? Wefelt we could. Based on our expe-
rience with early season ski and snowboard compaction
in our less serious terrain, we began to experiment work-
ing our normal closure areas a bit more at the beginning of
the winter. We found that with a combination of regular
early season explosives work, combined with saturation
bombing using ANFO and handcharges when a bit more
snow blows in, we were able to open several traditionally
closed areas. In the past, the skiing would have been con-
sidered poor at the initial opening, but the new breed of
aggressive skiers and snowboarders jump in regardlessand
are quite effective in compacting the slopes. Although it is
not the first time some of these areas have been opened,
they are now being opened earlier and more consistently
than in the past. Presently we are slowly expanding our
horizons in this regardand are continually reassessing tra-
ditional closures in attempts to open more terrain for our
guests. As a result, we are providing a better product for
our customers, a better ski area for management to adver-
tise, an interesting challengefor our staff and above all, a
safer environment.
In conclusion, the evolution of the new avalanchecon-
trol programme at the Lake Louise Ski Area has been an
interesting process, one which has taken far longer than
initially expected and one which continues to evolve. We
have found it essential that the Snow Safety programme
be efficient, integratedand open to the idea of change so it
can respond to the shifting demands of guests, manage-
ment and staff. What has emerged is an operation whose
staff are well-roundedin their skills andflexible inrespond-
ing to the variety of public safety problems faced at one of
Canada's major ski areas.
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